{"pageNumber":"426","pageRowStart":"10625","pageSize":"25","recordCount":16446,"records":[{"id":20643,"text":"ofr95338 - 1995 - Hydrologic and water-quality data for the lower Bradley River, Alaska, March 1993 to April 1994","interactions":[],"lastModifiedDate":"2022-12-27T21:38:30.518871","indexId":"ofr95338","displayToPublicDate":"1995-12-01T00:00:00","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":"95-338","title":"Hydrologic and water-quality data for the lower Bradley River, Alaska, March 1993 to April 1994","docAbstract":"A dam constructed at the outlet of Bradley Lake near Homer, Alaska has blocked natural flows to the lower Bradley River. To protect salmon egg incubation habitat during the period November 2 to April 30, a fish-water bypass was incorporated into the design of the dam to ensure a minimum discharge of 40 cubic feet per second in the lower river. This minimum flow determination was based on an open-water instream flow study that did not take into account effects of ice formation. A study was begun in March 1993 to determine winter flow conditions in the lower Bradley River. As a part of this study, data were collected at sites in the lower Bradley River to measure discharge, wetted perimeter, cross-sectional area, water depth, flow velocity, and specific conductance, as well as temperature and dissolved oxygen from both surface water and intragravel water. Discharge and specific conduc- tance in the Middle Fork Bradley River below North Fork Bradley River were also measured. This report presents data collected between March 1993 and April 1994.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr95338","usgsCitation":"Rickman, R.L., 1995, Hydrologic and water-quality data for the lower Bradley River, Alaska, March 1993 to April 1994: U.S. Geological Survey Open-File Report 95-338, iv, 30 p., https://doi.org/10.3133/ofr95338.","productDescription":"iv, 30 p.","costCenters":[{"id":525,"text":"Pacific Islands Water Science Center","active":true,"usgs":true}],"links":[{"id":411085,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_19162.htm","linkFileType":{"id":5,"text":"html"}},{"id":152248,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1995/0338/report-thumb.jpg"},{"id":50169,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1995/0338/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Alaska","otherGeospatial":"lower Bradley River","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -151.00006610933335,\n              59.84487029785086\n            ],\n            [\n              -151.00006610933335,\n              59.6471642653043\n            ],\n            [\n              -150.46582873962421,\n              59.6471642653043\n            ],\n            [\n              -150.46582873962421,\n              59.84487029785086\n            ],\n            [\n              -151.00006610933335,\n              59.84487029785086\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a29e4b07f02db6116e9","contributors":{"authors":[{"text":"Rickman, Ronald L. rrickman@usgs.gov","contributorId":5284,"corporation":false,"usgs":true,"family":"Rickman","given":"Ronald","email":"rrickman@usgs.gov","middleInitial":"L.","affiliations":[{"id":525,"text":"Pacific Islands Water Science Center","active":true,"usgs":true}],"preferred":true,"id":182988,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70185328,"text":"70185328 - 1995 - Simulation of aerobic and anaerobic biodegradation processes at a crude oil spill site","interactions":[],"lastModifiedDate":"2018-03-08T14:53:55","indexId":"70185328","displayToPublicDate":"1995-12-01T00:00:00","publicationYear":"1995","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3722,"text":"Water Resources Research","onlineIssn":"1944-7973","printIssn":"0043-1397","active":true,"publicationSubtype":{"id":10}},"title":"Simulation of aerobic and anaerobic biodegradation processes at a crude oil spill site","docAbstract":"<p><span>A two-dimensional, multispecies reactive solute transport model with sequential aerobic and anaerobic degradation processes was developed and tested. The model was used to study the field-scale solute transport and degradation processes at the Bemidji, Minnesota, crude oil spill site. The simulations included the biodegradation of volatile and nonvolatile fractions of dissolved organic carbon by aerobic processes, manganese and iron reduction, and methanogenesis. Model parameter estimates were constrained by published Monod kinetic parameters, theoretical yield estimates, and field biomass measurements. Despite the considerable uncertainty in the model parameter estimates, results of simulations reproduced the general features of the observed groundwater plume and the measured bacterial concentrations. In the simulation, 46% of the total dissolved organic carbon (TDOC) introduced into the aquifer was degraded. Aerobic degradation accounted for 40% of the TDOC degraded. Anaerobic processes accounted for the remaining 60% of degradation of TDOC: 5% by Mn reduction, 19% by Fe reduction, and 36% by methanogenesis. Thus anaerobic processes account for more than half of the removal of DOC at this site.</span></p>","language":"English","publisher":"American Geophysical Union","doi":"10.1029/95WR02567","usgsCitation":"Essaid, H.I., Bekins, B.A., Godsy, E.M., Warren, E., Baedecker, M.J., and Cozzarelli, I.M., 1995, Simulation of aerobic and anaerobic biodegradation processes at a crude oil spill site: Water Resources Research, v. 31, no. 12, p. 3309-3327, https://doi.org/10.1029/95WR02567.","productDescription":"19 p.","startPage":"3309","endPage":"3327","costCenters":[{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":337870,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"31","issue":"12","noUsgsAuthors":false,"publicationDate":"2010-07-09","publicationStatus":"PW","scienceBaseUri":"58d0ea1ee4b0236b68f67393","contributors":{"authors":[{"text":"Essaid, Hedeff I. 0000-0003-0154-8628 hiessaid@usgs.gov","orcid":"https://orcid.org/0000-0003-0154-8628","contributorId":2284,"corporation":false,"usgs":true,"family":"Essaid","given":"Hedeff","email":"hiessaid@usgs.gov","middleInitial":"I.","affiliations":[{"id":438,"text":"National Research Program - Western Branch","active":true,"usgs":true}],"preferred":true,"id":685193,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bekins, Barbara A. 0000-0002-1411-6018 babekins@usgs.gov","orcid":"https://orcid.org/0000-0002-1411-6018","contributorId":1348,"corporation":false,"usgs":true,"family":"Bekins","given":"Barbara","email":"babekins@usgs.gov","middleInitial":"A.","affiliations":[{"id":36183,"text":"Hydro-Ecological Interactions Branch","active":true,"usgs":true},{"id":436,"text":"National Research Program - Eastern Branch","active":true,"usgs":true},{"id":438,"text":"National Research Program - Western Branch","active":true,"usgs":true},{"id":37277,"text":"WMA - Earth System Processes Division","active":true,"usgs":true}],"preferred":true,"id":685194,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Godsy, E. Michael","contributorId":45842,"corporation":false,"usgs":true,"family":"Godsy","given":"E.","email":"","middleInitial":"Michael","affiliations":[],"preferred":false,"id":685195,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Warren, Ean ewarren@usgs.gov","contributorId":1351,"corporation":false,"usgs":true,"family":"Warren","given":"Ean","email":"ewarren@usgs.gov","affiliations":[{"id":438,"text":"National Research Program - Western Branch","active":true,"usgs":true}],"preferred":true,"id":685196,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Baedecker, Mary Jo mjbaedec@usgs.gov","contributorId":3346,"corporation":false,"usgs":true,"family":"Baedecker","given":"Mary","email":"mjbaedec@usgs.gov","middleInitial":"Jo","affiliations":[{"id":436,"text":"National Research Program - Eastern Branch","active":true,"usgs":true}],"preferred":false,"id":685197,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Cozzarelli, Isabelle M. 0000-0002-5123-1007 icozzare@usgs.gov","orcid":"https://orcid.org/0000-0002-5123-1007","contributorId":1693,"corporation":false,"usgs":true,"family":"Cozzarelli","given":"Isabelle","email":"icozzare@usgs.gov","middleInitial":"M.","affiliations":[{"id":436,"text":"National Research Program - Eastern Branch","active":true,"usgs":true},{"id":49175,"text":"Geology, Energy & Minerals Science Center","active":true,"usgs":true}],"preferred":true,"id":685198,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}}
,{"id":70195997,"text":"70195997 - 1995 - Accuracy of tretyakov precipitation gauge: Result of wmo intercomparison","interactions":[],"lastModifiedDate":"2018-03-13T10:56:41","indexId":"70195997","displayToPublicDate":"1995-12-01T00:00:00","publicationYear":"1995","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1924,"text":"Hydrological Processes","active":true,"publicationSubtype":{"id":10}},"title":"Accuracy of tretyakov precipitation gauge: Result of wmo intercomparison","docAbstract":"<p>The Tretyakov non-recording precipitation gauge has been used historically as the official precipitation measurement instrument in the Russian (formerly the USSR) climatic and hydrological station network and in a number of other European countries. From 1986 to 1993, the accuracy and performance of this gauge were evaluated during the WMO Solid Precipitation Measurement Intercomparison at 11 stations in Canada, the USA, Russia, Germany, Finland, Romania and Croatia. The double fence intercomparison reference (DFIR) was the reference standard used at all the Intercomparison stations in the Intercomparison. The Intercomparison data collected at the different sites are compatible with respect to the catch ratio (measured/DFIR) for the same gauge, when compared using mean wind speed at the height of the gauge orifice during the observation period.</p><p>The Intercomparison data for the Tretyakov gauge were compiled from measurements made at these WMO intercomparison sites. These data represent a variety of climates, terrains and exposures. The effects of environmental factors, such as wind speed, wind direction, type of precipitation and temperature, on gauge catch ratios were investigated. Wind speed was found to be the most important factor determining the gauge catch and air temperature had a secondary effect when precipitation was classified into snow, mixed and rain. The results of the analysis of gauge catch ratio versus wind speed and temperature on a daily time step are presented for various types of precipitation. Independent checks of the correction equations against the DFIR have been conducted at those Intercomparison stations and a good agreement (difference less than 10%) has been obtained. The use of such adjustment procedures should significantly improve the accuracy and homogeneity of gauge-measured precipitation data over large regions of the former USSR and central Europe.