{"pageNumber":"555","pageRowStart":"13850","pageSize":"25","recordCount":16449,"records":[{"id":27311,"text":"wri817 - 1981 - Ground-water potential of the glacial deposits near Logansport, Cass County, Indiana","interactions":[],"lastModifiedDate":"2024-08-06T14:40:50.128801","indexId":"wri817","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1981","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"81-7","title":"Ground-water potential of the glacial deposits near Logansport, Cass County, Indiana","docAbstract":"<p>The glacial deposits underlying a 260 square-mile area near Logansport, Indiana, range in thickness from 0 to 300 feet and consist of three semiconfined sand and gravel aquifer units separated and overlain by three semiconfining till units. The ground-water development potential of the lowest of the sand and gravel aquifers is considerable. Thickness of the aquifer is generally about 80 feet along the axis of the narrow buried valley that it fills. Maximum and average transmissivities of the aquifer are about 38,000 and 13,000 square feet per day, respectively. Withdrawal of 10 million gallons per day from the aquifer was simulated by a four-layer digital model of the study area. Simulated pumping centers were located in areas of high transmissivity and proximity to ground-water discharge. Results indicate an absence of hydrologic constraints to development of the quantities of ground water simulated in the model. However, the simulation of water-level declines of as much as 35 feet in the lowest aquifer indicates that interference with the operation of domestic wells is likely.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri817","collaboration":"Prepared in cooperation with the Indiana Department of Natural Resources and the city of Logansport","usgsCitation":"Gillies, D.C., 1981, Ground-water potential of the glacial deposits near Logansport, Cass County, Indiana: U.S. Geological Survey Water-Resources Investigations Report 81-7, vi, 98 p., https://doi.org/10.3133/wri817.","productDescription":"vi, 98 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":346,"text":"Indiana Water Science Center","active":true,"usgs":true}],"links":[{"id":432284,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1981/0007/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":158587,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1981/0007/report-thumb.jpg"}],"country":"United States","state":"Indiana","county":"Cass County","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"Polygon\",\"coordinates\":[[[-86.4672,40.9093],[-86.3553,40.9093],[-86.2933,40.9092],[-86.269,40.9087],[-86.2404,40.9082],[-86.1692,40.9098],[-86.1694,40.7424],[-86.1707,40.7157],[-86.1691,40.6798],[-86.1681,40.6435],[-86.1654,40.5633],[-86.241,40.5625],[-86.3572,40.5614],[-86.3748,40.5614],[-86.3739,40.6924],[-86.3915,40.6925],[-86.4054,40.6925],[-86.5248,40.6925],[-86.5237,40.7165],[-86.5237,40.7347],[-86.5728,40.7356],[-86.5819,40.7356],[-86.5802,40.824],[-86.5797,40.912],[-86.4672,40.9093]]]},\"properties\":{\"name\":\"Cass\",\"state\":\"IN\"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aa8e4b07f02db667403","contributors":{"authors":[{"text":"Gillies, Daniel C.","contributorId":39824,"corporation":false,"usgs":true,"family":"Gillies","given":"Daniel","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":197896,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":31045,"text":"ofr81149 - 1981 - Preliminary data from a series of artificial recharge experiments at Stanton, Texas","interactions":[],"lastModifiedDate":"2016-08-23T15:45:59","indexId":"ofr81149","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":"81-149","title":"Preliminary data from a series of artificial recharge experiments at Stanton, Texas","docAbstract":"<p>A series of artificial recharge experiments was conducted by the U.S. Geological Survey at an experimental site located in Stanton, Texas. Five tests were performed from March 1977 through December 1978 to: (1) Evaluate the hydraulic properties of the aquifer; (2) test sampling and monitoring equipment; (3) compare tracers for future use in hydrologic investigations; and (4) determine the radial and vertical distribution of hydraulic properties at the site. Suites of inorganic, and both volatile and nonvolatile organic tracers were used in the tests, and comparative data were obtained from sampling points at several radial distances and depths from the injection well. Hydraulic data from aquifer tests and geologic data from core material also were obtained during the investigation.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Denver, CO","doi":"10.3133/ofr81149","usgsCitation":"Bassett, R., Weeks, E., Ceazan, M., Perkins, S., Signor, D., Redinger, D., Malcolm, R., Aiken, G., Thurman, E., Avery, P., Wood, W., Thompson, G., and Stiles, G., 1981, Preliminary data from a series of artificial recharge experiments at Stanton, Texas: U.S. Geological Survey Open-File Report 81-149, ix, 235 p., https://doi.org/10.3133/ofr81149.","productDescription":"ix, 235 p.","costCenters":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"links":[{"id":164100,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1981/0149/report-thumb.jpg"},{"id":59601,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1981/0149/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Texas","city":"Stanton","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b06e4b07f02db69a244","contributors":{"authors":[{"text":"Bassett, R.L.","contributorId":13233,"corporation":false,"usgs":true,"family":"Bassett","given":"R.L.","email":"","affiliations":[],"preferred":false,"id":204666,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Weeks, E.P.","contributorId":38514,"corporation":false,"usgs":true,"family":"Weeks","given":"E.P.","email":"","affiliations":[],"preferred":false,"id":204669,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Ceazan, M.L.","contributorId":80015,"corporation":false,"usgs":true,"family":"Ceazan","given":"M.L.","email":"","affiliations":[],"preferred":false,"id":204673,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Perkins, S.G.","contributorId":93483,"corporation":false,"usgs":true,"family":"Perkins","given":"S.G.","email":"","affiliations":[],"preferred":false,"id":204675,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Signor, D. C.","contributorId":95100,"corporation":false,"usgs":true,"family":"Signor","given":"D. C.","affiliations":[],"preferred":false,"id":204676,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Redinger, D.L.","contributorId":103139,"corporation":false,"usgs":true,"family":"Redinger","given":"D.L.","email":"","affiliations":[],"preferred":false,"id":204678,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Malcolm, Ronald L.","contributorId":46075,"corporation":false,"usgs":true,"family":"Malcolm","given":"Ronald L.","affiliations":[],"preferred":false,"id":204670,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Aiken, G. R. 0000-0001-8454-0984","orcid":"https://orcid.org/0000-0001-8454-0984","contributorId":14452,"corporation":false,"usgs":true,"family":"Aiken","given":"G. R.","affiliations":[],"preferred":false,"id":204667,"contributorType":{"id":1,"text":"Authors"},"rank":8},{"text":"Thurman, E.M.","contributorId":102864,"corporation":false,"usgs":true,"family":"Thurman","given":"E.M.","affiliations":[],"preferred":false,"id":204677,"contributorType":{"id":1,"text":"Authors"},"rank":9},{"text":"Avery, P.A.","contributorId":52450,"corporation":false,"usgs":true,"family":"Avery","given":"P.A.","email":"","affiliations":[],"preferred":false,"id":204671,"contributorType":{"id":1,"text":"Authors"},"rank":10},{"text":"Wood, W.W.","contributorId":21974,"corporation":false,"usgs":true,"family":"Wood","given":"W.W.","email":"","affiliations":[],"preferred":false,"id":204668,"contributorType":{"id":1,"text":"Authors"},"rank":11},{"text":"Thompson, G.M.","contributorId":57246,"corporation":false,"usgs":true,"family":"Thompson","given":"G.M.","email":"","affiliations":[],"preferred":false,"id":204672,"contributorType":{"id":1,"text":"Authors"},"rank":12},{"text":"Stiles, G.K.","contributorId":91629,"corporation":false,"usgs":true,"family":"Stiles","given":"G.K.","email":"","affiliations":[],"preferred":false,"id":204674,"contributorType":{"id":1,"text":"Authors"},"rank":13}]}}
