{"pageNumber":"4097","pageRowStart":"102400","pageSize":"25","recordCount":184934,"records":[{"id":27796,"text":"wri914076 - 1993 - Hydrology, water quality, trophic status, and aquatic plants of Fowler Lake, Wisconsin","interactions":[],"lastModifiedDate":"2015-10-26T14:41:49","indexId":"wri914076","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1993","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":"91-4076","title":"Hydrology, water quality, trophic status, and aquatic plants of Fowler Lake, Wisconsin","docAbstract":"<p>The U.S. Geological Survey, in cooperation with the Fowler Lake Management District, completed a hydrologic and water-quality study of Fowler Lake in southeastern Wisconsin during calendar year 1984. Data on temperature, pH, specific conductance, and concentrations of dissolved oxygen, total phosphorus, dissolved orthophosphate phosphorus, and various nitrogen species were collected from January through November 1984. The water-quality data indicate that Fowler Lake can be classified as a mildly fertile lake with excellent water clarity as indicated by Secchi depth readings generally greater than 12 feet. Although phosphorus concentrations are generally less than 0.01 milligram per liter, the lake does produce dense stands of macrophytes during the open-water period. The lake is thermally stratified during the summer months, resulting in oxygen depletion in the deepest parts of the lake.</p>\n<p>The average hydraulic residence time for Fowler Lake during 1984 was 6.9 days, which is substantially less than the 305 days for upstream Okauchee Lake or the 145 days for downstream Lac La Belle. Precipitation during 1984 was about 27 percent higher than normal and streamflows in the area were about 55 percent higher than normal. The Oconomowoc River contributed 98 percent of the inflow and 88 percent of the phosphorus load to Fowler Lake.</p>\n<p>The low annual phosphorus input (28 pounds per square mile) to the lake from the Oconomowoc River shows the benefit of upstream lakes on the Oconomowoc River. Fourteen percent of the phosphorus input load to Fowler Lake is deposited in the lake sediments and the rest is transported through the lake by surface-water flow to downstream Lac La Belle. Dense growths of macrophytes in the lake change in composition seasonally; chara sp. (muskgrass) and Myriophyllum sp. (milfoil) are abundant in June and Najas marina and Vallesneria Americana (wild celery) are abundant in August.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri914076","collaboration":"Prepared in cooperation with the Fowler Lake Management District","usgsCitation":"Hughes, P., 1993, Hydrology, water quality, trophic status, and aquatic plants of Fowler Lake, Wisconsin: U.S. Geological Survey Water-Resources Investigations Report 91-4076, v, 44 p., https://doi.org/10.3133/wri914076.","productDescription":"v, 44 p.","numberOfPages":"47","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":677,"text":"Wisconsin Water Science Center","active":true,"usgs":true}],"links":[{"id":120157,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1991/4076/report-thumb.jpg"},{"id":56633,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1991/4076/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Wisconsin","county":"Waukesha County","city":"Oconomowoc","otherGeospatial":"Fowler Lake","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -88.50156784057617,\n              43.10023083967166\n            ],\n            [\n              -88.50156784057617,\n              43.138322400420535\n            ],\n            [\n              -88.44148635864256,\n              43.138322400420535\n            ],\n            [\n              -88.44148635864256,\n              43.10023083967166\n            ],\n            [\n              -88.50156784057617,\n              43.10023083967166\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0ce4b07f02db5fc6df","contributors":{"authors":[{"text":"Hughes, P.E.","contributorId":104083,"corporation":false,"usgs":true,"family":"Hughes","given":"P.E.","email":"","affiliations":[],"preferred":false,"id":198698,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":33150,"text":"b2039 - 1993 - Advances related to United States and international mineral resources; developing frameworks and exploration technologies","interactions":[],"lastModifiedDate":"2025-01-24T20:44:19.510156","indexId":"b2039","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1993","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":306,"text":"Bulletin","code":"B","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"2039","title":"Advances related to United States and international mineral resources; developing frameworks and exploration technologies","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/b2039","usgsCitation":"Detra, P.S., and Berger, B.R., 1993, Advances related to United States and international mineral resources; developing frameworks and exploration technologies: U.S. Geological Survey Bulletin 2039, iv, 277 p., https://doi.org/10.3133/b2039.","productDescription":"iv, 277 p.","costCenters":[],"links":[{"id":60966,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/2039/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":60967,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/bul/2039/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":163396,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/bul/2039/report-thumb.jpg"},{"id":401832,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_22292.htm","text":"Basement structure in the Railroad Valley - Grant Range region, east-central Nevada, from interpretation of potential field anomalies"},{"id":481178,"rank":5,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_22293.htm","text":"Structure and origin of the Ely copper deposit, east-central Vermont","linkFileType":{"id":5,"text":"html"}},{"id":481179,"rank":6,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_22294.htm","text":"40Ar/39Ar studies of fluid inclusions in vein quartz from Battle Mountain, Nevada","linkFileType":{"id":5,"text":"html"}},{"id":481180,"rank":7,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_22295.htm","text":"The effects of hydrothermally altered bedrock on natural forest vegetation in the Snow Camp - Saxapahaw area, North Carolina, and the resulting expressions in Landsat TM imaging","linkFileType":{"id":5,"text":"html"}},{"id":481181,"rank":8,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_22296.htm","text":"Aeromagnetic survey of north-central Minnesota","linkFileType":{"id":5,"text":"html"}},{"id":481182,"rank":9,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_22297.htm","text":"Locating buried conductive material along the Getchell trend, Osgood Mountains, Nevada: implications for gold exploration and the carbon-gold association (?)","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b04e4b07f02db699179","contributors":{"editors":[{"text":"Scott, Richard W. Jr.","contributorId":20797,"corporation":false,"usgs":true,"family":"Scott","given":"Richard","suffix":"Jr.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":749521,"contributorType":{"id":2,"text":"Editors"},"rank":1}],"authors":[{"text":"Detra, Pamela S.","contributorId":9313,"corporation":false,"usgs":true,"family":"Detra","given":"Pamela","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":210066,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Berger, Byron R. bberger@usgs.gov","contributorId":1490,"corporation":false,"usgs":true,"family":"Berger","given":"Byron","email":"bberger@usgs.gov","middleInitial":"R.","affiliations":[{"id":211,"text":"Crustal Geophysics and Geochemistry Science Center","active":true,"usgs":true}],"preferred":true,"id":210065,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":25900,"text":"wri924108 - 1993 - Preliminary results of the simulation of Oregon coastal basins using precipitation-runoff modeling system (PRMS)","interactions":[],"lastModifiedDate":"2022-10-13T19:06:30.133491","indexId":"wri924108","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1993","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":"92-4108","title":"Preliminary results of the simulation of Oregon coastal basins using precipitation-runoff modeling system (PRMS)","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri924108","usgsCitation":"Allen, R.L., and Laenen, A., 1993, Preliminary results of the simulation of Oregon coastal basins using precipitation-runoff modeling system (PRMS): U.S. Geological Survey Water-Resources Investigations Report 92-4108, vi, 97 p., https://doi.org/10.3133/wri924108.","productDescription":"vi, 97 p.","costCenters":[{"id":518,"text":"Oregon Water Science Center","active":true,"usgs":true}],"links":[{"id":408271,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_47671.htm","linkFileType":{"id":5,"text":"html"}},{"id":158148,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1992/4108/report-thumb.jpg"},{"id":54659,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1992/4108/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Oregon","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -123.8872,\n              44.5083\n            ],\n            [\n              -123.8333,\n              44.5083\n            ],\n            [\n              -123.8333,\n              44.5583\n            ],\n            [\n              -123.8872,\n              44.5583\n            ],\n            [\n              -123.8872,\n              44.5083\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aade4b07f02db66b2c6","contributors":{"authors":[{"text":"Allen, R. L.","contributorId":82356,"corporation":false,"usgs":true,"family":"Allen","given":"R.