{"pageNumber":"3194","pageRowStart":"79825","pageSize":"25","recordCount":184884,"records":[{"id":30870,"text":"wri004195 - 2000 - Geologic framework and hydrogeologic characteristics of the Edwards Aquifer outcrop, Medina County, Texas","interactions":[],"lastModifiedDate":"2017-03-29T16:27:49","indexId":"wri004195","displayToPublicDate":"2001-06-01T00:00:00","publicationYear":"2000","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"2000-4195","title":"Geologic framework and hydrogeologic characteristics of the Edwards Aquifer outcrop, Medina County, Texas","docAbstract":"<p>The hydrogeologic subdivisions of the Edwards aquifer outcrop in Medina County generally are porous and permeable. The most porous and permeable appear to be hydrogeologic subdivision VI, the Kirschberg evaporite member of the Kainer Formation; and hydrogeologic subdivision III, the leached and collapsed members, undivided, of the Person Formation. The most porous and permeable rocks of the Devils River Formation in Medina County appear to be in the top layer. The upper member of the Glen Rose Limestone, the lower confining unit, has much less porosity and permeability than that observed in the Edwards aquifer.</p><p>The Edwards aquifer has relatively large porosity and permeability resulting, in part, from the development or redistribution of secondary porosity. Lithology, stratigraphy, diagenesis, and karstification account for the effective porosity and permeability in the Edwards aquifer outcrop. Karst features that can greatly enhance effective porosity and permeability in the Edwards aquifer outcrop include sinkholes, dolines, and caves. The Edwards aquifer rocks in Medina County change from the eight-member Edwards Group to the essentially indivisible Devils River Formation. The facies change occurs along a line extending northwestward from just south of Medina Lake.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wri004195","collaboration":"In cooperation with the Edwards Aquifer Authority","usgsCitation":"Small, T.A., and Clark, A.K., 2000, Geologic framework and hydrogeologic characteristics of the Edwards Aquifer outcrop, Medina County, Texas: U.S. Geological Survey Water-Resources Investigations Report 2000-4195, Report: iii, 10 p.; Plate: 36 x 24 inches, https://doi.org/10.3133/wri004195.","productDescription":"Report: iii, 10 p.; Plate: 36 x 24 inches","costCenters":[{"id":583,"text":"Texas Water Science 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A.","contributorId":77533,"corporation":false,"usgs":true,"family":"Small","given":"Ted","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":204244,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Clark, Allan K. 0000-0003-0099-1521 akclark@usgs.gov","orcid":"https://orcid.org/0000-0003-0099-1521","contributorId":1279,"corporation":false,"usgs":true,"family":"Clark","given":"Allan","email":"akclark@usgs.gov","middleInitial":"K.","affiliations":[{"id":318,"text":"Geosciences and Environmental Change Science Center","active":true,"usgs":true},{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"preferred":true,"id":204243,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":30863,"text":"wri004082 - 2000 - Estimated effects on water quality of Lake Houston from interbasin transfer of water from the Trinity River, Texas","interactions":[],"lastModifiedDate":"2016-08-30T11:26:41","indexId":"wri004082","displayToPublicDate":"2001-06-01T00:00:00","publicationYear":"2000","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"2000-4082","title":"Estimated effects on water quality of Lake Houston from interbasin transfer of water from the Trinity River, Texas","docAbstract":"<p>The City of Houston is considering the transfer of water from the Trinity River to Lake Houston (on the San Jacinto River) to alleviate concerns about adequate water supplies for future water demands. The U.S. Geological Survey, in cooperation with the City of Houston, conducted a study to estimate the effects on the water quality of Lake Houston from the transfer of Trinity River water. </p><p>A water-quality model, CE–QUAL–W2, was used to simulate six water-quality properties and constituents for scenarios of interbasin transfer of Trinity River water. Three scenarios involved the transferred Trinity River water augmenting streamflow in the East Fork of Lake Houston, and three scenarios involved the transferred water replacing streamflow from the West Fork of the San Jacinto River.</p><p>The estimated effects on Lake Houston were determined by comparing volume-weighted daily mean water temperature, phosphorus, ammonia nitrogen, nitrite plus nitrate nitrogen, algal biomass, and dissolved oxygen simulated for each of the transfer scenarios to simulations for a base dataset. The effects of the interbasin transfer on Lake Houston do not appear to be detrimental to water temperature, ammonia nitrogen, or dissolved oxygen. Phosphorus and nitrite plus nitrate nitrogen showed fairly large changes when Trinity River water was transferred to replace West Fork San Jacinto River streamflow. Algal biomass showed large decreases when Trinity River water was transferred to augment East Fork Lake Houston streamflow and large increases when Trinity River water was transferred to replace West Fork San Jacinto River streamflow. Regardless of the scenario simulated, the model indicated that light was the limiting factor for algal biomass growth.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wri004082","usgsCitation":"Liscum, F., and East, J., 2000, Estimated effects on water quality of Lake Houston from interbasin transfer of water from the Trinity River, Texas: U.S. Geological Survey Water-Resources Investigations Report 2000-4082, iv, 50 p., https://doi.org/10.3133/wri004082.","productDescription":"iv, 50 p.","costCenters":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"links":[{"id":160296,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/wri004082.PNG"},{"id":328035,"rank":3,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/wri00-4082/pdf/wri00-4082.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":2738,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/wri00-4082/","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a81e4b07f02db64a1a0","contributors":{"authors":[{"text":"Liscum, Fred","contributorId":95463,"corporation":false,"usgs":true,"family":"Liscum","given":"Fred","email":"","affiliations":[],"preferred":false,"id":204230,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"East, Jeffery W. jweast@usgs.gov","contributorId":1683,"corporation":false,"usgs":true,"family":"East","given":"Jeffery W.","email":"jweast@usgs.gov","affiliations":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"preferred":true,"id":204229,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":24643,"text":"ofr00389 - 2000 - 20th century U.S. mineral prices decline in constant dollars","interactions":[],"lastModifiedDate":"2012-02-02T00:08:23","indexId":"ofr00389","displayToPublicDate":"2001-06-01T00:00:00","publicationYear":"2000","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":"2000-389","title":"20th century U.S. mineral prices decline in constant dollars","docAbstract":"Price indexes developed by the U.S. Geological Survey (USGS) indicate that the long-term constant dollar price of key U.S. mineral raw materials declined over the last century, even though the need for mineral raw materials increased during the same period. Technologies and reduced production costs have allowed mineral production to remain profitable, while lower priced mineral products from domestic and foreign sources helped fuel growth in other sectors of the economy.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr00389","issn":"0094-9140","usgsCitation":"Sullivan, D.E., Sznopek, J.L., and Wagner, L.A., 2000, 20th century U.S. mineral prices decline in constant dollars: U.S. Geological Survey Open-File Report 2000-389, 8 p., https://doi.org/10.3133/ofr00389.","productDescription":"8 p.","costCenters":[],"links":[{"id":157539,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":1910,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/openfile/of00-389/","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53cd4929e4b0b290850eeed0","contributors":{"authors":[{"text":"Sullivan, Daniel E.","contributorId":62198,"corporation":false,"usgs":true,"family":"Sullivan","given":"Daniel","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":192310,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Sznopek, John L.","contributorId":23936,"corporation":false,"usgs":true,"family":"Sznopek","given":"John","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":192309,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Wagner, Lorie A.","contributorId":95457,"corporation":false,"usgs":true,"family":"Wagner","given":"Lorie","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":192311,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":22086,"text":"ofr00492 - 2000 - Quantifying submarine groundwater discharge to Indian River Lagoon, Florida","interactions":[],"lastModifiedDate":"2012-02-02T00:07:51","indexId":"ofr00492","displayToPublicDate":"2001-06-01T00:00:00","publicationYear":"2000","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":"2000-492","title":"Quantifying submarine groundwater discharge to Indian River Lagoon, Florida","language":"ENGLISH","publisher":"U.S. Dept. of the Interior, U.S. Geological Survey,","doi":"10.3133/ofr00492","issn":"0094-9140","usgsCitation":"Swarzenski, P.W., Martin, J., Cable, J., Lindenberg, M., Boynton, B., Bowker, R., and Sigua, G., 2000, Quantifying submarine groundwater discharge to Indian River Lagoon, Florida: U.S. Geological Survey Open-File Report 2000-492, 4 p. :col. ill., col. maps ;28 cm., https://doi.org/10.3133/ofr00492.","productDescription":"4 p. :col. ill., col. maps ;28 cm.","costCenters":[],"links":[{"id":153779,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/2000/0492/report-thumb.jpg"},{"id":51528,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/2000/0492/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a86e4b07f02db64dbcd","contributors":{"authors":[{"text":"Swarzenski, Peter W. 0000-0003-0116-0578 pswarzen@usgs.gov","orcid":"https://orcid.org/0000-0003-0116-0578","contributorId":1070,"corporation":false,"usgs":true,"family":"Swarzenski","given":"Peter","email":"pswarzen@usgs.gov","middleInitial":"W.","affiliations":[{"id":520,"text":"Pacific Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":true,"id":187006,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Martin, J.B.","contributorId":32923,"corporation":false,"usgs":true,"family":"Martin","given":"J.B.","email":"","affiliations":[],"preferred":false,"id":187009,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Cable, J.E.","contributorId":25963,"corporation":false,"usgs":true,"family":"Cable","given":"J.E.","email":"","affiliations":[],"preferred":false,"id":187008,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Lindenberg, M.K.","contributorId":56254,"corporation":false,"usgs":true,"family":"Lindenberg","given":"M.K.","affiliations":[],"preferred":false,"id":187012,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Boynton, Betsy bboynton@usgs.gov","contributorId":3360,"corporation":false,"usgs":true,"family":"Boynton","given":"Betsy","email":"bboynton@usgs.gov","affiliations":[],"preferred":true,"id":187007,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Bowker, Rita","contributorId":33733,"corporation":false,"usgs":true,"family":"Bowker","given":"Rita","email":"","affiliations":[],"preferred":false,"id":187010,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Sigua, G.C.","contributorId":52994,"corporation":false,"usgs":true,"family":"Sigua","given":"G.C.","email":"","affiliations":[],"preferred":false,"id":187011,"contributorType":{"id":1,"text":"Authors"},"rank":7}]}}
