This report contains records of water-level measurements from wells in Arkansas that comprise the statewide observation-well network maintained by the U.S. Geological Survey, in cooperation with the Arkansas Geological Commission. The observation-well network is designed to provide data for evaluation of the regional trend of water-level changes in each of the principal water-bearing formations (aquifers) that are tapped by wells in the State.
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\"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b01e4b07f02db698598","contributors":{"authors":[{"text":"Edds, Joe","contributorId":48532,"corporation":false,"usgs":true,"family":"Edds","given":"Joe","email":"","affiliations":[],"preferred":false,"id":158170,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":8537,"text":"ofr82125 - 1981 - Salinity and temperature measurements in San Francisco Bay waters, 1980","interactions":[],"lastModifiedDate":"2016-07-27T11:44:01","indexId":"ofr82125","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1981","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":"82-125","title":"Salinity and temperature measurements in San Francisco Bay waters, 1980","docAbstract":"Measurements of salinity and temperature in waters of the San Francisco Bay estuarine system are presented. Sampling was conducted at selected locations (stations) and depths over the period between January-December 1980 at approximately two week intervals. Stations were located in deep channels and adjacent shallow water areas from Calaveras Point in South San Francisco Bay to the town of Rio Vista on the Sacramento River and to the Three-Mile Slough on the San Joaquin River. Numerical values of salinity, temperature, and station locations are tabulated. Contour maps of deep-channel salinity and temperature are presented and the analytical methods are briefly described.
","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr82125","usgsCitation":"Dedini, L., Schemel, L., and Tembreull, M., 1981, Salinity and temperature measurements in San Francisco Bay waters, 1980: U.S. Geological Survey Open-File Report 82-125, 130 p. :maps ;28 cm., https://doi.org/10.3133/ofr82125.","productDescription":"130 p. :maps ;28 cm.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":552,"text":"San Francisco Bay-Delta","active":false,"usgs":true},{"id":5079,"text":"Pacific Regional Director's Office","active":true,"usgs":true}],"links":[{"id":141672,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0125/report-thumb.jpg"},{"id":36116,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0125/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0ee4b07f02db5fdf97","contributors":{"authors":[{"text":"Dedini, L.A.","contributorId":54996,"corporation":false,"usgs":true,"family":"Dedini","given":"L.A.","affiliations":[],"preferred":false,"id":157898,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Schemel, L. E.","contributorId":89529,"corporation":false,"usgs":true,"family":"Schemel","given":"L. E.","affiliations":[],"preferred":false,"id":157899,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Tembreull, M.A.","contributorId":27448,"corporation":false,"usgs":true,"family":"Tembreull","given":"M.A.","email":"","affiliations":[],"preferred":false,"id":157897,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":9275,"text":"ofr8067 - 1981 - Digital models of ground-water flow in the Cape Cod aquifer system, Massachusetts","interactions":[{"subject":{"id":9275,"text":"ofr8067 - 1981 - Digital models of ground-water flow in the Cape Cod aquifer system, Massachusetts","indexId":"ofr8067","publicationYear":"1981","noYear":false,"title":"Digital models of ground-water flow in the Cape Cod aquifer system, Massachusetts"},"predicate":"SUPERSEDED_BY","object":{"id":1756,"text":"wsp2209 - 1985 - Digital models of ground-water flow in the Cape Cod aquifer system, Massachusetts","indexId":"wsp2209","publicationYear":"1985","noYear":false,"title":"Digital models of ground-water flow in the Cape Cod aquifer system, Massachusetts"},"id":1}],"supersededBy":{"id":1756,"text":"wsp2209 - 1985 - Digital models of ground-water flow in the Cape Cod aquifer system, Massachusetts","indexId":"wsp2209","publicationYear":"1985","noYear":false,"title":"Digital models of ground-water flow in the Cape Cod aquifer system, Massachusetts"},"lastModifiedDate":"2022-10-11T21:12:13.733432","indexId":"ofr8067","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1981","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":"80-67","title":"Digital models of ground-water flow in the Cape Cod aquifer system, Massachusetts","docAbstract":"The Cape Cod aquifer system was simulated with three-dimensional finite-difference ground-water-flow models. Five areas were modeled to provide tools that can be used to evaluate the hydrologic impacts of regional water development and waste disposal.
The model boundaries were selected to represent the natural hydrologic boundaries of the aquifer. The boundary between fresh and saline ground water is treated as an interface along which there is no dispersion. The saline-water zone is treated as static (nonflowing).
Comparisons of calculated and observed values of head, position of the boundary between fresh and saline water, and ground-water discharge at locations where data are available indicate that the simulated ground-water reservoirs generally agree with field conditions.
Model analyses indicate that the total steady-state freshwater-flow rate through the five modeled areas is approximately 412 cubic feet per second.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr8067","collaboration":"Prepared in cooperation with the Commonwealth of Massachusetts, Water Resources Commission Barnstable County, and the National Park Service","usgsCitation":"Guswa, J.H., and LeBlanc, D.R., 1981, Digital models of ground-water flow in the Cape Cod aquifer system, Massachusetts: U.S. Geological Survey Open-File Report 80-67, vi, 128 p., https://doi.org/10.3133/ofr8067.","productDescription":"vi, 128 p.","costCenters":[],"links":[{"id":408184,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1980/0067/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":140893,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1980/0067/report-thumb.jpg"}],"country":"United States","state":"Massachusetts","otherGeospatial":"Cape Cod","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -70.53497314453125,\n 41.549700145132725\n ],\n [\n -69.91973876953125,\n 41.549700145132725\n ],\n [\n -69.91973876953125,\n 42.11248648904184\n ],\n [\n -70.53497314453125,\n 42.11248648904184\n ],\n [\n -70.53497314453125,\n 41.549700145132725\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a91e4b07f02db656d6c","contributors":{"authors":[{"text":"Guswa, John H.","contributorId":97881,"corporation":false,"usgs":true,"family":"Guswa","given":"John","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":159403,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"LeBlanc, Denis R. 0000-0002-4646-2628 dleblanc@usgs.gov","orcid":"https://orcid.org/0000-0002-4646-2628","contributorId":1696,"corporation":false,"usgs":true,"family":"LeBlanc","given":"Denis","email":"dleblanc@usgs.gov","middleInitial":"R.","affiliations":[{"id":466,"text":"New England Water Science Center","active":true,"usgs":true}],"preferred":true,"id":159402,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":8900,"text":"ofr81342 - 1981 - Water resources of the Santa Ysabel and Mesa Grande Indian Reservations, San Diego County, California","interactions":[],"lastModifiedDate":"2012-02-02T00:06:16","indexId":"ofr81342","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1981","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":"81-342","title":"Water resources of the Santa Ysabel and Mesa Grande Indian Reservations, San Diego County, California","docAbstract":"The Santa Ysabel (consisting of three tracts) and Mesa Grande Indian Reservations are in north-central San Diego County, Calif. On both reservations fractured and weathered igneous and metamorphic rocks and alluvium are water bearing; however, no wells are known to derive their water entirely from alluvium. Well yields range from 2.5 to 250 gallons per minute. Springs occur where saturated fractured or weathered material intersects the land surface. Spring discharge ranged from 0 gallon per minute (November 1979) to 9.4 gallons per minute (November 1979). Few data are available for the surface water characteristics of the study area. One-time measurements of discharge at selected stream sites were made in late November 1979 and late May 1980; discharges ranged from less than 0.01 cubic foot per second to an estimated 3 cubic feet per second. Further study of the surface-water systems would provide a basis for estimating their development potential. The existing water-supply development on the Santa Ysabel Indian Reservation is adequate for the present residents. The Mesa Grande reservation was unoccupied in 1952, was reportedly unoccupied in November 1979, and has no developed water supply. Additional water can be developed for both reservations from the igneous and metamorphic rock, from presently undeveloped springs, and from perennial reaches of the larger streams. Except for excessive iron and sodium at some ground-water sites and excessive sodium at a few surface-water sites, the water is of suitable quality for domestic and agricultural use. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr81342","usgsCitation":"Freckleton, J.R., 1981, Water resources of the Santa Ysabel and Mesa Grande Indian Reservations, San Diego County, California (WRI/OFR): U.S. Geological Survey Open-File Report 81-342, iv, 31 p., 1 over-size sheet ;28 cm., https://doi.org/10.3133/ofr81342.","productDescription":"iv, 31 p., 1 over-size sheet ;28 cm.","costCenters":[],"links":[{"id":141704,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1981/0342/report-thumb.jpg"},{"id":36498,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1981/0342/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":36499,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1981/0342/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"edition":"WRI/OFR","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f4e4b07f02db5f036f","contributors":{"authors":[{"text":"Freckleton, John R.","contributorId":93051,"corporation":false,"usgs":true,"family":"Freckleton","given":"John","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":158515,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":10038,"text":"ofr81689 - 1981 - Plan of study for the regional aquifer-system analysis of the Snake River plain, Idaho and eastern Oregon","interactions":[],"lastModifiedDate":"2012-02-02T00:06:35","indexId":"ofr81689","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1981","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":"81-689","title":"Plan of study for the regional aquifer-system analysis of the Snake River plain, Idaho and eastern Oregon","docAbstract":"The 15,600-square-mile Snake River Plain is largely in southern Idaho and includes one of the Nation 's major regional aquifers. A comprehensive investigation of the area 's ground-water resources will be made as part of the U.S. Geological Survey 's Regional Aquifer-System Analysis (RASA) program. Basaltic and sedimentary rocks in the Snake River Plain yield large quantities of water that are vital to the area 's agricultural economy. Basaltic rocks predominate in the eastern Snake River Plain and have especially high water-yielding capabilities. Surface water, largely from the Snake River, is extensively used for irrigation and is a major source of recharge to the ground-water system. Springs issuing from basaltic rocks that form the Snake River Canyon wall near Twin Falls are the major points of ground-water discharge. Increased use of ground water for irrigation is causing concern as to the effect of large-scale withdrawals on spring flow. Ground-water flow models will be used to improve understanding of the hydrologic system, and, if feasible, to aid in evaluating management alternatives. Ground-water quality will be defined and geochemical techniques used to determine the effects of water-rock reactions on water quality. Several reports are planned on different phases of the project, concluding with a summary report. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr81689","usgsCitation":"Lindholm, G.F., 1981, Plan of study for the regional aquifer-system analysis of the Snake River plain, Idaho and eastern Oregon: U.S. Geological Survey Open-File Report 81-689, 23 p. :maps ;28 cm., https://doi.org/10.3133/ofr81689.","productDescription":"23 p. :maps ;28 cm.","costCenters":[],"links":[{"id":144871,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1981/0689/report-thumb.jpg"},{"id":37886,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1981/0689/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aa9e4b07f02db668077","contributors":{"authors":[{"text":"Lindholm, Gerald F.","contributorId":18374,"corporation":false,"usgs":true,"family":"Lindholm","given":"Gerald","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":160714,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":8705,"text":"ofr81904 - 1981 - Identification codes for organizations listed in computerized data systems of the U.S. Geological Survey","interactions":[{"subject":{"id":8705,"text":"ofr81904 - 1981 - Identification codes for organizations listed in computerized data systems of the U.S. Geological Survey","indexId":"ofr81904","publicationYear":"1981","noYear":false,"title":"Identification codes for organizations listed in computerized data systems of the U.S. Geological Survey"},"predicate":"SUPERSEDED_BY","object":{"id":8704,"text":"ofr82921 - 1982 - Identification codes for organizations listed in computerized data systems of the U.S. Geological Survey","indexId":"ofr82921","publicationYear":"1982","noYear":false,"title":"Identification codes for organizations listed in computerized data systems of the U.S. Geological Survey"},"id":1},{"subject":{"id":57096,"text":"ofr80555 - 1980 - Identification codes for organizations listed in computerized data systems of the U. S. Geological Survey","indexId":"ofr80555","publicationYear":"1980","noYear":false,"title":"Identification codes for organizations listed in computerized data systems of the U. S. Geological Survey"},"predicate":"SUPERSEDED_BY","object":{"id":8705,"text":"ofr81904 - 1981 - Identification codes for organizations listed in computerized data systems of the U.S. Geological Survey","indexId":"ofr81904","publicationYear":"1981","noYear":false,"title":"Identification codes for organizations listed in computerized data systems of the U.S. Geological Survey"},"id":2}],"supersededBy":{"id":8704,"text":"ofr82921 - 1982 - Identification codes for organizations listed in computerized data systems of the U.S. Geological Survey","indexId":"ofr82921","publicationYear":"1982","noYear":false,"title":"Identification codes for organizations listed in computerized data systems of the U.S. Geological Survey"},"lastModifiedDate":"2012-02-02T00:06:16","indexId":"ofr81904","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1981","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":"81-904","title":"Identification codes for organizations listed in computerized data systems of the U.S. Geological Survey","docAbstract":"This report contains codes for the identification of public and private organizations listed in computerized data systems. These codes are used by the U.S. Geological Survey 's National Water Data Exchange (NAWDEX), National Water Data Storage and Retrieval System (WATSTORE), National Cartographic Information Center (NCIC), and Office of Water Data Coordination (OWDC). The format structure of the codes is discussed and instructions are given for requesting new codes. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr81904","usgsCitation":"Edwards, M.D., and Myers, B.M., 1981, Identification codes for organizations listed in computerized data systems of the U.S. Geological Survey: U.S. Geological Survey Open-File Report 81-904, vi, 108 p. ;28 cm., https://doi.org/10.3133/ofr81904.","productDescription":"vi, 108 p. ;28 cm.","costCenters":[],"links":[{"id":94867,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1981/0904/report.pdf","size":"3989","linkFileType":{"id":1,"text":"pdf"}},{"id":141834,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1981/0904/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a09e4b07f02db5faac4","contributors":{"authors":[{"text":"Edwards, Melvin D.","contributorId":94305,"corporation":false,"usgs":true,"family":"Edwards","given":"Melvin","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":158186,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Myers, Beverly M.","contributorId":31733,"corporation":false,"usgs":true,"family":"Myers","given":"Beverly","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":158185,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":8234,"text":"ofr81412 - 1981 - Selected hydrologic and climatologic data from the Prairie Dog Creek Basin, southeastern Montana, water year 1979","interactions":[],"lastModifiedDate":"2022-11-04T17:28:11.083743","indexId":"ofr81412","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1981","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":"81-412","title":"Selected hydrologic and climatologic data from the Prairie Dog Creek Basin, southeastern Montana, water year 1979","docAbstract":"Hydrologic and climatologic data are being collected in a 19-square-mile (49-square-kilometer) basin in southeastern Montana to provide a base for development, calibration, and verification of a precipitation-runoff model. The study area and data-collection stations within the area are shown on a map. A summary of data collected at each station during the first year, beginning in October 1978, is provided in tables. The data include precipitation, snow depth and water content, air temperature, relative humidity, wind run, solar radiation, soil temperature and moisture, stream discharge, chemical analyses of water, and sediment content.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr81412","collaboration":"Prepared in cooperation with the U.S. Bureau of Land Management","usgsCitation":"Cary, L.E., and Johnson, J.D., 1981, Selected hydrologic and climatologic data from the Prairie Dog Creek Basin, southeastern Montana, water year 1979: U.S. Geological Survey Open-File Report 81-412, iv, 73 p., https://doi.org/10.3133/ofr81412.","productDescription":"iv, 73 p.","costCenters":[],"links":[{"id":409169,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1981/0412/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":141308,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1981/0412/report-thumb.jpg"}],"country":"United States","state":"Montana","otherGeospatial":"Prairie Dog Creek Basin","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -107.86376953125,\n 44.99588261816546\n ],\n [\n -106.512451171875,\n 44.99588261816546\n ],\n [\n -106.512451171875,\n 45.99314540468519\n ],\n [\n -107.86376953125,\n 45.99314540468519\n ],\n [\n -107.86376953125,\n 44.99588261816546\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a06e4b07f02db5f8ec7","contributors":{"authors":[{"text":"Cary, Lawrence E.","contributorId":43764,"corporation":false,"usgs":true,"family":"Cary","given":"Lawrence","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":157393,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Johnson, Joel D.","contributorId":60212,"corporation":false,"usgs":true,"family":"Johnson","given":"Joel","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":157394,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":10640,"text":"ofr81922 - 1981 - Hydrologic data for urban studies in the San Antonio, Texas, metropolitan area, 1978","interactions":[],"lastModifiedDate":"2022-11-16T19:38:09.654274","indexId":"ofr81922","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1981","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":"81-922","title":"Hydrologic data for urban studies in the San Antonio, Texas, metropolitan area, 1978","docAbstract":"Hydrologic investigations of urban drainage basins in Texas were begun by the U.S. Geological Survey in 1954. These studies are now in progress in Austin, Houston, and San Antonio. Studies were completed in the Fort Worth metropolitan area at the end of the 1977 water year, and in the Dallas metropolitan area at the end of the 1979 water year.
