{"pageNumber":"542","pageRowStart":"13525","pageSize":"25","recordCount":16455,"records":[{"id":70011297,"text":"70011297 - 1983 - Process and rate of dedolomitization: Mass transfer and C14 dating in a regional carbonate aquifer","interactions":[],"lastModifiedDate":"2024-01-03T12:27:00.499197","indexId":"70011297","displayToPublicDate":"1983-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1786,"text":"Geological Society of America Bulletin","active":true,"publicationSubtype":{"id":10}},"title":"Process and rate of dedolomitization: Mass transfer and C14 dating in a regional carbonate aquifer","docAbstract":"<div id=\"15274996\" class=\"article-section-wrapper js-article-section js-content-section  \" data-section-parent-id=\"0\"><p>Regional dedolomitization is the major process that controls the chemical character of water in the Mississippian Pahasapa Limestone (Madison equivalent) surrounding the Black Hills, South Dakota and Wyoming. The process of dedolomitization consists of dolomite dissolution and concurrent precipitation of calcite; it is driven by dissolution of gypsum.</p><p>Deuterium and oxygen isotopic data from the ground water, coupled with regional potentiometric maps, show that recharge occurs on the western slope of the Black Hills and that the water flows northward and westward toward the Powder River Basin. A significant part flows around the southern end of the Black Hills to replenish the aquifer to the east of the Hills. Depth of flow was inferred from interpretation of the silica geothermometer based on the temperature-dependent solubilities of quartz and chalcedony in water. Chemical effects of warm water in the Pahasapa Limestone include changes in the solubility products of minerals, conversion of gypsum to anhydrite, solution and precipitation of minerals, and increases in the tendency for outgassing of carbon dioxide. Where sulfate reduction is not important, sulfur isotope data show that (1) in the Mississippian aquifer, most of the sulfate is from dissolution of gypsum and (2) some wells and springs have a hydrologic connection with overlying Permian and Pennsylvanian evaporites. Sulfate ion concentration, a progress variable, shows a strong correlation with pH as a result of the combined effects of the dedolomitization reactions.</p><p>Mass-balance and mass-transfer calculations were used to adjust<span>&nbsp;</span><sup>14</sup>C values to determine a range of ground-water flow velocities between 2 and 20 m/yr. These velocities are characteristic of carbonate aquifers. The average rates of dolomite and gypsum dissolution are 1.7 × 10<sup>−4</sup><span>&nbsp;</span>and 3.4 × 10<sup>−4</sup><span>&nbsp;</span>mmol/kg of H<sub>2</sub>O/yr, respectively. The precipitation of calcite is occurring at the rate of 3.4 × 10<sup>−4</sup><span>&nbsp;</span>mmol/kg of H<sub>2</sub>O/yr. The close agreement among the model results demonstrates that dedolomitization is controlling water-rock interactions in this regional carbonate aquifer system.</p></div>","language":"English","publisher":"Geological Society of America","doi":"10.1130/0016-7606(1983)94<1415:PARODM>2.0.CO;2","usgsCitation":"Back, W., Hanshaw, B., Plummer, N., Rahn, P., Rightmire, C., and Rubin, M., 1983, Process and rate of dedolomitization: Mass transfer and C14 dating in a regional carbonate aquifer: Geological Society of America Bulletin, v. 94, no. 12, p. 1415-1429, https://doi.org/10.1130/0016-7606(1983)94<1415:PARODM>2.0.CO;2.","productDescription":"15 p.","startPage":"1415","endPage":"1429","numberOfPages":"15","costCenters":[],"links":[{"id":221228,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"94","issue":"12","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a8d86e4b0c8380cd7ec92","contributors":{"authors":[{"text":"Back, W.","contributorId":33839,"corporation":false,"usgs":true,"family":"Back","given":"W.","email":"","affiliations":[],"preferred":false,"id":360769,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hanshaw, B.B.","contributorId":25928,"corporation":false,"usgs":true,"family":"Hanshaw","given":"B.B.","email":"","affiliations":[],"preferred":false,"id":360768,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Plummer, Niel 0000-0002-4020-1013 nplummer@usgs.gov","orcid":"https://orcid.org/0000-0002-4020-1013","contributorId":190100,"corporation":false,"usgs":true,"family":"Plummer","given":"Niel","email":"nplummer@usgs.gov","affiliations":[{"id":436,"text":"National Research Program - Eastern Branch","active":true,"usgs":true}],"preferred":true,"id":360772,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Rahn, P.H.","contributorId":50657,"corporation":false,"usgs":true,"family":"Rahn","given":"P.H.","email":"","affiliations":[],"preferred":false,"id":360770,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Rightmire, C.T.","contributorId":63822,"corporation":false,"usgs":true,"family":"Rightmire","given":"C.T.","email":"","affiliations":[],"preferred":false,"id":360771,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Rubin, M.","contributorId":88079,"corporation":false,"usgs":true,"family":"Rubin","given":"M.","email":"","affiliations":[],"preferred":false,"id":360773,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}}