</p>","language":"English","publisher":"Wiley","doi":"10.1002/hyp.3360090805","usgsCitation":"Yang, D., Goodison, B.E., Metcalfe, J.R., Golubev, V.S., Elomaa, E., Gunther, T., Bates, R., Pangburn, T., Hanson, C.L., Emerson, D.G., Copaciu, V., and Milkovic, J., 1995, Accuracy of tretyakov precipitation gauge: Result of wmo intercomparison: Hydrological Processes, v. 9, no. 8, p. 877-895, https://doi.org/10.1002/hyp.3360090805.","productDescription":"19 p.","startPage":"877","endPage":"895","costCenters":[{"id":478,"text":"North Dakota Water Science Center","active":true,"usgs":true},{"id":34685,"text":"Dakota Water Science Center","active":true,"usgs":true}],"links":[{"id":352429,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"9","issue":"8","noUsgsAuthors":false,"publicationDate":"2006-07-31","publicationStatus":"PW","scienceBaseUri":"5aff209ce4b0da30c1bfd5bc","contributors":{"authors":[{"text":"Yang, Daqing","contributorId":203286,"corporation":false,"usgs":false,"family":"Yang","given":"Daqing","email":"","affiliations":[],"preferred":false,"id":730855,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Goodison, Barry E.","contributorId":203293,"corporation":false,"usgs":false,"family":"Goodison","given":"Barry","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":730856,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Metcalfe, John R.","contributorId":203294,"corporation":false,"usgs":false,"family":"Metcalfe","given":"John","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":730857,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Golubev, Valentin S.","contributorId":203295,"corporation":false,"usgs":false,"family":"Golubev","given":"Valentin","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":730858,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Elomaa, Esko","contributorId":203296,"corporation":false,"usgs":false,"family":"Elomaa","given":"Esko","email":"","affiliations":[],"preferred":false,"id":730859,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Gunther, Thilo","contributorId":203287,"corporation":false,"usgs":false,"family":"Gunther","given":"Thilo","email":"","affiliations":[],"preferred":false,"id":730860,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Bates, Roy","contributorId":203288,"corporation":false,"usgs":false,"family":"Bates","given":"Roy","email":"","affiliations":[],"preferred":false,"id":730861,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Pangburn, Timothy","contributorId":203289,"corporation":false,"usgs":false,"family":"Pangburn","given":"Timothy","email":"","affiliations":[],"preferred":false,"id":730862,"contributorType":{"id":1,"text":"Authors"},"rank":8},{"text":"Hanson, Clayton L.","contributorId":203290,"corporation":false,"usgs":false,"family":"Hanson","given":"Clayton","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":730863,"contributorType":{"id":1,"text":"Authors"},"rank":9},{"text":"Emerson, Douglas G.","contributorId":40579,"corporation":false,"usgs":true,"family":"Emerson","given":"Douglas","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":730864,"contributorType":{"id":1,"text":"Authors"},"rank":10},{"text":"Copaciu, Voilete","contributorId":203291,"corporation":false,"usgs":false,"family":"Copaciu","given":"Voilete","email":"","affiliations":[],"preferred":false,"id":730865,"contributorType":{"id":1,"text":"Authors"},"rank":11},{"text":"Milkovic, Janja","contributorId":203292,"corporation":false,"usgs":false,"family":"Milkovic","given":"Janja","email":"","affiliations":[],"preferred":false,"id":730866,"contributorType":{"id":1,"text":"Authors"},"rank":12}]}}
,{"id":26178,"text":"wri954119 - 1995 - Ground-water conditions and effects of mine dewatering in Desert Valley, Humboldt and Pershing Counties, northwestern Nevada, 1962-91","interactions":[],"lastModifiedDate":"2012-02-02T00:08:29","indexId":"wri954119","displayToPublicDate":"1995-12-01T00:00:00","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":"95-4119","title":"Ground-water conditions and effects of mine dewatering in Desert Valley, Humboldt and Pershing Counties, northwestern Nevada, 1962-91","docAbstract":"Desert Valley is a 1,200-square-mile, north- trending, structural basin, about 30 miles northwest of Winnemucca, Nevada. Unconsolidated basin-fill deposits exceeding 7,000 feet in thickness constitute the primary ground-water reservoir. Dewatering operations at an open-pit mine began in the Spring of 1985 in the northeast part of Desert Valley. Ground-water withdrawal for mine dewatering in 1991 was greater than three times the estimated average annual recharge from precipitation. The mine discharge water has been allowed to flow to areas west of the mine where it has created an artificial wetlands. This report documents the 1991 hydrologic conditions in Desert Valley and the change in conditions since predevelopment (pre-1962). It also summarizes the results of analyzing the simulated effects of open-pit mine dewatering on a basin-wide scale over time. Water-level declines associated with the dewatering have propagated north and south of the mine, but have been attenuated to the west due to the infiltration beneath the artificial wetlands. Maximum water-level declines beneath the open pits at the mine, as of Spring 1991, are about 300 feet. Changes in the hydrologic conditions since predevelopment are observed predominantly near the dewatering operations and the associated discharge lakes. General ground-water chemistry is essentially unchanged since pre- development. On the basis of a ground-water flow model used to simulate mine dewatering, a new equilibrium may slowly be approached only after 100 years of recovery from the time mine dewatering ceases.","language":"ENGLISH","publisher":"U.S. Geological Survey ;\r\nU.S. Geological Survey, Information Services [distributor],","doi":"10.3133/wri954119","usgsCitation":"Berger, D., 1995, Ground-water conditions and effects of mine dewatering in Desert Valley, Humboldt and Pershing Counties, northwestern Nevada, 1962-91: U.S. Geological Survey Water-Resources Investigations Report 95-4119, vi, 94 p. :ill., maps (some col.) ;28 cm., https://doi.org/10.3133/wri954119.","productDescription":"vi, 94 p. :ill., maps (some col.) ;28 cm.","costCenters":[],"links":[{"id":121861,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1995/4119/report-thumb.jpg"},{"id":54979,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1995/4119/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":54980,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1995/4119/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aafe4b07f02db66d312","contributors":{"authors":[{"text":"Berger, D.L.","contributorId":106904,"corporation":false,"usgs":true,"family":"Berger","given":"D.L.","email":"","affiliations":[],"preferred":false,"id":195945,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":19854,"text":"ofr95314 - 1995 - U.S. Geological Survey activities in New Mexico 1995","interactions":[],"lastModifiedDate":"2012-02-02T00:07:36","indexId":"ofr95314","displayToPublicDate":"1995-12-01T00:00:00","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":"95-314","title":"U.S. Geological Survey activities in New Mexico 1995","docAbstract":"The report provides an overview of the USGS in New Mexico, \r\nincluding activities of the Water Resources, Geologic, and National Mapping \r\nDivisions. Some USGS projects address hydrologic and geologic hazards, \r\nsuch as flood discharges, landslides, and land subsidence. Recent \r\nenvironmental assessments include participation in the Kirtland Air Force \r\nBase Installation Restoration Program, erosion on the Zuni Reservation, \r\nand ground-water contamination in eastern Bernalillo County. Water \r\navailability studies have focused on ground-water depletion in the \r\nAlbuquerque Basin, recharge in the Roswell Basin, and the water \r\nresources of Taos County. Irrigation drainage in the San Juan River area \r\nand trace metals in a reach of the Rio Grande have been investigated. \r\nThe National Water-Quality Assessment (NAWQA) program has two study \r\nunits partly located in New Mexico. Energy and mineral resource assess-\r\nments include gas resources in the San Juan Basin and environmental \r\nimpacts of mining in the Mimbres Resource Area. The USGS is studying the \r\nextent of suitable habitat for Mexican Spotted Owls. Also discussed are \r\ncartographic/thematic products and Geographical Information Systems; \r\nsurface-water, ground-water, and water-quality data-collection net-\r\nworks; and reports published from 1993 to 1995.","language":"ENGLISH","publisher":"U.S. Geological Survey ;\r\nU.S.G.S. Earth Science Information Center, Open-File Reports Section [distributor],","doi":"10.3133/ofr95314","usgsCitation":"Livingston, R.K., 1995, U.S. Geological Survey activities in New Mexico 1995: U.S. Geological Survey Open-File Report 95-314, 21 p. ill., col. maps ; 28 cm., https://doi.org/10.3133/ofr95314.","productDescription":"21 p. ill., col. maps ; 28 cm.","costCenters":[],"links":[{"id":152721,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1995/0314/report-thumb.jpg"},{"id":49333,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1995/0314/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a2ae4b07f02db61254e","contributors":{"authors":[{"text":"Livingston, Russell K.","contributorId":69582,"corporation":false,"usgs":true,"family":"Livingston","given":"Russell","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":181634,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":31683,"text":"ofr95299 - 1995 - Near field receiving water monitoring of trace metals in clams (Macoma balthica) and sediments near the Palo Alto and San Jose/Sunnyvale water quality control plants in South San Francisco Bay; June 1993 through October 1994","interactions":[],"lastModifiedDate":"2020-04-12T14:03:36.529767","indexId":"ofr95299","displayToPublicDate":"1995-12-01T00:00:00","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":"95-299","title":"Near field receiving water monitoring of trace metals in clams (Macoma balthica) and sediments near the Palo Alto and San Jose/Sunnyvale water quality control plants in South San Francisco Bay; June 1993 through October 1994","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr95299","usgsCitation":"Luoma, S., Cain, D., Brown, C.L., Hornberger, M.I., and Bouse-Schaenemann, R.M., 1995, Near field receiving water monitoring of trace metals in clams (Macoma balthica) and sediments near the Palo Alto and San Jose/Sunnyvale water quality control plants in South San Francisco Bay; June 1993 through October 1994: U.S. Geological Survey Open-File Report 95-299, 83 p. , https://doi.org/10.3133/ofr95299.","productDescription":"83 p. ","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":552,"text":"San Francisco Bay-Delta","active":false,"usgs":true},{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true},{"id":5079,"text":"Pacific Regional Director's Office","active":true,"usgs":true}],"links":[{"id":159999,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1995/0299/report-thumb.jpg"},{"id":59916,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1995/0299/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"California ","otherGeospatial":"South San Francisco Bay","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -122.464599609375,\n              37.39634613318923\n            ],\n            [\n              -121.86035156249999,\n              37.39634613318923\n            ],\n            [\n              -121.86035156249999,\n              37.75334401310656\n            ],\n            [\n              -122.464599609375,\n              37.75334401310656\n            ],\n            [\n              -122.464599609375,\n              37.39634613318923\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b00e4b07f02db697f8e","contributors":{"authors":[{"text":"Luoma, S. N.","contributorId":86353,"corporation":false,"usgs":true,"family":"Luoma","given":"S. N.","affiliations":[],"preferred":false,"id":206701,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Cain, D.J.","contributorId":68329,"corporation":false,"usgs":true,"family":"Cain","given":"D.J.","email":"","affiliations":[],"preferred":false,"id":206700,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Brown, C. L.","contributorId":35678,"corporation":false,"usgs":true,"family":"Brown","given":"C.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":206699,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Hornberger, Michelle I. 0000-0002-7787-3446","orcid":"https://orcid.org/0000-0002-7787-3446","contributorId":23574,"corporation":false,"usgs":true,"family":"Hornberger","given":"Michelle","email":"","middleInitial":"I.","affiliations":[],"preferred":false,"id":206697,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Bouse-Schaenemann, R. M.","contributorId":24392,"corporation":false,"usgs":true,"family":"Bouse-Schaenemann","given":"R.