Ground-water-flow modeling was used to estimate ground-water-flow paths and traveltimes to quantitatively assess the hydrologic processes affecting ground water and solute movement to drain laterals. Modeling results were used to calculate the depth distribution of ground water flowing into drain laterals at 1.8 meters (drain lateral 1) and 2.7 meters (drain lateral 2) below land surface. The simulations indicated that under nonirrigated conditions about 89 percent of the flow in drain lateral 2 was from ground water originating from depths greater than 6 meters below land surface. The deep ground water has higher selenium concentrations than shallow ground water. Simulation of irrigated conditions indicates that as recharge increases, the proportion of deep ground water entering the drain laterals decreases.
Ground-water-flow modeling also was used to estimate selenium loads in drain laterals for varying drain-lateral flow rates. Simulated loads are in general agreement with measured loads and increase with increasing drain-lateral flow. Simulations further indicate ground water that contains high-selenium concentrations probably will continue to enter drain lateral 2 for more than 8 years.
","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr90137","usgsCitation":"Fio, J., and Deverel, S.J., 1990, Ground-water flow and solute movement to drain laterals, western San Joaquin Valley, California; II, Quantitative hydrologic assessment: U.S. Geological Survey Open-File Report 90-137, iv, 15 p., https://doi.org/10.3133/ofr90137.","productDescription":"iv, 15 p.","costCenters":[{"id":154,"text":"California Water Science Center","active":true,"usgs":true}],"links":[{"id":359121,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1990/0137/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":151477,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1990/0137/report-thumb.jpg"}],"country":"United States","state":"California","otherGeospatial":"San Joaquin Valley","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -121.84,35.06 ], [ -121.84,38.17 ], [ -118.67,38.17 ], [ -118.67,35.06 ], [ -121.84,35.06 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ab0e4b07f02db66d5fc","contributors":{"authors":[{"text":"Fio, J.L.","contributorId":56662,"corporation":false,"usgs":true,"family":"Fio","given":"J.L.","affiliations":[],"preferred":false,"id":179952,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Deverel, S. J.","contributorId":65478,"corporation":false,"usgs":true,"family":"Deverel","given":"S.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":179953,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":18904,"text":"ofr90170 - 1990 - Statistical summaries of selected Iowa streamflow data through September 30, 1988","interactions":[],"lastModifiedDate":"2016-03-09T14:37:21","indexId":"ofr90170","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1990","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":"90-170","title":"Statistical summaries of selected Iowa streamflow data through September 30, 1988","docAbstract":"Statistical summaries of streamflow data collected at 144 active and discontinued stream-gaging stations in Iowa through water year 1988 are presented in the report. The summaries for each streamgaging station include: 1) station description, 2) the most recent stage-discharge rating table, 3) statistics of monthly and annual mean discharges, 4) boxplots of monthly and annual mean discharges, 5) monthly and annual flow durations, 6) probabilities of annual high discharges, 7) probabilities of annual low discharges, and 8) probabilities of seasonal low discharges. The minimum period of record at stations included in the report is 10 years. The location of each station is shown on a map of Iowa.
","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr90170","collaboration":"Prepared in cooperation with the U.S. Army Corps of Engineers, Iowa Department of Natural Resources, and Iowa Department of Transportation","usgsCitation":"Fischer, E., Melcher, N., and Kluesner, S., 1990, Statistical summaries of selected Iowa streamflow data through September 30, 1988: U.S. Geological Survey Open-File Report 90-170, x, 641 p.: ill.; 28 cm., https://doi.org/10.3133/ofr90170.","productDescription":"x, 641 p.: ill.; 28 cm.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":351,"text":"Iowa Water Science 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\"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49dce4b07f02db5e1bab","contributors":{"authors":[{"text":"Fischer, E.E.","contributorId":102480,"corporation":false,"usgs":true,"family":"Fischer","given":"E.E.","email":"","affiliations":[],"preferred":false,"id":179956,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Melcher, N.B.","contributorId":71554,"corporation":false,"usgs":true,"family":"Melcher","given":"N.B.","email":"","affiliations":[],"preferred":false,"id":179954,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Kluesner, S.P.","contributorId":75954,"corporation":false,"usgs":true,"family":"Kluesner","given":"S.P.","email":"","affiliations":[],"preferred":false,"id":179955,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":18913,"text":"ofr89623 - 1990 - Hydrologic data collected in the vicinity of the proposed gamma-ray and neutrino detector site, Hot Spring County, Arkansas, 1988-89","interactions":[],"lastModifiedDate":"2012-02-02T00:07:31","indexId":"ofr89623","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1990","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":"89-623","title":"Hydrologic data collected in the vicinity of the proposed gamma-ray and neutrino detector site, Hot Spring County, Arkansas, 1988-89","docAbstract":"An abandoned barite mine in Hot Spring County, Arkansas, has been selected as the location for a proposed gamma-ray and neutrino detector site. As part of the hydrologic evaluation of the site, the U.S. Geological Survey in cooperation with the Arkansas Geological Commission collected hydrologic data at selected locations in the vicinity of the abandoned barite mine. Data collected as part of the project included water quality, pond-evaluation, and precipitation data within the abandoned barite mine and flow and water quality data at selected sites in the vicinity of the mine. Water quality samples from within the abandoned mine were collected at three locations in the pond at selected depths. These data included field measurements of specific conductance, pH, water temperature, dissolved oxygen, major ions, and trace metals. Major ion and trace-metal samples were collected at six stream sites, one lake site, and two wastewater pond sites. Pond elevation and precipitation data from within the abandoned barite mine were measured during the period between July 1, 1988 and June 30, 1989. Twevle discharge measurements during the period between June 21, 1988, and June 26, 1989, were collected at six sites in the vicinity of the abandoned barite mine. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr89623","usgsCitation":"Fitzpatrick, D., and Westerfield, P., 1990, Hydrologic data collected in the vicinity of the proposed gamma-ray and neutrino detector site, Hot Spring County, Arkansas, 1988-89: U.S. Geological Survey Open-File Report 89-623, iv, 17 p. :ill. ;28 cm., https://doi.org/10.3133/ofr89623.","productDescription":"iv, 17 p. :ill. ;28 cm.","costCenters":[],"links":[{"id":151601,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1989/0623/report-thumb.jpg"},{"id":48311,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1989/0623/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a26e4b07f02db60f7ed","contributors":{"authors":[{"text":"Fitzpatrick, D. J.","contributorId":33313,"corporation":false,"usgs":true,"family":"Fitzpatrick","given":"D. 