{"pageNumber":"4127","pageRowStart":"103150","pageSize":"25","recordCount":166022,"records":[{"id":27810,"text":"wri894107 - 1989 - Estimating pumping time and ground-water withdrawals using energy- consumption data","interactions":[],"lastModifiedDate":"2012-02-02T00:08:43","indexId":"wri894107","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1989","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":"89-4107","title":"Estimating pumping time and ground-water withdrawals using energy- consumption data","docAbstract":"Evaluation of the hydrology of an aquifer requires knowledge about the volume of groundwater in storage and also about the volume of groundwater withdrawals. Totalizer flow meters may be installed at pumping plants to measure withdrawals; however, it generally is impractical to equip all pumping plants in an area with meters. A viable alternative is the use of rate-time methods. Rate-time methods may be used at individual pumping plants to decrease the data collection necessary for determining withdrawals. At sites where pumping-time measurement devices are not installed, pumping time may be determined on the basis of energy consumption and power demand. At pumping plants where energy consumption is metered, data acquired by reading of meters is used to estimate pumping time. Care needs to be taken to read these meters correctly. At pumping plants powered by electricity, the calculations need to be modified if transformers are present. At pumping plants powered by natural gas, the effects of the pressure-correction factor need to be included in the calculations. At pumping plants powered by gasoline, diesel oil, or liquid petroleum gas, the geometry of storage tanks needs to be analyzed as part of the calculations. The relation between power demand and pumping rate at a pumping plant can be described through the use of the power-consumption coefficient. Where equipment and hydrologic conditions are stable, this coefficient can be applied to total energy consumption at a site to estimate total groundwater withdrawals. Random sampling of power consumption coefficients can be used to estimate area-wide groundwater withdrawal. (USGS)","language":"ENGLISH","publisher":"Dept. of the Interior, U.S. Geological Survey :\r\nBooks and Open-File Reports Section [distributor],","doi":"10.3133/wri894107","usgsCitation":"Hurr, R., and Litke, D.W., 1989, Estimating pumping time and ground-water withdrawals using energy- consumption data: U.S. Geological Survey Water-Resources Investigations Report 89-4107, iv, 27 p. :ill. ;28 cm., https://doi.org/10.3133/wri894107.","productDescription":"iv, 27 p. :ill. ;28 cm.","costCenters":[],"links":[{"id":123160,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1989/4107/report-thumb.jpg"},{"id":56642,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1989/4107/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0ce4b07f02db5fc8c2","contributors":{"authors":[{"text":"Hurr, R. T.","contributorId":20713,"corporation":false,"usgs":true,"family":"Hurr","given":"R. T.","affiliations":[],"preferred":false,"id":198721,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Litke, D. W.","contributorId":94346,"corporation":false,"usgs":true,"family":"Litke","given":"D.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":198722,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":27909,"text":"wri884090 - 1989 - Test holes for monitoring surface-water/ground-water relations in the Cottonwood Creek area, Shasta and Tehama Counties, California, 1984-85","interactions":[],"lastModifiedDate":"2012-02-02T00:08:36","indexId":"wri884090","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1989","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":"88-4090","title":"Test holes for monitoring surface-water/ground-water relations in the Cottonwood Creek area, Shasta and Tehama Counties, California, 1984-85","docAbstract":"Ten test holes were drilled to obtain hydrogeologic information for an investigation of stream-aquifer interaction near proposed damsites on Cottonwood Creek and South Fork Cottonwood Creek, California. At each site, one deep well was completed below the first confining clay encountered in the upper Tehama Formation to determine hydraulic gradients between water-bearing deposits in the Tehama Formation and overlying channel deposits. At three sites along Cottonwood Creek, two shallow wells were drilled at each site on a line perpendicular to the stream channel to determine if groundwater in channel deposits is moving toward or away from the stream channel and to monitor water levels. Geophysical logs were correlated with lithologic logs compiled from analyses of drill cuttings to determine depths for setting well screens. After pumping to confirm hydraulic connection between each well and the Tehama Formation, water levels were monitored monthly from June 1984 to June 1985; at two sites, water levels were above the altitude of the stream channel bottom during all streamflow conditions. Tritium dating indicates two wells have water more than 100 years old; one well has either a mixture of old and new water or an intermediate-aged water. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri884090","usgsCitation":"Johnson, M.J., Houston, E., and Neil, J.M., 1989, Test holes for monitoring surface-water/ground-water relations in the Cottonwood Creek area, Shasta and Tehama Counties, California, 1984-85: U.S. Geological Survey Water-Resources Investigations Report 88-4090, iv, 28 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri884090.","productDescription":"iv, 28 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":158653,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1988/4090/report-thumb.jpg"},{"id":56727,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1988/4090/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b05e4b07f02db699d85","contributors":{"authors":[{"text":"Johnson, M. J.","contributorId":52988,"corporation":false,"usgs":true,"family":"Johnson","given":"M.