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":195444,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Laenen, Antonius","contributorId":107673,"corporation":false,"usgs":true,"family":"Laenen","given":"Antonius","email":"","affiliations":[],"preferred":false,"id":195445,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":25573,"text":"wri934114 - 1993 - Hydrogeology and land subsidence, Edwards Air Force Base, Antelope Valley, California, January 1989-December 1991","interactions":[],"lastModifiedDate":"2023-03-14T18:18:38.798728","indexId":"wri934114","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1993","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":"93-4114","title":"Hydrogeology and land subsidence, Edwards Air Force Base, Antelope Valley, California, January 1989-December 1991","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri934114","usgsCitation":"Londquist, C., Rewis, D., Galloway, D., and McCaffrey, W.F., 1993, Hydrogeology and land subsidence, Edwards Air Force Base, Antelope Valley, California, January 1989-December 1991: U.S. Geological Survey Water-Resources Investigations Report 93-4114, vi, 74 p., https://doi.org/10.3133/wri934114.","productDescription":"vi, 74 p.","costCenters":[{"id":35860,"text":"Ohio-Kentucky-Indiana Water Science Center","active":true,"usgs":true}],"links":[{"id":54292,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1993/4114/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":121657,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1993/4114/report-thumb.jpg"},{"id":414111,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_47828.htm","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"California","otherGeospatial":"Edwards Air Force Base","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -117.975,\n              34.8083\n            ],\n            [\n              -117.8833,\n              34.8083\n            ],\n            [\n              -117.8833,\n              34.8936\n            ],\n            [\n              -117.975,\n              34.8936\n            ],\n            [\n              -117.975,\n              34.8083\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a4be4b07f02db62558a","contributors":{"authors":[{"text":"Londquist, C.J.","contributorId":86796,"corporation":false,"usgs":true,"family":"Londquist","given":"C.J.","affiliations":[],"preferred":false,"id":194249,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Rewis, D. L.","contributorId":81514,"corporation":false,"usgs":true,"family":"Rewis","given":"D. L.","affiliations":[],"preferred":false,"id":194248,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Galloway, D. L. 0000-0003-0904-5355","orcid":"https://orcid.org/0000-0003-0904-5355","contributorId":31383,"corporation":false,"usgs":true,"family":"Galloway","given":"D. L.","affiliations":[{"id":35860,"text":"Ohio-Kentucky-Indiana Water Science Center","active":true,"usgs":true}],"preferred":false,"id":194247,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"McCaffrey, W. F.","contributorId":18001,"corporation":false,"usgs":true,"family":"McCaffrey","given":"W.","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":194246,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":61094,"text":"mf2221 - 1993 - Bathymetry, sidescan sonar image, and surficial geological interpretation of the inner shelf off Little Egg Inlet, New Jersey","interactions":[],"lastModifiedDate":"2012-02-10T00:10:48","indexId":"mf2221","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1993","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":325,"text":"Miscellaneous Field Studies Map","code":"MF","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"2221","title":"Bathymetry, sidescan sonar image, and surficial geological interpretation of the inner shelf off Little Egg Inlet, New Jersey","language":"ENGLISH","doi":"10.3133/mf2221","usgsCitation":"Twichell, D., and Able, K., 1993, Bathymetry, sidescan sonar image, and surficial geological interpretation of the inner shelf off Little Egg Inlet, New Jersey: U.S. Geological Survey Miscellaneous Field Studies Map 2221, 3 maps and 1 photomap ;each 48 x 50 cm., on sheets 126 x 86 cm. and 66 x 112 cm., folded in envelope 30 x 24 cm., https://doi.org/10.3133/mf2221.","productDescription":"3 maps and 1 photomap ;each 48 x 50 cm., on sheets 126 x 86 cm. and 66 x 112 cm., folded in envelope 30 x 24 cm.","costCenters":[],"links":[{"id":105311,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_5856.htm","linkFileType":{"id":5,"text":"html"},"description":"5856"},{"id":186772,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"scale":"0","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -74.28333333333333,39.45 ], [ -74.28333333333333,39.5 ], [ -74.21666666666667,39.5 ], [ -74.21666666666667,39.45 ], [ -74.28333333333333,39.45 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a6ce4b07f02db63e17a","contributors":{"authors":[{"text":"Twichell, D.C.","contributorId":84304,"corporation":false,"usgs":true,"family":"Twichell","given":"D.C.","affiliations":[],"preferred":false,"id":264975,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Able, K.W.","contributorId":66786,"corporation":false,"usgs":true,"family":"Able","given":"K.W.","email":"","affiliations":[],"preferred":false,"id":264974,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":21087,"text":"ofr9382 - 1993 - Ground Water in Kilauea Volcano and Adjacent Areas of Mauna Loa Volcano, Island of Hawaii","interactions":[],"lastModifiedDate":"2012-03-08T17:16:14","indexId":"ofr9382","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1993","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":"93-82","title":"Ground Water in Kilauea Volcano and Adjacent Areas of Mauna Loa Volcano, Island of Hawaii","docAbstract":"About 1,000 million gallons of water per day moves toward or into ground-water bodies of Kilauea Volcano from the lavas of Mauna Loa Volcano. This movement continues only to the northern boundaries of the east and southwest rift zones of Kilauea, where a substantial quantity of ground water is deflected downslope to other ground-water bodies or to the ocean. In the western part of Kilauea, the kaoiki fault system, which parallels the southwest rift zone, may be the main barrier to ground-water movement. The diversion of the ground water is manifested in the western part of Kilauea by the presence of large springs at the shore end of the Kaoiki fault system, and in the eastern part by the apparently large flow of unheated basal ground water north of the east rift zone. Thus, recharge to ground water in the rift zones of Kilauea and to the areas to the south of the rift zones may be largely by local rainfall. Recharge from rainfall for all of Kilauea is about 1,250 million gallons per day.\r\n\r\nBeneath the upper slopes of the Kilauea rift zones, ground-water levels are 2,000 feet or more above mean sea level, or more than 1,000 feet below land surface. Ground-water levels are at these high altitudes because numerous and closely spaced dikes at depth in the upper slopes impound the ground water. In the lower slopes, because the number of dikes decreases toward the surface, the presence of a sufficient number of dikes capable of impounding ground water at altitudes substantially above sea level is unlikely. In surrounding basal ground-water reservoirs, fresh basal ground water floats on seawater and, through a transition zone of mixed freshwater and seawater, discharges into the sea.