The Geological Survey, in cooperation with the Texas Department of Water Resources, expanded the existing streamflow network in the San Antonio metropolitan area in May 1968 to begin urban hydrology studies in this area. In September 1968, the program was further expanded to include the collection of water-quality data.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr81922","collaboration":"Prepared in cooperation with the Texas Department of Water Resources","usgsCitation":"Perez, R., 1981, Hydrologic data for urban studies in the San Antonio, Texas, metropolitan area, 1978: U.S. Geological Survey Open-File Report 81-922, 91 p., https://doi.org/10.3133/ofr81922.","productDescription":"91 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"links":[{"id":409400,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1981/0922/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":144071,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1981/0922/report-thumb.jpg"}],"country":"United States","state":"Texas","city":"San Antonio","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -98.8165283203125,\n 29.123373210819224\n ],\n [\n -98.19580078125,\n 29.123373210819224\n ],\n [\n -98.19580078125,\n 29.699982298744377\n ],\n [\n -98.8165283203125,\n 29.699982298744377\n ],\n [\n -98.8165283203125,\n 29.123373210819224\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a1be4b07f02db6079f2","contributors":{"authors":[{"text":"Perez, Roberto","contributorId":97114,"corporation":false,"usgs":true,"family":"Perez","given":"Roberto","email":"","affiliations":[],"preferred":false,"id":161726,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":11172,"text":"ofr81751 - 1981 - Description and preliminary interpretation of core CL-80-1, Clear Lake, Lake County, California","interactions":[],"lastModifiedDate":"2022-11-04T19:41:39.249905","indexId":"ofr81751","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1981","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":"81-751","title":"Description and preliminary interpretation of core CL-80-1, Clear Lake, Lake County, California","docAbstract":"Coring operations were conducted in the west basin of Clear Lake during July and August 1980 to produce a regional Quaternary reference section. A 177-m-long core (CL-80-1) was taken, which also augments and extends a previous study of eight shorter cores collected from Clear Lake in 1973. Core CL-80-1 was continuously cored in 7.5 m of water, and 66.5 percent recovery was achieved. The sediments are composed primarily of clayey and silty sapropelic mud similar to those presently being deposited in the lake, and are interbedded with local coarse sand and gravel deposits and thin volcanic ash beds. Coring was terminated when coarse rounded gravel and cobbles of Franciscan assemblage lithology were encountered. The location of core CL-80-1 is between two other core sites of the 1973 series of cores, one of which (CL-73-4) is 115 m long and contains a well-defined, uninterrupted pollen and physical stratigraphic record from the present to about 130,000 years ago. Paleomagnetic and preliminary pollen analyses of core CL-80-1 are complete and comparison of these results with those of core CL-73-4 suggest that the new core represents a record from the present to about 175,000 years ago.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr81751","usgsCitation":"Sims, J.D., Rymer, M.J., and Perkins, J.A., 1981, Description and preliminary interpretation of core CL-80-1, Clear Lake, Lake County, California: U.S. Geological Survey Open-File Report 81-751, 175 p., https://doi.org/10.3133/ofr81751.","productDescription":"175 p.","costCenters":[],"links":[{"id":409182,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1981/0751/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":143943,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1981/0751/report-thumb.jpg"}],"country":"United States","state":"California","county":"Lake County","otherGeospatial":"Clear Lake","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -121.25747680664064,\n 41.78360106648078\n ],\n [\n -121.01852416992186,\n 41.78360106648078\n ],\n [\n -121.01852416992186,\n 41.96663812286332\n ],\n [\n -121.25747680664064,\n 41.96663812286332\n ],\n [\n -121.25747680664064,\n 41.78360106648078\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ab0e4b07f02db66ddb4","contributors":{"authors":[{"text":"Sims, John D.","contributorId":60202,"corporation":false,"usgs":true,"family":"Sims","given":"John","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":162669,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Rymer, Michael J. mrymer@usgs.gov","contributorId":1522,"corporation":false,"usgs":true,"family":"Rymer","given":"Michael","email":"mrymer@usgs.gov","middleInitial":"J.","affiliations":[{"id":237,"text":"Earthquake Science Center","active":true,"usgs":true}],"preferred":true,"id":162668,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Perkins, James A.","contributorId":95481,"corporation":false,"usgs":true,"family":"Perkins","given":"James","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":162670,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":9299,"text":"ofr8276 - 1981 - Velocity observations of the Chattahoochee River at Atlanta, Georgia, September 28, 1981","interactions":[],"lastModifiedDate":"2020-06-15T15:02:58.728525","indexId":"ofr8276","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1981","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":"82-76","title":"Velocity observations of the Chattahoochee River at Atlanta, Georgia, September 28, 1981","docAbstract":"No abstract available.
