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It was done&nbsp;in cooperation with the State of Iowa and with other agencies.</p>\n<p>This report is one of a series issued by Iowa. General&nbsp;direction for the series is by Philip Cohen, Jr., Chief&nbsp;Hydrologist, U. S. Geological Survey, and R. J. Dingman, Assistant&nbsp;Chief Hydrologist for Scientific Publications and Data Management.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Iowa City","doi":"10.3133/wdrIA811","collaboration":"Prepared in cooperation with the Iowa Geological Survey and with other State and Federal agencies","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1982, Water resources data Iowa, water year 1981: U.S. Geological Survey Water Data Report IA-81-1, x, 252 p., https://doi.org/10.3133/wdrIA811.","productDescription":"x, 252 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":351,"text":"Iowa Water Science 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,{"id":40899,"text":"ofr82562 - 1982 - Potentiometric-surface map of water in the Judith River Formation in the northern Great Plains area of Montana","interactions":[],"lastModifiedDate":"2022-09-27T20:57:58.601919","indexId":"ofr82562","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","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":"82-562","title":"Potentiometric-surface map of water in the Judith River Formation in the northern Great Plains area of Montana","docAbstract":"<p>The potentiometric surface of the Judith River Formation is mapped at a scale of 1:1,000,000. The map is one of a series produced as part of a regional study of aquifers of Cenozoic and Mesozoic age in the northern Great Plains of Montana. The contour interval is 200 feet. Water in the Judith River Formation occurs under water-table and artesian conditions. The direction of regional ground-water movement is from west to east. Water is discharged from the Judith River Formation to the Milk River from near Havre, Montana, to Malta and to the Missouri River south of the Bearpaw and Little Rocky Mountains. The average discharge from 236 wells is about 10 gallons per minute, and the specific capacity of 186 wells averages 0.66 gallon per minute per foot of drawdown.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr82562","usgsCitation":"Levings, G., 1982, Potentiometric-surface map of water in the Judith River Formation in the northern Great Plains area of Montana: U.S. Geological Survey Open-File Report 82-562, 1 Plate: 40.47 × 23.06 inches, https://doi.org/10.3133/ofr82562.","productDescription":"1 Plate: 40.47 × 23.06 inches","costCenters":[],"links":[{"id":407485,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_75640.htm","linkFileType":{"id":5,"text":"html"}},{"id":78781,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/0562/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":172091,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"country":"United States","state":"Montana","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -111,\n              45\n            ],\n            [\n              -104.0418,\n              45\n            ],\n            [\n              -104.0418,\n              49\n            ],\n            [\n              -111,\n              49\n            ],\n            [\n              -111,\n              45\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae4e4b07f02db68a2f5","contributors":{"authors":[{"text":"Levings, Gary W.","contributorId":106889,"corporation":false,"usgs":true,"family":"Levings","given":"Gary W.","affiliations":[],"preferred":false,"id":224137,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":57344,"text":"wdrNE811 - 1982 - Water resources data Nebraska, water year 1981","interactions":[],"lastModifiedDate":"2020-12-07T21:42:26.43236","indexId":"wdrNE811","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":340,"text":"Water Data Report","code":"WDR","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"NE-81-1","title":"Water resources data Nebraska, water year 1981","docAbstract":"<p>No abstract available.&nbsp;</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wdrNE811","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1982, Water resources data Nebraska, water year 1981: U.S. Geological Survey Water Data Report NE-81-1, viii, 471 p., https://doi.org/10.3133/wdrNE811.","productDescription":"viii, 471 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,{"id":2570,"text":"wsp2084 - 1982 - Source areas of salinity and trends of salt loads in streamflow in the upper Colorado River, Texas","interactions":[],"lastModifiedDate":"2016-08-05T11:51:02","indexId":"wsp2084","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":341,"text":"Water Supply Paper","code":"WSP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"2084","title":"Source areas of salinity and trends of salt loads in streamflow in the upper Colorado River, Texas","docAbstract":"<p>A series of seven studies of the quality and quantity of low flows in a 35.5-mile reach of the Colorado River upstream from Colorado City, Tex., were made from February 1975 to March 1978 to delineate areas of saline inflows. These studies showed generally that ground water contributed throughout the reach is saline but that loads of dissolved-constituents in ground-water accretions are highest in three subreaches. Yields per mile of river channel from these subreaches during the low-flow studies averaged more than 5.5 tons of dissolved solids per day, of which more than 1.8 tons were sodium and 2.9 tons were chloride.</p>\n<p>Salt-load trend studies for three long-term continuous streamflow and daily water-quality stations show that the salinity of the flow upstream from Ira, Tex., {mile 826.3) increased significantly after 1963 but decreased significantly after 1970. Part of the reach upstream from Ira is proximate to oil fields, the production and open-pit disposal of oilfield brines in the area increased significantly in the early 1960's, but a ban on open-pit disposal was enacted in 1969. No significantly downward trend in the salinity of flow at other daily water-quality stations downstream from Ira occurred after the ban on open-pit disposal of oil-field brines.</p>\n<p>The low-flow and salt-load trend studies indicate that part of the salinity in the flow of the Colorado River has resulted from the inflow of oil-field brine, but preponderant evidence indicates that the major part of the salinity is of natural origin. Neither the ban on open-pit disposal nor pumping of saline ground water has significantly reduced the salinity of flow downstream from Cuthbert, Tex. {mile 810.6).