{"pageNumber":"544","pageRowStart":"13575","pageSize":"25","recordCount":16500,"records":[{"id":70011198,"text":"70011198 - 1983 - Conjunctive use of groundwater and surface water for irrigated agriculture: Risk aversion","interactions":[],"lastModifiedDate":"2018-02-07T13:41:14","indexId":"70011198","displayToPublicDate":"1983-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3722,"text":"Water Resources Research","onlineIssn":"1944-7973","printIssn":"0043-1397","active":true,"publicationSubtype":{"id":10}},"title":"Conjunctive use of groundwater and surface water for irrigated agriculture: Risk aversion","docAbstract":"<p><span>In examining the South Platte system in Colorado where surface water and groundwater are used conjunctively for irrigation, we find the actual installed well capacity is approximately sufficient to irrigate the entire area. This would appear to be an overinvestment in well capacity. In this paper we examine to what extent groundwater is being developed as insurance against periods of low streamflow. Using a simulation model which couples the hydrology of a conjunctive stream aquifer system to a behavioral-economic model which incorporates farmer behavior in such a system, we have investigated the economics of an area patterned after a reach of the South Platte Valley in Colorado. The results suggest that under current economic conditions the most reasonable groundwater pumping capacity is a total capacity capable of irrigating the available acreage with groundwater. Installing sufficient well capacity to irrigate all available acreage has two benefits: (1) this capacity maximizes the expected net benefits and (2) this capacity also minimizes the variation in annual income: it reduces the variance to essentially zero. As pumping capacity is installed in a conjunctive use system, the value of flow forecasts is diminished. Poor forecasts are compensated for by pumping groundwater.</span></p>","language":"English","publisher":"American Geophysical Union","doi":"10.1029/WR019i005p01111","usgsCitation":"Bredehoeft, J.D., and Young, R.A., 1983, Conjunctive use of groundwater and surface water for irrigated agriculture: Risk aversion: Water Resources Research, v. 19, no. 5, p. 1111-1121, https://doi.org/10.1029/WR019i005p01111.","productDescription":"11 p.","startPage":"1111","endPage":"1121","costCenters":[],"links":[{"id":221576,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Colorado","otherGeospatial":"South Platte River","volume":"19","issue":"5","noUsgsAuthors":false,"publicationDate":"2010-07-09","publicationStatus":"PW","scienceBaseUri":"5059f9c7e4b0c8380cd4d794","contributors":{"authors":[{"text":"Bredehoeft, John D.","contributorId":86747,"corporation":false,"usgs":true,"family":"Bredehoeft","given":"John","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":360516,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Young, Richard A.","contributorId":38975,"corporation":false,"usgs":true,"family":"Young","given":"Richard","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":360517,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":38584,"text":"pp1277 - 1983 - Hydrologic and geomorphic studies of the Platte River basin","interactions":[{"subject":{"id":8117,"text":"ofr811116 - 1981 - Simulated hydrologic effects of possible ground-water and surface-water management alternatives in and near the Platte River, south-central Nebraska","indexId":"ofr811116","publicationYear":"1981","noYear":false,"title":"Simulated hydrologic effects of possible ground-water and surface-water management alternatives in and near the Platte River, south-central Nebraska"},"predicate":"SUPERSEDED_BY","object":{"id":38584,"text":"pp1277 - 1983 - Hydrologic and geomorphic studies of the Platte River basin","indexId":"pp1277","publicationYear":"1983","noYear":false,"title":"Hydrologic and geomorphic studies of the Platte River basin"},"id":1}],"lastModifiedDate":"2025-08-22T19:13:25.616513","indexId":"pp1277","displayToPublicDate":"1983-01-01T00:00:00","publicationYear":"1983","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":"1277","title":"Hydrologic and geomorphic studies of the Platte River basin","docAbstract":"The channels of the Platte River and its major tributaries, the South Platte and North Platte Rivers in Colorado, Wyoming, and Nebraska, have undergone major changes in hydrologic regime and morphology since about 1860, when the water resources of the basin began to be developed for agricultural, municipal, and industrial uses. These water uses have continued to increase with growth in population and land development. Diversion of flow from channels, storage of water in reservoirs, and increased use of ground water have affected the distribution and timing of streamflows and the transport of fluvial sediments. All these factors have contributed to changes in channel geometry and the riverine environment.\r\n\r\nIn 1979, the U.S. Geological Survey began investigations in the Platte River basin to determine the effects of water use on the hydrology and morphology of the Platte River and its major tributaries. These investigations also considered the relationship of hydrologic regime to factors that control or affect the habitat of migratory waterfowl in the Platte River valley.\r\n\r\nThis volume brings together the results of several research studies on historical changes in channel morphology, surface-water hydrology, hydraulic geometry, sediment-transport and bedform processes, ground-water and surface-water relations, stochastic models of streamflow and precipitation, and methods for estimating discharge required to maintain channel width. In each of the studies, data on some segment of the Platte River hydrologic system were collected and interpreted. All the studies are interrelated; together they provide some degree of understanding of regime changes that are occurring. The hydrologic research described in the following chapters will be useful in decision-making pertaining to the management of water resources and migratory waterfowl habitats.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/pp1277","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1983, Hydrologic and geomorphic studies of the Platte River basin: U.S. Geological Survey Professional Paper 1277, 297 p., https://doi.org/10.3133/pp1277.","productDescription":"297 p.","costCenters":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true},{"id":5050,"text":"WY-MT Water Science Center","active":true,"usgs":true}],"links":[{"id":120025,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/1277/report-thumb.jpg"},{"id":65397,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/1277/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":416915,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_74514.htm","text":"Hydrologic and morphologic changes in channels of the Platte River Basin in Colorado, Wyoming, and Nebraska: a historical perspective","linkFileType":{"id":5,"text":"html"}},{"id":494561,"rank":9,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_74520.htm","text":"Simulated hydrologic effects of possible ground-water and surface-water management alternatives in and near the Platte River, south-central Nebraska","linkFileType":{"id":5,"text":"html"}},{"id":494560,"rank":8,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_74519.htm","text":"A stochastic streamflow model and precipitation model for the Platte River from Gothenburg to Grand Island, Nebraska","linkFileType":{"id":5,"text":"html"}},{"id":494559,"rank":7,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_74518.htm","text":"Relation of channel-width maintenance to sediment transport and river morphology: Platte River, south-central Nebraska","linkFileType":{"id":5,"text":"html"}},{"id":494562,"rank":10,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_74521.htm","text":"Ground-water hydrology of the Mormon Island Crane Meadows Wildlife area near Grand Island, Hall County, Nebraska","linkFileType":{"id":5,"text":"html"}},{"id":494558,"rank":6,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_74517.htm","text":"Interpretation of sediment data for the South Platte River in Colorado and Nebraska, and the North Platte and Platte Rivers in Nebraska","linkFileType":{"id":5,"text":"html"}},{"id":494557,"rank":5,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_74516.htm","text":"Hydraulic geometry of the Platte River near Overton, south-central Nebraska","linkFileType":{"id":5,"text":"html"}},{"id":494556,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_74515.htm","text":"Effects of water development on surface-water hydrology, Platte River Basin in Colorado, Wyoming, and Nebraska upstream from Duncan Nebraska","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Colorado, Nebraska, Wyoming","otherGeospatial":"Platte River basin","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -105.06337546697512,\n              39.229893136534116\n            ],\n            [\n              -102.18895980010433,\n              40.144489715784374\n            ],\n            [\n              -100.8494900961135,\n              40.3909684886664\n            ],\n            [\n              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,{"id":70185619,"text":"70185619 - 1983 - Complexation of copper by aquatic humic substances from different environments","interactions":[],"lastModifiedDate":"2020-01-20T19:52:46","indexId":"70185619","displayToPublicDate":"1983-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3352,"text":"Science of the Total Environment","active":true,"publicationSubtype":{"id":10}},"title":"Complexation of copper by aquatic humic substances from different environments","docAbstract":"<p>The copper-complexing properties of aquatic humic substances isolated from eighteen different environments were characterized by potentiometric titration, using a cupric ion selective electrode. Potentiometric data were analyzed using FITEQL, a computer program for the determination of chemical equilibrium constants from experimental data. All the aquatic humic substances could be modelled as having two types of Cu(II)-binding sites: one with K equal to about 10<sup>6</sup> and a concentration of 1.0 ± 0.4 × 10<sup>−6</sup> M(mg C)<sup>−1</sup> and another with K equal to about 10<sup>8</sup> and a concentration of 2.6 ± 1.6 × 10<sup>−7</sup> M(mg C)<sup>−1</sup>.