{"pageNumber":"470","pageRowStart":"11725","pageSize":"25","recordCount":16502,"records":[{"id":27097,"text":"wri914006 - 1991 - Hydrology and the hypothetical effects of reducing nutrient applications on water quality in the Bald Eagle Creek Headwaters, southeastern Pennsylvania prior to implementation of agricultural best-management practices","interactions":[],"lastModifiedDate":"2022-01-25T21:01:23.332146","indexId":"wri914006","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1991","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":"91-4006","title":"Hydrology and the hypothetical effects of reducing nutrient applications on water quality in the Bald Eagle Creek Headwaters, southeastern Pennsylvania prior to implementation of agricultural best-management practices","docAbstract":"The report characterizes a 0.43-square-mile agricultural watershed in York County, underlain by albite-chlorite and oligoclase-mica schist in the Lower Susquehanna River basin, that is being studied as part of the U.S. Environmental Protection Agency's Chesapeake Bay Program. The water quality of Bald Eagle Creek was studied from October 1985 through September 1987 prior to the implementation of Best-Management Practices to reduce nutrient and sediment discharge into Muddy Creek, a tributary to the Chesapeake Bay. About 88 percent of the watershed is cropland and pasture, and nearly 33 percent of the cropland is used for corn. The animal population is entirely dairy cattle. About 85,640 pounds of nitrogen (460 pounds per acre) and 21,800 pounds of phosphorus (117 pounds per acre) were applied to fields; 52 percent of the nitrogen and 69 percent of the phosphorus was from commercial fertilizer. Prior to fertilization, nitrate nitrogen in the soil ranged from 36 to 136 pounds per acre and phosphorus ranged from 0.89 to 5.7 pounds per acre in the top 4 feet of soil. Precipitation was about 18 percent below normal and streamflow about 35 percent below normal during the 2-year study. Eighty-four percent of the 20.44 inches of runoff was base flow. Median concentrations of total nitrogen and dissolved phosphorous in base flow were 0.05 and 0.04 milligrams per liter as phosphorus, respectively.\r\n\r\n      Concentrations of dissolved nitrate in base flow increased following wet periods after crops were harvested and manure was applied. During the growing season, concentrations decreased similarly to those observed in carbonate-rock areas as nutrient uptake and evapotranspiration by corn increased. About 4,550 pounds of suspended sediment, 5,250 pounds of nitrogen, and 66.6 pounds of phosphorus discharged in base flow during the 2-year period. The suspended sediment load was about 232,000 pounds in stormflow from 26 storms that contributed 51 percent of the total stormflow. The nitrogen load was about 651 pounds and the phosphorus load was about 74 pounds in stormflow from 16 storms that contributed 28 percent of the total stormflow. It is estimated that concentrations of total nitrogen and phosphorus in base flow need to be reduced by 12 and 48 percent, respectively, to detect changes during the nutrient-management phase. Likewise, loads to total nitrogen and phosphorus in base flow need to be reduced by 62 and 57 percent.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri914006","usgsCitation":"Fishel, D.K., Langland, M., and Truhlar, M.V., 1991, Hydrology and the hypothetical effects of reducing nutrient applications on water quality in the Bald Eagle Creek Headwaters, southeastern Pennsylvania prior to implementation of agricultural best-management practices: U.S. Geological Survey Water-Resources Investigations Report 91-4006, vi, 59 p., https://doi.org/10.3133/wri914006.","productDescription":"vi, 59 p.","costCenters":[{"id":532,"text":"Pennsylvania Water Science Center","active":true,"usgs":true}],"links":[{"id":394837,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_47448.htm"},{"id":123520,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1991/4006/report-thumb.jpg"},{"id":55961,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1991/4006/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Pennsylvania","otherGeospatial":"Bald Eagle Creek headwaters","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -76.4778,\n              39.7458\n            ],\n            [\n              -76.4653,\n              39.7458\n            ],\n            [\n              -76.4653,\n              39.7583\n            ],\n            [\n              -76.4778,\n              39.7583\n            ],\n            [\n              -76.4778,\n              39.7458\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4acce4b07f02db67e847","contributors":{"authors":[{"text":"Fishel, D. K.","contributorId":72028,"corporation":false,"usgs":true,"family":"Fishel","given":"D.","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":197546,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Langland, M. J.","contributorId":36173,"corporation":false,"usgs":true,"family":"Langland","given":"M. J.","affiliations":[],"preferred":false,"id":197545,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Truhlar, M. V.","contributorId":96724,"corporation":false,"usgs":true,"family":"Truhlar","given":"M.","email":"","middleInitial":"V.","affiliations":[],"preferred":false,"id":197547,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":30141,"text":"wri914132 - 1991 - Predevelopment hydrology of the Salt River Indian Reservation, East Salt River Valley, Arizona","interactions":[],"lastModifiedDate":"2012-02-02T00:09:03","indexId":"wri914132","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1991","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":"91-4132","title":"Predevelopment hydrology of the Salt River Indian Reservation, East Salt River Valley, Arizona","language":"ENGLISH","publisher":"U.S. Geological Survey ;\r\nBooks and Open-File Reports Section [distributor,","doi":"10.3133/wri914132","usgsCitation":"Thomsen, B.W., and Porcello, J., 1991, Predevelopment hydrology of the Salt River Indian Reservation, East Salt River Valley, Arizona: U.S. Geological Survey Water-Resources Investigations Report 91-4132, v, 37 p. :ill. ;28 cm., https://doi.org/10.3133/wri914132.","productDescription":"v, 37 p. :ill. ;28 cm.","costCenters":[],"links":[{"id":160415,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1991/4132/report-thumb.jpg"},{"id":58953,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1991/4132/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4acde4b07f02db67f409","contributors":{"authors":[{"text":"Thomsen, B. W.","contributorId":39768,"corporation":false,"usgs":true,"family":"Thomsen","given":"B.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":202753,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Porcello, J.J.","contributorId":11661,"corporation":false,"usgs":true,"family":"Porcello","given":"J.J.","email":"","affiliations":[],"preferred":false,"id":202752,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":26305,"text":"wri904075 - 1991 - Ground-water hydrology and the effects of vertical leakage and leachate migration on ground-water quality near the Shelby County landfill, Memphis, Tennessee","interactions":[],"lastModifiedDate":"2012-02-02T00:08:17","indexId":"wri904075","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1991","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":"90-4075","title":"Ground-water hydrology and the effects of vertical leakage and leachate migration on ground-water quality near the Shelby County landfill, Memphis, Tennessee","docAbstract":"An investigation of potential leakage of leachate from the Shelby County landfill near Memphis, West Tennessee, was conducted during 1986-87. The migration of leachate from the landfill to the shallow alluvial aquifer system and the potential leakage to the deeper confined Memphis aquifer of Tertiary age were investigated. A network of observation wells was drilled to determine water levels and aquifer properties in the shallow and deep aquifers as well as in the confining layer. Water samples were collected to define potential leachate occurrence.