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":198882,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Houston, E.R.","contributorId":67551,"corporation":false,"usgs":true,"family":"Houston","given":"E.R.","email":"","affiliations":[],"preferred":false,"id":198883,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Neil, J. M.","contributorId":27464,"corporation":false,"usgs":true,"family":"Neil","given":"J.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":198881,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":67108,"text":"i1803A - 1989 - Map showing exposures of limonitic rocks and hydrothermally altered rocks in the Dillon 1 degree by 2 degrees Quadrangle, Idaho and Montana","interactions":[],"lastModifiedDate":"2012-02-10T00:11:15","indexId":"i1803A","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1989","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":"1803","subseriesTitle":"NONE","chapter":"A","title":"Map showing exposures of limonitic rocks and hydrothermally altered rocks in the Dillon 1 degree by 2 degrees Quadrangle, Idaho and Montana","language":"ENGLISH","doi":"10.3133/i1803A","usgsCitation":"Segal, D.B., and Rowan, L.C., 1989, Map showing exposures of limonitic rocks and hydrothermally altered rocks in the Dillon 1 degree by 2 degrees Quadrangle, Idaho and Montana: U.S. Geological Survey IMAP 1803, 1 map :col. ;45 x 63 cm., on sheet 59 x 104 cm., folded in envelope 30 x 24 cm., https://doi.org/10.3133/i1803A.","productDescription":"1 map :col. ;45 x 63 cm., on sheet 59 x 104 cm., folded in envelope 30 x 24 cm.","costCenters":[],"links":[{"id":107132,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_9924.htm","linkFileType":{"id":5,"text":"html"},"description":"9924"},{"id":188041,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"scale":"250000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -114,45 ], [ -114,46 ], [ -112,46 ], [ -112,45 ], [ -114,45 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac9e4b07f02db67c869","contributors":{"authors":[{"text":"Segal, D. B.","contributorId":60236,"corporation":false,"usgs":true,"family":"Segal","given":"D.","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":275616,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Rowan, L. C.","contributorId":40584,"corporation":false,"usgs":true,"family":"Rowan","given":"L.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":275615,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":33327,"text":"b1542 - 1989 - Mineral resources of the Alpine Lakes Study Area and additions, Chelan, King, and Kittitas counties, Washington","interactions":[],"lastModifiedDate":"2012-02-02T00:09:17","indexId":"b1542","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1989","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":306,"text":"Bulletin","code":"B","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1542","title":"Mineral resources of the Alpine Lakes Study Area and additions, Chelan, King, and Kittitas counties, Washington","language":"ENGLISH","publisher":"U.S. G.P.O. ; For sale by the Books and Open-File Reports Section, U.S. Geological Survey,","doi":"10.3133/b1542","usgsCitation":"Water Resources Division, U.S. Geological Survey, and U.S. Bureau of Mines, 1989, Mineral resources of the Alpine Lakes Study Area and additions, Chelan, King, and Kittitas counties, Washington: U.S. Geological Survey Bulletin 1542, 1 portfolio (1 v., 2 maps) :ill., maps (some col.) ;24 cm., https://doi.org/10.3133/b1542.","productDescription":"1 portfolio (1 v., 2 maps) :ill., maps (some col.) ;24 cm.","costCenters":[],"links":[{"id":163718,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/bul/1542/report-thumb.jpg"},{"id":61153,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/1542/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":61154,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/1542/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":61155,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/bul/1542/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b08e4b07f02db69b3ec","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":529470,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"U.S. Bureau of Mines","contributorId":128223,"corporation":true,"usgs":false,"organization":"U.S. Bureau of Mines","id":529471,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":28392,"text":"wri894095 - 1989 - Peak-flow characteristics of small urban drainages along the Wasatch Front, Utah","interactions":[],"lastModifiedDate":"2012-02-02T00:08:49","indexId":"wri894095","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1989","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":"89-4095","title":"Peak-flow characteristics of small urban drainages along the Wasatch Front, Utah","docAbstract":"Designers and planners for local, State, and Federal agencies need up-to- date methods for determining peak-flow characteristics for urban drainages along the Wasatch Front, Utah. This report summarizes methods used to develop equations that estimate peak-flows for small urban drainages along the Wasatch Front. Mathematical equations were developed that estimate peak flows for recurrence intervals of 2, 5, 10, 25, 50 and 100 years, for small urban drainages. Data entry to the equations requires measurements of basin slope, size and percent impervious area. Rainfall and runoff data collected from eight urban drainages along the Wasatch Front from 1984-86, were used to calibrate a rainfall-runoff model called DR3M-II. Rainfall data collected from 1948-83 at the National Weather Service Salt Lake City Airport station provided additional long-term data to the calibrated models. Log Pearson fits made to the peak flow data were used to estimate the recurrence interval peaks for each basin. Paired stations on Little Cottonwood Creek near Salt Lake City were used to help determine the effects of intervening urban drainage on peaks of larger streams. In general, peaks on larger streams caused by snowmelt and peaks caused by rainfall (where urban areas may have a significant effect) did not occur simultaneously. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey ;\r\nBooks and Open-File Reports Section [distributor],","doi":"10.3133/wri894095","usgsCitation":"Lindskov, K., and Thompson, K.R., 1989, Peak-flow characteristics of small urban drainages along the Wasatch Front, Utah: U.S. Geological Survey Water-Resources Investigations Report 89-4095, v, 38 p. :ill. ;28 cm., https://doi.org/10.3133/wri894095.","productDescription":"v, 38 p. :ill. ;28 cm.","costCenters":[],"links":[{"id":123376,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1989/4095/report-thumb.jpg"},{"id":57191,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1989/4095/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae0e4b07f02db688575","contributors":{"authors":[{"text":"Lindskov, K.L.","contributorId":91077,"corporation":false,"usgs":true,"family":"Lindskov","given":"K.L.","affiliations":[],"preferred":false,"id":199720,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Thompson, K. R.","contributorId":92677,"corporation":false,"usgs":true,"family":"Thompson","given":"K.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":199721,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":4342,"text":"cir1026 - 1989 - Late Cenozoic history of the interior basins of Alaska and the Yukon","interactions":[],"lastModifiedDate":"2018-02-27T12:31:09","indexId":"cir1026","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1989","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":307,"text":"Circular","code":"CIR","onlineIssn":"2330-5703","printIssn":"1067-084X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"1026","title":"Late Cenozoic history of the interior basins of Alaska and the Yukon","language":"ENGLISH","publisher":"U.S. G.P.O. ;\r\nFree on application to the Books and Open-File Reports Section, U.S. Geological Survey,","doi":"10.3133/cir1026","usgsCitation":"1989, Late Cenozoic history of the interior basins of Alaska and the Yukon: U.S. Geological Survey Circular 1026, iv, 114 p. :ill., maps ;28 cm., https://doi.org/10.3133/cir1026.","productDescription":"iv, 114 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":31452,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/1989/1026/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":117337,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/circ/1989/1026/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1be4b07f02db6a8cb0","contributors":{"editors":[{"text":"Carter, L. David","contributorId":16827,"corporation":false,"usgs":true,"family":"Carter","given":"L.","email":"","middleInitial":"David","affiliations":[],"preferred":false,"id":729732,"contributorType":{"id":2,"text":"Editors"},"rank":1},{"text":"Hamilton, Thomas D.","contributorId":91474,"corporation":false,"usgs":true,"family":"Hamilton","given":"Thomas","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":729733,"contributorType":{"id":2,"text":"Editors"},"rank":2},{"text":"Galloway, John P. jgallway@usgs.gov","contributorId":3345,"corporation":false,"usgs":true,"family":"Galloway","given":"John","email":"jgallway@usgs.gov","middleInitial":"P.","affiliations":[],"preferred":true,"id":729734,"contributorType":{"id":2,"text":"Editors"},"rank":3}]}}
,{"id":4034,"text":"cir1024 - 1989 - California's unique geologic history and its role in mineral formation, with emphasis on the mineral resources of the California desert region","interactions":[],"lastModifiedDate":"2012-02-02T00:05:21","indexId":"cir1024","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1989","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":307,"text":"Circular","code":"CIR","onlineIssn":"2330-5703","printIssn":"1067-084X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"1024","title":"California's unique geologic history and its role in mineral formation, with emphasis on the mineral resources of the California desert region","language":"ENGLISH","publisher":"Dept. of the Interior, U.S. Geological Survey ;\r\nFor sale by the Books and Open-File Reports Section,","doi":"10.3133/cir1024","usgsCitation":"Dellinger, D.A., 1989, California's unique geologic history and its role in mineral formation, with emphasis on the mineral resources of the California desert region: U.S. Geological Survey Circular 1024, iii, 16 p. :ill., maps ;28 cm., https://doi.org/10.3133/cir1024.","productDescription":"iii, 16 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":117566,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/circ/1989/1024/report-thumb.jpg"},{"id":31127,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/1989/1024/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a06e4b07f02db5f8b9c","contributors":{"authors":[{"text":"Dellinger, D. A.","contributorId":6432,"corporation":false,"usgs":true,"family":"Dellinger","given":"D.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":148037,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":28438,"text":"wri884095 - 1989 - Withdrawals and consumptive use of water in Pennsylvania, 1984","interactions":[],"lastModifiedDate":"2022-12-02T22:36:58.350085","indexId":"wri884095","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1989","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":"88-4095","title":"Withdrawals and consumptive use of water in Pennsylvania, 1984","docAbstract":"Total accountable water withdrawals in Pennsylvania during 1984 were 14,033.66 Mga/d (million gallons per day); of that total, 5.2 percent (729.53 Mgal/d) was supplied from ground-water sources in 94.8 percent (13,302.12 Mgal/d) was supplied from surface-water sources. Thermoelectric power generation accounted for 71 percent of the total withdrawals (10,010.60 Mgal/d); this was followed by self-supplied industry, 15 percent (2,055.63 Mgal/d); public supply, 11 percent (1,600.02 Mgal/d); mining (147.73 Mgal/d), self- supplied domestic use (131.63 Mgal/d), livestock and poultry (83.52 Mgal/d) and irrigation (4.52 Mgal/d) collectively made up 3 percent. Total consumptive use of water was 615.22 Mgal/d; self-supplied industry is responsible for the greatest consumptive use--185.53 Mgal/d.