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The study was conducted from October 1985-October 1988 in cooperation with the State of New Hampshire Department of Environmental Services, Water Resources Division. The data include information on 1,232 inventory sites, 66 exploration boreholes drilled for this study, and grain-size analyses of 61 split-spoon sediment samples. Water-level data were collected from 33 observation wells drilled during the course of the project . Water-quality analyses collected during this study are presented for 24 observation and 6 public supply wells. Water-quality properties measured in the field include temperature, specific conductance, dissolved oxygen concentration, and pH. Samples from the 30 wells were analyzed in the laboratory for nutrients, common anions and cations, and selected volatile organic compounds . Streamflow data are presented for 16 sites.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr89390","usgsCitation":"Flanagan, S., and Stekl, P.J., 1990, Geohydrologic, ground-water quality, and streamflow data for the stratified-drift aquifers in the lower Merrimack and coastal river basins, southeastern New Hampshire: U.S. Geological Survey Open-File Report 89-390, Report: v, 130 p.; 3 Plates: 22.66 x 30.74 inches or smaller, https://doi.org/10.3133/ofr89390.","productDescription":"Report: v, 130 p.; 3 Plates: 22.66 x 30.74 inches or smaller","costCenters":[],"links":[{"id":48316,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1989/0390/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":48317,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1989/0390/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":1084,"rank":2,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/ofr89390/","linkFileType":{"id":5,"text":"html"}},{"id":151891,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":48318,"rank":5,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1989/0390/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":420159,"rank":6,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_17659.htm","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"New Hampshire","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -70.7337619808828,\n 42.95067873236033\n ],\n [\n -71.42609766102849,\n 43.06385519231904\n ],\n [\n -71.41252245161346,\n 42.67782617752644\n ],\n [\n -70.66045585004349,\n 42.67782617752644\n ],\n [\n -70.7337619808828,\n 42.95067873236033\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1be4b07f02db6a8d9a","contributors":{"authors":[{"text":"Flanagan, Sarah M.","contributorId":8492,"corporation":false,"usgs":true,"family":"Flanagan","given":"Sarah M.","affiliations":[],"preferred":false,"id":179982,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Stekl, Peter J.","contributorId":63415,"corporation":false,"usgs":true,"family":"Stekl","given":"Peter","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":179983,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":18928,"text":"ofr90569 - 1990 - Preliminary permeability and water-retention data for nonwelded and bedded tuff samples, Yucca Mountain area, Nye County, Nevada","interactions":[],"lastModifiedDate":"2012-02-02T00:07:30","indexId":"ofr90569","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1990","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":"90-569","title":"Preliminary permeability and water-retention data for nonwelded and bedded tuff samples, Yucca Mountain area, Nye County, Nevada","language":"ENGLISH","publisher":"U.S. Geological Survey :\r\nBooks and Open-File Reports Section [distributor],","doi":"10.3133/ofr90569","usgsCitation":"Flint, L.E., and Flint, A.L., 1990, Preliminary permeability and water-retention data for nonwelded and bedded tuff samples, Yucca Mountain area, Nye County, Nevada: U.S. Geological Survey Open-File Report 90-569, v, 57 p. :ill., maps ;28 cm., https://doi.org/10.3133/ofr90569.","productDescription":"v, 57 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":151715,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1990/0569/report-thumb.jpg"},{"id":48328,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1990/0569/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aafe4b07f02db66cd72","contributors":{"authors":[{"text":"Flint, Lorraine E. 0000-0002-7868-441X lflint@usgs.gov","orcid":"https://orcid.org/0000-0002-7868-441X","contributorId":1184,"corporation":false,"usgs":true,"family":"Flint","given":"Lorraine","email":"lflint@usgs.gov","middleInitial":"E.","affiliations":[{"id":154,"text":"California Water Science Center","active":true,"usgs":true}],"preferred":true,"id":179998,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Flint, Alan L. 0000-0002-5118-751X aflint@usgs.gov","orcid":"https://orcid.org/0000-0002-5118-751X","contributorId":1492,"corporation":false,"usgs":true,"family":"Flint","given":"Alan","email":"aflint@usgs.gov","middleInitial":"L.","affiliations":[{"id":154,"text":"California Water Science Center","active":true,"usgs":true},{"id":657,"text":"Western Geographic Science Center","active":true,"usgs":true}],"preferred":true,"id":179999,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":18981,"text":"ofr88305 - 1990 - Geohydrology and simulation of ground-water flow in the Mesilla Basin, Dona Ana County, New Mexico, and El Paso County, Texas","interactions":[{"subject":{"id":18981,"text":"ofr88305 - 1990 - Geohydrology and simulation of ground-water flow in the Mesilla Basin, Dona Ana County, New Mexico, and El Paso County, Texas","indexId":"ofr88305","publicationYear":"1990","noYear":false,"title":"Geohydrology and simulation of ground-water flow in the Mesilla Basin, Dona Ana County, New Mexico, and El Paso County, Texas"},"predicate":"SUPERSEDED_BY","object":{"id":38448,"text":"pp1407C - 1992 - Geohydrology and simulation of ground-water flow in the Mesilla Basin, Dona Ana County, New Mexico, and El Paso County, Texas, with a section on water quality and geochemistry","indexId":"pp1407C","publicationYear":"1992","noYear":false,"chapter":"C","title":"Geohydrology and simulation of ground-water flow in the Mesilla Basin, Dona Ana County, New Mexico, and El Paso County, Texas, with a section on water quality and geochemistry"},"id":1}],"supersededBy":{"id":38448,"text":"pp1407C - 1992 - Geohydrology and simulation of ground-water flow in the Mesilla Basin, Dona Ana County, New Mexico, and El Paso County, Texas, with a section on water quality and geochemistry","indexId":"pp1407C","publicationYear":"1992","noYear":false,"title":"Geohydrology and simulation of ground-water flow in the Mesilla Basin, Dona Ana County, New Mexico, and El Paso County, Texas, with a section on water quality and geochemistry"},"lastModifiedDate":"2021-02-04T17:37:27.297554","indexId":"ofr88305","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1990","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":"88-305","title":"Geohydrology and simulation of ground-water flow in the Mesilla Basin, Dona Ana County, New Mexico, and El Paso County, Texas","docAbstract":"No abstract available.