,{"id":26579,"text":"wri004084 - 2000 - Design, revision, and application of ground-water flow models for simulation of selected water-management scenarios in the coastal area of Georgia and adjacent parts of South Carolina and Florida","interactions":[],"lastModifiedDate":"2017-01-18T16:00:29","indexId":"wri004084","displayToPublicDate":"2001-06-01T00:00:00","publicationYear":"2000","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"2000-4084","title":"Design, revision, and application of ground-water flow models for simulation of selected water-management scenarios in the coastal area of Georgia and adjacent parts of South Carolina and Florida","docAbstract":"Ground-water flow models of the Floridan aquifer system in the coastal area of Georgia and adjacent parts of South Carolina and Florida, were revised and updated to ensure consistency among the various models used, and to facilitate evaluation of the effects of pumping on the ground-water level near areas of saltwater contamination. The revised models, developed as part of regional and areal assessments of ground-water resources in coastal Georgia, are--the Regional Aquifer-System Analysis (RASA) model, the Glynn County area (Glynn) model, and the Savannah area (Savannah) model. Changes were made to hydraulic-property arrays of the RASA and Glynn models to ensure consistency among all of the models; results of theses changes are evidenced in revised water budgets and calibration statistics. \r\n\r\nFollowing revision, the three models were used to simulate 32 scenarios of hypothetical changes in pumpage that ranged from about 82 million gallons per day (Mgal/d) lower to about 438 Mgal/d higher, than the May 1985 pumping rate of 308 Mgal/d. The scenarios were developed by the Georgia Department of Natural Resources, Environmental Protection Division and the Chatham County-Savannah Metropolitan Planning Commission to evaluate water-management alternatives in coastal Georgia. Maps showing simulated ground-water-level decline and diagrams presenting changes in simulated flow rates are presented for each scenario. \r\n\r\nScenarios were grouped on the basis of pumping location--entire 24-county area, central subarea, Glynn-Wayne-Camden County subarea, and Savannah-Hilton Head Island subarea. For those scenarios that simulated decreased pumpage, the water level at both Brunswick and Hilton Head Island rose, decreasing the hydraulic gradient and reducing the potential for saltwater contamination. Conversely, in response to scenarios of increased pumpage, the water level at both locations declined, increasing the hydraulic gradient and increasing the potential for saltwater contamination. Pumpage effects on ground-water levels and related saltwater contamination at Brunswick and Hilton Head Island generally diminish with increased distance from these areas. \r\n\r\nAdditional development of the Upper Floridan aquifer may be possible in parts of the coastal area without affecting saltwater contamination at Brunswick or Hilton Head Island, due to the presence of two hydrologic boundaries--the Gulf Trough, separating the northern and central subareas; and the hypothesized  Satilla Line,  separating the central and southern subareas. These boundaries diminish pumpage effects across them; and may enable greater ground-water withdrawal in areas north of the Gulf Trough and south of the  Satilla Line  without producing appreciable drawdown at Brunswick or Hilton Head Island.","language":"ENGLISH","publisher":"U.S. Department of the Interior, U.S. Geological Survey ;\r\nBranch of Information Services [distributor],","doi":"10.3133/wri004084","usgsCitation":"Clarke, J.S., and Krause, R.E., 2000, Design, revision, and application of ground-water flow models for simulation of selected water-management scenarios in the coastal area of Georgia and adjacent parts of South Carolina and Florida: U.S. Geological Survey Water-Resources Investigations Report 2000-4084, vii, 93 p. :ill. (some col.), maps (some col.) ;28 cm., https://doi.org/10.3133/wri004084.","productDescription":"vii, 93 p. :ill. (some col.), maps (some col.) ;28 cm.","costCenters":[{"id":13634,"text":"South Atlantic Water Science Center","active":true,"usgs":true}],"links":[{"id":157364,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":1980,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/wri/wri00-4084/","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Florida, Georgia, South Carolina","otherGeospatial":"Floridan aquifer system","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -83,30 ], [ -83,33 ], [ -80,33 ], [ -80,30 ], [ -83,30 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aa8e4b07f02db667db7","contributors":{"authors":[{"text":"Clarke, John S. jsclarke@usgs.gov","contributorId":400,"corporation":false,"usgs":true,"family":"Clarke","given":"John","email":"jsclarke@usgs.gov","middleInitial":"S.","affiliations":[{"id":316,"text":"Georgia Water Science Center","active":true,"usgs":true}],"preferred":true,"id":196651,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Krause, Richard E.","contributorId":40185,"corporation":false,"usgs":true,"family":"Krause","given":"Richard","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":196652,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":22402,"text":"ofr00466 - 2000 - MODFLOW-2000, the U.S. Geological Survey Modular Ground-Water Model; documentation of packages for simulating evapotranspiration with a segmented function (ETS1) and drains with return flow (DRT1)","interactions":[],"lastModifiedDate":"2019-02-05T16:11:13","indexId":"ofr00466","displayToPublicDate":"2001-06-01T00:00:00","publicationYear":"2000","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":"2000-466","title":"MODFLOW-2000, the U.S. Geological Survey Modular Ground-Water Model; documentation of packages for simulating evapotranspiration with a segmented function (ETS1) and drains with return flow (DRT1)","docAbstract":"<p>Two new packages for the U.S. Geological Survey modular finite-difference ground-water-flow model MODFLOW-2000 are documented. The new packages provide flexibility in simulating evapotranspiration and drain features not provided by the MODFLOW-2000 Evapotranspiration (EVT) and Drain (DRN) Packages. The report describes conceptualization of the packages, input instructions, listings and explanations of the source code, and example simulations.</p><p>The new Evapotranspiration Segments (ETS1) Package allows simulation of evapotranspiration with a user-defined relation between evapotranspiration rate and hydraulic head. This capability provides a degree of flexibility not supported by the EVT Package, which has been available in MODFLOW since its initial release. In the ETS1 Package, the relation of evapotranspiration rate to hydraulic head is conceptualized as a segmented line between an evaporation surface, defined as the elevation where the evapotranspiration rate reaches a maximum, and an elevation located at an extinction depth below the evaporation surface, where the evapotranspiration rate reaches zero. The user supplies input to define as many intermediate segment endpoints as desired to define the relation of evapotranspiration rate to head between these two elevations. The EVT Package, in contrast, simulates evapotranspiration with a single linear function.</p><p>The new Drain Return (DRT1) Package can be used to simulate the return flow of water discharged from a drain feature back into the ground-water system. The DRN Package, which has been available in MODFLOW since its initial release, does not have the capability to simulate return of flow. If the return-flow option of the DRT1 Package is selected, for each cell designated as a drain-return cell, the user has the option of specifying a proportion of the water simulated as leaving the ground-water system through the drain feature that is to be simulated as returning simultaneously to one other cell in the model.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr00466","issn":"0094-9140","usgsCitation":"Banta, E., 2000, MODFLOW-2000, the U.S. Geological Survey Modular Ground-Water Model; documentation of packages for simulating evapotranspiration with a segmented function (ETS1) and drains with return flow (DRT1): U.S. Geological Survey Open-File Report 2000-466, vi, 127 p., https://doi.org/10.3133/ofr00466.","productDescription":"vi, 127 p.","costCenters":[],"links":[{"id":155983,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/2000/0466/report-thumb.jpg"},{"id":51826,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/2000/0466/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a7fe4b07f02db648cd0","contributors":{"authors":[{"text":"Banta, Edward R.","contributorId":49820,"corporation":false,"usgs":true,"family":"Banta","given":"Edward R.","affiliations":[],"preferred":false,"id":188182,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":22521,"text":"ofr00495 - 2000 - Geologic datasets for weights of evidence analysis in northeast Washington: 1. Geologic raster data","interactions":[],"lastModifiedDate":"2023-06-22T13:28:41.577101","indexId":"ofr00495","displayToPublicDate":"2001-06-01T00:00:00","publicationYear":"2000","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":"2000-495","title":"Geologic datasets for weights of evidence analysis in northeast Washington: 1. Geologic raster data","docAbstract":"This dataset contains the combination of geology data (geologic units, faults, folds, and dikes) from 6 1:100,000 scale digital coverages in eastern Washington (Chewelah, Colville, Omak, Oroville, Nespelem, Republic). The data was converted to an Arc grid in ArcView using the Spatial Analyst extension.