\r\n\r\n      Trends in water withdrawals from 1950 to 1984 were examined for public supply, thermoelectric power generation and self-supplied industry. Total population and water withdrawals for public supply gradual increased in those years, whereas withdrawals for self-supplied industry and power generation increased until 1970 and then decreased.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri884095","usgsCitation":"Loper, C.A., Lent, S.D., and Wetzel, K.L., 1989, Withdrawals and consumptive use of water in Pennsylvania, 1984: U.S. Geological Survey Water-Resources Investigations Report 88-4095, iv, 50 p., https://doi.org/10.3133/wri884095.","productDescription":"iv, 50 p.","costCenters":[{"id":532,"text":"Pennsylvania Water Science Center","active":true,"usgs":true}],"links":[{"id":410028,"rank":2,"type":{"id":36,"text":"NGMDB Index 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,{"id":28711,"text":"wri894072 - 1989 - Tritium deposition in the continental United States, 1953-83","interactions":[],"lastModifiedDate":"2021-11-26T22:18:08.328543","indexId":"wri894072","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1989","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":"89-4072","title":"Tritium deposition in the continental United States, 1953-83","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri894072","usgsCitation":"Michel, R.L., 1989, Tritium deposition in the continental United States, 1953-83: U.S. Geological Survey Water-Resources Investigations Report 89-4072, iv, 46 p., https://doi.org/10.3133/wri894072.","productDescription":"iv, 46 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,{"id":27587,"text":"wri884234 - 1989 - Geohydrology of the alluvial and terrace deposits of the North Canadian River from Oklahoma City to Eufaula Lake, central Oklahoma","interactions":[],"lastModifiedDate":"2012-02-02T00:08:40","indexId":"wri884234","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1989","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":"88-4234","title":"Geohydrology of the alluvial and terrace deposits of the North Canadian River from Oklahoma City to Eufaula Lake, central Oklahoma","docAbstract":"This investigation was undertaken to describe the geohydrology of the alluvial and terrace deposits along the North Canadian River between Lake Overholser and Eufaula Lake, an area of about 1,835 square miles, and to determine the maximum annual yield of ground water.\r\nA 1982 water-level map of the alluvial and terrace aquifer was prepared using field data and published records. Data from test holes and other data from the files of the U.S. Geological Survey and the Oklahoma Water Resources Board were used to establish the approximate thickness of the alluvial and terrace deposits.\r\n\r\nThe North Canadian River from Lake Overholser, near Oklahoma City, to Eufaula Lake is paralleled by a 2- to 3-mile wide band of alluvium. Scattered terrace deposits on either side of the alluvium reach an extreme width of 8 miles. Rocks of Permian age bound the alluvial and terrace deposits from the west to the midpoint of the study area; Pennsylvanian rocks bound the alluvial and terrace deposits from that point eastward.\r\n\r\nThree major aquifers are present in the study area: the alluvial and terrace aquifer, consisting of alluvium and terrace deposits of Quaternary age in a narrow band on either side of the North Canadian River; the Garber-Wellington aquifer of Permian age, consisting of an upper unconfined zone and a lower confined zone separated by relatively impermeable shales; and the Ada-Vamoosa aquifer of Pennsylvanian age. At locations were the alluvial and terrace aquifer overlies either of the other aquifers, there is hydraulic continuity between the alluvial and terrace aquifer and the other aquifers, and water levels are the same.\r\n\r\nMost large-scale municipal and industrial pumping from the Garber-Wellington aquifer is from the lower zone and has little discernible effect upon the alluvial and terrace aquifer.\r\n\r\nThe total estimated base flow of the North Canadian River for the studied reach is 264 cubic feet per second. Evapotranspiration from the basin in August is about 60 cubic feet per second for the North Canadian River from Lake Overholser to a measuring station above Eufaula Lake. Estimated recharge rates to the alluvial and terrace aquifer in the basin range from 1.7 inches at the west edge of the study area to 7.0 inches at the east edge.\r\n\r\nTotal permitted withdrawal from the aquifer, according to records of the Oklahoma Water Resources Board, ranged from 2,107 acre-feet per year in 1942 to about 21,415 acre-feet per year in 1982.\r\n\r\nSimulations of the alluvial and terrace aquifer from Lake Overholser to Eufaula Lake were made using a finite-difference model developed by McDonald and Harbaugh (1984). The area of the aquifers was subdivided into a finite-difference grid having 30 rows and 57 columns with cells measuring 1 mile in the north-south direction and 2 miles in the east-west direction. The model was calibrated in two steps: A steady-state calibration simulated head distribution prior to extensive pumping of the aquifer in 1942, and a transient calibration simulated head distribution after extensive pumpage. The final horizontal hydraulic conductivity used for the alluvial and terrace aquifer was 0.0036 feet per second (310 feet per day) at all locations. The recharge rate for the alluvial and terrace aquifer ranged from 1.7 inch per year in the west to 7.0 inches per year in the east, and averaged about 3.3 inches per year. A specific yield of 15 percent was used for the transient simulation.