{"pageNumber":"555","pageRowStart":"13850","pageSize":"25","recordCount":16498,"records":[{"id":10911,"text":"ofr8178 - 1981 - Summary of U.S. Geological Survey investigations and hydrologic conditions in southwest Florida for 1979","interactions":[],"lastModifiedDate":"2014-06-11T08:26:00","indexId":"ofr8178","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":"81-78","title":"Summary of U.S. Geological Survey investigations and hydrologic conditions in southwest Florida for 1979","docAbstract":"This report summarizes the hydrologic setting and the water-resources investigations in the Southwest Florida Water management District performed by the U.S. Geological Survey, Water Resources Division, for fiscal year 1979. Hydrologic conditions in southwest Florida are described and illustrated by hydrographs of selected surface-water, ground-water, and lake-stage data-collection sites. In addition, summaries of water-use data and data on the regional observation monitor-well program are provided. The investigations are pay of the Federal program of appraising the nation's water resources.l The cooperative program for fiscal year 1979 included 37 investigations. Abstracts of 15 reports released during 1979 are included.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Tallahassee, FL","doi":"10.3133/ofr8178","collaboration":"Prepared in cooperation with the Southwest Florida Management District","usgsCitation":"Rollins, H., 1981, Summary of U.S. Geological Survey investigations and hydrologic conditions in southwest Florida for 1979: U.S. Geological Survey Open-File Report 81-78, vi, 93 p., https://doi.org/10.3133/ofr8178.","productDescription":"vi, 93 p.","numberOfPages":"101","costCenters":[],"links":[{"id":288251,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1981/0078/report.pdf"},{"id":288252,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"country":"United States","state":"Florida","county":"Charlotte County;Citrus County;De Soto County;Hardee County;Hernando County;Highlands County;Hillsborough County;Lake County;Levy County;Manatee County;Marion County;Pasco County;Pinellas County;Polk County;Sarasota County;Sumter County","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -83.1657,26.3087 ], [ -83.1657,29.5913 ], [ -80.8541,29.5913 ], [ -80.8541,26.3087 ], [ -83.1657,26.3087 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b04e4b07f02db699413","contributors":{"authors":[{"text":"Rollins, H.C.","contributorId":102885,"corporation":false,"usgs":true,"family":"Rollins","given":"H.C.","email":"","affiliations":[],"preferred":false,"id":162195,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":7422,"text":"ofr811187 - 1981 - Preliminary appraisal of the hydrology of the Blocker area, Pittsburg County, Oklahoma","interactions":[],"lastModifiedDate":"2012-02-02T00:06:04","indexId":"ofr811187","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":"81-1187","title":"Preliminary appraisal of the hydrology of the Blocker area, Pittsburg County, Oklahoma","docAbstract":"Bedrock in the Blocker area of southeastern Oklahoma consists principally of shale, siltstone, and sandstone of the Boggy and Savanna Formations of Pennsylvanian age. These rocks have been folded to form the Panther Mountain syncline on the south and the Kinta anticline on the north. Alluvium along streams is less than 15 feet thick and consists mainly of sandy silt. Water in bedrock is under artesian conditions. Well depths range from 11 to 213 feet and average 75 feet. In 86% of the wells measured, the water level was less than 30 feet below the land surface. Because the rocks have minimal permeability, well yields probably are less than 5 gallons per minute. Ground water is commonly a mixed cation bicarbonate type with dissolved solids ranging from about 300 to 2,000 milligrams per liter. No relationship between water chemistry and well depth or geographic distribution is apparent. Streams in the area are ephemeral and there are extended periods of no flow. Blue Creek was dry 30% of the time during 1976-80 and had flows of less than 0.1 cubic foot per second for at least 80 consecutive days. Stream water is generally a mixed cation sulfate type. The maximum dissolved-solids concentration determined in stream water was 3670 milligrams per liter. Maximum suspended sediment discharge, in tons per day, was about 235 for Blue Creek, 40 for Blue Creek tributary, and 630 for Mathuldy Creek. Silt-clay particles (diameters less than 0.062 millimeter) are the dominant sediment size. Surface mining for coal undoubtedly will have some effect on the environment. The most likely deleterious effects are increased sediment loads in streams and increased mineralization of stream waters. However, these effects should be of only limited extent and duration if appropriate mining and reclamation practices are followed. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr811187","usgsCitation":"Marcher, M.V., Bergman, D.L., Stoner, J., and Blumer, S.P., 1981, Preliminary appraisal of the hydrology of the Blocker area, Pittsburg County, Oklahoma: U.S. Geological Survey Open-File Report 81-1187, iv, 52 p. :ill., maps ;28 cm., https://doi.org/10.3133/ofr811187.","productDescription":"iv, 52 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":140449,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1981/1187/report-thumb.jpg"},{"id":34831,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1981/1187/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":34832,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1981/1187/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":34833,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1981/1187/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":34834,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1981/1187/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac9e4b07f02db67ca5b","contributors":{"authors":[{"text":"Marcher, Melvin V.","contributorId":11590,"corporation":false,"usgs":true,"family":"Marcher","given":"Melvin","email":"","middleInitial":"V.","affiliations":[],"preferred":false,"id":155545,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bergman, D. L.","contributorId":93038,"corporation":false,"usgs":true,"family":"Bergman","given":"D.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":155548,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Stoner, J.D.","contributorId":58261,"corporation":false,"usgs":true,"family":"Stoner","given":"J.D.","email":"","affiliations":[],"preferred":false,"id":155547,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Blumer, S. P.","contributorId":23938,"corporation":false,"usgs":true,"family":"Blumer","given":"S.","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":155546,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":9448,"text":"ofr81537 - 1981 - Hydrology of area 3, Eastern Coal Province, Pennsylvania","interactions":[],"lastModifiedDate":"2017-06-27T11:19:52","indexId":"ofr81537","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":"81-537","title":"Hydrology of area 3, Eastern Coal Province, Pennsylvania","docAbstract":"Hydrologic data are presented for area 3 of the Eastern Coal Province, 4,077 square miles of the lower Allegheny River basin in western Pennsylvania. Seventy-three streams were sampled three times during the 1979 and 1980 water years for specific conductance, pH, acidity, alkalinity, dissolved and total iron, dissolved and total manganese, dissolved sulfate, and dissolved solids. Benthic invertebrate populations were determined and botom material samples were analyzed for metals. Sixteen streams had pH, acidity, alkalinity, total iron, total manganese, and dissolved sulfate indicative of acid-mine drainage. These streams were most common in the Redbank and Blacklick Creek basins and in the Conemaugh and lower Kiskiminetas River basins. Benthic invertebrates were not found in 11 of 64 streams sampled. An additional 13 streams had low benthic invertebrate diversity indices. Low diversity indices were most common in the southern part of area 3. Low flow, mean flow, peak flow, and flow duration data are presented for gaging stations in area 3. Techniques for estimating these data for ungaged sites are presented and referenced. The functions of, and access to, the National Water Data Exchange, National Water Data Storage and Retrieval System, and Office of Water Data Coordination are explained. (USGS)","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr81537","usgsCitation":"Herb, W.J., Shaw, L.C., and Brown, D.E., 1981, Hydrology of area 3, Eastern Coal Province, Pennsylvania: U.S. Geological Survey Open-File Report 81-537, v, 60 p. :ill., col. maps ;28 cm., https://doi.org/10.3133/ofr81537.","productDescription":"v, 60 p. :ill., col. maps ;28 cm.","costCenters":[{"id":532,"text":"Pennsylvania Water Science Center","active":true,"usgs":true}],"links":[{"id":94920,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1981/0537/report.pdf","size":"22947","linkFileType":{"id":1,"text":"pdf"}},{"id":142228,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1981/0537/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae1e4b07f02db6887c2","contributors":{"authors":[{"text":"Herb, William J.","contributorId":79454,"corporation":false,"usgs":true,"family":"Herb","given":"William","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":159703,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Shaw, L. C.","contributorId":21162,"corporation":false,"usgs":true,"family":"Shaw","given":"L.