{"pageNumber":"501","pageRowStart":"12500","pageSize":"25","recordCount":68899,"records":[{"id":70144994,"text":"sir20155051 - 2015 - Flood-inundation maps for the White River at Indianapolis, Indiana, 2014","interactions":[],"lastModifiedDate":"2015-05-08T13:47:45","indexId":"sir20155051","displayToPublicDate":"2015-05-08T13:30:00","publicationYear":"2015","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":334,"text":"Scientific Investigations Report","code":"SIR","onlineIssn":"2328-0328","printIssn":"2328-031X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2015-5051","title":"Flood-inundation maps for the White River at Indianapolis, Indiana, 2014","docAbstract":"<p>Digital flood-inundation maps for a 6.4-mile reach of the White River in Indianapolis, Indiana, from 0.3 miles upstream of Michigan Street to the Harding Street Generating Station dam (at the confluence with Lick Creek), were created by the U.S. Geological Survey (USGS) in cooperation with the Indiana Office of Community and Rural Affairs. The flood-inundation maps, which can be accessed through the USGS Flood Inundation Mapping Science Web site at<span class=\"Apple-converted-space\">&nbsp;</span><a href=\"http://water.usgs.gov/osw/flood_inundation/\">http://water.usgs.gov/osw/flood_inundation/</a>, depict estimates of the areal extent and depth of flooding corresponding to selected water levels (stages) at the USGS streamgage on the White River at Indianapolis, Ind. (station number 03353000). Near-real-time stages at this streamgage may be obtained on the Internet from the USGS National Water Information System at<span class=\"Apple-converted-space\">&nbsp;</span><a href=\"http://waterdata.usgs.gov/\">http://waterdata.usgs.gov/</a>or the National Weather Service (NWS) Advanced Hydrologic Prediction Service at<a href=\"http://water.weather.gov/ahps/\">http://water.weather.gov/ahps/</a>, which also forecasts flood hydrographs at this site.</p>\n<p>Flood profiles were computed for the stream reach by means of a one-dimensional step-backwater model. The model was calibrated by using the current stage-discharge relations at three USGS streamgages: the White River at Indianapolis (station number 03353000), the White River at Michigan Street at Indianapolis (station number 03352953), and the White River at Stout Generating Station at Indianapolis (station number 03353611).</p>\n<p>The hydraulic model was then used to compute 11 water-surface profiles for flood stages at 1-foot (ft) intervals referenced to the White River at Indianapolis streamgage datum and ranging from 10 ft, or the NWS &ldquo;action stage,&rdquo; to 20 ft, which is the highest stage in the stage-discharge relation for the streamgage and the NWS &ldquo;moderate flood stage.&rdquo;</p>\n<p>The simulated water-surface profiles were then combined with a geographic information system digital elevation model (derived from light detection and ranging [lidar] data having a vertical 0.183-ft root mean squared error and 5.0-ft horizontal resolution) to delineate the area flooded at each water level.</p>\n<p>The availability of these maps, along with Internet information regarding current stage from the USGS streamgage and forecasted high-flow stages from the NWS, will provide emergency management personnel and residents with information that is critical for flood response activities such as evacuations and road closures, as well as for postflood recovery efforts.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/sir20155051","collaboration":"Prepared in cooperation with the Indiana Office of Community and Rural Affairs","usgsCitation":"Nystrom, E.A., 2015, Flood-inundation maps for the White River at Indianapolis, Indiana, 2014: U.S. Geological Survey Scientific Investigations Report 2015-5051, Report: iv, 12 p.; Downloads Directory, https://doi.org/10.3133/sir20155051.","productDescription":"Report: iv, 12 p.; Downloads Directory","numberOfPages":"20","onlineOnly":"Y","additionalOnlineFiles":"Y","ipdsId":"IP-061280","costCenters":[{"id":346,"text":"Indiana Water Science Center","active":true,"usgs":true}],"links":[{"id":300238,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/sir20155051.jpg"},{"id":300235,"rank":1,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/sir/2015/5051/"},{"id":300236,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/sir/2015/5051/pdf/sir2015-5051.pdf","text":"Report","size":"4.27 MB","linkFileType":{"id":1,"text":"pdf"},"description":"Report"},{"id":300237,"rank":3,"type":{"id":7,"text":"Companion Files"},"url":"https://pubs.usgs.gov/sir/2015/5051/downloads","text":"Downloads Directory","description":"Downloads Directory","linkHelpText":"Contains: geospatial database."}],"projection":"Transverse Mercator Projection","datum":"North American Datum of 1983","country":"United States","state":"Indiana","city":"Indianapolis","otherGeospatial":"White River","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -86.20121955871582,\n              39.781036016645544\n            ],\n            [\n              -86.18001937866211,\n              39.77773791337689\n            ],\n            [\n              -86.1709213256836,\n              39.767116946991244\n            ],\n            [\n              -86.16508483886719,\n              39.742306320384046\n            ],\n            [\n              -86.16911888122559,\n              39.71484585272144\n            ],\n            [\n              -86.17641448974608,\n              39.70758284298595\n            ],\n            [\n              -86.18611335754395,\n              39.70698856289375\n            ],\n            [\n              -86.18568420410156,\n              39.69629064595011\n            ],\n            [\n              -86.18894577026367,\n              39.69596043694606\n            ],\n            [\n              -86.21769905090332,\n              39.717090628297655\n            ],\n            [\n              -86.21769905090332,\n              39.72342842379847\n            ],\n            [\n              -86.1990737915039,\n              39.735574237097275\n            ],\n            [\n              -86.1796760559082,\n              39.73735632314099\n            ],\n            [\n              -86.17401123046875,\n              39.74316428375111\n            ],\n            [\n              -86.20121955871582,\n              39.781036016645544\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","publishingServiceCenter":{"id":6,"text":"Columbus PSC"},"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"554dd01ae4b082ec54129ee9","contributors":{"authors":[{"text":"Nystrom, Elizabeth A. 0000-0002-0886-3439 nystrom@usgs.gov","orcid":"https://orcid.org/0000-0002-0886-3439","contributorId":1072,"corporation":false,"usgs":true,"family":"Nystrom","given":"Elizabeth","email":"nystrom@usgs.gov","middleInitial":"A.","affiliations":[{"id":474,"text":"New York Water Science Center","active":true,"usgs":true}],"preferred":true,"id":546448,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70146524,"text":"fs20153035 - 2015 - Scientific information in support of water resource management of the Big River area, Rhode Island","interactions":[],"lastModifiedDate":"2018-05-17T13:17:37","indexId":"fs20153035","displayToPublicDate":"2015-05-08T10:30:00","publicationYear":"2015","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":"2015-3035","title":"Scientific information in support of water resource management of the Big River area, Rhode Island","docAbstract":"<p>The Rhode Island Water Resources Board (RIWRB) is concerned that the demand for water may exceed the available public water supply in central and southern Rhode Island. Although water is often assumed to be plentiful in Rhode Island because of abundant rainfall, an adequate supply of water is not always available everywhere in the state during dry periods. Concerns that water demand may exceed supply are greatest during the summer, when lower water levels and increased drought potential combine with seasonal increases in peak water demand (Rhode Island Water Resources Board, 2012). High summer water demands are due to increases in outdoor water use, such as lawn watering and agricultural irrigation, and to increased summer population in coastal areas. Water-supply concerns are particularly acute in central and southern Rhode Island, where groundwater is the primary source of drinking water.</p>\n<p>The Big River and Mishnock River Basins are subbasins of the South Branch of the Pawtuxet River Basin in central and southern Rhode Island. These basins&mdash;referred to together as &ldquo;the Big River area&rdquo; for the purposes of this report&mdash;are undeveloped relative to other nearby areas and provide a potential source of high-quality public drinking water for central and southern Rhode Island.</p>\n<p>After the severe drought of the 1960s, the State of Rhode Island acquired land in the Big River area with the intention of building a water-supply reservoir. The reservoir was not built because of concerns over potential environmental impacts and projected statewide water-supply needs (U.S. Environmental Protection Agency, 1989). The land acquired for the reservoir (13.4 mi<sup>2</sup>), called the Big River Management Area (BRMA), is currently managed by the RIWRB as a future source for public water supply and as open space. In the 1980s, the RIWRB began to consider whether the BRMA could supply water from its aquifers (groundwater). Groundwater withdrawals for public or other water-supply needs can alter the hydrologic conditions and ecologic communities of surrounding rivers, lakes, and wetlands by removing water from these systems. Consequently, the RIWRB was interested in determining optimal amounts of groundwater that could be withdrawn from the BRMA for public supply while minimizing the effects on rivers, lakes, streams, and wetlands that also rely on this water.</p>\n<p>For nearly two decades, the RIWRB has conducted a series of cooperative studies with the U.S. Geological Survey (USGS). The goals of these studies have been to (1) evaluate and characterize the water resources of the BRMA and the greater Big River area, and (2) identify sustainable levels of groundwater use that would minimize effects on water resources. This fact sheet describes the major findings of those studies.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/fs20153035","usgsCitation":"Armstrong, D.S., Masterson, J., Robinson, K.W., and Crawley, K.M., 2015, Scientific information in support of water resource management of the Big River area, Rhode Island: U.S. Geological Survey Fact Sheet 2015-3035, 6 p., https://doi.org/10.3133/fs20153035.","productDescription":"6 p.","numberOfPages":"6","onlineOnly":"N","additionalOnlineFiles":"N","ipdsId":"IP-013379","costCenters":[{"id":376,"text":"Massachusetts Water Science Center","active":true,"usgs":true},{"id":466,"text":"New England Water Science Center","active":true,"usgs":true}],"links":[{"id":300179,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/fs20153035.jpg"},{"id":300177,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/fs/2015/3035/pdf/fs2015-3035.pdf","text":"Report","size":"1.09 MB","linkFileType":{"id":1,"text":"pdf"},"description":"Report"},{"id":300176,"rank":1,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/fs/2015/3035/"}],"country":"United States","state":"Rhode Island","otherGeospatial":"Big River Basin, Mishnock River Basin, South Branch of the Pawtuxet River Basin","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -71.60133361816406,\n              41.69521873972819\n            ],\n            [\n              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PSC"},"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"554dd01be4b082ec54129eed","contributors":{"authors":[{"text":"Armstrong, David S. 0000-0003-1695-1233 darmstro@usgs.gov","orcid":"https://orcid.org/0000-0003-1695-1233","contributorId":1390,"corporation":false,"usgs":true,"family":"Armstrong","given":"David","email":"darmstro@usgs.gov","middleInitial":"S.","affiliations":[{"id":466,"text":"New England Water Science Center","active":true,"usgs":true}],"preferred":true,"id":545039,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Masterson, John P. 0000-0003-3202-4413 jpmaster@usgs.gov","orcid":"https://orcid.org/0000-0003-3202-4413","contributorId":140294,"corporation":false,"usgs":true,"family":"Masterson","given":"John P.","email":"jpmaster@usgs.gov","affiliations":[{"id":474,"text":"New York Water Science Center","active":true,"usgs":true}],"preferred":false,"id":545040,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Robinson, Keith W. kwrobins@usgs.gov","contributorId":2969,"corporation":false,"usgs":true,"family":"Robinson","given":"Keith","email":"kwrobins@usgs.gov","middleInitial":"W.","affiliations":[],"preferred":true,"id":545041,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Crawley, Kathleen M.","contributorId":140295,"corporation":false,"usgs":false,"family":"Crawley","given":"Kathleen","email":"","middleInitial":"M.","affiliations":[{"id":13446,"text":"Rhode Island Water Resources Board","active":true,"usgs":false}],"preferred":false,"id":545042,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70147544,"text":"ofr20151086 - 2015 - Gravity data from the Sierra Vista Subwatershed, Upper San Pedro Basin, Arizona","interactions":[],"lastModifiedDate":"2017-03-09T14:27:38","indexId":"ofr20151086","displayToPublicDate":"2015-05-08T09:15:00","publicationYear":"2015","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2015-1086","title":"Gravity data from the Sierra Vista Subwatershed, Upper San Pedro Basin, Arizona","docAbstract":"<p>Observations of very small changes of Earth&rsquo;s gravitational field (time-lapse gravity) provide a direct, non-invasive method for measuring changes in aquifer storage change. An existing network of gravity stations in the Sierra Vista Subwatershed was revised in 2014 to better understand the spatial distribution of changes in aquifer storage, especially with relation to ephemeral channel recharge and a groundwater cone of depression associated with pumping in the greater Sierra Vista area. In addition, the network was extended to provide baseline data for possible future enhanced-recharge projects.</p>\n<p>This report (1) summarizes changes to the Sierra Vista Subwatershed regional time-lapse gravity network with respect to station locations and (2) presents 2014 and 2015 gravity measurements and gravity values at each station. A prior gravity network, established between 2000 and 2005, was revised in 2014 to cover a larger number of stations over a smaller geographic area in order to decrease measurement and interpolation uncertainty. The network currently consists of 59 gravity stations, including 14 absolute-gravity stations. Following above-average rainfall during summer 2014, gravity increased at all but one of the absolute-gravity stations that were observed in both June 2014 and January 2015. This increase in gravity indicates increased groundwater storage in the aquifer and (or) unsaturated zone as a result of rainfall and infiltration.