{"pageNumber":"284","pageRowStart":"7075","pageSize":"25","recordCount":68835,"records":[{"id":70238061,"text":"70238061 - 2019 - Simulations of hydrology and water quality for irrigated fields near Yakima, Washington","interactions":[],"lastModifiedDate":"2022-11-09T14:53:52.300317","indexId":"70238061","displayToPublicDate":"2019-08-01T08:47:40","publicationYear":"2019","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"Simulations of hydrology and water quality for irrigated fields near Yakima, Washington","docAbstract":"Reliable tools are needed by farmers and managers to estimate and mitigate impacts of altered hydrology and degraded water quality downstream of agricultural areas. The Water, Energy, and Biogeochemical Model (WEBMOD) (Webb and Parkhurst 2017) was used to simulate daily variations of hydrology and water quality for 5 square kilometers of irrigated fields draining to the DR2 Drain, southeast of Yakima, WA.","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Working watersheds and coastal systems: Research and management for a changing future — Proceedings of the Sixth Interagency Conference on Research in the Watersheds","largerWorkSubtype":{"id":12,"text":"Conference publication"},"conferenceTitle":"Sixth Interagency Conference on Research in the Watersheds","conferenceDate":"July 23-26, 2018","conferenceLocation":"Shepherdstown, WV","language":"English","publisher":"U.S. Department of Agriculture Forest Service, Southern Research Station","collaboration":"EPA, USFS","usgsCitation":"Webb, R.M., 2019, Simulations of hydrology and water quality for irrigated fields near Yakima, Washington, <i>in</i> Working watersheds and coastal systems: Research and management for a changing future — Proceedings of the Sixth Interagency Conference on Research in the Watersheds, Shepherdstown, WV, July 23-26, 2018, p. 202-205.","productDescription":"4 p.","startPage":"202","endPage":"205","ipdsId":"IP-100453","costCenters":[{"id":37277,"text":"WMA - Earth System Processes Division","active":true,"usgs":true}],"links":[{"id":409260,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":409218,"type":{"id":15,"text":"Index Page"},"url":"https://www.fs.usda.gov/treesearch/pubs/59031"}],"country":"United States","state":"Washington","city":"Yakima","otherGeospatial":"Yakima River basin","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -120.56886577450334,\n              46.633070609190895\n            ],\n            [\n              -120.56886577450334,\n              46.12956834060162\n            ],\n            [\n              -119.41838691883319,\n              46.12956834060162\n            ],\n            [\n              -119.41838691883319,\n              46.633070609190895\n            ],\n            [\n              -120.56886577450334,\n              46.633070609190895\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Webb, Richard M. 0000-0001-9531-2207 rmwebb@usgs.gov","orcid":"https://orcid.org/0000-0001-9531-2207","contributorId":1570,"corporation":false,"usgs":true,"family":"Webb","given":"Richard","email":"rmwebb@usgs.gov","middleInitial":"M.","affiliations":[{"id":5044,"text":"National Research Program - Central Branch","active":true,"usgs":true},{"id":191,"text":"Colorado Water Science Center","active":true,"usgs":true}],"preferred":true,"id":856734,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70205781,"text":"70205781 - 2019 - Phylogeny and foraging mode correspond with thiaminase activity in freshwater fishes: Potential links to environmental factors","interactions":[],"lastModifiedDate":"2019-10-04T08:33:42","indexId":"70205781","displayToPublicDate":"2019-08-01T07:59:15","publicationYear":"2019","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1699,"text":"Freshwater Science","active":true,"publicationSubtype":{"id":10}},"title":"Phylogeny and foraging mode correspond with thiaminase activity in freshwater fishes: Potential links to environmental factors","docAbstract":"Knowledge of the dietary components of fish species is important for understanding their growth, survival, and recruitment. Deficiency in thiamine (vitamin B1) leading to reproductive failure and physiological illness among freshwater fishes has been attributed to thiaminase activity in fish in the Great Lakes and the New York Finger Lakes, but the causes of variation in thiaminase activity among freshwater fishes is unclear. We characterized thiaminase activity in 29 species of freshwater fishes across 7 ray-finned and 1 jawless family. All fish were further categorized by phylogeny, trophic category (trophic level and feeding mode), and native or non-native status to evaluate how ecological processes correspond with thiaminase activity. Thiaminase activity varied significantly across species, families, trophic factors, phylogenetic groups, and sites. Teleosts that were more recently derived had higher thiaminase activity than more basal species. Thiaminase activity was also higher among herbivores than omnivores or carnivores. This trend was clearest in the Cyprinidae family, which had the greatest range in thiaminase activity and a wide range in trophic-level position and trophic categories (herbivores, omnivores, and carnivores). Variation in average thiaminase activity of Spotfin Shiners (Cyprinella spiloptera) among sites within a watershed was correlated with anthropogenic and natural components of land cover. Our study contributes much-needed quantitative ecological information related to thiaminase activity in a suite of fish species that vary in evolutionary history, trophic level, and foraging modes. However, more studies are needed to identify interacting causes of thiaminase variation and examine the implications of these findings on the overall health of aquatic populations and freshwater ecosystems.","language":"English","publisher":"University of Chicago Press","doi":"10.1086/704927","usgsCitation":"Spooner, D., Boggs, K., Shull, D.R., Honeyfield, D.C., Wertz, T., and Sweet, S., 2019, Phylogeny and foraging mode correspond with thiaminase activity in freshwater fishes: Potential links to environmental factors: Freshwater Science, v. 3, no. 38, p. 605-615, https://doi.org/10.1086/704927.","productDescription":"11 p.","startPage":"605","endPage":"615","ipdsId":"IP-110044","costCenters":[{"id":365,"text":"Leetown Science Center","active":true,"usgs":true}],"links":[{"id":367946,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"3","issue":"38","publishingServiceCenter":{"id":10,"text":"Baltimore PSC"},"noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Spooner, Daniel E 0000-0002-5408-4364","orcid":"https://orcid.org/0000-0002-5408-4364","contributorId":219471,"corporation":false,"usgs":false,"family":"Spooner","given":"Daniel E","affiliations":[{"id":40002,"text":"Lock Haven University of Pennsylvania","active":true,"usgs":false}],"preferred":false,"id":772321,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Boggs, Kristin","contributorId":219472,"corporation":false,"usgs":false,"family":"Boggs","given":"Kristin","affiliations":[{"id":24583,"text":"former USGS employee","active":true,"usgs":false}],"preferred":false,"id":772322,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Shull, Dustin R.","contributorId":147947,"corporation":false,"usgs":false,"family":"Shull","given":"Dustin","email":"","middleInitial":"R.","affiliations":[{"id":16963,"text":"PA DEP","active":true,"usgs":false}],"preferred":false,"id":772323,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Honeyfield, Dale C. 0000-0003-3034-2047 honeyfie@usgs.gov","orcid":"https://orcid.org/0000-0003-3034-2047","contributorId":2774,"corporation":false,"usgs":true,"family":"Honeyfield","given":"Dale","email":"honeyfie@usgs.gov","middleInitial":"C.","affiliations":[{"id":365,"text":"Leetown Science Center","active":true,"usgs":true}],"preferred":true,"id":772324,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Wertz, Timothy","contributorId":66866,"corporation":false,"usgs":false,"family":"Wertz","given":"Timothy","affiliations":[{"id":17703,"text":"Pennsylvania Department of Environmental Protection","active":true,"usgs":false}],"preferred":false,"id":772325,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Sweet, Stephanie","contributorId":219473,"corporation":false,"usgs":false,"family":"Sweet","given":"Stephanie","affiliations":[{"id":24583,"text":"former USGS employee","active":true,"usgs":false}],"preferred":false,"id":772326,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}}
,{"id":70233214,"text":"70233214 - 2019 - Cross-scale interactions dictate regional lake carbon flux and productivity response to future climate","interactions":[],"lastModifiedDate":"2022-07-19T12:20:55.547259","indexId":"70233214","displayToPublicDate":"2019-08-01T07:16:12","publicationYear":"2019","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1807,"text":"Geophysical Research Letters","active":true,"publicationSubtype":{"id":10}},"title":"Cross-scale interactions dictate regional lake carbon flux and productivity response to future climate","docAbstract":"<div class=\"article-section__content en main\"><p>Lakes support globally important food webs through algal productivity and contribute significantly to the global carbon cycle. However, predictions of how broad-scale lake carbon flux and productivity may respond to future climate are extremely limited. Here, we used an integrated modeling framework to project changes in lake-specific and regional primary productivity and carbon fluxes under 21st century climate for thousands of lakes. We observed high uncertainty in whether lakes collectively were to increase or decrease lake CO<sub>2</sub><span>&nbsp;</span>emissions and carbon burial in our modeled region owing to divergence in projected regional water balance among climate models. Variation in projected air temperature influenced projected changes in lake primary productivity (but not CO<sub>2</sub><span>&nbsp;</span>emissions or carbon burial) as warmer air temperatures decreased productivity through reduced lake water volume. Cross-scale interactions between regional drivers and local characteristics dictated the magnitude and direction of lake-specific carbon flux and productivity responses to future climate.</p></div>","language":"English","publisher":"American Geophysical Union","doi":"10.1029/2019GL083478","usgsCitation":"Zwart, J.A., Hanson, Z., Read, J., Fienen, M., Hamlet, A.F., Bolster, D., and Jones, S., 2019, Cross-scale interactions dictate regional lake carbon flux and productivity response to future climate: Geophysical Research Letters, v. 46, no. 15, p. 8840-8851, https://doi.org/10.1029/2019GL083478.","productDescription":"12 p.","startPage":"8840","endPage":"8851","ipdsId":"IP-104891","costCenters":[{"id":474,"text":"New York Water Science Center","active":true,"usgs":true},{"id":37316,"text":"WMA - Integrated Information Dissemination Division","active":true,"usgs":true}],"links":[{"id":467402,"rank":1,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1029/2019gl083478","text":"Publisher Index Page"},{"id":437376,"rank":0,"type":{"id":30,"text":"Data Release"},"url":"https://doi.org/10.5066/P9S7EMTB","text":"USGS data release","linkHelpText":"Lake Biogeochemical Model Output for One Retrospective and 12 Future Climate Runs in Northern Wisconsin &amp; Michigan, USA"},{"id":404001,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"46","issue":"15","noUsgsAuthors":false,"publicationDate":"2019-08-08","publicationStatus":"PW","contributors":{"authors":[{"text":"Zwart, Jacob Aaron 0000-0002-3870-405X","orcid":"https://orcid.org/0000-0002-3870-405X","contributorId":237809,"corporation":false,"usgs":true,"family":"Zwart","given":"Jacob","email":"","middleInitial":"Aaron","affiliations":[{"id":37316,"text":"WMA - Integrated Information Dissemination Division","active":true,"usgs":true}],"preferred":true,"id":846818,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hanson, Zachary J","contributorId":293235,"corporation":false,"usgs":false,"family":"Hanson","given":"Zachary J","affiliations":[{"id":39516,"text":"University of Notre Dame","active":true,"usgs":false}],"preferred":false,"id":846819,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Read, Jordan 0000-0002-3888-6631","orcid":"https://orcid.org/0000-0002-3888-6631","contributorId":221385,"corporation":false,"usgs":true,"family":"Read","given":"Jordan","affiliations":[{"id":37316,"text":"WMA - Integrated Information Dissemination Division","active":true,"usgs":true}],"preferred":true,"id":846820,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Fienen, Michael N. 0000-0002-7756-4651","orcid":"https://orcid.org/0000-0002-7756-4651","contributorId":245632,"corporation":false,"usgs":true,"family":"Fienen","given":"Michael N.","affiliations":[{"id":474,"text":"New York Water Science Center","active":true,"usgs":true}],"preferred":true,"id":846821,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Hamlet, Alan F.","contributorId":266168,"corporation":false,"usgs":false,"family":"Hamlet","given":"Alan","email":"","middleInitial":"F.","affiliations":[{"id":39516,"text":"University of Notre Dame","active":true,"usgs":false}],"preferred":false,"id":846822,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Bolster, Diogo","contributorId":266171,"corporation":false,"usgs":false,"family":"Bolster","given":"Diogo","email":"","affiliations":[{"id":39516,"text":"University of Notre Dame","active":true,"usgs":false}],"preferred":false,"id":846823,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Jones, Stuart E.","contributorId":22222,"corporation":false,"usgs":false,"family":"Jones","given":"Stuart E.","affiliations":[{"id":6966,"text":"Department of Biological Sciences, University of Notre Dame","active":true,"usgs":false}],"preferred":false,"id":846824,"contributorType":{"id":1,"text":"Authors"},"rank":7}]}}
,{"id":70205670,"text":"70205670 - 2019 - Timescales of water-quality change in a karst aquifer, south-central Texas","interactions":[],"lastModifiedDate":"2021-04-02T14:41:48.358402","indexId":"70205670","displayToPublicDate":"2019-07-31T14:34:43","publicationYear":"2019","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":5836,"text":"Journal of Hydrology X","onlineIssn":"2589-9155","active":true,"publicationSubtype":{"id":10}},"title":"Timescales of water-quality change in a karst aquifer, south-central Texas","docAbstract":"<p><span>Understanding the drivers and timescales over which groundwater quality changes informs groundwater management, use, and protection. To better understand timescales of water-quality change over short (daily to monthly) and long (seasonal to decadal) timescales, the U.S. Geological Survey’s National Water-Quality Assessment (NAWQA) Enhanced Trends Network (ETN) program instrumented and sampled three wells in the Edwards aquifer in south-central Texas. The wells were instrumented to provide high-frequency continuous (subhourly) water-quality data (temperature, pH, specific conductance, and dissolved oxygen), which were augmented by the collection of discrete samples (about 6 per year) for a range of geochemical constituents (including selected isotopes and age tracers). ETN data (2013–2017) are considered with data from additional sites for the same time period, and also historical records (over more than 80 years) of climatic and hydrologic conditions. During the four-year study, hydrologic conditions transitioned from very dry to very wet. Sites in the updip/unconfined part of the aquifer showed notable changes in water level and geochemistry (1) in response to rainfall/recharge events, and (2) over the multiyear dry/wet cycle. Sites in the downdip/confined part of the aquifer showed changes in water level/spring discharge over similar timescales, although the response is more muted. Geochemistry at the downdip/confined sites, however, varied slowly and minimally, indicating that the geochemical response of the deeper aquifer is decoupled from recent hydrologic responses. Changes at the updip/unconfined sites reflect mixing with recent recharge, whereas the downdip/confined sites were dominated by mineral-solution reactions resulting from longer (decadal) residence times. Mean groundwater ages interpreted from measured age tracers and lumped parameter models range from 7 to &gt;700 years (where mixed with premodern downdip water) but were mostly modern. The aquifer is characterized by updip-to-downdip trends in geochemistry with respect to water-rock interaction and groundwater age. Fourier spectral analysis of historical records indicate hydrologic variability has occurred at dominant periods of 30 and 15 years; in conjunction with age tracers, these results provide insight into timescales at which the aquifer’s public supply is vulnerable to changes in the water quality of recharge.