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":159702,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Brown, Deborah E.","contributorId":92255,"corporation":false,"usgs":true,"family":"Brown","given":"Deborah","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":159704,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":3127,"text":"wsp2068 - 1981 - Hydrologic reconnaissance of the Wasatch Plateau-Book Cliffs coal-fields area, Utah","interactions":[{"subject":{"id":7233,"text":"ofr79988 - 1979 - Hydrologic reconnaissance of the Wasatch Plateau-Book Cliffs coal-fields area, Utah","indexId":"ofr79988","publicationYear":"1979","noYear":false,"title":"Hydrologic reconnaissance of the Wasatch Plateau-Book Cliffs coal-fields area, Utah"},"predicate":"SUPERSEDED_BY","object":{"id":3127,"text":"wsp2068 - 1981 - Hydrologic reconnaissance of the Wasatch Plateau-Book Cliffs coal-fields area, Utah","indexId":"wsp2068","publicationYear":"1981","noYear":false,"title":"Hydrologic reconnaissance of the Wasatch Plateau-Book Cliffs coal-fields area, Utah"},"id":1}],"lastModifiedDate":"2023-03-14T20:06:08.759442","indexId":"wsp2068","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1981","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":"2068","title":"Hydrologic reconnaissance of the Wasatch Plateau-Book Cliffs coal-fields area, Utah","docAbstract":"<p>Data obtained during a hydrologic reconnaissance in 1975-77 in the Wasatch Plateau-Book Cliffs coal-fields area of Utah were correlated with existing long-term data. Maps were prepared showing average precipitation, average streamflow, stream temperature, ground- and surface-water quality, sediment yield, and geology. Recommendations were made for additional study and suggested approaches for continued monitoring in the coalfields areas.</p><p>moDuring the 1931-75 water years, the minimum discharges for the five major streams that head in the area ranged from about 12,000 to 26,000 acre-feet per year, and the maximum discharges ranged from about 59,000 to 315,000 acre-feet per year. Correlations indicate that 3 years of low-flow records at stream sites in the Wasatch Plateau would allow the development of relationships with long-term sites that can be used to estimate future low-flow records within a standard error of about 20 percent.</p><p>Most water-quality degradation in streams occurs along the flanks of the Wasatch Plateau and Book Cliffs. In the uplands, dissolved-solids concentrations generally ranged from less than 100 to about 250 milligrams per liter, and in the lowlands, the concentrations ranged from about 250 to more than 6,000 milligrams per liter.</p><p>Most springs in the Wasatch Plateau and Book Cliffs discharge from the Star Point Sandstone or younger formations, and the water generally contains less than about 1,000 milligrams per liter of dissolved solids. The discharges of 65 springs ranged from about 0.2 to 200 gallons per minute. The Blackhawk Formation, which is the principal coal-bearing formation, produces water in many of the mines. The dissolved-solids concentration in water discharging from springs and mines in the Blackhawk ranged from about 60 to 800 milligrams per liter.</p><p>In the lowland areas, the Ferron Sandstone Member of the Maneos Shale appears to have the most potential for subsurface development of water of suitable chemical quality for human consumption. Three wells in the Ferron yielded water with dissolved-solids concentrations ranging from about 650 to 1,230 milligrams per liter.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Washington, D.C.","doi":"10.3133/wsp2068","collaboration":"Prepared in cooperation with the U.S. Bureau of Land Management and the U.S. Environmental Protection Agency","usgsCitation":"Waddell, K.M., Contratto, P., Sumsion, C.T., and Butler, J.R., 1981, Hydrologic reconnaissance of the Wasatch Plateau-Book Cliffs coal-fields area, Utah: U.S. Geological Survey Water Supply Paper 2068, Report: v, 45 p.; 9 Plates: 40.00 in x 30.19 inches or smaller; Table: 12.50 in. x 13.45 inches, https://doi.org/10.3133/wsp2068.","productDescription":"Report: v, 45 p.; 9 Plates: 40.00 in x 30.19 inches or smaller; Table: 12.50 in. x 13.45 inches","numberOfPages":"61","costCenters":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":414125,"rank":13,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_25489.htm","linkFileType":{"id":5,"text":"html"}},{"id":30038,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/2068/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":247290,"rank":11,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/2068/plate-9.pdf","linkFileType":{"id":1,"text":"pdf"},"linkHelpText":"Hydrgraphs for selected wells, Wasatch Plateau-Book Cliffs coal-fields area, Utah"},{"id":247284,"rank":5,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/2068/plate-3.pdf","text":"Plate 3","linkFileType":{"id":1,"text":"pdf"},"linkHelpText":"Map showing average discharges of streams, Wasatch Plateau-Book Cliffs coal-fields area, Utah"},{"id":247283,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/2068/plate-2.pdf","text":"Plate 2","linkFileType":{"id":1,"text":"pdf"},"linkHelpText":"Map showing average annual precipitation, 1931-75, Wasatch Plateau-Book Cliffs coal-fields area, Utah"},{"id":247282,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/2068/plate-1.pdf","text":"Plate 1","linkFileType":{"id":1,"text":"pdf"},"linkHelpText":"Map showing general geology of the Wasatch Plateau-Book Cliffs coal-fields area, Utah"},{"id":139323,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/2068/report-thumb.jpg"},{"id":247289,"rank":10,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/2068/plate-8.pdf","text":"Plate 8","linkFileType":{"id":1,"text":"pdf"},"linkHelpText":"Fence diagram showing stratigraphic units and concentrations of dissolved solids, Wasatch Plateau-Book Cliffs coal-fields area, Utah"},{"id":247288,"rank":9,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/2068/plate-7.pdf","text":"Plate 7","linkFileType":{"id":1,"text":"pdf"},"linkHelpText":"Map showing concentrations of dissolved solids in ground water, Wasatch Plateau-Book Cliffs coal-fields area, Utah"},{"id":247287,"rank":8,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/2068/plate-6.pdf","text":"Plate 6","linkFileType":{"id":1,"text":"pdf"},"linkHelpText":"Map showing estimated sediment yields, Wasatch Plateau-Book Cliffs coal-fields area, Utah"},{"id":247286,"rank":7,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/2068/plate-5.pdf","text":"Plate 5","linkFileType":{"id":1,"text":"pdf"},"linkHelpText":"Map showing concentrations of dissolved solids in surface water, Wasatch Plateau-Book Cliffs coal-fields area, Utah"},{"id":247285,"rank":6,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/2068/plate-4.pdf","text":"Plate 4","linkFileType":{"id":1,"text":"pdf"},"linkHelpText":"Map showing estimated range of stream temperature, Wasatch Plateau-Book Cliffs coal-fields area, Utah"},{"id":247291,"rank":12,"type":{"id":27,"text":"Table"},"url":"https://pubs.usgs.gov/wsp/2068/plate-table_2.pdf","text":"Table 2","linkFileType":{"id":1,"text":"pdf"},"linkHelpText":"Published stream-gaging records and ranges of annual discharge, 1931-75 water years"}],"country":"United States","state":"Utah","otherGeospatial":"Wasatch Plateau-Book Cliffs coal-fields area","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -111.54,\n              40.045\n            ],\n            [\n              -111.54,\n              38.687\n            ],\n            [\n              -109.059,\n              38.687\n            ],\n            [\n              -109.059,\n              40.045\n            ],\n            [\n              -111.54,\n              40.045\n            ]\n          ]\n       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Kay","contributorId":15598,"corporation":false,"usgs":true,"family":"Contratto","given":"P. Kay","affiliations":[],"preferred":false,"id":146300,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Sumsion, C. T.","contributorId":23129,"corporation":false,"usgs":true,"family":"Sumsion","given":"C.","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":146302,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Butler, John