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,{"id":33746,"text":"b2043 - 1993 - Landslide hazards in Vermont","interactions":[],"lastModifiedDate":"2012-02-02T00:09:24","indexId":"b2043","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":"2043","title":"Landslide hazards in Vermont","language":"ENGLISH","publisher":"U.S.G.P.O. ; U.S. Geological Survey, Map Distribution,","doi":"10.3133/b2043","usgsCitation":"Baskerville, C.A., Lee, F.T., and Ratte, C.A., 1993, Landslide hazards in Vermont: U.S. Geological Survey Bulletin 2043, iv, 23 p. ill., maps ;28 cm., https://doi.org/10.3133/b2043.","productDescription":"iv, 23 p. ill., maps ;28 cm.","costCenters":[],"links":[{"id":163867,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/bul/2043/report-thumb.jpg"},{"id":61619,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/bul/2043/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1fe4b07f02db6ab585","contributors":{"authors":[{"text":"Baskerville, Charles A.","contributorId":95935,"corporation":false,"usgs":true,"family":"Baskerville","given":"Charles","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":211866,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Lee, Fitzhugh T.","contributorId":82272,"corporation":false,"usgs":true,"family":"Lee","given":"Fitzhugh","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":211865,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Ratte, Charles A.","contributorId":100041,"corporation":false,"usgs":true,"family":"Ratte","given":"Charles","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":211867,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"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":34315,"text":"b1994 - 1993 - Geology of the New Tripoli Quadrangle, Lehigh, Berks, Schuylkill, and Carbon counties, Pennsylvania","interactions":[],"lastModifiedDate":"2012-02-02T00:09:33","indexId":"b1994","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":"1994","title":"Geology of the New Tripoli Quadrangle, Lehigh, Berks, Schuylkill, and Carbon counties, Pennsylvania","language":"ENGLISH","publisher":"U.S.G.P.O. ; U.S. Geological Survey, Map Distribution,","doi":"10.3133/b1994","usgsCitation":"Epstein, J., and Lyttle, P.T., 1993, Geology of the New Tripoli Quadrangle, Lehigh, Berks, Schuylkill, and Carbon counties, Pennsylvania: U.S. Geological Survey Bulletin 1994, iv, 19 p. ill., map (col.) ;28 cm., https://doi.org/10.3133/b1994.","productDescription":"iv, 19 p. ill., map (col.) ;28 cm.","costCenters":[],"links":[{"id":109812,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_22228.htm","linkFileType":{"id":5,"text":"html"},"description":"22228"},{"id":167392,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/bul/1994/report-thumb.jpg"},{"id":62209,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/1994/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":62210,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/bul/1994/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b23e4b07f02db6adee3","contributors":{"authors":[{"text":"Epstein, Jack Burton","contributorId":64625,"corporation":false,"usgs":true,"family":"Epstein","given":"Jack Burton","affiliations":[],"preferred":false,"id":212775,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Lyttle, Peter T. plyttle@usgs.gov","contributorId":293,"corporation":false,"usgs":true,"family":"Lyttle","given":"Peter","email":"plyttle@usgs.gov","middleInitial":"T.","affiliations":[],"preferred":true,"id":212774,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":16844,"text":"ofr93259B - 1993 - Analytical results and sample locality map of stream-sediment, heavy-mineral-concentrate, and rock samples from the Upper Leslie Gulch (OR-003-074) and Slocum Creek (OR-003-075) Wilderness Study Areas, Malheur County, Oregon","interactions":[],"lastModifiedDate":"2013-09-18T07:44:40","indexId":"ofr93259B","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":"93-259","chapter":"B","title":"Analytical results and sample locality map of stream-sediment, heavy-mineral-concentrate, and rock samples from the Upper Leslie Gulch (OR-003-074) and Slocum Creek (OR-003-075) Wilderness Study Areas, Malheur County, Oregon","language":"ENGLISH","publisher":"U.S. Dept. of the Interior, Geological Survey :[Books and Open-File Reports Section, distributor],","doi":"10.3133/ofr93259B","collaboration":"The USGS does not support this software or technical questions for the software associated with the publication.","usgsCitation":"Hageman, P., King, H.D., Jones, J.L., and Erickson, M.S., 1993, Analytical results and sample locality map of stream-sediment, heavy-mineral-concentrate, and rock samples from the Upper Leslie Gulch (OR-003-074) and Slocum Creek (OR-003-075) Wilderness Study Areas, Malheur County, Oregon: U.S. Geological Survey Open-File Report 93-259, 1 computer disk ;5 1/4 in., https://doi.org/10.3133/ofr93259B.","productDescription":"1 computer disk ;5 1/4 in.","costCenters":[],"links":[{"id":148292,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":277777,"type":{"id":4,"text":"Application Site"},"url":"https://pubs.usgs.gov/of/1993/0259b/application.zip"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4acce4b07f02db67e50d","contributors":{"authors":[{"text":"Hageman, P.  