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr20151086","collaboration":"Prepared in cooperation with The Nature Conservancy","usgsCitation":"Kennedy, J.R., 2015, Gravity data from the Sierra Vista Subwatershed, Upper San Pedro Basin, Arizona: U.S. Geological Survey Open-File Report 2015-1086, iv, 26 p., https://doi.org/10.3133/ofr20151086.","productDescription":"iv, 26 p.","numberOfPages":"34","onlineOnly":"Y","additionalOnlineFiles":"N","ipdsId":"IP-063495","costCenters":[{"id":128,"text":"Arizona Water Science Center","active":true,"usgs":true}],"links":[{"id":300169,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ofr20151086.JPG"},{"id":337238,"rank":4,"type":{"id":30,"text":"Data Release"},"url":"https://dx.doi.org/10.5066/F7SQ8XHX","text":"Gravity change from 2014 to 2015, Sierra Vista Subwatershed, Upper San Pedro Basin, Arizona"},{"id":300166,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2015/1086/"},{"id":300168,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/2015/1086/pdf/ofr2015-1086.pdf","size":"4 MB","linkFileType":{"id":1,"text":"pdf"}}],"scale":"100000","projection":"Universal Transverse Mercator projection","country":"United States","state":"Arizona","otherGeospatial":"Upper San Pedro Basin","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -110.37483215332031,\n              31.357741484720663\n            ],\n            [\n              -110.37483215332031,\n              31.65221239429719\n            ],\n            [\n              -110.0830078125,\n              31.65221239429719\n            ],\n            [\n              -110.0830078125,\n              31.357741484720663\n            ],\n            [\n              -110.37483215332031,\n              31.357741484720663\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","publishingServiceCenter":{"id":14,"text":"Menlo Park PSC"},"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"554dd01be4b082ec54129eeb","contributors":{"authors":[{"text":"Kennedy, Jeffrey R. 0000-0002-3365-6589 jkennedy@usgs.gov","orcid":"https://orcid.org/0000-0002-3365-6589","contributorId":2172,"corporation":false,"usgs":true,"family":"Kennedy","given":"Jeffrey","email":"jkennedy@usgs.gov","middleInitial":"R.","affiliations":[{"id":128,"text":"Arizona Water Science Center","active":true,"usgs":true}],"preferred":true,"id":546353,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70147793,"text":"70147793 - 2015 - The natural sediment regime in rivers: broadening the foundation for ecosystem management","interactions":[],"lastModifiedDate":"2015-05-07T11:03:59","indexId":"70147793","displayToPublicDate":"2015-05-07T12:00:00","publicationYear":"2015","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":997,"text":"BioScience","active":true,"publicationSubtype":{"id":10}},"title":"The natural sediment regime in rivers: broadening the foundation for ecosystem management","docAbstract":"<p><span>Water and sediment inputs are fundamental drivers of river ecosystems, but river management tends to emphasize flow regime at the expense of sediment regime. In an effort to frame a more inclusive paradigm for river management, we discuss sediment inputs, transport, and storage within river systems; interactions among water, sediment, and valley context; and the need to broaden the natural flow regime concept. Explicitly incorporating sediment is challenging, because sediment is supplied, transported, and stored by nonlinear and episodic processes operating at different temporal and spatial scales than water and because sediment regimes have been highly altered by humans. Nevertheless, managing for a desired balance between sediment supply and transport capacity is not only tractable, given current geomorphic process knowledge, but also essential because of the importance of sediment regimes to aquatic and riparian ecosystems, the physical template of which depends on sediment-driven river structure and function.</span></p>","language":"English","publisher":"Oxford University Press","doi":"10.1093/biosci/biv002","usgsCitation":"Wohl, E.E., Bledsoe, B.P., Jacobson, R.B., Poff, N.L., Rathburn, S.L., Walters, D., and Wilcox, A., 2015, The natural sediment regime in rivers: broadening the foundation for ecosystem management: BioScience, v. 65, p. 358-371, https://doi.org/10.1093/biosci/biv002.","productDescription":"14 p.","startPage":"358","endPage":"371","onlineOnly":"N","additionalOnlineFiles":"N","ipdsId":"IP-057453","costCenters":[{"id":192,"text":"Columbia Environmental Research Center","active":true,"usgs":true}],"links":[{"id":300160,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"65","edition":"4","publishingServiceCenter":{"id":4,"text":"Rolla PSC"},"noUsgsAuthors":false,"publicationDate":"2015-02-19","publicationStatus":"PW","scienceBaseUri":"554c7ea9e4b082ec54128487","contributors":{"authors":[{"text":"Wohl, Ellen E.","contributorId":16969,"corporation":false,"usgs":true,"family":"Wohl","given":"Ellen","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":546303,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bledsoe, Brian P.","contributorId":140605,"corporation":false,"usgs":false,"family":"Bledsoe","given":"Brian","email":"","middleInitial":"P.","affiliations":[{"id":13538,"text":"Department of Civil and Environmental Engineering, Colorado State University, Fort Collins, Colorado","active":true,"usgs":false}],"preferred":false,"id":546304,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Jacobson, Robert B. 0000-0002-8368-2064 rjacobson@usgs.gov","orcid":"https://orcid.org/0000-0002-8368-2064","contributorId":1289,"corporation":false,"usgs":true,"family":"Jacobson","given":"Robert","email":"rjacobson@usgs.gov","middleInitial":"B.","affiliations":[{"id":192,"text":"Columbia Environmental Research Center","active":true,"usgs":true}],"preferred":true,"id":546302,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Poff, N. LeRoy","contributorId":90843,"corporation":false,"usgs":true,"family":"Poff","given":"N.","email":"","middleInitial":"LeRoy","affiliations":[],"preferred":false,"id":546305,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Rathburn, Sara L.","contributorId":140606,"corporation":false,"usgs":false,"family":"Rathburn","given":"Sara","email":"","middleInitial":"L.","affiliations":[{"id":13539,"text":"Department of Geosciences, Colorado State University, Fort Collins, Colorado","active":true,"usgs":false}],"preferred":false,"id":546306,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Walters, David M. 0000-0002-4237-2158 waltersd@usgs.gov","orcid":"https://orcid.org/0000-0002-4237-2158","contributorId":4444,"corporation":false,"usgs":true,"family":"Walters","given":"David M.","email":"waltersd@usgs.gov","affiliations":[{"id":291,"text":"Fort Collins Science Center","active":true,"usgs":true}],"preferred":false,"id":546307,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Wilcox, Andrew C.","contributorId":25064,"corporation":false,"usgs":true,"family":"Wilcox","given":"Andrew C.","affiliations":[],"preferred":false,"id":546308,"contributorType":{"id":1,"text":"Authors"},"rank":7}]}}
,{"id":70147795,"text":"sir20125054 - 2015 - Indian National Gas Hydrate Program Expedition 01 report","interactions":[],"lastModifiedDate":"2015-05-07T09:36:21","indexId":"sir20125054","displayToPublicDate":"2015-05-07T10:00:00","publicationYear":"2015","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":334,"text":"Scientific Investigations Report","code":"SIR","onlineIssn":"2328-0328","printIssn":"2328-031X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2012-5054","title":"Indian National Gas Hydrate Program Expedition 01 report","docAbstract":"<p>Gas hydrate is a naturally occurring &ldquo;ice-like&rdquo; combination of natural gas and water that has the potential to serve as an immense resource of natural gas from the world&rsquo;s oceans and polar regions. However, gas-hydrate recovery is both a scientific and a technical challenge and much remains to be learned about the geologic, engineering, and economic factors controlling the ultimate energy resource potential of gas hydrate. The amount of natural gas contained in the world&rsquo;s gas-hydrate accumulations is enormous, but these estimates are speculative and range over three orders of magnitude from about 2,800 to 8,000,000 trillion cubic meters of gas. By comparison, conventional natural gas accumulations (reserves and undiscovered, technically recoverable resources) for the world are estimated at approximately 440 trillion cubic meters. Gas recovery from gas hydrate is hindered because the gas is in a solid form and because gas hydrate commonly occurs in remote Arctic and deep marine environments. Proposed methods of gas recovery from gas hydrate generally deal with disassociating or &ldquo;melting&rdquo; in situ gas hydrate by heating the reservoir beyond the temperature of gas-hydrate formation, or decreasing the reservoir pressure below hydrate equilibrium. The pace of energy-related gas hydrate assessment projects has accelerated over the past several years.</p>\n<p>The Indian National Gas Hydrate Program Expedition 01 was designed to study the gas-hydrate occurrences off the Indian Peninsula and along the Andaman convergent margin with special emphasis on understanding the geologic and geochemical controls on the occurrence of gas hydrate in these two diverse settings. During Indian National Gas Hydrate Program Expedition 01, dedicated gas-hydrate coring, drilling, and downhole logging operations were conducted from 28 April 2006 to 19 August 2006.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/sir20125054","usgsCitation":"Collett, T.S., Riedel, M., Boswell, R., Presley, J., Kumar, P., Sathe, A., Sethi, A., Lall, M., and NGHP Expedition Scientists, 2015, Indian National Gas Hydrate Program Expedition 01 report: U.S. Geological Survey Scientific Investigations Report 2012-5054, Report: xv, 1442 p.; 4 Appendices; Downloads Directory, https://doi.org/10.3133/sir20125054.","productDescription":"Report: xv, 1442 p.; 4 Appendices; Downloads Directory","onlineOnly":"Y","additionalOnlineFiles":"Y","temporalStart":"2006-04-28","temporalEnd":"2006-08-19","ipdsId":"IP-016709","costCenters":[{"id":164,"text":"Central Energy Resources Science 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,{"id":70156190,"text":"70156190 - 2015 - Temporal and basin-specific population trends of quagga mussels on soft sediment of a multi-basin reservoir","interactions":[],"lastModifiedDate":"2016-09-08T15:31:10","indexId":"70156190","displayToPublicDate":"2015-05-07T00:00:00","publicationYear":"2015","noYear":false,"publicationType":{"id":5,"text":"Book chapter"},"publicationSubtype":{"id":24,"text":"Book Chapter"},"title":"Temporal and basin-specific population trends of quagga mussels on soft sediment of a multi-basin reservoir","docAbstract":"Invasive quagga (Dreissena bugnesis) and zebra (Dreissena ploymorpha) mussels have rapidly spread throughout North America. Understanding the relationships between environmental variables and quagga mussels during the early stages of invasion will help management strategies and allow researchers to predict patterns of future invasions. Quagga mussels were detected in Lake Mead, NV/AZ in 2007, we monitored early invasion dynamics in 3 basins (Boulder Basin, Las Vegas Bay, Overton Arm) bi-annually from 2008-2011. Mean quagga density increased over time during the first year of monitoring and stabilized for the subsequent two years at the whole-lake scale (8 to 132 individuals·m-2, geometric mean), in Boulder Basin (73 to 875 individuals·m-2), and in Overton Arm(2 to 126 individuals·m-2). In Las Vegas Bay, quagga mussel density was low (9 to 44 individuals·m-2), which was correlated with high sediment metal concentrations and warmer (> 30°C) water temperatures associated with that basin. Carbon content in the sediment increased with depth in Lake Mead and during some sampling periods quagga density was also positively correlated with depth, but more research is required to determine the significance of this interaction. Laboratory growth experiments suggested that food quantity may limit quagga growth in Boulder Basin, indicating an opportunity for population expansion in this basin if primary productivity were to increase, but was not the case in Overton Arm. Overall quagga mussel density in Lake Mead is highly variable and patchy, suggesting that temperature, sediment size, and sediment metal concentrations, and sediment carbon content all contribute to mussel distribution patterns. Quagga mussel density in the soft sediment of Lake Mead expanded during initial colonization, and began to stabilize approximately 3 years after the initial invasion.","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Biology and management of invasive Quagga and Zebra Mussels in the western United States","language":"English","publisher":"CRC Press","collaboration":"University of Nevada-Reno; Desert Research Institute; National Park Service","usgsCitation":"Caldwell, T.J., Rosen, M.R., Chandra, S., Acharya, K., Caires, A.M., Davis, C.J., Thaw, M., and Webster, D.M., 2015, Temporal and basin-specific population trends of quagga mussels on soft sediment of a multi-basin reservoir, chap. <i>of</i> Biology and management of invasive Quagga and Zebra Mussels in the western United States, p. 33-52.","productDescription":"20 p.","startPage":"33","endPage":"52","ipdsId":"IP-052767","costCenters":[{"id":509,"text":"Office of the Associate Director for Water","active":true,"usgs":true}],"links":[{"id":328422,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":306642,"type":{"id":15,"text":"Index Page"},"url":"https://www.crcpress.com/Biology-and-Management-of-Invasive-Quagga-and-Zebra-Mussels-in-the-Western/Wong-Gerstenberger/9781466595613"}],"publishingServiceCenter":{"id":9,"text":"Reston PSC"},"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"57d28bafe4b0571647d0f94a","contributors":{"authors":[{"text":"Caldwell, Timothy J","contributorId":146463,"corporation":false,"usgs":false,"family":"Caldwell","given":"Timothy","email":"","middleInitial":"J","affiliations":[{"id":16704,"text":"University of Nevada - Reno","active":true,"usgs":false}],"preferred":false,"id":567980,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Rosen, Michael R. 0000-0003-3991-0522 mrosen@usgs.gov","orcid":"https://orcid.org/0000-0003-3991-0522","contributorId":495,"corporation":false,"usgs":true,"family":"Rosen","given":"Michael","email":"mrosen@usgs.gov","middleInitial":"R.","affiliations":[{"id":154,"text":"California Water Science Center","active":true,"usgs":true}],"preferred":true,"id":567979,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Chandra, Sudeep","contributorId":33195,"corporation":false,"usgs":false,"family":"Chandra","given":"Sudeep","affiliations":[{"id":12742,"text":"University of Nevada Reno","active":true,"usgs":false}],"preferred":false,"id":567981,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Acharya, Kumud","contributorId":146464,"corporation":false,"usgs":false,"family":"Acharya","given":"Kumud","email":"","affiliations":[{"id":16138,"text":"Desert Research Institute","active":true,"usgs":false}],"preferred":false,"id":567982,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Caires, Andrea M","contributorId":146465,"corporation":false,"usgs":false,"family":"Caires","given":"Andrea","email":"","middleInitial":"M","affiliations":[{"id":16704,"text":"University of Nevada - Reno","active":true,"usgs":false}],"preferred":false,"id":567983,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Davis, Clinton J.","contributorId":146466,"corporation":false,"usgs":false,"family":"Davis","given":"Clinton","email":"","middleInitial":"J.","affiliations":[{"id":16704,"text":"University of Nevada - Reno","active":true,"usgs":false}],"preferred":false,"id":567984,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Thaw, Melissa","contributorId":146467,"corporation":false,"usgs":false,"family":"Thaw","given":"Melissa","email":"","affiliations":[{"id":16138,"text":"Desert Research Institute","active":true,"usgs":false}],"preferred":false,"id":567985,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Webster, Daniel M. webster@usgs.gov","contributorId":3529,"corporation":false,"usgs":true,"family":"Webster","given":"Daniel","email":"webster@usgs.gov","middleInitial":"M.","affiliations":[{"id":436,"text":"National Research Program - Eastern Branch","active":true,"usgs":true}],"preferred":true,"id":567986,"contributorType":{"id":1,"text":"Authors"},"rank":8}]}}