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr00495","usgsCitation":"Boleneus, D.E., and Causey, J.D., 2000, Geologic datasets for weights of evidence analysis in northeast Washington: 1. Geologic raster data: U.S. Geological Survey Open-File Report 2000-495, Report: 35 p., Readme, Metadata, Digital Database, Complete Digital Package, https://doi.org/10.3133/ofr00495.","productDescription":"Report: 35 p., Readme, Metadata, Digital Database, Complete Digital Package","numberOfPages":"35","additionalOnlineFiles":"Y","costCenters":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"links":[{"id":281976,"rank":3,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ofr00495.jpg"},{"id":281973,"rank":2,"type":{"id":16,"text":"Metadata"},"url":"https://pubs.usgs.gov/of/2000/0495/of00-495.met"},{"id":281975,"rank":1,"type":{"id":7,"text":"Companion Files"},"url":"https://pubs.usgs.gov/of/2000/0495/newafull.tar.gz"},{"id":281974,"rank":4,"type":{"id":7,"text":"Companion Files"},"url":"https://pubs.usgs.gov/of/2000/0495/newa.tar.gz"},{"id":281972,"rank":6,"type":{"id":20,"text":"Read Me"},"url":"https://pubs.usgs.gov/of/2000/0495/00readme.txt","linkFileType":{"id":2,"text":"txt"}},{"id":1300,"rank":5,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2000/0495/","linkFileType":{"id":5,"text":"html"}},{"id":410875,"rank":7,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_34735.htm","linkFileType":{"id":5,"text":"html"}},{"id":52027,"rank":8,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/2000/0495/pdf/of00-495.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Washington","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -120,\n              48\n            ],\n            [\n              -120,\n              49\n            ],\n            [\n              -117,\n              49\n            ],\n            [\n              -117,\n              48\n            ],\n            [\n              -120,\n              48\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4acce4b07f02db67e92f","contributors":{"authors":[{"text":"Boleneus, David E.","contributorId":87167,"corporation":false,"usgs":true,"family":"Boleneus","given":"David","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":188396,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Causey, J. Douglas","contributorId":41398,"corporation":false,"usgs":true,"family":"Causey","given":"J.","email":"","middleInitial":"Douglas","affiliations":[],"preferred":false,"id":188395,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":28939,"text":"wri994291 - 2000 - Site Selection for a Deep Monitor Well, Kualapuu, Molokai, Hawaii","interactions":[],"lastModifiedDate":"2012-03-08T17:16:15","indexId":"wri994291","displayToPublicDate":"2001-06-01T00:00:00","publicationYear":"2000","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"99-4291","title":"Site Selection for a Deep Monitor Well, Kualapuu, Molokai, Hawaii","docAbstract":"Management of the ground-water resources near Kualapuu on the island of Molokai, Hawaii, is hindered by the uncertainty in the vertical salinity structure in the aquifer. In the State of Hawaii, vertical profiles of ground-water salinity are commonly obtained from deep monitor wells, and these profiles are used to estimate the thicknesses of the freshwater part of the ground-water flow system and the freshwater-saltwater transition zone. Information from a deep monitor well would improve the understanding of the ground-water flow system and the ability to effectively manage the ground-water resources near Kualapuu; however, as of mid-1999 no deep monitor wells had been drilled on the island of Molokai. \r\n\r\nSelection of an appropriate site for drilling a deep monitor well in the Kualapuu area depends partly on where future ground-water development may occur. Simulations using an areally two-dimensional, steady-state, sharp-interface ground-water flow model previously developed for the island of Molokai, Hawaii, indicate that the southeastern part of the Kualapuu area is a possible area of future ground-water development because (1) withdrawals from this area have a small effect on water levels at existing wells in the Kualapuu area (relative to effects from withdrawals in other parts of the Kualapuu area that are outside of the dike complex), and (2) model-calculated water levels in this part of the Kualapuu area are high relative to water levels in other parts of the Kualapuu area that are outside of the dike complex. \r\n\r\nAdditional site-selection criteria include (1) ground-water level, (2) ground-surface altitude, (3) land classification, ownership, and accessibility, (4) geology, (5) locations of existing production wells, and (6) historical ground-water quality information. A deep monitor well in the Kualapuu area will likely be most useful for management purposes if it is located (1) in the vicinity of future ground-water development, (2) in an area where water levels are between about 8 and 12 feet above sea level, (3) at a ground-surface altitude that is between about 1,000 and 1,100 feet, (4) on government-owned land, (5) outside of the dike complex and as far from known volcanic vents as possible, (6) at least about 1,000 feet from, but within the same hydrogeologic setting as, existing or proposed production wells, and (7) east of well 0902-01. A viable area for drilling a deep monitor well is about a half mile southeast of existing wells 0801-01 to -03 and a half mile north of a known volcanic vent, Puu Luahine.","language":"ENGLISH","publisher":"Geological Survey (U.S.)","doi":"10.3133/wri994291","usgsCitation":"Oki, D.S., 2000, Site Selection for a Deep Monitor Well, Kualapuu, Molokai, Hawaii: U.S. Geological Survey Water-Resources Investigations Report 99-4291, vi, 50 p., https://doi.org/10.3133/wri994291.","productDescription":"vi, 50 p.","costCenters":[{"id":525,"text":"Pacific Islands Water Science Center","active":true,"usgs":true}],"links":[{"id":95733,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1999/4291/report.pdf","size":"10061","linkFileType":{"id":1,"text":"pdf"}},{"id":158310,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1999/4291/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e486fe4b07f02db50c94e","contributors":{"authors":[{"text":"Oki, Delwyn S. 0000-0002-6913-8804 dsoki@usgs.gov","orcid":"https://orcid.org/0000-0002-6913-8804","contributorId":1901,"corporation":false,"usgs":true,"family":"Oki","given":"Delwyn","email":"dsoki@usgs.gov","middleInitial":"S.","affiliations":[{"id":525,"text":"Pacific Islands Water Science Center","active":true,"usgs":true}],"preferred":true,"id":200649,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":28942,"text":"wri004035 - 2000 - Use of a ground-penetrating radar system to detect pre- and post-flood scour at selected bridge sites in New Hampshire, 1996-98","interactions":[],"lastModifiedDate":"2022-02-22T22:44:08.983417","indexId":"wri004035","displayToPublicDate":"2001-06-01T00:00:00","publicationYear":"2000","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"2000-4035","title":"Use of a ground-penetrating radar system to detect pre- and post-flood scour at selected bridge sites in New Hampshire, 1996-98","docAbstract":"Ground-penetrating radar was used to measure the depth and extent of existing and infilled scour holes and previous scour surfaces at seven bridges in New Hampshire from April 1996 to November 1998. Ground-penetrating-radar survey techniques initially were used by the U.S. Geological Survey to study streambed scour at 30 bridges. Sixteen of the 30 bridges were re-surveyed where floods exceeded a 2-year recurrence interval. A 300-megahertz signal was used in the ground-penetrating radar system that penetrated through depths as great as 20 feet of water and as great as 32 feet of streambed materials. Existing scour-hole dimensions, infilled thickness, previous scour surfaces, and streambed materials were detected using ground-penetrating radar. Depths to riprap materials and pier footings were identified and verified with bridge plans. Post data-collection-processing techniques were applied to assist in the interpretation of the data, and the processed data were displayed and printed as line plots. Processing included distance normalization, migration, and filtering but processing was kept to a minimum and some interference from multiple reflections was left in the record. Of the 16 post-flood bridges, 22 ground-penetrating-radar cross sections at 7 bridges were compared and presented in this report. Existing scour holes were detected during 1996 (pre-flood) data collection in nine cross sections where scour depths ranged from 1 to 3 feet. New scour holes were detected during 1998 (post-flood) data collection in four cross sections where scour depths were as great as 4 feet deep. Infilled scour holes were detected in seven cross sections, where depths of infilling ranged from less than 1 to 4 feet. Depth of infilling by means of steel rod and hammer was difficult to verify in the field because of cobble and boulder streambeds or deep water. Previous scour surfaces in streambed materials were identified in 15 cross sections and the depths to these surfaces ranged from 1 to 10 feet below the streambed. Riprap materials or pier footings were identified in all cross sections. Calculated record depths generally agree with bridge plans. Pier footings were exposed at two bridges and steel pile was exposed at one bridge. Exposures were verified by field observations.