</p><p>A method is described for estimating the Cu(II)-binding sites associated with dissolved humic substances in natural water based on a measurement of dissolved organic carbon, which may be helpful in evaluating chemical processes controlling speciation of Cu and bioavailability of Cu to aquatic organisms.</p>","language":"English","publisher":"Elsevier","doi":"10.1016/S0048-9697(83)80008-4","usgsCitation":"McKnight, D.M., Feder, G., Thurman, E.M., and Wershaw, R.L., 1983, Complexation of copper by aquatic humic substances from different environments: Science of the Total Environment, v. 28, no. 1-3, p. 65-76, https://doi.org/10.1016/S0048-9697(83)80008-4.","productDescription":"12 p. ","startPage":"65","endPage":"76","costCenters":[{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":338320,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"28","issue":"1-3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"58d63040e4b05ec799131119","contributors":{"authors":[{"text":"McKnight, Diane M.","contributorId":59773,"corporation":false,"usgs":false,"family":"McKnight","given":"Diane","email":"","middleInitial":"M.","affiliations":[{"id":16833,"text":"INSTAAR, University of Colorado","active":true,"usgs":false}],"preferred":false,"id":686132,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Feder, Gerald L.","contributorId":60192,"corporation":false,"usgs":true,"family":"Feder","given":"Gerald L.","affiliations":[],"preferred":false,"id":686133,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Thurman, E. Michael","contributorId":9636,"corporation":false,"usgs":true,"family":"Thurman","given":"E.","email":"","middleInitial":"Michael","affiliations":[],"preferred":false,"id":686134,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Wershaw, Robert L. rwershaw@usgs.gov","contributorId":4856,"corporation":false,"usgs":true,"family":"Wershaw","given":"Robert","email":"rwershaw@usgs.gov","middleInitial":"L.","affiliations":[],"preferred":true,"id":686135,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70185617,"text":"70185617 - 1983 - Partition equilibriums of nonionic organic compounds between soil organic matter and water","interactions":[],"lastModifiedDate":"2020-01-20T19:51:56","indexId":"70185617","displayToPublicDate":"1983-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1565,"text":"Environmental Science & Technology","onlineIssn":"1520-5851","printIssn":"0013-936X","active":true,"publicationSubtype":{"id":10}},"title":"Partition equilibriums of nonionic organic compounds between soil organic matter and water","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"American Chemical Society","doi":"10.1021/es00110a009","usgsCitation":"Chiou, C.T., Porter, P.E., and Schmedding, D.W., 1983, Partition equilibriums of nonionic organic compounds between soil organic matter and water: Environmental Science & Technology, v. 17, no. 4, p. 227-231, https://doi.org/10.1021/es00110a009.","productDescription":"5 p. ","startPage":"227","endPage":"231","costCenters":[{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":338318,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"17","issue":"4","noUsgsAuthors":false,"publicationDate":"2002-05-01","publicationStatus":"PW","scienceBaseUri":"58d63041e4b05ec79913111d","contributors":{"authors":[{"text":"Chiou, Cary T. 0000-0002-8743-0702","orcid":"https://orcid.org/0000-0002-8743-0702","contributorId":189558,"corporation":false,"usgs":true,"family":"Chiou","given":"Cary","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":686128,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Porter, Paul E.","contributorId":189805,"corporation":false,"usgs":false,"family":"Porter","given":"Paul","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":686129,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Schmedding, David W.","contributorId":189818,"corporation":false,"usgs":false,"family":"Schmedding","given":"David","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":686130,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70185618,"text":"70185618 - 1983 - Bioavailability of trace metals to aquatic organisms — A review","interactions":[],"lastModifiedDate":"2020-01-26T09:44:09","indexId":"70185618","displayToPublicDate":"1983-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":5331,"text":"Science of Total Environment","active":true,"publicationSubtype":{"id":10}},"title":"Bioavailability of trace metals to aquatic organisms — A review","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"Elsevier","doi":"10.1016/S0048-9697(83)80004-7","usgsCitation":"Luoma, S.N., 1983, Bioavailability of trace metals to aquatic organisms — A review: Science of Total Environment, v. 28, no. 1-3, p. 1-22, https://doi.org/10.1016/S0048-9697(83)80004-7.","productDescription":"22 p. ","startPage":"1","endPage":"22","costCenters":[{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":338319,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"28","issue":"1-3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"58d63040e4b05ec79913111b","contributors":{"authors":[{"text":"Luoma, Samuel N. 0000-0001-5443-5091 snluoma@usgs.gov","orcid":"https://orcid.org/0000-0001-5443-5091","contributorId":2287,"corporation":false,"usgs":true,"family":"Luoma","given":"Samuel","email":"snluoma@usgs.gov","middleInitial":"N.","affiliations":[{"id":438,"text":"National Research Program - Western Branch","active":true,"usgs":true}],"preferred":true,"id":686131,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70174264,"text":"70174264 - 1982 - Enrichment and association of lead and bacteria at particulate surfaces in a salt-marsh surface layer","interactions":[],"lastModifiedDate":"2020-01-26T10:00:05","indexId":"70174264","displayToPublicDate":"2016-03-08T06:15:00","publicationYear":"1982","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2379,"text":"Journal of Marine Research","active":true,"publicationSubtype":{"id":10}},"title":"Enrichment and association of lead and bacteria at particulate surfaces in a salt-marsh surface layer","docAbstract":"<p><span>The particle-laden surface layer (approx 150-370 mu m) and subsurface waters of a South San Francisco Bay salt marsh were sampled over 2 tidal cycles and analyzed for particle numbers and particulate-associated and total concentrations of Pb and bacteria. Laboratory studies examined the ability of a bacterial isolate from the surface layer and a bacterial 'film-former' to sorb Pb at environmentally significant concentrations in seawater. Degrees by which Pb concentrated in the surface layer relative to the subsurface strongly correlated with enrichments of surface layer bacteria (bacterioneuston). A significant fraction of the bacterioneuston and surface layer Pb were associated with particles. Particle-bound bacterioneuston may interact with Pb at particulate surfaces in this microenvironment.