R.","contributorId":36540,"corporation":false,"usgs":true,"family":"Butler","given":"John","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":146303,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":10621,"text":"ofr811072 - 1981 - Results of exploratory drilling at Point MacKenzie, Alaska, 1981","interactions":[],"lastModifiedDate":"2012-02-02T00:06:21","indexId":"ofr811072","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":"81-1072","title":"Results of exploratory drilling at Point MacKenzie, Alaska, 1981","docAbstract":"The Matanuska-Susitna Borough anticipates industrial development near Point MacKenzie, Alaska. Because little hydrologic information is available for the area, the Borough contracted for the drilling of two test wells. It was found that: Both wells penetrated unconsolidated stratified clay, silt, sand, and gravel; each well penetrated a shallow unconfined and deeper confined aquifers; the water levels in the wells rise and fall with the tide; the chemical analyses indicate that the water quality meets the Alaska Drinking Water Standards, except for slightly high levels of manganese and pH; and the potential for saltwater intrusion should be evaluated as part of future studies. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr811072","usgsCitation":"Patrick, L., 1981, Results of exploratory drilling at Point MacKenzie, Alaska, 1981: U.S. Geological Survey Open-File Report 81-1072, ii, 11 p. ill. ;28 cm., https://doi.org/10.3133/ofr811072.","productDescription":"ii, 11 p. ill. ;28 cm.","costCenters":[],"links":[{"id":142488,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1981/1072/report-thumb.jpg"},{"id":38453,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1981/1072/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a4ae4b07f02db6248c1","contributors":{"authors":[{"text":"Patrick, Leslie","contributorId":36136,"corporation":false,"usgs":true,"family":"Patrick","given":"Leslie","email":"","affiliations":[],"preferred":false,"id":161695,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"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":"<p>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.</p><p>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.</p>","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":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":"<p>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.</p><p>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.</p><p>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.</p><p>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.</p><p>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.</p><p>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<br>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.</p><p>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.</p>","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 Plates","numberOfPages":"51","costCenters":[],"links":[{"id":359181,"rank":12,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1981/0483/plate-10.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":142797,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1981/0483/report-thumb.jpg"},{"id":359182,"rank":13,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1981/0483/plate-11.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":359183,"rank":14,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1981/0483/plate-12.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":359184,"rank":15,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1981/0483/plate-13.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":359185,"rank":16,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1981/0483/plate-14.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":359186,"rank":17,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1981/0483/plate-15.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":359176,"rank":7,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1981/0483/plate-5.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":359177,"rank":8,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1981/0483/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":359178,"rank":9,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1981/0483/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":359179,"rank":10,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1981/0483/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":359180,"rank":11,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1981/0483/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":359171,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1981/0483/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":359172,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1981/0483/plate-9.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":359173,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1981/0483/plate-8.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":359174,"rank":5,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1981/0483/plate-7.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":359175,"rank":6,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1981/0483/plate-6.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United 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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":8504,"text":"ofr81539 - 1981 - Hydrology of the coal-resource areas in the upper drainages of Huntington and Cottonwood creeks, central Utah","interactions":[],"lastModifiedDate":"2022-08-15T18:16:56.208692","indexId":"ofr81539","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":"81-539","title":"Hydrology of the coal-resource areas in the upper drainages of Huntington and Cottonwood creeks, central Utah","docAbstract":"<p>The hydrology of coal-resource areas in the upper drainages of Huntington and Cottonwood Creeks in central Utah was studied in order to better define the hydrologic system, to identify the hydrologic effects of underground coal mining, and to devise methods to detect the effects.</p><p>Discharge records from gaging stations in this mountainous area indicated that there are large differences in the annual discharge of streams per unit area of drainage. These differences are attributed to differences in precipitation, differences in evaporation and sublimation of the snowpack, and to subsurface movement of water out of some basins. Surface waters sampled during 1977-79 were of good chemical quality; dissolved-solids concentrations rarely exceeded 500 milligrams per liter.</p><p>The Star Point Sandstone and the lower coal-bearing part of the Blackhawk Formation, both of Cretaceous age, are saturated in some areas, and the aquifer yields water to underground coal mines. Most of the larger discharging springs in the study area issue from the Star Point-Blackhawk aquifer where faulted. Ground water also occurs in several water-bearing zones above the Star Point-Blackhawk aquifer. It is not known whether the water in these overlying units is part of a continuous zone of saturation or whether unsaturated zones occur between units and some water is perched.</p><p>Dissolved-solids concentrations in water from about 140 springs ranged from 50 to 750 milligrams per liter. The chemical characteristics of water from the water-bearing zones of different formations usually were very similar.</p><p>Dewatering of underground coal mines was the largest manmade discharge from the Star Point-Blackhawk aquifer in the study area during 1979. The dewatering of mines has decreased the amount of water in storage in the aquifer, but water-level data were not available to define the extent of the depletion. Other possible impacts due to mine dewatering include the diminution of spring flows and increases in ground-water recharge, both of which are more likely to occur where rocks have been fractured due to subsidence above mines. Also, the flows of streams that receive water discharged from mines probably have increased accordingly. The discharge of mine water into streams causes some degradation in surface-water quality, but the quality of ground water is probably not adversely affected by mining.</p><p>Some environmental changes associated with underground mining are difficult to detect without data collected over a long period. With respect to the ground-water system, the year-to-year similarity of spring-discharge recession curves may provide a method to detect some of these changes. Changes in the benthic-invertebrate population may help detect pollution of surface waters.</p><p>Comprehensive studies of the ground-water system are needed in conjunction with hydrologic monitoring in order to fully assess the hydrologic impacts of the underground coal mining.