{"pageNumber":"174","pageRowStart":"4325","pageSize":"25","recordCount":10956,"records":[{"id":70007325,"text":"sir20115195 - 2011 - Gas hydrate prospecting using well cuttings and mud-gas geochemistry from 35 wells, North Slope, Alaska","interactions":[],"lastModifiedDate":"2012-02-09T23:21:54","indexId":"sir20115195","displayToPublicDate":"2012-02-08T10:53:00","publicationYear":"2011","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":"2011-5195","title":"Gas hydrate prospecting using well cuttings and mud-gas geochemistry from 35 wells, North Slope, Alaska","docAbstract":"Gas hydrate deposits are common on the North Slope of Alaska around Prudhoe Bay; however, the extent of these deposits is unknown outside of this area. As part of a U.S. Geological Survey (USGS) and Bureau of Land Management gas hydrate research collaboration, well-cutting and mud-gas samples have been collected and analyzed from mainly industry-drilled wells on the North Slope for the purpose of prospecting for gas hydrate deposits. On the Alaska North Slope, gas hydrates are now recognized as an element within a petroleum systems approach or \"total petroleum system.\" Since 1979, 35 wells have been sampled from as far west as Wainwright to Prudhoe Bay in the east. Regionally, the USGS has assessed the gas hydrate resources of the North Slope and determined that there is about 85.4 trillion cubic feet of technically recoverable hydrate-bound gas within three assessment units. The assessment units are defined mainly by three separate stratigraphic sections and constrained by the physical temperatures and pressures where gas hydrate can form. Geochemical studies of known gas hydrate occurrences on the North Slope have shown a link between gas hydrate and more deeply buried conventional oil and gas deposits. The link is established when hydrocarbon gases migrate from depth and charge the reservoir rock within the gas hydrate stability zone. It is likely gases migrated into conventional traps as free gas and were later converted to gas hydrate in response to climate cooling concurrent with permafrost formation. Results from this study indicate that some thermogenic gas is present in 31 of the wells, with limited evidence of thermogenic gas in four other wells and only one well with no thermogenic gas. Gas hydrate is known to occur in one of the sampled wells, likely present in 22 others on the basis of gas geochemistry, and inferred by equivocal gas geochemistry in 11 wells, and one well was without gas hydrate. Gas migration routes are common in the North Slope and include faults and widespread, continuous shallowly dipping permeable sand sections that are potentially in communication with deeper oil and gas sources. The application of the petroleum system model with the geochemical evidence suggests that gas hydrate deposits may be widespread across the North Slope of Alaska.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/sir20115195","usgsCitation":"Lorenson, T., and Collett, T.S., 2011, Gas hydrate prospecting using well cuttings and mud-gas geochemistry from 35 wells, North Slope, Alaska: U.S. Geological Survey Scientific Investigations Report 2011-5195, iv, 25 p.; Appendices; Appendix 2 download; Appendix 3 download; Appendix 4 download, https://doi.org/10.3133/sir20115195.","productDescription":"iv, 25 p.; Appendices; Appendix 2 download; Appendix 3 download; Appendix 4 download","additionalOnlineFiles":"Y","costCenters":[{"id":164,"text":"Central Energy Resources Science Center","active":true,"usgs":true}],"links":[{"id":116461,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/sir_2011_5195.gif"},{"id":115783,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/sir/2011/5195/","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Alaska","otherGeospatial":"North Slope","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -162,69.5 ], [ -162,71.25 ], [ -144,71.25 ], [ -144,69.5 ], [ -162,69.5 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a14cfe4b0c8380cd54b93","contributors":{"authors":[{"text":"Lorenson, T.D. tlorenson@usgs.gov","contributorId":2622,"corporation":false,"usgs":true,"family":"Lorenson","given":"T.D.","email":"tlorenson@usgs.gov","affiliations":[{"id":186,"text":"Coastal and Marine Geology Program","active":true,"usgs":true}],"preferred":false,"id":356266,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Collett, Timothy S. 0000-0002-7598-4708 tcollett@usgs.gov","orcid":"https://orcid.org/0000-0002-7598-4708","contributorId":1698,"corporation":false,"usgs":true,"family":"Collett","given":"Timothy","email":"tcollett@usgs.gov","middleInitial":"S.","affiliations":[{"id":171,"text":"Central Mineral and Environmental Resources Science Center","active":true,"usgs":true},{"id":255,"text":"Energy Resources Program","active":true,"usgs":true},{"id":164,"text":"Central Energy Resources Science Center","active":true,"usgs":true},{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":true,"id":356265,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70003969,"text":"70003969 - 2011 - Using data from an encounter sampler to model fish dispersal","interactions":[],"lastModifiedDate":"2012-02-02T00:16:02","indexId":"70003969","displayToPublicDate":"2012-01-24T10:33:00","publicationYear":"2011","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2285,"text":"Journal of Fish Biology","active":true,"publicationSubtype":{"id":10}},"title":"Using data from an encounter sampler to model fish dispersal","docAbstract":"A method to estimate speed of free-ranging fishes using a passive sampling device is described and illustrated with data from the Everglades, U.S.A. Catch per unit effort (CPUE) from minnow traps embedded in drift fences was treated as an encounter rate and used to estimate speed, when combined with an independent estimate of density obtained by use of throw traps that enclose 1 m<sup>2</sup> of marsh habitat. Underwater video was used to evaluate capture efficiency and species-specific bias of minnow traps and two sampling studies were used to estimate trap saturation and diel-movement patterns; these results were used to optimize sampling and derive correction factors to adjust species-specific encounter rates for bias and capture efficiency. Sailfin mollies <i>Poecilia latipinna</i> displayed a high frequency of escape from traps, whereas eastern mosquitofish <i>Gambusia holbrooki</i> were most likely to avoid a trap once they encountered it; dollar sunfish <i>Lepomis marginatus</i> were least likely to avoid the trap once they encountered it or to escape once they were captured. Length of sampling and time of day affected CPUE; fishes generally had a very low retention rate over a 24 h sample time and only the Everglades pygmy sunfish <i>Elassoma evergladei</i> were commonly captured at night. Dispersal speed of fishes in the Florida Everglades, U.S.A., was shown to vary seasonally and among species, ranging from 0.05 to 0.15 m s<sup>-1</sup> for small poeciliids and fundulids to 0.1 to 1.8 m s<sup>-1</sup> for <i>L. marginatus</i>. Speed was generally highest late in the wet season and lowest in the dry season, possibly tied to dispersal behaviours linked to finding and remaining in dry-season refuges. These speed estimates can be used to estimate the diffusive movement rate, which is commonly employed in spatial ecological models.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Journal of Fish Biology","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"The Fisheries Society of the British Isles","doi":"10.1111/j.1095-8649.2010.02867.x","usgsCitation":"Obaza, A., DeAngelis, D., and Trexler, J., 2011, Using data from an encounter sampler to model fish dispersal: Journal of Fish Biology, v. 78, no. 2, p. 495-513, https://doi.org/10.1111/j.1095-8649.2010.02867.x.","productDescription":"18 p.","startPage":"495","endPage":"513","costCenters":[{"id":275,"text":"Florida Integrated Science Center","active":false,"usgs":true}],"links":[{"id":115757,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://dx.doi.org/10.1111/j.1095-8649.2010.02867.x","linkFileType":{"id":5,"text":"html"}},{"id":204582,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Florida","otherGeospatial":"Everglades","volume":"78","issue":"2","noUsgsAuthors":false,"publicationDate":"2011-01-07","publicationStatus":"PW","scienceBaseUri":"505bc042e4b08c986b32a00d","contributors":{"authors":[{"text":"Obaza, A.","contributorId":14109,"corporation":false,"usgs":true,"family":"Obaza","given":"A.","affiliations":[],"preferred":false,"id":349783,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"DeAngelis, D.L. 0000-0002-1570-4057","orcid":"https://orcid.org/0000-0002-1570-4057","contributorId":32470,"corporation":false,"usgs":true,"family":"DeAngelis","given":"D.L.","affiliations":[],"preferred":false,"id":349785,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Trexler, J.C.","contributorId":23108,"corporation":false,"usgs":true,"family":"Trexler","given":"J.C.","email":"","affiliations":[],"preferred":false,"id":349784,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70007204,"text":"ofr20111265 - 2011 - Impact of mine and natural sources of mercury on water, sediment, and biota in Harley Gulch adjacent to the Abbott-Turkey Run mine, Lake County, California","interactions":[],"lastModifiedDate":"2022-01-19T15:08:05.776269","indexId":"ofr20111265","displayToPublicDate":"2012-01-24T00:00:00","publicationYear":"2011","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":"2011-1265","title":"Impact of mine and natural sources of mercury on water, sediment, and biota in Harley Gulch adjacent to the Abbott-Turkey Run mine, Lake County, California","docAbstract":"<p><strong>Executive Summary</strong></p><p>Stable-isotope data indicate that there are three sources of water that effect the composition and Hg concentration of waters in Harley Gulch: (1) meteoric water that dominates water chemistry during the wet season; (2) thermal water effluent from the Turkey Run mine that effects the chemistry at sample site HG1; and (3) cold connate groundwater that dominates water chemistry during the dry season as it upwells and reaches the surface. The results from sampling executed for this study suggest four distinct areas in Harley Gulch: (1) the contaminated West Fork of Harley Gulch, consisting of the stream immediately downstream from the mine area and the wetlands upstream from Harley Gulch canyon (sample sites HG1-HG2, (2) the East Fork of Harley Gulch, where no mining has occurred (sample site HG3), (3) sample sites HG4-HG7, where a seasonal influx of saline groundwater alters stream chemistry, and (4) sample sites HG7-HG10, downstream in Harley Gulch towards the confluence with Cache Creek.</p><p><strong>West Fork: Mine Area and Wetlands</strong></p><p>The concentration of Hg in both storm sediment and active channel sediment was highest at sample site HG1, immediately downstream from the mine. The highest concentrations of total Hg (Hg<sub>T</sub>) in water also occurred at site HG1, and they decreased systematically downstream from the mine. The high concentration of HgT at site HG1 reflects input of thermal-water effluent from the Turkey Run mine which comprises most of the flow at this site during the dry season. During the May 2011 low-flow sampling, Hg<sub>T</sub> concentration was very high at site HG1, but the maximum in HgT concentration occurred at sample site HG1.5 in the middle of the wetland area. The high concentration of Hg<sub>T</sub> and isotopic chemistry at this site indicates that a significant input of connate groundwater into the creek at this location contributes to the high Hg concentration in water. At site HG1, just downstream from the thermal water input from the Turkey Run mine, water sampled in June 2010 was almost entirely composed of thermal-water effluent. During the storm sampling in March 2011, which resulted in the highest flows of the winter, thermal effluent was virtually undetectable at site HG1, and the water was all meteoric. During the May 2011 sampling event, the input of connate groundwater in the middle of the wetland area at site HG1.5 was dominant. Discharge from the adit and runoff from the mine contributes to the high Hg concentration at site HG1 under both high and low-flow conditions.</p><p><strong>East Fork: Background</strong></p><p>Hg levels in waters collected from the East Fork of Harley Gulch, where no mining has occurred, were as high as 32.8 parts per trillion (pptr). These levels of Hg in water are significantly higher than regional background Hg concentrations, which range from 4-7 pptr. These anomalous Hg concentrations are partially explained by the abundance of Hg-enriched groundwater in Harley Gulch.</p><p><strong>Sites HG4-HG7</strong></p><p>Downstream from the wetland, the aqueous concentration of HgT decreased, but remained above background levels as another input of connate groundwater occurs in the creek segment between sample sites HG4 and HG7. The input of connate groundwater in this segment of the creek is reflected in the increase in dissolved constituents characteristic of the connate groundwater, such as sulfate (SO4), chloride (Cl) and magnesium (Mg). Stable-isotope data for heavy isotopes d18O and d2D also confirm two areas of input of connate groundwater into Harley Gulch: the creek segment in the West Fork near sample site HG1.5 and the segment between sample sites HG4 and HG7. Downstream from the second area of input of connate groundwater, both HgF and Hg<sub>T</sub> concentrations decrease similarly, but the percentage of Hg in the filtered fraction increases. The decreases in HgT and HgF between sample sites HG5 and HG7 suggests that this second source of connate groundwater to Harley Gulch is distinct from the Hg-enriched source that enters the middle of the wetlands at sample site HG1.5. During low-flow conditions in June 2010, input of connate groundwater increased from sample site HG4 and reached a maximum near sample site HG7, where it dominated creek water chemistry. Waters collected from sample site HG7 during the June 2010 sampling event were the heaviest isotopically and contained high concentrations of Cl and SO4, constituents that are characteristically high in the connate groundwater. Both above and below sample site HG7, the amount of connate groundwater in the creek water decreased.</p><p><strong>Sites HG8-HG10</strong></p><p>Sediment with high Hg concentration is present throughout the West Fork of Harley Gulch below the mine and in the upper part of the Harley Gulch main stem to just above sample site HG10. At the sample site furthest downstream, HG10, Hg concentration is at background levels, as are cobalt (Co), nickel (Ni), and tungsten (W), indicating that the sediment is not significantly contaminated with Hg from the mine.