\r\n\r\nA depression in the water table within the shallow alluvial aquifer was defined from the water-level data. Drawdowns within the cone of depression are as much as 14 feet lower than the adjoining Wolf River. Recharge from the river and leachate from the landfill moves toward the depression. The presence of leachate within the shallow aquifer was confirmed from determinations of dissolved solids and dissolved chloride concentrations and comparisons with areas away from the aflected zone. Leakage from the water-table aquifer to the Memphis aquifer was confirmed from chemical analyses and hydraulic-head data. Dissolved-solids concentrations in water samples from the upper Memphis aquifer near the landfill are higher than in samples from the Memphis aquifer in unaffected areas. Tritium activities in water samples from the upper Memphis aquifer were as high as 34 pico-Curies per liter indicating recent recharge to the Memphis aquifer.\r\n\r\nThe presence of synthetic organic compounds and elevated concentrations of dissolved solids, chloride, and trace metals indicate the leachate has aflected water quality in the alluvial aquifer. Vertical migration of ground water could transmit leachate down to the Memphis aquifer. Although water-quality data indicate that water is leaking from the alluvial aquifer to the Memphis aquifer, most of the data do not indicate the occurrence of leachate in the Memphis aquifer. Chemical data from one well in the Memphis aquifer near the landfill indicates a slightly elevated dissolved-chloride concentration, but the data are limited.","language":"ENGLISH","publisher":"U.S. Geological Survey ;\r\nBooks and Open-File Reports Section [distributor],","doi":"10.3133/wri904075","usgsCitation":"Bradley, M.W., 1991, Ground-water hydrology and the effects of vertical leakage and leachate migration on ground-water quality near the Shelby County landfill, Memphis, Tennessee: U.S. Geological Survey Water-Resources Investigations Report 90-4075, v, 42 p. :ill. ;28 cm., https://doi.org/10.3133/wri904075.","productDescription":"v, 42 p. :ill. ;28 cm.","costCenters":[],"links":[{"id":1999,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/wri904075/","linkFileType":{"id":5,"text":"html"}},{"id":124920,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/wri_90_4075.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b00e4b07f02db69809d","contributors":{"authors":[{"text":"Bradley, M. W.","contributorId":40610,"corporation":false,"usgs":true,"family":"Bradley","given":"M.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":196146,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":30140,"text":"wri894174 - 1991 - Predevelopment hydrology of the Gila River Indian Reservation, south-central Arizona","interactions":[],"lastModifiedDate":"2012-02-02T00:09:03","indexId":"wri894174","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1991","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":"89-4174","title":"Predevelopment hydrology of the Gila River Indian Reservation, south-central Arizona","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri894174","usgsCitation":"Thomsen, B.W., and Eychaner, J., 1991, Predevelopment hydrology of the Gila River Indian Reservation, south-central Arizona: U.S. Geological Survey Water-Resources Investigations Report 89-4174, v, 44 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri894174.","productDescription":"v, 44 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":160414,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1989/4174/report-thumb.jpg"},{"id":58950,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1989/4174/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":58951,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1989/4174/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":58952,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1989/4174/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b08e4b07f02db69b3ed","contributors":{"authors":[{"text":"Thomsen, B. W.","contributorId":39768,"corporation":false,"usgs":true,"family":"Thomsen","given":"B.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":202751,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Eychaner, J.H.","contributorId":34511,"corporation":false,"usgs":true,"family":"Eychaner","given":"J.H.","affiliations":[],"preferred":false,"id":202750,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":30102,"text":"wri904084 - 1991 - Hydrology and potential effects of mining in the Quitchupah and Pines coal-lease tracts, central Utah","interactions":[],"lastModifiedDate":"2017-09-13T16:14:50","indexId":"wri904084","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1991","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":"90-4084","title":"Hydrology and potential effects of mining in the Quitchupah and Pines coal-lease tracts, central Utah","docAbstract":"<p>Bydrologic data were collected for the proposed Quitchupah and Pines coal-lease tracts in Sevier and Bnery Counties, Utah, in order to describe the hydrology and potential effects of mining on the hydrologic system. The Quitchupah and Pines coal-lease tracts are near the Southern Utah Fuel Company coal mine in an area of the central Wasatch Plateau that is characterized by a relatively flat plateau deeply dissected by steep-sided canyons.</p><p>Surface water in the Quitchupah and Pines study area drains to two perennial streams, Muddy Creek to the north and Quitchupah Creek to the south. Peak streamflow is usually in May and June in response to snowmelt runoff; however, thunderstorms can cause short-term high flows in late summer and fall. The specific conductance of surface water in and near the study area measured during the 1987 water year ranged from 440 (iS/cm to 860 (iS/cm. Suspended-sediment concentrations ranged from 17 to 10,900 mg/L in the Quitchupah Creek drainage and 34 to 312 mg/L in the Muddy Creek drainage.</p><p>Stable-isotope studies indicate that recharge to aquifers in the study area is by seepage of snowmelt into rock outcrops. Discharge from the aquifers is at springs, seeps, mines, and zones of seepage in streambeds. The chemical quality of ground water is related to the mineralogy of the formations with which the water has contact. Water from the upper part of the Cast legate Sandstone has the smallest concentration of dissolved solids, 61 mg/L, and water from the North Horn Formation has the largest concentration, 1,080 mg/L.</p><p>Observed effects of underground coal mining at the nearby active mine are considered indicative of the changes that can be expected in the Quitchupah and Pines coal-lease tracts. Subsidence above the mined area could cause dewatering of the Blackhawk Formation and the Star Point Sandstone, changes in the natural drainage patterns, and alteration of both surface- and ground-water quality. Additional studies are needed to gain a better understanding of the hydrologic effects of underground mining in the Quitchupah and Pines coal-lease tracts.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Salt Lake City, Utah","doi":"10.3133/wri904084","collaboration":"Prepared in cooperation with the U.S. Bureau of Land Management","usgsCitation":"Thiros, S.A., and Cordy, G., 1991, Hydrology and potential effects of mining in the Quitchupah and Pines coal-lease tracts, central Utah: U.S. Geological Survey Water-Resources Investigations Report 90-4084, Report: vii, 63 p.; Plate: 26.82 x 24.37 inches, https://doi.org/10.3133/wri904084.","productDescription":"Report: vii, 63 p.; Plate: 26.82 x 24.37 inches","numberOfPages":"72","costCenters":[],"links":[{"id":58920,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1990/4084/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":119617,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1990/4084/report-thumb.jpg"},{"id":58919,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1990/4084/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -111.4208,\n              39.03333\n            ],\n            [\n              -111.2583,\n              39.03333\n            ],\n            [\n               -111.2583,\n              38.95\n            ],\n            [\n              -111.3208,\n              38.95\n            ],\n            [\n              -111.3208,\n              38.88333\n            ],\n            [\n              -111.425,\n              38.88333\n            ],\n            [\n              -111.425,\n              38.93333\n            ],\n            [\n              -111.4589,\n               38.93333\n            ],\n            [\n              -111.4589,\n              38.9875\n            ],\n            [\n              -111.4208,\n              38.9875\n            ],\n            [\n              -111.4208,\n              39.03333\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a18e4b07f02db60517d","contributors":{"authors":[{"text":"Thiros, Susan A. 0000-0002-8544-553X sthiros@usgs.gov","orcid":"https://orcid.org/0000-0002-8544-553X","contributorId":965,"corporation":false,"usgs":true,"family":"Thiros","given":"Susan","email":"sthiros@usgs.gov","middleInitial":"A.","affiliations":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"preferred":true,"id":202681,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Cordy, G. E.","contributorId":59075,"corporation":false,"usgs":true,"family":"Cordy","given":"G. E.","affiliations":[],"preferred":false,"id":202680,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":29631,"text":"wri904200 - 1991 - Computer software for converting ground-water and water-quality data from the National Water Information System for use in a geographic information system","interactions":[],"lastModifiedDate":"2012-02-02T00:08:54","indexId":"wri904200","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1991","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":"90-4200","title":"Computer software for converting ground-water and water-quality data from the National Water Information System for use in a geographic information system","docAbstract":"A geographic information system (GIS) is computer software that provides the capabilities to rapidly display and analyze spatially referenced data. To use a GIS efficiently, software is needed that provides a link between existing spatially referenced data-base systems and the GIS.\r\nThe U.S. Geological Survey (USGS) stores large amounts of spatially referenced hydrologic data in computerized data-base systems. Currently, these data-base systems are physically located on computers that are installed in many USGS offices nationwide. This report describes software that can be used quickly and easily to convert site-description and water-quality data from these data-base systems to the GIS that is used by the USGS. The software described in this report is designed to be used with the same hardware and software that is available to most USGS personnel.","language":"ENGLISH","publisher":"U.S. Geological Survey ;\r\nBooks and Open-File Reports [distributor],","doi":"10.3133/wri904200","usgsCitation":"Scott, J.C., 1991, Computer software for converting ground-water and water-quality data from the National Water Information System for use in a geographic information system: U.S. Geological Survey Water-Resources Investigations Report 90-4200, iv, 55 p. :ill. ;28 cm., https://doi.org/10.3133/wri904200.","productDescription":"iv, 55 p. :ill. ;28 cm.","costCenters":[],"links":[{"id":122760,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1990/4200/report-thumb.jpg"},{"id":58451,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1990/4200/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b19e4b07f02db6a75e0","contributors":{"authors":[{"text":"Scott, J. C.","contributorId":75901,"corporation":false,"usgs":true,"family":"Scott","given":"J.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":201848,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":29443,"text":"wri904129 - 1991 - Hydrologic relations between streamflow and subalpine wetlands in Grand County, Colorado","interactions":[],"lastModifiedDate":"2012-02-02T00:08:56","indexId":"wri904129","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1991","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":"90-4129","title":"Hydrologic relations between streamflow and subalpine wetlands in Grand County, Colorado","language":"ENGLISH","publisher":"U.S. Geological Survey :\r\nBooks and Open-File Reports Section [distributor],","doi":"10.3133/wri904129","usgsCitation":"Ruddy, B.C., and Williams, R., 1991, Hydrologic relations between streamflow and subalpine wetlands in Grand County, Colorado: U.S. Geological Survey Water-Resources Investigations Report 90-4129, v, 53 p. :ill. ;28 cm., https://doi.org/10.3133/wri904129.","productDescription":"v, 53 p. :ill. ;28 cm.","costCenters":[],"links":[{"id":119601,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1990/4129/report-thumb.jpg"},{"id":58289,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1990/4129/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a18e4b07f02db605538","contributors":{"authors":[{"text":"Ruddy, B. C.","contributorId":65098,"corporation":false,"usgs":true,"family":"Ruddy","given":"B.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":201537,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Williams, R.S. Jr.","contributorId":46102,"corporation":false,"usgs":true,"family":"Williams","given":"R.S.","suffix":"Jr.","email":"","affiliations":[],"preferred":false,"id":201536,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":28960,"text":"wri914047 - 1991 - Hydrologic conditions and distribution of selected chemical constituents in water, Snake River Plain Aquifer, Idaho National Engineering Laboratory, Idaho, 1986 to 1988","interactions":[],"lastModifiedDate":"2012-02-02T00:08:35","indexId":"wri914047","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1991","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":"91-4047","title":"Hydrologic conditions and distribution of selected chemical constituents in water, Snake River Plain Aquifer, Idaho National Engineering Laboratory, Idaho, 1986 to 1988","language":"ENGLISH","publisher":"U.S. Geological Survey ;\r\nBooks and Open-File Reports Section [distributor,","doi":"10.3133/wri914047","usgsCitation":"Orr, B.R., and Cecil, L., 1991, Hydrologic conditions and distribution of selected chemical constituents in water, Snake River Plain Aquifer, Idaho National Engineering Laboratory, Idaho, 1986 to 1988: U.S. Geological Survey Water-Resources Investigations Report 91-4047, v, 56 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri914047.","productDescription":"v, 56 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":120064,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1991/4047/report-thumb.jpg"},{"id":57835,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1991/4047/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afde4b07f02db696c35","contributors":{"authors":[{"text":"Orr, B. R.","contributorId":46545,"corporation":false,"usgs":true,"family":"Orr","given":"B.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":200691,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Cecil, L.D.","contributorId":62616,"corporation":false,"usgs":true,"family":"Cecil","given":"L.D.","email":"","affiliations":[],"preferred":false,"id":200692,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