</p>\n<p>Diversion of saline low flows from the Colorado River at mile 799.3 upstream from Colorado City since January 1969 has resulted in significant improvement in the quality of water. Decreases in the discharge-weighted averages of dissolved solids and of chloride in the flow of the Colorado River at Colorado City (mile 796.3) during the 1969-78 water years were about 420 milligrams per liter and 280 milligrams per liter, respectfully.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wsp2084","usgsCitation":"Rawson, J., 1982, Source areas of salinity and trends of salt loads in streamflow in the upper Colorado River, Texas: U.S. Geological Survey Water Supply Paper 2084, v, 36 p., https://doi.org/10.3133/wsp2084.","productDescription":"v, 36 p.","numberOfPages":"44","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"links":[{"id":28840,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/2084/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":28841,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/2084/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":138591,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/2084/report-thumb.jpg"},{"id":28839,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/2084/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Texas","otherGeospatial":"Upper Colorado River","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a9be4b07f02db65e14c","contributors":{"authors":[{"text":"Rawson, Jack","contributorId":18345,"corporation":false,"usgs":true,"family":"Rawson","given":"Jack","affiliations":[],"preferred":false,"id":145418,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":56266,"text":"wdrPR79801 - 1982 - Water resources data for Puerto Rico, water years 1979-80","interactions":[],"lastModifiedDate":"2020-12-31T21:33:35.476061","indexId":"wdrPR79801","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","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":"PR-79-80-1","title":"Water resources data for Puerto Rico, water years 1979-80","docAbstract":"<p>No abstract available.&nbsp;</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wdrPR79801","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1982, Water resources data for Puerto Rico, water years 1979-80: U.S. Geological Survey Water Data Report PR-79-80-1, vi, 428 p., 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,{"id":47555,"text":"wdrAL811 - 1982 - Water resources data for Alabama, water year 1981","interactions":[],"lastModifiedDate":"2012-02-02T00:04:59","indexId":"wdrAL811","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","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":"AL-81-1","title":"Water resources data for Alabama, water year 1981","language":"ENGLISH","doi":"10.3133/wdrAL811","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1982, Water resources data for Alabama, water year 1981: U.S. Geological Survey Water Data Report AL-81-1, 552 p., https://doi.org/10.3133/wdrAL811.","productDescription":"552 p.","costCenters":[],"links":[{"id":135834,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49ffe4b07f02db5f7890","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":531756,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":13011,"text":"ofr821024 - 1982 - Guidelines and techniques for obtaining water samples that accurately represent the water chemistry of an aquifer","interactions":[],"lastModifiedDate":"2015-09-22T15:40:55","indexId":"ofr821024","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","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":"82-1024","title":"Guidelines and techniques for obtaining water samples that accurately represent the water chemistry of an aquifer","docAbstract":"<p>Obtaining ground-water samples that accurately represent the water chemistry of an aquifer is a complex task. Before a ground-water sampling program can be started, an understanding of the kind of chemical data needed and the potential changes in water chemistry resulting from various drilling, well-completion, and sampling techniques is needed. This report provides a basis for such an evaluation and permits a choice of techniques that will result in obtaining the best possible data for the time and money allocated.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Lakewood, CO","doi":"10.3133/ofr821024","usgsCitation":"Claassen, H.C., 1982, Guidelines and techniques for obtaining water samples that accurately represent the water chemistry of an aquifer: U.S. Geological Survey Open-File Report 82-1024, v, 49 p., https://doi.org/10.3133/ofr821024.","productDescription":"v, 49 p.","numberOfPages":"58","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":147145,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/1024/report-thumb.jpg"},{"id":41478,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/1024/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a82e4b07f02db64ae76","contributors":{"authors":[{"text":"Claassen, Hans C.","contributorId":25165,"corporation":false,"usgs":true,"family":"Claassen","given":"Hans","email":"","middleInitial":"C.","affiliations":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"preferred":false,"id":167132,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":26015,"text":"wri824016 - 1982 - Ground-water resources of the glacial outwash along the White River, Johnson and Morgan counties, Indiana","interactions":[],"lastModifiedDate":"2016-05-04T12:14:49","indexId":"wri824016","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","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":"82-4016","title":"Ground-water resources of the glacial outwash along the White River, Johnson and Morgan counties, Indiana","docAbstract":"<p>An 88-square-mile segment of the White River valley contains an unconfined sand and gravel aquifer ranging-from a featheredge zero, to 120 feet in saturated thickness. Hydraulic conductivity is 340 feet per day, and transmissivity is as much as 35,000 square feet per day. The aquifer, recharged primarily by precipitation, gains same recharge through interbedded till and outwash boundaries and through losing streams. A two-dimensional digital model was used to simulate the steady-state ground-water flow system. Sensitivity analyses tested the reaction of the model to adjustments in hydraulic conductivity, steam bed leakance, and recharge. Simulated pumpage of 20-, 66-, and 122-million gallons per day reduced streamflow by 5, 15, and 30% , respectively. A real drawdown did not exceed 25 feet. Ground water was a calcium bicarbonate type having a median pH of 7.1, a mean alkalinity of 240 milligrams per liter, a mean hardness of 280 milligrams per liter, a mean dissolved oxygen concentration of 2.2 milligrams per liter, a mean redox potential of +347 millivolts, and a mean dissolved-solids concentration of 366 milligrams per liter. Iron and manganese concentrations exceeded National Drinking Water Regulations in 15 and 49% of the analyses, respectively. Temperature and concentration of dissolved organic carbon varied seasonally. Dissolved carbon and manganese varied with seasonally. Dissolved carbon and manganese varied with differing boundary material, till and bedrock. (USGS)</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri824016","usgsCitation":"Bailey, Z., and Imbrigiotta, T., 1982, Ground-water resources of the glacial outwash along the White River, Johnson and Morgan counties, Indiana: U.S. Geological Survey Water-Resources Investigations Report 82-4016, vi, 89 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri824016.","productDescription":"vi, 89 p. :ill., maps ;28 cm.