{"pageNumber":"2002","pageRowStart":"50025","pageSize":"25","recordCount":184682,"records":[{"id":70179542,"text":"70179542 - 2009 - Delayed genetic effects of habitat fragmentation on the ecologically specialized Florida sand skink (<i>Plestiodon reynoldsi</i>)","interactions":[],"lastModifiedDate":"2017-01-04T12:31:12","indexId":"70179542","displayToPublicDate":"2009-10-01T00:00:00","publicationYear":"2009","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1324,"text":"Conservation Genetics","active":true,"publicationSubtype":{"id":10}},"title":"Delayed genetic effects of habitat fragmentation on the ecologically specialized Florida sand skink (<i>Plestiodon reynoldsi</i>)","docAbstract":"<p><span>Populations rarely show immediate genetic responses to habitat fragmentation, even in taxa that possess suites of traits known to increase their vulnerability to extinction. Thus conservation geneticists must consider the time scale over which contemporary evolutionary processes operate to accurately portray the effects of habitat isolation. Here, we examine the genetic impacts of fragmentation on the Florida sand skink </span><i class=\"EmphasisTypeItalic \">Plestiodon&nbsp;reynoldsi</i><span>, a sand swimming lizard that is highly adapted to the upland scrub habitat of central Florida. We studied fragments located on the southern Lake Wales Ridge, where human activity in the latter half of the 20th century has modified the natural patchiness of the landscape. Based on a relaxed molecular clock method, we estimate that sand skinks have persisted in this region for approximately 1.5&nbsp;million years and that the time frame of human disturbance is equivalent to fewer than 30 skink generations. Using genotypes from eight microsatellite loci, we screened for molecular signatures of this disturbance by assessing congruence between population structure, as inferred from spatially-informed Bayesian assignment tests, and the current geography of scrub fragments. We also tested for potential intrapopulation genetic effects of inbreeding in isolated populations by comparing the average pairwise relatedness of individuals within fragments of different areas and isolation. Our results indicate that although some patches show a higher degree of relatedness than expected under random mating, the genetic effects of recent isolation are not evident in this part of the species’ range. We argue that this result is an artefact of a time-lag in the response to disturbance, and that species-typical demographic features may explain the genetic inertia observed in these populations.</span></p>","language":"English","publisher":"Springer","doi":"10.1007/s10592-008-9707-x","usgsCitation":"Richmond, J.Q., Reid, D.T., Ashton, K.G., and Zamudio, K.R., 2009, Delayed genetic effects of habitat fragmentation on the ecologically specialized Florida sand skink (<i>Plestiodon reynoldsi</i>): Conservation Genetics, v. 10, no. 5, p. 1281-1297, https://doi.org/10.1007/s10592-008-9707-x.","productDescription":"17 p.","startPage":"1281","endPage":"1297","costCenters":[{"id":651,"text":"Western Ecological Research Center","active":true,"usgs":true}],"links":[{"id":332864,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"10","issue":"5","noUsgsAuthors":false,"publicationDate":"2008-09-24","publicationStatus":"PW","scienceBaseUri":"586e1826e4b0f5ce109fcae9","contributors":{"authors":[{"text":"Richmond, Jonathan Q. 0000-0001-9398-4894 jrichmond@usgs.gov","orcid":"https://orcid.org/0000-0001-9398-4894","contributorId":5400,"corporation":false,"usgs":true,"family":"Richmond","given":"Jonathan","email":"jrichmond@usgs.gov","middleInitial":"Q.","affiliations":[{"id":651,"text":"Western Ecological Research Center","active":true,"usgs":true}],"preferred":true,"id":657598,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Reid, Duncan T.","contributorId":177941,"corporation":false,"usgs":false,"family":"Reid","given":"Duncan","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":657599,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Ashton, Kyle G.","contributorId":177942,"corporation":false,"usgs":false,"family":"Ashton","given":"Kyle","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":657600,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Zamudio, Kelly R.","contributorId":8320,"corporation":false,"usgs":true,"family":"Zamudio","given":"Kelly","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":657601,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70043936,"text":"70043936 - 2009 - Regional classification of Pacific Northwest estuaries by wetland and land cover patterns","interactions":[],"lastModifiedDate":"2016-12-28T14:47:36","indexId":"70043936","displayToPublicDate":"2009-10-01T00:00:00","publicationYear":"2009","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":4,"text":"Other Government Series"},"title":"Regional classification of Pacific Northwest estuaries by wetland and land cover patterns","docAbstract":"Increased anthropogenic nutrient loading and the subsequent eutrophication of coastal\necosystems is a growing ecological and economic problem both in the United States and globally. Eutrophication can result in a range of ecological impacts including hypoxic conditions, fish kills, loss of submerged aquatic vegetation (SAV), degraded benthic conditions,\nharmful algal blooms, and detrimental increases in benthic macroalgae. The nature and severity of the impacts vary with the level of nutrient loading as well as with the estuary type and regional drivers.","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Classification of regional patterns of environmental drivers and benthic habitats in Pacific Northwest estuaries ","language":"English","publisher":"Enviromental Protection Agency","usgsCitation":"Lee, Brown, A.C., Clinton, J.P., and Hagerty, P., 2009, Regional classification of Pacific Northwest estuaries by wetland and land cover patterns, 73 p. .","productDescription":"73 p. ","startPage":"9","endPage":"81","ipdsId":"IP-016972","costCenters":[{"id":654,"text":"Western Fisheries Research Center","active":true,"usgs":true}],"links":[{"id":332599,"rank":1,"type":{"id":11,"text":"Document"},"url":"https://nepis.epa.gov/Exe/ZyNET.exe/P1006Q2H.txt?ZyActionD=ZyDocument&Client=EPA&Index=2006%20Thru%202010&Docs=&Query=&Time=&EndTime=&SearchMethod=1&TocRestrict=n&Toc=&TocEntry=&QField=&QFieldYear=&QFieldMonth=&QFieldDay=&UseQField=&IntQFieldOp=0&ExtQFieldOp=0&XmlQuery=&File=D%3A%5CZYFILES%5CINDEX%20DATA%5C06THRU10%5CTXT%5C00000016%5CP1006Q2H.txt&User=ANONYMOUS&Password=anonymous&SortMethod=h%7C-&MaximumDocuments=1&FuzzyDegree=0&ImageQuality=r75g8/r75g8/x150y150g16/i425&Display=hpfr&DefSeekPage=x&SearchBack=ZyActionL&Back=ZyActionS&BackDesc=Results%20page&MaximumPages=1&ZyEntry=1"},{"id":332600,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5864dd54e4b0cd2dabe7c1dd","contributors":{"authors":[{"text":"Lee, Henry II","contributorId":115628,"corporation":false,"usgs":true,"family":"Lee","suffix":"Henry II","affiliations":[],"preferred":false,"id":516951,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Brown, A Cheryl Cheryl","contributorId":115744,"corporation":false,"usgs":true,"family":"Brown","given":"A","suffix":"Cheryl","email":"","middleInitial":"Cheryl","affiliations":[],"preferred":false,"id":516952,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Clinton, J Patrick Patrick","contributorId":119995,"corporation":false,"usgs":true,"family":"Clinton","given":"J","suffix":"Patrick","email":"","middleInitial":"Patrick","affiliations":[],"preferred":false,"id":516955,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Hagerty, Patti Patti","contributorId":119397,"corporation":false,"usgs":true,"family":"Hagerty","given":"Patti","suffix":"Patti","email":"","affiliations":[],"preferred":false,"id":516954,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":70042163,"text":"70042163 - 2009 - National Wildlife Health Center's quarterly wildlife mortality report","interactions":[],"lastModifiedDate":"2023-10-13T16:45:36.120434","indexId":"70042163","displayToPublicDate":"2009-10-01T00:00:00","publicationYear":"2009","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3769,"text":"Wildlife Disease Association Newsletter","active":true,"publicationSubtype":{"id":10}},"title":"National Wildlife Health Center's quarterly wildlife mortality report","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"Wildlife Disease Association","publisherLocation":"Lawrence, KS","usgsCitation":"Schuler, K., Ballmann, A., and White, C.L., 2009, National Wildlife Health Center's quarterly wildlife mortality report: Wildlife Disease Association Newsletter, no. October 2009, p. 9-12.","productDescription":"4 p.","startPage":"9","endPage":"12","ipdsId":"IP-016854","costCenters":[{"id":456,"text":"National Wildlife Health Center","active":true,"usgs":true}],"links":[{"id":264855,"rank":1,"type":{"id":15,"text":"Index Page"},"url":"https://www.wildlifedisease.org/PersonifyEbusiness/Resources/Publications/Newsletter/Archive"},{"id":264856,"rank":2,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"issue":"October 2009","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"50e08cc9e4b0fec3206ee2a7","contributors":{"authors":[{"text":"Schuler, Krysten","contributorId":53735,"corporation":false,"usgs":true,"family":"Schuler","given":"Krysten","affiliations":[],"preferred":false,"id":470876,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Ballmann, Anne 0000-0002-0380-056X","orcid":"https://orcid.org/0000-0002-0380-056X","contributorId":104631,"corporation":false,"usgs":true,"family":"Ballmann","given":"Anne","affiliations":[],"preferred":false,"id":470877,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"White, C. LeAnn 0000-0002-5004-5165 clwhite@usgs.gov","orcid":"https://orcid.org/0000-0002-5004-5165","contributorId":4315,"corporation":false,"usgs":true,"family":"White","given":"C.","email":"clwhite@usgs.gov","middleInitial":"LeAnn","affiliations":[{"id":456,"text":"National Wildlife Health Center","active":true,"usgs":true}],"preferred":true,"id":470875,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":97886,"text":"ofr20091215 - 2009 - Climax-Type Porphyry Molybdenum Deposits","interactions":[],"lastModifiedDate":"2012-02-10T00:11:50","indexId":"ofr20091215","displayToPublicDate":"2009-10-01T00:00:00","publicationYear":"2009","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":"2009-1215","title":"Climax-Type Porphyry Molybdenum Deposits","docAbstract":"Climax-type porphyry molybdenum deposits, as defined here, are extremely rare; thirteen deposits are known, all in western North America and ranging in age from Late Cretaceous to mainly Tertiary. They are consistently found in a postsubduction, extensional tectonic setting and are invariably associated with A-type granites that formed after peak activity of a magmatic cycle. The deposits consist of ore shells of quartz-molybdenite stockwork veins that lie above and surrounding the apices of cupola-like, highly evolved, calc-alkaline granite and subvolcanic rhyolite-porphyry bodies. These plutons are invariably enriched in fluorine (commonly >1 percent), rubidium (commonly >500 parts per million), and niobium-tantalum (Nb commonly >50 parts per million). The deposits are relatively high grade (typically 0.1-0.3 percent Mo) and may be very large (typically 100-1,000 million tons). Molybdenum, as MoS2, is the primary commodity in all known deposits.