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,{"id":28924,"text":"wri914080 - 1991 - Hydrology and water quality near the South Well Field, southern Franklin County, Ohio, with emphasis on the simulation of ground-water flow and transport of Scioto River","interactions":[],"lastModifiedDate":"2012-02-02T00:08:47","indexId":"wri914080","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1991","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":"91-4080","title":"Hydrology and water quality near the South Well Field, southern Franklin County, Ohio, with emphasis on the simulation of ground-water flow and transport of Scioto River","language":"ENGLISH","publisher":"U.S. Geological Survey ;\r\nBooks and Open-File Reports Section [distributor],","doi":"10.3133/wri914080","usgsCitation":"Oblinger, C.J., Sheets, R.A., and Bair, E., 1991, Hydrology and water quality near the South Well Field, southern Franklin County, Ohio, with emphasis on the simulation of ground-water flow and transport of Scioto River: U.S. Geological Survey Water-Resources Investigations Report 91-4080, vii, 78 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri914080.","productDescription":"vii, 78 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":121718,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1991/4080/report-thumb.jpg"},{"id":57797,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1991/4080/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4acce4b07f02db67e87e","contributors":{"authors":[{"text":"Oblinger, C. J.","contributorId":21554,"corporation":false,"usgs":true,"family":"Oblinger","given":"C.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":200626,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Sheets, R. A.","contributorId":43381,"corporation":false,"usgs":true,"family":"Sheets","given":"R.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":200627,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Bair, E. Scott","contributorId":73231,"corporation":false,"usgs":true,"family":"Bair","given":"E. Scott","affiliations":[],"preferred":false,"id":200628,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":29839,"text":"wri904203 - 1991 - Reconnaissance investigation of water quality, bottom sediment, and biota associated with irrigation drainage in the Klamath Basin, California and Oregon, 1988-89","interactions":[],"lastModifiedDate":"2020-01-02T20:02:17","indexId":"wri904203","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1991","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":"90-4203","title":"Reconnaissance investigation of water quality, bottom sediment, and biota associated with irrigation drainage in the Klamath Basin, California and Oregon, 1988-89","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri904203","usgsCitation":"Sorenson, S.K., and Schwarzbach, S., 1991, Reconnaissance investigation of water quality, bottom sediment, and biota associated with irrigation drainage in the Klamath Basin, California and Oregon, 1988-89: U.S. Geological Survey Water-Resources Investigations Report 90-4203, v, 64 p. , https://doi.org/10.3133/wri904203.","productDescription":"v, 64 p. ","costCenters":[{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":159465,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1990/4203/report-thumb.jpg"},{"id":58637,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1990/4203/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"California, Oregon","otherGeospatial":"Klamath Basin","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -122.08007812499999,\n              41.9921602333763\n            ],\n            [\n              -122.40966796874999,\n              41.77131167976407\n            ],\n            [\n              -122.354736328125,\n              41.42625319507269\n            ],\n            [\n              -121.95922851562501,\n              40.9218144123785\n            ],\n            [\n              -120.673828125,\n              41.00477542222947\n            ],\n            [\n              -120.355224609375,\n              41.32732632036622\n            ],\n            [\n              -120.16845703125,\n              42.15525946577863\n            ],\n            [\n              -120.640869140625,\n              42.35042512243457\n            ],\n            [\n              -121.387939453125,\n              42.512601715736665\n            ],\n            [\n              -121.77246093750001,\n              42.44778143462245\n            ],\n            [\n              -122.01416015625,\n              42.76314586689492\n            ],\n            [\n              -122.14599609375001,\n              42.4234565179383\n            ],\n            [\n              -122.08007812499999,\n              41.9921602333763\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a6ce4b07f02db63eb1a","contributors":{"authors":[{"text":"Sorenson, S. K.","contributorId":28268,"corporation":false,"usgs":true,"family":"Sorenson","given":"S.","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":202219,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Schwarzbach, S.E.","contributorId":32467,"corporation":false,"usgs":true,"family":"Schwarzbach","given":"S.E.","affiliations":[],"preferred":false,"id":202220,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":30031,"text":"wri914122 - 1991 - Bibliography of Regional Aquifer-System Analysis Program of the US Geological Survey, 1978-91","interactions":[],"lastModifiedDate":"2017-12-06T14:05:31","indexId":"wri914122","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1991","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":"91-4122","title":"Bibliography of Regional Aquifer-System Analysis Program of the US Geological Survey, 1978-91","docAbstract":"<p>The Regional Aquifer-System Analysis (RASA) Program of the U.S. Geological Survey was initiated in 1978. The purpose of this program is to define the regional geohydrology and establish a framework of background information on geology, hydrology, and geochemistry of the Nation's important aquifer systems. This information is critically needed to develop an understanding of the Nation's major ground-water flow systems and to support better management of ground-water resources.</p><p>As of May 1991, 28 of the Nation's major aquifer systems have been identified for study under this program. Of these, 17 regional aquifer-system studies have been completed, and 8 studies are ongoing. Starting in 1988, the program devoted part of its resources to compilation of a Nationwide ground-water atlas that presents a comprehensive summary of the Nation's major ground-water resources. The atlas, which is designed in a graphical format supported by descriptive text, will serve as a basic reference for the location, geography, geology, and hydrologic characteristics of the major aquifers in the Nation.</p><p>This bibliography lists the published 876 reports resulting from various studies of the program, from 1978 through May 1991. The list of reports for each study is placed after a brief description of that study.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri914122","usgsCitation":"Sun, R.J., and Weeks, J., 1991, Bibliography of Regional Aquifer-System Analysis Program of the US Geological Survey, 1978-91: U.S. Geological Survey Water-Resources Investigations Report 91-4122, iv, 92 p., https://doi.org/10.3133/wri914122.","productDescription":"iv, 92 p.","costCenters":[],"links":[{"id":160098,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1991/4122/report-thumb.jpg"},{"id":349814,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1991/4122/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a51e4b07f02db629905","contributors":{"authors":[{"text":"Sun, Ren Jen","contributorId":68721,"corporation":false,"usgs":true,"family":"Sun","given":"Ren","email":"","middleInitial":"Jen","affiliations":[],"preferred":false,"id":202563,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Weeks, John B.","contributorId":36123,"corporation":false,"usgs":true,"family":"Weeks","given":"John B.","affiliations":[],"preferred":false,"id":202562,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":30027,"text":"wri914127 - 1991 - Field experiments and simulations of infiltration-rate response to changes in hydrologic conditions for an artificial-recharge test basin near Oakes, southeastern North Dakota","interactions":[],"lastModifiedDate":"2018-03-16T13:49:02","indexId":"wri914127","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1991","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":"91-4127","title":"Field experiments and simulations of infiltration-rate response to changes in hydrologic conditions for an artificial-recharge test basin near Oakes, southeastern North Dakota","docAbstract":"<p>Ponded depth in an artificial-recharge basin was used as a management option to conduct turbid water from the James River to the Oakes aquifer. Infiltration-rate response to changes in ponded depth was evaluated for a 15xl5-meter artificial-recharge test basin constructed in a medium-sandy soil in the irrigation area near Oakes, southeastern North Dakota. Field experiments conducted at the test basin