{"pageNumber":"532","pageRowStart":"13275","pageSize":"25","recordCount":68911,"records":[{"id":70150433,"text":"70150433 - 2014 - Monitoring fish distributions along electrofishing segments","interactions":[],"lastModifiedDate":"2015-07-24T12:04:15","indexId":"70150433","displayToPublicDate":"2014-12-01T00:00:00","publicationYear":"2014","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1552,"text":"Environmental Monitoring and Assessment","onlineIssn":"1573-2959","printIssn":"0167-6369","active":true,"publicationSubtype":{"id":10}},"title":"Monitoring fish distributions along electrofishing segments","docAbstract":"<p><span>Electrofishing is widely used to monitor fish species composition and relative abundance in streams and lakes. According to standard protocols, multiple segments are selected in a body of water to monitor population relative abundance as the ratio of total catch to total sampling&nbsp;effort. The standard protocol provides an assessment of fish distribution at a macrohabitat scale among segments, but not within segments. An ancillary protocol was developed for assessing fish distribution at a finer scale within electrofishing segments. The ancillary protocol was used to estimate spacing, dispersion, and association of two species along shore segments in two local reservoirs. The added information provided by the ancillary protocol may be useful for assessing fish distribution relative to fish of the same species, to fish of different species, and to environmental or habitat characteristics.</span></p>","language":"English","publisher":"Springer","doi":"10.1007/s10661-014-4053-6","usgsCitation":"Miranda, L.E., 2014, Monitoring fish distributions along electrofishing segments: Environmental Monitoring and Assessment, v. 186, no. 12, p. 8899-8905, https://doi.org/10.1007/s10661-014-4053-6.","productDescription":"7 p.","startPage":"8899","endPage":"8905","onlineOnly":"N","additionalOnlineFiles":"N","ipdsId":"IP-054281","costCenters":[{"id":198,"text":"Coop Res Unit Atlanta","active":true,"usgs":true}],"links":[{"id":305971,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Mississippi","otherGeospatial":"Oktibbeha County Lake; Ross Barnett Reservoir","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -90.11260986328125,\n              32.35444302709291\n            ],\n            [\n              -90.11260986328125,\n              32.55144352864431\n            ],\n            [\n              -89.89837646484375,\n              32.55144352864431\n            ],\n            [\n              -89.89837646484375,\n              32.35444302709291\n            ],\n            [\n              -90.11260986328125,\n              32.35444302709291\n            ]\n          ]\n        ]\n      }\n    },\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -88.95441055297852,\n              33.5004648191553\n            ],\n            [\n              -88.95441055297852,\n              33.5172111895567\n            ],\n            [\n              -88.92539978027344,\n              33.5172111895567\n            ],\n            [\n              -88.92539978027344,\n              33.5004648191553\n            ],\n            [\n              -88.95441055297852,\n              33.5004648191553\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"186","issue":"12","publishingServiceCenter":{"id":8,"text":"Raleigh PSC"},"noUsgsAuthors":false,"publicationDate":"2014-09-20","publicationStatus":"PW","scienceBaseUri":"55b361b3e4b09a3b01b5daad","contributors":{"authors":[{"text":"Miranda, Leandro E. 0000-0002-2138-7924 smiranda@usgs.gov","orcid":"https://orcid.org/0000-0002-2138-7924","contributorId":531,"corporation":false,"usgs":true,"family":"Miranda","given":"Leandro","email":"smiranda@usgs.gov","middleInitial":"E.","affiliations":[{"id":198,"text":"Coop Res Unit Atlanta","active":true,"usgs":true}],"preferred":true,"id":556876,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70162113,"text":"70162113 - 2014 - Effects of a dual-pump crude-oil recovery system, Bemidji, Minnesota, USA","interactions":[],"lastModifiedDate":"2018-09-14T16:48:59","indexId":"70162113","displayToPublicDate":"2014-12-01T00:00:00","publicationYear":"2014","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1866,"text":"Groundwater Monitoring & Remediation","active":true,"publicationSubtype":{"id":10}},"title":"Effects of a dual-pump crude-oil recovery system, Bemidji, Minnesota, USA","docAbstract":"<p><span>A crude-oil spill occurred in 1979 when a pipeline burst near Bemidji, MN. In 1998, the pipeline company installed a dual-pump recovery system designed to remove crude oil remaining in the subsurface at the site. The remediation from 1999 to 2003 resulted in removal of about 115,000 L of crude oil, representing between 36% and 41% of the volume of oil (280,000 to 316,000 L) estimated to be present in 1998. Effects of the 1999 to 2003 remediation on the dissolved plume were evaluated using measurements of oil thicknesses in wells plus measurements of dissolved oxygen in groundwater. Although the recovery system decreased oil thicknesses in the immediate vicinity of the remediation wells, average oil thicknesses measured in wells were largely unaffected. Dissolved-oxygen measurements indicate that a secondary plume was caused by disposal of the pumped water in an upgradient infiltration gallery; this plume expanded rapidly immediately following the start of the remediation in 1999. The result was expansion of the anoxic zone of groundwater upgradient and beneath the existing natural attenuation plume. Oil-phase recovery at this site was shown to be challenging, and considerable volumes of mobile and entrapped oil remain in the subsurface despite remediation efforts.</span></p>","language":"English","publisher":"Wiley","doi":"10.1111/gwmr.12040","usgsCitation":"Delin, G.N., and Herkelrath, W.N., 2014, Effects of a dual-pump crude-oil recovery system, Bemidji, Minnesota, USA: Groundwater Monitoring & Remediation, v. 34, no. 1, p. 57-67, https://doi.org/10.1111/gwmr.12040.","productDescription":"11 p.","startPage":"57","endPage":"67","onlineOnly":"N","additionalOnlineFiles":"N","ipdsId":"IP-038101","costCenters":[{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true},{"id":5063,"text":"Central Water Science Field Team","active":true,"usgs":true}],"links":[{"id":314279,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Minnesota","city":"Bemidji","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -95.15808105468749,\n              47.3220687602135\n            ],\n            [\n              -95.15808105468749,\n              47.6080148197327\n            ],\n            [\n              -94.603271484375,\n              47.6080148197327\n            ],\n            [\n              -94.603271484375,\n              47.3220687602135\n            ],\n            [\n              -95.15808105468749,\n              47.3220687602135\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"34","issue":"1","publishingServiceCenter":{"id":2,"text":"Denver PSC"},"noUsgsAuthors":false,"publicationDate":"2014-01-22","publicationStatus":"PW","scienceBaseUri":"5697833be4b039675d00a6dc","contributors":{"authors":[{"text":"Delin, Geoffrey N. 0000-0001-7991-6158 delin@usgs.gov","orcid":"https://orcid.org/0000-0001-7991-6158","contributorId":2610,"corporation":false,"usgs":true,"family":"Delin","given":"Geoffrey","email":"delin@usgs.gov","middleInitial":"N.","affiliations":[{"id":5063,"text":"Central Water Science Field Team","active":true,"usgs":true}],"preferred":true,"id":588582,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Herkelrath, William N. 0000-0002-6149-5524 wnherkel@usgs.gov","orcid":"https://orcid.org/0000-0002-6149-5524","contributorId":2612,"corporation":false,"usgs":true,"family":"Herkelrath","given":"William","email":"wnherkel@usgs.gov","middleInitial":"N.","affiliations":[{"id":438,"text":"National Research Program - Western Branch","active":true,"usgs":true}],"preferred":true,"id":588589,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70189809,"text":"70189809 - 2014 - Paleogeomorphology of the early Colorado River inferred from relationships in Mohave and Cottonwood Valleys, Arizona, California and Nevada","interactions":[],"lastModifiedDate":"2017-07-26T15:40:00","indexId":"70189809","displayToPublicDate":"2014-12-01T00:00:00","publicationYear":"2014","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1820,"text":"Geosphere","active":true,"publicationSubtype":{"id":10}},"title":"Paleogeomorphology of the early Colorado River inferred from relationships in Mohave and Cottonwood Valleys, Arizona, California and Nevada","docAbstract":"<p><span>Geologic investigations of late Miocene–early Pliocene deposits in Mohave and Cottonwood valleys provide important insights into the early evolution of the lower Colorado River system. In the latest Miocene these valleys were separate depocenters; the floor of Cottonwood Valley was ∼200 m higher than the floor of Mohave Valley. When Colorado River water arrived from the north after 5.6 Ma, a shallow lake in Cottonwood Valley spilled into Mohave Valley, and the river then filled both valleys to ∼560 m above sea level (asl) and overtopped the bedrock divide at the southern end of Mohave Valley. Sediment-starved water spilling to the south gradually eroded the outlet as siliciclastic Bouse deposits filled the lake upstream. When sediment accumulation reached the elevation of the lowering outlet, continued erosion of the outlet resulted in recycling of stored lacustrine sediment into downstream basins; depth of erosion of the outlet and upstream basins was limited by the water levels in downstream basins. The water level in the southern Bouse basin was ∼300 m asl (modern elevation) at 4.8 Ma. It must have drained and been eroded to a level &lt;150 m asl soon after that to allow for deep erosion of bedrock divides and basins upstream, leading to removal of large volumes of Bouse sediment prior to massive early Pliocene Colorado River aggradation. Abrupt lowering of regional base level due to spilling of a southern Bouse lake to the Gulf of California could have driven observed upstream river incision without uplift. Rapid uplift of the entire region immediately after 4.8 Ma would have been required to drive upstream incision if the southern Bouse was an estuary.</span></p>","language":"English","publisher":"Geological Society of America","doi":"10.1130/GES00988.1","usgsCitation":"Pearthree, P., and House, K., 2014, Paleogeomorphology of the early Colorado River inferred from relationships in Mohave and Cottonwood Valleys, Arizona, California and Nevada: Geosphere, v. 10, no. 6, p. 1139-1160, https://doi.org/10.1130/GES00988.1.","productDescription":"22 p.","startPage":"1139","endPage":"1160","ipdsId":"IP-053171","costCenters":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"links":[{"id":472623,"rank":0,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1130/ges00988.1","text":"Publisher Index Page"},{"id":344345,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Arizona, California, Nevada","otherGeospatial":"Colorado River, Cottonwood Valley, Mohave Valley","volume":"10","issue":"6","publishingServiceCenter":{"id":14,"text":"Menlo Park PSC"},"noUsgsAuthors":false,"publicationDate":"2014-11-12","publicationStatus":"PW","scienceBaseUri":"5979aa56e4b0ec1a488b8c19","contributors":{"authors":[{"text":"Pearthree, Philip","contributorId":195166,"corporation":false,"usgs":false,"family":"Pearthree","given":"Philip","affiliations":[],"preferred":false,"id":706436,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"House, Kyle 0000-0002-0019-8075 khouse@usgs.gov","orcid":"https://orcid.org/0000-0002-0019-8075","contributorId":2293,"corporation":false,"usgs":true,"family":"House","given":"Kyle","email":"khouse@usgs.gov","affiliations":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"preferred":true,"id":706435,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70186668,"text":"70186668 - 2014 - Widespread gas hydrate instability on the upper U.S. Beaufort margin","interactions":[],"lastModifiedDate":"2017-04-07T10:25:50","indexId":"70186668","displayToPublicDate":"2014-12-01T00:00:00","publicationYear":"2014","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2314,"text":"Journal of Geophysical Research B: Solid Earth","active":true,"publicationSubtype":{"id":10}},"title":"Widespread gas hydrate instability on the upper U.S. Beaufort margin","docAbstract":"<p><span>The most climate-sensitive methane hydrate deposits occur on upper continental slopes at depths close to the minimum pressure and maximum temperature for gas hydrate stability. At these water depths, small perturbations in intermediate ocean water temperatures can lead to gas hydrate dissociation. The Arctic Ocean has experienced more dramatic warming than lower latitudes, but observational data have not been used to study the interplay between upper slope gas hydrates and warming ocean waters. Here we use (a) legacy seismic data that constrain upper slope gas hydrate distributions on the U.S. Beaufort Sea margin, (b) Alaskan North Slope borehole data and offshore thermal gradients determined from gas hydrate stability zone thickness to infer regional heat flow, and (c) 1088 direct measurements to characterize multidecadal intermediate ocean warming in the U.S. Beaufort Sea. Combining these data with a three-dimensional thermal model shows that the observed gas hydrate stability zone is too deep by 100 to 250 m. The disparity can be partially attributed to several processes, but the most important is the reequilibration (thinning) of gas hydrates in response to significant (~0.5°C at 2σ certainty) warming of intermediate ocean temperatures over 39 years in a depth range that brackets the upper slope extent of the gas hydrate stability zone. Even in the absence of additional ocean warming, 0.44 to 2.2 Gt of methane could be released from reequilibrating gas hydrates into the sediments underlying an area of ~5–7.5 × 10</span><sup>3</sup><span> km</span><sup>2</sup><span> on the U.S. Beaufort Sea upper slope during the next century.