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":346,"text":"Indiana Water Science Center","active":true,"usgs":true}],"links":[{"id":54789,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1982/4016/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":123642,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1982/4016/report-thumb.jpg"}],"country":"United States","state":"Indiana","city":"Centerton, Indianapolis, Spencer","otherGeospatial":"White River Basin","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -86.87782287597656,\n              39.214167307512376\n            ],\n            [\n              -86.82701110839844,\n              39.19288388992811\n            ],\n            [\n              -86.73294067382812,\n              39.28223089949212\n            ],\n            [\n              -86.67526245117186,\n              39.322081212938706\n            ],\n            [\n              -86.64161682128906,\n              39.32155002466662\n            ],\n            [\n              -86.6443634033203,\n              39.34067026099156\n            ],\n            [\n              -86.53587341308594,\n              39.36668662525674\n            ],\n            [\n              -86.45484924316406,\n              39.40012200014591\n            ],\n            [\n              -86.44454956054688,\n              39.42452501272267\n            ],\n            [\n              -86.41365051269531,\n              39.48231543921616\n            ],\n            [\n              -86.32575988769531,\n              39.49291397824881\n            ],\n            [\n              -86.22207641601562,\n              39.6093912613121\n            ],\n            [\n              -86.22482299804688,\n              39.661213625756005\n            ],\n            [\n              -86.15409851074219,\n              39.75365697136308\n            ],\n            [\n              -86.20010375976561,\n              39.75893570672903\n            ],\n            [\n              -86.24679565429686,\n              39.658041943725856\n            ],\n            [\n              -86.24954223632812,\n              39.618912565294515\n            ],\n            [\n              -86.3580322265625,\n              39.51198727745152\n            ],\n            [\n              -86.4349365234375,\n              39.506689663850025\n            ],\n            [\n              -86.48918151855469,\n              39.40701936950632\n            ],\n            [\n              -86.65603637695312,\n              39.36084706023964\n            ],\n            [\n              -86.73019409179686,\n              39.34173234304089\n            ],\n            [\n              -86.87782287597656,\n              39.214167307512376\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afce4b07f02db696a47","contributors":{"authors":[{"text":"Bailey, Z. 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,{"id":27126,"text":"wri8221 - 1982 - Evaluation of the streamflow-data program in Pennsylvania","interactions":[],"lastModifiedDate":"2017-07-05T11:20:45","indexId":"wri8221","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","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":"82-21","title":"Evaluation of the streamflow-data program in Pennsylvania","docAbstract":"<p>The stream-gaging program in Pennsylvania is subject to budgetary&nbsp;constraints in the next several years. Elimination of those gaging stations&nbsp;that have no current-purpose use and little utility in providing regional&nbsp;flow-characteristic information is the most effective way to reduce costs.</p>\n<p>The efficient design of a network of gaging stations for obtaining regional information requires knowledge of the information in the data base and an assessment of the potential for improving the accuracy of data-transfer mechanisms. The analytical technique known as Network Analysis for Regional Information is used to assess acquired streamflow information and to evaluate its transferability within previously determined regions of homogenous streamflow characteristics. Regression equations that relate low-, mean-, and flood-flow characteristics to basin parameters are the data-transfer mechanisms used in the evaluation. This analysis showed that only minor improvements in the regression equations can be expected after 20 additional years of data collection at gages in the 1980 program. Transfer mechanisms with less model error are needed for improved data transferability.</p>\n<p>A more efficient program can be achieved by discontinuing selected gages in the planning-and-design network. To this end, 11 continuous-record and 25 partial-record gages were selected to be discontinued by April 1, 1980. Additionally, 6 continuous-record and 29 partial-record gages are suggested to be discontinued at the end of the 1985 water year.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri8221","collaboration":"Prepared in cooperation with the Pennsylvania Department of Environmental Resources","usgsCitation":"Flippo, H.N., 1982, Evaluation of the streamflow-data program in Pennsylvania: U.S. Geological Survey Water-Resources Investigations Report 82-21, Report: iv, 56 p.; Plate: 21.03 x 13.87 inches, https://doi.org/10.3133/wri8221.","productDescription":"Report: iv, 56 p.; Plate: 21.03 x 13.87 inches","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":532,"text":"Pennsylvania Water Science 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,{"id":43120,"text":"ofr822 - 1982 - Land use and land cover and associated maps for Pocatello, Idaho","interactions":[],"lastModifiedDate":"2012-02-02T00:05:01","indexId":"ofr822","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","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":"82-2","title":"Land use and land cover and associated maps for Pocatello, Idaho","language":"ENGLISH","doi":"10.3133/ofr822","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1982, Land