,{"id":70144868,"text":"sir20155049 - 2015 - Peak flow regression equations For small, ungaged streams in Maine: Comparing map-based to field-based variables","interactions":[],"lastModifiedDate":"2016-09-29T10:13:53","indexId":"sir20155049","displayToPublicDate":"2015-05-06T15:45:00","publicationYear":"2015","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":334,"text":"Scientific Investigations Report","code":"SIR","onlineIssn":"2328-0328","printIssn":"2328-031X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2015-5049","title":"Peak flow regression equations For small, ungaged streams in Maine: Comparing map-based to field-based variables","docAbstract":"<p><span>Regression equations to estimate peak streamflows with 1- to 500-year recurrence intervals (annual exceedance probabilities from 99 to 0.2 percent, respectively) were developed for small, ungaged streams in Maine. Equations presented here are the best available equations for estimating peak flows at ungaged basins in Maine with drainage areas from 0.3 to 12 square miles (mi</span><sup>2</sup><span>). Previously developed equations continue to be the best available equations for estimating peak flows for basin areas greater than 12 mi</span><sup>2</sup><span>. New equations presented here are based on streamflow records at 40 U.S. Geological Survey streamgages with a minimum of 10 years of recorded peak flows between 1963 and 2012. Ordinary least-squares regression techniques were used to determine the best explanatory variables for the regression equations. Traditional map-based explanatory variables were compared to variables requiring field measurements. Two field-based variables&mdash;culvert rust lines and bankfull channel widths&mdash;either were not commonly found or did not explain enough of the variability in the peak flows to warrant inclusion in the equations. The best explanatory variables were drainage area and percent basin wetlands; values for these variables were determined with a geographic information system. Generalized least-squares regression was used with these two variables to determine the equation coefficients and estimates of accuracy for the final equations.</span></p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/sir20155049","collaboration":"Prepared in cooperation with the Maine Department of Transportation","usgsCitation":"Lombard, P., and Hodgkins, G.A., 2015, Peak flow regression equations For small, ungaged streams in Maine: Comparing map-based to field-based variables: U.S. Geological Survey Scientific Investigations Report 2015-5049, vi, 12 p., https://doi.org/10.3133/sir20155049.","productDescription":"vi, 12 p.","numberOfPages":"22","onlineOnly":"Y","additionalOnlineFiles":"N","ipdsId":"IP-063561","costCenters":[{"id":371,"text":"Maine Water Science 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,{"id":70146536,"text":"ofr20151072 - 2015 - Summary of oceanographic and water-quality measurements in Rachel Carson National Wildlife Refuge, Wells, Maine, in 2013","interactions":[],"lastModifiedDate":"2015-05-06T14:44:48","indexId":"ofr20151072","displayToPublicDate":"2015-05-06T14:30:00","publicationYear":"2015","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2015-1072","title":"Summary of oceanographic and water-quality measurements in Rachel Carson National Wildlife Refuge, Wells, Maine, in 2013","docAbstract":"<p><span>Suspended-sediment transport is a critical element controlling the geomorphology of tidal wetland complexes. Wetlands rely on organic material and inorganic sediment deposition to maintain their elevation relative to sea level. The U.S. Geological Survey performed observational deployments to measure suspended-sediment concentration and water flow rates in the tidal channels of the wetlands in the Rachel Carson National Wildlife Refuge in Wells, Maine. The objective was to characterize the sediment-transport mechanisms that contribute to the net sediment budget of the wetland complex. We deployed a meteorological tower, optical turbidity sensors, and acoustic velocity meters at sites on Stephens Brook and the Ogunquit River between March 27 and December 9, 2013. This report presents the time-series oceanographic and atmospheric data collected during those field studies. The oceanographic parameters include water velocity, depth, turbidity, salinity, temperature, and pH. The atmospheric parameters include wind direction, speed, and gust; air temperature; air pressure; relative humidity; short wave radiation; and photosynthetically active radiation.</span></p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr20151072","usgsCitation":"Montgomery, E., Ganju, N., Dickhudt, P., Borden, J., Martini, M.A., and Brosnahan, S.M., 2015, Summary of oceanographic and water-quality measurements in Rachel Carson National Wildlife Refuge, Wells, Maine, in 2013: U.S. Geological Survey Open-File Report 2015-1072, Report: v, 17 p.; Appendixes 1-3; Dataset, https://doi.org/10.3133/ofr20151072.","productDescription":"Report: v, 17 p.; Appendixes 1-3; Dataset","numberOfPages":"28","onlineOnly":"Y","additionalOnlineFiles":"Y","temporalStart":"2013-03-27","temporalEnd":"2013-12-09","ipdsId":"IP-059849","costCenters":[{"id":678,"text":"Woods Hole Coastal and Marine Science 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,{"id":70155878,"text":"70155878 - 2015 - Coupled interactions between volatile activity and Fe oxidation state during arc crustal processes","interactions":[],"lastModifiedDate":"2015-08-17T10:46:18","indexId":"70155878","displayToPublicDate":"2015-05-06T11:45:00","publicationYear":"2015","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2420,"text":"Journal of Petrology","active":true,"publicationSubtype":{"id":10}},"title":"Coupled interactions between volatile activity and Fe oxidation state during arc crustal processes","docAbstract":"<p><span>Arc magmas erupted at the Earth&rsquo;s surface are commonly more oxidized than those produced at mid-ocean ridges. Possible explanations for this high oxidation state are that the transfer of fluids during the subduction process results in direct oxidation of the sub-arc mantle wedge, or that oxidation is caused by the effect of later crustal processes, including protracted fractionation and degassing of volatile-rich magmas. This study sets out to investigate the effect of disequilibrium crustal processes that may involve coupled changes in H</span><sub>2</sub><span>O content and Fe oxidation state, by examining the degassing and hydration of sulphur-free rhyolites. We show that experimentally hydrated melts record strong increases in Fe</span><sup>3+</sup><span>/&sum;Fe with increasing H</span><sub>2</sub><span>O concentration as a result of changes in water activity. This is relevant for the passage of H</span><sub>2</sub><span>O-undersaturated melts from the deep crust towards shallow crustal storage regions, and raises the possibility that vertical variations in&nbsp;</span><i>f</i><span>O</span><sub>2</sub><span>&nbsp;might develop within arc crust. Conversely, degassing experiments produce an increase in Fe</span><sup>3+</sup><span>/&sum;Fe with decreasing H</span><sub>2</sub><span>O concentration. In this case the oxidation is explained by loss of H</span><sub>2</sub><span>&nbsp;as well as H</span><sub>2</sub><span>O into bubbles during decompression, consistent with thermodynamic modelling, and is relevant for magmas undergoing shallow degassing en route to the surface. We discuss these results in the context of the possible controls on&nbsp;</span><i>f</i><span>O</span><sub>2</sub><span>&nbsp;during the generation, storage and ascent of magmas in arc settings, in particular considering the timescales of equilibration relative to observation as this affects the quality of the petrological record of magmatic&nbsp;</span><i>f</i><span>O</span><sub>2</sub><span>.</span></p>","language":"English","publisher":"Oxford University Press","publisherLocation":"Oxford","doi":"10.1093/petrology/egv017","usgsCitation":"Humphreys, M.C., Brooker, R., Fraser, D., Burgisser, A., Mangan, M.T., and McCammon, C., 2015, Coupled interactions between volatile activity and Fe oxidation state during arc crustal processes: Journal of Petrology, p. 1-20, https://doi.org/10.1093/petrology/egv017.","productDescription":"20 p.","startPage":"1","endPage":"20","numberOfPages":"20","onlineOnly":"N","additionalOnlineFiles":"N","ipdsId":"IP-055270","costCenters":[{"id":617,"text":"Volcano Science Center","active":true,"usgs":true}],"links":[{"id":472101,"rank":0,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1093/petrology/egv017","text":"Publisher Index Page"},{"id":306784,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"publishingServiceCenter":{"id":14,"text":"Menlo Park PSC"},"noUsgsAuthors":false,"publicationDate":"2015-05-06","publicationStatus":"PW","scienceBaseUri":"57f7ef2ae4b0bc0bec09ef46","contributors":{"authors":[{"text":"Humphreys, Madeleine C.S.","contributorId":103199,"corporation":false,"usgs":true,"family":"Humphreys","given":"Madeleine","email":"","middleInitial":"C.S.","affiliations":[],"preferred":false,"id":566661,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Brooker, R","contributorId":146223,"corporation":false,"usgs":false,"family":"Brooker","given":"R","email":"","affiliations":[{"id":16635,"text":"Bristol University","active":true,"usgs":false}],"preferred":false,"id":566662,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Fraser, D.C.","contributorId":35732,"corporation":false,"usgs":true,"family":"Fraser","given":"D.C.","email":"","affiliations":[],"preferred":false,"id":566663,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Burgisser, A","contributorId":146224,"corporation":false,"usgs":false,"family":"Burgisser","given":"A","affiliations":[{"id":16636,"text":"CNRS","active":true,"usgs":false}],"preferred":false,"id":566664,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Mangan, Margaret T. 0000-0002-5273-8053 mmangan@usgs.gov","orcid":"https://orcid.org/0000-0002-5273-8053","contributorId":3343,"corporation":false,"usgs":true,"family":"Mangan","given":"Margaret","email":"mmangan@usgs.gov","middleInitial":"T.","affiliations":[{"id":615,"text":"Volcano Hazards Program","active":true,"usgs":true},{"id":617,"text":"Volcano Science Center","active":true,"usgs":true},{"id":114,"text":"Alaska Science Center","active":true,"usgs":true}],"preferred":true,"id":566660,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"McCammon, C","contributorId":146225,"corporation":false,"usgs":false,"family":"McCammon","given":"C","email":"","affiliations":[{"id":13489,"text":"Bayerisches Geoinstitut, Universität Bayreuth, 95440 Bayreuth, Germany","active":true,"usgs":false}],"preferred":false,"id":566665,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}}
,{"id":70154770,"text":"70154770 - 2015 - A pheromone outweighs temperature in influencing migration of sea lamprey","interactions":[],"lastModifiedDate":"2016-06-23T08:50:58","indexId":"70154770","displayToPublicDate":"2015-05-06T11:00:00","publicationYear":"2015","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3908,"text":"Royal Society Open Science","active":true,"publicationSubtype":{"id":10}},"title":"A pheromone outweighs temperature in influencing migration of sea lamprey","docAbstract":"<p><span>Organisms continuously acquire and process information from surrounding cues. While some cues complement one another in delivering more reliable information, others may provide conflicting information. How organisms extract and use reliable information from a multitude of cues is largely unknown. We examined movement decisions of sea lampreys (</span><i>Petromyzon marinus</i><span>&nbsp;L.) exposed to a conspecific and an environmental cue during pre-spawning migration. Specifically, we predicted that the mature male-released sex pheromone 3-keto petromyzonol sulfate (3kPZS) will outweigh the locomotor inhibiting effects of cold stream temperature (less than 15&deg;C). Using large-scale stream bioassays, we found that 3kPZS elicits an increase (more than 40%) in upstream movement of pre-spawning lampreys when the water temperatures were below 15&deg;C. Both warming temperatures and conspecific cues increase upstream movement when the water temperature rose above 15&deg;C. These patterns define an interaction between abiotic and conspecific cues in modulating animal decision-making, providing an example of the hierarchy of contradictory information.</span></p>","language":"English","publisher":"Royal Society Publishing","publisherLocation":"London","doi":"10.1098/rsos.150009","usgsCitation":"Brant, C., Li, K., Johnson, N., and Li, W., 2015, A pheromone outweighs temperature in influencing migration of sea lamprey: Royal Society Open Science, v. 2, p. 1-7, https://doi.org/10.1098/rsos.150009.","productDescription":"7 p.","startPage":"1","endPage":"7","onlineOnly":"N","additionalOnlineFiles":"N","ipdsId":"IP-064542","costCenters":[{"id":324,"text":"Great Lakes Science Center","active":true,"usgs":true}],"links":[{"id":472102,"rank":0,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1098/rsos.150009","text":"Publisher Index Page"},{"id":308167,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"2","publishingServiceCenter":{"id":6,"text":"Columbus PSC"},"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"55fa92ace4b05d6c4e501a40","contributors":{"authors":[{"text":"Brant, Cory O.","contributorId":52872,"corporation":false,"usgs":true,"family":"Brant","given":"Cory O.","affiliations":[],"preferred":false,"id":564077,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Li, Ke","contributorId":172267,"corporation":false,"usgs":false,"family":"Li","given":"Ke","email":"","affiliations":[],"preferred":false,"id":640106,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Johnson, Nicholas S. njohnson@usgs.gov","contributorId":145449,"corporation":false,"usgs":true,"family":"Johnson","given":"Nicholas S.","email":"njohnson@usgs.gov","affiliations":[{"id":324,"text":"Great Lakes Science Center","active":true,"usgs":true}],"preferred":false,"id":564076,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Li, Weiming","contributorId":65440,"corporation":false,"usgs":true,"family":"Li","given":"Weiming","affiliations":[],"preferred":false,"id":564079,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70145549,"text":"ds932 - 2015 - Geospatial compilation and digital map of centerpivot irrigated areas in the mid-Atlantic region, United States","interactions":[],"lastModifiedDate":"2015-05-05T14:50:14","indexId":"ds932","displayToPublicDate":"2015-05-05T15:45:00","publicationYear":"2015","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":310,"text":"Data Series","code":"DS","onlineIssn":"2327-638X","printIssn":"2327-0271","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"932","title":"Geospatial compilation and digital map of centerpivot irrigated areas in the mid-Atlantic region, United States","docAbstract":"<p>To evaluate water availability within the Northern Atlantic Coastal Plain, the U.S. Geological Survey, in cooperation with the University of Delaware Agricultural Extension, created a dataset that maps the number of acres under center-pivot irrigation in the Northern Atlantic Coastal Plain study area. For this study, the extent of the Northern Atlantic Coastal Plain falls within areas of the States of New York, New Jersey, Delaware, Maryland, Virginia, and North Carolina. The irrigation dataset maps about 271,900 acres operated primarily under center-pivot irrigation in 57 counties. Manual digitizing was performed against aerial imagery in a process where operators used observable center-pivot irrigation signatures&mdash;such as irrigation arms, concentric wheel paths through cropped areas, and differential colors&mdash;to identify and map irrigated areas. The aerial imagery used for digitizing came from a variety of sources and seasons. The imagery contained a variety of spatial resolutions and included online imagery from the U.S. Department of Agriculture National Agricultural Imagery Program, Microsoft Bing Maps, and the Google Maps mapping service. The dates of the source images ranged from 2010 to 2012 for the U.S. Department of Agriculture imagery, whereas maps from the other mapping services were from 2013.