</span></p>","language":"English","publisher":"AGU","doi":"10.1002/2014JB011290","usgsCitation":"Phrampus, B.J., Hornbach, M.J., Ruppel, C., and Hart, P.E., 2014, Widespread gas hydrate instability on the upper U.S. Beaufort margin: Journal of Geophysical Research B: Solid Earth, v. 119, no. 12, p. 8594-8609, https://doi.org/10.1002/2014JB011290.","productDescription":"16 p.","startPage":"8594","endPage":"8609","ipdsId":"IP-059791","costCenters":[{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"links":[{"id":472616,"rank":0,"type":{"id":41,"text":"Open Access External Repository Page"},"url":"https://www.osti.gov/biblio/1402351","text":"External Repository"},{"id":339397,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Alaska","otherGeospatial":"Beaufort Sea","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -160,\n              69.5\n            ],\n            [\n              -140,\n              69.5\n            ],\n            [\n              -140,\n              72.5\n            ],\n            [\n              -160,\n              72.5\n            ],\n            [\n              -160,\n              69.5\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"119","issue":"12","publishingServiceCenter":{"id":11,"text":"Pembroke PSC"},"noUsgsAuthors":false,"publicationDate":"2014-12-09","publicationStatus":"PW","scienceBaseUri":"58e8a545e4b09da6799d63b1","chorus":{"doi":"10.1002/2014jb011290","url":"http://dx.doi.org/10.1002/2014jb011290","publisher":"Wiley-Blackwell","authors":"Phrampus Benjamin J., Hornbach Matthew J., Ruppel Carolyn D., Hart Patrick E.","journalName":"Journal of Geophysical Research: Solid Earth","publicationDate":"12/2014","auditedOn":"12/7/2014"},"contributors":{"authors":[{"text":"Phrampus, Benjamin J.","contributorId":190655,"corporation":false,"usgs":false,"family":"Phrampus","given":"Benjamin","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":690219,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hornbach, Matthew J.","contributorId":14258,"corporation":false,"usgs":true,"family":"Hornbach","given":"Matthew","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":690220,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Ruppel, Carolyn D. 0000-0003-2284-6632 cruppel@usgs.gov","orcid":"https://orcid.org/0000-0003-2284-6632","contributorId":145770,"corporation":false,"usgs":true,"family":"Ruppel","given":"Carolyn D.","email":"cruppel@usgs.gov","affiliations":[{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":false,"id":690218,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Hart, Patrick E. 0000-0002-5080-1426 hart@usgs.gov","orcid":"https://orcid.org/0000-0002-5080-1426","contributorId":2879,"corporation":false,"usgs":true,"family":"Hart","given":"Patrick","email":"hart@usgs.gov","middleInitial":"E.","affiliations":[{"id":520,"text":"Pacific Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":true,"id":690221,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70189303,"text":"70189303 - 2014 - The future of nearshore processes research","interactions":[],"lastModifiedDate":"2017-11-12T11:04:59","indexId":"70189303","displayToPublicDate":"2014-12-01T00:00:00","publicationYear":"2014","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":9,"text":"Other Report"},"title":"The future of nearshore processes research","docAbstract":"<p>The nearshore is the transition region between land and the continental shelf including (from onshore to offshore) coastal plains, wetlands, estuaries, coastal cliffs, dunes, beaches, surf zones (regions of wave breaking), and the inner shelf (Figure ES-1). Nearshore regions are vital to the national economy, security, commerce, and recreation. The nearshore is dynamically evolving, is often densely populated, and is under increasing threat from sea level rise, long-term erosion, extreme storms, and anthropogenic influences. Worldwide, almost one billion people live at elevations within 10 m of present sea level. Long-term erosion threatens communities, infrastructure, ecosystems, and habitat. Extreme storms can cause billions of dollars of damage. Degraded water quality impacts ecosystem and human health. Nearshore processes, the complex interactions between water, sediment, biota, and humans, must be understood and predicted to manage this often highly developed yet vulnerable nearshore environment. </p><p>Over the past three decades, the understanding of nearshore processes has improved. However, societal needs are growing with increased coastal urbanization and threats of future climate change, and significant scientific challenges remain. To address these challenges, members of academia, industry, and federal agencies (USGS, USACE, NPS, NOAA, FEMA, ONR) met at the “The Past and Future of Nearshore Processes Research: Reflections on the Sallenger Years and a New Vision for the Future” workshop to develop a nearshore processes research vision where societal needs and science challenges intersect. The resulting vision is comprised of three broad research themes: </p><p><ol><li>Long-term coastal evolution due to natural and anthropogenic processes: As global climate change alters the rates of sea level rise and potentially storm patterns and coastal urbanization increases over the coming decades, an understanding of coastal evolution is critical. Improved knowledge of long-term morphological, ecological, and societal processes and their interactions will result in an improved ability to simulate coastal change. This will enable proactive solutions for resilient coasts and better guidance for reducing coastal vulnerability.<br></li><li>Extreme Events: Flooding, erosion, and the subsequent recovery: Hurricane Sandy caused flooding and erosion along hundreds of miles of shoreline, flooded New York City, and impacted communities and infrastructure. Overall U.S. coastal extreme event related economic losses have increased substantially. Furthermore, climate change may cause an increase in coastal extreme events and rising sea levels could increase the occurrence of extreme events. Addressing this research theme will result in an improved understanding of the physical processes during extreme events, leading to improved models of flooding, erosion, and recovery. The resulting societal benefit will be more resilient coastal communities.<br></li><li>The physical, biological and chemical processes impacting human and ecosystem health: Nearshore regions are used for recreation, tourism, and human habitation, and provide habitat and valuable ecosystem services. These areas must be sustained for future generations, however overall coastal water quality is declining due to microbial pathogens, fertilizers, pesticides, and heavy metal contamination, threatening ecosystem and human health. To ensure sustainable nearshore regions, predictive real-time water- and sediment-based based pollutant modeling capabilities must be developed, which requires expanding our knowledge of the physics, chemistry, and biology of the nearshore. The resulting societal benefits will include better beach safety, healthier ecosystems, and improved mitigation and regulatory policies.<br></li></ol></p><p>The scientists and engineers of the U.S. nearshore community are poised to make significant progress on these research themes, which have significant societal impact. The U.S. nearshore community, including academic, government, and industry colleagues, recommends multi-agency investment into a coordinated development of observational and modeling research infrastructure to address these themes, as discussed in&nbsp;the whitepaper. The observational infrastructure should include development of new sensors and methods, focused observational programs, and expanded nearshore observing systems. The modeling infrastructure should include improved process representation, better model coupling, incorporation of data assimilation techniques, and testing of real-time models. The observations will provide test beds to compare and improve models.</p>","language":"English","publisher":"The Nearshore Processes Community","usgsCitation":"2014, The future of nearshore processes research, 32 p.","productDescription":"32 p.","ipdsId":"IP-063052","costCenters":[{"id":574,"text":"St. Petersburg Coastal and Marine Science Center","active":true,"usgs":true}],"links":[{"id":343516,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":343509,"type":{"id":11,"text":"Document"},"url":"https://scripps.ucsd.edu/centers/nearshorefuture/wp-content/uploads/sites/37/2014/12/Future_Nearshore_Processes_Research.pdf"}],"publishingServiceCenter":{"id":8,"text":"Raleigh PSC"},"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"59649235e4b0d1f9f05acd48","contributors":{"editors":[{"text":"Elko, Nicole A.","contributorId":50960,"corporation":false,"usgs":true,"family":"Elko","given":"Nicole","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":704063,"contributorType":{"id":2,"text":"Editors"},"rank":1},{"text":"Feddersen, Falk","contributorId":194420,"corporation":false,"usgs":false,"family":"Feddersen","given":"Falk","email":"","affiliations":[],"preferred":false,"id":704064,"contributorType":{"id":2,"text":"Editors"},"rank":2},{"text":"Foster, Diane","contributorId":194421,"corporation":false,"usgs":false,"family":"Foster","given":"Diane","affiliations":[],"preferred":false,"id":704065,"contributorType":{"id":2,"text":"Editors"},"rank":3},{"text":"Hapke, Cheryl J. 0000-0002-2753-4075 chapke@usgs.gov","orcid":"https://orcid.org/0000-0002-2753-4075","contributorId":2981,"corporation":false,"usgs":true,"family":"Hapke","given":"Cheryl","email":"chapke@usgs.gov","middleInitial":"J.","affiliations":[{"id":6676,"text":"USGS (retired)","active":true,"usgs":false}],"preferred":true,"id":704066,"contributorType":{"id":2,"text":"Editors"},"rank":4},{"text":"McNinch, Jesse E.","contributorId":93804,"corporation":false,"usgs":true,"family":"McNinch","given":"Jesse E.","affiliations":[],"preferred":false,"id":704067,"contributorType":{"id":2,"text":"Editors"},"rank":5},{"text":"Mulligan, Ryan P.","contributorId":194423,"corporation":false,"usgs":false,"family":"Mulligan","given":"Ryan","email":"","middleInitial":"P.","affiliations":[{"id":35723,"text":"Queen's University - Kingston, Ontario","active":true,"usgs":false}],"preferred":false,"id":704068,"contributorType":{"id":2,"text":"Editors"},"rank":6},{"text":"Tuba Ozkan-Haller, H.","contributorId":194424,"corporation":false,"usgs":false,"family":"Tuba Ozkan-Haller","given":"H.","email":"","affiliations":[],"preferred":false,"id":704069,"contributorType":{"id":2,"text":"Editors"},"rank":7},{"text":"Plant, Nathaniel G. 0000-0002-5703-5672 nplant@usgs.gov","orcid":"https://orcid.org/0000-0002-5703-5672","contributorId":3503,"corporation":false,"usgs":true,"family":"Plant","given":"Nathaniel","email":"nplant@usgs.gov","middleInitial":"G.","affiliations":[{"id":508,"text":"Office of the AD Hazards","active":true,"usgs":true},{"id":574,"text":"St. Petersburg Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":true,"id":704070,"contributorType":{"id":2,"text":"Editors"},"rank":8},{"text":"Raubenheimer, Britt","contributorId":194340,"corporation":false,"usgs":false,"family":"Raubenheimer","given":"Britt","email":"","affiliations":[],"preferred":false,"id":704071,"contributorType":{"id":2,"text":"Editors"},"rank":9}]}}
,{"id":70189185,"text":"70189185 - 2014 - The effects of changing land cover on streamflow simulation in Puerto Rico","interactions":[],"lastModifiedDate":"2017-07-06T14:43:52","indexId":"70189185","displayToPublicDate":"2014-12-01T00:00:00","publicationYear":"2014","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":"The effects of changing land cover on streamflow simulation in Puerto Rico","docAbstract":"<p><span>This study quantitatively explores whether land cover changes have a substantive impact on simulated streamflow within the tropical island setting of Puerto Rico. The Precipitation Runoff Modeling System (PRMS) was used to compare streamflow simulations based on five static parameterizations of land cover with those based on dynamically varying parameters derived from four land cover scenes for the period 1953-2012. The PRMS simulations based on static land cover illustrated consistent differences in simulated streamflow across the island. It was determined that the scale of the analysis makes a difference: large regions with localized areas that have undergone dramatic land cover change may show negligible difference in total streamflow, but streamflow simulations using dynamic land cover parameters for a highly altered subwatershed clearly demonstrate the effects of changing land cover on simulated streamflow. Incorporating dynamic parameterization in these highly altered watersheds can reduce the predictive uncertainty in simulations of streamflow using PRMS. Hydrologic models that do not consider the projected changes in land cover may be inadequate for water resource management planning for future conditions.</span></p>","language":"English","publisher":"Wiley","doi":"10.1111/jawr.12227","usgsCitation":"Van Beusekom, A.E., Hay, L.E., Viger, R.J., Gould, W.A., Collazo, J., and Henareh Khalyani, A., 2014, The effects of changing land cover on streamflow simulation in Puerto Rico: Journal of the American Water Resources Association, v. 50, no. 6, p. 1575-1593, https://doi.org/10.1111/jawr.12227.","productDescription":"19 p.","startPage":"1575","endPage":"1593","ipdsId":"IP-054092","costCenters":[{"id":5044,"text":"National Research Program - Central Branch","active":true,"usgs":true}],"links":[{"id":343436,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"Puerto 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,{"id":70177808,"text":"70177808 - 2014 - Comprehensive framework for ecological assessment of the Migratory Bird Habitat Initiative following the Deepwater Horizon oil spill","interactions":[],"lastModifiedDate":"2016-10-21T15:29:03","indexId":"70177808","displayToPublicDate":"2014-12-01T00:00:00","publicationYear":"2014","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3444,"text":"Southeastern Naturalist","active":true,"publicationSubtype":{"id":10}},"title":"Comprehensive framework for ecological assessment of the Migratory Bird Habitat Initiative following the Deepwater Horizon oil spill","docAbstract":"<p><span>Following the Deepwater Horizon oil spill in the Gulf of Mexico in April 2010, the USDA Natural Resources Conservation Service (NRCS) established and funded the Migratory Bird Habitat Initiative (MBHI), with the goal of improving and increasing wetland habitats on private lands to benefit wintering and migrating waterbirds displaced from oil-impacted coastal wetlands. The NRCS and conservation partners provided financial and technical assistance to landowners and managers of sites enrolled in various conservation easement programs, and incorporated approximately 190,000 ha of wetlands and agricultural lands in the Mississippi Alluvial Valley (MAV) and Gulf Coast regions in the MBHI. In fall 2010, the NRCS worked with scientists and graduate students from three universities and various conservation agencies to design and implement landscape-scale evaluations of (1) the use of MBHI-managed wetlands and comparable non-MBHI wetlands by </span><i>Charadriiformes</i><span>(shorebirds), </span><i>Anseriformes</i><span> (waterfowl), and other waterbirds; and (2) the relative effectiveness of different MBHI practices for providing habitat and food resources for migrating, resident, and wintering waterbirds. In this paper, we describe the scientific framework designed to evaluate the MBHI in improving waterbird habitats on private lands in the MAV, the Gulf Coast Prairies in Louisiana and Texas, and Gulf coastal wetlands of Mississippi and Alabama. The results of our evaluation will enhance our understanding of the influence of MBHI, other Farm Bill Conservation Initiative managed lands (e.g., Wetland Reserve Program), and selected agricultural working lands (e.g., </span><i>Oryza sativa</i><span> L. [Rice] fields in southern Louisiana and Texas) on wintering and migrating waterbirds. A proactive approach that uses science to evaluate governmental conservation programs is relevant and can inform development of meaningful public policy that likely will be needed for effective delivery of future conservation programs and to justify financial incentives paid to landowners to apply best management practices.