\r\n\r\nThe effect on surface-water quality owing to natural influx of water or sediment from a Climax-type mineralized area can extend many kilometers downstream from the mineralized area. Waste piles composed of quartz-silica-pyrite altered rocks will likely produce acidic drainage waters. The potential exists for concentrations of fluorine or rare metals in surface water and groundwater to exceed recommended limits for human consumption near both mined and unmined Climax-type deposits.","language":"ENGLISH","publisher":"U.S. Geological Survey","doi":"10.3133/ofr20091215","usgsCitation":"Ludington, S., and Plumlee, G.S., 2009, Climax-Type Porphyry Molybdenum Deposits: U.S. Geological Survey Open-File Report 2009-1215, 16 p., https://doi.org/10.3133/ofr20091215.","productDescription":"16 p.","onlineOnly":"Y","costCenters":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"links":[{"id":125503,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ofr_2009_1215.jpg"},{"id":13061,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2009/1215/","linkFileType":{"id":5,"text":"html"}}],"geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -140,15 ], [ -140,60 ], [ -75,60 ], [ -75,15 ], [ -140,15 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49b9e4b07f02db5cdb55","contributors":{"authors":[{"text":"Ludington, Steve","contributorId":106848,"corporation":false,"usgs":true,"family":"Ludington","given":"Steve","affiliations":[],"preferred":false,"id":303487,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Plumlee, Geoffrey S. 0000-0002-9607-5626 gplumlee@usgs.gov","orcid":"https://orcid.org/0000-0002-9607-5626","contributorId":960,"corporation":false,"usgs":true,"family":"Plumlee","given":"Geoffrey","email":"gplumlee@usgs.gov","middleInitial":"S.","affiliations":[{"id":211,"text":"Crustal Geophysics and Geochemistry Science Center","active":true,"usgs":true}],"preferred":true,"id":303486,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":97883,"text":"ofr20091213 - 2009 - Mississippi Valley-Type Lead-Zinc Deposit Model","interactions":[],"lastModifiedDate":"2012-02-02T00:15:03","indexId":"ofr20091213","displayToPublicDate":"2009-10-01T00:00:00","publicationYear":"2009","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":"2009-1213","title":"Mississippi Valley-Type Lead-Zinc Deposit Model","docAbstract":"Mississippi Valley-type (MVT) lead-zinc (Pb+Zn) deposits are found throughout the world, and these deposits are characteristically distributed over hundreds of square kilometers that define individual ore districts. The median size of individual MVT deposits is 7.0 million tonnes with grades of about 7.9 percent Pb+Zn metal. However, MVT deposits usually occur in extensive districts consisting of several to as many as 400 deposits. Nearly one-quarter of the world's sedimentary and volcanic rock-hosted Pb+Zn resources are found in these deposits, with by-product commodities including silver (Ag), copper (Cu), and indium (In) for some deposits. Environmentally, MVT deposits are less of a concern than other types of mineral deposits since the carbonate-host rocks mitigate many environmental concerns.","language":"ENGLISH","publisher":"U.S. Geological Survey","doi":"10.3133/ofr20091213","usgsCitation":"Leach, D.L., and Taylor, R.D., 2009, Mississippi Valley-Type Lead-Zinc Deposit Model: U.S. Geological Survey Open-File Report 2009-1213, iii, 5 p., https://doi.org/10.3133/ofr20091213.","productDescription":"iii, 5 p.","onlineOnly":"Y","costCenters":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"links":[{"id":118550,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ofr_2009_1213.jpg"},{"id":13058,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2009/1213/","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b05e4b07f02db699d0f","contributors":{"authors":[{"text":"Leach, David L.","contributorId":83902,"corporation":false,"usgs":true,"family":"Leach","given":"David","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":303454,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Taylor, Ryan D. 0000-0002-8845-5290 rtaylor@usgs.gov","orcid":"https://orcid.org/0000-0002-8845-5290","contributorId":3412,"corporation":false,"usgs":true,"family":"Taylor","given":"Ryan","email":"rtaylor@usgs.gov","middleInitial":"D.","affiliations":[{"id":171,"text":"Central Mineral and Environmental Resources Science Center","active":true,"usgs":true}],"preferred":true,"id":303453,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":97884,"text":"sir20095202 - 2009 - Production of a national 1:1,000,000-scale hydrography dataset for the United States: feature selection, simplification, and refinement","interactions":[],"lastModifiedDate":"2016-08-22T12:45:08","indexId":"sir20095202","displayToPublicDate":"2009-10-01T00:00:00","publicationYear":"2009","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":"2009-5202","title":"Production of a national 1:1,000,000-scale hydrography dataset for the United States: feature selection, simplification, and refinement","docAbstract":"<p>During 2006-09, the U.S. Geological Survey, in cooperation with the National Atlas of the United States, produced a 1:1,000,000-scale (1:1M) hydrography dataset comprising streams and waterbodies for the entire United States, including Puerto Rico and the U.S. Virgin Islands, for inclusion in the recompiled National Atlas. This report documents the methods used to select, simplify, and refine features in the 1:100,000-scale (1:100K) (1:63,360-scale in Alaska) National Hydrography Dataset to create the national 1:1M hydrography dataset. Custom tools and semi-automated processes were created to facilitate generalization of the 1:100K National Hydrography Dataset (1:63,360-scale in Alaska) to 1:1M on the basis of existing small-scale hydrography datasets. The first step in creating the new 1:1M dataset was to address feature selection and optimal data density in the streams network. Several existing methods were evaluated. The production method that was established for selecting features for inclusion in the 1:1M dataset uses a combination of the existing attributes and network in the National Hydrography Dataset and several of the concepts from the methods evaluated. The process for creating the 1:1M waterbodies dataset required a similar approach to that used for the streams dataset. Geometric simplification of features was the next step. Stream reaches and waterbodies indicated in the feature selection process were exported as new feature classes and then simplified using a geographic information system tool. The final step was refinement of the 1:1M streams and waterbodies. Refinement was done through the use of additional geographic information system tools.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/sir20095202","collaboration":"Prepared in cooperation with the National Atlas of the United States of America","usgsCitation":"Gary, R.H., Wilson, Z.D., Archuleta, C., Thompson, F.E., and Vrabel, J., 2009, Production of a national 1:1,000,000-scale hydrography dataset for the United States: feature selection, simplification, and refinement: U.S. Geological Survey Scientific Investigations Report 2009-5202, vi, 22 p., https://doi.org/10.3133/sir20095202.","productDescription":"vi, 22 p.","onlineOnly":"N","additionalOnlineFiles":"N","temporalStart":"2006-01-01","temporalEnd":"2009-12-31","costCenters":[{"id":583,"text":"Texas Water Science 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,{"id":97881,"text":"ofr20091177 - 2009 - Users' manual and installation guide for the EverVIEW Slice and Dice Tool (Version 1.0 Beta)","interactions":[],"lastModifiedDate":"2019-03-26T09:06:11","indexId":"ofr20091177","displayToPublicDate":"2009-10-01T00:00:00","publicationYear":"2009","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":"2009-1177","title":"Users' manual and installation guide for the EverVIEW Slice and Dice Tool (Version 1.0 Beta)","docAbstract":"Network Common Data Form (NetCDF) is a self-describing, machine-independent file format for storing array-oriented scientific data. Over the past few years, there has been a growing movement within the community of natural resource managers in The Everglades, Fla., to use NetCDF as the standard data container for datasets based on multidimensional arrays. As a consequence, a need arose for additional tools to view and manipulate NetCDF datasets, specifically to create subsets of large NetCDF files. To address this need, we created the EverVIEW Slice and Dice Tool to allow users to create subsets of grid-based NetCDF files. The major functions of this tool are (1) to subset NetCDF files both spatially and temporally; (2) to view the NetCDF data in table form; and (3) to export filtered data to a comma-separated value file format.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr20091177","usgsCitation":"Roszell, D., Conzelmann, C., Chimmula, S., Chandrasekaran, A., and Hunnicut, C., 2009, Users' manual and installation guide for the EverVIEW Slice and Dice Tool (Version 1.0 Beta): U.S. Geological Survey Open-File Report 2009-1177, v, 40 p., https://doi.org/10.3133/ofr20091177.","productDescription":"v, 40 p.","numberOfPages":"45","onlineOnly":"Y","costCenters":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"links":[{"id":125484,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ofr_2009_1177.jpg"},{"id":13056,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2009/1177/","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac7e4b07f02db67aeb8","contributors":{"authors":[{"text":"Roszell, Dustin","contributorId":100973,"corporation":false,"usgs":true,"family":"Roszell","given":"Dustin","affiliations":[],"preferred":false,"id":303449,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Conzelmann, Craig 0000-0002-4227-8719 conzelmannc@usgs.gov","orcid":"https://orcid.org/0000-0002-4227-8719","contributorId":2361,"corporation":false,"usgs":true,"family":"Conzelmann","given":"Craig","email":"conzelmannc@usgs.gov","affiliations":[{"id":17705,"text":"Wetland and Aquatic Research Center","active":true,"usgs":true},{"id":455,"text":"National Wetlands Research Center","active":true,"usgs":true}],"preferred":true,"id":303445,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Chimmula, Sumani","contributorId":45805,"corporation":false,"usgs":true,"family":"Chimmula","given":"Sumani","affiliations":[],"preferred":false,"id":303447,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Chandrasekaran, Anuradha","contributorId":23250,"corporation":false,"usgs":true,"family":"Chandrasekaran","given":"Anuradha","email":"","affiliations":[],"preferred":false,"id":303446,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Hunnicut, Christina 0000-0001-8624-6420","orcid":"https://orcid.org/0000-0001-8624-6420","contributorId":62317,"corporation":false,"usgs":true,"family":"Hunnicut","given":"Christina","affiliations":[{"id":17705,"text":"Wetland and Aquatic Research Center","active":true,"usgs":true}],"preferred":false,"id":303448,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":97880,"text":"tm5A10 - 2009 - Determination of glyphosate, its degradation product aminomethylphosphonic acid, and glufosinate, in water by isotope dilution and online solid-phase extraction and liquid chromatography/tandem mass spectrometry","interactions":[],"lastModifiedDate":"2019-08-15T12:38:42","indexId":"tm5A10","displayToPublicDate":"2009-10-01T00:00:00","publicationYear":"2009","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":335,"text":"Techniques and Methods","code":"TM","onlineIssn":"2328-7055","printIssn":"2328-7047","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"5-A10","title":"Determination of glyphosate, its degradation product aminomethylphosphonic acid, and glufosinate, in water by isotope dilution and online solid-phase extraction and liquid chromatography/tandem mass spectrometry","docAbstract":"The U.S. Geological Survey method (0-2141-09) presented is approved for the determination of glyphosate, its degradation product aminomethylphosphonic acid (AMPA), and glufosinate in water. It was was validated to demonstrate the method detection levels (MDL), compare isotope dilution to standard addition, and evaluate method and compound stability. The original method USGS analytical method 0-2136-01 was developed using liquid chromatography/mass spectrometry and quantitation by standard addition. Lower method detection levels and increased specificity were achieved in the modified method, 0-2141-09, by using liquid chromatography/tandem mass spectrometry (LC/MS/MS). The use of isotope dilution for glyphosate and AMPA and pseudo isotope dilution of glufosinate in place of standard addition was evaluated. Stable-isotope labeled AMPA and glyphosate were used as the isotope dilution standards. In addition, the stability of glyphosate and AMPA was studied in raw filtered and derivatized water samples.\r\n\r\nThe stable-isotope labeled glyphosate and AMPA standards were added to each water sample and the samples then derivatized with 9-fluorenylmethylchloroformate. After derivatization, samples were concentrated using automated online solid-phase extraction (SPE) followed by elution in-line with the LC mobile phase; the compounds separated and then were analyzed by LC/MS/MS using electrospray ionization in negative-ion mode with multiple-reaction monitoring. The deprotonated derivatized parent molecule and two daughter-ion transition pairs were identified and optimized for glyphosate, AMPA, glufosinate, and the glyphosate and AMPA stable-isotope labeled internal standards.\r\n\r\nQuantitative comparison between standard addition and isotope dilution was conducted using 473 samples analyzed between April 2004 and June 2006. The mean percent difference and relative standard deviation between the two quantitation methods was 7.6 plus or minus 6.30 (n = 179), AMPA 9.6 plus or minus 8.35 (n = 206), and glufosinate 9.3 plus or minus 9.16 (n = 16).\r\n\r\nThe analytical variation of the method, comparison of quantitation by isotope dilution and multipoint linear regressed standard curves, and method detection levels were evaluated by analyzing six sets of distilled-water, groundwater, and surface-water samples spiked in duplicate at 0.0, 0.05, 0.10 and 0.50 microgram per liter and analyzed on 6 different days during 1 month. The grand means of the normalized concentration percentage recovery for glyphosate, AMPA, and glufosinate among all three matrices and spiked concentrations ranged from 99 to 114 plus or minus 2 to 7 percent of the expected spiked concentration. The grand mean of the percentage difference between concentrations calculated by standard addition and linear regressed multipoint standard curves ranged from 8 to 15 plus or minus 2 to 9 percent for the three compounds. The method reporting levels calculated from all the 0.05- microgram per liter spiked samples were 0.02 microgram per liter for all three compounds.