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri004035","usgsCitation":"Olimpio, J.R., 2000, Use of a ground-penetrating radar system to detect pre- and post-flood scour at selected bridge sites in New Hampshire, 1996-98: U.S. Geological Survey Water-Resources Investigations Report 2000-4035, iv, 28 p., https://doi.org/10.3133/wri004035.","productDescription":"iv, 28 p.","costCenters":[],"links":[{"id":158553,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":396297,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_26848.htm"},{"id":2241,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/wri004035","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"New Hampshire","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -72,\n              42.783\n            ],\n            [\n              -71.25,\n              42.783\n            ],\n            [\n              -71.25,\n              44.5\n            ],\n            [\n              -72,\n              44.5\n            ],\n            [\n              -72,\n              42.783\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a18e4b07f02db605142","contributors":{"authors":[{"text":"Olimpio, Joseph R.","contributorId":57878,"corporation":false,"usgs":true,"family":"Olimpio","given":"Joseph","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":200654,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":69569,"text":"i2737 - 2000 - Earthquakes in and near the northeastern United States, 1638-1998","interactions":[],"lastModifiedDate":"2017-02-28T14:17:52","indexId":"i2737","displayToPublicDate":"2001-06-01T00:00:00","publicationYear":"2000","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":320,"text":"IMAP","code":"I","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"2737","subseriesTitle":"GIS","title":"Earthquakes in and near the northeastern United States, 1638-1998","docAbstract":"The data are those used to make a large-format, colored map of earthquakes in the northeastern United States and adjacent parts of Canada and the Atlantic Ocean (Wheeler, 2000; Wheeler and others, 2001; references in Data_Quality_Information, Lineage). The map shows the locations of 1,069 known earthquakes of magnitude 3.0 or larger, and is designed for a non-technical audience. Colored circles represent earthquake locations, colored and sized by magnitude. Short descriptions, colonial-era woodcuts, newspaper headlines, and photographs summarize the dates, times of day, damage, and other effects of notable earthquakes. The base map shows color-coded elevation, shaded to emphasize relief.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/i2737","usgsCitation":"Wheeler, R.L., Trevor, N., Tarr, A., and Crone, A.J., 2000, Earthquakes in and near the northeastern United States, 1638-1998: U.S. Geological Survey IMAP 2737, 1 map, https://doi.org/10.3133/i2737.","productDescription":"1 map","costCenters":[],"links":[{"id":188271,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":6198,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/imap/i-2737/","linkFileType":{"id":5,"text":"html"}},{"id":110179,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_37628.htm","linkFileType":{"id":5,"text":"html"},"description":"37628"}],"scale":"1","country":"United States","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -81,38 ], [ -81,48 ], [ -66,48 ], [ -66,38 ], [ -81,38 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a50e4b07f02db6296d3","contributors":{"authors":[{"text":"Wheeler, R. L.","contributorId":34916,"corporation":false,"usgs":true,"family":"Wheeler","given":"R.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":280615,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Trevor, N.K.","contributorId":68792,"corporation":false,"usgs":true,"family":"Trevor","given":"N.K.","email":"","affiliations":[],"preferred":false,"id":280616,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Tarr, Arthur C.","contributorId":75903,"corporation":false,"usgs":true,"family":"Tarr","given":"Arthur C.","affiliations":[],"preferred":false,"id":280617,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Crone, A. J.","contributorId":84363,"corporation":false,"usgs":true,"family":"Crone","given":"A.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":280618,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":24522,"text":"ofr00501 - 2000 - SEPM field guide to the Florida reef tract, Key Largo area","interactions":[],"lastModifiedDate":"2012-02-02T00:08:04","indexId":"ofr00501","displayToPublicDate":"2001-06-01T00:00:00","publicationYear":"2000","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":"2000-501","title":"SEPM field guide to the Florida reef tract, Key Largo area","language":"ENGLISH","publisher":"U.S. Dept. of the Interior, U.S. Geological Survey,","doi":"10.3133/ofr00501","issn":"0094-9140","usgsCitation":"Lead by Shinn, E.A., Halley, R., and Hine, A.C., 2000, SEPM field guide to the Florida reef tract, Key Largo area: U.S. Geological Survey Open-File Report 2000-501, 40 p. :ill., maps ;28 cm., https://doi.org/10.3133/ofr00501.","productDescription":"40 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":155928,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/2000/0501/report-thumb.jpg"},{"id":53573,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/2000/0501/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0ee4b07f02db5fe0d4","contributors":{"authors":[{"text":"Lead by Shinn, Eugene A.","contributorId":49399,"corporation":false,"usgs":true,"family":"Lead by Shinn","given":"Eugene","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":192074,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Halley, Robert B.","contributorId":45692,"corporation":false,"usgs":true,"family":"Halley","given":"Robert B.","affiliations":[{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":false,"id":192073,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Hine, Albert C.","contributorId":87580,"corporation":false,"usgs":true,"family":"Hine","given":"Albert","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":192075,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":22084,"text":"ofr00426 - 2000 - Quality-assurance plan for water-quality activities in the North Florida Program Office, Florida District","interactions":[],"lastModifiedDate":"2012-02-02T00:07:52","indexId":"ofr00426","displayToPublicDate":"2001-06-01T00:00:00","publicationYear":"2000","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":"2000-426","title":"Quality-assurance plan for water-quality activities in the North Florida Program Office, Florida District","docAbstract":"In accordance with guidelines set forth by the Office of Water Quality in the Water Resources Division of the U.S. Geological Survey, a quality-assurance plan was created for use by the Florida District's North Florida Program Office in conducting water-quality activities. This plan documents the standards, policies, and procedures used by the North Florida Program Office for activities related to the collection, processing, storage, analysis, and publication of water-quality data.","language":"ENGLISH","publisher":"U.S. Dept. of the Interior, U.S. Geological Survey ;\r\nBranch of Information Services [distributor],","doi":"10.3133/ofr00426","issn":"0094-9140","usgsCitation":"Berndt, M.P., and Katz, B.G., 2000, Quality-assurance plan for water-quality activities in the North Florida Program Office, Florida District: U.S. Geological Survey Open-File Report 2000-426, v, 54 p. ill. ;28 cm., https://doi.org/10.3133/ofr00426.","productDescription":"v, 54 p. ill. ;28 cm.","costCenters":[],"links":[{"id":1200,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/ofr95-770/","linkFileType":{"id":5,"text":"html"}},{"id":154735,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/2000/0426/report-thumb.jpg"},{"id":51526,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/2000/0426/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a87e4b07f02db64ecf0","contributors":{"authors":[{"text":"Berndt, Marian P. (compiler)","contributorId":66289,"corporation":false,"usgs":true,"family":"Berndt","given":"Marian","suffix":"(compiler)","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":187003,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Katz, Brian G. bkatz@usgs.gov","contributorId":1093,"corporation":false,"usgs":true,"family":"Katz","given":"Brian","email":"bkatz@usgs.gov","middleInitial":"G.","affiliations":[],"preferred":true,"id":187002,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":21638,"text":"ofr00470 - 2000 - Borehole velocity measurements and geological conditions at thirteen sites in the Los Angeles, California region","interactions":[],"lastModifiedDate":"2012-02-02T00:07:56","indexId":"ofr00470","displayToPublicDate":"2001-06-01T00:00:00","publicationYear":"2000","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":"2000-470","title":"Borehole velocity measurements and geological conditions at thirteen sites in the Los Angeles, California region","language":"ENGLISH","publisher":"U.S. Dept. of the Interior, U.S. Geological Survey,","doi":"10.3133/ofr00470","issn":"0566-8174","usgsCitation":"Gibbs, J., Tinsley, J.C., Boore, D., and Joyner, W.B., 2000, Borehole velocity measurements and geological conditions at thirteen sites in the Los Angeles, California region: U.S. Geological Survey Open-File Report 2000-470, 118 p. ill., maps ;28 cm., https://doi.org/10.3133/ofr00470.","productDescription":"118 p. ill., maps ;28 cm.","costCenters":[],"links":[{"id":154252,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/2000/0470/report-thumb.jpg"},{"id":51195,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/2000/0470/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a14e4b07f02db6029ab","contributors":{"authors":[{"text":"Gibbs, James F.","contributorId":95880,"corporation":false,"usgs":true,"family":"Gibbs","given":"James F.","affiliations":[],"preferred":false,"id":185011,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Tinsley, J. C.","contributorId":65827,"corporation":false,"usgs":true,"family":"Tinsley","given":"J.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":185009,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Boore, D.M. 0000-0002-8605-9673","orcid":"https://orcid.org/0000-0002-8605-9673","contributorId":64226,"corporation":false,"usgs":true,"family":"Boore","given":"D.M.","affiliations":[],"preferred":false,"id":185008,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Joyner, W. B.","contributorId":70746,"corporation":false,"usgs":true,"family":"Joyner","given":"W.","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":185010,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":6750,"text":"fs15100 - 2000 - Shallow ground-water quality in the Platte River Valley alluvium, Nebraska, October-November 1997","interactions":[],"lastModifiedDate":"2012-02-10T00:10:07","indexId":"fs15100","displayToPublicDate":"2001-06-01T00:00:00","publicationYear":"2000","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":"151-00","title":"Shallow ground-water quality in the Platte River Valley alluvium, Nebraska, October-November 1997","docAbstract":"Nitrate was detected in samples from 25 of 27 wells; concentrations in 6 of the samples exceeded the U.S. Environmental Protection Agency maximum contaminant level of 10 milligrams per liter for drinking water.