,{"id":70010367,"text":"70010367 - 1983 - An enriched finite element for simulation of groundwater flow to a well or drain - Comment","interactions":[],"lastModifiedDate":"2025-04-30T14:59:26.057359","indexId":"70010367","displayToPublicDate":"1983-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2342,"text":"Journal of Hydrology","active":true,"publicationSubtype":{"id":10}},"title":"An enriched finite element for simulation of groundwater flow to a well or drain - Comment","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"Elsevier","doi":"10.1016/0022-1694(83)90033-1","issn":"00221694","usgsCitation":"Kemblowski, M., 1983, An enriched finite element for simulation of groundwater flow to a well or drain - Comment: Journal of Hydrology, v. 60, no. 1-4, p. 381-382, https://doi.org/10.1016/0022-1694(83)90033-1.","productDescription":"2 p.","startPage":"381","endPage":"382","numberOfPages":"2","costCenters":[],"links":[{"id":219684,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"60","issue":"1-4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059ea3be4b0c8380cd4870f","contributors":{"authors":[{"text":"Kemblowski, M.","contributorId":54340,"corporation":false,"usgs":true,"family":"Kemblowski","given":"M.","affiliations":[],"preferred":false,"id":358754,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70011335,"text":"70011335 - 1983 - Nonequilibrium models for predicting forms of precipitated manganese oxides","interactions":[],"lastModifiedDate":"2020-01-20T19:56:53","indexId":"70011335","displayToPublicDate":"1983-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1759,"text":"Geochimica et Cosmochimica Acta","active":true,"publicationSubtype":{"id":10}},"title":"Nonequilibrium models for predicting forms of precipitated manganese oxides","docAbstract":"<p>Manganese oxides precipitated by bubbling air through 0.01 molar solutions of MnCl<sub>2</sub>, Mn(NO<sub>3</sub>)<sub>2</sub>, MnSO<sub>4</sub>, or Mn(ClO<sub>4</sub>)<sub>2</sub><span>&nbsp;</span>at a constantly maintained pH of 8.5 to 9.5 at temperatures of 25°C or higher consisted mainly of hausmannite, Mn<sub>3</sub>O<sub>4</sub>. At temperatures near 0°C, but with other conditions the same, the product is feitknechtite, βMnOOH, except that if the initial solution is MnSO<sub>4</sub><span>&nbsp;</span>and the temperature is near 0°C the product is a mixture of manganite, γMnOOH and groutite, αMnOOH.</p><p>All these oxides are metastable in aerated solution and alter by irreversible processes to more highly oxidized species during aging. A two-step nonequilibrium thermodynamic model predicts that the least stable species, βMnOOH, should be most readily converted to MnO<sub>2</sub>. Some preparations of βMnOOH aged in their native solution at 5°C attained a manganese oxidation state of +3.3 or more after 7 months. Hausmannite aged at 25°C altered to γMnOOH. The latter is more stable than a or βMnOOH, and manganese oxidation states above 3.0 were not reached in hausmannite precipitates during 4 months of aging. Initial precipitation of MnCO<sub>3</sub><span>&nbsp;</span>rather than a form of oxide is likely only where oxygen availability is very low.</p><p>Composition of solutions and oxidation state and morphology of solids were determined during the aging process by chemical analyses, X-ray and electron diffraction and transmission electron micrographs.</p>","language":"English","publisher":"Elsevier","doi":"10.1016/0016-7037(83)90219-3","issn":"00167037","usgsCitation":"Hem, J., and Lind, C.J., 1983, Nonequilibrium models for predicting forms of precipitated manganese oxides: Geochimica et Cosmochimica Acta, v. 47, no. 11, p. 2037-2046, https://doi.org/10.1016/0016-7037(83)90219-3.","productDescription":"10 p.","startPage":"2037","endPage":"2046","numberOfPages":"10","costCenters":[{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":220763,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"47","issue":"11","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a676fe4b0c8380cd73325","contributors":{"authors":[{"text":"Hem, J.D.","contributorId":54576,"corporation":false,"usgs":true,"family":"Hem","given":"J.D.","affiliations":[],"preferred":false,"id":360861,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Lind, Carol J.","contributorId":36110,"corporation":false,"usgs":true,"family":"Lind","given":"Carol","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":360860,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70011295,"text":"70011295 - 1983 - Simulation of solute transport in a mountain pool-and-riffle stream with a kinetic mass transfer model for