\r\n\r\nCompound stability experiments were conducted on 10 samples derivatized four times for periods between 136 to 269 days. The glyphosate and AMPA concentrations remained relatively constant in samples held up to 136 days before derivatization. The half life of glyphosate varied from 169 to 223 days in the underivatized samples. Derivatized samples were analyzed the day after derivitization, and again 54 and 64 days after derivatization. The derivatized samples analyzed at days 52 and 64 were within 20 percent of the concentrations of the derivatized samples analyzed the day after derivatization.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/tm5A10","usgsCitation":"Meyer, M.T., Loftin, K.A., Lee, E., Hinshaw, G.H., Dietze, J.E., and Scribner, E.A., 2009, Determination of glyphosate, its degradation product aminomethylphosphonic acid, and glufosinate, in water by isotope dilution and online solid-phase extraction and liquid chromatography/tandem mass spectrometry: U.S. Geological Survey Techniques and Methods 5-A10, vi, 33 p., https://doi.org/10.3133/tm5A10.","productDescription":"vi, 33 p.","costCenters":[{"id":353,"text":"Kansas Water Science Center","active":false,"usgs":true},{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":13055,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/tm/tm5a10/","linkFileType":{"id":5,"text":"html"}},{"id":118482,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/tm_5_a10.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aa8e4b07f02db6679b0","contributors":{"authors":[{"text":"Meyer, Michael T. 0000-0001-6006-7985 mmeyer@usgs.gov","orcid":"https://orcid.org/0000-0001-6006-7985","contributorId":866,"corporation":false,"usgs":true,"family":"Meyer","given":"Michael","email":"mmeyer@usgs.gov","middleInitial":"T.","affiliations":[{"id":353,"text":"Kansas Water Science Center","active":false,"usgs":true}],"preferred":true,"id":303439,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Loftin, Keith A. 0000-0001-5291-876X kloftin@usgs.gov","orcid":"https://orcid.org/0000-0001-5291-876X","contributorId":868,"corporation":false,"usgs":true,"family":"Loftin","given":"Keith","email":"kloftin@usgs.gov","middleInitial":"A.","affiliations":[{"id":353,"text":"Kansas Water Science Center","active":false,"usgs":true}],"preferred":true,"id":303440,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Lee, Edward A.","contributorId":47475,"corporation":false,"usgs":true,"family":"Lee","given":"Edward A.","affiliations":[],"preferred":false,"id":303442,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Hinshaw, Gary H.","contributorId":80774,"corporation":false,"usgs":true,"family":"Hinshaw","given":"Gary","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":303444,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Dietze, Julie E. 0000-0002-5936-5739 juliec@usgs.gov","orcid":"https://orcid.org/0000-0002-5936-5739","contributorId":3939,"corporation":false,"usgs":true,"family":"Dietze","given":"Julie","email":"juliec@usgs.gov","middleInitial":"E.","affiliations":[{"id":353,"text":"Kansas Water Science Center","active":false,"usgs":true}],"preferred":true,"id":303441,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Scribner, Elisabeth A.","contributorId":80265,"corporation":false,"usgs":true,"family":"Scribner","given":"Elisabeth","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":303443,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}}
,{"id":97888,"text":"ds438 - 2009 - Data from a Thick Unsaturated Zone Underlying Two Artificial Recharge Sites along Oro Grande Wash in the Western Part of the Mojave Desert, near Victorville, San Bernardino County, California, 2001-2006","interactions":[],"lastModifiedDate":"2012-03-08T17:16:27","indexId":"ds438","displayToPublicDate":"2009-10-01T00:00:00","publicationYear":"2009","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":"438","title":"Data from a Thick Unsaturated Zone Underlying Two Artificial Recharge Sites along Oro Grande Wash in the Western Part of the Mojave Desert, near Victorville, San Bernardino County, California, 2001-2006","docAbstract":"This report presents data on the physical and hydraulic properties of unsaturated alluvial deposits and on the chemical and isotopic composition of water collected at two recharge sites in the western part of the Mojave Desert, near Victorville, California, from 2001 to 2006. Unsaturated-zone monitoring sites were installed adjacent to the two recharge ponds using the ODEX air-hammer and air rotary method to depths of about 460 feet and 269 feet below land surface. Each of the two unsaturated-zone monitoring sites included a water-table well, matric-potential sensors, and suction-cup lysimeters installed in a single bore hole. Drilling procedures, lithologic and geophysical data, and site construction and instrumentation are described. Core material was analyzed for water content, bulk density, water potential, particle size, and water retention. The chemical composition of leachate from almost 400 samples of cores and cuttings was determined. Water from suction-cup lysimeters also was analyzed for chemical and isotopic composition. In addition, data on the chemical and isotopic composition of groundwater from the two water-table wells are reported along with chemical and isotopic composition of the surface water in the recharge ponds.","language":"ENGLISH","publisher":"U.S. Geological Survey","doi":"10.3133/ds438","collaboration":"Prepared in cooperation with the Victor Valley Water District, the Baldy Mesa Water District, and the Mojave Water Agency","usgsCitation":"Clark, D.A., Izbicki, J., Johnson, R.D., and Land, M., 2009, Data from a Thick Unsaturated Zone Underlying Two Artificial Recharge Sites along Oro Grande Wash in the Western Part of the Mojave Desert, near Victorville, San Bernardino County, California, 2001-2006: U.S. Geological Survey Data Series 438, viii, 93 p., https://doi.org/10.3133/ds438.","productDescription":"viii, 93 p.","costCenters":[{"id":154,"text":"California Water Science Center","active":true,"usgs":true}],"links":[{"id":126842,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ds_438.jpg"},{"id":13063,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/ds/438/","linkFileType":{"id":5,"text":"html"}}],"geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -117.75,34.25 ], [ -117.75,34.75 ], [ -117.16666666666667,34.75 ], [ -117.16666666666667,34.25 ], [ -117.75,34.25 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac9e4b07f02db67c8a4","contributors":{"authors":[{"text":"Clark, Dennis A. daclark@usgs.gov","contributorId":1477,"corporation":false,"usgs":true,"family":"Clark","given":"Dennis","email":"daclark@usgs.gov","middleInitial":"A.","affiliations":[],"preferred":true,"id":303491,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Izbicki, John A. 0000-0003-0816-4408 jaizbick@usgs.gov","orcid":"https://orcid.org/0000-0003-0816-4408","contributorId":1375,"corporation":false,"usgs":true,"family":"Izbicki","given":"John A.","email":"jaizbick@usgs.gov","affiliations":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"preferred":false,"id":303490,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Johnson, Russell D.","contributorId":21829,"corporation":false,"usgs":true,"family":"Johnson","given":"Russell","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":303493,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Land, Michael 0000-0001-5141-0307 mtland@usgs.gov","orcid":"https://orcid.org/0000-0001-5141-0307","contributorId":1479,"corporation":false,"usgs":true,"family":"Land","given":"Michael","email":"mtland@usgs.gov","affiliations":[{"id":154,"text":"California Water Science Center","active":true,"usgs":true}],"preferred":false,"id":303492,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":97879,"text":"ofr20091199 - 2009 - Summary of West Virginia Water-Resource Data through September 2008","interactions":[],"lastModifiedDate":"2012-03-08T17:16:28","indexId":"ofr20091199","displayToPublicDate":"2009-10-01T00:00:00","publicationYear":"2009","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":"2009-1199","title":"Summary of West Virginia Water-Resource Data through September 2008","docAbstract":"The West Virginia Water Science Center of the U.S. Geological Survey, in cooperation with State and Federal agencies, obtains a large amount of data pertaining to the water resources of West Virginia each water year. A water year is the 12-month period beginning October 1 and ending September 30. These data, accumulated during many years, constitute a valuable database for developing an improved understanding of the water resources of the State. These data are maintained in the National Water Information System (NWIS) and are available through its World-Wide Web interface, NWISWeb, at http://waterdata.usgs.gov/wv/nwis. Data can be retrieved in a variety of common formats, and a tutorial is available at http://nwis.waterdata.usgs.gov/tutorial. Location information for all continuous-record gaging stations operated in West Virginia through September 2008 is provided in this report, as well as statistical summaries of the available daily records. This report can serve as an index to the daily records data available on the World-Wide Web.\r\n\r\nHydrologic data for nearly all of the gaging stations identified in this report are also available in the annual publication series titled Water-Resources Data - West Virginia. This series of annual reports for West Virginia began with the 1961 water year with a report that contained only data relating to quantities of surface water. For the 1964 water year, a similar report was introduced that contained only data relating to water quality. Beginning with the 1975 water year, the report format was changed to include data on quantities of surface water, quality of surface water and groundwater, and groundwater levels.\r\n\r\nPrior to the introduction of the Water-Resources Data - West Virginia series and for several water years concurrent with it, water-resources data for West Virginia were published in U.S. Geological Survey Water-Supply Papers. Data on stream discharge and stage and on lake or reservoir contents and stage through September 1960 were published annually under the title Surface-Water Supply of the United States, Parts 6A and 6B. For the 1961 through 1970 water years, the data were published in two 5-year reports. Data on chemical quality, temperature, and suspended sediment for the 1941 through 1970 water years were published annually under the title Quality of Surface Water of the United States, and water levels for the 1935 through 1974 water years were published under the title Ground-Water Levels in the United States. Many of the above mentioned Water-Supply Papers are available at the USGS Publications Warehouse (http://pubs.er.usgs.gov), and most of the others may be found in the collections of large libraries or may be purchased from the U.S. Geological Survey, Books and Open-File Reports, Federal Center, Box 25425, Denver, Colorado 80225.\r\n\r\nAnnual reports on hydrologic data are published by the Geological Survey for all states, and each has an identification number consisting of the two-letter state abbreviation, the last two digits of the water year, and the volume number. For example, the 2005 water year report for West Virginia is identified as U.S. Geological Survey Water-Data Report WV-05-01. Water-Data Reports for West Virginia for 2001-2005 are available online at http://pubs.usgs.gov/wdr/#WV. Water-Data Reports for water years prior to 2006 are for sale in paper copy or microfiche by the National Technical Information Service, U.S. Department of Commerce, Springfield, Virginia 22161. Since the 2006 water year, the report is published online only and is available at http://wdr.water.usgs.gov/.