{"pageNumber":"1893","pageRowStart":"47300","pageSize":"25","recordCount":68925,"records":[{"id":15090,"text":"ofr88472 - 1988 - Water resources in the twenty-first century; a study of the implications of climate uncertainty","interactions":[{"subject":{"id":15090,"text":"ofr88472 - 1988 - Water resources in the twenty-first century; a study of the implications of climate uncertainty","indexId":"ofr88472","publicationYear":"1988","noYear":false,"title":"Water resources in the twenty-first century; a study of the implications of climate uncertainty"},"predicate":"SUPERSEDED_BY","object":{"id":3626,"text":"cir1030 - 1989 - Water resources in the twenty-first century; a study of the implications of climate uncertainty","indexId":"cir1030","publicationYear":"1989","noYear":false,"title":"Water resources in the twenty-first century; a study of the implications of climate uncertainty"},"id":1}],"supersededBy":{"id":3626,"text":"cir1030 - 1989 - Water resources in the twenty-first century; a study of the implications of climate uncertainty","indexId":"cir1030","publicationYear":"1989","noYear":false,"title":"Water resources in the twenty-first century; a study of the implications of climate uncertainty"},"lastModifiedDate":"2012-02-02T00:06:58","indexId":"ofr88472","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1988","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":"88-472","title":"Water resources in the twenty-first century; a study of the implications of climate uncertainty","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr88472","usgsCitation":"Moss, M.E., and Lins, H.F., 1988, Water resources in the twenty-first century; a study of the implications of climate uncertainty: U.S. Geological Survey Open-File Report 88-472, vi, 48 p. ill., maps ;28 cm., https://doi.org/10.3133/ofr88472.","productDescription":"vi, 48 p. ill., maps ;28 cm.","costCenters":[],"links":[{"id":148057,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1988/0472/report-thumb.jpg"},{"id":44007,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1988/0472/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f4e4b07f02db5f0940","contributors":{"authors":[{"text":"Moss, Marshall E.","contributorId":6830,"corporation":false,"usgs":true,"family":"Moss","given":"Marshall","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":170549,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Lins, Harry F. 0000-0001-5385-9247 hlins@usgs.gov","orcid":"https://orcid.org/0000-0001-5385-9247","contributorId":1505,"corporation":false,"usgs":true,"family":"Lins","given":"Harry","email":"hlins@usgs.gov","middleInitial":"F.","affiliations":[{"id":502,"text":"Office of Surface Water","active":true,"usgs":true}],"preferred":true,"id":170548,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":17446,"text":"ofr88172 - 1988 - Oklahoma; a summary of activities of the U.S. Geological Survey, Water Resources Division in fiscal years 1986-87","interactions":[],"lastModifiedDate":"2012-02-02T00:07:19","indexId":"ofr88172","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1988","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":"88-172","title":"Oklahoma; a summary of activities of the U.S. Geological Survey, Water Resources Division in fiscal years 1986-87","docAbstract":"The activities of the Oklahoma District, Water Resources Division, U.S. Geological Survey are summaried for fiscal years 1986-87. Included are summary statements of current and recently completed projects, alphabetical and numerical listings of surface-water stations, and a bibliography of Oklahoma reports. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr88172","usgsCitation":"Havens, J., 1988, Oklahoma; a summary of activities of the U.S. Geological Survey, Water Resources Division in fiscal years 1986-87: U.S. Geological Survey Open-File Report 88-172, iv, 141 p. :ill., maps ;28 cm., https://doi.org/10.3133/ofr88172.","productDescription":"iv, 141 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":150219,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1988/0172/report-thumb.jpg"},{"id":46597,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1988/0172/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b28e4b07f02db6b1494","contributors":{"authors":[{"text":"Havens, J.S.","contributorId":12043,"corporation":false,"usgs":true,"family":"Havens","given":"J.S.","email":"","affiliations":[],"preferred":false,"id":176421,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":44006,"text":"ofr88343 - 1988 - Water use in New Mexico, 1985","interactions":[],"lastModifiedDate":"2022-04-20T16:48:38.723392","indexId":"ofr88343","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1988","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":"88-343","title":"Water use in New Mexico, 1985","docAbstract":"<p>Water-use data are essential for managing the State's limited water resources. The New Mexico State Engineer Office (NMSEO) and the U.S. Geological Survey collect and publish data on water use at 5-year intervals. These data are used by Federal and State agencies, city and county planners, private industry, and irrigation districts. </p><p>This report graphically summarizes water-use data by county in New Mexico in 1985. The primary source of data was the NMSEO Technical Report 46 (Wilson, 1986), which contains detailed water-use information. The data presented here are in the same format (categories of use and units) as the technical report. The Survey' s national data-collection format differs from the NMSEO format in some category definitions, quantity of data reported, and units. T</p><p>The State Engineer Office defines a withdrawal as the amount of water removed from a surface- or ground-water source. A depletion is that part of a withdrawal consumed by man or livestock, included in crops or products, evaporated or transpired, or otherwise removed. In the figures and text referring to specific data, water use is synonymous with \"withdrawals,\" not consumptive use.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr88343","collaboration":"Prepared in cooperation with the New Mexico State Engineer Office","usgsCitation":"Garrabrant, L.A., 1988, Water use in New Mexico, 1985: U.S. Geological Survey Open-File Report 88-343, 1 Plate: 26.20 x 17.08 inches, https://doi.org/10.3133/ofr88343.","productDescription":"1 Plate: 26.20 x 17.08 inches","costCenters":[],"links":[{"id":399170,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1988/0343/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":169207,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1988/0343/report-thumb.jpg"}],"country":"United States","state":"New 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Mexico\",\"nation\":\"USA  \"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49aee4b07f02db5c7dc7","contributors":{"authors":[{"text":"Garrabrant, Lynn A.","contributorId":44212,"corporation":false,"usgs":true,"family":"Garrabrant","given":"Lynn","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":228975,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":14578,"text":"ofr88308 - 1988 - Water-quality data (July 1986 through September 1987) and statistical summaries (March 1985 through September 1987) for the Clark Fork and selected tributaries from Deer Lodge to Missoula, Montana","interactions":[],"lastModifiedDate":"2012-02-02T00:06:48","indexId":"ofr88308","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1988","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":"88-308","title":"Water-quality data (July 1986 through September 1987) and statistical summaries (March 1985 through September 1987) for the Clark Fork and selected tributaries from Deer Lodge to Missoula, Montana","docAbstract":"Water quality sampling was conducted at seven sites on the Clark Fork and selected tributaries from Deer Lodge to Missoula, Montana, from July 1986 through September 1987. This report presents tabulations and statistical summaries of the water quality data. The data presented in this report supplement previous data collected from March 1985 through June 1986 for six of the seven sites. Included in this report are tabulations of instantaneous values of streamflow, onsite water quality, hardness, and concentrations of trace elements and suspended sediment for periodic samples. Also included are tables and hydrographs of daily mean values for streamflow, suspended-sediment concentration, and suspended-sediment discharge at three mainstream stations and one tributary. Statistical summaries are presented for periodic water quality data collected from March 1986 through September 1987. Selected data are illustrated by graphs showing median concentrations to suspended-sediment concentrations, and median concentrations of trace elements in suspended sediment. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr88308","usgsCitation":"Lambing, J., 1988, Water-quality data (July 1986 through September 1987) and statistical summaries (March 1985 through September 1987) for the Clark Fork and selected tributaries from Deer Lodge to Missoula, Montana: U.S. Geological Survey Open-File Report 88-308, v, 55 p. :ill., maps ;28 cm., https://doi.org/10.3133/ofr88308.","productDescription":"v, 55 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":146599,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1988/0308/report-thumb.jpg"},{"id":43244,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1988/0308/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e5e4b07f02db5e6c81","contributors":{"authors":[{"text":"Lambing, J. H.","contributorId":100860,"corporation":false,"usgs":true,"family":"Lambing","given":"J. H.","affiliations":[],"preferred":false,"id":169678,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":44827,"text":"wri884131 - 1988 - Potentiometric surface of the Turpentine Run basin aquifer in the Tutu area, eastern St. Thomas, U.S. Virgin Islands, September 11, 1987","interactions":[],"lastModifiedDate":"2012-02-02T00:10:47","indexId":"wri884131","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1988","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":"88-4131","title":"Potentiometric surface of the Turpentine Run basin aquifer in the Tutu area, eastern St. Thomas, U.S. Virgin Islands, September 11, 1987","language":"ENGLISH","doi":"10.3133/wri884131","usgsCitation":"Graves, R.P., and Gonzalez, R., 1988, Potentiometric surface of the Turpentine Run basin aquifer in the Tutu area, eastern St. Thomas, U.S. Virgin Islands, September 11, 1987: U.S. Geological Survey Water-Resources Investigations Report 88-4131, 1 map : col. ; 43 x 43 cm., on sheet 56 x 96 cm., https://doi.org/10.3133/wri884131.","productDescription":"1 map : col. ; 43 x 43 cm., on sheet 56 x 96 cm.","costCenters":[],"links":[{"id":171286,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":82176,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1988/4131/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad4e4b07f02db682f1c","contributors":{"authors":[{"text":"Graves, Robert P. rggraves@usgs.gov","contributorId":2558,"corporation":false,"usgs":true,"family":"Graves","given":"Robert","email":"rggraves@usgs.gov","middleInitial":"P.","affiliations":[],"preferred":true,"id":230506,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Gonzalez, Ralph","contributorId":82700,"corporation":false,"usgs":true,"family":"Gonzalez","given":"Ralph","email":"","affiliations":[],"preferred":false,"id":230507,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":19023,"text":"ofr88170 - 1988 - Hydrologic and suspended-sediment data for Reelfoot Lake, Obion and Lake Counties, northwestern Tennessee, May 1985-September 1986","interactions":[],"lastModifiedDate":"2012-02-02T00:07:32","indexId":"ofr88170","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1988","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":"88-170","title":"Hydrologic and suspended-sediment data for Reelfoot Lake, Obion and Lake Counties, northwestern Tennessee, May 1985-September 1986","docAbstract":"Hydrologic data for Reelfoot Lake in Obion and Lake Counties, Tennessee, were collected at 4 surface water inflow stations, 1 outflow station, 2 rainfall stations, 2 lake elevation stations, and 29 wells for the period May 1, 1985 through September 30, 1986. Additionally, suspended-sediment data were collected at three stations on two of the major tributaries to the lake. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr88170","usgsCitation":"Garrett, J., 1988, Hydrologic and suspended-sediment data for Reelfoot Lake, Obion and Lake Counties, northwestern Tennessee, May 1985-September 1986: U.S. Geological Survey Open-File Report 88-170, iv, 50 p. :map ;28 cm., https://doi.org/10.3133/ofr88170.","productDescription":"iv, 50 p. :map ;28 cm.","costCenters":[],"links":[{"id":1095,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/ofr88-170","linkFileType":{"id":5,"text":"html"}},{"id":151335,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4acce4b07f02db67e9f3","contributors":{"authors":[{"text":"Garrett, J.W.","contributorId":87958,"corporation":false,"usgs":true,"family":"Garrett","given":"J.W.","email":"","affiliations":[],"preferred":false,"id":180168,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":67613,"text":"l210 - 1988 - Dillingham, Alaska, vegetation and land cover, 1974-77","interactions":[],"lastModifiedDate":"2012-02-10T00:11:22","indexId":"l210","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1988","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":321,"text":"Land Use and Land Cover","code":"L","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"210","title":"Dillingham, Alaska, vegetation and land cover, 1974-77","language":"ENGLISH","doi":"10.3133/l210","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1988, Dillingham, Alaska, vegetation and land cover, 1974-77: U.S. Geological Survey Land Use and Land Cover 210, 23 by 40 inches, https://doi.org/10.3133/l210.","productDescription":"23 by 40 inches","costCenters":[],"links":[{"id":188418,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":260919,"rank":900,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/l/210/plate-1.pdf"},{"id":260920,"rank":900,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/l/210/plate-2.pdf"}],"scale":"250000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -159,59 ], [ -159,60 ], [ -156,60 ], [ -156,59 ], [ -159,59 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a82e4b07f02db64accc","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":534359,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":1893,"text":"wsp2319 - 1988 - Effect of water quality on survival of Lahontan cutthroat trout eggs in the Truckee River, west-central Nevada and eastern California","interactions":[{"subject":{"id":19375,"text":"ofr84437 - 1984 - Effect of water quality on survival of Lahontan Cutthroat trout eggs in the , west-central Nevada and eastern California","indexId":"ofr84437","publicationYear":"1984","noYear":false,"title":"Effect of water quality on survival of Lahontan Cutthroat trout eggs in the , west-central Nevada and eastern California"},"predicate":"SUPERSEDED_BY","object":{"id":1893,"text":"wsp2319 - 1988 - Effect of water quality on survival of Lahontan cutthroat trout eggs in the Truckee River, west-central Nevada and eastern California","indexId":"wsp2319","publicationYear":"1988","noYear":false,"title":"Effect of water quality on survival of Lahontan cutthroat trout eggs in the Truckee River, west-central Nevada and eastern California"},"id":1}],"lastModifiedDate":"2016-01-12T11:44:23","indexId":"wsp2319","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1988","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":341,"text":"Water Supply Paper","code":"WSP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"2319","title":"Effect of water quality on survival of Lahontan cutthroat trout eggs in the Truckee River, west-central Nevada and eastern California","docAbstract":"The U.S. Fish and Wildlife Service has an ongoing program to assess the feasibility of reestablishing naturally spawning populations of Lahontan cutthroat trout in the Truckee River-Pyramid Lake system in Nevada. Previous in situ egg-survival studies have documented a 100 percent mortality of cutthroat trout eggs artificially planted in potential spawning gravels in the Truckee River downstream from Reno. The relation between ambient river-quality conditions and the observed mortality of eggs, however, has not been adequately documented. This study was designed to monitor the quality of surface and intragravel water during a trout-egg incubation period that began March 10, 1980. Five sites were monitored: two upstream from Reno (background sites), one near Reno, and two downstream from Wadsworth. \r\n\r\nAfter an incubation period of about 30 days, poor egg survival was recorded at all sites, including an unexpected high mortality at the upstream background sites. Analyses of the data indicated that the principal cause of egg mortality at the two downstream sites was low concentrations (less than 5 milligrams per liter) of intragravel dissolved oxygen. Low water temperatures, rather than degraded water-quality conditions, largely contributed to the poor survival at the upstream sites. \r\n\r\nBased on the results of this study, the following were considered unlikely to be mortality factors during the incubation period: (1) high water temperatures; (2) toxicity due to ammonia, nitrite, nitrate, arsenic, cadmium, copper, iron, lead, manganese, mercury, and zinc; and (3) decreasing intragravel dissolved oxygen caused by inflow of oxygen-poor ground water.