,{"id":26510,"text":"wri818 - 1981 - Selected hydrologic relationships for Soldier Creek, northeastern Kansas","interactions":[],"lastModifiedDate":"2017-12-06T13:05:19","indexId":"wri818","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1981","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"81-8","title":"Selected hydrologic relationships for Soldier Creek, northeastern Kansas","docAbstract":"<p>Hydrologic data from Soldier Creek basin were compared with relations from statewide data. The quantity and quality of streamflow were affected mostly by soils, slopes, and land use. Average annual precipitation during the study (196476) was 35.12 inches, or 2.3 percent greater than the long-term (1929-76) average. The average streamflow in Soldier Creek at Topeka, Kansas, was 23 percent greater than the long-term average.</p><p>In general, frequency curves of annual peak discharges compared poorly with curves from statewide relations due to the absence of extremely low peaks during the short period. A comparison of low-flow frequency for drainage areas of more than 100 square miles indicated that reasonable results will not be obtained for estimates of 7-day and 30-day average annual minimum discharges by linear extrapolation to basins of less than 100 square miles. Comparison of flow-duration curves confirms the extrapolation for basins of less than 100 square miles, although the percentage duration of mean flow is variable.</p><p>Water surveys showed that calcium, bicarbonate, and sulfate were the predominant ions and dissolved solids were derived mostly from limestones and shales. Suspended sediment at gaged sites ranged from 9.94 to 848 tons per day; yield per unit area increased significantly between sites due to changes in hillside slopes and land use.<br></p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri818","usgsCitation":"Carswell, W., 1981, Selected hydrologic relationships for Soldier Creek, northeastern Kansas: U.S. Geological Survey Water-Resources Investigations Report 81-8, 68 p., https://doi.org/10.3133/wri818.","productDescription":"68 p.","numberOfPages":"71","costCenters":[{"id":353,"text":"Kansas Water Science Center","active":false,"usgs":true}],"links":[{"id":349788,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1981/0008/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":157849,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1981/0008/report-thumb.jpg"}],"country":"United States","state":"Kansas","otherGeospatial":"Soldier Creek","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -96.05072021484375,\n              39.04265287290379\n            ],\n            [\n              -95.67169189453125,\n              39.04265287290379\n            ],\n            [\n              -95.67169189453125,\n              39.66914219401813\n            ],\n            [\n              -96.05072021484375,\n              39.66914219401813\n            ],\n            [\n              -96.05072021484375,\n              39.04265287290379\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49d6e4b07f02db5ddf31","contributors":{"authors":[{"text":"Carswell, William J. Jr. carswell@usgs.gov","contributorId":1787,"corporation":false,"usgs":true,"family":"Carswell","given":"William J.","suffix":"Jr.","email":"carswell@usgs.gov","affiliations":[{"id":423,"text":"National Geospatial Program","active":true,"usgs":true}],"preferred":false,"id":196517,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":31044,"text":"ofr8158 - 1981 - Methodology for hydrologic evaluation of a potential surface mine: East Trail Creek Basin, Big Horn County, Montana","interactions":[],"lastModifiedDate":"2023-01-17T22:20:28.567349","indexId":"ofr8158","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":"81-58","title":"Methodology for hydrologic evaluation of a potential surface mine: East Trail Creek Basin, Big Horn County, Montana","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr8158","usgsCitation":"Hadley, R.F., Frickel, D., Shown, L., and Miller, R., 1981, Methodology for hydrologic evaluation of a potential surface mine: East Trail Creek Basin, Big Horn County, Montana: U.S. Geological Survey Open-File Report 81-58, Report: vi, 79 p.; 1 Plate: 31.00 x 20.00 inches, https://doi.org/10.3133/ofr8158.","productDescription":"Report: vi, 79 p.; 1 Plate: 31.00 x 20.00 inches","costCenters":[],"links":[{"id":412005,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_12086.htm","linkFileType":{"id":5,"text":"html"}},{"id":59600,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1981/0058/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":20106,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1981/0058/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":163373,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1981/0058/report-thumb.jpg"}],"country":"United States","state":"Montana","county":"Big Horn County","otherGeospatial":"East Trail Creek Basin","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -106.4370,\n              45.119\n            ],\n            [\n              -106.4370,\n              45.023\n            ],\n            [\n              -106.209,\n              45.023\n            ],\n            [\n              -106.209,\n              45.119\n            ],\n            [\n              -106.4370,\n              45.119\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a51e4b07f02db629fc3","contributors":{"authors":[{"text":"Hadley, R. F.","contributorId":27028,"corporation":false,"usgs":true,"family":"Hadley","given":"R.","middleInitial":"F.","affiliations":[],"preferred":false,"id":204663,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Frickel, D. G.","contributorId":11213,"corporation":false,"usgs":true,"family":"Frickel","given":"D. G.","affiliations":[],"preferred":false,"id":204662,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Shown, L. M.","contributorId":43757,"corporation":false,"usgs":true,"family":"Shown","given":"L. M.","affiliations":[],"preferred":false,"id":204664,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Miller, R.F.","contributorId":83882,"corporation":false,"usgs":true,"family":"Miller","given":"R.F.","email":"","affiliations":[],"preferred":false,"id":204665,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":48728,"text":"ofr81546 - 1981 - Hydrologic monitoring in the area of the Tennessee-Tombigbee Waterway, Mississippi-Alabama","interactions":[],"lastModifiedDate":"2012-02-02T00:10:07","indexId":"ofr81546","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":"81-546","title":"Hydrologic monitoring in the area of the Tennessee-Tombigbee Waterway, Mississippi-Alabama","language":"ENGLISH","doi":"10.3133/ofr81546","usgsCitation":"Tomaszewski, D., 1981, Hydrologic monitoring in the area of the Tennessee-Tombigbee Waterway, Mississippi-Alabama: U.S. Geological Survey Open-File Report 81-546, 142 p. : ill., map ; 29 x 40 cm., https://doi.org/10.3133/ofr81546.","productDescription":"142 p. : ill., map ; 29 x 40 cm.","costCenters":[],"links":[{"id":162232,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad4e4b07f02db682f59","contributors":{"authors":[{"text":"Tomaszewski, D.J.","contributorId":67928,"corporation":false,"usgs":true,"family":"Tomaszewski","given":"D.J.","email":"","affiliations":[],"preferred":false,"id":238118,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":48714,"text":"ofr81410 - 1981 - Hydrologic data for the Cache Creek-Bear Thrust environmental impact statement near Jackson, Wyoming","interactions":[],"lastModifiedDate":"2012-02-02T00:10:22","indexId":"ofr81410","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":"81-410","title":"Hydrologic data for the Cache Creek-Bear Thrust environmental impact statement near Jackson, Wyoming","docAbstract":"Information on the quantity and quality of surface and ground water in an area of concern for the Cache Creek-Bear Thrust Environmental Impact Statement in northwestern Wyoming is presented without interpretation. The environmental impact statement is being prepared jointly by the U.S. Geological Survey and the U.S. Forest Service and concerns proposed exploration and development of oil and gas on leased Federal land near Jackson, Wyoming. Information includes data from a gaging station on Cache Creek and from wells, springs, and miscellaneous sites on streams. Data include streamflow, chemical and suspended-sediment quality of streams, and the occurrence and chemical quality of ground water. (USGS)","language":"ENGLISH","doi":"10.3133/ofr81410","usgsCitation":"Craig, G., Ringen, B.H., and Cox, E., 1981, Hydrologic data for the Cache Creek-Bear Thrust environmental impact statement near Jackson, Wyoming: U.S. Geological Survey Open-File Report 81-410, vii, 34 p. (some folded) : maps ; 29 cm., https://doi.org/10.3133/ofr81410.","productDescription":"vii, 34 p. (some folded) : maps ; 29 cm.","costCenters":[],"links":[{"id":169415,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1981/0410/report-thumb.jpg"},{"id":85507,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1981/0410/plate-01.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":85508,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1981/0410/plate-02.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":85509,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1981/0410/plate-03.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":85510,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1981/0410/plate-04.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":85511,"rank":404,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1981/0410/plate-05.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":85512,"rank":405,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1981/0410/plate-06.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":85513,"rank":406,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1981/0410/plate-07.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":85514,"rank":407,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1981/0410/plate-08.