</span></p>","language":"English","publisher":"Eagle Hill Institute","doi":"10.1656/058.013.0419","usgsCitation":"Davis, J., Webb, E.B., Kaminski, R.M., Barbour, P.J., and Vilella, F., 2014, Comprehensive framework for ecological assessment of the Migratory Bird Habitat Initiative following the Deepwater Horizon oil spill: Southeastern Naturalist, v. 13, no. 4, p. G66-G81, https://doi.org/10.1656/058.013.0419.","productDescription":"16 p.","startPage":"G66","endPage":"G81","ipdsId":"IP-053870","costCenters":[{"id":198,"text":"Coop Res Unit Atlanta","active":true,"usgs":true}],"links":[{"id":330330,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"13","issue":"4","publishingServiceCenter":{"id":8,"text":"Raleigh PSC"},"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5810c906e4b0f497e7973e89","contributors":{"authors":[{"text":"Davis, J. Brian","contributorId":172316,"corporation":false,"usgs":false,"family":"Davis","given":"J. Brian","affiliations":[{"id":17848,"text":"Mississippi State University","active":true,"usgs":false}],"preferred":false,"id":651854,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Webb, Elisabeth B. 0000-0003-3851-6056 ewebb@usgs.gov","orcid":"https://orcid.org/0000-0003-3851-6056","contributorId":3981,"corporation":false,"usgs":true,"family":"Webb","given":"Elisabeth","email":"ewebb@usgs.gov","middleInitial":"B.","affiliations":[{"id":199,"text":"Coop Res Unit Leetown","active":true,"usgs":true}],"preferred":true,"id":651855,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Kaminski, Richard M.","contributorId":78205,"corporation":false,"usgs":false,"family":"Kaminski","given":"Richard","email":"","middleInitial":"M.","affiliations":[{"id":17848,"text":"Mississippi State University","active":true,"usgs":false}],"preferred":false,"id":651856,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Barbour, Philip J.","contributorId":176199,"corporation":false,"usgs":false,"family":"Barbour","given":"Philip","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":651857,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Vilella, Francisco 0000-0003-1552-9989 fvilella@usgs.gov","orcid":"https://orcid.org/0000-0003-1552-9989","contributorId":171363,"corporation":false,"usgs":true,"family":"Vilella","given":"Francisco","email":"fvilella@usgs.gov","affiliations":[{"id":198,"text":"Coop Res Unit Atlanta","active":true,"usgs":true}],"preferred":true,"id":651848,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":70147001,"text":"70147001 - 2014 - Ecohydrology of dry regions: storage versus pulse soil water dynamics","interactions":[],"lastModifiedDate":"2015-04-24T14:17:53","indexId":"70147001","displayToPublicDate":"2014-12-01T00:00:00","publicationYear":"2014","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1478,"text":"Ecosystems","active":true,"publicationSubtype":{"id":10}},"title":"Ecohydrology of dry regions: storage versus pulse soil water dynamics","docAbstract":"<p><span>Although arid and semiarid regions are defined by low precipitation, the seasonal timing of temperature and precipitation can influence net primary production and plant functional type composition. The importance of precipitation seasonality is evident in semiarid areas of the western U.S., which comprise the Intermountain (IM) zone, a region that receives important winter precipitation and is dominated by woody plants and the Great Plains (GP), a region that receives primarily summer precipitation and is dominated by perennial grasses. Although these general relationships are well recognized, specific differences in water cycling between these regions have not been well characterized. We used a daily time step soil water simulation model and twenty sites from each region to analyze differences in soil water dynamics and ecosystem water balance. IM soil water patterns are characterized by storage of water during fall, winter, and spring resulting in relatively reliable available water during spring and early summer, particularly in deep soil layers. By contrast, GP soil water patterns are driven by pulse precipitation events during the warm season, resulting in fluctuating water availability in all soil layers. These contrasting patterns of soil water&mdash;storage versus pulse dynamics&mdash;explain important differences between the two regions. Notably, the storage dynamics of the IN sites increases water availability in deep soil layers, favoring the deeper rooted woody plants in that region, whereas the pulse dynamics of the Great Plains sites provide water primarily in surface layers, favoring the shallow-rooted grasses in that region. In addition, because water received when plants are either not active or only partially so is more vulnerable to evaporation and sublimation than water delivered during the growing season, IM ecosystems use a smaller fraction of precipitation for transpiration (47%) than GP ecosystems (49%). Recognizing the pulse-storage dichotomy in soil water regimes between the IM and GP regions may be useful for understanding the potential influence of climate changes on soil water patterns and resulting dominant plant functional groups in both regions.</span></p>","language":"English","publisher":"Springer","doi":"10.1007/s10021-014-9808-y","usgsCitation":"Lauenroth, W.K., Schlaepfer, D., and Bradford, J.B., 2014, Ecohydrology of dry regions: storage versus pulse soil water dynamics: Ecosystems, v. 17, no. 8, p. 1469-1479, https://doi.org/10.1007/s10021-014-9808-y.","productDescription":"11 p.","startPage":"1469","endPage":"1479","numberOfPages":"11","onlineOnly":"N","additionalOnlineFiles":"N","ipdsId":"IP-029594","costCenters":[{"id":568,"text":"Southwest Biological Science Center","active":true,"usgs":true}],"links":[{"id":299874,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"17","issue":"8","publishingServiceCenter":{"id":14,"text":"Menlo Park PSC"},"noUsgsAuthors":false,"publicationDate":"2014-10-01","publicationStatus":"PW","scienceBaseUri":"553b6943e4b0a658d79371b4","contributors":{"authors":[{"text":"Lauenroth, William K.","contributorId":80982,"corporation":false,"usgs":false,"family":"Lauenroth","given":"William","email":"","middleInitial":"K.","affiliations":[{"id":7098,"text":"University of Wyoming, Department of Botany, 1000 E. University Avenue, Laramie, WY 82071, USA","active":true,"usgs":false}],"preferred":false,"id":545573,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Schlaepfer, Daniel R.","contributorId":105189,"corporation":false,"usgs":false,"family":"Schlaepfer","given":"Daniel R.","affiliations":[{"id":7098,"text":"University of Wyoming, Department of Botany, 1000 E. University Avenue, Laramie, WY 82071, USA","active":true,"usgs":false}],"preferred":false,"id":545572,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Bradford, John B. 0000-0001-9257-6303 jbradford@usgs.gov","orcid":"https://orcid.org/0000-0001-9257-6303","contributorId":611,"corporation":false,"usgs":true,"family":"Bradford","given":"John","email":"jbradford@usgs.gov","middleInitial":"B.","affiliations":[{"id":568,"text":"Southwest Biological Science Center","active":true,"usgs":true}],"preferred":true,"id":545571,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70138723,"text":"70138723 - 2014 - Waterfowl habitat use and selection during the remigial moult period in the northern hemisphere","interactions":[],"lastModifiedDate":"2015-01-22T11:36:18","indexId":"70138723","displayToPublicDate":"2014-12-01T00:00:00","publicationYear":"2014","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3764,"text":"Wildfowl","onlineIssn":"2052-6458","printIssn":"0954-6324","active":true,"publicationSubtype":{"id":10}},"title":"Waterfowl habitat use and selection during the remigial moult period in the northern hemisphere","docAbstract":"<p><span>This paper reviews factors affecting site selection amongst waterfowl (Anatidae)&nbsp;during the flightless remigial moult, emphasising the roles of predation and food&nbsp;supply (especially protein and energy). The current literature suggests survival during&nbsp;flightless moult is at least as high as at other times of the annual cycle, but documented&nbsp;cases of predation of flightless waterfowl under particular conditions lead us to infer&nbsp;that habitat selection is generally highly effective in mitigating or avoiding predation.&nbsp;High energetic costs of feather replacement and specific amino-acid requirements for&nbsp;their construction imply adoption of special energetic and nutritional strategies at a&nbsp;time when flightlessness limits movements. Some waterfowl meet their energy needs&nbsp;from endogenous stores accumulated prior to remigial moult, others rely on&nbsp;exogenous supply, but this varies with species, age, reproductive status and site.&nbsp;Limited evidence suggests feather proteins are derived from endogenous and&nbsp;exogenous sources which may affect site selection. Remigial moult does not occur&nbsp;independently of other annual cycle events and is affected by reproductive investment&nbsp;and success. Hence, moult strategies are affected by age, sex and reproductive history,&nbsp;and may be influenced by the need to attain a certain internal state for the next stage&nbsp;in the annual cycle (e.g. autumn migration). We know little about habitat selection&nbsp;during moult and urge more research of this poorly known part of the annual cycle,&nbsp;with particular emphasis on identifying key concentrations and habitats for specific&nbsp;flyway populations and the effects of disturbance upon these. This knowledge will&nbsp;better inform conservation actions and management actions concerning waterfowl&nbsp;during moult and the habitats that they exploit.</span></p>","language":"English","publisher":"Wildfowl & Wetlands Trust","usgsCitation":"Fox, A.D., Flint, P.L., Hohman, W.L., and Savard, J.L., 2014, Waterfowl habitat use and selection during the remigial moult period in the northern hemisphere: Wildfowl, no. 4, p. 131-168.","productDescription":"38 p.","startPage":"131","endPage":"168","onlineOnly":"N","additionalOnlineFiles":"N","ipdsId":"IP-050972","costCenters":[{"id":117,"text":"Alaska Science Center Biology WTEB","active":true,"usgs":true}],"links":[{"id":297461,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":297434,"type":{"id":15,"text":"Index Page"},"url":"https://wildfowl.wwt.org.uk/index.php/wildfowl/article/view/2605/0"}],"issue":"4","publishingServiceCenter":{"id":12,"text":"Tacoma PSC"},"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"54dd2acfe4b08de9379b3219","contributors":{"authors":[{"text":"Fox, Anthony D.","contributorId":130960,"corporation":false,"usgs":false,"family":"Fox","given":"Anthony","email":"","middleInitial":"D.","affiliations":[{"id":7177,"text":"Dept of Bioscience, Aahus Univ, Denmark","active":true,"usgs":false}],"preferred":false,"id":538888,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Flint, Paul L. 0000-0002-8758-6993 pflint@usgs.gov","orcid":"https://orcid.org/0000-0002-8758-6993","contributorId":3284,"corporation":false,"usgs":true,"family":"Flint","given":"Paul","email":"pflint@usgs.gov","middleInitial":"L.","affiliations":[{"id":114,"text":"Alaska Science Center","active":true,"usgs":true},{"id":117,"text":"Alaska Science Center Biology WTEB","active":true,"usgs":true}],"preferred":true,"id":538887,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Hohman, William L.","contributorId":73141,"corporation":false,"usgs":false,"family":"Hohman","given":"William","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":538889,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Savard, Jean-Pierre L.","contributorId":101776,"corporation":false,"usgs":false,"family":"Savard","given":"Jean-Pierre","email":"","middleInitial":"L.","affiliations":[{"id":6962,"text":"Science and Technology Branch, Environment Canada","active":true,"usgs":false}],"preferred":false,"id":538890,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70124910,"text":"70124910 - 2014 - Unmanned aircraft systems (UAS) activities at the Department of the Interior","interactions":[],"lastModifiedDate":"2020-12-31T20:08:30.909493","indexId":"70124910","displayToPublicDate":"2014-12-01T00:00:00","publicationYear":"2014","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3052,"text":"Photogrammetric Engineering and Remote Sensing","active":true,"publicationSubtype":{"id":10}},"title":"Unmanned aircraft systems (UAS) activities at the Department of the Interior","docAbstract":"<p><span>The U.S. Department of the Interior (DOI) is responsible for protecting and managing the natural resources and heritage on almost 20% of the land in the United States. The DOI&rsquo;s mission requires access to remotely sensed