sorption","interactions":[],"lastModifiedDate":"2020-01-26T09:39:40","indexId":"70011295","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":"Simulation of solute transport in a mountain pool-and-riffle stream with a kinetic mass transfer model for sorption","docAbstract":"<p><span>In natural channels there are often long periods of low flow during which solutes have repeated opportunity for contact with relatively immobile bed materials. Such conditions can exist in very small pool-and-riffle mountain streams. If a solute can sorb onto bed materials, then both hydrodynamic and chemical processes control solute transport. A simulation of these processes is presented for a carefully controlled and intensively monitored strontium injection experiment. The numerical model couples nonreactive, transient storage with a kinetic mass transport model for sorption. The results are compared to both in-stream and on-sediment strontium measurements. In mountain streams the stream hydrology is complex and is governed by a wide variety of time and distance scales. The present simulations assist in interpreting the relative roles of hydrologic and sorptive kinetic processes, and indicate the practical limits of our process and parameter knowledge. The simulations are relatively insensitive to the details of the kinetic mechanisms and to the spatial variability of the stream parameters.</span></p>","language":"English","publisher":"American Geophysical Union","doi":"10.1029/WR019i003p00732","usgsCitation":"Bencala, K.E., 1983, Simulation of solute transport in a mountain pool-and-riffle stream with a kinetic mass transfer model for sorption: Water Resources Research, v. 19, no. 3, p. 732-738, https://doi.org/10.1029/WR019i003p00732.","productDescription":"7 p.","startPage":"732","endPage":"738","costCenters":[{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":221226,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"19","issue":"3","noUsgsAuthors":false,"publicationDate":"2010-07-09","publicationStatus":"PW","scienceBaseUri":"505b9083e4b08c986b319552","contributors":{"authors":[{"text":"Bencala, Kenneth E. kbencala@usgs.gov","contributorId":1541,"corporation":false,"usgs":true,"family":"Bencala","given":"Kenneth","email":"kbencala@usgs.gov","middleInitial":"E.","affiliations":[],"preferred":true,"id":360765,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":3192,"text":"wsp2195 - 1983 - Hydrology of the Ferron Sandstone aquifer and effects of proposed surface-coal mining in Castle Valley, Utah, with a section on stratigraphy and a section on leaching of overburden","interactions":[{"subject":{"id":23739,"text":"ofr81535 - 1981 - Hydrology of the Ferron sandstone aquifer and effects of proposed surface-coal mining in Castle Valley, Utah","indexId":"ofr81535","publicationYear":"1981","noYear":false,"title":"Hydrology of the Ferron sandstone aquifer and effects of proposed surface-coal mining in Castle Valley, Utah"},"predicate":"SUPERSEDED_BY","object":{"id":3192,"text":"wsp2195 - 1983 - Hydrology of the Ferron Sandstone aquifer and effects of proposed surface-coal mining in Castle Valley, Utah, with a section on stratigraphy and a section on leaching of overburden","indexId":"wsp2195","publicationYear":"1983","noYear":false,"title":"Hydrology of the Ferron Sandstone aquifer and effects of proposed surface-coal mining in Castle Valley, Utah, with a section on stratigraphy and a section on leaching of overburden"},"id":1}],"lastModifiedDate":"2023-11-29T22:45:01.092093","indexId":"wsp2195","displayToPublicDate":"1983-01-01T00:00:00","publicationYear":"1983","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":"2195","title":"Hydrology of the Ferron Sandstone aquifer and effects of proposed surface-coal mining in Castle Valley, Utah, with a section on stratigraphy and a section on leaching of overburden","docAbstract":"<p>Coal in the Ferron Sandstone Member of the Mancos Shale of Cretaceous age has traditionally been mined by underground techniques in the Emery Coal Field in the southern end of Castle Valley in east-central Utah. However, approximately 99 million tons are recoverable by surface mining. Ground water in the Ferron is the sole source of supply for the town of Emery, but the aquifer is essentially untapped outside the Emery area.</p><p>The Ferron Sandstone Member crops out along the eastern edge of Castle Valley and generally dips 2 ? to 10 ? to the northwest. Sandstones in the Ferron are enclosed between relatively impermeable shale in the Tununk and Blue Gate Members of the Mancos Shale. Along the outcrop, the Ferron ranges in thickness from about 80 feet in the northern part of Castle Valley to 850 feet in the southern part. The Ferron also generally thickens in the subsurface downdip from the outcrop. Records from wells and test holes indicate that the full thickness of the Ferron is saturated with water in most areas downdip from the outcrop area.