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wsp2319","collaboration":"Prepared in cooperation with the U.S. Fish and Wildlife Service and U.S. Bureau of Indian Affairs","usgsCitation":"Hoffman, R., and Scoppettone, G.G., 1988, Effect of water quality on survival of Lahontan cutthroat trout eggs in the Truckee River, west-central Nevada and eastern California: U.S. Geological Survey Water Supply Paper 2319, iv, 21 p. , https://doi.org/10.3133/wsp2319.","productDescription":"iv, 21 p. ","numberOfPages":"28","costCenters":[{"id":654,"text":"Western Fisheries Research Center","active":true,"usgs":true}],"links":[{"id":138403,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/2319/report-thumb.jpg"},{"id":27182,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/2319/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"California, Nevada","otherGeospatial":"Truckee River","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -120.72052001953125,\n              39.059716474034666\n            ],\n            [\n              -120.72052001953125,\n              40.23550866893913\n            ],\n            [\n              -118.12774658203125,\n              40.23550866893913\n            ],\n            [\n              -118.12774658203125,\n              39.059716474034666\n            ],\n            [\n              -120.72052001953125,\n              39.059716474034666\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a4be4b07f02db6253a9","contributors":{"authors":[{"text":"Hoffman, Ray J.","contributorId":53770,"corporation":false,"usgs":true,"family":"Hoffman","given":"Ray J.","affiliations":[],"preferred":false,"id":144324,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Scoppettone, Gary G.","contributorId":23925,"corporation":false,"usgs":true,"family":"Scoppettone","given":"Gary","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":144323,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":54332,"text":"wdrIL871 - 1988 - Water Resources Data, Illinois, Water Year 1987, Vol. 1","interactions":[],"lastModifiedDate":"2012-02-02T00:11:51","indexId":"wdrIL871","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1988","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":"IL-87-1","title":"Water Resources Data, Illinois, Water Year 1987, Vol. 1","language":"ENGLISH","doi":"10.3133/wdrIL871","usgsCitation":"Stahl, R., Fitzgerald, K.K., Richards, T., and Hayes, P., 1988, Water Resources Data, Illinois, Water Year 1987, Vol. 1: U.S. Geological Survey Water Data Report IL-87-1, NA, https://doi.org/10.3133/wdrIL871.","productDescription":"NA","costCenters":[],"links":[{"id":174271,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0ae4b07f02db5fb94d","contributors":{"authors":[{"text":"Stahl, R.L.","contributorId":35798,"corporation":false,"usgs":true,"family":"Stahl","given":"R.L.","email":"","affiliations":[],"preferred":false,"id":249930,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Fitzgerald, K. K.","contributorId":34501,"corporation":false,"usgs":true,"family":"Fitzgerald","given":"K.","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":249929,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Richards, T.E.","contributorId":64718,"corporation":false,"usgs":true,"family":"Richards","given":"T.E.","email":"","affiliations":[],"preferred":false,"id":249932,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Hayes, P.D.","contributorId":52644,"corporation":false,"usgs":true,"family":"Hayes","given":"P.D.","email":"","affiliations":[],"preferred":false,"id":249931,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":39654,"text":"pp1403A - 1988 - Summary of the hydrology of the Floridan aquifer system in Florida and in parts of Georgia, South Carolina, and Alabama","interactions":[],"lastModifiedDate":"2025-04-17T18:08:44.491095","indexId":"pp1403A","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1988","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":331,"text":"Professional Paper","code":"PP","onlineIssn":"2330-7102","printIssn":"1044-9612","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"1403","chapter":"A","title":"Summary of the hydrology of the Floridan aquifer system in Florida and in parts of Georgia, South Carolina, and Alabama","docAbstract":"The Floridan aquifer system is one of the major sources of ground-water supplies in the United States. This highly productive aquifer system underlies all of Florida, southern Georgia, and small parts of adjoining Alabama and South Carolina, for a total area of about 100,000 square miles. About 3 billion gallons of water per day is withdrawn from the aquifer for all uses, and, in many areas, the Floridan is the sole source of freshwater.\r\n\r\nThe aquifer system is a sequence of hydraulically connected carbonate rocks (principally limestone and some dolomite) that generally range in age from Late Paleocene to Early Miocene. The rocks vary in thickness from a featheredge where they crop out to more than 3,500 ft where the aquifer is deeply buried. The aquifer system generally consists of an upper aquifer and a lower aquifer, separated by a less permeable confining unit of highly variable properties. In parts of north Florida and southwest Georgia, there is little permeability contrast within the aquifer system. Thus in these areas the Floridan is effectively one continuous aquifer. The upper and lower aquifers are defined on the basis of permeability, and their boundaries locally do not coincide with those for either time-stratigraphic or rock-stratigraphic units.\r\n\r\nLow-permeability clastic rocks overlie much of the Floridan aquifer system. The lithology, thickness, and integrity of these low-permeability rocks have a controlling effect on the development of permeability and ground-water flow in the Floridan locally. \r\n\r\nThe Floridan aquifer system derives its permeability from openings that vary from fossil hashes and networks of many solution-widened joints to large cavernous openings in karst areas. Diffuse flow pre-dominates where the small openings occur, whereas conduit flow may occur where there are large cavernous openings. For the Upper Floridan aquifer, transmissivities are highest (greater than 1,000,000 ft squared per day) in the unconfined karst areas of central and northern Florida. Lowest transmissivities (less than 50,000 ft squared per day) occur in the Florida panhandle and southernmost Florida, where the Upper Floridan aquifer is confined by thick clay sections. The hydraulic properties of the Lower Floridan aquifer are not well known; however, this unit also contains intervals of very high transmissivity that have been attributed to paleokarst development.\r\n\r\nThe dominant feature of the Floridan flow system, both before and after ground-water development, is Upper Floridan aquifer springs, nearly all of which occur in unconfined and semiconfined parts of the aquifer in Florida. Before ground-water development, spring flow and point discharge to surface-water bodies was about 88 percent of the estimated 21,500 cubic ft per second total discharge. Current discharge (early 1980's) is about 24,100 cubic ft per second, 75 percent of which is spring flow and discharge to surface-water bodies, 17 percent is withdrawal from wells, and 8 percent is diffuse upward leakage.\r\n\r\nPumpage has been and continues to be supplied primarily by the diversion of natural outflow from the aquifer system and by induced recharge rather than by loss of water from aquifer storage. The approximately 3 billion gallons per day pumped from the Floridan aquifer system has resulted in long-term regional water-level declines of more than 10 ft in three broad areas of the flow system: (1) coastal Georgia and adjacent South Carolina and northeast Florida, (2) west-central Florida, and (3) the Florida panhandle. Saltwater has encroached as a result of pumping in a few coastal areas.\r\n\r\nIn general, the water chemistry in the Upper Floridan is related to flow and proximity to the freshwater-saltwater interface. In the unconfined or semiconfined areas where flow is vigorous, dissolved-solids concentrations are low (less than 250 milligrams per liter). Where the system is more tightly confined, flow is more sluggish and concentrations are higher (grea","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/pp1403A","usgsCitation":"Summary of the hydrology of the Floridan aquifer system in Florida and in parts of Georgia, South Carolina, and Alabama; 1988; PP; 1403-A; Johnston, Richard H.; Bush, Peter W.","productDescription":"Report: 24 p.; 4 Plates: 20.00 x 26.00 inches or smaller","numberOfPages":"24","costCenters":[{"id":27821,"text":"Caribbean-Florida Water Science Center","active":true,"usgs":true}],"links":[{"id":67366,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/1403a/report.pdf","text":"Report","size":"5.46 MB","linkFileType":{"id":1,"text":"pdf"},"description":"PP 1403-A"},{"id":67362,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/1403a/plate-1.pdf","size":"1.22 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Warehouse</a></p>","publishedDate":"1988-10-01","noUsgsAuthors":false,"publicationDate":"1988-10-01","publicationStatus":"PW","scienceBaseUri":"4f4e4b00e4b07f02db6980f5","contributors":{"authors":[{"text":"Johnston, Richard H.","contributorId":95860,"corporation":false,"usgs":true,"family":"Johnston","given":"Richard","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":221917,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bush, Peter