use and land cover and associated maps for Pocatello, Idaho: U.S. Geological Survey Open-File Report 82-2, maps ;44 x 66 cm., https://doi.org/10.3133/ofr822.","productDescription":"maps ;44 x 66 cm.","costCenters":[],"links":[{"id":135561,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b27e4b07f02db6b0653","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":530972,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":4657,"text":"twri03A9_1982 - 1982 - Measurement of time of travel and dispersion in streams by dye tracing","interactions":[],"lastModifiedDate":"2012-02-02T00:05:38","indexId":"twri03A9_1982","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":336,"text":"Techniques of Water-Resources Investigations","code":"TWRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"03-A9","title":"Measurement of time of travel and dispersion in streams by dye tracing","docAbstract":"The use of fluorescent dyes and tracing techniques provides\r\na means for measuring the time-of-travel and dispersion\r\ncharacteristics of steady and gradually varied flow in\r\nstreams. Measurements of the dispersion and concentration\r\nof dyes give insight into the behavior of soluble contaminants\r\nthat may be introduced into a stream.\r\nThis manual describes methods of measuring time of\r\ntravel of water and waterborne solutes by dye tracing. The\r\nfluorescent dyes, measuring equipment used, and the field\r\nand laboratory procedures are also described.\r\nMethods of analysis and presentation to illustrate time-oftravel\r\nand dispersion characteristics of streams are provided.","language":"ENGLISH","publisher":"U.S. G.P.O.,","doi":"10.3133/twri03A9_1982","usgsCitation":"Hubbard, E., Kilpatrick, F.A., Martens, L., and Wilson, J.F., 1982, Measurement of time of travel and dispersion in streams by dye tracing (1982): U.S. Geological Survey Techniques of Water-Resources Investigations 03-A9, ix, 44 p. :ill., maps ;26 cm., https://doi.org/10.3133/twri03A9_1982.","productDescription":"ix, 44 p. :ill., maps ;26 cm.","costCenters":[],"links":[{"id":139327,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":156,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/twri/twri3-a9/pdf/twri_3-a9_ver1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"edition":"1982","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a28e4b07f02db611238","contributors":{"authors":[{"text":"Hubbard, E. F.","contributorId":66666,"corporation":false,"usgs":true,"family":"Hubbard","given":"E. F.","affiliations":[],"preferred":false,"id":149567,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Kilpatrick, F. A.","contributorId":22319,"corporation":false,"usgs":true,"family":"Kilpatrick","given":"F.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":149565,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Martens, L.A.","contributorId":52166,"corporation":false,"usgs":true,"family":"Martens","given":"L.A.","email":"","affiliations":[],"preferred":false,"id":149566,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Wilson, J. F. Jr.","contributorId":99541,"corporation":false,"usgs":true,"family":"Wilson","given":"J.","suffix":"Jr.","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":149568,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":25682,"text":"wri824095 - 1982 - A Numerical model to evaluate proposed ground-water allocations in southwest Kansas","interactions":[],"lastModifiedDate":"2012-02-02T00:08:10","indexId":"wri824095","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","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":"82-4095","title":"A Numerical model to evaluate proposed ground-water allocations in southwest Kansas","docAbstract":"A computer model was developed to assist the Southwest Kansas Groundwater Management District No. 3 in the evaluation of applications to appropriate ground water. The model calculated the drawdown due from a proposed well at all existing wells in the section of the proposed well and at all wells in the adjacent eight sections. The depletion expected in the 9-square-mile area due to all existing wells and the proposed well is computed and compared with allowable limits defined by the management district. An optional program permits the evaluation of allowable depletion for one or more townships. All options are designed to run interactively, thus allowing for immediate evaluation of proposed ground-water withdrawals. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri824095","usgsCitation":"Jorgensen, D.G., Grubb, H.F., Baker, C., Hilmes, G., and Jenkins, E.D., 1982, A Numerical model to evaluate proposed ground-water allocations in southwest Kansas: U.S. Geological Survey Water-Resources Investigations Report 82-4095, 46 p. :ill., map ;28 cm., https://doi.org/10.3133/wri824095.","productDescription":"46 p. :ill., map ;28 cm.","costCenters":[],"links":[{"id":118717,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1982/4095/report-thumb.jpg"},{"id":54445,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1982/4095/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53cd495fe4b0b290850ef1c1","contributors":{"authors":[{"text":"Jorgensen, D. G.","contributorId":104527,"corporation":false,"usgs":true,"family":"Jorgensen","given":"D.","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":194642,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Grubb, H. F.","contributorId":16863,"corporation":false,"usgs":true,"family":"Grubb","given":"H.","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":194640,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Baker, C.H.","contributorId":8504,"corporation":false,"usgs":true,"family":"Baker","given":"C.H.","affiliations":[],"preferred":false,"id":194638,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Hilmes, G.E.","contributorId":34545,"corporation":false,"usgs":true,"family":"Hilmes","given":"G.E.","email":"","affiliations":[],"preferred":false,"id":194641,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Jenkins, E. D.","contributorId":9250,"corporation":false,"usgs":true,"family":"Jenkins","given":"E.","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":194639,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":27677,"text":"wri8175 - 1982 - Results of deep-well injection testing at Mulberry, Florida","interactions":[],"lastModifiedDate":"2012-02-02T00:08:42","indexId":"wri8175","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","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":"81-75","title":"Results of deep-well injection testing at Mulberry, Florida","docAbstract":"At the Kaiser Aluminum and Chemical Corporation plant, Mulberry, Fla., high-chloride, acidic