","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr8276","usgsCitation":"Hale, T., 1981, Velocity observations of the Chattahoochee River at Atlanta, Georgia, September 28, 1981: U.S. Geological Survey Open-File Report 82-76, iv, 64 p., https://doi.org/10.3133/ofr8276.","productDescription":"iv, 64 p.","costCenters":[{"id":13634,"text":"South Atlantic Water Science Center","active":true,"usgs":true}],"links":[{"id":375573,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0076/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":141225,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0076/report-thumb.jpg"}],"country":"United States","state":"Georgia","city":"Atlanta","otherGeospatial":"Chattahoochee River","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -84.56794738769531,\n 33.736902846767954\n ],\n [\n -84.43748474121094,\n 33.736902846767954\n ],\n [\n -84.43748474121094,\n 33.866424604507536\n ],\n [\n -84.56794738769531,\n 33.866424604507536\n ],\n [\n -84.56794738769531,\n 33.736902846767954\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a13e4b07f02db6022d6","contributors":{"authors":[{"text":"Hale, T.W.","contributorId":43763,"corporation":false,"usgs":true,"family":"Hale","given":"T.W.","email":"","affiliations":[],"preferred":false,"id":159444,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":9261,"text":"ofr80565 - 1981 - A qualitative appraisal of the hydrology of the Yemen Arab Republic from Landsat images","interactions":[{"subject":{"id":9261,"text":"ofr80565 - 1981 - A qualitative appraisal of the hydrology of the Yemen Arab Republic from Landsat images","indexId":"ofr80565","publicationYear":"1981","noYear":false,"title":"A qualitative appraisal of the hydrology of the Yemen Arab Republic from Landsat images"},"predicate":"SUPERSEDED_BY","object":{"id":1726,"text":"wsp1757P - 1984 - A qualitative appraisal of the hydrology of the Yemen Arab Republic from Landsat images","indexId":"wsp1757P","publicationYear":"1984","noYear":false,"chapter":"P","title":"A qualitative appraisal of the hydrology of the Yemen Arab Republic from Landsat images"},"id":1}],"supersededBy":{"id":1726,"text":"wsp1757P - 1984 - A qualitative appraisal of the hydrology of the Yemen Arab Republic from Landsat images","indexId":"wsp1757P","publicationYear":"1984","noYear":false,"title":"A qualitative appraisal of the hydrology of the Yemen Arab Republic from Landsat images"},"lastModifiedDate":"2022-08-02T18:34:12.527252","indexId":"ofr80565","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1981","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":"80-565","title":"A qualitative appraisal of the hydrology of the Yemen Arab Republic from Landsat images","docAbstract":"Landsat-1 and Landsat-2 images were analyzed in June 1976 to describe the flow regimens of streams and the regional distribution of vegetation in the Yemen Arab Republic (YAR). The findings provide a factual basis for planning a surface-water data collection program, and for preparing maps of plant distribution and agricultural land use. They lay the foundation for modernized water development, and for effecting a program of country-wide water management in the YAR.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr80565","collaboration":"Prepared in cooperation with the Yemen Arab Republic under the auspices of the U.S. Agency for International Development","usgsCitation":"Grolier, M.J., Tibbitts, G., and Ibrahim, M., 1981, A qualitative appraisal of the hydrology of the Yemen Arab Republic from Landsat images: U.S. Geological Survey Open-File Report 80-565, Report: viii, 103 p.; 1 Plate: 35.38 x 50.43 inches, https://doi.org/10.3133/ofr80565.","productDescription":"Report: viii, 103 p.; 1 Plate: 35.38 x 50.43 inches","costCenters":[],"links":[{"id":404682,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1980/0565/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":143585,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1980/0565/report-thumb.jpg"},{"id":404680,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1980/0565/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"Yemen Arab Republic","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n 41.748046875,\n 12.382928338487396\n ],\n [\n 54.228515625,\n 12.382928338487396\n ],\n [\n 54.228515625,\n 18.22935133838668\n ],\n [\n 41.748046875,\n 18.22935133838668\n ],\n [\n 41.748046875,\n 12.382928338487396\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1ae4b07f02db6a875d","contributors":{"authors":[{"text":"Grolier, Maurice J.","contributorId":98292,"corporation":false,"usgs":true,"family":"Grolier","given":"Maurice","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":159378,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Tibbitts, G. Chase","contributorId":79453,"corporation":false,"usgs":true,"family":"Tibbitts","given":"G. Chase","affiliations":[],"preferred":false,"id":159377,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Ibrahim, M.M.","contributorId":33339,"corporation":false,"usgs":true,"family":"Ibrahim","given":"M.M.","email":"","affiliations":[],"preferred":false,"id":159376,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":8532,"text":"ofr81919 - 1981 - Ground-water quality in the vicinity of landfill sites, southern Franklin County, Ohio","interactions":[],"lastModifiedDate":"2012-02-02T00:06:18","indexId":"ofr81919","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1981","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":"81-919","title":"Ground-water quality in the vicinity of landfill sites, southern Franklin County, Ohio","docAbstract":"The hydrogeology and ground-water quality in the vicinity of five landfills in southern Franklin County, Ohio, were investigated by use of data obtained from 46 existing wells, 1 seep, 1 surface-water site, and 1 leachate-collection site. Interpretation was based on data from the wells, a potentiometric-surface map, and chemical analyses. Four of the five landfills are in abandoned sand and gravel pits. Pumping of water from a quarry near the landfills has modified the local ground-water flow pattern, increased the hydraulic gradient, and lowered the water table. Ground water unaffected by the landfills is a hard, calcium bicarbonate type with concentrations of dissolved iron and dissolved sulfate as great as 3.0 milligrams per liter and 200 milligrams per liter, respectively. Water sampled from wells downgradient from two landfills shows an increase in sodium, chloride, and other constituents. The change in water quality cannot be traced directly to the landfills, however, because of well location and the presence of other potential sources of contamination. Chemical analysis of leachate from a collection unit at one landfill shows significant amounts of zinc, chromium, copper, and nickel, in addition to high total organic carbon, biochemical oxygen demand, and organic nitrogen. Concentrations of chloride, iron, lead, manganese and phenolic compounds exceed Ohio Environmental Protection Agency Water Quality Standards for drinking water. Water from unaffected wells within the study area have relatively small amounts of these constituents. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr81919","usgsCitation":"De Roche, J., and Razem, A., 1981, Ground-water quality in the vicinity of landfill sites, southern Franklin County, Ohio: U.S. Geological Survey Open-File Report 81-919, iv, 19 p. :ill., maps ;28 cm., https://doi.org/10.3133/ofr81919.","productDescription":"iv, 19 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":142796,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1981/0919/report-thumb.jpg"},{"id":36111,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1981/0919/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aa7e4b07f02db6671ee","contributors":{"authors":[{"text":"De Roche, J.T.","contributorId":66691,"corporation":false,"usgs":true,"family":"De Roche","given":"J.T.","affiliations":[],"preferred":false,"id":157888,"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":157887,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":8526,"text":"ofr80159 - 1981 - Hydrologic data for the alluvium and terrace aquifer of the Beaver-North Canadian River from the Panhandle to Canton Reservoir, northwestern Oklahoma","interactions":[],"lastModifiedDate":"2018-03-30T16:12:06","indexId":"ofr80159","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1981","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":"80-159","title":"Hydrologic data for the alluvium and terrace aquifer of the Beaver-North Canadian River from the Panhandle to Canton Reservoir, northwestern Oklahoma","docAbstract":"The U.S. Geological Survey has collected data on Oklahoma's groundwater resources since 1934. The data in this report were collected as part of a study in cooperation with the Oklahoma Water Resources Board to evaluate the geohydrology of the alluvium and terrace aquifer of the Beaver-North Canadian River 4] in northwestern Oklahoma. The data include records of approximately 900 wells, test-holes, and springs, results of chemical analyses of water from 30 wells tapping the aquifer, monthly water-level measurements for selected wells, and low-flow discharge measurements of the Beaver-North Canadian River and its tributaries (plate 1). All of the data were collected in the field during the period 1977-79. Information prior to this period is not included in this report but is contained in reports by Wood and Stacy (1965) and Morton (in press).
The stratigraphic nomenclature is that of the Oklahoma Geological Survey and does.not necessarily agree with that of the U.S. Geological Survey.