</span></p>","language":"English","publisher":"Elsevier","doi":"10.1016/j.hydroa.2019.100041","usgsCitation":"Musgrove, M., Solder, J.E., Opsahl, S.P., and Wilson, J.T., 2019, Timescales of water-quality change in a karst aquifer, south-central Texas: Journal of Hydrology X, v. 4, 100041, 16 p., https://doi.org/10.1016/j.hydroa.2019.100041.","productDescription":"100041, 16 p.","ipdsId":"IP-105452   ","costCenters":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true},{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":467403,"rank":4,"type":{"id":40,"text":"Open Access Publisher Index 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 \"}}]}","volume":"4","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Musgrove, MaryLynn 0000-0003-1607-3864 mmusgrov@usgs.gov","orcid":"https://orcid.org/0000-0003-1607-3864","contributorId":197013,"corporation":false,"usgs":true,"family":"Musgrove","given":"MaryLynn","email":"mmusgrov@usgs.gov","affiliations":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true},{"id":37277,"text":"WMA - Earth System Processes Division","active":true,"usgs":true}],"preferred":false,"id":772054,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Solder, John E. 0000-0002-0660-3326 jsolder@usgs.gov","orcid":"https://orcid.org/0000-0002-0660-3326","contributorId":171916,"corporation":false,"usgs":true,"family":"Solder","given":"John","email":"jsolder@usgs.gov","middleInitial":"E.","affiliations":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"preferred":true,"id":772058,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Opsahl, Stephen P. 0000-0002-4774-0415 sopsahl@usgs.gov","orcid":"https://orcid.org/0000-0002-4774-0415","contributorId":4713,"corporation":false,"usgs":true,"family":"Opsahl","given":"Stephen","email":"sopsahl@usgs.gov","middleInitial":"P.","affiliations":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"preferred":true,"id":772056,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Wilson, Jennifer T. 0000-0003-4481-6354 jenwilso@usgs.gov","orcid":"https://orcid.org/0000-0003-4481-6354","contributorId":1782,"corporation":false,"usgs":true,"family":"Wilson","given":"Jennifer","email":"jenwilso@usgs.gov","middleInitial":"T.","affiliations":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"preferred":true,"id":772057,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70204412,"text":"sir20195042 - 2019 - Lithostratigraphic, geophysical, and hydrogeologic observations from a boring drilled to bedrock in glacial sediments near Nantucket Sound in East Falmouth, Massachusetts","interactions":[],"lastModifiedDate":"2019-08-01T07:11:08","indexId":"sir20195042","displayToPublicDate":"2019-07-31T14:15:00","publicationYear":"2019","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":334,"text":"Scientific Investigations Report","code":"SIR","onlineIssn":"2328-0328","printIssn":"2328-031X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2019-5042","displayTitle":"Lithostratigraphic, Geophysical, and Hydrogeologic Observations From a Boring Drilled to Bedrock in Glacial Sediments Near Nantucket Sound in East Falmouth, Massachusetts","title":"Lithostratigraphic, geophysical, and hydrogeologic observations from a boring drilled to bedrock in glacial sediments near Nantucket Sound in East Falmouth, Massachusetts","docAbstract":"<p>In spring 2016, a 310-foot-deep boring (named MA–FSW 750) was drilled by the U.S. Geological Survey near Nantucket Sound in East Falmouth, Massachusetts, to investigate the hydrogeology of the southern coast of western Cape Cod. Few borings that are drilled to bedrock exist in the area, and the study area was selected to fill a gap between comprehensive geologic datasets inland to the north and marine geophysical data from beneath Nantucket Sound to the south. A permanent monitoring well (MA–FSW 750–0100) was installed in the boring upon the completion of the drilling and core collection. Observations from sediment cores and surface and borehole geophysical measurements were used to delineate three zones relevant to understanding groundwater flow at the study location. Shallow sands and gravels (0–107 feet [ft] below land surface [bls]) underlain by silt-rich fine and very fine sand (107–175 ft bls) form a zone of high permeability underlain by a zone of relatively lower permeability, referred to as the “shallow high-permeability” and “low-permeability” zones, respectively. A sharp lithological contact separating the shallow high-permeability and low-permeability zones may affect vertical flow of groundwater. Fine to coarse sand with intervals of clay and silt from 175 to 300 ft bls represent a deep zone of relatively high permeability, referred to as the “deep high-permeability” zone. A compacted, nonsorted unit (identified as basal till) and the bedrock surface were encountered at 300 and 305 ft bls, respectively. Hydraulic conductivity estimates from nuclear magnetic resonance logs and sediment grain-size distribution analyses indicated that the shallow high-permeability zone contributes substantially to the capacity of the aquifer to transmit groundwater at the study location. Results from geophysical surveys indicate a gradual transition from fresh to saline groundwater in the interval from 105 to 160 ft bls. Freshwater at the study site is present in the saturated unconsolidated sediments only in the 75 ft between 30 ft (the water table) and 105 ft bls in the shallow high-permeability zone. Sediments shallower than 175 ft bls closely resemble the downward fining post-Wisconsinan age deltaic and lacustrine deposits present in many parts of western Cape Cod; sediments deeper than 175 ft appear to be the product of earlier depositional processes more local to the southern coast of western Cape Cod. This study highlights how high-resolution observations of cored material coupled with a multitool geophysical approach can characterize a single boring to help better understand regional glacial history and hydrogeology.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/sir20195042","collaboration":"Prepared in cooperation with the Cape Cod Commission","usgsCitation":"Hull, R.B, Johnson, C.D., Stone, B.D., LeBlanc, D.R., McCobb, T.D., Phillips, S.N., Pappas, K.L., and Lane, J.W., 2019, Lithostratigraphic, geophysical, and hydrogeologic observations from a boring drilled to bedrock in glacial sediments near Nantucket sound in East Falmouth, Massachusetts: U.S. Geological Survey Scientific Investigations Report 2019–5042, 27 p., https://doi.org/10.3133/sir20195042.","productDescription":"Report: 27 p.; Data Releases","onlineOnly":"Y","additionalOnlineFiles":"N","ipdsId":"IP-088627","costCenters":[{"id":243,"text":"Eastern Geology and Paleoclimate Science Center","active":true,"usgs":true},{"id":466,"text":"New England Water Science Center","active":true,"usgs":true},{"id":37277,"text":"WMA - Earth System Processes Division","active":true,"usgs":true}],"links":[{"id":365906,"rank":4,"type":{"id":30,"text":"Data Release"},"url":"https://doi.org/10.5066/F7P26X0Z ","text":"USGS data release","description":"USGS data release","linkHelpText":"Geophysical data"},{"id":365905,"rank":3,"type":{"id":30,"text":"Data Release"},"url":" https://doi.org/10.5066/F7W66JPM","text":"USGS data release","description":"USGS data release","linkHelpText":"Lithostratigraphic and hydraulic data"},{"id":437379,"rank":5,"type":{"id":30,"text":"Data Release"},"url":"https://doi.org/10.5066/F7W66JPM","text":"USGS data release","linkHelpText":"Lithostratigrapic, Geophysical, and Hydrogeologic Observations from a Deep Boring in Glacial Sediments on Davis Neck near Nantucket Sound, East Falmouth, Western Cape Cod, Massachusetts"},{"id":365822,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/sir/2019/5042/coverthb.jpg"},{"id":365823,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/sir/2019/5042/sir20195042.pdf","text":"Report","size":"3.40 MB","linkFileType":{"id":1,"text":"pdf"},"description":"SIR 2019-5042"}],"country":"United States","state":"Massachusetts","otherGeospatial":"Nantucket Sound","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -70.69290161132811,\n              41.22824901518529\n            ],\n            [\n              -69.90875244140625,\n              41.22824901518529\n            ],\n            [\n              -69.90875244140625,\n              41.60312076451184\n            ],\n            [\n              -70.69290161132811,\n              41.60312076451184\n            ],\n            [\n              -70.69290161132811,\n              41.22824901518529\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","contact":"<p><a href=\"mailto:dc_nweng@usgs.gov\" data-mce-href=\"mailto:dc_nweng@usgs.gov\">Director</a>,<a href=\"https://newengland.water.usgs.gov\" data-mce-href=\"https://newengland.water.usgs.gov\"> New England Water Science Center</a><br>U.S. Geological Survey <br>331 Commerce Road, Suite 2 <br>Pembroke, NH 03275</p>","tableOfContents":"<ul><li>Abstract</li><li>Introduction</li><li>Methods of Well Construction, Data Collection, and Analysis</li><li>Lithostratigraphic Characterization of the Study Area</li><li>Hydrogeological Characterization of the Study Area</li><li>Summary</li><li>References Cited</li></ul>","publishingServiceCenter":{"id":11,"text":"Pembroke PSC"},"publishedDate":"2019-07-31","noUsgsAuthors":false,"publicationDate":"2019-07-31","publicationStatus":"PW","contributors":{"authors":[{"text":"Hull, Robert B. 0000-0002-0216-5250","orcid":"https://orcid.org/0000-0002-0216-5250","contributorId":215569,"corporation":false,"usgs":true,"family":"Hull","given":"Robert","email":"","middleInitial":"B.","affiliations":[{"id":466,"text":"New England Water Science Center","active":true,"usgs":true}],"preferred":true,"id":766765,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Johnson, Carole D. 0000-0001-6941-1578 cjohnson@usgs.gov","orcid":"https://orcid.org/0000-0001-6941-1578","contributorId":1891,"corporation":false,"usgs":true,"family":"Johnson","given":"Carole","email":"cjohnson@usgs.gov","middleInitial":"D.","affiliations":[{"id":37277,"text":"WMA - Earth System Processes Division","active":true,"usgs":true}],"preferred":true,"id":766766,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Stone, Byron D. 0000-0001-6092-0798 bdstone@usgs.gov","orcid":"https://orcid.org/0000-0001-6092-0798","contributorId":1702,"corporation":false,"usgs":true,"family":"Stone","given":"Byron","email":"bdstone@usgs.gov","middleInitial":"D.","affiliations":[{"id":243,"text":"Eastern Geology and Paleoclimate Science Center","active":true,"usgs":true},{"id":40020,"text":"Florence Bascom Geoscience Center","active":true,"usgs":true}],"preferred":true,"id":766768,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"LeBlanc, Denis R. 0000-0002-4646-2628 dleblanc@usgs.gov","orcid":"https://orcid.org/0000-0002-4646-2628","contributorId":1696,"corporation":false,"usgs":true,"family":"LeBlanc","given":"Denis","email":"dleblanc@usgs.gov","middleInitial":"R.","affiliations":[{"id":466,"text":"New England Water Science Center","active":true,"usgs":true}],"preferred":true,"id":766767,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"McCobb, Timothy D. 0000-0003-1533-847X","orcid":"https://orcid.org/0000-0003-1533-847X","contributorId":209977,"corporation":false,"usgs":true,"family":"McCobb","given":"Timothy D.","affiliations":[{"id":466,"text":"New England Water Science Center","active":true,"usgs":true}],"preferred":true,"id":766769,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Phillips, Stephanie N. 0000-0002-2022-7726","orcid":"https://orcid.org/0000-0002-2022-7726","contributorId":214857,"corporation":false,"usgs":true,"family":"Phillips","given":"Stephanie","email":"","middleInitial":"N.","affiliations":[{"id":37277,"text":"WMA - Earth System Processes Division","active":true,"usgs":true},{"id":493,"text":"Office of Ground Water","active":true,"usgs":true}],"preferred":true,"id":766770,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Pappas, Katherine L. 0000-0002-1030-6973","orcid":"https://orcid.org/0000-0002-1030-6973","contributorId":217436,"corporation":false,"usgs":true,"family":"Pappas","given":"Katherine","email":"","middleInitial":"L.","affiliations":[{"id":493,"text":"Office of Ground Water","active":true,"usgs":true}],"preferred":true,"id":766771,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Lane, John W. Jr. 0000-0002-3558-243X","orcid":"https://orcid.org/0000-0002-3558-243X","contributorId":210076,"corporation":false,"usgs":true,"family":"Lane","given":"John W.","suffix":"Jr.","affiliations":[{"id":37277,"text":"WMA - Earth System Processes Division","active":true,"usgs":true},{"id":493,"text":"Office of Ground Water","active":true,"usgs":true},{"id":486,"text":"OGW Branch of Geophysics","active":true,"usgs":true},{"id":34685,"text":"Dakota Water Science Center","active":true,"usgs":true}],"preferred":true,"id":766772,"contributorType":{"id":1,"text":"Authors"},"rank":8}]}}
,{"id":70203750,"text":"sir20195052 - 2019 - Hydrogeologic framework and delineation of transient areas contributing recharge and zones of contribution to selected wells in the upper Santa Fe Group aquifer, southeastern Albuquerque, New Mexico, 1900–2050","interactions":[],"lastModifiedDate":"2019-08-01T07:18:46","indexId":"sir20195052","displayToPublicDate":"2019-07-31T11:28:41","publicationYear":"2019","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":334,"text":"Scientific Investigations Report","code":"SIR","onlineIssn":"2328-0328","printIssn":"2328-031X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2019-5052","displayTitle":"Hydrogeologic Framework and Delineation of Transient Areas Contributing Recharge and Zones of Contribution to Selected Wells in the Upper Santa Fe Group Aquifer, Southeastern Albuquerque, New Mexico, 1900–2050","title":"Hydrogeologic framework and delineation of transient areas contributing recharge and zones of contribution to selected wells in the upper Santa Fe Group aquifer, southeastern Albuquerque, New Mexico, 1900–2050","docAbstract":"<p>The Santa Fe Group aquifer is an important source of water to communities within the Middle Rio Grande Basin, including the Albuquerque-Rio Rancho metropolitan area and Kirtland Air Force Base, New Mexico. In November 1999, Kirtland Air Force Base personnel observed fuel-stained soils at the Bulk Fuels Facility on the base. Subsequent pressure tests identified pipeline leaks. Fuels stored at the Bulk Fuels Facility have included aviation gasoline, jet propellant 4, and jet propellant 8. The fuels migrated about 480 feet down to the water table. Ethylene dibromide, the constituent making up the most extensive part of the plume and a component of leaded aviation gasoline, has formed a plume that, in December 2016, was 400 to 1,300 feet wide, extended about 5,800 feet northeast from the Bulk Fuels Facility, and was about 3,700 feet from the nearest downgradient water-supply well.</p><p>Prior to widespread development of groundwater resources in southeastern Albuquerque, groundwater near the present-day location of the Bulk Fuels Facility flowed to the southwest. Groundwater began flowing northeast in about 1980 towards a large area of lowered water levels caused by groundwater pumping.</p><p>In 2013 and 2014 the Albuquerque Bernalillo County Water Utility Authority, the U.S. Air Force, and the U.S. Geological Survey began a cooperative study to characterize the geology and hydrology of the Santa Fe Group aquifer in the vicinity of the ethylene dibromide plume and to develop a local-scale groundwater flow model to delineate areas contributing recharge and zones of contribution to selected water-supply wells.</p><p>For this study, a previously developed Middle Rio Grande Basin regional groundwater-flow model was updated, and a smaller local-scale model was developed. Advective groundwater-flow paths were delineated and visualized with the MODPATH particle-tracking program.</p><p>Of 11 wells included in the historical pumping analysis of areas contributing recharge, only wells K-3, K-7, and RC-4 derived a portion of their water from simulated recharge sources within the local-scale model. None of the areas contributing recharge overlap the Bulk Fuels Facility area or the ethylene dibromide plume footprint as delineated using December 2016 ethylene dibromide data.</p><p>For the historical pumping analysis of zones of contribution, particles for the 11 selected wells generally moved southwest from the north and east boundaries of the local-scale model, moved past their target well, but reversed direction and moved back towards their target well after 1980 when groundwater flow changed to the northeast. Of the 11 wells, only BR-5, RC-5, and VH-2 had 1980–2013 particle pathlines that overlap the December 2016 ethylene dibromide plume footprint, and wells BR-5 and VH-2 have 1980–2013 particle pathlines that overlap the Bulk Fuels Facility area. Particles that were north of the Bulk Fuels Facility when groundwater flow reversed direction would not have the opportunity to interact with the ethylene dibromide plume. Wells BR-5, K-15, and VH-2 did have particles southwest of the Bulk Fuels Facility in 1980. Particles traveling to BR-5 and K-15 passed under or very near the Bulk Fuels Facility area in the 1980–2013 period, but none of the pathlines were shallow enough to interact with ethylene dibromide at the Bulk Fuels Facility. A few particles traveling to VH-2 passed through the Bulk Fuels Facility area at shallow enough depths to interact with ethylene dibromide at the Bulk Fuels Facility in the 1980–2013 period. Ethylene dibromide has not been detected in water samples collected in 2012 through 2015 from the VH-2 well.</p><p>Of 10 water-supply wells near the ethylene dibromide plume included in the future pumping analysis of areas contributing recharge, only wells K-3, RC-3, and RC-4 had areas contributing recharge within the local-scale model. The areas contributing recharge for wells RC-3 and RC-4 do not overlap the Bulk Fuels Facility area or the December 2016 ethylene&nbsp;dibromide plume footprint, but K-3 derives part of its recharge prior to 1980 and during 1980–2015 from within the area of the December 2016 plume footprint.</p><p>The analysis of the future pumping scenarios indicated that wells BR-5, K-3, K-16, RC-5, and VH-2 have pathlines for 1980–2015 and wells K-16 and VH-2 have pathlines for 2015–50 that when projected in plan view pass through the December 2016 plume footprint. Of these five wells, only K-3 and RC-5 have pathlines for 1980–2015 that are above an elevation of 4,800 feet and could interact with the ethylene dibromide plume if ethylene dibromide was present when the particles were present.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/sir20195052","collaboration":"Prepared in cooperation with the Albuquerque Bernalillo County Water Utility Authority and the U.S. Air Force","usgsCitation":"Myers, N.C., and Friesz, P.J., 2019, Hydrogeologic framework and delineation of transient areas contributing recharge and zones of contribution to selected wells in the upper Santa Fe Group aquifer, southeastern Albuquerque, New Mexico, 1900–2050: U.S. Geological Survey Scientific Investigations Report 2019–5052, 73 p., https://doi.org/10.3133/sir20195052.","productDescription":"Report: viii, 73 p.; Data Release","numberOfPages":"86","onlineOnly":"Y","ipdsId":"IP-080008","costCenters":[{"id":466,"text":"New England Water Science Center","active":true,"usgs":true},{"id":472,"text":"New Mexico Water Science Center","active":true,"usgs":true}],"links":[{"id":365539,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/sir/2019/5052/sir20195052.pdf","text":"Report","size":"38.2 MB","linkFileType":{"id":1,"text":"pdf"},"description":"SIR 2019–5052"},{"id":365538,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/sir/2019/5052/coverthb.jpg"},{"id":365540,"rank":3,"type":{"id":30,"text":"Data Release"},"url":"https://doi.org/10.5066/F79P303S","text":"USGS data release ","description":"USGS Data Release","linkHelpText":"MODFLOW–LGR2 groundwater-flow model used to delineate transient areas contributing recharge and zones of contribution to selected wells in the upper Santa Fe Group aquifer, southeastern Albuquerque, New Mexico"}],"country":"United States","state":"New Mexico","county":"Bernalillo County","city":"Albuquerque","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"Polygon\",\"coordinates\":[[[-106.242,35.2147],[-106.2387,35.0549],[-106.2386,35.0408],[-106.2373,34.9568],[-106.1453,34.9547],[-106.1446,34.872],[-106.3328,34.8712],[-106.3569,34.8702],[-106.409,34.8687],[-106.4097,34.8914],[-106.417,34.8945],[-106.4221,34.9013],[-106.6755,34.9065],[-106.6838,34.9006],[-106.6917,34.901],[-106.6922,34.896],[-106.7139,34.8772],[-106.7127,34.8713],[-107.0181,34.8727],[-107.0227,34.8817],[-107.0641,34.9618],[-107.104,35.0395],[-107.1068,35.0454],[-107.1769,35.1809],[-107.1972,35.2197],[-107.1628,35.2192],[-107.1623,35.2192],[-107.1578,35.2192],[-107.1262,35.2186],[-107.1105,35.2188],[-107.0936,35.2189],[-107.0801,35.2186],[-107.0761,35.2186],[-107.0345,35.2185],[-106.9416,35.217],[-106.9337,35.2171],[-106.8808,35.2171],[-106.8622,35.2172],[-106.5955,35.2184],[-106.5645,35.2186],[-106.4964,35.2184],[-106.479,35.2176],[-106.4531,35.2172],[-106.3822,35.2175],[-106.3765,35.2175],[-106.242,35.2147]]]},\"properties\":{\"name\":\"Bernalillo\",\"state\":\"NM\"}}]}","contact":"<p><a data-mce-href=\"mailto:dc_nm@usgs.gov\" href=\"mailto:dc_nm@usgs.gov\">Director</a>, <a data-mce-href=\"https://www.usgs.gov/centers/nm-water\" href=\"https://www.usgs.gov/centers/nm-water\">New Mexico Water Science Center</a> <br>U.S. Geological Survey<br>6700 Edith Blvd. NE, Suite B <br>Albuquerque, NM 87113<br></p>","tableOfContents":"<ul><li>Acknowledgments</li><li>Abstract</li><li>Introduction</li><li>Hydrogeologic Framework</li><li>Numerical Groundwater-Flow Model Development and Calibration</li><li>Delineation of Transient Areas Contributing Recharge and Zones of Contribution to Selected Water-Supply Wells</li><li>Summary</li><li>References Cited</li></ul>","publishingServiceCenter":{"id":5,"text":"Lafayette PSC"},"publishedDate":"2019-07-31","noUsgsAuthors":false,"publicationDate":"2019-07-31","publicationStatus":"PW","contributors":{"authors":[{"text":"Myers, Nathan C. 