liquid wastes are injected into a dolomite section at depths below about 4,000 feet below land surface. In 1975, a satellite monitor well was drilled 2,291 feet from the injection well and a series of three injection tests were performed. Duration of the tests ranged from 240 to 10,020 minutes and injection rates ranged from 110 to 230 gallons per minute. Based on an evaluation of factors that affect hydraulic response, water-level data suitable for interpretation of hydraulic characteristics of the injection zone were identified to occur from 200 to 1,000 minutes during the 10,020-minute test. Transmissivity of the injection zone was computed to be within the range from 700 to 1,000 feet squared per day and storage coefficient of the injection zone was computed to be within the range from .00001 to .00005. The confining bed accepting most of the leakage appears to be the underlying bed. Also, it appears that the overlying beds are probably relatively impermeable and significantly retard the vertical movement of neutralized waste effluent. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey, Water Resources Division,","doi":"10.3133/wri8175","usgsCitation":"Hickey, J.J., and Wilson, W., 1982, Results of deep-well injection testing at Mulberry, Florida: U.S. Geological Survey Water-Resources Investigations Report 81-75, iv, 15 p. :ill., map ;28 cm., https://doi.org/10.3133/wri8175.","productDescription":"iv, 15 p. :ill., map ;28 cm.","costCenters":[],"links":[{"id":159041,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1981/0075/report-thumb.jpg"},{"id":56527,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1981/0075/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a19e4b07f02db605789","contributors":{"authors":[{"text":"Hickey, John J.","contributorId":39763,"corporation":false,"usgs":true,"family":"Hickey","given":"John","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":198517,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Wilson, W.E.","contributorId":100831,"corporation":false,"usgs":true,"family":"Wilson","given":"W.E.","email":"","affiliations":[],"preferred":false,"id":198518,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":4530,"text":"cir884 - 1982 - Annual report on Alaska's mineral resources","interactions":[],"lastModifiedDate":"2012-02-02T00:05:43","indexId":"cir884","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","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":"884","title":"Annual report on Alaska's mineral resources","language":"ENGLISH","publisher":"U.S. Dept. of the Interior, [Geological Survey,","doi":"10.3133/cir884","isbn":"0607887206 (pbk.)","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1982, Annual report on Alaska's mineral resources: U.S. Geological Survey Circular 884, v. 59 p. maps ;26 cm., https://doi.org/10.3133/cir884.","productDescription":"v. 59 p. maps ;26 cm.","costCenters":[],"links":[{"id":118454,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/circ/1982/0884/report-thumb.jpg"},{"id":31588,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/1982/0884/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac8e4b07f02db67b90d","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":528230,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":43952,"text":"ofr828 - 1982 - Land use and land cover and associatd maps for Danville, Illinois; Indiana","interactions":[],"lastModifiedDate":"2012-02-02T00:11:03","indexId":"ofr828","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","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":"82-8","title":"Land use and land cover and associatd maps for Danville, Illinois; Indiana","language":"ENGLISH","doi":"10.3133/ofr828","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1982, Land use and land cover and associatd maps for Danville, Illinois; Indiana: U.S. Geological Survey Open-File Report 82-8, maps ;45 x 69 cm., https://doi.org/10.3133/ofr828.","productDescription":"maps ;45 x 69 cm.","costCenters":[],"links":[{"id":167843,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b31e4b07f02db6b417f","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":531499,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":65397,"text":"i1427 - 1982 - Controlled photomosaic of the Amenthes Northwest Quadrangle of Mars","interactions":[],"lastModifiedDate":"2012-02-02T00:13:13","indexId":"i1427","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","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":"1427","subseriesTitle":"NONE","title":"Controlled photomosaic of the Amenthes Northwest Quadrangle of Mars","language":"ENGLISH","doi":"10.3133/i1427","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1982, Controlled photomosaic of the Amenthes Northwest Quadrangle of Mars: U.S. Geological Survey IMAP 1427, 1 photomosaic ;43 x 60 cm., on sheet 86 x 66 cm., folded in envelope 30 x 24 cm., https://doi.org/10.3133/i1427.","productDescription":"1 photomosaic ;43 x 60 cm., on sheet 86 x 66 cm., folded in envelope 30 x 24 cm.","costCenters":[],"links":[{"id":114903,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/imap/1427/report.pdf","size":"30","linkFileType":{"id":1,"text":"pdf"}},{"id":114904,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/imap/1427/plate-1.pdf","size":"7546","linkFileType":{"id":1,"text":"pdf"}},{"id":189046,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/imap/1427/report-thumb.jpg"}],"scale":"2000000","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae2e4b07f02db688ce6","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":533784,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":3209,"text":"wsp2185C - 1982 - Water quality of the French Broad River, North Carolina — An analysis of data collected at Marshall, 1958-1977","interactions":[],"lastModifiedDate":"2022-05-10T19:50:46.625055","indexId":"wsp2185C","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":341,"text":"Water Supply Paper","code":"WSP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"2185","chapter":"C","title":"Water quality of the French Broad River, North Carolina — An analysis of data collected at Marshall, 1958-1977","docAbstract":"An investigation of water quality in the French Broad River in North Carolina has resulted in the definition of variations in water quality, a determination of the degree to which the quality of water in the river has been affected by man 's activities, and an analysis of trends in the changing chemical quality of the river. The investigation centered on data collected during 1958-77 at the U.S. Geological Survey 's station at Marshall, N.C. The quality of water in the French Broad River at Marshall is suitable for most uses. None of the major