L. 0000-0002-3440-2150","orcid":"https://orcid.org/0000-0002-3440-2150","contributorId":27459,"corporation":false,"usgs":true,"family":"Hageman","given":"P.  L.","affiliations":[],"preferred":false,"id":173854,"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":173856,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Jones, J. L.","contributorId":27065,"corporation":false,"usgs":true,"family":"Jones","given":"J.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":173853,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Erickson, M. S.","contributorId":35302,"corporation":false,"usgs":true,"family":"Erickson","given":"M.","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":173855,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":38338,"text":"pp1542 - 1993 - Allostratigraphy of the U.S. middle Atlantic continental margin; characteristics, distribution, and depositional history of principal unconformity-bounded upper Cretaceous and Cenozoic sedimentary units","interactions":[],"lastModifiedDate":"2012-02-02T00:09:45","indexId":"pp1542","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1993","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":331,"text":"Professional Paper","code":"PP","onlineIssn":"2330-7102","printIssn":"1044-9612","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"1542","title":"Allostratigraphy of the U.S. middle Atlantic continental margin; characteristics, distribution, and depositional history of principal unconformity-bounded upper Cretaceous and Cenozoic sedimentary units","docAbstract":"Publication of Volumes 93 and 95 ('The New Jersey Transect') of the Deep Sea Drilling Project's Initial Reports completed a major phase of geological and geophysical research along the middle segment of the U. S. Atlantic continental margin. Relying heavily on data from these and related published records, we have integrated outcrop, borehole, and seismic-reflection data from this large area (500,000 km^2 ) to define the regional allostratigraphic framework for Upper Cretaceous and Cenozoic sedimentary rocks. The framework consists of 12 alloformations, which record the Late Cretaceous and Cenozoic depositional history of the contiguous Baltimore Canyon trough (including its onshore margin) and Hatteras basin (northern part). We propose stratotype sections for each alloformation and present a regional allostratigraphic reference section, which crosses these basins from the inner edge of the coastal plain to the inner edge of the abyssal plain. Selected supplementary reference sections on the coastal plain allow observation of the alloformations and their bounding unconformities in outcrop. \r\n\r\nOur analyses show that sediment supply and its initial dispersal on the middle segment of the U. S. Atlantic margin have been governed, in large part, by hinterland tectonism and subsequently have been modified by paleoclimate, sea-level changes, and oceanic current systems. Notable events in the Late Cretaceous to Holocene sedimentary evolution of this margin include (1) development of continental-rise depocenters in the northern part of the Hatteras basin during the Late Cretaceous; (2) the appear ance of a dual shelf-edge system, a marked decline in siliciclastic sediment accumulation rates, and widespread acceleration of carbonate production during high sea levels of the Paleogene; (3) rapid deposition and progradation of thick terrigenous delta complexes and development of abyssal depocenters during the middle Miocene to Quaternary interval; and (4) deep incision of the shelf edge by submarine canyons, especially during the Pleistocene. \r\n\r\nMassive downslope gravity flows have dominated both the depositional and erosional history of the middle segment of the U. S. Atlantic Continental Slope and Rise during most of the last 84 million years. The importance of periodic widespread erosion is recorded by well-documented unconformities, many of which can be traced from coastal-plain outcrops to coreholes on the continental slope and lower continental rise. These unconformities form the boundaries of the 12 allostratigraphic units we formally propose herein. Seven of the unconformities correlate with supercycle boundaries (sequence boundaries) that characterize the Exxon sequence-stratigraphy model.","language":"ENGLISH","doi":"10.3133/pp1542","usgsCitation":"Poag, C.W., and Ward, L.W., 1993, Allostratigraphy of the U.S. middle Atlantic continental margin; characteristics, distribution, and depositional history of principal unconformity-bounded upper Cretaceous and Cenozoic sedimentary units: U.S. Geological Survey Professional Paper 1542, 81 p., https://doi.org/10.3133/pp1542.","productDescription":"81 p.","costCenters":[],"links":[{"id":124830,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/1542/report-thumb.jpg"},{"id":64687,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/1542/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adfe4b07f02db687898","contributors":{"authors":[{"text":"Poag, C. Wylie 0000-0002-6240-4065 wpoag@usgs.gov","orcid":"https://orcid.org/0000-0002-6240-4065","contributorId":2565,"corporation":false,"usgs":true,"family":"Poag","given":"C.","email":"wpoag@usgs.gov","middleInitial":"Wylie","affiliations":[{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":true,"id":219639,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Ward, Lauck