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":85515,"rank":408,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1981/0410/plate-09.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":85516,"rank":409,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1981/0410/plate-10.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":85517,"rank":410,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1981/0410/plate-11.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":85518,"rank":411,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1981/0410/plate-12.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":85519,"rank":412,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1981/0410/plate-13.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":85520,"rank":413,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1981/0410/plate-14.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":85521,"rank":414,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1981/0410/plate-15.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":85522,"rank":415,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1981/0410/plate-16.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":85523,"rank":416,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1981/0410/plate-17.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":85524,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1981/0410/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a1ce4b07f02db6083c0","contributors":{"authors":[{"text":"Craig, G.S. Jr.","contributorId":73624,"corporation":false,"usgs":true,"family":"Craig","given":"G.S.","suffix":"Jr.","email":"","affiliations":[],"preferred":false,"id":238095,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Ringen, B. H.","contributorId":13987,"corporation":false,"usgs":true,"family":"Ringen","given":"B.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":238094,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Cox, E.R.","contributorId":6094,"corporation":false,"usgs":true,"family":"Cox","given":"E.R.","email":"","affiliations":[],"preferred":false,"id":238093,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":48683,"text":"ofr81217 - 1981 - Effects of placer mining on hydrologic systems in Alaska; status of knowledge","interactions":[],"lastModifiedDate":"2012-02-02T00:10:44","indexId":"ofr81217","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":"81-217","title":"Effects of placer mining on hydrologic systems in Alaska; status of knowledge","docAbstract":"The report briefly summarizes the current state of knowledge regarding placer mining in Alaska. A review of literature indicates that nearly all of the significant information on the effects of placer mining on the hydrologic system in Alaska is referenced in available reports. The addition of sediment, as well as other indirect changes this generates, appears to be the primary impact of placer mining on Alaskan streams. Other potential water-quality effects that should be considered are: increases in organic loading in the stream system; increases in minor element content; potential for acid drainage; and impacts on fish and other aquatic biota. Existing information is adequate to define parameters that may be affected by placer mining but inadequate to quantify changes resulting from an individual mining operation or to allow the prediction of the magnitude or duration of the impact. Additional studies that would improve the knowledge of the effects of placer mining include: short-term assessments, using available photographic information and existing hydrologic records, to document historical changes and active placer mining features; short-term studies using emperical sediment-transport formulas to estimate the effects of placer mine activities; and river quality assessments of selected basins affected by placer mining. (USGS)","language":"ENGLISH","doi":"10.3133/ofr81217","usgsCitation":"Madison, R.J., 1981, Effects of placer mining on hydrologic systems in Alaska; status of knowledge: U.S. Geological Survey Open-File Report 81-217, iii, 28 p. : ill. ; 29 cm., https://doi.org/10.3133/ofr81217.","productDescription":"iii, 28 p. : ill. ; 29 cm.","costCenters":[],"links":[{"id":171486,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1981/0217/report-thumb.jpg"},{"id":85491,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1981/0217/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a29e4b07f02db611af6","contributors":{"authors":[{"text":"Madison, R. J.","contributorId":84734,"corporation":false,"usgs":true,"family":"Madison","given":"R.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":238016,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":48679,"text":"ofr81205 - 1981 - Potentiometric surface of the Floridan aquifer in the Northwest Florida Water Management District, May 1980","interactions":[],"lastModifiedDate":"2012-02-02T00:10:44","indexId":"ofr81205","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":"81-205","title":"Potentiometric surface of the Floridan aquifer in the Northwest Florida Water Management District, May 1980","docAbstract":"A May 1980 potentiometric surface map of the Northwest Florida Water Management District depicts water levels in wells tapping the Floridan aquifer prior to summer pumpage. Compared to earlier potentiometric maps of the area, there are no significant differences in the 1980 map that are the result of hydrologic conditions. The addition of numerous new monitor wells in Jackson, Calhoun, Gadsden, and Liberty Counties, however, permitted refinement or better delineation of contours and a separation of water-bearing zones of the Floridan aquifer in the latter two counties. (USGS)","language":"ENGLISH","doi":"10.3133/ofr81205","usgsCitation":"Rosenau, J., and Milner, R., 1981, Potentiometric surface of the Floridan aquifer in the Northwest Florida Water Management District, May 1980: U.S. Geological Survey Open-File Report 81-205, 1 sheet; map 61 x 91 cm. fold. in envelope 25 x 31 cm., https://doi.org/10.3133/ofr81205.","productDescription":"1 sheet; map 61 x 91 cm. fold. in envelope 25 x 31 cm.","costCenters":[],"links":[{"id":171482,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a81e4b07f02db64a1f8","contributors":{"authors":[{"text":"Rosenau, J.C.","contributorId":99192,"corporation":false,"usgs":true,"family":"Rosenau","given":"J.C.","email":"","affiliations":[],"preferred":false,"id":238011,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Milner, R.S.","contributorId":75614,"corporation":false,"usgs":true,"family":"Milner","given":"R.S.","email":"","affiliations":[],"preferred":false,"id":238010,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":40197,"text":"ofr8198 - 1981 - Complete Bouguer map of the Medicine Lake quadrangle, California","interactions":[],"lastModifiedDate":"2023-08-02T19:07:50.97202","indexId":"ofr8198","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":"81-98","title":"Complete Bouguer map of the Medicine Lake quadrangle, California","docAbstract":"A mathematical technique, called kriging, was programmed for a computer to interpolate hydrologic data based on a network of measured values in west-central Kansas. The computer program generated estimated values at the center of each 1-mile section in the Western Kansas Groundwater Management District No. 1 and facilitated contouring of selected values that are needed in the effective management of ground water for irrigation. The kriging technique produced objective and reproducible maps that illustrated hydrologic conditions in the Ogallala aquifer, the principal source of water in west-central Kansas. Maps of the aquifer, which use a 3-year average, included the 1978-80 water-table altitudes, which ranged from about 2,580 to 3,720 feet; the 1978-80 saturated thicknesses, which ranged from about 0 to 250 feet; and the percentage changes in saturated thickness from 1950 to 1978-80, which ranged from about a 50-percent increase to a 100-percent decrease. A map showing errors of estimate also was provided as a measure of reliability for the 1978-80 water-table altitudes. Errors of estimate ranged from 2 to 24 feet. (USGS)","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr8198","usgsCitation":"Finn, C.A., 1981, Complete Bouguer map of the Medicine Lake quadrangle, California: U.S. Geological Survey Open-File Report 81-98, 1 Plate: 23.19 × 28.38 inches, https://doi.org/10.3133/ofr8198.","productDescription":"1 Plate: 23.19 × 28.38 inches","costCenters":[],"links":[{"id":171094,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":70456,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1981/0098/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":390218,"rank":2,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_12230.htm"}],"country":"United States","state":"California","otherGeospatial":"Medicine Lake quadrangle","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -121.75,\n              41.5\n            ],\n            [\n              -121.5,\n              41.5\n            ],\n            [\n              -121.5,\n              41.75\n            ],\n            [\n              -121.75,\n              41.75\n            ],\n            [\n              -121.75,\n              41.5\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1ae4b07f02db6a8400","contributors":{"authors":[{"text":"Finn, Carol A. 0000-0002-6178-0405 cfinn@usgs.gov","orcid":"https://orcid.org/0000-0002-6178-0405","contributorId":1326,"corporation":false,"usgs":true,"family":"Finn","given":"Carol","email":"cfinn@usgs.gov","middleInitial":"A.","affiliations":[{"id":211,"text":"Crustal Geophysics and Geochemistry Science Center","active":true,"usgs":true}],"preferred":true,"id":223104,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":48529,"text":"ofr80964 - 1981 - Water resources of Prince William Forest Park, Virginia","interactions":[],"lastModifiedDate":"2012-02-02T00:10:04","indexId":"ofr80964","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":"80-964","title":"Water resources of Prince William Forest Park, Virginia","docAbstract":"Prince William Forest Park is in the southern part of Prince William County, Va. Its natural beauty and nearness to Washington, D.C. have made it one of the most popular recreation areas in northern Virginia. To help the National Park Service plan the development of new facilities and effectively manage its total resources, the U.S. Geological Survey made a hydrologic study of the park from October 1972 to November 1975. The overall objective of the Survey 's study was to evalute the quantity and quality of the park 's water resources. Available information was compiled and analyzed, and new data on streamflow, ground-water levels, and the chemical quality of water were collected. Test wells were drilled and aquifer tests made at the sites of wells to evaluate the occurrence and availability of ground water. (USGS)","language":"ENGLISH","doi":"10.3133/ofr80964","usgsCitation":"Brown, G.A., 1981, Water resources of Prince William Forest Park, Virginia: U.S. Geological Survey Open-File Report 80-964, 2 maps on 2 sheets ; 51 x 52 cm. on sheets 101 x 108 cm., https://doi.org/10.3133/ofr80964.","productDescription":"2 maps on 2 sheets ; 51 x 52 cm. on sheets 101 x 108 cm.","costCenters":[],"links":[{"id":161959,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":85345,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1980/0964/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":85346,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1980/0964/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e48d2e4b07f02db54806d","contributors":{"authors":[{"text":"Brown, G. Allan","contributorId":29788,"corporation":false,"usgs":true,"family":"Brown","given":"G.","email":"","middleInitial":"Allan","affiliations":[],"preferred":false,"id":237684,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":36649,"text":"fwsobs81_26 - 1981 - Effects of habitat alterations on riparian plant and animal communities in Iowa","interactions":[],"lastModifiedDate":"2017-03-06T12:11:07","indexId":"fwsobs81_26","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1981","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":1,"text":"Federal Government Series"},"seriesTitle":{"id":20,"text":"FWS/OBS","active":false,"publicationSubtype":{"id":1}},"seriesNumber":"81/26","title":"Effects of habitat alterations on riparian plant and animal communities in Iowa","docAbstract":"<p>A large proportion of the streams in the Midwest have been channelized to facilitate wetlands drainage, reduce flooding, and encourage various floodplain development activities. Changes that result from stream channelization impact hydrological and ecological processes that in turn affect fish and wildlife populations. This study was conducted to better describe the changes that occur in riparian ecosystems located adjacent to selected Iowa streams.</p>","language":"English","publisher":"U.S. Fish and Wildlife Service","usgsCitation":"Best, L.B., Stauffer, D., Geier, A., Varland, K., Vogler, J., Dahlgren, R., and Landers, R., 1981, Effects of habitat alterations on riparian plant and animal communities in Iowa: FWS/OBS 81/26, 55 p.","productDescription":"55 p.","costCenters":[],"links":[{"id":164507,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a2ee4b07f02db6152f1","contributors":{"authors":[{"text":"Best, Louis B.","contributorId":52525,"corporation":false,"usgs":true,"family":"Best","given":"Louis","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":216732,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Stauffer, D.F.","contributorId":9317,"corporation":false,"usgs":true,"family":"Stauffer","given":"D.F.","email":"","affiliations":[],"preferred":false,"id":216728,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Geier, A.R.","contributorId":101720,"corporation":false,"usgs":true,"family":"Geier","given":"A.R.","email":"","affiliations":[],"preferred":false,"id":216733,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Varland, K.L.","contributorId":11668,"corporation":false,"usgs":true,"family":"Varland","given":"K.L.","email":"","affiliations":[],"preferred":false,"id":216729,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Vogler, J.P.","contributorId":104118,"corporation":false,"usgs":true,"family":"Vogler","given":"J.P.","email":"","affiliations":[],"preferred":false,"id":216734,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Dahlgren, R.B.","contributorId":18819,"corporation":false,"usgs":true,"family":"Dahlgren","given":"R.B.","email":"","affiliations":[],"preferred":false,"id":216731,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Landers, R.Q.","contributorId":12088,"corporation":false,"usgs":true,"family":"Landers","given":"R.Q.","email":"","affiliations":[],"preferred":false,"id":216730,"contributorType":{"id":1,"text":"Authors"},"rank":7}]}}
,{"id":25754,"text":"wri8136 - 1981 - Results of hydrologic tests and water-chemistry analyses, wells H-4A, H-4B, and H-4C, at the proposed waste isolation pilot plant site, southeastern New Mexico","interactions":[],"lastModifiedDate":"2025-07-21T17:28:21.92385","indexId":"wri8136","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1981","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"81-36","title":"Results of hydrologic tests and water-chemistry analyses, wells H-4A, H-4B, and H-4C, at the proposed waste isolation pilot plant site, southeastern New Mexico","docAbstract":"Data were collected during hydrologic testing at wells H-4A, H-4B, and H-4C in the southern part of the proposed Waste Isolation Pilot Plant site in southeastern New Mexico. The three water-bearing zones tested, the Magenta and Culebra Dolomite Members of the Rustler Formation and the Rustler Formation-Salado Formation contact, yield water to wells at rates less than 0.9 gallon per minute. Throughout the testing, water-pressure response in the tested zone was monitored by a pressure transducer system. Shut-in and slug tests were conducted to acquire the data from which the following values were derived. Calculated transmissivities for the Magenta, Culebra and the Rustler-Salado contact at wells H-4A, H-4B, and H-4C were 0.06, 0.9, and 0.0006 foot squared per day respectively. Water samples from the Magenta and Culebra had dissolved-solids concentrations of 22,300 and 18,100 milligrams per liter, respectively. The major chemical constituents of ground-water samples from these two zones were sodium, chloride, and sulfate. Water samples from the Rustler-Salado contact had a dissolved-solids concentration of 322,000 milligrams per liter and magnesium, sodium, and chloride were the major constituents. Radium-226, a naturally occurring radioactive element, was present in samples from all three zones. (USGS)","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri8136","usgsCitation":"Mercer, J.W., Davis, P., Dennehy, K., and Goetz, C.L., 1981, Results of hydrologic tests and water-chemistry analyses, wells H-4A, H-4B, and H-4C, at the proposed waste isolation pilot plant site, southeastern New Mexico: U.S. Geological Survey Water-Resources Investigations Report 81-36, vii, 92 p., https://doi.org/10.3133/wri8136.","productDescription":"vii, 92 p.","costCenters":[],"links":[{"id":157099,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1981/0036/report-thumb.jpg"},{"id":492651,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1981/0036/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"New 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L.","contributorId":55845,"corporation":false,"usgs":true,"family":"Goetz","given":"C.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":194935,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":31091,"text":"ofr81628 - 1981 - Hydrologic data for urban studies in the Austin, Texas, metropolitan area, 1979","interactions":[],"lastModifiedDate":"2025-09-11T16:18:31.221766","indexId":"ofr81628","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":"81-628","title":"Hydrologic data for urban studies in the Austin, Texas, metropolitan area, 1979","docAbstract":"<p>Hydrologic investigations of urban watersheds in Texas were begun by theU.S. Geological Survey in 1954. Studies are now in progress in Austin, Houston, and San Antonio. Studies have been completed in the Dallas and Fort Worth areas.