{"pageNumber":"2147","pageRowStart":"53650","pageSize":"25","recordCount":184617,"records":[{"id":86161,"text":"ofr20071225 - 2008 - Digital data for volcano hazards at Newberry Volcano, Oregon","interactions":[],"lastModifiedDate":"2019-04-03T16:31:29","indexId":"ofr20071225","displayToPublicDate":"2008-09-07T00:00:00","publicationYear":"2008","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":"2007-1225","title":"Digital data for volcano hazards at Newberry Volcano, Oregon","docAbstract":"Newberry volcano is a broad shield volcano located in central Oregon, the product of thousands of eruptions, beginning about 600,000 years ago. At least 25 vents on the flanks and summit have been active during the past 10,000 years. The most recent eruption 1,300 years ago produced the Big Obsidian Flow. Thus, the volcano's long history and recent activity indicate that Newberry will erupt in the future. Newberry Crater, a volcanic depression or caldera has been the focus of Newberry's volcanic activity for at least the past 10,000 years. Newberry National Volcanic Monument, which is managed by the U.S. Forest Service, includes the caldera and extends to the Deschutes River. Newberry volcano is quiet. Local earthquake activity (seismicity) has been trifling throughout historic time. Subterranean heat is still present, as indicated by hot springs in the caldera and high temperatures encountered during exploratory drilling for geothermal energy.\r\n\r\nThe report USGS Open-File Report 97-513 (Sherrod and others, 1997) describes the kinds of hazardous geologic events that might occur in the future at Newberry volcano. A hazard-zonation map is included to show the areas that will most likely be affected by renewed eruptions. When Newberry volcano becomes restless, the eruptive scenarios described herein can inform planners, emergency response personnel, and citizens about the kinds and sizes of events to expect. \r\n\r\nThe geographic information system (GIS) volcano hazard data layers used to produce the Newberry volcano hazard map in USGS Open-File Report 97-513 are included in this data set. Scientists at the USGS Cascades Volcano Observatory created a GIS data layer to depict zones subject to the effects of an explosive pyroclastic eruption (tephra fallout, pyroclastic flows, and ballistics), lava flows, volcanic gasses, and lahars/floods in Paulina Creek. A separate GIS data layer depicts drill holes on the flanks of Newberry Volcano that were used to estimate the probability of coverage by future lava flows.","language":"ENGLISH","publisher":"Geological Survey (U.S.)","doi":"10.3133/ofr20071225","usgsCitation":"Schilling, S., Doelger, S., Sherrod, D.R., Mastin, L., and Scott, W.E., 2008, Digital data for volcano hazards at Newberry Volcano, Oregon (Version 1.0): U.S. Geological Survey Open-File Report 2007-1225, Available online only, https://doi.org/10.3133/ofr20071225.","productDescription":"Available online only","onlineOnly":"Y","additionalOnlineFiles":"Y","costCenters":[{"id":615,"text":"Volcano Hazards Program","active":true,"usgs":true}],"links":[{"id":195293,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":11726,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2007/1225/","linkFileType":{"id":5,"text":"html"}}],"edition":"Version 1.0","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a9ae4b07f02db65d661","contributors":{"authors":[{"text":"Schilling, S. P.","contributorId":42606,"corporation":false,"usgs":true,"family":"Schilling","given":"S. P.","affiliations":[],"preferred":false,"id":297009,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Doelger, S.","contributorId":14901,"corporation":false,"usgs":true,"family":"Doelger","given":"S.","email":"","affiliations":[],"preferred":false,"id":297007,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Sherrod, D. R.","contributorId":44559,"corporation":false,"usgs":true,"family":"Sherrod","given":"D.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":297010,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Mastin, L.G.","contributorId":80313,"corporation":false,"usgs":true,"family":"Mastin","given":"L.G.","email":"","affiliations":[],"preferred":false,"id":297011,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Scott, W. E.","contributorId":22773,"corporation":false,"usgs":true,"family":"Scott","given":"W.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":297008,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":70205221,"text":"70205221 - 2008 - Groundwater: Pumping and land subsidence","interactions":[],"lastModifiedDate":"2020-10-23T12:11:43.430837","indexId":"70205221","displayToPublicDate":"2008-09-06T16:09:53","publicationYear":"2008","noYear":false,"publicationType":{"id":5,"text":"Book chapter"},"publicationSubtype":{"id":24,"text":"Book Chapter"},"title":"Groundwater: Pumping and land subsidence","docAbstract":"<p>No abstract available.</p>","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Encyclopedia of Water Science","largerWorkSubtype":{"id":15,"text":"Monograph"},"language":"English","publisher":"Taylor and Francis","usgsCitation":"Phillips, S.P., and Galloway, D.L., 2008, Groundwater: Pumping and land subsidence, chap. <i>of</i> Encyclopedia of Water Science, p. 466-470.","productDescription":"5 p.","startPage":"466","endPage":"470","numberOfPages":"5","costCenters":[{"id":154,"text":"California Water Science Center","active":true,"usgs":true},{"id":35860,"text":"Ohio-Kentucky-Indiana Water Science Center","active":true,"usgs":true}],"links":[{"id":367268,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":379665,"rank":2,"type":{"id":15,"text":"Index Page"},"url":"https://app.knovel.com/web/toc.v/cid:kpEWSVE007"}],"edition":"2","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"editors":[{"text":"Trimble, S.W.","contributorId":55492,"corporation":false,"usgs":true,"family":"Trimble","given":"S.W.","email":"","affiliations":[],"preferred":false,"id":770428,"contributorType":{"id":2,"text":"Editors"},"rank":1},{"text":"Stewart, B.A.","contributorId":207054,"corporation":false,"usgs":false,"family":"Stewart","given":"B.A.","affiliations":[{"id":37441,"text":"Northwest Indian Fisheries Commission, 6370 Martin Way E., Olympia, WA 98670","active":true,"usgs":false}],"preferred":false,"id":770429,"contributorType":{"id":2,"text":"Editors"},"rank":2},{"text":"Howell, T.A.","contributorId":199092,"corporation":false,"usgs":false,"family":"Howell","given":"T.A.","email":"","affiliations":[],"preferred":false,"id":770430,"contributorType":{"id":2,"text":"Editors"},"rank":3}],"authors":[{"text":"Phillips, Steven P. 0000-0002-5107-868X sphillip@usgs.gov","orcid":"https://orcid.org/0000-0002-5107-868X","contributorId":1506,"corporation":false,"usgs":true,"family":"Phillips","given":"Steven","email":"sphillip@usgs.gov","middleInitial":"P.","affiliations":[{"id":154,"text":"California Water Science Center","active":true,"usgs":true}],"preferred":true,"id":770425,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Galloway, Devin L. 0000-0003-0904-5355 dlgallow@usgs.gov","orcid":"https://orcid.org/0000-0003-0904-5355","contributorId":679,"corporation":false,"usgs":true,"family":"Galloway","given":"Devin","email":"dlgallow@usgs.gov","middleInitial":"L.","affiliations":[{"id":509,"text":"Office of the Associate Director for Water","active":true,"usgs":true},{"id":5058,"text":"Office of the Chief Scientist for Water","active":true,"usgs":true},{"id":5078,"text":"Southwest Regional Director's Office","active":true,"usgs":true},{"id":35860,"text":"Ohio-Kentucky-Indiana Water Science Center","active":true,"usgs":true},{"id":37277,"text":"WMA - Earth System Processes Division","active":true,"usgs":true}],"preferred":true,"id":770426,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":86147,"text":"mineral2008 - 2008 - Mineral Commodity Summaries 2008","interactions":[],"lastModifiedDate":"2013-02-04T10:57:50","indexId":"mineral2008","displayToPublicDate":"2008-09-04T00:00:00","publicationYear":"2008","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":323,"text":"Mineral Commodity Summaries","code":"MCS","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2008","title":"Mineral Commodity Summaries 2008","docAbstract":"Each chapter of the 2008 edition of the U.S. Geological Survey (USGS) Mineral Commodity Summaries (MCS) includes information on events, trends, and issues for each mineral commodity as well as discussions and tabular presentations on domestic industry structure, Government programs, tariffs, 5-year salient statistics, and world production and resources. The MCS is the earliest comprehensive source of 2007 mineral production data for the world. More than 90 individual minerals and materials are covered by two-page synopses.\n\nNational reserves and reserve base information for most mineral commodities found in this report, including those for the United States, are derived from a variety of sources. The ideal source of such information would be comprehensive evaluations that apply the same criteria to deposits in different geographic areas and report the results by country. In the absence of such evaluations, national reserves and reserve base estimates compiled by countries for selected mineral commodities are a primary source of national reserves and reserve base information. Lacking national assessment information by governments, sources such as academic articles, company reports, common business practice, presentations by company representatives, and trade journal articles, or a combination of these, serve as the basis for national reserves and reserve base information reported in the mineral commodity sections of this publication.\n\nA national estimate may be assembled from the following: historically reported reserves and reserve base information carried for years without alteration because no new information is available; historically reported reserves and reserve base reduced by the amount of historical production; and company reported reserves. International minerals availability studies conducted by the U.S. Bureau of Mines, before 1996, and estimates of identified resources by an international collaborative effort (the International Strategic Minerals Inventory) are the basis for some reserves and reserve base estimates.\n\nThe USGS collects information about the quantity and quality of mineral resources but does not directly measure reserves, and companies or governments do not directly report reserves or reserve base to the USGS.\n\nReassessment of reserves and reserve base is a continuing process and the intensity of this process differs for mineral commodities, countries, and time period.\n\nAbbreviations and units of measure, and definitions of selected terms used in the report, are in Appendix A and Appendix B, respectively. A resource/reserve classification for minerals, based on USGS Circular 831 (published with the U.S. Bureau of Mines) is Appendix C, and a directory of USGS minerals information country specialists and their responsibilities is Appendix D.\n\nThe USGS continually strives to improve the value of its publications to users. Constructive comments and suggestions by readers of the MCS 2008 are welcomed.","language":"ENGLISH","publisher":"U.S. Geological Survey","doi":"10.3133/mineral2008","isbn":"9781411320765","usgsCitation":"Mineral Commodity Summaries 2008; 2008; MINERAL; 2008; U.S. Geological Survey","productDescription":"202 p; 4 Appendixes (6 p.); Individual Commodity Data Sheets; Available Online, Printed, and on CD-ROM","additionalOnlineFiles":"Y","costCenters":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"links":[{"id":195530,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/mineral_2008.jpg"},{"id":11712,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://minerals.usgs.gov/minerals/pubs/mcs/","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a61e4b07f02db635765","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":534978,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":86145,"text":"sim2978 - 2008 - Regional Stratigraphy and Petroleum Systems of the Michigan Basin, North America","interactions":[],"lastModifiedDate":"2012-02-10T00:11:42","indexId":"sim2978","displayToPublicDate":"2008-09-03T00:00:00","publicationYear":"2008","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":333,"text":"Scientific Investigations Map","code":"SIM","onlineIssn":"2329-132X","printIssn":"2329-1311","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2978","title":"Regional Stratigraphy and Petroleum Systems of the Michigan Basin, North America","docAbstract":"Although more than 100 years of research have gone into deciphering the stratigraphy of the Michigan basin of North America, it remains a challenge to visualize the basin stratigraphy on a regional scale and to describe stratigraphic relations within the basin. Similar difficulties exist for visualizing and describing the regional distribution of petroleum source rocks and reservoir rocks. This publication addresses these difficulties by combining data on Paleozoic and Mesozoic stratigraphy and petroleum geology of the Michigan basin. The areal extent of this structural basin is presented along with data in eight schematic chronostratigraphic sections arranged from north to south, with time denoted in equal increments along the sections. The stratigraphic data are modified from American Association of Petroleum Geologists (AAPG) (1984), Johnson and others (1992), Sanford (1993), and Cross (1998), and the time scale is taken from Harland and others (1990). Informal North American chronostratigraphic terms from AAPG (1984) are shown in parentheses. Stratigraphic sequences as defined by Sloss (1963, 1988) and Wheeler (1963) also are included, as well as the locations of major petroleum source rocks and major petroleum plays. The stratigraphic units are colored according to predominant lithology, in order to emphasize general lithologic patterns and to provide a broad overview of the Michigan basin. For purposes of comparison, schematic depictions of stratigraphy and interpreted events in the Michigan basin and adjacent Appalachian basin are shown. The paper version of this map is available for purchase from the USGS Store.","language":"ENGLISH","publisher":"Geological Survey (U.S.)","doi":"10.3133/sim2978","isbn":"9781411319110","usgsCitation":"Swezey, C., 2008, Regional Stratigraphy and Petroleum Systems of the Michigan Basin, North America: U.S. Geological Survey Scientific Investigations Map 2978, Map Sheet: 51 x 42 inches, https://doi.org/10.3133/sim2978.","productDescription":"Map Sheet: 51 x 42 inches","costCenters":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"links":[{"id":110788,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_84305.htm","linkFileType":{"id":5,"text":"html"},"description":"84305"},{"id":190954,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":11730,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/sim/2978/","linkFileType":{"id":5,"text":"html"}}],"scale":"1","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -94,35 ], [ -94,48 ], [ -72,48 ], [ -72,35 ], [ -94,35 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adbe4b07f02db685bcf","contributors":{"authors":[{"text":"Swezey, Christopher S.","contributorId":52640,"corporation":false,"usgs":true,"family":"Swezey","given":"Christopher S.","affiliations":[],"preferred":false,"id":296941,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70212973,"text":"70212973 - 2008 - Anoxic mineralization: Environmental reality or experimental artifact?","interactions":[],"lastModifiedDate":"2020-09-02T15:29:12.359728","indexId":"70212973","displayToPublicDate":"2008-09-02T10:25:42","publicationYear":"2008","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1866,"text":"Groundwater Monitoring & Remediation","active":true,"publicationSubtype":{"id":10}},"title":"Anoxic mineralization: Environmental reality or experimental artifact?","docAbstract":"<p>No abstract available.&nbsp;</p>","language":"English","publisher":"Wily","doi":"10.1111/j.1745-6592.2007.00186.x","usgsCitation":"Bradley, P.M., Chapelle, F.H., and Loffler, F., 2008, Anoxic mineralization: Environmental reality or experimental artifact?: Groundwater Monitoring & Remediation, v. 28, no. 1, p. 47-49, https://doi.org/10.1111/j.1745-6592.2007.00186.x.","productDescription":"3 p.","startPage":"47","endPage":"49","costCenters":[{"id":559,"text":"South Carolina Water Science Center","active":true,"usgs":true},{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":378106,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"28","issue":"1","noUsgsAuthors":false,"publicationDate":"2008-02-20","publicationStatus":"PW","contributors":{"authors":[{"text":"Bradley, Paul M. 0000-0001-7522-8606 pbradley@usgs.gov","orcid":"https://orcid.org/0000-0001-7522-8606","contributorId":361,"corporation":false,"usgs":true,"family":"Bradley","given":"Paul","email":"pbradley@usgs.gov","middleInitial":"M.","affiliations":[{"id":13634,"text":"South Atlantic Water Science Center","active":true,"usgs":true}],"preferred":true,"id":797863,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Chapelle, Francis H. chapelle@usgs.gov","contributorId":1350,"corporation":false,"usgs":true,"family":"Chapelle","given":"Francis","email":"chapelle@usgs.gov","middleInitial":"H.","affiliations":[{"id":559,"text":"South Carolina Water Science Center","active":true,"usgs":true},{"id":13634,"text":"South Atlantic Water Science Center","active":true,"usgs":true}],"preferred":true,"id":797864,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Loffler, F.E.","contributorId":105882,"corporation":false,"usgs":true,"family":"Loffler","given":"F.E.","email":"","affiliations":[],"preferred":false,"id":797865,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70212972,"text":"70212972 - 2008 - Biodegradation in contaminated aquifers: Incorporating microbial/molecular methods","interactions":[],"lastModifiedDate":"2020-09-09T15:06:53.053014","indexId":"70212972","displayToPublicDate":"2008-09-02T10:13:57","publicationYear":"2008","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3825,"text":"Groundwater","active":true,"publicationSubtype":{"id":10}},"title":"Biodegradation in contaminated aquifers: Incorporating microbial/molecular methods","docAbstract":"<div class=\"abstract-group\"><div class=\"article-section__content en main\"><p>In order to evaluate natural attenuation in contaminated aquifers, there has been a recent recognition that a multidisciplinary approach, incorporating microbial and molecular methods, is required. Observed decreases in contaminant mass and identified footprints of biogeochemical reactions are often used as evidence of intrinsic bioremediation, but characterizing the structure and function of the microbial populations at contaminated sites is needed. In this paper, we review the experimental approaches and microbial methods that are available as tools to evaluate the controls on microbially mediated degradation processes in contaminated aquifers. We discuss the emerging technologies used in biogeochemical studies and present a synthesis of recent studies that serve as models of integrating microbiological approaches with more traditional geochemical and hydrogeologic approaches in order to address important biogeochemical questions about contaminant fate.</p></div></div>","language":"English","publisher":"Wiley","doi":"10.1111/j.1745-6584.2007.00409.x","usgsCitation":"Weiss, J., and Cozzarelli, I.M., 2008, Biodegradation in contaminated aquifers: Incorporating microbial/molecular methods: Groundwater, v. 46, no. 2, p. 305-322, https://doi.org/10.1111/j.1745-6584.2007.00409.x.","productDescription":"18 p.","startPage":"305","endPage":"322","costCenters":[{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true},{"id":37277,"text":"WMA - Earth System Processes Division","active":true,"usgs":true}],"links":[{"id":378105,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"46","issue":"2","noUsgsAuthors":false,"publicationDate":"2008-01-09","publicationStatus":"PW","contributors":{"authors":[{"text":"Weiss, J.","contributorId":193913,"corporation":false,"usgs":false,"family":"Weiss","given":"J.","affiliations":[],"preferred":false,"id":797861,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Cozzarelli, Isabelle M. 0000-0002-5123-1007 icozzare@usgs.gov","orcid":"https://orcid.org/0000-0002-5123-1007","contributorId":1693,"corporation":false,"usgs":true,"family":"Cozzarelli","given":"Isabelle","email":"icozzare@usgs.gov","middleInitial":"M.","affiliations":[{"id":436,"text":"National Research Program - Eastern Branch","active":true,"usgs":true},{"id":49175,"text":"Geology, Energy & Minerals Science Center","active":true,"usgs":true}],"preferred":true,"id":797862,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70212969,"text":"70212969 - 2008 - Mortality of ducklings of the black-bellied whistling duck (Dendrocygna autumnalis) during their premier swim in a hypersaline lake in south Texas","interactions":[],"lastModifiedDate":"2020-09-02T14:52:41.030314","indexId":"70212969","displayToPublicDate":"2008-09-02T09:50:07","publicationYear":"2008","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":5991,"text":"The Southwestern Naturalist","active":true,"publicationSubtype":{"id":10}},"displayTitle":"Mortality of ducklings of the black-bellied whistling duck (<i>Dendrocygna autumnalis</i>) during their premier swim in a Hypersaline Lake in south Texas","title":"Mortality of ducklings of the black-bellied whistling duck (Dendrocygna autumnalis) during their premier swim in a hypersaline lake in south Texas","docAbstract":"<div id=\"divARTICLECONTENTTop\"><div class=\"div0\"><div class=\"row ArticleContentRow\"><p id=\"ID0EF\" class=\"first\">Adult black-bellied whistling ducks (<span class=\"genus-species\">Dendrocygna autumnalis</span>) were observed leaving islands with recently hatched young in a South Texas hypersaline lake during summer 2003. We counted 216 ducklings from 20 broods attempting to make their first swim to the mainland, presumably heading for suitable rearing habitat. Of these, 144 (67%) either died in the water or on the salt-encrusted shoreline within minutes to a few hours of first entering the water. An additional 35 carcasses from unobserved broods were found. Nine carcasses of ducklings were necropsied and they had levels of sodium in the brain above the lethal threshold concentration for sodium poisoning. From our surveillance efforts, we documented a decrease in maximum number of adult black-bellied whistling ducks observed on the islands from 489 in 2002 to 138 in 2003.</p></div></div></div>","language":"English","publisher":"BioOne","doi":"10.1894/0038-4909(2008)53[230:MODOTB]2.0.CO;2","usgsCitation":"Stolley, D.S., Edmonds, S.T., and Meteyer, C.U., 2008, Mortality of ducklings of the black-bellied whistling duck (Dendrocygna autumnalis) during their premier swim in a hypersaline lake in south Texas: The Southwestern Naturalist, v. 53, no. 2, p. 230-235, https://doi.org/10.1894/0038-4909(2008)53[230:MODOTB]2.0.CO;2.","productDescription":"6 p.","startPage":"230","endPage":"235","costCenters":[{"id":456,"text":"National Wildlife Health Center","active":true,"usgs":true},{"id":34983,"text":"Contaminant Biology Program","active":true,"usgs":true}],"links":[{"id":378101,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","otherGeospatial":"South Texas","volume":"53","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Stolley, D. S.","contributorId":79449,"corporation":false,"usgs":true,"family":"Stolley","given":"D.","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":797852,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Edmonds, Samuel T.","contributorId":139995,"corporation":false,"usgs":false,"family":"Edmonds","given":"Samuel","email":"","middleInitial":"T.","affiliations":[{"id":6928,"text":"BioDiversity Research Institute, Gorham, ME 04038","active":true,"usgs":false}],"preferred":false,"id":797853,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Meteyer, Carol U. 0000-0002-4007-3410 cmeteyer@usgs.gov","orcid":"https://orcid.org/0000-0002-4007-3410","contributorId":127748,"corporation":false,"usgs":true,"family":"Meteyer","given":"Carol","email":"cmeteyer@usgs.gov","middleInitial":"U.","affiliations":[{"id":456,"text":"National Wildlife Health Center","active":true,"usgs":true},{"id":34983,"text":"Contaminant Biology Program","active":true,"usgs":true},{"id":5056,"text":"Office of the AD Energy and Minerals, and Environmental Health","active":true,"usgs":true}],"preferred":true,"id":797854,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70000158,"text":"70000158 - 2008 - Riparian vegetation dynamics and evapotranspiration in the riparian corridor in the delta of the Colorado River, Mexico","interactions":[],"lastModifiedDate":"2025-12-23T15:36:52.940089","indexId":"70000158","displayToPublicDate":"2008-09-01T23:09:22","publicationYear":"2008","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2258,"text":"Journal of Environmental Management","active":true,"publicationSubtype":{"id":10}},"title":"Riparian vegetation dynamics and evapotranspiration in the riparian corridor in the delta of the Colorado River, Mexico","docAbstract":"<p><span>Like other great desert rivers, the Colorado River in the United States and Mexico is highly regulated to provide water for human use. No water is officially allotted to support the natural ecosystems in the delta of the river in Mexico. However, precipitation is inherently variable in this watershed, and from 1981–2004, 15% of the mean annual flow of the Lower Colorado River has entered the riparian corridor below the last diversion point for water in Mexico. These flows include flood releases from US dams and much smaller administrative spills released back to the river from irrigators in the US and Mexico. These flows have germinated new cohorts of native cottonwood and willow trees and have established an active aquatic ecosystem in the riparian corridor in Mexico. We used ground and remote-sensing methods to determine the composition and fractional cover of the vegetation in the riparian corridor, its annual water consumption, and the sources of water that support the ecosystem. The study covered the period 2000–2004, a flood year followed by 4 dry years. The riparian corridor occupies 30,000</span><span>&nbsp;</span><span>ha between flood control levees in Mexico. Annual evapotranspiration (ET), estimated by Moderate Resolution Imaging Spectrometer (MODIS) satellite imagery calibrated against moisture flux tower data, was about 1.1</span><span>&nbsp;</span><span>m</span><span>&nbsp;</span><span>yr</span><sup>−1</sup><span>&nbsp;and was fairly constant throughout the study period despite a paucity of surface flows 2001–2004. Total ET averaged 3.4×10</span><sup>8</sup><span>&nbsp;</span><span>m</span><sup>3</sup><span>&nbsp;</span><span>yr</span><sup>−1</sup><span>, about 15% of Colorado River water entering Mexico from the US Surface flows could have played only a small part in supporting these high ET losses. We conclude that the riparian ET is supported mainly by the shallow regional aquifer, derived from agricultural return flows, that approaches the surface in the riparian zone. Nevertheless, surface flows are important in germinating cohorts of native trees, in washing salts from the soil and aquifer, and in providing aquatic habitat, thereby enriching the habitat value of the riparian corridor for birds and other wildlife. Conservation and water management strategies to enhance the delta habitats are discussed in light of the findings.