0000-0002-7469-3693","orcid":"https://orcid.org/0000-0002-7469-3693","contributorId":216132,"corporation":false,"usgs":true,"family":"Myers","given":"Nathan C.","affiliations":[{"id":472,"text":"New Mexico Water Science Center","active":true,"usgs":true}],"preferred":true,"id":763952,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Friesz, Paul J. 0000-0002-4660-2336","orcid":"https://orcid.org/0000-0002-4660-2336","contributorId":216133,"corporation":false,"usgs":true,"family":"Friesz","given":"Paul J.","affiliations":[{"id":466,"text":"New England Water Science Center","active":true,"usgs":true}],"preferred":true,"id":763953,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70204614,"text":"70204614 - 2019 - Hydrous heating experiments at 130°C yield insights into the occurrence of hydrogen sulfide and light alkanes in natural gas reservoirs","interactions":[],"lastModifiedDate":"2019-08-29T12:01:55","indexId":"70204614","displayToPublicDate":"2019-07-31T10:57:02","publicationYear":"2019","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2958,"text":"Organic Geochemistry","active":true,"publicationSubtype":{"id":10}},"title":"Hydrous heating experiments at 130°C yield insights into the occurrence of hydrogen sulfide and light alkanes in natural gas reservoirs","docAbstract":"<p><span>Improved understanding of the origin of produced volatiles from conventional reservoirs and unconventional source rocks is critical for petroleum exploration and production. A series of hydrous heating experiments using two immature Type II siliciclastic source rocks, Pennsylvanian Turner Mine shale (TMS) and Devonian New Albany Shale (NAS), at 130 °C over one to two years were conducted to assess gas generation at low temperature. Elemental sulfur (ES) was added to the NAS samples to evaluate the role of sulfur on thermochemical sulfate reduction (TSR). The produced volatile composition was investigated in situ using Raman spectroscopy at the end of the heating experiments. Results show that the two source rocks yield different types and concentrations of volatiles. Only CH</span><sub>4</sub><span>&nbsp;and CO</span><sub>2</sub><span>&nbsp;were detected following hydrous heating of the TMS source rock in contrast to CH</span><sub>4</sub><span>, C</span><sub>2</sub><span>H</span><sub>6</sub><span>, C</span><sub>3</sub><span>H</span><sub>8</sub><span>, and CO</span><sub>2</sub><span>&nbsp;which were observed in experiments using NAS. Variations in the produced volatiles are likely the result of compositional differences within the respective source rock organic matter. Experiments involving ES show strong H</span><sub>2</sub><span>S signals that are likely due to the formation of H</span><sub>2</sub><span>S from the reaction of ES with water at 130 °C. H</span><sub>2</sub><span>S signals correlate with a greater relative concentration of CH</span><sub>4</sub><span>&nbsp;and CO</span><sub>2</sub><span>&nbsp;compared to experiments where ES was not added, on a time-normalized basis. The correlation between the presence of H</span><sub>2</sub><span>S and an increase in CH</span><sub>4</sub><span>&nbsp;and CO</span><sub>2</sub><span>&nbsp;concentration could indicate the occurrence of TSR. Here we propose that H</span><sub>2</sub><span>S in siliciclastic shale can be generated in the presence of ES at low temperatures via both disproportionation of ES into H</span><sub>2</sub><span>S and SO</span><sub>4</sub><sup>2–</sup><span>, and TSR. Our findings from this study provide experimental evidence that may aid efforts to interpret the origin of H</span><sub>2</sub><span>S in low-temperature sedimentary basins.</span></p>","language":"English","publisher":"Elsevier","doi":"10.1016/j.orggeochem.2019.103901","usgsCitation":"Alrowaie, M., Jubb, A., Schimmelmann, A., Mastalerz, M., and Pratt, L., 2019, Hydrous heating experiments at 130°C yield insights into the occurrence of hydrogen sulfide and light alkanes in natural gas reservoirs: Organic Geochemistry, v. 137, 103901, 8 p., https://doi.org/10.1016/j.orggeochem.2019.103901.","productDescription":"103901, 8 p.","ipdsId":"IP-105974","costCenters":[{"id":241,"text":"Eastern Energy Resources Science Center","active":true,"usgs":true}],"links":[{"id":366290,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United 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University","active":true,"usgs":false}],"preferred":false,"id":767777,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Mastalerz, M.","contributorId":217905,"corporation":false,"usgs":false,"family":"Mastalerz","given":"M.","affiliations":[{"id":33640,"text":"Indiana Geological Survey","active":true,"usgs":false}],"preferred":false,"id":767778,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Pratt, L.M.","contributorId":217906,"corporation":false,"usgs":false,"family":"Pratt","given":"L.M.","email":"","affiliations":[{"id":37145,"text":"Indiana University","active":true,"usgs":false}],"preferred":false,"id":767779,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":70215401,"text":"70215401 - 2019 - Preface—Evaluating the response of critical zone processes to human impacts with sediment source fingerprinting","interactions":[],"lastModifiedDate":"2020-10-18T15:04:05.341997","indexId":"70215401","displayToPublicDate":"2019-07-31T09:58:39","publicationYear":"2019","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2457,"text":"Journal of Soils and Sediments","active":true,"publicationSubtype":{"id":10}},"title":"Preface—Evaluating the response of critical zone processes to human impacts with sediment source fingerprinting","docAbstract":"1) Background: Critical Zone Processes in the Anthropocene\n\nThe Earth’s Critical Zone encompasses a suite of interconnected processes in the near-surface lithosphere, pedosphere, biosphere, atmosphere, and hydrosphere (Brantley et al., 2007; Lin, 2010) (Fig. 1). Processes and interactions both within and between these various Critical Zone components supports life-sustaining ecosystem services and resources that establish the foundation for humanity (NRC, 2001). This includes the formation production of fertile soils, flourishing vegetation, productive rivers, lakes and oceans, and our life-sustaining atmosphere (Gaillardet, 2014; Guo and Lin, 2016).\n\nRapid population growth, land use intensification, and global environmental change are disturbing many of these fundamental Critical Zone processes. More than half of the Earth’s terrestrial surface is now impacted by anthropogenic activities (e.g., clearing, grazing, plowing, mining, and logging) (Hooke et al., 2012; Richter and Mobley, 2009). These changes are so widespread and pervasive that the great acceleration of socioeconomic development that occurred around 1950 (Fig. 2) has been recommended to delineate the dawn of the Anthropocene (Waters et al., 2016). Although the utility of adopting and delineating the Anthropocene as the current epoch is subject to debate (Crutzen, 2002; Ruddiman et al., 2015; Smith and Zeder, 2013), the concept effectively highlights both the nature and the extent of our global impact on Earth’s Critical Zone. \n\nSoil forming processes and ecosystem services provided by the pedosphere are central to the Critical Zone (Banwart et al., 2011; Lin, 2010). Many of these processes have been disturbed by the agricultural intensification that coincided with the great acceleration resulting in unsustainable land use practices now outpacing soil formation processes (Brantley et al., 2007). As agricultural landscapes now cover an area equivalent to what was scoured during the last glacial maximum (Amundson et al., 2007), the broad-scale intensification of anthropogenic activities has resulted in significant on- and off-site impacts. On-site, soil loss has resulted in decreases in soil fertility and agricultural yields (Ladha et al., 2009) threatening the ability to feed the world’s growing population (Brantley et al., 2007). Off-site, the excess delivery of particulate matter downstream is degrading riverine, lacustrine, and estuarine ecosystems (Bilotta and Brazier, 2008; Clark, 1985; Owens et al., 2005).\nThe challenge, as noted by Brantley et al., (2007), is that despite our society having over 10,000 years of experience working with soils, our conceptual and quantitative models remain inadequate at predicting Critical Zone dynamics under current conditions. Notwithstanding growing pressure for improved environmental management, we still have a limited capacity to predict changes in the Critical Zone in response to anthropogenic activities owing to the multiple spatial and temporal scales at which these complex processes and feedbacks are manifest. As river basin systems are impacted by many of these processes, a deep understanding of soil-sediment continuum dynamics may provide a valuable framework for evaluating the disturbance response of Critical Zone processes. Understanding these processes may also provide land and resource managers with the information necessary to manage both the on-site and off-site effects of accelerated soil erosion.","language":"English","publisher":"Springer","doi":"10.1007/s11368-019-02409-0","usgsCitation":"Laceby, J.P., Gellis, A.C., Koiter, A.J., Blake, W.H., and Evrard, O., 2019, Preface—Evaluating the response of critical zone processes to human impacts with sediment source fingerprinting: Journal of Soils and Sediments, v. 19, p. 3245-3254, https://doi.org/10.1007/s11368-019-02409-0.","productDescription":"10 p.","startPage":"3245","endPage":"3254","ipdsId":"IP-109272","costCenters":[{"id":41514,"text":"Maryland-Delaware-District of Columbia  Water Science Center","active":true,"usgs":true}],"links":[{"id":467405,"rank":0,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1007/s11368-019-02409-0","text":"Publisher Index Page"},{"id":379500,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"19","noUsgsAuthors":false,"publicationDate":"2019-07-31","publicationStatus":"PW","contributors":{"authors":[{"text":"Laceby, J. Patrick","contributorId":243321,"corporation":false,"usgs":false,"family":"Laceby","given":"J.","email":"","middleInitial":"Patrick","affiliations":[{"id":48685,"text":"Environmental Monitoring and Science Division, Alberta Environment and Parks, 3115 – 12 Street NE Calgary, Alberta, Canada","active":true,"usgs":false}],"preferred":false,"id":802032,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Gellis, Allen C. 0000-0002-3449-2889 agellis@usgs.gov","orcid":"https://orcid.org/0000-0002-3449-2889","contributorId":197684,"corporation":false,"usgs":true,"family":"Gellis","given":"Allen","email":"agellis@usgs.gov","middleInitial":"C.","affiliations":[{"id":374,"text":"Maryland Water Science Center","active":true,"usgs":true}],"preferred":true,"id":802037,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Koiter, Alexander J.","contributorId":243322,"corporation":false,"usgs":false,"family":"Koiter","given":"Alexander","email":"","middleInitial":"J.","affiliations":[{"id":48686,"text":"Department of Geography and Environment, Brandon University, 270 18th St, Brandon, MB R7A 6A9, Canada","active":true,"usgs":false}],"preferred":false,"id":802038,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Blake, Will H.","contributorId":243323,"corporation":false,"usgs":false,"family":"Blake","given":"Will","email":"","middleInitial":"H.","affiliations":[{"id":48687,"text":"School of Geography, Earth and Environmental Sciences, Plymouth University, Plymouth, PL4 8AA, UK","active":true,"usgs":false}],"preferred":false,"id":802039,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Evrard, Olivier","contributorId":243324,"corporation":false,"usgs":false,"family":"Evrard","given":"Olivier","email":"","affiliations":[{"id":48688,"text":"Laboratoire des Sciences du Climat et de l’Environnement, LSCE/IPSL, UMR 8212 (CEA-CNRS-UVSQ), Université Paris-Saclay, F-91191Gif-sur-Yvette Cedex, France","active":true,"usgs":false}],"preferred":false,"id":802040,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":70210860,"text":"70210860 - 2019 - Geochemical characterization of iron and steel slag and its potential to remove phosphate and neutralize acid","interactions":[],"lastModifiedDate":"2021-05-13T17:02:43.019363","indexId":"70210860","displayToPublicDate":"2019-07-31T08:17:07","publicationYear":"2019","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":5207,"text":"Minerals","active":true,"publicationSubtype":{"id":10}},"title":"Geochemical characterization of iron and steel slag and its potential to remove phosphate and neutralize acid","docAbstract":"Iron and steel slags from legacy and modern operations in the Chicago-Gary area of Illinois and Indiana, USA, are predominantly composed of Ca (10 - 44 wt. % CaO), Fe, (0.3 - 28 wt. % FeO), and Si (10 - 44 wt. % SiO2), with generally lesser amounts of Al (< 1  15 wt. % Al2O3), Mg (2  11 wt. % MgO), and Mn (0.3  9 wt. % MnO). Mineralogy is dominated by CaMgAl silicates, FeCa oxides, Ca-carbonates, and high temperature SiO2 phases. Chromium and Mn concentrations in most samples may be environmentally significant based on comparison with generic soil contaminant guidelines. However, simulated weathering tests suggest these elements are present in generally insoluble phases making use in water treatment applications possible; generation of high pH and alkaline solutions may be an issue. As for water treatment applications, batch and flow-through experiments document effective removal of phosphate from synthetic solutions for nearly all slag samples. Air-cooled fine fractions (< 10 mm) of modern slag were most effective; other types, including modern granulated, modern air-cooled coarse fractions (> 10 mm), and legacy slag removed phosphate, but to a lesser degree. An additional water treatment application is the use of slag to neutralize acidic waters. Most slag samples are extremely alkaline and have high net neutralization potentials (NNP) (400  830 kg CaCO3/t), with the highest approximately equivalent to 80% the neutralization potential of calcite. Overall, phosphate removal capacity and NNP correlate positively with total Ca content and the dissolution of Ca minerals facilitates secondary Ca phosphate formation and consumes acid during hydrolysis. Utilizing locally available slag to treat waste or agricultural waters in this region may be a higher value alternative than use in construction, potentially offsetting restoration costs to degraded legacy areas and decreasing steel manufacturers current waste footprint.","language":"English","publisher":"MDPI","doi":"10.3390/min9080468","usgsCitation":"Piatak, N.M., Seal,, R., Hoppe, D.A., Green, C.J., and Buszka, P.M., 2019, Geochemical characterization of iron and steel slag and its potential to remove phosphate and neutralize acid: Minerals, v. 9, no. 8, 468, 26 p., https://doi.org/10.3390/min9080468.","productDescription":"468, 26 p.","ipdsId":"IP-109123","costCenters":[{"id":245,"text":"Eastern Mineral and Environmental Resources Science Center","active":true,"usgs":true},{"id":346,"text":"Indiana Water Science Center","active":true,"usgs":true}],"links":[{"id":467407,"rank":3,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.3390/min9080468","text":"Publisher Index Page"},{"id":376012,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":385609,"rank":2,"type":{"id":30,"text":"Data Release"},"url":"https://doi.org/10.5066/P9X7SPIK","text":"USGS Data Release","description":"USGS Data Release","linkHelpText":"Geochemical characterization, acid neutralization potential, and phosphate removal capacity of modern and legacy iron and steel slag from the Chicago-Gary area of Illinois and Indiana, USA"}],"volume":"9","issue":"8","noUsgsAuthors":false,"publicationDate":"2019-07-31","publicationStatus":"PW","contributors":{"authors":[{"text":"Piatak, Nadine M. 0000-0002-1973-8537 npiatak@usgs.gov","orcid":"https://orcid.org/0000-0002-1973-8537","contributorId":193010,"corporation":false,"usgs":true,"family":"Piatak","given":"Nadine","email":"npiatak@usgs.gov","middleInitial":"M.","affiliations":[{"id":245,"text":"Eastern Mineral and Environmental Resources Science Center","active":true,"usgs":true}],"preferred":true,"id":791755,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Seal,, Robert R. II 0000-0003-0901-2529 rseal@usgs.gov","orcid":"https://orcid.org/0000-0003-0901-2529","contributorId":141204,"corporation":false,"usgs":true,"family":"Seal,","given":"Robert R.","suffix":"II","email":"rseal@usgs.gov","affiliations":[{"id":245,"text":"Eastern Mineral and Environmental Resources Science Center","active":true,"usgs":true}],"preferred":true,"id":791756,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Hoppe, Darryl Andre 0000-0003-3369-5577","orcid":"https://orcid.org/0000-0003-3369-5577","contributorId":225586,"corporation":false,"usgs":true,"family":"Hoppe","given":"Darryl","email":"","middleInitial":"Andre","affiliations":[{"id":245,"text":"Eastern Mineral and Environmental Resources Science Center","active":true,"usgs":true}],"preferred":true,"id":791757,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Green, Carlin J. 0000-0002-6557-6268 cjgreen@usgs.gov","orcid":"https://orcid.org/0000-0002-6557-6268","contributorId":193013,"corporation":false,"usgs":true,"family":"Green","given":"Carlin","email":"cjgreen@usgs.gov","middleInitial":"J.","affiliations":[{"id":245,"text":"Eastern Mineral and Environmental Resources Science Center","active":true,"usgs":true}],"preferred":true,"id":791758,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Buszka, Paul M. 0000-0001-8218-826X pmbuszka@usgs.gov","orcid":"https://orcid.org/0000-0001-8218-826X","contributorId":1786,"corporation":false,"usgs":true,"family":"Buszka","given":"Paul","email":"pmbuszka@usgs.gov","middleInitial":"M.","affiliations":[{"id":27231,"text":"Indiana-Kentucky Water Science Center","active":true,"usgs":true},{"id":346,"text":"Indiana Water Science Center","active":true,"usgs":true}],"preferred":true,"id":791759,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":70204407,"text":"fs20193038 - 2019 - Nutrients in northern Missouri streams","interactions":[],"lastModifiedDate":"2019-07-31T10:45:25","indexId":"fs20193038","displayToPublicDate":"2019-07-30T14:17:20","publicationYear":"2019","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":313,"text":"Fact Sheet","code":"FS","onlineIssn":"2327-6932","printIssn":"2327-6916","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2019-3038","displayTitle":"Nutrients in Northern Missouri Streams","title":"Nutrients in northern Missouri streams","docAbstract":"<p>Nutrients, specifically nitrogen and phosphorus, are necessary for healthy aquatic communities to thrive, but if nutrient concentrations are too high, water quality can be degraded and natural aquatic communities may be destroyed. Nutrients consistently have been listed nationally as one of the top five causes of stream and river impairments, and agriculture consistently has been identified as the leading known source. The Mississippi River watershed was identified as a top priority for nutrient reductions because of the predominant agricultural land use, the associated harmful effects of nutrient loading on local water bodies, and the resulting annual midsummer northern Gulf of Mexico hypoxic “dead” zone. In 2010, the Natural Resources Conservation Service started the Mississippi River Basin Healthy Watersheds Initiative, which offers financial and technical assistance for voluntary conservation practices on agricultural lands. The intention is to reduce nutrient and sediment export to waterways within the Mississippi River watershed. The U.S.