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":206698,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":17007,"text":"ofr94376 - 1995 - Concentrations and mass transport of pesticides and organic contaminants in the Mississippi River and some of its tributaries, 1987-89 and 1991-92","interactions":[],"lastModifiedDate":"2019-12-08T13:22:35","indexId":"ofr94376","displayToPublicDate":"1995-12-01T00:00:00","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":"94-376","title":"Concentrations and mass transport of pesticides and organic contaminants in the Mississippi River and some of its tributaries, 1987-89 and 1991-92","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr94376","usgsCitation":"Pereira, W.E., Moody, J.A., Hostettler, F., Rostad, C., and Leiker, T., 1995, Concentrations and mass transport of pesticides and organic contaminants in the Mississippi River and some of its tributaries, 1987-89 and 1991-92: U.S. Geological Survey Open-File Report 94-376, viii, 169 p. , https://doi.org/10.3133/ofr94376.","productDescription":"viii, 169 p. ","costCenters":[{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":148145,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1994/0376/report-thumb.jpg"},{"id":46140,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1994/0376/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","otherGeospatial":"Mississippi River","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -95.2294921875,\n              45.89000815866184\n            ],\n            [\n              -96.50390625,\n              46.07323062540835\n            ],\n            [\n              -95.185546875,\n              45.02695045318546\n            ],\n            [\n              -92.7685546875,\n              43.58039085560784\n            ],\n            [\n              -90.4833984375,\n              41.73852846935917\n            ],\n            [\n              -91.4501953125,\n              39.30029918615029\n            ],\n            [\n              -91.23046875,\n              35.137879119634185\n            ],\n            [\n              -92.0654296875,\n              31.541089879585808\n            ],\n            [\n              -91.7578125,\n              29.305561325527698\n            ],\n            [\n              -88.9892578125,\n              28.34306490482549\n            ],\n            [\n              -88.505859375,\n              30.29701788337205\n            ],\n            [\n              -90.65917968749999,\n              30.486550842588485\n            ],\n            [\n              -90.791015625,\n              32.13840869677249\n            ],\n            [\n              -89.82421875,\n              34.08906131584994\n            ],\n            [\n              -88.9453125,\n              35.96022296929667\n            ],\n            [\n              -88.9453125,\n              37.579412513438385\n            ],\n            [\n              -89.912109375,\n              39.70718665682654\n            ],\n            [\n              -89.384765625,\n              41.57436130598913\n            ],\n            [\n              -90.966796875,\n              44.05601169578525\n            ],\n            [\n              -95.2294921875,\n              45.89000815866184\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b16e4b07f02db6a560a","contributors":{"authors":[{"text":"Pereira, Wilfred E.","contributorId":95552,"corporation":false,"usgs":true,"family":"Pereira","given":"Wilfred","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":174533,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Moody, J. A.","contributorId":32930,"corporation":false,"usgs":true,"family":"Moody","given":"J.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":174531,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Hostettler, F. D.","contributorId":99563,"corporation":false,"usgs":true,"family":"Hostettler","given":"F. D.","affiliations":[],"preferred":false,"id":174535,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Rostad, C.E.","contributorId":50939,"corporation":false,"usgs":true,"family":"Rostad","given":"C.E.","email":"","affiliations":[],"preferred":false,"id":174532,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Leiker, T.J.","contributorId":96719,"corporation":false,"usgs":true,"family":"Leiker","given":"T.J.","email":"","affiliations":[],"preferred":false,"id":174534,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":21393,"text":"ofr95340 - 1995 - Origin of water that discharges from Calf Creek Spring, Garfield County, Utah","interactions":[],"lastModifiedDate":"2017-08-31T13:35:43","indexId":"ofr95340","displayToPublicDate":"1995-12-01T00:00:00","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":"95-340","title":"Origin of water that discharges from Calf Creek Spring, Garfield County, Utah","docAbstract":"<p>Calf Creek Spring provides drinking water to users of Calf Creek Campground, which is operated by the Bureau of Land Management in southcentral Utah. Use of all methods and tools available indicates that surface water from Calf Creek does not contribute to the discharge of Calf Creek Spring.</p><p>Microscopic Particulate Analysis of spring water indicates that the spring has a low risk of surface-water contamination, which is substantiated by a bacterial test of water from the point of discharge of Calf Creek Spring, the Calf Creek Spring collection box, a tap from the water distribution system, and Calf Creek near the picnic area. Bacteria colonies were found in Calf Creek near the picnic area.</p><p>Calf Creek Spring discharges from fractured Navajo Sandstone where the potential for contamination by animal or human microbes is slight. Calf Creek probably gains water along its entire length from the aquifer in the Navajo Sandstone. Once at the surface, water in Calf Creek is exposed to animal- and human-borne microbes. If the water level in the Navajo aquifer at the spring remains higher than the water level of the creek, mixing is unlikely to occur and contamination is unlikely. The water level of Calf Creek Spring in June 1994 was at least 4 feet above the water level of Calf Creek.</p><p>Water from Calf Creek Spring is a mixed type composed of magnesium, calcium, sodium, bicarbonate, and sulfate ions, and water from Calf Creek is a mixed type composed of calcium, magnesium, bicarbonate, sulfate, and chloride ions. Compositional similarity is not unusual if both water sources are derived from the Navajo aquifer.</p><p>Discharge and temperature measurements at the spring and in the creek in May and June 1994 vary independently and do not indicate a hydraulic connection. Turbidity measurements, though not conclusive, indicate that no direct hydraulic connection exists between Calf Creek and Calf Creek Spring.</p><p>Hydrologic characteristics of Calf Creek provide evidence that the probable long-term, sustainable source of water is the Navajo aquifer and not precipitation-derived runoff. Ground-water leakage from adjacent drainages could contribute to perennial flow in Calf Creek. Fractures modify the movement of ground water to discharge areas, such as Calf Creek Spring.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Salt Lake City, UT","doi":"10.3133/ofr95340","collaboration":"Prepared in cooperation with the Bureau of Land Management","usgsCitation":"Wilberg, D.E., 1995, Origin of water that discharges from Calf Creek Spring, Garfield County, Utah: U.S. Geological Survey Open-File Report 95-340, iv, 10 p., https://doi.org/10.3133/ofr95340.","productDescription":"iv, 10 p.","costCenters":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":50963,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1995/0340/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":154039,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1995/0340/report-thumb.jpg"}],"country":"United States","state":"Utah","county":"Garfield County","otherGeospatial":"Calf Creek Campground, Calf Creek Spring","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -111.41595840454102,\n              37.79154065815569\n            ],\n            [\n              -111.41115188598633,\n              37.79154065815569\n            ],\n            [\n              -111.41115188598633,\n              37.79893346559687\n            ],\n            [\n              -111.41595840454102,\n              37.79893346559687\n            ],\n            [\n              -111.41595840454102,\n              37.79154065815569\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4acce4b07f02db67e76a","contributors":{"authors":[{"text":"Wilberg, Dale E.","contributorId":101275,"corporation":false,"usgs":true,"family":"Wilberg","given":"Dale","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":184350,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":28318,"text":"wri954102 - 1995 - Variations in surface-water quality in the chain of lakes and its tributaries, Devils Lake basin, North Dakota, 1957-92","interactions":[],"lastModifiedDate":"2018-06-01T12:53:59","indexId":"wri954102","displayToPublicDate":"1995-12-01T00:00:00","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":"95-4102","title":"Variations in surface-water quality in the chain of lakes and its tributaries, Devils Lake basin, North Dakota, 1957-92","docAbstract":"<p>Located in the Devils Lake Basin, North Dakota, receives and stores runoff from the northern section of the basin and recharges Devils Lake. Hydrologic and water- quality conditions can vary greatly in the basin, resulting in potential economic damage. This report describes the seasonal and spatial variations in surface-water quality in the chain of lakes and its tributaries. &nbsp;</p>\n<p>Long-term trends in dissolved-solids and nutrient concentrations and instantaneous loads in tributaries upstream and downstream of the chain of lakes are not apparent. However,seasonal variations are apparent. Dissolved-solids concentrations were smaller, and nutrient concentrations were larger, during the spring than during the remainder of the year. Variations in dissolved-solids concentrations are caused by dilution and evaporation. Variations in nutrient concentrations are the result of biologic activity. Instantaneous dissolved-solids and nutrient loads were greater during the spring than during the remainder of the year because of seasonal differences in flow rates. &nbsp;</p>\n<p>Only minimal long-term trends and seasonal variations in dissolved-solids and nutrient concentrations in the chain of lakes are apparent. During the period of record, dissolved-solids concentrations in Sweetwater Lake generally increased, dissolved-solids concentrations in Lake Alice and Lake Irvine varied seasonally, and dissolved phosphorus concentrations in Lake Alice generally increased. &nbsp;</p>\n<p>Spatial variations in dissolved-solids and nutrient concentrations in the basin are apparent.\" &nbsp;The medians and ranges of dissolved-solids concentrations for the upstream stations were smaller than those for the lake stations and the downstream stations. Dissolved-solids concentrations were larger in Channel A than in Big Coulee, and nutrient concentrations were larger in Big Coulee than in Channel A.