\r\n\r\nArsenic was detected in samples from 23 of 27 wells, but all concentrations were below the U.S. Environmental Protection Agency maximum contaminant level of 50 micrograms per liter.\r\n\r\nRadon was detected in samples from all 27 wells.\r\n\r\nNo volatile organic compounds were detected with concentrations greater than the method detection limit.","language":"ENGLISH","publisher":"U.S. Geological Survey","doi":"10.3133/fs15100","usgsCitation":"Parnell, J.M., 2000, Shallow ground-water quality in the Platte River Valley alluvium, Nebraska, October-November 1997: U.S. Geological Survey Fact Sheet 151-00, 6 p., https://doi.org/10.3133/fs15100.","productDescription":"6 p.","temporalStart":"1997-10-01","temporalEnd":"1997-11-30","costCenters":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"links":[{"id":118146,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/fs/2000/0151/report-thumb.jpg"},{"id":13208,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://ne.water.usgs.gov/Nawqa/pubs/final.fs-151-00.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":34120,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/fs/2000/0151/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -102.5,40 ], [ -102.5,43 ], [ -95.5,43 ], [ -95.5,40 ], [ -102.5,40 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49d3e4b07f02db5dc3ad","contributors":{"authors":[{"text":"Parnell, James M.","contributorId":80677,"corporation":false,"usgs":true,"family":"Parnell","given":"James","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":153272,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":27355,"text":"wri994290 - 2000 - Development of a stream habitat index for use with an Index of Biotic Integrity in the St. Croix River Basin, Minnesota","interactions":[],"lastModifiedDate":"2018-03-12T11:20:16","indexId":"wri994290","displayToPublicDate":"2001-06-01T00:00:00","publicationYear":"2000","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"99-4290","title":"Development of a stream habitat index for use with an Index of Biotic Integrity in the St. Croix River Basin, Minnesota","docAbstract":"<p>More than 70 streams in the St. Croix River Basin in Minnesota were sampled for fish community composition and physical habitat during 1996&ndash;98. A habitat index was developed based on measurements, field observations, and land use. The objective was to develope a habitat index for use to evaluate water quality and the effects of nonpoint-source effects not associated with habitat degradation. Core habitat variables were determined with a concurrence analysis using principal components of two subsets of sites with pristine or least affected habitat. Although core habitat variables differed slightly between data sets, sufficient similarities allowed development of an index. The index (the sum of pluses or minuses dependent on the variable&rsquo;s correlation to biotic integrity), composed of 12 core habitat variables in 5 classification groups (hydrology, geomorphology, substrate, instream habitat, and riparian/land use), was able to distinguish sites with low Index of Biotic Integrity scores not related to habitat degradation.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Mounds View, MN","doi":"10.3133/wri994290","collaboration":"Prepared in cooperation with the Minnesota Pollution Control Agency","usgsCitation":"Goldstein, R.M., Lorenz, D., and Niemela, S., 2000, Development of a stream habitat index for use with an Index of Biotic Integrity in the St. Croix River Basin, Minnesota: U.S. Geological Survey Water-Resources Investigations Report 99-4290, iv, 14 p., https://doi.org/10.3133/wri994290.","productDescription":"iv, 14 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":392,"text":"Minnesota Water Science Center","active":true,"usgs":true}],"links":[{"id":321051,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/wri994290.JPG"},{"id":12256,"rank":1,"type":{"id":11,"text":"Document"},"url":"https://mn.water.usgs.gov/publications/pubs/99-4290.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Minnesota, Wisconsin","otherGeospatial":"St. Croix River Basin","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -93.109130859375, 45.334771196762766 ], [ -93.14208984375, 45.37916094640917 ], [ -93.1585693359375, 45.398449976304086 ], [ -93.16131591796875, 45.42544355958045 ], [ -93.17230224609375, 45.463983441272745 ], [ -93.16955566406249, 45.537136680398596 ], [ -93.13934326171875, 45.598665689820656 ], [ -93.12286376953124, 45.65052836822275 ], [ -93.1256103515625, 45.71193311776845 ], [ 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M.","contributorId":98305,"corporation":false,"usgs":true,"family":"Goldstein","given":"R.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":197972,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Lorenz, D. L.","contributorId":10776,"corporation":false,"usgs":true,"family":"Lorenz","given":"D. L.","affiliations":[],"preferred":false,"id":197970,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Niemela, Scott","contributorId":63056,"corporation":false,"usgs":true,"family":"Niemela","given":"Scott","affiliations":[],"preferred":false,"id":197971,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":30282,"text":"wri004019 - 2000 - Water-quality trend analysis and sampling design for the Souris River, Saskatchewan, North Dakota, and Manitoba","interactions":[],"lastModifiedDate":"2018-03-16T12:56:38","indexId":"wri004019","displayToPublicDate":"2001-06-01T00:00:00","publicationYear":"2000","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"2000-4019","title":"Water-quality trend analysis and sampling design for the Souris River, Saskatchewan, North Dakota, and Manitoba","docAbstract":"<p>The Souris River Basin is a 24,600-square-mile basin located in southeast Saskatchewan, north-central North Dakota, and southwest Manitoba.&nbsp; The Souris River Bilateral Water Quality Monitoring Group, formed in 1989 by the governments of Canada and the United States, is responsible for documenting trends in water quality in the Souris River and making recommendations for monitoring future water-quality conditions.&nbsp; This report presents results of a study conducted for the Bilateral Water Quality Monitoring Group by the U.S. Geological Survey, in cooperation with the North Dakota Department of Health, to analyze historic trends in water quality in the Souris River and to determine efficient sampling designs for monitoring future trends.&nbsp; U.S. Geological Survey and Environment Canada water-quality data collected during 1977-96 from four sites near the boundary crossings between Canada and the United States were included in the trend analysis.</p><p>&nbsp;A parametric time-series model was developed for detecting trends in historic constituent concentration data.&nbsp; The model can be applied to constituents that have at least 90 percent of observations above detection limits of the analyses, which, for the Souris River, includes most major ions and nutrients and many trace elements.&nbsp; The model can detect complex nonmonotonic trends in concentration in the presence of complex interannual and seasonal variability in daily discharge.&nbsp; A key feature of the model is its ability to handle highly irregular sampling intervals.&nbsp; For example, the intervals between concentration measurements may be be as short as 10 days to as long as several months, and the number of samples in any given year can range from zero to 36.</p><p>&nbsp;Results from the trend analysis for the Souris River indicated numerous trends in constituent concentration.&nbsp; The most significant trends at the two sites located near the upstream boundary crossing between Saskatchewan and North Dakota consisted of increases in concentrations of most major ions, dissolved boron, and dissolved arsenic during 1987-91 and decreases in concentrations of the same constituents during 1992-96.&nbsp; Significant trends at the two sites located near the downstream boundary crossing between North Dakota and Manitoba included increases in dissolved sodium, dissolved chloride, and total phosphorus during 1977-86, decreases in dissolved oxygen and dissolved boron and increases in total phosphorus and dissolved iron during 1987-91, and a decrease in total phosphorus during 1992-96.</p><p>&nbsp;The time-series model also was used to determine the sensitivity of various sampling designs for monitoring future water-quality trends in the Souris River.&nbsp; It was determined that at least two samples per year are required in each of three seasons--March through June, July through October, and November through February--to obtain reasonable sensitivity for detecting trends in each season.&nbsp; In addition, substantial improvements occurred in sensitivity for detecting trends by adding a third sample for major ions and trace elements in March through June, adding a third sample for nutrients in July through October, and adding a third sample for nutrients, trace elements, and dissolved oxygen in November through February.