W.","contributorId":44145,"corporation":false,"usgs":true,"family":"Ward","given":"Lauck","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":219640,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":35203,"text":"b2048 - 1993 - Object-oriented expert systems and their applications to sedimentary basin analysis","interactions":[],"lastModifiedDate":"2012-02-02T00:09:43","indexId":"b2048","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":"2048","title":"Object-oriented expert systems and their applications to sedimentary basin analysis","language":"ENGLISH","publisher":"U.S. G.P.O. ; U.S. Geological Survey, USGS Map Distribution,","doi":"10.3133/b2048","usgsCitation":"Miller, B., 1993, Object-oriented expert systems and their applications to sedimentary basin analysis: U.S. Geological Survey Bulletin 2048, iv, 31 p. ill. ;28 cm., https://doi.org/10.3133/b2048.","productDescription":"iv, 31 p. ill. ;28 cm.","costCenters":[],"links":[{"id":167474,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/bul/2048/report-thumb.jpg"},{"id":63079,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/bul/2048/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afce4b07f02db6965ba","contributors":{"authors":[{"text":"Miller, Betty M.","contributorId":92231,"corporation":false,"usgs":true,"family":"Miller","given":"Betty M.","affiliations":[],"preferred":false,"id":214248,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":19465,"text":"ofr93172 - 1993 - Water quality of an urban wet detention pond in Madison, Wisconsin, 1987-88","interactions":[],"lastModifiedDate":"2015-10-19T09:17:49","indexId":"ofr93172","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":"93-172","title":"Water quality of an urban wet detention pond in Madison, Wisconsin, 1987-88","docAbstract":"<p>A 5,670-sq m wet detention pond was monitored by the U.S. Geological Survey to determine its effect on the water quality of urban runoff. The pond has a drainage area of 0.96-sq km, composed primarily of single-family residential land use. Event-mean concentrations (EMC) were determined from samples collected for sediment, nutrients, and selected metals at the pond's inflow and outflow sites. EMC samples were collected for 64 runoff events during the study period from February 1987 to April 1988. Storm precipitation ranged from 1 to 51 mm during these events. Inflow and outflow EMC and constituent loads were compared to determine the trap efficiency of the pond. Trap efficiency varied considerably among water-quality constituents. In general, the detention pond decreased the EMC of sampled constituents at the outlet compared to the inlet. The median decrease in EMC for suspended solids was 88 percent, 60 percent for total chemical oxygen demand (COD), 43 percent for total phosphorus, 38 percent for total Kjeldahl nitrogen, 65 percent for total nitrite plus nitrate, and 71 percent for total lead. A notable exception to the general decrease in EMC is for chloride. The EMC for chloride was generally higher in outflow from the pond than in the inflow. This is attributed to an unmonitored influx of chloride to the pond during the winter that subsequently was flushed out during monitored runoff events. The total study-period loads of most constituents were less leaving the pond than the loads entering it. This decrease is attributed to the constituents transported on suspended sediment being deposited in the pond. The decrease in total load of suspended solids was 88 percent, 62 percent for total COD, 58 percent for total phosphorus, 46 percent for total Kjeldahl nitrogen, 62 percent for total nitrite plus nitrate, 97 percent for total copper, and 93 percent for total lead. (USGS)</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr93172","collaboration":"Prepared in cooperation with the Wisconsin Department of Natural Resources","usgsCitation":"House, L.B., Waschbusch, R., and Hughes, P., 1993, Water quality of an urban wet detention pond in Madison, Wisconsin, 1987-88: U.S. Geological Survey Open-File Report 93-172, v, 57 p., https://doi.org/10.3133/ofr93172.","productDescription":"v, 57 p.","numberOfPages":"62","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":677,"text":"Wisconsin Water Science Center","active":true,"usgs":true}],"links":[{"id":151548,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1993/0172/report-thumb.jpg"},{"id":48940,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1993/0172/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Wisconsin","county":"Dane","city":"Wisconsin","otherGeospatial":"Lake Wingra","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -89.45300102233885,\n              43.03533293549335\n            ],\n            [\n              -89.45300102233885,\n              43.07026720632101\n            ],\n            [\n              -89.40227508544922,\n              43.07026720632101\n            ],\n            [\n              -89.40227508544922,\n              43.03533293549335\n            ],\n            [\n              -89.45300102233885,\n              