{"pageNumber":"2199","pageRowStart":"54950","pageSize":"25","recordCount":68892,"records":[{"id":40806,"text":"ofr801280 - 1980 - Potentiometric surface of the Floridan Aquifer, Southwest Florida Water Management District, September 1980","interactions":[],"lastModifiedDate":"2012-02-02T00:11:09","indexId":"ofr801280","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1980","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":"80-1280","title":"Potentiometric surface of the Floridan Aquifer, Southwest Florida Water Management District, September 1980","docAbstract":"A September 1980 potentiometric-surface map of the Southwest Florida Water Management District depicts the annual high water-level period. Potentiometric levels rose 1 to 31 feet between May 1980 and September 1980 in the citrus and farming sections of southern Hillsborough, northern Hardee, southwestern Polk, northwestern DeSoto, and Manatee Counties. Water levels in these areas are widely affected by reduced pumping for irrigation and have the greatest range in fluctuations. Generally, potentiometric levels were lower than previous September levels except in Citrus, eastern Levy, and western Marion Counties where levels were 0 to 8 feet higher. (USGS)","language":"ENGLISH","doi":"10.3133/ofr801280","usgsCitation":"Yobbi, D.K., Woodham, W.M., and Schiner, G.R., 1980, Potentiometric surface of the Floridan Aquifer, Southwest Florida Water Management District, September 1980: U.S. Geological Survey Open-File Report 80-1280, 1 map ;79 x 56 cm., https://doi.org/10.3133/ofr801280.","productDescription":"1 map ;79 x 56 cm.","costCenters":[],"links":[{"id":176686,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":78690,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1980/1280/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad4e4b07f02db682fc9","contributors":{"authors":[{"text":"Yobbi, D. K.","contributorId":56622,"corporation":false,"usgs":true,"family":"Yobbi","given":"D.","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":223962,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Woodham, W. M.","contributorId":72356,"corporation":false,"usgs":true,"family":"Woodham","given":"W.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":223963,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Schiner, George R.","contributorId":22743,"corporation":false,"usgs":true,"family":"Schiner","given":"George","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":223961,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":40832,"text":"ofr80587 - 1980 - Potentiometric surface of the Floridan Aquifer, Southwest Florida Water Management District, May 1980","interactions":[],"lastModifiedDate":"2012-02-02T00:10:49","indexId":"ofr80587","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1980","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":"80-587","title":"Potentiometric surface of the Floridan Aquifer, Southwest Florida Water Management District, May 1980","docAbstract":"A May 1980 potentiometric-surface map of the Southwest Florida Water Management District depicts the annual low water-level period. Potentiometric levels decreased 5 to 36 feet between September 1979 and May 1980, in the citrus and farming sections of southern Hillsborough, southwestern Polk, northwestern DeSoto , Hardee, and Manatee Counties. Water levels in these areas are widely affected by pumping for irrigation and have the greatest range in fluctuations. Water-level decreases ranged from 0 to 8 feet in coastal, northern, and southern areas of the Water Management District. Generally, potentiometric levels were lower than previous May levels except in the northernmost and southernmost counties where water levels were 1 to 5 feet higher. (USGS)","language":"ENGLISH","doi":"10.3133/ofr80587","usgsCitation":"Yobbi, D.K., Woodham, W.M., and Schiner, G.R., 1980, Potentiometric surface of the Floridan Aquifer, Southwest Florida Water Management District, May 1980: U.S. Geological Survey Open-File Report 80-587, 1 map ;79 x 56 cm., https://doi.org/10.3133/ofr80587.","productDescription":"1 map ;79 x 56 cm.","costCenters":[],"links":[{"id":170973,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":78704,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1980/0587/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad4e4b07f02db683056","contributors":{"authors":[{"text":"Yobbi, D. K.","contributorId":56622,"corporation":false,"usgs":true,"family":"Yobbi","given":"D.","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":224010,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Woodham, W. M.","contributorId":72356,"corporation":false,"usgs":true,"family":"Woodham","given":"W.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":224011,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Schiner, George R.","contributorId":22743,"corporation":false,"usgs":true,"family":"Schiner","given":"George","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":224009,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":40931,"text":"ofr8069 - 1980 - Potentiometric surface map of the Floridan aquifer in the St. Johns River Water Management District and vicinity, Florida, May 1979","interactions":[],"lastModifiedDate":"2021-11-15T22:31:37.36515","indexId":"ofr8069","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1980","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":"80-69","title":"Potentiometric surface map of the Floridan aquifer in the St. Johns River Water Management District and vicinity, Florida, May 1979","docAbstract":"This map presents the potentiometric surface of the Floridan aquifer in the St. Johns River Water Management District and vicinity for May 1979. The Floridan aquifer is the principal source of potable water in the area. Water-level measurements were made on approximately 1200 wells and on several springs. The potentiometric surface is shown by 5-foot contour intervals except in the Fernandina Beach area where 20-foot intervals are used to show a deep cone of depression. This is the fourth map of a series covering the entire St. Johns River Water Management District and vicinity. Two maps cover the low water-level period in May and two show the high-water period in September. The potentiometric surface ranged from 125 feet above the National Vertical Datum of 1929 (NGVD) in Polk County to 120 feet below NGVD in Nassau County. (USGS)","doi":"10.3133/ofr8069","usgsCitation":"Laughlin, C.P., Hayes, E.C., and Schiner, G.R., 1980, Potentiometric surface map of the Floridan aquifer in the St. Johns River Water Management District and vicinity, Florida, May 1979: U.S. Geological Survey Open-File Report 80-69, 1 Plate: 26.07 × 44.82 inches, https://doi.org/10.3133/ofr8069.","productDescription":"1 Plate: 26.07 × 44.82 inches","costCenters":[],"links":[{"id":391711,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_75184.htm"},{"id":78822,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1980/0069/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":171438,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"country":"United States","state":"Florida","otherGeospatial":"St. Johns River Water Management District and vicinity","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -82.8333,\n              26.75\n            ],\n            [\n              -80,\n              26.75\n            ],\n            [\n              -80,\n              30.75\n            ],\n            [\n              -82.8333,\n              30.75\n            ],\n            [\n              -82.8333,\n              26.75\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad4e4b07f02db683175","contributors":{"authors":[{"text":"Laughlin, Charles P.","contributorId":6490,"corporation":false,"usgs":true,"family":"Laughlin","given":"Charles","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":224197,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hayes, E. C.","contributorId":47836,"corporation":false,"usgs":true,"family":"Hayes","given":"E.