</p><p>The Geological Survey, in cooperation with the Texas Department of Water Resources, began hydrologic studies in the Austin urban area in 1954. In cooperation with the city of Austin, the program was expanded in 1975 to include additional streamflow and rainfall gaging stations, and the collection of surface water-quality data. In 1978, the program was expanded to include a ground-water resources study of the South Austin metropolitan area in the Balcones fault zone.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr81628","usgsCitation":"Slade, R., Dorsey, M., Gordon, J., Mitchell, R., and Gaylord, J., 1981, Hydrologic data for urban studies in the Austin, Texas, metropolitan area, 1979: U.S. Geological Survey Open-File Report 81-628, 281 p., https://doi.org/10.3133/ofr81628.","productDescription":"281 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"links":[{"id":495330,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1981/0628/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":160830,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1981/0628/report-thumb.jpg"}],"country":"United States","state":"Texas","city":"Austin","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -98.09280395507812,\n              29.991812888666043\n            ],\n            [\n              -97.38006591796874,\n              29.991812888666043\n            ],\n            [\n              -97.38006591796874,\n              30.615459280672667\n            ],\n            [\n              -98.09280395507812,\n              30.615459280672667\n            ],\n            [\n              -98.09280395507812,\n              29.991812888666043\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a1ce4b07f02db607f18","contributors":{"authors":[{"text":"Slade, R.M.","contributorId":84364,"corporation":false,"usgs":true,"family":"Slade","given":"R.M.","affiliations":[],"preferred":false,"id":204939,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Dorsey, M.E.","contributorId":73997,"corporation":false,"usgs":true,"family":"Dorsey","given":"M.E.","email":"","affiliations":[],"preferred":false,"id":204938,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Gordon, J.D.","contributorId":26684,"corporation":false,"usgs":true,"family":"Gordon","given":"J.D.","email":"","affiliations":[],"preferred":false,"id":204936,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Mitchell, R.N.","contributorId":94301,"corporation":false,"usgs":true,"family":"Mitchell","given":"R.N.","email":"","affiliations":[],"preferred":false,"id":204940,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Gaylord, J.L.","contributorId":46520,"corporation":false,"usgs":true,"family":"Gaylord","given":"J.L.","email":"","affiliations":[],"preferred":false,"id":204937,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":7811,"text":"ofr81686 - 1981 - Analysis and computer simulation of stream-aquifer hydrology, Arkansas River valley, southwestern Kansas","interactions":[{"subject":{"id":7811,"text":"ofr81686 - 1981 - Analysis and computer simulation of stream-aquifer hydrology, Arkansas River valley, southwestern Kansas","indexId":"ofr81686","publicationYear":"1981","noYear":false,"title":"Analysis and computer simulation of stream-aquifer hydrology, Arkansas River valley, southwestern Kansas"},"predicate":"SUPERSEDED_BY","object":{"id":982,"text":"wsp2200 - 1983 - Analysis and computer simulation of stream-aquifer hydrology, Arkansas River Valley, southwestern Kansas","indexId":"wsp2200","publicationYear":"1983","noYear":false,"title":"Analysis and computer simulation of stream-aquifer hydrology, Arkansas River Valley, southwestern Kansas"},"id":1}],"supersededBy":{"id":982,"text":"wsp2200 - 1983 - Analysis and computer simulation of stream-aquifer hydrology, Arkansas River Valley, southwestern Kansas","indexId":"wsp2200","publicationYear":"1983","noYear":false,"title":"Analysis and computer simulation of stream-aquifer hydrology, Arkansas River Valley, southwestern Kansas"},"lastModifiedDate":"2025-12-08T19:05:44.313095","indexId":"ofr81686","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":"81-686","title":"Analysis and computer simulation of stream-aquifer hydrology, Arkansas River valley, southwestern Kansas","docAbstract":"<p>A study was made, in cooperation with the Division of Water Resources, Kansas State Board of Agriculture, to determine geohydrologic conditions underlying nearly 110,000 acres of the Arkansas River Valley between the Colorado-Kansas State line and the Bear Creek Fault zone in southwestern Kansas. The Arkansas River meanders atop and interacts hydraulically with the area's unconfined sand and gravel aquifer. Owing to decreasing recharge and increasing discharge during the 1970's, water levels declined an average of 4 feet during 1970-79. Average annual streamflow at Syracuse, Kansas, also decreased from 232 cubic feet per second during 1951-69 to 85 cubic feet per second during 1970-79.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr81686","usgsCitation":"Barker, R., Dunlap, L.E., and Sauer, C.G., 1981, Analysis and computer simulation of stream-aquifer hydrology, Arkansas River valley, southwestern Kansas: U.S. Geological Survey Open-File Report 81-686, Report: 130 p.; 1 Plate: 45.28 x 23.50 inches; 54 Figures: 12.40 x 8.24 inches or smaller, https://doi.org/10.3133/ofr81686.","productDescription":"Report: 130 p.; 1 Plate: 45.28 x 23.50 inches; 54 Figures: 12.40 x 8.24 inches or smaller","costCenters":[],"links":[{"id":495571,"rank":56,"type":{"id":29,"text":"Figure"},"url":"https://pubs.usgs.gov/of/1981/0686/figure-53.pdf","text":"Figure 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,{"id":57429,"text":"wdrOH802 - 1981 - Water resources data for Ohio, water year 1980: Volume 2. St. Lawrence River Basin","interactions":[],"lastModifiedDate":"2025-12-11T16:28:13.527222","indexId":"wdrOH802","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1981","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":340,"text":"Water Data Report","code":"WDR","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"OH-80-2","title":"Water resources data for Ohio, water year 1980: Volume 2. St. Lawrence River Basin","docAbstract":"<p>Water resources data for the 1980 water year for Ohio consist of records of stage, discharge, and water quality of streams; stage and contents, and water quality of lakes and reservoirs; and water levels and water quality of ground-water wells. This report in two volumes and one appendix contains records for water discharge at 169 gaging stations; stage and contents at 39 lakes and reservoirs; water quality at 57 gaging stations and 83 wells; and water levels at 183 observation wells. Also included are data from 84 crest-stage partial-record stations; 91 low-flow partial-record stations, and 537 coal hydrology synoptic sites. Additional water data were collected at various sites not involved in the systematic data-collection program and are published as miscellaneous measurements and analyses. These data represent that part of the National Water Data System collected by the U.S. Geological Survey and cooperating State and Federal agencies in Ohio.&nbsp;</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wdrOH802","collaboration":"Prepared in cooperation with the State of Ohio and with other agencies","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1981, Water resources data for Ohio, water year 1980: Volume 2. 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,{"id":9637,"text":"ofr81424 - 1981 - Outline for a hydrologic data base for Portugal","interactions":[],"lastModifiedDate":"2025-09-23T15:18:24.17282","indexId":"ofr81424","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":"81-424","title":"Outline for a hydrologic data base for Portugal","docAbstract":"<p>The Agency for International Development requested the assistance of the U.S. Geological Survey (USGS) to help the Government of Portugal in the investigation and management of ground water resources in the Algarve region. The assistance was to be provided in four specialty areas, but the scope of this report is limited to making recommendations on the design of a hydrologic data base for Portugal.</p><p>It is recommended that a small data base be developed initially to meet the needs for ground-water data in the Algarve region utilizing personnel in the Division of Geohydrology in the Directorate of Water Resources Development. This data base may eventually be expanded to cover all regions of Portugal and include all types of hydrologic data, including streamflow, precipitation, and surface-water quality, as well as groundwater data. Consideration should be given to implementing a commercial data base management system (DBMS) in 2-3 years when significant amounts of data, including surface-water data, begin to be entered from other regions of Portugal.</p><p>Training in computer programming and data base systems should be provided to provide a broad base of support for the data base system and groundwater modeling.</p><p>It is also recommended that a uniform system for identifying hydrologic sites and basins be developed for eventual use by all agencies (departments) involved in water resources development and management in Portugal.