43.03533293549335\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f7e4b07f02db5f2591","contributors":{"authors":[{"text":"House, L. B.","contributorId":49386,"corporation":false,"usgs":true,"family":"House","given":"L.","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":180958,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Waschbusch, R.J.","contributorId":107307,"corporation":false,"usgs":true,"family":"Waschbusch","given":"R.J.","affiliations":[],"preferred":false,"id":180960,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Hughes, P.E.","contributorId":104083,"corporation":false,"usgs":true,"family":"Hughes","given":"P.E.","email":"","affiliations":[],"preferred":false,"id":180959,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":29429,"text":"wri934139 - 1993 - Hydrology of Little Rock Lake in Vilas County, north-central Wisconsin","interactions":[],"lastModifiedDate":"2015-10-26T13:06:09","indexId":"wri934139","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":"93-4139","title":"Hydrology of Little Rock Lake in Vilas County, north-central Wisconsin","docAbstract":"<p>Water budgets were developed for Little Rock Lake for October 1983 through September 1990 as part of a study to evaluate the chemical and biological effects of artificially acidifying one basin of the two-basin lake. The 17.9-hectare seepage lake is situated in 60- to 90-meter-thick, predominantly sand and gravel glacial deposits of Vilas County, north-central Wisconsin. Annual precipitation during the study varied from 647 to 926 mm (millimeters). Average annual precipitation during 1951-80, based on nearby National Weather Service stations, was 825 mm. Annual evaporation from the lake surface ranged from 495 to 648 mm. Total lake-stage fluctuation was 930 mm during the study. Lake volume at the maximum stage was 31 percent greater than at the minimum lake stage. Inflow to the lake was dominated by precipitation, which was about 99 percent of total inflow. Ground-water inflow to the lake was transient, occurring only intermittently during October 1983 through September 1986, and amounted to only about 1 percent of total inflow. No ground water flowed into the lake from October 1986 through September 1990. Evaporation accounted for about two-thirds of total outflow from the lake, and lake water discharging to the underlying aquifer accounted for the remainder. The average hydraulic residence times for the 7-year study period were 3.9, 3.3, and 4 years for the entire lake, the south basin, and the north basin, respectively; corresponding chemical residence times were 10.9, 9.3, and 10 years.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri934139","collaboration":"Prepared in cooperation with the Wisconsin Department of Natural Resources","usgsCitation":"Rose, W.J., 1993, Hydrology of Little Rock Lake in Vilas County, north-central Wisconsin: U.S. Geological Survey Water-Resources Investigations Report 93-4139, v, 22 p., https://doi.org/10.3133/wri934139.","productDescription":"v, 22 p.","numberOfPages":"27","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":119511,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1993/4139/report-thumb.jpg"},{"id":58277,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1993/4139/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Wisconsin","county":"Vilas County","otherGeospatial":"Little Rock Lake","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"Polygon\",\"coordinates\":[[[-88.9879,46.0971],[-88.9329,46.0746],[-88.9332,45.9822],[-89.0478,45.9822],[-89.0477,45.8953],[-89.1091,45.8973],[-89.1752,45.8993],[-89.1754,45.859],[-89.3008,45.8606],[-89.3007,45.9014],[-89.3628,45.8987],[-89.4256,45.8987],[-89.5498,45.8988],[-89.6741,45.8987],[-89.7571,45.8985],[-89.797,45.898],[-89.8199,45.8984],[-89.9212,45.8981],[-89.9846,45.8974],[-90.0428,45.8972],[-90.0442,45.9823],[-90.0134,45.9824],[-89.9853,45.9821],[-89.9289,45.9818],[-89.9282,46.0693],[-89.9288,46.1558],[-89.9287,46.2428],[-89.929,46.3],[-89.7599,46.268],[-89.7368,46.2636],[-89.5829,46.2347],[-89.5331,46.2252],[-89.5133,46.2215],[-89.4272,46.2048],[-89.3759,46.1949],[-89.2666,46.1737],[-89.2302,46.1662],[-89.0854,46.1365],[-88.9879,46.0971]]]},\"properties\":{\"name\":\"Vilas\",\"state\":\"WI\"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a17e4b07f02db6048af","contributors":{"authors":[{"text":"Rose, W. J.","contributorId":14433,"corporation":false,"usgs":true,"family":"Rose","given":"W.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":201514,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":49682,"text":"ofr93609B - 1993 - Earthquake data report, September 1993","interactions":[],"lastModifiedDate":"2012-02-02T00:11:16","indexId":"ofr93609B","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":"93-609","chapter":"B","title":"Earthquake data report, September 1993","language":"ENGLISH","doi":"10.3133/ofr93609B","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1993, Earthquake data report, September 1993: U.S. Geological Survey Open-File Report 93-609, Five 5 1/4 inch diskettes, https://doi.org/10.3133/ofr93609B.","productDescription":"Five 5 1/4 inch diskettes","costCenters":[],"links":[{"id":176740,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a51e4b07f02db629878","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":532037,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":49677,"text":"ofr93607A - 1993 - Earthquake data report, July 1993","interactions":[],"lastModifiedDate":"2012-02-02T00:11:11","indexId":"ofr93607A","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":"93-607","chapter":"A","title":"Earthquake data report, July 