data over vast lands, including areas that are remote and potentially dangerous to access. Unmanned Aircraft Systems (UAS) technology has the potential to enable the DOI to be a better steward of the land by: (1) Improving natural hazard forecasting and the analysis of the impacts. (2) Improving the understanding of climate change to better plan for likely impacts. (3) Developing precipitation and evaporation forecasting to better manage water resources. (4) Monitoring Arctic ice change and its impacts on ecosystems, coasts, and transportation. (5) Increasing safety and effectiveness of wildland fire management. (6) Enhancing search and rescue capabilities. (7) Broadening the abilities to monitor environmental or landscape conditions and changes. (8) Better understanding and protecting the Nation&rsquo;s ecosystems. The initial operational testing and evaluations performed by the DOI have proven that UAS technology can be used to support many of the Department&rsquo;s activities. UAS technology provides scientists a way to look longer, closer and more frequently at some of Earth&rsquo;s most remote areas&mdash;places that were previously too dangerous or expensive to monitor in detail. The flexibility of operations and relative low cost to purchase and operate Small Unmanned Aerial System (sUAS) enhances the ability to track long-term landscape and environmental change. The initial testing indicates the operational costs are approximately 10% of traditional manned aircraft. In addition, users can quickly assess landscape-altering events such as wildland fires, floods and volcanoes. UAS technology will allow the DOI to do more with less and in the process enhance the Department&rsquo;s ability to provide unbiased scientific information to help stakeholders make informed decisions. It will also provide a digital baseline record that can be archived and used when monitoring future events or conditions. One possible future scenario has scientists carrying sUAS into the field allowing quick deployment and operation to observe the environment or for emergency response. This scenario could also include a persistent monitoring capability provided by a UAS that can stay airborne over a small geographic area for days or weeks, or possibly longer. While the DOI focus is on sUAS, the Department recognizes that larger UAS systems will also play a role in meeting its mission. The Department anticipates meeting long-duration or specialized acquisition commitments, such as state or national aerial photography, by collaboration with other agencies or through commercial contracts. Even though the DOI continues to evaluate UAS and sensor technology to meet the Department&rsquo;s mission, some of its bureaus are already moving towards an operational capability. The authors fully anticipate that by 2020 UAS will emerge as one of the primary platforms for DOI remote sensing applications.</span></p>","language":"English","publisher":"ASPRS","usgsCitation":"Quirk, B.K., and Hutt, M.E., 2014, Unmanned aircraft systems (UAS) activities at the Department of the Interior: Photogrammetric Engineering and Remote Sensing, v. 80, no. 12, p. 1089-1095.","productDescription":"7 p.","startPage":"1089","endPage":"1095","onlineOnly":"N","additionalOnlineFiles":"N","ipdsId":"IP-057845","costCenters":[{"id":498,"text":"Office of Land Remote Sensing (Geography)","active":true,"usgs":true}],"links":[{"id":324952,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"80","issue":"12","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5780cec1e4b08116168223f4","contributors":{"authors":[{"text":"Quirk, Bruce K. quirk@usgs.gov","contributorId":4285,"corporation":false,"usgs":true,"family":"Quirk","given":"Bruce","email":"quirk@usgs.gov","middleInitial":"K.","affiliations":[],"preferred":true,"id":519471,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hutt, Michael E. 0000-0002-3869-6096 mehutt@usgs.gov","orcid":"https://orcid.org/0000-0002-3869-6096","contributorId":5037,"corporation":false,"usgs":true,"family":"Hutt","given":"Michael","email":"mehutt@usgs.gov","middleInitial":"E.","affiliations":[],"preferred":true,"id":641982,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70137759,"text":"70137759 - 2014 - Book review: Implementing the Endangered Species Act on the Platte Basin water commons","interactions":[],"lastModifiedDate":"2018-01-05T11:17:43","indexId":"70137759","displayToPublicDate":"2014-12-01T00:00:00","publicationYear":"2014","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3580,"text":"The Prairie Naturalist","active":true,"publicationSubtype":{"id":10}},"title":"Book review: Implementing the Endangered Species Act on the Platte Basin water commons","docAbstract":"<p>The Platte River is a unique midcontinent ecosystem that is world-renowned for its natural resources, particularly the spectacular spring concentrations of migratory birds, such as sandhill cranes (<i>Grus canadensis</i>), ducks, and geese. The Platte River basin also provides habitat for four federally listed endangered or threatened species&mdash;interior least tern (<i>Sternula antillarum athalassos</i>), piping plover (<i>Charadrius melodus</i>), whooping crane (<i>G. americana</i>), and pallid sturgeon (<i>Scaphirhynchus albus</i>)&mdash;that require specific hydrological conditions in order for habitat to be suitable. Flows on the Platte River are subject to regulation by a number of dams, and it is heavily relied upon for irrigation in Colorado, Wyoming, and Nebraska. Accordingly, it also has become a political battleground for the simple reason that the demand for water exceeds supply. David Freeman&rsquo;s book takes a detailed look at water-use issues on the Platte River, focusing on how implementation of the Endangered Species Act influences decision-making about water allocations.&nbsp;</p>\n<p>Review info:&nbsp;<i>Implementing the Endangered Species Act on the Platte Basin Water Commons.</i>&nbsp;By David M. Freeman, 2010. ISBN: 978-1607320548, 483 pp.</p>","language":"English","publisher":"Great Plains Natural Science Society","usgsCitation":"Sherfy, M.H., 2014, Book review: Implementing the Endangered Species Act on the Platte Basin water commons: The Prairie Naturalist, v. 46, no. 1, p. 115-116.","productDescription":"2 p.","startPage":"115","endPage":"116","onlineOnly":"N","additionalOnlineFiles":"N","ipdsId":"IP-059916","costCenters":[{"id":480,"text":"Northern Prairie Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":297227,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":297137,"type":{"id":15,"text":"Index Page"},"url":"https://www.sdstate.edu/nrm/organizations/gpnss/tpn/2014-volume-46.cfm"}],"volume":"46","issue":"1","publishingServiceCenter":{"id":4,"text":"Rolla PSC"},"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"54dd2a5be4b08de9379b3006","contributors":{"authors":[{"text":"Sherfy, Mark H. 0000-0003-3016-4105 msherfy@usgs.gov","orcid":"https://orcid.org/0000-0003-3016-4105","contributorId":125,"corporation":false,"usgs":true,"family":"Sherfy","given":"Mark","email":"msherfy@usgs.gov","middleInitial":"H.","affiliations":[{"id":480,"text":"Northern Prairie Wildlife Research Center","active":true,"usgs":true}],"preferred":true,"id":538085,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70142989,"text":"70142989 - 2014 - Pollutant sensitivity of the endangered Tar River Spinymussel as assessed by single chemical and effluent toxicity tests","interactions":[],"lastModifiedDate":"2017-05-23T12:35:28","indexId":"70142989","displayToPublicDate":"2014-12-01T00:00:00","publicationYear":"2014","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":1,"text":"Federal Government Series"},"title":"Pollutant sensitivity of the endangered Tar River Spinymussel as assessed by single chemical and effluent toxicity tests","docAbstract":"<p>The federally endangered Tar River spinymussel (Elliptio steinstansana) is endemic to the Tar River and Neuse River systems in North Carolina. The extent to which water quality limits Tar River spinymussels’ recovery is important to establish, and one aspect of that is understanding the species’ pollutant sensitivity. The primary objectives of this study were to 1) develop captive propagation and culture methods for Tar River spinymussels; 2) determine the pollutant sensitivity of captively propagated Tar River spinymussels; 3) examine the utility of the non-endangered yellow lance (Elliptio lanceolata), yellow lampmussel (Lampsilis cariosa) and notched rainbow (Villosa constricta) as surrogates for the Tar River spinymussels’ chemical sensitivity; 4) develop a 7-d method for conducting effluent toxicity tests starting with newly transformed mussels; 5) assess the toxicity of municipal wastewater effluents discharged into the Tar River spinymussels’ current and historic habitat; and, 6) evaluate the protection afforded by existing effluent toxicity test requirements.</p>","language":"English","publisher":"U.S Fish and Wildlife Service ","usgsCitation":"Augspurger, T., Wang, N., Kunz, J.L., and Ingersoll, C.G., 2014, Pollutant sensitivity of the endangered Tar River Spinymussel as assessed by single chemical and effluent toxicity tests, viii, 46 p. .","productDescription":"viii, 46 p. ","ipdsId":"IP-063796","costCenters":[{"id":192,"text":"Columbia Environmental Research Center","active":true,"usgs":true}],"links":[{"id":328417,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":298561,"type":{"id":11,"text":"Document"},"url":"https://www.fws.gov/raleigh/pdfs/FinalP_Sensi_TRS.pdf"}],"publishingServiceCenter":{"id":4,"text":"Rolla PSC"},"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"57d28baee4b0571647d0f93d","contributors":{"authors":[{"text":"Augspurger, Thomas P.","contributorId":139666,"corporation":false,"usgs":false,"family":"Augspurger","given":"Thomas P.","affiliations":[{"id":12872,"text":"U.S. Fish and Wildlife Service, 551-F Pylon Drive, Raleigh, NC","active":true,"usgs":false}],"preferred":false,"id":542384,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Wang, Ning 0000-0002-2846-3352 nwang@usgs.gov","orcid":"https://orcid.org/0000-0002-2846-3352","contributorId":2818,"corporation":false,"usgs":true,"family":"Wang","given":"Ning","email":"nwang@usgs.gov","affiliations":[{"id":192,"text":"Columbia Environmental Research Center","active":true,"usgs":true}],"preferred":true,"id":542385,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Kunz, James L. 0000-0002-1027-158X jkunz@usgs.gov","orcid":"https://orcid.org/0000-0002-1027-158X","contributorId":3309,"corporation":false,"usgs":true,"family":"Kunz","given":"James","email":"jkunz@usgs.gov","middleInitial":"L.","affiliations":[{"id":192,"text":"Columbia Environmental Research Center","active":true,"usgs":true}],"preferred":true,"id":542386,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Ingersoll, Christopher G. 0000-0003-4531-5949 cingersoll@usgs.gov","orcid":"https://orcid.org/0000-0003-4531-5949","contributorId":2071,"corporation":false,"usgs":true,"family":"Ingersoll","given":"Christopher","email":"cingersoll@usgs.gov","middleInitial":"G.","affiliations":[{"id":192,"text":"Columbia Environmental Research Center","active":true,"usgs":true}],"preferred":true,"id":542383,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70138724,"text":"70138724 - 2014 - Drivers of waterfowl population dynamics: from teal to swans","interactions":[],"lastModifiedDate":"2015-01-21T15:12:25","indexId":"70138724","displayToPublicDate":"2014-12-01T00:00:00","publicationYear":"2014","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3764,"text":"Wildfowl","onlineIssn":"2052-6458","printIssn":"0954-6324","active":true,"publicationSubtype":{"id":10}},"title":"Drivers of waterfowl population dynamics: from teal to swans","docAbstract":"<p><span>Waterfowl</span><span>&nbsp;are among the best studied and most extensively monitored species in the&nbsp;world. Given their global importance for sport and subsistence hunting, viewing and&nbsp;ecosystem functioning, great effort has been devoted since the middle part&nbsp;</span><span>of</span><span>&nbsp;the&nbsp;20th century&nbsp;</span><span>to</span><span>&nbsp;understanding both the environmental and demographic mechanisms&nbsp;that influence&nbsp;</span><span>waterfowl</span><span>&nbsp;</span><span>population</span><span>&nbsp;and community dynamics. Here we use&nbsp;comparative approaches&nbsp;</span><span>to</span><span>&nbsp;summarise and contrast our understanding&nbsp;</span><span>of</span><span>waterfowl</span><span>&nbsp;</span><span>population</span><span>&nbsp;dynamics across species as short-lived as the&nbsp;</span><span>teal</span><span>&nbsp;Anas discors and A.crecca&nbsp;</span><span>to</span><span>&nbsp;those such as the swans Cygnus sp. which have long life-spans. Specifically, we focus&nbsp;on&nbsp;</span><span>population</span><span>&nbsp;responses&nbsp;</span><span>to</span><span>&nbsp;vital rate perturbations across life history strategies,&nbsp;discuss bottom-up and top-down responses&nbsp;</span><span>of</span><span>&nbsp;</span><span>waterfowl</span><span>populations&nbsp;</span><span>to</span><span>&nbsp;global&nbsp;change, and summarise our current understanding&nbsp;</span><span>of</span><span>&nbsp;density dependence across&nbsp;</span><span>waterfowl</span><span>&nbsp;species. We close by identifying research needs and highlight ways&nbsp;</span><span>to</span><span>&nbsp;overcome the challenges&nbsp;</span><span>of</span><span>&nbsp;sustainably managing&nbsp;</span><span>waterfowl</span><span>&nbsp;populations in the 21st&nbsp;century.