\r\n\r\nThe hydraulic conductivity of the dike-free lavas ranges from about 3,000 to about 7,000 feet per day. The conductivity in the upper slopes of the rift ranges from about 5 to 30 feet per day and that of the lower slopes of the east rift zone was calculated at about 7,000 feet per day.\r\n\r\nThe occurrence of heated basal water south of the lower east rift zone of Kilauea indicates the movement of a large quantity of geothermally heated ground water southward from the rift zone. There is little indication of similar movement of water from the upper slopes of the east rift zone, and there is no obvious movement of heated water from the lower east rift to the north because of the absence of heated ground water north of the rift zone.\r\n\r\nA broad range in temperature and chemical composition of geothermally modified ground water indicates several different sources. Four possible sources are (1) cold meteoric water, (2) cold seawater, (3) hydrothermal fluids of meteoric origin, and (4) hydrothermally modified seawater. The chloride-ion to magnesium-ion ratio of ground water indicates whether the water has been geothermally modified. A ratio greater than 15 to 1 generally denotes geothermally modified ground water.","language":"ENGLISH","publisher":"Geological Survey (U.S.)","doi":"10.3133/ofr9382","usgsCitation":"Takasaki, K.J., 1993, Ground Water in Kilauea Volcano and Adjacent Areas of Mauna Loa Volcano, Island of Hawaii: U.S. Geological Survey Open-File Report 93-82, iv, 28 p., https://doi.org/10.3133/ofr9382.","productDescription":"iv, 28 p.","costCenters":[{"id":525,"text":"Pacific Islands Water Science Center","active":true,"usgs":true}],"links":[{"id":154704,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1993/0082/report-thumb.jpg"},{"id":50680,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1993/0082/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e48cee4b07f02db545623","contributors":{"authors":[{"text":"Takasaki, Kiyoshi J.","contributorId":105700,"corporation":false,"usgs":true,"family":"Takasaki","given":"Kiyoshi","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":183817,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":25924,"text":"wri934074 - 1993 - Effects of agricultural and residential land use on ground-water quality, Anoka Sand Plain Aquifer, east-central Minnesota","interactions":[],"lastModifiedDate":"2018-03-05T10:15:09","indexId":"wri934074","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1993","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":"93-4074","title":"Effects of agricultural and residential land use on ground-water quality, Anoka Sand Plain Aquifer, east-central Minnesota","docAbstract":"<p>Water quality in the 1,700-square-mile Anoka Sand Plain aquifer is affected by irrigated and nonirrigated agriculture and by residential land use. Concentrations of sulfate, chloride, nitrite plus nitrate nitrogen, and pesticides in ground water are related to human activities; nitrite plus nitrate nitrogen concentrations are affected more than concentrations of other chemical constituents. Of the water samples collected from 100 wells during this study, samples from 30 wells had concentrations of nitrite plus nitrate nitrogen greater than 10 mg/L (milligrams per liter), which is the limit recommended for drinking water by the Minnesota Pollution Control Agency. Analysis of 360 water samples indicated that the median concentrations of nitrite plus nitrate nitrogen for undeveloped, nonirrigated-cultivated, irrigated, and residential lands were 0.22,2.0,5.3, and 4.2 mg/L, respectively.</p>\n<p>Differences in nitrite plus nitrate nitrogen concentrations at various depths below the water table were statistically significant. Median concentrations of nitrite plus nitrate nitrogen in groundwater samples less than 10 feet, 10 to 20 feet, and more than 20 feet below the water table were 5.1 mg/L, 2.7 mg/L, and less than 0.1 mg/L, respectively.</p>\n<p>Seasonal fluctuations in nitrite plus nitrate nitrogen concentrations at many wells were as great or greater than long-term change; however, the springtime median concentration of nitrite plus nitrate nitrogen increased steadily from 1984 (4.8 mg/L) through 1987 (5.5 mg/L).</p>\n<p>Triazine herbicides were detected in 11 of 18 samples analyzed for pesticides. Concentrations of atrazine were less than the 3 (J-g/L maximum contaminant level set for atrazine by the Minnesota Department of Health and by the U.S. Environmental Protection Agency.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Mounds View, MN","doi":"10.3133/wri934074","collaboration":"Prepared In cooperation with the Minnesota Department of Natural Resources, Division of Waters and the Soil and Water Conservation Districts of Anoka, Chisago, Isanti, Sherburne, and Stearns Counties","usgsCitation":"Anderson, H.W., 1993, Effects of agricultural and residential land use on ground-water quality, Anoka Sand Plain Aquifer, east-central Minnesota: U.S. Geological Survey Water-Resources Investigations Report 93-4074, vi, 62 p., https://doi.org/10.3133/wri934074.","productDescription":"vi, 62 p.","numberOfPages":"68","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":392,"text":"Minnesota Water Science 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,{"id":17423,"text":"ofr93128 - 1993 - National Research Program of the Water Resources Division, U. S. Geological Survey, Fiscal Year 1992","interactions":[],"lastModifiedDate":"2017-12-06T12:36:38","indexId":"ofr93128","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1993","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":"93-128","title":"National Research Program of the Water Resources Division, U. S. Geological Survey, Fiscal Year 1992","docAbstract":"<p>This report, one in a series of annual reports, provides current information about the National Research Program (NRP) of the U.S. Geological Survey's Water Resources Division (WRD) during fiscal year 1992. Organized by NRP's six research disciplines, the volume contains a summary of the problem, objective, approach, and progress for each project that was active during fiscal year 1992. It also contains bibliographic information that, because of the long-term nature of the program, covers a 5-year period. The bibliographic information does not include abstracts or informal reports. Rather it contains those reports that are readily available in the form of journal articles, U.S. Geological Survey (USGS) publications, book chapters, or books.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr93128","usgsCitation":"1993, National Research Program of the Water Resources Division, U. S. Geological Survey, Fiscal Year 1992: U.S. Geological Survey Open-File Report 93-128, viii, 392 p., https://doi.org/10.3133/ofr93128.","productDescription":"viii, 392 p.","costCenters":[],"links":[{"id":349764,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1993/0128/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":150617,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1993/0128/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b01e4b07f02db69875d","contributors":{"compilers":[{"text":"Nichols, Martha L.","contributorId":55457,"corporation":false,"usgs":true,"family":"Nichols","given":"Martha L.","affiliations":[],"preferred":false,"id":724184,"contributorType":{"id":3,"text":"Compilers"},"rank":1},{"text":"Friedman, Linda C.","contributorId":98702,"corporation":false,"usgs":true,"family":"Friedman","given":"Linda C.","affiliations":[],"preferred":false,"id":724185,"contributorType":{"id":3,"text":"Compilers"},"rank":2}]}}