&nbsp;Geological Survey Missouri Water Science Center and the Missouri Department of Natural Resources began a cooperative study in 2010 to compare temporal changes in total nitrogen and total phosphorus concentrations in the Lower Grand River.</p><p>Despite increases in conservation practice funding from the Mississippi River Basin Healthy Watersheds Initiative during 2011–15 for the Lower Grand River, decreases in flow-normalized total nitrogen and total phosphorus concentrations during this same period at the Grand River site were less than at the other long-term Missouri River tributary sites that did not receive additional funding. The flow-normalized total nitrogen and total phosphorus concentrations at the three long-term Missouri River tributary sites were related to the amount of agricultural land use within their watersheds and livestock manure may be a substantial source of stream nitrogen. Monthly total nitrogen and total phosphorus concentrations within the Lower Grand River increased with increased streamflow, indicating that the major sources of nitrogen and phosphorus are runoff or nutrients that are stored in soils within the streambank that mobilize during higher streamflows. Programs such as the Mississippi River Basin Healthy Watersheds Initiative are intended to encourage voluntary agricultural conservation practices to enhance soil health and reduce nutrient export to streams.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/fs20193038","collaboration":"Prepared in cooperation with Missouri Department of Natural Resources","usgsCitation":"Krempa, H.M., 2019, Nutrients in northern Missouri streams: U.S. Geological Survey Fact Sheet 2019–3038, 4 p., https://doi.org/10.3133/fs20193038.","productDescription":"4 p.","numberOfPages":"4","onlineOnly":"N","ipdsId":"IP-091415","costCenters":[{"id":36532,"text":"Central Midwest Water Science Center","active":true,"usgs":true}],"links":[{"id":366037,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/fs/2019/3038/fs20193038.pdf","text":"Report","size":"861 kB","linkFileType":{"id":1,"text":"pdf"},"description":"FS 2019–3038"},{"id":366036,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/fs/2019/3038/coverthb2.jpg"}],"country":"United States","state":"Missouri","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -95.2,\n              39.2\n            ],\n            [\n              -92.5,\n              39.2\n            ],\n            [\n              -92.5,\n              41.5\n            ],\n            [\n              -95.2,\n              41.5\n            ],\n            [\n              -95.2,\n              39.2\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","contact":"<p><a data-mce-href=\"mailto:%20dc_mo@usgs.gov\" href=\"mailto:%20dc_mo@usgs.gov\">Director</a>, <a data-mce-href=\"https://www.usgs.gov/centers/cm-water\" href=\"https://www.usgs.gov/centers/cm-water\">Central Midwest Water Science Center</a> <br>U.S. Geological Survey <br>1400 Independence Road <br>Rolla, MO 65401</p>","tableOfContents":"<ul><li>Introduction</li><li>Mississippi River Basin Healthy Watersheds Initiative</li><li>Nutrients in Northern Missouri Streams</li><li>Study Design</li><li>Nutrient Concentration Changes and Agricultural Practices</li><li>Reducing Nutrients in Waterways</li><li>References Cited</li></ul>","publishingServiceCenter":{"id":4,"text":"Rolla PSC"},"publishedDate":"2019-07-30","noUsgsAuthors":false,"publicationDate":"2019-07-30","publicationStatus":"PW","contributors":{"authors":[{"text":"Krempa, Heather 0000-0002-1556-6934","orcid":"https://orcid.org/0000-0002-1556-6934","contributorId":217386,"corporation":false,"usgs":true,"family":"Krempa","given":"Heather","affiliations":[{"id":396,"text":"Missouri Water Science Center","active":true,"usgs":true}],"preferred":true,"id":766687,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70205899,"text":"70205899 - 2019 - Reduced soil macropores and forest cover reduce warm-season baseflow below ecological thresholds in the upper Delaware River Basin","interactions":[],"lastModifiedDate":"2019-10-09T12:58:42","indexId":"70205899","displayToPublicDate":"2019-07-30T12:53:41","publicationYear":"2019","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2529,"text":"Journal of the American Water Resources Association","active":true,"publicationSubtype":{"id":10}},"title":"Reduced soil macropores and forest cover reduce warm-season baseflow below ecological thresholds in the upper Delaware River Basin","docAbstract":"We examined the impacts of changes in land cover and soil conditions on the flow regime of the upper Delaware River Basin using the Water Availability Tool for Environmental Resources (WATER). We simulated flows for two periods, circa 1600 and 1940, at three sites using the same temperature and precipitation conditions: the East Branch (EB), West Branch (WB), and mainstem Delaware River at Callicoon, NY. The 1600 period represented pristine forest and soils. The 1940 period included reduced forest cover, increased agriculture, and degraded soils with reduced soil macropore fractions. A model-sensitivity test examined the impact of soil macropore and land cover change separately. We assessed changes in flow regimes between the 1600 and 1940 periods using a variety of flow statistics, including established ecological limits of hydrologic alteration (ELOHA) thresholds. Reduced forest soil macropore fraction significantly reduced summer and fall base flows. The 1940 period had significantly lower Q50 flows (50% exceedance) than the 1600 period, as well as summer and fall Q90 and Q75-90 flows below the ELOHA thresholds. The 1- to 7-day minimum flows were also lower for the 1940 period, by 17% on the mainstem.  1940 flows were 6% more likely than the 1600 period to fall below the low-flow threshold for federally endangered dwarf wedgemussel (Alasmidonta heterodon) habitat. In contrast, the 1940 period had higher flows than the 1600 period from late fall to early winter.","language":"English","publisher":"Wiley","doi":"10.1111/1752-1688.12777","usgsCitation":"Endreny, T.A., Kwon, P.Y., Williamson, T.N., and Evans, R., 2019, Reduced soil macropores and forest cover reduce warm-season baseflow below ecological thresholds in the upper Delaware River Basin: Journal of the American Water Resources Association, v. 55, no. 5, p. 1268-1287, https://doi.org/10.1111/1752-1688.12777.","productDescription":"20 p.","startPage":"1268","endPage":"1287","ipdsId":"IP-091449","costCenters":[{"id":35860,"text":"Ohio-Kentucky-Indiana Water Science Center","active":true,"usgs":true}],"links":[{"id":368171,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"New York, Pennsylvania","otherGeospatial":"Upper Delaware River Basin","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -76.5966796875,\n              40.9964840143779\n            ],\n            [\n              -74.3389892578125,\n              40.9964840143779\n            ],\n            [\n              -74.3389892578125,\n              42.85583308674893\n            ],\n            [\n              -76.5966796875,\n              42.85583308674893\n            ],\n            [\n              -76.5966796875,\n              40.9964840143779\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"55","issue":"5","publishingServiceCenter":{"id":15,"text":"Madison PSC"},"noUsgsAuthors":false,"publicationDate":"2019-07-30","publicationStatus":"PW","contributors":{"authors":[{"text":"Endreny, Theodore A.","contributorId":195489,"corporation":false,"usgs":false,"family":"Endreny","given":"Theodore","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":772809,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Kwon, Peter Yong Seuk","contributorId":219658,"corporation":false,"usgs":false,"family":"Kwon","given":"Peter","email":"","middleInitial":"Yong Seuk","affiliations":[{"id":34139,"text":"Anchor QEA","active":true,"usgs":false}],"preferred":false,"id":772810,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Williamson, Tanja N. 0000-0002-7639-8495 tnwillia@usgs.gov","orcid":"https://orcid.org/0000-0002-7639-8495","contributorId":198329,"corporation":false,"usgs":true,"family":"Williamson","given":"Tanja","email":"tnwillia@usgs.gov","middleInitial":"N.","affiliations":[{"id":35860,"text":"Ohio-Kentucky-Indiana Water Science Center","active":true,"usgs":true}],"preferred":true,"id":772808,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Evans, Richard","contributorId":216306,"corporation":false,"usgs":false,"family":"Evans","given":"Richard","affiliations":[{"id":36189,"text":"National Park Service","active":true,"usgs":false}],"preferred":false,"id":772811,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70204576,"text":"70204576 - 2019 - Characterizing crop water use dynamics in the Central Valley of California using landsat-derived evapotranspiration","interactions":[],"lastModifiedDate":"2019-08-07T08:59:41","indexId":"70204576","displayToPublicDate":"2019-07-30T12:20:01","publicationYear":"2019","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3250,"text":"Remote Sensing","active":true,"publicationSubtype":{"id":10}},"title":"Characterizing crop water use dynamics in the Central Valley of California using landsat-derived evapotranspiration","docAbstract":"Understanding how different crops use water over time is essential for planning and managing water allocation, water rights, and agricultural production. The main objective of this paper is to characterize the spatiotemporal dynamics of crop water use in the Central Valley of California using Landsat-based annual actual evapotranspiration (ETa) from 2008 to 2018 derived from the Operational Simplified Surface Energy Balance (SSEBop) model. Crop water use for 10 crops is characterized at multiple scales. The Mann–Kendall trend analysis revealed a significant increase in area cultivated with almonds and their water use, with an annual rate of change of 16,327 ha in area and 13,488 ha-m in water use. Conversely, alfalfa showed a significant decline with 12,429 ha in area and 13,901 ha-m in water use per year during the same period. A pixel-based Mann–Kendall trend analysis showed the changing crop type and water use at the level of individual fields for all of Kern County in the Central Valley. This study demonstrates the useful application of historical Landsat ET to produce relevant water management information. Similar studies can be conducted at regional and global scales to understand and quantify the relationships between land cover change and its impact on water use.","language":"English","publisher":"MDPI","doi":"10.3390/rs11151782","usgsCitation":"Schauer, M., and Senay, G., 2019, Characterizing crop water use dynamics in the Central Valley of California using landsat-derived evapotranspiration: Remote Sensing, v. 15, no. 11, 22 p., https://doi.org/10.3390/rs11151782.","productDescription":"22 p.","ipdsId":"IP-085933","costCenters":[{"id":222,"text":"Earth Resources Observation and Science (EROS) Center","active":true,"usgs":true}],"links":[{"id":467408,"rank":0,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.3390/rs11151782","text":"Publisher Index Page"},{"id":366308,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United 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 \"}}]}","volume":"15","issue":"11","publishingServiceCenter":{"id":4,"text":"Rolla PSC"},"noUsgsAuthors":false,"publicationDate":"2019-07-30","publicationStatus":"PW","contributors":{"authors":[{"text":"Schauer, Matthew 0000-0002-4198-3379","orcid":"https://orcid.org/0000-0002-4198-3379","contributorId":216909,"corporation":false,"usgs":true,"family":"Schauer","given":"Matthew","email":"","affiliations":[{"id":222,"text":"Earth Resources Observation and Science (EROS) Center","active":true,"usgs":true}],"preferred":true,"id":767618,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Senay, Gabriel 0000-0002-8810-8539","orcid":"https://orcid.org/0000-0002-8810-8539","contributorId":216910,"corporation":false,"usgs":true,"family":"Senay","given":"Gabriel","affiliations":[{"id":222,"text":"Earth Resources Observation and Science (EROS) Center","active":true,"usgs":true}],"preferred":false,"id":767617,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70203970,"text":"ofr20191076 - 2019 - Baseline groundwater hydrology and water quality in and around Bluff, Utah","interactions":[],"lastModifiedDate":"2019-07-31T10:43:36","indexId":"ofr20191076","displayToPublicDate":"2019-07-30T10:29:09","publicationYear":"2019","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2019-1076","displayTitle":"Baseline Groundwater Hydrology and Water Quality In and Around Bluff, Utah","title":"Baseline groundwater hydrology and water quality in and around Bluff, Utah","docAbstract":"<div><div>Southeastern Utah has a long history of oil and gas production. Two new hydrocarbon extraction wells have been proposed several miles northeast of the town of Bluff, Utah. In response to concern about the impacts of oil and gas extraction in the area on drinking-water quality, this study provides groundwater quality and hydrologic baseline data obtained before drilling the new hydrocarbon extraction wells. Data from future monitoring can be compared to these baseline water-quality data to identify changes in water quality. The quality of drinking water in Bluff is generally good, making changes in water quality more easily identifiable. Potential degradation of water quality from the proposed production wells could take hundreds to thousands of years to reach public-supply wells. Because of the limited water supply in this area, high-quality groundwater will continue to be an important resource into the foreseeable future.</div></div>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr20191076","collaboration":"Prepared in cooperation with the Bureau of Land Management","usgsCitation":"Miller, O.L., 2019, Baseline groundwater hydrology and water quality in and around Bluff, Utah: U.S. Geological Survey Open-File Report 2019–1076, 24 p., https://doi.org/10.3133/ofr20191076.","productDescription":" viii, 24 p.","numberOfPages":"36","onlineOnly":"Y","ipdsId":"IP-098839","costCenters":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":365995,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/2019/1076/coverthb.jpg"},{"id":365996,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/2019/1076/ofr20191076.pdf","text":"Report","size":"8.7 MB","linkFileType":{"id":1,"text":"pdf"},"description":"OFR 2019-1076"}],"country":"United States","state":"Utah","city":"Bluff","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -109.6667,\n              37.58333\n            ],\n            [\n              -109.3333,\n              37.58333\n            ],\n            [\n              -109.3333,\n              37.25\n            ],\n            [\n              -109.6667,\n              37.25\n            ],\n            [\n              -109.6667,\n              37.58333\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","contact":"<p><a data-mce-href=\"https://www.usgs.gov/centers/ut-water/connect\" href=\"https://www.usgs.gov/centers/ut-water/connect\" target=\"_blank\" rel=\"noopener\">Director</a>, <br><a data-mce-href=\"https://ut.water.usgs.gov\" href=\"https://ut.water.usgs.gov\" target=\"_blank\" rel=\"noopener\">Utah Water Science Center</a><br><a data-mce-href=\"https://usgs.gov\" href=\"https://usgs.gov\" target=\"_blank\" rel=\"noopener\">U.S. Geological Survey</a><br>2329 West Orton Circle<br>Salt Lake City, Utah 84119-2047<br>801-908-5000<br></p>","tableOfContents":"<ul><li>Abstract</li><li>Introduction</li><li>Methods</li><li>Groundwater Hydrology and Water Quality</li><li>Conclusions and Future Monitoring</li><li>References Cited</li></ul>","publishingServiceCenter":{"id":1,"text":"Sacramento PSC"},"publishedDate":"2019-07-30","noUsgsAuthors":false,"publicationDate":"2019-07-30","publicationStatus":"PW","contributors":{"authors":[{"text":"Miller, Olivia L. 0000-0002-8846-7048","orcid":"https://orcid.org/0000-0002-8846-7048","contributorId":216556,"corporation":false,"usgs":true,"family":"Miller","given":"Olivia","email":"","middleInitial":"L.","affiliations":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"preferred":true,"id":765029,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70203755,"text":"ofr20191068 - 2019 - South Atlantic Water Science Center Strategic Science Plan: 2019–23","interactions":[],"lastModifiedDate":"2019-07-30T14:34:41","indexId":"ofr20191068","displayToPublicDate":"2019-07-30T09:45:00","publicationYear":"2019","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2019-1068","displayTitle":"South Atlantic Water Science Center Strategic Science Plan: 2019–23","title":"South Atlantic Water Science Center Strategic Science Plan: 2019–23","docAbstract":"<h1>Executive Summary</h1><p>The South Atlantic Water Science Center Strategic Science Planning Team has developed a unified strategic science plan to guide the science vision of the South Atlantic Water Science Center (SAWSC) in response to the merging of the Georgia, North Carolina, and South Carolina Water Science Centers. This plan proposes a path forward to keep SAWSC science activities relevant to the many diverse needs of stakeholders in the South Atlantic region (Georgia, North Carolina, and South Carolina) and considers the hydrologic setting and issues of the region. This plan advises the creation of five working groups to address five priority science topics for the period 2019–23 and beyond. The five priority science topics are (1) Foundational Data, (2) Effects of Land-Use Change, (3) Coastal Plain Science, (4) Water Availability, and (5) Hazards. From the goals laid forth in this plan for each priority science topic, the working groups plan to devise a set of strategic actions and milestones to be achieved by the SAWSC to provide valuable and relevant data, research, and assessments in the South Atlantic region. In this report, the “South Atlantic region” is used to describe the area encompassed by the States of North Carolina, South Carolina, and Georgia.