1993","language":"ENGLISH","doi":"10.3133/ofr93607A","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1993, Earthquake data report, July 1993: U.S. Geological Survey Open-File Report 93-607, p. 588, https://doi.org/10.3133/ofr93607A.","productDescription":"p. 588","costCenters":[],"links":[{"id":176110,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1993/0607a/report-thumb.jpg"},{"id":86273,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1993/0607a/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a52e4b07f02db62a7ec","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":532032,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":1096,"text":"wsp2392 - 1993 - Ground-water chemical evolution and diagenetic processes in the upper Floridan Aquifer, southern South Carolina and northeastern Georgia","interactions":[{"subject":{"id":18365,"text":"ofr8927 - 1988 - Ground-water chemical evolution and diagenetic processes in the Upper Floridan aquifer, southern South Carolina and northeastern Georgia","indexId":"ofr8927","publicationYear":"1988","noYear":false,"title":"Ground-water chemical evolution and diagenetic processes in the Upper Floridan aquifer, southern South Carolina and northeastern Georgia"},"predicate":"SUPERSEDED_BY","object":{"id":1096,"text":"wsp2392 - 1993 - Ground-water chemical evolution and diagenetic processes in the upper Floridan Aquifer, southern South Carolina and northeastern Georgia","indexId":"wsp2392","publicationYear":"1993","noYear":false,"title":"Ground-water chemical evolution and diagenetic processes in the upper Floridan Aquifer, southern South Carolina and northeastern Georgia"},"id":1}],"lastModifiedDate":"2019-12-30T10:52:04","indexId":"wsp2392","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1993","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":"2392","title":"Ground-water chemical evolution and diagenetic processes in the upper Floridan Aquifer, southern South Carolina and northeastern Georgia","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Government Printing Office","doi":"10.3133/wsp2392","usgsCitation":"Burt, R.A., 1993, Ground-water chemical evolution and diagenetic processes in the upper Floridan Aquifer, southern South Carolina and northeastern Georgia: U.S. Geological Survey Water Supply Paper 2392, vii, 76 p., https://doi.org/10.3133/wsp2392.","productDescription":"vii, 76 p.","costCenters":[{"id":13634,"text":"South Atlantic Water Science Center","active":true,"usgs":true}],"links":[{"id":25826,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/2392/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":137916,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/2392/report-thumb.jpg"}],"country":"United States","state":"Georgia, South Carolina","otherGeospatial":"Upper Floridan Aquifer","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -81.45263671875,\n              31.80289258670676\n            ],\n            [\n              -80.771484375,\n              31.80289258670676\n            ],\n            [\n              -80.771484375,\n              32.30570601389429\n            ],\n            [\n              -81.45263671875,\n              32.30570601389429\n            ],\n            [\n              -81.45263671875,\n              31.80289258670676\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aafe4b07f02db66d32a","contributors":{"authors":[{"text":"Burt, Ronald Allen","contributorId":54173,"corporation":false,"usgs":true,"family":"Burt","given":"Ronald","email":"","middleInitial":"Allen","affiliations":[],"preferred":false,"id":143171,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":30407,"text":"wri924165 - 1993 - Flood frequency of streams in rural basins of Tennessee","interactions":[],"lastModifiedDate":"2012-02-02T00:08:58","indexId":"wri924165","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":"92-4165","title":"Flood frequency of streams in rural basins of Tennessee","language":"ENGLISH","publisher":"U.S. Geological Survey ;\r\nBooks and Open-File Reports Section [distributor],","doi":"10.3133/wri924165","usgsCitation":"Weaver, J., and Gamble, C.R., 1993, Flood frequency of streams in rural basins of Tennessee: U.S. Geological Survey Water-Resources Investigations Report 92-4165, iv, 38 p. :ill. ;28 cm., https://doi.org/10.3133/wri924165.","productDescription":"iv, 38 p. :ill. ;28 cm.","costCenters":[],"links":[{"id":119406,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1992/4165/report-thumb.jpg"},{"id":59176,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1992/4165/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f2e4b07f02db5ef1c4","contributors":{"authors":[{"text":"Weaver, J.D.","contributorId":29466,"corporation":false,"usgs":true,"family":"Weaver","given":"J.D.","email":"","affiliations":[],"preferred":false,"id":203197,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Gamble, C. R.","contributorId":26727,"corporation":false,"usgs":true,"family":"Gamble","given":"C.