</p>\n<p>Most of the irrigation in the study area is on the Delmarva Peninsula, where about 75 percent of the total acreage was delineated and where corn and soy bean are the main crops. The methods used to develop this dataset focused primarily on identifying center-pivot irrigation systems. In some instances (such as in in Suffolk County, New York), irrigated rectangular fields were observed through the aerial imagery, and these were included within the dataset. Other irrigation methods included subsurface drip and flood irrigation, which are commonly used on vegetable crops such as peppers and tomatoes and forage crops such as alfalfa in parts the western United States. Some fruit and nursery stock crops also use subsurface drip and flood irrigation. Drip irrigation is especially apparent in New Jersey where large plantings of truck crops are common. Subsurface drip and flood irrigation methods were not accounted for in this dataset. The U.S. Geological Survey collected these data to enhance the understanding of irrigation water demand and associated groundwater withdrawals for the Northern Atlantic Coastal Plain.</p>\n<p>The digitized acreage totals were compared with the irrigation estimates provided by the U.S. Department of Agriculture farm and ranch irrigation survey, which is the most comprehensive source of information on irrigation water use within the agricultural industry. This survey collects information on a wide range of topics, including the amount of water used, total acres irrigated, crop specific data, and even energy costs. The U.S. Department of Agriculture samples data for both entire States and individual counties.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ds932","collaboration":"Prepared in cooperation with the University of Delaware Agricultural Extension","usgsCitation":"Finkelstein, J.S., and Nardi, M.R., 2015, Geospatial compilation and digital map of centerpivot irrigated areas in the mid-Atlantic region, United States: U.S. Geological Survey Data Series 932, HTML Document; Metadata; Data Files; Readme, https://doi.org/10.3133/ds932.","productDescription":"HTML Document; Metadata; Data Files; Readme","onlineOnly":"Y","additionalOnlineFiles":"Y","ipdsId":"IP-060776","costCenters":[{"id":474,"text":"New York Water Science Center","active":true,"usgs":true}],"links":[{"id":300118,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ds932.jpg"},{"id":300113,"rank":1,"type":{"id":15,"text":"Index 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,{"id":70141459,"text":"sir20155023 - 2015 - Water quality of the Little Arkansas River and <i>Equus</i> Beds Aquifer before and concurrent with large-scale artificial recharge, south-central Kansas, 1995-2012","interactions":[],"lastModifiedDate":"2015-05-07T09:43:27","indexId":"sir20155023","displayToPublicDate":"2015-05-05T11:45:00","publicationYear":"2015","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":334,"text":"Scientific Investigations Report","code":"SIR","onlineIssn":"2328-0328","printIssn":"2328-031X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2015-5023","title":"Water quality of the Little Arkansas River and <i>Equus</i> Beds Aquifer before and concurrent with large-scale artificial recharge, south-central Kansas, 1995-2012","docAbstract":"<p>The city of Wichita artificially recharged about 1 billion gallons of water into the&nbsp;<i>Equus</i>&nbsp;Beds aquifer during 2007&ndash;2012 as part of Phase I recharge of the Artificial Storage and Recovery project. This report, prepared in cooperation by the U.S. Geological Survey and the city of Wichita, Kansas, summarizes Little Arkansas River (source-water for artificial recharge) and<i>Equus</i>&nbsp;Beds aquifer water quality before (1995&ndash;2006) and during (2007&ndash;2012) Artificial Storage and Recovery Phase I recharge. Additionally, aquifer water-quality distribution maps are presented and water-quality changes associated with Phase I recharge timing are described.</p>\n<p>Computed chloride concentrations in the Little Arkansas River exceeded the Federal secondary maximum contaminant level (SMCL) about 20 percent of the time during 1999 through 2012, primarily during low-flow conditions. Groundwater chloride concentrations during 2001 through 2012 exceeded the SMCL in about 6 percent of shallow wells and 7 percent of deep wells, primarily near Burrton, Kansas and along the Arkansas River. Nearly all surface water nitrate plus nitrite concentrations during 1995 through 2012 were less than the Federal maximum contaminant level (MCL); groundwater nitrate plus nitrite concentrations exceeded the MCL in about 16 percent of shallow groundwater samples and were minimal in the deeper parts of the aquifer. Several trace elements frequently exceeded drinking water criteria, including arsenic, iron, and manganese.</p>\n<p>Recharge activities at Phase I recharge wells have not resulted in substantial effects on groundwater quality in the area, likely because the total amount of water recharged is relatively small (1 billion gallons) compared to aquifer storage volume (greater than 990 billion gallons in winter 2012). The eastward movement of the Burrton chloride plume is likely being slowed by a line of recharge locations associated with Phase I; however, chloride concentrations in deep groundwater still advanced to less than one half mile from the central part of the study area. Water-quality constituents of concern (major ions, nutrients, trace elements, triazine herbicides, and fecal indicator bacteria) have not increased substantially and are likely more affected by climatological (natural recharge by precipitation) and natural (geochemical oxidation/reduction, metabolic and decay rates) processes than artificial recharge. Arsenic remains a water-quality constituent of concern because of natural and continued persistence of concentrations exceeding the Federal maximum contaminant level of 10 micrograms per liter, especially in the deeper parts of the<i>Equus</i>&nbsp;Beds aquifer.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/sir20155023","collaboration":"Prepared in cooperation with the City of Wichita, Kansas, as part of the Equus Beds Groundwater Recharge Project","usgsCitation":"Tappa, D.J., Lanning-Rush, J., Klager, B.J., Hansen, C.V., and Ziegler, A., 2015, Water quality of the Little Arkansas River and <i>Equus</i> Beds Aquifer before and concurrent with large-scale artificial recharge, south-central Kansas, 1995-2012 (Version 1: Originally posted May 5, 2015; Version 1.1: May 6, 2015): U.S. Geological Survey Scientific Investigations Report 2015-5023, Report: ix, 67 p.; Downloads Directory, 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,{"id":70141460,"text":"fs20153010 - 2015 - Water quality of the Little Arkansas River and <i>Equus</i> Beds Aquifer before and concurrent with large-scale artificial recharge, south-central Kansas, 1995-2012","interactions":[],"lastModifiedDate":"2015-05-07T09:47:05","indexId":"fs20153010","displayToPublicDate":"2015-05-05T11:30:00","publicationYear":"2015","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":"2015-3010","title":"Water quality of the Little Arkansas River and <i>Equus</i> Beds Aquifer before and concurrent with large-scale artificial recharge, south-central Kansas, 1995-2012","docAbstract":"<p><span>This fact sheet describes baseline water quality of the&nbsp;</span><i>Equus</i><span>&nbsp;Beds aquifer and Little Arkansas River and water-quality effects of artificial recharge by the city of Wichita associated with Phase I (2007&ndash;present) of the Aquifer Storage and Recovery project. During 1995 through 2012, more than 8,800 surface water and groundwater water-quality samples were collected and analyzed for more than 400 compounds, including most of the compounds on the U.S. Environmental Protection Agency&rsquo;s primary drinking-water standards maximum contaminant level list and secondary drinkingwater regulations secondary maximum contaminant level list. Water-quality constituents of concern discussed in detail in this fact sheet are chloride, arsenic, total coliform bacteria, and atrazine. Sulfate, nitrate, iron, manganese, oxidation-reduction potential, and specific conductance also are constituents of concern and are discussed to a lesser extent.</span></p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/fs20153010","collaboration":"Prepared in cooperation with the City of Wichita, Kansas, as part of the Equus Beds Groundwater Recharge Project","usgsCitation":"Tappa, D., Lanning-Rush, J., and Ziegler, A., 2015, Water quality of the Little Arkansas River and <i>Equus</i> Beds Aquifer before and concurrent with large-scale artificial recharge, south-central Kansas, 1995-2012 (Version 1: Originally posted May 5, 2015; Version 1.1: May 6, 2015): U.S. Geological Survey Fact Sheet 2015-3010, 4 p., https://doi.org/10.3133/fs20153010.","productDescription":"4 p.","numberOfPages":"4","onlineOnly":"N","additionalOnlineFiles":"N","temporalStart":"1995-01-01","temporalEnd":"2012-12-31","ipdsId":"IP-057439","costCenters":[{"id":353,"text":"Kansas Water Science Center","active":false,"usgs":true}],"links":[{"id":300099,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/fs20153010.jpg"},{"id":300098,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/fs/2015/3010/pdf/fs2015-3010.pdf","size":"1.34 MB","linkFileType":{"id":1,"text":"pdf"}},{"id":300091,"rank":1,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/fs/2015/3010/"}],"country":"United States","state":"Kansas","otherGeospatial":"Little Arkansas River","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              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jlanning@usgs.gov","contributorId":5809,"corporation":false,"usgs":true,"family":"Lanning-Rush","given":"Jennifer L.","email":"jlanning@usgs.gov","affiliations":[{"id":353,"text":"Kansas Water Science Center","active":false,"usgs":true}],"preferred":false,"id":546186,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Ziegler, Andrew C. aziegler@usgs.gov","contributorId":433,"corporation":false,"usgs":true,"family":"Ziegler","given":"Andrew C.","email":"aziegler@usgs.gov","affiliations":[{"id":353,"text":"Kansas Water Science Center","active":false,"usgs":true}],"preferred":false,"id":546187,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70102607,"text":"sir20135040 - 2015 - Hydrology of the middle San Pedro area, southeastern Arizona","interactions":[],"lastModifiedDate":"2018-04-02T15:20:22","indexId":"sir20135040","displayToPublicDate":"2015-05-05T10:45:00","publicationYear":"2015","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":334,"text":"Scientific Investigations Report","code":"SIR","onlineIssn":"2328-0328","printIssn":"2328-031X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2013-5040","title":"Hydrology of the middle San Pedro area, southeastern Arizona","docAbstract":"<p>In the middle San Pedro Watershed in southeastern Arizona, groundwater is the primary source of water supply for municipal, domestic, industrial, and agricultural use. The watershed comprises two smaller subareas, the Benson subarea and the Narrows-Redington subarea. Early 21st century projections for heavy population growth in the watershed have not yet become a reality, but increased groundwater withdrawals could have undesired consequences - such as decreased base flow to the San Pedro River, and groundwater-level declines - that would lead to the need to deepen existing wells. This report describes the hydrology, hydrochemistry, water quality, and development of a groundwater budget for the middle San Pedro Watershed, focusing primarily on the elements of groundwater movement that could be most useful for the development of a groundwater model</p><p>Precipitation data from Tombstone, Arizona, and base flow at the stream-gaging station on the San Pedro River at Charleston both show relatively dry periods during the 1960s through the mid-1980s and in the mid-1990s to 2009, and wetter periods from the mid-1980s through the mid-1990s. Water levels in four out of five wells near the mountain fronts show cyclical patterns of recharge, with rates of recharge greatest in the early 1980s through the mid-1990s. Three wells near the San Pedro River recorded their lowest levels during the 1950s to the mid-1960s. The water-level record from one well, completed in the confined part of the coarse-grained lower basin fill, showed a decline of approximately 21 meters.</p><p>Annual flow of the San Pedro River, measured at the Charleston and Redington gages, has decreased since the 1940s. The median annual streamflow and base flow at the gaging station on the river near Tombstone has decreased by 50 percent between the periods 1968–1986 and 1997–2009. Estimates of streamflow infiltration along the San Pedro River during 1914–2009 have decreased 44 percent, with the largest decreases in the months June–October in the Benson subarea. In the Narrows-Redington subarea, streamflow infiltration has decreased about 65 percent during 1914–2009.</p><p>The average annual outflow (27.6 hm<sup>3</sup>/year [cubic hectometers per year]) from the Benson subarea aquifer for water years 2001 through 2009 exceeded the inflows (20.0 hm<sup>3</sup>/ yr) by 7.60 hm<sup>3</sup>/yr. In the Narrows-Redington subarea for the same period, the average annual outflow (15.7 hm<sup>3</sup>/yr) from the aquifer system exceeded the inflows (13.8 hm<sup>3</sup>/yr) by nearly 2 hm<sup>3</sup>/yr. The largest withdrawals of groundwater in both subareas are for irrigation; these withdrawals peaked in 1973 and have been steadily decreasing since then. Recharge from streamflow infiltration exceeded recharge from the mountain-front and from ephemeral channels in the Benson subarea. In the Narrows-Redington subarea, however, recharge from mountain-front and ephemeral channel recharge exceeded recharge from streamflow infiltration. Evapotranspiration by phreatophytes accounts for the largest outflow of groundwater for both subareas—78 percent of the outflow in the Narrows-Redington subarea and 62 percent of the outflow in the Benson subarea.