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":224199,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Schiner, George R.","contributorId":22743,"corporation":false,"usgs":true,"family":"Schiner","given":"George","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":224198,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":40932,"text":"ofr801002 - 1980 - Potentiometric surface map of the Floridan aquifer in the St. Johns River Water Management District and vicinity, Florida, May 1980","interactions":[],"lastModifiedDate":"2022-08-25T18:38:16.679385","indexId":"ofr801002","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1980","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":"80-1002","title":"Potentiometric surface map of the Floridan aquifer in the St. Johns River Water Management District and vicinity, Florida, May 1980","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr801002","usgsCitation":"Schiner, G.R., and Hayes, E.C., 1980, Potentiometric surface map of the Floridan aquifer in the St. Johns River Water Management District and vicinity, Florida, May 1980: U.S. Geological Survey Open-File Report 80-1002, 1 Plate: 27.24 × 45.25 inches, https://doi.org/10.3133/ofr801002.","productDescription":"1 Plate: 27.24 × 45.25 inches","costCenters":[],"links":[{"id":171439,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":78823,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1980/1002/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":405614,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_75323.htm","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Florida","otherGeospatial":"St. Johns River Water Management District and vicinity","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -82.5,\n              26.5\n            ],\n            [\n              -80.0333,\n              26.5\n            ],\n            [\n              -80.0333,\n              30.6606\n            ],\n            [\n              -82.5,\n              30.6606\n            ],\n            [\n              -82.5,\n              26.5\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad4e4b07f02db683161","contributors":{"authors":[{"text":"Schiner, George R.","contributorId":22743,"corporation":false,"usgs":true,"family":"Schiner","given":"George","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":224200,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hayes, Eugene C.","contributorId":46918,"corporation":false,"usgs":true,"family":"Hayes","given":"Eugene","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":224201,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":40956,"text":"ofr791585 - 1980 - Potentiometric map of the Ripley Aquifer in northeastern Mississippi, October and November 1978","interactions":[],"lastModifiedDate":"2012-02-02T00:10:33","indexId":"ofr791585","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1980","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":"79-1585","title":"Potentiometric map of the Ripley Aquifer in northeastern Mississippi, October and November 1978","docAbstract":"This potentiometric map of the Ripley aquifer in northeastern Mississippi is the fifth in a series of maps, prepared by the U.S. Geological Survey in cooperation with the Mississippi Department of Natural Resources, Bureau of Land and Water Resources, delineating the potentiometric surfaces of the major aquifers in Mississippi. In the outcrop area of the Ripley aquifer the potentiometric surface is strongly affected by recharge from precipitation, by topography, and by drainage of the aquifer by streams. The potentiometric surface slopes generally to the west away from the area of outcrop and is mildly affected by pumpage from wells and by discharge of flowing wells in the valleys. Historically, water levels in or near the outcrop have shown little or no long-term changes. (USGS)","language":"ENGLISH","doi":"10.3133/ofr791585","usgsCitation":"Wasson, B.E., 1980, Potentiometric map of the Ripley Aquifer in northeastern Mississippi, October and November 1978 (WRI/OFR): U.S. Geological Survey Open-File Report 79-1585, 1 map :col. ;54 x 30 cm. on sheet 64 x 69 cm. folded in envelope 31 x 23 cm., https://doi.org/10.3133/ofr791585.","productDescription":"1 map :col. ;54 x 30 cm. on sheet 64 x 69 cm. folded in envelope 31 x 23 cm.","costCenters":[],"links":[{"id":172579,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":78851,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1979/1585/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"edition":"WRI/OFR","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad4e4b07f02db683198","contributors":{"authors":[{"text":"Wasson, B. E.","contributorId":11204,"corporation":false,"usgs":true,"family":"Wasson","given":"B.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":224241,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":40987,"text":"ofr791587 - 1980 - Potentiometric map of the Coffee Sand Aquifer in northeastern Mississippi, October and November 1978","interactions":[],"lastModifiedDate":"2012-02-02T00:10:34","indexId":"ofr791587","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1980","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":"79-1587","title":"Potentiometric map of the Coffee Sand Aquifer in northeastern Mississippi, October and November 1978","docAbstract":"This potentiometric map of the Coffee Sand aquifer in northeastern Mississippi is the fourth in a series of maps, prepared by the U.S. Geological Survey in cooperation with the Mississippi Department of Natural Resources, Bureau of Land and Water Resources, delineating the potentiometric surfaces of the major aquifers in Mississippi. In the outcrop areas the potentiometric surface is strongly affected by recharge from precipitation, topography, and drainage of the aquifer by streams. The potentiometric surface slopes generally to the west away from the area of outcrop and is mildly affected by moderate ground-water withdrawals by wells in Tippah and Union County. Historically, water levels in or near the outcrop of the Coffee Sand have shown little or no long-term changes as shown by a hydrograph of one well in Alcorn County. In the downdip part of the aquifer water-level declines of 2 feet per year are common. (USGS)","language":"ENGLISH","doi":"10.3133/ofr791587","usgsCitation":"Wasson, B.E., 1980, Potentiometric map of the Coffee Sand Aquifer in northeastern Mississippi, October and November 1978 (WRI/OFR): U.S. Geological Survey Open-File Report 79-1587, 1 map :col. ;21 x 31 cm. on sheet 59 x 58 cm. folded in envelope 31 x 23 cm., https://doi.org/10.3133/ofr791587.","productDescription":"1 map :col. ;21 x 31 cm. on sheet 59 x 58 cm. folded in envelope 31 x 23 cm.","costCenters":[],"links":[{"id":173293,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1979/1587/report-thumb.jpg"},{"id":78871,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1979/1587/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"edition":"WRI/OFR","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b30e4b07f02db6b40ff","contributors":{"authors":[{"text":"Wasson, B. E.","contributorId":11204,"corporation":false,"usgs":true,"family":"Wasson","given":"B.