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri954102","usgsCitation":"Lent, R., and Zainhofsky, S., 1995, Variations in surface-water quality in the chain of lakes and its tributaries, Devils Lake basin, North Dakota, 1957-92: U.S. Geological Survey Water-Resources Investigations Report 95-4102, vi, 87 p., https://doi.org/10.3133/wri954102.","productDescription":"vi, 87 p.","numberOfPages":"95","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":478,"text":"North Dakota Water Science Center","active":true,"usgs":true},{"id":562,"text":"South Dakota Water Science Center","active":true,"usgs":true},{"id":34685,"text":"Dakota Water Science Center","active":true,"usgs":true}],"links":[{"id":159457,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/wri954102.jpg"},{"id":310512,"rank":1,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1995/4102/report.pdf","text":"Report","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"North Dakota","otherGeospatial":"Devils Lake","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -100.72265625,\n              47.47266286861342\n            ],\n            [\n              -100.72265625,\n              48.96579381461063\n            ],\n            [\n              -97.470703125,\n              48.96579381461063\n            ],\n            [\n              -97.470703125,\n              47.47266286861342\n            ],\n            [\n              -100.72265625,\n              47.47266286861342\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a14e4b07f02db602b1a","contributors":{"authors":[{"text":"Lent, R.M.","contributorId":80317,"corporation":false,"usgs":true,"family":"Lent","given":"R.M.","email":"","affiliations":[],"preferred":false,"id":199584,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Zainhofsky, S.D.","contributorId":78774,"corporation":false,"usgs":true,"family":"Zainhofsky","given":"S.D.","email":"","affiliations":[],"preferred":false,"id":199583,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":16794,"text":"ofr95373 - 1995 - Analytical data from phases I and II of the Willamette River basin water quality study, Oregon","interactions":[],"lastModifiedDate":"2017-02-07T09:56:12","indexId":"ofr95373","displayToPublicDate":"1995-12-01T00:00:00","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":"95-373","title":"Analytical data from phases I and II of the Willamette River basin water quality study, Oregon","docAbstract":"<p>This report presents trace-element, organic-compound (pesticides, volatile and semivolatile organic compounds, and dioxin and furan compounds), and nutrient concentration data from the analyses of water column, suspended-sediment, and bed-sediment samples collected by the U.S. Geological Survey as part of Phases I and II of the comprehensive Willamette River Basin Water Quality Study in western Oregon. The overall study was designed by the Oregon Department of Environmental Quality to acquire the technical and regulatory knowledge necessary to protect and enhance water quality in the Willamette River Basin.</p>\n<p>The data were collected at 50 sites, representing runoff from agricultural, forested, and urbanized subbasins. In Phase I, water samples were collected during high and low flows in 1992 and 1993 to represent a wide range of hydrologic conditions. Bed-sediment samples were collected during low flows in 1993. In Phase II, water samples were collected in the spring of 1994 after the first high-flow event following the application of agricultural fertilizers and pesticides and in the fall during the first high-flow events following the conclusion of the agricultural season.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Portland, OR","doi":"10.3133/ofr95373","usgsCitation":"Harrison, H.E., Anderson, C., Rinella, F., Gasser, T.M., and Pogue, T.R., 1995, Analytical data from phases I and II of the Willamette River basin water quality study, Oregon: U.S. Geological Survey Open-File Report 95-373, v, 171 p., https://doi.org/10.3133/ofr95373.","productDescription":"v, 171 p.","numberOfPages":"180","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":518,"text":"Oregon Water Science Center","active":true,"usgs":true}],"links":[{"id":149596,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1995/0373/report-thumb.jpg"},{"id":45854,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1995/0373/report.pdf","text":"Report","size":"537.32 KB","linkFileType":{"id":1,"text":"pdf"},"description":"Report"}],"country":"United States","state":"Oregon","otherGeospatial":"Sandy River Basin, Willamette River Basin","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -122.76123046875,\n              45.78284835197676\n            ],\n            [\n              -123.20068359374999,\n              45.521743896993634\n            ],\n            [\n              -123.6181640625,\n              45.259422036351694\n            ],\n            [\n              -123.79394531249999,\n              45.10454630976873\n            ],\n            [\n              -123.50830078125,\n              44.91813929958515\n            ],\n            [\n              -123.1787109375,\n              44.402391829093915\n            ],\n            [\n              -123.06884765625,\n              44.05601169578525\n            ],\n            [\n              -123.37646484374999,\n              43.77109381775651\n            ],\n            [\n              -123.15673828124999,\n              43.59630591596548\n            ],\n            [\n              -123.02490234375,\n              43.229195113965005\n            ],\n            [\n              -122.67333984374999,\n              43.13306116240612\n            ],\n            [\n              -121.904296875,\n              43.13306116240612\n            ],\n            [\n              -121.53076171875,\n              43.29320031385282\n            ],\n            [\n              -121.39892578125,\n              44.35527821160296\n            ],\n            [\n              -121.70654296874999,\n              45.089035564831036\n            ],\n            [\n              -121.6845703125,\n              45.47554027158593\n            ],\n            [\n              -121.640625,\n              45.72152152227954\n            ],\n            [\n              -122.08007812499999,\n              45.62940492064501\n            ],\n            [\n              -122.431640625,\n              45.537136680398596\n            ],\n            [\n              -122.76123046875,\n              45.69083283645816\n            ],\n            [\n              -122.76123046875,\n              45.78284835197676\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4acce4b07f02db67e52c","contributors":{"authors":[{"text":"Harrison, Howard E.","contributorId":8485,"corporation":false,"usgs":true,"family":"Harrison","given":"Howard","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":173628,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Anderson, Chauncey W. 0000-0002-1016-3781 chauncey@usgs.gov","orcid":"https://orcid.org/0000-0002-1016-3781","contributorId":1151,"corporation":false,"usgs":true,"family":"Anderson","given":"Chauncey W.","email":"chauncey@usgs.gov","affiliations":[{"id":518,"text":"Oregon Water Science Center","active":true,"usgs":true}],"preferred":false,"id":173627,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Rinella, Frank A.","contributorId":89515,"corporation":false,"usgs":true,"family":"Rinella","given":"Frank A.","affiliations":[],"preferred":false,"id":173631,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Gasser, Timothy M.","contributorId":54615,"corporation":false,"usgs":true,"family":"Gasser","given":"Timothy","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":173630,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Pogue, Ted R. Jr.","contributorId":13998,"corporation":false,"usgs":true,"family":"Pogue","given":"Ted","suffix":"Jr.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":173629,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":27488,"text":"wri944040 - 1995 - Hydrogeology and geochemistry of acid mine drainage in ground water in the vicinity of Penn Mine and Camanche Reservoir, Calaveras County, California: First-year summary","interactions":[],"lastModifiedDate":"2022-02-03T19:16:44.087572","indexId":"wri944040","displayToPublicDate":"1995-11-01T00:00:00","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":"94-4040","title":"Hydrogeology and geochemistry of acid mine drainage in ground water in the vicinity of Penn Mine and Camanche Reservoir, Calaveras County, California: First-year summary","docAbstract":"<p>Acid drainage from the Penn Mine in Calaveras County, California, has caused contamination of ground water between Mine Run Dam and Camanche Reservoir. The Penn Mine was first developed in the 1860's primarily for copper and later produced lesser amounts of zinc, lead, silver, and gold from steeply dipping massive sulfide lenses in metamorphic rocks. Surface disposal of sulfidic waste rock and tailings from mine operations has produced acidic drainage with pH values between 2.3 and 2.7 and elevated concentrations of sulfate and metals, including copper, zinc, cadmium, iron, and aluminum. During the mine's operation and after its subsequent abandonment in the late 1950's, acid mine drainage flowed down Mine Run into the Mokelumne River. Construction of Camanche Dam in 1963 flooded part of the Mokelumne River adjacent to Penn Mine. Surface-water diversions and unlined impoundments were constructed at Penn Mine in 1979 to reduce runoff from the mine, collect contaminated surface water, and enhance evaporation. Some of the contaminated surface water infiltrates the ground water and flows toward Camanche Reservoir.</p><p> Ground- water flow in the study area is controlled by the local hydraulic gradient and the hydraulic characteristics of two principal rock types, a Jurassic metavolcanic unit and the underlying Salt Spring slate. The hydraulic gradient is west from Mine Run impoundment toward Camanche Reservoir. The median hydraulic conductivity was about 10 to 50 times higher in the metavolcanic rock (0.1 foot per day) than in the slate (0.002 to 0.01 foot per day); most flow occurs in the metavolcanic rock where hydraulic conductivity is as high as 50 feet per day in two locations. The contact between the two rock units is a fault plane that strikes N20?W, dips 20?NE, and is a likely conduit for ground-water flow, based on down-hole measurements with a heatpulse flowmeter. </p><p>Analyses of water samples collected during April 1992 provide a comprehensive characterization of ground water below Mine Run Dam at the Penn Mine. Specific conductance of the samples ranged from 1,810 to 18,000 microsiemens per centimeter. pH values of sampled ground water ranged from 3.7 to 7.8. Dissolved constituents in ground water ranged from less than 0.010 to 86 milligrams per liter for copper, from less than 0.010 to 240 milligrams per liter for iron, from less than 0.01 to 250 milligrams per liter for aluminum, and from 0.020 to 600 milligrams per liter for zinc. A contaminated ground-water plume appears to originate in the metavolcanic unit along the north abutment of Mine Run Dam. The plume is characterized by low pH, high concentrations of sulfate and dissolved metals, and enrichment of the heavy stable isotopes of hydrogen and oxygen. Dissolved iron and sulfate correlate positively, suggesting pyrite as the probable source of these elements. The concentrations of some dissolved constituents apparently are controlled by equilibrium with solid mineral phases. Poorly crystalline hydrous ferric oxide and microcrystalline gibbsite are close to saturation in ground water with pH values between 4 and 7.8 and probably control the solubility of Fe<sup>3+</sup> and Al<sup>3+</sup>, respectively. </p><p>Using a range of bulk hydraulic conductivity values for the metavolcanic unit from the median value (0.1 foot per day) to the highest values (50 feet per day), together with a representative cross-sectional area (3,000 square feet) for the contaminated ground-water plume and a hydraulic gradient of 0.14 from August 1992, the following range in ground-water flow rates is estimated by Darcy's law: 42 to 21,000 cubic feet per day, or 10<sup>5</sup> to 5x10<sup>7</sup> gallons per year. Multiplying this estimated range in ground-water flow by representative metal concentrations from the contaminated plume gives the following estimates for annual metal transport to Camanche Reservoir by ground water: 86 to 42,000 pounds of copper; 310 to 150,000 pounds of zinc; and 1.5 to 750 pounds of cadmium.