Acknowledgement is extended to the residents of the study area for their cooperation in obtaining the data in this report.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr80159","usgsCitation":"Davis, R.E., Christenson, S.C., and Blumer, S.P., 1981, Hydrologic data for the alluvium and terrace aquifer of the Beaver-North Canadian River from the Panhandle to Canton Reservoir, northwestern Oklahoma: U.S. Geological Survey Open-File Report 80-159, Report: iii, 77 p.; Plate: 28.92 x 21.39 inches, https://doi.org/10.3133/ofr80159.","productDescription":"Report: iii, 77 p.; Plate: 28.92 x 21.39 inches","costCenters":[{"id":516,"text":"Oklahoma Water Science Center","active":true,"usgs":true}],"links":[{"id":142798,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"country":"United States","state":"Oklahoma","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -100,\n 36\n ],\n [\n -98.5,\n 36\n ],\n [\n -98.5,\n 37\n ],\n [\n -100,\n 37\n ],\n [\n -100,\n 36\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac9e4b07f02db67c62d","contributors":{"authors":[{"text":"Davis, Robert E.","contributorId":10403,"corporation":false,"usgs":true,"family":"Davis","given":"Robert","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":157872,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Christenson, Scott C. schris@usgs.gov","contributorId":980,"corporation":false,"usgs":true,"family":"Christenson","given":"Scott","email":"schris@usgs.gov","middleInitial":"C.","affiliations":[{"id":516,"text":"Oklahoma Water Science Center","active":true,"usgs":true}],"preferred":true,"id":157873,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Blumer, Stephen P. spblumer@usgs.gov","contributorId":2419,"corporation":false,"usgs":true,"family":"Blumer","given":"Stephen","email":"spblumer@usgs.gov","middleInitial":"P.","affiliations":[],"preferred":true,"id":157871,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":8525,"text":"ofr81483 - 1981 - Geohydrology and numerical simulation of the alluvium and terrace aquifer along the Beaver-North Canadian River from the Panhandle to Canton Lake, northwestern Oklahoma","interactions":[],"lastModifiedDate":"2018-11-05T11:39:46","indexId":"ofr81483","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1981","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":"81-483","title":"Geohydrology and numerical simulation of the alluvium and terrace aquifer along the Beaver-North Canadian River from the Panhandle to Canton Lake, northwestern Oklahoma","docAbstract":"A quantitative description of the hydrologic system in alluvium and terrace deposits along the Beaver-North Canadian River in northwestern Oklahoma is needed as an aid for planning and management of the aquifer. A two-dimensional finite-difference model was used to describe the aquifer and to predict the effects of future ground-water withdrawals.
The aquifer principally consists of three geologic units: Alluvium with an average thickness of 30 feet, low terrace deposits with an average thickness of 50 feet, and high terrace deposits with an average thickness of 70 feet. A thin cover of dune sand overlies much of the area and provides an excellent catchment for recharge, but is generally unsaturated.
Hydraulic conductivity of the aquifer ranges from 0 to 160 feet per day and averages 59 feet per day. Specific yield is estimated to be 0.29. Recharge to the aquifer is approximately 1 inch annually. Under present conditions (1978), most discharge is the result of ground-water flow to the Beaver-North Canadian River at a rate of 36 cubic feet per second and to pumpage for public-supply, industrial, and irrigation use at a rate of 28 cubic feet per second. In 1978, the aquifer had an average saturated thickness of 31 feet and contained 4.07 million acre-feet of water.
The model was used to predict future head response in the aquifer to various pumping stresses. For any one area, the pumping stress was applied until the saturated thickness for that area was less than 5 feet, at which time the pumping ceased.
The results of the modeled projections show that if the aquifer is stressed from 1978 to 1993 at the 1977 pumpage rates and well distribution, the average saturated thickness will decrease 1.0 foot and the volume of water in storage will be 3.94 million acre-feet, or 97 percent of the 1978 volume. If the aquifer is stressed at this same rate until 2020, the average saturated thickness will decrease an additional 0.7 foot and the volume of water in storage will be 3.84 million acre-feet, or 94 percent of the 1978 volume.
If all areas of the aquifer having a 1978 saturated thickness of 5 feet or more are stressed from 1978 to 1993 at a rate of approximately
1.4 acre-feet per acre per year, the average saturated thickness will decrease by 20.9 feet and the volume of water in storage will be 1.28 million acre-feet, or 31 percent of the 1978 volume. If the aquifer is stressed at this same rate until 2020, the average saturated thickness will decrease an additional 2.2 feet and the volume of water in storage will be 980,000 acre-feet, or 24 percent of the 1978 volume.
The water in the aquifer is generally of the calcium bicarbonate type and is suitable for most uses. Most of the 30 water samples analyzed contained less than 500 milligrams of dissolved solids per liter.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr81483","usgsCitation":"Davis, R.E., and Christenson, S.C., 1981, Geohydrology and numerical simulation of the alluvium and terrace aquifer along the Beaver-North Canadian River from the Panhandle to Canton Lake, northwestern Oklahoma: U.S. Geological Survey Open-File Report 81-483, Report: vi, 42 p.; 15 Plates, https://doi.org/10.3133/ofr81483.","productDescription":"Report: vi, 42 p.; 15 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Robert E.","contributorId":10403,"corporation":false,"usgs":true,"family":"Davis","given":"Robert","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":157870,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Christenson, Scott C. schris@usgs.gov","contributorId":980,"corporation":false,"usgs":true,"family":"Christenson","given":"Scott","email":"schris@usgs.gov","middleInitial":"C.","affiliations":[{"id":516,"text":"Oklahoma Water Science Center","active":true,"usgs":true}],"preferred":true,"id":157869,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":9033,"text":"ofr81172 - 1981 - Geophysical log suite from drill holes No. 1 and 2, Mariano Lake-Lake Valley Drilling Project, McKinley County, New Mexico","interactions":[],"lastModifiedDate":"2012-02-02T00:06:17","indexId":"ofr81172","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1981","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":"81-172","title":"Geophysical log suite from drill holes No. 1 and 2, Mariano Lake-Lake Valley Drilling Project, McKinley County, New Mexico","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr81172","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1981, Geophysical log suite from drill holes No. 1 and 2, Mariano Lake-Lake Valley Drilling Project, McKinley County, New Mexico: U.S. Geological Survey Open-File Report 81-172, 8 p., 7 over-size sheets ;28 cm., https://doi.org/10.3133/ofr81172.","productDescription":"8 p., 7 over-size sheets ;28 cm.","costCenters":[],"links":[{"id":142723,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1981/0172/report-thumb.jpg"},{"id":36667,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1981/0172/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":36668,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1981/0172/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":36669,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1981/0172/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":36670,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1981/0172/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":36671,"rank":404,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1981/0172/plate-5.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":36672,"rank":405,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1981/0172/plate-6.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":36673,"rank":406,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1981/0172/plate-7.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":36674,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1981/0172/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac8e4b07f02db67c0be","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":528882,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":10047,"text":"ofr81138 - 1981 - Hydrologic monitoring in the coal fields of central Utah, August 1978-September 1979","interactions":[],"lastModifiedDate":"2022-07-18T21:52:00.511532","indexId":"ofr81138","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1981","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":"81-138","title":"Hydrologic monitoring in the coal fields of central Utah, August 1978-September 1979","docAbstract":"Surface-water quantity and quality were observed at 12 gaging stations downstream from mined and lease areas in the Wasatch Plateau, Book Cliff's, and Emery coal fields in central Utah. Measurements of base flow were made at 52 additional sites in the region. The report describes the hydrologic setting of this important coal region and summarizes the surface-water data collected at the monitoring sites from August 1978 through September 1979. Coal mining and lease activities in each of the monitored basins also are described.