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr81424","usgsCitation":"Hutchison, N.E., 1981, Outline for a hydrologic data base for Portugal: U.S. Geological Survey Open-File Report 81-424, iv, 142 p., https://doi.org/10.3133/ofr81424.","productDescription":"iv, 142 p.","costCenters":[],"links":[{"id":495902,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1981/0424/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":141966,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1981/0424/report-thumb.jpg"}],"country":"Portugal","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -6.041841774705205,\n              42.33077581152199\n            ],\n            [\n              -9.882871059050842,\n              42.33077581152199\n            ],\n            [\n              -9.882871059050842,\n              36.77641394499072\n            ],\n            [\n              -6.041841774705205,\n              36.77641394499072\n            ],\n            [\n              -6.041841774705205,\n              42.33077581152199\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae4e4b07f02db68a3bd","contributors":{"authors":[{"text":"Hutchison, Norman E.","contributorId":71161,"corporation":false,"usgs":true,"family":"Hutchison","given":"Norman","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":160030,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":8969,"text":"ofr80422 - 1981 - Model of the ground-water flow system of the Gordo and Eutaw aquifers in west-central Alabama","interactions":[],"lastModifiedDate":"2025-09-15T15:48:19.995794","indexId":"ofr80422","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":"80-422","title":"Model of the ground-water flow system of the Gordo and Eutaw aquifers in west-central Alabama","docAbstract":"<p>Hydrologic conditions for a two-aquifer system consisting of the Gordo and Eutaw aquifers of Cretaceous age in west-central Alabama were simulated using a three-dimensional finite difference digital model. The model was calibrated to observed heads in the aquifers using a least squares method for obtaining the values for hydraulic parameters which provided the best fit to 28 calibration points in the model. The standard error of estimate for computed heads in the model is 3.46 feet.</p><p>Data collected during the period of 1900 to 1970 indicate that the modeled aquifer system is in a steady-state condition. The results of steady-state model simulations show that about 56 percent of the discharge from the system is by upward vertical leakage through confining beds to rivers, about 18 percent is to unregulated flowing wells, 10 percent is to pumped wells, and 16 percent is to boundaries. The areal distribution of water in the aquifer containing chloride concentrations greater than 1,000 mg/L appears to be related to flow patterns in the system.</p><p>Areas of greatest head loss in the system are those where there is natural discharge and pumpage. More than 80 percent of the head loss in the system can be attributed to natural discharge by upward leakage through the confining beds.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr80422","collaboration":"Prepared by the United States Geological Survey in cooperation with Geological Survey of Alabama","usgsCitation":"Gardner, R.A., 1981, Model of the ground-water flow system of the Gordo and Eutaw aquifers in west-central Alabama: U.S. Geological Survey Open-File Report 80-422, Report: 30 p.; 23 Figures: 7.61 x 10.38 inches or smaller, https://doi.org/10.3133/ofr80422.","productDescription":"Report: 30 p.; 23 Figures: 7.61 x 10.38 inches or smaller","costCenters":[],"links":[{"id":495502,"rank":24,"type":{"id":29,"text":"Figure"},"url":"https://pubs.usgs.gov/of/1980/0422/figure-24.pdf","text":"Figure 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,{"id":70011941,"text":"70011941 - 1981 - Patterns of groundwater salinity changes in a deep continental-oceanic transect off the southeastern Atlantic coast of the U.S.A.","interactions":[],"lastModifiedDate":"2025-04-10T23:08:29.015147","indexId":"70011941","displayToPublicDate":"1981-12-01T00:00:00","publicationYear":"1981","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2342,"text":"Journal of Hydrology","active":true,"publicationSubtype":{"id":10}},"title":"Patterns of groundwater salinity changes in a deep continental-oceanic transect off the southeastern Atlantic coast of the U.S.A.","docAbstract":"<p>Investigations of formation-fluid salinities in a transect from western Georgia to the edge of the Blake Plateau off the coast of Georgia show surprisingly similar hydrochemical features offshore and onshore. A fresh-brackish wedge of groundwater (&lt;25 g/kg total dissolved solids) lies beneath the shelf to a depth of <span>∼ </span>900 m. On land, brackish waters extend to a maximum depth of <span>∼ </span>1.2 km below sea level in Lowndes County, Georgia. In deeper horizons, hypersaline brines (&gt; 100 g/kg) occur in Lower Cretaceous (?) strata. These strata have a pronounced evaporitic (anhydritic) character in the offshore segment. Strong salinity gradients in interstitial waters signify buried evaporite deposits at drill sites beneath the Blake Plateau.&nbsp;</p>","language":"English","publisher":"Elsevier","doi":"10.1016/0022-1694(81)90154-2","issn":"00221694","usgsCitation":"Manheim, F., and Paull, C.K., 1981, Patterns of groundwater salinity changes in a deep continental-oceanic transect off the southeastern Atlantic coast of the U.S.A.: Journal of Hydrology, v. 54, no. 1-3, p. 95-105, https://doi.org/10.1016/0022-1694(81)90154-2.","productDescription":"11 p.","startPage":"95","endPage":"105","costCenters":[],"links":[{"id":221140,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Florida, Georgia, South Carolina","otherGeospatial":"southeastern Atlantic coast of the U.S.A.","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -78.96091688004468,\n              33.8070332900253\n            ],\n            [\n              -81.47050643744609,\n              33.8070332900253\n            ],\n            [\n              -81.47050643744609,\n              29.204934495587977\n            ],\n            [\n              -78.96091688004468,\n              29.204934495587977\n            ],\n            [\n              -78.96091688004468,\n              33.8070332900253\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","volume":"54","issue":"1-3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a75d3e4b0c8380cd77d78","contributors":{"authors":[{"text":"Manheim, F.T. 0000-0003-4005-4524","orcid":"https://orcid.org/0000-0003-4005-4524","contributorId":55421,"corporation":false,"usgs":true,"family":"Manheim","given":"F.T.","affiliations":[],"preferred":false,"id":362355,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Paull, C. K.","contributorId":86845,"corporation":false,"usgs":false,"family":"Paull","given":"C.","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":362356,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70012013,"text":"70012013 - 1981 - Geological considerations in hazardous waste disposal","interactions":[],"lastModifiedDate":"2025-04-10T23:01:49.439277","indexId":"70012013","displayToPublicDate":"1981-12-01T00:00:00","publicationYear":"1981","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2342,"text":"Journal of Hydrology","active":true,"publicationSubtype":{"id":10}},"title":"Geological considerations in hazardous waste disposal","docAbstract":"<p>Present regulations assume that long-term isolation of hazardous wastes - including toxic chemical, biological, radioactive, flammable and explosive wastes - may be effected by disposal in landfills that have liners of very low hydraulic conductivity. In reality, total isolation of wastes in humid areas is not possible; some migration of leachate from wastes buried in the gound will always occur. </p><p>Regulations should provide performance standards applicable on a site-by-site basis rather than rigid criteria for site selection and design. The performance standards should take into account several factors: (1) the categories, segregation, degradation and toxicity of the wastes; (2) the site hydrogeology, which governs the direction and rate of contaminant transport; (3) the attenuation of contaminants by geochemical interactions with geologic materials; and (4) the release rate of unattenuated pollutants to surface or groundwater. An adequate monitoring system is essential. The system should both test the extent to which the operation of the site meets performance standards and provide sufficient warning of pollution problems to allow implementation of remedial measures. </p><p>In recent years there has been a trend away from numerous, small disposal sites toward fewer and larger sites. The size of a disposal site should be based on the attenuation capacity of the geologic material, which has a finite, though generally not well-defined, limit. For slowly degradable wastes, engineered sites with leachate-collection systems appear to be only a temporary solution since the leachate collected will also require final disposal.