</span></p>","language":"English","publisher":"Elsevier","doi":"10.1016/j.jenvman.2007.04.010","issn":"03014797","usgsCitation":"Nagler, P.L., Glenn, E., Hinojosa-Huerta, O., Zamora, F., and Howard, K.A., 2008, Riparian vegetation dynamics and evapotranspiration in the riparian corridor in the delta of the Colorado River, Mexico: Journal of Environmental Management, v. 88, no. 4, p. 864-874, https://doi.org/10.1016/j.jenvman.2007.04.010.","productDescription":"11 p.","startPage":"864","endPage":"874","costCenters":[{"id":568,"text":"Southwest Biological Science Center","active":true,"usgs":true},{"id":35995,"text":"Geology, Geophysics, and Geochemistry Science Center","active":true,"usgs":true}],"links":[{"id":203726,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"88","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adbe4b07f02db685b0b","contributors":{"authors":[{"text":"Nagler, Pamela L. 0000-0003-0674-103X pnagler@usgs.gov","orcid":"https://orcid.org/0000-0003-0674-103X","contributorId":1398,"corporation":false,"usgs":true,"family":"Nagler","given":"Pamela","email":"pnagler@usgs.gov","middleInitial":"L.","affiliations":[{"id":568,"text":"Southwest Biological Science Center","active":true,"usgs":true}],"preferred":true,"id":344994,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Glenn, Edward P.","contributorId":56542,"corporation":false,"usgs":false,"family":"Glenn","given":"Edward P.","affiliations":[{"id":13060,"text":"Department of Soil, Water and Environmental Science, University of Arizona","active":true,"usgs":false}],"preferred":false,"id":344992,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Hinojosa-Huerta, Osvel","contributorId":167198,"corporation":false,"usgs":false,"family":"Hinojosa-Huerta","given":"Osvel","affiliations":[{"id":24640,"text":"Pronatura Noroeste","active":true,"usgs":false}],"preferred":false,"id":344996,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Zamora, Francisco","contributorId":80396,"corporation":false,"usgs":true,"family":"Zamora","given":"Francisco","email":"","affiliations":[],"preferred":false,"id":344995,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Howard, Keith A. 0000-0002-6462-2947 khoward@usgs.gov","orcid":"https://orcid.org/0000-0002-6462-2947","contributorId":3439,"corporation":false,"usgs":true,"family":"Howard","given":"Keith","email":"khoward@usgs.gov","middleInitial":"A.","affiliations":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"preferred":true,"id":344993,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":70199774,"text":"70199774 - 2008 - Primary production and carrying capacity of former salt ponds after reconnection to San Francisco Bay","interactions":[],"lastModifiedDate":"2018-10-17T10:58:24","indexId":"70199774","displayToPublicDate":"2008-09-01T15:01:42","publicationYear":"2008","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3750,"text":"Wetlands","onlineIssn":"1943-6246","printIssn":"0277-5212","active":true,"publicationSubtype":{"id":10}},"title":"Primary production and carrying capacity of former salt ponds after reconnection to San Francisco Bay","docAbstract":"<p><span>Over 6,110 ha of the commercial production salt ponds surrounding South San Francisco Bay, CA, have been decommissioned and reconnected to the bay, most as part of the largest wetlands restoration program in the western United States. These open water ponds are critical habitat for millions of birds annually and restoration program managers must determine the appropriate balance between retention of ponds versus re-conversion to tidal salt marsh, knowing that both are essential ecosystems for endangered bird species. Our study describes the ecological value of the new open water pond ecosystems as feeding habitats for birds. We used the oxygen rate of change method to determine ecosystem metabolic parameters from high resolution time-series of dissolved oxygen concentration. Areal gross primary production (8.17 g O</span><sub>2</sub><span>&nbsp;m</span><sup>−2</sup><span>&nbsp;d</span><sup>−1</sup><span>) was roughly double the world’s most productive estuaries. High rates of phytoplankton photosynthesis were balanced by equally high rates of community respiration (8.25 g O</span><sub>2</sub><span>m</span><sup>−2</sup><span>&nbsp;d</span><sup>−1</sup><span>). Metabolic equilibrium was delicately poised: sharp irradiance and temperature shifts triggered short term photosynthesis reduction resulting in oxygen depletion. We converted net primary production (NPP) into potential carrying capacity of the forage biota that support targeted pond waterbirds. NPP was processed through both a pelagic food web, resulting in forage biota for piscivorous birds and a benthic food web, resulting in forage biota for shorebirds and diving benthivores. Both food webs included efficient algal-based and inefficient detrital trophic pathways. The result of all primary production being routed through simple food webs was high potential forage production and energy supply to waterbirds, equivalent to 11–163 million planktivorous fish or 19–78 billion small estuarine clams within the 330-ha pond between May and October. Food quantity does not necessarily equal quality and these systems have the potential to produce toxic or inedible algae. Our study provides the first measurement of primary production in the open water ponds of San Francisco Bay and presents a novel approach for transforming primary production into forage production as a metric of an ecosystem’s energetic carrying capacity.</span></p>","language":"English","publisher":"Springer","doi":"10.1672/07-190.1","usgsCitation":"Thebault, J., Schraga, T., Cloern, J.E., and Dunlavey, E.G., 2008, Primary production and carrying capacity of former salt ponds after reconnection to San Francisco Bay: Wetlands, v. 28, no. 3, p. 841-851, https://doi.org/10.1672/07-190.1.","productDescription":"11 p.","startPage":"841","endPage":"851","costCenters":[{"id":154,"text":"California Water Science Center","active":true,"usgs":true},{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":476593,"rank":0,"type":{"id":41,"text":"Open Access External Repository Page"},"url":"https://hal.science/hal-00449352","text":"External Repository"},{"id":357906,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"California","otherGeospatial":"San Francisco Bay","volume":"28","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5c10d26be4b034bf6a7f9729","contributors":{"authors":[{"text":"Thebault, Julien","contributorId":208279,"corporation":false,"usgs":false,"family":"Thebault","given":"Julien","email":"","affiliations":[],"preferred":false,"id":746557,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Schraga, Tara 0000-0002-2108-5846 tschraga@usgs.gov","orcid":"https://orcid.org/0000-0002-2108-5846","contributorId":1118,"corporation":false,"usgs":true,"family":"Schraga","given":"Tara","email":"tschraga@usgs.gov","affiliations":[{"id":37277,"text":"WMA - Earth System Processes Division","active":true,"usgs":true},{"id":438,"text":"National Research Program - Western Branch","active":true,"usgs":true}],"preferred":true,"id":746558,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Cloern, James E. 0000-0002-5880-6862 jecloern@usgs.gov","orcid":"https://orcid.org/0000-0002-5880-6862","contributorId":1488,"corporation":false,"usgs":true,"family":"Cloern","given":"James","email":"jecloern@usgs.gov","middleInitial":"E.","affiliations":[{"id":37277,"text":"WMA - Earth System Processes Division","active":true,"usgs":true},{"id":438,"text":"National Research Program - Western Branch","active":true,"usgs":true}],"preferred":true,"id":746559,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Dunlavey, Eric G.","contributorId":208260,"corporation":false,"usgs":false,"family":"Dunlavey","given":"Eric","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":746560,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70159416,"text":"70159416 - 2008 - Mercury bioaccumulation and effects on birds in San Francisco Bay","interactions":[],"lastModifiedDate":"2015-11-16T15:12:47","indexId":"70159416","displayToPublicDate":"2008-09-01T05:15:00","publicationYear":"2008","noYear":false,"publicationType":{"id":18,"text":"Report"},"title":"Mercury bioaccumulation and effects on birds in San Francisco Bay","docAbstract":"<h1>Highlights</h1>\n<ul>\n<li>San Francisco Bay is an important wintering and breeding ground for more than 1 million waterbirds annually</li>\n<li>Mercury concentrations are highest in birds that eat fish and that reside in the Lower South Bay</li>\n<li>When Forster&rsquo;s terns arrive in the Bay in spring to breed, mercury concentrations in their blood increase by four-fold in a six week period</li>\n<li>Based on mercury concentrations in blood, nearly 60% of all breeding Forster&rsquo;s terns sampled in the Bay are at high risk of toxic effects</li>\n<li>One important piece of evidence of impairment of reproduction in Forster&rsquo;s terns is that average mercury concentrations in failed to-hatch eggs were statistically significantly higher than in randomly selected eggs</li>\n<li>Avian eggs represent an ideal matrix for assessing bioaccumulation because they are indicative of short-term, localized exposure and are central to predicting risk in multiple lifestages</li>\n</ul>","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"The pulse of the estuary: Monitoring and managing water quality in the San Francisco estuary","language":"English","publisher":"San Francisco Estuary Institute","publisherLocation":"Oakland, CA","usgsCitation":"Eagles-Smith, C.A., and Ackerman, J., 2008, Mercury bioaccumulation and effects on birds in San Francisco Bay, 9 p.","productDescription":"9 p.","startPage":"56","endPage":"64","onlineOnly":"N","additionalOnlineFiles":"N","ipdsId":"IP-007591","costCenters":[{"id":651,"text":"Western Ecological Research Center","active":true,"usgs":true}],"links":[{"id":311389,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":311388,"rank":1,"type":{"id":15,"text":"Index Page"},"url":"https://www.sfei.org/documents/pulse-estuary-monitoring-and-managing-water-quality-san-francisco-estuary"}],"country":"United States","state":"California","otherGeospatial":"San Francisco Bay","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -122.25585937500001,\n              37.85316995894978\n            ],\n            [\n              -122.20916748046876,\n              37.801103690609615\n            ],\n            [\n              -122.04986572265624,\n              37.642509774448754\n            ],\n            [\n              -121.904296875,\n 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jackerman@usgs.gov","orcid":"https://orcid.org/0000-0002-3074-8322","contributorId":147078,"corporation":false,"usgs":true,"family":"Ackerman","given":"Joshua T.","email":"jackerman@usgs.gov","affiliations":[{"id":651,"text":"Western Ecological Research Center","active":true,"usgs":true}],"preferred":false,"id":578499,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70176198,"text":"70176198 - 2008 - Reef communities in the Dry Tortugas (Florida, USA): Baseline surveys for the new no-take area","interactions":[],"lastModifiedDate":"2023-12-06T15:41:05.351689","indexId":"70176198","displayToPublicDate":"2008-09-01T00:00:00","publicationYear":"2008","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"Reef communities in the Dry Tortugas (Florida, USA): Baseline surveys for the new no-take area","docAbstract":"<p>To understand the current community structure on reefs in the Dry Tortugas, we conducted specieslevel surveys of macroalgae, coral diversity, herbivorous and game fishes, urchins, and substratum composition (e.g., rugosity) in shallow (3- to 5-m depth) low-relief reef and hardbottom habitats in October 2007. We had particular interest in the ecological process of herbivory inside and outside of the “no-take” Research Natural Area (RNA) designated by the U.S. National Park Service in 2007, and establishing a baseline to assess future changes to trophic functioning. <i>Diadema antillarum</i> and herbivorous fish abundance, percent cover of macroalgae, and species richness of corals and gorgonians at the 18 randomly selected survey sites were not significantly different inside vs. outside of the RNA. Mean densities of <i>D. antillarum</i> ranged from 0.01 to 0.54 individuals m<sup>-2</sup>, with 11 of the 18 sites having densities above 0.10 individuals m<sup>-2</sup>. Both <i>D. antillarum</i> density and coral species richness were positively correlated to rugosity of the substratum. <i>Diadema antillarum</i> density was also positively related to percentage of the substratum composed of <i>Acropora cervicornis</i> rubble. Improved trophic functioning and increases in <i>D. antillarum</i> can improve reef condition in the Dry Tortugas, and the RNA is an important management tool to achieve increases in reef resilience to global-scale stressors.