\r\n\r\nPermitted pumpage for 1942 through 1982 was used in the digital model to estimate the annual volume of water in storage in the alluvial and terrace aquifer for the years for this time period. The 1982 permitted pumpage rates were used for projections for 1983 to 2020. The estimated volume of water in storage was 1,940,000 acre-feet in 1982. Because the estimated recharge rate is equal to the allowed pumpage rate in 1982, the projected volume of water in storage in both 1993 and 2020 was 1,890,000 acre-feet.","language":"ENGLISH","publisher":"U.S. Geological Survey ;\r\nBooks and Open-file reports, Federal Center,","doi":"10.3133/wri884234","usgsCitation":"Havens, J., 1989, Geohydrology of the alluvial and terrace deposits of the North Canadian River from Oklahoma City to Eufaula Lake, central Oklahoma: U.S. Geological Survey Water-Resources Investigations Report 88-4234, vii, 32 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri884234.","productDescription":"vii, 32 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":121808,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1988/4234/report-thumb.jpg"},{"id":56439,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1988/4234/plate-01.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":56440,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1988/4234/plate-02.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":56441,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1988/4234/plate-03.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":56442,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1988/4234/plate-04.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":56443,"rank":404,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1988/4234/plate-05.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":56444,"rank":405,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1988/4234/plate-06.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":56445,"rank":406,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1988/4234/plate-07.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":56446,"rank":407,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1988/4234/plate-08.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":56447,"rank":408,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1988/4234/plate-09.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":56448,"rank":409,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1988/4234/plate-10.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":56449,"rank":410,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1988/4234/plate-11.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":56450,"rank":411,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1988/4234/plate-12.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":56451,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1988/4234/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1ae4b07f02db6a8888","contributors":{"authors":[{"text":"Havens, J.S.","contributorId":12043,"corporation":false,"usgs":true,"family":"Havens","given":"J.S.","email":"","affiliations":[],"preferred":false,"id":198372,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":38453,"text":"pp1409E - 1989 - Ground-water hydrology and simulated effects of development in Smith Creek valley, a hydrologically closed basin in Lander County, Nevada","interactions":[],"lastModifiedDate":"2012-02-02T00:10:02","indexId":"pp1409E","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1989","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":331,"text":"Professional Paper","code":"PP","onlineIssn":"2330-7102","printIssn":"1044-9612","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"1409","chapter":"E","title":"Ground-water hydrology and simulated effects of development in Smith Creek valley, a hydrologically closed basin in Lander County, Nevada","language":"ENGLISH","doi":"10.3133/pp1409E","usgsCitation":"Thomas, J.M., Carlton, S., and Hines, L., 1989, Ground-water hydrology and simulated effects of development in Smith Creek valley, a hydrologically closed basin in Lander County, Nevada: U.S. Geological Survey Professional Paper 1409, p. E1-E57, 2 plates in pocket, https://doi.org/10.3133/pp1409E.","productDescription":"p. E1-E57, 2 plates in pocket","costCenters":[],"links":[{"id":104637,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_4862.htm","linkFileType":{"id":5,"text":"html"},"description":"4862"},{"id":122090,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/1409e/report-thumb.jpg"},{"id":64944,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/1409e/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":64945,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/1409e/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":64946,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/1409e/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aaae4b07f02db668d86","contributors":{"authors":[{"text":"Thomas, J. M.","contributorId":62217,"corporation":false,"usgs":true,"family":"Thomas","given":"J.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":219849,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Carlton, S.M.","contributorId":18036,"corporation":false,"usgs":true,"family":"Carlton","given":"S.M.","email":"","affiliations":[],"preferred":false,"id":219847,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Hines, L.B.","contributorId":49406,"corporation":false,"usgs":true,"family":"Hines","given":"L.B.","email":"","affiliations":[],"preferred":false,"id":219848,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":3626,"text":"cir1030 - 1989 - Water resources in the twenty-first century; a study of the implications of climate uncertainty","interactions":[{"subject":{"id":15090,"text":"ofr88472 - 1988 - Water resources in the twenty-first century; a study of the implications of climate uncertainty","indexId":"ofr88472","publicationYear":"1988","noYear":false,"title":"Water resources in the twenty-first century; a study of the implications of climate uncertainty"},"predicate":"SUPERSEDED_BY","object":{"id":3626,"text":"cir1030 - 1989 - Water