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These data, accumulated during many water years, constitute a valuable database for developing an improved understanding of the water resources of the State. To make these data readily available to interested parties outside the USGS, the data are published annually in a report series entitled \"Water Resources Data for Arizona.\"</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wdrAZ011","collaboration":"Prepared in cooperation with the State of Arizona and with other agencies","usgsCitation":"McCormack, H., Fisk, G., Duet, N., Evans, D., and Castillo, N., 2002, Water resources data, Arizona, water year 2001: U.S. Geological Survey Water Data Report AZ-01-1, xxiii, 399 p., https://doi.org/10.3133/wdrAZ011.","productDescription":"xxiii, 399 p.","costCenters":[],"links":[{"id":174900,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wdr/2001/az-01-1/report-thumb.jpg"},{"id":413004,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wdr/2001/az-01-1/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United 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,{"id":69627,"text":"i2776 - 2002 - Geologic map of the southern Ivrea-Verbano zone, northwestern Italy","interactions":[],"lastModifiedDate":"2012-02-10T00:11:34","indexId":"i2776","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"2002","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":"2776","title":"Geologic map of the southern Ivrea-Verbano zone, northwestern Italy","language":"ENGLISH","doi":"10.3133/i2776","isbn":"060792120X","usgsCitation":"Quick, J.E., Sinigoi, S., Snoke, A., Kalakay, T., Mayer, A., and Peressini, G., 2002, Geologic map of the southern Ivrea-Verbano zone, northwestern Italy: U.S. Geological Survey IMAP 2776, 1 map : col. ; 111 x 78 cm., on sheet 145 x 102 cm., folded in envelope 30 x 24 cm. + 1 pamphlet (22 p. : ill., maps ; 28 cm.) , https://doi.org/10.3133/i2776.","productDescription":"1 map : col. ; 111 x 78 cm., on sheet 145 x 102 cm., folded in envelope 30 x 24 cm. + 1 pamphlet (22 p. : ill., maps ; 28 cm.) ","costCenters":[],"links":[{"id":191650,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/imap/2776/report-thumb.jpg"},{"id":91721,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/imap/2776/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":91722,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/imap/2776/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"25000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ 80.08333333333333,45.65 ], [ 80.08333333333333,45.9 ], [ 80.33333333333333,45.9 ], [ 80.33333333333333,45.65 ], [ 80.08333333333333,45.65 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae1e4b07f02db688896","contributors":{"authors":[{"text":"Quick, James E.","contributorId":21552,"corporation":false,"usgs":true,"family":"Quick","given":"James","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":280757,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Sinigoi, S.","contributorId":77245,"corporation":false,"usgs":true,"family":"Sinigoi","given":"S.","affiliations":[],"preferred":false,"id":280760,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Snoke, A.W.","contributorId":14899,"corporation":false,"usgs":true,"family":"Snoke","given":"A.W.","email":"","affiliations":[],"preferred":false,"id":280756,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Kalakay, T.J.","contributorId":46180,"corporation":false,"usgs":true,"family":"Kalakay","given":"T.J.","email":"","affiliations":[],"preferred":false,"id":280758,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Mayer, A.","contributorId":96780,"corporation":false,"usgs":true,"family":"Mayer","given":"A.","email":"","affiliations":[],"preferred":false,"id":280761,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Peressini, G.","contributorId":49876,"corporation":false,"usgs":true,"family":"Peressini","given":"G.","email":"","affiliations":[],"preferred":false,"id":280759,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}}
,{"id":51172,"text":"ofr02262 - 2002 - Fifty-year flood-inundation maps for Tocoa, Honduras","interactions":[],"lastModifiedDate":"2025-08-18T13:59:28.553702","indexId":"ofr02262","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"2002","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":"2002-262","title":"Fifty-year flood-inundation maps for Tocoa, Honduras","docAbstract":"After the devastating floods caused by Hurricane Mitch in 1998, maps of the areas and depths of the 50-year-flood inundation at 15 municipalities in Honduras were prepared as a tool for agencies involved in reconstruction and planning. This report, which is one in a series of 15, presents maps of areas in the municipality of Tocoa that would be inundated by a 50-year flood of Rio Tocoa. Geographic Information System (GIS) coverages of the flood inundation are available on a computer in the municipality of Tocoa as part of the Municipal GIS project and on the Internet at the Flood Hazard Mapping Web page (http://mitchnts1.cr.usgs.gov/projects/floodhazard.html). These coverages allow users to view the flood inundation in much more detail than is possible using the maps in this report.\r\n\r\nWater-surface elevations for an estimated 50-year-flood on Rio Tocoa at Tocoa were estimated using HEC-RAS, a one-dimensional, steady-flow, step-backwater computer program. The channel and floodplain cross sections used in HEC-RAS were developed from an airborne light-detection-and-ranging (LIDAR) topographic survey of the area and a ground survey at one bridge. There are no nearby long-term stream-gaging stations on Rio Tocoa; therefore, the 50-year-flood discharge for Rio Tocoa, 552 cubic meters per second, was estimated using a regression equation that relates the 50-year-flood discharge to drainage area and mean annual precipitation. The drainage area and mean annual precipitation estimated for Rio Tocoa at Tocoa are 204 square kilometers and 1,987 millimeters, respectively. It was assumed that a portion of the 50-year flood, 200 cubic meters per second, would escape the main channel and flow down a side channel before re-entering the main channel again near the lower end of the study area.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr02262","usgsCitation":"Kresch, D.L., Mastin, M.C., and Olsen, T.D., 2002, Fifty-year flood-inundation maps for Tocoa, Honduras: U.S. Geological Survey Open-File Report 2002-262, 13 p., https://doi.org/10.3133/ofr02262.","productDescription":"13 p.","costCenters":[],"links":[{"id":4576,"rank":2,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2002/ofr02262/index.html","linkFileType":{"id":5,"text":"html"}},{"id":179233,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"country":"Honduras","city":"Tocoa","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -89.43251127996213,\n              16.43006388749069\n            ],\n            [\n              -89.43251127996213,\n              12.876909617568344\n            ],\n            [\n              -82.7967072779427,\n              12.876909617568344\n            ],\n            [\n              -82.7967072779427,\n              16.43006388749069\n            ],\n            [\n              -89.43251127996213,\n              16.43006388749069\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49fbe4b07f02db5f47a3","contributors":{"authors":[{"text":"Kresch, David L.","contributorId":46084,"corporation":false,"usgs":true,"family":"Kresch","given":"David","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":243092,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Mastin, Mark C. 0000-0003-4018-7861 mcmastin@usgs.gov","orcid":"https://orcid.org/0000-0003-4018-7861","contributorId":1652,"corporation":false,"usgs":true,"family":"Mastin","given":"Mark","email":"mcmastin@usgs.gov","middleInitial":"C.","affiliations":[{"id":622,"text":"Washington Water Science Center","active":true,"usgs":true}],"preferred":true,"id":243090,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Olsen, T. D.","contributorId":41463,"corporation":false,"usgs":true,"family":"Olsen","given":"T.","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":243091,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":47459,"text":"wri024260 - 2002 - Water Quality of Camp Creek, Costello Creek, and Other Selected Streams on the South Side of Denali National Park and Preserve, Alaska","interactions":[],"lastModifiedDate":"2012-02-02T00:10:38","indexId":"wri024260","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"2002","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":"2002-4260","title":"Water Quality of Camp Creek, Costello Creek, and Other Selected Streams on the South Side of Denali National Park and Preserve, Alaska","docAbstract":"The Camp and Costello Creek watersheds are located on the south side of Denali National Park and Preserve. The Dunkle Mine, an abandoned coal mine, is located near the mouth of Camp Creek. Due to concern about runoff from the mine and its possible effects on the water quality and aquatic habitat of Camp Creek and its receiving stream, Costello Creek, these two streams were studied during the summer runoff months (June to September) in 1999 and 2000 as part of a cooperative study with the National Park Service. Since the south side of Denali National Park and Preserve is part of the U.S. Geological Survey?s National Water-Quality Assessment Cook Inlet Basin study unit, an additional part of this study included analysis of existing water-quality data at 23 sites located throughout the south side of Denali National Park and Preserve to compare with the water quality of Camp and Costello Creeks and to obtain a broader understanding of the water quality in this area of the Cook Inlet Basin.\r\n\r\nAnalysis of water column, bed sediment, fish, invertebrate, and algae data indicate no effects on the water quality of Camp Creek from the Dunkle Mine. Although several organic compounds were found in the streambed of Camp Creek, all concentrations were below recommended levels for aquatic life and most of the concentrations were below the minimum reporting level of 50 ?g/kg. Trace element concentrations of arsenic, chromium, and nickel in the bed sediments of Camp Creek exceeded threshold effect concentrations (TEC), but concentrations of these trace elements were also exceeded in streambed sediments of Costello Creek above Camp Creek. Since the percent organic carbon in Camp Creek is relatively high, the toxicity quotient of 0.55 is only slightly above the threshold value of 0.5. Costello Creek has a relatively low organic carbon content and has a higher toxicity quotient of 1.19.