,{"id":25136,"text":"cir930N - 1993 - International strategic minerals inventory summary report; rare-earth oxides","interactions":[],"lastModifiedDate":"2012-02-02T00:08:12","indexId":"cir930N","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1993","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":307,"text":"Circular","code":"CIR","onlineIssn":"2330-5703","printIssn":"1067-084X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"930","chapter":"N","title":"International strategic minerals inventory summary report; rare-earth oxides","docAbstract":"Bastnaesite, monazite, and xenotime are currently the most important rare-earth minerals. Bastnaesite occurs as a primary mineral in carbonatites. Monazite and xenotime also can be found in primary deposits but are recovered principally from heavy-mineral placers that are mined for titanium or tin. Each of these minerals has a different composition of the 15 rare-earth elements. \r\n\r\nWorld resources of economically exploitable rare-earth oxides (REO) are estimated at 93.4 million metric tons in place, composed of 93 percent in primary deposits and 7 percent in placers. The average mineral composition is 83 percent bastnaesite, 13 percent monazite, and 4 percent of 10 other minerals. Annual global production is about 67,000 metric tons of which 41 percent is from placers and 59 percent is from primary deposits; mining methods consist of open pits (94 percent) and dredging (6 percent). This output could be doubled if the operations that do not currently recover rare earths would do so. \r\n\r\nResources are more than sufficient to meet the demand for the predictable future. About 52 percent of the world's REO resources are located in China. Ranking of other countries is as follows: Namibia (22 percent), the United States (15 percent), Australia (6 percent), and India (3 percent); the remainder is in several other countries. Conversely, 38 percent of the production is in China, 33 percent in the United States, 12 percent in Australia, and 5 percent each in Malaysia and India. Several other countries, including Brazil, Canada, South Africa, Sri Lanka, and Thailand, make up the remainder. Markets for rare earths are mainly in the metallurgical, magnet, ceramic, electronic, chemical, and optical industries. Rare earths improve the physical and rolling properties of iron and steel and add corrosion resistance and strength to structural members at high temperatures. Samarium and neodymium are used in lightweight, powerful magnets for electric motors. Cerium and yttrium increase the density and heat resistance of sintered ceramics. Yttrium and gadolinium contribute to the efficiency of electronic switches and sensors. Cerium improves the effectiveness of catalysts in the petroleum and automotive industries. Cerium oxides speed glass melting and are used to polish glass by chemical, rather than mechanical, means. Cerium, europium, terbium, and yttrium, as phosphoric compounds, promote the vivid colors of television screens. Consumption of rare earths is expected to grow by about 2.6 percent per year.","language":"ENGLISH","publisher":"U.S. Dept. of the Interior, Geological Survey,","doi":"10.3133/cir930N","usgsCitation":"Jackson, W., and Christiansen, G., 1993, International strategic minerals inventory summary report; rare-earth oxides: U.S. Geological Survey Circular 930, v. :ill. ;26 cm.; 68 p., https://doi.org/10.3133/cir930N.","productDescription":"v. :ill. ;26 cm.; 68 p.","costCenters":[],"links":[{"id":124682,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/circ/1993/0930n/report-thumb.jpg"},{"id":54116,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/1993/0930n/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4887e4b07f02db519db9","contributors":{"authors":[{"text":"Jackson, W.D.","contributorId":45743,"corporation":false,"usgs":true,"family":"Jackson","given":"W.D.","email":"","affiliations":[],"preferred":false,"id":193287,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Christiansen, Grey","contributorId":14013,"corporation":false,"usgs":true,"family":"Christiansen","given":"Grey","email":"","affiliations":[],"preferred":false,"id":193286,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":25543,"text":"wri924184 - 1993 - Geophysical logging studies in the Snake River Plain Aquifer at the Idaho National Engineering Laboratory — Wells 44, 45, and 46","interactions":[],"lastModifiedDate":"2022-01-24T21:54:37.220993","indexId":"wri924184","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1993","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":"92-4184","title":"Geophysical logging studies in the Snake River Plain Aquifer at the Idaho National Engineering Laboratory — Wells 44, 45, and 46","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri924184","usgsCitation":"Morin, R.H., Barrash, W., Paillet, F.L., and Taylor, T., 1993, Geophysical logging studies in the Snake River Plain Aquifer at the Idaho National Engineering Laboratory — Wells 44, 45, and 46: U.S. Geological Survey Water-Resources Investigations Report 92-4184, v, 44 p., https://doi.org/10.3133/wri924184.","productDescription":"v, 44 p.","costCenters":[{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":394785,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_47726.htm"},{"id":54263,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1992/4184/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":118846,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1992/4184/report-thumb.jpg"}],"country":"United States","state":"Idaho","otherGeospatial":"Idaho National Engineering Laboratory","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -112.9583,\n              43.55\n            ],\n            [\n              -112.9167,\n              43.55\n            ],\n            [\n              -112.9167,\n              43.5833\n            ],\n            [\n              -112.9583,\n              43.5833\n            ],\n            [\n              -112.9583,\n              43.55\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac8e4b07f02db67bdab","contributors":{"authors":[{"text":"Morin, R. H.","contributorId":31794,"corporation":false,"usgs":true,"family":"Morin","given":"R.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":194124,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Barrash, Warren","contributorId":72829,"corporation":false,"usgs":true,"family":"Barrash","given":"Warren","affiliations":[],"preferred":false,"id":194127,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Paillet, Frederick L.","contributorId":63820,"corporation":false,"usgs":true,"family":"Paillet","given":"Frederick","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":194125,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Taylor, T. A.","contributorId":70014,"corporation":false,"usgs":true,"family":"Taylor","given":"T. A.","affiliations":[],"preferred":false,"id":194126,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":25620,"text":"wri934123 - 1993 - Laboratory procedures and data reduction techniques to determine rheologic properties of mass flows","interactions":[],"lastModifiedDate":"2012-02-02T00:08:21","indexId":"wri934123","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1993","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":"93-4123","title":"Laboratory procedures and data reduction techniques to determine rheologic properties of mass flows","docAbstract":"Determining the rheologic properties of coarse- grained mass flows is an important step to mathematically simulate potential inundation zones. Using the vertically rotating flume designed and built by the U.S. Geological Survey, laboratory procedures and subsequent data reduction have been developed to estimate shear stresses and strain rates of various flow materials. Although direct measurement of shear stress and strain rate currently (1992) are not possible in the vertically rotating flume, methods were derived to estimate these values from measurements of flow geometry, surface velocity, and flume velocity.","language":"ENGLISH","publisher":"U.S. Geological Survey ;\r\nEarth Science Information Center, Open-File Reports Section [distributor],","doi":"10.3133/wri934123","usgsCitation":"Holmes, R., Huizinga, R., Brown, S., and Jobson, H., 1993, Laboratory procedures and data reduction techniques to determine rheologic properties of mass flows: U.S. Geological Survey Water-Resources Investigations Report 93-4123, v, 17 p. :ill. ;28 cm., https://doi.org/10.3133/wri934123.","productDescription":"v, 17 p. :ill. ;28 cm.","costCenters":[],"links":[{"id":118968,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1993/4123/report-thumb.jpg"},{"id":54365,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1993/4123/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b32e4b07f02db6b4438","contributors":{"authors":[{"text":"Holmes, Robert R. Jr. 0000-0002-5060-3999","orcid":"https://orcid.org/0000-0002-5060-3999","contributorId":70429,"corporation":false,"usgs":true,"family":"Holmes","given":"Robert