&nbsp;</p>","language":"English","publisher":"Elsevier","doi":"10.1016/0022-1694(81)90168-2","issn":"00221694","usgsCitation":"Cartwright, K., Gilkeson, R.H., and Johnson, T., 1981, Geological considerations in hazardous waste disposal: Journal of Hydrology, v. 54, no. 1-3, p. 357-369, https://doi.org/10.1016/0022-1694(81)90168-2.","productDescription":"13 p.","startPage":"357","endPage":"369","costCenters":[],"links":[{"id":222235,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"54","issue":"1-3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a225de4b0c8380cd56f97","contributors":{"authors":[{"text":"Cartwright, K.","contributorId":50292,"corporation":false,"usgs":true,"family":"Cartwright","given":"K.","email":"","affiliations":[],"preferred":false,"id":362516,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Gilkeson, R. H.","contributorId":17764,"corporation":false,"usgs":false,"family":"Gilkeson","given":"R.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":362514,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Johnson, T.M.","contributorId":22332,"corporation":false,"usgs":true,"family":"Johnson","given":"T.M.","affiliations":[],"preferred":false,"id":362515,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70186168,"text":"70186168 - 1981 - Role of numerical simulation in analysis of ground-water quality problems","interactions":[],"lastModifiedDate":"2021-03-25T20:00:11.444584","indexId":"70186168","displayToPublicDate":"1981-11-01T00:00:00","publicationYear":"1981","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3352,"text":"Science of the Total Environment","active":true,"publicationSubtype":{"id":10}},"title":"Role of numerical simulation in analysis of ground-water quality problems","docAbstract":"<p><span>The increasing public awareness and concern about the hazards of toxic chemicals contaminating aquifers has created an increased need for predictive capabilities to analyze ground-water contamination problems. Several digital models to simulate the movement and concentration of ground-water contaminants have been documented recently. Most simulate the transport and dispersion of a nonreactive solute, but some include mathematically simple reaction terms to represent decay and sorption processes. For applications to field problems, these solute-transport models impose data requirements that, in general, exceed our practical capabilities to accurately describe the field properties and stresses of the hydraulic and chemical systems. Thus, interpretations based on model analyses must recognize the significance of uncertainties in input data. Models of ground-water systems should be regarded as just one tool among many that can be used in the analysis of a ground-water quality problem. Numerical simulation can help the analyst integrate available data, evaluate conceptual models, test hypotheses pertaining to flow and quality changes, and predict system responses to alternative stresses. The models do not replace field data, but they do offer a feedback mechanism that can help to guide the design of a more effective and more efficient data-collection program.</span></p>","language":"English","publisher":"Elsevier","doi":"10.1016/0048-9697(81)90163-7","usgsCitation":"Konikow, L.F., 1981, Role of numerical simulation in analysis of ground-water quality problems: Science of the Total Environment, v. 21, p. 299-312, https://doi.org/10.1016/0048-9697(81)90163-7.","productDescription":"14 p.","startPage":"299","endPage":"312","costCenters":[{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":338831,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"21","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"58de1955e4b02ff32c699ce1","contributors":{"authors":[{"text":"Konikow, Leonard F. 0000-0002-0940-3856 lkonikow@usgs.gov","orcid":"https://orcid.org/0000-0002-0940-3856","contributorId":158,"corporation":false,"usgs":true,"family":"Konikow","given":"Leonard","email":"lkonikow@usgs.gov","middleInitial":"F.","affiliations":[{"id":436,"text":"National Research Program - Eastern Branch","active":true,"usgs":true}],"preferred":true,"id":687740,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70185632,"text":"70185632 - 1981 - Subsurface injection of liquid waste in Florida, United States of America","interactions":[],"lastModifiedDate":"2020-01-26T10:02:17","indexId":"70185632","displayToPublicDate":"1981-11-01T00:00:00","publicationYear":"1981","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":5331,"text":"Science of Total Environment","active":true,"publicationSubtype":{"id":10}},"title":"Subsurface injection of liquid waste in Florida, United States of America","docAbstract":"<p><span>In 1979, liquid waste was injected into the subsurface of Florida by 10 injection systems at an aggregate average rate of 165,000 m</span><sup>3</sup><span>/d. All the systems inject into carbonate rocks that contain salty water. Extensive precautions are taken in the construction of the injection wells and in the monitoring of their operation to provide assurance that overlying and laterally contiguous freshwater resources do not become contaminated with either the injected waste or the saltwater displaced by the waste. Several concerns relating to the effectiveness of the confining bed above the injection zone for containing the injected wastes have arisen over the years. These concerns accentuate the value of a well-planned and implemented monitoring program from which one can evaluate the potential impact of waste injection on the subsurface environment.</span></p>","language":"English","publisher":"Elsevier","doi":"10.1016/0048-9697(81)90146-7","usgsCitation":"Vecchioli, J., 1981, Subsurface injection of liquid waste in Florida, United States of America: Science of Total Environment, v. 21, p. 127-136, https://doi.org/10.1016/0048-9697(81)90146-7.","productDescription":"10 p. ","startPage":"127","endPage":"136","costCenters":[{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":338333,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Florida","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -87.62695312499999,\n              30.524413269923986\n            ],\n            [\n              -83.935546875,\n              29.84064389983441\n            ],\n            [\n              -82.353515625,\n              26.588527147308614\n            ],\n            [\n              -80.68359375,\n              25.403584973186703\n            ],\n            [\n              -79.716796875,\n              26.980828590472107\n            ],\n            [\n              -81.03515625,\n              29.916852233070173\n            ],\n            [\n              -81.298828125,\n              30.826780904779774\n            ],\n            [\n              -87.62695312499999,\n              31.203404950917395\n            ],\n            [\n              -87.62695312499999,\n              30.524413269923986\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"21","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"58d63042e4b05ec799131129","contributors":{"authors":[{"text":"Vecchioli, John","contributorId":36113,"corporation":false,"usgs":true,"family":"Vecchioli","given":"John","email":"","affiliations":[],"preferred":false,"id":686165,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70203088,"text":"70203088 - 1981 - Reservoir analysis of the Denver earthquakes: A case of induced seismicity","interactions":[],"lastModifiedDate":"2019-07-17T16:06:40","indexId":"70203088","displayToPublicDate":"1981-04-18T11:29:00","publicationYear":"1981","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2316,"text":"Journal of Geophysical Research D: Atmospheres","active":true,"publicationSubtype":{"id":10}},"title":"Reservoir analysis of the Denver earthquakes: A case of induced seismicity","docAbstract":"<p><span>Injection of fluid wastes into the fractured Precambrian crystalline bedrock beneath the Rocky Mountain Arsenal near Denver triggered earthquakes in the 1960's. An analysis, based on the assumption that fluid flow in the fractured reservoir can be approximated by flow in a porous medium, is presented. The configuration and hydrologic properties of the reservoir are determined from two lines of evidence: (1) locations of earthquake hypocenters determined by seismic arrays installed at the Arsenal and (2) observed long-term decline in fluid levels in the injection well. Together these two sets of data indicate that a long, narrow reservoir, aligned in the direction N 60°W, exists. The reservoir is 3.35 km in width, extends 30.5 km to the northwest and infinitely to the southeast, and spans a depth interval from 3.7 to 7.0 km below land surface. It has a transmissivity of 1.08×10-5 m2/s and a storage coefficient of 1.0×10-5. Computed pressure buildup along the length of the reservoir is compared with the spatial distribution of earthquake epicenters. The comparison shows that earthquakes are confined to that part of the reservoir where the pressure buildup exceeds 32 bars. This critical value is interpreted as the pressure buildup above which earthquakes occur. The migration of earthquake epicenters away from the injection well, a phenomenon noted by previous investigators, can be accounted for by the outward propagation of the critical pressure buildup. The analysis is extended to examining the effects of rapid flow in fractures opened by high injection pressure. The results show that the effect is confined to a small region within 1 km of the injection well. The existence of a critical pressure buildup above which earthquakes occur is completely consistent with the theory on the role of fluid pressure in fault movement as presented by Hubbert and Rubey.