\r\n\r\nWhen substantial errors in published records are discovered, the records are revised. Such revisions are routine and are made to records regardless of the age of the original records. Revisions have been made for many stations for which data are published in this report. The USGS National Water Information System always contains the most recent data revisions. For critical a","language":"ENGLISH","publisher":"U.S. Geological Survey","doi":"10.3133/ofr20091199","collaboration":"Prepared in cooperation with the West Virginia Division of Water and Waste Management","usgsCitation":"Evaldi, R., Ward, S., and White, J., 2009, Summary of West Virginia Water-Resource Data through September 2008: U.S. Geological Survey Open-File Report 2009-1199, xxi, 326 p., https://doi.org/10.3133/ofr20091199.","productDescription":"xxi, 326 p.","costCenters":[{"id":642,"text":"West Virginia Water Science Center","active":true,"usgs":true}],"links":[{"id":118539,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ofr_2009_1199.jpg"},{"id":13054,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2009/1199/","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b04e4b07f02db6993b3","contributors":{"authors":[{"text":"Evaldi, R. D.","contributorId":93909,"corporation":false,"usgs":true,"family":"Evaldi","given":"R. D.","affiliations":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"preferred":false,"id":303437,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Ward, S.M.","contributorId":93920,"corporation":false,"usgs":true,"family":"Ward","given":"S.M.","email":"","affiliations":[],"preferred":false,"id":303438,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"White, J.S.","contributorId":66362,"corporation":false,"usgs":true,"family":"White","given":"J.S.","email":"","affiliations":[],"preferred":false,"id":303436,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":97878,"text":"ofr20091158 - 2009 - Recent subsidence and erosion at diverse wetland sites in the southeastern Mississippi Delta Plain","interactions":[],"lastModifiedDate":"2019-09-18T15:45:04","indexId":"ofr20091158","displayToPublicDate":"2009-10-01T00:00:00","publicationYear":"2009","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":"2009-1158","title":"Recent subsidence and erosion at diverse wetland sites in the southeastern Mississippi Delta Plain","docAbstract":"A prior study (U.S. Geological Survey Open-File Report 2005-1216) examined historical land- and water-area changes and estimated magnitudes of land subsidence and erosion at five wetland sites in the Terrebonne hydrologic basin of the Mississippi delta plain. The present study extends that work by analyzing interior wetland loss and relative magnitudes of subsidence and erosion at five additional wetland sites in the adjacent Barataria hydrologic basin. The Barataria basin sites were selected for their diverse physical settings and their recent (post-1978) conversion from marsh to open water. Historical aerial photography, datum-corrected marsh elevations and water depths, sediment cores, and radiocarbon dates were integrated to evaluate land-water changes in the Mississippi delta plain on both historical and geological time scales. \r\n\r\nThe thickness of the organic-rich sediments (peat) and the elevation of the stratigraphic contact between peat and underlying mud were compared at marsh and open-water sites across areas of formerly continuous marsh to estimate magnitudes of recent delta-plain elevation loss caused by vertical erosion and subsidence of the wetlands. Results of these analyses indicate that erosion exceeded subsidence at most of the study areas, although both processes have contributed to historical wetland loss. Comparison of these results with prior studies indicates that subsidence largely caused rapid interior wetland loss in the Terrebonne basin before 1978, whereas erosional processes primarily caused more gradual interior wetland loss in the Barataria basin after 1978.\r\n\r\nDecadal variations in rates of relative sea-level rise at a National Ocean Service tide gage, elevation changes between repeat benchmark-leveling surveys, and GPS height monitoring at three National Geodetic Survey Continuously Operating Reference Stations indicate that subsidence rates since the early 1990s are substantially lower than those previously reported and are similar in magnitude to time-averaged subsidence rates at geological time scales. The historical decrease in land-loss rates across the Mississippi delta plain generally is consistent with the recent decrease in subsidence rates within the same region.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr20091158","isbn":"9781411325296","usgsCitation":"Morton, R., Bernier, J., and Kelso, K.W., 2009, Recent subsidence and erosion at diverse wetland sites in the southeastern Mississippi Delta Plain: U.S. Geological Survey Open-File Report 2009-1158, vi, 221 p. , https://doi.org/10.3133/ofr20091158.","productDescription":"vi, 221 p. ","additionalOnlineFiles":"Y","costCenters":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"links":[{"id":126598,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ofr_2009_1158.jpg"},{"id":13053,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2009/1158/","linkFileType":{"id":5,"text":"html"}},{"id":367516,"rank":3,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/2009/1158/pdf/ofr2009-1158.pdf"}],"country":"United States","state":"Louisiana","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -90.75,29 ], [ -90.75,30 ], [ -89.25,30 ], [ -89.25,29 ], [ -90.75,29 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a51e4b07f02db62a2d5","contributors":{"authors":[{"text":"Morton, Robert A.","contributorId":88333,"corporation":false,"usgs":true,"family":"Morton","given":"Robert A.","affiliations":[],"preferred":false,"id":303435,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bernier, Julie 0000-0002-9918-5353 jbernier@usgs.gov","orcid":"https://orcid.org/0000-0002-9918-5353","contributorId":3549,"corporation":false,"usgs":true,"family":"Bernier","given":"Julie","email":"jbernier@usgs.gov","affiliations":[{"id":574,"text":"St. Petersburg Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":true,"id":303433,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Kelso, Kyle W. 0000-0003-0615-242X kkelso@usgs.gov","orcid":"https://orcid.org/0000-0003-0615-242X","contributorId":4307,"corporation":false,"usgs":true,"family":"Kelso","given":"Kyle","email":"kkelso@usgs.gov","middleInitial":"W.","affiliations":[{"id":574,"text":"St. Petersburg Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":true,"id":303434,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":97877,"text":"sir20095153 - 2009 - Hydrogeology and Ground-Water Flow in the Opequon Creek Watershed area, Virginia and West Virginia","interactions":[],"lastModifiedDate":"2024-03-05T12:10:33.414941","indexId":"sir20095153","displayToPublicDate":"2009-10-01T00:00:00","publicationYear":"2009","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":"2009-5153","title":"Hydrogeology and Ground-Water Flow in the Opequon Creek Watershed area, Virginia and West Virginia","docAbstract":"Due to increasing population and economic development in the northern Shenandoah Valley of Virginia and West Virginia, water availability has become a primary concern for water-resource managers in the region. To address these issues, the U.S. Geological Survey (USGS), in cooperation with the West Virginia Department of Health and Human Services and the West Virginia Department of Environmental Protection, developed a numerical steady-state simulation of ground-water flow for the 1,013-square-kilometer Opequon Creek watershed area. The model was based on data aggregated for several recently completed and ongoing USGS hydrogeologic investigations conducted in Jefferson, Berkeley, and Morgan Counties in West Virginia and Clarke, Frederick, and Warren Counties in Virginia. A previous detailed hydrogeologic assessment of the watershed area of Hopewell Run (tributary to the Opequon Creek), which includes the USGS Leetown Science Center in Jefferson County, West Virginia, provided key understanding of ground-water flow processes in the aquifer.\r\n\r\nThe ground-water flow model developed for the Opequon Creek watershed area is a steady-state, three-layer representation of ground-water flow in the region. The primary objective of the simulation was to develop water budgets for average and drought hydrologic conditions. The simulation results can provide water managers with preliminary estimates on which water-resource decisions may be based.\r\n\r\nResults of the ground-water flow simulation of the Opequon Creek watershed area indicate that hydrogeologic concepts developed for the Hopewell Run watershed area can be extrapolated to the larger watershed model. Sensitivity analyses conducted as part of the current modeling effort and geographic information system analyses of spring location and yield reveal that thrust and cross-strike faults and low-permeability bedding, which provide structural and lithologic controls, respectively, on ground-water flow, must be incorporated into the model to develop a realistic simulation of ground-water flow in the larger Opequon Creek watershed area.\r\n\r\nIn the model, recharge for average hydrologic conditions was 689 m3/d/km2 (cubic meters per day per square kilometer) over the entire Opequon Creek watershed area. Mean and median measured base flows at the streamflow-gaging station on the Opequon Creek near Martinsburg, West Virginia, were 604,384 and 349,907 m3/d (cubic meters per day), respectively. The simulated base flow of 432,834 m3/d fell between the mean and median measured stream base flows for the station. Simulated base-flow yields for subwatersheds during average conditions ranged from 0 to 2,643 m3/d/km2, and the median for the entire Opequon Creek watershed area was 557 m3/d/km2.\r\n\r\nA drought was simulated by reducing model recharge by 40 percent, a rate that approximates the recharge during the prolonged 16-month drought that affected the region from November 1998 to February 2000. Mean and median measured streamflows for the Opequon Creek watershed area at the Martinsburg, West Virginia, streamflow-gaging station during the 1999 drought were 341,098 and 216,551 m3/d, respectively. The simulated drought base flow at the station of 252,356 m3/d is within the range of flows measured during the 1999 drought. Recharge was 413 m3/d/km2 over the entire watershed during the simulated drought, and was 388 m3/d/km2 at the gaging station. Simulated base-flow yields for drought conditions ranged from 0 to 1,865 m3/d/km2 and averaged 327 m3/d/km2 over the entire Opequon Creek watershed.\r\n\r\nWater budgets developed from the simulation results indicate a substantial component of direct ground-water discharge to the Potomac River. This phenomenon had long been suspected but had not been quantified. During average conditions, approximately 564,176 m3/d of base flow discharges to the Potomac River. An additional 124,379 m3/d of ground water is also estimated to discharge directly to the Potomac River and rep","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/sir20095153","collaboration":"Prepared in cooperation with the West Virginia Department of Health and Human Services and the West Virginia Department of Environmental Protection","usgsCitation":"Kozar, M.D., and Weary, D.J., 2009, Hydrogeology and Ground-Water Flow in the Opequon Creek Watershed area, Virginia and West Virginia: U.S. Geological Survey Scientific Investigations Report 2009-5153, vi, 63 p., https://doi.org/10.3133/sir20095153.","productDescription":"vi, 63 p.","temporalStart":"1998-11-01","temporalEnd":"2000-02-28","costCenters":[{"id":365,"text":"Leetown Science Center","active":true,"usgs":true},{"id":50464,"text":"Eastern Ecological Science Center","active":true,"usgs":true}],"links":[{"id":118456,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/sir_2009_5153.jpg"},{"id":13052,"rank":2,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/sir/2009/5153/","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a4de4b07f02db627839","contributors":{"authors":[{"text":"Kozar, Mark D. 0000-0001-7755-7657 mdkozar@usgs.gov","orcid":"https://orcid.org/0000-0001-7755-7657","contributorId":1963,"corporation":false,"usgs":true,"family":"Kozar","given":"Mark","email":"mdkozar@usgs.gov","middleInitial":"D.","affiliations":[{"id":37280,"text":"Virginia and West Virginia Water Science Center ","active":true,"usgs":true}],"preferred":true,"id":303432,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Weary, David J. 0000-0002-6115-6397 dweary@usgs.gov","orcid":"https://orcid.org/0000-0002-6115-6397","contributorId":545,"corporation":false,"usgs":true,"family":"Weary","given":"David","email":"dweary@usgs.gov","middleInitial":"J.","affiliations":[{"id":40020,"text":"Florence Bascom Geoscience Center","active":true,"usgs":true},{"id":243,"text":"Eastern Geology and Paleoclimate Science Center","active":true,"usgs":true}],"preferred":true,"id":303431,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":97875,"text":"sir20095193 - 2009 - Vegetation Status of the Keoladeo National Park, Bharatpur, Rajasthan, India (April 2009)","interactions":[],"lastModifiedDate":"2012-02-02T00:14:26","indexId":"sir20095193","displayToPublicDate":"2009-10-01T00:00:00","publicationYear":"2009","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":"2009-5193","title":"Vegetation Status of the Keoladeo National Park, Bharatpur, Rajasthan, India (April 2009)","docAbstract":"The biodiversity of aquatic plant species may be reduced in the future by drought and/or climate change in monsoonal wetlands. After a number of years of low water levels, the aquatic vegetation of the Keoladeo National Park in Bharatpur, Rajasthan, India, was assessed. Though likely reduced in areal extent, most of the aquatic species were found in locations in the park that contained the seed bank of aquatic species in the 1980s. Some of the species of concern observed included Cyperus rotundus, Nymphoides indica, Paspalum distichum, Potamogeton