</span></p>","language":"English","publisher":"Yale University","usgsCitation":"Harvey, R., Lion, L.W., Young, L., and Leckie, J., 1982, Enrichment and association of lead and bacteria at particulate surfaces in a salt-marsh surface layer: Journal of Marine Research, v. 40, no. 44, p. 1201-1211.","productDescription":"11 p.","startPage":"1201","endPage":"1211","numberOfPages":"11","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":552,"text":"San Francisco Bay-Delta","active":false,"usgs":true},{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true},{"id":5079,"text":"Pacific Regional Director's Office","active":true,"usgs":true}],"links":[{"id":324782,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":324781,"rank":1,"type":{"id":11,"text":"Document"},"url":"https://www.researchgate.net/publication/286952397_Enrichment_and_association_of_lead_and_bacteria_at_particulate_surfaces_in_a_salt-marsh_surface_layer_San_Francisco_Bay","text":"Enrichment and association of lead and bacteria at particulate surfaces in a salt-marsh surface-layer","description":"Enrichment and association of lead and bacteria at particulate surfaces in a salt-marsh surface-layer"}],"country":"United States","state":"California","county":"San Francisco","city":"San Francisco","otherGeospatial":"San Francisco Bay area","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -123.01940917968751,\n              37.23470197166817\n            ],\n            [\n              -123.01940917968751,\n              38.22307753495298\n            ],\n            [\n              -121.5472412109375,\n              38.22307753495298\n            ],\n            [\n              -121.5472412109375,\n              37.23470197166817\n            ],\n            [\n              -123.01940917968751,\n              37.23470197166817\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"40","issue":"44","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"577e2bade4b0ef4d2f4459dc","contributors":{"authors":[{"text":"Harvey, R.W. 0000-0002-2791-8503","orcid":"https://orcid.org/0000-0002-2791-8503","contributorId":11757,"corporation":false,"usgs":true,"family":"Harvey","given":"R.W.","affiliations":[],"preferred":false,"id":641650,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Lion, Leonard W.","contributorId":156349,"corporation":false,"usgs":false,"family":"Lion","given":"Leonard","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":641651,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Young, L.Y.","contributorId":76547,"corporation":false,"usgs":true,"family":"Young","given":"L.Y.","email":"","affiliations":[],"preferred":false,"id":641652,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Leckie, J.O.","contributorId":32692,"corporation":false,"usgs":true,"family":"Leckie","given":"J.O.","email":"","affiliations":[],"preferred":false,"id":641653,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70043399,"text":"70043399 - 1982 - Hydrology of the Beryl-Enterprise area, Escalante Desert, Utah, with emphasis on ground water; With a section on surface water","interactions":[{"subject":{"id":10426,"text":"ofr81533 - 1981 - Hydrology of the Beryl-Enterprise area, Escalante Desert, Utah, with emphasis on ground water","indexId":"ofr81533","publicationYear":"1981","noYear":false,"title":"Hydrology of the Beryl-Enterprise area, Escalante Desert, Utah, with emphasis on ground water"},"predicate":"SUPERSEDED_BY","object":{"id":70043399,"text":"70043399 - 1982 - Hydrology of the Beryl-Enterprise area, Escalante Desert, Utah, with emphasis on ground water; With a section on surface water","indexId":"70043399","publicationYear":"1982","noYear":false,"title":"Hydrology of the Beryl-Enterprise area, Escalante Desert, Utah, with emphasis on ground water; With a section on surface water"},"id":1}],"lastModifiedDate":"2016-12-17T12:48:26","indexId":"70043399","displayToPublicDate":"2013-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":4,"text":"Other Government Series"},"seriesTitle":{"id":294,"text":"Technical Publication","active":false,"publicationSubtype":{"id":4}},"seriesNumber":"73","title":"Hydrology of the Beryl-Enterprise area, Escalante Desert, Utah, with emphasis on ground water; With a section on surface water","docAbstract":"<p>An investigation of the water resources of the Beryl-Enterprise area, Escalante Desert, Utah (pl. 1), was made during 1976-78 as part of a cooperative program with the Utah Department of Natural Resources, Division of Water Rights. Wells were the most important source of water for all purposes in the Beryl-Enterprise area during 1978, but it has not always been so. For nearly a century after the first settlers arrived in about 1860, streams supplied most of the irrigation water and springs supplied much of the water for domestic and stock use. A few shallow wells were dug by the early settlers for domestic and stock water, but the widespread use of ground water did not start until the 1920's when shallow wells were first dug to supply irrigation water. Ground-water withdrawals from wells, principally for irrigation, have increased nearly every year since the 1920's. The quantity withdrawn from wells surpassed that diverted from surface sources during the mid-1940's and was about eight times that amount during the 1970's. As a result, water levels have declined measurably throughout the area resulting in administrative water-rights problems.</p><p>The primary purpose of this report is to describe the water resources with emphasis on ground water. The surface-water resources are evaluated only as they pertain to the understanding of the ground-water resources. A secondary purpose is to discuss the extent and effects of the development of ground water in order to provide the hydrologic information needed for the orderly and optimum development of the resource and for the effective administration and adjudication of water rights in the area. The hydrologic data on which this report is based are given in a companion report by Mower (1981).</p>","language":"English","publisher":"Utah Department of Natural Resources, Division of Water Rights","publisherLocation":"Salt Lake City, Utah","collaboration":"Prepared by the United State Geological Survey in cooperation with the Utah Department of Natural Resources Division of Water Rights","usgsCitation":"Mower, R.W., and Sandberg, G.W., 1982, Hydrology of the Beryl-Enterprise area, Escalante Desert, Utah, with emphasis on ground water; With a section on surface water: Technical Publication 73, vi, 66 p.","productDescription":"vi, 66 p.","numberOfPages":"86","costCenters":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":267297,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":331998,"rank":3,"type":{"id":11,"text":"Document"},"url":"https://waterrights.utah.gov/docSys/v920/w920/w920009y.pdf"},{"id":331997,"rank":2,"type":{"id":15,"text":"Index Page"},"url":"https://www.waterrights.utah.gov/cgi-bin/libview.exe?Modinfo=Viewpub&LIBNUM=20-5-730"}],"country":"United States","state":"Utah","otherGeospatial":"Escalante Desert","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -114.1,\n              37.6\n            ],\n            [\n              -114.1,\n              38.3\n            ],\n            [\n              -113,\n              38.3\n            ],\n            [\n              -113,\n              37.6\n            ],\n            [\n              -114.1,\n              37.6\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"511b7282e4b0e3ef7b6f1e3c","contributors":{"authors":[{"text":"Mower, Reed W.","contributorId":32503,"corporation":false,"usgs":true,"family":"Mower","given":"Reed","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":473505,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Sandberg, George Woodard","contributorId":87434,"corporation":false,"usgs":true,"family":"Sandberg","given":"George","email":"","middleInitial":"Woodard","affiliations":[],"preferred":false,"id":473506,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":98348,"text":"wri82350 - 1982 - Physical, Hydrological, and Biological Characteristics of the Loxahatchee River Estuary, Florida","interactions":[],"lastModifiedDate":"2012-11-15T13:00:55","indexId":"wri82350","displayToPublicDate":"2010-04-28T00:00:00","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":"82-350","title":"Physical, Hydrological, and Biological Characteristics of the Loxahatchee River Estuary, Florida","docAbstract":"The Loxahatchee River estuary empties into the Atlantic Ocean at Jupiter Inlet in southeastern Florida. Although relatively small, the estuary is important for its esthetic value and for its sport fishing, boating, recreation, tourism, and prime residential development. In recent years, the condition of the estuary has become of concern to many citizens and agencies of the State. In response to this concern, the U.S. Geological Survey planned and carried out an in-depth environmental investigation. The events that led to the investigation and the objectives of the investigation are outlined in a recent U.S. Geological Survey report by McPherson and Sabanskas (WRI 80-1109).","language":"ENGLISH","publisher":"U.S. Geological Survey","doi":"10.3133/wri82350","collaboration":"Prepared in cooperation with the Florida Department of Environmental Regulation, South Florida Water Management District, Palm Beach County, Martin County, Jupiter Inlet District, Loxahatchee River Environmental Control District, Town of Jupiter, Village of Tequesta, Jupiter Inlet Colony, U.S. Army Corps of Engineers","usgsCitation":"McPherson, B.F., Sabanskas, M., and Long, W.A., 1982, Physical, Hydrological, and Biological Characteristics of the Loxahatchee River Estuary, Florida (WRI/OFR): U.S. Geological Survey Water-Resources Investigations Report 82-350, 1 map, https://doi.org/10.3133/wri82350.","productDescription":"1 map","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"links":[{"id":125898,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/wri_82_350.jpg"},{"id":13597,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/wri/wri82-350/","linkFileType":{"id":5,"text":"html"}}],"geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -80.11777777777777,26.933888888888887 ], [ -80.11777777777777,26.966944444444444 ], [ -80.1,26.966944444444444 ], [ -80.1,26.933888888888887 ], [ -80.11777777777777,26.933888888888887 ] ] ] } } ] }","edition":"WRI/OFR","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adbe4b07f02db685ab5","contributors":{"authors":[{"text":"McPherson, Benjamin