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr20111265","collaboration":"Prepared in cooperation with the Bureau of Land Management","usgsCitation":"Rytuba, J.J., Hothem, R.L., Brussee, B.E., and Goldstein, D., 2011, Impact of mine and natural sources of mercury on water, sediment, and biota in Harley Gulch adjacent to the Abbott-Turkey Run mine, Lake County, California: U.S. Geological Survey Open-File Report 2011-1265, ix, 105 p., https://doi.org/10.3133/ofr20111265.","productDescription":"ix, 105 p.","onlineOnly":"Y","costCenters":[{"id":663,"text":"Western Mineral and Environmental Resources Science Center-Menlo Park Office","active":false,"usgs":true},{"id":34983,"text":"Contaminant Biology Program","active":true,"usgs":true}],"links":[{"id":116447,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ofr_2011_1265.gif"},{"id":115690,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2011/1265/","linkFileType":{"id":5,"text":"html"}},{"id":394515,"rank":3,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/2011/1265/of2011-1265.pdf","text":"Report","size":"9 MB","linkFileType":{"id":1,"text":"pdf"},"description":"Report"}],"country":"United States","state":"California","county":"Lake County","otherGeospatial":"Harley Gulch","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -122.47550010681154,\n              38.98630040014555\n            ],\n            [\n              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,{"id":70007191,"text":"ofr20111315 - 2011 - Bathymetry and digital elevation models of Coyote Creek and Alviso Slough, South San Francisco Bay, California","interactions":[],"lastModifiedDate":"2020-07-09T18:09:19.490137","indexId":"ofr20111315","displayToPublicDate":"2012-01-23T13:04:00","publicationYear":"2011","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":"2011-1315","title":"Bathymetry and digital elevation models of Coyote Creek and Alviso Slough, South San Francisco Bay, California","docAbstract":"<p>In 2010, the U.S. Geological Survey (USGS), Pacific Coastal and Marine Science Center completed three cruises to map the bathymetry of the main channel and shallow intertidal mudflats in the southernmost part of south San Francisco Bay. The three surveys were merged to generate comprehensive maps of Coyote Creek (from Calaveras Point east to the railroad bridge) and Alviso Slough (from the bay to the town of Alviso) to establish baseline bathymetry prior to the breaching of levees adjacent to Alviso and Guadalupe Sloughs as part of the South Bay Salt Pond Restoration Project (<span><a href=\"http://www.southbayrestoration.org\" data-mce-href=\"http://www.southbayrestoration.org\">http://www.southbayrestoration.org</a></span>). Since 2010, the USGS has conducted fourteen additional surveys to monitor bathymetric change in this region as restoration progresses.</p><p>The bathymetric surveys were conducted using the state-of-the-art research vessel R/V <i>Parke Snavely </i>outfitted with an interferometric sidescan sonar for swath mapping in extremely shallow water. This publication provides high-resolution bathymetric data collected by the USGS. For the 2010 baseline survey we have merged the bathymetry with aerial lidar data that were collected for the USGS during the same time period to create a seamless, high-resolution digital elevation model (DEM) of the study area. The series of bathymetric datasets are provided at 1 m resolution and the 2010 bathymetric/topographic DEM at 2 m resolution. The data are formatted as both X, Y, Z text files and ESRI Arc ASCII files that are accompanied by Federal Geographic Data Committee (FGDC) compliant metadata.<br></p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr20111315","usgsCitation":"Foxgrover, A.C., Finlayson, D.P., Jaffe, B.E., and Fregoso, T.A., 2011, Bathymetry and digital elevation models of Coyote Creek and Alviso Slough, South San Francisco Bay, California (ver. 5.0, June 2020): U.S. Geological Survey Open-File Report 2011–1315, 21 p., https://doi.org/10.3133/ofr20111315.","productDescription":"Report: iv, 21 p.; Metadata; Companion File","numberOfPages":"21","onlineOnly":"Y","additionalOnlineFiles":"Y","temporalStart":"2010-01-01","temporalEnd":"2019-04-01","costCenters":[{"id":520,"text":"Pacific Coastal and Marine Science Center","active":true,"usgs":true}],"links":[{"id":316658,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/2011/1315/ofr20111315_v5.pdf","text":"Report","size":"9 MB","linkFileType":{"id":1,"text":"pdf"}},{"id":352734,"rank":5,"type":{"id":25,"text":"Version History"},"url":"https://pubs.usgs.gov/of/2011/1315/versionHist.txt","text":"Version History","size":"4 KB","linkFileType":{"id":2,"text":"txt"}},{"id":284380,"rank":4,"type":{"id":16,"text":"Metadata"},"url":"https://pubs.usgs.gov/of/2011/1315/of2011-1315_metadata"},{"id":284381,"rank":3,"type":{"id":7,"text":"Companion Files"},"url":"https://pubs.usgs.gov/of/2011/1315/of2011-1315_data","text":"Data folder"},{"id":116371,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/2011/1315/images/coverthb.jpg"}],"country":"United States","state":"California","otherGeospatial":"Alviso Slough, Coyote Creek, San Francisco Bay","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -122.51,37.44 ], [ -122.51,38.14 ], [ -122.03,38.14 ], [ -122.03,37.44 ], [ -122.51,37.44 ] ] ] } } ] }","edition":"Version 1.0: January 5, 2012; Version 2.0: March 24, 2014; Version 3.0: September 24, 2015; Version 4.0: March 26, 2018; Version 5.0: June 24, 2020","contact":"<p><a href=\"https://www.usgs.gov/centers/pcmsc\" data-mce-href=\"https://www.usgs.gov/centers/pcmsc\">Pacific Coastal and Marine Science Center</a><br><a href=\"https://www.usgs.gov/\" data-mce-href=\"https://www.usgs.gov/\">U.S. Geological Survey</a><br>2885 Mission Street<br>Santa Cruz, CA 95060</p>","tableOfContents":"<ul><li>Contents<br></li><li>Abstract<br></li><li>Introduction<br></li><li>Data Collection<br></li><li>Processing Procedures<br></li><li>Digital Elevation Model Production<br></li><li>Estimates of Bathymetric Uncertainty<br></li><li>Data Tables<br></li><li>Acknowledgments<br></li><li>References Cited<br></li><li>Appendix A<br></li><li>Appendix B<br></li></ul><p><br data-mce-bogus=\"1\"></p>","publishingServiceCenter":{"id":14,"text":"Menlo Park PSC"},"publishedDate":"2012-01-05","revisedDate":"2020-06-24","noUsgsAuthors":false,"publicationDate":"2012-01-05","publicationStatus":"PW","scienceBaseUri":"53cd4ef4e4b0b290850f2678","contributors":{"authors":[{"text":"Foxgrover, Amy C. 0000-0003-0638-5776 afoxgrover@usgs.gov","orcid":"https://orcid.org/0000-0003-0638-5776","contributorId":3261,"corporation":false,"usgs":true,"family":"Foxgrover","given":"Amy","email":"afoxgrover@usgs.gov","middleInitial":"C.","affiliations":[{"id":520,"text":"Pacific Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":true,"id":356038,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Finlayson, David P. dfinlayson@usgs.gov","contributorId":1381,"corporation":false,"usgs":true,"family":"Finlayson","given":"David","email":"dfinlayson@usgs.gov","middleInitial":"P.","affiliations":[{"id":520,"text":"Pacific Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":true,"id":356036,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Jaffe, Bruce E. 0000-0002-8816-5920 bjaffe@usgs.gov","orcid":"https://orcid.org/0000-0002-8816-5920","contributorId":2049,"corporation":false,"usgs":true,"family":"Jaffe","given":"Bruce","email":"bjaffe@usgs.gov","middleInitial":"E.","affiliations":[{"id":520,"text":"Pacific Coastal and Marine Science Center","active":true,"usgs":true},{"id":186,"text":"Coastal and Marine Geology Program","active":true,"usgs":true}],"preferred":true,"id":356037,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Fregoso, Theresa A. 0000-0001-7802-5812 tfregoso@usgs.gov","orcid":"https://orcid.org/0000-0001-7802-5812","contributorId":2571,"corporation":false,"usgs":true,"family":"Fregoso","given":"Theresa","email":"tfregoso@usgs.gov","middleInitial":"A.","affiliations":[{"id":520,"text":"Pacific Coastal and Marine Science Center","active":true,"usgs":true},{"id":186,"text":"Coastal and Marine Geology Program","active":true,"usgs":true}],"preferred":true,"id":356039,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70007139,"text":"70007139 - 2011 - Non-genetic data supporting genetic evidence for the eastern wolf","interactions":[],"lastModifiedDate":"2018-01-04T11:20:58","indexId":"70007139","displayToPublicDate":"2012-01-12T16:12:00","publicationYear":"2011","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2898,"text":"Northeastern Naturalist","active":true,"publicationSubtype":{"id":10}},"title":"Non-genetic data supporting genetic evidence for the eastern wolf","docAbstract":"Two schools of thought dominate the molecular-genetics literature on <i>Canis</i> spp. (wolves) in the western Great Lakes region of the US and Canada: (1) they are hybrids between <i>Canis lupus</i> (Gray Wolf) and <i>Canis latrans</i> (Coyote), or (2) they are hybrids between the Gray Wolf and <i>Canis lycaon</i> (Eastern Wolf). This article presents 3 types of non-genetic evidence that bears on the controversy and concludes that all 3 support the second interpretation.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Northeastern Naturalist","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"Humboldt Field Research Institute","publisherLocation":"Steuben, ME","doi":"10.1656/045.018.0409","usgsCitation":"Mech, L.D., 2011, Non-genetic data supporting genetic evidence for the eastern wolf: Northeastern Naturalist, v. 18, no. 4, p. 521-526, https://doi.org/10.1656/045.018.0409.","productDescription":"6 p.","startPage":"521","endPage":"526","costCenters":[{"id":480,"text":"Northern Prairie Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":204630,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":115670,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://dx.doi.org/10.1656/045.018.0409","linkFileType":{"id":5,"text":"html"}}],"country":"United States;Canada","otherGeospatial":"Great Lakes Region","volume":"18","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a6746e4b0c8380cd73259","contributors":{"authors":[{"text":"Mech, L. David 0000-0003-3944-7769 david_mech@usgs.gov","orcid":"https://orcid.org/0000-0003-3944-7769","contributorId":2518,"corporation":false,"usgs":true,"family":"Mech","given":"L.","email":"david_mech@usgs.gov","middleInitial":"David","affiliations":[{"id":480,"text":"Northern Prairie Wildlife Research Center","active":true,"usgs":true}],"preferred":true,"id":355919,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70005854,"text":"70005854 - 2011 - The influence of the Atlantic Warm Pool on the Florida panhandle sea breeze","interactions":[],"lastModifiedDate":"2021-04-29T19:30:03.836197","indexId":"70005854","displayToPublicDate":"2012-01-08T09:33:00","publicationYear":"2011","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":8111,"text":"Journal of Geophysical Research Atmospheres","active":true,"publicationSubtype":{"id":10}},"title":"The influence of the Atlantic Warm Pool on the Florida panhandle sea breeze","docAbstract":"<p><span class=\"paraNumber\"><span>&nbsp;</span></span><span>In this paper we examine the variations of the boreal summer season sea breeze circulation along the Florida panhandle coast from relatively high resolution (10 km) regional climate model integrations. The 23 year climatology (1979–2001) of the multidecadal dynamically downscaled simulations forced by the National Centers for Environmental Prediction–Department of Energy (NCEP‐DOE) Reanalysis II at the lateral boundaries verify quite well with the observed climatology. The variations at diurnal and interannual time scales are also well simulated with respect to the observations. We show from composite analyses made from these downscaled simulations that sea breezes in northwestern Florida are associated with changes in the size of the Atlantic Warm Pool (AWP) on interannual time scales. In large AWP years when the North Atlantic Subtropical High becomes weaker and moves further eastward relative to the small AWP years, a large part of the southeast U.S. including Florida comes under the influence of relatively strong anomalous low‐level northerly flow and large‐scale subsidence consistent with the theory of the Sverdrup balance. This tends to suppress the diurnal convection over the Florida panhandle coast in large AWP years. This study is also an illustration of the benefit of dynamic downscaling in understanding the low‐frequency variations of the sea breeze.</span></p>","language":"English","publisher":"American Geophysical Union","publisherLocation":"Washington, D.C.","doi":"10.1029/2010JD015367","usgsCitation":"Misra, V., Moeller, L., Stefanova, L., Chan, S., O’Brien, J.J., Smith, T.J., and Plant, N., 2011, The influence of the Atlantic Warm Pool on the Florida panhandle sea breeze: Journal of Geophysical Research Atmospheres, v. 116, no. 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Steven","contributorId":16971,"corporation":false,"usgs":true,"family":"Chan","given":"Steven","affiliations":[],"preferred":false,"id":353386,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"O’Brien, James J.","contributorId":100997,"corporation":false,"usgs":true,"family":"O’Brien","given":"James","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":353391,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Smith, Thomas J. III tom_j_smith@usgs.gov","contributorId":1615,"corporation":false,"usgs":true,"family":"Smith","given":"Thomas","suffix":"III","email":"tom_j_smith@usgs.gov","middleInitial":"J.","affiliations":[{"id":566,"text":"Southeast Ecological Science Center","active":true,"usgs":true}],"preferred":false,"id":353385,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Plant, Nathaniel 0000-0002-5703-5672","orcid":"https://orcid.org/0000-0002-5703-5672","contributorId":81234,"corporation":false,"usgs":true,"family":"Plant","given":"Nathaniel","affiliations":[{"id":574,"text":"St. Petersburg Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":true,"id":353390,"contributorType":{"id":1,"text":"Authors"},"rank":7}]}}