pectinatus, Scirpus tuberosus, and Vallisneria natans. While it is likely that the abundance of these species has declined over time, this cannot be determined quantitatively without detailed field studies designed to replicate the 1980s analyses.","language":"ENGLISH","publisher":"U.S. Geological Survey","doi":"10.3133/sir20095193","usgsCitation":"Middleton, B.A., 2009, Vegetation Status of the Keoladeo National Park, Bharatpur, Rajasthan, India (April 2009): U.S. Geological Survey Scientific Investigations Report 2009-5193, iv, 8 p., https://doi.org/10.3133/sir20095193.","productDescription":"iv, 8 p.","onlineOnly":"Y","temporalStart":"2009-04-01","temporalEnd":"2009-04-30","costCenters":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"links":[{"id":118492,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/sir_2009_5193.jpg"},{"id":13050,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/sir/2009/5193/","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4affe4b07f02db697df7","contributors":{"authors":[{"text":"Middleton, Beth A. 0000-0002-1220-2326 middletonb@usgs.gov","orcid":"https://orcid.org/0000-0002-1220-2326","contributorId":2029,"corporation":false,"usgs":true,"family":"Middleton","given":"Beth","email":"middletonb@usgs.gov","middleInitial":"A.","affiliations":[{"id":17705,"text":"Wetland and Aquatic Research Center","active":true,"usgs":true}],"preferred":true,"id":303426,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":97874,"text":"fs20093075 - 2009 - Acid rain effects on Adirondack streams— Results from the 2003–05 Western Adirondack Stream Survey (the WASS Project)","interactions":[],"lastModifiedDate":"2021-08-31T21:36:29.730555","indexId":"fs20093075","displayToPublicDate":"2009-10-01T00:00:00","publicationYear":"2009","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":"2009-3075","title":"Acid rain effects on Adirondack streams— Results from the 2003–05 Western Adirondack Stream Survey (the WASS Project)","docAbstract":"Traditionally lakes have been the focus of acid rain assessments in the Adirondack region of New York. However, there is a growing recognition of the importance of streams as environmental indicators. Streams, like lakes, also provide important aquatic habitat, but streams more closely reflect acid rain effects on soils and forests and are more prone to acidification than lakes. Therefore, a large-scale assessment of streams was undertaken in the drainage basins of the Oswegatchie and Black Rivers; an area of 4,585 km2 in the western Adirondack region where acid rain levels tend to be highest in New York State.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/fs20093075","usgsCitation":"Lawrence, G.B., Roy, K.M., Baldigo, B.P., Simonin, H.A., Passy, S.I., Bode, R.W., and Capone, S.B., 2009, Acid rain effects on Adirondack streams— Results from the 2003–05 Western Adirondack Stream Survey (the WASS Project): U.S. Geological Survey Fact Sheet 2009-3075, 6 p., https://doi.org/10.3133/fs20093075.","productDescription":"6 p.","temporalStart":"2003-01-01","temporalEnd":"2005-12-31","costCenters":[{"id":474,"text":"New York Water Science Center","active":true,"usgs":true}],"links":[{"id":118571,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/fs_2009_3075.jpg"},{"id":13049,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/fs/2009/3075/","linkFileType":{"id":5,"text":"html"}},{"id":388491,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_87429.htm"}],"country":"United States","state":"New York","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -75.5,43.25 ], [ -75.5,44.5 ], [ -74.5,44.5 ], [ -74.5,43.25 ], [ -75.5,43.25 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b13e4b07f02db6a31e7","contributors":{"authors":[{"text":"Lawrence, Gregory B. 0000-0002-8035-2350 glawrenc@usgs.gov","orcid":"https://orcid.org/0000-0002-8035-2350","contributorId":867,"corporation":false,"usgs":true,"family":"Lawrence","given":"Gregory","email":"glawrenc@usgs.gov","middleInitial":"B.","affiliations":[{"id":474,"text":"New York Water Science Center","active":true,"usgs":true}],"preferred":true,"id":303419,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Roy, Karen M.","contributorId":16942,"corporation":false,"usgs":true,"family":"Roy","given":"Karen","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":303421,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Baldigo, Barry P. 0000-0002-9862-9119 bbaldigo@usgs.gov","orcid":"https://orcid.org/0000-0002-9862-9119","contributorId":1234,"corporation":false,"usgs":true,"family":"Baldigo","given":"Barry","email":"bbaldigo@usgs.gov","middleInitial":"P.","affiliations":[{"id":474,"text":"New York Water Science Center","active":true,"usgs":true}],"preferred":true,"id":303420,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Simonin, Howard A.","contributorId":90841,"corporation":false,"usgs":true,"family":"Simonin","given":"Howard","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":303425,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Passy, Sophia I.","contributorId":49067,"corporation":false,"usgs":true,"family":"Passy","given":"Sophia","email":"","middleInitial":"I.","affiliations":[],"preferred":false,"id":303424,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Bode, Robert W.","contributorId":47856,"corporation":false,"usgs":true,"family":"Bode","given":"Robert","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":303423,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Capone, Susan B.","contributorId":20438,"corporation":false,"usgs":true,"family":"Capone","given":"Susan","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":303422,"contributorType":{"id":1,"text":"Authors"},"rank":7}]}}
,{"id":97873,"text":"ofr20091209 - 2009 - Geologic Criteria for the Assessment of Sedimentary Exhalative (Sedex) Zn-Pb-Ag Deposits","interactions":[],"lastModifiedDate":"2012-02-02T00:14:27","indexId":"ofr20091209","displayToPublicDate":"2009-10-01T00:00:00","publicationYear":"2009","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":"2009-1209","title":"Geologic Criteria for the Assessment of Sedimentary Exhalative (Sedex) Zn-Pb-Ag Deposits","docAbstract":"Sedex deposits account for more than 50 percent of the world's zinc and lead reserves and furnish more than 25 percent of the world's production of these two metals. This report draws on previous syntheses as well as on topical studies of deposits in sedex basins to determine the characteristics and processes that produced sedex deposits. This analysis also uses studies of the tectonic, sedimentary, and fluid evolution of modern and ancient sedimentary basins and mass balance constraints to identify the hydrothermal processes that are required to produce sedex deposits.\r\n\r\nThis report demonstrates how a genetic model can be translated into geologic criteria that can be used in the U.S. Geological Survey National Assessments for sedex zinc-lead-silver deposits to define permissive tracts, assess the relative prospectivity of permissive tracts, and map favorability within permissive tracts.","language":"ENGLISH","publisher":"U.S. Geological Survey","doi":"10.3133/ofr20091209","usgsCitation":"Emsbo, P., 2009, Geologic Criteria for the Assessment of Sedimentary Exhalative (Sedex) Zn-Pb-Ag Deposits: U.S. Geological Survey Open-File Report 2009-1209, iv, 21 p., https://doi.org/10.3133/ofr20091209.","productDescription":"iv, 21 p.","onlineOnly":"Y","costCenters":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"links":[{"id":118548,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ofr_2009_1209.jpg"},{"id":13048,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2009/1209/","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1ae4b07f02db6a86dd","contributors":{"authors":[{"text":"Emsbo, Poul 0000-0001-9421-201X pemsbo@usgs.gov","orcid":"https://orcid.org/0000-0001-9421-201X","contributorId":997,"corporation":false,"usgs":true,"family":"Emsbo","given":"Poul","email":"pemsbo@usgs.gov","affiliations":[{"id":35995,"text":"Geology, Geophysics, and Geochemistry Science Center","active":true,"usgs":true},{"id":171,"text":"Central Mineral and Environmental Resources Science Center","active":true,"usgs":true}],"preferred":true,"id":303418,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":97871,"text":"ds473 - 2009 - Summary of Seepage Investigations in the Yakima River Basin, Washington","interactions":[],"lastModifiedDate":"2012-03-08T17:16:26","indexId":"ds473","displayToPublicDate":"2009-10-01T00:00:00","publicationYear":"2009","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":"473","title":"Summary of Seepage Investigations in the Yakima River Basin, Washington","docAbstract":"Discharge data collected by the U.S. Geological Survey, Washington State Department of Ecology, and Yakama Nation for seepage investigations in the Yakima River basin are made available as downloadable Microsoft Excel files. These data were collected for more than a century at various times for several different studies and are now available in one location to facilitate future analysis by interested parties.","language":"ENGLISH","publisher":"U.S. Geological Survey","doi":"10.3133/ds473","collaboration":"Prepared in cooperation with the Bureau of Reclamation, Washington State Department of Ecology, and Yakama Nation","usgsCitation":"Magirl, C., Julich, R.J., Welch, W., Curran, C., Mastin, M.C., and Vaccaro, J.J., 2009, Summary of Seepage Investigations in the Yakima River Basin, Washington: U.S. Geological Survey Data Series 473, Available online, https://doi.org/10.3133/ds473.","productDescription":"Available online","onlineOnly":"Y","additionalOnlineFiles":"Y","costCenters":[{"id":622,"text":"Washington Water Science Center","active":true,"usgs":true}],"links":[{"id":118594,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ds_473.jpg"},{"id":13046,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/ds/473/","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b03e4b07f02db698fa6","contributors":{"authors":[{"text":"Magirl, C. S. 0000-0002-9922-6549","orcid":"https://orcid.org/0000-0002-9922-6549","contributorId":73699,"corporation":false,"usgs":true,"family":"Magirl","given":"C. S.","affiliations":[],"preferred":false,"id":303412,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Julich, R. J.","contributorId":85666,"corporation":false,"usgs":true,"family":"Julich","given":"R.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":303413,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Welch, W.B.","contributorId":53895,"corporation":false,"usgs":true,"family":"Welch","given":"W.B.","affiliations":[],"preferred":false,"id":303410,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Curran, C.R.","contributorId":72082,"corporation":false,"usgs":true,"family":"Curran","given":"C.R.","email":"","affiliations":[],"preferred":false,"id":303411,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Mastin, M. C.","contributorId":90782,"corporation":false,"usgs":true,"family":"Mastin","given":"M.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":303414,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Vaccaro, J. J.","contributorId":48173,"corporation":false,"usgs":true,"family":"Vaccaro","given":"J.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":303409,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}}