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":224288,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":40988,"text":"ofr791584 - 1980 - Potentiometric map of the Eutaw-McShan Aquifer in northeastern Mississippi, September, October, and November 1978","interactions":[],"lastModifiedDate":"2012-02-02T00:10:34","indexId":"ofr791584","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1980","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":"79-1584","title":"Potentiometric map of the Eutaw-McShan Aquifer in northeastern Mississippi, September, October, and November 1978","docAbstract":"This potentiometric map of the Eutaw-McShan aquifer in northeastern Mississippi is the third in a series of maps, prepared by the U.S. Geological Survey in cooperation with the Mississippi Department of Natural Resources, Bureau of Land and Water Resources, delineating the potentiometric surfaces of the major aquifers in Mississippi. From its outcrop area the Eutaw-McShan aquifer dips about 30 feet per mile to the west and southwest. Thickness of the aquifer commonly is between 200 and 300 feet in most of the area, and commonly about one-half this thickness consists of sand. In the outcrop area the potentiometric surface is strongly affected by recharge from precipitation, topography, and drainage of the aquifer by streams. The potentiometric surface of the aquifer slopes generally to the west away from the area of outcrop and it is strongly affected by large ground-water withdrawals at or near Tupelo, Aberdeen, and West Point. Historically, water levels in or near the outcrop of the Eutaw-McShan aquifer have shown little or no long-term changes. Withdrawals of water by wells from the downdip area have caused long-term water-level declines of 1 to 2 feet per year in much of the confined part of the aquifer. Water-level declines during recent years in several observation wells in Lee County ranged from 2 to 9 feet per year. One hydrograph in Clay County that is near the center of the depression in the potentiometric surface at West Point shows about 5 feet per year of water-level decline since 1972. (USGS)","language":"ENGLISH","doi":"10.3133/ofr791584","usgsCitation":"Wasson, B.E., 1980, Potentiometric map of the Eutaw-McShan Aquifer in northeastern Mississippi, September, October, and November 1978 (WRI/OFR): U.S. Geological Survey Open-File Report 79-1584, 1 map :col. ;48 x 39 cm. on sheet 64 x 80 cm. folded in envelope 31 x 23 cm., https://doi.org/10.3133/ofr791584.","productDescription":"1 map :col. ;48 x 39 cm. on sheet 64 x 80 cm. folded in envelope 31 x 23 cm.","costCenters":[],"links":[{"id":173294,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":78872,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1979/1584/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"edition":"WRI/OFR","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b31e4b07f02db6b4123","contributors":{"authors":[{"text":"Wasson, B. E.","contributorId":11204,"corporation":false,"usgs":true,"family":"Wasson","given":"B.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":224289,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":40991,"text":"ofr80590 - 1980 - Potentiometric map of the Meridian-Upper Wilcox Aquifer in Mississippi, fall 1979","interactions":[],"lastModifiedDate":"2012-02-02T00:10:34","indexId":"ofr80590","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1980","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":"80-590","title":"Potentiometric map of the Meridian-Upper Wilcox Aquifer in Mississippi, fall 1979","docAbstract":"The potentiometric map of the Meridian-upper Wilcox aquifer is one of a series of maps, prepared by the U.S. Geological Survey in cooperation with the Mississippi Department of Natural Resources, Bureau of Land and Water Resources, delineating the potentiometric surfaces of the major aquifers in Mississippi. In the outcrop area of the Meridian-upper Wilcox aquifer the potentiometric surface is strongly affected by recharge from precipitation, by topography, and by drainage of the aquifer by streams. The potentiometric surface slopes downward generally to the west away from the area of outcrop and is strongly affected by large groundwater withdrawals in the Greenwood, Indianola, Marks, Grenada, and Memphis areas. Historically, water levels in or near the outcrop of the Meridian-upper Wilcox have shown little or no long-term changes, but during the past 20 years water levels have declined from 1 to 2 feet per year in much of the confined part of the aquifer. (USGS)","language":"ENGLISH","doi":"10.3133/ofr80590","usgsCitation":"Wasson, B.E., 1980, Potentiometric map of the Meridian-Upper Wilcox Aquifer in Mississippi, fall 1979 (WRI/OFR): U.S. Geological Survey Open-File Report 80-590, 1 map :col. ;86 x 75 cm., https://doi.org/10.3133/ofr80590.","productDescription":"1 map :col. ;86 x 75 cm.","costCenters":[],"links":[{"id":173383,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":78875,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1980/0590/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"edition":"WRI/OFR","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad4e4b07f02db683233","contributors":{"authors":[{"text":"Wasson, B. E.","contributorId":11204,"corporation":false,"usgs":true,"family":"Wasson","given":"B.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":224292,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":41748,"text":"ofr80337 - 1980 - Approximate water-level changes in wells in the Chicot and Evangeline aquifers in the Houston-Galveston region, Texas, 1977-80 and 1979-80","interactions":[],"lastModifiedDate":"2016-08-11T11:10:45","indexId":"ofr80337","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1980","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":"80-337","title":"Approximate water-level changes in wells in the Chicot and Evangeline aquifers in the Houston-Galveston region, Texas, 1977-80 and 1979-80","docAbstract":"<p>This report, which was prepared in cooperation with the cities of Houston and Galveston, the Harris Galveston Coastal Subsidence Distract, and the Texas Department of Water Resources, presents data on water-level changes during 1977-80 and 1979-80 in the Chicot and Evangelina aquifers (figs. 1-4). &nbsp;During these periods, ground water pumping decreased in Galveston County and southern Harris County and increased in northern and western Harris County (Gabrysch, 1979).</p>\n<p>Water levels in about 550 wells were used to construct the maps showing water level changes.