R.","suffix":"Jr.","affiliations":[],"preferred":false,"id":194438,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Huizinga, R.J.","contributorId":36970,"corporation":false,"usgs":true,"family":"Huizinga","given":"R.J.","affiliations":[],"preferred":false,"id":194436,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Brown, S.M.","contributorId":88776,"corporation":false,"usgs":true,"family":"Brown","given":"S.M.","email":"","affiliations":[],"preferred":false,"id":194439,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Jobson, H.E.","contributorId":44952,"corporation":false,"usgs":true,"family":"Jobson","given":"H.E.","affiliations":[],"preferred":false,"id":194437,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":54939,"text":"wdrPA911 - 1993 - Water resources data, Pennsylvania, water year 1991. Volume 1. Delaware River Basin","interactions":[],"lastModifiedDate":"2020-05-13T17:16:47.072539","indexId":"wdrPA911","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1993","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":"PA-91-1","title":"Water resources data, Pennsylvania, water year 1991. Volume 1. Delaware River Basin","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wdrPA911","usgsCitation":"Kolva, J., White, T., Druther, R., and Moleski, P., 1993, Water resources data, Pennsylvania, water year 1991. Volume 1. Delaware River Basin: U.S. Geological Survey Water Data Report PA-91-1, xi, 342 p., https://doi.org/10.3133/wdrPA911.","productDescription":"xi, 342 p.","costCenters":[],"links":[{"id":374785,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wdr/1991/pa-91-1/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":177552,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wdr/1991/pa-91-1/report-thumb.jpg"}],"country":"United States","state":"Pennsylvania ","otherGeospatial":"Delaware River Basin","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -75.772705078125,\n              39.76632525654491\n            ],\n            [\n              -75.4541015625,\n              39.93501296038254\n            ],\n            [\n              -75.65185546874999,\n              39.80853604144591\n            ],\n            [\n              -75.08056640625,\n              40.212440718286466\n            ],\n            [\n              -75.157470703125,\n              40.455307212131494\n            ],\n            [\n              -74.783935546875,\n              41.43449030894922\n            ],\n            [\n              -75.311279296875,\n              41.918628865183045\n            ],\n            [\n              -75.618896484375,\n              42.02481360781777\n            ],\n            [\n              -76.09130859375,\n              41.934976500546604\n            ],\n            [\n              -76.31103515625,\n              41.20345619205131\n            ],\n            [\n              -76.365966796875,\n              40.64730356252251\n            ],\n            [\n              -76.904296875,\n              40.052847601823984\n            ],\n            [\n              -76.80541992187499,\n              39.690280594818034\n            ],\n            [\n              -75.772705078125,\n              39.76632525654491\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a09e4b07f02db5fad77","contributors":{"authors":[{"text":"Kolva, J.R.","contributorId":64264,"corporation":false,"usgs":true,"family":"Kolva","given":"J.R.","email":"","affiliations":[],"preferred":false,"id":252088,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"White, T.E.","contributorId":89213,"corporation":false,"usgs":true,"family":"White","given":"T.E.","email":"","affiliations":[],"preferred":false,"id":252089,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Druther, R.L.","contributorId":94376,"corporation":false,"usgs":true,"family":"Druther","given":"R.L.","email":"","affiliations":[],"preferred":false,"id":252090,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Moleski, P.","contributorId":44983,"corporation":false,"usgs":true,"family":"Moleski","given":"P.","email":"","affiliations":[],"preferred":false,"id":252087,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":25608,"text":"wri934033 - 1993 - Hydrology, vegetation, and soils of four north Florida River flood plains with an evaluation of state and federal wetland determinations","interactions":[],"lastModifiedDate":"2012-02-02T00:08:24","indexId":"wri934033","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1993","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":"93-4033","title":"Hydrology, vegetation, and soils of four north Florida River flood plains with an evaluation of state and federal wetland determinations","docAbstract":"A study of hydrologic conditions, vegetation, and soils was made in wetland forests of four north Florida streams from 1987 to 1990. The study was conducted by the U.S. Geological Survey in cooperation with the Florida Department of Environmental Regulation to support State and Federal efforts to improve wetland delineation methodology in flood plains. \r\n\r\nPlant communities and soils were described and related to topographic position and long-term hydrologic conditions at 10 study plots located on 4 streams. Detailed appendixes give average duration, frequency, and depth of flooding; canopy, subcanopy, and ground-cover vegetation; and taxonomic classification, series, and profile descriptions of soils for each plot. Topographic relief, range in stage, and depth of flooding were greatest on the alluvial flood plain of the Ochlockonee River, the largest of the four streams. Soils were silty in the lower elevations of the flood plain, and tree communities were distinctly different in each topographic zone. The Aucilla River flood plain was dominated by levees and terraces with very few depressions or low backwater areas. Oaks dominated the canopy of both lower and upper terraces of the Aucilla flood plain. Telogia Creek is a blackwater stream that is a major tributary of the Ochlockonee River. Its low, wet flood plain was dominated by Wyssa ogeche (Ogeechee tupelo) trees, had soils with mucky horizons, and was inundated by frequent floods of very short duration. The St. Marks River, a spring-fed stream with high base flow, had the least topographic relief and lowest range in stage of the four streams. St. Marks soils had a higher clay content than the other streams, and limestone bedrock was relatively close to the surface. \r\n\r\nWetland determinations of the study plots based on State and Federal regulatory criteria were evaluated. Most State and Federal wetland determinations are based primarily on vegetation and soil characteristics because hydrologic records are usually not available. In this study, plots were located near long-term gaging stations, thus wetland determinations based on plant and soil characteristics could be evaluated at sites where long-term hydrologic conditions were known. Inconsistencies among hydrology, vegetation, and soil determinations were greatest on levee communities of the Ochlockonee and Aucilla River flood plains. Duration of average annual longest flood was almost 2 weeks for both plots. The wetland species list currently used (1991) by the State lacks many ground-cover species common to forested flood plains of north Florida rivers. There were 102 ground-cover species considered upland plants by the State that were present on the nine annually flooded plots of this study. Among them were 34 species that grew in areas continuously flooded for an average of 5 weeks or more each year. Common flood-plain species considered upland plants by the State were: Hypoxis leptocarpa (yellow star-grass), and two woody vines, Brunnichia ovata (ladies' eardrops) and Campsis radicans (trumpet-creeper), which were common in areas flooded continuously for 6 to 9 weeks a year; Sebastiania fruticosa (Sebastian-bush), Chasmanthium laxum (spikegrass), and Panicum dichotomum (panic grass), which typically grew in areas flooded an average of 2 to 3 weeks or more per year; Vitis rotundifolia (muscadine) and Toxicodendron radicans (poison-ivy), usually occurring in areas flooded an average of 1 to 2 weeks a year; and Quercus virginiana (live oak) present most often in areas flooded approximately 1 week a year. \r\n\r\nFederal wetland regulations (1989) limited wetland jurisdiction to only those areas that are inundated or saturated during the growing season. However, year-round hydrologic records were chosen in this report to describe the influence of hydrology on vegetation, because saturation, inundation, or flowing water can have a variety of both beneficial and adverse effects on flood-plain vegetation at any time of the ","language":"ENGLISH","publisher":"U.S. Dept. of the Interior, U.S. Geological Survey ;\r\nU.S.G.S. Earth Science Information Center, Open-File Reports Section [distributor],","doi":"10.3133/wri934033","usgsCitation":"Light, H., Darst, M.R., MacLaughlin, M., and Sprecher, S., 1993, Hydrology, vegetation, and soils of four north Florida River flood plains with an evaluation of state and federal wetland determinations: U.S. Geological Survey Water-Resources Investigations Report 93-4033, x, 94 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri934033.","productDescription":"x, 94 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":1933,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/wri934033","linkFileType":{"id":5,"text":"html"}},{"id":118762,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/wri_93_4033.