,{"id":97869,"text":"ofr20091194 - 2009 - Preliminary Physical Stratigraphy and Geophysical Data From the USGS Dixon Core, Onslow County, North Carolina","interactions":[],"lastModifiedDate":"2012-02-10T00:11:47","indexId":"ofr20091194","displayToPublicDate":"2009-10-01T00:00:00","publicationYear":"2009","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":"2009-1194","title":"Preliminary Physical Stratigraphy and Geophysical Data From the USGS Dixon Core, Onslow County, North Carolina","docAbstract":"In October through November 2006, scientists from the U. S. Geological Survey (USGS) Eastern Region Earth Surface Processes Team (EESPT) and the Raleigh (N.C.) Water Science Center (WSC), in cooperation with the North Carolina Geological Survey (NCGS) and the Onslow County Water and Sewer Authority (ONWASA), drilled a stratigraphic test hole and well in Onslow County, N.C. The Dixon corehole was cored on ONWASA water utility property north of the town of Dixon, N.C., in the Sneads Ferry 7.5-minute quadrangle at latitude 34deg33'35' N, longitude 77deg26'54' W (decimal degrees 34.559722 and -77.448333). The site elevation is 66.0 feet (ft) above mean sea level as determined using a Paulin precision altimeter. The corehole attained a total depth of 1,010 ft and was continuously cored by the USGS EESPT drilling crew. A groundwater monitoring well was installed in the screened interval between 234 and 254 ft below land surface. The section cored at this site includes Upper Cretaceous, Paleogene, and Neogene sediments. The Dixon core is stored at the NCGS Coastal Plain core storage facility in Raleigh. \r\n\r\nThe Dixon corehole is the fourth and last in a series of planned North Carolina benchmark coreholes drilled by the USGS Coastal Carolina Project. These coreholes explore the physical stratigraphy, facies, and thickness of Cretaceous, Paleogene, and Neogene Coastal Plain sediments in North Carolina. Correlations of lithologies, facies, and sequence stratigraphy can be made with the Hope Plantation corehole, N.C., near Windsor in Bertie County (Weems and others, 2007); the Elizabethtown corehole, near Elizabethtown, N.C., in Bladen County (Self-Trail and others, 2004b); the Smith Elementary School corehole, near Cove City, N.C., in Craven County (Harris and Self-Trail, 2006; Crocetti, 2007); the Kure Beach corehole, near Wilmington, N.C., in New Hanover County (Self-Trail and others, 2004a); the Esso#1, Esso #2, Mobil #1, and Mobil #2 cores in Albermarle and Pamlico Sounds, N.C. (Zarra, 1989); and the Cape Fear River outcrops in Bladen County, N.C. (Farrell, 1998; Farrell and others, 2001). This report contains the lithostratigraphic summary recorded at the drill site, core photographs, geophysical data, and calcareous nannofossil biostratigraphic correlations.","language":"ENGLISH","publisher":"U.S. Geological Survey","doi":"10.3133/ofr20091194","collaboration":"Prepared in cooperation with the North Carolina Geological Survey and the University of North Carolina, Wilmington","usgsCitation":"Seefelt, E., Gonzalez, W.A., Self-Trail, J.M., Weems, R.E., Edwards, L.E., Pierce, H., and Durand, C.T., 2009, Preliminary Physical Stratigraphy and Geophysical Data From the USGS Dixon Core, Onslow County, North Carolina: U.S. Geological Survey Open-File Report 2009-1194, v, 135 p., https://doi.org/10.3133/ofr20091194.","productDescription":"v, 135 p.","temporalStart":"2006-10-01","temporalEnd":"2006-11-30","costCenters":[{"id":239,"text":"Eastern Earth Surface Processes Science Center","active":false,"usgs":true}],"links":[{"id":118536,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ofr_2009_1194.jpg"},{"id":13044,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2009/1194/","linkFileType":{"id":5,"text":"html"}}],"geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -80,33.5 ], [ -80,37 ], [ -75,37 ], [ -75,33.5 ], [ -80,33.5 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4acce4b07f02db67e48d","contributors":{"authors":[{"text":"Seefelt, Ellen 0000-0001-6822-7402 eseefelt@usgs.gov","orcid":"https://orcid.org/0000-0001-6822-7402","contributorId":2953,"corporation":false,"usgs":true,"family":"Seefelt","given":"Ellen","email":"eseefelt@usgs.gov","affiliations":[{"id":40020,"text":"Florence Bascom Geoscience Center","active":true,"usgs":true},{"id":243,"text":"Eastern Geology and Paleoclimate Science Center","active":true,"usgs":true}],"preferred":true,"id":303403,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Gonzalez, Wilma Aleman B.","contributorId":61717,"corporation":false,"usgs":true,"family":"Gonzalez","given":"Wilma","email":"","middleInitial":"Aleman B.","affiliations":[],"preferred":false,"id":303404,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Self-Trail, Jean M. jstrail@usgs.gov","contributorId":2205,"corporation":false,"usgs":true,"family":"Self-Trail","given":"Jean","email":"jstrail@usgs.gov","middleInitial":"M.","affiliations":[{"id":596,"text":"U.S. Geological Survey National Center","active":false,"usgs":true}],"preferred":false,"id":303400,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Weems, Robert E. 0000-0002-1907-7804 rweems@usgs.gov","orcid":"https://orcid.org/0000-0002-1907-7804","contributorId":2663,"corporation":false,"usgs":true,"family":"Weems","given":"Robert","email":"rweems@usgs.gov","middleInitial":"E.","affiliations":[{"id":243,"text":"Eastern Geology and Paleoclimate Science Center","active":true,"usgs":true},{"id":40020,"text":"Florence Bascom Geoscience Center","active":true,"usgs":true}],"preferred":true,"id":303402,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Edwards, Lucy E. 0000-0003-4075-3317 leedward@usgs.gov","orcid":"https://orcid.org/0000-0003-4075-3317","contributorId":2647,"corporation":false,"usgs":true,"family":"Edwards","given":"Lucy","email":"leedward@usgs.gov","middleInitial":"E.","affiliations":[{"id":243,"text":"Eastern Geology and Paleoclimate Science Center","active":true,"usgs":true},{"id":40020,"text":"Florence Bascom Geoscience Center","active":true,"usgs":true}],"preferred":true,"id":303401,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Pierce, Herbert A.","contributorId":83093,"corporation":false,"usgs":true,"family":"Pierce","given":"Herbert A.","affiliations":[],"preferred":false,"id":303406,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Durand, Colleen T.","contributorId":80495,"corporation":false,"usgs":true,"family":"Durand","given":"Colleen","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":303405,"contributorType":{"id":1,"text":"Authors"},"rank":7}]}}
,{"id":70157338,"text":"70157338 - 2009 - Use of the U.S. Geological Survey StreamStats Web Application for dam safety analysis","interactions":[],"lastModifiedDate":"2021-10-26T16:59:07.032562","indexId":"70157338","displayToPublicDate":"2009-10-01T00:00:00","publicationYear":"2009","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"Use of the U.S. Geological Survey StreamStats Web Application for dam safety analysis","docAbstract":"<p>No abstract available.</p>","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Dam Safety 2009 conference proceedings","largerWorkSubtype":{"id":12,"text":"Conference publication"},"conferenceTitle":"2009 ASDSO Annual Conference","conferenceDate":"September 27-October 1 2009","conferenceLocation":"Hollywood, Florida","language":"English","publisher":"Association of State Dam Safety Officials","usgsCitation":"Guthrie, J.D., Ries, K., and Steeves, P.A., 2009, Use of the U.S. Geological Survey StreamStats Web Application for dam safety analysis, <i>in</i> Dam Safety 2009 conference proceedings, Hollywood, Florida, September 27-October 1 2009.","onlineOnly":"N","additionalOnlineFiles":"N","ipdsId":"IP-015144","costCenters":[{"id":502,"text":"Office of Surface Water","active":true,"usgs":true}],"links":[{"id":308300,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"55fd35c1e4b05d6c4e502c87","contributors":{"authors":[{"text":"Guthrie, John D. jdguthrie@usgs.gov","contributorId":2391,"corporation":false,"usgs":true,"family":"Guthrie","given":"John","email":"jdguthrie@usgs.gov","middleInitial":"D.","affiliations":[{"id":547,"text":"Rocky Mountain Geographic Science Center","active":true,"usgs":true}],"preferred":false,"id":572744,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Ries, Kernell G. III kries@usgs.gov","contributorId":1913,"corporation":false,"usgs":true,"family":"Ries","given":"Kernell G.","suffix":"III","email":"kries@usgs.gov","affiliations":[{"id":502,"text":"Office of Surface Water","active":true,"usgs":true}],"preferred":false,"id":572745,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Steeves, Peter A. 0000-0001-7558-9719 psteeves@usgs.gov","orcid":"https://orcid.org/0000-0001-7558-9719","contributorId":1873,"corporation":false,"usgs":true,"family":"Steeves","given":"Peter","email":"psteeves@usgs.gov","middleInitial":"A.","affiliations":[{"id":41514,"text":"Maryland-Delaware-District of Columbia  Water Science Center","active":true,"usgs":true}],"preferred":true,"id":572746,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70236353,"text":"70236353 - 2009 - To burn or not to burn Oriental bittersweet: A fire manager’s conundrum","interactions":[],"lastModifiedDate":"2022-09-02T18:04:37.442301","indexId":"70236353","displayToPublicDate":"2009-09-30T12:45:25","publicationYear":"2009","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":1,"text":"Federal Government Series"},"title":"To burn or not to burn Oriental bittersweet: A fire manager’s conundrum","docAbstract":"<p>Oriental bittersweet (<i>Celastrus orbiculatus</i>) is a highly invasive liana (woody vine) that occurs throughout the Eastern United States. This twining plant can blanket and girdle adjacent vegetation, affecting succession and damaging trees. In areas where prescribed fire is a management tool, the response of Oriental bittersweet to fire needs to be quantified, rather than relying on anecdotal evidence. Currently, in areas already infested with this species, there are no strategies for prioritizing pre- or post-fire treatments on Oriental bittersweet. This largely results from a lack of understanding of the nature of post-fire resprouting by this species. Sprouting of bittersweet can at least double with fire and sprouts appear to respond to fire with an increase in growth rate (Pavlovic and Young pers. obs.). Beyond this basic need to understand the interaction between fire and Oriental bittersweet resprouting, we need to investigate how fire may interact with light, soil moisture, litter and other environmental factors to either increase or decrease abundance of this species. Finally, it is unknown how fire regimes influence the distribution of Oriental bittersweet on the landscape; thus we need to model the distribution of Oriental bittersweet in a fire impacted landscape. If we determine through our research that fire enhances the spread of this species, modification of fire suppression tactics and potential fire exclusion zones may be necessary. Thus we will be able to provide land managers throughout the Eastern US with data-driven decision support tools for more successful management of this species in fire dependent and invaded areas.</p>","language":"English","publisher":"Joint Fire Science Program","usgsCitation":"Pavlovic, N.B., Leicht-Young, S.A., Frohnapple, K., and Mulconrey, N., 2009, To burn or not to burn Oriental bittersweet: A fire manager’s conundrum, 22 p.","productDescription":"22 p.","costCenters":[],"links":[{"id":406160,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":406159,"rank":1,"type":{"id":11,"text":"Document"},"url":"https://www.firescience.gov/projects/08-1-2-10/project/08-1-2-10_jfspbittersweetfirstprogressreport2009.pdf","size":"1539 KB","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Indiana","otherGeospatial":"Indiana Dunes National Lakeshore","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  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-87.3248291015625,\n              41.62493858776385\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Pavlovic, Noel B. 0000-0002-2335-2274 npavlovic@usgs.gov","orcid":"https://orcid.org/0000-0002-2335-2274","contributorId":1976,"corporation":false,"usgs":true,"family":"Pavlovic","given":"Noel","email":"npavlovic@usgs.gov","middleInitial":"B.","affiliations":[{"id":324,"text":"Great Lakes Science Center","active":true,"usgs":true}],"preferred":true,"id":850730,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Leicht-Young, Stacey A.","contributorId":80506,"corporation":false,"usgs":false,"family":"Leicht-Young","given":"Stacey","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":850731,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Frohnapple, Krystal kfrohnapple@usgs.gov","contributorId":4110,"corporation":false,"usgs":true,"family":"Frohnapple","given":"Krystal","email":"kfrohnapple@usgs.gov","affiliations":[{"id":324,"text":"Great Lakes Science Center","active":true,"usgs":true}],"preferred":true,"id":850732,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Mulconrey, Neal","contributorId":152092,"corporation":false,"usgs":false,"family":"Mulconrey","given":"Neal","email":"","affiliations":[{"id":18866,"text":"Indiana Dunes National Lakeshore","active":true,"usgs":false}],"preferred":false,"id":850733,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70209652,"text":"70209652 - 2009 - The dynamic interaction of climate, vegetation, and dust emission, Mojave Desert, USA","interactions":[],"lastModifiedDate":"2020-04-17T16:34:12.620776","indexId":"70209652","displayToPublicDate":"2009-09-30T11:27:52","publicationYear":"2009","noYear":false,"publicationType":{"id":5,"text":"Book chapter"},"publicationSubtype":{"id":24,"text":"Book Chapter"},"title":"The dynamic interaction of climate, vegetation, and dust emission, Mojave Desert, USA","docAbstract":"<p>No abstract available.