</p>","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"11th International Coral Reef Symposium Proceedings","largerWorkSubtype":{"id":12,"text":"Conference publication"},"conferenceTitle":"11th International Coral Reef Symposium","conferenceDate":"July 7-11, 2008","conferenceLocation":"Fort Lauderdale, FL","language":"English","publisher":"National Coral Reef Institute","usgsCitation":"Kuffner, I., Paul, V.J., Ritson-Williams, R., Hickey, T.D., and Walters, L.J., 2008, Reef communities in the Dry Tortugas (Florida, USA): Baseline surveys for the new no-take area, <i>in</i> 11th International Coral Reef Symposium Proceedings, Fort Lauderdale, FL, July 7-11, 2008, p. 311-315.","productDescription":"5 p.","startPage":"311","endPage":"315","costCenters":[{"id":574,"text":"St. Petersburg Coastal and Marine Science Center","active":true,"usgs":true}],"links":[{"id":328160,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Florida","otherGeospatial":"Dry Tortugas","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -82.87293267880368,\n              24.55321585229916\n            ],\n            [\n              -82.7590919208673,\n              24.637907312883186\n            ],\n            [\n              -82.74989266770086,\n              24.711051251916132\n            ],\n            [\n              -82.82808631961629,\n              24.73716368465955\n            ],\n            [\n              -82.91547922469873,\n              24.720452358950936\n            ],\n            [\n              -82.97757418357308,\n              24.65880995780614\n            ],\n            [\n              -82.97987399686482,\n              24.563674687708854\n            ],\n            [\n              -82.87293267880368,\n              24.55321585229916\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"57c95130e4b0f2f0cec15c02","contributors":{"authors":[{"text":"Kuffner, I. B.","contributorId":40328,"corporation":false,"usgs":true,"family":"Kuffner","given":"I. B.","affiliations":[],"preferred":false,"id":889730,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Paul, V. J.","contributorId":332232,"corporation":false,"usgs":false,"family":"Paul","given":"V.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":889731,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Ritson-Williams, R.","contributorId":88546,"corporation":false,"usgs":true,"family":"Ritson-Williams","given":"R.","affiliations":[],"preferred":false,"id":889732,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Hickey, T. D. tdhickey@usgs.gov","contributorId":2494,"corporation":false,"usgs":true,"family":"Hickey","given":"T.","email":"tdhickey@usgs.gov","middleInitial":"D.","affiliations":[],"preferred":true,"id":889733,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Walters, L. 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,{"id":70179452,"text":"70179452 - 2008 - Survival and migration behavior of juvenile salmonids at Lower Granite Dam, 2006","interactions":[],"lastModifiedDate":"2017-01-03T11:53:42","indexId":"70179452","displayToPublicDate":"2008-09-01T00:00:00","publicationYear":"2008","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":4,"text":"Other Government Series"},"title":"Survival and migration behavior of juvenile salmonids at Lower Granite Dam, 2006","docAbstract":"<p>We described behavior and estimated passage and survival parameters of juvenile salmonids during spring and summer migration periods at Lower Granite Dam in 2006. During the spring, the study was designed to examine the effects of the Behavioral Guidance Structure (BGS) by using a randomized-block BGS Stored / BGS Deployed treatment design. The summer study was designed to compare passage and survival through Lower Granite Dam using a randomized-block design during two spill treatments while the BGS was in the stored position. We used the Route Specific Survival Model to estimate survival and passage probabilities of hatchery yearling Chinook salmon, hatchery juvenile steelhead, and hatchery and wild subyearling Chinook salmon. We also estimated fish guidance efficiency (FGE), fish passage efficiency (FPE), Removable Spillway Weir passage effectiveness (RPE), spill passage effectiveness (SPY), and combined spill and RSW passage effectiveness. </p>","language":"English","publisher":"U.S. Army Corps of Engineers","usgsCitation":"Beeman, J.W., Fielding, S.D., Braatz, A.C., Wilkerson, T.S., Pope, A.C., Walker, C.E., Hardiman, J.M., Perry, R.W., and Counihan, T.D., 2008, Survival and migration behavior of juvenile salmonids at Lower Granite Dam, 2006, xx., 96 p. .","productDescription":"xx., 96 p. ","costCenters":[{"id":654,"text":"Western Fisheries Research Center","active":true,"usgs":true}],"links":[{"id":332742,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Idaho, Oregon,Washington","otherGeospatial":"Clearwater River, Columbia River, Snake River","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -119.37744140625,\n              45.97024259702345\n            ],\n            [\n              -119.091796875,\n              46.042735653846506\n            ],\n            [\n              -119.05883789062501,\n              46.27863122156088\n            ],\n            [\n              -118.52600097656249,\n              46.64189395892872\n            ],\n            [\n          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jbeeman@usgs.gov","contributorId":2646,"corporation":false,"usgs":true,"family":"Beeman","given":"John","email":"jbeeman@usgs.gov","middleInitial":"W.","affiliations":[{"id":654,"text":"Western Fisheries Research Center","active":true,"usgs":true}],"preferred":true,"id":657284,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Fielding, Scott D.","contributorId":41115,"corporation":false,"usgs":true,"family":"Fielding","given":"Scott","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":657285,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Braatz, Amy C.","contributorId":57989,"corporation":false,"usgs":true,"family":"Braatz","given":"Amy","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":657286,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Wilkerson, Tamara S.","contributorId":177853,"corporation":false,"usgs":false,"family":"Wilkerson","given":"Tamara","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":657287,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Pope, Adam C. 0000-0002-7253-2247 apope@usgs.gov","orcid":"https://orcid.org/0000-0002-7253-2247","contributorId":5664,"corporation":false,"usgs":true,"family":"Pope","given":"Adam","email":"apope@usgs.gov","middleInitial":"C.","affiliations":[{"id":654,"text":"Western Fisheries Research Center","active":true,"usgs":true}],"preferred":false,"id":657288,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Walker, Christopher E.","contributorId":65938,"corporation":false,"usgs":true,"family":"Walker","given":"Christopher","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":657289,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Hardiman, Jill M. 0000-0002-3661-9695 jhardiman@usgs.gov","orcid":"https://orcid.org/0000-0002-3661-9695","contributorId":2672,"corporation":false,"usgs":true,"family":"Hardiman","given":"Jill","email":"jhardiman@usgs.gov","middleInitial":"M.","affiliations":[{"id":654,"text":"Western Fisheries Research Center","active":true,"usgs":true}],"preferred":true,"id":657290,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Perry, Russell W. 0000-0003-4110-8619 rperry@usgs.gov","orcid":"https://orcid.org/0000-0003-4110-8619","contributorId":2820,"corporation":false,"usgs":true,"family":"Perry","given":"Russell","email":"rperry@usgs.gov","middleInitial":"W.","affiliations":[{"id":654,"text":"Western Fisheries Research Center","active":true,"usgs":true}],"preferred":true,"id":657291,"contributorType":{"id":1,"text":"Authors"},"rank":8},{"text":"Counihan, Timothy D. 0000-0003-4967-6514 tcounihan@usgs.gov","orcid":"https://orcid.org/0000-0003-4967-6514","contributorId":4211,"corporation":false,"usgs":true,"family":"Counihan","given":"Timothy","email":"tcounihan@usgs.gov","middleInitial":"D.","affiliations":[{"id":654,"text":"Western Fisheries Research Center","active":true,"usgs":true}],"preferred":true,"id":657292,"contributorType":{"id":1,"text":"Authors"},"rank":9}]}}
,{"id":70159349,"text":"70159349 - 2008 - The need for a national LIDAR dataset","interactions":[],"lastModifiedDate":"2017-05-16T16:08:41","indexId":"70159349","displayToPublicDate":"2008-09-01T00:00:00","publicationYear":"2008","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3052,"text":"Photogrammetric Engineering and Remote Sensing","active":true,"publicationSubtype":{"id":10}},"title":"The need for a national LIDAR dataset","docAbstract":"<p>On May 21st and 22nd 2008, the U.S. Geological Survey (USGS), the National Aeronautics and Space Administration (NASA), and the Association of American State Geologists (AASG) hosted the Second National Light Detection and Ranging (Lidar) Initiative Strategy Meeting at USGS Headquarters in Reston, Virginia. The USGS is taking the lead in cooperation with many partners to design and implement a future high-resolution National Lidar Dataset. Initial work is focused on determining viability, developing requirements and specifi cations, establishing what types of information contained in a lidar signal are most important, and identifying key stakeholders and their respective roles. In February 2007, USGS hosted the fi rst National Lidar Initiative Strategy Meeting at USGS Headquarters in Virginia. The presentations and a published summary report from the fi rst meeting can be found on the Center for Lidar Information Coordination and Knowledge (CLICK) Website: http://lidar.cr.usgs.gov. The fi rst meeting demonstrated the public need for consistent lidar data at the national scale. The goals of the second meeting were to further expand on the ideas and information developed in the fi rst meeting, to bring more stakeholders together, to both refi ne and expand on the requirements and capabilities needed, and to discuss an organizational and funding approach for an initiative of this magnitude. The approximately 200 participants represented Federal, State, local, commercial and academic interests. The second meeting included a public solicitation for presentations and posters to better democratize the workshop. All of the oral presentation abstracts that were submitted were accepted, and the 25 poster submissions augmented and expanded upon the oral presentations. The presentations from this second meeting, including audio, can be found on CLICK at http://lidar.cr.usgs.gov/national_lidar_2008.php. Based on the presentations and the discussion sessions, the following points were emphasized throughout the meeting</p>","language":"English","publisher":"ASPRS","usgsCitation":"Stoker, J.M., Harding, D., and Parrish, J., 2008, The need for a national LIDAR dataset: Photogrammetric Engineering and Remote Sensing, v. 74, no. 9, p. 1066-1068.","productDescription":"3 p.","startPage":"1066","endPage":"1068","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":222,"text":"Earth Resources Observation and Science (EROS) Center","active":true,"usgs":true}],"links":[{"id":310496,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":310493,"rank":1,"type":{"id":15,"text":"Index Page"},"url":"https://info.asprs.org/publications/pers/2008journal/september/"}],"volume":"74","issue":"9","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"562a08f6e4b011227bf1fdf1","contributors":{"authors":[{"text":"Stoker, Jason M. 0000-0003-2455-0931 jstoker@usgs.gov","orcid":"https://orcid.org/0000-0003-2455-0931","contributorId":3021,"corporation":false,"usgs":true,"family":"Stoker","given":"Jason","email":"jstoker@usgs.gov","middleInitial":"M.","affiliations":[{"id":223,"text":"Earth Resources Observation and Science (EROS) Center (Geography)","active":false,"usgs":true},{"id":423,"text":"National Geospatial Program","active":true,"usgs":true}],"preferred":true,"id":578120,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Harding, David","contributorId":108018,"corporation":false,"usgs":true,"family":"Harding","given":"David","affiliations":[],"preferred":false,"id":578121,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Parrish, Jay","contributorId":64987,"corporation":false,"usgs":true,"family":"Parrish","given":"Jay","email":"","affiliations":[],"preferred":false,"id":578122,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70179524,"text":"70179524 - 2008 - Reef fishes have higher parasite richness at unfished Palmyra Atoll compared to fished Kiritimati Island","interactions":[],"lastModifiedDate":"2017-01-04T11:33:14","indexId":"70179524","displayToPublicDate":"2008-09-01T00:00:00","publicationYear":"2008","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1443,"text":"EcoHealth","active":true,"publicationSubtype":{"id":10}},"title":"Reef fishes have higher parasite richness at unfished Palmyra Atoll compared to fished Kiritimati Island","docAbstract":"<p><span>We compared parasite communities at two coral atolls in the Line Islands chain of the central Pacific (Kiritimati Island and Palmyra Atoll). Palmyra Atoll is relatively pristine while Kiritimati Island is heavily fished. At each island, we sampled five fish species for helminth and arthropod endoparasites: </span><i class=\"EmphasisTypeItalic \">Chromis margaritifer</i><span>, </span><i class=\"EmphasisTypeItalic \">Plectroglyphidodon dickii,</i><i class=\"EmphasisTypeItalic \">Paracirrhites arcatus</i><span>, </span><i class=\"EmphasisTypeItalic \">Acanthurus nigricans</i><span>, and </span><i class=\"EmphasisTypeItalic \">Lutjanus bohar</i><span>. The surveys found monogeneans, digeneans, cestodes, nematodes, acanthocephalans, and copepods. Parasite richness was higher at Palmyra compared to Kiritimati for all five fish species. Fishes from Palmyra also tended to have more parasites species per host, higher parasite prevalence, and higher parasite abundance than did fishes from Kiritimati. The lower parasitism at Kiritimati may result from a simplified food web due to over fishing. Low biodiversity could impair parasite transmission by reducing the availability of hosts required by parasites with complex life cycles. Most notably, the lower abundances of larval shark tapeworms at Kiritimati presumably reflect the fact that fishing has greatly depleted sharks there in comparison to Palmyra.