,{"id":70007076,"text":"sir20115164 - 2011 - Pathogenic bacteria and microbial-source tracking markers in Brandywine Creek Basin, Pennsylvania and Delaware, 2009-10","interactions":[],"lastModifiedDate":"2019-07-19T09:18:06","indexId":"sir20115164","displayToPublicDate":"2012-01-04T00:00:00","publicationYear":"2011","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":"2011-5164","title":"Pathogenic bacteria and microbial-source tracking markers in Brandywine Creek Basin, Pennsylvania and Delaware, 2009-10","docAbstract":"The City of Wilmington, Delaware, is in the downstream part of the Brandywine Creek Basin, on the main stem of Brandywine Creek. Wilmington uses this stream, which drains a mixed-land-use area upstream, for its main drinking-water supply. Because the stream is used for drinking water, Wilmington is in need of information about the occurrence and distribution of specific fecally derived pathogenic bacteria (disease-causing bacteria) and their relations to commonly measured fecal-indicator bacteria (FIB), as well as information regarding the potential sources of the fecal pollution and pathogens in the basin. This study focused on five routinely sampled sites within the basin, one each on the West Branch and the East Branch of Brandywine Creek and at three on the main stem below the confluence of the West and East Branches. These sites were sampled monthly for 1 year. Targeted event samples were collected on two occasions during high flow and two occasions during normal flow. On the basis of this study, high flows in the Brandywine Creek Basin were related to increases in FIB densities, and in the frequency of selected pathogen and source markers, in the West Branch and main stem of Brandywine Creek, but not in the East Branch. Water exceeding the moderate fullbody-contact single-sample recreational water-quality criteria (RWQC) for <em>Escherichia coli (E. coli)</em> was more likely to contain selected markers for pathogenic <em>E. coli</em> (<em>eaeA</em>,<em>stx</em><sub>1</sub>, and <em>rfb</em><sub>O157</sub> gene markers) and bovine fecal sources (<em>E. hirae</em> and LTIIa gene markers), whereas samples exceeding the enterococci RWQC were more likely to contain the same pathogenic markers but also were more likely to carry a marker indicative of human source (<em>esp</em> gene marker). On four sample dates, during high flow between October and March, the West Branch was the only observed potential contributor of selected pathogen and bovine source markers to the main stem of Brandywine Creek. Indeed, the <em>stx</em><sub>2</sub> marker, which indicates a highly virulent type of pathogenic <em>E. coli</em>, was found only in the West Branch and main stem at high flow but was not found in the East Branch under similar conditions. However, it must be noted that throughout the entire year of sampling there were occasions, during both high and normal flows, when both the East and West Branches were potential contributors of pathogen and microbial-source tracking markers to the main stem. Therefore, this study indicates that under selected conditions (high flow, October through March), West Branch Brandywine Creek Basin was the most likely source of elevated FIB densities in the main stem. These elevated densities are associated with more frequent detection of selected pathogenic <em>E. coli</em> markers (<em>rfb</em><sub>O157</sub> <em>stx</em><sub>1</sub>) and are associated with MST markers of bovine source. However, during other times of the year, both the West Branch and East Branch Basins are acting as potential sources of FIB and fecally derived pathogens.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/sir20115164","collaboration":"Prepared in cooperation with the City of Wilmington, Delaware","usgsCitation":"Duris, J.W., Reif, A.G., Olson, L.E., and Johnson, H., 2011, Pathogenic bacteria and microbial-source tracking markers in Brandywine Creek Basin, Pennsylvania and Delaware, 2009-10: U.S. Geological Survey Scientific Investigations Report 2011-5164, vi, 22 p., https://doi.org/10.3133/sir20115164.","productDescription":"vi, 22 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":382,"text":"Michigan Water Science Center","active":true,"usgs":true},{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":116340,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/sir_2011_5164.jpg"},{"id":112426,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/sir/2011/5164/","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Pennsylvania, Delaware","otherGeospatial":"Brandywine Creek Basin","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -76,39.666666666666664 ], [ -76,40.166666666666664 ], [ -75.5,40.166666666666664 ], [ -75.5,39.666666666666664 ], [ -76,39.666666666666664 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a7597e4b0c8380cd77c26","contributors":{"authors":[{"text":"Duris, Joseph W. 0000-0002-8669-8109 jwduris@usgs.gov","orcid":"https://orcid.org/0000-0002-8669-8109","contributorId":1981,"corporation":false,"usgs":true,"family":"Duris","given":"Joseph","email":"jwduris@usgs.gov","middleInitial":"W.","affiliations":[{"id":532,"text":"Pennsylvania Water Science Center","active":true,"usgs":true},{"id":382,"text":"Michigan Water Science Center","active":true,"usgs":true}],"preferred":false,"id":355783,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Reif, Andrew G. 0000-0002-5054-5207 agreif@usgs.gov","orcid":"https://orcid.org/0000-0002-5054-5207","contributorId":2632,"corporation":false,"usgs":true,"family":"Reif","given":"Andrew","email":"agreif@usgs.gov","middleInitial":"G.","affiliations":[{"id":532,"text":"Pennsylvania Water Science Center","active":true,"usgs":true}],"preferred":true,"id":355785,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Olson, Leif E. leolson@usgs.gov","contributorId":2108,"corporation":false,"usgs":true,"family":"Olson","given":"Leif","email":"leolson@usgs.gov","middleInitial":"E.","affiliations":[],"preferred":true,"id":355784,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Johnson, Heather E.","contributorId":207837,"corporation":false,"usgs":false,"family":"Johnson","given":"Heather E.","affiliations":[{"id":382,"text":"Michigan Water Science Center","active":true,"usgs":true},{"id":12456,"text":"former USGS scientist","active":true,"usgs":false}],"preferred":false,"id":744846,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70171021,"text":"70171021 - 2011 - Potential climate change effects on water tables and pyrite oxidation in headwater catchments in Colorado","interactions":[],"lastModifiedDate":"2016-05-17T12:03:16","indexId":"70171021","displayToPublicDate":"2012-01-02T01:15:00","publicationYear":"2011","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"title":"Potential climate change effects on water tables and pyrite oxidation in headwater catchments in Colorado","docAbstract":"<p>A water, energy, and biogeochemical model (WEBMOD) was constructed to simulate hydrology and pyrite oxidation for the period October 1992 through September 1997. The hydrologic model simulates processes in Loch Vale, a 6.6-km&sup2; granitic watershed that drains the east side of the Continental Divide. Parameters describing pyrite oxidation were derived sulfate concentrations measured in pore water and stream water in Handcart Gulch, a naturally acidic watershed in the Colorado Mineral Belt. Average monthly differences in precipitation and temperature between current and future climates, as predicted by using six global circulation models and three carbondioxide emission scenarios, were input into WEBMOD to identify possible shifts in the quantity and quality of the water flowing from the watershed for the period 2005 through 2100. Initial results suggest that increased air temperatures will result in earlier snowmelt compared to current conditions. Average sulfate concentrations and acidity in streams draining hydrothermally altered terrain may decrease as water tables rise in response to greater overall precipitation and earlier snowmelt, although a net increase of sulfate load was simulated as a result of greater overall discharge. Evapotranspiration is expected to increase but not enough to offset the increase in precipitation.</p>","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Observing, studying, and managing for change - Proceedings of the Fourth Interagency Conference on Research in the Watersheds: U.S. Geological Survey Scientific Investigations Report 2011–5169","largerWorkSubtype":{"id":5,"text":"USGS Numbered Series"},"conferenceTitle":"The Fourth Interagency Conference on Research in the Watersheds","conferenceDate":"September 26-30, 2011","conferenceLocation":"Fairbanks, AK","language":"English","publisher":"U.S. Geological Survey","usgsCitation":"Webb, R.M., Mast, M.A., Manning, A.H., Clow, D.W., and Campbell, D.H., 2011, Potential climate change effects on water tables and pyrite oxidation in headwater catchments in Colorado, <i>in</i> Observing, studying, and managing for change - Proceedings of the Fourth Interagency Conference on Research in the Watersheds: U.S. Geological Survey Scientific Investigations Report 2011–5169, Fairbanks, AK, September 26-30, 2011, p. 23-33.","productDescription":"11 p.","startPage":"23","endPage":"33","onlineOnly":"N","additionalOnlineFiles":"N","ipdsId":"IP-032633","costCenters":[{"id":5044,"text":"National Research Program - Central Branch","active":true,"usgs":true}],"links":[{"id":321302,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":321301,"rank":1,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/sir/2011/5169/SIR11-5169_508_Session-1B.pdf","text":"Report","size":"3.95 MB","linkFileType":{"id":1,"text":"pdf"},"description":"Report"},{"id":321311,"rank":2,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/sir/2011/5169/"}],"country":"United States","state":"Colorado","otherGeospatial":"Handcart Gulch, Loch Vale","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -106.5234375,\n              39.232253141714885\n            ],\n            [\n              -106.5234375,\n              40.95501133048621\n            ],\n            [\n              -105.0677490234375,\n              40.95501133048621\n            ],\n            [\n              -105.0677490234375,\n              39.232253141714885\n            ],\n            [\n              -106.5234375,\n              39.232253141714885\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","publishingServiceCenter":{"id":2,"text":"Denver PSC"},"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"574d65fde4b07e28b6684a21","contributors":{"editors":[{"text":"Medley, C. Nicholas","contributorId":146966,"corporation":false,"usgs":false,"family":"Medley","given":"C.","email":"","middleInitial":"Nicholas","affiliations":[],"preferred":false,"id":629579,"contributorType":{"id":2,"text":"Editors"},"rank":1},{"text":"Patterson, Glenn","contributorId":86476,"corporation":false,"usgs":true,"family":"Patterson","given":"Glenn","affiliations":[],"preferred":false,"id":629580,"contributorType":{"id":2,"text":"Editors"},"rank":2},{"text":"Parker, Melanie J. mparker@usgs.gov","contributorId":670,"corporation":false,"usgs":true,"family":"Parker","given":"Melanie","email":"mparker@usgs.gov","middleInitial":"J.","affiliations":[],"preferred":true,"id":629581,"contributorType":{"id":2,"text":"Editors"},"rank":3}],"authors":[{"text":"Webb, Richard M. 0000-0001-9531-2207 rmwebb@usgs.gov","orcid":"https://orcid.org/0000-0001-9531-2207","contributorId":1570,"corporation":false,"usgs":true,"family":"Webb","given":"Richard","email":"rmwebb@usgs.gov","middleInitial":"M.","affiliations":[{"id":5044,"text":"National Research Program - Central Branch","active":true,"usgs":true},{"id":191,"text":"Colorado Water Science Center","active":true,"usgs":true}],"preferred":true,"id":629569,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Mast, M. Alisa 0000-0001-6253-8162 mamast@usgs.gov","orcid":"https://orcid.org/0000-0001-6253-8162","contributorId":827,"corporation":false,"usgs":true,"family":"Mast","given":"M.","email":"mamast@usgs.gov","middleInitial":"Alisa","affiliations":[{"id":191,"text":"Colorado Water Science Center","active":true,"usgs":true}],"preferred":true,"id":629568,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Manning, Andrew H. 0000-0002-6404-1237 amanning@usgs.gov","orcid":"https://orcid.org/0000-0002-6404-1237","contributorId":1305,"corporation":false,"usgs":true,"family":"Manning","given":"Andrew","email":"amanning@usgs.gov","middleInitial":"H.","affiliations":[{"id":171,"text":"Central Mineral and Environmental Resources Science Center","active":true,"usgs":true}],"preferred":true,"id":629565,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Clow, David W. 0000-0001-6183-4824 dwclow@usgs.gov","orcid":"https://orcid.org/0000-0001-6183-4824","contributorId":1671,"corporation":false,"usgs":true,"family":"Clow","given":"David","email":"dwclow@usgs.gov","middleInitial":"W.","affiliations":[{"id":191,"text":"Colorado Water Science Center","active":true,"usgs":true}],"preferred":true,"id":629567,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Campbell, Donald H. dhcampbe@usgs.gov","contributorId":1670,"corporation":false,"usgs":true,"family":"Campbell","given":"Donald","email":"dhcampbe@usgs.gov","middleInitial":"H.","affiliations":[],"preferred":true,"id":629566,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":70003809,"text":"70003809 - 2011 - Severe bill deformity of an American Kestrel wintering in California","interactions":[],"lastModifiedDate":"2019-11-07T15:46:42","indexId":"70003809","displayToPublicDate":"2012-01-01T22:15:00","publicationYear":"2011","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3743,"text":"Western Birds","active":true,"publicationSubtype":{"id":10}},"title":"Severe bill deformity of an American Kestrel wintering in California","docAbstract":"<p>During a recent survey for West Nile virus in wild birds around the Sonny Bono Salton Sea National Wildlife Refuge, Imperial County, California (Dusek et al. 2010), we captured a female American Kestrel (<i>Falco</i> <i>sparverius</i>) with a severe bill deformity (Figure 1). The kestrel was captured on 9 March 2006, at 08:45, approximately 0.25 km south of the intersection of Wiest and Lindsey roads (33° &nbsp;08' 42' N, 115° 26' 59' W) and 6 km east-northeast of Calipatria. It was caught on a bal-chatri trap baited with a domestic mouse (Berger and Mueller 1959), as were all the 208 kestrels captured during this study. The bird was initially perched on a high transmission line running along Wiest Road and was caught within 10 minutes of our setting the trap. In examining the bird, we observed that the maxilla beyond the cere was missing. The upper bill structure from the palatine process, which included part of the maxilla, the entire premaxilla, and the external rhamphotheca (the hardened keratin layer cover­ ing the premaxilla) was missing rostral to the bird's cere and nares (Threlfall 1968, Lucas and Stettenheim 1972, Proctor and Lynch 1993). The epidermal layer of the cere appeared to have fused over the remaining area between the nares where the upper bill normally would have been. The deformation did not appear to be recent or related to our trapping, as there were no obvious abrasions or open wounds in the region surrounding the nares and oropharynx or signs of recent trauma surrounding the oropharynx area. Both nares were clearly defined, and the tongue protruded from the open oropharynx area. After completing the physical examination, measurements, and obtaining a blood sample for testing for West Nile virus, we released the kestrel at the location of capture. After its release, we monitored the kestrel's behavior for approximately 30 minutes but did not observe any additional hunting.