</p>","language":"English","publisher":"U.S. Geologoical Survey","doi":"10.3133/ofr80337","usgsCitation":"Gabrysch, R., and Ranzau, C., 1980, Approximate water-level changes in wells in the Chicot and Evangeline aquifers in the Houston-Galveston region, Texas, 1977-80 and 1979-80: U.S. Geological Survey Open-File Report 80-337, 5 p., https://doi.org/10.3133/ofr80337.","productDescription":"5 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"links":[{"id":176677,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1980/0337/report-thumb.jpg"},{"id":79466,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1980/0337/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac5e4b07f02db67a141","contributors":{"authors":[{"text":"Gabrysch, R.K.","contributorId":105691,"corporation":false,"usgs":true,"family":"Gabrysch","given":"R.K.","affiliations":[],"preferred":false,"id":225472,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Ranzau, C.E. Jr.","contributorId":41831,"corporation":false,"usgs":true,"family":"Ranzau","given":"C.E.","suffix":"Jr.","email":"","affiliations":[],"preferred":false,"id":225471,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":41289,"text":"ofr80428 - 1980 - Preliminary bathymetry: Approaches to Unakwik Inlet, Alaska","interactions":[],"lastModifiedDate":"2021-12-09T20:14:21.720437","indexId":"ofr80428","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1980","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":"80-428","title":"Preliminary bathymetry: Approaches to Unakwik Inlet, Alaska","docAbstract":"<p>A map, scale 1:20,000, shows water depths, rocks, and hazards to navigation. These data are noted on track lines run by the Research Vessel Growler in Alaskan waters, where data on navigation shown on published charts are nonexistant, preliminary, or out dated.&nbsp;</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr80428","usgsCitation":"Post, A., 1980, Preliminary bathymetry: Approaches to Unakwik Inlet, Alaska: U.S. Geological Survey Open-File Report 80-428, 1 Plate: 39.00 × 46.00 inches, https://doi.org/10.3133/ofr80428.","productDescription":"1 Plate: 39.00 × 46.00 inches","costCenters":[],"links":[{"id":108034,"rank":700,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_11633.htm","linkFileType":{"id":5,"text":"html"},"description":"11633"},{"id":20002,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1980/0428/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":171419,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"country":"United States","state":"Alaska","otherGeospatial":"Unakwik Inlet","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -147.6947021484375,\n              60.86764961744716\n            ],\n            [\n              -147.35687255859375,\n              60.86764961744716\n            ],\n            [\n              -147.35687255859375,\n              61.01572481397616\n            ],\n            [\n              -147.6947021484375,\n              61.01572481397616\n            ],\n            [\n              -147.6947021484375,\n              60.86764961744716\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac9e4b07f02db67c9f4","contributors":{"authors":[{"text":"Post, Austin","contributorId":90709,"corporation":false,"usgs":true,"family":"Post","given":"Austin","affiliations":[],"preferred":false,"id":224783,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":41290,"text":"ofr80426 - 1980 - Preliminary bathymetry— Esther Passage and channels east to Eaglek Island, Alaska","interactions":[],"lastModifiedDate":"2021-11-17T19:48:58.829524","indexId":"ofr80426","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1980","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":"80-426","title":"Preliminary bathymetry— Esther Passage and channels east to Eaglek Island, Alaska","docAbstract":"<p>A map, scale 1:20,000, shows water depths, rocks, and hazards to navigation. These data are noted on track lines run by the Research Vessel Growler in Alaskan waters, where data on navigation shown on published charts are nonexistant, preliminary, or out dated.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr80426","usgsCitation":"Post, A., 1980, Preliminary bathymetry— Esther Passage and channels east to Eaglek Island, Alaska: U.S. Geological Survey Open-File Report 80-426, 1 Plate: 52.00 × 36.00 inches, https://doi.org/10.3133/ofr80426.","productDescription":"1 Plate: 52.00 × 36.00 inches","costCenters":[],"links":[{"id":171517,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":20001,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1980/0426/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":391812,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_11631.htm"}],"country":"United States","state":"Alaska","otherGeospatial":"Eagle Island, Esther Passage","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -148.033,\n              60.783\n            ],\n            [\n              -147.667,\n              60.783\n            ],\n            [\n              -147.667,\n              60.925\n            ],\n            [\n              -148.033,\n              60.925\n            ],\n            [\n              -148.033,\n              60.783\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac9e4b07f02db67c9ec","contributors":{"authors":[{"text":"Post, Austin","contributorId":90709,"corporation":false,"usgs":true,"family":"Post","given":"Austin","affiliations":[],"preferred":false,"id":224784,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":41293,"text":"ofr80424 - 1980 - Preliminary bathymetry of McCarty Fiord and Neoglacial changes of McCarty Glacier, Alaska","interactions":[],"lastModifiedDate":"2012-02-02T00:10:49","indexId":"ofr80424","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1980","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":"80-424","title":"Preliminary bathymetry of McCarty Fiord and Neoglacial changes of McCarty Glacier, Alaska","docAbstract":"Preliminary bathymetry (at 1:20,000 scale) and other scientific studies of McCarty Fiord, Alaska, Conducted by the Research Vessel Growler in 1978, showed this 15 mile-long waterway to be a narrow, deeply scoured basin enclosed by a terminal-moraine shoal. This valley was formerly filled by McCarty Glacier, which began a drastic retreat shortly after 1909; the glacier reached shallow water at the head of the fiord around 1960. The relative rate of retreat in deep water and on land is disclosed by the slower melting of stagnent ice left in a side valley. Soundings and profiles show the main channel to extend to a depth as great as 957 feet and to have the typical ' U ' shape of a glacier-eroded valley; since the glacier 's retreat, sediments have formed a nearly level deposit in the deepest part of the fiord. Old forest debris dated by carbon-14 indicates that a neoglacial advance of the glacier began before 3,395 years B.P. (before present); by 1,500 B.P. the glacier filled most of the fiord, and before the glacier culminated its advance around 1860 , two glacier-dammed lakes were formed in side valleys. (USGS)","language":"ENGLISH","doi":"10.3133/ofr80424","usgsCitation":"Post, A., 1980, Preliminary bathymetry of McCarty Fiord and Neoglacial changes of McCarty Glacier, Alaska: U.S. Geological Survey Open-File Report 80-424, 4 maps ;89 x 67 cm., https://doi.org/10.3133/ofr80424.","productDescription":"4 maps ;89 x 67 cm.","costCenters":[],"links":[{"id":171520,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":19997,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1980/0424/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":19998,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1980/0424/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":19999,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1980/0424/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":20000,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1980/0424/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac9e4b07f02db67c836","contributors":{"authors":[{"text":"Post, Austin","contributorId":90709,"corporation":false,"usgs":true,"family":"Post","given":"Austin","affiliations":[],"preferred":false,"id":224787,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":41294,"text":"ofr80414 - 1980 - Preliminary bathymetry of Northwestern Fiord and neoglacial changes of Northwestern