</p>","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Arid environments and wind erosion","largerWorkSubtype":{"id":15,"text":"Monograph"},"language":"English","publisher":"Nova Science Publishers","usgsCitation":"Urban, F., Reynolds, R.L., and Fulton, R., 2009, The dynamic interaction of climate, vegetation, and dust emission, Mojave Desert, USA, chap. <i>of</i> Arid environments and wind erosion, p. 243-267.","productDescription":"15 p.","startPage":"243","endPage":"267","costCenters":[{"id":318,"text":"Geosciences and Environmental Change Science Center","active":true,"usgs":true}],"links":[{"id":374096,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Arizona, California, Nevada","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -116.64184570312501,\n              34.35704160076073\n            ],\n            [\n              -114.60937499999999,\n              34.35704160076073\n            ],\n            [\n              -114.60937499999999,\n              36.05798104702501\n            ],\n            [\n              -116.64184570312501,\n              36.05798104702501\n            ],\n            [\n              -116.64184570312501,\n              34.35704160076073\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Urban, Frank 0000-0002-1329-1703 furban@usgs.gov","orcid":"https://orcid.org/0000-0002-1329-1703","contributorId":127827,"corporation":false,"usgs":true,"family":"Urban","given":"Frank","email":"furban@usgs.gov","affiliations":[{"id":318,"text":"Geosciences and Environmental Change Science Center","active":true,"usgs":true}],"preferred":true,"id":787392,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Reynolds, Richard L. 0000-0002-4572-2942 rreynolds@usgs.gov","orcid":"https://orcid.org/0000-0002-4572-2942","contributorId":139068,"corporation":false,"usgs":true,"family":"Reynolds","given":"Richard","email":"rreynolds@usgs.gov","middleInitial":"L.","affiliations":[{"id":318,"text":"Geosciences and Environmental Change Science Center","active":true,"usgs":true}],"preferred":true,"id":787393,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Fulton, R.","contributorId":30447,"corporation":false,"usgs":true,"family":"Fulton","given":"R.","email":"","affiliations":[],"preferred":false,"id":787394,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70204144,"text":"70204144 - 2009 - Spectroscopic analysis of arsenic uptake in Pteris Ferns","interactions":[],"lastModifiedDate":"2019-07-10T10:04:57","indexId":"70204144","displayToPublicDate":"2009-09-30T10:24:37","publicationYear":"2009","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3250,"text":"Remote Sensing","active":true,"publicationSubtype":{"id":10}},"displayTitle":"Spectroscopic analysis of arsenic uptake in <i>Pteris</i> Ferns","title":"Spectroscopic analysis of arsenic uptake in Pteris Ferns","docAbstract":"<div class=\"art-abstract in-tab hypothesis_container\"><span>Two arsenic-accumulating&nbsp;</span><span class=\"html-italic\"><i>Pteris</i><span>&nbsp;</span></span><span>ferns (</span><span class=\"html-italic\"><i>Pteris cretica mayii</i><span>&nbsp;</span></span><span>and&nbsp;</span><i><span class=\"html-italic\">Pteris multifida</span></i><span>), along with a non-accumulating control fern (</span><i><span class=\"html-italic\">Nephrolepis exaltata</span></i><span>) were grown in greenhouse conditions in clean sand spiked with 0, 20, 50, 100 and 200 ppm sodium arsenate. Spectral data were collected for each of five replicates prior to harvest at 4-week intervals. Fern samples were analyzed for total metals content and Partial Least Squares and Stepwise Linear Regression techniques were used to develop models from the spectral data. Results showed that&nbsp;</span><i><span class=\"html-italic\">Pteris cretica mayii</span></i><span>&nbsp;and&nbsp;</span><i><span class=\"html-italic\">Pteris multifida</span></i><span>&nbsp;are confirmed hyperaccumulators of inorganic arsenic and that reasonably accurate predictive models of arsenic concentration can be developed from the first derivative of spectral reflectance of the hyperaccumulating&nbsp;</span><span class=\"html-italic\"><i>Pteris</i><span>&nbsp;</span></span><span>ferns. Both the arsenic uptake and spectral results indicate that there is some species-specific variability but the results compare favorably with previously published data and additional research is recommended.</span></div>","language":"English","publisher":"MDPI","doi":"10.3390/rs1040644","usgsCitation":"Slonecker, E.T., Haack, B.N., and Price, S.D., 2009, Spectroscopic analysis of arsenic uptake in Pteris Ferns: Remote Sensing, v. 1, no. 4, p. 644-675, https://doi.org/10.3390/rs1040644.","productDescription":"32 p.","startPage":"644","endPage":"675","costCenters":[{"id":242,"text":"Eastern Geographic Science Center","active":true,"usgs":true}],"links":[{"id":476061,"rank":0,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.3390/rs1040644","text":"Publisher Index Page"},{"id":365367,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"1","issue":"4","noUsgsAuthors":false,"publicationDate":"2009-09-30","publicationStatus":"PW","contributors":{"authors":[{"text":"Slonecker, E. Terrence 0000-0002-5793-0503 tslonecker@usgs.gov","orcid":"https://orcid.org/0000-0002-5793-0503","contributorId":168591,"corporation":false,"usgs":true,"family":"Slonecker","given":"E.","email":"tslonecker@usgs.gov","middleInitial":"Terrence","affiliations":[{"id":242,"text":"Eastern Geographic Science Center","active":true,"usgs":true},{"id":36171,"text":"National Civil Applications Center","active":true,"usgs":true}],"preferred":true,"id":765696,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Haack, Barry N. bhaack@usgs.gov","contributorId":4261,"corporation":false,"usgs":true,"family":"Haack","given":"Barry","email":"bhaack@usgs.gov","middleInitial":"N.","affiliations":[{"id":242,"text":"Eastern Geographic Science Center","active":true,"usgs":true}],"preferred":true,"id":765697,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Price, Susan D. sprice@usgs.gov","contributorId":3825,"corporation":false,"usgs":true,"family":"Price","given":"Susan","email":"sprice@usgs.gov","middleInitial":"D.","affiliations":[],"preferred":true,"id":765698,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70003854,"text":"70003854 - 2009 - Magma evolution and ascent at the craters of the moon and neighboring volcanic fields, southern Idaho, USA: Implications for the evolution of polygenetic and monogenetic volcanic fields","interactions":[],"lastModifiedDate":"2021-03-05T18:13:52.41254","indexId":"70003854","displayToPublicDate":"2009-09-30T00:00:00","publicationYear":"2009","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2420,"text":"Journal of Petrology","active":true,"publicationSubtype":{"id":10}},"title":"Magma evolution and ascent at the craters of the moon and neighboring volcanic fields, southern Idaho, USA: Implications for the evolution of polygenetic and monogenetic volcanic fields","docAbstract":"The evolution of polygenetic and monogenetic volcanic fields must reflect differences in magma processing during ascent. To assess their evolution we use thermobarometry and geochemistry to evaluate ascent paths for neighboring, nearly coeval volcanic fields in the Snake River Plain, in south-central Idaho, derived from (1) dominantly Holocene polygenetic evolved lavas from the Craters of the Moon lava field (COME) and (2) Quaternary non-evolved, olivine tholeiites (NEOT) from nearby monogenetic volcanic fields. These data show that NEOT have high magmatic temperatures (1205 + or - 27 degrees C) and a narrow temperature range (< 25 degrees C) at any given depth; NEOT parent magmas partially crystallize within the middle crust (14-17 km), but with little time for cooling or assimilation. In contrast, COME magmas partially crystallize at similar depths, but at any given depth exhibit lower temperatures (by ~40 degrees C), and wider temperature ranges (>50 degrees C). Prolonged storage of COME magmas allows them to evolve to higher <sup>87</sup>Sr/<sup>86</sup>Sr and SiO<sub>2</sub>, and lower MgO and <sup>143</sup>Nd/<sup>144</sup>Nd. Most importantly, ascent paths control evolution: NEOT often erupt near the axis of the plain where high-flux (Yellowstone-related), pre-Holocene magmatic activity replaces granitic middle crust with basaltic sills, resulting in a net increase in NEOT magma buoyancy. COME flows erupt off-axis, where felsic crustal lithologies sometimes remain intact, providing a barrier to ascent and a source for crustal contamination. A three-stage ascent process explains the entire range of erupted compositions. Stage 1 (40-20 km): picrites are transported to the middle crust, undergoing partial crystallization of olivine + or - clinopyroxene. COME magmas pass through unarmored conduits and assimilate 1% or less of ancient gabbroic crust having high Sr and <sup>87</sup>Sr/<sup>86</sup>Sr and low SiO<sub>2</sub>. Stage 2 (20-10 km): magmas are stored within the middle crust, and evolve to moderate MgO (10%). NEOT magmas, reaching 10% MgO, are positively buoyant and migrate through the middle crust. COME magmas remain negatively buoyant and so crystallize further and assimilate middle crust. Stage 3 (15-0 km): final ascent and eruption occurs when volatile contents, increased by differentiation, are sufficient (1-2 wt % H<sub>2</sub>O) to provide magma buoyancy through the middle (and upper) crust.","language":"English","publisher":"Oxford Journals","doi":"10.1093/petrology/egp045","usgsCitation":"Putirka, K.D., Kuntz, M., Unruh, D., and Vaid, N., 2009, Magma evolution and ascent at the craters of the moon and neighboring volcanic fields, southern Idaho, USA: Implications for the evolution of polygenetic and monogenetic volcanic fields: Journal of Petrology, v. 50, no. 9, p. 1639-1665, https://doi.org/10.1093/petrology/egp045.","productDescription":"27 p.","startPage":"1639","endPage":"1665","costCenters":[{"id":308,"text":"Geology and Environmental Change Science Center","active":false,"usgs":true}],"links":[{"id":476062,"rank":0,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1093/petrology/egp045","text":"Publisher Index Page"},{"id":384097,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Idaho","otherGeospatial":"southern  Idaho","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -117.29003906249997,\n              41.902277040963696\n            ],\n            [\n              -111.09374999999999,\n              41.902277040963696\n            ],\n            [\n              -111.09374999999999,\n              45.42929873257375\n            ],\n            [\n              -117.29003906249997,\n              45.42929873257375\n            ],\n            [\n              -117.29003906249997,\n              41.902277040963696\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"50","issue":"9","noUsgsAuthors":false,"publicationDate":"2009-07-13","publicationStatus":"PW","scienceBaseUri":"4f4e4a7fe4b07f02db649213","contributors":{"authors":[{"text":"Putirka, Keith D.","contributorId":89652,"corporation":false,"usgs":true,"family":"Putirka","given":"Keith","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":349162,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Kuntz, Mel A. 0000-0001-8828-5474","orcid":"https://orcid.org/0000-0001-8828-5474","contributorId":6446,"corporation":false,"usgs":true,"family":"Kuntz","given":"Mel A.","affiliations":[],"preferred":false,"id":349160,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Unruh, Daniel M.","contributorId":96291,"corporation":false,"usgs":true,"family":"Unruh","given":"Daniel M.","affiliations":[],"preferred":false,"id":349163,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Vaid, Nitin","contributorId":37878,"corporation":false,"usgs":true,"family":"Vaid","given":"Nitin","email":"","affiliations":[],"preferred":false,"id":349161,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70237068,"text":"70237068 - 2009 - An evaluation of the genus Kincaidiana Altman, 1936, with the designation of Altmanella n. gen. (Annelida, Clitellata, Lumbriculidae)","interactions":[],"lastModifiedDate":"2022-09-29T12:13:18.153132","indexId":"70237068","displayToPublicDate":"2009-09-29T07:11:56","publicationYear":"2009","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3814,"text":"Zootaxa","onlineIssn":"1175-5334","printIssn":"1175-5326","active":true,"publicationSubtype":{"id":10}},"title":"An evaluation of the genus Kincaidiana Altman, 1936, with the designation of Altmanella n. gen. (Annelida, Clitellata, Lumbriculidae)","docAbstract":"<p>A review of morphological characters for the western Nearctic genus<span>&nbsp;</span><i>Kincaidiana</i><span>&nbsp;</span>indicated that the two described species should be assigned to separate genera.<span>&nbsp;</span><i>Kincaidiana</i><span>&nbsp;</span><i>freidris</i><span>&nbsp;</span>Cook was transferred to a new genus,<span>&nbsp;</span><i>Altmanella.</i><span>&nbsp;</span>New material resembling<span>&nbsp;</span><i>A.</i><span>&nbsp;</span><i>freidris</i><span>&nbsp;</span>was obtained from many sites throughout western North America. Morphology of the male reproductive structures varied among populations, and the most distinctive morphological differences were accounted for by splitting the taxon into two species, which roughly corresponded to large scale regional patterns. Typical<span>&nbsp;</span><i>A.</i><span>&nbsp;</span><i>freidris</i><span>&nbsp;</span>occurred in several Pacific Coast drainages.<span>&nbsp;</span><i>Altmanella</i><span>&nbsp;</span><i>idahoensis</i><span>&nbsp;</span><strong>n.</strong><span>&nbsp;</span><strong>sp.,</strong><span>&nbsp;</span>mostly associated with the Snake River drainage, was distinguished from<span>&nbsp;</span><i>A.</i><span>&nbsp;</span><i>freidris</i><span>&nbsp;</span>by shorter and less muscular atria and penial structures. A second new lumbriculid species with the same basic arrangement of reproductive organs was collected in southeastern North America, and was provisionally assigned to<span>&nbsp;</span><i>Altmanella.