W.","contributorId":57820,"corporation":false,"usgs":true,"family":"Bush","given":"Peter","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":221916,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":49032,"text":"ofr8894 - 1988 - Water-resources activities in New York, 1987-88","interactions":[],"lastModifiedDate":"2012-02-02T00:10:43","indexId":"ofr8894","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1988","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":"88-94","title":"Water-resources activities in New York, 1987-88","docAbstract":"The U.S. Geological Survey conducted more than 35 water resources projects in New York in 1987-88. These studies, done largely through cooperative joint-funding programs with the state, County, and local agencies, encompass statewide networks of measurement stations that provide continuous records of streamflow, groundwater levels, and water quality; they also address regional and local problems as well as critical problems of national scope. Some of the questions addressed by these studies are the effect of sewers on groundwater levels and streamflow on Long Island; the occurrence and transport of PCB residues within the upper Hudson River basin; the effect of acid rain on streams in the Catskill Mountains; the frequency and magnitude of floods statewide; the role of wetlands in improving the chemical quality of landfill leachate; the direction of groundwater movement from waste disposal sites near the Niagara River; and the location and potential well yields of stratified-drift aquifers in upstate New York. (USGS)","language":"ENGLISH","doi":"10.3133/ofr8894","usgsCitation":"Marshall, M.P., and Finch, A.J., 1988, Water-resources activities in New York, 1987-88: U.S. Geological Survey Open-File Report 88-94, 56 p.  ill., maps ; 28 cm., https://doi.org/10.3133/ofr8894.","productDescription":"56 p.  ill., maps ; 28 cm.","costCenters":[],"links":[{"id":171808,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1988/0094/report-thumb.jpg"},{"id":85890,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1988/0094/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b15e4b07f02db6a4bab","contributors":{"authors":[{"text":"Marshall, Mary P. (compiler)","contributorId":12546,"corporation":false,"usgs":true,"family":"Marshall","given":"Mary","suffix":"(compiler)","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":238872,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Finch, Anne J.","contributorId":102494,"corporation":false,"usgs":true,"family":"Finch","given":"Anne","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":238873,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":44020,"text":"ofr88330 - 1988 - Water-table map of Brewster and Harwich, Massachusetts: September 21 to October 22, 1987","interactions":[],"lastModifiedDate":"2012-02-02T00:11:03","indexId":"ofr88330","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1988","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":"88-330","title":"Water-table map of Brewster and Harwich, Massachusetts: September 21 to October 22, 1987","language":"ENGLISH","doi":"10.3133/ofr88330","issn":"ma","usgsCitation":"Johnson, D.G., and Davis, N.M., 1988, Water-table map of Brewster and Harwich, Massachusetts: September 21 to October 22, 1987: U.S. Geological Survey Open-File Report 88-330, 1 map ;sheet 84 x 71 cm., https://doi.org/10.3133/ofr88330.","productDescription":"1 map ;sheet 84 x 71 cm.","costCenters":[],"links":[{"id":168351,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":81439,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1988/0330/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e2e4b07f02db5e4d31","contributors":{"authors":[{"text":"Johnson, David G.","contributorId":108166,"corporation":false,"usgs":true,"family":"Johnson","given":"David","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":229007,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Davis, Nancy M.","contributorId":18824,"corporation":false,"usgs":true,"family":"Davis","given":"Nancy","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":229006,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":44705,"text":"wri884062 - 1988 - Bathymetry of Lakes Marion and Moultrie, South Carolina, 1984-85","interactions":[],"lastModifiedDate":"2017-01-25T08:50:05","indexId":"wri884062","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1988","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":"88-4062","title":"Bathymetry of Lakes Marion and Moultrie, South Carolina, 1984-85","docAbstract":"Lakes Marion and Moultrie are two large, interconnected reservoirs in the Coastal Plain of South Carolina. Bathymetric surveys during 1984-85 determined that, for the full-pool water surface elevation of 76.8 ft, the volume of Lake Marion is 1,425 ,000 acre-ft, and for the full-pool water surface elevation of 75.0 ft, the volume of Lake Moultrie is 1,060,000 acre-ft. These volumes are considered accurate to within 5%. Comparison with volumes determined in 1941, when the reservoirs were filled, shows decreased in volume of 73,000 acre-ft in Lake Marion and 30,000 acre-ft in Lake Moultrie. These changes in volume, however, are subject to relatively large possible error because they represent relatively small differences between relatively large volumes, and because the accuracy of the 1941 volumes is not known. Measurements of sediment inflow and outflow and of deposition rate suggest the volume losses were more likely about 29,000 acre-ft in Lake Marion and about 1,600 acre-ft in Lake Moultrie. The discrepancy in the estimate of volume changes does not affect the accuracy of the volume computation or the maps. 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Carolina\",\"nation\":\"USA  \"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a6ce4b07f02db63e4d1","contributors":{"authors":[{"text":"Patterson, Glenn G.","contributorId":9653,"corporation":false,"usgs":true,"family":"Patterson","given":"Glenn","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":230289,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Logan, S.W.","contributorId":53404,"corporation":false,"usgs":true,"family":"Logan","given":"S.W.","email":"","affiliations":[],"preferred":false,"id":230290,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":30430,"text":"wri854327 - 1988 - Rainfall-runoff relationships of the Hop Brook basin, Manchester, Connecticut","interactions":[],"lastModifiedDate":"2012-02-02T00:08:56","indexId":"wri854327","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1988","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":"85-4327","title":"Rainfall-runoff relationships of the Hop Brook basin, Manchester, Connecticut","language":"ENGLISH","publisher":"U.S. Dept. of the Interior, Geological Survey ;\r\nWestern Distribution Branch,","doi":"10.3133/wri854327","usgsCitation":"Weiss, L., 1988, Rainfall-runoff relationships of the Hop Brook basin, Manchester, Connecticut: U.S. Geological Survey Water-Resources Investigations Report 85-4327, v, 22 p. :ill., 1 map ;28 cm., https://doi.org/10.3133/wri854327.","productDescription":"v, 22 p. :ill., 1 map ;28 cm.","costCenters":[],"links":[{"id":159747,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1985/4327/report-thumb.jpg"},{"id":59208,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1985/4327/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":59209,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1985/4327/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a80e4b07f02db64960d","contributors":{"authors":[{"text":"Weiss, L.A.","contributorId":95098,"corporation":false,"usgs":true,"family":"Weiss","given":"L.A.","affiliations":[],"preferred":false,"id":203236,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":27164,"text":"wri874260 - 1988 - Hydrogeology and flow of water in a sand and gravel aquifer contaminated by wood-preserving compounds, Pensacola, Florida","interactions":[],"lastModifiedDate":"2012-02-02T00:08:26","indexId":"wri874260","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1988","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":"87-4260","title":"Hydrogeology and flow of water in a sand and gravel aquifer contaminated by wood-preserving compounds, Pensacola, Florida","docAbstract":"The sand and gravel aquifer in southern Escambia County, Florida , is a typical surficial aquifer composed of quartz sands and gravels interbedded locally with silts and clays. Problems of groundwater contamination from leaking surface impoundments are common in surficial aquifers and are a subject of increasing concern and attention. A potentially widespread contamination problem involves organic chemicals from wood-preserving processes. Because creosote is the most extensively used industrial preservative in the United States, an abandoned wood-treatment plant near Pensacola was chosen for investigation. This report describes the hydrogeology and groundwater flow system of the sand and gravel aquifer near the plant. A three-dimensional simulation of groundwater flow in the aquifer was evaluated under steady-state conditions. The model was calibrated on the basis of observed water levels from January 1986. Calibration criteria included reproducing all water levels within the accuracy of the data (one-half contour interval in most cases). Sensitivity analysis showed that the simulations were most sensitive to recharge and vertical leakance of the confining units between layers 1 and 2, and relatively insensitive to changes in hydraulic conductivity and transmissivity and to other changes in vertical leakance. Applications of the results of the calibrated flow model in evaluation of solute transport may require further discretization of the contaminated area, including more sublayers, than were needed for calibration of the groundwater flow system itself. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri874260","usgsCitation":"Franks, B., 1988, Hydrogeology and flow of water in a sand and gravel aquifer contaminated by wood-preserving compounds, Pensacola, Florida: U.S. Geological Survey Water-Resources Investigations Report 87-4260, v, 72 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri874260.","productDescription":"v, 72 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":123427,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1987/4260/report-thumb.jpg"},{"id":56040,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1987/4260/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b23e4b07f02db6ade66","contributors":{"authors":[{"text":"Franks, B.J.","contributorId":107739,"corporation":false,"usgs":true,"family":"Franks","given":"B.J.","email":"","affiliations":[],"preferred":false,"id":197671,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":25386,"text":"wri854127 - 1988 - Alternative sources of large seasonal ground-water supplies in the headwaters of the Susquehanna River basin, New York","interactions":[],"lastModifiedDate":"2012-02-02T00:08:29","indexId":"wri854127","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1988","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":"85-4127","title":"Alternative sources of large seasonal ground-water supplies in the headwaters of the Susquehanna River basin, New York","docAbstract":"The northern divide of the Susquehanna River basin crosses 29 broad valleys that contain thick glacial deposits but are drained only by small headwater streams. Much groundwater could be withdrawn from sand and gravel deposits in these valleys with little immediate effect on streamflow. A digital model of the headwater reach of one typical valley suggests that pumping 10.8 million gal/day for 2 months every summer would lower the water table as much as 33 ft, cause the upper 1,900 ft of the stream draining the valley to go dry, and reduce streamflow downvalley by 1.2 million gal/day by the time pumping ceased. Saturated thickness of surficial sand and gravel exceeds 40 ft in about half the headwater valley reaches; the valley floor areas range from 0.2 to 9 sq mi. Seepage losses from small streams that carry runoff from adjacent till-covered uplands are a major source of recharge to aquifers in these valleys under natural conditions and would increase if the water table were lowered by seasonal withdrawals. Some aquifers beneath extensive clay layers in these and other valleys of the Susquehanna River basin may be partially independent of streams but not easily evaluated. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri854127","usgsCitation":"Randall, A., Snavely, D.S., Holecek, T., and Waller, R., 1988, Alternative sources of large seasonal ground-water supplies in the headwaters of the Susquehanna River basin, New York: U.S. Geological Survey Water-Resources Investigations Report 85-4127, v, 121 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri854127.","productDescription":"v, 121 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":122814,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1985/4127/report-thumb.jpg"},{"id":54120,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1985/4127/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adde4b07f02db686aed","contributors":{"authors":[{"text":"Randall, A. D.","contributorId":81077,"corporation":false,"usgs":true,"family":"Randall","given":"A. D.","affiliations":[],"preferred":false,"id":193479,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Snavely, D. S.","contributorId":103692,"corporation":false,"usgs":true,"family":"Snavely","given":"D.","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":193480,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Holecek, T.P.","contributorId":76358,"corporation":false,"usgs":true,"family":"Holecek","given":"T.P.","email":"","affiliations":[],"preferred":false,"id":193478,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Waller, R.M.","contributorId":13659,"corporation":false,"usgs":true,"family":"Waller","given":"R.M.","email":"","affiliations":[],"preferred":false,"id":193477,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":27099,"text":"wri884087 - 1988 - Preimpoundment hydrologic conditions in the Swatara Creek (1981-84) and estimated postimpoundment water quality in and downstream from the planned Swatara State Park Reservoir, Lebanon and Schuylkill counties, Pennsylvania","interactions":[],"lastModifiedDate":"2021-09-10T18:34:56.459331","indexId":"wri884087","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1988","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":"88-4087","title":"Preimpoundment hydrologic conditions in the Swatara Creek (1981-84) and estimated postimpoundment water quality in and downstream from the planned Swatara State Park Reservoir, Lebanon and Schuylkill counties, Pennsylvania","docAbstract":"The hydrology and water quality of Swatara Creek were studied by the U.S. Geological Survey in cooperation with the Pennsylvania Department of Environmental Resources, Bureau of State Parks, from July 1981 through September 1984. The purpose of the study was to determine the effects of anthracite-coal mining and other point and nonpoint sources on the water quality of a planned 10,500 acre-foot reservoir. The Swatara State Park Reservoir is planned to be used for recreation and drinking-water supply for the city of Lebanon and surrounding communities.\r\n\r\n      Annual precipitation during 1982, 1983, and 1984 was about 8 percent below, near normal, and 29 percent above the long-term average, respectively. The average annual precipitation during a year with near-normal precipitation, the 1983 water year, was 47 inches at Pine Grove. Mean streamflows during 1982, 1983, and 1984 were about 15 percent below, 4 percent above, and 50 percent above the long-term average, respectively. The average streamflow to the planned reservoir area during the 1983 water year was about 220 cubic feet per second.\r\n\r\n      Inflows to, and downstream discharge from, the planned reservoir wer poorly buffered. Median alkalinity ranged from 4 to 7 mg/L (milligrams per liter) and median acidity ranged from 2 to 5 mg/L at the three sampling locations. Maximum total-recoverable iron, aluminum, and manganese concentrations were 100,000, 66,000, and 2,300 micrograms per liter, respectively. During 1983 the annual discharges of total-recoverable iron, aluminum, and manganese to the planned reservoir area were estimated to be 692, 300, and 95 tons, respectively. About 87 percent of the total-recoverable iron and 91 percent of total-recoverable sluminum measured was in the suspended phase. The data indicated that mine drainage affects the quality of Swatara Creek and will affect the quality of the planned reservoir.\r\n\r\n      In addition to mine drainage, point-source nutrient and metal discharges will probably affect the planned reservoir. For example, in September 1983, Swatara Creek was sampled downstream from a point source. A dissolved- phosphorus concentration of 14 mg/L and total ammonia plus organic nitrogen concentration of 8.2 mg/L were measured. At the same location, concentrations of total-recoverable aluminum, chromium, copper, iron, and lead were 35, 300, 110, 1,300, and 32 micrograms per liter, respectively.\r\n\r\n      Inflows to the planned Swatara State Park Reservoir are estimated to be acidic and rich in nutrients and select metals. Unless an effort is made to improve the quality of water from point and nonpoint sources, these conditions may impair the planned uses for the reservoir. Conservation releases from the reservoir need to be carefully controlled or these conditions also may degrade the water quality downstream.