</span></p>","language":"English","publisher":"Wildfowl and Wetlands Trust","usgsCitation":"Koons, D.N., Gunnarsson, G., Schmutz, J.A., and Rotella, J.J., 2014, Drivers of waterfowl population dynamics: from teal to swans: Wildfowl, no. Special Issue 4, p. 169-191.","productDescription":"23 p.","startPage":"169","endPage":"191","numberOfPages":"23","onlineOnly":"N","additionalOnlineFiles":"N","ipdsId":"IP-052740","costCenters":[{"id":117,"text":"Alaska Science Center Biology WTEB","active":true,"usgs":true}],"links":[{"id":297447,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":297435,"type":{"id":15,"text":"Index Page"},"url":"https://wildfowl.wwt.org.uk/index.php/wildfowl/article/view/2606"}],"issue":"Special Issue 4","publishingServiceCenter":{"id":12,"text":"Tacoma PSC"},"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"54dd2a6de4b08de9379b3057","contributors":{"authors":[{"text":"Koons, David N.","contributorId":28137,"corporation":false,"usgs":false,"family":"Koons","given":"David","email":"","middleInitial":"N.","affiliations":[{"id":6621,"text":"Colorado State University","active":true,"usgs":false}],"preferred":false,"id":538939,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Gunnarsson, Gunnar","contributorId":138846,"corporation":false,"usgs":false,"family":"Gunnarsson","given":"Gunnar","email":"","affiliations":[],"preferred":false,"id":538940,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Schmutz, Joel A. 0000-0002-6516-0836 jschmutz@usgs.gov","orcid":"https://orcid.org/0000-0002-6516-0836","contributorId":1805,"corporation":false,"usgs":true,"family":"Schmutz","given":"Joel","email":"jschmutz@usgs.gov","middleInitial":"A.","affiliations":[{"id":114,"text":"Alaska Science Center","active":true,"usgs":true},{"id":117,"text":"Alaska Science Center Biology WTEB","active":true,"usgs":true}],"preferred":true,"id":538891,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Rotella, Jay J.","contributorId":37271,"corporation":false,"usgs":false,"family":"Rotella","given":"Jay","email":"","middleInitial":"J.","affiliations":[{"id":5098,"text":"Department of Ecology, Montana State University","active":true,"usgs":false}],"preferred":false,"id":538941,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70135094,"text":"70135094 - 2014 - Geomorphological Fieldwork","interactions":[],"lastModifiedDate":"2015-11-02T15:49:17","indexId":"70135094","displayToPublicDate":"2014-12-01T00:00:00","publicationYear":"2014","noYear":false,"publicationType":{"id":4,"text":"Book"},"publicationSubtype":{"id":13,"text":"Handbook"},"title":"Geomorphological Fieldwork","docAbstract":"<p>Geomorphological Fieldwork addresses a topic that always remains popular within the geosciences and environmental science. More specifically, the volume conveys a growing legacy of field-based learning for young geomorphologists that can be used as a student book for field-based university courses and postgraduate research requiring fieldwork or field schools. The editors have much experience of field-based learning within geomorphology and extend this to physical geography. The topics covered are relevant to basic geomorphology as well as applied approaches in environmental and cultural geomorphology. The book integrates a physical-human approach to geography, but focuses on physical geography and geomorphology from an integrated field-based geoscience perspective.</p>","language":"English","publisher":"Elsevier","collaboration":"None","usgsCitation":"Thornbush, M.J., Allen, C.D., and Fitzpatrick, F., 2014, Geomorphological Fieldwork (1), v. 18, 286 p.","productDescription":"286 p.","onlineOnly":"N","additionalOnlineFiles":"N","ipdsId":"IP-060392","costCenters":[{"id":677,"text":"Wisconsin Water Science Center","active":true,"usgs":true}],"links":[{"id":310964,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":296500,"type":{"id":15,"text":"Index Page"},"url":"https://store.elsevier.com/product.jsp?isbn=9780444634023&_requestid=464841"}],"volume":"18","edition":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"56389754e4b0d6133fe72fb7","contributors":{"authors":[{"text":"Thornbush, Mary J","contributorId":127795,"corporation":false,"usgs":false,"family":"Thornbush","given":"Mary","email":"","middleInitial":"J","affiliations":[{"id":7157,"text":"University of Birmingham","active":true,"usgs":false}],"preferred":false,"id":526796,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Allen, Casey D","contributorId":127796,"corporation":false,"usgs":false,"family":"Allen","given":"Casey","email":"","middleInitial":"D","affiliations":[{"id":7158,"text":"Unversity of Colorado Denver","active":true,"usgs":false}],"preferred":false,"id":526797,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Fitzpatrick, Faith A. 0000-0002-9748-7075 fafitzpa@usgs.gov","orcid":"https://orcid.org/0000-0002-9748-7075","contributorId":127794,"corporation":false,"usgs":true,"family":"Fitzpatrick","given":"Faith A.","email":"fafitzpa@usgs.gov","affiliations":[{"id":677,"text":"Wisconsin Water Science Center","active":true,"usgs":true}],"preferred":false,"id":526795,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70139633,"text":"70139633 - 2014 - Water and food acquisition and their consequences for life history and metabolism of North American tortoises","interactions":[],"lastModifiedDate":"2020-07-03T15:26:08.56516","indexId":"70139633","displayToPublicDate":"2014-12-01T00:00:00","publicationYear":"2014","noYear":false,"publicationType":{"id":5,"text":"Book chapter"},"publicationSubtype":{"id":24,"text":"Book Chapter"},"chapter":"10","title":"Water and food acquisition and their consequences for life history and metabolism of North American tortoises","docAbstract":"<p>No abstract available.</p>","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Biology and conservation of North American tortoises","largerWorkSubtype":{"id":15,"text":"Monograph"},"language":"English","publisher":"Johns Hopkins University Press","publisherLocation":"Baltimore, MD","usgsCitation":"Esque, T., Drake, K.K., and Nussear, K.E., 2014, Water and food acquisition and their consequences for life history and metabolism of North American tortoises, chap. 10 <i>of</i> Biology and conservation of North American tortoises, p. 85-95.","productDescription":"11 p.","startPage":"85","endPage":"95","numberOfPages":"11","onlineOnly":"N","additionalOnlineFiles":"N","ipdsId":"IP-045684","costCenters":[{"id":651,"text":"Western Ecological Research Center","active":true,"usgs":true}],"links":[{"id":298331,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":297606,"type":{"id":15,"text":"Index Page"},"url":"https://muse.jhu.edu/books/9781421413785"}],"otherGeospatial":"North America","publishingServiceCenter":{"id":1,"text":"Sacramento PSC"},"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"54faddbce4b02419550db6e8","contributors":{"authors":[{"text":"Esque, Todd C. tesque@usgs.gov","contributorId":138964,"corporation":false,"usgs":true,"family":"Esque","given":"Todd C.","email":"tesque@usgs.gov","affiliations":[{"id":651,"text":"Western Ecological Research Center","active":true,"usgs":true}],"preferred":false,"id":539469,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Drake, K. Kristina 0000-0003-0711-7634 kdrake@usgs.gov","orcid":"https://orcid.org/0000-0003-0711-7634","contributorId":3799,"corporation":false,"usgs":true,"family":"Drake","given":"K.","email":"kdrake@usgs.gov","middleInitial":"Kristina","affiliations":[{"id":651,"text":"Western Ecological Research Center","active":true,"usgs":true}],"preferred":true,"id":539467,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Nussear, Kenneth E. knussear@usgs.gov","contributorId":2695,"corporation":false,"usgs":true,"family":"Nussear","given":"Kenneth","email":"knussear@usgs.gov","middleInitial":"E.","affiliations":[{"id":651,"text":"Western Ecological Research Center","active":true,"usgs":true}],"preferred":true,"id":539468,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70138810,"text":"70138810 - 2014 - Contaminants of emerging concern in fresh leachate from landfills in the conterminous United States","interactions":[],"lastModifiedDate":"2021-05-28T14:04:02.346801","indexId":"70138810","displayToPublicDate":"2014-12-01T00:00:00","publicationYear":"2014","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1566,"text":"Environmental Science: Processes and Impacts","active":true,"publicationSubtype":{"id":10}},"title":"Contaminants of emerging concern in fresh leachate from landfills in the conterminous United States","docAbstract":"<p><span>To better understand the composition of contaminants of emerging concern (CECs) in landfill leachate, fresh leachate from 19 landfills was sampled across the United States during 2011. The sampled network included 12 municipal and 7 private landfills with varying landfill waste compositions, geographic and climatic settings, ages of waste, waste loads, and leachate production. A total of 129 out of 202 CECs were detected during this study, including 62 prescription pharmaceuticals, 23 industrial chemicals, 18 nonprescription pharmaceuticals, 16 household chemicals, 6 steroid hormones, and 4 plant/animal sterols. CECs were detected in every leachate sample, with the total number of detected CECs in samples ranging from 6 to 82 (median = 31). Bisphenol A (BPA), cotinine, and&nbsp;</span><i>N</i><span>,</span><i>N</i><span>-diethyltoluamide (DEET) were the most frequently detected CECs, being found in 95% of the leachate samples, followed by lidocaine (89%) and camphor (84%). Other frequently detected CECs included benzophenone, naphthalene, and amphetamine, each detected in 79% of the leachate samples. CEC concentrations spanned six orders of magnitude, ranging from ng L</span><small><sup>&minus;1</sup></small><span>&nbsp;to mg L</span><small><sup>&minus;1</sup></small><span>. Industrial and household chemicals were measured in the greatest concentrations, composing more than 82% of the total measured CEC concentrations. Maximum concentrations for three household and industrial chemicals,&nbsp;</span><i>para</i><span>-cresol (7</span><img src=\"http://www.rsc.org/images/entities/char_2009.gif\" border=\"0\" alt=\" \" /><span>020</span><img src=\"http://www.rsc.org/images/entities/char_2009.gif\" border=\"0\" alt=\" \" /><span>000 ng L</span><small><sup>&minus;1</sup></small><span>), BPA (6</span><img src=\"http://www.rsc.org/images/entities/char_2009.gif\" border=\"0\" alt=\" \" /><span>380</span><img src=\"http://www.rsc.org/images/entities/char_2009.gif\" border=\"0\" alt=\" \" /><span>000 ng L</span><small><sup>&minus;1</sup></small><span>), and phenol (1</span><img src=\"http://www.rsc.org/images/entities/char_2009.gif\" border=\"0\" alt=\" \" /><span>550</span><img src=\"http://www.rsc.org/images/entities/char_2009.gif\" border=\"0\" alt=\" \" /><span>000 ng L</span><small><sup>&minus;1</sup></small><span>), were the largest measured, with these CECs composing 70% of the total measured CEC concentrations. Nonprescription pharmaceuticals represented 12%, plant/animal sterols 4%, prescription pharmaceuticals 1%, and steroid hormones &lt;1% of the total measured CEC concentrations. Leachate from landfills in areas receiving greater amounts of precipitation had greater frequencies of CEC detections and concentrations in leachate than landfills receiving less precipitation.</span></p>","language":"English","publisher":"Royal Society of Chemistry","doi":"10.1039/C4EM00124A","usgsCitation":"Masoner, J.R., Kolpin, D.W., Furlong, E.T., Cozzarelli, I.M., Gray, J.L., and Schwab, E.A., 2014, Contaminants of emerging concern in fresh leachate from landfills in the conterminous United States: Environmental Science: Processes and Impacts, v. 16, p. 2335-2354, https://doi.org/10.1039/C4EM00124A.","productDescription":"20 p.","startPage":"2335","endPage":"2354","onlineOnly":"N","additionalOnlineFiles":"N","ipdsId":"IP-057814","costCenters":[{"id":452,"text":"National Water Quality Laboratory","active":true,"usgs":true},{"id":516,"text":"Oklahoma Water Science Center","active":true,"usgs":true},{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":297457,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -97.18505859374999,\n              25.97779895546436\n            ],\n            [\n              -97.42675781249999,\n              25.878994400196202\n            ],\n            [\n              -98.2177734375,\n              26.115985925333536\n            ],\n            [\n              -99.0966796875,\n              26.47057302237511\n            ],\n            [\n              -99.580078125,\n              27.625140335093324\n            ],\n            [\n              -100.283203125,\n              28.265682390146477\n            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easchwab@usgs.gov","contributorId":4222,"corporation":false,"usgs":true,"family":"Schwab","given":"Eric","email":"easchwab@usgs.gov","middleInitial":"A.","affiliations":[{"id":503,"text":"Office of Water Quality","active":true,"usgs":true},{"id":143,"text":"Branch of Quality Systems","active":true,"usgs":true}],"preferred":true,"id":538917,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}}