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr20191068","usgsCitation":"Cuffney, T.F., Garcia, A.M., Horowitz, A.J., LaFontaine, J.H., Landmeyer, J.E., McKee, A.M., McSwain, K.B., Painter, J.A., Shelton, J.M., and Smith, C.A., 2019, South Atlantic Water Science Center strategic science plan—2019–23: U.S. Geological Survey Open-File Report 2019–1068, 31 p., https://doi.org/10.3133/ofr20191068.","productDescription":"v, 31 p.","onlineOnly":"Y","ipdsId":"IP-090584","costCenters":[{"id":13634,"text":"South Atlantic Water Science Center","active":true,"usgs":true}],"links":[{"id":365956,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/2019/1068/ofr20191068.pdf","text":"Report","size":"6.11 MB","linkFileType":{"id":1,"text":"pdf"},"description":"OFR 2019-1068"},{"id":365955,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/2019/1068/coverthb.jpg"}],"contact":"<p>Director,&nbsp;<a href=\"https://www.usgs.gov/centers/sa-water\" data-mce-href=\"https://www.usgs.gov/centers/sa-water\">South Atlantic Water Science Center</a><br>U.S. Geological Survey<br>720 Gracern Road<br>Stephenson Center, Suite 129<br>Columbia, SC 29210</p>","tableOfContents":"<ul><li>Executive Summary</li><li>Mission Statement</li><li>Introduction</li><li>Core Strengths</li><li>Setting</li><li>Vision for Science</li><li>Priority Science Topics and Associated Science Goals</li><li>References Cited</li><li>Appendix 1. Recommended Strategic Actions and Milestones</li><li>References Cited</li></ul>","publishingServiceCenter":{"id":9,"text":"Reston PSC"},"publishedDate":"2019-07-30","noUsgsAuthors":false,"publicationDate":"2019-07-30","publicationStatus":"PW","contributors":{"authors":[{"text":"Cuffney, Thomas F. 0000-0003-1164-5560","orcid":"https://orcid.org/0000-0003-1164-5560","contributorId":205649,"corporation":false,"usgs":true,"family":"Cuffney","given":"Thomas","email":"","middleInitial":"F.","affiliations":[{"id":13634,"text":"South Atlantic Water Science Center","active":true,"usgs":true}],"preferred":true,"id":763970,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Garcia, Ana M. 0000-0002-5388-1281 agarcia@usgs.gov","orcid":"https://orcid.org/0000-0002-5388-1281","contributorId":207567,"corporation":false,"usgs":true,"family":"Garcia","given":"Ana","email":"agarcia@usgs.gov","middleInitial":"M.","affiliations":[{"id":13634,"text":"South Atlantic Water Science Center","active":true,"usgs":true},{"id":37778,"text":"WMA - Integrated Modeling and Prediction Division","active":true,"usgs":true}],"preferred":true,"id":763971,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Horowitz, Arthur J. 0000-0002-3296-730X horowitz@usgs.gov","orcid":"https://orcid.org/0000-0002-3296-730X","contributorId":1400,"corporation":false,"usgs":true,"family":"Horowitz","given":"Arthur","email":"horowitz@usgs.gov","middleInitial":"J.","affiliations":[{"id":316,"text":"Georgia Water Science Center","active":true,"usgs":true},{"id":13634,"text":"South Atlantic Water Science Center","active":true,"usgs":true}],"preferred":true,"id":763972,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"LaFontaine, Jacob H. 0000-0003-4923-2630 jlafonta@usgs.gov","orcid":"https://orcid.org/0000-0003-4923-2630","contributorId":2258,"corporation":false,"usgs":true,"family":"LaFontaine","given":"Jacob","email":"jlafonta@usgs.gov","middleInitial":"H.","affiliations":[{"id":13634,"text":"South Atlantic Water Science Center","active":true,"usgs":true},{"id":316,"text":"Georgia Water Science Center","active":true,"usgs":true}],"preferred":true,"id":763969,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Landmeyer, James E. 0000-0002-5640-3816","orcid":"https://orcid.org/0000-0002-5640-3816","contributorId":216137,"corporation":false,"usgs":true,"family":"Landmeyer","given":"James","email":"","middleInitial":"E.","affiliations":[{"id":13634,"text":"South Atlantic Water Science Center","active":true,"usgs":true}],"preferred":true,"id":763973,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"McKee, Anna M. 0000-0003-2790-5320 amckee@usgs.gov","orcid":"https://orcid.org/0000-0003-2790-5320","contributorId":166725,"corporation":false,"usgs":true,"family":"McKee","given":"Anna","email":"amckee@usgs.gov","middleInitial":"M.","affiliations":[{"id":13634,"text":"South Atlantic Water Science Center","active":true,"usgs":true}],"preferred":true,"id":763974,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"McSwain, Kristen B. 0000-0001-8869-8324","orcid":"https://orcid.org/0000-0001-8869-8324","contributorId":216138,"corporation":false,"usgs":true,"family":"McSwain","given":"Kristen","email":"","middleInitial":"B.","affiliations":[{"id":13634,"text":"South Atlantic Water Science Center","active":true,"usgs":true}],"preferred":true,"id":763975,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Painter, Jaime A. 0000-0001-8883-9158 jpainter@usgs.gov","orcid":"https://orcid.org/0000-0001-8883-9158","contributorId":1466,"corporation":false,"usgs":true,"family":"Painter","given":"Jaime","email":"jpainter@usgs.gov","middleInitial":"A.","affiliations":[{"id":13634,"text":"South Atlantic Water Science Center","active":true,"usgs":true},{"id":316,"text":"Georgia Water Science Center","active":true,"usgs":true}],"preferred":true,"id":763976,"contributorType":{"id":1,"text":"Authors"},"rank":8},{"text":"Shelton, John M. 0000-0002-4787-9572 jmshelto@usgs.gov","orcid":"https://orcid.org/0000-0002-4787-9572","contributorId":1751,"corporation":false,"usgs":true,"family":"Shelton","given":"John","email":"jmshelto@usgs.gov","middleInitial":"M.","affiliations":[{"id":13634,"text":"South Atlantic Water Science Center","active":true,"usgs":true}],"preferred":true,"id":767152,"contributorType":{"id":1,"text":"Authors"},"rank":9},{"text":"Smith, Christopher A. 0000-0001-5069-5232","orcid":"https://orcid.org/0000-0001-5069-5232","contributorId":216139,"corporation":false,"usgs":true,"family":"Smith","given":"Christopher","email":"","middleInitial":"A.","affiliations":[{"id":13634,"text":"South Atlantic Water Science Center","active":true,"usgs":true}],"preferred":true,"id":763978,"contributorType":{"id":1,"text":"Authors"},"rank":10}]}}
,{"id":70204624,"text":"70204624 - 2019 - Uncertainty of reference pixel soil moisture averages sampled at SMAP core validation sites","interactions":[],"lastModifiedDate":"2019-08-07T09:41:38","indexId":"70204624","displayToPublicDate":"2019-07-29T09:40:15","publicationYear":"2019","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2344,"text":"Journal of Hydrometeorology","active":true,"publicationSubtype":{"id":10}},"title":"Uncertainty of reference pixel soil moisture averages sampled at SMAP core validation sites","docAbstract":"Despite extensive efforts to maximize ground coverage and improve upscaling functions within core validation sites (CVS) of the NASA Soil Moisture Active/Passive (SMAP) mission, spatial averages of point-scale soil moisture observations often fail to accurately capture the true average of the reference pixels. Therefore, some level of pixel-scale sampling error from in situ observations must be considered during the validation of SMAP soil moisture retrievals. Here, uncertainties in the SMAP core site average soil moisture (CSASM) due to spatial sampling errors are examined and their impact on CSASM-based SMAP calibration and validation metrics is discussed. The estimated uncertainty (due to spatial sampling limitations) of mean CSASM over time is found to be large, translating into relatively large sampling uncertainty levels for SMAP retrieval bias when calculated against CSASM. As a result, CSASM-based SMAP bias estimates are statistically insignificant at nearly all SMAP CVS. In addition, observations from temporary networks suggest that these (already large) bias uncertainties may be underestimated due to under-sampled spatial variability. The unbiased root-mean-square error (ubRMSE) of CSASM is estimated via two approaches: classical sampling theory and triple collocation, both of which suggest that CSASM ubRMSE is generally within the range 0.01 to 0.02 m3/m3. Although limitations in both methods likely lead to underestimation of ubRMSE, the results suggest that CSASM captures the temporal dynamics of the footprint-scale soil moisture relatively well and is thus a reliable reference for SMAP ubRMSE calculations. Therefore, spatial sampling errors are revealed to have very different impacts on efforts to estimate SMAP bias and ubRMSE metrics using CVS data.","language":"English","publisher":"American Meteorological Soceity","doi":"10.1175/JHM-D-19-0049.1","usgsCitation":"Chen, F., Crow, W., Cosh, M., Colliander, A., Asanuma, J., Berg, A., Bosch, D., Caldwell, T., Holifield-Collins, C., Martinez-Fernandez, J., McNairn, H., Starks, P., Su, Z., and Walker, J., 2019, Uncertainty of reference pixel soil moisture averages sampled at SMAP core validation sites: Journal of Hydrometeorology, v. 20, no. 8, p. 1553-1569, https://doi.org/10.1175/JHM-D-19-0049.1.","productDescription":"17 p.","startPage":"1553","endPage":"1569","ipdsId":"IP-109001","costCenters":[{"id":465,"text":"Nevada Water Science Center","active":true,"usgs":true}],"links":[{"id":467413,"rank":0,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1175/jhm-d-19-0049.1","text":"Publisher Index Page"},{"id":366327,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"20","issue":"8","publishingServiceCenter":{"id":1,"text":"Sacramento PSC"},"noUsgsAuthors":false,"publicationDate":"2019-07-29","publicationStatus":"PW","contributors":{"authors":[{"text":"Chen, Fan","contributorId":217917,"corporation":false,"usgs":false,"family":"Chen","given":"Fan","email":"","affiliations":[{"id":39715,"text":"SSAI/Hydrology and Remote Sensing Laboratory, Agricultural Research Service, USDA, Beltsville, MD","active":true,"usgs":false}],"preferred":false,"id":767813,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Crow, W.T","contributorId":217918,"corporation":false,"usgs":false,"family":"Crow","given":"W.T","email":"","affiliations":[{"id":39716,"text":"Hydrology and Remote Sensing Laboratory, Agricultural Research Service, USDA, Beltsville, MD","active":true,"usgs":false}],"preferred":false,"id":767814,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Cosh, M.H.","contributorId":217919,"corporation":false,"usgs":false,"family":"Cosh","given":"M.H.","email":"","affiliations":[{"id":39717,"text":"SSAI/Hydrology and Remote Sensing Laboratory, Agricultural Research Service, USDA, Beltsville, MD.","active":true,"usgs":false}],"preferred":false,"id":767815,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Colliander, A.","contributorId":217920,"corporation":false,"usgs":false,"family":"Colliander","given":"A.","email":"","affiliations":[{"id":18954,"text":"Jet Propulsion Laboratory, California Institute of Technology, Pasadena, CA","active":true,"usgs":false}],"preferred":false,"id":767816,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Asanuma, J.","contributorId":217921,"corporation":false,"usgs":false,"family":"Asanuma","given":"J.","email":"","affiliations":[{"id":39718,"text":"University of Tsukuba, Tsukuba, Japan","active":true,"usgs":false}],"preferred":false,"id":767817,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Berg, A.","contributorId":217922,"corporation":false,"usgs":false,"family":"Berg","given":"A.","email":"","affiliations":[{"id":39719,"text":"Department of Geography, Environment and Geomatics, University of Guelph, Canada","active":true,"usgs":false}],"preferred":false,"id":767818,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Bosch, D.D.","contributorId":217923,"corporation":false,"usgs":false,"family":"Bosch","given":"D.D.","email":"","affiliations":[{"id":39720,"text":"Southeast Watershed Research Lab, Agricultural Research Service, USDA, Tifton, 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J.","contributorId":217926,"corporation":false,"usgs":false,"family":"Martinez-Fernandez","given":"J.","email":"","affiliations":[{"id":39722,"text":"University of Salamanca, Villamayor, Spain","active":true,"usgs":false}],"preferred":false,"id":767822,"contributorType":{"id":1,"text":"Authors"},"rank":10},{"text":"McNairn, H.","contributorId":217927,"corporation":false,"usgs":false,"family":"McNairn","given":"H.","email":"","affiliations":[{"id":39723,"text":"Agriculture and Agri-Food Canada, Ottawa, Ontario, Canada","active":true,"usgs":false}],"preferred":false,"id":767823,"contributorType":{"id":1,"text":"Authors"},"rank":11},{"text":"Starks, P.J.","contributorId":217928,"corporation":false,"usgs":false,"family":"Starks","given":"P.J.","email":"","affiliations":[{"id":39724,"text":"Grazinglands Research Laboratory, Agricultural Research Service, USDA, El Reno, 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,{"id":70205961,"text":"70205961 - 2019 - Evaluation of stream and wetlands restoration using UAS-based thermal infrared mapping","interactions":[],"lastModifiedDate":"2021-04-27T16:13:54.55326","indexId":"70205961","displayToPublicDate":"2019-07-29T06:51:18","publicationYear":"2019","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3709,"text":"Water","active":true,"publicationSubtype":{"id":10}},"title":"Evaluation of stream and wetlands restoration using UAS-based thermal infrared mapping","docAbstract":"Large-scale wetland restoration often focuses on repairing the hydrologic connections degraded by anthropogenic modifications. Of these hydrologic connections, groundwater discharge is an important target, as these surface water ecosystem control points are important to thermal stability, among other ecosystem services. However, evaluating the effectiveness of the restoration activities on establishing groundwater discharge connection is often difficult over the vast area and often challenging or inaccessible terrain of wetlands.  Unoccupied aerial systems (UAS) are now routinely used for collecting aerial imagery and creating digital surface models (DSM).  Lightweight thermal infrared (TIR) sensors provide another payload option for generation of sub-meter resolution aerial TIR orthophotos. This technology allows for the rapid and safe survey of groundwater discharge areas. Aerial TIR water-surface data were collected March 2019 at Tidmarsh Farms, a former commercial cranberry peatland located in coastal Massachusetts, USA (41°54'17.6\"N 70°34'17.4\"W), where stream and wetland restoration actions were completed in 2016. Here we present a 0.4 km2 georeferenced, temperature calibrated TIR orthophoto of the area. The image represents a mosaic of nearly 900 TIR images captured by UAS in a single morning with a total flight time of 36 minutes, and is supported by a DSM derived from UAS visible imagery. The survey was conducted in winter to maximize temperature contrast between relatively warm groundwater and colder ambient surface environment; lower-density groundwater rises above cool surface waters and thus can be imaged by a UAS.  The resulting TIR orthomosaic shows fine detail of seepage distribution and downstream influence along the several restored channel forms, which was an objective of the ecological restoration design. The restored stream channel has increased connectivity to peatland groundwater discharge, reducing the ecosystem thermal stressors.  Such aerial techniques can be used to guide ecological restoration design and assess post-restoration outcomes, especially in settings where ecosystem structure and function is governed by groundwater and surface water interaction.","language":"English","publisher":"MDPI","doi":"10.3390/w11081568","usgsCitation":"Harvey, M., Hare, D., Hackman, A., Davenport, G., Haynes, A., Helton, A., Lane, J.W., and Briggs, M., 2019, Evaluation of stream and wetlands restoration using UAS-based thermal infrared mapping: Water, v. 11, no. 8, 1568, 13 p., https://doi.org/10.3390/w11081568.","productDescription":"1568, 13 p.","ipdsId":"IP-109877","costCenters":[{"id":37277,"text":"WMA - Earth System Processes Division","active":true,"usgs":true}],"links":[{"id":467416,"rank":0,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.3390/w11081568","text":"Publisher Index Page"},{"id":368290,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"11","issue":"8","publishingServiceCenter":{"id":14,"text":"Menlo Park PSC"},"noUsgsAuthors":false,"publicationDate":"2019-07-29","publicationStatus":"PW","contributors":{"authors":[{"text":"Harvey, Mark","contributorId":190941,"corporation":false,"usgs":false,"family":"Harvey","given":"Mark","email":"","affiliations":[],"preferred":false,"id":773064,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hare, Danielle K.","contributorId":219738,"corporation":false,"usgs":false,"family":"Hare","given":"Danielle","middleInitial":"K.","affiliations":[{"id":36710,"text":"University of Connecticut","active":true,"usgs":false}],"preferred":false,"id":773065,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Hackman, Alex","contributorId":219739,"corporation":false,"usgs":false,"family":"Hackman","given":"Alex","email":"","affiliations":[{"id":40057,"text":"Massachusetts DER","active":true,"usgs":false}],"preferred":false,"id":773066,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Davenport, Glorianna","contributorId":219740,"corporation":false,"usgs":false,"family":"Davenport","given":"Glorianna","email":"","affiliations":[{"id":40058,"text":"The Living Observatory","active":true,"usgs":false}],"preferred":false,"id":773067,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Haynes, Adam","contributorId":216657,"corporation":false,"usgs":false,"family":"Haynes","given":"Adam","affiliations":[{"id":36710,"text":"University of Connecticut","active":true,"usgs":false}],"preferred":false,"id":773068,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Helton, Ashley","contributorId":219741,"corporation":false,"usgs":false,"family":"Helton","given":"Ashley","affiliations":[{"id":36710,"text":"University of Connecticut","active":true,"usgs":false}],"preferred":false,"id":773069,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Lane, John W. 0000-0002-3558-243X","orcid":"https://orcid.org/0000-0002-3558-243X","contributorId":219742,"corporation":false,"usgs":true,"family":"Lane","given":"John","email":"","middleInitial":"W.","affiliations":[{"id":37277,"text":"WMA - Earth System Processes Division","active":true,"usgs":true}],"preferred":true,"id":773070,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Briggs, Martin 0000-0003-3206-4132","orcid":"https://orcid.org/0000-0003-3206-4132","contributorId":219737,"corporation":false,"usgs":true,"family":"Briggs","given":"Martin","affiliations":[{"id":37277,"text":"WMA - Earth System Processes Division","active":true,"usgs":true}],"preferred":true,"id":773063,"contributorType":{"id":1,"text":"Authors"},"rank":8}]}}