","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr88305","usgsCitation":"Frenzel, P.F., Kaehler, C., and Anderholm, S., 1990, Geohydrology and simulation of ground-water flow in the Mesilla Basin, Dona Ana County, New Mexico, and El Paso County, Texas: U.S. Geological Survey Open-File Report 88-305, Report: xii, 179 p.; 5 Plates: 17.29 x 20.97 inches or smaller, https://doi.org/10.3133/ofr88305.","productDescription":"Report: xii, 179 p.; 5 Plates: 17.29 x 20.97 inches or smaller","costCenters":[],"links":[{"id":383000,"rank":7,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1988/0305/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":382999,"rank":6,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1988/0305/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":382998,"rank":5,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1988/0305/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":382997,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1988/0305/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":382996,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1988/0305/plate-5.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":382995,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1988/0305/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":151775,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1988/0305/report-thumb.jpg"}],"country":"United States","state":"New Mexico, Texas","county":"Dona Ana County, New Mexico, El Paso County, Texas","otherGeospatial":"Mesilla Basin","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -106.85302734374999,\n 31.53640812943961\n ],\n [\n -105.7159423828125,\n 31.53640812943961\n ],\n [\n -105.7159423828125,\n 32.368363067704706\n ],\n [\n -106.85302734374999,\n 32.368363067704706\n ],\n [\n -106.85302734374999,\n 31.53640812943961\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1be4b07f02db6a8c5b","contributors":{"authors":[{"text":"Frenzel, P. 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The nitrate nitrogen concentration of the mixture in the well can be predicted for steady-state conditions by calculating the concentration that results from the total weight of nitrogen and total volume of water entering the zone of contribution to the well. These calculations will allow water-quality managers to predict the nitrate concentrations that would be produced by different types and levels of development, and to plan development accordingly. Computations for different development schemes provide a technical basis for planners and managers to compare water quality effects and to select alternatives that limit nitrate concentration in wells. Appendix A contains tables of nitrate loads and water volumes from common sources for use with the accounting model. Appendix B describes the preparation of a spreadsheet for the nitrate loading calculations with a software package generally available for desktop computers. 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1990 - Bibliography on sampling ground water for organic compounds","interactions":[],"lastModifiedDate":"2012-02-02T00:07:24","indexId":"ofr90564","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1990","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":"90-564","title":"Bibliography on sampling ground water for organic compounds","language":"ENGLISH","publisher":"U.S. Geological Survey ;\r\nBooks and Open-File Reports Section [distributor],","doi":"10.3133/ofr90564","usgsCitation":"Gibs, J., Imbrigiotta, T., and Turner, K., 1990, Bibliography on sampling ground water for organic compounds: U.S. Geological Survey Open-File Report 90-564, iii, 22 p. ;28 cm., https://doi.org/10.3133/ofr90564.","productDescription":"iii, 22 p. ;28 cm.","costCenters":[],"links":[{"id":151107,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1990/0564/report-thumb.jpg"},{"id":48519,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1990/0564/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a4ce4b07f02db626a82","contributors":{"authors":[{"text":"Gibs, Jacob jgibs@usgs.gov","contributorId":1729,"corporation":false,"usgs":true,"family":"Gibs","given":"Jacob","email":"jgibs@usgs.gov","affiliations":[],"preferred":true,"id":180275,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Imbrigiotta, T.E. 0000-0003-1716-4768","orcid":"https://orcid.org/0000-0003-1716-4768","contributorId":86355,"corporation":false,"usgs":true,"family":"Imbrigiotta","given":"T.E.","affiliations":[],"preferred":false,"id":180277,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Turner, K.S.","contributorId":52986,"corporation":false,"usgs":true,"family":"Turner","given":"K.S.","email":"","affiliations":[],"preferred":false,"id":180276,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":19082,"text":"ofr90353 - 1990 - The U.S. Geological Survey Federal-State cooperative water-resources program fiscal year 1989","interactions":[],"lastModifiedDate":"2012-02-02T00:07:24","indexId":"ofr90353","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1990","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":"90-353","title":"The U.S. Geological Survey Federal-State cooperative water-resources program fiscal year 1989","language":"ENGLISH","publisher":"Dept. of the Interior, U.S. Geological Survey ;\r\nBooks and Open-File Reports Section [distributor],","doi":"10.3133/ofr90353","usgsCitation":"Gilbert, B., and Mann, W., 1990, The U.S. Geological Survey Federal-State cooperative water-resources program fiscal year 1989: U.S. Geological Survey Open-File Report 90-353, iii, 49 p. :ill. ;28 cm., https://doi.org/10.3133/ofr90353.","productDescription":"iii, 49 p. :ill. ;28 cm.","costCenters":[],"links":[{"id":151001,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1990/0353/report-thumb.jpg"},{"id":48521,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1990/0353/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4abce4b07f02db673460","contributors":{"authors":[{"text":"Gilbert, B.K.","contributorId":32167,"corporation":false,"usgs":true,"family":"Gilbert","given":"B.K.","email":"","affiliations":[],"preferred":false,"id":180282,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Mann, W.B.","contributorId":60230,"corporation":false,"usgs":true,"family":"Mann","given":"W.B.","affiliations":[],"preferred":false,"id":180283,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":19103,"text":"ofr90147 - 1990 - Aquifer-characteristic and water-chemistry data from wells on or near Navajo tribal lands in the Zuni River basin and Whitewater Arroyo drainage, west-central New Mexico","interactions":[],"lastModifiedDate":"2012-02-02T00:07:25","indexId":"ofr90147","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1990","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":"90-147","title":"Aquifer-characteristic and water-chemistry data from wells on or near Navajo tribal lands in the Zuni River basin and Whitewater Arroyo drainage, west-central New Mexico","language":"ENGLISH","publisher":"U.S. Geological Survey ;\r\nBooks and Open-File Reports [distributor],","doi":"10.3133/ofr90147","usgsCitation":"Goetz, C.L., 1990, Aquifer-characteristic and water-chemistry data from wells on or near Navajo tribal lands in the Zuni River basin and Whitewater Arroyo drainage, west-central New Mexico: U.S. Geological Survey Open-File Report 90-147, iv, 33 p. :maps ;28 cm., https://doi.org/10.3133/ofr90147.","productDescription":"iv, 33 p. :maps ;28 cm.","costCenters":[],"links":[{"id":150649,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1990/0147/report-thumb.jpg"},{"id":48539,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1990/0147/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":48540,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1990/0147/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac5e4b07f02db679ee4","contributors":{"authors":[{"text":"Goetz, C. L.","contributorId":55845,"corporation":false,"usgs":true,"family":"Goetz","given":"C.