resources in the twenty-first century; a study of the implications of climate uncertainty","indexId":"cir1030","publicationYear":"1989","noYear":false,"title":"Water resources in the twenty-first century; a study of the implications of climate uncertainty"},"id":1}],"lastModifiedDate":"2012-02-02T00:05:34","indexId":"cir1030","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1989","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":307,"text":"Circular","code":"CIR","onlineIssn":"2330-5703","printIssn":"1067-084X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"1030","title":"Water resources in the twenty-first century; a study of the implications of climate uncertainty","docAbstract":"The interactions of the water resources on and within the surface of the Earth with the atmosphere that surrounds it are exceedingly complex. Increased uncertainty can be attached to the availability of water of usable quality in the 21st century, therefore, because of potential anthropogenic changes in the global climate system. For the U.S. Geological Survey to continue to fulfill its mission with respect to assessing the Nation's water resources, an expanded program to study the hydrologic implications of climate uncertainty will be required. The goal for this program is to develop knowledge and information concerning the potential water-resources implications for the United States of uncertainties in climate that may result from both anthropogenic and natural changes of the Earth's atmosphere. Like most past and current water-resources programs of the Geological Survey, the climate-uncertainty program should be composed of three elements: (1) research, (2) data collection, and (3) interpretive studies. However, unlike most other programs, the climate-uncertainty program necessarily will be dominated by its research component during its early years. \r\n\r\nCritical new concerns to be addressed by the research component are (1) areal estimates of evapotranspiration, (2) hydrologic resolution within atmospheric (climatic) models at the global scale and at mesoscales, (3) linkages between hydrology and climatology, and (4) methodology for the design of data networks that will help to track the impacts of climate change on water resources. Other ongoing activities in U.S. Geological Survey research programs will be enhanced to make them more compatible with climate-uncertainty research needs. \r\n\r\nThe existing hydrologic data base of the Geological Survey serves as a key element in assessing hydrologic and climatologic change. However, this data base has evolved in response to other needs for hydrologic information and probably is not as sensitive to climate change as is desirable. Therefore, as measurement and network-design methodologies are improved to account for climate-change potential, new data-collection activities will be added to the existing programs. One particular area of data-collection concern pertains to the phenomenon of evapotranspiration. \r\n\r\nInterpretive studies of the hydrologic implications of climate uncertainty will be initiated by establishing several studies at the river-basin scale in diverse hydroclimatic and demographic settings. These studies will serve as tests of the existing methodologies for studying the impacts of climate change and also will help to define subsequent research priorities. A prototype for these studies was initiated in early 1988 in the Delaware River basin.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/cir1030","usgsCitation":"Moss, M.E., and Lins, H.F., 1989, Water resources in the twenty-first century; a study of the implications of climate uncertainty: U.S. Geological Survey Circular 1030, vi, 25 p. :ill., maps ;28 cm., https://doi.org/10.3133/cir1030.","productDescription":"vi, 25 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":124405,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/circ/1989/1030/report-thumb.jpg"},{"id":30669,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/1989/1030/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f4e4b07f02db5f0951","contributors":{"authors":[{"text":"Moss, Marshall E.","contributorId":6830,"corporation":false,"usgs":true,"family":"Moss","given":"Marshall","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":147282,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Lins, Harry F. 0000-0001-5385-9247 hlins@usgs.gov","orcid":"https://orcid.org/0000-0001-5385-9247","contributorId":1505,"corporation":false,"usgs":true,"family":"Lins","given":"Harry","email":"hlins@usgs.gov","middleInitial":"F.","affiliations":[{"id":502,"text":"Office of Surface Water","active":true,"usgs":true}],"preferred":true,"id":147281,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":13017,"text":"ofr89222 - 1989 - Multichannel seismic-reflection profiles collected in May 1981, between latitudes 40 degrees 40' and 45 degrees 00' north, offshore of Northern California and southern Oregon","interactions":[],"lastModifiedDate":"2012-02-02T00:06:51","indexId":"ofr89222","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1989","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":"89-222","title":"Multichannel seismic-reflection profiles collected in May 1981, between latitudes 40 degrees 40' and 45 degrees 00' north, offshore of Northern California and southern Oregon","language":"ENGLISH","publisher":"U.S. Dept. of the Interior, Geological Survey,","doi":"10.3133/ofr89222","usgsCitation":"Clarke, S.H., and McClellan, P., 1989, Multichannel seismic-reflection profiles collected in May 1981, between latitudes 40 degrees 40' and 45 degrees 00' north, offshore of Northern California and southern Oregon: U.S. Geological Survey Open-File Report 89-222, 4 p. :maps ;28 cm., https://doi.org/10.3133/ofr89222.","productDescription":"4 p. :maps ;28 cm.","costCenters":[],"links":[{"id":147170,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1989/0222/report-thumb.jpg"},{"id":41483,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1989/0222/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":41484,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1989/0222/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":41485,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1989/0222/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b02e4b07f02db698b3a","contributors":{"authors":[{"text":"Clarke, S. H. Jr.","contributorId":44913,"corporation":false,"usgs":true,"family":"Clarke","given":"S.","suffix":"Jr.