{"pageNumber":"1621","pageRowStart":"40500","pageSize":"25","recordCount":68937,"records":[{"id":65604,"text":"i2417 - 1995 - Controlled photomosaic of the MTM 45022 Quadrangle, Acidalia Planitia region of Mars","interactions":[],"lastModifiedDate":"2012-02-10T00:11:06","indexId":"i2417","displayToPublicDate":"1995-06-01T00:00:00","publicationYear":"1995","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":320,"text":"IMAP","code":"I","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"2417","subseriesTitle":"NONE","title":"Controlled photomosaic of the MTM 45022 Quadrangle, Acidalia Planitia region of Mars","language":"ENGLISH","doi":"10.3133/i2417","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1995, Controlled photomosaic of the MTM 45022 Quadrangle, Acidalia Planitia region of Mars: U.S. Geological Survey IMAP 2417, 1 remote-sensing image ;62 x 45 cm., on sheet 97 x 56 cm., folded in envelope 30 x 24 cm., https://doi.org/10.3133/i2417.","productDescription":"1 remote-sensing image ;62 x 45 cm., on sheet 97 x 56 cm., folded in envelope 30 x 24 cm.","costCenters":[],"links":[{"id":189422,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":101054,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/imap/2417/plate-1.pdf","size":"9679","linkFileType":{"id":1,"text":"pdf"}}],"scale":"502000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ 20,42.5 ], [ 20,47.5 ], [ 25,47.5 ], [ 25,42.5 ], [ 20,42.5 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae0e4b07f02db688256","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":533992,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":18653,"text":"ofr9549 - 1995 - Acetic acid leachability of lead from clinoptilolite-rich rocks that extracted heavy metals from polluted drainage water in Colorado","interactions":[],"lastModifiedDate":"2012-02-02T00:07:28","indexId":"ofr9549","displayToPublicDate":"1995-06-01T00:00:00","publicationYear":"1995","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":"95-49","title":"Acetic acid leachability of lead from clinoptilolite-rich rocks that extracted heavy metals from polluted drainage water in Colorado","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr9549","usgsCitation":"Desborough, G.A., 1995, Acetic acid leachability of lead from clinoptilolite-rich rocks that extracted heavy metals from polluted drainage water in Colorado: U.S. Geological Survey Open-File Report 95-49, i, 10 p. ill. ;28 cm., https://doi.org/10.3133/ofr9549.","productDescription":"i, 10 p. ill. ;28 cm.","costCenters":[],"links":[{"id":151723,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1995/0049/report-thumb.jpg"},{"id":47990,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1995/0049/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b13e4b07f02db6a3552","contributors":{"authors":[{"text":"Desborough, George A.","contributorId":101661,"corporation":false,"usgs":true,"family":"Desborough","given":"George","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":179498,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":65518,"text":"i2422 - 1995 - Controlled photomosaic of the MTM 00142 Quadrangle, Gordii Dorsum region of Mars","interactions":[],"lastModifiedDate":"2012-02-10T00:11:08","indexId":"i2422","displayToPublicDate":"1995-06-01T00:00:00","publicationYear":"1995","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":320,"text":"IMAP","code":"I","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"2422","subseriesTitle":"NONE","title":"Controlled photomosaic of the MTM 00142 Quadrangle, Gordii Dorsum region of Mars","language":"ENGLISH","doi":"10.3133/i2422","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1995, Controlled photomosaic of the MTM 00142 Quadrangle, Gordii Dorsum region of Mars: U.S. Geological Survey IMAP 2422, 1 remote-sensing image ;61 x 62 cm., on sheet 97 x 69 cm., folded in envelope 30 x 24 cm., https://doi.org/10.3133/i2422.","productDescription":"1 remote-sensing image ;61 x 62 cm., on sheet 97 x 69 cm., folded in envelope 30 x 24 cm.","costCenters":[],"links":[{"id":190068,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":100975,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/imap/2422/plate-1.pdf","size":"13307","linkFileType":{"id":1,"text":"pdf"}}],"scale":"502000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ 140,-2.5 ], [ 140,2.5 ], [ 145,2.5 ], [ 145,-2.5 ], [ 140,-2.5 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae2e4b07f02db688b8e","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":533905,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":18655,"text":"ofr9556 - 1995 - Extraction of metals from raw clinoptilolite-rich rocks exposed to water in heavy-metal-polluted drainages","interactions":[],"lastModifiedDate":"2012-02-02T00:07:28","indexId":"ofr9556","displayToPublicDate":"1995-06-01T00:00:00","publicationYear":"1995","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":"95-56","title":"Extraction of metals from raw clinoptilolite-rich rocks exposed to water in heavy-metal-polluted drainages","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr9556","usgsCitation":"Desborough, G.A., and Frishman, D., 1995, Extraction of metals from raw clinoptilolite-rich rocks exposed to water in heavy-metal-polluted drainages: U.S. Geological Survey Open-File Report 95-56, iii, 30 p. ill., map ;28 cm., https://doi.org/10.3133/ofr9556.","productDescription":"iii, 30 p. ill., map ;28 cm.","costCenters":[],"links":[{"id":151725,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1995/0056/report-thumb.jpg"},{"id":47992,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1995/0056/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a06e4b07f02db5f8a14","contributors":{"authors":[{"text":"Desborough, George A.","contributorId":101661,"corporation":false,"usgs":true,"family":"Desborough","given":"George","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":179501,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Frishman, David","contributorId":40214,"corporation":false,"usgs":true,"family":"Frishman","given":"David","email":"","affiliations":[],"preferred":false,"id":179500,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":29384,"text":"wri944003 - 1995 - Factors affecting water quality and net flux of solutes in two stream basins in the Quabbin Reservoir drainage basin, central Massachusetts, 1983-85","interactions":[],"lastModifiedDate":"2022-02-16T21:40:08.31276","indexId":"wri944003","displayToPublicDate":"1995-06-01T00:00:00","publicationYear":"1995","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":"94-4003","title":"Factors affecting water quality and net flux of solutes in two stream basins in the Quabbin Reservoir drainage basin, central Massachusetts, 1983-85","docAbstract":"The factors that affect stream-water quality were studied at West Branch Swift River (Swift River), and East Branch Fever Brook (Fever Brook), two forested watersheds that drain into the Quabbin Reservoir, central Massachusetts, from December 1983 through August 1985. Spatial and temporal variations of chemistry of precipitation, surface water; and ground water and the linkages between chemical changes and hydrologic processes were used to identify the mechanisms that control stream chemistry. Precipitation chemistry was dominated by hydrogen ion (composite p.H 4.23), sulfate, and nitrate. Inputs of hydrogen and nitrate from pre- cipitation were almost entirely retained in the basins, whereas input of sulfate was approximately balanced by export by streamflow draining the basins. Both streams were poorly buffered, with mean pH near 5.7, mean alkalinity less than 30 microequivalents per liter, and sulfate concen- trations greater than 130 microequivalents per liter. Sodium and chloride, derived primarily from highway deicing salts, were the dominant solutes at Fever Brook. After adjustments for deicing salts, fluxes of base cations during the 21-month study were 2,014 and 1,429 equivalents per hectare in Swift River and Fever Brook, respectively. Base cation fluxes were controlled primarily by weathering of hornblende (Fever Brook) and plagioclase (Swift River). The overall weathering rate was greater in the Swift River Basin because easily weathered gabbro underlies one subbasin which comprises 11.2 percent of the total basin area but contributed about 77 percent of the total alkalinity. Alkalinity export was nearly equal in the two basins, however, because some alkalinity was generated in wetlands in the Fever Brook Basin through bacterial sulfate reduction coupled with organic-carbon oxidation.