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":180309,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":19110,"text":"ofr90193 - 1990 - Data that describe at-a-point temporal variations in the transport rate and particle-size distribution of bedload; East Fork River, Wyoming, and Fall River, Colorado","interactions":[],"lastModifiedDate":"2012-02-02T00:07:25","indexId":"ofr90193","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1990","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":"90-193","title":"Data that describe at-a-point temporal variations in the transport rate and particle-size distribution of bedload; East Fork River, Wyoming, and Fall River, Colorado","docAbstract":"Data from the East Fork River, Wyoming, and the Fall River, Colorado, that document at-a-point temporal variations in the transport rate and particle-size distribution of bedload, associated with the downstream migration of dunes, are presented. Bedload sampling was undertaken, using a 76.2 x 76.2 mm Helley-Smith sampler, on three separate occasions at each site in June 1988. In each instance, the sampling time was 30 seconds and the sampling intervals 5 minutes. The sampling period ranged from 4.92 to 8.25 hours. Water stage did not vary appreciably during any of the sampling periods. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey ;\r\nBooks and Open-File Reports [distributor],","doi":"10.3133/ofr90193","usgsCitation":"Gomez, B., and Emmett, W.W., 1990, Data that describe at-a-point temporal variations in the transport rate and particle-size distribution of bedload; East Fork River, Wyoming, and Fall River, Colorado: U.S. Geological Survey Open-File Report 90-193, iv, 48 p. ;28 cm., https://doi.org/10.3133/ofr90193.","productDescription":"iv, 48 p. ;28 cm.","costCenters":[],"links":[{"id":150674,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1990/0193/report-thumb.jpg"},{"id":48546,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1990/0193/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac5e4b07f02db679c55","contributors":{"authors":[{"text":"Gomez, Basil","contributorId":65475,"corporation":false,"usgs":true,"family":"Gomez","given":"Basil","email":"","affiliations":[],"preferred":false,"id":180321,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Emmett, W. W.","contributorId":107695,"corporation":false,"usgs":true,"family":"Emmett","given":"W.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":180322,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":19226,"text":"ofr90392 - 1990 - A computer program for calculating subregional water budgets using results from the U.S. Geological Survey Modular Three-Dimensional Finite- Difference Ground-Water Flow Model","interactions":[],"lastModifiedDate":"2012-02-02T00:07:32","indexId":"ofr90392","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1990","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":"90-392","title":"A computer program for calculating subregional water budgets using results from the U.S. Geological Survey Modular Three-Dimensional Finite- Difference Ground-Water Flow Model","language":"ENGLISH","publisher":"U.S. Geological Survey ;\r\nBooks and Open-File Reports Section [distributor],","doi":"10.3133/ofr90392","usgsCitation":"Harbaugh, A., 1990, A computer program for calculating subregional water budgets using results from the U.S. Geological Survey Modular Three-Dimensional Finite- Difference Ground-Water Flow Model: U.S. Geological Survey Open-File Report 90-392, iii, 46 p. ;28 cm., https://doi.org/10.3133/ofr90392.","productDescription":"iii, 46 p. ;28 cm.","costCenters":[],"links":[{"id":151382,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1990/0392/report-thumb.jpg"},{"id":48686,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1990/0392/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b27e4b07f02db6b09a9","contributors":{"authors":[{"text":"Harbaugh, A.W.","contributorId":15208,"corporation":false,"usgs":true,"family":"Harbaugh","given":"A.W.","email":"","affiliations":[],"preferred":false,"id":180521,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":19244,"text":"ofr90398 - 1990 - Water-quality trends and basin activities and characteristics for the Albemarle-Pamlico estuarine system, North Carolina and Virginia","interactions":[],"lastModifiedDate":"2016-12-16T09:56:08","indexId":"ofr90398","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1990","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":"90-398","title":"Water-quality trends and basin activities and characteristics for the Albemarle-Pamlico estuarine system, North Carolina and Virginia","docAbstract":"The Albemarle-Pamlico estuarine system has a total basin area of nearly 31,000 square miles and includes the Neuse, Tar, Pamlico, Roanoke, Chowan, and Alligator Rivers, and the Albemarle, Pamlico, Currituck, Croatan, and Roanoke Sounds. Albemarle Sound receives the greatest freshwater inflow of all the sounds in the estuarine system. Inflow to this sound averages about 13,500 cubic feet per second. Inflow to Pamlico Sound from the Pamlico River averages around 5,400 cubic feet per second, and average inflow into the Neuse River estuary is about 6,100 cubic feet per second. Approximately one-half of the inflow into the system is from ground-water discharge.\r\n\r\nThe Neuse River basin has had the greatest increases in wastewater discharges (650 percent since the 1950's) and had the greatesttotal wastewater discharges of any of the basins in the study area, averaging about 200 million gallons per day in 1988. Wastewater discharges into the Neuse and Tar Rivers were nearly equal to the 7-day, 10-year low flows for these rivers.\r\n\r\nLand-use data compiled in 1973 for the lower parts of the Neuse River basin and lower part of the Tar-Pamlico River basin indicate that 25 percent of the area was evergreen forest, 25 percent was forested wetlands, 20 percent was cropland and pasture, 12 percent was mixed forest, 10 percent was nonforested wetland, and 4 percent was urban. The amount of nonforested wetland in the part of the study area along the Outer Banks declined 6.5 percent from 1973 to 1983.\r\n\r\nThe numbers of farms and acreage in agricultural use in the study area have declined since the 1920's. A decrease of more than 60 percentin the number of farms was shown between the early 1950's and 1982. Fertilizer sales increased through the 1970's, but declined in the 1980's. Manufacturing employment has increased in the last 30 years, while agricultural employment has decreased.\r\n\r\nData from seven stations of the U.S. Geological Survey National Stream Quality Accounting Network were used to evaluate water quality for the major streams flowing into the Albemarle-Pamlico estuarine system. Water-quality data for 296 stations in the estuarine system were examined for the period 1945-88.