Glacier, Alaska","interactions":[],"lastModifiedDate":"2021-11-01T21:57:47.033928","indexId":"ofr80414","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1980","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":"80-414","title":"Preliminary bathymetry of Northwestern Fiord and neoglacial changes of Northwestern Glacier, Alaska","docAbstract":"The first preliminary bathymetry (at 1:20,000 scale) and other scientific investigations of Northwestern Fiord, Alaska, were conducted by the Research Vessel Growler in 1978, disclosing this 10.5-mile-long branched waterway to be a deep basin enclosed by a terminal-moraine shoal. The basin was formerly filled by Northwestern Glacier, which began a drastic retreat around 1909 and reached the head of the main arm around 1960. Soundings and profiles show the main channel to be as much as 970 feet deep and to have the typical U shape of a severely glacially eroded valley; since the glacier 's retreat, sediments have formed nearly level deposits in the deepest reaches, while the rest of the basin has a hard, rocky bottom. Preneoglacial forest debris dated by carbon-14 indicates Northwestern Glacier to have advanced into the fiord prior to 1,385 years before present (B.P.); a branch glacier evidently advanced into forest 1,635 years B.P. The combined glaciers from several arms culminated on the present terminal-moraine shoal around 1894. (USGS)","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr80414","usgsCitation":"Post, A., 1980, Preliminary bathymetry of Northwestern Fiord and neoglacial changes of Northwestern Glacier, Alaska: U.S. Geological Survey Open-File Report 80-414, 2 Plates: 40.00 × 43.00 inches and 39.00 × 42.00 inches, https://doi.org/10.3133/ofr80414.","productDescription":"2 Plates: 40.00 × 43.00 inches and 39.00 × 42.00 inches","costCenters":[],"links":[{"id":391245,"rank":5,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_11627.htm"},{"id":171627,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":19992,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1980/0414/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":19993,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1980/0414/plate-1-preview.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":19994,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1980/0414/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Alaska","otherGeospatial":"Northwestern Fiord, Northwestern Glacier","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -150.15,\n              59.7\n            ],\n            [\n              -149.817,\n              59.7\n            ],\n            [\n              -149.817,\n              59.867\n            ],\n            [\n              -150.15,\n              59.867\n            ],\n            [\n              -150.15,\n              59.7\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac9e4b07f02db67c983","contributors":{"authors":[{"text":"Post, Austin","contributorId":90709,"corporation":false,"usgs":true,"family":"Post","given":"Austin","affiliations":[],"preferred":false,"id":224788,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":41508,"text":"ofr80615 - 1980 - Aeromagnetic map of southeastern Ohio","interactions":[],"lastModifiedDate":"2012-02-02T00:10:51","indexId":"ofr80615","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1980","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":"80-615","title":"Aeromagnetic map of southeastern Ohio","language":"ENGLISH","doi":"10.3133/ofr80615","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1980, Aeromagnetic map of southeastern Ohio: U.S. Geological Survey Open-File Report 80-615, 1 map ;45 x 56 cm., https://doi.org/10.3133/ofr80615.","productDescription":"1 map ;45 x 56 cm.","costCenters":[],"links":[{"id":170709,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":79232,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1980/0615/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afee4b07f02db6972da","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":530437,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":41532,"text":"ofr80831 - 1980 - Aeroradioactivity map of the Manistique Lakes area, Michigan","interactions":[],"lastModifiedDate":"2012-02-02T00:10:32","indexId":"ofr80831","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1980","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":"80-831","title":"Aeroradioactivity map of the Manistique Lakes area, Michigan","language":"ENGLISH","doi":"10.3133/ofr80831","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1980, Aeroradioactivity map of the Manistique Lakes area, Michigan: U.S. Geological Survey Open-File Report 80-831, 1 map ;178 x 153 cm. on 4 sheets., https://doi.org/10.3133/ofr80831.","productDescription":"1 map ;178 x 153 cm. on 4 sheets.","costCenters":[],"links":[{"id":173117,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":20036,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1980/0831/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":20037,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1980/0831/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":20034,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1980/0831/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":20035,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1980/0831/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae4e4b07f02db689a6e","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":530458,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":41560,"text":"ofr80671 - 1980 - Aeromagnetic map of the Pecos area, New Mexico","interactions":[],"lastModifiedDate":"2012-02-02T00:10:53","indexId":"ofr80671","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1980","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":"80-671","title":"Aeromagnetic map of the Pecos area, New Mexico","language":"ENGLISH","doi":"10.3133/ofr80671","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1980, Aeromagnetic map of the Pecos area, New Mexico: U.S. Geological Survey Open-File Report 80-671, 1 map ;225 x 141 cm. on 4 sheets 108 x 130 cm. or smaller., https://doi.org/10.3133/ofr80671.","productDescription":"1 map ;225 x 141 cm. on 4 sheets 108 x 130 cm. or smaller.","costCenters":[],"links":[{"id":171012,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":20013,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1980/0671/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":20014,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1980/0671/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":20015,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1980/0671/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":20016,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1980/0671/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4af3e4b07f02db691b56","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":530473,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":42468,"text":"ofr80164 - 1980 - Seasonal and annual variations in the potentiometric surface of the Floridan Aquifer in Duval County, Florida, 1960-77","interactions":[],"lastModifiedDate":"2013-01-24T07:28:52","indexId":"ofr80164","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1980","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":"80-164","title":"Seasonal and annual variations in the potentiometric surface of the Floridan Aquifer in Duval County, Florida, 1960-77","docAbstract":"Potentiometric levels of the Floridan aquifer in Duval County, Fla., are constantly