</span></p>","language":"English","publisher":"American Geophysical Union","doi":"10.1029/JB086iB02p00903","usgsCitation":"Hsieh, P.A., and Bredehoeft, J.D., 1981, Reservoir analysis of the Denver earthquakes: A case of induced seismicity: Journal of Geophysical Research D: Atmospheres, v. 86, no. B2, p. 903-920, https://doi.org/10.1029/JB086iB02p00903.","productDescription":"18 p.","startPage":"903","endPage":"920","costCenters":[{"id":234,"text":"Earthquake Hazards Program","active":true,"usgs":true},{"id":237,"text":"Earthquake Science Center","active":true,"usgs":true},{"id":37277,"text":"WMA - Earth System Processes Division","active":true,"usgs":true}],"links":[{"id":480567,"rank":0,"type":{"id":41,"text":"Open Access External Repository Page"},"url":"https://doi.org/10.1029/jb086ib02p00903","text":"External Repository"},{"id":363032,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Colorado","otherGeospatial":"Rocky Mountain Arsenal","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -105.99609375,\n              39.00851330385611\n            ],\n            [\n              -103.73291015625,\n              39.00851330385611\n            ],\n            [\n              -103.73291015625,\n              40.5930995321649\n            ],\n            [\n              -105.99609375,\n              40.5930995321649\n            ],\n            [\n              -105.99609375,\n              39.00851330385611\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"86","issue":"B2","noUsgsAuthors":false,"publicationDate":"2012-09-20","publicationStatus":"PW","contributors":{"authors":[{"text":"Hsieh, Paul A. 0000-0003-4873-4874 pahsieh@usgs.gov","orcid":"https://orcid.org/0000-0003-4873-4874","contributorId":1634,"corporation":false,"usgs":true,"family":"Hsieh","given":"Paul","email":"pahsieh@usgs.gov","middleInitial":"A.","affiliations":[{"id":39113,"text":"WMA - Office of Quality Assurance","active":true,"usgs":true},{"id":37277,"text":"WMA - Earth System Processes Division","active":true,"usgs":true},{"id":438,"text":"National Research Program - Western Branch","active":true,"usgs":true}],"preferred":true,"id":761107,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bredehoeft, John D.","contributorId":86747,"corporation":false,"usgs":true,"family":"Bredehoeft","given":"John","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":761108,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70122670,"text":"70122670 - 1981 - Satellite observations of a geothermal submarine spring off Florida west coast","interactions":[],"lastModifiedDate":"2014-08-27T11:35:09","indexId":"70122670","displayToPublicDate":"1981-01-01T11:30:27","publicationYear":"1981","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"seriesNumber":"TPS81-1","title":"Satellite observations of a geothermal submarine spring off Florida west coast","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Satellite hydrology: proceedings of the Fifth Annual William T. Pecora Memorial Symposium on Remote Sensing, Sioux Falls, South Dakota, June 10-15, 1979","largerWorkSubtype":{"id":12,"text":"Conference publication"},"language":"English","publisher":"American Water Resources Association","publisherLocation":"Minneapolis, MN","usgsCitation":"Kohout, F.A., Munson, R., Turner, R.M., and Royal, W., 1981, Satellite observations of a geothermal submarine spring off Florida west coast, <i>in</i> Satellite hydrology: proceedings of the Fifth Annual William T. Pecora Memorial Symposium on Remote Sensing, Sioux Falls, South Dakota, June 10-15, 1979, p. 570-578.","productDescription":"9 p.","startPage":"570","endPage":"578","numberOfPages":"9","costCenters":[{"id":186,"text":"Coastal and Marine Geology Program","active":true,"usgs":true}],"links":[{"id":293101,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Florida","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -87.9755,24.5211 ], [ -87.9755,31.001 ], [ -80.6683,31.001 ], [ -80.6683,24.5211 ], [ -87.9755,24.5211 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53fef0eae4b01f35f8fd6a2d","contributors":{"editors":[{"text":"Deutch, Morris","contributorId":113798,"corporation":false,"usgs":true,"family":"Deutch","given":"Morris","email":"","affiliations":[],"preferred":false,"id":509971,"contributorType":{"id":2,"text":"Editors"},"rank":1},{"text":"Wiesnet, Donald R.","contributorId":106875,"corporation":false,"usgs":true,"family":"Wiesnet","given":"Donald","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":509969,"contributorType":{"id":2,"text":"Editors"},"rank":2},{"text":"Rango, Albert","contributorId":112973,"corporation":false,"usgs":true,"family":"Rango","given":"Albert","email":"","affiliations":[],"preferred":false,"id":509970,"contributorType":{"id":2,"text":"Editors"},"rank":3}],"authors":[{"text":"Kohout, F. A.","contributorId":11593,"corporation":false,"usgs":true,"family":"Kohout","given":"F.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":499581,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Munson, R.C.","contributorId":46016,"corporation":false,"usgs":true,"family":"Munson","given":"R.C.","email":"","affiliations":[],"preferred":false,"id":499582,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Turner, R. M.","contributorId":62585,"corporation":false,"usgs":true,"family":"Turner","given":"R.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":499583,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Royal, W.R.","contributorId":103189,"corporation":false,"usgs":true,"family":"Royal","given":"W.R.","email":"","affiliations":[],"preferred":false,"id":499584,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70039239,"text":"70039239 - 1981 - Maps for America: cartographic products of the U.S. Geological Survey and others","interactions":[],"lastModifiedDate":"2016-12-09T14:41:03","indexId":"70039239","displayToPublicDate":"1981-01-01T11:24:00","publicationYear":"1981","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"title":"Maps for America: cartographic products of the U.S. Geological Survey and others","docAbstract":"<p>\"Maps for America\" was originally published in 1979 as a Centennial Volume commemorating the Geological Survey's hundred years of service (1879-1979) in the earth sciences. It was an eminently fitting Centennial Year publication, for, since its establishment, the Geological Survey has continuously carried on an extensive program of mapping to provide knowledge of the topography, geology, hydrology, and natural resources of our Nation. This volume contains an organized presentation of information about the maps produced by the Geological Survey and other American organizations, public and private. Such maps are important tools for those in government and in private endeavors who are working to assure the wisest choices in managing the Nation's resources. They are particularly supportive of the Department of the Interior's role as the Nation's principal conservation agency. The second edition of \"Maps for America\" is intended primarily to replenish the dwindling supply of copies of the book, but it also contains a number of changes to correct or update the text and to provide more suitable illustrations in certain instances.</p>","language":"English","publisher":"U.S. Government Printing Office","publisherLocation":"Washington, D.C.","doi":"10.3133/70039239","usgsCitation":"Thompson, M., 1981, Maps for America: cartographic products of the U.S. Geological Survey and others (2nd), xiv, 265 p., https://doi.org/10.3133/70039239.","productDescription":"xiv, 265 p.","numberOfPages":"286","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":261452,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/unnumbered/70039239/report-thumb.jpg"},{"id":261451,"rank":800,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/unnumbered/70039239/report.pdf"}],"country":"United States","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -125.15625000000001,\n              25.16517336866393\n            ],\n            [\n              -125.15625000000001,\n              48.922499263758255\n            ],\n            [\n              -67.5,\n              48.922499263758255\n            ],\n            [\n              -67.5,\n              25.16517336866393\n            ],\n            [\n              -125.15625000000001,\n              25.16517336866393\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","edition":"2nd","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a50abe4b0c8380cd6b848","contributors":{"authors":[{"text":"Thompson, Morris M.","contributorId":21288,"corporation":false,"usgs":true,"family":"Thompson","given":"Morris M.","affiliations":[],"preferred":false,"id":465855,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
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