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac9e4b07f02db67c954","contributors":{"authors":[{"text":"Light, H.M.","contributorId":43389,"corporation":false,"usgs":true,"family":"Light","given":"H.M.","email":"","affiliations":[],"preferred":false,"id":194391,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Darst, M. R.","contributorId":75187,"corporation":false,"usgs":true,"family":"Darst","given":"M.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":194392,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"MacLaughlin, M.T.","contributorId":17651,"corporation":false,"usgs":true,"family":"MacLaughlin","given":"M.T.","email":"","affiliations":[],"preferred":false,"id":194389,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Sprecher, S.W.","contributorId":19911,"corporation":false,"usgs":true,"family":"Sprecher","given":"S.W.","email":"","affiliations":[],"preferred":false,"id":194390,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":25605,"text":"wri934183 - 1993 - Hydrology of Park County, Wyoming, exclusive of Yellowstone National Park","interactions":[],"lastModifiedDate":"2012-02-02T00:08:24","indexId":"wri934183","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1993","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":"93-4183","title":"Hydrology of Park County, Wyoming, exclusive of Yellowstone National Park","docAbstract":"The climate of Park County, Wyoming, ranges from desert to alpine tundra. Average annual precipitation ranges from 6 to 40 inches. Ground water is present throughout most of the county, but supplies adequate for stock or domestic use are not readily available in areas of greatest need. The chemical quality of most of the water sampled was of suitable quality for livestock, but most of the water was not suitable for drinking, and the water from bedrock aquifers generally was not suitable for irrigation. Unconsolidated deposits are a principal source of ground water in the county. However, ground water is found in deposits topographically higher than stream level only where surface water has been applied for irrigation; those unconsolidated deposits beneath areas that are not irrigated, such as Polecat Bench, are dry. The conversion of irrigated land to urban development poses problems in some areas because yields of water-supply wells will be adversely affected by reduced recharge. The trend toward urban development also increases the risk of contamination of the ground water by septic tanks, petroleum products, and toxic and hazardous wastes. Perennial streams originate in the mountains and in areas where drainage from irrigated land is adequate to sustain flow. The average annual runoff from streams originating in the mountains is as large as 598 acre-feet per square mile, and the average annual runoff from streams originating in badlands and plains is as low as 14.8 acre-feet per square mile.","language":"ENGLISH","publisher":"U.S. Dept. of the Interior, U.S. Geological Survey ;\r\nEarth Science Information Center, Open-File Reports Section [distributor],","doi":"10.3133/wri934183","usgsCitation":"Lowry, M., Smalley, M., Mora, K.L., Stockdale, R., and Martin, M., 1993, Hydrology of Park County, Wyoming, exclusive of Yellowstone National Park: U.S. Geological Survey Water-Resources Investigations Report 93-4183, v, 67 p. :ill., maps (some col.) ;28 cm., https://doi.org/10.3133/wri934183.","productDescription":"v, 67 p. :ill., maps (some col.) ;28 cm.","costCenters":[],"links":[{"id":123948,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1993/4183/report-thumb.jpg"},{"id":54348,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1993/4183/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":54349,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1993/4183/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afbe4b07f02db696070","contributors":{"authors":[{"text":"Lowry, M.E.","contributorId":55807,"corporation":false,"usgs":true,"family":"Lowry","given":"M.E.","email":"","affiliations":[],"preferred":false,"id":194378,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Smalley, M.L.","contributorId":87585,"corporation":false,"usgs":true,"family":"Smalley","given":"M.L.","email":"","affiliations":[],"preferred":false,"id":194380,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Mora, K. L.","contributorId":55008,"corporation":false,"usgs":true,"family":"Mora","given":"K.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":194377,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Stockdale, R.G.","contributorId":24384,"corporation":false,"usgs":true,"family":"Stockdale","given":"R.G.","email":"","affiliations":[],"preferred":false,"id":194376,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Martin, M.W.","contributorId":76785,"corporation":false,"usgs":true,"family":"Martin","given":"M.W.","email":"","affiliations":[],"preferred":false,"id":194379,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":25135,"text":"cir930M - 1993 - International strategic minerals inventory summary report; niobium (columbium) and tantalum","interactions":[],"lastModifiedDate":"2012-02-02T00:08:12","indexId":"cir930M","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1993","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":307,"text":"Circular","code":"CIR","onlineIssn":"2330-5703","printIssn":"1067-084X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"930","chapter":"M","title":"International strategic minerals inventory summary report; niobium (columbium) and tantalum","docAbstract":"Major world resources of niobium and tantalum are described in this summary report of information in the International Strategic Minerals Inventory (ISMI). ISMI is a cooperative data-collection effort of earth-science and mineral-resource agencies in Australia, Canada, the Federal Republic of Germany, the Republic of South Africa, the United Kingdom, and the United States of America. Part I of this report presents an overview of the resources and potential supply of niobium and tantalum based on inventory information; Part II contains tables of both geologic and mineral-resource information and includes production data collected by ISMI participants. \r\n\r\nNiobium is used principally as an alloying element in special steels and superalloys, and tantalum is used mainly in electronics. Minerals in the columbite-tantalite series are principal ore minerals of niobium and tantalum. Pyrochlore is a principal source of niobium. These minerals are found in carbonatite, certain rocks in alkaline igneous complexes, pegmatite, and placer deposits. ISMI estimates show that there are over 7 million metric tons of niobium and almost 0.5 million metric tons of tantalum in known deposits, outside of China and the former Soviet Union, for which reliable estimates have been made. \r\n\r\nBrazilian deposits, followed by Canadian deposits, contain by far the largest source of niobium. Tantalum production is spread widely among several countries, and Brazil and Canada are the most significant of these producers. Brazil's position is further strengthened by potential byproduct columbite from tin mining. Present economically exploitable resources of niobium appear to be sufficient for the near future, but Brazil will continue to be the predominant world supplier of ferrocolumbium. Tantalum, a byproduct of tin production, has been captive to the fluctuations of that market, but resources in pegmatite in Canada and Australia make it likely that future increases in the present modest demand will be met.","language":"ENGLISH","publisher":"U.S. Dept. of the Interior, Geological Survey,","doi":"10.3133/cir930M","usgsCitation":"Crockett, R., and Sutphin, D.M., 1993, International strategic minerals inventory summary report; niobium (columbium) and tantalum: U.S. Geological Survey Circular 930, v. :ill. ;26 cm.; 36 p., https://doi.org/10.3133/cir930M.","productDescription":"v. :ill. ;26 cm.; 36 p.","costCenters":[],"links":[{"id":124561,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/circ/1993/0930m/report-thumb.jpg"},{"id":54115,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/1993/0930m/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e48b1e4b07f02db53052d","contributors":{"authors":[{"text":"Crockett, R.N.","contributorId":6890,"corporation":false,"usgs":true,"family":"Crockett","given":"R.N.","email":"","affiliations":[],"preferred":false,"id":193284,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Sutphin, D. M.","contributorId":27424,"corporation":false,"usgs":true,"family":"Sutphin","given":"D.