changing in response to gains of water to the aquifer, primarily by recharge from rainfall; and losses from the aquifer, primarily by withdrawals from hundreds of wells. Seasonal variations of the potentiometric level in one well at Jacksonville was 4.2 feet during 1976. During the 18 year period from 1960 to 1977 the mean annual decline of potentiometric levels in the county was about 8 feet because of a large increase in withdrawals and to a lesser extent a decline in average annual rainfall in recharge areas. Maps of the potentiometric surface in 1960 and 1977 indicate that the greatest decline was more than 20 feet in the south-central part of the county. The decline was less than 5 feet in the western part of the county. (Kosco-USGS)","language":"ENGLISH","doi":"10.3133/ofr80164","usgsCitation":"Leve, G.W., 1980, Seasonal and annual variations in the potentiometric surface of the Floridan Aquifer in Duval County, Florida, 1960-77 (WRI/OFR): U.S. Geological Survey Open-File Report 80-164, 1 map : col. ;96 x 68 cm. fold. in envelope 30 x 23 cm., https://doi.org/10.3133/ofr80164.","productDescription":"1 map : col. ;96 x 68 cm. fold. in envelope 30 x 23 cm.","costCenters":[],"links":[{"id":135406,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":80234,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1980/0164/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":266349,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1980/0164/report.pdf"}],"edition":"WRI/OFR","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0ce4b07f02db5fc46b","contributors":{"authors":[{"text":"Leve, Gilbert W.","contributorId":91463,"corporation":false,"usgs":true,"family":"Leve","given":"Gilbert","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":226552,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":42458,"text":"ofr80562 - 1980 - Preliminary map showing availability of water from glacial-drift aquifers in McHenry County, north-central North Dakota","interactions":[],"lastModifiedDate":"2018-03-21T16:09:12","indexId":"ofr80562","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1980","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":"80-562","title":"Preliminary map showing availability of water from glacial-drift aquifers in McHenry County, north-central North Dakota","docAbstract":"<p><span>This preliminary map is the first product of the ground-water resources study of&nbsp;McHenry County</span><span>.&nbsp; This study is part of a statewide program to determine the location, extent, chemical quality, and hydrologic characteristics of the ground-water reservoirs (aquifers) in North Dakota.&nbsp; The study was made by the U.S. Geological Survey in cooperation with the North Dakota State Water Commission, the North Dakota Geological Survey, and the&nbsp;McHenry County Water Management District.</span></p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr80562","usgsCitation":"Randich, P., 1980, Preliminary map showing availability of water from glacial-drift aquifers in McHenry County, north-central North Dakota: U.S. Geological Survey Open-File Report 80-562, 25.86 x 30.92 inches, https://doi.org/10.3133/ofr80562.","productDescription":"25.86 x 30.92 inches","costCenters":[{"id":478,"text":"North Dakota Water Science Center","active":true,"usgs":true},{"id":34685,"text":"Dakota Water Science Center","active":true,"usgs":true}],"links":[{"id":136634,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":80221,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1980/0562/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ab0e4b07f02db66d6cc","contributors":{"authors":[{"text":"Randich, P.G.","contributorId":69953,"corporation":false,"usgs":true,"family":"Randich","given":"P.G.","affiliations":[],"preferred":false,"id":226528,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":42455,"text":"ofr80504W - 1980 - Preliminary map showing availability of ground water from glacial-drift aquifers in Sheridan County, central North Dakota","interactions":[],"lastModifiedDate":"2018-02-14T16:23:51","indexId":"ofr80504W","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1980","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":"80-504","chapter":"W","title":"Preliminary map showing availability of ground water from glacial-drift aquifers in Sheridan County, central North Dakota","docAbstract":"<p>This preliminary map is the first product of a study of the ground-water resources of Sheridan County.&nbsp; The study is part of a statewide program to determine the location, extent, and hydrologic characteristics of the ground-water reservoirs (aquifers) in North Dakota.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr80504W","usgsCitation":"Burkart, M.R., and Randich, P., 1980, Preliminary map showing availability of ground water from glacial-drift aquifers in Sheridan County, central North Dakota: U.S. Geological Survey Open-File Report 80-504, 21.87 x 22.20 inches, https://doi.org/10.3133/ofr80504W.","productDescription":"21.87 x 22.20 inches","costCenters":[{"id":478,"text":"North Dakota Water Science Center","active":true,"usgs":true},{"id":34685,"text":"Dakota Water Science Center","active":true,"usgs":true}],"links":[{"id":136613,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":80219,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1980/0504w/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ab0e4b07f02db66d6d8","contributors":{"authors":[{"text":"Burkart, M. R.","contributorId":42190,"corporation":false,"usgs":true,"family":"Burkart","given":"M.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":226524,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Randich, P.G.","contributorId":69953,"corporation":false,"usgs":true,"family":"Randich","given":"P.G.","affiliations":[],"preferred":false,"id":226525,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":41630,"text":"ofr801126 - 1980 - Aeromagnetic map of the northern part of the Ajo 1° by 2° quadrangle, Arizona","interactions":[],"lastModifiedDate":"2021-09-29T21:41:22.621148","indexId":"ofr801126","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1980","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":"80-1126","title":"Aeromagnetic map of the northern part of the Ajo 1° by 2° quadrangle, Arizona","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr801126","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1980, Aeromagnetic map of the northern part of the Ajo 1° by 2° quadrangle, Arizona: U.S. Geological Survey Open-File Report 80-1126, 1 Plate: 35.33 × 15.29 inches, https://doi.org/10.3133/ofr801126.","productDescription":"1 Plate: 35.33 × 15.29 inches","costCenters":[],"links":[{"id":170795,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":390002,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_11481.htm"},{"id":79366,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1980/1126/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Arizona","otherGeospatial":"Ajo 1° by 2° quadrangle","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -114.125,\n              32.625\n            ],\n            [\n              -111.875,\n              32.625\n            ],\n            [\n              -111.875,\n              33.125\n            ],\n            [\n              -114.125,\n              33.125\n            ],\n            [\n              -114.125,\n              32.625\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae6e4b07f02db68b782","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":530525,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":28473,"text":"wri8072 - 1980 - Calibration and testing of selected portable flowmeters for use on large irrigation systems","interactions":[],"lastModifiedDate":"2017-12-06T13:50:58","indexId":"wri8072","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1980","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":"80-72","title":"Calibration and testing of selected portable flowmeters for use on large irrigation systems","docAbstract":"<p>Existing methods for measuring discharge of irrigation systems in the High Plains region are not suitable to provide the pumpage data required by the High Plains Regional Aquifer System Analysis. Three portable flowmeters that might be suitable for obtaining fast and accurate discharge measure-ments on large irrigation systems were tested during 1979 under both laboratory and field conditions: propeller type gated-pipe meter, a Doppler meter, and a transient-time meter.