</p><p>Precipitation, surface-water, and groundwater chemistry and isotope data indicated the relative age and residence time of groundwater, the amount of interaction between geologic sources and groundwater, and how recharge elevation and season were related to the presence of modern water. The bedrock aquifer receives modern recharge (</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/sir20135040","collaboration":"Prepared in cooperation with the Arizona Department of Water Resources","usgsCitation":"Cordova, J.T., Dickinson, J.E., Beisner, K.R., Hopkins, C.B., Kennedy, J.R., Pool, D.R., Glenn, E.P., Nagler, P.L., and Thomas, B.E., 2015, Hydrology of the middle San Pedro Watershed, southeastern Arizona: U.S. Geological Survey Scientific Investigations Report 2013–5040, 77 p., https://dx.doi.org/10.3133/sir20135040.","productDescription":"vii, 77 p.","numberOfPages":"88","onlineOnly":"Y","additionalOnlineFiles":"N","ipdsId":"IP-037275","costCenters":[{"id":128,"text":"Arizona Water Science 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Park Avenue<br />Tucson, AZ 85719<br /><a href=\"http://az.water.usgs.gov/\">http://az.water.usgs.gov/</a></p>","tableOfContents":"<ul>\n<li>Abstract</li>\n<li>Acknowledgments</li>\n<li>Introduction</li>\n<li>Climate</li>\n<li>Surface Water</li>\n<li>Hydrogeology</li>\n<li>Groundwater Budgets</li>\n<li>Groundwater Discharge</li>\n<li>Hydrochemistry and Water Quality</li>\n<li>Study Limitations and Considerations for Future Data Collection and Analysis</li>\n<li>Summary and Conclusions</li>\n<li>References Cited</li>\n<li>Appendix</li>\n</ul>","publishingServiceCenter":{"id":14,"text":"Menlo Park PSC"},"publishedDate":"2015-05-05","noUsgsAuthors":false,"publicationDate":"2015-05-05","publicationStatus":"PW","scienceBaseUri":"5549dba1e4b064e4207ca3f4","contributors":{"authors":[{"text":"Cordova, Jeffrey T. jcordova@usgs.gov","contributorId":1845,"corporation":false,"usgs":true,"family":"Cordova","given":"Jeffrey T.","email":"jcordova@usgs.gov","affiliations":[{"id":472,"text":"New Mexico Water Science Center","active":true,"usgs":true}],"preferred":false,"id":518735,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Dickinson, Jesse E. 0000-0002-0048-0839 jdickins@usgs.gov","orcid":"https://orcid.org/0000-0002-0048-0839","contributorId":152545,"corporation":false,"usgs":true,"family":"Dickinson","given":"Jesse","email":"jdickins@usgs.gov","middleInitial":"E.","affiliations":[{"id":128,"text":"Arizona Water Science Center","active":true,"usgs":true}],"preferred":true,"id":546099,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Beisner, Kimberly R. 0000-0002-2077-6899 kbeisner@usgs.gov","orcid":"https://orcid.org/0000-0002-2077-6899","contributorId":2733,"corporation":false,"usgs":true,"family":"Beisner","given":"Kimberly","email":"kbeisner@usgs.gov","middleInitial":"R.","affiliations":[{"id":128,"text":"Arizona Water Science Center","active":true,"usgs":true},{"id":472,"text":"New Mexico Water Science Center","active":true,"usgs":true}],"preferred":true,"id":546100,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Hopkins, Candice B. 0000-0003-3207-7267 chopkins@usgs.gov","orcid":"https://orcid.org/0000-0003-3207-7267","contributorId":1379,"corporation":false,"usgs":true,"family":"Hopkins","given":"Candice","email":"chopkins@usgs.gov","middleInitial":"B.","affiliations":[{"id":343,"text":"Idaho Water Science Center","active":true,"usgs":true}],"preferred":true,"id":546101,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Kennedy, Jeffrey R. 0000-0002-3365-6589 jkennedy@usgs.gov","orcid":"https://orcid.org/0000-0002-3365-6589","contributorId":2172,"corporation":false,"usgs":true,"family":"Kennedy","given":"Jeffrey","email":"jkennedy@usgs.gov","middleInitial":"R.","affiliations":[{"id":128,"text":"Arizona Water Science Center","active":true,"usgs":true}],"preferred":true,"id":546102,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Pool, Donald R. drpool@usgs.gov","contributorId":1121,"corporation":false,"usgs":true,"family":"Pool","given":"Donald","email":"drpool@usgs.gov","middleInitial":"R.","affiliations":[{"id":128,"text":"Arizona Water Science Center","active":true,"usgs":true}],"preferred":true,"id":546103,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Glenn, Edward P.","contributorId":19289,"corporation":false,"usgs":true,"family":"Glenn","given":"Edward","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":546104,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Nagler, Pamela L. 0000-0003-0674-103X pnagler@usgs.gov","orcid":"https://orcid.org/0000-0003-0674-103X","contributorId":1398,"corporation":false,"usgs":true,"family":"Nagler","given":"Pamela","email":"pnagler@usgs.gov","middleInitial":"L.","affiliations":[{"id":568,"text":"Southwest Biological Science Center","active":true,"usgs":true}],"preferred":true,"id":546105,"contributorType":{"id":1,"text":"Authors"},"rank":8},{"text":"Thomas, Blakemore E.","contributorId":93871,"corporation":false,"usgs":true,"family":"Thomas","given":"Blakemore","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":546106,"contributorType":{"id":1,"text":"Authors"},"rank":9}]}}
,{"id":70137292,"text":"ofr20151002 - 2015 - Quantification of shoreline change along Hatteras Island, North Carolina: Oregon Inlet to Cape Hatteras, 1978-2002, and associated vector shoreline data","interactions":[],"lastModifiedDate":"2015-05-05T08:22:49","indexId":"ofr20151002","displayToPublicDate":"2015-05-05T09:15:00","publicationYear":"2015","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2015-1002","title":"Quantification of shoreline change along Hatteras Island, North Carolina: Oregon Inlet to Cape Hatteras, 1978-2002, and associated vector shoreline data","docAbstract":"<p><span>Shoreline change spanning twenty-four years was assessed along the coastline of Cape Hatteras National Seashore, at Hatteras Island, North Carolina. The shorelines used in the analysis were generated from georeferenced historical aerial imagery and are used to develop shoreline change rates for Hatteras Island, from Oregon Inlet to Cape Hatteras. A total of 14 dates of aerial photographs ranging from 1978 through 2002 were obtained from the U.S. Army Corp of Engineers Field Research Facility in Duck, North Carolina, and scanned to generate digital imagery. The digital imagery was georeferenced and high water line shorelines (interpreted from the wet/dry line) were digitized from each date to produce a time series of shorelines for the study area. Rates of shoreline change were calculated for three periods: the full span of the time series, 1978 through 2002, and two approximately decadal subsets, 1978&ndash;89 and 1989&ndash;2002.</span></p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr20151002","usgsCitation":"Hapke, C.J., and Henderson, R., 2015, Quantification of shoreline change along Hatteras Island, North Carolina: Oregon Inlet to Cape Hatteras, 1978-2002, and associated vector shoreline data: U.S. Geological Survey Open-File Report 2015-1002, Report: v, 13 p.; Downloads Directory, https://doi.org/10.3133/ofr20151002.","productDescription":"Report: v, 13 p.; Downloads Directory","numberOfPages":"19","onlineOnly":"Y","additionalOnlineFiles":"Y","temporalStart":"1978-01-01","temporalEnd":"2002-12-31","ipdsId":"IP-058211","costCenters":[{"id":574,"text":"St. Petersburg Coastal and Marine Science 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rehenderson@usgs.gov","contributorId":140552,"corporation":false,"usgs":true,"family":"Henderson","given":"Rachel E.","email":"rehenderson@usgs.gov","affiliations":[{"id":574,"text":"St. Petersburg Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":false,"id":546115,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70155953,"text":"70155953 - 2015 - Wind River subbasin restoration: Annual report of U.S. Geological Survey activities January 2014 through December 2014","interactions":[],"lastModifiedDate":"2016-05-03T13:55:18","indexId":"70155953","displayToPublicDate":"2015-05-05T05:15:00","publicationYear":"2015","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":4,"text":"Other Government Series"},"title":"Wind River subbasin restoration: Annual report of U.S. Geological Survey activities January 2014 through December 2014","docAbstract":"<h1>Executive Summary</h1>\n<p>The Wind River subbasin in southwest Washington State provides habitat for a population of wild Lower Columbia River steelhead <i>Oncorhynchus mykiss</i>, which are listed as threatened under the Endangered Species Act. No hatchery steelhead have been planted in the Wind River subbasin since 1994, and hatchery adults are estimated to be less than one percent of adults in any year (Thomas Buehrens, Washington Department of Fish and Wildlife, personal communication). Numerous restoration actions have been implemented in the subbasin, including the removal of Hemlock Dam on Trout Creek in 2009. We used Passive Integrated Transponder (PIT) tagging and a series of instream PIT-tag interrogation systems (PTIS) to investigate life-histories, populations, and efficacy of habitat restoration actions for these steelhead. Data from our study, and companion work by Washington Department of Fish and Wildlife (WDFW), will contribute to Bonneville Power Administration&rsquo;s (BPA) Research Monitoring and Evaluation (RM&amp;E) Program Strategy of Fish Population Status Monitoring (<a href=\"http://www.cbfish.org/ProgramStrategy.mvc/ViewProgramStrategySummary/1\">www.cbfish.org/ProgramStrategy.mvc/ViewProgramStrategySummary/1</a>), specifically the sub-strategies of: 1) Assessing the Status and Trends of Diversity of Natural Origin Fish Populations and to Uncertainties Research regarding differing life histories of a wild steelhead population, 2) Assessing the Status and Trend of Adult Natural Origin Fish Populations, and 3) Monitoring and Evaluating the Effectiveness of Tributary Habitat Actions Relative to Environmental, Physical, or Biological Performance Objectives.</p>\n<p>During summer 2014, we PIT-tagged steelhead parr in headwater areas of the Wind River subbasin to investigate life-history diversity, specifically to compare fate of those juvenile steelhead that move downstream prior to smolting with those that remain in their natal areas until smolting. A series of instream PTISs monitored movement of these fish. We added a new multi-antenna PTIS on Trout Creek and made improvements to two of our smaller tributary PTISs during 2014. Detections at the instream PTISs showed trends of parr emigration during summer and fall, in addition to the expected movement of parr and smolts in spring. Long-term monitoring of PIT-tagged fish will provide information on contribution of various life-history&nbsp;strategies to smolt production and adult returns, as well as helping to identify factors influencing parr movement.</p>\n<p>Movements of PIT-tagged adult steelhead were tracked with our instream PTISs. These data will contribute to a better understanding of timing and distribution of spawning by this population of wild steelhead within the Wind River subbasin. Additionally, these data have provided information on timing of adult movements to various parts of the watershed, which is allowing us to assess adult use of tributary watersheds within the Wind River subbasin. These data are contributing to evaluating steelhead response to the removal of Hemlock Dam from Trout Creek. Hemlock Dam, which was located at rkm 2.0 of Trout Creek, was removed in summer 2009 and had contributed to hydrologic impairment of Trout Creek and potentially caused some deterrent to upstream adult steelhead migration.</p>\n<p>Evaluating restoration efforts is of interest to many managers and agencies so that funding and time are allocated for best results. The evaluation of various life-histories of Lower Columbia River steelhead within the Wind River subbasin provides information to better track populations, and more effectively direct habitat restoration and water allocation planning. Increasingly detailed Viable Salmonid Population information (Crawford and Rumsey 2009), such as that provided by PIT-tagging and instream PTISs networks like those we build and operate in the Wind River subbasin, provide data to better inform policy and management, as life-history strategies and production bottlenecks are identified and understood.</p>","language":"English","publisher":"Bonneville Power Administration","collaboration":"Report covers work performed under Bonneville Power Administration contract #(s) 63276, 66668","usgsCitation":"Jezorek, I.G., and Connolly, P., 2015, Wind River subbasin restoration: Annual report of U.S. Geological Survey activities January 2014 through December 2014, 58 p.","productDescription":"58 p.","startPage":"58 p.","onlineOnly":"N","additionalOnlineFiles":"N","ipdsId":"IP-064417","costCenters":[{"id":654,"text":"Western Fisheries Research Center","active":true,"usgs":true}],"links":[{"id":320550,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":320576,"type":{"id":11,"text":"Document"},"url":"https://pisces.bpa.gov/release/documents/DocumentViewer.aspx?doc=P144015","text":"Report","size":"763.04 KB","linkFileType":{"id":1,"text":"pdf"},"description":"Report"}],"country":"United States","state":"Washington","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -122.04540252685548,\n              45.7964939814375\n            ],\n            [\n              -122.04540252685548,\n              45.96952673162373\n            ],\n            [\n              -121.89571380615234,\n              45.96952673162373\n            ],\n            [\n              -121.89571380615234,\n              45.7964939814375\n            ],\n            [\n              -122.04540252685548,\n              45.7964939814375\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","publishingServiceCenter":{"id":12,"text":"Tacoma PSC"},"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5720913ae4b071321fe656bf","contributors":{"authors":[{"text":"Jezorek, Ian G. 0000-0002-3842-3485 ijezorek@usgs.gov","orcid":"https://orcid.org/0000-0002-3842-3485","contributorId":3572,"corporation":false,"usgs":true,"family":"Jezorek","given":"Ian","email":"ijezorek@usgs.gov","middleInitial":"G.","affiliations":[{"id":654,"text":"Western Fisheries Research Center","active":true,"usgs":true}],"preferred":true,"id":567343,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Connolly, Patrick J. 0000-0001-7365-7618 pconnolly@usgs.gov","orcid":"https://orcid.org/0000-0001-7365-7618","contributorId":2920,"corporation":false,"usgs":true,"family":"Connolly","given":"Patrick J.","email":"pconnolly@usgs.gov","affiliations":[{"id":654,"text":"Western Fisheries Research Center","active":true,"usgs":true}],"preferred":true,"id":567344,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70147158,"text":"ofr20151081 - 2015 - Storm tide monitoring during the blizzard of January 26-28, 2015, in eastern Massachusetts","interactions":[],"lastModifiedDate":"2015-05-01T14:55:29","indexId":"ofr20151081","displayToPublicDate":"2015-05-01T15:45:00","publicationYear":"2015","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2015-1081","title":"Storm tide monitoring during the blizzard of January 26-28, 2015, in eastern Massachusetts","docAbstract":"<p>The U.S. Geological Survey (USGS) deployed a temporary monitoring network of six storm surge sensors and four barometric pressure sensors along the Atlantic coast in eastern Massachusetts, from Plymouth to Newburyport, before the blizzard of January 26&ndash;28, 2015 (Blizzard of January 2015), to record the timing and magnitude of storm tide at select locations where forecasters had predicted the potential for coastal flooding. Additionally, water-level data were recorded and transmitted in near real-time from four permanent USGS tidal stations&mdash;three on Cape Cod and one near the mouth of the Merrimack River in Newburyport. The storm surge sensors were deployed at previously established fixed sites outfitted with presurveyed mounting brackets. The mounting brackets were installed in 2014 as part of the USGS Surge, Wave, and Tide Hydrodynamic (SWaTH) Network (<a href=\"http://pubs.usgs.gov/of/2015/1081/508pdf/ofr20150-1081.pdf\">https://water.usgs.gov/floods/STN/</a>), which was funded through congressional supplemental appropriations for the U.S. Department of the Interior after the devastating landfall of Hurricane Sandy on October 29, 2012 (Simmons and others, 2014). The USGS received this funding to enable better understanding of coastal flooding hazards in the region, to improve preparedness for future coastal storms, and to increase the resilience of coastal cities, infrastructure, and natural systems in the region (Buxton and others, 2013). The USGS established 163 monitoring locations along the New England coast for the SWaTH Network, including 70 sites in Massachusetts.