F.","contributorId":17965,"corporation":false,"usgs":true,"family":"McPherson","given":"Benjamin","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":305053,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Sabanskas, Maryann","contributorId":31455,"corporation":false,"usgs":true,"family":"Sabanskas","given":"Maryann","email":"","affiliations":[],"preferred":false,"id":305054,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Long, William A.","contributorId":10120,"corporation":false,"usgs":true,"family":"Long","given":"William","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":305052,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":80037,"text":"ofr811103 - 1982 - Chloride Concentration in Water from the Upper Permeable Zone of the Tertiary Limestone Aquifer System, Southeastern United States","interactions":[],"lastModifiedDate":"2012-02-10T00:11:39","indexId":"ofr811103","displayToPublicDate":"2007-06-20T00:00:00","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":"81-1103","title":"Chloride Concentration in Water from the Upper Permeable Zone of the Tertiary Limestone Aquifer System, Southeastern United States","docAbstract":"INTRODUCTION\r\n\r\nThe tertiary limestone aquifer system of the southeastern United States is a sequence of carbonate rocks referred to as the Floridan aquifer in Florida and the principal artesian aquifer in Georgia, Alabama, and South Carolina. More than 3 billion gallons of water are pumped daily from the limestone aquifer; and the system is the principal source of municipal, industrial, and agricultural water supply in south Georgia and most of Florida.\r\n\r\nThe aquifer system includes units of Paleocene to early Miocene age that combine to form a continuous carbonate sequence that is hydraulically connected in varying degrees. In a small area near Brunswick, Ga., a thin sequence of rocks of Late Cretaceous age is part of the system. In and directly downdip from much of the outcrop area, the system consists of one continuous permeable unit. Further downdip the aquifer system generally consists of two major permeable zones separated by a less-permeable unit of highly variable hydraulic properties (very leaky to virtually nonleaky). Conditions for the system vary from unconfined to confined depending upon whether the argillaceous Miocene and younger rocks that form the upper confining unit have been removed by erosion.\r\n\r\nThis report is one of a series of preliminary products depicting the hydrogeologic framework, water chemistry, and hydrology of the aquifer system. The map shows the distribution of chloride ions in water from the upper permeable zone of the limestone aquifer system. The upper permeable zone consists of several formations, primarily the Tampa, Suwannee, Ocala, and Avon Park Limestones (Miller 1981a, b).\r\n\r\nChloride concentrations of water within the upper permeable zone vary from nearly zero in recharge areas to many thousands of milligrams per liter (mg/L) in coastal discharge areas. Where the aquifer system discharges into the sea, the upper permeable zone contains increasing amounts of seawater. In these areas, wells that fully penetrate the upper permeable zone will yield water with chloride concentrations that approach that of seawater, about 19500 mg/L.","language":"ENGLISH","publisher":"Geological Survey (U.S.)","doi":"10.3133/ofr811103","usgsCitation":"Sprinkle, C.L., 1982, Chloride Concentration in Water from the Upper Permeable Zone of the Tertiary Limestone Aquifer System, Southeastern United States (WRI/OFR 81-1103): U.S. Geological Survey Open-File Report 81-1103, Map: 35 x 44 inches, https://doi.org/10.3133/ofr811103.","productDescription":"Map: 35 x 44 inches","costCenters":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"links":[{"id":192151,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1981/1103/report-thumb.jpg"},{"id":91219,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1981/1103/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -89,24 ], [ -89,34 ], [ -80,34 ], [ -80,24 ], [ -89,24 ] ] ] } } ] }","edition":"WRI/OFR 81-1103","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49dde4b07f02db5e253c","contributors":{"authors":[{"text":"Sprinkle, Craig L.","contributorId":41802,"corporation":false,"usgs":true,"family":"Sprinkle","given":"Craig","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":291538,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":45949,"text":"ofr821010 - 1982 - Percentage change in saturated thickness of the High Plains Aquifer, west-central Kansas, 1950 to average 1980-82","interactions":[],"lastModifiedDate":"2012-02-02T00:10:57","indexId":"ofr821010","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":"82-1010","title":"Percentage change in saturated thickness of the High Plains Aquifer, west-central Kansas, 1950 to average 1980-82","docAbstract":"A statistical technique, called kriging, was programmed for a computer to interpolate hydrologic data based on a network of 296 measured values in west-central Kansas and eastern Colorado. The computer program generated estimated values of selected hydrologic data at the center of each 1-mile section in the Western Kansas Groundwater Management District No. 1. This program facilitated contouring of the data that are needed to aid in the management of ground water for irrigation. The kriging technique produced a map that illustrates the percentage change in saturated thickness of the High Plains aquifer from 1950 to average 1980-82 in west-central Kansas. Estimated changes in saturated thickness of the aquifer, as shown on the map, range from about a 50% increase to a 100% decrease. (USGS)","language":"ENGLISH","doi":"10.3133/ofr821010","usgsCitation":"Pabst, M.E., 1982, Percentage change in saturated thickness of the High Plains Aquifer, west-central Kansas, 1950 to average 1980-82: U.S. Geological Survey Open-File Report 82-1010, 1 map :photocopy ;85 x 128 cm., https://doi.org/10.3133/ofr821010.","productDescription":"1 map :photocopy ;85 x 128 cm.","costCenters":[],"links":[{"id":168091,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":20762,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/1010/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae0e4b07f02db6884f2","contributors":{"authors":[{"text":"Pabst, Marilyn E.","contributorId":25566,"corporation":false,"usgs":true,"family":"Pabst","given":"Marilyn","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":232361,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":10587,"text":"ofr82649 - 1982 - January 1982 water levels, and data related to water-level changes, western and south-central Kansas","interactions":[],"lastModifiedDate":"2012-02-02T00:06:25","indexId":"ofr82649","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":"82-649","title":"January 1982 water levels, and data related to water-level changes, western and south-central Kansas","docAbstract":"Water-level measurements were made, mostly in January 1982, in about 1,530 wells in western and south-central Kansas. The measurements were made in mid-winter when pumping was minimal and water levels had recovered, for the most part, from the effects of pumping during the previous irrigation season. Annual hydrologic data are provided for relating water-level changes from a ' base-reference year ' (predevelopment year), a year of abnormally high rainfall and minimum pumpage (1966 or 1974), and each of seven consecutive years of measurement (1976-82), the ' base-reference year ' is designated as 1940 for the southwestern area, 1944 for the south-central area, and 1950 for the northwestern and west-central areas. Water levels for the ' base-reference year ' are established by measurements made during that year and by interpretation of maps showing water-level altitudes. Data also are provided for relating the average annual water-level changes, saturated thicknesses of the deposits, and percentage changes in saturated thicknesses. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr82649","usgsCitation":"Pabst, M., 1982, January 1982 water levels, and data related to water-level changes, western and south-central Kansas: U.S. Geological Survey Open-File Report 82-649, 167 p. :map ;28 cm., https://doi.org/10.3133/ofr82649.","productDescription":"167 p. :map ;28 cm.","costCenters":[],"links":[{"id":143111,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0649/report-thumb.jpg"},{"id":38413,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0649/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aa7e4b07f02db666fde","contributors":{"authors":[{"text":"Pabst, M.E.","contributorId":17608,"corporation":false,"usgs":true,"family":"Pabst","given":"M.E.","email":"","affiliations":[],"preferred":false,"id":161637,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":27335,"text":"wri824068 - 1982 - Digital model of the Bates Creek alluvial aquifer near Casper, Wyoming","interactions":[],"lastModifiedDate":"2017-09-20T16:54:35","indexId":"wri824068","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":"82-4068","title":"Digital model of the Bates Creek alluvial aquifer near Casper, Wyoming","docAbstract":"A digital model was used to simulate ground-water flow within the Bates Creek alluvial aquifer, southwest of Casper, Wyoming. Hydrologic data collected during 1977 and 1978 were used to develop the flow model under steady-state and transient conditions. Three scenarios for operating the stream-aquifer system were evaluated with the digital model. The scenarios represent no ground-water pumping, pumping by all existing wells , and pumping by all existing and proposed wells. The model simulations used average values of stream discharge, ground-water pumpage and water use as input parameters. A decrease in the quantitity of ground-water discharge to Bates Creek is predicted to occur through 1988 as a result of pumping. The magnitude and timing of the predicted decrease in ground-water discharge may differ from actual ground-water discharge if hydrologic conditions through 1988 vary significantly from the averaged input values used in the simulations. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri824068","usgsCitation":"Glover, K.C., 1982, Digital model of the Bates Creek alluvial aquifer near Casper, Wyoming: U.S. Geological Survey Water-Resources Investigations Report 82-4068, v, 50 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri824068.","productDescription":"v, 50 p. :ill., maps ;28 cm.","costCenters":[{"id":5050,"text":"WY-MT Water Science Center","active":true,"usgs":true}],"links":[{"id":124053,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1982/4068/report-thumb.jpg"},{"id":56199,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1982/4068/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a96e4b07f02db65aa1c","contributors":{"authors":[{"text":"Glover, K. C.","contributorId":14828,"corporation":false,"usgs":true,"family":"Glover","given":"K.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":197938,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":55217,"text":"wdrIA811 - 1982 - Water resources data Iowa, water year 1981","interactions":[],"lastModifiedDate":"2016-03-02T14:56:10","indexId":"wdrIA811","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":"IA-81-1","title":"Water resources data Iowa, water year 1981","docAbstract":"<p>This report was prepared by personnel of the Iowa district of&nbsp;the Water Resources Division of the U.S. Geological Survey under&nbsp;the supervision of 0. G. Lara, Acting District Chief, and Alfred&nbsp;Clebsch, Jr., Regional Hydrologist, Central Region. 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":68419,"text":"ha645 - 1982 - Dissolved-solids concentrations of ground water in the Sacramento Valley, California","interactions":[],"lastModifiedDate":"2012-02-10T00:11:12","indexId":"ha645","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":318,"text":"Hydrologic Atlas","code":"HA","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"645","title":"Dissolved-solids concentrations of ground water in the Sacramento Valley, California","docAbstract":"The general quality of the ground water in the Sacramento Valley , Calif., in terms of dissolved-solids concentration is considered good for irrigation, domestic, and most other uses. This map shows the distribution of dissolved-solids concentrations and is based on about 1,330 chemical analyses collected from about 900 wells between 1974 and 1978. On the west side of the valley some of the smaller streams contribute water of higher dissolved-solids concentrations to the ground water. The sources of these waters are thought to be the upper Cretaceous Chico Formation or marine deposits of Early Cretaceous age that are exposed in the Coast Ranges. (USGS)","language":"ENGLISH","doi":"10.3133/ha645","usgsCitation":"Fogelman, R.P., 1982, Dissolved-solids concentrations of ground water in the Sacramento Valley, California: U.S. Geological Survey Hydrologic Atlas 645, 1 map :col. ;70 x 99 cm., on sheet 76 x 112 cm., folded in envelope 32 x 24 cm., https://doi.org/10.3133/ha645.","productDescription":"1 map :col. ;70 x 99 cm., on sheet 76 x 112 cm., folded in envelope 32 x 24 cm.","costCenters":[],"links":[{"id":188901,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":89942,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/645/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -122.75,38.083333333333336 ], [ -122.75,40.333333333333336 ], [ -120.75,40.333333333333336 ], [ -120.75,38.083333333333336 ], [ -122.75,38.083333333333336 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a81e4b07f02db64a1ed","contributors":{"authors":[{"text":"Fogelman, Ronald P.","contributorId":62597,"corporation":false,"usgs":true,"family":"Fogelman","given":"Ronald","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":278186,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":11399,"text":"ofr82628 - 1982 - Water resources of southeastern Oahu, Hawaii","interactions":[],"lastModifiedDate":"2012-02-02T00:06:21","indexId":"ofr82628","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":"82-628","title":"Water resources of southeastern Oahu, Hawaii","docAbstract":"Southeastern Oahu comprises the eastern end of the Koolau Range and is divided into two roughly equal parts by the crest of the range. The northside of the crest is commonly called the windward side and the southside, the leeward. Precipitous cliffs aproned by a gently sloping landscape are the main topographic features on the windward side. The leeward side is a gentle lava-flow slope incised by steep narrow valleys. \r\n\r\nThe main Koolau fissure zone, including the caldera, lies on the windward side. The leeward side includes minor rift zones that are perpendicular to and intersect the main fissure zone. Dikes in the main fissure zone strike from nearly east-west in the eastern end to about N. 55? W. in the western part. Dikes in the minor rift zones strike from north-south to slightly northeasterly. \r\n\r\nWater use is about 18 Mgal/d (million gallons per day) of which only 4 Mgal/d is obtained locally from ground-water sources. About a third of the 14 Mgal/d deficit is imported from sources northwest of the study area on the windward side and the remainder from sources in the Honolulu and Pearl Harbor areas on the leeward side. The 4 Mgal/d being developed represents only about 3 percent of the area's rainfall compared to a development-rainfall ratio of 20 percent for the rest of the island. \r\n\r\nStreams are short and flashy. Perennial streamflow to the sea occurs only in Maunawili Valley and in the Waimanalo area. Mean annual discharge is estimated at 20 Mgal/d in the windward side and at 15 Mgal/d on the leeward side. Low flow, expressed as the flow that is equaled or exceeded 90 percent of the time, is 5 Mgal/d windward of the crest and zero leeward of it. Most fresh ground water occurs in lava flows of the Koolau Volcanics. It is impounded by dikes in the rift zones and floats on saline ground water as lenses outside the rift zones. Small but important bodies of freshwater are perched in volcanic rocks of the Honolulu Group in Maunawili Valley. Fresh ground water occurs in near-shore calcareous sands that overlie a clay horizon in the Waimanalo area. Deeply buried talus and alluvium also carry fresh ground water in the Waimanalo area. \r\n\r\nWells tapping saline ground water in fresh lava flows of the Honolulu Group provide water for a sea-life park in the Makapuu area. The same aquifer is tapped by wells for disposal of the saline waste water. \r\n\r\nThe current development scheme in the windward side that utilizes only the free-flow equilibrium discharge of dike-impounded water is inefficient and does not cope with the annual weather cycle. The flow available for development under this scheme is greatest in the rainy winter months when demand is the lowest and least in the summer months when demand is the highest. A more optimal scheme would be to change this natural flow pattern by depleting storage by pumping to increase flow in the high-demand summer months and allowing the depleted storage to recover naturally in the low-demand winter months. Depleting storage would lower water levels which would provide more room for infiltration and provide less opportunity for evapotranspiration. \r\n\r\nThe basal-water reservoir in the leeward side is isolated hydrologically from abutting reservoirs outside the area and can and should be fully exploited. The existing development of the basal-water reservoir is small compared to the natural ground-water flow and that part not being developed is wasting to the sea. Because the area is hydrologically isolated, development will not be detrimental to or reduce the ground-water supply outside the area.