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri884087","usgsCitation":"Fishel, D.K., 1988, Preimpoundment hydrologic conditions in the Swatara Creek (1981-84) and estimated postimpoundment water quality in and downstream from the planned Swatara State Park Reservoir, Lebanon and Schuylkill counties, Pennsylvania: U.S. Geological Survey Water-Resources Investigations Report 88-4087, Report: vi, 108 p.; 2 Plates: 16.57 × 10.53 inches and 16.40 × 7.99 inches, https://doi.org/10.3133/wri884087.","productDescription":"Report: vi, 108 p.; 2 Plates: 16.57 × 10.53 inches and 16.40 × 7.99 inches","costCenters":[{"id":532,"text":"Pennsylvania Water Science Center","active":true,"usgs":true}],"links":[{"id":158966,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1988/4087/report-thumb.jpg"},{"id":55964,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1988/4087/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":55963,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1988/4087/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":55962,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1988/4087/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":389084,"rank":5,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_47007.htm"}],"country":"United States","state":"Pennsylvania","otherGeospatial":"Swatara Creek","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -76.6375,\n              40.4569\n            ],\n            [\n              -76.21,\n              40.4569\n            ],\n            [\n              -76.21,\n              40.66\n            ],\n            [\n              -76.6375,\n              40.66\n            ],\n            [\n              -76.6375,\n              40.4569\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4acce4b07f02db67e77d","contributors":{"authors":[{"text":"Fishel, D. K.","contributorId":72028,"corporation":false,"usgs":true,"family":"Fishel","given":"D.","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":197550,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":25706,"text":"wri884115 - 1988 - Phytoplankton populations in lakes in Loch Vale, Rocky Mountain National Park, Colorado: Sensitivity to acidic conditions and nitrate enrichment","interactions":[],"lastModifiedDate":"2020-11-09T17:40:24.076318","indexId":"wri884115","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1988","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":"88-4115","title":"Phytoplankton populations in lakes in Loch Vale, Rocky Mountain National Park, Colorado: Sensitivity to acidic conditions and nitrate enrichment","docAbstract":"<p>No abstract available.&nbsp;</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wri884115","usgsCitation":"McKnight, D.M., Miller, C., Smith, R., Baron, J., and Spaulding, S.A., 1988, Phytoplankton populations in lakes in Loch Vale, Rocky Mountain National Park, Colorado: Sensitivity to acidic conditions and nitrate enrichment: U.S. Geological Survey Water-Resources Investigations Report 88-4115, vi, 102 p., https://doi.org/10.3133/wri884115.","productDescription":"vi, 102 p.","costCenters":[{"id":40553,"text":"WMA - Office of the Chief Operating Officer","active":true,"usgs":true}],"links":[{"id":156914,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"country":"United States","state":"Colorado","otherGeospatial":"Rocky Mountain National Park","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -105.6745719909668,\n              40.282144825334825\n            ],\n            [\n              -105.63457489013672,\n              40.282144825334825\n            ],\n            [\n              -105.63457489013672,\n              40.309247135103334\n            ],\n            [\n              -105.6745719909668,\n              40.309247135103334\n            ],\n            [\n              -105.6745719909668,\n              40.282144825334825\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adae4b07f02db68591d","contributors":{"authors":[{"text":"McKnight, Diane M.","contributorId":59773,"corporation":false,"usgs":false,"family":"McKnight","given":"Diane","email":"","middleInitial":"M.","affiliations":[{"id":16833,"text":"INSTAAR, University of Colorado","active":true,"usgs":false}],"preferred":false,"id":194739,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Miller, Christine","contributorId":21582,"corporation":false,"usgs":true,"family":"Miller","given":"Christine","affiliations":[],"preferred":false,"id":194740,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Smith, Richard","contributorId":34172,"corporation":false,"usgs":true,"family":"Smith","given":"Richard","email":"","affiliations":[],"preferred":false,"id":194741,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Baron, Jill 0000-0002-5902-6251 jill_baron@usgs.gov","orcid":"https://orcid.org/0000-0002-5902-6251","contributorId":194124,"corporation":false,"usgs":true,"family":"Baron","given":"Jill","email":"jill_baron@usgs.gov","affiliations":[{"id":291,"text":"Fort Collins Science Center","active":true,"usgs":true}],"preferred":true,"id":194742,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Spaulding, Sarah A. 0000-0002-9787-7743 sspaulding@usgs.gov","orcid":"https://orcid.org/0000-0002-9787-7743","contributorId":1157,"corporation":false,"usgs":true,"family":"Spaulding","given":"Sarah","email":"sspaulding@usgs.gov","middleInitial":"A.","affiliations":[{"id":451,"text":"National Water Quality Assessment Program","active":true,"usgs":true}],"preferred":true,"id":194743,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":27179,"text":"wri874279 - 1988 - Effects of fluctuating river-pool stages on ground-water levels in the adjacent alluvial aquifer in the lower Arkansas River, Arkansas","interactions":[],"lastModifiedDate":"2012-02-02T00:08:26","indexId":"wri874279","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1988","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":"87-4279","title":"Effects of fluctuating river-pool stages on ground-water levels in the adjacent alluvial aquifer in the lower Arkansas River, Arkansas","docAbstract":"The U.S. Geological Survey conducted a study in cooperation with the U.S. Army Corps of Engineers to determine the effect of fluctuating the lower Arkansas River. A network of 41 wells was used to delineate 4 cross sections adjacent to river pools 2 and 5 of the McClellan-Kerr Arkansas River Navigation System to examine groundwater levels at various distances from the river. The hydraulic gradient of water levels in the alluvial aquifer along these cross sections indicates that the river is losing water to the adjacent aquifer. The effect on groundwater levels in the alluvial aquifer caused by pool-stage fluctuations was most pronounced at distances less than about 2 miles from the Arkansas River. At distances greater than about 2 miles, the changes in groundwater levels probably were the result of water levels rising in the aquifer since the heavy summer irrigation withdrawals have ceased. An equation useful for estimating the distribution of head change an aquifer in response to river-pool-stage changes, was applied to the study area to estimate the effect of a 1-foot rise in pool stage on water levels in the adjacent alluvial aquifer after equilibrium conditions have been established. The theoretical head change (rise) in the aquifer was estimated to range from 1-foot at the Arkansas River to 0.57 foot at a distance of 5 miles away from the river. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri874279","usgsCitation":"Freiwald, D., and Grosz, G., 1988, Effects of fluctuating river-pool stages on ground-water levels in the adjacent alluvial aquifer in the lower Arkansas River, Arkansas: U.S. Geological Survey Water-Resources Investigations Report 87-4279, iv, 22 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri874279.","productDescription":"iv, 22 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":124180,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1987/4279/report-thumb.jpg"},{"id":56055,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1987/4279/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a2ce4b07f02db6140f1","contributors":{"authors":[{"text":"Freiwald, D.A.","contributorId":39000,"corporation":false,"usgs":true,"family":"Freiwald","given":"D.A.","email":"","affiliations":[],"preferred":false,"id":197697,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Grosz, G.D.","contributorId":90340,"corporation":false,"usgs":true,"family":"Grosz","given":"G.D.","email":"","affiliations":[],"preferred":false,"id":197698,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":26225,"text":"wri874250 - 1988 - Determination of evaporation and seepage losses, Upper Lake Mary near Flagstaff, Arizona","interactions":[],"lastModifiedDate":"2012-02-02T00:08:31","indexId":"wri874250","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1988","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":"87-4250","title":"Determination of evaporation and seepage losses, Upper Lake Mary near Flagstaff, Arizona","docAbstract":"Two mass-transfer equations were developed to compute evaporation as a part of the evaporation were seepage-loss study for the Upper Lake Mary Reservoir near Flagstaff, Arizona, which has a capacity of 15,620 acre-feet and a surface area of 876 acres. The mass-transfer equations do not require an independent measure of evaporation to define the mass-transfer coefficient. Data from other evaporation studies were used to define the mass-transfer coefficient as a function of wind shear and atmospheric stability. Long-term seepage losses were determined by use of a seepage-probability curve-derived from a stage-seepage relation and defined by several selected short-term water budgets-and a lake-stage probability curve. Seepage curves were derived for several different amounts of assumed reservoir sealing. The long-term water saving that would result from each increment of lake-bottom sealing were computed. The study revealed that the evaporation loss was 27 percent of 2 ,100 acre-feet per year of the total reservoir inflow during 1950-71; seepage loss was 45 percent or 3,500 acre-feet per year. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri874250","usgsCitation":"Blee, J., 1988, Determination of evaporation and seepage losses, Upper Lake Mary near Flagstaff, Arizona: U.S. Geological Survey Water-Resources Investigations Report 87-4250, vi, 39 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri874250.","productDescription":"vi, 39 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":119090,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1987/4250/report-thumb.jpg"},{"id":55025,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1987/4250/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aa8e4b07f02db667809","contributors":{"authors":[{"text":"Blee, J.W.","contributorId":63815,"corporation":false,"usgs":true,"family":"Blee","given":"J.W.","email":"","affiliations":[],"preferred":false,"id":196015,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":27084,"text":"wri874168 - 1988 - Hydrology and water quality of Delavan Lake in southeastern Wisconsin","interactions":[],"lastModifiedDate":"2015-10-20T10:48:18","indexId":"wri874168","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1988","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":"87-4168","title":"Hydrology and water quality of Delavan Lake in southeastern Wisconsin","docAbstract":"<p>Delavan Lake is a eutrophic, recreational lake in a densely populated area of southeastern Wisconsin. Sewage effluent and septic tank drainage were diverted out of the drainage basin of the lake to improve its water quality in 1981. The worst known blue-green algal bloom occurred in the lake in the summer of 1983. A comprehensive hydrologic and water-quality investigation was started in October 1983 to determine why the water quality in the lake apparently had not improved after cessation of influxes of waste waters. This report describes the hydrology and water quality of Delavan Lake and its drainage basin during the 1984 and 1985 water years.</p>\n<p>All major external inputs and outputs of phosphorus and nitrogen to the lake were measured to assess the importance of each source. Internal loading of phosphorus was calculated as a residual of a mass-balance budget. The in-lake phosphorus mass during the 2-year study shows a gradual declining trend that suggests an improving lake condition but also could be due to a random phosphorus decline. Future monitoring will be needed to determine whether the decline in phosphorus has indeed occurred as a result of waste-water diversion.</p>\n<p>Continuous streamflow and water-quality monitoring in the subbasins of the Delavan Lake watershed showed a wide range of annual phosphorus and nitrogen yields during the study. Jackson Creek tributary, which predominantly drains the city of Elkhorn, had the highest average yields of phosphorus (838 pounds per square mile) and Kjeldahl nitrogen (3,600 pounds per square mile). These yields were almost three times those found in the Jackson Creek basin, which has the largest livestock population. The other major tributary, Delavan Lake tributary 2, had much lower average annual yields of phosphorus (53.1 pounds per square mile) and Kjeldahl nitrogen (550 pounds per square mile). The lower yields in this tributary result from significantly reduced runoff caused by storage and evapotranspiration in a large pond that is surrounded by a wetland in the stream's basin.</p>\n<p>External loading of phosphorus and nitrogen were sufficient to cause eutrophic conditions. Internal loading of phosphorus was more than two times the external phosphorus supply. Most of the internal loading occurred when the hypolimnion was anoxic during summer. Internal loading of phosphorus during the 1985 water year was significantly reduced from that of 1984 because of a shorter anoxic period.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri874168","collaboration":"Prepared in cooperation with the Delevan Lake Sanitary District","usgsCitation":"Field, S.J., and Duerk, M., 1988, Hydrology and water quality of Delavan Lake in southeastern Wisconsin: U.S. Geological Survey Water-Resources Investigations Report 87-4168, vi, 107 p., https://doi.org/10.3133/wri874168.","productDescription":"vi, 107 p.","numberOfPages":"112","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":677,"text":"Wisconsin Water Science Center","active":true,"usgs":true}],"links":[{"id":55950,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1987/4168/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":123372,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1987/4168/report-thumb.jpg"}],"country":"United States","state":"Wisconsin","otherGeospatial":"Delevan Lake","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -88.53675842285156,\n              42.74449090412214\n            ],\n            [\n              -88.72695922851562,\n              42.597070956721446\n            ],\n            [\n              -88.71253967285156,\n              42.54751604081074\n            ],\n            [\n              -88.6328887939453,\n              42.54144538620976\n            ],\n            [\n              -88.58894348144531,\n              42.55763248666914\n            ],\n            [\n              -88.53813171386719,\n              42.60465241823049\n            ],\n            [\n              -88.48663330078125,\n              42.627896481020855\n            ],\n            [\n              -88.45916748046875,\n              42.63042248679955\n            ],\n            [\n              -88.43170166015625,\n              42.63698962207662\n            ],\n            [\n              -88.41522216796875,\n              42.6450712987999\n            ],\n            [\n              -88.39462280273438,\n              42.67082463742399\n            ],\n            [\n              -88.38363647460938,\n              42.69303463329987\n            ],\n            [\n              -88.44612121582031,\n              42.72532590823042\n            ],\n            [\n              -88.53675842285156,\n              42.74449090412214\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a18e4b07f02db604c0c","contributors":{"authors":[{"text":"Field, S. J.","contributorId":50540,"corporation":false,"usgs":true,"family":"Field","given":"S.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":197529,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Duerk, M.D.","contributorId":18806,"corporation":false,"usgs":true,"family":"Duerk","given":"M.D.","affiliations":[],"preferred":false,"id":197528,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":26177,"text":"wri864351 - 1988 - Ground-water flow near two radioactive-waste-disposal areas at the Western New York Nuclear Service Center, Cattaraugus County, New York: Results of flow simulation","interactions":[],"lastModifiedDate":"2024-06-17T19:20:12.719862","indexId":"wri864351","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1988","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":"86-4351","title":"Ground-water flow near two radioactive-waste-disposal areas at the Western New York Nuclear Service Center, Cattaraugus County, New York: Results of flow simulation","docAbstract":"<p>Two adjacent burial areas were excavated in a clay-rich till at a radioactive waste disposal site near West Valley in Cattaraugus County, N.Y.: (1) which contains mainly low-level radioactive wastes generated onsite by a nuclear fuel reprocessing plant, has been in operation since 1966; and (2) which contains commercial low-level radioactive wastes, was operated during 1963-75. Groundwater below the upper 3 meters of till generally moves downward through a 20- to 30-meter thick sequence of tills underlain by lacustrine and kame-delta deposits of fine sand and silt. Groundwater in the weathered, upper 3 meters of till can move laterally for several meters before either moving downward into the kame-delta deposits or discharging to the land surface. A two-dimensional finite-element model that simulates two vertical sections was used to evaluate hydrologic factors that control groundwater flow in the till. Conditions observed during March 1983 were reproduced accurately in steady-state simulations that used four isotropic units of differing hydraulic conductivity to represent two fractured and weathered till units near land surfaces, an intermediate group of isolated till zones that contain significant amounts of fine sand and silt, and a sequence of till units at depths that have been consolidated by overburden pressure. Recharge rates used in the best-fit simulation ranged from 1.4 cm/yr along smooth, sloping or compacted surfaces to 3.8 cm/yr near swampy areas. Values of hydraulic conductivity and infiltration used in the calibrated best-fit model were nearly identical to values used in a previous model analysis of the nearby commercial-waste burial area. Results of the model simulations of a burial pit assumed to be filled with water indicate that water near the bottom of the burial pit would migrate laterally in the shallow, weathered till for 5 to 6 meters before moving downward into the unweathered till, and water near the top of the pit would move laterally less than 20 meters before moving downward into the unweathered till. These results indicate that subsurface migration of radionuclides in groundwater to points of discharge to land surface is unlikely as long as the water level does not rise into the reworked cover material.