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri944003","usgsCitation":"Rittmaster, R., and Shanley, J.B., 1995, Factors affecting water quality and net flux of solutes in two stream basins in the Quabbin Reservoir drainage basin, central Massachusetts, 1983-85: U.S. Geological Survey Water-Resources Investigations Report 94-4003, v, 66 p., https://doi.org/10.3133/wri944003.","productDescription":"v, 66 p.","costCenters":[],"links":[{"id":58230,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1994/4003/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":123548,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1994/4003/report-thumb.jpg"},{"id":396050,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_47918.htm"}],"country":"United States","state":"Massachusetts","otherGeospatial":"Quabbin Reservoir drainage basin","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -72.4167,\n              42.4583\n            ],\n            [\n              -72.1833,\n              42.4583\n            ],\n            [\n              -72.1833,\n              42.5458\n            ],\n            [\n              -72.4167,\n              42.5458\n            ],\n            [\n              -72.4167,\n              42.4583\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a05e4b07f02db5f879b","contributors":{"authors":[{"text":"Rittmaster, R. L.","contributorId":55861,"corporation":false,"usgs":true,"family":"Rittmaster","given":"R. L.","affiliations":[],"preferred":false,"id":201444,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Shanley, J. B.","contributorId":52226,"corporation":false,"usgs":true,"family":"Shanley","given":"J.","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":201443,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":35240,"text":"b2094B - 1995 - Lead isotopes from the Upper Mississippi Valley district: A regional perspective","interactions":[],"lastModifiedDate":"2022-05-02T20:06:00.095314","indexId":"b2094B","displayToPublicDate":"1995-06-01T00:00:00","publicationYear":"1995","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":"2094","chapter":"B","title":"Lead isotopes from the Upper Mississippi Valley district: A regional perspective","docAbstract":"New lead isotopic data on galena from within and peripheral to the Upper Mississippi Valley lead-zinc district make it possible, by extending coverage to outlying locations, to trace the pathway traversed by the mineralizing fluids beyond the boundary of the main district. All but one of the samples exhibit elevated ratios of the radiogenic isotopes typical of the Upper Mississippi Valley ore deposits; 206PbP04Pb ranges from 19.38 to 24.46, 207PbP04Pb ranges from 15.73 to 16.24, and 208PbP04Pb ranges from 39.24 to 43.69. Galena from the Pints quarry near Waterloo, Iowa, has distinctly lower values of these ratios and may not be related paragenetically to the other samples. Otherwise, the lowest ratios are for samples in the southern part of the region in north-central Illinois, and the highest ratios are for samples to the northeast of the main district in the vicinity of Madison, Wisconsin. Thus, an isotopic pattern rather similar to that observed originally by Heyl and others (1966) prevails regionally, although the predominant fluid flow is now believed to have emanated from the Illinois Basin rather than from the Forest City Basin. Metal-bearing brines being driven northward out of the Illinois Basin probably played the key role in mineralization of the Upper Mississippi Valley district.\r\n\r\nBoth the new and the previously reported lead ratios for the Upper Mississippi Valley district are plotted on 207PbP04Pb and Pb208/pb204Pb versus 206PbP04Pb diagrams, which permit their comparison and the calculation of refined slopes for the expanded data set. A two-stage model age for the time of mineralization can be determined from the 207PbP04Pb_Pb206/Pb204 slope, provided that the source age of the lead is known. With our limited know ledge of this source age, the time of mineralization cannot be tightly constrained but is permissive of a Permian or younger lateral secretion event, as suggested by other geochronological results.","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Evolution of sedimentary basins - Illinois Basin","largerWorkSubtype":{"id":5,"text":"USGS Numbered Series"},"language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/b2094B","usgsCitation":"Millen, T.M., Zartman, R.E., and Heyl, A.V., 1995, Lead isotopes from the Upper Mississippi Valley district: A regional perspective: U.S. Geological Survey Bulletin 2094, iii, 13 p., https://doi.org/10.3133/b2094B.","productDescription":"iii, 13 p.","costCenters":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"links":[{"id":167399,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/bul/2094b/report-thumb.jpg"},{"id":63119,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/bul/2094b/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":399986,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_22394.htm"}],"country":"United States","state":"Illinois, Iowa, Wisconsin","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -92.25,\n              41.5\n            ],\n            [\n              -88,\n              41.5\n            ],\n            [\n              -88,\n              43.5\n            ],\n            [\n              -92.25,\n              43.5\n            ],\n            [\n              -92.25,\n              41.5\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1be4b07f02db6a8945","contributors":{"authors":[{"text":"Millen, Timothy M.","contributorId":79538,"corporation":false,"usgs":true,"family":"Millen","given":"Timothy","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":214306,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Zartman, Robert E.","contributorId":47356,"corporation":false,"usgs":true,"family":"Zartman","given":"Robert","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":214305,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Heyl, Allen Van","contributorId":91078,"corporation":false,"usgs":true,"family":"Heyl","given":"Allen","email":"","middleInitial":"Van","affiliations":[],"preferred":false,"id":214307,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70203373,"text":"70203373 - 1995 - The biogeochemistry of wetlands in the San Luis Valley, Colorado: The effects of acid drainage from natural and mine sources","interactions":[],"lastModifiedDate":"2019-05-10T08:59:07","indexId":"70203373","displayToPublicDate":"1995-05-08T11:35:31","publicationYear":"1995","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":9,"text":"Other Report"},"title":"The biogeochemistry of wetlands in the San Luis Valley, Colorado: The effects of acid drainage from natural and mine sources","docAbstract":"<p>The Summitville Mine, located near the old mining town of Summitville in Rio Grande County, Colorado, operated between July 1986 and December 1992 as a large-tonnage open-pit heap-leach gold mine. During its 6 years of existence the trace metal levels in drainage water from the mine site were elevated over historical (pre-1986) levels (Moran and Wentz, 1974) due to input from three sources—heap leach water, seeps that occur throughout the mine workings, and an increase in the metal load of water coming from the old Reynolds Adit. Mine-drainage waters flow into Wightman Fork, a small tributary of the Alamosa River, which in turn flows east into the San Luis Valley. The increase in the trace metal burden of the Alamosa River watershed is of concern to farmers, land owners, and Federal and State wildlife agencies.</p><p><br>The information presented here is largely abstracted from reports previously published (Balistrieri and others, 1995; Gough and others, 1995).