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":193285,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":25594,"text":"wri914169 - 1993 - Hydrologic conditions in the upper Rockaway River basin, New Jersey, 1984-86","interactions":[],"lastModifiedDate":"2012-02-02T00:08:29","indexId":"wri914169","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1993","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":"91-4169","title":"Hydrologic conditions in the upper Rockaway River basin, New Jersey, 1984-86","language":"ENGLISH","publisher":"U.S. Dept. of the Interior, U.S. Geological Survey ;\r\nBooks and Open-File Reports Section [distributor],","doi":"10.3133/wri914169","usgsCitation":"Schaefer, F., Harte, P., Smith, J.A., and Kurtz, B.A., 1993, Hydrologic conditions in the upper Rockaway River basin, New Jersey, 1984-86: U.S. Geological Survey Water-Resources Investigations Report 91-4169, vi, 103 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri914169.","productDescription":"vi, 103 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":118830,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1991/4169/report-thumb.jpg"},{"id":54337,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1991/4169/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":54338,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1991/4169/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":54339,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1991/4169/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a28e4b07f02db6113f8","contributors":{"authors":[{"text":"Schaefer, F. L.","contributorId":91085,"corporation":false,"usgs":true,"family":"Schaefer","given":"F. L.","affiliations":[],"preferred":false,"id":194339,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Harte, P. T. 0000-0002-7718-1204","orcid":"https://orcid.org/0000-0002-7718-1204","contributorId":36143,"corporation":false,"usgs":true,"family":"Harte","given":"P. T.","affiliations":[],"preferred":false,"id":194337,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Smith, J. A.","contributorId":101646,"corporation":false,"usgs":true,"family":"Smith","given":"J.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":194340,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Kurtz, B. A.","contributorId":47825,"corporation":false,"usgs":true,"family":"Kurtz","given":"B.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":194338,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":61081,"text":"mf2207 - 1993 - Maps showing distribution of selected minerals in the nonmagnetic heavy-mineral fraction of stream-sediment samples, Medfra Quadrangle, Alaska","interactions":[],"lastModifiedDate":"2012-02-10T00:10:36","indexId":"mf2207","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1993","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":325,"text":"Miscellaneous Field Studies Map","code":"MF","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"2207","title":"Maps showing distribution of selected minerals in the nonmagnetic heavy-mineral fraction of stream-sediment samples, Medfra Quadrangle, Alaska","language":"ENGLISH","doi":"10.3133/mf2207","usgsCitation":"Tripp, R.B., and King, H.D., 1993, Maps showing distribution of selected minerals in the nonmagnetic heavy-mineral fraction of stream-sediment samples, Medfra Quadrangle, Alaska: U.S. Geological Survey Miscellaneous Field Studies Map 2207, 2 maps ;each 45 x 61 cm., on sheet 104 x 135 cm., folded in envelope 30 x 24 cm., https://doi.org/10.3133/mf2207.","productDescription":"2 maps ;each 45 x 61 cm., on sheet 104 x 135 cm., folded in envelope 30 x 24 cm.","costCenters":[],"links":[{"id":105302,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_5839.htm","linkFileType":{"id":5,"text":"html"},"description":"5839"},{"id":180376,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"scale":"0","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -156,63 ], [ -156,64 ], [ -153,64 ], [ -153,63 ], [ -156,63 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a19e4b07f02db6057a2","contributors":{"authors":[{"text":"Tripp, R. B.","contributorId":88707,"corporation":false,"usgs":true,"family":"Tripp","given":"R.","middleInitial":"B.","affiliations":[],"preferred":false,"id":264950,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"King, H. D.","contributorId":89113,"corporation":false,"usgs":true,"family":"King","given":"H.","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":264951,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":54968,"text":"wdrSC921 - 1993 - Water resources data, South Carolina, water year 1992","interactions":[],"lastModifiedDate":"2025-03-14T15:24:20.476464","indexId":"wdrSC921","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1993","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":"SC-92-1","title":"Water resources data, South Carolina, water year 1992","docAbstract":"<p>Water Resources data for the 1992 water year for South Carolina consists of records of stage, discharge, and water quality of streams; stage and contents of lakes and reservoirs; and levels of ground-water wells. This volume contains records for water discharge at 126 gaging stations, stage only at 25 gaging stations, stage and contents at 12 lakes and reservoirs, water-quality at 35 gaging stations and at one observation well, and water levels at 45 observation wells. Also included are data for 80 crest-stage partial-record stations and discharge measurement information at 4 locations. Locations of these sites are shown on figures 3, 4, 5, 6, and 7. Additional water data were collected at various sites not involved in the systematic data-collection program. These data represent that part of the National Water Data System collected by the U.S. Geological Survey and cooperating State and Federal agencies in South Carolina. </p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wdrSC921","collaboration":"Prepared in cooperation with the State of South Carolina and with other agencies.","usgsCitation":"Bennett, C., Cooney, T., Jones, K., and Gissendanner, J., 1993, Water resources data, South Carolina, water year 1992: U.S. Geological Survey Water Data Report SC-92-1, xii, 480 p., https://doi.org/10.3133/wdrSC921.","productDescription":"xii, 480 p.","costCenters":[{"id":13634,"text":"South Atlantic Water Science 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Carolina\",\"nation\":\"USA  \"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a09e4b07f02db5fab59","contributors":{"authors":[{"text":"Bennett, C.S.","contributorId":13273,"corporation":false,"usgs":true,"family":"Bennett","given":"C.S.","email":"","affiliations":[],"preferred":false,"id":252159,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Cooney, T.W.","contributorId":25194,"corporation":false,"usgs":true,"family":"Cooney","given":"T.W.","email":"","affiliations":[],"preferred":false,"id":252160,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Jones, K.H.","contributorId":93566,"corporation":false,"usgs":true,"family":"Jones","given":"K.H.","email":"","affiliations":[],"preferred":false,"id":252162,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Gissendanner, J.W.","contributorId":39856,"corporation":false,"usgs":true,"family":"Gissendanner","given":"J.W.","affiliations":[],"preferred":false,"id":252161,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":25584,"text":"wri934047 - 1993 - Hydrogeology, simulated ground-water flow, and ground-water quality, Wright-Patterson Air Force Base, Ohio","interactions":[],"lastModifiedDate":"2012-02-02T00:08:29","indexId":"wri934047","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1993","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":"93-4047","title":"Hydrogeology, simulated ground-water flow, and ground-water quality, Wright-Patterson Air Force Base, Ohio","docAbstract":"Ground water is the primary source of water in the Wright-Patterson Air Force Base area. The aquifer consists of glacial sands and gravels that fill a buried bedrock-valley system. Consolidated rocks in the area consist of poorly permeable Ordovician shale of the Richmondian stage, in the upland areas, the Brassfield Limestone of Silurian age. The valleys are filled with glacial sediments of Wisconsinan age consisting of clay-rich tills and coarse-grained outwash deposits. Estimates of hydraulic conductivity of the shales based on results of displacement/recovery tests range from 0.0016 to 12 feet per day; estimates for the glacial sediments range from less than 1 foot per day to more than 1,000 feet per day.