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr81539","collaboration":"Prepared in cooperation with the Utah Department of Natural Resources and Energy, Division of Oil, Gas, and Mining","usgsCitation":"Danielson, T.W., ReMillard, M.D., and Fuller, R.H., 1981, Hydrology of the coal-resource areas in the upper drainages of Huntington and Cottonwood creeks, central Utah: U.S. Geological Survey Open-File Report 81-539, Report: vi, 85 p.; 2 Plates: 24.71 x 37.66 inches and 24.58 x 37.93 inches, https://doi.org/10.3133/ofr81539.","productDescription":"Report: vi, 85 p.; 2 Plates: 24.71 x 37.66 inches and 24.58 x 37.93 inches","costCenters":[],"links":[{"id":405144,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1981/0539/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":405143,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1981/0539/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":405142,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1981/0539/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":143564,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1981/0539/report-thumb.jpg"}],"country":"United States","state":"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              -111.39175415039062,\n              39.13645165015621\n            ],\n            [\n              -111.13014221191406,\n              39.13645165015621\n            ],\n            [\n              -111.13014221191406,\n              39.35022841846271\n            ],\n            [\n              -111.39175415039062,\n              39.35022841846271\n            ],\n            [\n              -111.39175415039062,\n              39.13645165015621\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0ce4b07f02db5fc78b","contributors":{"authors":[{"text":"Danielson, T. W.","contributorId":48590,"corporation":false,"usgs":true,"family":"Danielson","given":"T.","middleInitial":"W.","affiliations":[],"preferred":false,"id":157825,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"ReMillard, Michael D.","contributorId":95748,"corporation":false,"usgs":true,"family":"ReMillard","given":"Michael","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":157827,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Fuller, Richard H.","contributorId":66236,"corporation":false,"usgs":true,"family":"Fuller","given":"Richard","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":157826,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":7610,"text":"ofr81348 - 1981 - Water-resources investigations of the U.S. Geological Survey in Kansas; fiscal years 1979 and 1980","interactions":[],"lastModifiedDate":"2017-09-29T08:00:09","indexId":"ofr81348","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":"81-348","title":"Water-resources investigations of the U.S. Geological Survey in Kansas; fiscal years 1979 and 1980","docAbstract":"<p>Activities of the U.S. Geological Survey in Kansas include the systematic collection and analysis of data to describe the framework of hydrologic systems, assess the water resources, define existing or potential problems in the quantity or quality of water, and provide information for optimum development and management of resources. Streamflow studies are made to determine availability of supplies and relations to rainfall runoff, urbanization, flood frequencies, and sediment-transport. Ground-water studies are made to determine the quantity of supplies available in aquifer systems, the effects of natural or artificial contamination, and the effects of withdrawals by irrigation, industrial, and municipal supplies. Water-quality studies are made to define physical, chemical, and biological characteristics in streams and principal aquifers, and to evaluate the chemical changes due to urbanization and surface mining.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr81348","usgsCitation":"McGovern, H.E., and Combs, L., 1981, Water-resources investigations of the U.S. Geological Survey in Kansas; fiscal years 1979 and 1980: U.S. Geological Survey Open-File Report 81-348, 107 p., https://doi.org/10.3133/ofr81348.","productDescription":"107 p.","numberOfPages":"111","costCenters":[{"id":353,"text":"Kansas Water Science Center","active":false,"usgs":true}],"links":[{"id":346196,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1981/0348/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":139976,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1981/0348/report-thumb.jpg"}],"country":"United 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,{"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":"<p>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.</p><p>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).</p><p>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.</p><p>Model analyses indicate that the total steady-state freshwater-flow rate through the five modeled areas is approximately 412 cubic feet per second.</p>","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":7611,"text":"ofr81683 - 1981 - Water-resources investigations of the U.S. Geological Survey in Missouri, fiscal year 1981","interactions":[],"lastModifiedDate":"2022-08-16T17:40:29.394795","indexId":"ofr81683","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":"81-683","title":"Water-resources investigations of the U.S. Geological Survey in Missouri, fiscal year 1981","docAbstract":"<p>Water-resources investigations of the U.S. Geological Survey in Missouri consist of collecting hydrologic data and making interpretative investigations. The data and the results of the investigations are published or released by either the U.S. Geological Survey or by cooperating agencies. This report describes the data-collection activities and investigations in Missouri for the 1981 fiscal year and provides an extensive list of water-resources references for the State of Missouri.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr81683","usgsCitation":"Kratzer, W.M., 1981, Water-resources investigations of the U.S. Geological Survey in Missouri, fiscal year 1981: U.S. Geological Survey Open-File Report 81-683, i, 60 p., https://doi.org/10.3133/ofr81683.","productDescription":"i, 60 p.","costCenters":[],"links":[{"id":405197,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1981/0683/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":140080,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1981/0683/report-thumb.jpg"}],"country":"United States","state":"Missouri","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"Polygon\",\"coordinates\":[[[-89.545006,36.336809],[-89.605668,36.342234],[-89.615841,36.336085],[-89.620255,36.323006],[-89.611819,36.309088],[-89.578492,36.288317],[-89.554289,36.277751],[-89.539487,36.277368],[-89.534507,36.261802],[-89.539229,36.248821],[-89.562206,36.250909],[-89.577544,36.242262],[-89.602374,36.238106],[-89.642182,36.249486],[-89.678046,36.248284],[-89.695235,36.252766],[-89.705328,36.239898],[-89.69263,36.224959],[-89.607004,36.171179],[-89.591605,36.144096],[-89.59307,36.129699],[-89.601936,36.11947],[-89.666598,36.095802],[-89.678821,36.084636],[-89.688577,36.029238],[-89.706932,36.000981],[-90.37789,35.995683],[-90.351732,36.025347],[-90.34909,36.040131],[-90.339343,36.047112],[-90.333261,36.067504],[-90.320746,36.071326],[-90.320662,36.087138],[-90.29991,36.098236],[-90.294492,36.112949],[-90.266256,36.120559],[-90.235585,36.139474],[-90.231386,36.147348],[-90.23537,36.159153],[-90.220425,36.184764],[-90.21128,36.183392],[-90.188189,36.20536],[-90.152497,36.215582],[-90.14224,36.227522],[-90.126366,36.229367],[-90.130114,36.240307],[-90.118219,36.253491],[-90.114922,36.265595],[-90.086471,36.271531],[-90.06398,36.303038],[-90.081961,36.322097],[-90.074074,36.342895],[-90.077695,36.348478],[-90.066297,36.3593],[-90.064514,36.382085],[-90.078671,36.399116],[-90.138512,36.413952],[-90.134231,36.422827],[-90.143743,36.424433],[-90.143798,36.428483],[-90.134136,36.436602],[-90.137323,36.455411],[-90.141101,36.461791],[-90.155804,36.463555],[-90.152888,36.47093],[-90.142222,36.470554],[-90.143683,36.476029],[-90.158838,36.479558],[-90.159305,36.492446],[-90.152481,36.497952],[-94.617919,36.499414],[-94.617975,37.722176],[-94.607354,39.113444],[-94.589933,39.140403],[-94.591933,39.155003],[-94.608834,39.160503],[-94.640035,39.153103],[-94.662435,39.157603],[-94.663835,39.179103],[-94.680336,39.184303],[-94.714137,39.170403],[-94.741938,39.170203],[-94.763138,39.179903],[-94.781518,39.206146],[-94.811663,39.206594],[-94.831679,39.215938],[-94.835056,39.220658],[-94.825663,39.241729],[-94.831471,39.256273],[-94.84632,39.268481],[-94.887056,39.28648],[-94.905329,39.311952],[-94.910017,39.352543],[-94.88136,39.370383],[-94.879281,39.37978],[-94.885026,39.389801],[-94.901823,39.392798],[-94.92311,39.384492