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr82628","usgsCitation":"Takasaki, K., and Mink, J., 1982, Water resources of southeastern Oahu, Hawaii: U.S. Geological Survey Open-File Report 82-628, viii, 97 p. :ill., maps ;28 cm., https://doi.org/10.3133/ofr82628.","productDescription":"viii, 97 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":142573,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0628/report-thumb.jpg"},{"id":39220,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0628/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49dee4b07f02db5e3158","contributors":{"authors":[{"text":"Takasaki, K. J.","contributorId":44523,"corporation":false,"usgs":true,"family":"Takasaki","given":"K. J.","affiliations":[],"preferred":false,"id":163073,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Mink, John F.","contributorId":89510,"corporation":false,"usgs":true,"family":"Mink","given":"John F.","affiliations":[],"preferred":false,"id":163074,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":48795,"text":"ofr82694 - 1982 - Submersed aquatic vegetation in the tidal Potomac River and Estuary of Maryland, Virginia and the District of Columbia; Hydrologic data report, May, 1978 to November, 1981","interactions":[],"lastModifiedDate":"2012-02-02T00:10:22","indexId":"ofr82694","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":"82-694","title":"Submersed aquatic vegetation in the tidal Potomac River and Estuary of Maryland, Virginia and the District of Columbia; Hydrologic data report, May, 1978 to November, 1981","language":"ENGLISH","doi":"10.3133/ofr82694","usgsCitation":"Paschal, J.E., Miller, D.R., Bartow, N.C., and Carter, V., 1982, Submersed aquatic vegetation in the tidal Potomac River and Estuary of Maryland, Virginia and the District of Columbia; Hydrologic data report, May, 1978 to November, 1981: U.S. Geological Survey Open-File Report 82-694, 220 p., https://doi.org/10.3133/ofr82694.","productDescription":"220 p.","costCenters":[],"links":[{"id":169706,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0694/report-thumb.jpg"},{"id":85626,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0694/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b05e4b07f02db699b89","contributors":{"authors":[{"text":"Paschal, James E. Jr.","contributorId":45768,"corporation":false,"usgs":true,"family":"Paschal","given":"James","suffix":"Jr.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":238272,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Miller, Darin R.","contributorId":64713,"corporation":false,"usgs":true,"family":"Miller","given":"Darin","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":238274,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Bartow, Nancy C.","contributorId":56203,"corporation":false,"usgs":true,"family":"Bartow","given":"Nancy","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":238273,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Carter, Virginia","contributorId":12018,"corporation":false,"usgs":true,"family":"Carter","given":"Virginia","email":"","affiliations":[],"preferred":false,"id":238271,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":10051,"text":"ofr82164 - 1982 - Hydrologic data for urban studies in the Houston, Texas, metropolitan area, 1979","interactions":[],"lastModifiedDate":"2017-04-19T10:18:01","indexId":"ofr82164","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":"82-164","title":"Hydrologic data for urban studies in the Houston, Texas, metropolitan area, 1979","docAbstract":"<p>Hydrologic investigations of urban watersheds in Texas were begun by the U.S. Geological Survey in 1954. Studies are now in progress in Austin, Houston, and San Antonio.</p><p>The U.S. Geological Survey, in cooperation with the city of Houston, began studies in the Houston metropolitan area in 1964. The program was expanded in 1968 to include collection of water-quality data. The objectives of the Houston urban-hydrology study are as follows:</p><ol><li>To determine, on the basis of historical data and hydro!ogic analyses, the magnitude and frequency of flood peaks and flood volumes.</li><li>To determine the effect of urban development on flood peaks and volumes.</li><li>To ascertain the variation in water quality for different flow conditions and different seasons.</li></ol><p>This report, the sixteenth in a series of reports to be published annually, is primarily applicable to objective 2. The report presents hydro!ogic data collected in the Houston urban area for the 1979 water year (October 1, 1978 to September 30, 1979).</p><p>A report by Johnson and Sayre (1973) utilized records collected from 1965 to 1969 to make a study of the effects of urbanization on floods in the Houston area. The report also summarizes various basin parameters. A report by Waddell, Massey, and Jennings (1979) presents data on computed runoff from the Houston area and computed concentrations and loads of selected waterquality constituents combined in the inflow to Galveston Bay. The study utilized a variation of the \"STORM\" model developed by the Hydro!ogic Engineering Center of the U.S. Army Corps of Engineers. A report prepared by Li scum and Massey (1980) presents a technique for estimating the magnitude and frequency of floods in the Houston area from drainage areas, bank-full conveyance, and percentage of urban development.</p><p>A definition of terms related to streamflow, water quality, and other hydrologic data, as used in this report, are defined in \"U.S. Geological Survey, Water-resources data for Texas, volume 2, 1979.\"</p><p>To facilitate the publication and distribution of this report at the earliest feasible time, some material has been included that does not conform to the formal publications standards of the U.S. Geological Survey.</p><p>&nbsp;</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr82164","collaboration":"Prepared in cooperation with the City of Houston","usgsCitation":"Liscum, F., Weigel, J.F., and Bruchmiller, J., 1982, Hydrologic data for urban studies in the Houston, Texas, metropolitan area, 1979: U.S. Geological Survey Open-File Report 82-164, 308 p., https://doi.org/10.3133/ofr82164.","productDescription":"308 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"links":[{"id":145609,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0164/report-thumb.jpg"},{"id":37900,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0164/report.pdf","text":"Report","size":"6.18 MB","linkFileType":{"id":1,"text":"pdf"},"description":"Report"}],"country":"United States","state":"Texas","city":"Houston","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -95.36819458007811,\n              30.039377605001338\n            ],\n            [\n              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Fred","contributorId":95463,"corporation":false,"usgs":true,"family":"Liscum","given":"Fred","email":"","affiliations":[],"preferred":false,"id":160733,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Weigel, Jay F.","contributorId":19560,"corporation":false,"usgs":true,"family":"Weigel","given":"Jay","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":160732,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Bruchmiller, J.P.","contributorId":102490,"corporation":false,"usgs":true,"family":"Bruchmiller","given":"J.P.","email":"","affiliations":[],"preferred":false,"id":160734,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":68529,"text":"ha655 - 1982 - Flood of April 1979 on Pearl River in Jackson, Mississippi and vicinity","interactions":[],"lastModifiedDate":"2012-02-10T00:11:28","indexId":"ha655","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":318,"text":"Hydrologic Atlas","code":"HA","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"655","title":"Flood of April 1979 on Pearl River in Jackson, Mississippi and vicinity","language":"ENGLISH","doi":"10.3133/ha655","usgsCitation":"Carroon, L., 1982, Flood of April 1979 on Pearl River in Jackson, Mississippi and vicinity: U.S. Geological Survey Hydrologic Atlas 655, 2 maps :col. ;35 x 101 cm., folded in envelope 31 x 25 cm., https://doi.org/10.3133/ha655.","productDescription":"2 maps :col. ;35 x 101 cm., folded in envelope 31 x 25 cm.","costCenters":[],"links":[{"id":185711,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":90131,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/655/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":90132,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/655/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"24000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -90.33333333333333,32.15 ], [ -90.33333333333333,32.43333333333333 ], [ -90,32.43333333333333 ], [ -90,32.15 ], [ -90.33333333333333,32.15 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f2e4b07f02db5eefcb","contributors":{"authors":[{"text":"Carroon, L.E.","contributorId":29880,"corporation":false,"usgs":true,"family":"Carroon","given":"L.E.","affiliations":[],"preferred":false,"id":278403,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":27657,"text":"wri824019 - 1982 - Model modifications for simulation of flow through stratified rocks in eastern Ohio","interactions":[],"lastModifiedDate":"2012-02-02T00:08:37","indexId":"wri824019","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":"82-4019","title":"Model modifications for simulation of flow through stratified rocks in eastern Ohio","docAbstract":"A quasi three-dimensional groundwater flow model is being used as part of a study to determine impacts of coal-strip mining on local hydrologic systems. Modifications to the model were necessary to simulate local hydrologic conditions properly. Perched water tables required that the method of calculating vertical flow rate be changed. A head-dependent spring-discharge function and a head-dependent stream aquifer-interchange function were added to the program. Modifications were also made to allow recharge from precipitation to any layer. The modified program, data deck instructions, and sample input and output are presented. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri824019","usgsCitation":"Helgesen, J.O., Razem, A., and Larson, S.P., 1982, Model modifications for simulation of flow through stratified rocks in eastern Ohio: U.S. Geological Survey Water-Resources Investigations Report 82-4019, iv, 113 p. :ill. ;28 cm., https://doi.org/10.3133/wri824019.","productDescription":"iv, 113 p. :ill. ;28 cm.","costCenters":[],"links":[{"id":122914,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1982/4019/report-thumb.jpg"},{"id":56512,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1982/4019/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b05e4b07f02db699a2f","contributors":{"authors":[{"text":"Helgesen, J. O.","contributorId":62600,"corporation":false,"usgs":true,"family":"Helgesen","given":"J.","email":"","middleInitial":"O.","affiliations":[],"preferred":false,"id":198482,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Razem, A. C.","contributorId":34924,"corporation":false,"usgs":true,"family":"Razem","given":"A. C.","affiliations":[],"preferred":false,"id":198481,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Larson, S. P.","contributorId":34903,"corporation":false,"usgs":true,"family":"Larson","given":"S.","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":198480,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":10536,"text":"ofr802046 - 1982 - Ground-water levels and water quality in an area near Topaz Lake, Douglas County, Nevada","interactions":[],"lastModifiedDate":"2022-04-18T16:03:53.25151","indexId":"ofr802046","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":"80-2046","title":"Ground-water levels and water quality in an area near Topaz Lake, Douglas County, Nevada","docAbstract":"<p>Intensive residential development of land along the northwest shore of Topaz Lake has raised concern regarding the adequacy of the water supply and possible effects of septic-tank effluents on the quality of local ground water and the lake. Existing data on water levels, well construction, and water quality were compiled, and a limited program of water-level measurement and water-quality sampling was conducted during 1976-77 to provide documentation of current hydrologic conditions against which effects of future development may be measured.<br></p><p>Water-level measurements show the presence of small independent aquifers near the periphery of the alluvial fan covering the study area and a main alluvial aquifer in which water levels fluctuate in direct response to annual changes in lake stage.</p><p>The sampled ground water can be grouped into four chemical types--three based on the relative proportions of sulfate and bicarbonate and one based on an increased proportion of chloride plus nitrate.</p><p>Frequency distributions of the observed occurrences of nitrate (as NO3), phosphate (as PO4), and chloride in ground water indicate thresholds for background concentrations of these constituents at 0 to 3, 0 to 0.35, and 0 to 6 milligrams per liter, respectively. Above-background concentrations of nitrate and phosphate in ground water may be attributable, in part, to natural sources of these constituents; however, septic-tank effluents have increased the concentrations of nitrate, chloride, and perhaps phosphate in at least two areas of the current development. Sampling for dissolved organic carbon and coliform bacteria in ground water detected no contamination by these potential indicators of pollution.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr802046","collaboration":"Prepared in cooperation with the Nevada Division of Environmental Protection","usgsCitation":"Nowlin, J.O., 1982, Ground-water levels and water quality in an area near Topaz Lake, Douglas County, Nevada: U.S. Geological Survey Open-File Report 80-2046, vii, 76 p., https://doi.org/10.3133/ofr802046.","productDescription":"vii, 76 p.","costCenters":[],"links":[{"id":398930,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1980/2046/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":142983,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1980/2046/report-thumb.jpg"}],"country":"United States","state":"Nevada","county":"Douglas County","otherGeospatial":"Topaz Lake","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -119.55596923828124,\n              38.67371706140244\n            ],\n            [\n              -119.49279785156249,\n              38.67371706140244\n            ],\n            [\n              -119.49279785156249,\n              38.717126039425644\n            ],\n            [\n              -119.55596923828124,\n              38.717126039425644\n            ],\n            [\n              -119.55596923828124,\n              38.67371706140244\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aa9e4b07f02db66889b","contributors":{"authors":[{"text":"Nowlin, Jon O.","contributorId":34937,"corporation":false,"usgs":true,"family":"Nowlin","given":"Jon","email":"","middleInitial":"O.","affiliations":[],"preferred":false,"id":161561,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":57242,"text":"wdrWV81A - 1982 - Water resources data, West Virginia water year 1981, Appendix - coal areas and special projects","interactions":[],"lastModifiedDate":"2025-02-26T20:04:09.912054","indexId":"wdrWV81A","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":"WV-81-A","title":"Water resources data, West Virginia water year 1981, Appendix - coal areas and special projects","docAbstract":"<p>The first section of this report contains data collected during the 1981 water year for the West Virginia Coal Hydrology monitoring project. Records consist of discharge and water-quality data collected at 246 sites in July, at 29 sites in August, and sediment data for 235 sites collected in July.</p><p>The second section of this report contains data collected during the period January 1978 to December 1981 for the water resources study of the Tug Fork and Twelvepole Creek basins. Records consist of physical data for 347 wells, water level data for two wells, quality analyses of water from 328 wells, and discharge, chemical and biological data for 91 sites sampled several times.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wdrWV81A","collaboration":"Prepared in cooperation with the State of West Virginia and other agencies","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1982, Water resources data, West Virginia water year 1981, Appendix - coal areas and special projects: U.S. Geological Survey Water Data Report WV-81-A, v, 197 p., https://doi.org/10.3133/wdrWV81A.","productDescription":"v, 197 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,{"id":30344,"text":"wri8234 - 1982 - Water-quality characteristics of Everglades National Park, 1959-77, with reference to the effects of water management","interactions":[],"lastModifiedDate":"2019-08-05T12:06:39","indexId":"wri8234","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":"82-34","title":"Water-quality characteristics of Everglades National Park, 1959-77, with reference to the effects of water management","docAbstract":"The U.S. Geological Survey has collected water-quality data in the Everglades National Park since 1959. Major ions, macronutrients, trace elements, and pesticides are the primary chemical groups analyzed. The period of record and frequency of sampling vary for each chemical group, with the longest record for the major ions and the shortest for the macronutrients. Within the park there are three major drainageways: Big Cypress Swamp, Shark River Slough, and Taylor Slough. Each drainageway exhibits unique hydrologic conditions, yet there is a high degree of homogeneity in water-quality characteristics among these areas. Seasonal changes in major-ion, trace-element, and macronutrient concentrations are marked in the shallow marsh. Concentrations generally increase in the dry season due to evapotranspiration, changes in chemical equilibria, and precipitation. Water-management practices in south Florida have changed the water quality in the Shark River Slough. Most major-ion, dissolved-solid, and iron concentrations and color levels have steadily increased since 1963. The water quality in the other two drainageways has not changed since sampling began. Chlorinated-hydrocarbon insecticide residues in bottom material were found in low concentration at every sampling station in the park. (USGS)","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wri8234","usgsCitation":"Waller, B.G., 1982, Water-quality characteristics of Everglades National Park, 1959-77, with reference to the effects of water management: U.S. Geological Survey Water-Resources Investigations Report 82-34, vi, 51 p. , https://doi.org/10.3133/wri8234.","productDescription":"vi, 51 p. ","costCenters":[],"links":[{"id":366265,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1982/0034/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":159310,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1982/0034/report-thumb.jpg"}],"country":"United States","state":"Florida","otherGeospatial":"Everglades National Park","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -81.15600585937499,\n              