\r\n\r\nAnalysis of the water-quality data for other streams located in the south side of Denali National Park and Preserve indicate similarities to Camp Creek and Costello Creek. Most of the streams are calcium bicarbonate/calcium bicarbonate-sulfate type water with the exception of two streams that are calcium sulfate and magnesium sulfate type water. Trace element concentrations of arsenic, chromium, and nickel in the bed sediments of 9 streams exceeded the TEC or the probable effect concentration (PEC). Seven streams exceeded the threshold value of the toxicity quotient. Analysis of trace element concentrations in bed sediment and basin characteristics for 16 watersheds by cluster and discriminant analysis techniques indicated that the watersheds could be separated into two groups based on their basin characteristics.","language":"ENGLISH","doi":"10.3133/wri024260","usgsCitation":"Brabets, T.P., and Whitman, M.S., 2002, Water Quality of Camp Creek, Costello Creek, and Other Selected Streams on the South Side of Denali National Park and Preserve, Alaska: U.S. Geological Survey Water-Resources Investigations Report 2002-4260, 60 p., https://doi.org/10.3133/wri024260.","productDescription":"60 p.","costCenters":[],"links":[{"id":3985,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/wri024260/","linkFileType":{"id":5,"text":"html"}},{"id":173419,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b04e4b07f02db69925d","contributors":{"authors":[{"text":"Brabets, Timothy P. tbrabets@usgs.gov","contributorId":2087,"corporation":false,"usgs":true,"family":"Brabets","given":"Timothy","email":"tbrabets@usgs.gov","middleInitial":"P.","affiliations":[],"preferred":true,"id":235427,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Whitman, Matthew S.","contributorId":67961,"corporation":false,"usgs":false,"family":"Whitman","given":"Matthew","email":"","middleInitial":"S.","affiliations":[{"id":7217,"text":"Bureau of Land Management","active":true,"usgs":false}],"preferred":false,"id":235428,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":54465,"text":"wdrCT011 - 2002 - Water Resources Data, Connecticut, Water Year 2001","interactions":[],"lastModifiedDate":"2012-02-02T00:11:38","indexId":"wdrCT011","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"2002","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":340,"text":"Water Data Report","code":"WDR","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"CT-01-1","title":"Water Resources Data, Connecticut, Water Year 2001","language":"ENGLISH","doi":"10.3133/wdrCT011","usgsCitation":"Morrison, J., Provencher, P., Martin, J., and Norris, J., 2002, Water Resources Data, Connecticut, Water Year 2001: U.S. Geological Survey Water Data Report CT-01-1, 376 p., https://doi.org/10.3133/wdrCT011.","productDescription":"376 p.","costCenters":[],"links":[{"id":5556,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://ct.water.usgs.gov/annual.data/WY2001/bookadr2001.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":178283,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0be4b07f02db5fbcde","contributors":{"authors":[{"text":"Morrison, J.","contributorId":98804,"corporation":false,"usgs":true,"family":"Morrison","given":"J.","affiliations":[],"preferred":false,"id":250469,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Provencher, P.L.","contributorId":51778,"corporation":false,"usgs":true,"family":"Provencher","given":"P.L.","email":"","affiliations":[],"preferred":false,"id":250466,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Martin, J.W.","contributorId":71510,"corporation":false,"usgs":true,"family":"Martin","given":"J.W.","email":"","affiliations":[],"preferred":false,"id":250468,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Norris, J.R.","contributorId":67153,"corporation":false,"usgs":true,"family":"Norris","given":"J.R.","email":"","affiliations":[],"preferred":false,"id":250467,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":55071,"text":"wdrWA011 - 2002 - Water resources data, Washington, water year 2001","interactions":[],"lastModifiedDate":"2023-02-06T20:18:01.842421","indexId":"wdrWA011","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"2002","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":340,"text":"Water Data Report","code":"WDR","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"WA-01-1","title":"Water resources data, Washington, water year 2001","docAbstract":"<p>The Washington Water Science Center of the U.S. Geological Survey (USGS), in cooperation with State, local, and other Federal agencies, obtains a large amount of data pertaining to the water resources of Washington each water year. These data, accumulated during many water years, constitute a valuable data base for developing an improved understanding of the water resources of the State. To make these data readily available to interested parties outside the Geological Survey, the data are published annually in this report series entitled \"Water Resources Data— Washington.\"</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wdrWA011","collaboration":"Prepared in cooperation with the State of Washington and with other agencies","usgsCitation":"Kimbrough, R.A., Ruppert, G., Wiggins, W., Smith, R.R., Knowles, S., and Renslow, V., 2002, Water resources data, Washington, water year 2001: U.S. Geological Survey Water Data Report WA-01-1, xxxviii, 576 p., https://doi.org/10.3133/wdrWA011.","productDescription":"xxxviii, 576 p.","costCenters":[],"links":[{"id":412753,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wdr/2001/wa-01-1/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":175134,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wdr/2001/wa-01-1/report-thumb.jpg"}],"country":"United 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,{"id":44592,"text":"wri20024031 - 2002 - Field tests of diffusion samplers for inorganic constituents in wells and at a ground-water discharge zone","interactions":[],"lastModifiedDate":"2012-02-02T00:10:30","indexId":"wri20024031","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"2002","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":"2002-4031","title":"Field tests of diffusion samplers for inorganic constituents in wells and at a ground-water discharge zone","docAbstract":"Field tests were performed on two types of diffusion samplers to collect representative samples of inorganic constituents from ground water in wells and at an arsenic-contaminated ground-water-discharge zone beneath a stream. Nylon-screen samplers and dialysis samplers were tested for the collection of arsenic, calcium, chloride, iron, manganese, sulfate, and dissolved oxygen. The investigations were conducted at the Naval Industrial Reserve Ordnance Plant (NIROP), Fridley, Minnesota, and at the Naval Air Station Fort Worth Joint Reserve Base (NAS Fort Worth JRB), Texas.\r\n\r\n            \r\n\r\nData indicate that, in general, nylon-screen and dialysis diffusion samplers are capable of obtaining concentrations of inorganic solutes in ground water that correspond to concentrations obtained by low-flow sampling. Diffusion samplers offer a potentially time-saving approach to well sampling. Particular care must be taken, however, when sampling for iron and other metals, because of the potential for iron precipitation by oxygenation and when dealing with chemically stratified sampling intervals. Simple nylon-screen jar samplers buried beneath creekbed sediment appear to be effective tools for locating discharge zones of arsenic contaminated ground water.\r\n\r\n \r\n\r\nAlthough the LDPE samplers have proven to be inexpensive and simple to use in wells, they are limited by their inability to provide a representative sample of ionic solutes. The success of nylon-screen samplers in sediment studies suggests that these simple samplers may be useful for collecting water samples for inorganic constituents in wells. Results using dialysis bags deployed in wells suggest that these types of samplers have the potential to provide a representative sample of both VOCs and ionic solutes from ground water (Kaplan and others, 1991; Theodore A. Ehlke, U.S. Geological Survey, written commun., 2001).\r\n\r\n \r\n\r\nThe purpose of this report is to provide results of field tests investigating the potential to use diffusion samplers to collect representative samples of inorganic constituents from ground water in wells and at an arsenic-contaminated ground-water-discharge zone beneath a stream. The investigations were performed at NIROP, Fridley, Minn. (fig. 1) and at NAS Fort Worth JRB, Texas (fig. 2). Two types of samplers were tested. One type was a nylon-screen sampler, which consisted of a 30-mL jar filled with deionized water, with its opening covered by a nylon screen. The second type was a dialysis sampler that consisted of a tube of dialysis membrane filled with deionized water. The nylon-screen samplers were deployed in wells at NIROP Fridley and NAS Fort Worth JRB and beneath the ground-water/surface water interface of a stream at NAS Fort Worth JRB. The dialysis samplers were deployed only in wells at NAS Fort Worth JRB.","language":"ENGLISH","publisher":"U.S. Geological Survey","doi":"10.3133/wri20024031","usgsCitation":"Vroblesky, D.A., Petkewich, M.D., and Campbell, T.R., 2002, Field tests of diffusion samplers for inorganic constituents in wells and at a ground-water discharge zone: U.S. Geological Survey Water-Resources Investigations Report 2002-4031, 24 p., https://doi.org/10.3133/wri20024031.","productDescription":"24 p.","costCenters":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"links":[{"id":172928,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":13229,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/wri/wri024031/","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a06e4b07f02db5f8959","contributors":{"authors":[{"text":"Vroblesky, Don A. vroblesk@usgs.gov","contributorId":413,"corporation":false,"usgs":true,"family":"Vroblesky","given":"Don","email":"vroblesk@usgs.gov","middleInitial":"A.","affiliations":[],"preferred":true,"id":230053,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Petkewich, Matthew D. 0000-0002-5749-6356 mdpetkew@usgs.gov","orcid":"https://orcid.org/0000-0002-5749-6356","contributorId":982,"corporation":false,"usgs":true,"family":"Petkewich","given":"Matthew","email":"mdpetkew@usgs.gov","middleInitial":"D.","affiliations":[{"id":559,"text":"South Carolina Water Science Center","active":true,"usgs":true},{"id":13634,"text":"South Atlantic Water Science Center","active":true,"usgs":true}],"preferred":true,"id":230054,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Campbell, Ted R.","contributorId":41881,"corporation":false,"usgs":true,"family":"Campbell","given":"Ted","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":230055,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":50693,"text":"ofr02371 - 2002 - Geochemical Sediment Analysis Procedures","interactions":[],"lastModifiedDate":"2012-02-02T00:11:23","indexId":"ofr02371","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"2002","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":"2002-371","title":"Geochemical Sediment Analysis Procedures","language":"ENGLISH","doi":"10.3133/ofr02371","usgsCitation":"Jablonski, S., Mecray, E., Munson, J., and Blackwood, D., 2002, Geochemical Sediment Analysis Procedures: U.S. Geological Survey Open-File Report 2002-371, text, images, and files, https://doi.org/10.3133/ofr02371.","productDescription":"text, images, and