\r\n\r\nThe statistical test used for trend analysis was the Seasonal Kendall test (Hirsch and others, 1982). This nonparametric procedure is useful for analyses of water-quality properties that show non-normally distributed frequency distributions. The Seasonal Kendall trend analyses of water-quality data indicate that change has occurred in the water quality of the Albemarle-Pamlico estuarine system from 1945 to 1988. Dissolved-oxygen concentrations increased at a mean rate of 0.1 milligram per liter per year throughout the estuarine system, except in the Chowan River where decreases of approximately 0.06 milligram per liter per year occurred. In general, pH increased in streams throughout the area at a mean rate of 0.04 pH unit per year, except in the Pamlico River where pH decreased by 0.03 pH unit per year. A general increase in pH and dissolved-oxygen concentrations (if daytime measurements) might be indicative of more productive estuary conditions for algal growth. Suspended-solids concentrations decreased throughout the area at a mean rate of 1.1 milligrams per liter per year, probably as a result of a general decrease in suspended inorganic material. Increasing trends of salinity concentrations, as much as 0.1 part per thousand per year, were detected in Albemarle Sound. \r\n\r\nTotal ammonia plus organic nitrogen concentrations decreased (-0.03 milligram per liter per year) in streams throughout most of the area but increased (0.02 milligram per liter per year) in the Pamlico River. However, ammonia nitrogen concentrations decreased (-0.0035 milligram per liter per year) in the Pamlico River; therefore, increases in organic nitrogen probably caused the observed increase in combined ammonia plus organic nitrogen concentrations. This probably results from increas","language":"ENGLISH","publisher":"U.S. Geological Survey ;\r\nBooks and Open-File Reports [distributor],","doi":"10.3133/ofr90398","usgsCitation":"Harned, D., and Davenport, M., 1990, Water-quality trends and basin activities and characteristics for the Albemarle-Pamlico estuarine system, North Carolina and Virginia: U.S. Geological Survey Open-File Report 90-398, xii, 164 p. (some folded) :ill., maps ;28 cm., https://doi.org/10.3133/ofr90398.","productDescription":"xii, 164 p. (some folded) :ill., maps ;28 cm.","costCenters":[{"id":13634,"text":"South Atlantic Water Science Center","active":true,"usgs":true}],"links":[{"id":152032,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1990/0398/report-thumb.jpg"},{"id":48699,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1990/0398/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":48700,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1990/0398/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":48701,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1990/0398/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":48702,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1990/0398/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":48703,"rank":404,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1990/0398/plate-5.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":48704,"rank":405,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1990/0398/plate-6.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":48705,"rank":406,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1990/0398/plate-7.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":48706,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1990/0398/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United 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Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"87-121","title":"Thermal-pulse flowmeter for measuring slow water velocities in boreholes","language":"ENGLISH","publisher":"U.S. Geological Survey :\r\nBooks and Open-File Reports Section [distributor],","doi":"10.3133/ofr87121","usgsCitation":"Hess, A., 1990, Thermal-pulse flowmeter for measuring slow water velocities in boreholes: U.S. Geological Survey Open-File Report 87-121, v, 70 p. :ill. ;28 cm., https://doi.org/10.3133/ofr87121.","productDescription":"v, 70 p. :ill. ;28 cm.","costCenters":[],"links":[{"id":151851,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1987/0121/report-thumb.jpg"},{"id":48796,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1987/0121/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a56e4b07f02db62de49","contributors":{"authors":[{"text":"Hess, A.E.","contributorId":71979,"corporation":false,"usgs":true,"family":"Hess","given":"A.E.","email":"","affiliations":[],"preferred":false,"id":180690,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":19342,"text":"ofr90190 - 1990 - Water-quality, well-construction, and ground-water level data for an investigation of radionuclides in ground water, Hickman and Maury counties, Tennessee","interactions":[],"lastModifiedDate":"2012-02-02T00:07:29","indexId":"ofr90190","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1990","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":"90-190","title":"Water-quality, well-construction, and ground-water level data for an investigation of radionuclides in ground water, Hickman and Maury counties, Tennessee","docAbstract":"Water quality, well construction, and groundwater level data were collected for an investigation of radionuclides in groundwater in Maury and Hickman Counties, Tennessee. Seventeen wells and 3 springs were sampled in Hickman County, and 20 wells were sampled in Maury County. Samples from each site were analyzed for radionuclides, common and trace inorganic ions, indicators of redox conditions, selected nutrients, total organic carbon, and selected physical characteristics. Well-construction data were obtained to help determine the source of the water. Where possible, groundwater level measurements were made for each well sampled. Samples were collected from May 1989 through mid-August 1989. Data are presented in tables. Maps of each county show the location of the sites sampled. (USGS)","language":"ENGLISH","publisher":"Dept. of the Interior, U.S. Geological Survey ;\r\nBooks and Open-File Reports [distributor],","doi":"10.3133/ofr90190","usgsCitation":"Hileman, G.E., 1990, Water-quality, well-construction, and ground-water level data for an investigation of radionuclides in ground water, Hickman and Maury counties, Tennessee: U.S. Geological Survey Open-File Report 90-190, iv, 13 p. :ill. ;28 cm., https://doi.org/10.3133/ofr90190.","productDescription":"iv, 13 p. :ill. ;28 cm.","costCenters":[],"links":[{"id":1096,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/ofr_90-190","linkFileType":{"id":5,"text":"html"}},{"id":151784,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e6e4b07f02db5e7834","contributors":{"authors":[{"text":"Hileman, G. E.","contributorId":11639,"corporation":false,"usgs":true,"family":"Hileman","given":"G.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":180720,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":19426,"text":"ofr90149 - 1990 - The effects of the 1988 drought on water resources in Wisconsin","interactions":[],"lastModifiedDate":"2015-10-19T10:49:16","indexId":"ofr90149","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1990","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":"90-149","title":"The effects of the 1988 drought on water resources in Wisconsin","docAbstract":"The 1988 drought was one of the most severe droughts since weather records have been kept in Wisconsin. This fact sheet describes the cause of the drought and its effects on the water resources, water use, and agriculture in the State.