<br></p>","language":"English","publisher":"Colorado Geological Survey","usgsCitation":"Gough, L.P., Balistrieri, L.S., Lichte, F., Yanosky, T., Severson, R.C., and Archuleta, A., 1995, The biogeochemistry of wetlands in the San Luis Valley, Colorado: The effects of acid drainage from natural and mine sources, 7 p.","productDescription":"7 p.","costCenters":[{"id":211,"text":"Crustal Geophysics and Geochemistry Science Center","active":true,"usgs":true},{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"links":[{"id":363594,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":363593,"rank":1,"type":{"id":11,"text":"Document"},"url":"https://2fdpn7hy0ht206jws2e9og41.wpengine.netdna-cdn.com/wp-content/uploads/2013/08/11.pdf"}],"country":"United States","state":"Colorado","otherGeospatial":"San Luis Valley","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Gough, Larry P. lgough@usgs.gov","contributorId":1230,"corporation":false,"usgs":true,"family":"Gough","given":"Larry","email":"lgough@usgs.gov","middleInitial":"P.","affiliations":[],"preferred":true,"id":762368,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Balistrieri, Laurie S. 0000-0002-6359-3849 balistri@usgs.gov","orcid":"https://orcid.org/0000-0002-6359-3849","contributorId":1406,"corporation":false,"usgs":true,"family":"Balistrieri","given":"Laurie","email":"balistri@usgs.gov","middleInitial":"S.","affiliations":[{"id":200,"text":"Coop Res Unit Seattle","active":true,"usgs":true},{"id":191,"text":"Colorado Water Science Center","active":true,"usgs":true},{"id":662,"text":"Western Mineral and Environmental Resources Science Center","active":true,"usgs":true},{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"preferred":true,"id":762369,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Lichte, F.E.","contributorId":99108,"corporation":false,"usgs":true,"family":"Lichte","given":"F.E.","affiliations":[],"preferred":false,"id":762370,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Yanosky, T.M.","contributorId":42263,"corporation":false,"usgs":true,"family":"Yanosky","given":"T.M.","email":"","affiliations":[],"preferred":false,"id":762371,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Severson, Ronald C.","contributorId":104885,"corporation":false,"usgs":true,"family":"Severson","given":"Ronald","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":762372,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Archuleta, A.S.","contributorId":55374,"corporation":false,"usgs":true,"family":"Archuleta","given":"A.S.","email":"","affiliations":[],"preferred":false,"id":762373,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}}
,{"id":1003115,"text":"1003115 - 1995 - Responses of bluegills and black crappies to dissolved oxygen, temperature, and current in backwater lakes of the upper Mississippi River during winter","interactions":[],"lastModifiedDate":"2025-03-27T17:19:31.92655","indexId":"1003115","displayToPublicDate":"1995-05-05T00:00:00","publicationYear":"1995","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2886,"text":"North American Journal of Fisheries Management","active":true,"publicationSubtype":{"id":10}},"title":"Responses of bluegills and black crappies to dissolved oxygen, temperature, and current in backwater lakes of the upper Mississippi River during winter","docAbstract":"<p><span>We conducted a radiotelemetry study to examine the effects of dissolved oxygen (DO), water temperature, and current velocity on winter habitat selection by bluegills&nbsp;</span><i>Lepomis macrochirus</i><span>&nbsp;and black crappies&nbsp;</span><i>Pomoxis nigromaculatus</i><span>&nbsp;in the Finger Lakes backwater complex, Pool 5, on the upper Mississippi River. When DO was above 2 mg/L, both species selected areas with water temperature greater than 1°C and undetectable current. As dissolved oxygen concentrations fell below 2 mg/L, fish moved to areas with higher DO, despite water temperatures of 1°C and lower and current velocities of 1 cm/s. Areas with water temperature less than 1°C and current velocity greater than 1 cm/s were avoided. To incorporate the winter habitat requirements of bluegills and black crappies into habitat restoration projects, we recommend designs that allow the inflow of oxygenated water to maintain adequate DO without substantially decreasing temperature and increasing current velocity.</span></p>","language":"English","publisher":"Wiley","doi":"10.1577/1548-8675(1995)015<0390:ROBABC>2.3.CO;2","usgsCitation":"Knights, B., Johnson, B., and Sandheinrich, M., 1995, Responses of bluegills and black crappies to dissolved oxygen, temperature, and current in backwater lakes of the upper Mississippi River during winter: North American Journal of Fisheries Management, v. 15, no. 2, p. 390-399, https://doi.org/10.1577/1548-8675(1995)015<0390:ROBABC>2.3.CO;2.","productDescription":"10 p.","startPage":"390","endPage":"399","costCenters":[{"id":606,"text":"Upper Midwest Environmental Sciences Center","active":true,"usgs":true}],"links":[{"id":134407,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Minnesota","otherGeospatial":"Finger Lakes, upper Mississippi River","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -92.206752114294,\n              44.45479584495959\n            ],\n            [\n              -92.206752114294,\n              44.191646363835275\n            ],\n            [\n              -91.81219600968318,\n              44.191646363835275\n            ],\n            [\n              -91.81219600968318,\n              44.45479584495959\n            ],\n            [\n              -92.206752114294,\n              44.45479584495959\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","volume":"15","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a1ae4b07f02db6062b6","contributors":{"authors":[{"text":"Knights, B.C. 0000-0001-8526-8468","orcid":"https://orcid.org/0000-0001-8526-8468","contributorId":42937,"corporation":false,"usgs":true,"family":"Knights","given":"B.C.","affiliations":[],"preferred":false,"id":312761,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Johnson, Barry L.","contributorId":95009,"corporation":false,"usgs":true,"family":"Johnson","given":"Barry L.","affiliations":[],"preferred":false,"id":312763,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Sandheinrich, M.B.","contributorId":76263,"corporation":false,"usgs":true,"family":"Sandheinrich","given":"M.B.","affiliations":[],"preferred":false,"id":312762,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70170589,"text":"70170589 - 1995 - Transport of agricultural chemicals to ground water, Princeton, Minnesota, 1991-93","interactions":[],"lastModifiedDate":"2018-03-12T10:37:36","indexId":"70170589","displayToPublicDate":"1995-05-01T14:15:00","publicationYear":"1995","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"Transport of agricultural chemicals to ground water, Princeton, Minnesota, 1991-93","docAbstract":"<p>No abstract available.</p>","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Clean Water - Clean Environment - 21st Century","largerWorkSubtype":{"id":12,"text":"Conference publication"},"conferenceTitle":"Clean Water - Clean Environment - 21st Century","conferenceDate":"March 5-8, 1995","conferenceLocation":"Kansas City, MO","language":"English","publisher":"American Society of Agricultural Engineers","publisherLocation":"Kansas City, MO","usgsCitation":"Delin, G., 1995, Transport of agricultural chemicals to ground water, Princeton, Minnesota, 1991-93, <i>in</i> Clean Water - Clean Environment - 21st Century, Kansas City, MO, March 5-8, 1995, p. 57-60.","productDescription":"4 p.","startPage":"57","endPage":"60","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":392,"text":"Minnesota Water Science Center","active":true,"usgs":true}],"links":[{"id":320598,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Minnesota","city":"Princeton","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5721e2cfe4b0b13d39130442","contributors":{"authors":[{"text":"Delin, G. N.","contributorId":12834,"corporation":false,"usgs":true,"family":"Delin","given":"G. N.","affiliations":[],"preferred":false,"id":627782,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":6703,"text":"fs00295_moore - 1995 - Assessment of ground-water supply potential of bedrock in New Hampshire","interactions":[],"lastModifiedDate":"2012-02-02T00:05:46","indexId":"fs00295_moore","displayToPublicDate":"1995-05-01T00:00:00","publicationYear":"1995","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":313,"text":"Fact Sheet","code":"FS","onlineIssn":"2327-6932","printIssn":"2327-6916","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"002-95","title":"Assessment of ground-water supply potential of bedrock