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":203196,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":21289,"text":"ofr9184 - 1993 - Streamgaging cableways","interactions":[{"subject":{"id":21289,"text":"ofr9184 - 1993 - Streamgaging cableways","indexId":"ofr9184","publicationYear":"1993","noYear":false,"title":"Streamgaging cableways"},"predicate":"SUPERSEDED_BY","object":{"id":4725,"text":"twri03A21 - 1995 - Stream-gaging cableways","indexId":"twri03A21","publicationYear":"1995","noYear":false,"title":"Stream-gaging cableways"},"id":1}],"supersededBy":{"id":4725,"text":"twri03A21 - 1995 - Stream-gaging cableways","indexId":"twri03A21","publicationYear":"1995","noYear":false,"title":"Stream-gaging cableways"},"lastModifiedDate":"2021-01-05T18:05:07.400883","indexId":"ofr9184","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":"91-84","title":"Streamgaging cableways","docAbstract":"<p>No abstract available.&nbsp;</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr9184","usgsCitation":"Wagner, C.R., 1993, Streamgaging cableways (Revised - 1993): U.S. Geological Survey Open-File Report 91-84, ix, 90 p., https://doi.org/10.3133/ofr9184.","productDescription":"ix, 90 p.","costCenters":[],"links":[{"id":155290,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"edition":"Revised - 1993","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b15e4b07f02db6a4c8f","contributors":{"authors":[{"text":"Wagner, C. Russell","contributorId":93475,"corporation":false,"usgs":true,"family":"Wagner","given":"C.","email":"","middleInitial":"Russell","affiliations":[],"preferred":false,"id":184154,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":1268,"text":"wsp2397 - 1993 - Delineation of recharge areas for selected wells in the St. Peter-Prairie du Chien-Jordan aquifer, Rochester, Minnesota","interactions":[{"subject":{"id":18642,"text":"ofr90397 - 1991 - Delineation of recharge areas for selected wells in the St. Peter-Prairie du Chien-Jordan Aquifer, Rochester, Minnesota","indexId":"ofr90397","publicationYear":"1991","noYear":false,"title":"Delineation of recharge areas for selected wells in the St. Peter-Prairie du Chien-Jordan Aquifer, Rochester, Minnesota"},"predicate":"SUPERSEDED_BY","object":{"id":1268,"text":"wsp2397 - 1993 - Delineation of recharge areas for selected wells in the St. Peter-Prairie du Chien-Jordan aquifer, Rochester, Minnesota","indexId":"wsp2397","publicationYear":"1993","noYear":false,"title":"Delineation of recharge areas for selected wells in the St. Peter-Prairie du Chien-Jordan aquifer, Rochester, Minnesota"},"id":1}],"lastModifiedDate":"2024-01-11T00:00:40.643267","indexId":"wsp2397","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1993","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":"2397","title":"Delineation of recharge areas for selected wells in the St. Peter-Prairie du Chien-Jordan aquifer, Rochester, Minnesota","docAbstract":"<p>Accurate delineation of recharge areas for wells is an important requisite to protecting ground-water quality. Zones of transport and zones of contribution are two types of recharge areas that can be delineated. Analytical-calculation, numerical-modeling, and hydrogeologic-mapping methods were used to delineate recharge areas for two high-capacity wells (greater than about 200 gallons per minute discharge) completed in a karstic aquifer in the city of Rochester, in southeastern Minnesota. One well is less than 1,000 feet from a river in an area where the aquifer is unconfined, whereas the other well is more than 2,000 feet from a stream in an area where a bedrock confining unit is present.</p>\n<p>Ground-water travel times from points along the top of the aquifer to a pumped well are identified by use of a constructed map showing lines of equal advective travel time. A zone of transport, therefore, is defined by the area bounded by lines of equal travel time. Zones of transport are delineated by analytical models (calculations) and by numerical models that account for hydrologic factors. Analytical models that were used include fixed-radius (Theis drawdown, Theis time-of-travel, and volumetric equation) and variable shape. Numerical modeling was done with the U.S. Geological Survey three-dimensional ground-water-flow model MODFLOW and particle-tracking code MODPATH. The zone-of-transport areas for each of the two wells calculated by the various analytical models were very similar. The Theis-drawdown method yielded results that compared least favorably with results from the other analytical methods. The zone-of-transport areas computed by use of the numerical model were generally larger than areas computed by use of analytical models.</p>\n<p>Hydrogeologic mapping and numerical modeling were used to delineate zones of contribution to wells, defined as all parts of a ground-water-flow system that could supply water to a well. The zones of contribution delineated by use of numerical modeling have similar orientation (parallel to regional flow directions) but significantly different areas than the zones of contribution delineated by use of hydrogeologic mapping. Differences in computed areas of recharge are attributed to the capability of the numerical model to more accurately represent (1) the three-dimensional flow system, (2) hydrologic boundaries such as streams, (3) variable recharge, and (4) the influence of nearby pumped wells, compared to the analytical models.