&nbsp;</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wri944040","usgsCitation":"Hamlin, S.N., and Alpers, C.N., 1995, Hydrogeology and geochemistry of acid mine drainage in ground water in the vicinity of Penn Mine and Camanche Reservoir, Calaveras County, California: First-year summary: U.S. Geological Survey Water-Resources Investigations Report 94-4040, v, 45 p., https://doi.org/10.3133/wri944040.","productDescription":"v, 45 p.","costCenters":[{"id":589,"text":"Toxic Substances Hydrology 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,{"id":17246,"text":"ofr9542 - 1995 - Hydrologic effects associated with the June 28, 1992 Landers, California, earthquake sequence","interactions":[],"lastModifiedDate":"2019-09-06T15:51:29","indexId":"ofr9542","displayToPublicDate":"1995-11-01T00:00:00","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":"95-42","title":"Hydrologic effects associated with the June 28, 1992 Landers, California, earthquake sequence","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr9542","usgsCitation":"Roeloffs, E., Danskin, W., Farrar, C.D., Galloway, D., Hamlin, S.N., Quilty, E., Quinn, H., Schaefer, D.H., Sorey, M., and Woodcock, D., 1995, Hydrologic effects associated with the June 28, 1992 Landers, California, earthquake sequence: U.S. Geological Survey Open-File Report 95-42, Report: iv, 68 p., https://doi.org/10.3133/ofr9542.","productDescription":"Report: iv, 68 p.","numberOfPages":"72","costCenters":[{"id":615,"text":"Volcano Hazards Program","active":true,"usgs":true},{"id":35860,"text":"Ohio-Kentucky-Indiana Water Science Center","active":true,"usgs":true}],"links":[{"id":46395,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1995/0042/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":149339,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1995/0042/report-thumb.jpg"}],"country":"United States","state":"California, Nevada, Oregon","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -125.0244140625,\n              32.2313896627376\n            ],\n            [\n              -113.97216796875,\n              32.2313896627376\n            ],\n            [\n              -113.97216796875,\n              42.98857645832184\n            ],\n            [\n              -125.0244140625,\n              42.98857645832184\n            ],\n            [\n              -125.0244140625,\n              32.2313896627376\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a1be4b07f02db607165","contributors":{"authors":[{"text":"Roeloffs, E.A.","contributorId":88742,"corporation":false,"usgs":true,"family":"Roeloffs","given":"E.A.","email":"","affiliations":[],"preferred":false,"id":175593,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Danskin, W.R. 0000-0001-8672-5501","orcid":"https://orcid.org/0000-0001-8672-5501","contributorId":22713,"corporation":false,"usgs":true,"family":"Danskin","given":"W.R.","affiliations":[],"preferred":false,"id":175585,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Farrar, C. 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H.","contributorId":84763,"corporation":false,"usgs":true,"family":"Schaefer","given":"D.","middleInitial":"H.","affiliations":[],"preferred":false,"id":175591,"contributorType":{"id":1,"text":"Authors"},"rank":8},{"text":"Sorey, M.L.","contributorId":73185,"corporation":false,"usgs":true,"family":"Sorey","given":"M.L.","affiliations":[],"preferred":false,"id":175590,"contributorType":{"id":1,"text":"Authors"},"rank":9},{"text":"Woodcock, D.E.","contributorId":8499,"corporation":false,"usgs":true,"family":"Woodcock","given":"D.E.","email":"","affiliations":[],"preferred":false,"id":175584,"contributorType":{"id":1,"text":"Authors"},"rank":10}]}}
,{"id":29380,"text":"wri954033 - 1995 - A strategy for delineating the area of ground-water contribution to wells completed in fractured bedrock aquifers in Pennsylvania","interactions":[],"lastModifiedDate":"2017-06-19T11:38:13","indexId":"wri954033","displayToPublicDate":"1995-11-01T00:00:00","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":"95-4033","title":"A strategy for delineating the area of ground-water contribution to wells completed in fractured bedrock aquifers in Pennsylvania","docAbstract":"Delineating a contributing area to a well completed in a fractured bedrock aquifer in Pennsylvania is difficult because the hydrogeologic characteristics of fractured rocks are extremely complex. Because of this complexity, a single method or technique to delineate a contributing area will not be applicable for all wells completed in fractured-bedrock aquifers. Therefore, a strategy for refining the understanding of boundary conditions and major heterogeneities that control ground-water flow and sources of water to a supply well is suggested.\r\n\r\n      The strategy is based on developing and refining a conceptual model for the sources of water to the well. Specifically, the strategy begins with an initial conceptual model of the ground-water-flow system, then requires the collection of hydrogeologic information to refine the conceptual model in a stepwise manner from one or more of sic categories: (1) hydrogeologic mapping, (2) water-level and streamflow measurements, (3) geochemistry, (4) geophysics and borehole flowmetering, (5) aquifer testing, and (6) tracer testing.\r\n\r\n      During the refinement process, the applicability of treating the fratured-rock aquifer as a hydrologic continuum is evaluated, and the contributing area is delineated. Choice of the method used to delineate the contributing area is less important than insuring that the method is consistent with the refined conceptual model. By use of such a strategy, the improved understanding of the ground-water-flow system will lead to a technically defensible delineation of the contributing area.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri954033","usgsCitation":"Risser, D.W., and Barton, G.J., 1995, A strategy for delineating the area of ground-water contribution to wells completed in fractured bedrock aquifers in Pennsylvania: U.S. Geological Survey Water-Resources Investigations Report 95-4033, vi, 30 p. :ill., map ;28 cm., https://doi.org/10.3133/wri954033.","productDescription":"vi, 30 p. :ill., map ;28 cm.","costCenters":[{"id":532,"text":"Pennsylvania Water Science Center","active":true,"usgs":true}],"links":[{"id":122616,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1995/4033/report-thumb.jpg"},{"id":58225,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1995/4033/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b17e4b07f02db6a62e8","contributors":{"authors":[{"text":"Risser, D. W.","contributorId":48211,"corporation":false,"usgs":true,"family":"Risser","given":"D.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":201435,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Barton, G. J.","contributorId":58660,"corporation":false,"usgs":true,"family":"Barton","given":"G.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":201436,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":27131,"text":"wri954085 - 1995 - User's manual for ANNIE, version 2, a computer program for interactive hydrologic data management","interactions":[],"lastModifiedDate":"2012-02-02T00:08:41","indexId":"wri954085","displayToPublicDate":"1995-11-01T00:00:00","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":"95-4085","title":"User's manual for ANNIE, version 2, a computer program for interactive hydrologic data management","language":"ENGLISH","publisher":"Dept. of the Interior, U.S. Geological Survey ;\r\nU.S.G.S. Earth Science Information Center, Open-File Reports Section [distributor],","doi":"10.3133/wri954085","usgsCitation":"Flynn, K., Hummel, P., Lumb, A., and Kittle, J., 1995, User's manual for ANNIE, version 2, a computer program for interactive hydrologic data management: U.S. Geological Survey Water-Resources Investigations Report 95-4085, iv, 211 p. :ill. ;28 cm., https://doi.org/10.3133/wri954085.","productDescription":"iv, 211 p. :ill. ;28 cm.","costCenters":[],"links":[{"id":158734,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1995/4085/report-thumb.jpg"},{"id":55991,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1995/4085/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a16e4b07f02db603deb","contributors":{"authors":[{"text":"Flynn, K.M.","contributorId":57503,"corporation":false,"usgs":true,"family":"Flynn","given":"K.M.","email":"","affiliations":[],"preferred":false,"id":197605,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hummel, P.R.","contributorId":73642,"corporation":false,"usgs":true,"family":"Hummel","given":"P.R.","email":"","affiliations":[],"preferred":false,"id":197607,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Lumb, A.M.","contributorId":70019,"corporation":false,"usgs":true,"family":"Lumb","given":"A.M.","affiliations":[],"preferred":false,"id":197606,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Kittle, J.L. Jr.","contributorId":89574,"corporation":false,"usgs":true,"family":"Kittle","given":"J.L.","suffix":"Jr.","affiliations":[],"preferred":false,"id":197608,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":19683,"text":"ofr95305 - 1995 - Hydrologic data for the Usquepaug-Queen River basin, Rhode Island","interactions":[],"lastModifiedDate":"2012-02-02T00:07:38","indexId":"ofr95305","displayToPublicDate":"1995-11-01T00:00:00","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":"95-305","title":"Hydrologic data for the Usquepaug-Queen River basin, Rhode Island","docAbstract":"The Usquepaug-Queen River ground-water reservoir in Rhode Island is part of the stratified-drift aquifer along the Usquepaug-Queen River and its tributaries. The thickest, most permeable parts of the aquifer form the Usquepaug-Queen River ground-water reservoir. The 36.1-square mile study area comprises parts of Washington and Kent counties, and includes parts of the towns of Exeter, North Kingstown, Richmond, South Kingstown, and West Greenwich. The report presents geologic and hydrologic information needed for the prediction and management of hydrologic effects of proposed ground-water development. The report describes aquifer lithology, provides historical data on water-level and aquifer-storage changes, provides information on ground-water quality, and presents natural flow characteristics and water quality of streams in the Usquepaug-Queen River area. The data includes 275 ground-water sites; lithologic logs of 66 ground-water sites; water levels for 43 ground- water sites; chemical analyses of 36 ground-water sites; stream discharge measurements from the continuous-record gaging station on the Usquepaug- Queen River; discharge measurements at 10 partial- record stations in the area; chemical analyses of 17 stream sites; and the data from 14 slug tests conducted at ground-water sites.","language":"ENGLISH","publisher":"U.S. Geological Survey ;\r\nU.S.G.S. Earth Science Information Center, Open-File Reports Section [distributor],","doi":"10.3133/ofr95305","usgsCitation":"Kliever, J.D., 1995, Hydrologic data for the Usquepaug-Queen River basin, Rhode Island: U.S. Geological Survey Open-File Report 95-305, iv, 68 p. ill., maps ;28 cm., https://doi.org/10.3133/ofr95305.","productDescription":"iv, 68 p. ill., maps ;28 cm.","costCenters":[],"links":[{"id":152427,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1995/0305/report-thumb.jpg"},{"id":19361,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1995/0305/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":49166,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1995/0305/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a1ce4b07f02db608204","contributors":{"authors":[{"text":"Kliever, John D.","contributorId":46976,"corporation":false,"usgs":true,"family":"Kliever","given":"John","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":181328,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":18375,"text":"ofr95372 - 1995 - Characterizing water quality in the North Fork-Fall Creek Hydrologic Unit Area, Tennessee","interactions":[],"lastModifiedDate":"2026-04-08T19:12:13.256494","indexId":"ofr95372","displayToPublicDate":"1995-11-01T00:00:00","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":"95-372","title":"Characterizing water quality in the North Fork-Fall Creek Hydrologic Unit Area, Tennessee","docAbstract":"The North Fork-Fall Creek Watershed in Bedford County, Tennessee is a karst terrain with a complex interconnection between ground water and the surface water-drainage network. Multiple sources of agricultural and domestic contamination make the effective design of best management practices difficult. Ongoing investigations by the U.S. Geological Survey and several county, State, and Federal agricultural agencies are attempting to refine source identification and improve the effectiveness of best management practices in the basin.