in New Hampshire","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/fs00295_moore","usgsCitation":"Moore, R.B., and Clark, S.F., 1995, Assessment of ground-water supply potential of bedrock in New Hampshire: U.S. Geological Survey Fact Sheet 002-95, 1 sheet : ill. ; 28 cm. ill. ;, https://doi.org/10.3133/fs00295_moore.","productDescription":"1 sheet : ill. ; 28 cm. ill. ;","costCenters":[],"links":[{"id":118439,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/fs/1995/0002/report-thumb.jpg"},{"id":34100,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/fs/1995/0002/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4abae4b07f02db671f85","contributors":{"authors":[{"text":"Moore, Richard Bridge","contributorId":90712,"corporation":false,"usgs":true,"family":"Moore","given":"Richard","email":"","middleInitial":"Bridge","affiliations":[],"preferred":false,"id":153188,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Clark, Stewart F. 0000-0001-8841-2728 sclark@usgs.gov","orcid":"https://orcid.org/0000-0001-8841-2728","contributorId":3658,"corporation":false,"usgs":true,"family":"Clark","given":"Stewart","email":"sclark@usgs.gov","middleInitial":"F.","affiliations":[{"id":466,"text":"New England Water Science Center","active":true,"usgs":true}],"preferred":true,"id":153187,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":6641,"text":"fs09095 - 1995 - Water-quality assessment of the Trinity River Basin, Texas—Data collection, 1992–95","interactions":[],"lastModifiedDate":"2016-08-16T15:52:17","indexId":"fs09095","displayToPublicDate":"1995-05-01T00:00:00","publicationYear":"1995","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":313,"text":"Fact Sheet","code":"FS","onlineIssn":"2327-6932","printIssn":"2327-6916","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"090-95","title":"Water-quality assessment of the Trinity River Basin, Texas—Data collection, 1992–95","docAbstract":"<p>Assessment activities in the Trinity River Basin study unit of the National Water-Quality Assessment (NAWQA) Program began in October 1991 with 2 years dedicated to planning, analyzing existing information, and designing data-collection networks. In October 1993, a 3-year intensive data-collection program was initiated. Guidelines were provided by the NAWQA Program National Synthesis team, and suggestions for networks and surveys were made by the study unit&rsquo;s liaison committee. This fact sheet describes the data-collection activities.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Austin, TX","doi":"10.3133/fs09095","usgsCitation":"Land, L.F., 1995, Water-quality assessment of the Trinity River Basin, Texas—Data collection, 1992–95: U.S. Geological Survey Fact Sheet 090-95, 2 p., https://doi.org/10.3133/fs09095.","productDescription":"2 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"links":[{"id":122638,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/fs_090_95.bmp"},{"id":690,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/fs09095/","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Texas","otherGeospatial":"Trinity River Basin","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e5e4b07f02db5e6dbb","contributors":{"authors":[{"text":"Land, Larry F.","contributorId":60612,"corporation":false,"usgs":true,"family":"Land","given":"Larry","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":153088,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":5074,"text":"fs07995 - 1995 - Aerial infrared surveys in the investigation of geothermal and volcanic heat sources","interactions":[],"lastModifiedDate":"2012-02-02T00:05:51","indexId":"fs07995","displayToPublicDate":"1995-05-01T00:00:00","publicationYear":"1995","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":313,"text":"Fact Sheet","code":"FS","onlineIssn":"2327-6932","printIssn":"2327-6916","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"079-95","title":"Aerial infrared surveys in the investigation of geothermal and volcanic heat sources","docAbstract":"This factsheet briefly summarizes and clarifies the application of aerial infrared surveys in geophysical exploration for geothermal energy sources and environmental monitoring for potential volcanic hazards.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/fs07995","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1995, Aerial infrared surveys in the investigation of geothermal and volcanic heat sources: U.S. Geological Survey Fact Sheet 079-95, [4] p. : ill. ; 28 cm. ill. ;, https://doi.org/10.3133/fs07995.","productDescription":"[4] p. : ill. ; 28 cm. ill. ;","costCenters":[],"links":[{"id":139787,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b02e4b07f02db698d70","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":528435,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":6660,"text":"fs07394 - 1995 - Floods in southeast Texas, October 1994","interactions":[],"lastModifiedDate":"2016-08-16T15:43:47","indexId":"fs07394","displayToPublicDate":"1995-05-01T00:00:00","publicationYear":"1995","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":313,"text":"Fact Sheet","code":"FS","onlineIssn":"2327-6932","printIssn":"2327-6916","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"073-94","title":"Floods in southeast Texas, October 1994","docAbstract":"<p>Rainfall in southeast Texas, which ranged in amounts from about 8 to more than 28 inches during October 15&ndash;19, 1994, caused severe flooding in parts of a 38-county area. A combination of meteorological events&mdash;residual atmospheric moisture over southern Texas associated with Hurricane Rosa from the Pacific Coast of Mexico and low-level moisture from the Gulf of Mexico drawn inland to a warm front by a strong low-pressure system over the southern Rocky Mountains&mdash;spawned vigorous thunderstorms that produced rainfall amounts that may exceed records for the area.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Houston, TX","doi":"10.3133/fs07394","usgsCitation":"Liscum, F., and East, J., 1995, Floods in southeast Texas, October 1994: U.S. Geological Survey Fact Sheet 073-94, 2 p., https://doi.org/10.3133/fs07394.","productDescription":"2 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"links":[{"id":719,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/fs-073-94/","linkFileType":{"id":5,"text":"html"}},{"id":117419,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/fs_073_94.bmp"}],"country":"United States","state":"Texas","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e2e4b07f02db5e4a21","contributors":{"authors":[{"text":"Liscum, Fred","contributorId":95463,"corporation":false,"usgs":true,"family":"Liscum","given":"Fred","email":"","affiliations":[],"preferred":false,"id":153116,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"East, Jeffery W. jweast@usgs.gov","contributorId":1683,"corporation":false,"usgs":true,"family":"East","given":"Jeffery W.","email":"jweast@usgs.gov","affiliations":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"preferred":true,"id":153115,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70185367,"text":"70185367 - 1995 - Combining the Neuman and Boulton models for flow to a well in an unconfined aquifer","interactions":[],"lastModifiedDate":"2017-03-21T12:06:52","indexId":"70185367","displayToPublicDate":"1995-05-01T00:00:00","publicationYear":"1995","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3825,"text":"Groundwater","active":true,"publicationSubtype":{"id":10}},"title":"Combining the Neuman and Boulton models for flow to a well in an unconfined aquifer","docAbstract":"<p><span>A Laplace transform solution is presented for flow to a well in a homogeneous, water-table aquifer with noninstanta-neous drainage of water from the zone above the water table. The Boulton convolution integral is combined with Darcy's law and used as an upper boundary condition to replace the condition used by Neuman. Boulton's integral derives from the assumption that water drained from the unsaturated zone is released gradually in a manner that varies exponentially with time in response to a unit decline in hydraulic head, whereas the condition used by Newman assumes that the water is released instantaneously. The result is a solution that reduces to the solution obtained by Neuman as the rate of release of water from the zone above the water table increases. A dimensionless fitting parameter, </span><i>γ</i><span>, is introduced that incorporates vertical hydraulic conductivity, saturated thickness, specific yield, and an empirical constant </span><i>α</i><sub>1</sub><span>, similar to Boulton's </span><i>α</i><span>. Results show that theoretical drawdown in water-table piezometers is amplified by noninstantaneous drainage from the unsaturated zone to a greater extent than drawdown in piezometers located at depth in the saturated zone. This difference provides a basis for evaluating </span><i>γ</i><span> by type-curve matching in addition to the other dimensionless parameters. Analysis of drawdown in selected piezometers from the published results of two aquifer tests conducted in relatively homogeneous glacial outwash deposits but with significantly different hydraulic conductivities reveals improved comparison between the theoretical type curves and the hydraulic head measured in water-table piezometers.