,{"id":70129182,"text":"70129182 - 2014 - Eruptions at Lone Star geyser, Yellowstone National Park, USA: 2. Constraints on subsurface dynamics","interactions":[],"lastModifiedDate":"2019-03-14T08:19:45","indexId":"70129182","displayToPublicDate":"2014-12-01T00:00:00","publicationYear":"2014","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2314,"text":"Journal of Geophysical Research B: Solid Earth","active":true,"publicationSubtype":{"id":10}},"title":"Eruptions at Lone Star geyser, Yellowstone National Park, USA: 2. Constraints on subsurface dynamics","docAbstract":"<p><span>We use seismic, tilt, lidar, thermal, and gravity data from 32 consecutive eruption cycles of Lone Star geyser in Yellowstone National Park to identify key subsurface processes throughout the geyser's eruption cycle. Previously, we described measurements and analyses associated with the geyser's erupting jet dynamics. Here we show that seismicity is dominated by hydrothermal tremor (~5&ndash;40&thinsp;Hz) attributed to the nucleation and/or collapse of vapor bubbles. Water discharge during eruption preplay triggers high-amplitude tremor pulses from a back azimuth aligned with the geyser cone, but during the rest of the eruption cycle it is shifted to the east-northeast. Moreover, ~4&thinsp;min period ground surface displacements recur every 26&thinsp;&plusmn;&thinsp;8&thinsp;min and are uncorrelated with the eruption cycle. Based on these observations, we conclude that (1) the dynamical behavior of the geyser is controlled by the thermo-mechanical coupling between the geyser conduit and a laterally offset reservoir periodically filled with a highly compressible two-phase mixture, (2) liquid and steam slugs periodically ascend into the shallow crust near the geyser system inducing detectable deformation, (3) eruptions occur when the pressure decrease associated with overflow from geyser conduit during preplay triggers an unstable feedback between vapor generation (cavitation) and mass discharge, and (4) flow choking at a constriction in the conduit arrests the runaway process and increases the saturated vapor pressure in the reservoir by a factor of ~10 during eruptions.</span></p>","language":"English","publisher":"AGU Publications","doi":"10.1002/2014JB011526","usgsCitation":"Vandemeulebrouck, J., Sohn, R.A., Rudolph, M., Hurwitz, S., Manga, M., Johnston, M.J., Soule, S., McPhee, D., Glen, J., Karlstrom, L., and Murphy, F., 2014, Eruptions at Lone Star geyser, Yellowstone National Park, USA: 2. Constraints on subsurface dynamics: Journal of Geophysical Research B: Solid Earth, v. 119, no. 12, p. 8688-8707, https://doi.org/10.1002/2014JB011526.","productDescription":"20 p.","startPage":"8688","endPage":"8707","onlineOnly":"N","additionalOnlineFiles":"N","ipdsId":"IP-060505","costCenters":[{"id":438,"text":"National Research Program - Western Branch","active":true,"usgs":true},{"id":615,"text":"Volcano Hazards Program","active":true,"usgs":true}],"links":[{"id":472627,"rank":0,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1002/2014jb011526","text":"Publisher Index Page"},{"id":325073,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Wyoming","otherGeospatial":"Lone Star geyser, Yellowstone National Park","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -111.05804443359375,\n              44.39454219215587\n            ],\n            [\n              -111.05804443359375,\n              44.69013547299005\n            ],\n            [\n              -110.57189941406249,\n              44.69013547299005\n            ],\n            [\n              -110.57189941406249,\n              44.39454219215587\n            ],\n            [\n              -111.05804443359375,\n              44.39454219215587\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"119","issue":"12","noUsgsAuthors":false,"publicationDate":"2014-12-05","publicationStatus":"PW","scienceBaseUri":"579dcfdee4b0589fa1cbd7e5","contributors":{"authors":[{"text":"Vandemeulebrouck, Jean","contributorId":101973,"corporation":false,"usgs":true,"family":"Vandemeulebrouck","given":"Jean","email":"","affiliations":[],"preferred":false,"id":519816,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Sohn, Robert A.","contributorId":37258,"corporation":false,"usgs":true,"family":"Sohn","given":"Robert","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":519813,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Rudolph, Maxwell L.","contributorId":42122,"corporation":false,"usgs":true,"family":"Rudolph","given":"Maxwell L.","affiliations":[],"preferred":false,"id":519814,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Hurwitz, Shaul 0000-0001-5142-6886 shaulh@usgs.gov","orcid":"https://orcid.org/0000-0001-5142-6886","contributorId":2169,"corporation":false,"usgs":true,"family":"Hurwitz","given":"Shaul","email":"shaulh@usgs.gov","affiliations":[{"id":438,"text":"National Research Program - Western Branch","active":true,"usgs":true},{"id":617,"text":"Volcano Science Center","active":true,"usgs":true}],"preferred":true,"id":519809,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Manga, Michael","contributorId":66559,"corporation":false,"usgs":true,"family":"Manga","given":"Michael","affiliations":[],"preferred":false,"id":519815,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Johnston, Malcolm J.S.","contributorId":105171,"corporation":false,"usgs":true,"family":"Johnston","given":"Malcolm","email":"","middleInitial":"J.S.","affiliations":[],"preferred":false,"id":519807,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Soule, S. Adam","contributorId":116966,"corporation":false,"usgs":true,"family":"Soule","given":"S. Adam","affiliations":[],"preferred":false,"id":519817,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"McPhee, Darcy 0000-0002-5177-3068 dmcphee@usgs.gov","orcid":"https://orcid.org/0000-0002-5177-3068","contributorId":2621,"corporation":false,"usgs":true,"family":"McPhee","given":"Darcy","email":"dmcphee@usgs.gov","affiliations":[{"id":412,"text":"National Cooperative Geologic Mapping Program","active":false,"usgs":true}],"preferred":true,"id":519810,"contributorType":{"id":1,"text":"Authors"},"rank":8},{"text":"Glen, Jonathan M. G.","contributorId":45756,"corporation":false,"usgs":true,"family":"Glen","given":"Jonathan M. G.","affiliations":[],"preferred":false,"id":519808,"contributorType":{"id":1,"text":"Authors"},"rank":9},{"text":"Karlstrom, Leif","contributorId":23048,"corporation":false,"usgs":false,"family":"Karlstrom","given":"Leif","affiliations":[],"preferred":false,"id":519812,"contributorType":{"id":1,"text":"Authors"},"rank":10},{"text":"Murphy, Fred fmurphy@usgs.gov","contributorId":4572,"corporation":false,"usgs":true,"family":"Murphy","given":"Fred","email":"fmurphy@usgs.gov","affiliations":[{"id":438,"text":"National Research Program - Western Branch","active":true,"usgs":true}],"preferred":true,"id":519811,"contributorType":{"id":1,"text":"Authors"},"rank":11}]}}
,{"id":70196600,"text":"70196600 - 2014 - Layered hydrothermal barite-sulfide mound field, East Diamante Caldera, Mariana volcanic arc","interactions":[],"lastModifiedDate":"2018-06-27T15:58:46","indexId":"70196600","displayToPublicDate":"2014-12-01T00:00:00","publicationYear":"2014","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1472,"text":"Economic Geology","active":true,"publicationSubtype":{"id":10}},"title":"Layered hydrothermal barite-sulfide mound field, East Diamante Caldera, Mariana volcanic arc","docAbstract":"<p>East Diamante is a submarine volcano in the southern Mariana arc that is host to a complex caldera ~5 × 10 km (elongated ENE-WSW) that is breached along its northern and southwestern sectors. A large field of barite-sulfide mounds was discovered in June 2009 and revisited in July 2010 with the R/V<span>&nbsp;</span><i>Natsushima</i>, using the ROV<span>&nbsp;</span><i>Hyper-Dolphin</i>. The mound field occurs on the northeast flank of a cluster of resurgent dacite domes in the central caldera, near an active black smoker vent field. A<span>&nbsp;</span><sup>40</sup>Ar/<sup>39</sup>Ar age of 20,000 ± 4000 years was obtained from a dacite sample. The mound field is aligned along a series of fractures and extends for more than 180 m east-west and &gt;120 m north-south. Individual mounds are typically 1 to 3 m tall and 0.5 to 2 m wide, with lengths from about 3 to 8 m. The mounds are dominated by barite + sphalerite layers with the margins of each layer composed of barite with disseminated sulfides. Rare, inactive spires and chimneys sit atop some mounds and also occur as clusters away from the mounds. Iron and Mn oxides are currently forming small (&lt;1-m diam, ~0.5-m tall) knolls on the top surface of some of the barite-sulfide mounds and may also drape their flanks. Both diffusely and focused fluids emanate from the small oxide knolls. Radiometric ages of the layered barite-sulfide mounds and chimneys vary from ~3,920 to 3,350 years. One layer, from an outcrop of 10- to 100-cm-thick Cu-rich layers, is notably younger with an age of 2,180 years. The Fe-Mn oxides were &lt;5 years old at the time of collection in 2009.</p><p>Most mound, chimney, and layered outcrop samples are dominated by barite, silica, and sphalerite; other sulfides, in decreasing order of abundance, are galena, chalcopyrite, and rare pyrite. Anglesite, cerussite, and unidentified Pb oxychloride and Pb phosphate minerals occur as late-stage interstitial phases. The samples contain high Zn (up to 23 wt %), Pb (to 16 wt %), Ag (to 487 ppm), and Au (to 19 ppm) contents. Some layered outcrop samples are dominated by chalcopyrite resulting in ≤4.78 wt % Cu in a bulk sample (28 wt % for a single lens), with a mean of 0.28 wt % for other samples. Other significant metal enrichments are Sb (to 1,320 ppm), Cd (to 1,150 ppm), and Hg (to 55 ppm).</p><p>The East Diamante mound field has a unique set of characteristics compared to other hydrothermal sites in the Mariana arc and elsewhere. The geochemical differences may predominantly reflect the distribution of fractures and faults and consequently the rock/water ratio, temperature of the fluid in the upper parts of the circulation system, and extensive and prolonged mixing with seawater. The location of mineralization is controlled by fractures. Following resurgent doming within the caldera, mineralization resulted from focused flow along small segments of linear fractures rather than from a point source, typical of hydrothermal chimney fields. Based on the mineral assemblage, the maximum fluid temperatures were ~260°C, near the boiling point for the water depths of the mound field (367–406 m). Lateral fluid flow within the mounds precipitated interstitial sphalerite, silica, and Pb minerals within a network of barite with disseminated sulfides; silica was the final phase to precipitate. The current low-temperature precipitation of Fe and Mn oxides and silica may represent rejuvenation of the system.</p>","language":"English","publisher":"Society of Economic Geologists","doi":"10.2113/econgeo.109.8.2179","usgsCitation":"Hein, J.R., de Ronde, C.E., Koski, R.A., Ditchburn, R.G., Mizell, K., Tamura, Y., Stern, R.J., Conrad, T., Ishizuka, O., and Leybourne, M.I., 2014, Layered hydrothermal barite-sulfide mound field, East Diamante Caldera, Mariana volcanic arc: Economic Geology, v. 109, no. 8, p. 2179-2206, https://doi.org/10.2113/econgeo.109.8.2179.","productDescription":"28 p.","startPage":"2179","endPage":"2206","ipdsId":"IP-049293","costCenters":[{"id":520,"text":"Pacific Coastal and Marine Science Center","active":true,"usgs":true}],"links":[{"id":353613,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"109","issue":"8","noUsgsAuthors":false,"publicationDate":"2014-10-30","publicationStatus":"PW","scienceBaseUri":"5afeed73e4b0da30c1bfc708","contributors":{"authors":[{"text":"Hein, James R. 0000-0002-5321-899X jhein@usgs.gov","orcid":"https://orcid.org/0000-0002-5321-899X","contributorId":2828,"corporation":false,"usgs":true,"family":"Hein","given":"James","email":"jhein@usgs.gov","middleInitial":"R.","affiliations":[{"id":520,"text":"Pacific Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":false,"id":733756,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"de Ronde, Cornel E. J.","contributorId":98109,"corporation":false,"usgs":true,"family":"de Ronde","given":"Cornel","email":"","middleInitial":"E. J.","affiliations":[],"preferred":false,"id":733757,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Koski, Randolph A. rkoski@usgs.gov","contributorId":2949,"corporation":false,"usgs":true,"family":"Koski","given":"Randolph","email":"rkoski@usgs.gov","middleInitial":"A.","affiliations":[],"preferred":true,"id":733758,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Ditchburn, Robert G.","contributorId":204359,"corporation":false,"usgs":false,"family":"Ditchburn","given":"Robert","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":733759,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Mizell, Kira 0000-0002-5066-787X kmizell@usgs.gov","orcid":"https://orcid.org/0000-0002-5066-787X","contributorId":4914,"corporation":false,"usgs":true,"family":"Mizell","given":"Kira","email":"kmizell@usgs.gov","affiliations":[{"id":520,"text":"Pacific Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":true,"id":733760,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Tamura, Yoshihiko","contributorId":204360,"corporation":false,"usgs":false,"family":"Tamura","given":"Yoshihiko","email":"","affiliations":[],"preferred":false,"id":733761,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Stern, Robert J.","contributorId":204361,"corporation":false,"usgs":false,"family":"Stern","given":"Robert","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":733762,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Conrad, Tracey tconrad@usgs.gov","contributorId":5021,"corporation":false,"usgs":true,"family":"Conrad","given":"Tracey","email":"tconrad@usgs.gov","affiliations":[],"preferred":true,"id":733763,"contributorType":{"id":1,"text":"Authors"},"rank":8},{"text":"Ishizuka, Osamu","contributorId":204362,"corporation":false,"usgs":false,"family":"Ishizuka","given":"Osamu","affiliations":[],"preferred":false,"id":733764,"contributorType":{"id":1,"text":"Authors"},"rank":9},{"text":"Leybourne, Matthew I.","contributorId":204363,"corporation":false,"usgs":false,"family":"Leybourne","given":"Matthew","email":"","middleInitial":"I.","affiliations":[],"preferred":false,"id":733765,"contributorType":{"id":1,"text":"Authors"},"rank":10}]}}