indicated that the clogged soil surface was easily scoured by currents caused by the addition of turbid water to increase ponded depth. Field measurements and computer-model simulations indicated that infiltration-rate response to an increase in ponded depth would be large for a clogged soil condition consisting of a surface filter-cake layer 0.1 centimeter in depth underlain by a sediment-clogged layer extending from 0.1 to 23 centimeters beneath the basin floor. Simulated infiltration-rate response to changes in ponded depth for surface filter-cake layer impedance values ranging from 0 to 1,000 hours indicated that infiltration-rate response would approach and remain near the maximum value for impedance values greater than 10 hours. The smallest infiltration-rate response would occur for impedance values less than 1 hour. For the case of a ground-water mound intersecting the basin floor, the percentage of infiltration-rate response to changes in ponded depth was not influenced by basin geometry, basin surface area, or underlying aquifer hydraulic conductivity. The simulated infiltration-rate response to changes in ponded depth increased when the water-table depth was shallow. Total recharge per unit area was greater for artificial-recharge basins having a less compact geometry than for artificial-recharge basins having a more compact geometry, for artificial-recharge basins having a small surface area than for artificial-recharge basins having a large surface area, and for artificial-recharge basins where underlying aquifer hydraulic conductivity was large rather than small. Artificial-recharge basin conditions most conducive to an effective infiltration-rate response to changes in ponded depth were least conducive to an enhanced total recharge.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri914127","usgsCitation":"Sumner, D.M., Schuh, W., and Cline, R., 1991, Field experiments and simulations of infiltration-rate response to changes in hydrologic conditions for an artificial-recharge test basin near Oakes, southeastern North Dakota: U.S. Geological Survey Water-Resources Investigations Report 91-4127, v, 46 p., https://doi.org/10.3133/wri914127.","productDescription":"v, 46 p.","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":119390,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1991/4127/report-thumb.jpg"},{"id":58831,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1991/4127/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49fce4b07f02db5f598b","contributors":{"authors":[{"text":"Sumner, D. M.","contributorId":100827,"corporation":false,"usgs":true,"family":"Sumner","given":"D.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":202554,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Schuh, W.M.","contributorId":76367,"corporation":false,"usgs":true,"family":"Schuh","given":"W.M.","email":"","affiliations":[],"preferred":false,"id":202553,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Cline, R.L.","contributorId":41473,"corporation":false,"usgs":true,"family":"Cline","given":"R.L.","email":"","affiliations":[],"preferred":false,"id":202552,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":26228,"text":"wri904047 - 1991 - Hydrology and water chemistry of an abandoned surface coal mine, southwestern Henry County, Missouri — 1984-86","interactions":[],"lastModifiedDate":"2022-01-25T21:05:36.879428","indexId":"wri904047","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1991","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":"90-4047","title":"Hydrology and water chemistry of an abandoned surface coal mine, southwestern Henry County, Missouri — 1984-86","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri904047","usgsCitation":"Blevins, D.W., 1991, Hydrology and water chemistry of an abandoned surface coal mine, southwestern Henry County, Missouri — 1984-86: U.S. Geological Survey Water-Resources Investigations Report 90-4047, vii, 52 p., https://doi.org/10.3133/wri904047.","productDescription":"vii, 52 p.","costCenters":[],"links":[{"id":394838,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_47325.htm"},{"id":55028,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1990/4047/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":119092,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1990/4047/report-thumb.jpg"}],"country":"United States","state":"Missouri","county":"Henry County","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -94.0167,\n              38.2594\n            ],\n            [\n              -93.98,\n              38.2594\n            ],\n            [\n              -93.98,\n              38.2972\n            ],\n            [\n              -94.0167,\n              38.2972\n            ],\n            [\n              -94.0167,\n              38.2594\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a18e4b07f02db604f1a","contributors":{"authors":[{"text":"Blevins, D. W.","contributorId":75940,"corporation":false,"usgs":true,"family":"Blevins","given":"D.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":196020,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":29489,"text":"wri904164 - 1991 - A steady-state unsaturated-zone model to simulate pesticide transport","interactions":[],"lastModifiedDate":"2019-12-28T10:18:57","indexId":"wri904164","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1991","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":"90-4164","title":"A steady-state unsaturated-zone model to simulate pesticide transport","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey ","doi":"10.3133/wri904164","usgsCitation":"Rutledge, A.T., and Helgesen, J.O., 1991, A steady-state unsaturated-zone model to simulate pesticide transport: U.S. Geological Survey Water-Resources Investigations Report 90-4164, iv, 13 p. , https://doi.org/10.3133/wri904164.","productDescription":"iv, 13 p. ","costCenters":[{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":119615,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1990/4164/report-thumb.jpg"},{"id":58330,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1990/4164/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b17e4b07f02db6a6298","contributors":{"authors":[{"text":"Rutledge, A. T.","contributorId":38532,"corporation":false,"usgs":true,"family":"Rutledge","given":"A.","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":201600,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Helgesen, J. O.","contributorId":62600,"corporation":false,"usgs":true,"family":"Helgesen","given":"J.","email":"","middleInitial":"O.","affiliations":[],"preferred":false,"id":201601,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":26258,"text":"wri844300 - 1991 - The effects of coal mining on the hydrologic environment of selected stream basins in southern West Virginia","interactions":[],"lastModifiedDate":"2012-02-02T00:08:22","indexId":"wri844300","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1991","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":"84-4300","title":"The effects of coal mining on the hydrologic environment of selected stream basins in southern West Virginia","language":"ENGLISH","publisher":"U.S. Geological Survey ;\r\nBooks and Open-File Services [distributor],","doi":"10.3133/wri844300","usgsCitation":"Borchers, J.W., Ehlke, T.A., Mathes, M., and Downs, S.C., 1991, The effects of coal mining on the hydrologic environment of selected stream basins in southern West Virginia: U.S. Geological Survey Water-Resources Investigations Report 84-4300, viii, 119 p. (some folded) :ill., maps ;28 cm., https://doi.org/10.3133/wri844300.","productDescription":"viii, 119 p. (some folded) :ill., maps ;28 cm.","costCenters":[],"links":[{"id":157786,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1984/4300/report-thumb.jpg"},{"id":55059,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1984/4300/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a9be4b07f02db65df85","contributors":{"authors":[{"text":"Borchers, J. W.","contributorId":74414,"corporation":false,"usgs":true,"family":"Borchers","given":"J.