files","costCenters":[],"links":[{"id":4167,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2002/of02-371/","linkFileType":{"id":5,"text":"html"}},{"id":178434,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b24e4b07f02db6ae9b4","contributors":{"authors":[{"text":"Jablonski, Sarah","contributorId":39047,"corporation":false,"usgs":true,"family":"Jablonski","given":"Sarah","email":"","affiliations":[],"preferred":false,"id":242090,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Mecray, E.L.","contributorId":14840,"corporation":false,"usgs":true,"family":"Mecray","given":"E.L.","email":"","affiliations":[],"preferred":false,"id":242089,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Munson, J.M.","contributorId":70474,"corporation":false,"usgs":true,"family":"Munson","given":"J.M.","email":"","affiliations":[],"preferred":false,"id":242091,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Blackwood, D.S.","contributorId":98747,"corporation":false,"usgs":true,"family":"Blackwood","given":"D.S.","email":"","affiliations":[],"preferred":false,"id":242092,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":45004,"text":"wri024014 - 2002 - Simulation of Fish, Mud, and Crystal Lakes and the shallow ground-water system, Dane County, Wisconsin","interactions":[],"lastModifiedDate":"2023-04-04T19:27:29.165878","indexId":"wri024014","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"2002","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":"2002-4014","title":"Simulation of Fish, Mud, and Crystal Lakes and the shallow ground-water system, Dane County, Wisconsin","docAbstract":"<p>A new MODFLOW lake package (LAK3) that simulates ground-water/lake interaction was used in simulation of Fish, Mud and Crystal Lakes?three shallow seepage lakes located in northwestern Dane County, Wis. The simulations were done to help determine the cause of increasing lake stages and provide a tool to estimate the effect of pumping water from Fish lake on future lake stages. The ground-water-flow model was developed using a telescopic-mesh refinement of the Dane and southwestern Columbia Counties regional model previously developed by the U.S. Geological Survey and the Wisconsin Geological and Natural History Survey. The parameter estimation model, UCODE, was coupled to the steadystate ground-water model to automate and optimize the calibration procedure. The steady-state model was calibrated to measured ground-water levels, Spring Creek streamflow measured at Lodi, and Fish and Crystal Lake stages. The results of the steady-state model were used as initial conditions in a transient simulation beginning in 1966 and ending in 1998. Recharge based on annual baseflow in Black Earth Creek, runoff based on measured coefficients, and precipitation and evaporation from the lake surfaces, were varied during the transient simulation. Measured Fish Lake stage was matched to simulated stage to calibrate the transient model.</p>\n<p>Model results suggest that the increase in regional ground-water recharge resulted in increased ground-water flow to the lake, which in turn resulted in increased lake stages. Simulation results of withdrawal of water from Fish Lake at 500 gallons per minute, assuming 1990?98 climatic conditions, indicate that after 1 year of pumping the stage of Fish and Mud Lakes would be reduced more than 1 foot and the stage of Crystal Lake would be reduced by less than 0.2 foot. When pumping is stopped, the lake stages would recover to near pre-pumping levels within about 3 years. When pumping is extended to 5 years, Fish and Mud Lake stage would be reduced by a maximum of 3.8 feet and Crystal Lake stage is reduced a maximum of 0.8 feet. After 4 years of recovery, Fish and Mud Lake stages are within 0.9 foot of prepumping levels and Crystal Lake stage is within 0.7 foot.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri024014","collaboration":"Prepared in cooperation with the Dane County Lakes and Watershed Commission, Wisconsin Department of Natural Resources","usgsCitation":"Krohelski, J.T., Lin, Y., Rose, W., and Hunt, R.J., 2002, Simulation of Fish, Mud, and Crystal Lakes and the shallow ground-water system, Dane County, Wisconsin: U.S. Geological Survey Water-Resources Investigations Report 2002-4014, iv, 17 p., https://doi.org/10.3133/wri024014.","productDescription":"iv, 17 p.","numberOfPages":"22","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":677,"text":"Wisconsin Water Science Center","active":true,"usgs":true}],"links":[{"id":168078,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/2002/4014/report-thumb.jpg"},{"id":82257,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/2002/4014/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":415183,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_51399.htm","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Wisconsin","county":"Dane County","otherGeospatial":"Crystal Lake, Fish Lake, Mud Lake","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -89.67950820922852,\n              43.27989227476815\n            ],\n            [\n              -89.67950820922852,\n              43.30138362431441\n            ],\n            [\n              -89.60294723510741,\n              43.30138362431441\n            ],\n            [\n              -89.60294723510741,\n              43.27989227476815\n            ],\n            [\n              -89.67950820922852,\n              43.27989227476815\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49afe4b07f02db5c8486","contributors":{"authors":[{"text":"Krohelski, James T.","contributorId":52223,"corporation":false,"usgs":true,"family":"Krohelski","given":"James","email":"","middleInitial":"T.","affiliations":[{"id":677,"text":"Wisconsin Water Science Center","active":true,"usgs":true}],"preferred":false,"id":230896,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Lin, Yu-Feng","contributorId":108167,"corporation":false,"usgs":true,"family":"Lin","given":"Yu-Feng","affiliations":[],"preferred":false,"id":230897,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Rose, William J. wjrose@usgs.gov","contributorId":2182,"corporation":false,"usgs":true,"family":"Rose","given":"William J.","email":"wjrose@usgs.gov","affiliations":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"preferred":false,"id":230895,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Hunt, Randall J. 0000-0001-6465-9304 rjhunt@usgs.gov","orcid":"https://orcid.org/0000-0001-6465-9304","contributorId":1129,"corporation":false,"usgs":true,"family":"Hunt","given":"Randall","email":"rjhunt@usgs.gov","middleInitial":"J.","affiliations":[{"id":677,"text":"Wisconsin Water Science Center","active":true,"usgs":true}],"preferred":true,"id":230894,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":54990,"text":"wdrTN011 - 2002 - Water resources data, Tennessee, water year 2001","interactions":[],"lastModifiedDate":"2020-11-05T21:50:06.198977","indexId":"wdrTN011","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"2002","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":340,"text":"Water Data Report","code":"WDR","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"TN-01-1","title":"Water resources data, Tennessee, water year 2001","docAbstract":"<p>No abstract available.&nbsp;</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wdrTN011","usgsCitation":"Flohr, D., Garrett, J., Hamilton, J., and Phillips, T., 2002, Water resources data, Tennessee, water year 2001: U.S. Geological Survey Water Data Report TN-01-1, xxii, 369 p., https://doi.org/10.3133/wdrTN011.","productDescription":"xxii, 369 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 \"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a09e4b07f02db5fa9e1","contributors":{"authors":[{"text":"Flohr, D.F.","contributorId":52259,"corporation":false,"usgs":true,"family":"Flohr","given":"D.F.","email":"","affiliations":[],"preferred":false,"id":252240,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Garrett, J.W.","contributorId":87958,"corporation":false,"usgs":true,"family":"Garrett","given":"J.W.","email":"","affiliations":[],"preferred":false,"id":252241,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Hamilton, J.T.","contributorId":99215,"corporation":false,"usgs":true,"family":"Hamilton","given":"J.T.","email":"","affiliations":[],"preferred":false,"id":252242,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Phillips, T.D.","contributorId":43845,"corporation":false,"usgs":true,"family":"Phillips","given":"T.D.","email":"","affiliations":[],"preferred":false,"id":252239,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":44964,"text":"wri024027 - 2002 - Ground-cover vegetation in wetland forests of the lower Suwannee River floodplain, Florida, and potential impacts of flow reductions","interactions":[],"lastModifiedDate":"2012-02-02T00:10:12","indexId":"wri024027","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"2002","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":"2002-4027","title":"Ground-cover vegetation in wetland forests of the lower Suwannee River floodplain, Florida, and potential impacts of flow reductions","docAbstract":"Ground-cover vegetation was surveyed in wetland forests in the lower Suwannee River floodplain, Florida, in a study conducted by the U.S. Geological Survey in cooperation with the Suwannee River Water Management District from 1996 to 1999. Increased water use in the basin, supplied primarily from ground water, could reduce ground-water discharge to the river and flows in the lower Suwannee River. Many of the 282 ground-cover species found in wetland forests of the floodplain have distributions that are related to flow-dependent hydrologic characteristics of forest types, and their distributions would change if flows were reduced. Overall species diversity in the floodplain might decrease, and the composition of ground-cover vegetation in all forest types might change with flow reductions. \r\n\r\nThe study area included forests within the 10-year floodplain of the lower Suwannee River from its confluence with the Santa Fe River to the lower limit of forests near the Gulf of Mexico. The floodplain is divided into three reaches (riverine, upper tidal, and lower tidal) due to variations in hydrology, vegetation, and soils with proximity to the coast. The riverine (non-tidal) reach had the greatest number of total species (203) and species unique to that reach (81). Mitchella repens, Toxicodendron radicans, and Axonopus furcatus were the most frequently dominant species in riverine bottomland hardwoods. Free-floating aquatic species, such as Spirodela punctata and Lemna valdiviana, were the dominant species in the wettest riverine swamps. The upper tidal reach had the lowest number of total species (116), only two species unique to that reach, and the lowest density of ground cover (26 percent). Panicum commutatum and Crinum americanum were frequent dominant species in upper tidal forests. The lower tidal reach had the highest ground-cover density (43 percent) and the second highest number of total species (183) and number of species unique to that reach (55). Saururus cernuus and species of Carex were frequently