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr90149","usgsCitation":"Holmstrom, B.K., and Ellefson, B., 1990, The effects of the 1988 drought on water resources in Wisconsin: U.S. Geological Survey Open-File Report 90-149, 2 p., https://doi.org/10.3133/ofr90149.","productDescription":"2 p.","numberOfPages":"2","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":677,"text":"Wisconsin Water Science Center","active":true,"usgs":true}],"links":[{"id":48899,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1990/0149/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":152638,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1990/0149/report-thumb.jpg"}],"country":"United 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\"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a9be4b07f02db65de01","contributors":{"authors":[{"text":"Holmstrom, B. K.","contributorId":90728,"corporation":false,"usgs":true,"family":"Holmstrom","given":"B.","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":180884,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Ellefson, B.R.","contributorId":83927,"corporation":false,"usgs":true,"family":"Ellefson","given":"B.R.","email":"","affiliations":[],"preferred":false,"id":180883,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":19440,"text":"ofr90357 - 1990 - Executive summary; assessing the response of Emerald Lake, an alpine watershed in Sequoia National Park, California, to acidification during snowmelt using a simple hydrochemical model","interactions":[],"lastModifiedDate":"2012-02-02T00:07:42","indexId":"ofr90357","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1990","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":"90-357","title":"Executive summary; assessing the response of Emerald Lake, an alpine watershed in Sequoia National Park, California, to acidification during snowmelt using a simple hydrochemical model","language":"ENGLISH","publisher":"U.S. Geological Survey ;\r\nBooks and Open-File Reports Section [distributor],","doi":"10.3133/ofr90357","usgsCitation":"Hooper, R.P., West, C., and Peters, N., 1990, Executive summary; assessing the response of Emerald Lake, an alpine watershed in Sequoia National Park, California, to acidification during snowmelt using a simple hydrochemical model: U.S. Geological Survey Open-File Report 90-357, 4 p. ;28 cm., https://doi.org/10.3133/ofr90357.","productDescription":"4 p. ;28 cm.","costCenters":[],"links":[{"id":153441,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1990/0357/report-thumb.jpg"},{"id":48913,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1990/0357/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a07e4b07f02db5f94b9","contributors":{"authors":[{"text":"Hooper, R. P.","contributorId":26321,"corporation":false,"usgs":true,"family":"Hooper","given":"R.","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":180906,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"West, C.T.","contributorId":104930,"corporation":false,"usgs":true,"family":"West","given":"C.T.","email":"","affiliations":[],"preferred":false,"id":180908,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Peters, N.E.","contributorId":33332,"corporation":false,"usgs":true,"family":"Peters","given":"N.E.","email":"","affiliations":[],"preferred":false,"id":180907,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":19464,"text":"ofr8952 - 1990 - Data on polychlorinated biphenyls, dieldrin, lead, and cadmium in Wisconsin and Upper Michigan tributaries to Green Bay, July 1987 through April 1988","interactions":[],"lastModifiedDate":"2015-10-08T13:06:26","indexId":"ofr8952","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1990","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":"89-52","title":"Data on polychlorinated biphenyls, dieldrin, lead, and cadmium in Wisconsin and Upper Michigan tributaries to Green Bay, July 1987 through April 1988","docAbstract":"A reconnaissance study was conducted of 22 streams tributary to Green Bay to determine whether any of the streams contribute toxic substances to the bay. This effort was part of a comprehensive investigation of Green Bay funded by the U.S. Environmental Protection Agency, Great Lakes National Program Office.
\nThe U.S. Geological Survey sampled the bottom sediments and water columns of 11 streams tributary to western Green Bay for polychlorinated biphenyls, lead, and cadmium. Four of these streams also were sampled for dieldrin, a pesticide previously used in the watershed. An additional 11 streams tributary to eastern Green Bay were sampled for dieldrin in the bottom sediment and storm runoff. Samples were collected from July 1987 through April 1988.
\nNeither dieldrin nor cadmium was detected in any of the sampled tributaries. Detectable concentrations of polychlorinated biphenyls and lead were found at only three sites. Polychorinated biphenyls (0.10 microgram per gram) and lead (10 milligrams per kilogram) were found in the bottom sediment of Duck Creek, a western-shore tributary near the city of Green Bay. Lead (10 milligrams per kilogram) also was found in the bottom sediment of the Suamico River near the mouth, about 5 miles north of Duck Creek. Lead (4 micrograms per liter) was detected in a spring-runoff sample from the Fishdam River, a tributary from upper Michigan.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr8952","collaboration":"Prepared in cooperation with the U.S. Environmental Protection Agency Great Lakes Program Office","usgsCitation":"House, L.B., 1990, Data on polychlorinated biphenyls, dieldrin, lead, and cadmium in Wisconsin and Upper Michigan tributaries to Green Bay, July 1987 through April 1988: U.S. Geological Survey Open-File Report 89-52, iv, 7 p., https://doi.org/10.3133/ofr8952.","productDescription":"iv, 7 p.","numberOfPages":"11","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":677,"text":"Wisconsin Water Science Center","active":true,"usgs":true}],"links":[{"id":151524,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1989/0052/report-thumb.jpg"},{"id":48939,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1989/0052/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Wisconsin","otherGeospatial":"Escanaba River, Fox River, Green Bay, Lake Michigan, Menominee River, Oconto River, Peshtigo River","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -87.154541015625,\n 46.21785176740299\n ],\n [\n -86.077880859375,\n 45.69850658738848\n ],\n [\n -87.33032226562499,\n 44.213709909702054\n ],\n [\n -88.209228515625,\n 44.457309801319305\n ],\n [\n -88.494873046875,\n 44.56699093657141\n ],\n [\n -88.714599609375,\n 44.69989765840318\n ],\n [\n -88.08837890625,\n 45.42158812329091\n ],\n [\n -87.659912109375,\n 45.805828539928356\n ],\n [\n -87.396240234375,\n 46.08847179577592\n ],\n [\n -87.34130859375,\n 46.22545288226939\n ],\n [\n -87.154541015625,\n 46.21785176740299\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac9e4b07f02db67c813","contributors":{"authors":[{"text":"House, L. B.","contributorId":49386,"corporation":false,"usgs":true,"family":"House","given":"L.","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":180957,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":19620,"text":"ofr90106 - 1990 - Ground-water levels in Wyoming, 1980 through September 1989","interactions":[],"lastModifiedDate":"2012-02-02T00:07:43","indexId":"ofr90106","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1990","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":"90-106","title":"Ground-water levels in Wyoming, 1980 through September 1989","docAbstract":"Groundwater levels are measured periodically in a network of 92 observation wells in Wyoming, mostly in areas where groundwater is used in large quantities for irrigation or municipal purposes. The program is conducted by the U.S. Geological Survey in cooperation with the Wyoming State Engineer. This report contains hydrographs for 92 observation wells showing water-level fluctuations from 1980 through September 1989. Also included in the report are maps showing locations of observation wells and tables listing well depths, use of water, geologic source, records available, and highest and lowest water levels for the period of record. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey ;\r\nBooks and Open-File Reports Section [distributor],","doi":"10.3133/ofr90106","usgsCitation":"Kennedy, H., and Green, S.L., 1990, Ground-water levels in Wyoming, 1980 through September 1989: U.S. Geological Survey Open-File Report 90-106, iv, 132 p. :ill. ;28 cm., https://doi.org/10.3133/ofr90106.","productDescription":"iv, 132 p. :ill. ;28 cm.","costCenters":[],"links":[{"id":153444,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1990/0106/report-thumb.jpg"},{"id":49095,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1990/0106/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b01e4b07f02db698572","contributors":{"authors":[{"text":"Kennedy, H.I.","contributorId":54214,"corporation":false,"usgs":true,"family":"Kennedy","given":"H.I.","email":"","affiliations":[],"preferred":false,"id":181225,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Green, S. L.","contributorId":83525,"corporation":false,"usgs":true,"family":"Green","given":"S.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":181226,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":19639,"text":"ofr88725 - 1990 - Ground-water resources of the Arkansas River basin in Arkansas","interactions":[],"lastModifiedDate":"2012-02-02T00:07:43","indexId":"ofr88725","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1990","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":"88-725","title":"Ground-water resources of the Arkansas River basin in Arkansas","docAbstract":"The Arkansas River basin in Arkansas lies almost entirely within the Interior Highlands physiographic division. The Interior Highlands consist of hilly to mountainous terrain underlain by sandstone, shale, limestone, and dolomite. That part of the basin southeast of Little Rock lies within the Gulf Coastal Plain and is characterized by flat to hilly topography. Significant water-yielding units within the Arkansas River basin include subsurface Paleozoic units such as the Eminence and Potosi Dolomites, the Gasconade Dolomite, and the Van Buren Formations, and Roubidoux Formation as well as outcrops of Paleozoic rocks, the Sparta Sand, and Quaternary deposits. The quality of groundwater withdrawn from the various aquifers in the study area is generally suitable for most uses, although commonly very hard and highly mineralized. Only the Sparta Sand yields a soft, less mineralized water. Yields from the different water-bearing units are highly variable. Several of the subsurface Paleozoic rocks rarely yield more than 10 gal/min. In the Coastal Plain, the Sparta Sand and the Quaternary deposits yield as much as 2,000 and 2,500 gal/min, respectively. Several studies have indicated substantial bacterial contamination of both wells and springs in this part of the study area. Also, nitrate concentrations that exceed U.S. Environmental Protection Agency primary drinking water standards occur in some areas. (USGS)","language":"ENGLISH","publisher":"Dept. of the Interior, U.S. Geological Survey ;\r\nBooks and Open-File Reports [distributor],","doi":"10.3133/ofr88725","usgsCitation":"Kilpatrick, J.M., and Ludwig, A.H., 1990, Ground-water resources of the Arkansas River basin in Arkansas: U.S. Geological Survey Open-File Report 88-725, iv, 45 p. :ill. ;28 cm., https://doi.org/10.3133/ofr88725.","productDescription":"iv, 45 p. :ill. ;28 cm.","costCenters":[],"links":[{"id":153325,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1988/0725/report-thumb.jpg"},{"id":49107,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1988/0725/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b23e4b07f02db6ae11b","contributors":{"authors":[{"text":"Kilpatrick, J. M.","contributorId":80706,"corporation":false,"usgs":true,"family":"Kilpatrick","given":"J.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":181254,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Ludwig, A. H.","contributorId":63007,"corporation":false,"usgs":true,"family":"Ludwig","given":"A.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":181253,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":19640,"text":"ofr88724 - 1990 - Ground-water resources of the upper White River basin in Arkansas","interactions":[],"lastModifiedDate":"2012-02-02T00:07:39","indexId":"ofr88724","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1990","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":"88-724","title":"Ground-water resources of the upper White River basin in Arkansas","docAbstract":"The upper White River basin in Arkansas lies almost entirely within the Ozark Plateaus physiographic province, which consists of deeply dissected plateaus underlain by limestone, shale, and dolomite. Significant water-yielding units within the upper White River basin include the Eminence and Potosi Dolomites, the Roubidou Formation, the Gasconade Dolomite and the Van Buren Formation, outcrops of undifferentiated Paleozoic rocks, the Nacatoch Sand, and quaternary deposits. Water in the Quaternary deposits is the most heavily used, but areally, other units are significant sources of groundwater for domestic and rural use. The quality of groundwater withdrawn from the various units generally is suitable for most uses, although groundwater in the study area is typically very hard. Iron concentrations commonly exceed allowable limits. Yields from the different water-yielding units are highly variable. The Eminence and Potosi Dolomites are known to yield as much as 230 gal/min. Nearer the surface, the Gunter Sandstone Member of the Van Buren Formation yields as much as 500 gal/min. Above the Gunter Sandstone, the Roubidoux Formation yields as much as 450 gal/min to wells. In contrast to the high yields from these deeper units , the outcrops of Paleozoic rocks commonly yield less than 10 gal/min. The Quaternary deposits yield as much as 2,500 gal/min of very hard water. Elevated nitrate concentrations that exceed U.S. Environmental Protection Agency primary drinking-water standards occur in Marion County. In addition, saline water is present in the Quaternary deposits near Bald Knob and Cord, Arkansas. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey ;\r\nU.S. Geological Survey, Books and Open-File Reports [distributor],","doi":"10.3133/ofr88724","usgsCitation":"Kilpatrick, J.M., and Ludwig, A.H., 1990, Ground-water resources of the upper White River basin in Arkansas: U.S. Geological Survey Open-File Report 88-724, v, 48 p. :ill. ;28 cm., https://doi.org/10.3133/ofr88724.","productDescription":"v, 48 p. :ill. ;28 cm.","costCenters":[],"links":[{"id":152110,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1988/0724/report-thumb.jpg"},{"id":49108,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1988/0724/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afce4b07f02db696a5e","contributors":{"authors":[{"text":"Kilpatrick, J. M.","contributorId":80706,"corporation":false,"usgs":true,"family":"Kilpatrick","given":"J.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":181256,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Ludwig, A. H.","contributorId":63007,"corporation":false,"usgs":true,"family":"Ludwig","given":"A.