</i><span>&nbsp;</span>However, in contrast to the petiolate atria and large penial structures of<span>&nbsp;</span><i>A.</i><span>&nbsp;</span><i>freidris</i><span>&nbsp;</span>and<span>&nbsp;</span><i>A.</i><span>&nbsp;</span><i>idahoensis,</i><span>&nbsp;</span><i>Altmanella</i><span>&nbsp;</span><i>lenati</i><span>&nbsp;</span><strong>n.</strong><span>&nbsp;</span><strong>sp.</strong><span>&nbsp;</span>has tubular atria and simple male porophores.</p>","language":"English","publisher":"Biotaxa","doi":"10.11646/zootaxa.2077.1.1","usgsCitation":"Fend, S.V., 2009, An evaluation of the genus Kincaidiana Altman, 1936, with the designation of Altmanella n. gen. (Annelida, Clitellata, Lumbriculidae): Zootaxa, v. 2077, no. 1, 30 p., https://doi.org/10.11646/zootaxa.2077.1.1.","productDescription":"30 p.","costCenters":[{"id":438,"text":"National Research Program - Western Branch","active":true,"usgs":true}],"links":[{"id":407568,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"2077","issue":"1","noUsgsAuthors":false,"publicationDate":"2009-04-20","publicationStatus":"PW","contributors":{"authors":[{"text":"Fend, Steven V. 0000-0002-4638-6602 svfend@usgs.gov","orcid":"https://orcid.org/0000-0002-4638-6602","contributorId":3591,"corporation":false,"usgs":true,"family":"Fend","given":"Steven","email":"svfend@usgs.gov","middleInitial":"V.","affiliations":[{"id":438,"text":"National Research Program - Western Branch","active":true,"usgs":true}],"preferred":true,"id":853240,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":97853,"text":"sir20095140 - 2009 - Hydrologic Conditions that Influence Streamflow Losses in a Karst Region of the Upper Peace River, Polk County, Florida","interactions":[],"lastModifiedDate":"2012-02-10T00:11:46","indexId":"sir20095140","displayToPublicDate":"2009-09-29T00:00:00","publicationYear":"2009","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":"2009-5140","title":"Hydrologic Conditions that Influence Streamflow Losses in a Karst Region of the Upper Peace River, Polk County, Florida","docAbstract":"The upper Peace River from Bartow to Fort Meade, Florida, is described as a groundwater recharge area, reflecting a reversal from historical groundwater discharge patterns that existed prior to the 1950s. The upper Peace River channel and floodplain are characterized by extensive karst development, with numerous fractures, crevasses, and sinks that have been eroded in the near-surface and underlying carbonate bedrock. With the reversal in groundwater head gradients, river water is lost to the underlying groundwater system through these karst features. An investigation was conducted to evaluate the hydrologic conditions that influence streamflow losses in the karst region of the upper Peace River. \r\n\r\nThe upper Peace River is located in a basin that has been altered substantially by phosphate mining and increases in groundwater use. These alterations have changed groundwater flow patterns and caused streamflow declines through time. Hydrologic factors that have had the greatest influence on streamflow declines in the upper Peace River include the lowering of the potentiometric surfaces of the intermediate aquifer system and Upper Floridan aquifer beneath the riverbed elevation due to below-average rainfall (droughts), increases in groundwater use, and the presence of numerous karst features in the low-water channel and floodplain that enhance the loss of streamflow.\r\n\r\nSeepage runs conducted along the upper Peace River, from Bartow to Fort Meade, indicate that the greatest streamflow losses occurred along an approximate 2-mile section of the river beginning about 1 mile south of the Peace River at Bartow gaging station. Along the low-water and floodplain channel of this 2-mile section, there are about 10 prominent karst features that influence streamflow losses. Losses from the individual karst features ranged from 0.22 to 16 cubic feet per second based on measurements made between 2002 and 2007. The largest measured flow loss for all the karst features was about 50 cubic feet per second, or about 32 million gallons per day, on June 28, 2002. \r\n\r\nStreamflow losses varied throughout the year, and were related to seasonal fluctuations in groundwater levels. When groundwater levels were at their lowest level at the end of the dry season (May and June), there was an increased potential for streamflow losses. During this study, the largest streamflow losses occurred at the beginning of the summer rainy season when discharge in the river increased and large volumes of water were needed to replenish unfilled cavities and void spaces in the underlying aquifers.\r\n\r\nThe underlying geology along the upper Peace River and floodplain is highly karstified, and aids in the movement and amount of streamflow that is lost to the groundwater system in this region. Numerous karst features and fractured carbonates and cavernous zones observed in geologic cores and geophysical logs indicate an active, well-connected, groundwater flow system. Aquifer and dye tests conducted along the upper Peace River indicate the presence of cavernous and highly transmissive layers within the floodplain area that can store and transport large volumes of water in underground cavities. A discharge measurement made during this study indicates that the cavernous system associated with Dover Sink can accept over 10 million gallons per day (16 cubic feet per second) of streamflow before the localized aquifer storage volume is replenished and the level of the sink is stabilized.","language":"ENGLISH","publisher":"U.S. Geological Survey","doi":"10.3133/sir20095140","isbn":"9781411325456","collaboration":"Prepared in cooperation with the Southwest Florida Water Management District","usgsCitation":"Metz, P.A., and Lewelling, B., 2009, Hydrologic Conditions that Influence Streamflow Losses in a Karst Region of the Upper Peace River, Polk County, Florida: U.S. Geological Survey Scientific Investigations Report 2009-5140, x, 82 p., https://doi.org/10.3133/sir20095140.","productDescription":"x, 82 p.","temporalStart":"2001-10-01","temporalEnd":"2007-09-30","costCenters":[{"id":275,"text":"Florida Integrated Science Center","active":false,"usgs":true}],"links":[{"id":125609,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/sir_2009_5140.jpg"},{"id":13028,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/sir/2009/5140/","linkFileType":{"id":5,"text":"html"}}],"geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -82.08333333333333,27.583333333333332 ], [ -82.08333333333333,28.166666666666668 ], [ -81.5,28.166666666666668 ], [ -81.5,27.583333333333332 ], [ -82.08333333333333,27.583333333333332 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a2de4b07f02db614457","contributors":{"authors":[{"text":"Metz, P. A.","contributorId":68706,"corporation":false,"usgs":true,"family":"Metz","given":"P.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":303355,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Lewelling, B. R.","contributorId":17969,"corporation":false,"usgs":true,"family":"Lewelling","given":"B. R.","affiliations":[],"preferred":false,"id":303354,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":97855,"text":"ofr20091162 - 2009 - Rainfall, discharge, and water-quality data during stormwater monitoring, July 1, 2008, to June 30, 2009; Halawa Stream drainage basin and the H-1 storm drain, Oahu, Hawaii","interactions":[],"lastModifiedDate":"2022-06-15T18:12:43.09528","indexId":"ofr20091162","displayToPublicDate":"2009-09-29T00:00:00","publicationYear":"2009","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":"2009-1162","title":"Rainfall, discharge, and water-quality data during stormwater monitoring, July 1, 2008, to June 30, 2009; Halawa Stream drainage basin and the H-1 storm drain, Oahu, Hawaii","docAbstract":"Storm runoff water-quality samples were collected as part of the State of Hawaii Department of Transportation Stormwater Monitoring Program. The program is designed to assess the effects of highway runoff and urban runoff on Halawa Stream, and to assess the effects from the H-1 storm drain on Manoa Stream. For this program, rainfall data were collected at three stations, continuous discharge data at five stations, and water-quality data at six stations, which include the five continuous discharge stations. This report summarizes rainfall, discharge, and water-quality data collected between July 1, 2008, and June 30, 2009. \r\n\r\nWithin the Halawa Stream drainage area, three storms (October 25 and December 11, 2008, and February 3, 2009) were sampled during July 1, 2008, to June 30, 2009. A total of 43 environmental samples were collected during these three storms. During the storm of October 25, 2009, 31 samples were collected and analyzed individually for metals only. The other 12 samples from the other two storms were analyzed for some or all of the following analytes: total suspended solids, total dissolved solids, nutrients, chemical oxygen demand, and selected trace metals (cadmium, chromium, copper, lead, and zinc). Additionally, grab samples were analyzed for some or all of the following analytes: oil and grease, total petroleum hydrocarbons, fecal coliform, and biological oxygen demand. Some grab and composite samples were analyzed for only a partial list of these analytes, either because samples could not be delivered to the laboratory in a timely manner, or an insufficient volume of sample was collected by the automatic samplers. Two quality-assurance/quality-control samples were collected after cleaning automatic sampler lines to verify that the sampling lines were not contaminated. \r\n\r\nFour environmental samples were collected at the H-1 Storm Drain during July 1, 2008, to June 30, 2009. An oil and grease sample and a composite sample were collected during the storm on November 15, 2008, and two composite samples were collected during the January 11, 2009, storm. All samples at this site were collected using an automatic sampler. Samples were analyzed for some or all of the following analytes: total suspended solids, nutrients, oil and grease, total petroleum hydrocarbons, and selected trace metals (cadmium, chromium, copper, lead, nickel, and zinc). One qualityassurance/quality-control sample was collected after cleaning automatic sampler lines to verify that the sampling lines were not contaminated. \r\n\r\nDuring the storm of January 11, 2009, the two composite samples collected at H-1 Storm Drain were collected about three hours apart. Higher constituent concentrations were detected in the first 2 composite sample relative to the second composite sample, although the average discharge was higher during the period when the second sample was collected.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr20091162","collaboration":"Prepared in cooperation with the State of Hawaii Department of Transportation","usgsCitation":"Presley, T.K., and Jamison, M.T., 2009, Rainfall, discharge, and water-quality data during stormwater monitoring, July 1, 2008, to June 30, 2009; Halawa Stream drainage basin and the H-1 storm drain, Oahu, Hawaii: U.S. Geological Survey Open-File Report 2009-1162, Report: vi, 48 p.; 2 Tables, https://doi.org/10.3133/ofr20091162.","productDescription":"Report: vi, 48 p.; 2 Tables","onlineOnly":"Y","additionalOnlineFiles":"Y","temporalStart":"2008-07-01","temporalEnd":"2009-06-30","costCenters":[{"id":525,"text":"Pacific Islands Water Science Center","active":true,"usgs":true}],"links":[{"id":118525,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ofr_2009_1162.jpg"},{"id":13030,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2009/1162/","linkFileType":{"id":5,"text":"html"}},{"id":402218,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_87413.htm","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Hawaii","otherGeospatial":"Oahu","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -157.93190002441406,\n              21.36996550312423\n            ],\n            [\n              -157.81654357910156,\n              21.36996550312423\n            ],\n            [\n              -157.81654357910156,\n              21.420791878140957\n            ],\n            [\n              -157.93190002441406,\n              21.420791878140957\n            ],\n            [\n              -157.93190002441406,\n              21.36996550312423\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adbe4b07f02db685f32","contributors":{"authors":[{"text":"Presley, Todd K. 0000-0001-5851-0634 tkpresle@usgs.gov","orcid":"https://orcid.org/0000-0001-5851-0634","contributorId":2671,"corporation":false,"usgs":true,"family":"Presley","given":"Todd","email":"tkpresle@usgs.gov","middleInitial":"K.","affiliations":[],"preferred":true,"id":303357,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Jamison, Marcael T. J.","contributorId":6817,"corporation":false,"usgs":true,"family":"Jamison","given":"Marcael","email":"","middleInitial":"T. J.","affiliations":[],"preferred":false,"id":303358,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
]}