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":196073,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Ehlke, T. A.","contributorId":106477,"corporation":false,"usgs":true,"family":"Ehlke","given":"T.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":196074,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Mathes, M.V. Jr.","contributorId":47412,"corporation":false,"usgs":true,"family":"Mathes","given":"M.V.","suffix":"Jr.","email":"","affiliations":[],"preferred":false,"id":196072,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Downs, S. C.","contributorId":36956,"corporation":false,"usgs":true,"family":"Downs","given":"S.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":196071,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":27681,"text":"wri904146 - 1991 - Preliminary geologic and hydrologic evaluation of a small watershed near Plains, Georgia","interactions":[],"lastModifiedDate":"2020-04-30T17:45:48.848533","indexId":"wri904146","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1991","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":"90-4146","title":"Preliminary geologic and hydrologic evaluation of a small watershed near Plains, Georgia","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri904146","usgsCitation":"Hicks, D., McConnell, J.B., and Asmussen, L.E., 1991, Preliminary geologic and hydrologic evaluation of a small watershed near Plains, Georgia: U.S. Geological Survey Water-Resources Investigations Report 90-4146, iv, 30 p. , https://doi.org/10.3133/wri904146.","productDescription":"iv, 30 p. ","costCenters":[{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true},{"id":13634,"text":"South Atlantic Water Science Center","active":true,"usgs":true}],"links":[{"id":56534,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1990/4146/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":159009,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1990/4146/report-thumb.jpg"}],"country":"United States","state":"Georgia","city":"Plains","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -84.47113037109375,\n              31.962066108310047\n            ],\n            [\n              -84.3585205078125,\n              31.962066108310047\n            ],\n            [\n              -84.3585205078125,\n              32.05522664981892\n            ],\n            [\n              -84.47113037109375,\n              32.05522664981892\n            ],\n            [\n              -84.47113037109375,\n              31.962066108310047\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac9e4b07f02db67c2f9","contributors":{"authors":[{"text":"Hicks, D.W.","contributorId":61795,"corporation":false,"usgs":true,"family":"Hicks","given":"D.W.","email":"","affiliations":[],"preferred":false,"id":198526,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"McConnell, James B.","contributorId":28224,"corporation":false,"usgs":true,"family":"McConnell","given":"James","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":198525,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Asmussen, Loris E.","contributorId":62248,"corporation":false,"usgs":true,"family":"Asmussen","given":"Loris","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":198527,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":31066,"text":"wsp2370B - 1991 - Geology and water resources of Owens Valley, California","interactions":[{"subject":{"id":12080,"text":"ofr88715 - 1989 - Geology and water resources of Owens Valley, California","indexId":"ofr88715","publicationYear":"1989","noYear":false,"title":"Geology and water resources of Owens Valley, California"},"predicate":"SUPERSEDED_BY","object":{"id":31066,"text":"wsp2370B - 1991 - Geology and water resources of Owens Valley, California","indexId":"wsp2370B","publicationYear":"1991","noYear":false,"chapter":"B","title":"Geology and water resources of Owens Valley, California"},"id":1}],"lastModifiedDate":"2012-02-02T00:09:08","indexId":"wsp2370B","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1991","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":"2370","chapter":"B","title":"Geology and water resources of Owens Valley, California","docAbstract":"Owens Valley, a long, narrow valley located along the east flank of the Sierra Nevada in east-central California, is the main source of water for the city of Los Angeles. The city diverts most of the surface water in the valley into the Owens River-Los Angeles Aqueduct system, which transports the water more than 200 miles south to areas of distribution and use. Additionally, ground water is pumped or flows from wells to supplement the surface-water diversions to the river-aqueduct system. Pumpage from wells needed to supplement water export has increased since 1970, when a second aqueduct was put into service, and local concerns have been expressed that the increased pumpage may have had a detrimental effect on the environment and the indigenous alkaline scrub and meadow plant communities in the valley. The scrub and meadow communities depend on soil moisture derived from precipitation and the unconfined part of a multilayered aquifer system. This report, which describes the hydrogeology of the aquifer system and the water resources of the valley, is one in a series designed to (1) evaluate the effects that groundwater pumping has on scrub and meadow communities and (2) appraise alternative strategies to mitigate any adverse effects caused by, pumping. \r\n\r\nTwo principal topographic features are the surface expression of the geologic framework--the high, prominent mountains on the east and west sides of the valley and the long, narrow intermountain valley floor. The mountains are composed of sedimentary, granitic, and metamorphic rocks, mantled in part by volcanic rocks as well as by glacial, talus, and fluvial deposits. The valley floor is underlain by valley fill that consists of unconsolidated to moderately consolidated alluvial fan, transition-zone, glacial and talus, and fluvial and lacustrine deposits. The valley fill also includes interlayered recent volcanic flows and pyroclastic rocks. The bedrock surface beneath the valley fill is a narrow, steep-sided graben that is structurally separated into the Bishop Basin to the north and the Owens Lake Basin to the south. These two structural basins are separated by (1) a bedrock high that is the upper bedrock block of an east-west normal fault, (2) a horst block of bedrock (the Poverty Hills), and (3) Quaternary basalt flows and cinder cones that intercalate and intrude the sedimentary deposits of the valley fill. The resulting structural separation of the basins allowed separate development of fluvial and lacustrine depositional systems in each basin. \r\n\r\nNearly all the ground water in Owens Valley flows through and is stored in the saturated valley fill. The bedrock, which surrounds and underlies the valley fill, is virtually impermeable. Three hydrogeologic units compose the valley-fill aquifer system, a defined subdivision of the ground-water system, and a fourth represents the valley fill below the aquifer system and above the bedrock. The aquifer system is divided into horizontal hydrogeologic units on the basis of either (1) uniform hydrologic characteristics of a specific lithologic layer or (2) distribution of the vertical hydraulic head. Hydrogeologic unit 1 is the upper unit and represents the unconfined part of the system, hydrogeologic unit 2 represents the confining unit (or units), and hydrogeologic unit 3 represents the confined part of the aquifer system. Hydrogeologic unit 4 represents the deep part of the ground-water system and lies below the aquifer system. Hydrogeologic unit 4 transmits or stores much less water than hydrogeologic unit 3 and represents either a moderately consolidated valley fill or a geologic unit in the valley fill defined on the basis of geophysical data. \r\n\r\nNearly all the recharge to the aquifer system is from infiltration of runoff from snowmelt and rainfall on the Sierra Nevada. In contrast, little recharge occurs to the system by runoff from the White and Inyo Mountains or from direct precipitation on the valley floor. Ground wat","language":"ENGLISH","publisher":"U.S. G.P.O. ;For sale by the Books and Open-File Reports