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri004019","usgsCitation":"Vecchia, A.V., 2000, Water-quality trend analysis and sampling design for the Souris River, Saskatchewan, North Dakota, and Manitoba: U.S. Geological Survey Water-Resources Investigations Report 2000-4019, iv, 77 p., https://doi.org/10.3133/wri004019.","productDescription":"iv, 77 p.","costCenters":[{"id":478,"text":"North Dakota Water Science Center","active":true,"usgs":true},{"id":34685,"text":"Dakota Water Science Center","active":true,"usgs":true}],"links":[{"id":159690,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":2444,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://nd.water.usgs.gov/pubs/wri/wri004019/","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae5e4b07f02db68a4ba","contributors":{"authors":[{"text":"Vecchia, Aldo V. 0000-0002-2661-4401","orcid":"https://orcid.org/0000-0002-2661-4401","contributorId":41810,"corporation":false,"usgs":true,"family":"Vecchia","given":"Aldo","email":"","middleInitial":"V.","affiliations":[],"preferred":false,"id":202981,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":30067,"text":"wri004092 - 2000 - The effects of calcium magnesium acetate (CMA) deicing material on the water quality of Bear Creek, Clackamas County, Oregon, 1999","interactions":[],"lastModifiedDate":"2022-10-26T16:21:36.132248","indexId":"wri004092","displayToPublicDate":"2001-06-01T00:00:00","publicationYear":"2000","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"2000-4092","title":"The effects of calcium magnesium acetate (CMA) deicing material on the water quality of Bear Creek, Clackamas County, Oregon, 1999","docAbstract":"<p>This report presents the results of a study by the U.S. Geological Survey, done in cooperation with the Oregon Department of Transportation (ODOT), to evaluate the effects of the highway deicing material, calcium magnesium acetate (CMA), on the water quality of Bear Creek, in the Cascade Range of Oregon. ODOT began using CMA (an alternative deicer that has fewer adverse environmental effects than road salt) in the mid-1990s and began this study with the USGS to ensure that there were no unexpected effects on the water quality of Bear Creek. Streamflow, precipitation, dissolved oxygen, pH, specific conductance, and water temperature were measured continuously through the 1998?99 winter. There was no measurable effect of the application of CMA to Highway 26 on the biochemical oxygen demand (BOD), calcium concentration, or magnesium concentration of Bear Creek and its tributaries. BOD was small in all of the water samples, some of which were collected before CMA application, and some of which were collected after application. Five-day BOD values ranged from 0.1 milligrams per liter to 1.5 milligrams per liter, and 20-day BOD values ranged from 0.2 milligrams per liter to 2.0 milligrams per liter. Dissolved copper concentrations in a small tributary ditch on the north side of Highway 26 exceeded the U.S. Environmental Protection Agency aquatic life criteria on three occasions. These exceedances were probably not caused by the application of CMA because (1) one of the samples was a background sample (no recent CMA application), and (2) dissolved copper was not detected in Bear Creek water samples to which CMA was added during laboratory experiments.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri004092","usgsCitation":"Tanner, D.Q., and Wood, T.M., 2000, The effects of calcium magnesium acetate (CMA) deicing material on the water quality of Bear Creek, Clackamas County, Oregon, 1999: U.S. Geological Survey Water-Resources Investigations Report 2000-4092, iv, 22 p., https://doi.org/10.3133/wri004092.","productDescription":"iv, 22 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":518,"text":"Oregon Water Science Center","active":true,"usgs":true}],"links":[{"id":160126,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":408755,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_27445.htm","linkFileType":{"id":5,"text":"html"}},{"id":2494,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/2000/4092/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Oregon","county":"Clackamas County","otherGeospatial":"Bear Creek","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -121.95,\n              45.35\n            ],\n            [\n              -121.95,\n              45.329\n            ],\n            [\n              -121.908,\n              45.329\n            ],\n            [\n              -121.908,\n              45.35\n            ],\n            [\n              -121.95,\n              45.35\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a9be4b07f02db65e019","contributors":{"authors":[{"text":"Tanner, Dwight Q.","contributorId":93452,"corporation":false,"usgs":true,"family":"Tanner","given":"Dwight","email":"","middleInitial":"Q.","affiliations":[],"preferred":false,"id":202620,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Wood, Tamara M. 0000-0001-6057-8080 tmwood@usgs.gov","orcid":"https://orcid.org/0000-0001-6057-8080","contributorId":1164,"corporation":false,"usgs":true,"family":"Wood","given":"Tamara","email":"tmwood@usgs.gov","middleInitial":"M.","affiliations":[{"id":518,"text":"Oregon Water Science Center","active":true,"usgs":true}],"preferred":true,"id":202619,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":31203,"text":"ofr0114 - 2000 - Publications of the Volcano Hazards Program 1999","interactions":[],"lastModifiedDate":"2012-02-02T00:09:05","indexId":"ofr0114","displayToPublicDate":"2001-06-01T00:00:00","publicationYear":"2000","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":"2001-14","title":"Publications of the Volcano Hazards Program 1999","language":"ENGLISH","doi":"10.3133/ofr0114","usgsCitation":"Nathenson, M., 2000, Publications of the Volcano Hazards Program 1999: U.S. Geological Survey Open-File Report 2001-14, 10 p., https://doi.org/10.3133/ofr0114.","productDescription":"10 p.","costCenters":[],"links":[{"id":160327,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":2741,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2001/of01-014/","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a90e4b07f02db655e8e","contributors":{"authors":[{"text":"Nathenson, Manuel 0000-0002-5216-984X mnathnsn@usgs.gov","orcid":"https://orcid.org/0000-0002-5216-984X","contributorId":1358,"corporation":false,"usgs":true,"family":"Nathenson","given":"Manuel","email":"mnathnsn@usgs.gov","affiliations":[{"id":617,"text":"Volcano Science Center","active":true,"usgs":true}],"preferred":true,"id":205319,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":24829,"text":"ofr00390 - 2000 - Research, methodology, and applications of probabilistic seismic-hazard mapping of the Central and Eastern United States; minutes of a workshop on June 13-14, 2000, at Saint Louis University","interactions":[],"lastModifiedDate":"2017-03-07T11:02:51","indexId":"ofr00390","displayToPublicDate":"2001-06-01T00:00:00","publicationYear":"2000","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":"2000-390","title":"Research, methodology, and applications of probabilistic seismic-hazard mapping of the Central and Eastern United States; minutes of a workshop on June 13-14, 2000, at Saint Louis University","docAbstract":"<p>The U.S. Geological Survey (USGS) is updating and revising its 1996 national seismic-hazard maps for release in 2001. Part of this process is the convening of four regional workshops with earth scientists and other users of the maps. The second of these workshops was sponsored by the USGS and the Mid-America Earthquake Center, and was hosted by Saint Louis University on June 13-14, 2000.</p><p>The workshop concentrated on the central and eastern U.S. (CEUS) east of the Rocky Mountains. The tasks of the workshop were to (1) evaluate new research findings that are relevant to seismic hazard mapping, (2) discuss modifications in the inputs and methodology used in the national maps, (3) discuss concerns by engineers and other users about the scientific input to the maps and the use of the hazard maps in building codes, and (4) identify needed research in the CEUS that can improve the seismic hazard maps and reduce their uncertainties.</p><p>&nbsp;These minutes summarize the workshop discussions. This is not a transcript; some individual remarks and short discussions of side issues and logistics were omitted. Named speakers were sent a draft of the minutes with a request for corrections of any errors in remarks attributed to them. Nine people returned corrections, amplifications, or approvals of their remarks as reported. The rest of this document consists of the meeting agenda, discussion summaries, and a list of the 60 attendees.</p>","language":"English","publisher":"U.S. Department of the Interior, U.S. Geological Survey,","publisherLocation":"Reston, VA","doi":"10.3133/ofr00390","issn":"0094-9140","usgsCitation":"Wheeler, R.L., and Perkins, D.M., 2000, Research, methodology, and applications of probabilistic seismic-hazard mapping of the Central and Eastern United States; minutes of a workshop on June 13-14, 2000, at Saint Louis University: U.S. Geological Survey Open-File Report 2000-390, 18 p., https://doi.org/10.3133/ofr00390.","productDescription":"18 p.","costCenters":[],"links":[{"id":157127,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/2000/0390/report-thumb.jpg"},{"id":53833,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/2000/0390/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":1848,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2000/ofr-00-0390/","linkFileType":{"id":5,"text":"html"}}],"country":"United States","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a54e4b07f02db62c3b0","contributors":{"authors":[{"text":"Wheeler, Russell L. wheeler@usgs.gov","contributorId":858,"corporation":false,"usgs":true,"family":"Wheeler","given":"Russell","email":"wheeler@usgs.gov","middleInitial":"L.","affiliations":[],"preferred":false,"id":192640,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Perkins, David M. perkins@usgs.gov","contributorId":2114,"corporation":false,"usgs":true,"family":"Perkins","given":"David","email":"perkins@usgs.gov","middleInitial":"M.","affiliations":[{"id":301,"text":"Geologic Hazards Team","active":false,"usgs":true}],"preferred":true,"id":192641,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":28699,"text":"wri004020 - 2000 - Environmental setting and its relations to water quality in the Kanawha River basin","interactions":[],"lastModifiedDate":"2012-02-02T00:08:46","indexId":"wri004020","displayToPublicDate":"2001-06-01T00:00:00","publicationYear":"2000","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"2000-4020","title":"Environmental setting and its relations to water quality in the Kanawha River basin","docAbstract":"The Kanawha River and its major tributary, the New River, drain 12,233 mi2 in West Virginia, Virginia, and North Carolina. Altitude ranges from about 550 ft to more than 4,700 ft. The Kanawha River Basin is mountainous, and includes parts of three physiographic provinces, the Blue Ridge (17 percent), Valley and Ridge (23 percent), and Appalachian Plateaus (60 percent). In the Appalachian Plateaus Province, little of the land is flat, and most of the flat land is in the flood plains and terraces of streams; this has caused most development in this part of the basin to be near streams. The Blue Ridge Province is composed of crystalline rocks, and the Valley and Ridge and Appalachian Plateaus Provinces contain both carbonate and clastic rocks. Annual precipitation ranges from about 36 in. to more than 60 in., and is orographically affected, both locally and regionally. Average annual air temperature ranges from about 43?F to about 55?F, and varies with altitude but not physiographic province. Precipitation is greatest in the summer and least in the winter, and has the least seasonal variation in the Blue Ridge Province.