dissolved constituents and nutrients, nor defined properties such as hardness, alkalinity and color, exceed suggested limits for drinking waters. Chromium, lead, selenium, and zinc are the only trace metals to occasionally exceed drinking water standards. Dissolved oxygen levels are high year round, remaining near or above the saturation level even at higher summer temperatures. Results of tests for biological oxygen demand and chemical oxygen demand characterize the French Broad at Marshall as a clean river. However, 58% of samples analyzed for fecal coliform bacteria during 1974-77 exceeded recommended limits for bathing waters. In 1958, an estimated 64% of the dissolved solids load in the river at Marshall was due to pollution. By 1966, 74% of the dissolved load could be attributed to pollution. Loads of dissolved solids, sodium, sulfate, and calcium showed the most dramatic increases, coinciding with general increases in population and industrial employment. New wastewater treatment facilities and improved industrial technology have apparently combined to curb pollution and reverse the earlier trend. In 1977 water quality had returned at least to levels of 1958.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wsp2185C","usgsCitation":"Daniel, C.C., Wilder, H.B., and Weiner, M.S., 1982, Water quality of the French Broad River, North Carolina — An analysis of data collected at Marshall, 1958-1977: U.S. Geological Survey Water Supply Paper 2185, iv, 28 p., https://doi.org/10.3133/wsp2185C.","productDescription":"iv, 28 p.","costCenters":[{"id":13634,"text":"South Atlantic Water Science Center","active":true,"usgs":true}],"links":[{"id":400460,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_25470.htm"},{"id":138136,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/2185a/report-thumb.jpg"},{"id":91273,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/2185a/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"North Carolina","city":"Marshall","otherGeospatial":"French Broad River","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -83,\n              36\n            ],\n            [\n              -82.25,\n              36\n            ],\n            [\n              -82.25,\n              35.067\n            ],\n            [\n              -83,\n              35.067\n            ],\n            [\n              -83,\n              36\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a07e4b07f02db5f9940","contributors":{"authors":[{"text":"Daniel, C. C. III","contributorId":71953,"corporation":false,"usgs":true,"family":"Daniel","given":"C.","suffix":"III","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":146437,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Wilder, Hugh B.","contributorId":83899,"corporation":false,"usgs":true,"family":"Wilder","given":"Hugh","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":146438,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Weiner, M. S.","contributorId":55806,"corporation":false,"usgs":true,"family":"Weiner","given":"M.","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":146436,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":3189,"text":"wsp2185D - 1982 - Water quality of the Neuse River, North Carolina - Variability, pollution loads, and long-term trends","interactions":[],"lastModifiedDate":"2017-02-01T10:01:53","indexId":"wsp2185D","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":341,"text":"Water Supply Paper","code":"WSP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"2185","chapter":"D","title":"Water quality of the Neuse River, North Carolina - Variability, pollution loads, and long-term trends","docAbstract":"Interpretation of water-quality data collected by the U.S. Geological Survey for the Neuse River, North Carolina, has identified water-quality variations, charactrized the current condition of the river in reference to water-quality standards, estimated the degree of pollution caused by man, and evaluated long-term trends in concentrations of major dissolved constituents. \r\n\r\nTwo sampling stations, Neuse River near Clayton (02087500) and Neuse River at Kinston (02089500) have more than 12 years of water-quality data collected during the period from 1955 to 1978. The Clayton station provides information on the upper fourth of the basin (1,129 mi 2) which includes several urbanized areas, including Raleigh, N.C., and part of Durham, N.C. The Kinston station provides information from the predominantly rural midsection of the basin (2,690 mi2). A network of temporary stations on small rural streams in the Neuse River and adjacent basins provide an estimate of baseline or es- sentially unpolluted water quality. \r\n\r\nOverall, the water quality of the Neuse River is satisfactory for most uses. However, dissolved-oxygen, iron, and manganese concentrations, pH, and bacterial concentrations often reach undesirable levels. Concentrations of cadmium, and lead also periodically peak at or above criterion levels for domestic water supply sources. Nutrient levels are generally high enough to allow rich algal growth. \r\n\r\nSediment concentrations in the Neuse are high in comparison to pristine streams, however, the impacts of these high levels are difficult to quantify. Sediment and nutrient concentrations peak on the leading edge of flood discharges at Clayton. At Kinston, however, the discharge and sediment concentration peak almost simultaneously. \r\n\r\nChanges in algal dominance, from genera usually associated with organically enriched waters to genera that are less tolerant to organic enrichment, indicate improvement in water qualiy of the Neuse since 1973. These changes, along with a reduction in total organic carbon concentrations, coincide with activation in 1976 of a new waste-water treatment plant for the Raleigh metropolitan area. \r\n\r\nThe amount of dissolved inorganic pollution in the Neuse was determined by subtacting estimated natural loads of dissolved constituents from measured total loads. Pollution makes up approximately 50 percent of the total dissolved material transported by the Neuse. \r\n\r\nTwo different data transformation methods allowed trends to be identified in constituent concentrations. Both methods recomputed concentrations as if they were determined at a constant discharge over the period of record. Although little change since 1956 can be seen in many constituents, increases of over 50 percent are shown for potassium and sulfate concentrations. These long-term rises indicate the increasing impact that man has had on the Neuse River, in spite of improved waste-water treatment in the basin. The increase in sulfate is probably largely due to increased long-term imputs of sulfur compounds from acid precipitation.","language":"ENGLISH","publisher":"U.S. G.P.O.,","doi":"10.3133/wsp2185D","usgsCitation":"Harned, D.A., 1982, Water quality of the Neuse River, North Carolina - Variability, pollution loads, and long-term trends: U.S. Geological Survey Water Supply Paper 2185, 1 v. (various pagings) : ill., maps ; 28 cm. ;44 p., https://doi.org/10.3133/wsp2185D.","productDescription":"1 v. 