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr95372","usgsCitation":"Byl, T., and Mattraw, H., 1995, Characterizing water quality in the North Fork-Fall Creek Hydrologic Unit Area, Tennessee: U.S. Geological Survey Open-File Report 95-372, 2 p. ill. ;28 cm., https://doi.org/10.3133/ofr95372.","productDescription":"2 p.","costCenters":[],"links":[{"id":1098,"rank":2,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/1995/ofr_95-372/index.html","linkFileType":{"id":5,"text":"html"}},{"id":151976,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"country":"United 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 \"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e2e4b07f02db5e4caa","contributors":{"authors":[{"text":"Byl, Thomas Duane","contributorId":65491,"corporation":false,"usgs":true,"family":"Byl","given":"Thomas Duane","affiliations":[],"preferred":false,"id":179007,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Mattraw, H. C.","contributorId":45712,"corporation":false,"usgs":true,"family":"Mattraw","given":"H. C.","affiliations":[],"preferred":false,"id":179006,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70185316,"text":"70185316 - 1995 - Use of a reactive gas transport model to determine rates of hydrocarbon biodegradation in unsaturated porous media","interactions":[],"lastModifiedDate":"2018-03-08T10:06:58","indexId":"70185316","displayToPublicDate":"1995-11-01T00:00:00","publicationYear":"1995","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3722,"text":"Water Resources Research","onlineIssn":"1944-7973","printIssn":"0043-1397","active":true,"publicationSubtype":{"id":10}},"title":"Use of a reactive gas transport model to determine rates of hydrocarbon biodegradation in unsaturated porous media","docAbstract":"<p><span>A mathematical model is presented that simulates the transport and reaction of any number of gaseous phase constituents (e.g. CO</span><sub>2</sub><span>, O</span><sub>2</sub><span>, N</span><sub>2</sub><span>, and hydrocarbons) in unsaturated porous media. The model was developed as part of a method to determine rates of hydrocarbon biodegradation associated with natural cleansing at petroleum product spill sites. The one-dimensional model can be applied to analyze data from column experiments or from field sites where gas transport in the unsaturated zone is approximately vertical. A coupled, non-Fickian constitutive relation between fluxes and concentration gradients, together with the capability of incorporating heterogeneity with respect to model parameters, results in model applicability over a wide range of experimental and field conditions. When applied in a calibration mode, the model allows for the determination of constituent production/consumption rates as a function of the spatial coordinate. Alternatively, the model can be applied in a predictive mode to obtain the distribution of constituent concentrations and fluxes on the basis of assumed values of model parameters and a biodegradation hypothesis. Data requirements for the model are illustrated by analyzing data from a column experiment designed to determine the aerobic degradation rate of toluene in sediments collected from a gasoline spill site in Galloway Township, New Jersey.</span></p>","language":"English","publisher":"American Geophysical Union","doi":"10.1029/95WR02077","usgsCitation":"Baehr, A.L., and Baker, R.J., 1995, Use of a reactive gas transport model to determine rates of hydrocarbon biodegradation in unsaturated porous media: Water Resources Research, v. 31, no. 11, p. 2877-2882, https://doi.org/10.1029/95WR02077.","productDescription":"6 p. ","startPage":"2877","endPage":"2882","costCenters":[{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":337859,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"31","issue":"11","noUsgsAuthors":false,"publicationDate":"2010-07-09","publicationStatus":"PW","scienceBaseUri":"58d0ea1ee4b0236b68f67397","contributors":{"authors":[{"text":"Baehr, Arthur L.","contributorId":104523,"corporation":false,"usgs":true,"family":"Baehr","given":"Arthur","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":685143,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Baker, Ronald J. rbaker@usgs.gov","contributorId":1436,"corporation":false,"usgs":true,"family":"Baker","given":"Ronald","email":"rbaker@usgs.gov","middleInitial":"J.","affiliations":[{"id":470,"text":"New Jersey Water Science Center","active":true,"usgs":true}],"preferred":true,"id":685144,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":16988,"text":"ofr95156 - 1995 - Collection of short papers on Beaver Creek watershed studies in West Tennessee, 1989-94","interactions":[],"lastModifiedDate":"2026-04-08T15:29:53.205243","indexId":"ofr95156","displayToPublicDate":"1995-11-01T00:00:00","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":"95-156","title":"Collection of short papers on Beaver Creek watershed studies in West Tennessee, 1989-94","docAbstract":"In 1989, the U.S. Geological Survey began a scientific investigation to evaluate the effect of agricultural activities on water quality and the effectiveness of agricultural best management practices in the Beaver Creek watershed, West Tennessee. The project is being conducted jointly with other Federal, State, county agencies, the farming community, and academic institutions, in support of the U.S. Department of Agriculture's Hydrologic Unit Area program. The Beaver Creek project has evolved into a long-term watershed assessment and monitoring program. In 1991, a grant was received to develop and evaluate sampling strategies for higher order streams. During the summer of 1992, a reconnaissance of water-quality conditions for the shallow aquifers in Shelby, Tipton, Fayette, and Haywood Counties was conducted and included 89 domestic wells in the Beaver Creek watershed. Results from this effort lead to the development of a 1-year program to evaluate cause- and-effect relations that can explain the observed water-quality conditions for the shallow aquifers in the watershed. In 1992 the USGS, in cooperation with the Soil Conservation Service and the Shelby County Soil Conservation District, began an evaluation of in-stream processes and in-stream resource-management systems. In 1993, a biomonitoring program was established in the watershed. This collection of eight articles and abstracts was originally published in the American Water Resources Association National Symposium on Water Quality Proceedings for the national conference held in Chicago in 1994 and describes what has been learned in the study to date.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr95156","usgsCitation":"Doyle, W.H., and Baker, E.G., 1995, Collection of short papers on Beaver Creek watershed studies in West Tennessee, 1989-94: U.S. Geological Survey Open-File Report 95-156, v, 54 p. :ill., maps ;28 cm., https://doi.org/10.3133/ofr95156.","productDescription":"v, 54 p.","costCenters":[],"links":[{"id":149633,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":1019,"rank":2,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/1995/ofr_95-156/index.html","linkFileType":{"id":5,"text":"html"}}],"country":"United 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,{"id":16920,"text":"ofr95291 - 1995 - Benthic macrofauna data for San Francisco Bay, California, September 1986","interactions":[],"lastModifiedDate":"2020-05-01T14:34:41.168578","indexId":"ofr95291","displayToPublicDate":"1995-11-01T00:00:00","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":"95-291","title":"Benthic macrofauna data for San Francisco Bay, California, September 1986","docAbstract":"<p>Benthic macrofauna were collected during September 1986 to evaluate locations for long-term monitoring stations as part of the U.S. Geological Survey Regional Effects Monitoring Program in San Francisco Bay, California. Three to ten replicate samples were collected with a modified Van Veen sampler (0.05 m<sup>2</sup> area) at ten locations. One box core sample (0.06 m<sup>2</sup> area) was collected at seven to the ten locations. Six of the box core samples were split into an upper 10 cm sample and a deeper sample before analysis. Macrofauna specimens were identified to the lowest possible taxon, usually genus and species, then counted. An average of 88 percent of the benthic macrofauna specimens were identified to the species level. The fraction identified varied among stations from 54 to 98 percent. Nematodes and oligochaetes accounted for most of the unidentified specimens. Relative to the total number of species identified in five replicates at each location, an average of 90 percent of the species were collected with three replicates. In general, species with high to moderate abundances were present in all replicates, and species collected only after three or more replicates averaged less than one specimen per replicate. Results from the box cores showed that the dominant species were most abundant in the upper 10 cm, the depth of sediment that can be adequately sampled with a modified Van Veen sampler. On the basis of the number of species and their abundances at each location, seven of the ten locations were selected for sampling in the regular program, which began in March 1987.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr95291","usgsCitation":"Schemel, L.E., Thompson, J., Harmon, J., and Yost, B.T., 1995, Benthic macrofauna data for San Francisco Bay, California, September 1986: U.S. Geological Survey Open-File Report 95-291, iii, 33 p. , https://doi.org/10.3133/ofr95291.","productDescription":"iii, 33 p. ","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":552,"text":"San Francisco Bay-Delta","active":false,"usgs":true},{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true},{"id":5079,"text":"Pacific Regional Director's Office","active":true,"usgs":true}],"links":[{"id":46032,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1995/0291/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":149415,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1995/0291/report-thumb.jpg"}],"country":"United States","state":"California","otherGeospatial":"San Francisco Bay","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -122.98645019531249,\n              37.38761749978395\n            ],\n            [\n              -121.83288574218749,\n              37.38761749978395\n            ],\n            [\n              -121.83288574218749,\n              38.21660403859855\n            ],\n            [\n              -122.98645019531249,\n              38.21660403859855\n            ],\n            [\n              -122.98645019531249,\n              37.38761749978395\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a3ae4b07f02db61dffb","contributors":{"authors":[{"text":"Schemel, Laurence E. lschemel@usgs.gov","contributorId":4085,"corporation":false,"usgs":true,"family":"Schemel","given":"Laurence","email":"lschemel@usgs.gov","middleInitial":"E.","affiliations":[],"preferred":true,"id":174185,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Thompson, J.K.","contributorId":103300,"corporation":false,"usgs":true,"family":"Thompson","given":"J.K.","email":"","affiliations":[],"preferred":false,"id":174188,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Harmon, J.G.","contributorId":90753,"corporation":false,"usgs":true,"family":"Harmon","given":"J.G.","email":"","affiliations":[],"preferred":false,"id":174187,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Yost, B. 