Section,","doi":"10.3133/wsp2370B","usgsCitation":"Hollett, K.J., Danskin, W.R., McCaffrey, W.F., and Walti, C.L., 1991, Geology and water resources of Owens Valley, California: U.S. Geological Survey Water Supply Paper 2370, 77 p. 2 plates n pocket. Supercedes Open-file report 88-715., https://doi.org/10.3133/wsp2370B.","productDescription":"77 p. 2 plates n pocket. Supercedes Open-file report 88-715.","numberOfPages":"77","costCenters":[],"links":[{"id":160629,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/2370b/report-thumb.jpg"},{"id":247342,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/2370b/plate-1.pdf","size":"3064","linkFileType":{"id":1,"text":"pdf"}},{"id":247343,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/2370b/plate-2.pdf","size":"3753","linkFileType":{"id":1,"text":"pdf"}},{"id":59626,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/2370b/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad6e4b07f02db684167","contributors":{"authors":[{"text":"Hollett, Kenneth J.","contributorId":40580,"corporation":false,"usgs":true,"family":"Hollett","given":"Kenneth","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":204818,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Danskin, Wesley R. 0000-0001-8672-5501 wdanskin@usgs.gov","orcid":"https://orcid.org/0000-0001-8672-5501","contributorId":1034,"corporation":false,"usgs":true,"family":"Danskin","given":"Wesley","email":"wdanskin@usgs.gov","middleInitial":"R.","affiliations":[{"id":154,"text":"California Water Science Center","active":true,"usgs":true}],"preferred":true,"id":204817,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"McCaffrey, William F.","contributorId":99155,"corporation":false,"usgs":true,"family":"McCaffrey","given":"William","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":204820,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Walti, Caryl L.","contributorId":64698,"corporation":false,"usgs":true,"family":"Walti","given":"Caryl","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":204819,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":25808,"text":"wri914084 - 1991 - U.S. Geological Survey research in radioactive waste disposal - Fiscal years 1986-1990","interactions":[{"subject":{"id":70194903,"text":"70194903 - 1991 - Beatty, Nevada: A section in U.S. Geological Survey research in radioactive waste disposal - Fiscal years 1986-1990 (WRI 91-4084)","indexId":"70194903","publicationYear":"1991","noYear":false,"displayTitle":"Beatty, Nevada: A section in <i>U.S. Geological Survey research in radioactive waste disposal - Fiscal years 1986-1990 (WRI 91-4084)</i>","title":"Beatty, Nevada: A section in U.S. Geological Survey research in radioactive waste disposal - Fiscal years 1986-1990 (WRI 91-4084)"},"predicate":"IS_PART_OF","object":{"id":25808,"text":"wri914084 - 1991 - U.S. Geological Survey research in radioactive waste disposal - Fiscal years 1986-1990","indexId":"wri914084","publicationYear":"1991","noYear":false,"title":"U.S. Geological Survey research in radioactive waste disposal - Fiscal years 1986-1990"},"id":1}],"lastModifiedDate":"2018-01-27T11:58:12","indexId":"wri914084","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1991","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":"91-4084","title":"U.S. Geological Survey research in radioactive waste disposal - Fiscal years 1986-1990","docAbstract":"<p>The report summarizes progress on geologic and hydrologic research related to the disposal of radioactive wastes. The research efforts are categorized according to whether they are related most directly to: (1) high-level wastes, (2) transuranic wastes, (3) low-level and mixed low-level and hazardous wastes, or (4) uranium mill tailings. Included is research applicable to the identification and geohydrologic characterization of waste-disposal sites, to investigations of specific sites where wastes have been stored, to development of techniques and methods for characterizing disposal sites, and to studies of geologic and hydrologic processes related to the transport and/or retention of waste radionuclides.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wri914084","collaboration":"A summary of work done in part in cooperation with the U.S. Department of Energy","usgsCitation":"1991, U.S. Geological Survey research in radioactive waste disposal - Fiscal years 1986-1990: U.S. Geological Survey Water-Resources Investigations Report 91-4084, vi, 90 p., https://doi.org/10.3133/wri914084.","productDescription":"vi, 90 p.","costCenters":[],"links":[{"id":158408,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1991/4084/report-thumb.jpg"},{"id":54559,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1991/4084/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a29e4b07f02db6119e5","contributors":{"compilers":[{"text":"Trask, N.J.","contributorId":31729,"corporation":false,"usgs":true,"family":"Trask","given":"N.J.","email":"","affiliations":[],"preferred":false,"id":726053,"contributorType":{"id":3,"text":"Compilers"},"rank":1},{"text":"Stevens, P. R.","contributorId":90289,"corporation":false,"usgs":true,"family":"Stevens","given":"P.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":726054,"contributorType":{"id":3,"text":"Compilers"},"rank":2}]}}
,{"id":29779,"text":"wri904076 - 1991 - Hydrogeology and ground-water flow in the carbonate rocks of the Little Lehigh Creek basin, Lehigh County, Pennsylvania","interactions":[],"lastModifiedDate":"2017-06-12T13:29:40","indexId":"wri904076","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1991","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":"90-4076","title":"Hydrogeology and ground-water flow in the carbonate rocks of the Little Lehigh Creek basin, Lehigh County, Pennsylvania","docAbstract":"<p>The Little Lehigh Creek basin is underlain mainly by a complex assemblage of highly-deformed Cambrian and Ordovician carbonate rocks. The Leithsville Formation, Allentown Dolomite, Beekmantown Group, and Jacksonburg Limestone act as a single hydrologic unit. Ground water moves through fractures and other secondary openings and generally is under water-table conditions. Median annual ground-water discharge (base flow) to Little Lehigh Creek near Allentown (station 01451500) during 1946-86 was 12.97 inches or 82 percent of streamflow. Average annual recharge for 1975-83 was 21.75 inches. Groundwater and surface-water divides do not coincide in the basin. Ground-water underflow from the Little Lehigh Creek basin to the Cedar Creek basin in 1987 was 4 inches per year. A double-mass curve analysis of the relation of cumulative precipitation at Allentown to the flow of Schantz Spring for 1956-84 showed that cessation of quarry pumping and development of ground water for public supply in the Schantz Spring basin did not affect the flow of Schantz Spring. Ground-water flow in the Little Lehigh Creek basin was simulated using a finite-difference, two-dimensional computer model. The geologic units in the modeled area were simulated as a single water-table aquifer. The 134-squaremile area of carbonate rocks between the Lehigh River and Sacony Creek was modeled to include the natural hydrologic boundaries of the ground-water-flow system. The ground-water-flow model was calibrated under steady-state conditions using 1975-83 average recharge, evapotranspiration, and pumping rates. Each geologic unit was assigned a different hydraulic conductivity. Initial aquifer hydraulic conductivity was estimated from specific-capacity data. The average (1975-83) water budget for the Little Lehigh Creek basin was simulated. The simulated base flow from the carbonate rocks of the Little Lehigh Creek basin above gaging station 01451500 is 11.85 inches per year. The simulated ground-water underflow from the Little Lehigh Creek basin to the Cedar Creek basin is 4.04 inches per year. For steady-state calibration, the root-mean-squared difference between observed and simulated heads was 21.19 feet. The effects of increased ground-water development on base flow and underflow out of the Little Lehigh Creek basin for average and drought conditions were simulated by locating a hypothetical well field in different parts of