,{"id":70160895,"text":"70160895 - 2014 - Characterizing phosphorus dynamics in tile-drained agricultural fieldsof eastern Wisconsin","interactions":[],"lastModifiedDate":"2016-01-04T14:59:21","indexId":"70160895","displayToPublicDate":"2014-11-27T00:00:00","publicationYear":"2014","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2342,"text":"Journal of Hydrology","active":true,"publicationSubtype":{"id":10}},"title":"Characterizing phosphorus dynamics in tile-drained agricultural fieldsof eastern Wisconsin","docAbstract":"<p><span>Artificial subsurface drainage provides an avenue for the rapid transfer of phosphorus (P) from agricultural fields to surface waters. This is of particular interest in eastern Wisconsin, where there is a concentrated population of dairy farms and high clay content soils prone to macropore development. Through collaboration with private landowners, surface and tile drainage was measured and analyzed for dissolved reactive P (DRP) and total P (TP) losses at four field sites in eastern Wisconsin between 2005 and 2009. These sites, which received frequent manure applications, represent a range of crop management practices which include: two chisel plowed corn fields (CP1, CP2), a no-till corn&ndash;soybean field (NT), and a grazed pasture (GP). Subsurface drainage was the dominant pathway of water loss at each site accounting for 66&ndash;96% of total water discharge. Average annual flow-weighted (FW) TP concentrations were 0.88, 0.57, 0.21, and 1.32&nbsp;mg&nbsp;L</span><sup>&minus;1</sup><span>&nbsp;for sites CP1, CP2, NT, and GP, respectively. Low TP concentrations at the NT site were due to tile drain interception of groundwater flow where large volumes of tile drainage water diluted the FW-TP concentrations. Subsurface pathways contributed between 17% and 41% of the TP loss across sites. On a drainage event basis, total drainage explained between 36% and 72% of the event DRP loads across CP1, CP2, and GP; there was no relationship between event drainflow and event DRP load at the NT site. Manure applications did not consistently increase P concentrations in drainflow, but annual FW-P concentrations were greater in years receiving manure applications compared to years without manure application. Based on these field measures, P losses from tile drainage must be integrated into field level P budgets and P loss calculations on heavily manured soils, while also acknowledging the unique drainage patterns observed in eastern Wisconsin.</span></p>","language":"English","publisher":"Elsevier","doi":"10.1016/j.jhydrol.2014.08.016","collaboration":"University of Wisconsin-Madison; University of Wisconsin-Extension Discovery Farms","usgsCitation":"Madison, A., Ruark, M., Stuntebeck, T.D., Komiskey, M.J., Good, L.W., Drummy, N., and Cooley, E., 2014, Characterizing phosphorus dynamics in tile-drained agricultural fieldsof eastern Wisconsin: Journal of Hydrology, v. 519 A, p. 892-901, https://doi.org/10.1016/j.jhydrol.2014.08.016.","productDescription":"10 p.","startPage":"892","endPage":"901","onlineOnly":"N","additionalOnlineFiles":"N","ipdsId":"IP-055251","costCenters":[{"id":677,"text":"Wisconsin Water Science Center","active":true,"usgs":true}],"links":[{"id":313245,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":313242,"type":{"id":15,"text":"Index Page"},"url":"https://www.sciencedirect.com/science/article/pii/S0022169414006143"}],"country":"United States","state":"Wisconsin","otherGeospatial":"Eastern Wisconsin","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -87.48825073242188,\n              44.48817848394613\n            ],\n            [\n              -87.57545471191406,\n              44.49503597386932\n            ],\n            [\n              -87.56309509277344,\n              44.42544404744875\n            ],\n            [\n              -87.506103515625,\n              44.42054008115568\n            ],\n  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A","publishingServiceCenter":{"id":6,"text":"Columbus PSC"},"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"568ba5c7e4b0e7594ee77661","contributors":{"authors":[{"text":"Madison, Allison","contributorId":151055,"corporation":false,"usgs":false,"family":"Madison","given":"Allison","email":"","affiliations":[{"id":16925,"text":"University of Wisconsin-Madison","active":true,"usgs":false}],"preferred":false,"id":584193,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Ruark, Matthew","contributorId":151056,"corporation":false,"usgs":false,"family":"Ruark","given":"Matthew","affiliations":[{"id":16925,"text":"University of Wisconsin-Madison","active":true,"usgs":false}],"preferred":false,"id":584194,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Stuntebeck, Todd D. 0000-0002-8405-7295 tdstunte@usgs.gov","orcid":"https://orcid.org/0000-0002-8405-7295","contributorId":902,"corporation":false,"usgs":true,"family":"Stuntebeck","given":"Todd","email":"tdstunte@usgs.gov","middleInitial":"D.","affiliations":[{"id":37947,"text":"Upper Midwest Water Science Center","active":true,"usgs":true},{"id":677,"text":"Wisconsin Water Science Center","active":true,"usgs":true}],"preferred":true,"id":584191,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Komiskey, Matthew J. 0000-0003-2962-6974 mjkomisk@usgs.gov","orcid":"https://orcid.org/0000-0003-2962-6974","contributorId":1776,"corporation":false,"usgs":true,"family":"Komiskey","given":"Matthew","email":"mjkomisk@usgs.gov","middleInitial":"J.","affiliations":[{"id":37947,"text":"Upper Midwest Water Science Center","active":true,"usgs":true}],"preferred":true,"id":584192,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Good, Laura W.","contributorId":151057,"corporation":false,"usgs":false,"family":"Good","given":"Laura","email":"","middleInitial":"W.","affiliations":[{"id":16925,"text":"University of Wisconsin-Madison","active":true,"usgs":false}],"preferred":false,"id":584195,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Drummy, Nancy","contributorId":151058,"corporation":false,"usgs":false,"family":"Drummy","given":"Nancy","email":"","affiliations":[{"id":18174,"text":"University of Wisconsin-Extension Discovery Farms","active":true,"usgs":false}],"preferred":false,"id":584196,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Cooley, Eric","contributorId":151059,"corporation":false,"usgs":false,"family":"Cooley","given":"Eric","email":"","affiliations":[{"id":18174,"text":"University of Wisconsin-Extension Discovery Farms","active":true,"usgs":false}],"preferred":false,"id":584197,"contributorType":{"id":1,"text":"Authors"},"rank":7}]}}
,{"id":70135293,"text":"70135293 - 2014 - Investigating organic matter in Fanno Creek, Oregon, Part 3 of 3: identifying and quantifying sources of organic matter to an urban stream","interactions":[],"lastModifiedDate":"2014-12-12T10:26:17","indexId":"70135293","displayToPublicDate":"2014-11-27T00:00:00","publicationYear":"2014","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2342,"text":"Journal of Hydrology","active":true,"publicationSubtype":{"id":10}},"title":"Investigating organic matter in Fanno Creek, Oregon, Part 3 of 3: identifying and quantifying sources of organic matter to an urban stream","docAbstract":"<p><span>The sources, transport, and characteristics of organic matter (OM) in Fanno Creek, an urban stream in northwest Oregon, were assessed and quantified using: (1) optical instruments to calculate transported loads of dissolved, particulate, and total organic carbon, (2) fluorescence spectroscopy and stable isotope ratios (&delta;</span><sup>13</sup><span>C, &delta;</span><sup>15</sup><span>N) to elucidate sources and chemical properties of OM throughout the basin, and (3) synoptic sampling to investigate seasonal and hydrologic variations in the characteristics and quantity of OM. Results from this study indicate that of the roughly 324 (&plusmn;2.9%) metric tons (tonnes, t) of organic carbon exported from the basin during March 2012 to March 2013, most of the OM in Fanno Creek was dissolved (72%) and was present year-round at concentrations exceeding 3&ndash;4 milligrams of carbon per liter, whereas particulate carbon typically was mobilized and transported only by higher-flow conditions. The isotopic and fluorescence characteristics of Fanno Creek OM indicate that the carbon originates primarily from terrestrial inputs, most likely riparian vegetative biomass that enters the stream via litterfall and overland transport and then travels through the system episodically as a result of hydrologic processes. The amount of OM exported from the Fanno Creek drainage over the course of a year in this study is consistent with previous estimates of annual riparian litterfall in or near the creek. Although the creek channel is actively eroding, most bank material has too little OM for that to be a dominant source of OM to the stream. Fluorescence data revealed that the OM contains primarily humic and fulvic-like components that become less aromatic as the OM moves downstream. The most significant seasonal variation was associated with OM transported in the first storms of the autumn season (fall flush). That material was characteristically different, with a larger fraction of microbially derived OM that probably resulted from an accumulation of easy-to-mobilize and decomposing material in the streambed during previous months of summertime low-flow conditions. The first fall flush produced the highest concentrations of OM of the entire year, and the resulting load of mobilized and decomposing OM resulted in a significant oxygen demand immediately downstream in the Tualatin River.</span></p>","language":"English","publisher":"Elsevier","doi":"10.1016/j.jhydrol.2014.07.033","usgsCitation":"Goldman, J.H., Rounds, S.A., Keith, M., and Sobieszczyk, S., 2014, Investigating organic matter in Fanno Creek, Oregon, Part 3 of 3: identifying and quantifying sources of organic matter to an urban stream: Journal of Hydrology, v. 519, no. Part D, p. 3028-3041, https://doi.org/10.1016/j.jhydrol.2014.07.033.","productDescription":"14 p.","startPage":"3028","endPage":"3041","numberOfPages":"14","onlineOnly":"N","additionalOnlineFiles":"N","ipdsId":"IP-050727","costCenters":[{"id":518,"text":"Oregon Water Science Center","active":true,"usgs":true}],"links":[{"id":296635,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"projection":"Universal Transverse Mercator projection","datum":"North American Datum of 1983","country":"United States","state":"Oregon","otherGeospatial":"Fanno Creek","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -122.8216552734375,\n              45.37240823082044\n            ],\n            [\n              -122.8216552734375,\n              45.50875295937584\n            ],\n            [\n              -122.66853332519531,\n              45.50875295937584\n            ],\n            [\n              -122.66853332519531,\n              45.37240823082044\n            ],\n            [\n              -122.8216552734375,\n              45.37240823082044\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"519","issue":"Part D","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"548c1fd4e4b0ca8c43c3696f","contributors":{"authors":[{"text":"Goldman, Jami H. 0000-0001-5466-912X jgoldman@usgs.gov","orcid":"https://orcid.org/0000-0001-5466-912X","contributorId":4848,"corporation":false,"usgs":true,"family":"Goldman","given":"Jami","email":"jgoldman@usgs.gov","middleInitial":"H.","affiliations":[{"id":518,"text":"Oregon Water Science Center","active":true,"usgs":true}],"preferred":true,"id":527017,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Rounds, Stewart A. 0000-0002-8540-2206 sarounds@usgs.gov","orcid":"https://orcid.org/0000-0002-8540-2206","contributorId":905,"corporation":false,"usgs":true,"family":"Rounds","given":"Stewart","email":"sarounds@usgs.gov","middleInitial":"A.","affiliations":[{"id":518,"text":"Oregon Water Science Center","active":true,"usgs":true}],"preferred":true,"id":527018,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Keith, Mackenzie K. mkeith@usgs.gov","contributorId":4140,"corporation":false,"usgs":true,"family":"Keith","given":"Mackenzie K.","email":"mkeith@usgs.gov","affiliations":[{"id":518,"text":"Oregon Water Science Center","active":true,"usgs":true}],"preferred":false,"id":527019,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Sobieszczyk, Steven 0000-0002-0834-8437 ssobie@usgs.gov","orcid":"https://orcid.org/0000-0002-0834-8437","contributorId":885,"corporation":false,"usgs":true,"family":"Sobieszczyk","given":"Steven","email":"ssobie@usgs.gov","affiliations":[{"id":518,"text":"Oregon Water Science Center","active":true,"usgs":true}],"preferred":true,"id":527020,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70135297,"text":"70135297 - 2014 - Investigating organic matter in Fanno Creek, Oregon, Part 2 of 3: sources, sinks, and transport of organic matter with fine sediment","interactions":[],"lastModifiedDate":"2018-01-23T11:28:51","indexId":"70135297","displayToPublicDate":"2014-11-27T00:00:00","publicationYear":"2014","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2342,"text":"Journal of Hydrology","active":true,"publicationSubtype":{"id":10}},"title":"Investigating organic matter in Fanno Creek, Oregon, Part 2 of 3: sources, sinks, and transport of organic matter with fine sediment","docAbstract":"<p><span>Organic matter (OM) is abundant in Fanno Creek, Oregon, USA, and has been tied to a variety of water-quality concerns, including periods of low dissolved oxygen downstream in the Tualatin River, Oregon. The key sources of OM in Fanno Creek and other Tualatin River tributaries have not been fully identified, although isotopic analyses from previous studies indicated a predominantly terrestrial source. This study investigates the role of fine sediment erosion and deposition (mechanisms and spatial patterns) in relation to OM transport. Geomorphic mapping within the Fanno Creek floodplain shows that a large portion (approximately 70%) of the banks are eroding or subject to erosion, likely as a result of the imbalance caused by anthropogenic alteration. Field measurements of long- and short-term bank erosion average 4.2&nbsp;cm/year and average measurements of deposition for the watershed are 4.8&nbsp;cm/year. The balance between average annual erosion and deposition indicates an export of 3,250&nbsp;metric tons (tonnes, t) of fine sediment to the Tualatin River&mdash;about twice the average annual export of 1,880&nbsp;t of sediment at a location 2.4&nbsp;km from the creek&rsquo;s mouth calculated from suspended sediment load regressions from continuous turbidity data and suspended sediment samples. Carbon content from field samples of bank material, combined with fine sediment export rates, indicates that about 29&ndash;67&nbsp;t of carbon, or about 49&ndash;116&nbsp;t of OM, from bank sediment may be exported to the Tualatin River from Fanno Creek annually, an estimate that is a lower bound because it does not account for the mass wasting of organic-rich O and A soil horizons that enter the stream.