</span></p>","language":"English","publisher":"Wiley","doi":"10.1111/j.1745-6584.1995.tb00293.x","usgsCitation":"Moench, A.F., 1995, Combining the Neuman and Boulton models for flow to a well in an unconfined aquifer: Groundwater, v. 33, no. 3, p. 378-384, https://doi.org/10.1111/j.1745-6584.1995.tb00293.x.","productDescription":"7 p. ","startPage":"378","endPage":"384","costCenters":[{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":337928,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"33","issue":"3","noUsgsAuthors":false,"publicationDate":"2005-08-04","publicationStatus":"PW","scienceBaseUri":"58d23b94e4b0236b68f82922","contributors":{"authors":[{"text":"Moench, Allen F. afmoench@usgs.gov","contributorId":3903,"corporation":false,"usgs":true,"family":"Moench","given":"Allen","email":"afmoench@usgs.gov","middleInitial":"F.","affiliations":[],"preferred":true,"id":685352,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":6597,"text":"fs13295 - 1995 - Echo-sounding method aids earthquake hazard studies","interactions":[],"lastModifiedDate":"2014-04-03T09:24:42","indexId":"fs13295","displayToPublicDate":"1995-05-01T00:00:00","publicationYear":"1995","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":313,"text":"Fact Sheet","code":"FS","onlineIssn":"2327-6932","printIssn":"2327-6916","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"132-95","title":"Echo-sounding method aids earthquake hazard studies","docAbstract":"<p>Dramatic examples of catastrophic damage from an earthquake occurred in 1989, when the M 7.1 Lorna Prieta rocked \nthe San Francisco Bay area, and in 1994, when the M 6.6 Northridge earthquake jolted southern California. The \nsurprising amount and distribution of damage to private property and infrastructure emphasizes the importance of \nseismic-hazard research in urbanized areas, where the potential for damage and loss of life is greatest.</p>\n<br/>\n<p>During April 1995, a group of scientists from the U.S. Geological Survey and the University of \nTennessee, using an echo-sounding method described below, is collecting data in San Antonio \nPark, California, to examine the Monte Vista fault which runs through this park. The Monte Vista \nfault in this vicinity shows evidence of movement within the last 10,000 years or so. The data will \ngive them a \"picture\" of the subsurface rock deformation near this fault. The data will also be used \nto help locate a trench that will be dug across the fault by scientists from William Lettis & \nAssociates.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/fs13295","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1995, Echo-sounding method aids earthquake hazard studies: U.S. Geological Survey Fact Sheet 132-95, 1 p., https://doi.org/10.3133/fs13295.","productDescription":"1 p.","numberOfPages":"1","costCenters":[],"links":[{"id":140000,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/fs13295.jpg"},{"id":285408,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/fs/0132-95/report.pdf"}],"country":"United States","state":"California","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -123.0,37.0 ], [ -123.0,39.0 ], [ -121.0,39.0 ], [ -121.0,37.0 ], [ -123.0,37.0 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a4ee4b07f02db627eba","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":528746,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":4488,"text":"cir1120H - 1995 - Flood volumes in the upper Mississippi River basin, April 1 through September 30, 1993","interactions":[],"lastModifiedDate":"2018-03-16T14:06:45","indexId":"cir1120H","displayToPublicDate":"1995-05-01T00:00:00","publicationYear":"1995","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":"1120","chapter":"H","title":"Flood volumes in the upper Mississippi River basin, April 1 through September 30, 1993","docAbstract":"<p>Previous maximum flows on many streams and rivers were exceeded during the flood of 1993 in the upper Mississippi River Basin. Not only were peak discharges exceeded at many streamflow-gaging stations, but flood volumes were significantly higher than previous maximums. Rainfall amounts that were greater than 50 inches were recorded in parts of Kansas, Missouri, and Iowa from April 1 through September 30, 1993 . As a result of the excess rainfall, 53 of the 60 stations discussed in this report had flow volumes that were greater than twice the mean flow volume for April through September. The Mississippi River at St. Louis, Missouri, remained above flood stage for 144 days from April 1 to September 30, 1993, compared with 81 days during the 1973 flood. Of the 60 stations, 24 recorded new maximum 3-day flood volumes, and 47 recorded new maximum 120- day flood volumes. This indicates that the flooding of 1993 is significant with respect to its long duration and magnitude of flow . The same aspect is indicated in the frequency analysis of the 1993 flood. During the 1993 flood, the 100- year 3-day flows were exceeded at 22 stations, and the 120-day flows were exceeded at 43 stations.&nbsp;</p>","language":"English","publisher":"U.S. Government Printing Office","publisherLocation":"Washington, D.C.","doi":"10.3133/cir1120H","usgsCitation":"Southard, R.E., 1995, Flood volumes in the upper Mississippi River basin, April 1 through September 30, 1993: U.S. Geological Survey Circular 1120, v, 32 p., https://doi.org/10.3133/cir1120H.","productDescription":"v, 32 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":351,"text":"Iowa Water Science Center","active":true,"usgs":true},{"id":478,"text":"North Dakota Water Science Center","active":true,"usgs":true},{"id":34685,"text":"Dakota Water Science Center","active":true,"usgs":true}],"links":[{"id":533,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/circ1120-h","linkFileType":{"id":5,"text":"html"}},{"id":123580,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/cir_1120_H.bmp"}],"country":"United States","otherGeospatial":"Upper Mississippi River basin","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -87.802734375,\n              42.66628070564928\n            ],\n            [\n              -87.802734375,\n              42.35854391749705\n            ],\n            [\n              -87.8466796875,\n              42.22851735620852\n            ],\n            [\n              -87.64892578125,\n              42.08191667830631\n            ],\n            [\n              -87.4951171875,\n              41.72213058512578\n            ],\n   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      42.87596410238254\n            ],\n            [\n              -87.802734375,\n              42.66628070564928\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","tableOfContents":"<ul>\n<li>Foreword</li>\n<li>Abstract</li>\n<li>Introduction</li>\n<li>Precipitation, April 1 through September 30, 1993</li>\n<li>Flood volumes, April 1 through September 30, 1993</li>\n<li>Effects of reservoirs on floods</li>\n<li>Elevation and contents of selected reservoirs</li>\n<li>Summary</li>\n<li>Selected references</li>\n</ul>","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49dfe4b07f02db5e3c13","contributors":{"authors":[{"text":"Southard, Rodney E. 0000-0001-8024-9698 southard@usgs.gov","orcid":"https://orcid.org/0000-0001-8024-9698","contributorId":3880,"corporation":false,"usgs":true,"family":"Southard","given":"Rodney","email":"southard@usgs.gov","middleInitial":"E.","affiliations":[],"preferred":true,"id":149324,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":65594,"text":"i2413 - 1995 - Controlled photomosaic of the MTM 45002 Quadrangle, Acidalia Planitia region of Mars","interactions":[],"lastModifiedDate":"2012-02-10T00:11:06","indexId":"i2413","displayToPublicDate":"1995-05-01T00:00:00","publicationYear":"1995","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":320,"text":"IMAP","code":"I","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"2413","subseriesTitle":"NONE","title":"Controlled photomosaic of the MTM 45002 Quadrangle, Acidalia Planitia region of Mars","language":"ENGLISH","doi":"10.3133/i2413","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1995, Controlled photomosaic of the MTM 45002 Quadrangle, Acidalia Planitia region of Mars: U.S. Geological Survey IMAP 2413, 1 remote-sensing image ;62 x 45 cm., on sheet 97 x 57 cm., folded in envelope 30 x 24 cm., https://doi.org/10.3133/i2413.","productDescription":"1 remote-sensing image ;62 x 45 cm., on sheet 97 x 57 cm., folded in envelope 30 x 24 cm.","costCenters":[],"links":[{"id":190460,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":101044,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/imap/2413/plate-1.pdf","size":"12498","linkFileType":{"id":1,"text":"pdf"}}],"scale":"502000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ 0,42.5 ], [ 0,47.5 ], [ 5,47.5 ], [ 5,42.5 ], [ 0,42.5 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae0e4b07f02db6880db","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":533982,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":5512,"text":"fs08895 - 1995 - National Water-Quality Assessment Program— Pesticides in the Trinity River Basin study unit, Texas, 1968-91","interactions":[],"lastModifiedDate":"2016-08-16T15:49:56","indexId":"fs08895","displayToPublicDate":"1995-05-01T00:00:00","publicationYear":"1995","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":313,"text":"Fact Sheet","code":"FS","onlineIssn":"2327-6932","printIssn":"2327-6916","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"088-95","title":"National Water-Quality Assessment Program— Pesticides in the Trinity River Basin study unit, Texas, 1968-91","docAbstract":"<p>The Trinity River Basin National Water Quality Assessment (NAWQA) study-unit staff began assessment activities in 1991, and in 1992, undertook a retrospective review of existing data on pesticides. The main purpose of this review was to aid in the design of a pesticide-sampling network for the study unit. The review consisted of the compilation, screening, and analysis of available pesticide-sample information. In addition, important environmental factors, which influence the occurrence and distribution of pesticides in the study unit, were identified and compiled. A report of this review and analysis will be released in 1995 (Ulery and Brown, in press). This fact sheet provides a brief overview of significant findings.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Austin, TX","doi":"10.3133/fs08895","usgsCitation":"Ulery, R., 1995, National Water-Quality Assessment Program— Pesticides in the Trinity River Basin study unit, Texas, 1968-91: U.S. Geological Survey Fact Sheet 088-95, 2 p., https://doi.org/10.3133/fs08895.","productDescription":"2 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"links":[{"id":117887,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/fs_088_95.bmp"},{"id":110,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/fs-088-95/","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Texas","otherGeospatial":"Trinity River Basin","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b01e4b07f02db69864d","contributors":{"authors":[{"text":"Ulery, R.L.","contributorId":46507,"corporation":false,"usgs":true,"family":"Ulery","given":"R.L.","email":"","affiliations":[],"preferred":false,"id":151109,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70185371,"text":"70185371 - 1995 - Measurements of aquifer-storage change and specific yield using gravity surveys","interactions":[],"lastModifiedDate":"2017-03-21T12:21:41","indexId":"70185371","displayToPublicDate":"1995-05-01T00:00:00","publicationYear":"1995","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3825,"text":"Groundwater","active":true,"publicationSubtype":{"id":10}},"title":"Measurements of aquifer-storage change and specific yield using gravity surveys","docAbstract":"<p>Pinal Creek is an intermittent stream that drains a 200-square-mile alluvial basin in central Arizona. Large changes in water levels and aquifer storage occur in an alluvial aquifer near the stream in response to periodic recharge and ground-water withdrawals. Outflow components of the ground-water budget and hydraulic properties of the alluvium are well-defined by field measurements; however, data are insufficient to adequately describe recharge, aquifer-storage change, and specific-yield values. An investigation was begun to assess the utility of temporal-gravity surveys to directly measure aquifer-storage change and estimate values of specific yield.</p><p>The temporal-gravity surveys measured changes in the differences in gravity between two reference stations on bedrock and six stations at wells; changes are caused by variations in aquifer storage. Specific yield was estimated by dividing storage change by water-level change. Four surveys were done between February 21, 1991, and March 31, 1993. Gravity increased as much as 158 microGal ± 1 to 6 microGal, and water levels rose as much as 58 feet. Average specific yield at wells ranged from 0.16 to 0.21, and variations in specific yield with depth correlate with lithologic variations. Results indicate that temporal-gravity surveys can be used to estimate aquifer-storage change and specific yield of water-table aquifers where significant variations in water levels occur. Direct measurement of aquifer-storage change can eliminate a major unknown from the ground-water budget of arid basins and improve residual estimates of recharge.</p>","language":"English","publisher":"Wiley","doi":"10.1111/j.1745-6584.1995.tb00299.x","usgsCitation":"Pool, D.R., and Eychaner, J., 1995, Measurements of aquifer-storage change and specific yield using gravity surveys: Groundwater, v. 33, no. 3, p. 425-432, https://doi.org/10.1111/j.1745-6584.1995.tb00299.x.","productDescription":"8 p. ","startPage":"425","endPage":"432","costCenters":[{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":337932,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"33","issue":"3","noUsgsAuthors":false,"publicationDate":"2005-08-04","publicationStatus":"PW","scienceBaseUri":"58d23b94e4b0236b68f82920","contributors":{"authors":[{"text":"Pool, D. R.","contributorId":75581,"corporation":false,"usgs":true,"family":"Pool","given":"D.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":685359,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Eychaner, J.H.","contributorId":34511,"corporation":false,"usgs":true,"family":"Eychaner","given":"J.H.","affiliations":[],"preferred":false,"id":685360,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70185365,"text":"70185365 - 1995 - Use of a square-array direct-current resistivity method to detect fractures in crystalline bedrock in New Hampshire","interactions":[],"lastModifiedDate":"2019-10-14T12:46:21","indexId":"70185365","displayToPublicDate":"1995-05-01T00:00:00","publicationYear":"1995","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3825,"text":"Groundwater","active":true,"publicationSubtype":{"id":10}},"title":"Use of a square-array direct-current resistivity method to detect fractures in crystalline bedrock in New Hampshire","docAbstract":"<p>Azimuthal square-array direct-current (dc) resistivity soundings were used to detect fractures in bedrock in the Mirror Lake watershed in Grafton County, New Hampshire. Soundings were conducted at a site where crystalline bedrock underlies approximately 7 m (meters) of glacial drift. Measured apparent resistivities changed with the orientation of the array. Graphical interpretation of the square-array data indicates that a dominant fracture set and (or) foliation in the bedrock is oriented at 030° (degrees). Interpretation of crossed square-array data indicates an orientation of 027° and an anisotropy factor of 1.31. Assuming that anisotropy is due to fractures, the secondary porosity is estimated to range from 0.01 to 0.10.