],[-94.942039,39.389499],[-94.946293,39.405646],[-94.972952,39.421705],[-94.982144,39.440552],[-95.0375,39.463689],[-95.045716,39.472459],[-95.052177,39.499996],[-95.082714,39.516712],[-95.109304,39.542285],[-95.113077,39.559133],[-95.103228,39.577783],[-95.089515,39.581028],[-95.064519,39.577115],[-95.049277,39.589583],[-95.046361,39.599557],[-95.055152,39.621657],[-95.053367,39.630347],[-95.027644,39.665454],[-95.018318,39.672869],[-94.984149,39.67785],[-94.971317,39.68641],[-94.971206,39.729305],[-94.965318,39.739065],[-94.948726,39.745593],[-94.902612,39.724202],[-94.875643,39.730494],[-94.862943,39.742994],[-94.860743,39.763094],[-94.869644,39.772894],[-94.912293,39.759338],[-94.934262,39.773642],[-94.935206,39.78313],[-94.929654,39.788282],[-94.884084,39.794234],[-94.875944,39.813294],[-94.878677,39.826522],[-94.886933,39.833098],[-94.916918,39.836138],[-94.942567,39.856602],[-94.928466,39.876344],[-94.929574,39.888754],[-94.95154,39.900533],[-94.986975,39.89667],[-95.00844,39.900596],[-95.024389,39.891202],[-95.027931,39.871522],[-95.037767,39.865542],[-95.085003,39.861883],[-95.128166,39.874165],[-95.140601,39.881688],[-95.143802,39.901918],[-95.149657,39.905948],[-95.179453,39.900062],[-95.199347,39.902709],[-95.206326,39.912121],[-95.20069,39.928155],[-95.204428,39.938949],[-95.250254,39.948644],[-95.269886,39.969396],[-95.302507,39.984357],[-95.315271,40.01207],[-95.356876,40.031522],[-95.387195,40.02677],[-95.40726,40.033112],[-95.416824,40.043235],[-95.42164,40.058952],[-95.409856,40.07432],[-95.407591,40.09803],[-95.394216,40.108263],[-95.39284,40.115887],[-95.398667,40.126419],[-95.428749,40.135577],[-95.436348,40.15872],[-95.460746,40.169173],[-95.479193,40.185652],[-95.482757,40.197346],[-95.469718,40.227908],[-95.477501,40.24272],[-95.490333,40.248966],[-95.521925,40.24947],[-95.552473,40.261904],[-95.556325,40.267714],[-95.550966,40.285947],[-95.562157,40.297359],[-95.581787,40.29958],[-95.610439,40.31397],[-95.642262,40.306025],[-95.657328,40.310856],[-95.653729,40.322582],[-95.625204,40.334288],[-95.623728,40.346567],[-95.641027,40.366399],[-95.643934,40.386849],[-95.659134,40.40869],[-95.65819,40.44188],[-95.693133,40.469396],[-95.699969,40.505275],[-95.661687,40.517309],[-95.652262,40.538114],[-95.655848,40.546609],[-95.671754,40.562626],[-95.678718,40.56256],[-95.694147,40.556942],[-95.69505,40.533124],[-95.708591,40.521551],[-95.722444,40.528118],[-95.75711,40.52599],[-95.769281,40.536656],[-95.763366,40.550797],[-95.773549,40.578205],[-95.765645,40.585208],[-94.632035,40.571186],[-94.080463,40.572899],[-92.689854,40.589884],[-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,{"id":7616,"text":"ofr81347 - 1981 - Water-resources investigations of the USGS in Texas, fiscal year 1981","interactions":[],"lastModifiedDate":"2017-07-12T10:45:50","indexId":"ofr81347","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":"81-347","title":"Water-resources investigations of the USGS in Texas, fiscal year 1981","docAbstract":"<p>Water-resources investigations in Texas consist of the collection of basic records through the hydrologic-data network, interpretive studies, and research projects. The hydrologic records and the results of investigations are published by the Geological Survey or by cooperating agencies. This report describes the water-resources projects and activities of the Geological Survey in Texas for the 1981 fiscal year (October 1, 1980 to September 30, 1981).</p><p>The Geological Survey's investigations of the water resources of Texas are under the general direction of Jack Rawson, Acting District Chief. The Texas District office is in the Federal Building, 300 East Eighth Street, Austin, Texas 78701.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr81347","usgsCitation":"Mitchell, A.A., and Buckner, H., 1981, Water-resources investigations of the USGS in Texas, fiscal year 1981: U.S. Geological Survey Open-File Report 81-347, 44 p., https://doi.org/10.3133/ofr81347.","productDescription":"44 p.","numberOfPages":"47","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"links":[{"id":140092,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1981/0347/report-thumb.jpg"},{"id":343678,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1981/0347/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United 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,{"id":6396,"text":"pp1044I - 1981 - The geothermal hydrology of Warner Valley, Oregon: A reconnaissance study","interactions":[],"lastModifiedDate":"2021-12-23T22:37:05.37152","indexId":"pp1044I","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1981","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":"1044","chapter":"I","title":"The geothermal hydrology of Warner Valley, Oregon: A reconnaissance study","docAbstract":"<p>No abstract available.</p>","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Geohydrology of geothermal systems","largerWorkSubtype":{"id":5,"text":"USGS Numbered Series"},"language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/pp1044I","usgsCitation":"Sammel, E.A., and Craig, R.W., 1981, The geothermal hydrology of Warner Valley, Oregon: A reconnaissance study: U.S. Geological Survey Professional Paper 1044, Report: 147 p.; 1 Plate: 28.50 × 40.00 inches, https://doi.org/10.3133/pp1044I.","productDescription":"Report: 147 p.; 1 Plate: 28.50 × 40.00 inches","costCenters":[],"links":[{"id":33769,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/1044i/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":33770,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/1044i/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":121573,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/1044i/report-thumb.jpg"},{"id":393395,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_4698.htm"}],"country":"United States","state":"Oregon","otherGeospatial":"Warner Valley","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -120.125,\n              42.5167\n            ],\n            [\n              -119.6250,\n              42.5167\n            ],\n            [\n              -119.6250,\n              42\n            ],\n            [\n              -120.125,\n              42\n            ],\n            [\n              -120.125,\n              42.5167\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a9ae4b07f02db65d59d","contributors":{"authors":[{"text":"Sammel, Edward A.","contributorId":78320,"corporation":false,"usgs":true,"family":"Sammel","given":"Edward","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":152647,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Craig, Robert W.","contributorId":37729,"corporation":false,"usgs":true,"family":"Craig","given":"Robert","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":152646,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"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":"<p>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.&nbsp;</p>","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":8926,"text":"ofr81210 - 1981 - Hydrologic effects of highway-deicing chemicals in Massachusetts; executive summary","interactions":[],"lastModifiedDate":"2012-02-02T00:06:09","indexId":"ofr81210","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":"81-210","title":"Hydrologic effects of highway-deicing chemicals in Massachusetts; executive summary","docAbstract":"Methods of estimating annual mean and annual maximum chloride concentrations in streams were developed through multiple and simple linear regression techniques using data collected during the 1972-77 water years. Independent variables are easily obtainable parameters, such as total salt application within a basin, annual precipitation, and drainage basin characteristics. Methods for obtaining gross estimates of chloride loads and sodium loads from salt-application data and estimates of nonhighway-related chloride and sodium were suggested. A chloride budget was calculated for a small basin draining a section of interstate highway. The chloride budget was described in terms of the percentages in direct runoff to the stream, in ground-water discharges to the stream, in storage in the ground, and the amount unaccounted for. Attempts were made to relate chloride concentrations in ground water adjacent to highways to quantities of salt applied to the highways on an annual basis, annual precipitation, depth of the wells below land surface, depth of the well below water table, and the distance of the well from the edge of the pavement. Little correlation was observed between annual salt-application values and annual mean chloride concentrations in ground water near highways. The irregular distribution of highway runoff, due to topographic differences between sites, and variations in runoff resulting from individual storms seem to be the causes of the lack of significant correlation between annual quantities of salt applied and chloride concentrations in ground water near highways. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr81210","usgsCitation":"Frost, L., Pollock, S., and Wakelee, R., 1981, Hydrologic effects of highway-deicing chemicals in Massachusetts; executive summary: U.S. Geological Survey Open-File Report 81-210, iii, 13 p. :ill. ;28 cm., https://doi.org/10.3133/ofr81210.","productDescription":"iii, 13 p. :ill. ;28 cm.","costCenters":[],"links":[{"id":141156,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1981/0210/report-thumb.jpg"},{"id":36534,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1981/0210/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1ae4b07f02db6a87f9","contributors":{"authors":[{"text":"Frost, L.R. Jr.","contributorId":56219,"corporation":false,"usgs":true,"family":"Frost","given":"L.R.","suffix":"Jr.","email":"","affiliations":[],"preferred":false,"id":158561,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Pollock, S.J.","contributorId":101260,"corporation":false,"usgs":true,"family":"Pollock","given":"S.J.","email":"","affiliations":[],"preferred":false,"id":158562,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Wakelee, R.F.","contributorId":108109,"corporation":false,"usgs":true,"family":"Wakelee","given":"R.F.","email":"","affiliations":[],"preferred":false,"id":158563,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":9424,"text":"ofr811107 - 1981 - Hydrologic almanac of Florida","interactions":[],"lastModifiedDate":"2012-02-02T00:06:15","indexId":"ofr811107","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":"81-1107","title":"Hydrologic almanac of Florida","docAbstract":"This first edition is a ready reference source of information on various facts and features about water in Florida. It is aimed primarily to help bust politicians, writers, agency officials, water managers, planners, consultants, educators, hydrologists, engineers, scientists, and the general public answer questions that arise on comparative and statistical aspects on the hydrology of Florida. It contains statistical comparative data, much of which was especially prepared for the almanac, a glossary of technical terms, tabular material, and conversion factors. Also included is a selective bibliography of 174 reports on water in Florida. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr811107","usgsCitation":"Heath, R.C., and Conover, C.S., 1981, Hydrologic almanac of Florida: U.S. Geological Survey Open-File Report 81-1107, xii, 251 ill., maps ;28 cm., https://doi.org/10.3133/ofr811107.","productDescription":"xii, 251 ill., maps ;28 cm.","costCenters":[],"links":[{"id":141843,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1981/1107/report-thumb.jpg"},{"id":37134,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1981/1107/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a29e4b07f02db611937","contributors":{"authors":[{"text":"Heath, Richard C.","contributorId":96263,"corporation":false,"usgs":true,"family":"Heath","given":"Richard","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":159663,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Conover, Clyde Stuart","contributorId":42197,"corporation":false,"usgs":true,"family":"Conover","given":"Clyde","email":"","middleInitial":"Stuart","affiliations":[],"preferred":false,"id":159662,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":9353,"text":"ofr81135 - 1981 - Hydrology of area 22, Eastern Coal Province, Alabama","interactions":[],"lastModifiedDate":"2012-02-02T00:06:27","indexId":"ofr81135","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":"81-135","title":"Hydrology of area 22, Eastern Coal Province, Alabama","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr81135","usgsCitation":"Harkins, J.R., and and others, 1981, Hydrology of area 22, Eastern Coal Province, Alabama: U.S. Geological Survey Open-File Report 81-135, v, 72 p. :ill. (some col.), maps (some col.) ;28 cm., https://doi.org/10.3133/ofr81135.","productDescription":"v, 72 p. :ill. (some col.), maps (some col.) ;28 cm.","costCenters":[],"links":[{"id":94918,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1981/0135/report.pdf","size":"18190","linkFileType":{"id":1,"text":"pdf"}},{"id":144149,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1981/0135/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a14e4b07f02db602bca","contributors":{"authors":[{"text":"Harkins, Joe R.","contributorId":28982,"corporation":false,"usgs":true,"family":"Harkins","given":"Joe","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":159532,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"and others","contributorId":127886,"corporation":true,"usgs":false,"organization":"and others","id":528901,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":7623,"text":"ofr81493 - 1981 - A wind powered, ground-water monitoring installation at a radioactive waste management site in Idaho","interactions":[],"lastModifiedDate":"2022-08-12T19:20:57.323917","indexId":"ofr81493","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":"81-493","title":"A wind powered, ground-water monitoring installation at a radioactive waste management site in Idaho","docAbstract":"<p>In 1971, four wells were drilled just outside a radioactive solid waste storage and disposal facility located on the Idaho National Engineering Laboratory in southeastern Idaho. This facility, the Radioactive Waste Management Complex (RWMC), has been in use since 1952. These wells serve several purposes: to study the geology and hydrology at the RWMC, to determine the potential for radioactive waste migration, and to obtain water samples to determine if waste products are migrating downward into the Snake River Plain aquifer.</p><p>Special efforts are made to insure that surface contamination does not enter the wells by either water, wind, or contaminated equipment. A submersible pump and a continuous water-level measuring device were installed in each well. Permanent installation of this equipment allowed the well heads to be sealed while providing for collection of data from these wells.</p><p>The water-level measuring device is a small diameter, differential-pressure, transducer probe. The transducer produces a variable-reluctance signal which is converted to an analog signal and recorded as the depth to water on a strip chart recorder. Windmill-charged storage batteries provide power for the water-level measuring system. This system is reliable, sensitive, and relatively maintenance free.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr81493","usgsCitation":"Bagby, J.C., Ghering, G., Jensen, R.G., and Barr, A.G., 1981, A wind powered, ground-water monitoring installation at a radioactive waste management site in Idaho: U.S. Geological Survey Open-File Report 81-493, ii, 28 p., https://doi.org/10.3133/ofr81493.","productDescription":"ii, 28 p.","costCenters":[],"links":[{"id":405121,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1981/0493/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":139729,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1981/0493/report-thumb.jpg"}],"country":"United 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,{"id":12259,"text":"ofr811186 - 1981 - Reconnaissance of the ground-water resources of Kings and Queens counties, New York","interactions":[],"lastModifiedDate":"2012-02-02T00:06:41","indexId":"ofr811186","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":"81-1186","title":"Reconnaissance of the ground-water resources of Kings and Queens counties, New York","docAbstract":"Western Long Island 's ground-water resources are being considered for redevelopment as a supplemental source of public water supply. The ground-water reservoir in Kings and Queens Counties had supplied an average of more than 120 million gallons per day for industrial and public water supply from 1904 to 1947. However, deterioration of groundwater quality from induced encroachment of salty ground-water caused the total cessation of pumping for public supply in Kings County in 1947 and in western Queens County in 1974. This investigation was designed to make a preliminary evaluation of the present groundwater quality and to review hydrologic information pertinent to the formulation of an appropriate development plan. Detailed hydrogeologic mapping was done to define the geometry of the ground-water system. The history of ground-water development and the consequent responses of ground-water levels and quantity were summarized. A well network was established to monitor ground-water levels and ground-water quality in Kings and Queens Counties. The distribution of chloride and nitrate in ground-water was used to identify contamination from salt-water intrusion and surface sources. A limited source of potable ground-water is available in the Magothy-Jameco and Lloyd aquifers; however, an accurate estimate of the quantity of water available or a draft rate suitable for maintaining a useable ground-water quality is undetermined. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr811186","usgsCitation":"Buxton, H., Soren, J., Posner, A., and Shernoff, P., 1981, Reconnaissance of the ground-water resources of Kings and Queens counties, New York: U.S. Geological Survey Open-File Report 81-1186, 64 p., ill., maps ;28 cm., https://doi.org/10.3133/ofr811186.","productDescription":"64 p., ill., maps ;28 cm.","costCenters":[],"links":[{"id":145567,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1981/1186/report-thumb.jpg"},{"id":40423,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1981/1186/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac9e4b07f02db67c497","contributors":{"authors":[{"text":"Buxton, H. T.","contributorId":67873,"corporation":false,"usgs":true,"family":"Buxton","given":"H. T.","affiliations":[],"preferred":false,"id":165675,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Soren, Julian","contributorId":54184,"corporation":false,"usgs":true,"family":"Soren","given":"Julian","email":"","affiliations":[],"preferred":false,"id":165674,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Posner, Alex","contributorId":18376,"corporation":false,"usgs":true,"family":"Posner","given":"Alex","email":"","affiliations":[],"preferred":false,"id":165672,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Shernoff, P. K.","contributorId":22779,"corporation":false,"usgs":true,"family":"Shernoff","given":"P. K.","affiliations":[],"preferred":false,"id":165673,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":9611,"text":"ofr81811 - 1981 - Ground-water data for Michigan, 1980","interactions":[],"lastModifiedDate":"2017-07-12T10:38:15","indexId":"ofr81811","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":"81-811","title":"Ground-water data for Michigan, 1980","docAbstract":"<p>The purpose of this report is to make available the 1980 records of water levels and related data for the principal aquifers of the State. This report is written for municipalities, industries, institutions, consultants, drillers, hydrologists and other people interested in the ground-water resources.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Lansing, MI","doi":"10.3133/ofr81811","usgsCitation":"Huffman, G., 1981, Ground-water data for Michigan, 1980: U.S. Geological Survey Open-File Report 81-811, iv, 57 p., https://doi.org/10.3133/ofr81811.","productDescription":"iv, 57 p.","numberOfPages":"65","costCenters":[{"id":382,"text":"Michigan Water Science Center","active":true,"usgs":true}],"links":[{"id":343665,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1981/0811/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":141718,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1981/0811/report-thumb.jpg"}],"country":"United 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,{"id":7757,"text":"ofr81421 - 1981 - Background hydrologic information in potential lignite mining areas in Mississippi, August 1980","interactions":[],"lastModifiedDate":"2022-11-04T17:29:59.898863","indexId":"ofr81421","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":"81-421","title":"Background hydrologic information in potential lignite mining areas in Mississippi, August 1980","docAbstract":"<p>The U.S. Geological Survey in cooperation with Mississippi Bureau of Geology is conducting a hydrologic data-collection program in the potential lignite-producing areas in Mississippi. During the week of August 25-28, 1980, hydrologic data on channel characteristics were collected at 15 sites on small streams draining potential lignite mining areas in east-central Mississippi. Streamflow measurements were made and water-quality samples were collected at 11 of the 15 sites.</p><p>Main channel widths at the 15 sampling sites in east-central Mississippi ranged from 126 feet on Sucarnoochee Creek to 15 feet on Houston Creek. Maximum water depth ranged from 7 feet on Pawticfaw Creek and Tallahatta Creek to one-half foot on Okatibbee Creek. The maximum stream discharge measured was 56 cubic feet per second on Pawticfaw Creek. Four sites had no discharge. Specific conductance at sampling sites ranged from 115 micromhos on Ponta Creek to 26 micromhos on Sucarnoochee Creek. The dissolved-oxygen concentration was 5.7 milligrams per liter or higher at all sites. The concentration of suspended sediment was not greater than 38 milligrams per liter at any site. Concentrations of calcium, magnesium, sodium, potassium, chloride, and sulfate were less than 10 milligrams per liter in all samples, but were highest at site 10 on Ponta Creek. Bottom-material samples commonly contained iron, manganese, and zinc.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr81421","collaboration":"Prepared in cooperation with the Mississippi Department of Natural Resources, Bureau of Geology","usgsCitation":"Arthur, J.K., 1981, Background hydrologic information in potential lignite mining areas in Mississippi, August 1980: U.S. Geological Survey Open-File Report 81-421, 19 p., https://doi.org/10.3133/ofr81421.","productDescription":"19 p.","costCenters":[],"links":[{"id":409171,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1981/0421/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":142244,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1981/0421/report-thumb.jpg"}],"country":"United 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 \"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afee4b07f02db69794b","contributors":{"authors":[{"text":"Arthur, J. K.","contributorId":56223,"corporation":false,"usgs":true,"family":"Arthur","given":"J.","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":156548,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":7810,"text":"ofr81634 - 1981 - Hydrogeologic data from test drilling near Verna, Florida, 1978","interactions":[],"lastModifiedDate":"2013-08-02T07:16:24","indexId":"ofr81634","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":"81-634","title":"Hydrogeologic data from test drilling near Verna, Florida, 1978","docAbstract":"Four test wells were drilled in the vicinity of the city of Sarasota well field near Verna, Fla., to provide hydrologic and geologic information. An expedient and economical method of air lifting water samples from isolated water-producing zones while drilling was utilized. Lithologic logs of drill cuttings and geophysical logs, including point resistance and spontaneous potential electric logs, gamma-ray logs, and caliper logs, were made. Chemical quality of water was determined for principal producing zones at each well. Dissolved solids from composite water samples ranged from 313 milligrams per liter in test well 0-1 north of the well field to 728 milligrams per liter in test well 0-3 within the well field. Each test well was pumped to determine maximum discharge, water-level drawdown, and recovery time. A leaking pump column on test well 0-1 prevented accurate measurement of drawdown on the well. Test well 0-2, located east of the well field, had a pumping rate of 376 gallons per minute and 13.11 feet of drawdown after 3 hours and 50 minutes; test well 0-3 had a maximum yield of 320 gallons per minute, a drawdown of 31.91 feet after 2 hours and 35 minutes of pumping, had a recovery time of 20 minutes; and test well 0-4, south of the well field, had a pumping rate of 200 gallons per minute with 63.34 feet of drawdown after 2 hours and 35 minutes. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr81634","usgsCitation":"Barker, M., Bowman, G., and Sutcliffe, H., 1981, Hydrogeologic data from test drilling near Verna, Florida, 1978: U.S. Geological Survey Open-File Report 81-634, iii, 29 p. ill., maps ;28 cm., https://doi.org/10.3133/ofr81634.","productDescription":"iii, 29 p. ill., maps ;28 cm.","costCenters":[],"links":[{"id":140400,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1981/0634/report-thumb.jpg"},{"id":275908,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1981/0634/report.pdf"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a50e4b07f02db628b35","contributors":{"authors":[{"text":"Barker, Michael","contributorId":34917,"corporation":false,"usgs":true,"family":"Barker","given":"Michael","email":"","affiliations":[],"preferred":false,"id":156647,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bowman, Geronia","contributorId":50890,"corporation":false,"usgs":true,"family":"Bowman","given":"Geronia","email":"","affiliations":[],"preferred":false,"id":156648,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Sutcliffe, Horace","contributorId":28598,"corporation":false,"usgs":true,"family":"Sutcliffe","given":"Horace","affiliations":[],"preferred":false,"id":156646,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":9202,"text":"ofr81141 - 1981 - Preliminary hydrologic evaluation of the North Horn Mountain coal-resource area, Utah","interactions":[],"lastModifiedDate":"2017-09-02T10:36:23","indexId":"ofr81141","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":"81-141","title":"Preliminary hydrologic evaluation of the North Horn Mountain coal-resource area, Utah","docAbstract":"<p>North Horn Mountain is part of a deeply dissected plateau in central Utah which is characterized by deep, narrow, steep-walled canyons with local relief of more than 1,000 feet. Geologic units exposed in the North Horn Mountain area range in age from Late Cretaceous to Holocene and contain two mineable seams of Cretaceous coal. The area is in the drainage basin of the San Rafael River, in the Colorado River Basin. Runoff from the mountain is ephemeral. This runoff to the San Rafael River is by way of Cottonwood and Perron Creeks and represents less than 10 percent of their average annual runoff. Probable peak discharges (100-year flood) for the ephemeral streams draining North Horn Mountain are estimated to range from 200 to 380 cubic feet per second.