</p>\n<p>The Blizzard of January 2015 was a powerful and destructive storm that threatened public safety and led to widespread cancellations and delays at transportation hubs, schools, and businesses in Massachusetts, including, for example, the closure of General Edward Lawrence Logan (Boston-Logan) International Airport and cancellation of all flights on January 27 and a statewide travel ban issued for January 28. A total of 24.6 inches of snowfall and winds up to 45 miles per hour (mi/hr) were recorded at the airport. Several coastal communities were affected and experienced flooding, overwash, and damage to seawalls, dwellings, and other infrastructure. In Scituate, the National Guard was sent to rescue people from flooding, and power was cut to some areas of the town to prevent electrical fires.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr20151081","usgsCitation":"Massey, A.J., and Verdi, R.J., 2015, Storm tide monitoring during the blizzard of January 26-28, 2015, in eastern Massachusetts: U.S. Geological Survey Open-File Report 2015-1081, iv, 7 p., https://doi.org/10.3133/ofr20151081.","productDescription":"iv, 7 p.","numberOfPages":"16","onlineOnly":"Y","additionalOnlineFiles":"N","temporalStart":"2015-01-26","temporalEnd":"2015-01-28","ipdsId":"IP-064196","costCenters":[{"id":466,"text":"New England Water Science 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ajmassey@usgs.gov","orcid":"https://orcid.org/0000-0003-3995-8657","contributorId":1862,"corporation":false,"usgs":true,"family":"Massey","given":"Andrew","email":"ajmassey@usgs.gov","middleInitial":"J.","affiliations":[{"id":376,"text":"Massachusetts Water Science Center","active":true,"usgs":true},{"id":466,"text":"New England Water Science Center","active":true,"usgs":true}],"preferred":true,"id":545712,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Verdi, Richard J. 0000-0002-7093-9203 rverdi@usgs.gov","orcid":"https://orcid.org/0000-0002-7093-9203","contributorId":1098,"corporation":false,"usgs":true,"family":"Verdi","given":"Richard","email":"rverdi@usgs.gov","middleInitial":"J.","affiliations":[{"id":502,"text":"Office of Surface Water","active":true,"usgs":true},{"id":376,"text":"Massachusetts Water Science Center","active":true,"usgs":true}],"preferred":true,"id":545713,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70155516,"text":"70155516 - 2015 - Temporal patterns in adult salmon migration timing across southeast Alaska","interactions":[],"lastModifiedDate":"2015-08-10T10:49:46","indexId":"70155516","displayToPublicDate":"2015-05-01T12:00:00","publicationYear":"2015","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1837,"text":"Global Change Biology","active":true,"publicationSubtype":{"id":10}},"title":"Temporal patterns in adult salmon migration timing across southeast Alaska","docAbstract":"<p>Pacific salmon migration timing can drive population productivity, ecosystem dynamics, and human harvest. Nevertheless, little is known about long-term variation in salmon migration timing for multiple species across broad regions. We used long-term data for five Pacific salmon species throughout rapidly warming southeast Alaska to describe long-term changes in salmon migration timing, interannual phenological synchrony, relationships between climatic variation and migratory timing, and to test whether long-term changes in migration timing are related to glaciation in headwater streams. Temporal changes in the median date of salmon migration timing varied widely across species. Most sockeye populations are migrating later over time (11 of 14), but pink, chum, and especially coho populations are migrating earlier than they did historically (16 of 19 combined). Temporal trends in duration and interannual variation in migration timing were highly variable across species and populations. The greatest temporal shifts in the median date of migration timing were correlated with decreases in the duration of migration timing, suggestive of a loss of phenotypic variation due to natural selection. Pairwise interannual correlations in migration timing varied widely but were generally positive, providing evidence for weak region-wide phenological synchrony. This synchrony is likely a function of climatic variation, as interannual variation in migration timing was related to climatic phenomenon operating at large- (Pacific decadal oscillation), moderate- (sea surface temperature), and local-scales (precipitation). Surprisingly, the presence or the absence of glaciers within a watershed was unrelated to long-term shifts in phenology. Overall, there was extensive heterogeneity in long-term patterns of migration timing throughout this climatically and geographically complex region, highlighting that future climatic change will likely have widely divergent impacts on salmon migration timing. Although salmon phenological diversity will complicate future predictions of migration timing, this variation likely acts as a major contributor to population and ecosystem resiliency in southeast Alaska.</p>","language":"English","publisher":"Wiley","publisherLocation":"Hoboken, NJ","doi":"10.1111/gcb.12829","usgsCitation":"Kovach, R., Ellison, S., Pyare, S., and Tallmon, D., 2015, Temporal patterns in adult salmon migration timing across southeast Alaska: Global Change Biology, v. 21, no. 5, p. 1821-1833, https://doi.org/10.1111/gcb.12829.","productDescription":"13 p.","startPage":"1821","endPage":"1833","numberOfPages":"13","onlineOnly":"N","additionalOnlineFiles":"N","ipdsId":"IP-061254","costCenters":[{"id":481,"text":"Northern Rocky Mountain Science Center","active":true,"usgs":true}],"links":[{"id":472105,"rank":0,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1111/gcb.12829","text":"Publisher Index Page"},{"id":306531,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Alaska","otherGeospatial":"Southeast Alaska","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -141.35009765625,\n              59.60109549032134\n            ],\n            [\n              -134.80224609375,\n              60.941106295036136\n            ],\n            [\n              -130.693359375,\n              60.27251459483244\n            ],\n            [\n              -128.64990234375,\n              58.90464570302001\n            ],\n            [\n              -128.38623046875,\n              56.48676175249086\n            ],\n            [\n              -127.77099609374999,\n              55.29162848682989\n            ],\n            [\n              -129.9462890625,\n              54.23955053156179\n            ],\n            [\n              -132.91259765625,\n              53.46189043285914\n            ],\n            [\n              -141.35009765625,\n              59.60109549032134\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"21","issue":"5","publishingServiceCenter":{"id":2,"text":"Denver PSC"},"noUsgsAuthors":false,"publicationDate":"2015-02-06","publicationStatus":"PW","scienceBaseUri":"55c9cb39e4b08400b1fdb72e","chorus":{"doi":"10.1111/gcb.12829","url":"http://dx.doi.org/10.1111/gcb.12829","publisher":"Wiley-Blackwell","authors":"Kovach Ryan P., Ellison Stephen C., Pyare Sanjay, Tallmon David A.","journalName":"Global Change Biology","publicationDate":"2/6/2015","auditedOn":"6/11/2015"},"contributors":{"authors":[{"text":"Kovach, Ryan P.","contributorId":126724,"corporation":false,"usgs":false,"family":"Kovach","given":"Ryan P.","affiliations":[{"id":6580,"text":"University of Montana, Flathead Lake Biological Station, Polson, Montana 59860, USA","active":true,"usgs":false}],"preferred":false,"id":565655,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Ellison, Stephen","contributorId":145919,"corporation":false,"usgs":false,"family":"Ellison","given":"Stephen","email":"","affiliations":[{"id":16298,"text":"University of Alaska Southeast","active":true,"usgs":false}],"preferred":false,"id":565656,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Pyare, Sanjay","contributorId":47135,"corporation":false,"usgs":true,"family":"Pyare","given":"Sanjay","email":"","affiliations":[],"preferred":false,"id":565657,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Tallmon, David","contributorId":145920,"corporation":false,"usgs":false,"family":"Tallmon","given":"David","affiliations":[{"id":16298,"text":"University of Alaska Southeast","active":true,"usgs":false}],"preferred":false,"id":565658,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70148076,"text":"70148076 - 2015 - AMDTreat 5.0+ with PHREEQC titration module to compute caustic chemical quantity, effluent quality, and sludge volume","interactions":[],"lastModifiedDate":"2020-02-25T15:43:38","indexId":"70148076","displayToPublicDate":"2015-05-01T11:45:00","publicationYear":"2015","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2745,"text":"Mine Water and the Environment","active":true,"publicationSubtype":{"id":10}},"title":"AMDTreat 5.0+ with PHREEQC titration module to compute caustic chemical quantity, effluent quality, and sludge volume","docAbstract":"<p>Alkaline chemicals are commonly added to discharges from coal mines to increase pH and decrease concentrations of acidity and dissolved aluminum, iron, manganese, and associated metals. The annual cost of chemical treatment depends on the type and quantities of chemicals added and sludge produced. The AMDTreat computer program, initially developed in 2003, is widely used to compute such costs on the basis of the user-specified flow rate and water quality data for the untreated AMD. Although AMDTreat can use results of empirical titration of net-acidic or net-alkaline effluent with caustic chemicals to accurately estimate costs for treatment, such empirical data are rarely available. A titration simulation module using the geochemical program PHREEQC has been incorporated with AMDTreat 5.0+ to improve the capability of AMDTreat to estimate: (1) the quantity and cost of caustic chemicals to attain a target pH, (2) the chemical composition of the treated effluent, and (3) the volume of sludge produced by the treatment. The simulated titration results for selected caustic chemicals (NaOH, CaO, Ca(OH)2, Na2CO3, or NH3) without aeration or with pre-aeration can be compared with or used in place of empirical titration data to estimate chemical quantities, treated effluent composition, sludge volume (precipitated metals plus unreacted chemical), and associated treatment costs. This paper describes the development, evaluation, and potential utilization of the PHREEQC titration module with the new AMDTreat 5.0+ computer program available at http://www.amd.osmre.gov/.</p>","language":"English","publisher":"International Mine Water Association","publisherLocation":"Berlin","doi":"10.1007/s10230-014-0292-6","usgsCitation":"Cravotta, C., Means, B.P., Arthur, W., McKenzie, R.M., and Parkhurst, D.L., 2015, AMDTreat 5.0+ with PHREEQC titration module to compute caustic chemical quantity, effluent quality, and sludge volume: Mine Water and the Environment, v. 34, no. 2, p. 136-152, https://doi.org/10.1007/s10230-014-0292-6.","productDescription":"17 p.","startPage":"136","endPage":"152","numberOfPages":"17","onlineOnly":"N","additionalOnlineFiles":"N","ipdsId":"IP-043936","costCenters":[{"id":532,"text":"Pennsylvania Water Science Center","active":true,"usgs":true},{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":300543,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"34","issue":"2","publishingServiceCenter":{"id":10,"text":"Baltimore PSC"},"noUsgsAuthors":false,"publicationDate":"2014-07-27","publicationStatus":"PW","scienceBaseUri":"555c5eafe4b0a92fa7eacbf0","contributors":{"authors":[{"text":"Cravotta, Charles A. III 0000-0003-3116-4684 cravotta@usgs.gov","orcid":"https://orcid.org/0000-0003-3116-4684","contributorId":138829,"corporation":false,"usgs":true,"family":"Cravotta","given":"Charles A.","suffix":"III","email":"cravotta@usgs.gov","affiliations":[{"id":532,"text":"Pennsylvania Water Science Center","active":true,"usgs":true}],"preferred":false,"id":547174,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Means, Brent P","contributorId":140842,"corporation":false,"usgs":false,"family":"Means","given":"Brent","email":"","middleInitial":"P","affiliations":[{"id":13592,"text":"US Office of Surface Mining","active":true,"usgs":false}],"preferred":false,"id":547176,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Arthur, Willam","contributorId":140844,"corporation":false,"usgs":false,"family":"Arthur","given":"Willam","email":"","affiliations":[{"id":13592,"text":"US Office of Surface Mining","active":true,"usgs":false}],"preferred":false,"id":547178,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"McKenzie, Robert M","contributorId":140843,"corporation":false,"usgs":false,"family":"McKenzie","given":"Robert","email":"","middleInitial":"M","affiliations":[{"id":13592,"text":"US Office of Surface Mining","active":true,"usgs":false}],"preferred":false,"id":547177,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Parkhurst, David L. 0000-0003-3348-1544 dlpark@usgs.gov","orcid":"https://orcid.org/0000-0003-3348-1544","contributorId":1088,"corporation":false,"usgs":true,"family":"Parkhurst","given":"David","email":"dlpark@usgs.gov","middleInitial":"L.","affiliations":[{"id":5044,"text":"National Research Program - Central Branch","active":true,"usgs":true}],"preferred":true,"id":547175,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":70148402,"text":"70148402 - 2015 - Experimental dosing of wetlands with coagulants removes mercury from surface water and decreases mercury bioaccumulation in fish","interactions":[],"lastModifiedDate":"2018-09-04T15:40:13","indexId":"70148402","displayToPublicDate":"2015-05-01T10:45:00","publicationYear":"2015","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1565,"text":"Environmental Science & Technology","onlineIssn":"1520-5851","printIssn":"0013-936X","active":true,"publicationSubtype":{"id":10}},"title":"Experimental dosing of wetlands with coagulants removes mercury from surface water and decreases mercury bioaccumulation in fish","docAbstract":"<p><span>Mercury pollution is widespread globally, and strategies for managing mercury contamination in aquatic environments are necessary. We tested whether coagulation with metal-based salts could remove mercury from wetland surface waters and decrease mercury bioaccumulation in fish. In a complete randomized block design, we constructed nine experimental wetlands in California’s Sacramento–San Joaquin Delta, stocked them with mosquitofish (</span><i>Gambusia affinis</i><span>), and then continuously applied agricultural drainage water that was either untreated (control), or treated with polyaluminum chloride or ferric sulfate coagulants. Total mercury and methylmercury concentrations in surface waters were decreased by 62% and 63% in polyaluminum chloride treated wetlands and 50% and 76% in ferric sulfate treated wetlands compared to control wetlands. Specifically, following coagulation, mercury was transferred from the filtered fraction of water into the particulate fraction of water which then settled within the wetland. Mosquitofish mercury concentrations were decreased by 35% in ferric sulfate treated wetlands compared to control wetlands. There was no reduction in mosquitofish mercury concentrations within the polyaluminum chloride treated wetlands, which may have been caused by production of bioavailable methylmercury within those wetlands. Coagulation may be an effective management strategy for reducing mercury contamination within wetlands, but further studies should explore potential effects on wetland ecosystems.