</p><p>Interpretations of azimuthal square-array data are supported by other geophysical data, including azimuthal seismic-refraction surveys and azimuthal Schlumberger dc-resistivity soundings at the Camp Osceola well field. Dominant fracture trends indicated by these geophysical methods are 022° (seismic-refraction) and 037° (dc-resistivity). Fracture mapping of bedrock outcrops at a site within 250 m indicates that the maximum fracture-strike frequency is oriented at 030°.</p><p>The square-array dc-resistivity sounding method is more sensitive to a given rock anisotropy than the more commonly used Schlumberger and Wenner arrays. An additional advantage of the square-array method is that it requires about 65 percent less surface area than an equivalent survey using a Schlumberger or Wenner array.</p>","language":"English ","publisher":"Wiley","doi":"10.1111/j.1745-6584.1995.tb00304.x","usgsCitation":"Lane, J., Haeni, F., and Watson, W., 1995, Use of a square-array direct-current resistivity method to detect fractures in crystalline bedrock in New Hampshire: Groundwater, v. 33, no. 3, p. 476-485, https://doi.org/10.1111/j.1745-6584.1995.tb00304.x.","productDescription":"10 p. ","startPage":"476","endPage":"485","costCenters":[{"id":493,"text":"Office of Ground Water","active":true,"usgs":true},{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":337926,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"New Hampshire","otherGeospatial":"Mirror Lake ","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -71.28607749938965,\n              43.65495633091365\n            ],\n            [\n              -71.30135536193848,\n              43.64557859436532\n            ],\n            [\n              -71.29483222961426,\n              43.62259384514501\n            ],\n            [\n              -71.27921104431152,\n              43.62228318022435\n            ],\n            [\n              -71.27483367919922,\n              43.62128904169025\n            ],\n            [\n              -71.27483367919922,\n              43.620232751485744\n            ],\n            [\n              -71.2708854675293,\n              43.61725018485249\n            ],\n            [\n              -71.26032829284668,\n              43.61408104569764\n            ],\n            [\n              -71.25543594360352,\n              43.61246534185104\n            ],\n            [\n              -71.25423431396483,\n              43.60842589232491\n            ],\n            [\n              -71.21526718139648,\n              43.628806806433296\n            ],\n            [\n              -71.23114585876465,\n              43.65365223004351\n            ],\n            [\n              -71.28607749938965,\n              43.65495633091365\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"33","issue":"3","noUsgsAuthors":false,"publicationDate":"2005-08-04","publicationStatus":"PW","scienceBaseUri":"58d23b94e4b0236b68f82924","contributors":{"authors":[{"text":"Lane, J.W. Jr.","contributorId":66723,"corporation":false,"usgs":true,"family":"Lane","given":"J.W.","suffix":"Jr.","email":"","affiliations":[],"preferred":false,"id":685344,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Haeni, F.P.","contributorId":87105,"corporation":false,"usgs":true,"family":"Haeni","given":"F.P.","affiliations":[],"preferred":false,"id":685345,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Watson, W.M.","contributorId":189601,"corporation":false,"usgs":false,"family":"Watson","given":"W.M.","email":"","affiliations":[],"preferred":false,"id":685346,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70185363,"text":"70185363 - 1995 - Effects of colloids on metal transport in a river receiving acid mine drainage, upper Arkansas River, Colorado, U.S.A.","interactions":[],"lastModifiedDate":"2019-02-22T07:42:43","indexId":"70185363","displayToPublicDate":"1995-05-01T00:00:00","publicationYear":"1995","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":835,"text":"Applied Geochemistry","active":true,"publicationSubtype":{"id":10}},"title":"Effects of colloids on metal transport in a river receiving acid mine drainage, upper Arkansas River, Colorado, U.S.A.","docAbstract":"<p><span>Inflows of metal-rich, acidic water that drain from mine dumps and tailings piles in the Leadville, Colorado, area enter the non-acidic water in the upper Arkansas River. Hydrous iron oxides precipitate as colloids and move downstream in suspension, particularly downstream from California Gulch, which has been the major source of metal loads. The colloids influence the concentrations of metals dissolved in the water and the concentrations in bed sediments. To determine the role of colloids, samples of water, colloids, and fine-grained bed sediment were obtained at stream-gaging sites on the upper Arkansas River and at the mouths of major tributaries over a 250-km reach. Dissolved and colloidal metal concentrations in the water column were operationally defined using tangential-flow filtration through 0.001-pm membranes to separate the water and the colloids. Surface-extractable and total bed sediment metal concentrations were obtained on the &lt;60-μm fraction of the bed sediment. The highest concentrations of metals in water, colloids, and bed sediments occurred just downstream from California Gulch. Iron dominated the colloid composition, but substantial concentrations of As, Cd, Cu, Mn, Pb, and Zn also occurred in the colloidal solids. The colloidal load decreased by one half in the first 50 km downstream from the mining inflows due to sedimentation of aggregated colloids to the streambed. Nevertheless, a substantial load of colloids was transported through the entire study reach to Pueblo Reservoir. Dissolved metals were dominated by Mn and Zn, and their concentrations remained relatively high throughout the 250-km reach. The composition of extractable and total metals in bed sediment for several kilometers downstream from California Gulch is similar to the composition of the colloids that settle to the bed. Substantial concentrations of Mn and Zn were extractable, which is consistent with sediment-water chemical reaction. Concentrations of Cd, Pb, and Zn in bed sediment clearly result from the influence of mining near Leadville. Concentrations of Fe and Cu in bed sediments are nearly equal to concentrations in colloids for about 10 km downstream from California Gulch. Farther downstream, concentrations of Fe and Cu in tributary sediments mask the signal of mining inflows. These results indicate that colloids indeed influence the occurrence and transport of metals in rivers affected by mining.</span></p>","language":"English","publisher":"Elsevier","doi":"10.1016/0883-2927(95)00011-8","usgsCitation":"Kimball, B.A., 1995, Effects of colloids on metal transport in a river receiving acid mine drainage, upper Arkansas River, Colorado, U.S.A.: Applied Geochemistry, v. 10, no. 3, p. 285-306, https://doi.org/10.1016/0883-2927(95)00011-8.","productDescription":"22 p. 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,{"id":70185383,"text":"70185383 - 1995 - Chemical and isotopic methods for quantifying ground-water recharge in a regional, semiarid environment","interactions":[],"lastModifiedDate":"2019-02-25T10:26:45","indexId":"70185383","displayToPublicDate":"1995-05-01T00:00:00","publicationYear":"1995","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3825,"text":"Groundwater","active":true,"publicationSubtype":{"id":10}},"title":"Chemical and isotopic methods for quantifying ground-water recharge in a regional, semiarid environment","docAbstract":"<p><span>The High Plains aquifer underlying the semiarid Southern High Plains of Texas and New Mexico, USA was used to illustrate solute and isotopic methods for evaluating recharge fluxes, runoff, and spatial and temporal distribution of recharge. The chloride mass-balance method can provide, under certain conditions, a time-integrated technique for evaluation of recharge flux to regional aquifers that is independent of physical parameters. Applying this method to the High Plains aquifer of the Southern High Plains suggests that recharge flux is approximately 2% of precipitation, or approximately 11 ± 2 mm/y, consistent with previous estimates based on a variety of physically based