</p>","language":"English","publisher":"Western Field Ornithologists","usgsCitation":"Iko, W.M., and Dusek, R., 2011, Severe bill deformity of an American Kestrel wintering in California: Western Birds, v. 42, no. 4, p. 251-254.","productDescription":"4 p.","startPage":"251","endPage":"254","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":291,"text":"Fort Collins Science Center","active":true,"usgs":true},{"id":456,"text":"National Wildlife Health Center","active":true,"usgs":true}],"links":[{"id":257352,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United 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,{"id":70037739,"text":"70037739 - 2011 - Notes on the distribution of eastern woodrats and hispid cotton rats in south-central Nebraska","interactions":[],"lastModifiedDate":"2017-08-31T13:49:48","indexId":"70037739","displayToPublicDate":"2012-01-01T13:46:00","publicationYear":"2011","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3111,"text":"Prairie Naturalist","active":true,"publicationSubtype":{"id":10}},"title":"Notes on the distribution of eastern woodrats and hispid cotton rats in south-central Nebraska","docAbstract":"The eastern woodrat (<i>Neotoma floridana</i>) and hispid cotton rat (<i>Sigmodon hispidus</i>) reach distributional limits in southern Nebraska (Jones 1964, Farney 1975). In the last half century, both species have expanded their distributional ranges in the region (Kugler and Geluso 2009, Wright et al. 2010). Herein, we report new localities of occurrence for both species that extend known distributional boundaries in south-central Nebraska beyond those reported by Kugler and Geluso (2009) and Wright et al. (2010).","language":"English","publisher":"South Dakota State University","publisherLocation":"Brookings, SD","usgsCitation":"Wills, H., Geluso, K., Smits, E., Springer, J., and Newton, W., 2011, Notes on the distribution of eastern woodrats and hispid cotton rats in south-central Nebraska: Prairie Naturalist, v. 43, no. 3/4, p. 127-129.","productDescription":"3 p.","startPage":"127","endPage":"129","numberOfPages":"3","costCenters":[{"id":480,"text":"Northern Prairie Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":257574,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Nebraska","volume":"43","issue":"3/4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a6885e4b0c8380cd73868","contributors":{"authors":[{"text":"Wills, H.D.","contributorId":44028,"corporation":false,"usgs":true,"family":"Wills","given":"H.D.","email":"","affiliations":[],"preferred":false,"id":462553,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Geluso, Keith","contributorId":94637,"corporation":false,"usgs":true,"family":"Geluso","given":"Keith","email":"","affiliations":[],"preferred":false,"id":462555,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Smits, E.J.","contributorId":39225,"corporation":false,"usgs":true,"family":"Smits","given":"E.J.","email":"","affiliations":[],"preferred":false,"id":462552,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Springer, J.T.","contributorId":73869,"corporation":false,"usgs":true,"family":"Springer","given":"J.T.","email":"","affiliations":[],"preferred":false,"id":462554,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Newton, W.E.","contributorId":13567,"corporation":false,"usgs":true,"family":"Newton","given":"W.E.","email":"","affiliations":[],"preferred":false,"id":462551,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":70003947,"text":"70003947 - 2011 - Nesting success and resource selection of greater sage grouse in South Dakota: Chapter 8","interactions":[],"lastModifiedDate":"2018-08-15T15:29:33","indexId":"70003947","displayToPublicDate":"2012-01-01T13:43:37","publicationYear":"2011","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3490,"text":"Studies in Avian Biology; Ecology, Conservation, and Management of Grouse","active":true,"publicationSubtype":{"id":10}},"title":"Nesting success and resource selection of greater sage grouse in South Dakota: Chapter 8","docAbstract":"Declines of Greater Sage-Grouse (<i>Centrocercus urophasianus</i>) in South Dakota are a concern because further population declines may lead to isolation from populations in Wyoming and Montana. Furthermore, little information exists about reproductive ecology and resource selection of sage grouse on the eastern edge of their distribution. We investigated Greater Sage-Grouse nesting success and resource selection in South Dakota during 2006-2007. Radiomarked females were tracked to estimate nesting rates, nest success, and habitat resources selected for nesting. Nest initiation was 98.0%, with a maximum likelihood estimate of nest success of 45.6 &plusmn; 5.3%. Females selected nest sites that had greater sagebrush canopy cover and visual obstruction of the nest bowl compared to random sites. Nest survival models indicated that taller grass surrounding nests increased nest survival. Tall grass may supplement the low sagebrush cover in this area in providing suitable nest sites for Greater Sage-Grouse. Land managers on the eastern edge of Greater Sage-Grouse range could focus on increasing sagebrush density while maintaining tall grass by developing range management practices that accomplish this goal. To achieve nest survival rates similar to other populations, predictions from our models suggest 26 cm grass height would result in approximately 50% nest survival. Optimal conditions could be accomplished by adjusting livestock grazing systems and stocking rates.","language":"English","publisher":"University of California Press","publisherLocation":"Berkeley, CA","usgsCitation":"Kaczor, N., Jensen, K.C., Klaver, R.W., Rumble, M.A., Herman-Brunson, K.M., and Swanson, C., 2011, Nesting success and resource selection of greater sage grouse in South Dakota: Chapter 8: Studies in Avian Biology; Ecology, Conservation, and Management of Grouse, v. 39, p. 107-118.","productDescription":"12 p.","startPage":"107","endPage":"118","costCenters":[{"id":222,"text":"Earth Resources Observation and Science (EROS) Center","active":true,"usgs":true}],"links":[{"id":257333,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":257326,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://www.treesearch.fs.fed.us/pubs/39755","linkFileType":{"id":5,"text":"html"}}],"country":"United 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W.","contributorId":43217,"corporation":false,"usgs":true,"family":"Kaczor","given":"Nicholas W.","affiliations":[],"preferred":false,"id":349663,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Jensen, Kent C.","contributorId":66530,"corporation":false,"usgs":false,"family":"Jensen","given":"Kent","email":"","middleInitial":"C.","affiliations":[{"id":16687,"text":"Department of Natural Resource Management, South Dakota State University, Brookings, SD","active":true,"usgs":false}],"preferred":false,"id":349667,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Klaver, Robert W. 0000-0002-3263-9701 bklaver@usgs.gov","orcid":"https://orcid.org/0000-0002-3263-9701","contributorId":3285,"corporation":false,"usgs":true,"family":"Klaver","given":"Robert","email":"bklaver@usgs.gov","middleInitial":"W.","affiliations":[{"id":199,"text":"Coop Res Unit Leetown","active":true,"usgs":true},{"id":222,"text":"Earth Resources Observation and Science (EROS) Center","active":true,"usgs":true}],"preferred":true,"id":349661,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Rumble, Mark A.","contributorId":84615,"corporation":false,"usgs":true,"family":"Rumble","given":"Mark","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":349668,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Herman-Brunson, Katie M.","contributorId":66109,"corporation":false,"usgs":true,"family":"Herman-Brunson","given":"Katie","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":349666,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Swanson, Christopher C.","contributorId":58505,"corporation":false,"usgs":true,"family":"Swanson","given":"Christopher C.","affiliations":[],"preferred":false,"id":349665,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}}
,{"id":70003958,"text":"70003958 - 2011 - Timing of seasonal migration in mule deer: effects of climate, plant phenology, and life-history characteristics","interactions":[],"lastModifiedDate":"2012-06-08T17:03:14","indexId":"70003958","displayToPublicDate":"2012-01-01T13:03:36","publicationYear":"2011","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1475,"text":"Ecosphere","active":true,"publicationSubtype":{"id":10}},"title":"Timing of seasonal migration in mule deer: effects of climate, plant phenology, and life-history characteristics","docAbstract":"Phenological events of plants and animals are sensitive to climatic processes. Migration is a life-history event exhibited by most large herbivores living in seasonal environments, and is thought to occur in response to dynamics of forage and weather. Decisions regarding when to migrate, however, may be affected by differences in life-history characteristics of individuals. Long-term and intensive study of a population of mule deer (<i>Odocoileus hemionus</i>) in the Sierra Nevada, California, USA, allowed us to document patterns of migration during 11 years that encompassed a wide array of environmental conditions. We used two new techniques to properly account for interval-censored data and disentangle effects of broad-scale climate, local weather patterns, and plant phenology on seasonal patterns of migration, while incorporating effects of individual life-history characteristics. Timing of autumn migration varied substantially among individual deer, but was associated with the severity of winter weather, and in particular, snow depth and cold temperatures. Migratory responses to winter weather, however, were affected by age, nutritional condition, and summer residency of individual females. Old females and those in good nutritional condition risked encountering severe weather by delaying autumn migration, and were thus risk-prone with respect to the potential loss of foraging opportunities in deep snow compared with young females and those in poor nutritional condition. Females that summered on the west side of the crest of the Sierra Nevada delayed autumn migration relative to east-side females, which supports the influence of the local environment on timing of migration. In contrast, timing of spring migration was unrelated to individual life-history characteristics, was nearly twice as synchronous as autumn migration, differed among years, was related to the southern oscillation index, and was influenced by absolute snow depth and advancing phenology of plants. Plasticity in timing of migration in response to climatic conditions and plant phenology may be an adaptive behavioral strategy, which should reduce the detrimental effects of trophic mismatches between resources and other life-history events of large herbivores. Failure to consider effects of nutrition and other life-history traits may cloud interpretation of phenological patterns of mammals and conceal relationships associated with climate change.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Ecosphere","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"Ecological Society of America","publisherLocation":"Ithaca, NY","doi":"10.1890/ES10-00096.1","usgsCitation":"Monteith, K.L., Bleich, V.C., Stephenson, T.R., Pierce, B.M., Conner, M.M., Klaver, R.W., and Bowyer, R., 2011, Timing of seasonal migration in mule deer: effects of climate, plant phenology, and life-history characteristics: Ecosphere, v. 2, no. 4, 34 p.; art47, https://doi.org/10.1890/ES10-00096.1.","productDescription":"34 p.; art47","costCenters":[{"id":222,"text":"Earth Resources Observation and Science (EROS) Center","active":true,"usgs":true}],"links":[{"id":474803,"rank":10000,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1890/es10-00096.1","text":"Publisher Index Page"},{"id":257330,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":257323,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1890/ES10-00096.1","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"California","otherGeospatial":"Sierra Nevada","volume":"2","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505bb3f5e4b08c986b3260c3","contributors":{"authors":[{"text":"Monteith, Kevin L.","contributorId":83400,"corporation":false,"usgs":true,"family":"Monteith","given":"Kevin","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":349718,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bleich, Vernon C.","contributorId":10293,"corporation":false,"usgs":true,"family":"Bleich","given":"Vernon","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":349716,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Stephenson, Thomas R.","contributorId":64114,"corporation":false,"usgs":true,"family":"Stephenson","given":"Thomas","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":349717,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Pierce, Beck M.","contributorId":87038,"corporation":false,"usgs":true,"family":"Pierce","given":"Beck","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":349719,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Conner, Mary M.","contributorId":95342,"corporation":false,"usgs":true,"family":"Conner","given":"Mary","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":349720,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Klaver, Robert W. 0000-0002-3263-9701 bklaver@usgs.gov","orcid":"https://orcid.org/0000-0002-3263-9701","contributorId":3285,"corporation":false,"usgs":true,"family":"Klaver","given":"Robert","email":"bklaver@usgs.gov","middleInitial":"W.","affiliations":[{"id":199,"text":"Coop Res Unit Leetown","active":true,"usgs":true},{"id":222,"text":"Earth Resources Observation and Science (EROS) Center","active":true,"usgs":true}],"preferred":true,"id":349714,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Bowyer, R. Terry","contributorId":9533,"corporation":false,"usgs":true,"family":"Bowyer","given":"R. Terry","affiliations":[],"preferred":false,"id":349715,"contributorType":{"id":1,"text":"Authors"},"rank":7}]}}