the basin. Steady-state simulations were used to represent equilibrium conditions, which would be the maximum expected long-term effect. Increased ground-water development was simulated as hypothetical well fields pumping at the rate of 15, 25, and 45 million gallons per day in addition to existing ground-water withdrawals. Four hypothetical well fields were located near and away from Little Lehigh Creek in upstream and downstream areas. The effects of pumping a well field in different parts of the Little Lehigh Creek basin were compared. Pumping a well field located near the headwaters of Little Lehigh Creek and away from the stream would have greatest effect on inducing underflow from the Sacony Greek basin and the least effect on reducing base flow and underflow to the Ceda^r Creek basin. Pumping a well field located near the headwaters of Little Leh|igh Creek near the stream would have less impact on inducing underflow from|the Sacony Creek basin and a greater impact on reducing the base flow of Little Lehigh Creek because more of the pumpage would come from diverted base flow. Pumping a well field located in the downstream area of the Little Lehigh Creek basin away from the stream would have the greatest effect on the underflow to the Cedar Creek basin. Pumping a well field located in the downstream area of the Little Lehigh Creek basin near the stream would have the greatest effect on reducing the base flow of Little Lehigh Cteek. Model simulations show that groundwater withdrawals do not cause a proportional reduction in base flow. Under average conditions, ground-water withdrawals are equal to 48 to 70 percent of simulated base-flow reductions; under drought conditions, ground-water withdrawals are equal to 35 to 73 percent of simulated base-flow reductions. The hydraulic effects of pumping largely depend on well location. In the Little Lehigh basin, surface-water and ground-water divides do not coincide, and ground-water development, especially near surface-water divides, can cause ground-water divides to shift and induce ground-water underflow from adjacent basins. Large-scale ground-water pumping in a basin may not produce expected reductions of base flow in that basin because of shifts in the ground-water divide; however, such shifts can reduce base flow in adjacent surface-water basins.&nbsp;</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri904076","usgsCitation":"Sloto, R., Cecil, L., and Senior, L., 1991, Hydrogeology and ground-water flow in the carbonate rocks of the Little Lehigh Creek basin, Lehigh County, Pennsylvania: U.S. Geological Survey Water-Resources Investigations Report 90-4076, viii, 84 p. :ill., maps ;28 cm. [PGS 83 p.], https://doi.org/10.3133/wri904076.","productDescription":"viii, 84 p. :ill., maps ;28 cm. [PGS 83 p.]","costCenters":[{"id":532,"text":"Pennsylvania Water Science Center","active":true,"usgs":true}],"links":[{"id":119627,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1990/4076/report-thumb.jpg"},{"id":58581,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1990/4076/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":58582,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1990/4076/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a4be4b07f02db625696","contributors":{"authors":[{"text":"Sloto, R. A.","contributorId":36155,"corporation":false,"usgs":true,"family":"Sloto","given":"R. A.","affiliations":[],"preferred":false,"id":202110,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Cecil, L.D.","contributorId":62616,"corporation":false,"usgs":true,"family":"Cecil","given":"L.D.","email":"","affiliations":[],"preferred":false,"id":202111,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Senior, L.A.","contributorId":32958,"corporation":false,"usgs":true,"family":"Senior","given":"L.A.","email":"","affiliations":[],"preferred":false,"id":202109,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":29647,"text":"wri904109 - 1991 - Geologic setting and water quality of selected basins in the active coal-mining areas of Ohio, 1987-88","interactions":[],"lastModifiedDate":"2012-02-02T00:08:54","indexId":"wri904109","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1991","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":"90-4109","title":"Geologic setting and water quality of selected basins in the active coal-mining areas of Ohio, 1987-88","docAbstract":"This report presents hydrologic data from selected drainage basins in the active coal-mining areas of Ohio from July 1987 through October 1988. The study area is mostly within the unglaciated part of eastern Ohio along the western edge of the Appalachian Plateaus physiographic province. The 1987-88 work is the second phase of a 7-year study to assess baseline water quality in Ohio's coal region.\r\n\r\nThe data collection network consisted of 41 long-term surface-water sites in 21 basins. The sites were measured and sampled twice yearly at low flow. In addition, six individual basins (three each year) selected for a more detailed representation of surface-water and ground-water quality. In 1987, the Sandy Creek, Middle Tuscarawas River and Sugar Creek, and Lower Tuscarawas River basins were chosen. In 1988, the Short and Wheeling Creeks, Upper Wills Creek, and Upper Raccoon Creek basins were chosen.\r\n\r\nBecause of their proximity to the glaciated region and outwash drainage, the basins studied intensively in 1987 contain more shallow productive aquifers than do the basins studied in detail for 1988, in which shallow ground-water sources are very localized.\r\n\r\nChemical analyses for 202 surface-water and 24 ground-water samples are presented. For field measurements made at surface-water sites, the specific conductance ranged from 295 to 3150 ? S/cm (microsiemens per centimeter at 25 degrees Celsius). For pH, the range was 2.8 to 8.6. Alkalinity ranged from 5 to 305 mg/L (milligrams per liter) as CaCO3.","language":"ENGLISH","publisher":"U.S. Geological Survey ;\r\nBooks and Open-File Reports Section [distributor],","doi":"10.3133/wri904109","usgsCitation":"Sedam, A., 1991, Geologic setting and water quality of selected basins in the active coal-mining areas of Ohio, 1987-88: U.S. Geological Survey Water-Resources Investigations Report 90-4109, vii, 97 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri904109.","productDescription":"vii, 97 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":124829,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1990/4109/report-thumb.jpg"},{"id":58465,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1990/4109/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b00e4b07f02db698041","contributors":{"authors":[{"text":"Sedam, A. C.","contributorId":32530,"corporation":false,"usgs":true,"family":"Sedam","given":"A. C.","affiliations":[],"preferred":false,"id":201882,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":30310,"text":"wri914091 - 1991 - Plan to evaluate the effects of hydrogeologic conditions and human activities on water quality in the coastal plain of New York and New Jersey","interactions":[],"lastModifiedDate":"2020-01-02T19:43:42","indexId":"wri914091","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1991","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":"91-4091","title":"Plan to evaluate the effects of hydrogeologic conditions and human activities on water quality in the coastal plain of New York and New Jersey","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri914091","usgsCitation":"Vowinkel, E., and Siwiec, S.F., 1991, Plan to evaluate the effects of hydrogeologic conditions and human activities on water quality in the coastal plain of New York and New Jersey: U.S. Geological Survey Water-Resources Investigations Report 91-4091, v, 42 p. , https://doi.org/10.3133/wri914091.","productDescription":"v, 42 p. ","costCenters":[{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":119474,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1991/4091/report-thumb.jpg"},{"id":59102,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1991/4091/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"New York, New 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