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Washington, D.C.","doi":"10.3133/wsp2397","collaboration":"Prepared in cooperation with the U.S. Environmental Protection Agency","usgsCitation":"Delin, G., and Almendinger, J.E., 1993, Delineation of recharge areas for selected wells in the St. Peter-Prairie du Chien-Jordan aquifer, Rochester, Minnesota: U.S. Geological Survey Water Supply Paper 2397, v, 39 p., https://doi.org/10.3133/wsp2397.","productDescription":"v, 39 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":392,"text":"Minnesota Water Science Center","active":true,"usgs":true}],"links":[{"id":424298,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_25297.htm","linkFileType":{"id":5,"text":"html"}},{"id":137455,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/2397/report-thumb.jpg"},{"id":26223,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/2397/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Minnesota","city":"Rochester","otherGeospatial":"St. Peter-Prairie du Chien-Jordan aquifer","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -92.74658203125,\n              43.898881944430414\n            ],\n            [\n              -92.74658203125,\n              44.11815563115412\n            ],\n            [\n              -92.35519409179688,\n              44.11815563115412\n            ],\n            [\n              -92.35519409179688,\n              43.898881944430414\n            ],\n            [\n              -92.74658203125,\n              43.898881944430414\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ab9e4b07f02db6712f6","contributors":{"authors":[{"text":"Delin, G. N.","contributorId":12834,"corporation":false,"usgs":true,"family":"Delin","given":"G. N.","affiliations":[],"preferred":false,"id":143469,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Almendinger, James Edward","contributorId":43330,"corporation":false,"usgs":true,"family":"Almendinger","given":"James","email":"","middleInitial":"Edward","affiliations":[],"preferred":false,"id":143470,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":1008,"text":"wsp2396 - 1993 - Numerical simulation of ground-water flow in the central part of the western San Joaquin Valley, California","interactions":[{"subject":{"id":18103,"text":"ofr91535 - 1992 - Numerical simulation of ground-water flow in the central part of the western San Joaquin Valley, California","indexId":"ofr91535","publicationYear":"1992","noYear":false,"title":"Numerical simulation of ground-water flow in the central part of the western San Joaquin Valley, California"},"predicate":"SUPERSEDED_BY","object":{"id":1008,"text":"wsp2396 - 1993 - Numerical simulation of ground-water flow in the central part of the western San Joaquin Valley, California","indexId":"wsp2396","publicationYear":"1993","noYear":false,"title":"Numerical simulation of ground-water flow in the central part of the western San Joaquin Valley, California"},"id":1}],"lastModifiedDate":"2012-02-02T00:05:16","indexId":"wsp2396","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1993","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":"2396","title":"Numerical simulation of ground-water flow in the central part of the western San Joaquin Valley, California","docAbstract":"The occurrence of selenium in agricultural drain water in the central part of the western San Joaquin Valley, California, has focused concern on strategies for managing shallow, saline ground water. To assess alternatives to agricultural drains, a three-dimensional, finite-difference numerical model of the regional groundwater flow system was developed. This report documents the mathematical approach used to model the flow system, the data base on which the model is based, and the methods used to calibrate the model. \r\n\r\nThe 550-square-mile study area includes parts of the Panoche Creek alluvial fan and parts of the Little Panoche Creek and Cantua Creek alluvial fans. The model simulates transient flow in the semiconfined and confined zones above and below the Corcoran Clay Member of the Tulare Formation of Pleistocene age. The model incorporates areally distributed ground-water recharge, areally and vertically distributed pumping, regional-collector drains in the Wesdands Water District (operative from 1980 to 1985), on-farm drains in parts of the Panoche, Broadview, and Firebaugh Water Districts, and bare-soil evaporation (which occurs if the water table is within 7 feet of land surface). \r\n\r\nThe model also incorporates texture-based estimates of hydraulic conductivity, where texture is defined as the fraction of coarse-grained deposits present in a given subsurface interval. The numerical model was developed using hydrologic data from 1972 to 1988. Most of the parameters incorporated into the model were evaluated independently of the model, including system geometry, the distribution of texture, the altitudes of the water table and potentiometric surface of the confined zone in 1972 (initial condition), the hydraulic conductivity of coarse-grained deposits derived from the Coast Ranges, the hydraulic conductivity of coarse-grained deposits derived from the Sierra Nevada, specific storage, recharge, pumping, and parameters needed to incorporate drains and bare-soil evaporation. Four parameters were calibration variables: the hydraulic conductivity of fine-grained deposits in the semiconfined zone, the hydraulic conductivity of the Corcoran Clay Member, specific yield, and the transmissivity of the confined zone. \r\n\r\nThe model was calibrated in two phases. In the first phase, a steady-state model of the ground-water flow system in 1984 was used to