,{"id":70005649,"text":"70005649 - 2011 - The dazed and confused identity of Agassiz's land tortoise, Gopherus agassizii (Testudines, Testudinidae) with the description of a new species, and its consequences for conservation","interactions":[],"lastModifiedDate":"2021-05-21T20:01:21.966498","indexId":"70005649","displayToPublicDate":"2012-01-01T12:03:00","publicationYear":"2011","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3808,"text":"ZooKeys","active":true,"publicationSubtype":{"id":10}},"displayTitle":"The dazed and confused identity of Agassiz's land tortoise, <i>Gopherus agassizii</i> (Testudines, Testudinidae) with the description of a new species, and its consequences for conservation","title":"The dazed and confused identity of Agassiz's land tortoise, Gopherus agassizii (Testudines, Testudinidae) with the description of a new species, and its consequences for conservation","docAbstract":"We investigate a cornucopia of problems associated with the identity of the desert tortoise, <i>Gopherus agassizii</i> Cooper. The date of publication is found to be 1861, rather than 1863. Only one of the three original cotypes exists, and it is designated as the lectotype of the species. Another cotype is found to have been destroyed in the 1906 San Francisco earthquake and subsequent fire. The third is lost. The lectotype is genetically confirmed to be from California, and not Arizona, USA as sometimes reported. Maternally, the holotype of <i>G. lepidocephalus</i> Ottley et Vel&#225;zques Solis, 1989 from the Cape Region of Baja California Sur, Mexico is also from the Mojavian population of the desert tortoise, and not from Tiburon Island, Sonora, Mexico as previously proposed. A suite of characters serve to diagnose tortoises west and north of the Colorado River, the Mojavian population, from those east and south of the river in Arizona, USA and Sonora and Sinaloa, Mexico, the Sonoran population. Species recognition is warranted and because <i>G. lepidocephalus</i> is from the Mojavian population no names are available for the Sonoran species. Thus, a new species, <i>Gopherus morafkai</i> sp. n., is named and this action reduces the distribution of <i>G. agassizii</i> to only 30% of its former range. This reduction has important implications for the conservation and protection of <i>G. agassizii</i>, which may deserve a higher level of protection.","language":"English","publisher":"Pensoft Publishers","publisherLocation":"Sofia, Bulgaria","doi":"10.3897/zookeys.113.1353","usgsCitation":"Murphy, R.K., Berry, K., Edwards, T., Leviton, A.E., Lathrop, A., and Riedle, J., 2011, The dazed and confused identity of Agassiz's land tortoise, Gopherus agassizii (Testudines, Testudinidae) with the description of a new species, and its consequences for conservation: ZooKeys, v. 113, p. 39-71, https://doi.org/10.3897/zookeys.113.1353.","productDescription":"33 p.","startPage":"39","endPage":"71","numberOfPages":"33","costCenters":[{"id":651,"text":"Western Ecological Research Center","active":true,"usgs":true}],"links":[{"id":474805,"rank":1,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.3897/zookeys.113.1353","text":"Publisher Index Page"},{"id":204352,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"Mexico. 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Daren","contributorId":10919,"corporation":false,"usgs":true,"family":"Riedle","given":"J. Daren","affiliations":[],"preferred":false,"id":353001,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}}
,{"id":70037807,"text":"70037807 - 2011 - Use of cranial characters in taxonomy of the Minnesota wolf (<i>Canis</i> sp.)","interactions":[],"lastModifiedDate":"2018-01-04T11:40:11","indexId":"70037807","displayToPublicDate":"2012-01-01T09:04:46","publicationYear":"2011","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1176,"text":"Canadian Journal of Zoology","active":true,"publicationSubtype":{"id":10}},"title":"Use of cranial characters in taxonomy of the Minnesota wolf (<i>Canis</i> sp.)","docAbstract":"Minnesota wolves (<i>Canis</i> sp.) sometimes are reported to have affinity to a small, narrow-skulled eastern form (<i>Canis lupus lycaon</i> Schreber, 1775) and sometimes to a larger, broader western form (<i>Canis lupus nubilus</i> Say, 1823). We found that pre-1950 Minnesota wolf skulls were similar in size to those of wolves from southeastern Ontario and smaller than those of western wolves. However, Minnesota wolf skulls during 1970&ndash;1976 showed a shift to the larger, western form. Although Minnesota skull measurements after 1976 were unavailable, rostral ratios from 1969 through 1999 were consistent with hybridization between the smaller eastern wolf and the western form. Our findings help resolve the different taxonomic interpretations of Minnesota skull morphology and are consistent with molecular evidence of recent hybridization or intergradation of the two forms of wolves in Minnesota. Together these data indicate that eastern- and western-type wolves historically mixed and hybridized in Minnesota and continue to do so. Our findings are relevant to a recent government proposal to delist wolves from the endangered species list in Minnesota and surrounding states.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Canadian Journal of Zoology","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"NRC Research Press","publisherLocation":"Ottawa, ON","doi":"10.1139/z11-097","usgsCitation":"Mech, L.D., Nowak, R.M., and Weisberg, S., 2011, Use of cranial characters in taxonomy of the Minnesota wolf (<i>Canis</i> sp.): Canadian Journal of Zoology, v. 89, no. 12, p. 1188-1194, https://doi.org/10.1139/z11-097.","productDescription":"7 p.","startPage":"1188","endPage":"1194","costCenters":[{"id":480,"text":"Northern Prairie Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":257194,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":257183,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1139/z11-097","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Minnesota","volume":"89","issue":"12","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505bbedde4b08c986b32981a","contributors":{"authors":[{"text":"Mech, L. David 0000-0003-3944-7769 david_mech@usgs.gov","orcid":"https://orcid.org/0000-0003-3944-7769","contributorId":2518,"corporation":false,"usgs":true,"family":"Mech","given":"L.","email":"david_mech@usgs.gov","middleInitial":"David","affiliations":[{"id":480,"text":"Northern Prairie Wildlife Research Center","active":true,"usgs":true}],"preferred":true,"id":462777,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Nowak, Ronald M.","contributorId":25622,"corporation":false,"usgs":true,"family":"Nowak","given":"Ronald","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":462778,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Weisberg, Sanford","contributorId":36002,"corporation":false,"usgs":true,"family":"Weisberg","given":"Sanford","email":"","affiliations":[],"preferred":false,"id":462779,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70042247,"text":"sir201151204 - 2011 - Baseline hydrologic studies in the lower Elwha River prior to dam removal","interactions":[],"lastModifiedDate":"2016-12-19T13:31:43","indexId":"sir201151204","displayToPublicDate":"2012-01-01T00:00:00","publicationYear":"2011","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":"2011-5120-4","title":"Baseline hydrologic studies in the lower Elwha River prior to dam removal","docAbstract":"After the removal of two large, long‑standing dams on the Elwha River, Washington, the additional load of sediment and wood is expected to affect the hydrology of the lower river, its estuary, and the alluvial aquifer underlying the surrounding flood plain. To better understand the surface-water and groundwater characteristics of the river and estuary before dam removal, several hydrologic data sets were collected and analyzed. An experiment using a dye tracer characterized transient storage, and it was determined that the low‑flow channel of the lower Elwha River was relatively simple; 1–6 percent of the median travel time of dye was attributed to transient‑storage processes. Water data from monitoring wells adjacent to the main‑stem river indicated a strong hydraulic connectivity between stage in the river and groundwater levels in the flood plain. Analysis of temperature data from the monitoring wells showed that changes in the groundwater temperature responded weeks or months after water temperature changed in the river. A seepage investigation indicated that water from the river was moving into the aquifer (losing\nreach) between 1.7 and 2.8 kilometers from the river mouth. Surface‑water measurements and temperature and salinity data collected throughout the estuary helped to characterize the magnitude and nature of water movement in and out of the estuary. Salinity and stage sensors positioned in the estuarine network showed a strong surface‑water connection between the river and estuary waters east of the river. In contrast, there was a weaker connection between the river and estuarine water bodies west of the river.","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Coastal habitats of the Elwha River, Washington--biological and physical patterns and processes prior to dam removal (Chapter 2011-5120)","largerWorkSubtype":{"id":5,"text":"USGS Numbered Series"},"language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/sir201151204","collaboration":"This report is Chapter 4 in <i>Coastal habitats of the Elwha River, Washington--biological and physical patterns and processes prior to dam removal</i>.  For more information, see: <a href=\"http://pubs.usgs.gov/sir/2011/5120/\" target=\"_blank\">Scientific Investigations Report 2011-5120</a>","usgsCitation":"Magirl, C.S., Curran, C.A., Sheibley, R.W., Warrick, J., Czuba, J., Czuba, C.R., Gendaszek, A.S., Shafroth, P.B., Duda, J., and Foreman, J.R., 2011, Baseline hydrologic studies in the lower Elwha River prior to dam removal: U.S. Geological Survey Scientific Investigations Report 2011-5120-4, 36 p., https://doi.org/10.3133/sir201151204.","productDescription":"36 p.","startPage":"75","endPage":"110","costCenters":[{"id":654,"text":"Western Fisheries Research Center","active":true,"usgs":true}],"links":[{"id":264925,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":264924,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/sir/2011/5120/pdf/sir20115120_ch4.pdf"}],"country":"United States","state":"Washington","otherGeospatial":"Elwha River","geographicExtents":"{\n  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0000-0002-0205-3814","orcid":"https://orcid.org/0000-0002-0205-3814","contributorId":48255,"corporation":false,"usgs":true,"family":"Warrick","given":"Jonathan A.","affiliations":[],"preferred":false,"id":471091,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Czuba, Jonathan A.","contributorId":19917,"corporation":false,"usgs":true,"family":"Czuba","given":"Jonathan A.","affiliations":[{"id":622,"text":"Washington Water Science Center","active":true,"usgs":true}],"preferred":false,"id":471090,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Czuba, Christiana R. cczuba@usgs.gov","contributorId":4555,"corporation":false,"usgs":true,"family":"Czuba","given":"Christiana","email":"cczuba@usgs.gov","middleInitial":"R.","affiliations":[{"id":392,"text":"Minnesota Water Science Center","active":true,"usgs":true}],"preferred":false,"id":471089,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Gendaszek, Andrew S. 0000-0002-2373-8986 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J.","affiliations":[],"preferred":false,"id":471092,"contributorType":{"id":1,"text":"Authors"},"rank":9},{"text":"Foreman, James R. 0000-0003-0535-4580 jforeman@usgs.gov","orcid":"https://orcid.org/0000-0003-0535-4580","contributorId":3669,"corporation":false,"usgs":true,"family":"Foreman","given":"James","email":"jforeman@usgs.gov","middleInitial":"R.","affiliations":[{"id":622,"text":"Washington Water Science Center","active":true,"usgs":true}],"preferred":false,"id":471088,"contributorType":{"id":1,"text":"Authors"},"rank":10}]}}