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":167139,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"McClellan, P.H.","contributorId":62611,"corporation":false,"usgs":true,"family":"McClellan","given":"P.H.","email":"","affiliations":[],"preferred":false,"id":167140,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":15279,"text":"ofr89427 - 1989 - The Lakhra Anticline, an active feature of Pleistocene to recent age in southern Pakistan","interactions":[],"lastModifiedDate":"2012-02-02T00:06:46","indexId":"ofr89427","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1989","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":"89-427","title":"The Lakhra Anticline, an active feature of Pleistocene to recent age in southern Pakistan","language":"ENGLISH","publisher":"Geological Survey of Pakistan, U.S. Geological Survey,","doi":"10.3133/ofr89427","usgsCitation":"Outerbridge, W., and Kahn, R.A., 1989, The Lakhra Anticline, an active feature of Pleistocene to recent age in southern Pakistan: U.S. Geological Survey Open-File Report 89-427, 32, p. ill. ;28 cm., https://doi.org/10.3133/ofr89427.","productDescription":"32, p. ill. ;28 cm.","costCenters":[],"links":[{"id":146382,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1989/0427/report-thumb.jpg"},{"id":44208,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1989/0427/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac8e4b07f02db67c01d","contributors":{"authors":[{"text":"Outerbridge, William F.","contributorId":40181,"corporation":false,"usgs":true,"family":"Outerbridge","given":"William F.","affiliations":[],"preferred":false,"id":170874,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Kahn, Rafiq A.","contributorId":48190,"corporation":false,"usgs":true,"family":"Kahn","given":"Rafiq","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":170875,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":57330,"text":"wdrVA881 - 1989 - Water resources data for Virginia, water year 1988","interactions":[],"lastModifiedDate":"2020-11-25T17:50:15.380404","indexId":"wdrVA881","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1989","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":"VA-88-1","title":"Water resources data for Virginia, water year 1988","docAbstract":"<p>No abstract available.&nbsp;</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wdrVA881","usgsCitation":"Prugh, B., Easton, F., and Lynch, D.D., 1989, Water resources data for Virginia, water year 1988: U.S. Geological Survey Water Data Report VA-88-1, xiv, 447 p., https://doi.org/10.3133/wdrVA881.","productDescription":"xiv, 447 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D.","contributorId":12075,"corporation":false,"usgs":true,"family":"Lynch","given":"D.","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":256727,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":57336,"text":"wdrWV871 - 1989 - Water resources data for West Virginia, water year 1987","interactions":[],"lastModifiedDate":"2025-02-28T14:21:59.445889","indexId":"wdrWV871","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1989","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":"WV-87-1","title":"Water resources data for West Virginia, water year 1987","docAbstract":"<p>Water-resources data for the 1987 water year for West Virginia consist of records of stage, discharge, and water quality of streams; contents of reservoirs; and water levels of observation wells. This report contains discharge records for 83 streamflow-gaging stations; stage only records for 7 gaging stations, and 2 crest-stage partial-record stations; (2) contents for 1 reservoir, and change in contents for 1 reservoir; (3) water-quality records for 20 streamflow-gaging stations; and (4) water-level records for 34 observation wells. Locations of these sites are shown on figures 4 and 5. Additional water data were collected at various sites, not involved in the systematic data collection program, and are published as miscellaneous measurements. These data represent that part of the National Water Data System collected by the U.S. Geological Survey and cooperating State and Federal agencies in West Virginia. </p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wdrWV871","collaboration":"Prepared in cooperation with the State of West Virginia and with other agencies","usgsCitation":"Ward, S., Hobba, W., Taylor, F., and Ferrell, G., 1989, Water resources data for West Virginia, water year 1987: U.S. Geological Survey Water Data Report WV-87-1, viii, 228 p., https://doi.org/10.3133/wdrWV871.","productDescription":"viii, 228 p.","costCenters":[],"links":[{"id":184499,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wdr/1987/wv-87-1/report-thumb.jpg"},{"id":482591,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wdr/1987/wv-87-1/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"West 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,{"id":67354,"text":"i1896 - 1989 - Geologic map of the Sedona 30' x 60' Quadrangle, Yavapai and Coconino counties, Arizona","interactions":[{"subject":{"id":16479,"text":"ofr86164 - 1986 - Preliminary geologic map of the Sedona 30' by 60' Quadrangle, Yavapai and Coconino Counties, Arizona","indexId":"ofr86164","publicationYear":"1986","noYear":false,"title":"Preliminary geologic map of the Sedona 30' by 60' Quadrangle, Yavapai and Coconino Counties, Arizona"},"predicate":"SUPERSEDED_BY","object":{"id":67354,"text":"i1896 - 1989 - Geologic map of the Sedona 30' x 60' Quadrangle, Yavapai and