\r\n\r\nIn 1990, the population of the basin was about 870,000, of whom about 25 percent lived in the Charleston, W. Va. metropolitan area. About 75 million tons of coal were mined in the Kanawha River Basin in 1998. This figure represents about 45 percent of the coal mined in West Virginia, and about seven percent of the coal mined in the United States. Dominant forest types in the basin are Northern Hardwood, Oak-Pine, and Mixed Mesophytic. Agricultural land use is more common in the Valley and Ridge and Blue Ridge Provinces than in the Appalachian Plateaus Province. Cattle are the principal agricultural products of the basin.\r\n\r\nStreams in the Blue Ridge Province and Allegheny Highlands have the most runoff in the basin, and streams in the Valley and Ridge Province and the southwestern Appalachian Plateaus have the least runoff. Streamflow is greatest in the spring and least in the autumn. About 61 percent of the basin's population use surface water from public supply for their domestic needs; about 30 percent use self-supplied ground water, and about nine percent use ground water from public supply. In 1995, total withdrawal of water in the basin was about 1,130 Mgal/d. Total consumptive use was about 118 Mgal/d. Surface water in the Blue Ridge Province is usually dilute (less than 100 mg/L dissolved solids) and well aerated. Dissolved- solids concentrations in streams of the Valley and Ridge Province at low flow are typically greater (150-180 mg/L) than those in the Blue Ridge Province. The Appalachian Plateaus Province contains streams with the most dilute (less than 30 mg/L dissolved solids) and least dilute (more than 500 mg/L dissolved solids) water in the basin.\r\n\r\nCoal mining has degraded more miles of streams in the basin than any other land use. Streams that receive coal-mine drainage may be affected by sedimentation, and typically contain high concentrations of sulfate, iron, and manganese. Other major water-quality issues include inadequate domestic sewage treatment, present and historic disposal of industrial wastes, and logging, which results in the addition of sediment, nutrients, and other constituents to the water.\r\n\r\nOne hundred eighteen fish species are reported from the Kanawha River system downstream from Kanawha Falls. Of these, 15 are listed as possible, probable, or known introductions. None of these fish species is endemic to the Kanawha River Basin. The New River system has only 46 native fishes, the lowest ratio of native fishes to drainage area of any river system in the eastern United States, and the second-highest proportion of endemic fish species (eight of 46) of any river system in the eastern United States.","language":"ENGLISH","publisher":"U.S. Dept. of the Interior, U.S. Geological Survey ;\r\nBranch of Information Services [distributor],","doi":"10.3133/wri004020","usgsCitation":"Messinger, T., and Hughes, C., 2000, Environmental setting and its relations to water quality in the Kanawha River basin: U.S. Geological Survey Water-Resources Investigations Report 2000-4020, vii, 57 p. :ill., maps (some col.) ;28 cm., https://doi.org/10.3133/wri004020.","productDescription":"vii, 57 p. :ill., maps (some col.) ;28 cm.","costCenters":[],"links":[{"id":159208,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":2274,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/wri004020/","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a9ae4b07f02db65dacb","contributors":{"authors":[{"text":"Messinger, Terence 0000-0003-4084-9298 tmessing@usgs.gov","orcid":"https://orcid.org/0000-0003-4084-9298","contributorId":2717,"corporation":false,"usgs":true,"family":"Messinger","given":"Terence","email":"tmessing@usgs.gov","affiliations":[{"id":642,"text":"West Virginia Water Science Center","active":true,"usgs":true}],"preferred":true,"id":200252,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hughes, C.A.","contributorId":13278,"corporation":false,"usgs":true,"family":"Hughes","given":"C.A.","email":"","affiliations":[],"preferred":false,"id":200253,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":28619,"text":"wri994289 - 2000 - Quantity and chemical quality of recharge, and updated water budgets, for the basin-fill aquifer in Eagle Valley, western Nevada","interactions":[],"lastModifiedDate":"2013-07-08T13:14:23","indexId":"wri994289","displayToPublicDate":"2001-06-01T00:00:00","publicationYear":"2000","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"99-4289","title":"Quantity and chemical quality of recharge, and updated water budgets, for the basin-fill aquifer in Eagle Valley, western Nevada","language":"ENGLISH","publisher":"U.S. Dept. of the Interior, U.S. Geological Survey ;Information Services [distributor],","doi":"10.3133/wri994289","usgsCitation":"Maurer, D.K., and Thodal, C.E., 2000, Quantity and chemical quality of recharge, and updated water budgets, for the basin-fill aquifer in Eagle Valley, western Nevada: U.S. Geological Survey Water-Resources Investigations Report 99-4289, iv, 46 p. :ill. (some col.), col. maps ;28 cm., https://doi.org/10.3133/wri994289.","productDescription":"iv, 46 p. :ill. (some col.), col. maps ;28 cm.","costCenters":[],"links":[{"id":159116,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1999/4289/report-thumb.jpg"},{"id":274648,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1999/4289/report.pdf"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a82e4b07f02db64ad77","contributors":{"authors":[{"text":"Maurer, Douglas K. dkmaurer@usgs.gov","contributorId":2308,"corporation":false,"usgs":true,"family":"Maurer","given":"Douglas","email":"dkmaurer@usgs.gov","middleInitial":"K.","affiliations":[],"preferred":true,"id":200125,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Thodal, Carl E. 0000-0003-0782-3280 cethodal@usgs.gov","orcid":"https://orcid.org/0000-0003-0782-3280","contributorId":2292,"corporation":false,"usgs":true,"family":"Thodal","given":"Carl","email":"cethodal@usgs.gov","middleInitial":"E.","affiliations":[{"id":465,"text":"Nevada Water Science Center","active":true,"usgs":true}],"preferred":true,"id":200124,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":28142,"text":"wri20004031 - 2000 - Water-quality assessment of part of the Upper Mississippi River Basin, Minnesota and Wisconsin: Trace elements in streambed sediment and fish livers, 1995-96","interactions":[],"lastModifiedDate":"2022-06-30T20:40:33.874372","indexId":"wri20004031","displayToPublicDate":"2001-06-01T00:00:00","publicationYear":"2000","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"2000-4031","title":"Water-quality assessment of part of the Upper Mississippi River Basin, Minnesota and Wisconsin: Trace elements in streambed sediment and fish livers, 1995-96","docAbstract":"<p>Trace elements were analyzed in streambed sediment and fish livers in part of the Upper Mississippi River Basin as part of the U.S. Geological Survey&rsquo;s National Water-Quality Assessment Program. The purpose of this report was to describe the occurrence and distribution of trace elements, describe the relations of concentrations measured to natural and anthropogenic factors, and describe any relation between concentrations in streambed sediment and fish livers. The study unit included the part of the Upper Mississippi River Basin from the river&rsquo;s source in northern Minnesota to the outlet of Lake Pepin, a natural lake on the river located near Red Wing, Minnesota. Streambed sediment samples were collected from 27 sites located throughout the study unit, and fish were obtained from 25 sites.</p>\n<p>The occurrence and distribution of trace elements in streambed sediment were related to land use and the composition of surficial glacial deposits covering the study unit. Concentrations of antimony, arsenic, cadmium, copper, lead, mercury, nickel, and zinc in streambed sediment were primarily related to urban land use. Concentrations of these elements generally were greatest in streambed sediment collected at sites within or near urban areas in the study unit. The greatest concentrations of most of these elements were measured in streambed sediment obtained from Shingle Creek. Lead concentrations in streambed sediment Shingle Creek increased in the downstream direction. This pattern probably reflects the past use of leaded gasoline, pesticides, or paints.</p>\n<p>Cadmium concentrations in sediment from the Mississippi River were greatest at Nininger, Minnesota and in Lake Pepin. This pattern suggested that inputs of cadmium into the river were from the TCMA.</p>\n<p>Arsenic concentrations were greatest in streambed sediment collected from Cedar Creek, Shingle Creek, and the Vermillion River. Increased arsenic and iron concentrations in sediment from Cedar Creek, the Vermillion River, and the most upstream site on Shingle Creek suggested a local source of sulfide minerals or preferential sorption of arsenic to streambed sediment. The greatest concentrations of mercury were measured in streambed sediment collected from the Mississippi River at Grand Rapids and Minneapolis, Minnesota; Shingle Creek at 46th Street in Minneapolis, Minnesota; the Namekagon River above Spring Lake Creek near Hayward, Wisconsin; the St. Croix River at Hudson, Wisconsin; and the Vermillion River near Empire, Minnesota.</p>\n<p>In fish livers, all of the trace elements analyzed were detected except antimony, beryllium, cobalt, and uranium. Trace element concentrations in fish livers generally did not show any pronounced patterns. Ranges for concentrations of arsenic, cadmium, chromium, copper, lead, mercury, nickel, selenium, and zinc were similar to those measured in 20 other NAWQA studies across the United States. Cadmium concentrations in fish livers were moderately correlated to fish length and weight. There were no relations between trace element concentrations in fish livers and streambed sediment.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Mounds View, MN","doi":"10.3133/wri20004031","usgsCitation":"Kroening, S.E., Fallon, J.D., and Lee, K., 2000, Water-quality assessment of part of the Upper Mississippi River Basin, Minnesota and Wisconsin: Trace elements in streambed sediment and fish livers, 1995-96: U.S. Geological Survey Water-Resources Investigations Report 2000-4031, vi, 26 p., https://doi.org/10.3133/wri20004031.","productDescription":"vi, 26 p.","onlineOnly":"N","additionalOnlineFiles":"N","temporalStart":"1995-01-01","temporalEnd":"1996-12-31","costCenters":[{"id":392,"text":"Minnesota Water Science Center","active":true,"usgs":true}],"links":[{"id":120068,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/wri_2000_4031.jpg"},{"id":402789,"rank":3,"type":{"id":36,"text":"NGMDB Index 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,{"id":27861,"text":"wri934167 - 2000 - Water resources of the Blackstone River basin, Massachusetts","interactions":[],"lastModifiedDate":"2018-01-11T14:04:58","indexId":"wri934167","displayToPublicDate":"2001-06-01T00:00:00","publicationYear":"2000","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"93-4167","title":"Water resources of the Blackstone River basin, Massachusetts","docAbstract":"<p>By 2020, demand for water in the Blackstone River Basin is expected to be 52 million gallons per day, one-third greater than the demand of 39 million gallons per day in 1980. Most of this increase is expected to be supplied by increased withdrawals of ground water from stratified-drift aquifers in the eastern and northern parts of the basin. Increased withdrawals from stratified-drift aquifers along the Blackstone River and in the western part of the basin also are expected.