Where possible, hydrologic impacts of coal mining are evaluated. Impacts include increases in streamflow and degradation of surface-water quality due to water discharged from underground mines. Other impacts include removal of water from ground-water storage, changes in the natural ground-water flow system, and possibly the diminution of spring flows.
Adequacy of the monitoring network to detect hydrologic changes due to mining is evaluated. In order to fully assess and quantify the impacts, comprehensive studies and monitoring of the ground-water system and water produced in mines are needed.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr81138","usgsCitation":"Lines, G.C., and Plantz, G.G., 1981, Hydrologic monitoring in the coal fields of central Utah, August 1978-September 1979: U.S. Geological Survey Open-File Report 81-138, Report: vi, 56 p.; 1 Plate: 20.45 x 23.78 inches, https://doi.org/10.3133/ofr81138.","productDescription":"Report: vi, 56 p.; 1 Plate: 20.45 x 23.78 inches","costCenters":[],"links":[{"id":403968,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1981/0138/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":403967,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1981/0138/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":144541,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1981/0138/report-thumb.jpg"}],"country":"Utah","otherGeospatial":"central Utah","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -113.62060546875,\n 38.18638677411551\n ],\n [\n -109.951171875,\n 38.18638677411551\n ],\n [\n -109.951171875,\n 39.65645604812829\n ],\n [\n -113.62060546875,\n 39.65645604812829\n ],\n [\n -113.62060546875,\n 38.18638677411551\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a1ae4b07f02db606612","contributors":{"authors":[{"text":"Lines, Gregory C.","contributorId":50502,"corporation":false,"usgs":true,"family":"Lines","given":"Gregory","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":160726,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Plantz, Gerald G.","contributorId":96149,"corporation":false,"usgs":true,"family":"Plantz","given":"Gerald","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":160727,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":10048,"text":"ofr81216 - 1981 - Hydrologic studies of the U.S. Geological Survey in major coal-resource areas of Utah through 1980","interactions":[],"lastModifiedDate":"2024-11-25T22:52:45.7993","indexId":"ofr81216","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1981","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":"81-216","title":"Hydrologic studies of the U.S. Geological Survey in major coal-resource areas of Utah through 1980","docAbstract":"Increased interest in coal has created greater interest in water, both for environmental and water-supply reasons. This report summarizes hydrologic studies conducted in and near the major coal fields of Utah (fig. 1) by the U.S. Geological Survey through 1980. It is intended as a reference for those people dealing with coal-related hydrologic problems.
Published reports and reports in preparation at the time of this compilation are summarized in an annotated bibliography. The 4? reports in the annotated bibliography deal with many components of the hydrologic system. Most of the reports are interpretive in nature, but some contain only hydrologic data. The reports deal with such varied subjects as the magnitude and frequency of floods, availability of ground water, and hydrologic impacts of coal mining.
Seven hydrologic studies that are active in 1980 in Utah coal-resource areas are described. In addition to these seven, studies, that part of the Geological Survey statewide data-collection network in the vicinity of the major coal fields is described.
The hydrologic studies are conducted and reports prepared, for the most part, by personnel of the Water Resources Division, Utah District. tost of the studies and data-collection programs are in cooperation with other Federal, State, and local agencies. Utah Power and Light Co. provides stream- flow data collected at one gaging station.
","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Salt Lake City, UT","doi":"10.3133/ofr81216","usgsCitation":"Lines, G.C., 1981, Hydrologic studies of the U.S. Geological Survey in major coal-resource areas of Utah through 1980: U.S. Geological Survey Open-File Report 81-216, Report: iii, 20 p.; 1 Plate: 17.80 in. x 16.68 in., https://doi.org/10.3133/ofr81216.","productDescription":"Report: iii, 20 p.; 1 Plate: 17.80 in. x 16.68 in.","numberOfPages":"22","costCenters":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":37895,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1981/0216/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":145820,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1981/0216/report-thumb.jpg"},{"id":37894,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1981/0216/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":392142,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_11967.htm"}],"country":"United States","state":"Utah","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -113.333,\n 37\n ],\n [\n -109.044,\n 37\n ],\n [\n -109.044,\n 40.75\n ],\n [\n -113.333,\n 40.75\n ],\n [\n -113.333,\n 37\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a18e4b07f02db605291","contributors":{"authors":[{"text":"Lines, Gregory C.","contributorId":50502,"corporation":false,"usgs":true,"family":"Lines","given":"Gregory","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":160728,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":10125,"text":"ofr81220 - 1981 - Potentially favorable areas for large-yield wells in the Red River Formation and Madison Limestone in parts of Montana, North Dakota, South Dakota, Wyoming, and Nebraska","interactions":[{"subject":{"id":10125,"text":"ofr81220 - 1981 - Potentially favorable areas for large-yield wells in the Red River Formation and Madison Limestone in parts of Montana, North Dakota, South Dakota, Wyoming, and Nebraska","indexId":"ofr81220","publicationYear":"1981","noYear":false,"title":"Potentially favorable areas for large-yield wells in the Red River Formation and Madison Limestone in parts of Montana, North Dakota, South Dakota, Wyoming, and Nebraska"},"predicate":"SUPERSEDED_BY","object":{"id":45714,"text":"pp1273E - 1983 - Potentially favorable areas for large-yield wells in the Red River Formation and Madison Limestone in parts of Montana, North Dakota, South Dakota, and Wyoming","indexId":"pp1273E","publicationYear":"1983","noYear":false,"chapter":"E","title":"Potentially favorable areas for large-yield wells in the Red River Formation and Madison Limestone in parts of Montana, North Dakota, South Dakota, and Wyoming"},"id":1}],"supersededBy":{"id":45714,"text":"pp1273E - 1983 - Potentially favorable areas for large-yield wells in the Red River Formation and Madison Limestone in parts of Montana, North Dakota, South Dakota, and Wyoming","indexId":"pp1273E","publicationYear":"1983","noYear":false,"title":"Potentially favorable areas for large-yield wells in the Red River Formation and Madison Limestone in parts of Montana, North Dakota, South Dakota, and Wyoming"},"lastModifiedDate":"2022-08-09T15:28:15.441093","indexId":"ofr81220","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1981","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":"81-220","title":"Potentially favorable areas for large-yield wells in the Red River Formation and Madison Limestone in parts of Montana, North Dakota, South Dakota, Wyoming, and Nebraska","docAbstract":"The need for large quantities of energy has created interest in the Fort Union coal region of the Northern Great Plains. Extensive development of this coal, which may include onsite steam-power generation, gasification, liquefaction, and slurry-pipeline transport of the coal from this region, would place a heavy demand on the region's limited streamflow. Paleozoic rocks that underlie the Fort Union coal region and aquifers in these rocks, including the Red River Formation and the Madison Limestone, might supply, at least on a temporary basis, a significant part of the water required for coal development. The area of study covers approximately 200,000 square miles, and includes eastern Montana, western North Dakota and South Dakota, northeastern Wyoming, and northwestern Nebraska. This report, one of a series in the Madison Limestone study, uses hydrologic and geologic data to outline potentially favorable areas for well construction - that is, areas in which there is a good probability that large-yield wells (more than 500 gallons per minute) can be completed in the Red River Formation and in the Madison Limestone. Potentially favorable areas in terms of aquifer characteristics, for both the Red River Formation and the Madison Limestone, are given a numerical evaluation from 1 to 3 based on the number of the following criteria that are met: (1) the presence of more than 100 feet of relatively porous rock, (2) the presence of more than 100 feet of dolomite, and (3) the presence of known geologic structures which could affect yield. Areas rated 3 are those in which all three criteria are satisfied; areas rated 2 are those in which two criteria are satisfied; and areas rated 1 are those in which only one criterion is satisfied. The criteria selected for this analysis were chosen because they can be recognized and mapped over the entire study area. Local features such as minor structures, solution zones, and rock facies of small extent were not included in this regional evaluation. In addition, water quality was considered in a general way in defining the favorable areas, by excluding areas in which the electrical resistivity of formation water, as calculated from geophysical well logs, was less than 1 ohm-meter. The numerical scales of the Red River Formation and Madison Limestone are summed to show potentially favorable areas for the combined aquifers. Certain additional factors which may be important to a prospective water user were not included in the numerical ranking - these include depths to the two aquifers, calcite saturation, water temperature, total dissolved solids, and piezometric head in relation to land surface. For a complete evaluation, potential users should consider these factors plus local structures, facies, and solution zones in conjunction with the numerical rankings reflecting aquifer characteristics. To facilitate consideration of piezometric head, maps are included in this report showing areas in which the piezometric head falls in certain ranges with respect to land surface.