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,{"id":20819,"text":"ofr94711W - 1995 - Hydrologic data from the lower Cedar River Basin, Iowa, 1989-91","interactions":[],"lastModifiedDate":"2019-12-08T13:11:21","indexId":"ofr94711W","displayToPublicDate":"1995-11-01T00:00:00","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":"94-711","chapter":"W","title":"Hydrologic data from the lower Cedar River Basin, Iowa, 1989-91","docAbstract":"<p>Hydrologic data were collected from May 1989 through July 1991 from the Cedar River and the adjacent alluvial aquifer. The data were collected during various flow regimes of the river to evaluate the movement of agricultural chemicals between surface water and ground water. Water-quality samples from 34 surface-water sites and 95 ground-water sites were analyzed for 11 herbicides, 2 dealkylated atrazine metabolites, and nitrate. Specific conductance, pH, water temperature, and dissolved oxygen were measured at the time of sampling. Discharge and water-quality data from two seepage investigations were collected to identify gaining and losing reaches of the river and to help delineate where agricultural chemicals enter the river. Ancillary data on ground-water levels and river stage also were collected.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Iowa City","doi":"10.3133/ofr94711W","usgsCitation":"Schulmeyer, P., Barnes, K., and Squillace, P.J., 1995, Hydrologic data from the lower Cedar River Basin, Iowa, 1989-91: U.S. Geological Survey Open-File Report 94-711, iv, 116 p., https://doi.org/10.3133/ofr94711W.","productDescription":"iv, 116 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":351,"text":"Iowa Water Science Center","active":true,"usgs":true},{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":50401,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1994/0711w/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":153390,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1994/0711w/report-thumb.jpg"}],"country":"United 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,{"id":18966,"text":"ofr94709W - 1995 - Statistical summaries of surface-water hydrologic data collected in the Suwannee River Water Management District, Florida, 1906-93","interactions":[],"lastModifiedDate":"2019-08-29T07:48:08","indexId":"ofr94709W","displayToPublicDate":"1995-11-01T00:00:00","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":"94-709","chapter":"W","title":"Statistical summaries of surface-water hydrologic data collected in the Suwannee River Water Management District, Florida, 1906-93","docAbstract":"<p>Since 1906, hydrologic data have been collected systematically on streams and lakes in the Suwannee River Water Management District (SRWMD) by the U.S. Geological Survey (USGS), the SRWMD, and other agencies. Records of stream discharge and stream and lake stage in the SRWMD (fig. 1), collected largely in cooperation with the SRWMD since 1975, have been published for many years in the USGS annual report series \"Water Resources Data for Florida.\"</p><p>Streamflow and stream and lake elevation statistics are given in this report for sites shown in figure 1. All 27 daily streamflow stations shown are (or were) operated by the USGS in cooperation with the SRWMD; all 18 lake stage stations shown are now (1994) operated by the SRWMD, but were operated until the late 1970’s by the USGS in cooperation with the SRWMD. All unregulated stream stations which have three or more years of continuous record are included in this report. All unregulated lake stations having at least three years of intermittent lake elevation readings are also included. There are many other sites in the SRWMD for which shorter records or miscellaneous measurements are available but are not included because statistical summaries for such stations require interpretive analysis beyond the scope of this report.</p><p>Basic hydrologic data have long been recognized as fundamental to the analysis of magnitude and frequency of floods, availability of water supplies, potential for reservoir storage, and permitting of waste discharges. Also, in recent times, scientists and water managers have become more aware of the complex relations between flows and water levels and the terrestrial and aquatic plant and&nbsp;animal life in wetland ecosystems. In 1994, the SRWMD and the USGS began a long-term program of cooperative studies designed to better understand minimum and maximum flow and water levels needed to manage the surface and ground water resources of the District and maintain or improve the various ecosystems therein. Information presented in this report, together with frequency analysis of station data, flow regionalization, studies of the relation of salinity to flow in the lower Suwannee River, definition of ground-water surface-water interactions, surface- and ground-water quality studies, and studies of interaction between surface-water bodies and wetlands, will provide the basis for the SRWMD to establish minimum flow and level requirements for streams and lakes in the SRWMD area.</p><p>This report is a necessary first step in the longterm program of study because it contains basic stream discharge and stream and lake elevation statistics, most of which are not contained in the annual report \"Water Resources Data for Florida.\" These statistics, most of which were generated using a U.S. Geological Survey computer program, ADAPS, Automatic Data Processing System, characterize normal flows and levels and departures from normal due to floods and droughts or seasonal climatic variations. Specifically, the report presents for the period of record of each stream or lake gaging station, as appropriate:</p><ul><li>Minimum, maximum, and mean of monthly mean stream elevations and discharges in graphical and tabular form.</li><li>For streams, annual mean discharge, highest and lowest annual mean discharge, highest and lowest daily mean discharge, minimum annual seven-day mean discharge, instantaneous peak discharge and elevation, instantaneous minimum discharge, and basin yield.</li><li>Duration of annual daily mean stream elevation and discharge. Duration of daily values are shown in both graphical and tabular form.</li><li>Duration of daily mean stream elevations and discharge, by months, in tables.</li><li>Minimum and maximum 1-,3-,7-,14-,30-, 60-,&nbsp;90-,120-, and 183-consecutive day stream elevations and discharges (with rankings) for each year of record.</li><li>Mean monthly lake elevations and statistics by month, including number of monthly values, mean, variance, standard deviation, skewness, and coefficient of variation.</li></ul><p>For convenience, a GLOSSARY of commonly used terms related to the collection and reporting of surface-water elevations and discharge is included before the Introduction section of this report.</p><p>The authors wish to acknowledge Natalie Rackley, formerly of the U.S. Geological Survey, and T.W. Grubbs, U.S. Geological Survey, for their computer assistance in the compilation of station records, and Jim Tomberlin, U.S. Geological Survey, for the mapping of stream and lake gaging stations.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr94709W","collaboration":"Prepared in cooperation with the Suwannee River Water Management District","usgsCitation":"Franklin, M., Giese, G.L., and Mixson, P., 1995, Statistical summaries of surface-water hydrologic data collected in the Suwannee River Water Management District, Florida, 1906-93: U.S. Geological Survey Open-File Report 94-709, viii, 173 p., https://doi.org/10.3133/ofr94709W.","productDescription":"viii, 173 p.","costCenters":[],"links":[{"id":151500,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1994/0709w/report-thumb.jpg"},{"id":48377,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1994/0709w/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Florida","otherGeospatial":"Suwannee River Water Management District","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -84,\n              29\n            ],\n            [\n              -82,\n              29\n            ],\n            [\n              -82,\n              30.7\n            ],\n            [\n              -84,\n              30.7\n            ],\n            [\n              -84,\n              29\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49dce4b07f02db5e14a8","contributors":{"authors":[{"text":"Franklin, M.A.","contributorId":13631,"corporation":false,"usgs":true,"family":"Franklin","given":"M.A.","email":"","affiliations":[],"preferred":false,"id":180064,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Giese, G. 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,{"id":19941,"text":"ofr94506 - 1995 - Pesticides in the atmosphere; distribution, trends, and governing factors","interactions":[],"lastModifiedDate":"2013-05-22T15:26:15","indexId":"ofr94506","displayToPublicDate":"1995-11-01T00:00:00","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":"94-506","title":"Pesticides in the atmosphere; distribution, trends, and governing factors","docAbstract":"A comprehensive review of existing literature on the occurrence and distribution of pesticides in the atmosphere of the United States and adjoining Canadian provinces showed that the atmosphere is an important part of the hydrologic cycle that acts to distribute and deposit pesticides in areas far removed from their application sites. A compilation of existing data shows that pesticides have been detected in the atmosphere throughout the nation. Most of the available information on pesticides in the atmosphere is from small-scale, short-term studies that seldom lasted more than one year. Only two national-scale, multi-year studies were done since the late 1960's that analyzed for a wide variety of pesticides in air that were in current use at the time. Another large-scale study was done during 1990-91, but was limited to the midwestern and northeastern United States and only analyzed for two classes of herbicides in wet deposition. Most of the pesticides analyzed for were detected in either air or rain, and represent about 25 percent of the total number of insecticides, herbicides, and fungicides in current use. The geographical distribution of studies, and the type of sampling and analysis were highly variable with most of the historical study efforts concentrated in the Great Lakes area and California. Air and rain were the main atmospheric matrices sampled, but pesticides were also detected in fog and snow. Reported pesticide concentrations in air and rain were frequently positively correlated to their regional agricultural use. Deviations from this relation could usually be explained by non-agricultural use of pesticides, sampling and analytical difficulties, and environmental persistence. High concentrations of locally used pesticides were found to occur seasonally, usually in conjunction with spring planting of row crops and warm temperatures, but high concentrations also occurred during winter months in those areas where dormant orchards were sprayed. The environmentally more persistent pesticides were detected in the