constrain the relation between the hydraulic conductivity of fine-grained deposits in the semiconfined zone and the hydraulic conductivity of the Corcoran Clay Member, thus reducing the number of independent variables from four to three. In the second phase of calibration, the change in altitude of the water table from 1972 to 1984, the change in altitude of the potentiometric surface of the confined zone from 1972 to 1984, and the number of model cells subject to bare-soil evaporation from 1972 to 1988 were used to evaluate the remaining three variables. \r\n\r\nThe calibrated model reproduces the average change in water-table altitude (1972-84) to within 0.4 foot (average measured change 11.5 feet) and the average change in confined zone head (1972- 84) to within 19 feet (average measured change 120 feet). The simulated time-series record of the total number of model cells subject to bare-soil evaporation (each cell is 1 mile square) is within the range of the measured data. The measured values are at a minimum in October and a maximum in July. The October values ranged from 103 in 1972 to 132 in 1984 (the drains were closed in 1985) to 151 in 1988. The July values ranged from 144 in 1973 to 198 in 1984, to 204 in 1988. The simulated values ranged from 103 in 1972 to 161 in 1984, to 208 in 1988.","language":"ENGLISH","publisher":"U.S. G.P.O. ;\r\nFor sale by the Books and Open-File Reports Section, U.S. Geological Survey,","doi":"10.3133/wsp2396","usgsCitation":"Belitz, K., Phillips, S.P., and Gronberg, J., 1993, Numerical simulation of ground-water flow in the central part of the western San Joaquin Valley, California: U.S. Geological Survey Water Supply Paper 2396, vi, 69 p. :ill., maps ;28 cm., https://doi.org/10.3133/wsp2396.","productDescription":"vi, 69 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":137965,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/2396/report-thumb.jpg"},{"id":25588,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/2396/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afce4b07f02db69680d","contributors":{"authors":[{"text":"Belitz, Kenneth 0000-0003-4481-2345 kbelitz@usgs.gov","orcid":"https://orcid.org/0000-0003-4481-2345","contributorId":442,"corporation":false,"usgs":true,"family":"Belitz","given":"Kenneth","email":"kbelitz@usgs.gov","affiliations":[{"id":27111,"text":"National Water Quality Program","active":true,"usgs":true},{"id":451,"text":"National Water Quality Assessment Program","active":true,"usgs":true},{"id":466,"text":"New England Water Science Center","active":true,"usgs":true},{"id":503,"text":"Office of Water Quality","active":true,"usgs":true},{"id":376,"text":"Massachusetts Water Science Center","active":true,"usgs":true}],"preferred":true,"id":143013,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Phillips, Steven P. 0000-0002-5107-868X sphillip@usgs.gov","orcid":"https://orcid.org/0000-0002-5107-868X","contributorId":1506,"corporation":false,"usgs":true,"family":"Phillips","given":"Steven","email":"sphillip@usgs.gov","middleInitial":"P.","affiliations":[{"id":154,"text":"California Water Science Center","active":true,"usgs":true}],"preferred":true,"id":143014,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Gronberg, Jo Ann M.","contributorId":18342,"corporation":false,"usgs":true,"family":"Gronberg","given":"Jo Ann M.","affiliations":[],"preferred":false,"id":143015,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":30646,"text":"wri924003 - 1993 - Effects of stormwater detention on the chemical quality of runoff from a small residential development, Monroe County, New York","interactions":[],"lastModifiedDate":"2012-02-02T00:09:00","indexId":"wri924003","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":"92-4003","title":"Effects of stormwater detention on the chemical quality of runoff from a small residential development, Monroe County, New York","language":"ENGLISH","publisher":"U.S. Geological Survey ;\r\nU.S. Geological Survey, Books and Open-File Reports [distributor],","doi":"10.3133/wri924003","usgsCitation":"Zarriello, P.J., and Sherwood, D.A., 1993, Effects of stormwater detention on the chemical quality of runoff from a small residential development, Monroe County, New York: U.S. Geological Survey Water-Resources Investigations Report 92-4003, vi, 57 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri924003.","productDescription":"vi, 57 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":122177,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1992/4003/report-thumb.jpg"},{"id":59419,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1992/4003/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":59420,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1992/4003/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a28e4b07f02db610b29","contributors":{"authors":[{"text":"Zarriello, Philip J.","contributorId":21588,"corporation":false,"usgs":false,"family":"Zarriello","given":"Philip","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":203597,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Sherwood, D. A.","contributorId":65824,"corporation":false,"usgs":true,"family":"Sherwood","given":"D.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":203598,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
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