dominant in lower tidal swamps. Lower tidal hammocks, the most elevated lower tidal forests, were dominated by Osmunda cinnamomea and Chasmanthium laxum. \r\n\r\nFlow reductions in the lower Suwannee River could change the flow-dependent hydrologic characteristics of wetland forests. Decreases in inundation and saturation in riverine forests could result in a decrease in the number and extent of semi-permanently inundated ponds. As a result, several species of free-floating, aquatic plants that grow only in riverine floodplain ponds might decrease in abundance or disappear if flows were reduced. Decreases in inundation and saturation could also result in a shift to more upland species in all riverine forests and upper tidal bottomland hardwoods. Upland species and some exotic species might increase in abundance in the floodplain, invading forests where hydrologic conditions have been altered by flow reductions. Depth and duration of inundation due to river flooding could decrease in all riverine and upper tidal forests, probably resulting in a shift of species to those that are typically found in forests with shallower, shorter-duration floods. Salinity in the lower tidal reach and adjacent areas of the upper tidal reach might increase with flow reductions, and the distribution of species might change due to varying tolerances of salinity among species. Species with low salt-tolerance unique to the lower tidal reach might disappear from the floodplain, and species with high salinity tolerance could increase in abundance, replacing less salt-tolerant species.","language":"ENGLISH","doi":"10.3133/wri024027","usgsCitation":"Darst, M.R., Light, H.M., and Lewis, L.J., 2002, Ground-cover vegetation in wetland forests of the lower Suwannee River floodplain, Florida, and potential impacts of flow reductions: U.S. Geological Survey Water-Resources Investigations Report 2002-4027, xii, 46 p. : col. ill., col. maps ; 28 cm., https://doi.org/10.3133/wri024027.","productDescription":"xii, 46 p. : col. ill., col. maps ; 28 cm.","costCenters":[],"links":[{"id":3838,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/wri024027","linkFileType":{"id":5,"text":"html"}},{"id":161518,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b23e4b07f02db6ae390","contributors":{"authors":[{"text":"Darst, Melanie R.","contributorId":93042,"corporation":false,"usgs":true,"family":"Darst","given":"Melanie","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":230784,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Light, Helen M.","contributorId":18355,"corporation":false,"usgs":true,"family":"Light","given":"Helen","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":230782,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Lewis, Lori J.","contributorId":73655,"corporation":false,"usgs":true,"family":"Lewis","given":"Lori","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":230783,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":44998,"text":"wri014266S - 2002 - Huracan Mitch, caudal de creciente en tramos de rios seleccionados en Honduras","interactions":[],"lastModifiedDate":"2026-02-03T14:23:10.459179","indexId":"wri014266S","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"2002","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":"2001-4266S","title":"Huracan Mitch, caudal de creciente en tramos de rios seleccionados en Honduras","docAbstract":"<p>No abstract available.</p>","language":"Spanish","publisher":"U.S. Geological Survey","doi":"10.3133/wri014266S","usgsCitation":"Smith, M.E., Phillips, J.V., and Spahr, N.E., 2002, Huracan Mitch, caudal de creciente en tramos de rios seleccionados en Honduras: U.S. Geological Survey Water-Resources Investigations Report 2001-4266S, 8 p., https://doi.org/10.3133/wri014266S.","productDescription":"8 p.","costCenters":[],"links":[{"id":252079,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/2001/4266s/report-thumb.jpg"},{"id":247726,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/2001/4266s/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a52e4b07f02db62a509","contributors":{"authors":[{"text":"Smith, Mark E.","contributorId":75584,"corporation":false,"usgs":true,"family":"Smith","given":"Mark","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":230882,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Phillips, Jeffrey V.","contributorId":86327,"corporation":false,"usgs":true,"family":"Phillips","given":"Jeffrey","email":"","middleInitial":"V.","affiliations":[],"preferred":false,"id":230883,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Spahr, Norman E. nspahr@usgs.gov","contributorId":1977,"corporation":false,"usgs":true,"family":"Spahr","given":"Norman","email":"nspahr@usgs.gov","middleInitial":"E.","affiliations":[],"preferred":true,"id":230881,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":45008,"text":"wri014100 - 2002 - Hydrogeology and simulation of ground-water flow in the aquifers underlying Belvidere, Illinois","interactions":[],"lastModifiedDate":"2012-02-02T00:10:55","indexId":"wri014100","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"2002","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":"2001-4100","title":"Hydrogeology and simulation of ground-water flow in the aquifers underlying Belvidere, Illinois","docAbstract":"The U.S. Geological Survey investigated the\r\nground-water-flow system and distribution of\r\ncontaminants in the vicinity of Belvidere, Illinois,\r\nduring 1992?2000. The study included the\r\ncompilation, collection, and analyses of\r\nhydrogeologic and water-quality data and\r\nsimulation of the ground-water-flow system.\r\nHydrogeologic data include lithologic,\r\nstratigraphic, geophysical, hydraulic-property,\r\nwater-level, ground-water withdrawal, and\r\nstreamflow data. Water-quality data include\r\nanalyses of water samples primarily for volatile\r\norganic compounds (VOC?s) and selectively for\r\ntritium and inorganic constituents. Data were\r\ncollected from about 250 wells and 21 surfacewater\r\nsites. These data were used (1) to describe\r\nthe hydrogeologic framework of the ground-waterflow\r\nsystem, preferential pathways and directions\r\nof ground-water movement and contaminant\r\ndistribution, ground-water/surface-water relations,\r\nand the water budget and (2) to develop and\r\ncalibrate the ground-water-flow model.\r\nThe glacial drift (sand and gravel with some\r\nclay) and Galena-Platteville (fractured dolomite)\r\naquifers and the sandstone aquifers of the\r\nCambrian-Ordovician aquifer system compose the\r\nground-water-flow system underlying Belvidere\r\nand vicinity. The Glenwood confining unit\r\nseparates the Galena-Platteville aquifer from the\r\nunderlying sandstone aquifers. The Galena-\r\nPlatteville aquifer and confining unit may be\r\nabsent in parts of the Troy Bedrock Valley, about\r\n1.5 miles west of Belvidere.\r\nThroughout the study area, the Kishwaukee\r\nRiver and its tributaries seem to be gaining flow\r\nfrom shallow ground-water discharge.\r\nPotentiometric levels in the glacial drift and\r\nGalena-Platteville aquifers range from about 900\r\nfeet above sea level in the upland areas to 740 feet\r\nalong the Kishwaukee River.\r\nEstimated horizontal hydraulic conductivity\r\nof the glacial drift aquifer ranges from about 0.13\r\nto 280 feet per day. The Galena-Platteville aquifer\r\nis a dual-porosity unit with the greatest percentage\r\nof flow through fractures and bedding-plane\r\npartings. Estimated horizontal hydraulic\r\nconductivity ranges from about 0.005 to 2,500\r\nfeet per day. Estimated horizontal hydraulic\r\nconductivity of the St. Peter aquifer (the uppermost\r\nsandstone aquifer of the Cambrian-Ordovician\r\naquifer system ranges from about 4.7 to 17.5 feet\r\nper day.\r\nVolatile organic compounds have been\r\ndetected in all aquifers underlying Belvidere.\r\nTrichloroethene and tetrachloroethene are the\r\nprincipal VOC?s detected at concentrations above\r\nregulatory levels, with the largest number of\r\ndetections and highest concentrations in the glacial\r\ndrift aquifer. VOC?s generally are not detected in\r\nthe glacial drift aquifer farther than 1,000 feet from\r\nknown or potential source areas (industrial or\r\ndisposal sites), because most source areas are near\r\nthe Kishwaukee River, where shallow ground\r\nwater discharges. Across most of the study area,\r\nthe Glenwood confining unit seems to restrict\r\ndownward movement of VOC?s into the\r\nunderlying St. Peter aquifer; in the immediate\r\nvicinity of Belvidere, downward movement also\r\nseems restricted by lateral movement toward the\r\nmunicipal wells through permeable intervals in the\r\n2 Hydrogeology and Simulation of Ground-Water Flow in the Aquifers Underlying Belvidere, Illinois\r\nGalena-Platteville aquifer. Fractures and (or)\r\nunused wells that may penetrate the confining unit\r\nseem to provide local pathways for limited\r\nmovement of VOC?s to the sandstone aquifers. At\r\nleast two municipal wells seem to intercept the\r\nbedding-plane partings at about 525 and 485 feet\r\nabove sea level. Water levels in the lower one-third\r\nof the Galena-Platteville aquifer rapidly respond to\r\nwithdrawals at these wells.\r\nThe ground-water-flow system underlying\r\nBelvidere was simulated to test the conceptual\r\nmodel of the system. The three-dimensional,\r\nsteady-state model represents the glacial drift,\r\nGalena-Platteville, and sandstone aquifers\r\nsep","language":"ENGLISH","doi":"10.3133/wri014100","usgsCitation":"Mills, P., Nazimek, J., Halford, K.J., and Yeskis, D., 2002, Hydrogeology and simulation of ground-water flow in the aquifers underlying Belvidere, Illinois: U.S. Geological Survey Water-Resources Investigations Report 2001-4100, vi, 103 p. (1 folded) : ill., maps ; 28 cm. , https://doi.org/10.3133/wri014100.","productDescription":"vi, 103 p. (1 folded) : ill., maps ; 28 cm. ","costCenters":[],"links":[{"id":120217,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/wri_2001_4100.jpg"},{"id":3876,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://il.water.usgs.gov/pubs/wrir01_4100.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a4ae4b07f02db625238","contributors":{"authors":[{"text":"Mills, P.C. pcmills@usgs.gov","contributorId":3810,"corporation":false,"usgs":true,"family":"Mills","given":"P.C.","email":"pcmills@usgs.gov","affiliations":[{"id":344,"text":"Illinois Water Science Center","active":true,"usgs":true}],"preferred":true,"id":230903,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Nazimek, J.E.","contributorId":43414,"corporation":false,"usgs":true,"family":"Nazimek","given":"J.E.","affiliations":[],"preferred":false,"id":230904,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Halford, K. J. 0000-0002-7322-1846","orcid":"https://orcid.org/0000-0002-7322-1846","contributorId":61077,"corporation":false,"usgs":true,"family":"Halford","given":"K.