\r\n\r\nGround water flow from the uplands towards the valleys and the major rivers in the region, the Great Miami and the Mad Rivers. Hydraulic-head data indicate that ground water flows between the bedrock and unconsolidated deposits. Data from a gain/loss study of the Mad River System and hydrographs from nearby wells reveal that the reach of the river next to Wright-Patterson Air Force Base is a ground-water discharge area.\r\n\r\nA steady-state, three-dimensional ground-water-flow model was developed to simulate ground-water flow in the region. The model contains three layers and encompasses about 100 square miles centered on Wright-Patterson Air Force Base. Ground water enters the modeled area primarily by river leakage and underflow at the model boundary. Ground water exits the modeled area primarily by flow through the valleys at the model boundaries and through production wells. A model sensitivity analysis involving systematic changes in values of hydrologic parameters in the model indicates that the model is most sensitive to decreases in riverbed conductance and vertical conductance between the upper two layers. The analysis also indicates that the contribution of water to the buried-valley aquifer from the bedrock that forms the valley walls is about 2 to 4 percent of the total ground-water flow in the study area.\r\n\r\nGround waters in the vicinity of Wright-Patterson Air Force Base can be classified into two compositional groups on the basis of their chemical composition: calcium magnesium bicarbonate-type and sodium chloride-type waters. Calcium magnesium bicarbonate-type waters are found in the glacial deposits and the Brassfield Limestone, whereas the sodium chloride waters are exclusively associated with the shales. Equilibrium speciation calculations indicate that ground water of the glacial drift aquifer is in equilibrium with calcite, dolomite, and chalcedony, but is undersaturated with respect to gypsum and fluorite. Waters from the shales are slightly supersaturated with respect to calcite, dolomite, and siderite but are undersaturated with respect to chalcedony. Simple-mass balance calculations treating boron as a conservative species indicate that little (< 5 percent) or no recharge from the shales to the glacial drift aquifer takes place.\r\n\r\nData on the stable isotopes of oxygen and hydrogen indicate a meteoric origin for all ground water beneath Wright-Patterson Air Force Base, but the data were inconclusive with respect to identification of distinct isotopic differences between water collected from the glacial drift and bedrock aquifers. Tritium concentrations used to distinguish waters having a pre-and post-1953 recharge component indicate that most water entered the glacial drift aquifer after 1953. This finding indicates that recharge from shallow to deep parts (greater than 150 feet) of the aquifer takes place over time intervals of a few years or decades. However, the fact that some deep parts of the glacial aquifer did not contain measurable tritium indicates that ground-water flow from recharge zones to these parts of the aquifer takes decades or longer.","language":"ENGLISH","publisher":"U.S. Geological Survey ;\r\nBooks and Open-File Reports Section [distributor],","doi":"10.3133/wri934047","usgsCitation":"Dumouchelle, D., Schalk, C.W., Rowe, G., and De Roche, J., 1993, Hydrogeology, simulated ground-water flow, and ground-water quality, Wright-Patterson Air Force Base, Ohio: U.S. Geological Survey Water-Resources Investigations Report 93-4047, viii, 152 p. :ill. (some col.) ;28 cm., https://doi.org/10.3133/wri934047.","productDescription":"viii, 152 p. :ill. (some col.) ;28 cm.","costCenters":[],"links":[{"id":124919,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1993/4047/report-thumb.jpg"},{"id":54318,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1993/4047/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a2de4b07f02db614a47","contributors":{"authors":[{"text":"Dumouchelle, D.H.","contributorId":83144,"corporation":false,"usgs":true,"family":"Dumouchelle","given":"D.H.","affiliations":[],"preferred":false,"id":194293,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Schalk, C. W.","contributorId":64286,"corporation":false,"usgs":true,"family":"Schalk","given":"C.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":194291,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Rowe, G.L.","contributorId":23978,"corporation":false,"usgs":true,"family":"Rowe","given":"G.L.","affiliations":[],"preferred":false,"id":194290,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"De Roche, J.T.","contributorId":66691,"corporation":false,"usgs":true,"family":"De Roche","given":"J.T.","affiliations":[],"preferred":false,"id":194292,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":54942,"text":"wdrPA921 - 1993 - Water resources data, Pennsylvania, water year 1992. Volume 1. Delaware River Basin","interactions":[],"lastModifiedDate":"2020-10-06T20:56:16.514991","indexId":"wdrPA921","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1993","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":"PA-92-1","title":"Water resources data, Pennsylvania, water year 1992. Volume 1. Delaware River Basin","docAbstract":"<p>No abstract available.&nbsp;</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wdrPA921","usgsCitation":"White, K.E., White, T., Druther, R., and Moleski, P., 1993, Water resources data, Pennsylvania, water year 1992. Volume 1. Delaware River Basin: U.S. Geological Survey Water Data Report PA-92-1, xi, 340 p., https://doi.org/10.3133/wdrPA921.","productDescription":"xi, 340 p.","costCenters":[],"links":[{"id":177555,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wdr/1992/pa-92-1/report-thumb.jpg"},{"id":379122,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wdr/1992/pa-92-1/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United 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,{"id":54944,"text":"wdrPA923 - 1993 - Water resources data, Pennsylvania, water year 1992. Volume 3: Ohio and St. Lawrence River basins","interactions":[],"lastModifiedDate":"2024-07-29T21:21:21.068832","indexId":"wdrPA923","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1993","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":"PA-92-3","title":"Water resources data, Pennsylvania, water year 1992. Volume 3: Ohio and St. Lawrence River basins","docAbstract":"<p>Water resources data for the 1992 water year for Pennsylvania consists of records of discharge and water quality of streams; contents and elevations of lakes and reservoirs; and water levels of ground-water wells. This report, Volume 3, includes records from the Ohio and St. Lawrence River basins. Specifically, it contains: (1) discharge records for 69 continuous record streamflow-gaging stations and 12 partial-record stations; (2) elevation and contents records for 3 lakes and reservoirs; (3) water-quality records for 3 streamflow-gaging stations and 36 partial-record stations; and (4) water-level records for 20 network observation wells. Locations of these sites are shown on figures 4-5. Additional water data were collected at various sites not involved in the systematic data-collection program and are published as miscellaneous measurements and analyses. These data, together with the data in Volume 1 and 2, represent that part of the National Water Data System operated by the U.S. Geological Survey and cooperating State, Local, and Federal agencies in Pennsylvania.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wdrPA923","collaboration":"Prepared in cooperation with the Pennsylvania Department of Environmental Resources, the U.S. Army Corps of Engineers, Pittsburgh District, and with other State, municipal, and Federal agencies","usgsCitation":"Lescinsky, J.B., Coll, M., and Siwicki, R., 1993, Water resources data, Pennsylvania, water year 1992. 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