</p><p>Tests in the Emery area indicate that transmissivity of the Ferron sandstone aquifer ranges from about 200 to 700 feet squared per day where the Ferron is fully saturated. Aquifer transmissivity is greatest near the Paradise Valley-Joes Valley fault system where permeability has been increased by fracturing. Storage coefficient ranges from about 10 .6 to 10 -3 where the Ferron sandstone aquifer is confined and probably averages 5 x 10<sup>-2</sup> where it is unconfined.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Washington, D.C.","doi":"10.3133/wsp2195","collaboration":"Prepared in cooperation with the United States Bureau of Land Management","usgsCitation":"Lines, G.C., Morrissey, D.J., Ryer, T.A., and Fuller, R.H., 1983, Hydrology of the Ferron Sandstone aquifer and effects of proposed surface-coal mining in Castle Valley, Utah, with a section on stratigraphy and a section on leaching of overburden: U.S. Geological Survey Water Supply Paper 2195, Report: vi, 40 p.; 3 Plates: 17.00 x 27.20 inches, https://doi.org/10.3133/wsp2195.","productDescription":"Report: vi, 40 p.; 3 Plates: 17.00 x 27.20 inches","numberOfPages":"46","costCenters":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":30174,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/2195/plate-1.pdf","text":"Plate 1","linkFileType":{"id":1,"text":"pdf"},"linkHelpText":"Map showing location of selected wells, springs, and test holes in and near Castle Valley, Utah, where ground-water information is available, 1980"},{"id":30175,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/2195/plate-2.pdf","text":"Plate 2","linkFileType":{"id":1,"text":"pdf"},"linkHelpText":"Map showing the thickness of the Ferron sandstone member of the Mancos shale in Castle Valley, Utah"},{"id":423046,"rank":6,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_25538.htm","linkFileType":{"id":5,"text":"html"}},{"id":138109,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/2195/report-thumb.jpg"},{"id":30177,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/2195/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":30176,"rank":5,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/2195/plate-3.pdf","text":"Plate 3","linkFileType":{"id":1,"text":"pdf"},"linkHelpText":"Map showing the altitude of the top of the Ferron Sandstone member of the Mancos Shale in Castle Valley, Utah"}],"country":"United States","state":"Utah","otherGeospatial":"Castle Valley","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -110.5,\n              39.75\n            ],\n            [\n              -111.5,\n              39.75\n            ],\n            [\n              -111.5,\n              38.5\n            ],\n            [\n              -110.5,\n              38.5\n            ],\n            [\n              -110.5,\n              39.75\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aa7e4b07f02db667150","contributors":{"authors":[{"text":"Lines, Gregory C.","contributorId":50502,"corporation":false,"usgs":true,"family":"Lines","given":"Gregory","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":146406,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Morrissey, Daniel J.","contributorId":89875,"corporation":false,"usgs":true,"family":"Morrissey","given":"Daniel","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":146408,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Ryer, Thomas A.","contributorId":100359,"corporation":false,"usgs":true,"family":"Ryer","given":"Thomas","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":146409,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Fuller, Richard H.","contributorId":66236,"corporation":false,"usgs":true,"family":"Fuller","given":"Richard","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":146407,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":10046,"text":"ofr83216 - 1983 - Water resources and potential hydrologic effects of oil-shale development in the southeastern Uinta Basin, Utah and Colorado","interactions":[{"subject":{"id":10046,"text":"ofr83216 - 1983 - Water resources and potential hydrologic effects of oil-shale development in the southeastern Uinta Basin, Utah and Colorado","indexId":"ofr83216","publicationYear":"1983","noYear":false,"title":"Water resources and potential hydrologic effects of oil-shale development in the southeastern Uinta Basin, Utah and Colorado"},"predicate":"SUPERSEDED_BY","object":{"id":38571,"text":"pp1307 - 1984 - Water resources and potential hydrologic effects of oil-shale development in the southeastern Uinta Basin, Utah and Colorado","indexId":"pp1307","publicationYear":"1984","noYear":false,"title":"Water resources and potential hydrologic effects of oil-shale development in the southeastern Uinta Basin, Utah and Colorado"},"id":1}],"supersededBy":{"id":38571,"text":"pp1307 - 1984 - Water resources and potential hydrologic effects of oil-shale development in the southeastern Uinta Basin, Utah and Colorado","indexId":"pp1307","publicationYear":"1984","noYear":false,"title":"Water resources and potential hydrologic effects of oil-shale development in the southeastern Uinta Basin, Utah and Colorado"},"lastModifiedDate":"2023-07-14T15:19:32.387946","indexId":"ofr83216","displayToPublicDate":"1983-01-01T00:00:00","publicationYear":"1983","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":"83-216","title":"Water resources and potential hydrologic effects of oil-shale development in the southeastern Uinta Basin, Utah and Colorado","docAbstract":"<p>No abstract available.