</span></p>","language":"English","publisher":"American Chemical Society","doi":"10.1021/acs.est.5b00655","usgsCitation":"Ackerman, J., Kraus, T.E., Fleck, J., Krabbenhoft, D.P., Horwarth, W.R., Bachand, S., Herzog, M.P., Hartman, C.A., and Bachand, P., 2015, Experimental dosing of wetlands with coagulants removes mercury from surface water and decreases mercury bioaccumulation in fish: Environmental Science & Technology, v. 49, no. 10, p. 6304-6311, https://doi.org/10.1021/acs.est.5b00655.","productDescription":"8 p.","startPage":"6304","endPage":"6311","onlineOnly":"N","additionalOnlineFiles":"N","ipdsId":"IP-061945","costCenters":[{"id":154,"text":"California Water Science Center","active":true,"usgs":true},{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true},{"id":651,"text":"Western Ecological Research Center","active":true,"usgs":true}],"links":[{"id":300962,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"California","otherGeospatial":"Sacramento-San Joaquin Delta","volume":"49","issue":"10","publishingServiceCenter":{"id":1,"text":"Sacramento PSC"},"noUsgsAuthors":false,"publicationDate":"2015-05-04","publicationStatus":"PW","scienceBaseUri":"556ed3bbe4b0d9246a9fa7d7","chorus":{"doi":"10.1021/acs.est.5b00655","url":"http://dx.doi.org/10.1021/acs.est.5b00655","publisher":"American Chemical Society (ACS)","authors":"Ackerman Joshua T., Kraus Tamara E. C., Fleck Jacob A., Krabbenhoft David P., Horwath William R., Bachand Sandra M., Herzog Mark P., Hartman C. Alex, Bachand Philip A. M.","journalName":"Environmental Science & Technology","publicationDate":"5/19/2015","auditedOn":"7/24/2015"},"contributors":{"authors":[{"text":"Ackerman, Joshua T. 0000-0002-3074-8322 jackerman@usgs.gov","orcid":"https://orcid.org/0000-0002-3074-8322","contributorId":147078,"corporation":false,"usgs":true,"family":"Ackerman","given":"Joshua T.","email":"jackerman@usgs.gov","affiliations":[{"id":651,"text":"Western Ecological Research Center","active":true,"usgs":true}],"preferred":false,"id":548006,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Kraus, Tamara E.C. 0000-0002-5187-8644 tkraus@usgs.gov","orcid":"https://orcid.org/0000-0002-5187-8644","contributorId":1452,"corporation":false,"usgs":true,"family":"Kraus","given":"Tamara","email":"tkraus@usgs.gov","middleInitial":"E.C.","affiliations":[{"id":154,"text":"California Water Science Center","active":true,"usgs":true}],"preferred":false,"id":548007,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Fleck, Jacob A. 0000-0002-3217-3972 jafleck@usgs.gov","orcid":"https://orcid.org/0000-0002-3217-3972","contributorId":141024,"corporation":false,"usgs":true,"family":"Fleck","given":"Jacob A.","email":"jafleck@usgs.gov","affiliations":[{"id":651,"text":"Western Ecological Research Center","active":true,"usgs":true}],"preferred":false,"id":548008,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Krabbenhoft, David P. 0000-0003-1964-5020 dpkrabbe@usgs.gov","orcid":"https://orcid.org/0000-0003-1964-5020","contributorId":1658,"corporation":false,"usgs":true,"family":"Krabbenhoft","given":"David","email":"dpkrabbe@usgs.gov","middleInitial":"P.","affiliations":[{"id":677,"text":"Wisconsin Water Science Center","active":true,"usgs":true},{"id":5044,"text":"National Research Program - Central Branch","active":true,"usgs":true},{"id":37464,"text":"WMA - Laboratory & Analytical Services Division","active":true,"usgs":true},{"id":37947,"text":"Upper Midwest Water Science Center","active":true,"usgs":true}],"preferred":true,"id":548009,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Horwarth, William R.","contributorId":141025,"corporation":false,"usgs":false,"family":"Horwarth","given":"William","email":"","middleInitial":"R.","affiliations":[{"id":7214,"text":"University of California, Davis","active":true,"usgs":false}],"preferred":false,"id":548010,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Bachand, Sandra M.","contributorId":45542,"corporation":false,"usgs":false,"family":"Bachand","given":"Sandra M.","affiliations":[{"id":12526,"text":"Bachand & Associates","active":true,"usgs":false}],"preferred":false,"id":548011,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Herzog, Mark P. 0000-0002-5203-2835 mherzog@usgs.gov","orcid":"https://orcid.org/0000-0002-5203-2835","contributorId":131158,"corporation":false,"usgs":true,"family":"Herzog","given":"Mark","email":"mherzog@usgs.gov","middleInitial":"P.","affiliations":[{"id":651,"text":"Western Ecological Research Center","active":true,"usgs":true}],"preferred":true,"id":548012,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Hartman, C. Alex 0000-0002-7222-1633 chartman@usgs.gov","orcid":"https://orcid.org/0000-0002-7222-1633","contributorId":131157,"corporation":false,"usgs":true,"family":"Hartman","given":"C.","email":"chartman@usgs.gov","middleInitial":"Alex","affiliations":[{"id":651,"text":"Western Ecological Research Center","active":true,"usgs":true}],"preferred":true,"id":548013,"contributorType":{"id":1,"text":"Authors"},"rank":8},{"text":"Bachand, Philip","contributorId":81013,"corporation":false,"usgs":false,"family":"Bachand","given":"Philip","email":"","affiliations":[{"id":12526,"text":"Bachand & Associates","active":true,"usgs":false}],"preferred":false,"id":548014,"contributorType":{"id":1,"text":"Authors"},"rank":9}]}}
,{"id":70148061,"text":"70148061 - 2015 - Inter-laboratory variation in the chemical analysis of acidic forest soil reference samples from eastern North America","interactions":[],"lastModifiedDate":"2015-05-18T09:22:41","indexId":"70148061","displayToPublicDate":"2015-05-01T10:30:00","publicationYear":"2015","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1475,"text":"Ecosphere","active":true,"publicationSubtype":{"id":10}},"title":"Inter-laboratory variation in the chemical analysis of acidic forest soil reference samples from eastern North America","docAbstract":"<p>Long-term forest soil monitoring and research often requires a comparison of laboratory data generated at different times and in different laboratories. Quantifying the uncertainty associated with these analyses is necessary to assess temporal changes in soil properties. Forest soil chemical properties, and methods to measure these properties, often differ from agronomic and horticultural soils. Soil proficiency programs do not generally include forest soil samples that are highly acidic, high in extractable Al, low in extractable Ca and often high in carbon. To determine the uncertainty associated with specific analytical methods for forest soils, we collected and distributed samples from two soil horizons (Oa and Bs) to 15 laboratories in the eastern United States and Canada. Soil properties measured included total organic carbon and nitrogen, pH and exchangeable cations. Overall, results were consistent despite some differences in methodology. We calculated the median absolute deviation (MAD) for each measurement and considered the acceptable range to be the median 6 2.5 3 MAD. Variability among laboratories was usually as low as the typical variability within a laboratory. A few areas of concern include a lack of consistency in the measurement and expression of results on a dry weight basis, relatively high variability in the C/N ratio in the Bs horizon, challenges associated with determining exchangeable cations at concentrations near the lower reporting range of some laboratories and the operationally defined nature of aluminum extractability. Recommendations include a continuation of reference forest soil exchange programs to quantify the uncertainty associated with these analyses in conjunction with ongoing efforts to review and standardize laboratory methods.</p>","language":"English","publisher":"Ecological Society of America","publisherLocation":"Washington, D.C.","doi":"10.1890/ES14-00209.1","collaboration":"New York State Energy Research and Development Authority; USGS","usgsCitation":"Ross, D., Bailiey, S.W., Briggs, R., Curry, J., Fernandez, I.J., Fredriksen, G., Goodale, C.L., Hazlett, P.W., Heine, P.R., Johnson, C.E., Larson, J.T., Lawrence, G.B., Kolka, R.K., , O., Pare, D., Richter, D.D., Shirmer, C.D., and Warby, R.A., 2015, Inter-laboratory variation in the chemical analysis of acidic forest soil reference samples from eastern North America: Ecosphere, v. 6, no. 5, p. 1-22, https://doi.org/10.1890/ES14-00209.1.","productDescription":"22 p.","startPage":"1","endPage":"22","numberOfPages":"22","onlineOnly":"N","additionalOnlineFiles":"N","ipdsId":"IP-060718","costCenters":[{"id":474,"text":"New York Water Science Center","active":true,"usgs":true}],"links":[{"id":490035,"rank":0,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1890/es14-00209.1","text":"Publisher Index Page"},{"id":300461,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"6","issue":"5","publishingServiceCenter":{"id":11,"text":"Pembroke PSC"},"noUsgsAuthors":false,"publicationDate":"2015-05-08","publicationStatus":"PW","scienceBaseUri":"555b0d50e4b0a92fa7eac62b","contributors":{"authors":[{"text":"Ross, Donald S.","contributorId":9565,"corporation":false,"usgs":true,"family":"Ross","given":"Donald S.","affiliations":[],"preferred":false,"id":547022,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bailiey, Scott W","contributorId":140803,"corporation":false,"usgs":false,"family":"Bailiey","given":"Scott","email":"","middleInitial":"W","affiliations":[{"id":13575,"text":"Research Geologist, Hubbard Brook Experimental Forest, USDA Forest Service, North Woodstock, NH","active":true,"usgs":false}],"preferred":false,"id":547023,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Briggs, Russell D","contributorId":140804,"corporation":false,"usgs":false,"family":"Briggs","given":"Russell D","affiliations":[{"id":13576,"text":"Professor, Div of Environmental Science, SUNY College of ESF, Syracuse NY","active":true,"usgs":false}],"preferred":false,"id":547024,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Curry, Johanna","contributorId":140805,"corporation":false,"usgs":false,"family":"Curry","given":"Johanna","email":"","affiliations":[{"id":13577,"text":"Supervisor, Great Lakes Forestry Centre, Sault Ste. Marie, Canada","active":true,"usgs":false}],"preferred":false,"id":547025,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Fernandez, Ivan J.","contributorId":80174,"corporation":false,"usgs":true,"family":"Fernandez","given":"Ivan","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":547026,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Fredriksen, Guinevere","contributorId":140806,"corporation":false,"usgs":false,"family":"Fredriksen","given":"Guinevere","email":"","affiliations":[{"id":13578,"text":"Research Support Spec I, Ecology & Evolutionary Biology, Cornell University, Ithaca NY","active":true,"usgs":false}],"preferred":false,"id":547027,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Goodale, Christine L.","contributorId":22638,"corporation":false,"usgs":true,"family":"Goodale","given":"Christine","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":547028,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Hazlett, Paul W.","contributorId":101177,"corporation":false,"usgs":true,"family":"Hazlett","given":"Paul","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":547029,"contributorType":{"id":1,"text":"Authors"},"rank":8},{"text":"Heine, Paul R","contributorId":140807,"corporation":false,"usgs":false,"family":"Heine","given":"Paul","email":"","middleInitial":"R","affiliations":[{"id":13579,"text":"Lab Admin, Nicholas School of the Environment, Duke University, Durham NC","active":true,"usgs":false}],"preferred":false,"id":547030,"contributorType":{"id":1,"text":"Authors"},"rank":9},{"text":"Johnson, Chris E.","contributorId":17539,"corporation":false,"usgs":true,"family":"Johnson","given":"Chris","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":547031,"contributorType":{"id":1,"text":"Authors"},"rank":10},{"text":"Larson, John T","contributorId":140808,"corporation":false,"usgs":false,"family":"Larson","given":"John","email":"","middleInitial":"T","affiliations":[{"id":13580,"text":"Chemist, National Research Station, USDA Forest Service, Grand Rapids MN","active":true,"usgs":false}],"preferred":false,"id":547032,"contributorType":{"id":1,"text":"Authors"},"rank":11},{"text":"Lawrence, Gregory B. 0000-0002-8035-2350 glawrenc@usgs.gov","orcid":"https://orcid.org/0000-0002-8035-2350","contributorId":867,"corporation":false,"usgs":true,"family":"Lawrence","given":"Gregory","email":"glawrenc@usgs.gov","middleInitial":"B.","affiliations":[{"id":474,"text":"New York Water Science Center","active":true,"usgs":true}],"preferred":true,"id":547021,"contributorType":{"id":1,"text":"Authors"},"rank":12},{"text":"Kolka, Randy K","contributorId":140809,"corporation":false,"usgs":false,"family":"Kolka","given":"Randy","email":"","middleInitial":"K","affiliations":[{"id":13581,"text":"Research Soil Scientist, National Research Station, USDA Forest Service, Grand Rapids MN","active":true,"usgs":false}],"preferred":false,"id":547033,"contributorType":{"id":1,"text":"Authors"},"rank":13},{"text":" Ouimet","contributorId":140810,"corporation":false,"usgs":false,"given":"Ouimet","email":"","affiliations":[{"id":13582,"text":"Director of Forestry Research, Dept of Natural Resources & Wildlife, Quebec, Canada","active":true,"usgs":false}],"preferred":false,"id":547034,"contributorType":{"id":1,"text":"Authors"},"rank":14},{"text":"Pare, D","contributorId":140812,"corporation":false,"usgs":false,"family":"Pare","given":"D","affiliations":[{"id":13584,"text":"Natural Resources Canada, Canadian Forest Service","active":true,"usgs":false}],"preferred":false,"id":547038,"contributorType":{"id":1,"text":"Authors"},"rank":15},{"text":"Richter, Daniel D.","contributorId":99458,"corporation":false,"usgs":true,"family":"Richter","given":"Daniel","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":547035,"contributorType":{"id":1,"text":"Authors"},"rank":16},{"text":"Shirmer, Charles D","contributorId":140811,"corporation":false,"usgs":false,"family":"Shirmer","given":"Charles","email":"","middleInitial":"D","affiliations":[{"id":13583,"text":"Instructional Support Specialist, Dept of Forest & Natural Resources Mgmt, SUNY College of ESF, Syracuse NY","active":true,"usgs":false}],"preferred":false,"id":547036,"contributorType":{"id":1,"text":"Authors"},"rank":17},{"text":"Warby, Richard A.F.","contributorId":94950,"corporation":false,"usgs":true,"family":"Warby","given":"Richard","email":"","middleInitial":"A.F.","affiliations":[],"preferred":false,"id":547037,"contributorType":{"id":1,"text":"Authors"},"rank":18}]}}