</span></p>","language":"English","publisher":"Elsevier","doi":"10.1016/j.jhydrol.2014.07.027","usgsCitation":"Keith, M., Sobieszczyk, S., Goldman, J.H., and Rounds, S.A., 2014, Investigating organic matter in Fanno Creek, Oregon, Part 2 of 3: sources, sinks, and transport of organic matter with fine sediment: Journal of Hydrology, v. 519, no. Part D, p. 3010-3027, https://doi.org/10.1016/j.jhydrol.2014.07.027.","productDescription":"18 p.","startPage":"3010","endPage":"3027","numberOfPages":"18","onlineOnly":"N","additionalOnlineFiles":"N","ipdsId":"IP-050175","costCenters":[{"id":518,"text":"Oregon Water Science Center","active":true,"usgs":true}],"links":[{"id":296634,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"projection":"Universal Transverse Mercator projection","datum":"North American Datum of 1983","country":"United States","state":"Oregon","otherGeospatial":"Fanno Creek","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -122.8216552734375,\n              45.37240823082044\n            ],\n            [\n              -122.8216552734375,\n              45.50875295937584\n            ],\n            [\n              -122.66853332519531,\n              45.50875295937584\n            ],\n            [\n              -122.66853332519531,\n              45.37240823082044\n            ],\n            [\n              -122.8216552734375,\n              45.37240823082044\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"519","issue":"Part D","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"548c1fd3e4b0ca8c43c3696d","contributors":{"authors":[{"text":"Keith, Mackenzie K. mkeith@usgs.gov","contributorId":4140,"corporation":false,"usgs":true,"family":"Keith","given":"Mackenzie K.","email":"mkeith@usgs.gov","affiliations":[{"id":518,"text":"Oregon Water Science Center","active":true,"usgs":true}],"preferred":false,"id":527021,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Sobieszczyk, Steven 0000-0002-0834-8437 ssobie@usgs.gov","orcid":"https://orcid.org/0000-0002-0834-8437","contributorId":885,"corporation":false,"usgs":true,"family":"Sobieszczyk","given":"Steven","email":"ssobie@usgs.gov","affiliations":[{"id":518,"text":"Oregon Water Science Center","active":true,"usgs":true}],"preferred":true,"id":527022,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Goldman, Jami H. 0000-0001-5466-912X jgoldman@usgs.gov","orcid":"https://orcid.org/0000-0001-5466-912X","contributorId":4848,"corporation":false,"usgs":true,"family":"Goldman","given":"Jami","email":"jgoldman@usgs.gov","middleInitial":"H.","affiliations":[{"id":518,"text":"Oregon Water Science Center","active":true,"usgs":true}],"preferred":true,"id":527023,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Rounds, Stewart A. 0000-0002-8540-2206 sarounds@usgs.gov","orcid":"https://orcid.org/0000-0002-8540-2206","contributorId":905,"corporation":false,"usgs":true,"family":"Rounds","given":"Stewart","email":"sarounds@usgs.gov","middleInitial":"A.","affiliations":[{"id":518,"text":"Oregon Water Science Center","active":true,"usgs":true}],"preferred":true,"id":527024,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70147492,"text":"70147492 - 2014 - The effects of spilled oil on coastal ecosystems: Lessons from the Exxon Valdez spill","interactions":[],"lastModifiedDate":"2020-07-03T15:26:56.426156","indexId":"70147492","displayToPublicDate":"2014-11-27T00:00:00","publicationYear":"2014","noYear":false,"publicationType":{"id":5,"text":"Book chapter"},"publicationSubtype":{"id":24,"text":"Book Chapter"},"chapter":"11","title":"The effects of spilled oil on coastal ecosystems: Lessons from the Exxon Valdez spill","docAbstract":"<p class=\"do-not-mathjax\">Oil spilled from ships or other sources into the marine environment often occurs in close proximity to coastlines, and oil frequently accumulates in coastal habitats. As a consequence, a rich, albeit occasionally controversial, body of literature describes a broad range of effects of spilled oil across several habitats, communities, and species in coastal environments. This statement is not to imply that spilled oil has less of an effect in pelagic marine ecosystems, but rather that marine spills occurring offshore may be less likely to be detected, and associated effects are more difficult to monitor, evaluate, and quantify (Peterson <span class=\"italic do-not-mathjax\">et al</span>., 2012). As a result, we have a much greater awareness of coastal pollution, which speaks to our need to improve our capacities in understanding the ecology of the open oceans. Conservation of coastal ecosystems and assessment of risks associated with oil spills can be facilitated through a better understanding of processes leading to direct and indirect responses of species and systems to oil exposure.</p><p class=\"do-not-mathjax\">It is also important to recognize that oil spilled from ships represents only ~9% of the nearly 700&nbsp;000 barrels of petroleum that enter waters of North America annually from anthropogenic sources (NRC, 2003). The immediate effects of large spills can be defined as acute, due to the obvious and dramatic effects that are observed. In contrast, the remaining 625&nbsp;000 barrels that are released each year can be thought of as chronic non-point pollution, resulting from oil entering the coastal ocean as runoff in a more consistent but much less conspicuous rate. In this chapter, we primarily address the effects of large oil spills that occur near coastlines and consider their potential for both acute and chronic effects on coastal communities. As described below, in some instances, the effects from chronic exposure may meet or exceed the more evident acute effects from large spills. Consequently, although quantifying chronic effects from low exposure rates can be challenging and time-consuming, the results of such efforts provide insights into the understudied effects of chronic non-point oil pollution.</p>","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Coastal conservation","largerWorkSubtype":{"id":15,"text":"Monograph"},"language":"English","publisher":"Cambridge University Press","publisherLocation":"Cambridge, UK","doi":"10.1017/CBO9781139137089.013","usgsCitation":"Bodkin, J.L., Esler, D., Rice, S.D., Matkin, C.O., Ballachey, B.E., Maslo, B., and Lockwood, J.L., 2014, The effects of spilled oil on coastal ecosystems: Lessons from the Exxon Valdez spill, chap. 11 <i>of</i> Coastal conservation, p. 311-346, https://doi.org/10.1017/CBO9781139137089.013.","productDescription":"36 p.","startPage":"311","endPage":"346","ipdsId":"IP-044510","costCenters":[{"id":116,"text":"Alaska Science Center Biology 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,{"id":70168815,"text":"70168815 - 2014 - Response of plant community structure and primary productivity to experimental drought and flooding in an Alaskan fen","interactions":[],"lastModifiedDate":"2016-03-04T10:51:09","indexId":"70168815","displayToPublicDate":"2014-11-26T11:45:00","publicationYear":"2014","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1170,"text":"Canadian Journal of Forest Research","active":true,"publicationSubtype":{"id":10}},"title":"Response of plant community structure and primary productivity to experimental drought and flooding in an Alaskan fen","docAbstract":"<p>Northern peatlands represent a long-term net sink for atmospheric CO<sub>2</sub>, but these ecosystems can shift from net carbon (C) sinks to sources based on changing climate and environmental conditions. In particular, changes in water availability associated with climate control peatland vegetation and carbon uptake processes. We examined the influence of changing hydrology on plant species abundance and ecosystem primary production in an Alaskan fen by manipulating the water table in field treatments to mimic either sustained flooding (raised water table) or drought (lowered water table) conditions for 6 years. We found that water table treatments altered plant species abundance by increasing sedge and grass cover in the raised water table treatment and reducing moss cover while increasing vascular green area in the lowered water table treatment. Gross primary productivity was lower in the lowered treatment than in the other plots, although there were no differences in total biomass or vascular net primary productivity among the treatments. Overall, our results indicate that vegetation abundance was more sensitive to variation in water table than total biomass and vascular biomass accrual. Finally, in our experimental peatland, drought had stronger consequences for change in vegetation abundance and ecosystem function than sustained flooding.</p>","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Canadian Journal of Forest Research","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"National Research Council of Canada","publisherLocation":"Ottawa","doi":"10.1139/cjfr-2014-0100","usgsCitation":"Churchill, A., Turetsky, M.R., McGuire, A.D., and Hollingsworth, T.N., 2014, Response of plant community structure and primary productivity to experimental drought and flooding in an Alaskan fen: Canadian Journal of Forest Research, v. 45, no. 2, p. 185-193, https://doi.org/10.1139/cjfr-2014-0100.","productDescription":"9 p.","startPage":"185","endPage":"193","numberOfPages":"9","onlineOnly":"N","additionalOnlineFiles":"N","ipdsId":"IP-049060","costCenters":[{"id":200,"text":"Coop Res Unit 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,{"id":70129824,"text":"fs20143111 - 2014 - The 3D Elevation Program: summary for Ohio","interactions":[],"lastModifiedDate":"2016-08-17T15:17:51","indexId":"fs20143111","displayToPublicDate":"2014-11-25T14:45:00","publicationYear":"2014","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":"2014-3111","title":"The 3D Elevation Program: summary for Ohio","docAbstract":"<p>Elevation data are essential to a broad range of applications, including forest resources management, wildlife and habitat management, national security, recreation, and many others. For the State of Ohio, elevation data are critical for agriculture and precision farming, natural resources conservation, flood risk management, infrastructure and construction management, water supply and quality, and other business uses. Today, high-density light detection and ranging (lidar) data are the primary sources for deriving elevation models and other datasets. Federal, State, Tribal, and local agencies work in partnership to (1) replace data that are older and of lower quality and (2) provide coverage where publicly accessible data do not exist. A joint goal of State and Federal partners is to acquire consistent, statewide coverage to support existing and emerging applications enabled by lidar data.</p>\n<p>The National Enhanced Elevation Assessment evaluated multiple elevation data acquisition options to determine the optimal data quality and data replacement cycle relative to cost to meet the identified requirements of the user community. The evaluation demonstrated that lidar acquisition at quality level 2 for the conterminous United States and quality level 5 interferometric synthetic aperture radar (ifsar) data for Alaska with a 6- to 10-year acquisition cycle provided the highest benefit/cost ratios. The 3D Elevation Program (3DEP) initiative selected an 8-year acquisition cycle for the respective quality levels. 3DEP, managed by the U.S. Geological Survey, the Office of Management and Budget Circular A&ndash;16 lead agency for terrestrial elevation data, responds to the growing need for high-quality topographic data and a wide range of other 3D representations of the Nation's natural and constructed features.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/fs20143111","usgsCitation":"Carswell, W., 2014, The 3D Elevation Program: summary for Ohio (Version 1.0: Originally posted November 25, 2014; Version 1.1: June 25, 2015): U.S. Geological Survey Fact Sheet 2014-3111, 2 p., https://doi.org/10.3133/fs20143111.","productDescription":"2 p.","numberOfPages":"2","onlineOnly":"Y","additionalOnlineFiles":"N","ipdsId":"IP-059922","costCenters":[{"id":423,"text":"National Geospatial 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,{"id":70133415,"text":"fs20143116 - 2014 - Public-supply water use in Kansas, 1990-2012","interactions":[],"lastModifiedDate":"2014-11-25T11:07:11","indexId":"fs20143116","displayToPublicDate":"2014-11-25T12:00:00","publicationYear":"2014","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":"2014-3116","title":"Public-supply water use in Kansas, 1990-2012","docAbstract":"<p>This fact sheet describes water-use data collection and quantities of surface water and groundwater diverted for public supply in Kansas for the years 1990 through 2012. Data used in this fact sheet are from the Kansas Department of Agriculture&rsquo;s Division of Water Resources and the Kansas Water Office. Water used for public supply represents about 10 percent of all reported water withdrawals in Kansas. Between 1990 and 2012, annual withdrawals for public supply ranged from a low of 121 billion gallons in 1993 to a high of 159 billion gallons in 2012. Differences in annual withdrawals were associated primarily with climatic fluctuations. Six suppliers distributed about one-half of the total water withdrawn for public supply, and nearly three-quarters of the surface water. Surface water represented between 52 and 61 percent of total annual withdrawals for public supply. The proportion of surface water obtained through contracts from Federal reservoirs increased from less than 5 percent in the 1990s to 8 percent in 2011 and 2012. More than 99 percent of the reported water withdrawn for public supply in Kansas in 2012 was metered, which was an increase from 92 percent in 1990. State population increased steadily from 2.5 million people in 1990 to 2.9 million in 2012. Recent estimates indicate that about 95 percent of the total population was served by public water supply; the remainder obtained water from other sources such as private wells. Average per capita water use as calculated for State conservation planning purposes varied by region of the State. The smallest regional average water use for the years 1990&ndash;2012 was 98 gallons per person per day in easternmost Kansas, and the largest regional average water use was 274 gallons per person per day in westernmost Kansas.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/fs20143116","collaboration":"Kansas Department of Agriculture, Division of Water Resources","usgsCitation":"Kenny, J.F., 2014, Public-supply water use in Kansas, 1990-2012: U.S. Geological Survey Fact Sheet 2014-3116, 4 p., https://doi.org/10.3133/fs20143116.","productDescription":"4 p.","onlineOnly":"Y","additionalOnlineFiles":"N","temporalStart":"1990-01-01","ipdsId":"IP-059749","costCenters":[{"id":353,"text":"Kansas Water Science Center","active":false,"usgs":true}],"links":[{"id":296295,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/fs20143116.jpg"},{"id":296293,"rank":1,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/fs/2014/3116/"},{"id":296294,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/fs/2014/3116/pdf/fs2014-3116.pdf","text":"Report"}],"country":"United States","state":"Kansas","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"54759a1ce4b042f27ef134d8","contributors":{"authors":[{"text":"Kenny, Joan F. jkenny@usgs.gov","contributorId":3676,"corporation":false,"usgs":true,"family":"Kenny","given":"Joan","email":"jkenny@usgs.gov","middleInitial":"F.","affiliations":[{"id":353,"text":"Kansas Water Science Center","active":false,"usgs":true}],"preferred":false,"id":525133,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
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