,{"id":70203633,"text":"70203633 - 2019 - Enabling real-time user interaction for decision support: Experiences extending a local agave platform metadata service","interactions":[],"lastModifiedDate":"2019-12-02T13:34:30","indexId":"70203633","displayToPublicDate":"2019-07-28T15:42:09","publicationYear":"2019","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"displayTitle":"Enabling Real-Time User Interaction For Decision Support: Experiences Extending A Local Agave Platform Metadata Service","title":"Enabling real-time user interaction for decision support: Experiences extending a local agave platform metadata service","docAbstract":"<p><span>The University of Hawai'i Information Technology Services Cyber-infrastructure team in partnership with the United States Geological Survey developed the Hawai'i groundwater recharge tool, a decision support tool, as part of the 'Ike Wai Gateway to support water sustainability research for the state of Hawai'i. To enable the development of the tool within the existing University of Hawai'i Agave platform that the 'Ike Wai Gateway is built on, the Metadata application programmatic interface (API) and Agave infrastructure needed to be extended to store and retrieve spatial data and handle a larger number of requests. The development team successfully added the functionality to the local University of Hawai'i Agave platform instance to support the storage of deserialized vector data and metadata that can be spatially queried across hundreds of thousands of records to enable decision support applications within a science gateway.</span></p>","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Proceeding PEARC '19: Proceedings of the Practice and Experience in Advanced Research Computing on Rise of the Machines (learning)","largerWorkSubtype":{"id":12,"text":"Conference publication"},"conferenceTitle":"Rise of the Machines (Learning): Practice and Experience in Advanced Research Computing","conferenceDate":"July 28-August 1, 2019","conferenceLocation":"Chicago, IL","language":"English","publisher":"Association for Computing Machinery","doi":"10.1145/3332186.3332252","usgsCitation":"Cleveland, S.B., McClean, J.H., Rotzoll, K., Izuka, S.K., and Jacobs, G.A., 2019, Enabling real-time user interaction for decision support: Experiences extending a local agave platform metadata service, <i>in</i> Proceeding PEARC '19: Proceedings of the Practice and Experience in Advanced Research Computing on Rise of the Machines (learning), v. 19, Chicago, IL, July 28-August 1, 2019, 8, 5 p., https://doi.org/10.1145/3332186.3332252.","productDescription":"8, 5 p.","ipdsId":"IP-107140","costCenters":[{"id":525,"text":"Pacific Islands Water Science Center","active":true,"usgs":true}],"links":[{"id":467417,"rank":0,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1145/3332186.3332252","text":"Publisher Index Page"},{"id":367616,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Hawaii","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -156.7529296875,\n              18.57336188365185\n            ],\n            [\n              -154.3798828125,\n              18.57336188365185\n            ],\n            [\n              -154.3798828125,\n              20.427012814257385\n            ],\n            [\n              -156.7529296875,\n              20.427012814257385\n            ],\n            [\n              -156.7529296875,\n              18.57336188365185\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"19","publishingServiceCenter":{"id":14,"text":"Menlo Park PSC"},"noUsgsAuthors":false,"publicationDate":"2019-07-28","publicationStatus":"PW","contributors":{"authors":[{"text":"Cleveland, Sean B.","contributorId":215893,"corporation":false,"usgs":false,"family":"Cleveland","given":"Sean","email":"","middleInitial":"B.","affiliations":[{"id":36402,"text":"University of Hawaii","active":true,"usgs":false}],"preferred":false,"id":763341,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"McClean, Jared H.","contributorId":215894,"corporation":false,"usgs":false,"family":"McClean","given":"Jared","email":"","middleInitial":"H.","affiliations":[{"id":37291,"text":"University of Hawaii at Hilo","active":true,"usgs":false}],"preferred":false,"id":763342,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Rotzoll, Kolja 0000-0002-5910-888X","orcid":"https://orcid.org/0000-0002-5910-888X","contributorId":201087,"corporation":false,"usgs":false,"family":"Rotzoll","given":"Kolja","affiliations":[],"preferred":false,"id":763343,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Izuka, Scot K. 0000-0002-8758-9414 skizuka@usgs.gov","orcid":"https://orcid.org/0000-0002-8758-9414","contributorId":2645,"corporation":false,"usgs":true,"family":"Izuka","given":"Scot","email":"skizuka@usgs.gov","middleInitial":"K.","affiliations":[{"id":525,"text":"Pacific Islands Water Science Center","active":true,"usgs":true}],"preferred":true,"id":763340,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Jacobs, Gwen A.","contributorId":215071,"corporation":false,"usgs":false,"family":"Jacobs","given":"Gwen","email":"","middleInitial":"A.","affiliations":[{"id":36402,"text":"University of Hawaii","active":true,"usgs":false}],"preferred":false,"id":763344,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":70206989,"text":"70206989 - 2019 - Permeability variation and anisotropy of gas hydrate-bearing pressure-core sediments recovered from the Krishna–Godavari Basin, offshore India","interactions":[],"lastModifiedDate":"2019-12-03T07:12:01","indexId":"70206989","displayToPublicDate":"2019-07-26T15:21:42","publicationYear":"2019","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2682,"text":"Marine and Petroleum Geology","active":true,"publicationSubtype":{"id":10}},"title":"Permeability variation and anisotropy of gas hydrate-bearing pressure-core sediments recovered from the Krishna–Godavari Basin, offshore India","docAbstract":"Permeability measurements were conducted on gas hydrate-bearing pressure-core sediments recovered from the Krishna-Godavari Basin during India's National Gas Hydrate Program Expedition 02. Pressure cores collected in the deep seabed of the Indian Ocean were cut and stored under high pressure and low temperature on the D/V Chikyu using pressure core analyzing tools. A total of 25 1.2-m storage chambers were transferred to Japan from India for pressure core studies using pressure-core analysis tools at the National Institute of Advanced Industrial Science and Technology. The sediment core's pressure and temperature were maintained within the hydrate stability conditions during the entire process of transfer and loading into a triaxial testing apparatus called TACTT, which can simulate the in-situ stress state under triaxial conditions. The hydrate saturation of the samples was in the range of 50¬90%. It was found that the initial effective water permeability was in range of 0.01 mD to tens of mD, depending on the hydrate saturation and the mean particle size of the host sediment. The hydrate pore space morphology is also a critical factor, and results suggest hydrates are forming in the pore centers, but also as a sediment grain coating. In a first for gas hydrate-bearing pressure cores, the permeability anisotropy was established via vertical and horizontal flow tests combined with a pore fluid flow simulation. The horizontal/vertical permeability ratio was found to be 4. Additionally, the effective stress dependency of permeability was investigated by performing flow tests at different effective stresses. Due to decreasing porosity and particle crushing, the permeability dropped by approximately 90% for an effective stress increase of 10 MPa.","language":"English","publisher":"Elsevier","doi":"10.1016/j.marpetgeo.2018.07.006","usgsCitation":"Yoneda, J., Oshima, M., Kida, M., Kato, A., Konno, Y., Jin, Y., Jang, J., Waite, W., Kumar, P., and Tenma, N., 2019, Permeability variation and anisotropy of gas hydrate-bearing pressure-core sediments recovered from the Krishna–Godavari Basin, offshore India: Marine and Petroleum Geology, v. 108, p. 254-536, https://doi.org/10.1016/j.marpetgeo.2018.07.006.","productDescription":"13 p.","startPage":"254","endPage":"536","ipdsId":"IP-096275","costCenters":[{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"links":[{"id":467419,"rank":0,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1016/j.marpetgeo.2018.07.006","text":"Publisher Index 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Panvel, Navi Mumbai, India","active":true,"usgs":false}],"preferred":false,"id":776482,"contributorType":{"id":1,"text":"Authors"},"rank":9},{"text":"Tenma, Norio","contributorId":220803,"corporation":false,"usgs":false,"family":"Tenma","given":"Norio","email":"","affiliations":[{"id":40273,"text":"National Institute of Advanced Industrial Science and Technology","active":true,"usgs":false}],"preferred":false,"id":776483,"contributorType":{"id":1,"text":"Authors"},"rank":10}]}}
,{"id":70205197,"text":"70205197 - 2019 - Estimating offsets for avian displacement effects of anthropogenic impacts","interactions":[],"lastModifiedDate":"2019-12-03T09:45:19","indexId":"70205197","displayToPublicDate":"2019-07-26T15:21:26","publicationYear":"2019","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1450,"text":"Ecological Applications","active":true,"publicationSubtype":{"id":10}},"title":"Estimating offsets for avian displacement effects of anthropogenic impacts","docAbstract":"Biodiversity offsetting, or compensatory mitigation, is increasingly being used in temperate grassland ecosystems to compensate for unavoidable environmental damage from anthropogenic developments such as transportation infrastructure, urbanization, and energy development. Pursuit of energy independence in the United States will expand domestic energy production.  Concurrent with this increased growth is increased disruption to wildlife habitats, including avian displacement from suitable breeding habitat.  Recent studies at energy-extraction and -generation facilities have provided evidence for behavioral avoidance and thus reduced use of habitat by breeding waterfowl and grassland birds in the vicinity of energy infrastructure.  To quantify and compensate for this loss in value of avian breeding habitat, it is necessary to determine a biologically-based currency so that the sufficiency of offsets in terms of biological equivalent value can be obtained.  We describe a method for quantifying the amount of habitat needed to provide equivalent biological value for avifauna displaced by energy and transportation infrastructure, based on the ability to define five metrics: impact distance, impact area, pre-impact density, percent displacement, and offset density.  We calculate percent displacement values for breeding waterfowl and grassland birds and demonstrate the applicability of our avian-impact offset method using examples for wind and oil infrastructure.  We also apply our method to an example in which the biological value of the offset habitat is similar to the impacted habitat, based on similarity in habitat type (e.g., native prairie), geographical location, land use, and landscape composition, as well as to an example in which the biological value of the offset habitat is dissimilar to the impacted habitat.  We provide a worksheet that informs potential users how to apply our method to their specific developments and a framework for developing decision-support tools aimed at achieving landscape-level conservation goals.","language":"English","publisher":"Wiley","doi":"10.1002/eap.1983","usgsCitation":"Shaffer, J.A., Loesch, C.R., and Buhl, D.A., 2019, Estimating offsets for avian displacement effects of anthropogenic impacts: Ecological Applications, v. 29, no. 8, e01983, 15 p., https://doi.org/10.1002/eap.1983.","productDescription":"e01983, 15 p.","ipdsId":"IP-101351","costCenters":[{"id":480,"text":"Northern Prairie Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":467420,"rank":0,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1002/eap.1983","text":"Publisher Index Page"},{"id":367231,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"29","issue":"8","publishingServiceCenter":{"id":4,"text":"Rolla PSC"},"noUsgsAuthors":false,"publicationDate":"2019-08-30","publicationStatus":"PW","contributors":{"authors":[{"text":"Shaffer, Jill A. 0000-0003-3172-0708 jshaffer@usgs.gov","orcid":"https://orcid.org/0000-0003-3172-0708","contributorId":3184,"corporation":false,"usgs":true,"family":"Shaffer","given":"Jill","email":"jshaffer@usgs.gov","middleInitial":"A.","affiliations":[{"id":480,"text":"Northern Prairie Wildlife Research Center","active":true,"usgs":true}],"preferred":true,"id":770322,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Loesch, Charles R. 0000-0003-3090-1566","orcid":"https://orcid.org/0000-0003-3090-1566","contributorId":213437,"corporation":false,"usgs":false,"family":"Loesch","given":"Charles","email":"","middleInitial":"R.","affiliations":[{"id":36188,"text":"U.S. Fish and Wildlife Service","active":true,"usgs":false}],"preferred":false,"id":770323,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Buhl, Deborah A. 0000-0002-8563-5990 dbuhl@usgs.gov","orcid":"https://orcid.org/0000-0002-8563-5990","contributorId":146226,"corporation":false,"usgs":true,"family":"Buhl","given":"Deborah","email":"dbuhl@usgs.gov","middleInitial":"A.","affiliations":[{"id":480,"text":"Northern Prairie Wildlife Research Center","active":true,"usgs":true}],"preferred":true,"id":770324,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70203598,"text":"pp1842A - 2019 - The effects of management practices on grassland birds — An introduction to North American grasslands and the practices used to manage grasslands and grassland birds","interactions":[{"subject":{"id":70203598,"text":"pp1842A - 2019 - The effects of management practices on grassland birds — An introduction to North American grasslands and the practices used to manage grasslands and grassland birds","indexId":"pp1842A","publicationYear":"2019","noYear":false,"chapter":"A","displayTitle":"The Effects of Management Practices on Grassland Birds—An Introduction to North American Grasslands and the Practices Used to Manage Grasslands and Grassland Birds","title":"The effects of management practices on grassland birds — An introduction to North American grasslands and the practices used to manage grasslands and grassland birds"},"predicate":"IS_PART_OF","object":{"id":70203022,"text":"pp1842 - 2019 - The effects of management practices on grassland birds","indexId":"pp1842","publicationYear":"2019","noYear":false,"title":"The effects of management practices on grassland birds"},"id":1}],"isPartOf":{"id":70203022,"text":"pp1842 - 2019 - The effects of management practices on grassland birds","indexId":"pp1842","publicationYear":"2019","noYear":false,"title":"The effects of management practices on grassland birds"},"lastModifiedDate":"2023-12-20T21:00:48.691686","indexId":"pp1842A","displayToPublicDate":"2019-07-26T15:03:05","publicationYear":"2019","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":331,"text":"Professional Paper","code":"PP","onlineIssn":"2330-7102","printIssn":"1044-9612","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"1842","chapter":"A","displayTitle":"The Effects of Management Practices on Grassland Birds—An Introduction to North American Grasslands and the Practices Used to Manage Grasslands and Grassland Birds","title":"The effects of management practices on grassland birds — An introduction to North American grasslands and the practices used to manage grasslands and grassland birds","docAbstract":"<p>The Great Plains of North America is defined as the land mass that encompasses the entire central portion of the North American continent that, at the time of European settlement, was an unbroken expanse of primarily herbaceous vegetation. The Great Plains extend from central Saskatchewan and Alberta to central Mexico and from Indiana to the Rocky Mountains. The expanses of herbaceous vegetation are often referred to as native prairie or native grasslands. Native grasslands share the characteristics of a general uniformity in vegetation structure, dominance by grasses and forbs, a near absence of trees and shrubs, annual precipitation ranging from 25 to 100 centimeters, extreme intra-annual fluctuations in temperature and precipitation, and a flat to rolling topography over which fires can spread. To the west of the Great Plains lie the sagebrush communities of the Great Basin, which extend from British Columbia and Saskatchewan to northern Arizona and New Mexico and from the eastern slopes of the Sierra Nevada and Cascade mountain ranges to western South Dakota. Sagebrush communities share similar characteristics to native grasslands, but their location east of the Rocky Mountains creates a more moderating influence from prevailing westerly winds that affect timing of peak precipitation and growth form of dominant vegetation. Native grasslands and sagebrush communities harbor a diverse array of grassland, wetland, and woodland plant and animal communities that are uniquely adapted to the natural forces of the Great Plains and Great Basin, namely the interactive forces of climate, fire, and grazing. The arrival of European settlers to North America brought profound change to native grassland and sagebrush communities, including the establishment of permanent towns and cities, the proliferation of cropland-based agricultural systems, and the suppression of wildfires. The near extirpation of bison by the 1860s paved the way for dramatic changes in the dominant grazers and a shift in the disturbance patterns that historically influenced vegetation structure. The greatest threat to native grasslands and sagebrush communities in modern times is their loss due to conversion to rowcrop agriculture and to urbanization. Concomitant with habitat loss is a precipitous decline in populations of bird species that evolved with, and are uniquely adapted to, the native grassland and sagebrush habitats. Avian population trends are linked strongly to agricultural land use. Besides outright loss of suitable breeding habitat, agricultural practices affect birds through factors such as pesticide exposure, habitat fragmentation, shifts in predator community composition, and occurrence of brood parasites. Bird populations face other stressors, such as loss of habitat to and behavioral avoidance of urbanized areas, roads, and infrastructure associated with energy production.</p><p>Despite the many anthropogenic changes to North American grassland and sagebrush communities, some bird species are adaptable and opportunistic in their habitat selection and now utilize one or more human-created habitats. Human-created habitats include pastures, hayfields, agricultural terraces, crop buffer strips, field borders, grassed waterways, fencerows, road rights-of-way, airports, reclaimed coal mines, and planted wildlife cover. Fields of seeded grasslands enrolled in Federal long-term set-aside programs, such as the Conservation Reserve Program in the United States and the Permanent Cover Program in Canada, provide important nesting habitat for grassland bird species. The array of habitats used by birds makes habitat and avian management a complex undertaking, and the scale (for example, local, regional, international) at which management actions can be implemented are such that a universal approach to managing grasslands for the conservation of the entire suite of bird species does not exist. Experienced land managers recognize that it is impossible to manage for all bird species simultaneously, and thus, prioritization is necessary towards those habitats or bird species that the manager or management agency ranks highest for a specific region or management unit. The primary tools available for management are burning, grazing, mowing, herbicide application, and idling, but before choosing a particular practice, a manager will want to consider issues of seasonality, intensity, and frequency.</p><p>Despite the thousands of studies that are cited in this compendium, much remains unknown about the effects of management practices on bird species. The series of species accounts in this compendium review the current state of knowledge regarding management of grassland and sagebrush bird species and summarize information on the effects of management practices on individual species. The accounts do not give definitive statements on the effects of management practices for any particular species, primarily because there are very few replicated studies in which identical management practices have been applied in the same geographical area with consistent results, which are elements necessary to provide concrete recommendations for the management of a particular species in a particular area. Documentation of the effects of management treatments on individual species through statistically sound methods that incorporate multiple years and locations will further scientists’ and land managers’ knowledge far more than 1–2-year studies that are limited in scope as well as time, but studies of that scope and breadth are rare.</p>","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"The effects of management practices on grassland birds (Professional Paper 1842)","largerWorkSubtype":{"id":5,"text":"USGS Numbered Series"},"language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/pp1842A","usgsCitation":"Shaffer, J.A., and DeLong, J.P., 2019, The effects of management practices on grassland birds—An introduction to North American grasslands and the practices used to manage grasslands and grassland birds (ver. 1.1, March 2022), chap. A <i>of</i> Johnson, D.H., Igl, L.D., Shaffer, J.A., and DeLong, J.P., eds., The effects of management practices on grassland birds: U.S. Geological Survey Professional Paper 1842, 63 p., https://doi.org/10.3133/pp1842A.","productDescription":"v, 63 p.","numberOfPages":"74","onlineOnly":"Y","additionalOnlineFiles":"Y","ipdsId":"IP-097670","costCenters":[{"id":480,"text":"Northern Prairie Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":397809,"rank":3,"type":{"id":25,"text":"Version History"},"url":"https://pubs.usgs.gov/pp/1842/a/versionhist.txt","size":"1 kB","linkFileType":{"id":2,"text":"txt"}},{"id":365495,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/1842/a/pp1842a.pdf","text":"Report","size":"8.74 MB","linkFileType":{"id":1,"text":"pdf"},"description":"PP 1842 Chapter A"},{"id":365494,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/1842/a/coverthb2.jpg"}],"edition":"Version 1.0: July 26, 2019; Version 1.1: March 31, 2022","contact":"<p>Director, <a href=\"https://www.usgs.gov/centers/npwrc\" data-mce-href=\"https://www.usgs.gov/centers/npwrc\">Northern Prairie Wildlife Research Center</a> <br>U.S. Geological Survey<br>8711 37th Street Southeast <br>Jamestown, ND 58401</p>","tableOfContents":"<ul><li>Acknowledgments</li><li>North American Grassland and Wetland Habitats</li><li>North American Grassland and Wetland Habitats after European Settlement</li><li>North American Sagebrush Habitats Before and After European Settlement</li><li>Grassland Birds</li><li>Maintaining and Managing Grasslands for Grassland Birds</li><li>Final Thoughts</li><li>Summary</li><li>References</li></ul>","publishingServiceCenter":{"id":4,"text":"Rolla PSC"},"publishedDate":"2019-07-26","revisedDate":"2022-03-31","noUsgsAuthors":false,"publicationDate":"2019-07-26","publicationStatus":"PW","contributors":{"authors":[{"text":"Shaffer, Jill A. 0000-0003-3172-0708 jshaffer@usgs.gov","orcid":"https://orcid.org/0000-0003-3172-0708","contributorId":3184,"corporation":false,"usgs":true,"family":"Shaffer","given":"Jill","email":"jshaffer@usgs.gov","middleInitial":"A.","affiliations":[{"id":480,"text":"Northern Prairie Wildlife Research Center","active":true,"usgs":true}],"preferred":true,"id":763281,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"DeLong, John P. 0000-0003-0558-8213","orcid":"https://orcid.org/0000-0003-0558-8213","contributorId":215841,"corporation":false,"usgs":false,"family":"DeLong","given":"John P.","affiliations":[{"id":16610,"text":"University of Nebraska-Lincoln","active":true,"usgs":false}],"preferred":false,"id":763282,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