&nbsp;</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri864351","usgsCitation":"Bergeron, M.P., and Bugliosi, E., 1988, Ground-water flow near two radioactive-waste-disposal areas at the Western New York Nuclear Service Center, Cattaraugus County, New York: Results of flow simulation: U.S. Geological Survey Water-Resources Investigations Report 86-4351, v, 30 p., https://doi.org/10.3133/wri864351.","productDescription":"v, 30 p.","costCenters":[],"links":[{"id":430319,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_36662.htm","linkFileType":{"id":5,"text":"html"}},{"id":54978,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1986/4351/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":124281,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1986/4351/report-thumb.jpg"}],"country":"United States","state":"New York","county":"Cattaraugus County","otherGeospatial":"Western New York Nuclear Service Center","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -78.662,\n              42.459\n            ],\n            [\n              -78.662,\n              42.446\n            ],\n            [\n              -78.644,\n              42.446\n            ],\n            [\n              -78.644,\n              42.459\n            ],\n            [\n              -78.662,\n              42.459\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aabe4b07f02db6698fe","contributors":{"authors":[{"text":"Bergeron, M. P.","contributorId":42969,"corporation":false,"usgs":true,"family":"Bergeron","given":"M.","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":195943,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bugliosi, E. F.","contributorId":70738,"corporation":false,"usgs":true,"family":"Bugliosi","given":"E. F.","affiliations":[],"preferred":false,"id":195944,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":14984,"text":"ofr8886 - 1988 - Geohydrologic data from the Floridan aquifer system in Florida and in parts of Georgia, South Carolina, and Alabama","interactions":[],"lastModifiedDate":"2016-12-15T13:51:52","indexId":"ofr8886","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1988","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":"88-86","title":"Geohydrologic data from the Floridan aquifer system in Florida and in parts of Georgia, South Carolina, and Alabama","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr8886","usgsCitation":"Miller, J.A., 1988, Geohydrologic data from the Floridan aquifer system in Florida and in parts of Georgia, South Carolina, and Alabama: U.S. Geological Survey Open-File 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,{"id":4687,"text":"twri02D2 - 1988 - Application of seismic-refraction techniques to hydrologic studies","interactions":[{"subject":{"id":13950,"text":"ofr84746 - 1986 - Application of seismic-refraction techniques to hydrologic studies","indexId":"ofr84746","publicationYear":"1986","noYear":false,"title":"Application of seismic-refraction techniques to hydrologic studies"},"predicate":"SUPERSEDED_BY","object":{"id":4687,"text":"twri02D2 - 1988 - Application of seismic-refraction techniques to hydrologic studies","indexId":"twri02D2","publicationYear":"1988","noYear":false,"title":"Application of seismic-refraction techniques to hydrologic studies"},"id":1}],"lastModifiedDate":"2019-10-15T07:46:19","indexId":"twri02D2","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1988","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":336,"text":"Techniques of Water-Resources Investigations","code":"TWRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"02-D2","title":"Application of seismic-refraction techniques to hydrologic studies","docAbstract":"During the past 30 years, seismic-refraction methods have been used extensively in petroleum, mineral, and engineering investigations and to some extent for hydrologic applications.  Recent advances in equipment, sound sources, and computer interpretation techniques make seismic refraction a highly effective and economical means of obtaining subsurface data in hydrologic studies.  Aquifers that can be defined by one or more high-seismic-velocity surface, such as (1) alluvial or glacial deposits in consolidated rock valleys, (2) limestone or sandstone underlain by metamorphic or igneous rock, or (3) saturated unconsolidated deposits overlain by unsaturated unconsolidated deposits, are ideally suited for seismic-refraction methods.  These methods allow economical collection of subsurface data, provide the basis for more efficient collection of data by test drilling or aquifer tests, and result in improved hydrologic studies.  This manual briefly reviews the basics of seismic-refraction theory and principles.  It emphasizes the use of these techniques in hydrologic investigations and describes the planning, equipment, field procedures, and interpretation techniques needed for this type of study.  Further-more, examples of the use of seismic-refraction techniques in a wide variety of hydrologic studies are presented.","language":"English","publisher":"U.S. Government Printing Office","doi":"10.3133/twri02D2","issn":"0565-596X","usgsCitation":"Haeni, F., 1988, Application of seismic-refraction techniques to hydrologic studies: U.S. Geological Survey Techniques of Water-Resources Investigations 02-D2, x, 86 p. , https://doi.org/10.3133/twri02D2.","productDescription":"x, 86 p. ","costCenters":[{"id":493,"text":"Office of Ground Water","active":true,"usgs":true}],"links":[{"id":139165,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":247,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/twri/twri2d2/","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac6e4b07f02db67a89a","contributors":{"authors":[{"text":"Haeni, F.P.","contributorId":87105,"corporation":false,"usgs":true,"family":"Haeni","given":"F.P.","affiliations":[],"preferred":false,"id":149624,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":57448,"text":"wdrMS871 - 1988 - Water resources data for Mississippi, water year 1987","interactions":[],"lastModifiedDate":"2025-08-28T13:41:03.782564","indexId":"wdrMS871","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1988","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":"MS-87-1","title":"Water resources data for Mississippi, water year 1987","docAbstract":"<p>Water resources data for the 1987 water year for Mississippi consist of records of stage, discharge, and water quality of streams; stage, and water quality of lakes and reservoirs; and water levels and water quality of ground-water wells. This report contains records of water discharge at 78 gaging stations; stage records for 18 of these gaging stations; stage only at 5 gaging stations; water quality for 11 stations, 3 precipitation quality stations, and 120 wells; and water levels for 498 observation wells. Also included are peak-discharge data for 56 crest-stage partial record stations, discharge data at 263 low-flow partial-record stations, and water quality data at 2 partial-record or miscellaneous sites. Locations of these sites are shown on Figures 4-6. Additional water data were collected at various sites, not part of the systematic data collection program, and are published as miscellaneous measurements. These data represent that part of the National Water Data System operated by the U.S. Geological Survey and cooperating State and Federal agencies in Mississippi. </p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wdrMS871","collaboration":"Prepared in cooperation with the Mississippi Department of Natural Resources and with other State, county, municipal, and Federal agencies","usgsCitation":"Tharpe, E., Plunkett, M., Morris, F., and Oakley, W.T., 1988, Water resources data for Mississippi, water year 1987: U.S. Geological Survey Water Data Report MS-87-1, viii, 408 p., https://doi.org/10.3133/wdrMS871.","productDescription":"viii, 408 p.","costCenters":[],"links":[{"id":494987,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wdr/1987/ms-87-1/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":174621,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wdr/1987/ms-87-1/report-thumb.jpg"}],"country":"United 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