</p><p>The gated-pipe meter was found to be difficult to use and sensitive to particulate matter in the fluid. The Doppler meter, while easy to use, would not function suitably on steel pipe 6 inches or larger in diameter, or on aluminum pipe larger than 8 inches in diameter. The transient-time meter was more difficult to use than the other two meters; however, this instrument provided a high degree of accuracy and reliability under a variety of conditions. Of the three meters tested, only the transient-time meter was found to be suitable for providing reliable discharge measurements on the variety of irrigation systems used in the High Plains region.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri8072","usgsCitation":"Luckey, R.R., Heimes, F.J., and Gaggiani, N.G., 1980, Calibration and testing of selected portable flowmeters for use on large irrigation systems: U.S. Geological Survey Water-Resources Investigations Report 80-72, iv, 21 p., https://doi.org/10.3133/wri8072.","productDescription":"iv, 21 p.","numberOfPages":"29","costCenters":[],"links":[{"id":159131,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1980/0072/report-thumb.jpg"},{"id":349807,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1980/0072/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"High Plains Aquifer","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -106,\n              32\n            ],\n            [\n              -96,\n              32\n            ],\n            [\n              -96,\n              43.5\n            ],\n            [\n              -106,\n              43.5\n            ],\n            [\n              -106,\n              32\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a07e4b07f02db5f95c7","contributors":{"authors":[{"text":"Luckey, Richard R.","contributorId":17980,"corporation":false,"usgs":true,"family":"Luckey","given":"Richard","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":199864,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Heimes, Frederick J.","contributorId":20787,"corporation":false,"usgs":true,"family":"Heimes","given":"Frederick","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":199865,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Gaggiani, Neville G. gaggiani@usgs.gov","contributorId":3280,"corporation":false,"usgs":true,"family":"Gaggiani","given":"Neville","email":"gaggiani@usgs.gov","middleInitial":"G.","affiliations":[],"preferred":true,"id":199863,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":28066,"text":"wri8076 - 1980 - Simulation of water-quality data at selected stream sites in the Missouri River Basin, Montana","interactions":[],"lastModifiedDate":"2018-11-14T10:15:59","indexId":"wri8076","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1980","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":"80-76","title":"Simulation of water-quality data at selected stream sites in the Missouri River Basin, Montana","docAbstract":"<p>Modification of sampling programs at some water-quality stations in the Missouri River basin in Montana has eliminated the means by which solute loads have been directly obtained in past years. To compensate for this loss, water-quality and streamflow data were statistically analyzed and solute loads were simulated using computer techniques.</p><p>Functional relationships existing between specific conductance and solute concentration for monthly samples were used to develop linear regression models. The models were then used to simulate daily solute concentrations using daily specific conductance as the independent variable. Once simulated, the solute concentrations, in milligrams per liter, were transformed into daily solute loads, in tons, using mean daily streamflow records.</p><p>Computer output was formatted into tables listing simulated mean monthly solute concentrations, in milligrams per liter, and the monthly and annual solute loads, in tons, for water years 1975-78.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri8076","usgsCitation":"Knapton, J.R., and Jacobson, M., 1980, Simulation of water-quality data at selected stream sites in the Missouri River Basin, Montana: U.S. Geological Survey Water-Resources Investigations Report 80-76, iv, 30 p., https://doi.org/10.3133/wri8076.","productDescription":"iv, 30 p.","costCenters":[],"links":[{"id":359416,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1980/0076/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":158011,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1980/0076/report-thumb.jpg"}],"country":"United States","state":"Montana","otherGeospatial":"Missouri River 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,{"id":28481,"text":"wri79114 - 1980 - Methods and applications of digital-model simulation of the Red River alluvial aquifer: Shreveport to the mouth of the Black River, Louisiana","interactions":[],"lastModifiedDate":"2019-11-06T15:26:07","indexId":"wri79114","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1980","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":"79-114","title":"Methods and applications of digital-model simulation of the Red River alluvial aquifer: Shreveport to the mouth of the Black River, Louisiana","docAbstract":"The Red River Waterways Project provides for the construction of five locks and dams on the Red River from the Mississippi River to Shreveport, La. The methodology used by the U.S. Geological Survey in studying the effects of the navigation pools on the ground-water-flow regime involved digital modeling of steady- and nonsteady-state conditions. The steady-state model, GWFLOW, computes the head response in an aquifer due to various boundary conditions. The nonsteady-state model, SUPERMOCK, was designed to simulate transient stress and response in an alluvial-flow system. In addition to the simulation models several computer programs were developed during the study to aid in the preparation of field data for input to the models and in the calibration of the models. Calibration techniques unique to each of the models were developed for the investigation. (USGS)","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wri79114","usgsCitation":"Ludwig, A.H., and Terry, J.E., 1980, Methods and applications of digital-model simulation of the Red River alluvial aquifer: Shreveport to the mouth of the Black River, Louisiana: U.S. Geological Survey Water-Resources Investigations Report 79-114, vi, 103 p. , https://doi.org/10.3133/wri79114.","productDescription":"vi, 103 p. ","costCenters":[],"links":[{"id":159194,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1979/0114/report-thumb.jpg"},{"id":369020,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1979/0114/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Louisiana","city":"Shreveport","otherGeospatial":"Black River","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -93.8507080078125,\n              31.6042705179912\n            ],\n            [\n              -91.77703857421875,\n              31.6042705179912\n            ],\n            [\n              -91.77703857421875,\n              32.55144352864431\n            ],\n            [\n              -93.8507080078125,\n              32.55144352864431\n            ],\n            [\n              -93.8507080078125,\n              31.6042705179912\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a51e4b07f02db62a091","contributors":{"authors":[{"text":"Ludwig, A. H.","contributorId":63007,"corporation":false,"usgs":true,"family":"Ludwig","given":"A.