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2020 - The effects of management practices on grassland birds—Prairie Falcon (<i>Falco mexicanus</i>)","indexId":"pp1842S","publicationYear":"2020","noYear":false,"chapter":"S","displayTitle":"The Effects of Management Practices on Grassland Birds—Prairie Falcon (<i>Falco mexicanus</i>)","title":"The effects of management practices on grassland birds—Prairie Falcon (<i>Falco mexicanus</i>)"},"predicate":"IS_PART_OF","object":{"id":70203022,"text":"pp1842 - 2019 - The effects of management practices on grassland birds","indexId":"pp1842","publicationYear":"2019","noYear":false,"title":"The effects of management practices on grassland birds"},"id":27},{"subject":{"id":70214136,"text":"pp1842KK - 2020 - The effects of management practices on grassland birds—Nelson’s Sparrow (<i>Ammospiza nelsoni nelsoni</i>)","indexId":"pp1842KK","publicationYear":"2020","noYear":false,"chapter":"KK","displayTitle":"The Effects of Management Practices on Grassland Birds—Nelson’s Sparrow (<i>Ammospiza nelsoni nelsoni</i>)","title":"The effects of management practices on grassland birds—Nelson’s Sparrow (<i>Ammospiza nelsoni nelsoni</i>)"},"predicate":"IS_PART_OF","object":{"id":70203022,"text":"pp1842 - 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2022 - The effects of management practices on grassland birds—Burrowing Owl (<i>Athene cunicularia hypugaea</i>)","indexId":"pp1842P","publicationYear":"2022","noYear":false,"chapter":"P","displayTitle":"The Effects of Management Practices on Grassland Birds—Burrowing Owl (<i>Athene cunicularia hypugaea</i>)","title":"The effects of management practices on grassland birds—Burrowing Owl (<i>Athene cunicularia hypugaea</i>)"},"predicate":"IS_PART_OF","object":{"id":70203022,"text":"pp1842 - 2019 - The effects of management practices on grassland birds","indexId":"pp1842","publicationYear":"2019","noYear":false,"title":"The effects of management practices on grassland birds"},"id":34},{"subject":{"id":70239898,"text":"pp1842Z - 2023 - The effects of management practices on grassland birds—Clay-colored Sparrow (<i>Spizella pallida</i>)","indexId":"pp1842Z","publicationYear":"2023","noYear":false,"chapter":"Z","displayTitle":"The Effects of Management Practices on Grassland Birds—Clay-Colored Sparrow (<i>Spizella pallida</i>)","title":"The effects of management practices on grassland birds—Clay-colored Sparrow (<i>Spizella pallida</i>)"},"predicate":"IS_PART_OF","object":{"id":70203022,"text":"pp1842 - 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2019 - The effects of management practices on grassland birds","indexId":"pp1842","publicationYear":"2019","noYear":false,"title":"The effects of management practices on grassland birds"},"id":39},{"subject":{"id":70263193,"text":"pp1842BB - 2025 - The effects of management practices on grassland birds—Field Sparrow (<em>Spizella pusilla</em>)","indexId":"pp1842BB","publicationYear":"2025","noYear":false,"chapter":"BB","displayTitle":"The Effects of Management Practices on Grassland Birds—Field Sparrow (<em>Spizella pusilla</em>)","title":"The effects of management practices on grassland birds—Field Sparrow (<em>Spizella pusilla</em>)"},"predicate":"IS_PART_OF","object":{"id":70203022,"text":"pp1842 - 2019 - The effects of management practices on grassland birds","indexId":"pp1842","publicationYear":"2019","noYear":false,"title":"The effects of management practices on grassland birds"},"id":40}],"lastModifiedDate":"2023-12-20T21:18:53.916204","indexId":"pp1842","displayToPublicDate":"2019-07-26T15:02:05","publicationYear":"2019","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":331,"text":"Professional Paper","code":"PP","onlineIssn":"2330-7102","printIssn":"1044-9612","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"1842","displayTitle":"The Effects of Management Practices on Grassland Birds","title":"The effects of management practices on grassland birds","docAbstract":"<p><span>Since the mid-1960s, populations of grassland birds have been declining more precipitously than any other group of birds in North America. These long-term declines highlight the need to better understand the habitat requirements of grassland birds and how management practices affect individual species and their habitats. Although resource managers have long recognized that every management approach contains inherent advantages and disadvantages, depending on the species in question, they are often faced with making critical management decisions armed with little or no information. The need for information on management and its effects on grassland birds was identified by the U.S. Prairie Pothole Joint Venture, a part of the North American Waterfowl Management Plan, in support of its objective to stabilize or increase populations of declining grassland- and wetland-associated wildlife species in the Prairie Pothole Region. In 1996, scientists from the U.S. Geological Survey’s Northern Prairie Wildlife Research Center began a long-term, collaborative effort to review and synthesize literature on the effects of management practices on grassland bird species. Major funding for this effort was provided by the Prairie Pothole Joint Venture, U.S. Fish and Wildlife Service, and the U.S. Geological Survey; additional funding was provided by the U.S. Forest Service, The Nature Conservancy, and the Plains and Potholes Landscape Conservation Cooperative. This compendium on “The Effects of Management Practices on Grassland Birds” is a culmination of that work. More than 6,000 published and unpublished publications have been consulted and several thousand publications have been incorporated and synthesized in species accounts for 40 North American grassland bird species. The 40 species represent a taxonomically diverse group that includes grouse, shorebirds, owls, diurnal raptors, and many songbirds. The focus of this effort is on management of breeding habitat, with an emphasis on the Great Plains. The accounts provide land managers with a summary of information on the effects of specific management practices on grassland birds and help to identify the most critical research gaps in our understanding of grassland bird ecology, habitat needs, and responses to management practices.</span></p><p><span>This compendium is organized into three primary sections: an introduction, species accounts, and a concluding chapter. The introduction provides an overview of grasslands, the processes under which grasslands formed, the influence of anthropogenic changes to grasslands, the effects of those changes on grassland bird populations, and the management tools available to land managers. The bulk of this compendium is the individual species accounts, covering 40 species of North American grassland birds arranged in taxonomic order. Each species account includes information on species range, suitable breeding habitat, area requirements and landscape associations, breeding-season phenology, species’ response to management, and management recommendations. Information on rates of brood parasitism by the Brown-headed Cowbird (<i>Molothrus ater</i>) in grassland bird nests is summarized in a chapter at the end of this report. The final chapter includes concluding remarks concerning habitat requirements and management effects on grassland birds.</span></p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/pp1842","usgsCitation":"Johnson, D.H., Igl, L.D., Shaffer, J.A., and DeLong, J.P., eds., 2019, The effects of management practices on grassland birds (ver. 1.2, June 2023): U.S. Geological Survey Professional Paper 1842, https://doi.org/10.3133/pp1842.","productDescription":"18 p.","numberOfPages":"18","onlineOnly":"Y","additionalOnlineFiles":"Y","ipdsId":"IP-097134","costCenters":[{"id":480,"text":"Northern Prairie Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":418327,"rank":3,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/1842/coverthb3.jpg"},{"id":365492,"rank":1,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/1842/pp1842.pdf","text":"Front Material","size":"3.04 MB","linkFileType":{"id":1,"text":"pdf"},"description":"PP 1842"},{"id":397800,"rank":2,"type":{"id":25,"text":"Version History"},"url":"https://pubs.usgs.gov/pp/1842/versionhist.txt","text":"Version History","size":"1 kB","linkFileType":{"id":2,"text":"txt"}}],"edition":"Version 1.0: July 26, 2019; Version 1.1: March 31, 2022; Version 1.2: June 21, 2023","contact":"<p>Director, <a data-mce-href=\"https://www.usgs.gov/centers/npwrc\" href=\"https://www.usgs.gov/centers/npwrc\">Northern Prairie Wildlife Research Center</a> <br>U.S. Geological Survey<br>8711 37th Street Southeast <br>Jamestown, ND 58401</p>","tableOfContents":"<ul><li>Foreword</li><li>Preface</li><li>Chapters</li></ul>","publishingServiceCenter":{"id":4,"text":"Rolla PSC"},"publishedDate":"2019-07-26","revisedDate":"2023-06-21","noUsgsAuthors":false,"publicationDate":"2019-07-26","publicationStatus":"PW","contributors":{"editors":[{"text":"Johnson, Douglas H. 0000-0002-7778-6641","orcid":"https://orcid.org/0000-0002-7778-6641","contributorId":214802,"corporation":false,"usgs":true,"family":"Johnson","given":"Douglas H.","affiliations":[{"id":480,"text":"Northern Prairie Wildlife Research Center","active":true,"usgs":true}],"preferred":true,"id":760816,"contributorType":{"id":2,"text":"Editors"},"rank":1},{"text":"Igl, Lawrence D. 0000-0003-0530-7266","orcid":"https://orcid.org/0000-0003-0530-7266","contributorId":214801,"corporation":false,"usgs":true,"family":"Igl","given":"Lawrence D.","affiliations":[{"id":480,"text":"Northern Prairie Wildlife Research Center","active":true,"usgs":true}],"preferred":true,"id":760815,"contributorType":{"id":2,"text":"Editors"},"rank":2},{"text":"Shaffer, Jill A. 0000-0003-3172-0708","orcid":"https://orcid.org/0000-0003-3172-0708","contributorId":214803,"corporation":false,"usgs":true,"family":"Shaffer","given":"Jill A.","affiliations":[{"id":480,"text":"Northern Prairie Wildlife Research Center","active":true,"usgs":true}],"preferred":true,"id":760817,"contributorType":{"id":2,"text":"Editors"},"rank":3},{"text":"DeLong, John P. 0000-0003-0558-8213","orcid":"https://orcid.org/0000-0003-0558-8213","contributorId":149794,"corporation":false,"usgs":false,"family":"DeLong","given":"John","email":"","middleInitial":"P.","affiliations":[{"id":12505,"text":"University of Nebraska - Lincoln","active":true,"usgs":false}],"preferred":false,"id":760818,"contributorType":{"id":2,"text":"Editors"},"rank":4}]}}
,{"id":70206126,"text":"70206126 - 2019 - Invasive silver carp may compete with unionid mussels for algae: First experimental evidence","interactions":[],"lastModifiedDate":"2019-10-24T06:25:58","indexId":"70206126","displayToPublicDate":"2019-07-25T16:35:38","publicationYear":"2019","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":862,"text":"Aquatic Conservation: Marine and Freshwater Ecosystems","active":true,"publicationSubtype":{"id":10}},"title":"Invasive silver carp may compete with unionid mussels for algae: First experimental evidence","docAbstract":"1.\tUnionid mussels are imperiled throughout the United States, where their global diversity is highest.  Silver carp (Hypophthalmichthys molitrix Valenciennes in Cuvier & Valenciennes, 1844), an invasive planktivorous fish, has spread throughout Midwestern rivers and currently threatens the Great Lakes.  Because silver carp remove plankton and other particles from the water column, they may compete with mussels for food resources.  This would be among the first examples of a direct competitive interaction between fish and mussels.\n\n2.\tTo examine the potential for competition, a 30-d tank experiment was performed with 2-yr old fatmucket mussels (Lampsilis siliquoidea Barnes, 1823) and age-1 silver carp in three treatments: fatmucket only, silver carp only, and fatmucket + silver carp.  All tanks were given a commercial algal-based diet daily and dry mass of suspended particles (an estimate of available food) and NH4, NO3, and NO2 concentrations were quantified every 5 d to track food availability and changes in nutrients.  Initial and final silver carp total length (mm) and mass (g), and fatmucket length (mm), height (mm), and surface area (mm2) were measured. \n \n3.\tSurvival was 100% over the test duration for both species.  Fatmucket grew less in the fatmucket + silver carp treatment, while silver carp growth was low regardless of treatment.  Fatmucket also exhibited increased movement in the presence of silver carp.  Suspended particles did not differ among treatments.  Dissolved nitrogen concentrations were higher in the silver carp treatments, suggesting that silver carp increase nutrient availability in aquatic systems.\n\n4.\tOverall, the slower growth rates observed in the fatmucket + silver carp treatment compared to the mussel only treatment suggest exploitative competition between invasive planktivorous silver carp and fatmucket and this competition could contribute to additional stress on already imperiled mussels.","language":"English","publisher":"Wiley","doi":"10.1002/aqc.3185","usgsCitation":"Tristano, E.P., Coulter, A.A., Newton, T., and Garvey, J.#., 2019, Invasive silver carp may compete with unionid mussels for algae: First experimental evidence: Aquatic Conservation: Marine and Freshwater Ecosystems, v. 29, no. 10, p. 1749-1757, https://doi.org/10.1002/aqc.3185.","productDescription":"9 p.","startPage":"1749","endPage":"1757","ipdsId":"IP-093782","costCenters":[{"id":606,"text":"Upper Midwest Environmental Sciences Center","active":true,"usgs":true}],"links":[{"id":368539,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","otherGeospatial":"Midwest","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -104.1064453125,\n              48.8936153614802\n            ],\n            [\n              -104.3701171875,\n              40.91351257612758\n            ],\n            [\n              -102.74414062499999,\n              40.713955826286046\n            ],\n            [\n              -101.953125,\n              39.53793974517628\n            ],\n            [\n              -98.4375,\n              38.89103282648846\n            ],\n            [\n              -96.416015625,\n              39.16414104768742\n  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PSC"},"noUsgsAuthors":false,"publicationDate":"2019-07-25","publicationStatus":"PW","contributors":{"authors":[{"text":"Tristano, Elizabeth P","contributorId":219966,"corporation":false,"usgs":false,"family":"Tristano","given":"Elizabeth","email":"","middleInitial":"P","affiliations":[{"id":13212,"text":"Southern Illinois University","active":true,"usgs":false}],"preferred":false,"id":773673,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Coulter, Alison A.","contributorId":187652,"corporation":false,"usgs":false,"family":"Coulter","given":"Alison","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":773674,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Newton, Teresa 0000-0001-9351-5852 tnewton@usgs.gov","orcid":"https://orcid.org/0000-0001-9351-5852","contributorId":150098,"corporation":false,"usgs":true,"family":"Newton","given":"Teresa","email":"tnewton@usgs.gov","affiliations":[{"id":606,"text":"Upper Midwest Environmental Sciences Center","active":true,"usgs":true}],"preferred":true,"id":773672,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Garvey, James #","contributorId":219967,"corporation":false,"usgs":false,"family":"Garvey","given":"James","email":"","middleInitial":"#","affiliations":[{"id":13212,"text":"Southern Illinois University","active":true,"usgs":false}],"preferred":false,"id":773675,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70205196,"text":"70205196 - 2019 - Wetland management strategy to reduce mercury export in water and bioaccumulation in fish","interactions":[],"lastModifiedDate":"2019-10-09T09:57:15","indexId":"70205196","displayToPublicDate":"2019-07-25T15:27:08","publicationYear":"2019","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1571,"text":"Environmental Toxicology and Chemistry","active":true,"publicationSubtype":{"id":10}},"title":"Wetland management strategy to reduce mercury export in water and bioaccumulation in fish","docAbstract":"<p>Wetland environments provide numerous ecosystem services but also facilitate methylmercury (MeHg) production and bioaccumulation. We developed a wetland‐management technique to reduce MeHg concentrations in wetland fish and water. We physically modified seasonal wetlands by constructing open‐ and deep‐water treatment cells at the downstream end of seasonal wetlands to promote naturally occurring MeHg‐removal processes. We assessed the effectiveness of reducing mercury (Hg) concentrations in surface water and western mosquitofish that were caged at specific locations within 4 control and 4 treatment wetlands. Methylmercury concentrations in wetland water were successfully decreased within treatment cells during only the third year of study; however, treatment cells were not effective for reducing total Hg concentrations. Furthermore, treatment cells were not effective for reducing total Hg concentrations in wetland fish. Mercury concentrations in fish were not correlated with total Hg concentrations in filtered, particulate, or whole water; and the slope of the correlation with water MeHg concentrations differed between months. Fish total Hg concentrations were weakly correlated with water MeHg concentrations in April when fish were introduced into cages but were not correlated in May when fish were retrieved from cages. Fish total Hg concentrations were greater in treatment wetlands than in control wetlands the year after the treatment wetlands’ construction but declined by the second year. During the third year, fish total Hg concentrations increased in both control and treatment wetlands after an unexpected regional flooding event. Overall, we found limited support for the use of open‐ and deep‐water treatment cells at the downstream end of wetlands to reduce MeHg concentrations in water but not fish. We suggest that additional evaluation over a longer period of time is necessary.