,{"id":70003815,"text":"70003815 - 2011 - Key science issues in the central and eastern United States for the next version of the USGS National Seismic Hazard Maps","interactions":[],"lastModifiedDate":"2013-02-14T14:35:53","indexId":"70003815","displayToPublicDate":"2012-01-01T00:00:00","publicationYear":"2011","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":18,"text":"Abstract or summary"},"title":"Key science issues in the central and eastern United States for the next version of the USGS National Seismic Hazard Maps","docAbstract":"The USGS National Seismic Hazard Maps are updated about every six years by incorporating newly vetted science on earthquakes and ground motions. The 2008 hazard maps for the central and eastern United States region (CEUS) were updated by using revised New Madrid and Charleston source models, an updated seismicity catalog and an estimate of magnitude uncertainties, a distribution of maximum magnitudes, and several new ground-motion prediction equations. The new models resulted in significant ground-motion changes at 5 Hz and 1 Hz spectral acceleration with 5% damping compared to the 2002 version of the hazard maps. The 2008 maps have now been incorporated into the 2009 NEHRP Recommended Provisions, the 2010 ASCE-7 Standard, and the 2012 International Building Code. The USGS is now planning the next update of the seismic hazard maps, which will be provided to the code committees in December 2013. Science issues that will be considered for introduction into the CEUS maps include: 1) updated recurrence models for New Madrid sources, including new geodetic models and magnitude estimates; 2) new earthquake sources and techniques considered in the 2010 model developed by the nuclear industry; 3) new NGA-East ground-motion models (currently under development); and 4) updated earthquake catalogs. We will hold a regional workshop in late 2011 or early 2012 to discuss these and other issues that will affect the seismic hazard evaluation in the CEUS.","largerWorkTitle":"Seismological Society of America, 2011 Annual Meeting","language":"English","publisher":"Seismological Society of America","usgsCitation":"Peterson, M., and Mueller, C., 2011, Key science issues in the central and eastern United States for the next version of the USGS National Seismic Hazard Maps, <i>in</i> Seismological Society of America, 2011 Annual Meeting.","ipdsId":"IP-026828","costCenters":[{"id":300,"text":"Geologic Hazards Science Center","active":true,"usgs":true}],"links":[{"id":267418,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"511e158de4b071e86a19a45f","contributors":{"authors":[{"text":"Peterson, M.D.","contributorId":90614,"corporation":false,"usgs":true,"family":"Peterson","given":"M.D.","email":"","affiliations":[],"preferred":false,"id":348985,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Mueller, C.S.","contributorId":45310,"corporation":false,"usgs":true,"family":"Mueller","given":"C.S.","email":"","affiliations":[],"preferred":false,"id":348984,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70042248,"text":"sir201151205 - 2011 - Coastal processes of the Elwha River delta: Chapter 5 in <i>Coastal habitats of the Elwha River, Washington--biological and physical patterns and processes prior to dam removal</i>","interactions":[],"lastModifiedDate":"2012-12-29T20:11:21","indexId":"sir201151205","displayToPublicDate":"2012-01-01T00:00:00","publicationYear":"2011","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":"2011-5120-5","title":"Coastal processes of the Elwha River delta: Chapter 5 in <i>Coastal habitats of the Elwha River, Washington--biological and physical patterns and processes prior to dam removal</i>","docAbstract":"To understand the effects of increased sediment supply from dam removal on marine habitats around the Elwha River delta, a basic understanding of the region’s coastal processes is necessary. This chapter provides a summary of the physical setting of the coast near the Elwha River delta, for the purpose of synthesizing the processes that move and disperse sediment discharged by the river. One fundamental property of this coastal setting is the difference between currents in the surfzone with those in the coastal waters offshore of the surfzone. Surfzone currents are largely dictated by the direction and size of waves, and the waves that attack the Elwha River delta predominantly come from Pacific Ocean swell from the west. This establishes surfzone currents and littoral sediment transport that are eastward along much of the delta. Offshore of the surfzone the currents are largely influenced by tidal circulation and the physical constraint to flow provided by the delta’s headland. During both ebbing and flooding tides, the flow separates from the coast at the tip of the delta’s headland, and this produces eddies on the downstream side of the headland. Immediately offshore of the Elwha River mouth, this creates a situation in which the coastal currents are directed toward the east much more frequently than toward the west. This suggests that Elwha River sediment will be more likely to move toward the east in the coastal system.","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Coastal habitats of the Elwha River, Washington--biological and physical patterns and processes prior to dam removal (SIR 2011-5120)","largerWorkSubtype":{"id":5,"text":"USGS Numbered Series"},"language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/sir201151205","collaboration":"This report is Chapter 5 in in <i>Coastal habitats of the Elwha River, Washington--biological and physical patterns and processes prior to dam removal</i>.  For more information, see: <a href=\"http://pubs.usgs.gov/sir/2011/5120/\" target=\"_blank\">Scientific Investigations Report 2011-5120</a>","usgsCitation":"Warrick, J., Stevens, A., Miller, I.M., and Gelfenbaum, G., 2011, Coastal processes of the Elwha River delta: Chapter 5 in <i>Coastal habitats of the Elwha River, Washington--biological and physical patterns and processes prior to dam removal</i>: U.S. Geological Survey Scientific Investigations Report 2011-5120-5, 20 p., https://doi.org/10.3133/sir201151205.","productDescription":"20 p.","startPage":"111","endPage":"130","costCenters":[{"id":654,"text":"Western Fisheries Research Center","active":true,"usgs":true}],"links":[{"id":264927,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":264926,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/sir/2011/5120/pdf/sir20115120_ch5.pdf"}],"country":"United States","state":"Washington","otherGeospatial":"Elwha River","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -123.5832,46.794 ], [ -123.5832,47.9652 ], [ -123.448,47.9652 ], [ -123.448,46.794 ], [ -123.5832,46.794 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"50e5d0fce4b0a4aa5bb0b0bd","contributors":{"editors":[{"text":"Duda, Jeffrey J.","contributorId":68854,"corporation":false,"usgs":true,"family":"Duda","given":"Jeffrey J.","affiliations":[],"preferred":false,"id":509133,"contributorType":{"id":2,"text":"Editors"},"rank":1},{"text":"Warrick, Jonathan A. 0000-0002-0205-3814","orcid":"https://orcid.org/0000-0002-0205-3814","contributorId":48255,"corporation":false,"usgs":true,"family":"Warrick","given":"Jonathan A.","affiliations":[],"preferred":false,"id":509132,"contributorType":{"id":2,"text":"Editors"},"rank":2},{"text":"Magirl, Christopher S. 0000-0002-9922-6549 magirl@usgs.gov","orcid":"https://orcid.org/0000-0002-9922-6549","contributorId":1822,"corporation":false,"usgs":true,"family":"Magirl","given":"Christopher","email":"magirl@usgs.gov","middleInitial":"S.","affiliations":[{"id":128,"text":"Arizona Water Science Center","active":true,"usgs":true},{"id":622,"text":"Washington Water Science Center","active":true,"usgs":true}],"preferred":true,"id":509131,"contributorType":{"id":2,"text":"Editors"},"rank":3}],"authors":[{"text":"Warrick, Jonathan A. 0000-0002-0205-3814","orcid":"https://orcid.org/0000-0002-0205-3814","contributorId":48255,"corporation":false,"usgs":true,"family":"Warrick","given":"Jonathan A.","affiliations":[],"preferred":false,"id":471094,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Stevens, Andrew W.","contributorId":89093,"corporation":false,"usgs":true,"family":"Stevens","given":"Andrew W.","affiliations":[],"preferred":false,"id":471096,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Miller, Ian M. 0000-0002-3289-6337","orcid":"https://orcid.org/0000-0002-3289-6337","contributorId":41951,"corporation":false,"usgs":false,"family":"Miller","given":"Ian","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":471093,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Gelfenbaum, Guy","contributorId":79844,"corporation":false,"usgs":true,"family":"Gelfenbaum","given":"Guy","affiliations":[],"preferred":false,"id":471095,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70173434,"text":"70173434 - 2011 - <i>Cambarus (Puncticambarus) smilax</i>, a new species of crayfish (Crustacea: Decapoda: Cambaridae) from the Greenbrier River basin of West Virginia","interactions":[],"lastModifiedDate":"2016-06-20T16:39:41","indexId":"70173434","displayToPublicDate":"2012-01-01T00:00:00","publicationYear":"2011","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3147,"text":"Proceedings of the Biological Society of Washington","active":true,"publicationSubtype":{"id":10}},"title":"<i>Cambarus (Puncticambarus) smilax</i>, a new species of crayfish (Crustacea: Decapoda: Cambaridae) from the Greenbrier River basin of West Virginia","docAbstract":"<p><i>Cambarus</i><span>&nbsp;(</span><i>Puncticambarus</i><span>)&nbsp;</span><i>smilax</i><span>&nbsp;is a stream-dwelling crayfish that appears to be endemic to the Greenbrier River basin in the Valley and Ridge province of West Virginia. Within the Greenbrier system it occurs primarily in tributaries to the Greenbrier mainstem, with stable populations in the East and West Fork, and Thorny, Knapp, and Deer creeks. The new species is morphologically most similar to&nbsp;</span><i>C.</i><span>&nbsp;(</span><i>P.</i><span>)&nbsp;</span><i>robustus</i><span>, from which it can be distinguished by a combination of the following characters: adult palm length comprising 73&ndash;76% of palm width as opposed to 63&ndash;70% in&nbsp;</span><i>C.</i><span>&nbsp;(</span><i>P.</i><span>)</span><i>robustus</i><span>; ventral surface of chela of cheliped with 0&ndash;2 subpalmar tubercles compared to 3&ndash;6 subpalmar tubercles in&nbsp;</span><i>C.</i><span>&nbsp;(</span><i>P.</i><span>)&nbsp;</span><i>robustus</i><span>; lack of tubercles on the dorsal surface of chela; longer, more tapering, less rectangular rostrum (47&ndash;52% rostrum width/length ratio) compared to&nbsp;</span><i>C.</i><span>&nbsp;(</span><i>P.</i><span>)&nbsp;</span><i>robustus</i><span>shorter, less tapering rectangular rostrum (54&ndash;63% rostrum width/length ratio); and the central projection of the form-I male gonopod curved &le;90 degrees to the shaft.</span></p>","language":"English","publisher":"Biological Society of Washington","doi":"10.2988/10-09.1","usgsCitation":"Loughman, Z.J., Simon, T.P., and Welsh, S., 2011, <i>Cambarus (Puncticambarus) smilax</i>, a new species of crayfish (Crustacea: Decapoda: Cambaridae) from the Greenbrier River basin of West Virginia: Proceedings of the Biological Society of Washington, v. 124, no. 2, p. 99-111, https://doi.org/10.2988/10-09.1.","productDescription":"13 p.","startPage":"99","endPage":"111","onlineOnly":"N","additionalOnlineFiles":"N","ipdsId":"IP-023052","costCenters":[{"id":199,"text":"Coop Res Unit Leetown","active":true,"usgs":true}],"links":[{"id":324037,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"West Virginia","otherGeospatial":"Greenbrier River basin, Valley and Ridge province","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n 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PSC"},"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"576913ade4b07657d19fef7a","contributors":{"authors":[{"text":"Loughman, Zachary J.","contributorId":76157,"corporation":false,"usgs":false,"family":"Loughman","given":"Zachary","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":639914,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Simon, Thomas P.","contributorId":77081,"corporation":false,"usgs":true,"family":"Simon","given":"Thomas","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":639915,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Welsh, Stuart A. 0000-0003-0362-054X swelsh@usgs.gov","orcid":"https://orcid.org/0000-0003-0362-054X","contributorId":152088,"corporation":false,"usgs":true,"family":"Welsh","given":"Stuart A.","email":"swelsh@usgs.gov","affiliations":[{"id":199,"text":"Coop Res Unit 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,{"id":70154900,"text":"70154900 - 2011 - Persistence of the longnose darter (<i>P. nasuta</i>) in Lee Creek, Oklahoma","interactions":[],"lastModifiedDate":"2015-09-16T09:40:05","indexId":"70154900","displayToPublicDate":"2012-01-01T00:00:00","publicationYear":"2011","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3894,"text":"Proceedings of the Oklahoma Academy of Science","active":true,"publicationSubtype":{"id":10}},"title":"Persistence of the longnose darter (<i>P. nasuta</i>) in Lee Creek, Oklahoma","docAbstract":"<p>The longnose darter Percina nasuta (Bailey) is one of Oklahoma&rsquo;s rarest fish species (1) and is listed by the state as endangered. Throughout the rest of its range, which includes Missouri, Arkansas and the far eastern portion of Oklahoma, the longnose darter is classified as &ldquo;rare&rdquo; or &ldquo;threatened&rdquo; (2, 3, 4, 5, 6, 1). This species inhabits both slow- and fast-water habitats with cobble and gravel substrates in medium to large streams (7, 8, 1). Oklahoma populations of longnose darter are known to occur only in the Poteau River and Lee Creek drainages in Le Flore and Sequoyah counties, respectively (9, 10). Cross and Moore (9) collected longnose darters from the Poteau River in 1947. The species was not collected in a subsequent survey of the Poteau River in 1974 (11), possibly because of the effects from the Wister Dam, which was completed in 1949. Darters are especially susceptible to flow alterations from dams (2, 12). This, together with the 1992 completion of Lee Creek Reservoir in Arkansas, has raised concern for the Lee Creek population of longnose darters (13).</p>\n<p>Lee Creek is one of Oklahoma&rsquo;s six rivers designated as \"scenic\" by the Oklahoma Legislature. Lee Creek is located&nbsp;on the Oklahoma-Arkansas border in far eastern Oklahoma. The headwaters originate in northwestern Arkansas and flow south towards the Arkansas River. While the majority of the stream is in Arkansas, a portion flows into Oklahoma northwest of Uniontown, AR and continues for 28.2 river-km before crossing back into Arkansas near Van Buren, AR. The hydrology of lower Lee Creek has been altered by Lee Creek Reservoir near Van Buren, AR. It was believed that pre-impounded Lee Creek had the largest existing population of longnose darters (8). However, the most recent fish surveys in Lee Creek were conducted approximately twenty years ago. Robinson (8) surveyed Lee Creek in Arkansas, upstream of the Oklahoma border, and found longnose darters upstream of Natural Dam, AR. Wagner et al. (10) were the last to document longnose darter presence in the Oklahoma segment of Lee Creek. No efforts to collect this species in Oklahoma have occurred since the completion of Lee Creek Reservoir. Our objective was to determine whether the species persist in this segment of its historic range since impoundment.