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":230905,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Yeskis, D.J.","contributorId":105334,"corporation":false,"usgs":true,"family":"Yeskis","given":"D.J.","affiliations":[],"preferred":false,"id":230906,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":44659,"text":"fs06102 - 2002 - Homeland security and the National map","interactions":[{"subject":{"id":44659,"text":"fs06102 - 2002 - Homeland security and the National map","indexId":"fs06102","publicationYear":"2002","noYear":false,"title":"Homeland security and the National map"},"predicate":"SUPERSEDED_BY","object":{"id":47836,"text":"fs02703 - 2003 - Hazards, Disasters, and <i>The National Map</i>","indexId":"fs02703","publicationYear":"2003","noYear":false,"title":"Hazards, Disasters, and <i>The National Map</i>"},"id":1}],"supersededBy":{"id":47836,"text":"fs02703 - 2003 - Hazards, Disasters, and <i>The National Map</i>","indexId":"fs02703","publicationYear":"2003","noYear":false,"title":"Hazards, Disasters, and <i>The National Map</i>"},"lastModifiedDate":"2012-03-16T17:16:06","indexId":"fs06102","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"2002","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":"061-02","title":"Homeland security and the National map","language":"ENGLISH","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/fs06102","usgsCitation":"Water Resources Division, U.S. Geological Survey, 2002, Homeland security and the National map: U.S. Geological Survey Fact Sheet 061-02, 2 p., https://doi.org/10.3133/fs06102.","productDescription":"2 p.","costCenters":[],"links":[{"id":168353,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a54e4b07f02db62bebc","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":531550,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":44578,"text":"wri024291 - 2002 - Effects of hardened low-water crossings on stream habitat, water quality, and periphyton in four streams at the Fort Polk Military Reservation, Vernon Parish, Louisiana, October 1998 through November 1999","interactions":[],"lastModifiedDate":"2012-02-02T00:11:01","indexId":"wri024291","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"2002","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":"2002-4291","title":"Effects of hardened low-water crossings on stream habitat, water quality, and periphyton in four streams at the Fort Polk Military Reservation, Vernon Parish, Louisiana, October 1998 through November 1999","language":"ENGLISH","doi":"10.3133/wri024291","usgsCitation":"Tollett, R.W., Bryan, B.W., and Bryan, C.F., 2002, Effects of hardened low-water crossings on stream habitat, water quality, and periphyton in four streams at the Fort Polk Military Reservation, Vernon Parish, Louisiana, October 1998 through November 1999: U.S. Geological Survey Water-Resources Investigations Report 2002-4291, vi, 70 p. : ill. (some col.), maps ; 28 cm., https://doi.org/10.3133/wri024291.","productDescription":"vi, 70 p. : ill. (some col.), maps ; 28 cm.","costCenters":[],"links":[{"id":122803,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/2002/4291/report-thumb.jpg"},{"id":81930,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/2002/4291/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a2ae4b07f02db6128da","contributors":{"authors":[{"text":"Tollett, Roland W. 0000-0002-4726-5845 rtollett@usgs.gov","orcid":"https://orcid.org/0000-0002-4726-5845","contributorId":1896,"corporation":false,"usgs":true,"family":"Tollett","given":"Roland","email":"rtollett@usgs.gov","middleInitial":"W.","affiliations":[{"id":24708,"text":"Lower Mississippi-Gulf Water Science Center","active":true,"usgs":true}],"preferred":true,"id":230030,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bryan, Barbara W.","contributorId":102938,"corporation":false,"usgs":true,"family":"Bryan","given":"Barbara","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":230031,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Bryan, C. Fredrick","contributorId":104553,"corporation":false,"usgs":true,"family":"Bryan","given":"C.","email":"","middleInitial":"Fredrick","affiliations":[],"preferred":false,"id":230032,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":44620,"text":"wri024069 - 2002 - Relation of Environmental characteristics to the composition of aquatic assemblages along a gradient of urban land use in New Jersey, 1996-98","interactions":[],"lastModifiedDate":"2012-02-02T00:11:00","indexId":"wri024069","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"2002","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":"2002-4069","title":"Relation of Environmental characteristics to the composition of aquatic assemblages along a gradient of urban land use in New Jersey, 1996-98","docAbstract":"Community data from 36 watersheds were used to evaluate the response of fish, invertebrate, and algal assemblages in New Jersey streams to environmental characteristics along a gradient of urban land use that ranged from 3 to 96 percent. Aquatic assemblages were sampled at 36 sites during 1996-98, and more than 400 environmental attributes at multiple spatial scales were summarized. Data matrices were reduced to 43, 170, and 103 species of fish, invertebrates, and algae, respectively, by means of a predetermined joint frequency and relative abundance approach. White sucker (Catostomus commersoni) and Tessellated darter (Etheostoma olmstedi) were the most abundant fishes, accounting for more than 20 and 17 percent, respectively, of the mean abundance. Net-spinning caddisflies (Hydropsychidae) were the most commonly occurring benthic invertebrates and were found at all but one of the 36 sampling sites. Blue-green (for example, Calothrix sp. and Oscillatoria sp.) and green (for example, Protoderma viride) algae were the most widely distrib-uted algae; however, more than 81 percent of the algal taxa collected were diatoms. Principal-component and correlation analyses were used to reduce the dimensionality of the environmental data. Multiple linear regression analysis of extracted ordination axes then was used to develop models that expressed effects of increasing urban land use on the structure of aquatic assemblages. Significant environmental variables identified by using multiple linear regression analysis then were included in a direct gradient analysis. Partial canonical correspondence analysis of relativized abundance data was used to restrict further the effects of residual natural variability, and to identify relations among the environmental variables and the structure of fish, invertebrate, and algal assemblages along an urban land-use gradient. Results of this approach, combined with the results of the multiple linear regression analyses, were used to identify human population density (311-37,594 persons/km2), amount and type of impervious surface cover (0.12-1,350 km2), nutrient concentrations (for example, 0.01-0.29 mg/L of phosphorus), hydrologic instability (for example, 100-8,955 ft3/s for 2-year peak flow), the amount of forest and wetlands in a basin (0.01-6.25 km2), and substrate quality (0-87 percent cobble substrate) as variables that are highly correlated with aquatic-assemblage structure. Species distributions in ordination space clearly indicate that tolerant species are more abundant in the streams impaired by urbanization and sensitive taxa are more closely associated with the least impaired basins. The distinct differences in aquatic assemblages along the urban land-use gradient demonstrate the deleterious effects of urbanization on assemblage structure and indicate that conserving landscape attributes that mitigate anthropogenic influences (for example, stormwater-management practices emphasizing infiltration and preservation of existing forests, wetlands, and riparian corridors) will help to maintain the relative abundance of sensitive taxa. Complementary multiple linear regression models indicate that aquatic community indices were correlated with many of the anthropogenic factors that were found to be significant along the urban land-use gradient. These indices appear to be effective in differentiating the moderately and severely impaired streams from the minimally impaired streams. Evaluation of disturbance thresholds for aquatic assemblages indicates that moderate to severe impairment is detectable in New Jersey streams when impervious surface cover in the drainage basin reaches approximately 18 percent.","language":"ENGLISH","doi":"10.3133/wri024069","usgsCitation":"Kennen, J., and Ayers, M.A., 2002, Relation of Environmental characteristics to the composition of aquatic assemblages along a gradient of urban land use in New Jersey, 1996-98: U.S. Geological Survey Water-Resources Investigations Report 2002-4069, ix, 77 p. : ill. (some col.), maps (some col.) ; 28 cm., https://doi.org/10.3133/wri024069.","productDescription":"ix, 77 p. : ill. (some col.), maps (some col.) ; 28 cm.","costCenters":[],"links":[{"id":3721,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/wri024069","linkFileType":{"id":5,"text":"html"}},{"id":168644,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac9e4b07f02db67c34d","contributors":{"authors":[{"text":"Kennen, Jonathan G. 0000-0002-5426-4445 jgkennen@usgs.gov","orcid":"https://orcid.org/0000-0002-5426-4445","contributorId":574,"corporation":false,"usgs":true,"family":"Kennen","given":"Jonathan G.","email":"jgkennen@usgs.gov","affiliations":[{"id":470,"text":"New Jersey Water Science Center","active":true,"usgs":true}],"preferred":true,"id":230126,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Ayers, Mark A.","contributorId":84730,"corporation":false,"usgs":true,"family":"Ayers","given":"Mark","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":230127,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":44610,"text":"wri024274 - 2002 - Preliminary assessment of using tree-tissue analysis and passive-diffusion samplers to evaluate trichloroethene contamination of ground water at Site SS-34N, McChord Air Force Base, Washington, 2001","interactions":[],"lastModifiedDate":"2012-02-02T00:11:05","indexId":"wri024274","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"2002","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":"2002-4274","title":"Preliminary assessment of using tree-tissue analysis and passive-diffusion samplers to evaluate trichloroethene contamination of ground water at Site SS-34N, McChord Air Force Base, Washington, 2001","docAbstract":"Two low-cost innovative sampling procedures for characterizing trichloroethene (TCE) contamination in ground water were evaluated for use at McChord Air Force Base (AFB) by the U.S. Geological Survey, in cooperation with the U.S. Air Force McChord Air Force Base Installation Restoration Program, in 2001. Previous attempts to characterize the source of ground-water contamination in the heterogeneous glacial outwash aquifer at McChord site SS-34N using soil-gas surveys, direct-push exploration, and more than a dozen ground-water monitoring wells have had limited success. The procedures assessed in this study involved analysis of tree-tissue samples to map underlying ground-water contamination and deploying passive-diffusion samplers to measure TCE concentrations in existing monitoring wells. These procedures have been used successfully at other U.S. Department