</span></p>","language":"English","publisher":"Springer","doi":"10.1007/s10393-008-0196-7","usgsCitation":"Lafferty, K.D., Shaw, J., and Kuris, A.M., 2008, Reef fishes have higher parasite richness at unfished Palmyra Atoll compared to fished Kiritimati Island: EcoHealth, v. 5, no. 3, p. 338-345, https://doi.org/10.1007/s10393-008-0196-7.","productDescription":"8 p.","startPage":"338","endPage":"345","costCenters":[{"id":651,"text":"Western Ecological Research Center","active":true,"usgs":true}],"links":[{"id":476594,"rank":0,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1007/s10393-008-0196-7","text":"Publisher Index Page"},{"id":332853,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"5","issue":"3","noUsgsAuthors":false,"publicationDate":"2008-10-10","publicationStatus":"PW","scienceBaseUri":"586e182ee4b0f5ce109fcb13","contributors":{"authors":[{"text":"Lafferty, Kevin D. 0000-0001-7583-4593 klafferty@usgs.gov","orcid":"https://orcid.org/0000-0001-7583-4593","contributorId":1415,"corporation":false,"usgs":true,"family":"Lafferty","given":"Kevin","email":"klafferty@usgs.gov","middleInitial":"D.","affiliations":[{"id":651,"text":"Western Ecological Research Center","active":true,"usgs":true}],"preferred":true,"id":657558,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Shaw, Jenny C.","contributorId":7196,"corporation":false,"usgs":true,"family":"Shaw","given":"Jenny C.","affiliations":[],"preferred":false,"id":657559,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Kuris, Armand M.","contributorId":54332,"corporation":false,"usgs":true,"family":"Kuris","given":"Armand","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":657560,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70198267,"text":"70198267 - 2008 - Magmatically triggered slow slip at Kilauea Volcano, Hawaii","interactions":[],"lastModifiedDate":"2020-06-19T19:47:22.400524","indexId":"70198267","displayToPublicDate":"2008-08-29T00:00:00","publicationYear":"2008","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3338,"text":"Science","active":true,"publicationSubtype":{"id":10}},"title":"Magmatically triggered slow slip at Kilauea Volcano, Hawaii","docAbstract":"<p><span>We demonstrate that a recent dike intrusion probably triggered a slow fault-slip event (SSE) on Kilauea volcano's mobile south flank. Our analysis combined models of Advanced Land Observing Satellite interferometric dike-intrusion displacement maps with continuous Global Positioning System (GPS) displacement vectors to show that deformation nearly identical to four previous SSEs at Kilauea occurred at far-field sites shortly after the intrusion. We model stress changes because of both secular deformation and the intrusion and find that both would increase the Coulomb failure stress on possible SSE slip surfaces by roughly the same amount. These results, in concert with the observation that none of the previous SSEs at Kilauea was directly preceded by intrusions but rather occurred during times of normal background deformation, suggest that both extrinsic (intrusion-triggering) and intrinsic (secular fault creep) fault processes can lead to SSEs.</span></p>","language":"English","publisher":"AAAS","doi":"10.1126/science.1159007","usgsCitation":"Brooks, B.A., Foster, J., Sandwell, D., Wolfe, C.J., Okubo, P.G., Poland, M.P., and Myer, D., 2008, Magmatically triggered slow slip at Kilauea Volcano, Hawaii: Science, v. 321, no. 5893, https://doi.org/10.1126/science.1159007.","productDescription":"1 p.","startPage":"1177","costCenters":[{"id":615,"text":"Volcano Hazards Program","active":true,"usgs":true},{"id":617,"text":"Volcano Science Center","active":true,"usgs":true}],"links":[{"id":361758,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Hawaii","otherGeospatial":"Kilauea Volcano","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -155.5938720703125,\n              18.92187618976372\n            ],\n            [\n              -155.3082275390625,\n              19.160735484156255\n            ],\n            [\n              -154.7479248046875,\n              19.331878440818787\n            ],\n            [\n              -154.7149658203125,\n              19.54943746814108\n            ],\n            [\n              -155.1983642578125,\n              19.564966221479995\n            ],\n            [\n              -155.3631591796875,\n              19.580493479202527\n            ],\n            [\n              -155.6158447265625,\n              19.48730751856426\n            ],\n            [\n              -155.6817626953125,\n              19.088075584093136\n            ],\n            [\n              -155.5938720703125,\n              18.92187618976372\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"321","issue":"5893","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Brooks, Benjamin A. 0000-0001-7954-6281 bbrooks@usgs.gov","orcid":"https://orcid.org/0000-0001-7954-6281","contributorId":5237,"corporation":false,"usgs":true,"family":"Brooks","given":"Benjamin","email":"bbrooks@usgs.gov","middleInitial":"A.","affiliations":[{"id":237,"text":"Earthquake Science Center","active":true,"usgs":true}],"preferred":true,"id":740804,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Foster, James","contributorId":38598,"corporation":false,"usgs":true,"family":"Foster","given":"James","affiliations":[],"preferred":false,"id":740805,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Sandwell, David","contributorId":190237,"corporation":false,"usgs":false,"family":"Sandwell","given":"David","email":"","affiliations":[],"preferred":false,"id":740806,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Wolfe, Cecily J. 0000-0003-3144-5697 cwolfe@usgs.gov","orcid":"https://orcid.org/0000-0003-3144-5697","contributorId":191613,"corporation":false,"usgs":true,"family":"Wolfe","given":"Cecily","email":"cwolfe@usgs.gov","middleInitial":"J.","affiliations":[{"id":234,"text":"Earthquake Hazards Program","active":true,"usgs":true}],"preferred":true,"id":740807,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Okubo, Paul G. 0000-0002-0381-6051 pokubo@usgs.gov","orcid":"https://orcid.org/0000-0002-0381-6051","contributorId":2730,"corporation":false,"usgs":true,"family":"Okubo","given":"Paul","email":"pokubo@usgs.gov","middleInitial":"G.","affiliations":[{"id":617,"text":"Volcano Science Center","active":true,"usgs":true}],"preferred":false,"id":740808,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Poland, Michael P. 0000-0001-5240-6123 mpoland@usgs.gov","orcid":"https://orcid.org/0000-0001-5240-6123","contributorId":146118,"corporation":false,"usgs":true,"family":"Poland","given":"Michael","email":"mpoland@usgs.gov","middleInitial":"P.","affiliations":[{"id":617,"text":"Volcano Science Center","active":true,"usgs":true}],"preferred":true,"id":740809,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Myer, David","contributorId":206497,"corporation":false,"usgs":false,"family":"Myer","given":"David","email":"","affiliations":[],"preferred":false,"id":740810,"contributorType":{"id":1,"text":"Authors"},"rank":7}]}}
,{"id":86144,"text":"sir20085120 - 2008 - Flood of April 2007 in New Hampshire","interactions":[],"lastModifiedDate":"2012-03-08T17:16:28","indexId":"sir20085120","displayToPublicDate":"2008-08-28T00:00:00","publicationYear":"2008","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":"2008-5120","title":"Flood of April 2007 in New Hampshire","docAbstract":"During April 16-18, 2007, central and southeastern New Hampshire experienced severe flooding as a result of up to 7 inches of rainfall from a storm that stalled off the New England coast. As a result of the flooding, a Presidential Disaster Declaration was issued on April 27, 2007. On that day, disaster declarations were announced for Grafton, Hillsborough, Merrimack, Rockingham, and Strafford Counties. On May 10, 2007, Belknap County was added to the disaster declaration.\r\n\r\nFollowing the flooding, the U.S. Geological Survey, in a cooperative investigation with the Federal Emergency Management Agency, determined the peak stages, peak discharges, and recurrence-interval estimates of the April 2007 flood at 57 streamgages and 4 ungaged sites in and adjacent to the counties named in the disaster declaration. Data from flood-insurance studies published by the Federal Emergency Management Agency also were compiled for each streamgage site for comparison purposes.\r\n\r\nThe peak discharges during the April 2007 flood were the highest ever recorded at five long-term (more than 10 years of record) streamgage sites on the New Hampshire-Salmon Falls River at Milton, Cocheco River near Rochester, Oyster River near Durham, Contoocook River at Peterborough, and South Branch Piscataquog River near Goffstown. In addition, peak discharges equaled or exceeded a 100-year recurrence interval at 10 streamgages and a 50-year recurrence interval at 16 streamgages. The most severe flooding occurred in Rockingham, Strafford, Merrimack, and Hillsborough Counties.","language":"ENGLISH","publisher":"Geological Survey (U.S.)","doi":"10.3133/sir20085120","collaboration":"Prepared in cooperation with the Federal Emergency Management Agency","usgsCitation":"Flynn, R.H., 2008, Flood of April 2007 in New Hampshire: U.S. Geological Survey Scientific Investigations Report 2008-5120, vi, 48 p., https://doi.org/10.3133/sir20085120.","productDescription":"vi, 48 p.","temporalStart":"2007-04-16","temporalEnd":"2007-04-18","costCenters":[{"id":468,"text":"New Hampshire-Vermont Water Science Center","active":false,"usgs":true}],"links":[{"id":194298,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":11711,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/sir/2008/5120/","linkFileType":{"id":5,"text":"html"}}],"geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -72.58333333333333,42.666666666666664 ], [ -72.58333333333333,45.333333333333336 ], [ -70.58333333333333,45.333333333333336 ], [ -70.58333333333333,42.666666666666664 ], [ -72.58333333333333,42.666666666666664 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f1e4b07f02db5ee8bf","contributors":{"authors":[{"text":"Flynn, Robert H. rflynn@usgs.gov","contributorId":2137,"corporation":false,"usgs":true,"family":"Flynn","given":"Robert","email":"rflynn@usgs.gov","middleInitial":"H.","affiliations":[{"id":405,"text":"NH/VT office of New England Water Science Center","active":true,"usgs":true}],"preferred":true,"id":296940,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":86143,"text":"pp1754 - 2008 - Nutrient Concentrations and Their Relations to the Biotic Integrity of Nonwadeable Rivers in Wisconsin","interactions":[],"lastModifiedDate":"2018-02-06T12:30:21","indexId":"pp1754","displayToPublicDate":"2008-08-28T00:00:00","publicationYear":"2008","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":331,"text":"Professional Paper","code":"PP","onlineIssn":"2330-7102","printIssn":"1044-9612","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"1754","title":"Nutrient Concentrations and Their Relations to the Biotic Integrity of Nonwadeable Rivers in Wisconsin","docAbstract":"Excessive nutrient [phosphorus (P) and nitrogen (N)] input from point and nonpoint sources is frequently associated with degraded water quality in streams and rivers. Point-source discharges of nutrients are fairly constant and are controlled by the U.S. Environmental Protection Agency's (USEPA) National Pollutant Discharge Elimination System. To reduce inputs from nonpoint sources, agricultural performance standards and regulations for croplands and livestock operations are being proposed by various States. In addition, the USEPA is establishing regionally based nutrient criteria that can be refined by each State to determine whether actions are needed to improve water quality. More confidence in the environmental benefits of the proposed performance standards and nutrient criteria would be possible with improved understanding of the biotic responses to a range of nutrient concentrations in different environmental settings. \r\n\r\nTo achieve this general goal, the U.S. Geological Survey and the Wisconsin Department of Natural Resources collected data from 282 streams and rivers throughout Wisconsin during 2001 through 2003 to: (1) describe how nutrient concentrations and biotic-community structure differ throughout the State, (2) determine which environmental characteristics are most strongly related to the distribution of nutrient concentrations and biotic-community structure, (3) determine reference conditions for water quality and biotic indices for streams and rivers in the State, (4) determine how the biotic communities in streams and rivers in different areas of the State respond to differences in nutrient concentrations, (5) determine the best regionalization scheme to describe the patterns in reference conditions and the corresponding responses in water quality and the biotic communities (primarily for smaller streams), and (6) develop algorithms to estimate nutrient concentrations in streams and rivers from a combination of biotic indices. The ultimate goal of this study is to provide the information needed to guide the development of regionally based nutrient criteria for Wisconsin streams and rivers. In this report, data collected, primarily in 2003, from 42 nonwadeable rivers are used to describe nutrient concentrations and their relations to the biotic integrity of rivers in Wisconsin. In a separate report by Robertson and others (2006a), the data collected from 240 wadeable streams are used to describe these relations in streams in Wisconsin.