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,{"id":3187,"text":"wsp2185A - 1982 - Program for evaluating stream quality in North Carolina","interactions":[],"lastModifiedDate":"2017-02-01T09:59:04","indexId":"wsp2185A","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":341,"text":"Water Supply Paper","code":"WSP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"2185","chapter":"A","title":"Program for evaluating stream quality in North Carolina","docAbstract":"The design and objectives of the program for evaluating stream quality in North Carolina are described. Using water-quality and streamflow data collected since the 1940?s, a study is underway to define certain variations in water quality, to quantify the effects of man?s activities on water quality, and to determine long-term trends at key locations on the State?s major rivers. Data collected from 47 unpolluted stream sites were used to estimate average concentrations for naturally occurring constituents during periods of high and low flow. Methods are described for estimating constituent loads derived from both natural sources and sources of pollution.","language":"ENGLISH","publisher":"U.S. G.P.O.,","doi":"10.3133/wsp2185A","usgsCitation":"Wilder, H.B., and Simmons, C.E., 1982, Program for evaluating stream quality in North Carolina: U.S. Geological Survey Water Supply Paper 2185, 1 v. (various pagings) : ill., maps ; 28 cm. ;15 p., https://doi.org/10.3133/wsp2185A.","productDescription":"1 v. (various pagings) : ill., maps ; 28 cm. ;15 p.","costCenters":[{"id":13634,"text":"South Atlantic Water Science Center","active":true,"usgs":true}],"links":[{"id":138301,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/2185a/report-thumb.jpg"},{"id":30171,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/2185a/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"North 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Carolina\",\"nation\":\"USA  \"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a9be4b07f02db65e106","contributors":{"authors":[{"text":"Wilder, Hugh B.","contributorId":83899,"corporation":false,"usgs":true,"family":"Wilder","given":"Hugh","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":146398,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Simmons, Clyde E.","contributorId":71528,"corporation":false,"usgs":true,"family":"Simmons","given":"Clyde","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":146397,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":27046,"text":"wri8249 - 1982 - Streamflow losses to Madison Group rocks in the Little Belt and Big Snowy Mountains, Montana","interactions":[],"lastModifiedDate":"2019-08-05T11:31:54","indexId":"wri8249","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","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":"82-49","title":"Streamflow losses to Madison Group rocks in the Little Belt and Big Snowy Mountains, Montana","docAbstract":"Four streams originating in the Little Belt and Big Snowy Mountains in central Montana were measured in 1975 to determine streamflow losses across outcrops of the Madison Group (Mississippian age). Based on streamflow data obtained for 39 months at two streamflow-gaging stations on the Middle Fork Judith River, the average daily loss was 9.1 cubic feet per second or about 6,600 acre-feet per year. Seepage measurements on other stream reaches indicated losses of 7.6 cubic feet per second on the south Fork Judith River, 9.2 cubic feet per second in Yogo Creek, as much as 64 cubic feet per second in Dry Wolf Creek, and about 60 cubic feet per second in Rock Creek. (USGS)","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wri8249","usgsCitation":"Feltis, R., and Shields, R.R., 1982, Streamflow losses to Madison Group rocks in the Little Belt and Big Snowy Mountains, Montana: U.S. Geological Survey Water-Resources Investigations Report 82-49, 16 p. , https://doi.org/10.3133/wri8249.","productDescription":"16 p. ","costCenters":[],"links":[{"id":158971,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1982/0049/report-thumb.jpg"},{"id":366250,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1982/0049/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Montana","otherGeospatial":"Big Snowy Mountains, Little Belt Mountains","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -109.7314453125,\n              46.619261036171515\n            ],\n            [\n              -108.797607421875,\n              46.619261036171515\n            ],\n            [\n              -108.797607421875,\n              46.98774725646568\n            ],\n            [\n              -109.7314453125,\n              46.98774725646568\n            ],\n            [\n              -109.7314453125,\n              46.619261036171515\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b15e4b07f02db6a4d9c","contributors":{"authors":[{"text":"Feltis, R.D.","contributorId":93467,"corporation":false,"usgs":true,"family":"Feltis","given":"R.D.","affiliations":[],"preferred":false,"id":197465,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Shields, Ronald R.","contributorId":64655,"corporation":false,"usgs":true,"family":"Shields","given":"Ronald","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":197464,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":57263,"text":"wdrID811 - 1982 - Water Resources Data, Idaho, Water Year 1981--Volume 1. Great Basin and Snake River Basin above King Hill","interactions":[],"lastModifiedDate":"2012-02-02T00:12:22","indexId":"wdrID811","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","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":"ID-81-1","title":"Water Resources Data, Idaho, Water Year 1981--Volume 1. Great Basin and Snake River Basin above King Hill","language":"ENGLISH","doi":"10.3133/wdrID811","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1982, Water Resources Data, Idaho, Water Year 1981--Volume 1. Great Basin and Snake River Basin above King Hill: U.S. Geological Survey Water Data Report ID-81-1, 447 p., 12 Fig., https://doi.org/10.3133/wdrID811.","productDescription":"447 p., 12 Fig.","costCenters":[],"links":[{"id":183482,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0ae4b07f02db5fba0e","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":533050,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":36685,"text":"fwsobs80_40_13 - 1982 - Liming of acidified waters: a review of methods and effects on aquatic ecosystems","interactions":[],"lastModifiedDate":"2012-02-02T00:10:03","indexId":"fwsobs80_40_13","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":1,"text":"Federal Government Series"},"seriesTitle":{"id":20,"text":"FWS/OBS","active":false,"publicationSubtype":{"id":1}},"seriesNumber":"80/40.13","title":"Liming of acidified waters: a review of methods and effects on aquatic ecosystems","language":"ENGLISH","publisher":"U.S. Fish and Wildlife Service","usgsCitation":"Fraser, J.E., and Britt, D.L., 1982, Liming of acidified waters: a review of methods and effects on aquatic ecosystems: FWS/OBS 80/40.13, xv, 189 p. : ill., maps; 28 cm.","productDescription":"xv, 189 p. : ill., maps; 28 cm.","costCenters":[],"links":[{"id":161745,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b16e4b07f02db6a5289","contributors":{"authors":[{"text":"Fraser, James E.","contributorId":92310,"corporation":false,"usgs":true,"family":"Fraser","given":"James","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":216788,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Britt, Douglas L.","contributorId":16056,"corporation":false,"usgs":true,"family":"Britt","given":"Douglas","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":216787,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":5853,"text":"pp1237 - 1982 - Geochemistry of some rocks, mine spoils, stream sediments, soils, plants, and waters in the Western Energy Region of the conterminous United States, with sections on field studies","interactions":[],"lastModifiedDate":"2012-02-02T00:05:52","indexId":"pp1237","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","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":"1237","title":"Geochemistry of some rocks, mine spoils, stream sediments, soils, plants, and waters in the Western Energy Region of the conterminous United States, with sections on field studies","language":"ENGLISH","publisher":"U.S. G.P.O.,","doi":"10.3133/pp1237","usgsCitation":"Ebens, R.J., and Shacklette, H.T., 1982, Geochemistry of some rocks, mine spoils, stream sediments, soils, plants, and waters in the Western Energy Region of the conterminous United States, with sections on field studies: U.S. Geological Survey Professional Paper 1237, 173 p., https://doi.org/10.3133/pp1237.","productDescription":"173 p.","costCenters":[],"links":[{"id":121433,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/1237/report-thumb.jpg"},{"id":32641,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/1237/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1ee4b07f02db6aa6ba","contributors":{"authors":[{"text":"Ebens, Richard J.","contributorId":22335,"corporation":false,"usgs":true,"family":"Ebens","given":"Richard","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":151684,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Shacklette, Hansford T.","contributorId":43339,"corporation":false,"usgs":true,"family":"Shacklette","given":"Hansford","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":151685,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":7235,"text":"ofr81809 - 1982 - Hydrology of area 15, Eastern Coal province, Kentucky and Tennessee","interactions":[],"lastModifiedDate":"2012-02-02T00:05:50","indexId":"ofr81809","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","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":"81-809","title":"Hydrology of area 15, Eastern Coal province, Kentucky and Tennessee","docAbstract":"Area 15, in Eastern Kentucky and Tennessee consists of 3,095 square miles in the Cumberland, Rockcastle and Laurel River basins. The area is underlain by Permian, Pennsylvanian, Mississippian rocks. The Breathitt Formation of Pennsylvanian age crops out in about 75% of the area and contains most of the coal. About 22 million tons of coal were produced in the area in 1978, 52% from surface mines. The terrain is steep with acidic soils. Forestry and pastures are the principal land uses. Precipitation ranges from 47 to 54 inches per year, and the 24-hour 10-year frequency storm averages 4.5 inches. Flood prone areas along the rivers have been defined or can be determined from relations with drainage area and physiography. Low flows are poorly sustained, with most streams draining less than 100 square miles approaching a 7-day 10-year minimum flow of zero. Ground water is generally of good quality, although high iron concentrations are common. Sandstones are the principal aquifers. Water levels fluctuate seasonally, and yields of wells are usually less than 50 gallons per minute but range from about 1 to 250. Mine drainage affects the quality of streamflow at most sites in mined basins. Sulfate concentrations are as high as 1,000 milligrams per liter. Other constituents such as iron and manganese also occur in higher concentrations in waters of mined basins. Acid mine drainage generally is neutralized near its source. Most of the water in streams has pH values in the 7-8 range. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr81809","usgsCitation":"Leist, D.W., Quinones, F., Mull, D.S., and Young, M., 1982, Hydrology of area 15, Eastern Coal province, Kentucky and Tennessee: U.S. Geological Survey Open-File Report 81-809, v, 81 p. :ill., maps (some col.) ;28 cm., https://doi.org/10.3133/ofr81809.","productDescription":"v, 81 p. :ill., maps (some col.) ;28 cm.","costCenters":[],"links":[{"id":94753,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1981/0809/report.pdf","size":"27226","linkFileType":{"id":1,"text":"pdf"}},{"id":139835,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1981/0809/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a17e4b07f02db604250","contributors":{"authors":[{"text":"Leist, David W.","contributorId":77521,"corporation":false,"usgs":true,"family":"Leist","given":"David","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":154860,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Quinones, Ferdinand","contributorId":44138,"corporation":false,"usgs":true,"family":"Quinones","given":"Ferdinand","email":"","affiliations":[],"preferred":false,"id":154859,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Mull, D. S.","contributorId":43331,"corporation":false,"usgs":true,"family":"Mull","given":"D.","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":154858,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Young, Mary","contributorId":81898,"corporation":false,"usgs":true,"family":"Young","given":"Mary","affiliations":[],"preferred":false,"id":154861,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
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