measurements. The method is useful because long-term average precipitation and chloride concentrations in rain and ground water have less uncertainty and are generally less expensive to acquire than physically based parameters commonly used in analyzing recharge. Spatial and temporal distribution of recharge was evaluated by use of δ</span><sup>2</sup><span>H, δ</span><sup>18</sup><span>O, and tritium concentrations in both ground water and the unsaturated zone. Analyses suggest that nearly half of the recharge to the Southern High Plains occurs as piston flow through playa basin floors that occupy approximately 6% of the area, and that macropore recharge may be important in the remaining recharge. Tritium and chloride concentrations in the unsaturated zone were used in a new equation developed to quantify runoff. Using this equation and data from a representative basin, runoff was found to be 24 ± 3 mm/y; that is in close agreement with values obtained from water-balance measurements on experimental watersheds in the area. Such geochemical estimates are possible because tritium is used to calculate a recharge flux that is independent of precipitation and runoff, whereas recharge flux based on chloride concentration in the unsaturated zone is dependent upon the amount of runoff. The difference between these two estimates yields the amount of runoff to the basin.</span></p>","language":"English","publisher":"Wiley","doi":"10.1111/j.1745-6584.1995.tb00302.x","usgsCitation":"Wood, W., and Sanford, W.E., 1995, Chemical and isotopic methods for quantifying ground-water recharge in a regional, semiarid environment: Groundwater, v. 33, no. 3, p. 458-468, https://doi.org/10.1111/j.1745-6584.1995.tb00302.x.","productDescription":"11 p. ","startPage":"458","endPage":"468","costCenters":[{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":337946,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"33","issue":"3","noUsgsAuthors":false,"publicationDate":"2005-08-04","publicationStatus":"PW","scienceBaseUri":"58d23b94e4b0236b68f8291e","contributors":{"authors":[{"text":"Wood, Warren W.","contributorId":47770,"corporation":false,"usgs":false,"family":"Wood","given":"Warren W.","affiliations":[{"id":6601,"text":"Michigan State University","active":true,"usgs":false}],"preferred":false,"id":685397,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Sanford, Ward E. 0000-0002-6624-0280 wsanford@usgs.gov","orcid":"https://orcid.org/0000-0002-6624-0280","contributorId":2268,"corporation":false,"usgs":true,"family":"Sanford","given":"Ward","email":"wsanford@usgs.gov","middleInitial":"E.","affiliations":[{"id":436,"text":"National Research Program - Eastern Branch","active":true,"usgs":true},{"id":37778,"text":"WMA - Integrated Modeling and Prediction Division","active":true,"usgs":true}],"preferred":true,"id":685398,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":5053,"text":"fs04695 - 1995 - U. S. Geological Survey programs in Virginia","interactions":[],"lastModifiedDate":"2012-02-02T00:05:42","indexId":"fs04695","displayToPublicDate":"1995-05-01T00:00:00","publicationYear":"1995","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":313,"text":"Fact Sheet","code":"FS","onlineIssn":"2327-6932","printIssn":"2327-6916","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"046-95","title":"U. S. Geological Survey programs in Virginia","language":"ENGLISH","publisher":"The Survey,","doi":"10.3133/fs04695","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1995, U. S. Geological Survey programs in Virginia: U.S. Geological Survey Fact Sheet 046-95, 4 p., https://doi.org/10.3133/fs04695.","productDescription":"4 p.","costCenters":[],"links":[{"id":368,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://water.usgs.gov/wid/html/va.html","linkFileType":{"id":5,"text":"html"}},{"id":123044,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/fs/1995/0046/report-thumb.jpg"},{"id":31867,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/fs/1995/0046/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a2ce4b07f02db613b08","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":528427,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":3868,"text":"cir1112 - 1995 - Design of the National Water-Quality Assessment Program; occurrence and distribution of water-quality conditions","interactions":[],"lastModifiedDate":"2012-02-02T00:05:36","indexId":"cir1112","displayToPublicDate":"1995-05-01T00:00:00","publicationYear":"1995","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":"1112","title":"Design of the National Water-Quality Assessment Program; occurrence and distribution of water-quality conditions","docAbstract":"The National Water-Quality Assessment Program assesses the status of and trends in the quality of the Nation's ground- and surface-water resources. The occurrence and distribution assessment component characterizes broad-scale water-quality conditions in relation to major contaminant sources and background conditions in each study area. The surface-water design focuses on streams. The ground-water design focuses on major aquifers, with emphasis on recently recharged ground water associated with human activities.","language":"ENGLISH","publisher":"U.S. Geological Survey ;\r\nU.S.G.S. Information Services [distributor],","doi":"10.3133/cir1112","usgsCitation":"Gilliom, R.J., Alley, W., and Gurtz, M.E., 1995, Design of the National Water-Quality Assessment Program; occurrence and distribution of water-quality conditions: U.S. Geological Survey Circular 1112, vi, 33 p. :ill. (chiefly col.), col. maps ;28 cm., https://doi.org/10.3133/cir1112.","productDescription":"vi, 33 p. :ill. (chiefly col.), col. maps ;28 cm.","costCenters":[],"links":[{"id":78,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/circ/circ1112/","linkFileType":{"id":5,"text":"html"}},{"id":120928,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/circ/1995/1112/report-thumb.jpg"},{"id":30960,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/1995/1112/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aa8e4b07f02db667e11","contributors":{"authors":[{"text":"Gilliom, Robert J. rgilliom@usgs.gov","contributorId":488,"corporation":false,"usgs":true,"family":"Gilliom","given":"Robert","email":"rgilliom@usgs.gov","middleInitial":"J.","affiliations":[{"id":451,"text":"National Water Quality Assessment Program","active":true,"usgs":true}],"preferred":true,"id":147757,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Alley, William M.","contributorId":93030,"corporation":false,"usgs":true,"family":"Alley","given":"William M.","affiliations":[],"preferred":false,"id":147759,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Gurtz, Martin E. megurtz@usgs.gov","contributorId":2987,"corporation":false,"usgs":true,"family":"Gurtz","given":"Martin","email":"megurtz@usgs.gov","middleInitial":"E.","affiliations":[{"id":451,"text":"National Water Quality Assessment Program","active":true,"usgs":true}],"preferred":false,"id":147758,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":5339,"text":"fs00295 - 1995 - United States Geological Survey : programs in Alabama","interactions":[],"lastModifiedDate":"2012-02-02T00:05:43","indexId":"fs00295","displayToPublicDate":"1995-05-01T00:00:00","publicationYear":"1995","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":313,"text":"Fact Sheet","code":"FS","onlineIssn":"2327-6932","printIssn":"2327-6916","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"002-95","title":"United States Geological Survey : programs in Alabama","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/fs00295","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1995, United States Geological Survey : programs in Alabama: U.S. Geological Survey Fact Sheet 002-95, 4 p. : ill. ; 28 cm. ill., https://doi.org/10.3133/fs00295.","productDescription":"4 p. : ill. ; 28 cm. ill.","costCenters":[],"links":[{"id":383,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://water.usgs.gov/wid/html/al.html","linkFileType":{"id":5,"text":"html"}},{"id":117645,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/fs_002_95.bmp"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a25e4b07f02db60efbb","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":528503,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
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