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr81220","usgsCitation":"MacCary, L., Cushing, E.M., and Brown, D.L., 1981, Potentially favorable areas for large-yield wells in the Red River Formation and Madison Limestone in parts of Montana, North Dakota, South Dakota, Wyoming, and Nebraska: U.S. Geological Survey Open-File Report 81-220, Report: vi, 29 p.; 1 Plate: 17.86 x 21.76 inches, https://doi.org/10.3133/ofr81220.","productDescription":"Report: vi, 29 p.; 1 Plate: 17.86 x 21.76 inches","costCenters":[],"links":[{"id":405012,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1981/0220/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":405011,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1981/0220/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":145531,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1981/0220/report-thumb.jpg"}],"country":"United States","state":"Montana, Nebraska, North Dakota, South Dakota, Wyoming","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -115.13671875,\n 40.111688665595956\n ],\n [\n -96.328125,\n 40.111688665595956\n ],\n [\n -96.328125,\n 49.03786794532644\n ],\n [\n -115.13671875,\n 49.03786794532644\n ],\n [\n -115.13671875,\n 40.111688665595956\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1ae4b07f02db6a86be","contributors":{"authors":[{"text":"MacCary, L.M.","contributorId":13200,"corporation":false,"usgs":true,"family":"MacCary","given":"L.M.","email":"","affiliations":[],"preferred":false,"id":160852,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Cushing, E. M.","contributorId":94273,"corporation":false,"usgs":true,"family":"Cushing","given":"E.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":160854,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Brown, David L.","contributorId":55425,"corporation":false,"usgs":true,"family":"Brown","given":"David","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":160853,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":11214,"text":"ofr82387 - 1981 - Reconnaissance investigation of brine in the eastern Rub al Khali, Kingdom of Saudi Arabia","interactions":[],"lastModifiedDate":"2012-02-02T00:06:36","indexId":"ofr82387","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1981","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":"82-387","title":"Reconnaissance investigation of brine in the eastern Rub al Khali, Kingdom of Saudi Arabia","docAbstract":"Al Uruq al Mu'taridah-Umm as Samim area is located in a large topographic depression in the eastern Rub al Khali desert where playas several thousand square kilometers in area are exposedo A crust of eolian sand cemented with gypsum and halite has formed on many playa surfaces. Anhydrite nodules are common in the sampled area, where the depth to ground water generally exceeds 172 Cmo The chemistry of the three ground-water samples collected near the water well Ramallah-1 (lat 22?10'20'' N., long 54?20'37'' E.) is similar to that of sabkhah-related brines on the coast of the United Arab Emirates. Although there is no indication of economic quantities of evaporite minerals in the sampled area, the extent of the depression and its unique geologic environment recommend it for resource-evaluation studies.","language":"ENGLISH","publisher":"Ministry of Petroleum and Mineral Resources, Deputy Ministry for Mineral Resources,","doi":"10.3133/ofr82387","usgsCitation":"Smith, C.L., 1981, Reconnaissance investigation of brine in the eastern Rub al Khali, Kingdom of Saudi Arabia: U.S. Geological Survey Open-File Report 82-387, iii, 16 p. :ill., maps ;28 cm., https://doi.org/10.3133/ofr82387.","productDescription":"iii, 16 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":144522,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0387/report-thumb.jpg"},{"id":39005,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0387/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a4de4b07f02db626d4c","contributors":{"authors":[{"text":"Smith, C. L.","contributorId":100842,"corporation":false,"usgs":true,"family":"Smith","given":"C.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":162744,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":9101,"text":"ofr81817 - 1981 - Water-resources investigations of the U.S. Geological Survey in Montana, October 1980 through September 1981","interactions":[],"lastModifiedDate":"2012-02-02T00:06:14","indexId":"ofr81817","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1981","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":"81-817","title":"Water-resources investigations of the U.S. Geological Survey in Montana, October 1980 through September 1981","docAbstract":"The report describes the investigative efforts of the U.S. Geological Survey toward the water resources of Montana. Hydrologic information and knowledge of the water resources are gained and disseminated principally by programs of (1) collecting hydrologic data on a continuing basis, (2) conducting water-resources appraisals of surface and ground water, (3) conducting supportive research in hydrology and related fields, (4) disseminating water data and results of investigations to the public, (5) coordinating acquisition of water data by Federal agencies, and (6) providing technical assistance in hydrologic fields to other government agencies. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr81817","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1981, Water-resources investigations of the U.S. Geological Survey in Montana, October 1980 through September 1981: U.S. Geological Survey Open-File Report 81-817, iv, 50 p. ill., maps ;28 cm., https://doi.org/10.3133/ofr81817.","productDescription":"iv, 50 p. ill., maps ;28 cm.","costCenters":[],"links":[{"id":141898,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1981/0817/report-thumb.jpg"},{"id":36719,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1981/0817/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a08e4b07f02db5f9c7d","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":528899,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":11218,"text":"ofr81118 - 1981 - Leachability of uranium and other elements from freshly erupted volcanic ash","interactions":[{"subject":{"id":11218,"text":"ofr81118 - 1981 - Leachability of uranium and other elements from freshly erupted volcanic ash","indexId":"ofr81118","publicationYear":"1981","noYear":false,"title":"Leachability of uranium and other elements from freshly erupted volcanic ash"},"predicate":"SUPERSEDED_BY","object":{"id":70011897,"text":"70011897 - 1982 - Leachability of uranium and other elements from freshly erupted volcanic ash","indexId":"70011897","publicationYear":"1982","noYear":false,"title":"Leachability of uranium and other elements from freshly erupted volcanic ash"},"id":1}],"supersededBy":{"id":70011897,"text":"70011897 - 1982 - Leachability of uranium and other elements from freshly erupted volcanic ash","indexId":"70011897","publicationYear":"1982","noYear":false,"title":"Leachability of uranium and other elements from freshly erupted volcanic ash"},"lastModifiedDate":"2025-05-14T19:49:48.648787","indexId":"ofr81118","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1981","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":"81-118","title":"Leachability of uranium and other elements from freshly erupted volcanic ash","docAbstract":"A study of leaching of freshly erupted basaltic and dacitic air-fall ash and bomb fragment samples, unaffected by rain, shows that glass dissolution is the dominant orocess by which uranium is initially mobilized from air-fall volcanic ash. Si, Li, and V are also Preferentially mobilized by glass dissolution. Gaseous transfer followed by fixation of soluble uranium species on volcanic-ash particles is not an important process affecting uranium mobility. Gaseous transfer, however, may be important in forming water-soluble phases, adsorbed to ash surfaces, enriched in the economically and environmentally important elements Zn, Cu, Cd, Ph, B, F, and Ba. Quick removal of these adsorbed elements by the first exposure of freshly erupted ash to rain and surface water may pose short-term hazards to certain forms of aquatic and terrestrial life. Such rapid release of material may also represent the first step in transportation of economically important elements to environments favorable for precipitation into deposits of commercial interest.