&nbsp;</p>","language":"English","publisher":"U.S. 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,{"id":21016,"text":"ofr8333 - 1983 - Hydrology of area 6, Eastern Coal Province, Maryland, West Virginia and Pennsylvania","interactions":[],"lastModifiedDate":"2023-03-29T19:53:53.242091","indexId":"ofr8333","displayToPublicDate":"1983-01-01T00:00:00","publicationYear":"1983","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":"83-33","title":"Hydrology of area 6, Eastern Coal Province, Maryland, West Virginia and Pennsylvania","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr8333","usgsCitation":"Staubitz, W., and Sobashinski, J.R., 1983, Hydrology of area 6, Eastern Coal Province, Maryland, West Virginia and Pennsylvania: U.S. Geological Survey Open-File Report 83-33, 131 p., https://doi.org/10.3133/ofr8333.","productDescription":"131 p.","costCenters":[],"links":[{"id":414908,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_13985.htm","linkFileType":{"id":5,"text":"html"}},{"id":153732,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1983/0033/report-thumb.jpg"},{"id":95445,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1983/0033/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Maryland, Pennsylvania, West Virginia","otherGeospatial":"Eastern Coal Province","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -79.488,\n              39.958\n            ],\n            [\n              -79.488,\n              39.071\n            ],\n            [\n              -78.558,\n              39.071\n            ],\n            [\n              -78.558,\n              39.958\n            ],\n            [\n              -79.488,\n              39.958\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a13e4b07f02db601f58","contributors":{"authors":[{"text":"Staubitz, W. W.","contributorId":73209,"corporation":false,"usgs":true,"family":"Staubitz","given":"W. W.","affiliations":[],"preferred":false,"id":183688,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Sobashinski, John R.","contributorId":16856,"corporation":false,"usgs":true,"family":"Sobashinski","given":"John","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":183687,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"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":47673,"text":"wri811182 - 1983 - Historical changes to Lake Washington and route of the Lake Washington Ship Canal, King County, Washington","interactions":[],"lastModifiedDate":"2022-08-29T13:55:24.290547","indexId":"wri811182","displayToPublicDate":"1983-01-01T00:00:00","publicationYear":"1983","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":"81-1182","title":"Historical changes to Lake Washington and route of the Lake Washington Ship Canal, King County, Washington","docAbstract":"<p><span>Lake Washington, in the midst of the greater Seattle metropolitan area of the Puget Sound region (fig. 1), is an exceptional commercial, recreational, and esthetic resource for the region . In the past 130 years, Lake Washington has been changed from a \" wild \" lake in a wilderness setting to a regulated lake surrounded by a growing metropolis--a transformation that provides an unusual opportunity to study changes to a lake's shoreline and hydrologic characteristics -resulting from urbanization.</span></p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri811182","usgsCitation":"Chrzastowski, M.J., 1983, Historical changes to Lake Washington and route of the Lake Washington Ship Canal, King County, Washington: U.S. Geological Survey Water-Resources Investigations Report 81-1182, Report: 9 p.; Plate: 33.53 x 57.12 inches, https://doi.org/10.3133/wri811182.","productDescription":"Report: 9 p.; Plate: 33.53 x 57.12 inches","numberOfPages":"9","costCenters":[],"links":[{"id":162048,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ofr811182.jpg"},{"id":405790,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1981/1182/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":405789,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1981/1182/report.pdf","text":"Report","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Washington","county":"King County","otherGeospatial":"Lake Washington","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -122.46871948242186,\n              47.30903424774781\n            ],\n            [\n              -122.46871948242186,\n              47.96510025611191\n            ],\n            [\n              -121.40991210937499,\n              47.96510025611191\n            ],\n            [\n              -121.40991210937499,\n              47.30903424774781\n            ],\n            [\n              -122.46871948242186,\n              47.30903424774781\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae1e4b07f02db6885d4","contributors":{"authors":[{"text":"Chrzastowski, Michael J.","contributorId":28643,"corporation":false,"usgs":true,"family":"Chrzastowski","given":"Michael","email":"","middleInitial":"J.","affiliations":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"preferred":false,"id":235985,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"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              -97.26109805609099,\n              40.4570069139221\n            ],\n            [\n              -95.81030659908853,\n              40.76732232232118\n            ],\n            [\n              -96.23779355385292,\n              42.11319257035615\n            ],\n            [\n              -96.82014771860239,\n              42.56341058787868\n            ],\n            [\n              -102.92550353390914,\n              42.57699651556365\n            ],\n            [\n              -105.05465161293671,\n              43.44397434759969\n            ],\n            [\n              -107.66814025908258,\n              43.491370497698284\n            ],\n            [\n              -107.35007550814393,\n              42.01749793928926\n            ],\n            [\n              -105.81098030047286,\n              39.62779224334653\n            ],\n            [\n              -105.06337546697512,\n              39.229893136534116\n            ]\n          ]\n        ],\n        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,{"id":28089,"text":"wri834053 - 1983 - Ground water in the northeast part of Twentynine Palms Marine Corps Base, Bagdad area, California","interactions":[],"lastModifiedDate":"2023-04-11T19:27:17.935961","indexId":"wri834053","displayToPublicDate":"1983-01-01T00:00:00","publicationYear":"1983","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":"83-4053","title":"Ground water in the northeast part of Twentynine Palms Marine Corps Base, Bagdad area, California","docAbstract":"<p>The hydrologic characteristics of the Bagdad area, in the northeast part of Twentynine Palms Marine Corps Base, were investigated to determine the feasibility of obtaining a supply of ground water. Five test holes were drilled and three of these were completed with 6-inch casings. Ground water in the eastern part of the study area is high in dissolved solids; water from well 5N/11E-36H1 contains 252,000 milligrams per liter of dissolved solids, and well 4N/12E-7R1 contains 21,800 milligrams per liter of dissolved solids. The dissolved-solids concentration in water from the test wells on the west side of Ludlow fault is much lower; the dissolved solids in water from the three test wells ranges from 669 to 961 milligrams per liter. The recommended limits for chloride and fluoride were exceeded in water from test well 4N/10E-21K1, arsenic and fluoride in water from well 5N/9E-3B1, and chloride in water from test well 6N/9E-34F1. An estimated 640,000 acre-feet of water is stored in the alluvium west of the Ludlow fault, sufficient to provide for several small diameter wells for many years.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri834053","usgsCitation":"Koehler, J.H., 1983, Ground water in the northeast part of Twentynine Palms Marine Corps Base, Bagdad area, California: U.S. Geological Survey Water-Resources Investigations Report 83-4053, iv, 15 p., https://doi.org/10.3133/wri834053.","productDescription":"iv, 15 p.","costCenters":[],"links":[{"id":415591,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_35692.htm","linkFileType":{"id":5,"text":"html"}},{"id":56908,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1983/4053/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":123623,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1983/4053/report-thumb.jpg"}],"country":"United States","state":"Calilfornia","otherGeospatial":"Twentynine Palms Marine Corps Base","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -116.74714785522053,\n              34.772980861725955\n            ],\n            [\n              -116.74714785522053,\n              34.196058657436936\n            ],\n            [\n              -115.70337642189573,\n              34.196058657436936\n            ],\n            [\n              -115.70337642189573,\n              34.772980861725955\n            ],\n            [\n              -116.74714785522053,\n              34.772980861725955\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ab0e4b07f02db66d7b2","contributors":{"authors":[{"text":"Koehler, J. H.","contributorId":108108,"corporation":false,"usgs":true,"family":"Koehler","given":"J.