\r\n\r\nReference water-quality conditions for nonwadeable rivers were found to be similar throughout Wisconsin (approximately 0.035 milligrams per liter (mg/L) for total P (TP), 0.500 mg/L for total N (TN), 4 micrograms per liter for suspended chlorophyll a (SCHL), and greater than 110 centimeters for Secchi-tube depth (SD)). For each category of the biotic community (SCHL, macroinvertebrates, and fish), a few indices were more strongly related to differences in nutrient concentrations than were others. For the indices most strongly related to nutrient concentrations, reference conditions were obtained with a regression approach, from values corresponding to the worst 75th-percentile value from a subset of minimally impacted streams (streams having reference nutrient concentrations), and from the best 25th-percentile value of all the data.\r\n\r\nConcentrations of TP and TN in nonwadeable rivers increased as the percentage of agricultural land in the basin increased; these increases resulted in increased SCHL concentrations and decreased SDs. The responses in SDs and SCHL concentrations to changes in nutrient concentrations were similar throughout most of the State except in rivers in the southeastern part, where SCHL concentrations were lower than would be expected given their nutrient concentrations. Rivers in the southeastern part of the State had high concentrations of total suspended sediment compared to the SCHL concentrations.\r\n\r\nMany biotic indices responded to increases in nu","language":"ENGLISH","publisher":"Geological Survey (U.S.)","doi":"10.3133/pp1754","isbn":"9781411321717","collaboration":"Prepared in cooperation with the Wisconsin Department of Natural Resources","usgsCitation":"Robertson, D.M., Weigel, B.M., and Graczyk, D., 2008, Nutrient Concentrations and Their Relations to the Biotic Integrity of Nonwadeable Rivers in Wisconsin (Version 1.0): U.S. Geological Survey Professional Paper 1754, xii, 81 p., https://doi.org/10.3133/pp1754.","productDescription":"xii, 81 p.","temporalStart":"2003-01-01","temporalEnd":"2003-12-31","costCenters":[{"id":677,"text":"Wisconsin Water Science Center","active":true,"usgs":true}],"links":[{"id":195397,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/pp1754.png"},{"id":11710,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/pp/1754/","linkFileType":{"id":5,"text":"html"}}],"geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -92.91666666666667,42.5 ], [ -92.91666666666667,47.083333333333336 ], [ -86.75,47.083333333333336 ], [ -86.75,42.5 ], [ -92.91666666666667,42.5 ] ] ] } } ] }","edition":"Version 1.0","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a17e4b07f02db604579","contributors":{"authors":[{"text":"Robertson, Dale M. 0000-0001-6799-0596 dzrobert@usgs.gov","orcid":"https://orcid.org/0000-0001-6799-0596","contributorId":150760,"corporation":false,"usgs":true,"family":"Robertson","given":"Dale","email":"dzrobert@usgs.gov","middleInitial":"M.","affiliations":[{"id":37947,"text":"Upper Midwest Water Science Center","active":true,"usgs":true}],"preferred":true,"id":296937,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Weigel, Brian M.","contributorId":98407,"corporation":false,"usgs":true,"family":"Weigel","given":"Brian","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":296938,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Graczyk, David J.","contributorId":107265,"corporation":false,"usgs":true,"family":"Graczyk","given":"David J.","affiliations":[{"id":677,"text":"Wisconsin Water Science Center","active":true,"usgs":true}],"preferred":false,"id":296939,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":86142,"text":"ofr20081226 - 2008 - Study design and percent recoveries of anthropogenic organic compounds with and without the addition of ascorbic acid to preserve water samples containing free chlorine, 2004-06","interactions":[],"lastModifiedDate":"2021-05-27T14:40:19.040652","indexId":"ofr20081226","displayToPublicDate":"2008-08-28T00:00:00","publicationYear":"2008","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":"2008-1226","title":"Study design and percent recoveries of anthropogenic organic compounds with and without the addition of ascorbic acid to preserve water samples containing free chlorine, 2004-06","docAbstract":"The National Water-Quality Assessment (NAWQA) Program of the U.S. Geological Survey (USGS) began implementing Source Water-Quality Assessments (SWQAs) in 2002 that focus on characterizing the quality of source water and finished water of aquifers and major rivers used by some of the larger community water systems in the United States. As used for SWQA studies, source water is the raw (ambient) water collected at the supply well prior to water treatment (for ground water) or the raw (ambient) water collected from the river near the intake (for surface water). Finished water is the water that is treated, which typically involves, in part, the addition of chlorine or other disinfection chemicals to remove pathogens, and is ready to be delivered to consumers. Finished water is collected before the water enters the distribution system.\r\n\r\nThis report describes the study design and percent recoveries of anthropogenic organic compounds (AOCs) with and without the addition of ascorbic acid to preserve water samples containing free chlorine. The percent recoveries were determined by using analytical results from a laboratory study conducted in 2004 by the USGS's National Water Quality Laboratory (NWQL) and from data collected during 2004-06 for a field study currently (2008) being conducted by the USGS's NAWQA Program.\r\n\r\nThe laboratory study was designed to determine if preserving samples with ascorbic acid (quenching samples) adversely affects analytical performance under controlled conditions. During the laboratory study, eight samples of reagent water were spiked for each of five analytical schedules evaluated. Percent recoveries from these samples were then compared in two ways: (1) four quenched reagent spiked samples analyzed on day 0 were compared with four quenched reagent spiked samples analyzed on day 7 or 14, and (2) the combined eight quenched reagent spiked samples analyzed on day 0, 7, or 14 were compared with eight laboratory reagent spikes (LRSs). Percent recoveries from the quenched reagent spiked samples that were analyzed at two different times (day 0 and day 7 or 14) can be used to determine the stability of the quenched samples held for an amount of time representative of the normal amount of time between sample collection and analysis. The comparison between the quenched reagent spiked samples and the LRSs can be used to determine if quenching samples adversely affects the analytical performance under controlled conditions.\r\n\r\nThe field study began in 2004 and is continuing today (February 2008) to characterize the effect of quenching on field-matrix spike recoveries and to better understand the potential oxidation and transformation of 277 AOCs. Three types of samples were collected from 11 NAWQA Study Units across the Nation: (1) quenched finished-water samples (not spiked), (2) quenched finished-water spiked samples, and (3) nonquenched finished-water spiked samples. Percent recoveries of AOCs in quenched and nonquenched finished-water spiked samples collected during 2004-06 are presented. Comparisons of percent recoveries between quenched and nonquenched spiked samples can be used to show how quenching affects finished-water samples. A maximum of 6 surface-water and 7 ground-water quenched finished-water spiked samples paired with nonquenched finished-water spiked samples were analyzed. Analytical results for the field study are presented in two ways: (1) by surface-water supplies or ground-water supplies, and (2) by use (or source) group category for surface-water and ground-water supplies. Graphical representations of percent recoveries for the quenched and nonquenched finished-water spiked samples also are presented.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr20081226","usgsCitation":"Valder, J., Delzer, G.C., Price, C.V., and Sandstrom, M.W., 2008, Study design and percent recoveries of anthropogenic organic compounds with and without the addition of ascorbic acid to preserve water samples containing free chlorine, 2004-06 (Version 1.0): U.S. Geological Survey Open-File Report 2008-1226, viii, 86 p., https://doi.org/10.3133/ofr20081226.","productDescription":"viii, 86 p.","additionalOnlineFiles":"Y","temporalStart":"2004-01-01","temporalEnd":"2006-12-31","costCenters":[{"id":452,"text":"National Water Quality Laboratory","active":true,"usgs":true},{"id":562,"text":"South Dakota Water Science Center","active":true,"usgs":true},{"id":34685,"text":"Dakota Water Science Center","active":true,"usgs":true}],"links":[{"id":195199,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":11709,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2008/1226/","linkFileType":{"id":5,"text":"html"}}],"edition":"Version 1.0","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b05e4b07f02db699d1b","contributors":{"authors":[{"text":"Valder, Joshua F. 0000-0003-3733-8868 jvalder@usgs.gov","orcid":"https://orcid.org/0000-0003-3733-8868","contributorId":1431,"corporation":false,"usgs":true,"family":"Valder","given":"Joshua F.","email":"jvalder@usgs.gov","affiliations":[{"id":562,"text":"South Dakota Water Science Center","active":true,"usgs":true}],"preferred":false,"id":296936,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Delzer, Gregory C. 0000-0002-7077-4963 gcdelzer@usgs.gov","orcid":"https://orcid.org/0000-0002-7077-4963","contributorId":986,"corporation":false,"usgs":true,"family":"Delzer","given":"Gregory","email":"gcdelzer@usgs.gov","middleInitial":"C.","affiliations":[{"id":562,"text":"South Dakota Water Science Center","active":true,"usgs":true}],"preferred":true,"id":296935,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Price, Curtis V. 0000-0002-4315-3539 cprice@usgs.gov","orcid":"https://orcid.org/0000-0002-4315-3539","contributorId":983,"corporation":false,"usgs":true,"family":"Price","given":"Curtis","email":"cprice@usgs.gov","middleInitial":"V.","affiliations":[{"id":562,"text":"South Dakota Water Science Center","active":true,"usgs":true}],"preferred":true,"id":296934,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Sandstrom, Mark W. 0000-0003-0006-5675 sandstro@usgs.gov","orcid":"https://orcid.org/0000-0003-0006-5675","contributorId":706,"corporation":false,"usgs":true,"family":"Sandstrom","given":"Mark","email":"sandstro@usgs.gov","middleInitial":"W.","affiliations":[{"id":503,"text":"Office of Water Quality","active":true,"usgs":true},{"id":452,"text":"National Water Quality Laboratory","active":true,"usgs":true},{"id":5046,"text":"Branch of Analytical Serv (NWQL)","active":true,"usgs":true},{"id":37464,"text":"WMA - Laboratory & Analytical Services Division","active":true,"usgs":true}],"preferred":true,"id":296933,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70199789,"text":"70199789 - 2008 - Origin, conditions, and timing of gas generation in the Lewis Shale, San Juan Basin, New Mexico ","interactions":[],"lastModifiedDate":"2018-09-28T11:26:39","indexId":"70199789","displayToPublicDate":"2008-08-27T11:03:52","publicationYear":"2008","noYear":false,"publicationType":{"id":5,"text":"Book chapter"},"publicationSubtype":{"id":24,"text":"Book Chapter"},"title":"Origin, conditions, and timing of gas generation in the Lewis Shale, San Juan Basin, New Mexico ","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Gas shale in the Rocky Mountains and beyond","largerWorkSubtype":{"id":13,"text":"Handbook"},"language":"English","publisher":"The Rocky Mountain Association of Geologists","usgsCitation":"Fishman, N.S., Parris, T., Hall, D.L., Lillis, P.G., and Pawlewicz, M.J., 2008, Origin, conditions, and timing of gas generation in the Lewis Shale, San Juan Basin, New Mexico , chap. <i>of</i> Gas shale in the Rocky Mountains and beyond, CD ROM.","productDescription":"CD ROM","costCenters":[{"id":164,"text":"Central Energy Resources Science Center","active":true,"usgs":true}],"links":[{"id":357886,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":357882,"rank":1,"type":{"id":15,"text":"Index Page"},"url":"https://www.rmag.org/index.php?option=com_content&view=article&id=96:gas-shale&catid=20:site-content"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5c10d26de4b034bf6a7f9733","contributors":{"editors":[{"text":"Hill, David G.","contributorId":208269,"corporation":false,"usgs":false,"family":"Hill","given":"David","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":746616,"contributorType":{"id":2,"text":"Editors"},"rank":1},{"text":"Lillis, Paul G. 0000-0002-7508-1699 plillis@usgs.gov","orcid":"https://orcid.org/0000-0002-7508-1699","contributorId":1817,"corporation":false,"usgs":true,"family":"Lillis","given":"Paul","email":"plillis@usgs.gov","middleInitial":"G.","affiliations":[{"id":164,"text":"Central Energy Resources Science Center","active":true,"usgs":true}],"preferred":true,"id":746617,"contributorType":{"id":2,"text":"Editors"},"rank":2},{"text":"Curtis, John B.","contributorId":70972,"corporation":false,"usgs":false,"family":"Curtis","given":"John","email":"","middleInitial":"B.","affiliations":[{"id":6606,"text":"Colorado School of Mines","active":true,"usgs":false}],"preferred":false,"id":746618,"contributorType":{"id":2,"text":"Editors"},"rank":3}],"authors":[{"text":"Fishman, Neil