of Defense sites and have resulted in cost avoidance and accelerated site characterization. Despite the presence of TCE in ground water at site SS-34N, TCE was not detected in any of the 20 trees sampled at the site during either early spring or late summer sampling. The reason the tree tissue procedure was not successful at the McChord AFB site SS-34N may have been due to an inability of tree roots to extract moisture from a water table 30 feet below the land surface, or that concentrations of TCE in ground water were not large enough to be detectable in the tree tissue at the sampling point. Passive-diffusion samplers were placed near the top, middle, and bottom of screened intervals in three monitoring wells and TCE was observed in all samplers. Concentrations of TCE from the passive-diffusion samplers were generally similar to concentrations found in samples collected in the same wells using conventional pumping methods. In contrast to conventional pumping methods, the collection of ground-water samples using the passive-diffusion samples did not generate waste purge water that would require hazardous-waste disposal. In addition, the results from the passive-diffusion samples may show that TCE concentrations are stratified across some screened intervals. The overall results of the limited test of passive-diffusion samplers at site SS-34N were similar to more detailed tests conducted at other contaminated sites across the country and indicate that further evaluation of the use of passive-diffusion samplers at McChord site SS-34N is warranted.","language":"ENGLISH","doi":"10.3133/wri024274","usgsCitation":"Cox, S., 2002, Preliminary assessment of using tree-tissue analysis and passive-diffusion samplers to evaluate trichloroethene contamination of ground water at Site SS-34N, McChord Air Force Base, Washington, 2001: U.S. Geological Survey Water-Resources Investigations Report 2002-4274, 21 p., https://doi.org/10.3133/wri024274.","productDescription":"21 p.","costCenters":[],"links":[{"id":167972,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":3712,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/wri024274/","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac9e4b07f02db67c9c5","contributors":{"authors":[{"text":"Cox, S.E.","contributorId":66663,"corporation":false,"usgs":true,"family":"Cox","given":"S.E.","email":"","affiliations":[],"preferred":false,"id":230099,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":53283,"text":"wdrNE021 - 2002 - Water Resources Data--Nebraska, Water Year 2002","interactions":[],"lastModifiedDate":"2012-02-02T00:11:41","indexId":"wdrNE021","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"2002","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":340,"text":"Water Data Report","code":"WDR","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"NE-02-1","title":"Water Resources Data--Nebraska, Water Year 2002","docAbstract":"The Water Resources Discipline of the U.S. Geological Survey (USGS), in cooperation with State and local agencies, obtains a large amount of data pertaining to the water resources of Nebraska each water year. These data, accumulated during many water years, constitute a valuable data base for developing an improved understanding of the water resources of the State. To make these data readily available to interested parties outside the USGS, the data are published annually in this report series entitled ?Water Resources Data - Nebraska.'\r\n\r\nThe Nebraska water resources data report for water year 2002 includes records of stage, discharge, and water quality of streams; stage and/or contents of lakes and reservoirs; and water levels and quality of ground water in wells. This report contains records of stream stage for 3 stations; stream discharge for 96 continuous and 5 crest-state gaging stations, and 3 miscellaneous and 55 low-flow sites; stream water quality for 23 gaging stations and 5 miscellaneous sites; water elevation and/or contents for 1 lake and 1 reservoir; ground-water levels for 43 observation wells; and ground-water quality for 115 wells. These data represent that part of the National Water Data System collected in and near Nebraska by the U.S. Geological Survey and cooperating local, state and Federal agencies.","language":"ENGLISH","doi":"10.3133/wdrNE021","usgsCitation":"Hitch, D., Hull, S., and Walczyk, V., 2002, Water Resources Data--Nebraska, Water Year 2002: U.S. Geological Survey Water Data Report NE-02-1, 436 p., https://doi.org/10.3133/wdrNE021.","productDescription":"436 p.","costCenters":[],"links":[{"id":4986,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/wdrne02/","linkFileType":{"id":5,"text":"html"}},{"id":177299,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a08e4b07f02db5fa423","contributors":{"authors":[{"text":"Hitch, D.E.","contributorId":72425,"corporation":false,"usgs":true,"family":"Hitch","given":"D.E.","email":"","affiliations":[],"preferred":false,"id":247175,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hull, S.H.","contributorId":44576,"corporation":false,"usgs":true,"family":"Hull","given":"S.H.","email":"","affiliations":[],"preferred":false,"id":247174,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Walczyk, V.C.","contributorId":40270,"corporation":false,"usgs":true,"family":"Walczyk","given":"V.C.","email":"","affiliations":[],"preferred":false,"id":247173,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":32684,"text":"fs07802 - 2002 - Availability of Ground-Water Data for California, Water Year 2001","interactions":[],"lastModifiedDate":"2012-02-02T00:09:15","indexId":"fs07802","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"2002","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":"078-02","title":"Availability of Ground-Water Data for California, Water Year 2001","language":"ENGLISH","doi":"10.3133/fs07802","usgsCitation":"Huff, J., 2002, Availability of Ground-Water Data for California, Water Year 2001: U.S. Geological Survey Fact Sheet 078-02, NA, https://doi.org/10.3133/fs07802.","productDescription":"NA","costCenters":[],"links":[{"id":119422,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/fs_078_02.jpg"},{"id":3260,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/FS/fs07802/","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aa9e4b07f02db667fa7","contributors":{"authors":[{"text":"Huff, Julia A.","contributorId":23130,"corporation":false,"usgs":true,"family":"Huff","given":"Julia A.","affiliations":[],"preferred":false,"id":208923,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":42338,"text":"ofr02167 - 2002 - Altitude and configuration of the potentiometric surface in Highland and West Fallowfield Townships, Chester County, Pennsylvania, March through July, 2001","interactions":[],"lastModifiedDate":"2016-10-21T10:27:32","indexId":"ofr02167","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"2002","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":"2002-167","title":"Altitude and configuration of the potentiometric surface in Highland and West Fallowfield Townships, Chester County, Pennsylvania, March through July, 2001","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr02167","usgsCitation":"Mohammad, A., 2002, Altitude and configuration of the potentiometric surface in Highland and West Fallowfield Townships, Chester County, Pennsylvania, March through July, 2001: U.S. Geological Survey Open-File Report 2002-167, 17.74 x 19.69 inches, https://doi.org/10.3133/ofr02167.","productDescription":"17.74 x 19.69 inches","costCenters":[{"id":532,"text":"Pennsylvania Water Science Center","active":true,"usgs":true}],"links":[{"id":135398,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ofr02167.PNG"},{"id":330291,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/2002/0167/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Pennsylvania","county":"Chester County","otherGeospatial":"Highland Township, West Fallowfield Township","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"Polygon\",\"coordinates\":[[[-75.6968,40.2417],[-75.6912,40.2388],[-75.6894,40.2378],[-75.6864,40.2387],[-75.6784,40.2436],[-75.6741,40.2458],[-75.6705,40.2466],[-75.6645,40.2461],[-75.6549,40.2428],[-75.6478,40.2404],[-75.6406,40.2371],[-75.6304,40.2347],[-75.6209,40.2305],[-75.6186,40.2277],[-75.6151,40.2245],[-75.6114,40.2244],[-75.6078,40.2258],[-75.6047,40.2275],[-75.6059,40.2294],[-75.6076,40.2326],[-75.6088,40.2348],[-75.6081,40.2366],[-75.605,40.2389],[-75.6014,40.2379],[-75.5997,40.2365],[-75.5973,40.2347],[-75.591,40.2214],[-75.5835,40.21],[-75.5801,40.2045],[-75.5796,40.2004],[-75.5766,40.1981],[-75.5724,40.1967],[-75.5694,40.1966],[-75.5676,40.1975],[-75.5645,40.2006],[-75.5644,40.2029],[-75.5655,40.207],[-75.5661,40.2093],[-75.5636,40.2101],[-75.5606,40.2096],[-75.5589,40.2073],[-75.5554,40.2023],[-75.5503,40.19],[-75.544,40.1794],[-75.5387,40.1739],[-75.527,40.1664],[-75.5275,40.1492],[-75.5239,40.1468],[-75.5184,40.1475],[-75.5127,40.1595],[-75.503,40.1593],[-75.5,40.1563],[-75.5036,40.1506],[-75.5107,40.1422],[-75.5088,40.1347],[-75.4905,40.1253],[-75.4729,40.1287],[-75.4611,40.1241],[-75.4627,40.119],[-75.4691,40.1169],[-75.4719,40.1116],[-75.4693,40.1066],[-75.4618,40.1027],[-75.4633,40.0971],[-75.4563,40.0945],[-75.4558,40.0876],[-75.4401,40.0941],[-75.4369,40.0899],[-75.42,40.0966],[-75.3927,40.0604],[-75.3669,40.0723],[-75.361,40.0668],[-75.3702,40.062],[-75.3732,40.0602],[-75.3811,40.0572],[-75.4012,40.0475],[-75.4025,40.0471],[-75.4086,40.0436],[-75.4128,40.0418],[-75.4106,40.0373],[-75.4076,40.0336],[-75.406,40.0295],[-75.4139,40.0242],[-75.4207,40.0202],[-75.4311,40.0118],[-75.4508,39.9958],[-75.452,39.9949],[-75.4532,39.994],[-75.4521,39.9926],[-75.4455,39.9925],[-75.4437,39.9925],[-75.4412,39.9933],[-75.4401,39.9915],[-75.4372,39.9865],[-75.4385,39.9842],[-75.4398,39.9811],[-75.4399,39.9793],[-75.4423,39.9788],[-75.4446,39.9807],[-75.4726,39.968],[-75.4993,39.9557],[-75.5024,39.9544],[-75.5079,39.9518],[-75.5152,39.9483],[-75.5224,39.9452],[-75.5243,39.9443],[-75.5202,39.9397],[-75.5191,39.9374],[-75.5306,39.9322],[-75.526,39.9239],[-75.5315,39.9218],[-75.5366,39.9305],[-75.5427,39.9274],[-75.5398,39.9242],[-75.5447,39.922],[-75.5424,39.9183],[-75.5502,39.9152],[-75.5468,39.9093],[-75.5553,39.9058],[-75.5576,39.9086],[-75.5601,39.9072],[-75.5583,39.904],[-75.562,39.9023],[-75.5711,39.897],[-75.573,39.8943],[-75.5714,39.8879],[-75.5799,39.8835],[-75.5822,39.8854],[-75.5834,39.8849],[-75.5852,39.8863],[-75.5888,39.8846],[-75.5842,39.8804],[-75.5981,39.8747],[-75.5952,39.8724],[-75.5934,39.8697],[-75.5935,39.8683],[-75.5959,39.8652],[-75.599,39.862],[-75.6003,39.8602],[-75.6015,39.858],[-75.601,39.8562],[-75.5975,39.8539],[-75.5939,39.8515],[-75.5946,39.8488],[-75.5965,39.8457],[-75.5978,39.8416],[-75.5973,39.8379],[-75.6146,39.835],[-75.6308,39.8314],[-75.6464,39.827],[-75.647,39.8268],[-75.6661,39.82],[-75.6775,39.8156],[-75.6928,39.8074],[-75.7056,39.7991],[-75.7177,39.7912],[-75.724,39.7866],[-75.7268,39.7845],[-75.7378,39.775],[-75.7476,39.7653],[-75.7551,39.756],[-75.7611,39.7478],[-75.7662,39.7393],[-75.77,39.731],[-75.7723,39.7231],[-75.7875,39.7231],[-76.0148,39