</p>","language":"English","publisher":"Oklahoma Academy of Science","publisherLocation":"Weatherford, OK","usgsCitation":"Gatlin, M.R., and Long, J.M., 2011, Persistence of the longnose darter (<i>P. nasuta</i>) in Lee Creek, Oklahoma: Proceedings of the Oklahoma Academy of Science, v. 91, p. 11-14.","productDescription":"4 p.","startPage":"11","endPage":"14","onlineOnly":"N","additionalOnlineFiles":"N","ipdsId":"IP-026882","costCenters":[{"id":198,"text":"Coop Res Unit Atlanta","active":true,"usgs":true}],"links":[{"id":308156,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":308155,"rank":1,"type":{"id":15,"text":"Index Page"},"url":"https://digital.library.okstate.edu/OAS/oas_htm_files/v91/index.html"}],"country":"United States","state":"Oklahoma","otherGeospatial":"Lee Creek","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -103.0078125,\n              37.00255267215955\n            ],\n            [\n              -94.54833984375,\n              37.03763967977139\n            ],\n            [\n              -94.5703125,\n              36.527294814546245\n            ],\n            [\n              -94.41650390625,\n              35.496456056584165\n            ],\n            [\n              -94.46044921875,\n              33.578014746143985\n            ],\n            [\n              -95.16357421875,\n              33.8521697014074\n            ],\n            [\n              -95.44921875,\n              33.779147331286474\n            ],\n            [\n              -95.6689453125,\n              33.88865750124075\n            ],\n            [\n              -96.43798828125,\n              33.54139466898275\n            ],\n            [\n              -96.8115234375,\n              33.76088200086917\n            ],\n            [\n              -97.2509765625,\n              33.65120829920497\n            ],\n            [\n              -98.2177734375,\n              33.97980872872457\n            ],\n            [\n              -99.20654296875,\n              34.161818161230386\n            ],\n            [\n              -99.42626953125,\n              34.32529192442733\n            ],\n            [\n              -99.68994140625,\n              34.21634468843465\n            ],\n            [\n              -100.01953125,\n              34.615126683462194\n            ],\n            [\n              -100.04150390625,\n              36.527294814546245\n            ],\n            [\n              -103.0517578125,\n              36.491973470593685\n            ],\n            [\n              -103.0078125,\n              37.00255267215955\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"91","publishingServiceCenter":{"id":8,"text":"Raleigh PSC"},"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"55fa92c7e4b05d6c4e501ab5","contributors":{"authors":[{"text":"Gatlin, Michael R.","contributorId":141324,"corporation":false,"usgs":false,"family":"Gatlin","given":"Michael","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":564835,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Long, James M. 0000-0002-8658-9949 jmlong@usgs.gov","orcid":"https://orcid.org/0000-0002-8658-9949","contributorId":3453,"corporation":false,"usgs":true,"family":"Long","given":"James","email":"jmlong@usgs.gov","middleInitial":"M.","affiliations":[{"id":198,"text":"Coop Res Unit Atlanta","active":true,"usgs":true}],"preferred":true,"id":564327,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70046493,"text":"70046493 - 2011 - Guidance manual for forensic analysis of perchlorate in groundwater using chlorine and oxygen isotopic analyses","interactions":[],"lastModifiedDate":"2019-07-26T14:46:51","indexId":"70046493","displayToPublicDate":"2011-12-31T15:40:24","publicationYear":"2011","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":4,"text":"Other Government Series"},"title":"Guidance manual for forensic analysis of perchlorate in groundwater using chlorine and oxygen isotopic analyses","docAbstract":"Increased health concerns about perchlorate (ClO4-) during the past decade and subsequent regulatory considerations have generated appreciable interest in source identification. The key objective of the isotopic techniques described in this guidance manual is to provide evidence concerning the origin of ClO4- in soils and groundwater and, more specifically, whether that ClO4- is synthetic or natural. Chlorine and oxygen isotopic analyses of ClO4- provide the primary direct approach whereby different sources of ClO4- can be distinguished from each other. These techniques measure the relative abundances of the stable isotopes of chlorine (37Cl and 35Cl) and oxygen (18O, 17O, and 16O) in ClO4- using isotope-ratio mass spectrometry (IRMS). In addition, the relative abundance of the radioactive chlorine isotope 36Cl is measured using accelerator mass spectrometry (AMS). Taken together, these measurements provide four independent quantities that can be used to distinguish natural and synthetic ClO4- sources, to discriminate different types of natural ClO4-, and to detect ClO4- biodegradation in the environment. Other isotopic, chemical, and geochemical techniques that can be applied in conjunction with isotopic analyses of ClO4- to provide supporting data in forensic studies are also described. This guidance manual is intended to provide details of the methodology used to (1) collect ClO4- samples from the environment, particularly from groundwater, which is the main medium of interest for ClO4- source identification; (2) purify the collected ClO4- samples; (3) conduct oxygen (O) and chlorine (Cl) isotopic analyses on the purified samples; and (4) determine probable sources using the resulting isotope data. Current practices for groundwater sampling and quality assurance for sample collection, purification, and measurement of Cl and O isotopes in ClO4- are provided. A detailed case study of source evaluation in groundwater on Long Island is given along with the current literature on the subject of ClO4- source discrimination. ClO4- in the environment is derived from both synthetic and natural sources. Synthetic ClO4- salts, including ammonium perchlorate (NH4ClO4) and potassium perchlorate (KClO4), have been widely used as oxidants by the military and aerospace industry. A variety of commercial products also contain synthetic ClO4-,including fireworks, matches, air bags, chlorine bleach, safety flares, perchloric acid, and chlorate herbicides. Historical disposal practices by the military, aerospace industry, and chemical manufacturers have resulted in groundwater and drinking water contamination with ClO4- in the United States. Isolated contamination from\nfireworks, road flares, explosives, and perchloric acid has also been reported. However, ClO4- is also a naturally occurring anion. It is present with sodium nitrate (NaNO3) in surficial deposits in the Atacama Desert of Chile at an average concentration of around 0.1% (by mass) of the total soluble salt, and these deposits (sometimes referred to as “Chilean caliche”) were widely used in the United States during the first half of the 20th century as a source of inorganic nitrogen\nfertilizer. Natural ClO4- that is not associated with Chilean fertilizers has also recently been detected in the vadose zone, groundwaters, and mineral deposits collected from the arid southwestern United States, including 155,000 km2 of groundwater in the Southern High Plains (SHP) of Texas and New Mexico. In addition to synthetic sources, natural ClO4- from both Chilean fertilizers and indigenous sources represents a potentially large source of ClO4- in groundwater and drinking water in the United States.","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","usgsCitation":"U.S. Geological Survey, 2011, Guidance manual for forensic analysis of perchlorate in groundwater using chlorine and oxygen isotopic analyses.","ipdsId":"IP-033887","costCenters":[{"id":436,"text":"National Research Program - Eastern Branch","active":true,"usgs":true},{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":365960,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW"}
,{"id":70209241,"text":"70209241 - 2011 - The role of backbarrier infilling in the formation of barrier island systems","interactions":[],"lastModifiedDate":"2020-03-27T06:31:57","indexId":"70209241","displayToPublicDate":"2011-12-31T11:35:31","publicationYear":"2011","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"The role of backbarrier infilling in the formation of barrier island systems","docAbstract":"<p><span>Barrier islands develop through a variety of processes, including spit accretion, barrier elongation, and inlet filling. New geophysical and sedimentological data provide a means of documenting the presence of a paleoinlet within a barrier lithosome in the western Gulf of Maine, illuminating the process of backbarrier infilling and its effect on barrier and tidal inlet morphodynamics. The transport of sediment into the backbarrier through tidal inlets as well as sediment contribution from nearby rivers led to bay infilling, formation of tidal flats and marshes, and a vast reduction in the bay tidal prism. Using existing marsh stratigraphy and high resolution imaging of a paleo inlet, this study investigates the effects of this diminishing tidal prism and inlet closure process. Chronostratigraphic reconstructions and digital backstripping of the backbarrier explain rates and timing of infilling and eventual conversion of an open water lagoon to the modern high marsh and tidal creek system.</span></p>","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"The Proceedings of the Coastal Sediments 2011","largerWorkSubtype":{"id":12,"text":"Conference publication"},"conferenceTitle":"Coastal Sediments 2011","conferenceDate":"May 2-6, 2011","conferenceLocation":"Miami, FL","language":"English","publisher":"World Scientific","doi":"10.1142/9789814355537_0091","usgsCitation":"Hein, C.J., FitzGerald, D.M., Carruthers, E.A., Stone, B.D., and Gontz, A.M., 2011, The role of backbarrier infilling in the formation of barrier island systems, <i>in</i> The Proceedings of the Coastal Sediments 2011, v. 2011, Miami, FL, May 2-6, 2011, p. 1203-1216, https://doi.org/10.1142/9789814355537_0091.","productDescription":"14 p.","startPage":"1203","endPage":"1216","costCenters":[{"id":243,"text":"Eastern Geology and Paleoclimate Science Center","active":true,"usgs":true},{"id":40020,"text":"Florence Bascom Geoscience Center","active":true,"usgs":true}],"links":[{"id":373510,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","otherGeospatial":"Gulf of Maine","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -71.54296874999999,\n              41.77131167976407\n            ],\n            [\n              -70.4443359375,\n              41.21172151054787\n            ],\n            [\n              -66.70898437499999,\n              42.8115217450979\n            ],\n            [\n              -64.6875,\n              44.213709909702054\n            ],\n            [\n              -64.8193359375,\n              45.706179285330855\n            ],\n            [\n              -67.3681640625,\n              45.213003555993964\n            ],\n            [\n              -71.05957031249999,\n              43.83452678223682\n            ],\n            [\n              -71.54296874999999,\n              41.77131167976407\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"2011","noUsgsAuthors":false,"publicationDate":"2012-06-07","publicationStatus":"PW","contributors":{"authors":[{"text":"Hein, Christopher J.","contributorId":39893,"corporation":false,"usgs":true,"family":"Hein","given":"Christopher","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":785520,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"FitzGerald, Duncan M.","contributorId":48077,"corporation":false,"usgs":true,"family":"FitzGerald","given":"Duncan","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":785521,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Carruthers, Emily A.","contributorId":59709,"corporation":false,"usgs":true,"family":"Carruthers","given":"Emily","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":785522,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Stone, Byron D. 0000-0001-6092-0798 bdstone@usgs.gov","orcid":"https://orcid.org/0000-0001-6092-0798","contributorId":1702,"corporation":false,"usgs":true,"family":"Stone","given":"Byron","email":"bdstone@usgs.gov","middleInitial":"D.","affiliations":[{"id":243,"text":"Eastern Geology and Paleoclimate Science Center","active":true,"usgs":true},{"id":40020,"text":"Florence Bascom Geoscience Center","active":true,"usgs":true}],"preferred":true,"id":785523,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Gontz, Allen M.","contributorId":79784,"corporation":false,"usgs":true,"family":"Gontz","given":"Allen","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":785524,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":70242023,"text":"70242023 - 2011 - Traverse of the major fault systems of the Taconian deformational front, the Vermont Valley and core of the Green Mountain massif, southern Vermont","interactions":[],"lastModifiedDate":"2023-04-04T13:58:52.268584","indexId":"70242023","displayToPublicDate":"2011-12-31T08:53:49","publicationYear":"2011","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"Traverse of the major fault systems of the Taconian deformational front, the Vermont Valley and core of the Green Mountain massif, southern Vermont","docAbstract":"<p>No abstract available.</p>","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Guidebook for field trips in Vermont and adjacent New York","largerWorkSubtype":{"id":12,"text":"Conference publication"},"conferenceTitle":"New England Intercollegiate Geological Conference, 103rd Annual Meeting","conferenceDate":"Sep 30-Oct 2, 2011","conferenceLocation":"Middlebury, VT","language":"English","publisher":"Middlebury College","usgsCitation":"Ratcliffe, N.M., Kunk, M.J., Burton, W.C., and Walsh, G.J., 2011, Traverse of the major fault systems of the Taconian deformational front, the Vermont Valley and core of the Green Mountain massif, southern Vermont, <i>in</i> Guidebook for field trips in Vermont and adjacent New York, v. 103, Middlebury, VT, Sep 30-Oct 2, 2011, p. A3-1-A3-35.","productDescription":"35 p.","startPage":"A3-1","endPage":"A3-35","costCenters":[{"id":243,"text":"Eastern Geology and Paleoclimate Science Center","active":true,"usgs":true},{"id":40020,"text":"Florence Bascom Geoscience Center","active":true,"usgs":true}],"links":[{"id":415167,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Vermont","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -72.34635266089448,\n              43.852053468058216\n            ],\n            [\n              -73.27663927311744,\n              43.852053468058216\n            ],\n            [\n              -73.27663927311744,\n              42.73631457537158\n            ],\n            [\n              -72.34635266089448,\n              42.73631457537158\n            ],\n            [\n              -72.34635266089448,\n              43.852053468058216\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","volume":"103","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Ratcliffe, Nicholas M. 0000-0002-7922-5784 nratclif@usgs.gov","orcid":"https://orcid.org/0000-0002-7922-5784","contributorId":4167,"corporation":false,"usgs":true,"family":"Ratcliffe","given":"Nicholas","email":"nratclif@usgs.gov","middleInitial":"M.","affiliations":[],"preferred":true,"id":868572,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Kunk, Michael J. 0000-0003-4424-7825 mkunk@usgs.gov","orcid":"https://orcid.org/0000-0003-4424-7825","contributorId":200968,"corporation":false,"usgs":true,"family":"Kunk","given":"Michael","email":"mkunk@usgs.gov","middleInitial":"J.","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":868573,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Burton, William