S.","contributorId":106464,"corporation":false,"usgs":true,"family":"Fishman","given":"Neil","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":746611,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Parris, Thomas","contributorId":69063,"corporation":false,"usgs":true,"family":"Parris","given":"Thomas","affiliations":[],"preferred":false,"id":746612,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Hall, Donald L.","contributorId":208270,"corporation":false,"usgs":false,"family":"Hall","given":"Donald","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":746615,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Lillis, Paul G. 0000-0002-7508-1699 plillis@usgs.gov","orcid":"https://orcid.org/0000-0002-7508-1699","contributorId":1817,"corporation":false,"usgs":true,"family":"Lillis","given":"Paul","email":"plillis@usgs.gov","middleInitial":"G.","affiliations":[{"id":164,"text":"Central Energy Resources Science Center","active":true,"usgs":true}],"preferred":true,"id":746613,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Pawlewicz, Mark J. pawlewicz@usgs.gov","contributorId":752,"corporation":false,"usgs":true,"family":"Pawlewicz","given":"Mark","email":"pawlewicz@usgs.gov","middleInitial":"J.","affiliations":[{"id":164,"text":"Central Energy Resources Science Center","active":true,"usgs":true}],"preferred":true,"id":746614,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":86141,"text":"fs20083070 - 2008 - Debris-Flow Hazards within the Appalachian Mountains of the Eastern United States","interactions":[],"lastModifiedDate":"2012-02-10T00:10:10","indexId":"fs20083070","displayToPublicDate":"2008-08-27T00:00:00","publicationYear":"2008","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":313,"text":"Fact Sheet","code":"FS","onlineIssn":"2327-6932","printIssn":"2327-6916","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2008-3070","title":"Debris-Flow Hazards within the Appalachian Mountains of the Eastern United States","docAbstract":"Tropical storms, including hurricanes, often inflict major damage to property and disrupt the lives of people living in coastal areas of the Eastern United States. These storms also are capable of generating catastrophic landslides within the steep slopes of the Appalachian Mountains. Heavy rainfall from hurricanes, cloudbursts, and thunderstorms can generate rapidly moving debris flows that are among the most dangerous and damaging type of landslides. This fact sheet explores the nature and occurrence of debris flows in the central and southern Appalachian Mountains, which extend from central Pennsylvania to northern Alabama.","language":"ENGLISH","publisher":"Geological Survey (U.S.)","doi":"10.3133/fs20083070","usgsCitation":"Wieczorek, G.F., and Morgan, B.A., 2008, Debris-Flow Hazards within the Appalachian Mountains of the Eastern United States: U.S. Geological Survey Fact Sheet 2008-3070, 4 p., https://doi.org/10.3133/fs20083070.","productDescription":"4 p.","onlineOnly":"Y","costCenters":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"links":[{"id":122398,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/fs_2008_3070.jpg"},{"id":11708,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/fs/2008/3070/","linkFileType":{"id":5,"text":"html"}}],"geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -86,34 ], [ -86,43 ], [ -72,43 ], [ -72,34 ], [ -86,34 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4abbe4b07f02db67297f","contributors":{"authors":[{"text":"Wieczorek, Gerald F.","contributorId":81889,"corporation":false,"usgs":true,"family":"Wieczorek","given":"Gerald","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":296932,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Morgan, Benjamin A.","contributorId":32158,"corporation":false,"usgs":true,"family":"Morgan","given":"Benjamin","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":296931,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70236461,"text":"70236461 - 2008 - Short-term response of methane fluxes and methanogen activity to water table and soil warming manipulations in an Alaskan peatland","interactions":[],"lastModifiedDate":"2022-09-07T16:06:07.384529","indexId":"70236461","displayToPublicDate":"2008-08-26T10:48:53","publicationYear":"2008","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":7359,"text":"Journal of Geophysical Research Biogeosciences","active":true,"publicationSubtype":{"id":10}},"title":"Short-term response of methane fluxes and methanogen activity to water table and soil warming manipulations in an Alaskan peatland","docAbstract":"<p><span>Growing season CH</span><sub>4</sub><span>&nbsp;fluxes were monitored over a two year period following the start of ecosystem-scale manipulations of water table position and surface soil temperatures in a moderate rich fen in interior Alaska. The largest CH</span><sub>4</sub><span>&nbsp;fluxes occurred in plots that received both flooding (raised water table position) and soil warming, while the lowest fluxes occurred in unwarmed plots in the lowered water table treatment. A combination of treatment and soil hydroclimate variables explained more than 70% of the variation in ln-transformed CH</span><sub>4</sub><span>&nbsp;fluxes, with mean daily water table position representing the strongest predictor. We used quantitative PCR of the&nbsp;</span><i>α</i><span>-subunit of mcr operon to explore the influence of soil climate manipulations on methanogen abundances. Methanogen abundances were greatest in warmed plots, and showed a positive relationship with mean daily CH</span><sub>4</sub><span>&nbsp;fluxes. Our results show that water table manipulations that led to soil inundation (flooding) had a stronger effect on CH</span><sub>4</sub><span>&nbsp;fluxes than water table drawdown. Seasonal CH</span><sub>4</sub><span>&nbsp;fluxes increased by 80–300% under the combined wetter and warmer soil climate treatments. Thus, while warming is expected to increase CH</span><sub>4</sub><span>&nbsp;emissions from Alaskan wetlands, higher water table positions caused by increases in precipitation or disturbances such as permafrost thaw that lead to thermokarst and flooding in wetlands will stimulate CH</span><sub>4</sub><span>&nbsp;emissions beyond the effects of soil warming alone. Consequently, we argue that modeling the effects of climate change on Alaskan wetland CH</span><sub>4</sub><span>&nbsp;emissions needs to consider the interactive effects of soil warming and water table position on CH</span><sub>4</sub><span>&nbsp;production and transport.</span></p>","language":"English","publisher":"American Geophysical Union","doi":"10.1029/2007JG000496","usgsCitation":"Turetsky, M.R., Treat, C., Waldrop, M., Waddington, J., Harden, J.W., and McGuire, A.D., 2008, Short-term response of methane fluxes and methanogen activity to water table and soil warming manipulations in an Alaskan peatland: Journal of Geophysical Research Biogeosciences, v. 113, no. G3, G00A10, 15 p., https://doi.org/10.1029/2007JG000496.","productDescription":"G00A10, 15 p.","costCenters":[{"id":200,"text":"Coop Res Unit Seattle","active":true,"usgs":true},{"id":617,"text":"Volcano Science Center","active":true,"usgs":true}],"links":[{"id":476595,"rank":0,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1029/2007jg000496","text":"Publisher Index Page"},{"id":406321,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Alaska","otherGeospatial":"Bonanza Creek Experimental Forest","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -147.95,\n              64.9\n            ],\n            [\n              -147.75,\n              64.9\n            ],\n            [\n              -147.75,\n              64.76\n            ],\n            [\n              -147.95,\n              64.76\n            ],\n            [\n              -147.95,\n              64.9\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"113","issue":"G3","noUsgsAuthors":false,"publicationDate":"2008-08-26","publicationStatus":"PW","contributors":{"authors":[{"text":"Turetsky, M. R.","contributorId":216779,"corporation":false,"usgs":false,"family":"Turetsky","given":"M.","email":"","middleInitial":"R.","affiliations":[{"id":12660,"text":"University of Guelph","active":true,"usgs":false}],"preferred":false,"id":851095,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Treat, C. C.","contributorId":257236,"corporation":false,"usgs":false,"family":"Treat","given":"C. C.","affiliations":[{"id":51984,"text":"University of Finland","active":true,"usgs":false}],"preferred":false,"id":851096,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Waldrop, M. P. 0000-0003-1829-7140","orcid":"https://orcid.org/0000-0003-1829-7140","contributorId":105104,"corporation":false,"usgs":true,"family":"Waldrop","given":"M. P.","affiliations":[],"preferred":false,"id":851097,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Waddington, J. M.","contributorId":105938,"corporation":false,"usgs":false,"family":"Waddington","given":"J. M.","affiliations":[],"preferred":false,"id":851098,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Harden, Jennifer W. 0000-0002-6570-8259 jharden@usgs.gov","orcid":"https://orcid.org/0000-0002-6570-8259","contributorId":1971,"corporation":false,"usgs":true,"family":"Harden","given":"Jennifer","email":"jharden@usgs.gov","middleInitial":"W.","affiliations":[{"id":615,"text":"Volcano Hazards Program","active":true,"usgs":true},{"id":617,"text":"Volcano Science Center","active":true,"usgs":true},{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"preferred":true,"id":851099,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"McGuire, A. David 0000-0003-4646-0750 ffadm@usgs.gov","orcid":"https://orcid.org/0000-0003-4646-0750","contributorId":166708,"corporation":false,"usgs":true,"family":"McGuire","given":"A.","email":"ffadm@usgs.gov","middleInitial":"David","affiliations":[{"id":200,"text":"Coop Res Unit Seattle","active":true,"usgs":true}],"preferred":false,"id":851100,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}}
,{"id":86137,"text":"ds357 - 2008 - Bathymetric Surveys of Lake Arthur and Raccoon Lake, Pennsylvania, June 2007","interactions":[],"lastModifiedDate":"2017-06-27T11:14:57","indexId":"ds357","displayToPublicDate":"2008-08-26T00:00:00","publicationYear":"2008","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":310,"text":"Data Series","code":"DS","onlineIssn":"2327-638X","printIssn":"2327-0271","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"357","title":"Bathymetric Surveys of Lake Arthur and Raccoon Lake, Pennsylvania, June 2007","docAbstract":"In spring of 2007, bathymetric surveys of two Pennsylvania State Park lakes were performed to collect accurate data sets of lake-bed elevations and to develop methods and techniques to conduct similar surveys across the state. The lake-bed elevations and associated geographical position data can be merged with land-surface elevations acquired through Light Detection and Ranging (LIDAR) techniques. Lake Arthur in Butler County and Raccoon Lake in Beaver County were selected for this initial data-collection activity. In order to establish accurate water-surface elevations during the surveys, benchmarks referenced to NAVD 88 were established on land at each lake by use of differential global positioning system (DGPS) surveys. Bathymetric data were collected using a single beam, 210 kilohertz (kHz) echo sounder and were coupled with the DGPS position data utilizing a computer software package. Transects of depth data were acquired at predetermined intervals on each lake, and the shoreline was delineated using a laser range finder and compass module. Final X, Y, Z coordinates of the geographic positions and lake-bed elevations were referenced to NAD 83 and NAVD 88 and are available to create bathymetric maps of the lakes.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ds357","collaboration":"Prepared in cooperation with the Pennsylvania Department of Conservation and Natural Resources","usgsCitation":"Hittle, C.D., and Ruby, A.T., 2008, Bathymetric Surveys of Lake Arthur and Raccoon Lake, Pennsylvania, June 2007: U.S. Geological Survey Data Series 357, Report: iv, 10 p.; Appendix (ZIP File), https://doi.org/10.3133/ds357.","productDescription":"Report: iv, 10 p.; Appendix (ZIP File)","onlineOnly":"Y","additionalOnlineFiles":"Y","temporalStart":"2007-06-01","temporalEnd":"2007-06-30","costCenters":[{"id":532,"text":"Pennsylvania Water Science Center","active":true,"usgs":true}],"links":[{"id":195179,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":11704,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/ds/357/","linkFileType":{"id":5,"text":"html"}}],"geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -80.58333333333333,40.333333333333336 ], [ -80.58333333333333,41 ], [ -79.58333333333333,41 ], [ -79.58333333333333,40.333333333333336 ], [ -80.58333333333333,40.333333333333336 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a6fe4b07f02db640aa5","contributors":{"authors":[{"text":"Hittle, Clinton D. cdhittle@usgs.gov","contributorId":2436,"corporation":false,"usgs":true,"family":"Hittle","given":"Clinton","email":"cdhittle@usgs.gov","middleInitial":"D.","affiliations":[],"preferred":true,"id":296921,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Ruby, A. Thomas III","contributorId":48270,"corporation":false,"usgs":true,"family":"Ruby","given":"A.","suffix":"III","email":"","middleInitial":"Thomas","affiliations":[],"preferred":false,"id":296922,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":86134,"text":"ofr20081263 - 2008 - The National Map 2.0 Tactical Plan: \"Toward the (Integrated) National Map\"","interactions":[],"lastModifiedDate":"2012-02-02T00:14:30","indexId":"ofr20081263","displayToPublicDate":"2008-08-23T00:00:00","publicationYear":"2008","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":"2008-1263","title":"The National Map 2.0 Tactical Plan: \"Toward the (Integrated) National Map\"","docAbstract":"The National Map's 2-year goal, as described in this plan, is to provide a range of geospatial products and services that meet the basic goals of the original vision for The National Map while furthering the National Spatial Data Infrastructure that underpins U.S. Geological Survey (USGS) science. To accomplish this goal, the National Geospatial Program (NGP) will acquire, store, maintain, and distribute base map data. The management team for the NGP sets priorities for The National Map in three areas: Data and Products, Services, and Management. Priorities for fiscal years 2008 and 2009 (October 1, 2007 through September 30, 2009), involving the current data inventory, data acquisition, and the integration of data, are (1) incorporating current data from Federal, State, and local organizations into The National Map to the degree possible, given data availability and program resources; (2) collaborating with other USGS programs to incorporate data that support the USGS Science Strategy; (3) supporting the Department of the Interior (DOI) high-priority geospatial information needs; (4) emergency response; (5) homeland security, natural hazards; and (6) graphics products delivery.