,{"id":70144914,"text":"sir20155052 - 2015 - Dam-breach analysis and flood-inundation mapping for selected dams in Oklahoma City, Oklahoma, and near Atoka, Oklahoma","interactions":[],"lastModifiedDate":"2015-05-01T09:03:41","indexId":"sir20155052","displayToPublicDate":"2015-05-01T08:15:00","publicationYear":"2015","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":334,"text":"Scientific Investigations Report","code":"SIR","onlineIssn":"2328-0328","printIssn":"2328-031X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2015-5052","title":"Dam-breach analysis and flood-inundation mapping for selected dams in Oklahoma City, Oklahoma, and near Atoka, Oklahoma","docAbstract":"<p>Dams provide beneficial functions such as flood control, recreation, and storage of water supplies, but they also entail risk; dam breaches and resultant floods can cause substantial property damage and loss of life. The State of Oklahoma requires each owner of a high-hazard dam, which the Federal Emergency Management Agency defines as dams for which failure or improper operation probably will cause loss of human life, to develop an emergency action plan specific to that dam. Components of an emergency action plan are to simulate a flood resulting from a possible dam breach and map the resulting downstream flood-inundation areas. The resulting flood-inundation maps can provide valuable information to city officials, emergency managers, and local residents for planning an emergency response if a dam breach occurs.</p>\n<p>This report presents results of a cooperative study by the U.S. Geological Survey and the City of Oklahoma City to model dam-breach scenarios at 11 dams controlled and operated by Oklahoma City, Okla., and to map the potential flood-inundation areas of such dam breaches. To assist the City of Oklahoma City with completion of the emergency action plans for the 11 dams, the U.S. Geological Survey used light detection and ranging (lidar) elevation data (2004), which produced a 2-foot contour elevation map for the flood plains around Oklahoma City. A 5-meter Digital Terrain Map was used to model the flood plain below Atoka Reservoir in southeastern Oklahoma.</p>\n<p>Digital-elevation models, field survey measurements, hydraulic data, and hydrologic data (U.S. Geological Survey streamflow-gaging stations North Canadian River below Lake Overholser near Oklahoma City, Okla. [07241000], and North Canadian River at Britton Road at Oklahoma City, Okla. [07241520]), were used as inputs for the one-dimensional dynamic (unsteady-flow) models using Hydrologic Engineering Centers River Analysis System (HEC&ndash;RAS) software. The modeled flood elevations were exported to a geographic information system to produce flood-inundation maps. Water-surface profiles were developed for a 75-percent probable maximum flood dam-breach scenario and a sunny-day dam-breach scenario, as well as for maximum flood-inundation elevations and flood-wave arrival times at selected bridge crossings. Points of interest such as community-services offices, recreational areas, water-treatment plants, and wastewater-treatment plants were identified on the flood-inundation maps.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/sir20155052","collaboration":"Prepared in cooperation with the City of Oklahoma City, Oklahoma","usgsCitation":"Shivers, M.J., Smith, S.J., Grout, T.S., and Lewis, J.M., 2015, Dam-breach analysis and flood-inundation mapping for selected dams in Oklahoma City, Oklahoma, and near Atoka, Oklahoma: U.S. Geological Survey Scientific Investigations Report 2015-5052, iv, 62 p., https://doi.org/10.3133/sir20155052.","productDescription":"iv, 62 p.","numberOfPages":"70","onlineOnly":"N","additionalOnlineFiles":"N","ipdsId":"IP-062194","costCenters":[{"id":516,"text":"Oklahoma Water Science 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,{"id":70160543,"text":"70160543 - 2015 - First record of a banded Sandwich Tern (Thalasseus sandvicensis) moving from England to the United States","interactions":[],"lastModifiedDate":"2015-12-22T16:27:52","indexId":"70160543","displayToPublicDate":"2015-05-01T00:00:00","publicationYear":"2015","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3731,"text":"Waterbirds","onlineIssn":"19385390","printIssn":"15244695","active":true,"publicationSubtype":{"id":10}},"title":"First record of a banded Sandwich Tern (Thalasseus sandvicensis) moving from England to the United States","docAbstract":"<p>A Sandwich Tern (Thalasseus sandvicensis sandvicensis) banded as a chick in 2002 at Coquet Island off the northeast coast of Great Britain was observed at two locations on Cape Cod, Massachusetts, USA, in August and September 2013. This is the first record of a banded Sandwich Tern from the United Kingdom being observed in the United States.</p>","language":"English","publisher":"Waterbird Society","doi":"10.1675/063.038.0407","usgsCitation":"Spendelow, J.A., 2015, First record of a banded Sandwich Tern (Thalasseus sandvicensis) moving from England to the United States: Waterbirds, v. 38, no. 4, p. 425-426, https://doi.org/10.1675/063.038.0407.","productDescription":"2 p.","startPage":"425","endPage":"426","onlineOnly":"N","additionalOnlineFiles":"N","ipdsId":"IP-066219","costCenters":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":312752,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":312735,"type":{"id":15,"text":"Index Page"},"url":"https://www.bioone.org/doi/abs/10.1675/063.038.0407"}],"country":"United States","state":"Massachusetts","otherGeospatial":"Cape Cod","geographicExtents":"{\n  \"type\": 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,{"id":70157064,"text":"70157064 - 2015 - Comparison of three preservation techniques for slowing dissolution of calcareous nannofossils in organic rich sediments","interactions":[],"lastModifiedDate":"2016-02-11T10:59:46","indexId":"70157064","displayToPublicDate":"2015-05-01T00:00:00","publicationYear":"2015","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2735,"text":"Micropaleontology","active":true,"publicationSubtype":{"id":10}},"title":"Comparison of three preservation techniques for slowing dissolution of calcareous nannofossils in organic rich sediments","docAbstract":"<p><span>In an attempt to halt or reduce dissolution of calcareous nannofossils in organic and/or pyrite-rich sediments, three different methods of short-term storage preservation were tested for efficacy: vacuum packing, argon gas replacement, and buffered water. Abundance counts of calcareous nannofossil assemblages over a six month period showed that none of the three preservation methods were consistently effective in reducing assemblage loss due to dissolution. In most cases, the control slides made at the drill site had more abundant calcareous nannofossil assemblages than those slides made from sediments stored via vacuum packing, argon gas replacement, or buffered water. Thin section and XRD analyses showed that in most cases, &lt;1% pyrite was needed to drive the oxidation-reduction reaction that resulted in dissolution, even in carbonate-rich sediments.</span></p>","language":"English","publisher":"Micropaleontology Press","usgsCitation":"Seefelt, E., Self-Trail, J., and Schultz, A.P., 2015, Comparison of three preservation techniques for slowing dissolution of calcareous nannofossils in organic rich sediments: Micropaleontology, v. 61, no. 3, p. 149-164.","productDescription":"16 p.","startPage":"149","endPage":"164","onlineOnly":"N","additionalOnlineFiles":"N","ipdsId":"IP-063641","costCenters":[{"id":243,"text":"Eastern Geology and Paleoclimate Science Center","active":true,"usgs":true}],"links":[{"id":308498,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":308497,"rank":1,"type":{"id":15,"text":"Index Page"},"url":"https://www.micropress.org/microaccess/micropaleontology/issue-315/article-1920"}],"country":"United States","state":"Georgia, Maryland, North Carolina","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -77.47558593749999,\n              34.52918706954935\n            ],\n            [\n              -77.47558593749999,\n              34.68291096793206\n            ],\n            [\n              -77.266845703125,\n              34.68291096793206\n            ],\n            [\n              -77.266845703125,\n              34.52918706954935\n            ],\n            [\n              -77.47558593749999,\n              34.52918706954935\n            ]\n          ]\n        ]\n      }\n    },\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -81.5240478515625,\n              32.17096283641326\n            ],\n            [\n              -81.5240478515625,\n              32.2801666335657\n            ],\n            [\n              -81.37847900390625,\n              32.2801666335657\n            ],\n            [\n              -81.37847900390625,\n              32.17096283641326\n            ],\n            [\n              -81.5240478515625,\n              32.17096283641326\n            ]\n          ]\n        ]\n      }\n    },\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -76.11328125,\n              38.856820134743636\n            ],\n            [\n              -76.11328125,\n              39.06184913429154\n            ],\n            [\n              -75.8056640625,\n              39.06184913429154\n            ],\n            [\n              -75.8056640625,\n              38.856820134743636\n            ],\n            [\n              -76.11328125,\n              38.856820134743636\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"61","issue":"3","publishingServiceCenter":{"id":9,"text":"Reston PSC"},"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"56051ebae4b058f706e512b4","contributors":{"authors":[{"text":"Seefelt, Ellen 0000-0001-6822-7402 eseefelt@usgs.gov","orcid":"https://orcid.org/0000-0001-6822-7402","contributorId":2953,"corporation":false,"usgs":true,"family":"Seefelt","given":"Ellen","email":"eseefelt@usgs.gov","affiliations":[{"id":40020,"text":"Florence Bascom Geoscience Center","active":true,"usgs":true},{"id":243,"text":"Eastern Geology and Paleoclimate Science Center","active":true,"usgs":true}],"preferred":true,"id":571447,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Self-Trail, Jean 0000-0002-3018-4985 jstrail@usgs.gov","orcid":"https://orcid.org/0000-0002-3018-4985","contributorId":147370,"corporation":false,"usgs":true,"family":"Self-Trail","given":"Jean","email":"jstrail@usgs.gov","affiliations":[{"id":243,"text":"Eastern Geology and Paleoclimate Science Center","active":true,"usgs":true},{"id":40020,"text":"Florence Bascom Geoscience Center","active":true,"usgs":true}],"preferred":true,"id":571448,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Schultz, Arthur P. aschultz@usgs.gov","contributorId":3252,"corporation":false,"usgs":true,"family":"Schultz","given":"Arthur","email":"aschultz@usgs.gov","middleInitial":"P.","affiliations":[{"id":243,"text":"Eastern Geology and Paleoclimate Science Center","active":true,"usgs":true}],"preferred":true,"id":571449,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70157197,"text":"70157197 - 2015 - Structure, diversity, and biophysical properties of old-growth forestsin the Klamath region, USA","interactions":[],"lastModifiedDate":"2022-11-04T17:23:39.737409","indexId":"70157197","displayToPublicDate":"2015-05-01T00:00:00","publicationYear":"2015","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2900,"text":"Northwest Science","onlineIssn":"2161-9859","printIssn":"0029-344X","active":true,"publicationSubtype":{"id":10}},"title":"Structure, diversity, and biophysical properties of old-growth forestsin the Klamath region, USA","docAbstract":"<p><span>The diverse old-growth forests in Klamath region of northern California and southern Oregon provide valuable ecosystem services (e.g., maintaining watersheds, wildlife habitat, recreation), but may be vulnerable to a wide range of stressors, including invasive species, disrupted disturbance regimes, and climatic change. Yet our understanding of how forest structure in the Klamath region relates to the current physical environment is limited. Here we provide present-day benchmarks for old-growth forest structure across a climatic gradient ranging from coastal to dry interior sites. We established 16 large (1 ha) forest plots where all stems &gt; 5 cm in diameter were identified to species and mapped. Climate across these sites was highly variable, with estimated actual evapotranspiration correlated to several basic measures of forest structure, including plot basal area, stem size-class inequality, tree species diversity and, to a lesser extent, tree species richness. Analyses of the spatial arrangement of stems indicated a high degree of non-uniformity, with 75% of plots showing significant stem clumping at small spatial scales (0 to 10 m). Downscaled predictions of future site water balance suggest changes will be dominated by rapidly increasing climatic water deficit (D, a biologically meaningful index of drought). While these plots give a picture of current conditions, continued monitoring of these stands is needed to describe forest dynamics and to detect forest responses to ongoing and future stressors.</span></p>","language":"English","publisher":"Northwest Scientific Association","doi":"10.3955/046.089.0208","usgsCitation":"van Mantgem, P.J., and Starr, D.A., 2015, Structure, diversity, and biophysical properties of old-growth forestsin the Klamath region, USA: Northwest Science, v. 89, no. 2, p. 170-181, https://doi.org/10.3955/046.089.0208.","productDescription":"12 p.","startPage":"170","endPage":"181","onlineOnly":"N","additionalOnlineFiles":"N","ipdsId":"IP-057175","costCenters":[{"id":651,"text":"Western Ecological Research Center","active":true,"usgs":true}],"links":[{"id":308319,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","otherGeospatial":"Klamath region","geographicExtents":"{\n  \"type\": 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