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":199198,"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":68293,"text":"ha644 - 1982 - Geohydrology of the Standing Rock Indian Reservation, North and South Dakota","interactions":[],"lastModifiedDate":"2018-03-08T13:17:42","indexId":"ha644","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":"644","title":"Geohydrology of the Standing Rock Indian Reservation, North and South Dakota","docAbstract":"<p>Effective improvement of economic and social conditions of Indians living on the Standing Rock Indian Reservation has been hampered by lack of adequate and reliable information about the quantity and quality of water supplies available for development.&nbsp; Compounding the problem is the recent filling of Oahe Reservoir (now Lake Oahe), which flooded about 55,000 acres of Indian land, and the consequent relocation of many residents.&nbsp; This report summarizes the results of a water-resources study made at the request of the U.S. Bureau of Indian Affairs.&nbsp; It is intended to provide some of the needed information on water supplies that could be used to alleviate the problems mentioned.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ha644","usgsCitation":"Howells, L.W., 1982, Geohydrology of the Standing Rock Indian Reservation, North and South Dakota: U.S. Geological Survey Hydrologic Atlas 644, 5 Plates, https://doi.org/10.3133/ha644.","productDescription":"5 Plates","costCenters":[{"id":478,"text":"North Dakota Water Science Center","active":true,"usgs":true},{"id":34685,"text":"Dakota Water Science Center","active":true,"usgs":true}],"links":[{"id":89717,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/644/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":89718,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/644/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":89716,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/644/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":89719,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/644/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":89720,"rank":404,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/644/plate-5.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":186623,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"scale":"250000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -102,45.483333333333334 ], [ -102,46.5 ], [ -100.41666666666667,46.5 ], [ -100.41666666666667,45.483333333333334 ], [ -102,45.483333333333334 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1be4b07f02db6a88bf","contributors":{"authors":[{"text":"Howells, Lewis W.","contributorId":17600,"corporation":false,"usgs":true,"family":"Howells","given":"Lewis","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":277977,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"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":68190,"text":"ha656 - 1982 - Flood of May 24-25, 1981, in the Austin, Texas, metropolitan area","interactions":[],"lastModifiedDate":"2016-08-05T12:04:49","indexId":"ha656","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":"656","title":"Flood of May 24-25, 1981, in the Austin, Texas, metropolitan area","docAbstract":"<p>Hydrologic data pertaining to the magnitude and areal extent of flooding that occurred on May 24-25, 1981, along Shoal, Walnut, and Little Walnut Creeks in the Austin, Texas, metropolitan area are presented in this atlas. &nbsp;The flood boundary maps and other flood data provide a technical data base for land-use planning.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ha656","usgsCitation":"Massey, B., Reeves, W., and Lear, W., 1982, Flood of May 24-25, 1981, in the Austin, Texas, metropolitan area: U.S. Geological Survey Hydrologic Atlas 656, 2 Plates: 34.50 x 32.25 inches and 34.50 x 32.25 inches, https://doi.org/10.3133/ha656.","productDescription":"2 Plates: 34.50 x 32.25 inches and 34.50 x 32.25 inches","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"links":[{"id":185565,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ha656.PNG"},{"id":89517,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/656/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":89518,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/656/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"20000","country":"United States","state":"Texas","city":"Austin","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f2e4b07f02db5eed33","contributors":{"authors":[{"text":"Massey, B.C.","contributorId":102483,"corporation":false,"usgs":true,"family":"Massey","given":"B.C.","email":"","affiliations":[],"preferred":false,"id":277810,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Reeves, W.E.","contributorId":79518,"corporation":false,"usgs":true,"family":"Reeves","given":"W.E.","email":"","affiliations":[],"preferred":false,"id":277809,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Lear, W.A.","contributorId":46617,"corporation":false,"usgs":true,"family":"Lear","given":"W.A.","email":"","affiliations":[],"preferred":false,"id":277808,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"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":68251,"text":"ha658 - 1982 - Dissolved solids and sodium in water from the High Plains aquifer in parts of Colorado, Kansas, Nebraska, New Mexico, Oklahoma, South Dakota, Texas, and Wyoming","interactions":[],"lastModifiedDate":"2012-02-02T00:13:21","indexId":"ha658","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":"658","title":"Dissolved solids and sodium in water from the High Plains aquifer in parts of Colorado, Kansas, Nebraska, New Mexico, Oklahoma, South Dakota, Texas, and Wyoming","docAbstract":"In 1978, the U.S. Geological Survey initiated a 5-year study of the High Plains regional aquifer to provide: (1) Hydrologic information needed to evaluate the effects of continued ground-water development; and (2) computer models to predict aquifer response to changes in ground-water development. The plan of study for the High Plains Regional Aquifer-System Analysis was described by Weeks (1978). A description of the High Plains aquifer and a map of the 1978 water table were presented by Gutentag and Weeks (1980). Maps of the bedrock geology, altitude of aquifer base, and saturated thickness of the High Plains aquifer were published by Weeks and Gutentag (1981). Water-level and saturated-thickness changes, from predevelopment to 1980, were mapped by Luckey, Gutentag, and Weeks (1981). This report describes the areal distribution of dissolved solids and sodium in the water of the High Plains aquifer. Data used in this study were provided by the U.S. Geological Survey and State agencies in each of the eight States in the High Plains. Their contribution is an integral part of this investigation.","language":"ENGLISH","doi":"10.3133/ha658","usgsCitation":"Krothe, N.C., Oliver, J.W., and Weeks, J., 1982, Dissolved solids and sodium in water from the High Plains aquifer in parts of Colorado, Kansas, Nebraska, New Mexico, Oklahoma, South Dakota, Texas, and Wyoming: U.S. Geological Survey Hydrologic Atlas 658, 2 maps :col. ;54 x 38 cm., on sheets 74 x 104 cm., folded in envelope 30 x 24 cm., https://doi.org/10.3133/ha658.","productDescription":"2 maps :col. ;54 x 38 cm., on sheets 74 x 104 cm., folded in envelope 30 x 24 cm.","costCenters":[],"links":[{"id":189677,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":89636,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/658/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":89637,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/658/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a81e4b07f02db64a250","contributors":{"authors":[{"text":"Krothe, Noel C.","contributorId":41466,"corporation":false,"usgs":true,"family":"Krothe","given":"Noel","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":277911,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Oliver, Joseph W.","contributorId":77970,"corporation":false,"usgs":true,"family":"Oliver","given":"Joseph","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":277912,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Weeks, John B.","contributorId":36123,"corporation":false,"usgs":true,"family":"Weeks","given":"John B.","affiliations":[],"preferred":false,"id":277910,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"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":56645,"text":"fwsobs82_09 - 1982 - Ecoregion, land-surface form, and hydrologic unit maps of the U.S","interactions":[],"lastModifiedDate":"2012-02-02T00:12:04","indexId":"fwsobs82_09","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":"82/09","title":"Ecoregion, land-surface form, and hydrologic unit maps of the U.S","language":"ENGLISH","publisher":"U.S. Fish and Wildlife Service","usgsCitation":"Bailey, R.G., and Cushwa, C.T., 1982, Ecoregion, land-surface form, and hydrologic unit maps of the U.S: FWS/OBS 82/09, 3 maps on 3 sheets : one col.; sheets 62 x 94 cm. or smaller, folded to 28 x 23 cm., in envelope 30 x 24 cm.","productDescription":"3 maps on 3 sheets : one col.; sheets 62 x 94 cm. or smaller, folded to 28 x 23 cm., in envelope 30 x 24 cm.","costCenters":[],"links":[{"id":180939,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a4be4b07f02db6259da","contributors":{"authors":[{"text":"Bailey, Robert G. (compiler)","contributorId":29061,"corporation":false,"usgs":true,"family":"Bailey","given":"Robert","suffix":"(compiler)","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":255589,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Cushwa, Charles T.","contributorId":44207,"corporation":false,"usgs":true,"family":"Cushwa","given":"Charles","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":255590,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"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}]}}
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