</p><p>The eastern and northern parts of the Blackstone River Basin contain numerous small, discontinuous aquifers which, as a group, comprise the largest ground-water resource of the study area. Fifteen aquifers, ranging in areal extent from 0.57 to 4.3 square miles, were identified. These aquifers have maximum saturated thicknesses ranging from less than 10 feet to 105 feet and maximum transmissivities ranging from less than 1,000 to more than 20,000 feet squared per day. Yields of nine study aquifers were estimated by use of digital ground-water-flow models. Yields depend on the hydraulic properties of the aquifer and the amount of streamflow available for depletion by wells. If streamflow is maintained at 98-percent duration, long-term yields from the aquifers that would be expected to be equaled or exceeded 50 percent of the time range from 0.22 to 11 million gallons per day, and long-term yields equaled or exceeded 95 percent of the time range from 0.06 to 1.0 million gallons per day. If streamflow is maintained at 99.5-percent duration, long-term yields equaled or exceeded 50 percent of the time range from 0.22 to 11 million gallons per day, long-term yields equaled or exceeded 95 percent of the time range from 0.04 to 1.4 million gallons per day, and longterm yields equaled or exceeded 98 percent of the time range from 0.02 to 0.39 million gallons per day. Maintaining streamflow at 98-percent duration is a more restrictive criterion than maintaining streamflow at 99.5-percent duration. </p><p>The upper Lake Quinsigamond, upper West River, and Stone Brook aquifers are capable of sustaining withdrawals of at least 1 million gallons per day more than their rates in the mid-1980s. The upper Mill River and Auburn aquifers are not capable of sustaining additional withdrawals of 0.25 million gallons per day. Ground-water quality in the Auburn aquifer has been degraded by activities and contaminants associated with urbanization.</p><p>A nearly continuous deposit of stratified drift almost 30 miles long and from 400 feet to more than 1 mile wide occupies lowland areas along the southeastern part of the Blackstone River. These deposits were divided into four aquifers ranging in areal extent from 1.8 to 3.5 square miles. These aquifers have maximum saturated thicknesses ranging from 54 to 170 feet and maximum transmissivities ranging from less than 1,500 to more than 20,000 feet squared per day. The Blackstone River receives substantial amounts of treated municipal wastewater. Infiltration of poor-quality surface water has significantly increased the specific conductance and the concentrations of all major ions, ammonia,&nbsp;iron, and manganese in the water pumped from at least two wells near the river. These wells derive about 41 and 48 percent of their yield from infiltrated surface water. At both sites, aquifer heterogeneity controlled the movement of infiltrated water to the wells. At one of these sites, where the flow of infiltrated water was tracked (by use of a digital model) in three dimensions, infiltrated water moved to the well through gravel layers that did not constitute the entire thickness of the aquifer. Changes in stream discharge that resulted in changes in surface-water quality also affected the quality of ground water at that site. </p><p>The western part of the Blackstone River Basin contains the smallest aquifers evaluated in the study area. Six aquifers, ranging in areal extent from 0.05 to 1.3 square miles, were identified. The hydraulic properties of most of these aquifers have not been determined, but available data indicate that maximum saturated thicknesses range from 28 to 71 feet and maximum transmissivities range from 2,300 to 15,000 feet squared per day.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri934167","collaboration":"Prepared in cooperation with the Massachusetts Department of Environmental Management, Office of Water Resources","usgsCitation":"Izbicki, J., 2000, Water resources of the Blackstone River basin, Massachusetts: U.S. Geological Survey Water-Resources Investigations Report 93-4167, Report: vi, 115 p.; 2 Plates: 46.47 x 34.00 inches and 46.67 x 34.00, https://doi.org/10.3133/wri934167.","productDescription":"Report: vi, 115 p.; 2 Plates: 46.47 x 34.00 inches and 46.67 x 34.00","costCenters":[],"links":[{"id":56684,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1993/4167/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":119867,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1993/4167/report-thumb.jpg"},{"id":350422,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1993/4167/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":350421,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1993/4167/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"48000","country":"United States","state":"Massachusetts","otherGeospatial":"Blackstone River Basin","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -71.93367004394531,\n              41.9\n            ],\n            [\n              -71.3,\n              41.9\n            ],\n            [\n              -71.3,\n              42.371227435069805\n            ],\n            [\n              -71.93367004394531,\n              42.371227435069805\n            ],\n            [\n              -71.93367004394531,\n              41.9\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f4e4b07f02db5f05ec","contributors":{"authors":[{"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":198801,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":28549,"text":"wri004076 - 2000 - Spatial and seasonal variability of nutrients, pesticides, bacteria, and suspended sediment in the Santee River basin and coastal drainages, North and South Carolina, 1995-97","interactions":[],"lastModifiedDate":"2019-12-30T11:51:54","indexId":"wri004076","displayToPublicDate":"2001-06-01T00:00:00","publicationYear":"2000","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"2000-4076","title":"Spatial and seasonal variability of nutrients, pesticides, bacteria, and suspended sediment in the Santee River basin and coastal drainages, North and South Carolina, 1995-97","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri004076","usgsCitation":"Maluk, T.L., 2000, Spatial and seasonal variability of nutrients, pesticides, bacteria, and suspended sediment in the Santee River basin and coastal drainages, North and South Carolina, 1995-97: U.S. Geological Survey Water-Resources Investigations Report 2000-4076, vi, 46 p., https://doi.org/10.3133/wri004076.","productDescription":"vi, 46 p.","costCenters":[{"id":13634,"text":"South Atlantic Water Science Center","active":true,"usgs":true}],"links":[{"id":276448,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/2000/4076/report.pdf"},{"id":159163,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/2000/4076/report-thumb.jpg"}],"country":"United States","state":"North Carolina, South Carolina","otherGeospatial":"Santee River Basin","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -79.8046875,\n              33.137551192346145\n            ],\n            [\n              -79.013671875,\n              32.47269502206151\n            ],\n            [\n              -77.6513671875,\n              33.90689555128866\n            ],\n            [\n              -77.783203125,\n              34.59704151614417\n            ],\n            [\n              -79.4970703125,\n              36.4566360115962\n            ],\n            [\n              -80.244140625,\n              36.38591277287651\n            ],\n            [\n              -80.771484375,\n              36.27970720524017\n            ],\n            [\n              -82.265625,\n              35.71083783530009\n            ],\n            [\n              -82.001953125,\n              34.66935854524543\n            ],\n            [\n              -79.8046875,\n              33.137551192346145\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e5e4b07f02db5e6ec0","contributors":{"authors":[{"text":"Maluk, Terry L.","contributorId":82690,"corporation":false,"usgs":true,"family":"Maluk","given":"Terry","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":200009,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":27888,"text":"wri994282 - 2000 - Precipitation-runoff simulations for the upper part of the Truckee River basin, California and Nevada","interactions":[],"lastModifiedDate":"2012-02-02T00:08:40","indexId":"wri994282","displayToPublicDate":"2001-06-01T00:00:00","publicationYear":"2000","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"99-4282","title":"Precipitation-runoff simulations for the upper part of the Truckee River basin, California and Nevada","language":"ENGLISH","publisher":"U.S. Dept. of the Interior, U.S. Geological Survey ;\r\nInformation Services,","doi":"10.3133/wri994282","usgsCitation":"Jeton, A.E., 2000, Precipitation-runoff simulations for the upper part of the Truckee River basin, California and Nevada: U.S. Geological Survey Water-Resources Investigations Report 99-4282, iv, 41 p. :ill., col. map ;28 cm., https://doi.org/10.3133/wri994282.","productDescription":"iv, 41 p. :ill., col. map ;28 cm.","costCenters":[],"links":[{"id":158698,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1999/4282/report-thumb.jpg"},{"id":56709,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1999/4282/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad0e4b07f02db680c3a","contributors":{"authors":[{"text":"Jeton, Anne E.","contributorId":45351,"corporation":false,"usgs":true,"family":"Jeton","given":"Anne","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":198853,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
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