25.13533901613099\n            ],\n            [\n              -80.48583984375,\n              25.13533901613099\n            ],\n            [\n              -80.48583984375,\n              25.517657429994035\n            ],\n            [\n              -81.15600585937499,\n              25.517657429994035\n            ],\n            [\n              -81.15600585937499,\n              25.13533901613099\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a9ae4b07f02db65d9f0","contributors":{"authors":[{"text":"Waller, Bradley G.","contributorId":83492,"corporation":false,"usgs":true,"family":"Waller","given":"Bradley","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":203093,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":18910,"text":"ofr82858 - 1982 - Hydrology of area 29, Eastern Region, Interior Coal Province, Illinois","interactions":[],"lastModifiedDate":"2012-02-02T00:07:32","indexId":"ofr82858","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":"82-858","title":"Hydrology of area 29, Eastern Region, Interior Coal Province, Illinois","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr82858","usgsCitation":"Fitzgerald, K.K., Peters, C., and Zuehls, E., 1982, Hydrology of area 29, Eastern Region, Interior Coal Province, Illinois: U.S. Geological Survey Open-File Report 82-858, v, 70 p. :ill. (some col.), maps (some col.) ;28 cm., https://doi.org/10.3133/ofr82858.","productDescription":"v, 70 p. :ill. (some col.), maps (some col.) ;28 cm.","costCenters":[],"links":[{"id":95418,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0858/report.pdf","size":"21673","linkFileType":{"id":1,"text":"pdf"}},{"id":94523,"rank":800,"type":{"id":11,"text":"Document"},"url":"https://hdl.handle.net/2027/mdp.39015048193042"},{"id":151499,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0858/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a13e4b07f02db6021e6","contributors":{"authors":[{"text":"Fitzgerald, K. K.","contributorId":34501,"corporation":false,"usgs":true,"family":"Fitzgerald","given":"K.","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":179968,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Peters, C.A.","contributorId":29794,"corporation":false,"usgs":true,"family":"Peters","given":"C.A.","email":"","affiliations":[],"preferred":false,"id":179967,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Zuehls, E.E.","contributorId":19942,"corporation":false,"usgs":true,"family":"Zuehls","given":"E.E.","email":"","affiliations":[],"preferred":false,"id":179966,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":26851,"text":"wri824111 - 1982 - Geologic and well-construction data for the H-9 borehole complex near the proposed Waste Isolation Pilot Plant site, southeastern New Mexico","interactions":[],"lastModifiedDate":"2012-02-02T00:08:21","indexId":"wri824111","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":"82-4111","title":"Geologic and well-construction data for the H-9 borehole complex near the proposed Waste Isolation Pilot Plant site, southeastern New Mexico","docAbstract":"The H-9 complex, a group of three closely spaced boreholes, is located 5.5 miles south of the proposed Waste Isolation Pilot Plant (WIPP) site in east-central Eddy County, New Mexico. The holes were drilled during July, August, and September 1979 to obtain geologic and hydrologic data to better define the regional ground-water-flow system. The geologic data presented in this report are part of a site-characterization study for the possible storage of defense-associated radioactive wastes within salt beds of the Salado Formation of Permian age. The geologic data include detailed descriptions of cores, cuttings, and geophysical logs. Each borehole was designed to penetrate a distinct water-bearing zone: H-9a (total depth 559 feet) was completed just below the Magenta Dolomite Member of the Rustler Formation; H-9b (total depth 708 feet) was completed just below the Culebra Dolomite Member of the Rustler Formation; H-9c (total depth 816 feet) was completed below the Rustler Formation-Salado Formation contact. The geologic units penetrated in borehole H-9c are eolian sand of Holocene age (0-5 feet); the Gatuna Formation of Pleistocene age; (5-25 feet); and the Dewey Lake Red Beds (25-455 feet), the Rustler Formation (455.791 feet), and part of the Salado Formation (791-816 feet), all of Permian age. Three sections (494-501 feet, 615-625 feet, 692-712 feet) in the Rustler Formation penetrated by borehole H-9c are composed of remnant anhydrite (locally altered to gypsum) and clay and silt residue from the dissolution of much thicker seams of argillaceous and silty halite. This indicates that the eastward-moving dissolution within the Rustler Formation, found just to the west of the WIPP site, is present at the H-9 site. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri824111","usgsCitation":"Drellack, S., and Wells, J., 1982, Geologic and well-construction data for the H-9 borehole complex near the proposed Waste Isolation Pilot Plant site, southeastern New Mexico: U.S. Geological Survey Water-Resources Investigations Report 82-4111, iv, 36 p. :ill., map ;28 cm., https://doi.org/10.3133/wri824111.","productDescription":"iv, 36 p. :ill., map ;28 cm.","costCenters":[],"links":[{"id":123764,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1982/4111/report-thumb.jpg"},{"id":55740,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1982/4111/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":55741,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1982/4111/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b17e4b07f02db6a64b5","contributors":{"authors":[{"text":"Drellack, S.L.","contributorId":19973,"corporation":false,"usgs":true,"family":"Drellack","given":"S.L.","affiliations":[],"preferred":false,"id":197118,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Wells, J.G.","contributorId":85198,"corporation":false,"usgs":true,"family":"Wells","given":"J.G.","email":"","affiliations":[],"preferred":false,"id":197119,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":10860,"text":"ofr82980 - 1982 - Integrated model of the shallow and deep hydrothermal systems in the East Mesa area, Imperial Valley, California","interactions":[],"lastModifiedDate":"2012-02-02T00:06:34","indexId":"ofr82980","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":"82-980","title":"Integrated model of the shallow and deep hydrothermal systems in the East Mesa area, Imperial Valley, California","docAbstract":"Geological, geophysical, thermal, petrophysical and hydrological data available for the East Mesa hydrothermal system that are pertinent to the construction of a computer model of the natural flow of heat and fluid mass within the system are assembled and correlated. A conceptual model of the full system is developed and a subregion selected for quantitative modeling. By invoking the .Boussinesq approximation, valid for describing the natural flow of heat and mass in a liquid hydrothermal system, it is found practical to carry computer simulations far enough in time to ensure that steady-state conditions are obtained. Initial calculations for an axisymmetric model approximating the system demonstrate that the vertical formation permeability of the deep East Mesa system must be very low (kv ~ 0.25 to 0.5 md). Since subsurface temperature and surface heat flow data exhibit major deviations from the axisymmetric approximation, exploratory three-dimensional calculations are performed to assess the effects of various mechanisms which might operate to produce such observed asymmetries. A three-dimensional model evolves from this iterative data synthesis and computer analysis which includes a hot fluid convective source distributed along a leaky fault radiating northward from the center of the hot spot and realistic variations in the reservoir formation properties.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr82980","usgsCitation":"Riney, T.D., Pritchett, J., and Rice, L., 1982, Integrated model of the shallow and deep hydrothermal systems in the East Mesa area, Imperial Valley, California: U.S. Geological Survey Open-File Report 82-980, 118 p., ill., maps ;28 cm., https://doi.org/10.3133/ofr82980.","productDescription":"118 p., ill., maps ;28 cm.","costCenters":[],"links":[{"id":144916,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0980/report-thumb.jpg"},{"id":38644,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0980/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e499ee4b07f02db5bcb4b","contributors":{"authors":[{"text":"Riney, T. David","contributorId":92674,"corporation":false,"usgs":true,"family":"Riney","given":"T.","email":"","middleInitial":"David","affiliations":[],"preferred":false,"id":162090,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Pritchett, J.W.","contributorId":29433,"corporation":false,"usgs":true,"family":"Pritchett","given":"J.W.","email":"","affiliations":[],"preferred":false,"id":162088,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Rice, L.F.","contributorId":59799,"corporation":false,"usgs":true,"family":"Rice","given":"L.F.","email":"","affiliations":[],"preferred":false,"id":162089,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
]}