</p><p>The chemical quality of surface water in the area is good. The water is generally of a calcium magnesium bicarbonate type with average dissolved solids less than 500 milligrams per liter. Annual sediment yield in most of the area ranges from 0.1 to 0.2 acre-foot per square mile but locally is as high as 1.0 acre-foot per square mile. Most of the sediment is eroded during cloudbursts.</p><p>Most of the ground water above the coal on North Horn Mountain probably is in perched aquifers. These aquifers support the flow of small seeps and springs. In some areas, the regional water table appears to extend upward into the coal. The principal source of recharge is precipitation that probably moves to aquifers along faults, joints, or fractures. This movement is apparently quite rapid. The dissolved-solids concentrations of ground water in the North Horn Mountain area range from less than 500 to about 1,000 milligrams per liter.</p><p>Coal mining on North Horn Mountain should have minor \"effects on the quantity and quality of surface water. The maximum predicted decrease in the annual flow of Ferron and Cottonwood Creeks is less than U percent. The sediment loads of affected streams could be significantly increased if construction were to take place during the summer cloudburst season. Subsidence, which usually follows underground coal mining, could create rock fractures through which a perched aquifer might be drained, thus depleting the flow of seeps or springs fed by that aquifer. It is considered unlikely that the mining will adversely affect the chemical quality of the ground water.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Salt Lake City, UT","doi":"10.3133/ofr81141","collaboration":"Prepared in cooperation with the U.S. Bureau of Land Management","usgsCitation":"Graham, M., Tooley, J.E., and Price, D., 1981, Preliminary hydrologic evaluation of the North Horn Mountain coal-resource area, Utah: U.S. Geological Survey Open-File Report 81-141, 34 p., https://doi.org/10.3133/ofr81141.","productDescription":"34 p.","numberOfPages":"34","costCenters":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":141972,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1981/0141/report-thumb.jpg"},{"id":36811,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1981/0141/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Utah","otherGeospatial":"North Horn Mountain","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4abce4b07f02db6732e3","contributors":{"authors":[{"text":"Graham, M.J.","contributorId":61424,"corporation":false,"usgs":true,"family":"Graham","given":"M.J.","email":"","affiliations":[],"preferred":false,"id":159277,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Tooley, John E.","contributorId":83528,"corporation":false,"usgs":true,"family":"Tooley","given":"John","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":159278,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Price, Don","contributorId":30608,"corporation":false,"usgs":true,"family":"Price","given":"Don","email":"","affiliations":[],"preferred":false,"id":159276,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":9612,"text":"ofr81204 - 1981 - Hydrology of area 16, Eastern Coal Province, Virginia-Tennessee","interactions":[],"lastModifiedDate":"2012-02-02T00:06:15","indexId":"ofr81204","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":"81-204","title":"Hydrology of area 16, Eastern Coal Province, Virginia-Tennessee","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr81204","usgsCitation":"Hufschmidt, P.W., 1981, Hydrology of area 16, Eastern Coal Province, Virginia-Tennessee: U.S. Geological Survey Open-File Report 81-204, v, 74 p. :ill., maps (some col.) ;28 cm., https://doi.org/10.3133/ofr81204.","productDescription":"v, 74 p. :ill., maps (some col.) ;28 cm.","costCenters":[],"links":[{"id":94933,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1981/0204/report.pdf","size":"16082","linkFileType":{"id":1,"text":"pdf"}},{"id":141734,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1981/0204/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a17e4b07f02db60462a","contributors":{"authors":[{"text":"Hufschmidt, Peter W.","contributorId":85185,"corporation":false,"usgs":true,"family":"Hufschmidt","given":"Peter","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":159995,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":8925,"text":"ofr81209 - 1981 - Hydrologic effects of highway-deicing chemicals in Massachusetts","interactions":[],"lastModifiedDate":"2012-02-02T00:06:09","indexId":"ofr81209","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":"81-209","title":"Hydrologic effects of highway-deicing chemicals in Massachusetts","docAbstract":"Methods of estimating annual mean and annual maximum chloride concentrations and sodium concentrations in streams were developed using multiple and simple linear regression techniques and data collected during the 1972-77 water years. Independent variables are easily obtainable parameters such as total salt application within a basin, annual precipitation, and drainage basin characteristics. Methods for obtaining gross estimates of chloride loads and sodium loads from salt-application data and estimates of nonhighway-related chloride and sodium were suggested. A chloride budget was calculated for a small drainage basin containing a section of interstate highway. The chloride budget was described in terms of the percentages in direct runoff to the stream, in ground-water discharges to the stream, in storage in the ground, and in the amount unaccounted for. Attempts were made to relate chloride concentrations in ground water adjacent to highways to quantities of salt applied to the highways on an annual basis, annual precipitation, depth of the wells below land surface, depth of wells below the water table, and distance of well from edge of pavement. Little correlation was observed between annual salt-application values and annual mean chloride concentrations in ground water near highways. The irregular distribution of highway runoff, due to topographic differences between sites, and variations in salting and runoff during individual storm events seem to affect correlation between quantities of salt applied and chloride concentrations in ground water near highways. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr81209","usgsCitation":"Frost, L., Pollock, S., and Wakelee, R., 1981, Hydrologic effects of highway-deicing chemicals in Massachusetts: U.S. Geological Survey Open-File Report 81-209, vii, 63 p. :ill., map ;28 cm., https://doi.org/10.3133/ofr81209.","productDescription":"vii, 63 p. :ill., map ;28 cm.","costCenters":[],"links":[{"id":141137,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1981/0209/report-thumb.jpg"},{"id":36533,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1981/0209/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1ee4b07f02db6a9f28","contributors":{"authors":[{"text":"Frost, L.R. Jr.","contributorId":56219,"corporation":false,"usgs":true,"family":"Frost","given":"L.R.","suffix":"Jr.","email":"","affiliations":[],"preferred":false,"id":158558,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Pollock, S.J.","contributorId":101260,"corporation":false,"usgs":true,"family":"Pollock","given":"S.J.","email":"","affiliations":[],"preferred":false,"id":158559,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Wakelee, R.F.","contributorId":108109,"corporation":false,"usgs":true,"family":"Wakelee","given":"R.F.","email":"","affiliations":[],"preferred":false,"id":158560,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
]}