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":199881,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Terry, J. E.","contributorId":87930,"corporation":false,"usgs":true,"family":"Terry","given":"J.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":199882,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":28282,"text":"wri79112 - 1980 - Estimated water use in Florida, 1977","interactions":[],"lastModifiedDate":"2019-12-05T08:37:54","indexId":"wri79112","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1980","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":"79-112","title":"Estimated water use in Florida, 1977","docAbstract":"During 1977, an average of 21,466 million gallons of water was withdrawn daily for use in Florida--an increase of 6,153 million gallons per day since 1970. The 1977 daily use was 14,812 million gallons of saline water and 6,654 million gallons of freshwater. Most of the saline water, largely surface water, was pumped from tidal estuaries. Only 107.6 million gallons per day of saline water--less than 1 percent--was obtained from wells. Thermoelectric power generation used virtually all the saline water, 14,738 million gallons per day, whereas all other industrial uses were only 73 million gallons of saline water per day. The freshwater supply was almost equally divided between ground water (53 percent) and surface water (47 percent). Of the total freshwater used, 43 percent was for irrigation--an average of 2,873 million gallons of freshwater daily on the average. The remaining daily use of freshwater was 21 percent for thermoelectric power generation, 19 percent for public supply; 14 percent for industrial use other than thermoelectric power generation; and 3 percent for domestic and rural use. Irrigation was also responsible for the greatest consumption during 1977, with 1,255 million gallons consumed daily which also includes 192 million gallons per day conveyance loss. (Kosco-USGS)","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wri79112","usgsCitation":"Leach, S.D., and Healy, H.G., 1980, Estimated water use in Florida, 1977: U.S. Geological Survey Water-Resources Investigations Report 79-112, iv, 76 p. , https://doi.org/10.3133/wri79112.","productDescription":"iv, 76 p. 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,{"id":28356,"text":"wri8093 - 1980 - Investigation of artificial recharge of aquifers in Nebraska","interactions":[],"lastModifiedDate":"2024-07-30T14:26:01.843492","indexId":"wri8093","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1980","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":"80-93","title":"Investigation of artificial recharge of aquifers in Nebraska","docAbstract":"<p>Large withdrawals of ground water for irrigation are causing progressive declines of ground-water levels in some areas of Nebraska. An investigation was conducted to determine the technical feasibility of artificially recharging aquifers through wells and through surface spreading by means of impoundments, pits, and canals. Information gained from a literature search and from preliminary tests was used to design several artificial-recharge experiments. The experiments showed that large quantities of water can be recharged through wells and by surface spreading if conditions are favorable.</p><p>In the well experiments, about 0.5 billion gallons of water from an aquifer recharged by the Platte River was transported 3 miles by pipeline and recharged through a well into a Pleistocene sand and gravel aquifer near Aurora where ground-water levels are declining. The recharge rate was about 730 gallons per minute during two tests of 6 and 8 months duration. The rise in ground-water levels due to recharge extended more than a mile from the recharge well in both tests.</p><p>The pattern of ground-water-level buildup during the 8-month test was similar to that during the 6-month test. Two-thirds of the way through the test the rate of water-level buildup in the recharge well increased greatly because casing failure allowed a large amount of sediment to enter the well.</p><p>Although the chemical quality of the recharge water was markedly different from that of the native aquifer water, no evidence of clogging due to chemical reaction was detected; also, there was no evidence of clogging due to air entrainment or bacterial growth. Evaluation of water-level changes in the recharge well and in observation wells during the 6-month test indicated some clogging of the aquifer in the immediate vicinity of the recharge well due to a small amount (0.04 milligram per liter) of fine sediment in the recharge water. Analysis of water-level buildup in the recharge well during the 6-month test indicated that recharge could have continued at a rate of about 700 gallons per minute for several years before rehabilitation of the recharge well would have been necessary.</p><p>In surface-spreading experiments, the maximum sustained infiltration rates from a 24-foot-diameter ring infiltrometer set in loess at the well-recharge site near Aurora were about 0.5 foot per day during a 140day test. The recharge water caused water levels in a perched zone of saturation at depths between 36 and 38 feet to rise 15 feet, to within 21 feet of the surface, indicating that if the test had continued or if the impoundment area had been larger, the water level in the perched zone of saturation might have risen to the surface thereby reducing the infiltration rate.</p><p>The maximum sustained infiltration rate from a similar experiment in the Sand Hills near Tryon was 11 feet per day. Perching layers also retarded downward infiltration and caused lateral movement of water in the subsurface at this site.</p><p>Infiltration rates from re-use pits near the Aurora site ranged from 0.01 to 1.60 feet per day, indicating that the permeability of the subsurface material is extremely variable and that perching layers probably are absent in some areas.</p><p>Flow measurements in an irrigation canal excavated in loess near Farwell indicate an infiltration rate of 0.36 foot per day from a 2.7mile reach.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri8093","collaboration":"Prepared in cooperation with the Old West Regional Commission; the Nebraska Resources Center, Institute of Agriculture and Natural Resources, The University of Nebraska-Lincoln and the Nebraska Natural Resources Commission","usgsCitation":"Lichtler, W.F., Stannard, D.I., and Kouma, E., 1980, Investigation of artificial recharge of aquifers in Nebraska: U.S. Geological Survey 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