&nbsp;</p>","language":"English","publisher":"Wiley","doi":"10.1002/etc.4535","usgsCitation":"Ackerman, J., Fleck, J., Eagles-Smith, C.A., Marvin-DiPasquale, M.C., Windham-Myers, L., Herzog, M.P., and McQuillen, H.L., 2019, Wetland management strategy to reduce mercury export in water and bioaccumulation in fish: Environmental Toxicology and Chemistry, v. 38, no. 10, p. 2178-2196, https://doi.org/10.1002/etc.4535.","productDescription":"19 p.","startPage":"2178","endPage":"2196","ipdsId":"IP-104169","costCenters":[{"id":154,"text":"California Water Science Center","active":true,"usgs":true},{"id":289,"text":"Forest and Rangeland Ecosys Science Center","active":true,"usgs":true},{"id":651,"text":"Western Ecological Research Center","active":true,"usgs":true},{"id":37277,"text":"WMA - Earth System Processes Division","active":true,"usgs":true}],"links":[{"id":437381,"rank":0,"type":{"id":30,"text":"Data Release"},"url":"https://doi.org/10.5066/P9NUANQU","text":"USGS data release","linkHelpText":"Wetland Management Strategy to Reduce Mercury Export in Water and Bioaccumulation in Fish"},{"id":367232,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"38","issue":"10","publishingServiceCenter":{"id":1,"text":"Sacramento PSC"},"noUsgsAuthors":false,"publicationDate":"2019-07-25","publicationStatus":"PW","contributors":{"authors":[{"text":"Ackerman, Joshua T. 0000-0002-3074-8322 jackerman@usgs.gov","orcid":"https://orcid.org/0000-0002-3074-8322","contributorId":147078,"corporation":false,"usgs":true,"family":"Ackerman","given":"Joshua T.","email":"jackerman@usgs.gov","affiliations":[{"id":651,"text":"Western Ecological Research Center","active":true,"usgs":true}],"preferred":false,"id":770315,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Fleck, Jacob 0000-0002-3217-3972 jafleck@usgs.gov","orcid":"https://orcid.org/0000-0002-3217-3972","contributorId":168694,"corporation":false,"usgs":true,"family":"Fleck","given":"Jacob","email":"jafleck@usgs.gov","affiliations":[{"id":154,"text":"California Water Science Center","active":true,"usgs":true}],"preferred":true,"id":770316,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Eagles-Smith, Collin A. 0000-0003-1329-5285 ceagles-smith@usgs.gov","orcid":"https://orcid.org/0000-0003-1329-5285","contributorId":505,"corporation":false,"usgs":true,"family":"Eagles-Smith","given":"Collin","email":"ceagles-smith@usgs.gov","middleInitial":"A.","affiliations":[{"id":290,"text":"Forest and Rangeland Ecosystem Science Center","active":false,"usgs":true},{"id":289,"text":"Forest and Rangeland Ecosys Science Center","active":true,"usgs":true},{"id":518,"text":"Oregon Water Science Center","active":true,"usgs":true}],"preferred":true,"id":770317,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Marvin-DiPasquale, Mark C. 0000-0002-8186-9167 mmarvin@usgs.gov","orcid":"https://orcid.org/0000-0002-8186-9167","contributorId":1485,"corporation":false,"usgs":true,"family":"Marvin-DiPasquale","given":"Mark","email":"mmarvin@usgs.gov","middleInitial":"C.","affiliations":[{"id":37277,"text":"WMA - Earth System Processes Division","active":true,"usgs":true},{"id":438,"text":"National Research Program - Western Branch","active":true,"usgs":true}],"preferred":true,"id":770318,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Windham-Myers, Lisamarie lwindham-myers@usgs.gov","contributorId":218804,"corporation":false,"usgs":true,"family":"Windham-Myers","given":"Lisamarie","email":"lwindham-myers@usgs.gov","affiliations":[{"id":37277,"text":"WMA - Earth System Processes Division","active":true,"usgs":true}],"preferred":true,"id":770319,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Herzog, Mark P. 0000-0002-5203-2835 mherzog@usgs.gov","orcid":"https://orcid.org/0000-0002-5203-2835","contributorId":131158,"corporation":false,"usgs":true,"family":"Herzog","given":"Mark","email":"mherzog@usgs.gov","middleInitial":"P.","affiliations":[{"id":651,"text":"Western Ecological Research Center","active":true,"usgs":true}],"preferred":true,"id":770320,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"McQuillen, Harry L.","contributorId":218805,"corporation":false,"usgs":false,"family":"McQuillen","given":"Harry","email":"","middleInitial":"L.","affiliations":[{"id":6696,"text":"BLM","active":true,"usgs":false}],"preferred":false,"id":770321,"contributorType":{"id":1,"text":"Authors"},"rank":7}]}}
,{"id":70204480,"text":"ofr20191079 - 2019 - Effects of microcystin-LR on juvenile Lost River suckers (Deltistes luxatus) during feeding trials, Upper Klamath Lake, Oregon, 2014−16","interactions":[],"lastModifiedDate":"2019-07-26T09:26:00","indexId":"ofr20191079","displayToPublicDate":"2019-07-25T14:52:04","publicationYear":"2019","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2019-1079","displayTitle":"Effects of Microcystin-LR on Juvenile Lost River Suckers (<em>Deltistes luxatus</em>) during Feeding Trials, Upper Klamath Lake, Oregon, 2014−16","title":"Effects of microcystin-LR on juvenile Lost River suckers (Deltistes luxatus) during feeding trials, Upper Klamath Lake, Oregon, 2014−16","docAbstract":"<h1>Executive Summary</h1><p class=\"p1\">Historically, populations of Lost River suckers (<span class=\"s1\"><i>Deltistes luxatus</i>) </span>of the Upper Klamath Basin were so numerous that they were commercially harvested; however, declining numbers throughout the 20th century led to the listing of the species under the United States Endangered Species Act in 1988. Habitat destruction, poor water quality, competition with (and predation by) nonnative species, especially fathead minnows (<i>Pimephales promelas</i>) and yellow perch (<i>Perca flavescens</i>), are hypothesized as primary causes of population decline (U.S. Fish and Wildlife Service, 2013). Age data indicate that almost all adult suckers presently in Upper Klamath Lake spawning populations were hatched in the early 1990s. While entrainment of young fish (especially larvae) may contribute, catch-at-length and age data suggest consistently high mortality during the first year of life may be preventing the recruitment of young adults. The specific causes of juvenile sucker mortality are unknown; however, the absence of juvenile suckers in trap net catches coincides with degraded water quality associated with the decay of cyanobacteria blooms and exposure to toxic microcystin produced by <i>Microcystis </i>cyanobacteria.</p><p class=\"p1\">Water-quality data collected in Upper Klamath Lake from 2011 to 2016 suggest that microcystin concentrations in Upper Klamath Lake reached potentially lethal levels based on literature findings from studies on a variety of fish species. We conducted a laboratory feeding trial to determine if microcystin toxicity could potentially be a direct cause of juvenile Lost River sucker mortality. We examined the effects of environmentally relevant doses of microcystin on the survival and health of hatchery-reared juvenile Lost River suckers. Results from this laboratory study suggest that Lost River suckers are very tolerant of the microcystin-LR toxin. Histopathological analysis revealed no evidence of tissue changes associated with microcystin-LR exposure. Although no direct effects of microcystin-LR exposure were detected, suckers could potentially be negatively affected through added energy expenditures and stress associated with excretion of microcystin. Furthermore, microcystin may adversely affect other organisms in Upper Klamath Lake that could alter food availability or habitat of the suckers.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr20191079","collaboration":"Prepared in cooperation with the U.S. Fish and Wildlife Service and Bureau of Reclamation","usgsCitation":"Martin, B.A., Echols, K.R., Elliott, D.G., Feltz, K., Conway, C.M., and Burdick, S.M., 2019, Effects of microcystin-LR on juvenile Lost River suckers (Deltistes luxatus) during feeding trials, Upper Klamath Lake, Oregon, 2014−16: U.S. Geological Survey Open−File Report 2019–1079, 22 p., https://doi.org/10.3133/ofr20191079.","productDescription":"vi, 22 p.","onlineOnly":"Y","ipdsId":"IP-106575","costCenters":[{"id":192,"text":"Columbia Environmental Research Center","active":true,"usgs":true},{"id":654,"text":"Western Fisheries Research Center","active":true,"usgs":true}],"links":[{"id":365967,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/2019/1079/coverthb.jpg"},{"id":365968,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/2019/1079/ofr20191079.pdf","text":"Report","size":"7.2 MB","linkFileType":{"id":1,"text":"pdf"},"description":"OFR 2019-1079"}],"country":"United States","state":"Oregon","otherGeospatial":"Upper Klamath Lake","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -122.08625793457031,\n              42.48222557002593\n            ],\n            [\n              -122.09449768066405,\n              42.47361631282951\n            ],\n            [\n              -122.05879211425781,\n              42.43004544849287\n            ],\n   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       [\n              -122.03407287597655,\n              42.500959270579585\n            ],\n            [\n              -122.04849243164061,\n              42.49589666159403\n            ],\n            [\n              -122.05879211425781,\n              42.48425110546248\n            ],\n            [\n              -122.06359863281249,\n              42.461460050936715\n            ],\n            [\n              -122.07527160644531,\n              42.46399280017058\n            ],\n            [\n              -122.08625793457031,\n              42.48222557002593\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","contact":"<p>Director, <a href=\"https://www.usgs.gov/centers/wfrc\" target=\"_blank\" rel=\"noopener\" data-mce-href=\"https://www.usgs.gov/centers/wfrc\">Western Fisheries Research Center</a><br>U.S. Geological Survey<br>6505 NE 65th Street<br>Seattle, Washington 98115-5016</p>","tableOfContents":"<ul><li>Executive Summary</li><li>Introduction</li><li>Methods</li><li>Results</li><li>Discussion</li><li>Acknowledgments</li><li>References Cited</li></ul>","publishedDate":"2019-07-25","noUsgsAuthors":false,"publicationDate":"2019-07-25","publicationStatus":"PW","contributors":{"authors":[{"text":"Martin, Barbara A. 0000-0002-9415-6377 barbara_ann_martin@usgs.gov","orcid":"https://orcid.org/0000-0002-9415-6377","contributorId":2855,"corporation":false,"usgs":true,"family":"Martin","given":"Barbara","email":"barbara_ann_martin@usgs.gov","middleInitial":"A.","affiliations":[{"id":654,"text":"Western Fisheries Research Center","active":true,"usgs":true}],"preferred":true,"id":767170,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Echols, Kathy R. 0000-0003-2631-9143 kechols@usgs.gov","orcid":"https://orcid.org/0000-0003-2631-9143","contributorId":2799,"corporation":false,"usgs":true,"family":"Echols","given":"Kathy","email":"kechols@usgs.gov","middleInitial":"R.","affiliations":[{"id":192,"text":"Columbia Environmental Research Center","active":true,"usgs":true}],"preferred":true,"id":767171,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Elliott, Diane G. 0000-0002-4809-6692 dgelliott@usgs.gov","orcid":"https://orcid.org/0000-0002-4809-6692","contributorId":2947,"corporation":false,"usgs":true,"family":"Elliott","given":"Diane","email":"dgelliott@usgs.gov","middleInitial":"G.","affiliations":[{"id":654,"text":"Western Fisheries Research Center","active":true,"usgs":true}],"preferred":true,"id":767172,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Feltz, Kevin 0000-0003-3928-0954 kfeltz@usgs.gov","orcid":"https://orcid.org/0000-0003-3928-0954","contributorId":100521,"corporation":false,"usgs":true,"family":"Feltz","given":"Kevin","email":"kfeltz@usgs.gov","affiliations":[],"preferred":false,"id":767173,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Conway, Carla M. 0000-0002-3851-3616 cmconway@usgs.gov","orcid":"https://orcid.org/0000-0002-3851-3616","contributorId":2946,"corporation":false,"usgs":true,"family":"Conway","given":"Carla","email":"cmconway@usgs.gov","middleInitial":"M.","affiliations":[{"id":654,"text":"Western Fisheries Research Center","active":true,"usgs":true}],"preferred":true,"id":767174,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Burdick, Summer M. 0000-0002-3480-5793 sburdick@usgs.gov","orcid":"https://orcid.org/0000-0002-3480-5793","contributorId":3448,"corporation":false,"usgs":true,"family":"Burdick","given":"Summer","email":"sburdick@usgs.gov","middleInitial":"M.","affiliations":[{"id":654,"text":"Western Fisheries Research Center","active":true,"usgs":true}],"preferred":true,"id":767175,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}}
,{"id":70204345,"text":"ds1116 - 2019 - Water-level data for the Albuquerque Basin and adjacent areas, central New Mexico, period of record through September 30, 2018","interactions":[],"lastModifiedDate":"2021-08-26T14:16:26.144304","indexId":"ds1116","displayToPublicDate":"2019-07-25T12:57:30","publicationYear":"2019","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":310,"text":"Data Series","code":"DS","onlineIssn":"2327-638X","printIssn":"2327-0271","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1116","displayTitle":"Water-Level Data for the Albuquerque Basin and Adjacent Areas, Central New Mexico, Period of Record Through September 30, 2018","title":"Water-level data for the Albuquerque Basin and adjacent areas, central New Mexico, period of record through September 30, 2018","docAbstract":"<p>The Albuquerque Basin, located in central New Mexico, is about 100 miles long and 25–40 miles wide. The basin is hydrologically defined as the extent of consolidated and unconsolidated deposits of Tertiary and Quaternary age that encompasses the structural Rio Grande Rift between San Acacia to the south and Cochiti Lake to the north. A 20-percent population increase in the basin from 1990 to 2000 and a 22-percent population increase from 2000 to 2010 resulted in an increased demand for water in areas within the basin. Drinking-water supplies throughout the basin were obtained solely from groundwater resources until December 2008, when the Albuquerque Bernalillo County Water Utility Authority (ABCWUA) began treatment and distribution of surface water from the Rio Grande through the San Juan-Chama Drinking Water Project.</p><p>An initial network of wells was established by the U.S. Geological Survey (USGS) in cooperation with the City of Albuquerque from April 1982 through September 1983 to monitor changes in groundwater levels throughout the Albuquerque Basin. In 1983, this network consisted of 6 wells with analog-to-digital recorders and 27 wells where water levels were measured monthly. As of 2018, the network consisted of 120 wells and piezometers. (A piezometer is a specialized well open to a specific depth in the aquifer, often of small diameter and nested with other piezometers open to different depths.) The USGS, in cooperation with the ABCWUA, the New Mexico Office of the State Engineer, and Bernalillo County, measures water levels from the 120 wells and piezometers in the network; this report, prepared in cooperation with the ABCWUA, presents water-level data collected by USGS personnel at those 120 sites through water year 2018 (October 1, 2017, through September 30, 2018). Water levels that were collected from wells in previous water years were published in previous USGS reports.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ds1116","collaboration":"Prepared in cooperation with the Albuquerque Bernalillo County Water Utility Authority","usgsCitation":"Ritchie, A.B., and Galanter, A.E., 2019, Water-level data for the Albuquerque Basin and adjacent areas, central New Mexico, period of record through September 30, 2018 (ver. 1.1, August 2021): U.S. Geological Survey Data Series 1116, 40 p., https://doi.org/10.3133/ds1116.","productDescription":"iii, 40 p.","numberOfPages":"49","onlineOnly":"Y","ipdsId":"IP-108049","costCenters":[{"id":472,"text":"New Mexico Water Science Center","active":true,"usgs":true}],"links":[{"id":365903,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/ds/1116/coverthb2.jpg"},{"id":388360,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/ds/1116/ds1116.pdf","text":"Report","size":"5.57 MB","linkFileType":{"id":1,"text":"pdf"},"description":"DS 1116"},{"id":388361,"rank":3,"type":{"id":25,"text":"Version History"},"url":"https://pubs.usgs.gov/ds/1116/versionHist.txt","text":"Version History","size":"554 B","linkFileType":{"id":2,"text":"txt"},"description":"DS 1116 Verson History"}],"country":"United States","state":"New Mexico","otherGeospatial":"Albuquerque Basin","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -107,\n              34.85\n            ],\n            [\n              -106.375,\n              34.85\n            ],\n            [\n              -106.375,\n              35.4\n            ],\n            [\n              -107,\n              35.4\n            ],\n            [\n              -107,\n              34.85\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","edition":"Version 1.1: August 2021","contact":"<p><a href=\"mailto:%20dc_nm@usgs.gov\" data-mce-href=\"mailto:%20dc_nm@usgs.gov\">Director</a>, <a href=\"https://www.usgs.gov/centers/nm-water\" data-mce-href=\"https://www.usgs.gov/centers/nm-water\">New Mexico Water Science Center</a><br>U.S. Geological Survey<br>6700 Edith Blvd. NE<br>Albuquerque, NM 87113</p>","tableOfContents":"<ul><li>Abstract</li><li>Introduction</li><li>Water-Level Data</li><li>Acknowledgments</li><li>References Cited</li></ul>","publishingServiceCenter":{"id":5,"text":"Lafayette PSC"},"publishedDate":"2019-07-25","revisedDate":"2021-08-25","noUsgsAuthors":false,"publicationDate":"2019-07-25","publicationStatus":"PW","contributors":{"authors":[{"text":"Ritchie, Andre B. 0000-0003-1289-653X","orcid":"https://orcid.org/0000-0003-1289-653X","contributorId":214611,"corporation":false,"usgs":true,"family":"Ritchie","given":"Andre","email":"","middleInitial":"B.","affiliations":[{"id":472,"text":"New Mexico Water Science Center","active":true,"usgs":true}],"preferred":true,"id":766445,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Galanter, Amy E. 0000-0002-2960-0136","orcid":"https://orcid.org/0000-0002-2960-0136","contributorId":214612,"corporation":false,"usgs":true,"family":"Galanter","given":"Amy E.","affiliations":[{"id":472,"text":"New Mexico Water Science Center","active":true,"usgs":true}],"preferred":true,"id":766446,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
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