C. 0000-0001-7519-5787 bburton@usgs.gov","orcid":"https://orcid.org/0000-0001-7519-5787","contributorId":1293,"corporation":false,"usgs":true,"family":"Burton","given":"William","email":"bburton@usgs.gov","middleInitial":"C.","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":868574,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Walsh, Gregory J. 0000-0003-4264-8836 gwalsh@usgs.gov","orcid":"https://orcid.org/0000-0003-4264-8836","contributorId":873,"corporation":false,"usgs":true,"family":"Walsh","given":"Gregory","email":"gwalsh@usgs.gov","middleInitial":"J.","affiliations":[{"id":40020,"text":"Florence Bascom Geoscience Center","active":true,"usgs":true}],"preferred":true,"id":868575,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70192431,"text":"70192431 - 2011 - Introduction","interactions":[],"lastModifiedDate":"2018-02-15T14:45:15","indexId":"70192431","displayToPublicDate":"2011-12-31T00:00:00","publicationYear":"2011","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2832,"text":"Natural Resources Research","onlineIssn":"1573-8981","printIssn":"1520-7439","active":true,"publicationSubtype":{"id":10}},"title":"Introduction","docAbstract":"<p>The Energy Minerals Division (EMD) of the American Association of Petroleum Geologists (AAPG) is a membership-based, technical interest group having the primary goal of advancing the science of geology, especially as it relates to exploration, discovery, and production of unconventional energy resources. Current research on unconventional energy resources is rapidly changing and exploration and development efforts for these resources are constantly expanding. Nine summaries derived from 2011 committee reports presented at the EMD Annual Meeting in Houston, Texas in April, 2011, are contained in this review. The complete set of committee reports is available to AAPG members at http://emd.aapg.org/members_only/ annual2011/index.cfm. This report updates the 2006 and 2009 EMD unconventional energy review published in this journal (American Association of Petroleum Geologists, Energy Minerals Division 2007, 2009). </p>","language":"English","publisher":"springer","doi":"10.1007/s11053-011-9157-x","usgsCitation":"Warwick, P.D., 2011, Introduction: Natural Resources Research, v. 20, no. 4, p. 279-280, https://doi.org/10.1007/s11053-011-9157-x.","productDescription":"1 p.","startPage":"279","endPage":"280","ipdsId":"IP-029172","costCenters":[{"id":241,"text":"Eastern Energy Resources Science Center","active":true,"usgs":true}],"links":[{"id":348886,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","volume":"20","issue":"4","publicComments":"This publication is a section in a larger report, <i>Unconventional Energy Resources: 2011 Review</i>, which occupies pages 279-328 of volume 20, issue 4 of <i>Natural Resources Research</i> journal.","publishingServiceCenter":{"id":9,"text":"Reston PSC"},"noUsgsAuthors":false,"publicationDate":"2011-11-09","publicationStatus":"PW","scienceBaseUri":"5a6107a3e4b06e28e9c255e0","contributors":{"authors":[{"text":"Warwick, Peter D. 0000-0002-3152-7783 pwarwick@usgs.gov","orcid":"https://orcid.org/0000-0002-3152-7783","contributorId":762,"corporation":false,"usgs":true,"family":"Warwick","given":"Peter","email":"pwarwick@usgs.gov","middleInitial":"D.","affiliations":[{"id":241,"text":"Eastern Energy Resources Science Center","active":true,"usgs":true}],"preferred":false,"id":715799,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70174126,"text":"70174126 - 2011 - Managing white-tailed deer: Eastern North America","interactions":[],"lastModifiedDate":"2021-04-20T15:01:46.14178","indexId":"70174126","displayToPublicDate":"2011-12-31T00:00:00","publicationYear":"2011","noYear":false,"publicationType":{"id":5,"text":"Book chapter"},"publicationSubtype":{"id":24,"text":"Book Chapter"},"chapter":"16","title":"Managing white-tailed deer: Eastern North America","docAbstract":"<p><span>The ability of the white-tailed deer to adapt to and thrive in a wide variety of habitats requires different approaches to managing this species. Variation in both the population dynamics of the species and in the social and political factors that inuence how humans value white-tailed deer also necessitate different approaches. Consequently, providing an overview of the management of white-tailed deer in eastern North America runs the gamut from a species limited by snow depths in the remote boreal forests of Canada to a species inhabiting metropolitan areas. In this chapter, we address issues that inuence deer management among ecoregions that have similar deer population characteristics and related management concerns.</span></p>","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Biology and management of white-tailed deer","largerWorkSubtype":{"id":15,"text":"Monograph"},"language":"English","publisher":"Taylor & Francis","usgsCitation":"Diefenbach, D.R., and Shea, S.M., 2011, Managing white-tailed deer: Eastern North America, chap. 16 <i>of</i> Biology and management of white-tailed deer, p. 481-500.","productDescription":"20 p,","startPage":"481","endPage":"500","ipdsId":"IP-024298","costCenters":[{"id":199,"text":"Coop Res Unit Leetown","active":true,"usgs":true}],"links":[{"id":385222,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"Canada, United States","otherGeospatial":"Eastern North America","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -79.8046875,\n              26.115985925333536\n            ],\n            [\n              -81.2109375,\n              30.751277776257812\n            ],\n            [\n              -73.47656249999999,\n              36.31512514748051\n            ],\n            [\n              -51.67968749999999,\n              48.69096039092549\n            ],\n            [\n              -62.57812500000001,\n              60.413852350464914\n            ],\n            [\n              -80.15625,\n              63.074865690586634\n            ],\n            [\n              -81.9140625,\n              53.54030739150022\n            ],\n            [\n              -88.59374999999999,\n              46.800059446787316\n            ],\n            [\n              -90.3515625,\n              30.751277776257812\n            ],\n            [\n              -82.6171875,\n              28.304380682962783\n            ],\n            [\n              -81.73828125,\n              25.878994400196202\n            ],\n            [\n              -80.595703125,\n              24.607069137709683\n            ],\n            [\n              -79.8046875,\n              26.115985925333536\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","publishingServiceCenter":{"id":9,"text":"Reston PSC"},"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5853ba44e4b0e2663625f2cc","contributors":{"authors":[{"text":"Diefenbach, Duane R. 0000-0001-5111-1147 drd11@usgs.gov","orcid":"https://orcid.org/0000-0001-5111-1147","contributorId":5235,"corporation":false,"usgs":true,"family":"Diefenbach","given":"Duane","email":"drd11@usgs.gov","middleInitial":"R.","affiliations":[{"id":199,"text":"Coop Res Unit Leetown","active":true,"usgs":true}],"preferred":true,"id":640969,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Shea, Stephen M.","contributorId":257543,"corporation":false,"usgs":false,"family":"Shea","given":"Stephen","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":655995,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70006368,"text":"ofr20111308 - 2011 - Postwildfire preliminary debris flow hazard assessment for the area burned by the 2011 Las Conchas Fire in north-central New Mexico","interactions":[],"lastModifiedDate":"2012-03-08T17:16:43","indexId":"ofr20111308","displayToPublicDate":"2011-12-30T14:32:00","publicationYear":"2011","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":"2011-1308","title":"Postwildfire preliminary debris flow hazard assessment for the area burned by the 2011 Las Conchas Fire in north-central New Mexico","docAbstract":"<p>The Las Conchas Fire during the summer of 2011 was the largest in recorded history for the state of New Mexico, burning 634 square kilometers in the Jemez Mountains of north-central New Mexico. The burned landscape is now at risk of damage from postwildfire erosion, such as that caused by debris flows and flash floods. This report presents a preliminary hazard assessment of the debris-flow potential from 321 basins burned by the Las Conchas Fire. A pair of empirical hazard-assessment models developed using data from recently burned basins throughout the intermountain western United States was used to estimate the probability of debris-flow occurrence and volume of debris flows at the outlets of selected drainage basins within the burned area. The models incorporate measures of burn severity, topography, soils, and storm rainfall to estimate the probability and volume of debris flows following the fire.</p> <p>In response to a design storm of 28.0 millimeters of rain in 30 minutes (10-year recurrence interval), the probabilities of debris flows estimated for basins burned by the Las Conchas Fire were greater than 80 percent for two-thirds (67 percent) of the modeled basins. Basins with a high (greater than 80 percent) probability of debris-flow occurrence were concentrated in tributaries to Santa Clara and Rio del Oso Canyons in the northeastern part of the burned area; some steep areas in the Valles Caldera National Preserve, Los Alamos, and Guaje Canyons in the east-central part of the burned area; tributaries to Peralta, Colle, Bland, and Cochiti canyons in the southwestern part of the burned area; and tributaries to Frijoles, Alamo, and Capulin Canyons in the southeastern part of the burned area (within Bandelier National Monument). Estimated debris-flow volumes ranged from 400 cubic meters to greater than 72,000 cubic meters. The largest volumes (greater than 40,000 cubic meters) were estimated for basins in Santa Clara, Los Alamos, and Water Canyons, and for two basins at the northeast edge of the burned area tributary to Rio del Oso and Vallecitos Creek.</p> <p>The Combined Relative Debris-Flow Hazard Rankings identify the areas of highest probability of the largest debris flows. Basins with high Combined Relative Debris-Flow Hazard Rankings include upper Santa Clara Canyon in the northern section of the burn scar, and portions of Peralta, Colle, Bland, Cochiti, Capulin, Alamo, and Frijoles Canyons in the southern section of the burn scar. Three basins with high Combined Relative Debris-Flow Hazard Rankings also occur in areas upstream from the city of Los Alamos&mdash;the city is home to and surrounded by numerous technical sites for the Los Alamos National Laboratory.</p> <p>Potential debris flows in the burned area could affect the water supply for Santa Clara Pueblo and several recreational lakes, as well as recreational and archeological resources in Bandelier National Monument. Debris flows could damage bridges and culverts along State Highway 501 and other roadways. Additional assessment is necessary to determine if the estimated volume of material is sufficient to travel into areas downstream from the modeled basins along the valley floors, where they could affect human life, property, agriculture, and infrastructure in those areas. Additionally, further investigation is needed to assess the potential for debris flows to affect structures at or downstream from basin outlets and to increase the threat of flooding downstream by damaging or blocking flood mitigation structures. The maps presented here may be used to prioritize areas where erosion mitigation or other protective measures may be necessary within a 2- to 3-year window of vulnerability following the Las Conchas Fire.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr20111308","usgsCitation":"Tillery, A.C., Darr, M.J., Cannon, S.H., and Michael, J.A., 2011, Postwildfire preliminary debris flow hazard assessment for the area burned by the 2011 Las Conchas Fire in north-central New Mexico: U.S. Geological Survey Open-File Report 2011-1308, v, 11 p.; 3 Plates - Plate 1: 20.35 x 32.35 inches, Plate 2: 20.21 x 32.41 inches, Plate 3: 20.41 x 32.41 inches, https://doi.org/10.3133/ofr20111308.","productDescription":"v, 11 p.; 3 Plates - Plate 1: 20.35 x 32.35 inches, Plate 2: 20.21 x 32.41 inches, Plate 3: 20.41 x 32.41 inches","onlineOnly":"Y","temporalStart":"2011-06-01","temporalEnd":"2011-08-31","costCenters":[{"id":472,"text":"New Mexico Water Science Center","active":true,"usgs":true}],"links":[{"id":116198,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ofr_2011_1308.png"},{"id":112410,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2011/1308/","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"New Mexico","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -106.61749999999999,35.6 ], [ -106.61749999999999,36.08416666666667 ], [ -106.25083333333333,36.08416666666667 ], [ -106.25083333333333,35.6 ], [ -106.61749999999999,35.6 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a7ea0e4b0c8380cd7a65e","contributors":{"authors":[{"text":"Tillery, Anne C. 0000-0002-9508-7908 atillery@usgs.gov","orcid":"https://orcid.org/0000-0002-9508-7908","contributorId":2549,"corporation":false,"usgs":true,"family":"Tillery","given":"Anne","email":"atillery@usgs.gov","middleInitial":"C.","affiliations":[{"id":472,"text":"New Mexico Water Science Center","active":true,"usgs":true}],"preferred":true,"id":354396,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Darr, Michael J. mjdarr@usgs.gov","contributorId":4239,"corporation":false,"usgs":true,"family":"Darr","given":"Michael","email":"mjdarr@usgs.gov","middleInitial":"J.","affiliations":[],"preferred":true,"id":354397,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Cannon, Susan H. cannon@usgs.gov","contributorId":1019,"corporation":false,"usgs":true,"family":"Cannon","given":"Susan","email":"cannon@usgs.gov","middleInitial":"H.","affiliations":[{"id":300,"text":"Geologic Hazards Science Center","active":true,"usgs":true}],"preferred":true,"id":354394,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Michael, John A. jmichael@usgs.gov","contributorId":1877,"corporation":false,"usgs":true,"family":"Michael","given":"John","email":"jmichael@usgs.gov","middleInitial":"A.","affiliations":[{"id":218,"text":"Denver Federal Center","active":false,"usgs":true}],"preferred":false,"id":354395,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
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