Coconino counties, Arizona","indexId":"i1896","publicationYear":"1989","noYear":false,"title":"Geologic map of the Sedona 30' x 60' Quadrangle, Yavapai and Coconino counties, Arizona"},"id":1}],"lastModifiedDate":"2012-02-10T00:11:14","indexId":"i1896","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1989","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":"1896","subseriesTitle":"NONE","title":"Geologic map of the Sedona 30' x 60' Quadrangle, Yavapai and Coconino counties, Arizona","language":"ENGLISH","doi":"10.3133/i1896","usgsCitation":"Weir, G.W., Ulrich, G., and Nealey, L., 1989, Geologic map of the Sedona 30' x 60' Quadrangle, Yavapai and Coconino counties, Arizona: U.S. Geological Survey IMAP 1896, 1 map :col. ;56 x 92 cm., on sheet 89 x 137 cm., folded in envelope 30 x 24 cm., https://doi.org/10.3133/i1896.","productDescription":"1 map :col. ;56 x 92 cm., on sheet 89 x 137 cm., folded in envelope 30 x 24 cm.","costCenters":[],"links":[{"id":107169,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_9975.htm","linkFileType":{"id":5,"text":"html"},"description":"9975"},{"id":188542,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"scale":"100000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -112,34.5 ], [ -112,35 ], [ -111,35 ], [ -111,34.5 ], [ -112,34.5 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae6e4b07f02db68af91","contributors":{"authors":[{"text":"Weir, G. W.","contributorId":107290,"corporation":false,"usgs":true,"family":"Weir","given":"G.","middleInitial":"W.","affiliations":[],"preferred":false,"id":276044,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Ulrich, G. E.","contributorId":88737,"corporation":false,"usgs":true,"family":"Ulrich","given":"G. E.","affiliations":[],"preferred":false,"id":276042,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Nealey, L.D.","contributorId":97921,"corporation":false,"usgs":true,"family":"Nealey","given":"L.D.","email":"","affiliations":[],"preferred":false,"id":276043,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":19233,"text":"ofr89396 - 1989 - Well installation and documentation, and ground-water sampling protocols for the pilot National Water-Quality Assessment Program","interactions":[],"lastModifiedDate":"2012-02-02T00:07:28","indexId":"ofr89396","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1989","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":"89-396","title":"Well installation and documentation, and ground-water sampling protocols for the pilot National Water-Quality Assessment Program","docAbstract":"Several pilot projects are being conducted as part of the National Water Quality Assessment (NAWQA) Program. The purpose of the pilot program is to test and refine concepts for a proposed full-scale program. Three of the pilot projects are specifically designed to assess groundwater. The purpose of this report is to describe the criteria that are being used in the NAWQA pilot projects for selecting and documenting wells, installing new wells, and sampling wells for different water quality constituents. Guidelines are presented for the selection of wells for sampling. Information needed to accurately document each well includes site characteristics related to the location of the well, land use near the well, and important well construction features. These guidelines ensure the consistency of the information collected and will provide comparable data for interpretive purposes. Guidelines for the installation of wells are presented and include procedures that need to be followed for preparations prior to drilling, the selection of the drilling technique and casing type, the grouting procedure, and the well-development technique. A major component of the protocols is related to water quality sampling. Tasks are identified that need to be completed prior to visiting the site for sampling. Guidelines are presented for purging the well prior t sampling, both in terms of the volume of water pumped and the chemical stability of field parameters. Guidelines are presented concerning sampler selection as related to both inorganic and organic constituents. Documentation needed to describe the measurements and observations related to sampling each well and treating and preserving the samples are also presented. Procedures are presented for the storage and shipping of water samples, equipment cleaning, and quality assurance. Quality assurance guidelines include the description of the general distribution of the various quality assurance samples (blanks, spikes, duplicates, and reference samples) that will be used in the pilot program. (Lantz-PTT)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr89396","usgsCitation":"Hardy, M.A., Leahy, P., and Alley, W., 1989, Well installation and documentation, and ground-water sampling protocols for the pilot National Water-Quality Assessment Program: U.S. Geological Survey Open-File Report 89-396, iv, 36 p. :ill. ;28 cm., https://doi.org/10.3133/ofr89396.","productDescription":"iv, 36 p. :ill. ;28 cm.","costCenters":[],"links":[{"id":151990,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1989/0396/report-thumb.jpg"},{"id":48691,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1989/0396/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b01e4b07f02db69897d","contributors":{"authors":[{"text":"Hardy, M. A.","contributorId":54223,"corporation":false,"usgs":true,"family":"Hardy","given":"M.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":180532,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Leahy, P.P.","contributorId":104896,"corporation":false,"usgs":true,"family":"Leahy","given":"P.P.","email":"","affiliations":[],"preferred":false,"id":180533,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Alley, W.M.","contributorId":6853,"corporation":false,"usgs":true,"family":"Alley","given":"W.M.","email":"","affiliations":[],"preferred":false,"id":180531,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
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