\r\n\r\nThe management team identified known constraints, enablers, and drivers for the acquisition and integration of data. The NGP management team also identified customer-focused products and services of The National Map. Ongoing planning and management activities direct the development and delivery of these products and services. Management of work flow processes to support The National Map priorities are identified and established through a business-driven prioritization process.\r\n\r\nThis tactical plan is primarily for use as a document to guide The National Map program for the next two fiscal years. The document is available to the public because of widespread interest in The National Map.\r\n\r\nThe USGS collaborates with a broad range of customers and partners who are essential to the success of The National Map, including the science community, State and Federal agencies involved in homeland security, planners and emergency responders at the local level, and private companies. Partner contributions and data remain a primary input and foundation of The National Map. Partnership strategies for each of The National Map's component data themes are outlined in this plan. Because of the importance of The National Map customers, a reassessment of customer needs will be completed during 2008. Results of the assessment will be incorporated into future decisions and priorities.\r\n\r\nA performance milestone matrix has been developed that contains the full list of milestones, major deliverables, and major tasks. The matrix forms the basis for reporting on accomplishments and issues. However, a number of risks, dependencies, and issues have been identified that could affect meeting milestones in the matrix, such as: the USGS is not the Circular A-16 lead for boundaries, transportation, and structures; availability of sufficient and sustainable funding; availability of Federal workforce and contractors with necessary skills, and numerous competing customer and stakeholder requirements.","language":"ENGLISH","publisher":"Geological Survey (U.S.)","doi":"10.3133/ofr20081263","usgsCitation":"Zulick, C.A., 2008, The National Map 2.0 Tactical Plan: \"Toward the (Integrated) National Map\": U.S. Geological Survey Open-File Report 2008-1263, ix, 58 p., https://doi.org/10.3133/ofr20081263.","productDescription":"ix, 58 p.","onlineOnly":"Y","temporalStart":"2007-10-01","temporalEnd":"2009-09-30","costCenters":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"links":[{"id":195296,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ofr20081263.jpg"},{"id":11701,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2008/1263/","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac7e4b07f02db67b00a","contributors":{"authors":[{"text":"Zulick, Carl A.","contributorId":18866,"corporation":false,"usgs":true,"family":"Zulick","given":"Carl","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":296915,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":86132,"text":"sir20085118 - 2008 - Aquifer Tests and Characterization of Transmissivity, Ada-Vamoosa Aquifer on the Osage Reservation, Osage County, Oklahoma, 2006","interactions":[],"lastModifiedDate":"2012-02-10T00:11:42","indexId":"sir20085118","displayToPublicDate":"2008-08-23T00:00:00","publicationYear":"2008","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":"2008-5118","title":"Aquifer Tests and Characterization of Transmissivity, Ada-Vamoosa Aquifer on the Osage Reservation, Osage County, Oklahoma, 2006","docAbstract":"The Ada-Vamoosa aquifer of northeastern Oklahoma is a sedimentary bedrock aquifer of Pennsylvanian age that crops out over 800 square miles of the Osage Reservation. The Osage Nation needed additional information regarding the production potential of the aquifer to aid them in future development planning. To address this need, the U.S. Geological Survey, in cooperation with the Osage Nation, conducted a study of aquifer properties in the Ada-Vamoosa aquifer. This report presents the results of the aquifer tests from 20 wells in the Ada-Vamoosa aquifer and one well in a minor aquifer east of the Ada-Vamoosa outcrop on the Osage Reservation. Well information for 17 of the 21 wells in this report was obtained from the Indian Health Service. Data collected by the U.S. Geological Survey during this investigation are pumping well data from four domestic wells collected during the summer of 2006. Transmissivity values were calculated from well pumping data or were estimated from specific capacity values depending on the reliability of the data. The estimated transmissivity values are 1.1 to 4.3 times greater than the calculated transmissivity values. The calculated and estimated transmissivity values range from 5 to 1,000 feet squared per day.","language":"ENGLISH","publisher":"Geological Survey (U.S.)","doi":"10.3133/sir20085118","collaboration":"Prepared in cooperation with the Osage Tribal Council","usgsCitation":"Abbott, M.M., and DeHay, K., 2008, Aquifer Tests and Characterization of Transmissivity, Ada-Vamoosa Aquifer on the Osage Reservation, Osage County, Oklahoma, 2006 (Version 1.0): U.S. Geological Survey Scientific Investigations Report 2008-5118, iv, 10 p., https://doi.org/10.3133/sir20085118.","productDescription":"iv, 10 p.","onlineOnly":"Y","temporalStart":"2006-01-01","temporalEnd":"2006-12-31","costCenters":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"links":[{"id":121165,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/sir_2008_5118.jpg"},{"id":11699,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/sir/2008/5118/","linkFileType":{"id":5,"text":"html"}}],"geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -97.16666666666667,36.083333333333336 ], [ -97.16666666666667,37.083333333333336 ], [ -95.91666666666667,37.083333333333336 ], [ -95.91666666666667,36.083333333333336 ], [ -97.16666666666667,36.083333333333336 ] ] ] } } ] }","edition":"Version 1.0","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac5e4b07f02db67a067","contributors":{"authors":[{"text":"Abbott, Marvin M.","contributorId":89106,"corporation":false,"usgs":true,"family":"Abbott","given":"Marvin","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":296913,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"DeHay, Kelli","contributorId":14064,"corporation":false,"usgs":true,"family":"DeHay","given":"Kelli","affiliations":[],"preferred":false,"id":296912,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":86133,"text":"sir20085112 - 2008 - Precipitation-Frequency and Discharge-Frequency Relations for Basins Less than 32 Square Miles in Kansas","interactions":[],"lastModifiedDate":"2012-03-08T17:16:26","indexId":"sir20085112","displayToPublicDate":"2008-08-23T00:00:00","publicationYear":"2008","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":"2008-5112","title":"Precipitation-Frequency and Discharge-Frequency Relations for Basins Less than 32 Square Miles in Kansas","docAbstract":"Precipitation-frequency and discharge-frequency relations for small drainage basins with areas less than 32 square miles in Kansas were evaluated to reduce the uncertainty of discharge-frequency estimates. Gaged-discharge records were used to develop discharge-frequency equations for the ratio of discharge to drainage area (Q/A) values using data from basins with variable soil permeability, channel slope, and mean annual precipitation. Soil permeability and mean annual precipitation are the dominant basin characteristics in the multiple linear regression analyses.\r\n\r\nIn addition, 28 discharge measurements at ungaged sites by indirect surveying methods and by velocity meters also were used in this analysis to relate precipitation-recurrence interval to discharge-recurrence interval. Precipitation-recurrence interval for each of these discharge measurements were estimated from weather-radar estimates of precipitation and from nearby raingages. Time of concentration for each basin for each of the ungaged sites was computed and used to determine the precipitation-recurrence interval based on precipitation depth and duration. The ratio of discharge/drainage area (Q/A) value for each event was then assigned to that precipitation-recurrence interval. \r\n\r\nThe relation between the ratio of discharge/drainage area (Q/A) and precipitation-recurrence interval for all 28 measured events resulted in a correlation coefficient of 0.79. Using basins less than 5.4 mi2 only, the correlation decreases to 0.74. However, when basins greater than 5.4 and less than 32 mi2 are examined the relation improves to a correlation coefficient of 0.95.\r\n\r\nThere were a sufficient number of discharge and radar-measured precipitation events for both the 5-year (8 events) and the 100-year (11 events) recurrence intervals to examine the effect of basin characteristics on the Q/A values for basins less than 32 mi2. At the 5-year precipitation-/discharge-recurrence interval, channel slope was a significant predictor (r=0.99) of Q/A. Permeability (r=0.68) also had a significant effect on Q/A values for the 5-year recurrence interval. At the 100-year recurrence interval, permeability, channel slope, and mean annual precipitation did not have a significant effect on Q/A; however, time of concentration was a significant factor in determining Q/A for the 100-year events with greater times of concentration resulting in lower Q/A values. Additional high-recurrence interval (5-, 10-, 25-, 50-, and 100-year) precipitation/discharge data are needed to confirm these relations suggested above. Discharge data with attendant basin-wide precipitation data from precipitation-radar estimates provides a unique opportunity to study the effects of basin characteristics on the relation between precipitation recurrence interval and discharge-recurrence interval.\r\n\r\nDischarge-frequency values from the Q/A equations, the rational method, and the Kansas discharge-frequency equations (KFFE) were compared to 28 measured weather-radar precipitation-/discharge-frequency values. The association between precipitation frequency from weather-radar estimates and the frequency of the resulting discharge was shown in these comparisons. The measured and Q/A equation computed discharges displayed the best equality from low to high discharges of the three methods. Here the slope of the line was nearly 1:1 (y=0.9844x0.9677). Comparisons with the rational method produced a slope greater than 1:1 (y=0.0722x1.235), and the KFFE equations produced a slope less than 1:1 (y=5.9103x0.7475). The Q/A equation standard error of prediction averaged 0.1346 log units for the 5.4-to 32-square-mile group and 0.0944 log units for the less than 5.4-square mile group. The KFFE standard error averaged 0.2107 log units for the less-than-30-square-mile equations. Using the Q/A equations for determining discharge frequency values for ungaged sites thus appears to be a good alternative to the other two methods because of this s","language":"ENGLISH","publisher":"Geological Survey (U.S.)","doi":"10.3133/sir20085112","collaboration":"Prepared in cooperation with the Kansas Department of Transportation","usgsCitation":"Perry, C.A., 2008, Precipitation-Frequency and Discharge-Frequency Relations for Basins Less than 32 Square Miles in Kansas: U.S. Geological Survey Scientific Investigations Report 2008-5112, vi, 25 p., https://doi.org/10.3133/sir20085112.","productDescription":"vi, 25 p.","costCenters":[{"id":353,"text":"Kansas Water Science Center","active":false,"usgs":true}],"links":[{"id":195795,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":11700,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/sir/2008/5112/","linkFileType":{"id":5,"text":"html"}}],"geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -102.08333333333333,37 ], [ -102.08333333333333,40 ], [ -94.58333333333333,40 ], [ -94.58333333333333,37 ], [ -102.08333333333333,37 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b08e4b07f02db69bae3","contributors":{"authors":[{"text":"Perry, Charles A. cperry@usgs.gov","contributorId":2093,"corporation":false,"usgs":true,"family":"Perry","given":"Charles","email":"cperry@usgs.gov","middleInitial":"A.","affiliations":[],"preferred":true,"id":296914,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
]}