.7228],[-76.1392,39.7223],[-76.1373,39.7262],[-76.1337,39.728],[-76.1307,39.728],[-76.1266,39.7265],[-76.1236,39.7242],[-76.1188,39.726],[-76.1187,39.7301],[-76.1205,39.7333],[-76.1198,39.7364],[-76.1144,39.7368],[-76.1115,39.735],[-76.1121,39.7318],[-76.1134,39.7287],[-76.1104,39.7268],[-76.1051,39.7254],[-76.0996,39.7285],[-76.0965,39.7326],[-76.0959,39.7362],[-76.0988,39.738],[-76.1018,39.7399],[-76.1018,39.7421],[-76.1011,39.7449],[-76.0957,39.7448],[-76.0909,39.7452],[-76.0873,39.7474],[-76.0842,39.7537],[-76.0841,39.7592],[-76.0804,39.7609],[-76.0678,39.7626],[-76.066,39.7644],[-76.0654,39.7671],[-76.0659,39.7708],[-76.0628,39.7734],[-76.0616,39.7752],[-76.0615,39.7789],[-76.0567,39.7802],[-76.0537,39.7819],[-76.0506,39.7846],[-76.0481,39.79],[-76.0444,39.7963],[-76.0377,39.8026],[-76.0352,39.808],[-76.0303,39.813],[-76.0308,39.8175],[-76.032,39.8207],[-76.0265,39.8247],[-76.0253,39.826],[-76.0252,39.8301],[-76.0234,39.831],[-76.0191,39.8319],[-76.0191,39.8337],[-76.0202,39.8378],[-76.023,39.8464],[-76.0217,39.8518],[-76.0211,39.8537],[-76.0181,39.8545],[-76.0163,39.854],[-76.0127,39.8531],[-76.0103,39.8531],[-76.0091,39.8544],[-76.007,39.8666],[-76.0051,39.8712],[-76.0039,39.873],[-76.0015,39.8738],[-75.9991,39.8734],[-75.9974,39.8715],[-75.9956,39.8701],[-75.9932,39.8697],[-75.9926,39.8706],[-75.9908,39.8719],[-75.9877,39.8732],[-75.9871,39.8746],[-75.9877,39.8768],[-75.9912,39.8801],[-75.9905,39.8828],[-75.9899,39.8868],[-75.9879,39.8927],[-75.9885,39.895],[-75.9902,39.8977],[-75.9943,39.901],[-75.9961,39.9028],[-75.9957,39.9236],[-75.9962,39.9259],[-75.998,39.9273],[-75.9968,39.9282],[-75.9938,39.9277],[-75.9926,39.9268],[-75.9914,39.9272],[-75.9902,39.9286],[-75.9859,39.9308],[-75.9841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Abdul","contributorId":55405,"corporation":false,"usgs":true,"family":"Mohammad","given":"Abdul","email":"","affiliations":[],"preferred":false,"id":226319,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":52700,"text":"fs09102 - 2002 - Age of ground water at city of Lincoln's municipal well field near Ashland, Nebraska","interactions":[],"lastModifiedDate":"2012-02-02T00:11:58","indexId":"fs09102","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"2002","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":"091-02","title":"Age of ground water at city of Lincoln's municipal well field near Ashland, Nebraska","language":"ENGLISH","publisher":"Geological Survey (U.S.)","doi":"10.3133/fs09102","usgsCitation":"Steele, G.V., 2002, Age of ground water at city of Lincoln's municipal well field near Ashland, Nebraska: U.S. Geological Survey Fact Sheet 091-02, 6 p., https://doi.org/10.3133/fs09102.","productDescription":"6 p.","costCenters":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"links":[{"id":125230,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/fs/2002/0091/report-thumb.jpg"},{"id":87028,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/fs/2002/0091/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae3e4b07f02db689311","contributors":{"authors":[{"text":"Steele, Gregory V. gvsteele@usgs.gov","contributorId":783,"corporation":false,"usgs":true,"family":"Steele","given":"Gregory","email":"gvsteele@usgs.gov","middleInitial":"V.","affiliations":[{"id":464,"text":"Nebraska Water Science Center","active":true,"usgs":true}],"preferred":true,"id":245859,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":44921,"text":"wri024226 - 2002 - Magnitude and extent of arsenic and thallium concentrations in ground water and sediments at the Charleston Naval Complex, North Charleston, South Carolina, 1994-99","interactions":[],"lastModifiedDate":"2014-04-09T15:28:58","indexId":"wri024226","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"2002","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":"2002-4226","title":"Magnitude and extent of arsenic and thallium concentrations in ground water and sediments at the Charleston Naval Complex, North Charleston, South Carolina, 1994-99","docAbstract":"Water-quality samples were collected quarterly\nduring 1994-99 from 604 wells screened in the\nsurficial aquifer system beneath the Charleston Naval\nComplex, North Charleston, South Carolina. Arsenic\nand thallium were selected for analysis because\nconcentrations of these metals in some wells\nconsistently exceeded the established (2001) drinking water\nmaximum contaminant levels of 10 and\n2 micrograms per liter, respectively. The analysis was\nconducted to determine the magnitude and spatial\ndistribution of arsenic and thallium in ground water at\nthe Charleston Naval Complex and to quantify arsenic\nand thallium concentrations in a dated sediment core\nfrom Shipyard Creek marsh near the southern\nboundary of the Naval Complex.\nThe surficial aquifer system beneath the\nCharleston Naval Complex consists of an unconfined\nupper surficial aquifer and a confined lower surficial\naquifer. Hydraulic connection between the two aquifers\nis limited or nonexistent throughout the system at the\nNaval Complex. The Charleston Naval Complex is\ndivided into nine operational units designated as zones\nA through I. Arsenic and thallium concentration data\nwere compiled and interpreted for the two surficial\naquifers within each zone.\nMean arsenic (n=603) and thallium (n=604)\nconcentrations were calculated for water samples from\neach well screened in the upper and lower surficial\naquifers. In the upper surficial aquifer, mean arsenic\nconcentrations ranged from 0.9 to 339 micrograms\nper liter and exceeded 10 micrograms per liter in\n29 percent of the wells. In the lower surficial aquifer,\nmean arsenic concentrations ranged from 1.0 to\n97.4 micrograms per liter and exceeded 10 micrograms\nper liter in 23 percent of the wells. The greatest number\nof water samples with mean arsenic concentrations\nexceeding 10 micrograms per liter were collected from\nwells in the upper surficial aquifer at zone E in the\nnorthwestern part of the study area.\nWell clusters, defined as three or more wells in\na solid-waste management unit or area of concern,\nwhere the mean arsenic concentration exceeded\n10 micrograms per liter, were identified in association\nwith 12 sites in the upper surficial aquifer-solid-waste\nmanagement unit 039 (a drum-storage area) in zone A;\nsolid-waste management units 044 (coal-storage area)\nand 047 (burning dump) in zone C; solid-waste\nmanagement unit 065 (lead-storage area) and area of\nconcern 556 (dry docks 3 and 4) in zone E; areas of\nconcern 609 (building 1346 gas station) and 613\n(locomotive shop) in zone F; solid-waste management\nunits 006 (public works storage yard) and 008 (oil\nsludge pit), and area of concern 709 (fuel-delivery\nsystem wells 12, 13, and 14) in zone G; and solid-waste\nmanagement units 009 (closed landfill) and 196 (south\nlandfill) in zone H. One well cluster was identified in\nthe lower surficial aquifer in association with solidwaste\nmanagement unit 009 (closed landfill) in zone H.\nMean thallium concentrations in water from all\nwells ranged from less than 1.6 to 32.6 micrograms per\nliter in water samples from the upper surficial aquifer,\nand from less than 1.6 to 67.7 micrograms per liter in\nwater samples from the lower surficial aquifer. Mean\nthallium concentrations equal to or greater than\n10 micrograms per liter were present in water samples\nfrom 21 of 604 wells (3.5 percent). Of the 21 wells,\n14 wells were located at solid-waste management unit\n009 (closed landfill) in zone H near Shipyard Creek,\n8 wells in the upper aquifer, and 6 wells in the lower aquifer. One well cluster where thallium exceeded\n10 micrograms per liter was identified in association\nwith solid-waste management unit 009 (closed landfill)\nin the upper surficial aquifer.\nMean arsenic and thallium concentrations in\nwater were calculated for all wells screened in one\naquifer and located in a single zone, and are referred to\nas zone mean concentration in this report. Zone mean\narsenic concentrations in all nine zones ranged from\n3.2 to 18 micrograms per liter in water samples from\nthe upper surficial aquifer and from 2.7 to 22 micrograms\nper liter in water samples from the lower\nsurficial aquifer. Zone mean thallium concentrations in\nall nine zones ranged from 3.2 to 13 micrograms per\nliter in water samples from the upper surficial aquifer\nand from 3.2 to 14 micrograms per liter in water\nsamples from the lower surficial aquifer.\nGround-water samples rarely had elevated\n(equal to or greater than 10 micrograms per liter)\nconcentrations of both arsenic and thallium. Water\nsamples had coincident elevated arsenic and thallium\nconcentrations in 10 wells in zone H, 1 well in zone A,\nand 1 well in zone B.\nSediment quality at Shipyard Creek marsh was\ninvestigated by collecting an 11.8-foot -long sediment\ncore (SYC-1) adjacent to zone I. The mean arsenic\nconcentration in sediment samples from SYC-1\n(n= 160) was 3.05 milligrams per kilogram plus or\nminus 0.92. The mean arsenic concentration and\nstandard deviation calculated for SYC-1 sediment\nsamples fall within the standard error for the\nbackground mean arsenic concentration reported for\nSouth Carolina sediments (1.5 milligrams per kilogram\nplus or minus 2. 7). All but one sample (core depth\n=50 inches) was less than the threshold-effects level of\n7.24 milligrams per kilogram. Acid extracts of the\nsediment samples were analyzed for thallium\nconcentration, but none were detected. These data\nindicate no obvious change in arsenic or thallium\nconcentrations with depth in the core.