atmosphere at low concen- trations throughout the year. Deposition of airborne pesticides can have significant effects on water quality, but neither the nature of nor the magnitude of these effects can be determined with certainty on the basis of the type of data currently available. The lack of consistent, long-term regional and national monitoring and study of pesticides in atmospheric matrices severely limits assessment capability.","language":"ENGLISH","publisher":"U.S. Geological Survey ;Earth Science Information Center, Open-File Reports Section [distributor],","doi":"10.3133/ofr94506","usgsCitation":"Majewski, M.S., and Capel, P.D., 1995, Pesticides in the atmosphere; distribution, trends, and governing factors: U.S. Geological Survey Open-File Report 94-506, xiii, 191 p. :ill., maps ;28 cm., https://doi.org/10.3133/ofr94506.","productDescription":"xiii, 191 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":152407,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1994/0506/report-thumb.jpg"},{"id":272568,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1994/0506/report.pdf"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afee4b07f02db697904","contributors":{"authors":[{"text":"Majewski, Michael S. majewski@usgs.gov","contributorId":440,"corporation":false,"usgs":true,"family":"Majewski","given":"Michael","email":"majewski@usgs.gov","middleInitial":"S.","affiliations":[{"id":154,"text":"California Water Science Center","active":true,"usgs":true}],"preferred":true,"id":181770,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Capel, Paul D. 0000-0003-1620-5185 capel@usgs.gov","orcid":"https://orcid.org/0000-0003-1620-5185","contributorId":1002,"corporation":false,"usgs":true,"family":"Capel","given":"Paul","email":"capel@usgs.gov","middleInitial":"D.","affiliations":[{"id":451,"text":"National Water Quality Assessment Program","active":true,"usgs":true},{"id":392,"text":"Minnesota Water Science Center","active":true,"usgs":true},{"id":37778,"text":"WMA - Integrated Modeling and Prediction Division","active":true,"usgs":true}],"preferred":true,"id":181771,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70185355,"text":"70185355 - 1995 - Modeling hexavalent chromium reduction in groundwater in field-scale transport and laboratory batch experiments","interactions":[],"lastModifiedDate":"2018-03-08T14:55:21","indexId":"70185355","displayToPublicDate":"1995-11-01T00:00:00","publicationYear":"1995","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3722,"text":"Water Resources Research","onlineIssn":"1944-7973","printIssn":"0043-1397","active":true,"publicationSubtype":{"id":10}},"title":"Modeling hexavalent chromium reduction in groundwater in field-scale transport and laboratory batch experiments","docAbstract":"<p><span>A plausible and consistent model is developed to obtain a quantitative description of the gradual disappearance of hexavalent chromium (Cr(VI)) from groundwater in a small-scale field tracer test and in batch kinetic experiments using aquifer sediments under similar chemical conditions. The data exhibit three distinct timescales. Fast reduction occurs in well-stirred batch reactors in times much less than 1 hour and is followed by slow reduction over a timescale of the order of 2 days. In the field, reduction occurs on a timescale of the order of 8 days. The model is based on the following hypotheses. The chemical reduction reaction occurs very fast, and the longer timescales are caused by diffusion resistance. Diffusion into the secondary porosity of grains causes the apparent slow reduction rate in batch experiments. In the model of the field experiments, the reducing agent, heavy Fe(II)-bearing minerals, is heterogeneously distributed in thin strata located between larger nonreducing sand lenses that comprise the bulk of the aquifer solids. It is found that reducing strata of the order of centimeters thick are sufficient to contribute enough diffusion resistance to cause the observed longest timescale in the field. A one-dimensional advection/dispersion model is formulated that describes the major experimental trends. Diffusion rates are estimated in terms of an elementary physical picture of flow through a stratified medium containing identically sized spherical grains. Both reduction and sorption reactions are included. Batch simulation results are sensitive to the fraction of reductant located at or near the surface of grains, which controls the amount of rapid reduction, and the secondary porosity, which controls the rate of slow reduction observed in batch experiments. Results of Cr(VI) transport simulations are sensitive to the thickness and relative size of the reducing stratum. Transport simulation results suggest that nearly all of the reductant must be located in the reducing stratum. Within this context and as long as there is adequate reductive capacity present, the transport simulation results are insensitive to the parameters important for the batch simulations. The results illustrate how a combination of field measurements and batch laboratory studies can be used to improve predictive modeling of contaminant transport.</span></p>","language":"English","publisher":"American Geophysical Union","doi":"10.1029/95WR02104","usgsCitation":"Friedly, J., Davis, J., and Kent, D., 1995, Modeling hexavalent chromium reduction in groundwater in field-scale transport and laboratory batch experiments: Water Resources Research, v. 31, no. 11, p. 2783-2794, https://doi.org/10.1029/95WR02104.","productDescription":"12 p. ","startPage":"2783","endPage":"2794","costCenters":[{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":337916,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"31","issue":"11","noUsgsAuthors":false,"publicationDate":"2010-07-09","publicationStatus":"PW","scienceBaseUri":"58d23b92e4b0236b68f8290a","contributors":{"authors":[{"text":"Friedly, J.C.","contributorId":189596,"corporation":false,"usgs":false,"family":"Friedly","given":"J.C.","affiliations":[],"preferred":false,"id":685306,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Davis, J.A.","contributorId":71694,"corporation":false,"usgs":true,"family":"Davis","given":"J.A.","email":"","affiliations":[],"preferred":false,"id":685307,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Kent, D.B.","contributorId":16588,"corporation":false,"usgs":true,"family":"Kent","given":"D.B.","email":"","affiliations":[],"preferred":false,"id":685308,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70185325,"text":"70185325 - 1995 - An empirical model of the phytoplankton chlorophyll : carbon ratio-the conversion factor between productivity and growth rate","interactions":[],"lastModifiedDate":"2019-02-25T07:56:08","indexId":"70185325","displayToPublicDate":"1995-11-01T00:00:00","publicationYear":"1995","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2620,"text":"Limnology and Oceanography","active":true,"publicationSubtype":{"id":10}},"title":"An empirical model of the phytoplankton chlorophyll : carbon ratio-the conversion factor between productivity and growth rate","docAbstract":"<p><span>We present an empirical model that describes the ratio of phytoplankton chlorophyll </span><i>a</i><span> to carbon, Chl: C, as a function of temperature, daily irradiance, and nutrient-limited growth rate. Our model is based on 219 published measurements of algal cultures exposed to light-limited or nutrient-limited growth conditions. We illustrate an approach for using this estimator of Chl: C to calculate phytoplankton population growth rate from measured primary productivity. This adaptive Chl: C model gives rise to interactive light-nutrient effects in which growth efficiency increases with nutrient availability under low-light conditions. One implication of this interaction is the enhancement of phytoplankton growth efficiency, in addition to enhancement of biomass yield, as a response to eutrophication.</span></p>","language":"English","publisher":"Wiley","doi":"10.4319/lo.1995.40.7.1313","usgsCitation":"Cloern, J.E., Grenz, C., and Vidergar-Lucas, L., 1995, An empirical model of the phytoplankton chlorophyll : carbon ratio-the conversion factor between productivity and growth rate: Limnology and Oceanography, v. 40, no. 7, p. 1313-1321, https://doi.org/10.4319/lo.1995.40.7.1313.","productDescription":"9 p. ","startPage":"1313","endPage":"1321","costCenters":[{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":479203,"rank":0,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.4319/lo.1995.40.7.1313","text":"Publisher Index Page"},{"id":337866,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"40","issue":"7","noUsgsAuthors":false,"publicationDate":"2003-12-22","publicationStatus":"PW","scienceBaseUri":"58d0ea1ee4b0236b68f67395","contributors":{"authors":[{"text":"Cloern, James E. 0000-0002-5880-6862 jecloern@usgs.gov","orcid":"https://orcid.org/0000-0002-5880-6862","contributorId":1488,"corporation":false,"usgs":true,"family":"Cloern","given":"James","email":"jecloern@usgs.gov","middleInitial":"E.","affiliations":[{"id":438,"text":"National Research Program - Western Branch","active":true,"usgs":true},{"id":37277,"text":"WMA - Earth System Processes Division","active":true,"usgs":true}],"preferred":true,"id":685176,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Grenz, Christian","contributorId":189559,"corporation":false,"usgs":false,"family":"Grenz","given":"Christian","email":"","affiliations":[],"preferred":false,"id":685177,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Vidergar-Lucas, Lisa","contributorId":189560,"corporation":false,"usgs":false,"family":"Vidergar-Lucas","given":"Lisa","email":"","affiliations":[],"preferred":false,"id":685178,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70185714,"text":"70185714 - 1995 - Evaluation of lipid-containing semipermeable membrane devices for monitoring organochlorine contaminants in the Upper Mississippi river","interactions":[],"lastModifiedDate":"2017-03-28T10:30:11","indexId":"70185714","displayToPublicDate":"1995-11-01T00:00:00","publicationYear":"1995","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1571,"text":"Environmental Toxicology and Chemistry","active":true,"publicationSubtype":{"id":10}},"title":"Evaluation of lipid-containing semipermeable membrane devices for monitoring organochlorine contaminants in the Upper Mississippi river","docAbstract":"<p><span>Organochlorine contaminants sequestered in lipid-containing semipermeable membrane devices (SPMDs) were compared to those found in tangential-flow ultrafilter permeates as part of a pilot study at 10 sites in the Upper Mississippi River system. Caged and feral fish from three primary sites were also analyzed for comparison. Concentrated organochlorine (OC) compounds were readily extracted from the SPMDs by dialysis into hexane, and samples were analyzed by gas chromatography-negative chemical ionization-mass spectrometry. Fish and water samples were processed by conventional methods. Reasonable agreement was found between analyte SPMD-derived water concentrations and measured values of ultrafilter permeates; however, concentrations of the same analytes in caged fish did not appear to be proportional to water concentrations derived from SPMDs and ultrafilter permeates. The greatest number of OC compounds was detected in SPMDs; fewer were detected in caged fish and feral fish.</span></p>","language":"English","publisher":"Wiley","doi":"10.1002/etc.5620141109","usgsCitation":"Ellis, G.S., Rostad, C.E., Huckins, J.N., Schmitt, C.J., and MacCarthy, P., 1995, Evaluation of lipid-containing semipermeable membrane devices for monitoring organochlorine contaminants in the Upper Mississippi river: Environmental Toxicology and Chemistry, v. 14, no. 11, p. 1875-1884, https://doi.org/10.1002/etc.5620141109.","productDescription":"10 p. 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