Ash samples collected from the active Guatemalan volcanoes Fuego and Pacaya (high-Al basalts) and Santiaguito (hornblende-hypersthene dacite); bomb fragments from Augustine volcano (andesite-dacite), Alaska, and Heimaey (basalt), Vestmann Islands, Iceland; and fragments of \"rhyolitic\" pumice from various historic eruptions were subjected to three successive leaches with a constant water-to-ash weight ratio of 4:1. The volcanic material was successively leached by (1) distilled-deionized water (pH = 5.0-5.5) at room temperature for 24 hours, which removes water-soluble cases and salts adsorbed on ash surfaces during eruption; (2) dilute HC1 solution (pH = 3.5-4.0) at room temperature for 24 hours, which continues the attack initiated by the water and also attacks acid-soluble sulfides and oxides; '3) a solution 0.05 M in both Na2CO3 and NaHCO3 (pH = 9.9) at 80°C for one week, which preferentially dissolves volcanic class. The first two leaches mimic interaction of ash with rain produced in the vicinity of an active eruption. The third leach accelerates the effect of prolonged contact of volcanic ash with alkaline ground water present during ash diagenesis.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr81118","usgsCitation":"Smith, D., Zielinski, R.A., and Rose, W.I., 1981, Leachability of uranium and other elements from freshly erupted volcanic ash: U.S. Geological Survey Open-File Report 81-118, iii, 95 p., https://doi.org/10.3133/ofr81118.","productDescription":"iii, 95 p.","costCenters":[],"links":[{"id":144547,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1981/0118/report-thumb.jpg"},{"id":393800,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1981/0118/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1be4b07f02db6a8996","contributors":{"authors":[{"text":"Smith, David B. 0000-0001-8396-9105 dsmith@usgs.gov","orcid":"https://orcid.org/0000-0001-8396-9105","contributorId":1274,"corporation":false,"usgs":true,"family":"Smith","given":"David B.","email":"dsmith@usgs.gov","affiliations":[{"id":218,"text":"Denver Federal Center","active":false,"usgs":true}],"preferred":false,"id":162750,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Zielinski, Robert A. 0000-0002-4047-5129 rzielinski@usgs.gov","orcid":"https://orcid.org/0000-0002-4047-5129","contributorId":1593,"corporation":false,"usgs":true,"family":"Zielinski","given":"Robert","email":"rzielinski@usgs.gov","middleInitial":"A.","affiliations":[{"id":164,"text":"Central Energy Resources Science Center","active":true,"usgs":true}],"preferred":true,"id":162751,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Rose, William I. Jr.","contributorId":71556,"corporation":false,"usgs":true,"family":"Rose","given":"William","suffix":"Jr.","email":"","middleInitial":"I.","affiliations":[],"preferred":false,"id":162752,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":9552,"text":"ofr811061 - 1981 - Flow model of Saginaw River near Saginaw, Michigan","interactions":[],"lastModifiedDate":"2017-07-12T10:39:57","indexId":"ofr811061","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1981","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":"81-1061","title":"Flow model of Saginaw River near Saginaw, Michigan","docAbstract":"An unsteady-flow simulation model was applied to a 19.5-mile reach of Saginaw River. The model provides a method of determining instantaneous discharge for flows from -8,000 to 12,000 cubic feet per second. The currently used slope-rating method can be utilized to compute discharge only under steady and high-flow conditions. Unsteady flow frequently occurs in the Saginaw River as a result of lake seiching.
Model computations are based on solution of the continuity and momentum flow equations, on hydraulic characteristics of Saginaw River, and on time-dependent boundary conditions. An implicit, finite-difference technique is used to solve the one-dimensional flow equations. Channel storage and conveyance characteristics were obtained from data collected during a 1979 field survey and through model calibration. Boundary conditions are specified by stage or discharge data at the model extremities. Optionally, wind velocity data are incorporated in the flow simulations.
The model can simulate instantaneous stage and discharge data and summarize or plot the data. Simulations of low-flows are sensitive to small errors in stage data and to gentle breezes. Simulation of high flows for present channel conditions requires additional data and further study.
","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Lansing, MI","doi":"10.3133/ofr811061","usgsCitation":"Holtschlag, D.J., 1981, Flow model of Saginaw River near Saginaw, Michigan: U.S. Geological Survey Open-File Report 81-1061, v, 20 p., https://doi.org/10.3133/ofr811061.","productDescription":"v, 20 p.","numberOfPages":"30","costCenters":[{"id":382,"text":"Michigan Water Science Center","active":true,"usgs":true}],"links":[{"id":141685,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1981/1061/report-thumb.jpg"},{"id":343667,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1981/1061/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Michigan","otherGeospatial":"Saginaw River","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -84.40521240234375,\n 43.29320031385282\n ],\n [\n -83.69384765625,\n 43.29320031385282\n ],\n [\n -83.69384765625,\n 43.79092385423618\n ],\n [\n -84.40521240234375,\n 43.79092385423618\n ],\n [\n -84.40521240234375,\n 43.29320031385282\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49d8e4b07f02db5df2d6","contributors":{"authors":[{"text":"Holtschlag, David J. 0000-0001-5185-4928 dholtschlag@usgs.gov","orcid":"https://orcid.org/0000-0001-5185-4928","contributorId":5447,"corporation":false,"usgs":true,"family":"Holtschlag","given":"David","email":"dholtschlag@usgs.gov","middleInitial":"J.","affiliations":[{"id":382,"text":"Michigan Water Science Center","active":true,"usgs":true}],"preferred":true,"id":159878,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":10622,"text":"ofr81417 - 1981 - Quantitative geomorphology of drainage basins in Sumter National Forest, South Carolina","interactions":[],"lastModifiedDate":"2012-02-02T00:06:21","indexId":"ofr81417","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1981","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":"81-417","title":"Quantitative geomorphology of drainage basins in Sumter National Forest, South Carolina","docAbstract":"This report describes a computer program, written in Basic, that facilitates quantitative analysis of drainage basins and channel networks. The program was used to inventory 2,000 small watersheds in Sumter National Forest, South Carolina during 1980 and 1981. Drainage basins and stream segments were delineated in color on mylar overlays over U.S. Geological Survey 1:24 ,000-scale maps. Drainage basin characteristics were quantified and stored on eight-inch diskettes. The program can produce printouts and plots that summarize geomorphic data for each watershed. The program is adaptable to other locations. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr81417","usgsCitation":"Patterson, G.G., 1981, Quantitative geomorphology of drainage basins in Sumter National Forest, South Carolina: U.S. Geological Survey Open-File Report 81-417, iv, 59 p. ;28 cm., https://doi.org/10.3133/ofr81417.","productDescription":"iv, 59 p. ;28 cm.","costCenters":[],"links":[{"id":142489,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1981/0417/report-thumb.jpg"},{"id":38454,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1981/0417/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a86e4b07f02db64db3c","contributors":{"authors":[{"text":"Patterson, Glenn G.","contributorId":9653,"corporation":false,"usgs":true,"family":"Patterson","given":"Glenn","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":161696,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ]}