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":181255,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":19725,"text":"ofr88465 - 1990 - Geohydrologic data from test hole USW UZ-7, Yucca Mountain area, Nye County, Nevada","interactions":[],"lastModifiedDate":"2012-02-02T00:07:46","indexId":"ofr88465","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1990","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":"88-465","title":"Geohydrologic data from test hole USW UZ-7, Yucca Mountain area, Nye County, Nevada","docAbstract":"This report contains a description of the methods used in drilling and coring of the test-hole USW UZ-7, a description of the methods used in collecting, handling, and testing of test-hole samples; Lithologic information from the test hole; and water-content, water-potential, bulk-density, grain-density, porosity, and tritium data for the test hole. Test-hole USW UZ-7 was drilled and cored to a total depth of 62.94 m. The drilling was done using air as a drilling fluid to minimize disturbance to the water content of cores, drill-bit cuttings, and borehole wall-rock. Beginning at the land surface, the unsaturated-zone rock that was penetrated consisted of alluvium; welded and partially to nonwelded ash-flow tuff; bedded and reworked ash-fall tuff; nonwelded ash-flow tuff; and welded ash-flow tuff. Values of gravimetric water content and water potential of alluvium were intermediate between the extreme values in welded and nonwelded units of tuff. Gravimetric water content was largest in bedded and nonwelded ash-fall tuffs and was smallest in welded ash-flow tuff. Values of water potential were more negative in densely welded ash-flow tuffs and were less negative in bedded and nonwelded ash-fall tuffs. Bulk density was largest in densely welded ash-flow tuffs and smallest in nonwelded and bedded ash-fall tuffs. Grain density was uniform but was slightly larger in nonwelded and bedded ash-fall tuffs than in welded ash-flow tuffs. Porosity trends were opposite to bulk-density trends. Tritium content in alluvium was smallest near the alluvium-bedrock contact, markedly increased in the middle of the deposit, and decreased in the near-surface zone of the deposit. (Author 's abstract)","language":"ENGLISH","publisher":"U.S. Geological Survey ;\r\nBooks and Open-File Reports Sections [distributor],","doi":"10.3133/ofr88465","usgsCitation":"Kume, J., and Hammermeister, D., 1990, Geohydrologic data from test hole USW UZ-7, Yucca Mountain area, Nye County, Nevada: U.S. Geological Survey Open-File Report 88-465, v, 37 p. :ill., map ;28 cm., https://doi.org/10.3133/ofr88465.","productDescription":"v, 37 p. :ill., map ;28 cm.","costCenters":[],"links":[{"id":154075,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1988/0465/report-thumb.jpg"},{"id":49199,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1988/0465/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1be4b07f02db6a8cf0","contributors":{"authors":[{"text":"Kume, Jack","contributorId":100843,"corporation":false,"usgs":true,"family":"Kume","given":"Jack","email":"","affiliations":[],"preferred":false,"id":181400,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hammermeister, D.P.","contributorId":27066,"corporation":false,"usgs":true,"family":"Hammermeister","given":"D.P.","affiliations":[],"preferred":false,"id":181399,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":19726,"text":"ofr90187 - 1990 - A finite-element model for simulation of two-dimensional steady-state ground-water flow in confined aquifers","interactions":[],"lastModifiedDate":"2016-08-15T10:06:06","indexId":"ofr90187","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1990","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":"90-187","title":"A finite-element model for simulation of two-dimensional steady-state ground-water flow in confined aquifers","docAbstract":"A computer program based on the Galerkin finite-element method was developed to simulate two-dimensional steady-state ground-water flow in either isotropic or anisotropic confined aquifers. The program may also be used for unconfined aquifers of constant saturated thickness. Constant head, constant flux, and head-dependent flux boundary conditions can be specified in order to approximate a variety of natural conditions, such as a river or lake boundary, and pumping well. The computer program was developed for the preliminary simulation of ground-water flow in the Edwards-Trinity Regional aquifer system as part of the Regional Aquifer-Systems Analysis Program. Results of the program compare well to analytical solutions and simulations .from published finite-difference models. A concise discussion of the Galerkin method is presented along with a description of the program. Provided in the Supplemental Data section are a listing of the computer program, definitions of selected program variables, and several examples of data input and output used in verifying the accuracy of the program.
","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Austin, TX","doi":"10.3133/ofr90187","usgsCitation":"Kuniansky, E., 1990, A finite-element model for simulation of two-dimensional steady-state ground-water flow in confined aquifers: U.S. Geological Survey Open-File Report 90-187, iv, 77 p., https://doi.org/10.3133/ofr90187.","productDescription":"iv, 77 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"links":[{"id":49200,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1990/0187/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":154123,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1990/0187/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b24e4b07f02db6aeba3","contributors":{"authors":[{"text":"Kuniansky, E. L.","contributorId":82342,"corporation":false,"usgs":true,"family":"Kuniansky","given":"E. L.","affiliations":[],"preferred":false,"id":181401,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":19751,"text":"ofr90168 - 1990 - Water-quality data (October 1988 through September 1989) and statistical summaries (March 1985 through September 1989) for the Clark Fork and selected tributaries from Galen to Missoula, Montana","interactions":[],"lastModifiedDate":"2012-02-02T00:07:53","indexId":"ofr90168","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1990","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":"90-168","title":"Water-quality data (October 1988 through September 1989) and statistical summaries (March 1985 through September 1989) for the Clark Fork and selected tributaries from Galen to Missoula, Montana","docAbstract":"Water quality sampling was conducted at eight sites on the Clark Fork and selected tributaries from Galen to Missoula, from October 1988 through September 1989. This report presents tabulations and statistical summaries of the water quality data. Included are tabulations of streamflow, onsite water quality, and concentrations of trace elements and suspended sediment for periodic samples. Also included are tables and hydrographs of daily mean values for streamflow, suspended-sediment concentration, and suspended-sediment discharge at three mainstem stations and one tributary. Statistical summaries are presented for periodic water quality data collected from March 1985 through September 1989. Selected data are illustrated by graphs showing median concentrations of trace elements in water, relation of trace-element concentrations to suspended-sediment concentrations, and median concentrations of trace elements in suspended sediment. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey ;\r\nU.S. Geological Survey, Books and Open-File Reports [distributor],","doi":"10.3133/ofr90168","usgsCitation":"Lambing, J., 1990, Water-quality data (October 1988 through September 1989) and statistical summaries (March 1985 through September 1989) for the Clark Fork and selected tributaries from Galen to Missoula, Montana: U.S. Geological Survey Open-File Report 90-168, iv, 68 p. :ill. ;28 cm., https://doi.org/10.3133/ofr90168.","productDescription":"iv, 68 p. :ill. ;28 cm.","costCenters":[],"links":[{"id":154636,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1990/0168/report-thumb.jpg"},{"id":49223,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1990/0168/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e3e4b07f02db5e5a08","contributors":{"authors":[{"text":"Lambing, J. H.","contributorId":100860,"corporation":false,"usgs":true,"family":"Lambing","given":"J. H.","affiliations":[],"preferred":false,"id":181444,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ]}