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Columbia, SC","doi":"10.3133/wri024226","collaboration":"Prepared in cooperation with the Southern Division Naval Facilities Engineering Command","usgsCitation":"Mirecki, J.E., and Falls, W.F., 2002, Magnitude and extent of arsenic and thallium concentrations in ground water and sediments at the Charleston Naval Complex, North Charleston, South Carolina, 1994-99: U.S. Geological Survey Water-Resources Investigations Report 2002-4226, Report: v, 37 p.;. Plate 1: 33.12 inches x 42.37 inches; Plate 2: 32.76 inches x 42.26 inches, https://doi.org/10.3133/wri024226.","productDescription":"Report: v, 37 p.;. Plate 1: 33.12 inches x 42.37 inches; Plate 2: 32.76 inches x 42.26 inches","additionalOnlineFiles":"Y","costCenters":[],"links":[{"id":162166,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/wri024226.jpg"},{"id":286077,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/2002/4226/report.pdf"},{"id":286075,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/2002/4226/plate-1.pdf"},{"id":286076,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/2002/4226/plate-2.pdf"}],"country":"United States","state":"South Carolina","city":"Charleston","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -79.973339,32.829574 ], [ -79.973339,32.871134 ], [ -79.934701,32.871134 ], [ -79.934701,32.829574 ], [ -79.973339,32.829574 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a80e4b07f02db6494f6","contributors":{"authors":[{"text":"Mirecki, June Elizabeth","contributorId":48225,"corporation":false,"usgs":true,"family":"Mirecki","given":"June","email":"","middleInitial":"Elizabeth","affiliations":[],"preferred":false,"id":230683,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Falls, W. Fred 0000-0003-2928-9795 wffalls@usgs.gov","orcid":"https://orcid.org/0000-0003-2928-9795","contributorId":107754,"corporation":false,"usgs":true,"family":"Falls","given":"W.","email":"wffalls@usgs.gov","middleInitial":"Fred","affiliations":[],"preferred":false,"id":230684,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":44949,"text":"wri024151 - 2002 - Characterization of selenium in the lower Gunnison River basin, Colorado, 1988-2000","interactions":[],"lastModifiedDate":"2012-02-02T00:10:12","indexId":"wri024151","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"2002","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":"2002-4151","title":"Characterization of selenium in the lower Gunnison River basin, Colorado, 1988-2000","docAbstract":"Selenium concentrations in certain water bodies in the lower Gunnison River Basin, including the lower Gunnison River and lower Uncompahgre River, have exceeded the Colorado water-quality standard of 5 micrograms per liter for selenium. A task force was formed in 1998 that consists of various government agencies, private irrigation companies, and local residents to address the selenium concerns in the lower Gunnison River Basin. The task force, working with the National Irrigation Water Quality Program, needed more detailed information on selenium loading in the basin to develop viable alternatives for remediating selenium in the lower Gunnison River Basin. \r\n\r\nIn 1999-2000, the U.S. Geological Survey collected selenium data for tributaries of the Gunnison River downstream from the North Fork of the Gunnison and in the North Fork Basin. The largest selenium load in a tributary stream was in the Uncompahgre River, which accounted for about 38 percent of the selenium load in the Gunnison River at Whitewater. The North Fork of the Gunnison River accounted for about 7 percent of the selenium load in the Gunnison River. Two tributaries east of Delta, Sunflower Drain and Bonafide Ditch, consist primarily of irrigation return flows and were other major selenium sources to the Gunnison River. \r\n\r\nSome tributaries in the lower North Fork Basin had selenium concentrations exceeding 5 micrograms per liter. Except for several streams draining the Uncompahgre Plateau, many tributaries to the Gunnison River downstream from the North Fork had selenium concentrations exceeding 5 micrograms per liter. Except during occasional rain and snowmelt events, selenium loading from nonirrigated desert areas was minimal. \r\n\r\nDetailed characterization studies were done in 1999-2000 on Cedar Creek and Loutzenhizer Arroyo, which contribute the largest tributary selenium loads to the Uncompahgre River. Selenium concentrations in Cedar Creek downstream from Miguel Road ranged from 12 to 28 micrograms per liter in November 1999. Montrose Arroyo was the largest selenium source to Cedar Creek. On an annual basis, about 20 percent of the selenium load in Cedar Creek originates in the basin upstream from Miguel Road. \r\n\r\nSelenium concentrations in Loutzenhizer Arroyo ranged from 157 to 347 micrograms per liter in February 2000. A significant increase in selenium concentrations occurred in the stream reach between the Selig Canal and Falcon Road (LZU7). Although selenium concentrations in the west tributary of Loutzenhizer Arroyo were lower than in the main stem, the west tributary contributed about 41 percent of the selenium load. Downstream from the confluence with the west tributary to the mouth, selenium concentrations in the arroyo gradually decreased, and the increase in selenium load in the lower reach was small.","language":"ENGLISH","doi":"10.3133/wri024151","usgsCitation":"Butler, D.L., and Leib, K.J., 2002, Characterization of selenium in the lower Gunnison River basin, Colorado, 1988-2000: U.S. Geological Survey Water-Resources Investigations Report 2002-4151, iv, 26 p. : ill., col. maps ; 28 cm., https://doi.org/10.3133/wri024151.","productDescription":"iv, 26 p. : ill., col. maps ; 28 cm.","costCenters":[],"links":[{"id":162004,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":3823,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/wri024151","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aa9e4b07f02db66810c","contributors":{"authors":[{"text":"Butler, David L.","contributorId":12843,"corporation":false,"usgs":true,"family":"Butler","given":"David","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":230754,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Leib, Kenneth J. 0000-0002-0373-0768 kjleib@usgs.gov","orcid":"https://orcid.org/0000-0002-0373-0768","contributorId":701,"corporation":false,"usgs":true,"family":"Leib","given":"Kenneth","email":"kjleib@usgs.gov","middleInitial":"J.","affiliations":[],"preferred":true,"id":230753,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":47800,"text":"fs12302 - 2002 - Effects of shrubland changes on birds in the Intermountain West","interactions":[],"lastModifiedDate":"2017-03-31T11:41:54","indexId":"fs12302","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"2002","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":"123-02","title":"Effects of shrubland changes on birds in the Intermountain West","docAbstract":"We are integrating field surveys with information obtained from satellite imagery to determine how birds respond to the habitat changes in shrubland regions in the Intermountain West. Our objectives are to determine the primary causes that change shrubland habitats, the spatial and temporal scales at which shrubland landscapes change, and the mechanisms by which distribution and abundance of bird populations are influenced by habitat change.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/fs12302","usgsCitation":"Knick, S.T., and Loveland, T., 2002, Effects of shrubland changes on birds in the Intermountain West: U.S. Geological Survey Fact Sheet 123-02, 1 p., https://doi.org/10.3133/fs12302.","productDescription":"1 p.","onlineOnly":"Y","costCenters":[{"id":290,"text":"Forest and Rangeland Ecosystem Science Center","active":false,"usgs":true}],"links":[{"id":4012,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/fs/2002/0123/fs12302.pdf","text":"Report","size":"420 KB","linkFileType":{"id":1,"text":"pdf"},"description":"FS 123-02"},{"id":120205,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/fs/2002/0123/coverthb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a28e4b07f02db61098c","contributors":{"authors":[{"text":"Knick, Steven T. 0000-0003-4025-1704 steve_knick@usgs.gov","orcid":"https://orcid.org/0000-0003-4025-1704","contributorId":159,"corporation":false,"usgs":true,"family":"Knick","given":"Steven","email":"steve_knick@usgs.gov","middleInitial":"T.","affiliations":[{"id":290,"text":"Forest and Rangeland Ecosystem Science Center","active":false,"usgs":true},{"id":289,"text":"Forest and Rangeland Ecosys Science Center","active":true,"usgs":true}],"preferred":true,"id":236266,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Loveland, Thomas R. 0000-0003-3114-6646 loveland@usgs.gov","orcid":"https://orcid.org/0000-0003-3114-6646","contributorId":3005,"corporation":false,"usgs":true,"family":"Loveland","given":"Thomas R.","email":"loveland@usgs.gov","affiliations":[{"id":223,"text":"Earth Resources Observation and Science (EROS) Center (Geography)","active":false,"usgs":true}],"preferred":false,"id":236267,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":50680,"text":"ofr02325 - 2002 - Lake belt study area: High-resolution seismic-reflection survey, Miami-Dade County Florida","interactions":[],"lastModifiedDate":"2025-04-10T15:40:37.924649","indexId":"ofr02325","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"2002","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":"2002-325","title":"Lake belt study area: High-resolution seismic-reflection survey, Miami-Dade County Florida","docAbstract":"<h1>Executive Summary &nbsp;</h1><p>The Northwest Dade County Freshwater Lake Plan Area (commonly referred to as the Lake Belt Area) is vital to the future planning and development of southeastern Florida. This area is located within one of the most environmentally sensitive parts of the state – the eastern borders of the Everglades National Park (ENP). The Lake Belt Area and Water Conservation Area BB (WCA BB) provide half of the limestone mining resources used in the state every year. Starting in the mid-1800s canals and levees were built in the area to drain and help develop economic and water resources including protection from floods and droughts. These construction projects have changed the natural water flow (hydropattern and hydroperiod) through the hydrologic system. Changes to the hydropattern and hydroperiod of the area have also had an adverse impact by disrupting the normal breeding patterns of species within the Everglades ecosystem</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr02325","productDescription":"viii, 24 p.","costCenters":[{"id":27821,"text":"Caribbean-Florida Water Science Center","active":true,"usgs":true}],"links":[{"id":170041,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/2002/0325/coverthb.jpg"},{"id":390974,"rank":2,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_54122.htm"},{"id":4155,"rank":3,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/2002/0325/ofr02-325.pdf","text":"Report","size":"499 KB MB","linkFileType":{"id":1,"text":"pdf"},"description":"OFR 02-325"}],"country":"United States","state":"Florida","county":"Miami-Dad County","otherGeospatial":"Lake belt study area","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -80.52154541015625,\n              25.64895443060557\n            ],\n            [\n              -80.25787353515625,\n              25.64895443060557\n            ],\n            [\n              -80.25787353515625,\n              25.94322678532246\n            ],\n            [\n              -80.52154541015625,\n              25.94322678532246\n            ],\n            [\n              -80.52154541015625,\n              25.64895443060557\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","contact":"<p><a href=\"https://www.usgs.gov/centers/car-fl-water\" data-mce-href=\"https://www.usgs.gov/centers/car-fl-water\">Caribbean-Florida Water Science Center</a><br>U.S. Geological Survey<br>3321 College Avenue<br>Davie, FL 33314</p><p><a href=\"../contact\" data-mce-href=\"../contact\">Contact Pubs Warehouse</a></p>","publishedDate":"2003-10-01","noUsgsAuthors":false,"publicationDate":"2003-10-01","publicationStatus":"PW","scienceBaseUri":"4f4e4b32e4b07f02db6b441f","contributors":{"authors":[{"text":"Kindinger, Jack L. jkindinger@usgs.gov","contributorId":815,"corporation":false,"usgs":true,"family":"Kindinger","given":"Jack","email":"jkindinger@usgs.gov","middleInitial":"L.","affiliations":[{"id":574,"text":"St. Petersburg Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":false,"id":242065,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
]}