This bibliography contains a complete listing of reports prepared by personnel of the U.S. Geological Survey from 1886 through December 31, 1993, that discuss the water resources of Utah. The reports were prepared primarily by personnel of the Water Resources Division, Utah District, in cooperation with State, other Federal, and local agencies. Several reports were prepared as a part of studies directly funded by the U.S. Geological Survey, and several were prepared by contractors for the U.S. Geological Survey.
The bibliography is divided into three major parts: (1) publications of the U.S. Geological Survey; (2) publications prepared by the U.S. Geological Survey in cooperation with and published by agencies of the State of Utah; and (3) reports printed in other publications reports prepared by the U.S. Geological Survey but published by other agencies or by professional organizations.
Publications of the U.S. Geological Survey still in print may be purchased from the U.S. Geological Survey, Earth Science Information Center, Open-File Reports Section, Box 25286, MS 517, Denver Federal Center, Denver, Colorado 80225. Publications that are out of print at the time of this compilation are marked with an asterisk (*). Except for water-supply papers, most publications that are out of print and unavailable for purchase may be examined at the U.S. Geological Survey Earth Science Information Center, 2222 West 2300 South, 2nd Floor, Salt Lake City, Utah 84119.
Reports published by the Utah Department of Natural Resources, Divisions of Water Rights and Water Resources, are available on request from these agencies or from the U.S. Geological Survey, Water Resources Division, Room 1016 Administration Building, 1745 West 1700 South, Salt Lake City, Utah 84104. Water-Resources Bulletins of the Utah Geological Survey may be purchased from that agency at 2363 Foothill Drive, Salt Lake City, Utah 84109-1491.
Inquiries as to the availability of reports listed as \"reports printed in other publications\" must be addressed to the professional organization or agency that published them. Most of these reports are available in larger libraries, such as the library of the University of Utah.
Most open-file reports are available for inspection at the U.S. Geological Survey, Water Resources Division, Room 1016 Administration Building, 1745 West 1700 South, Salt Lake City, Utah 84104. A small number of the open-file reports that have been duplicated as Utah basic- (or hydrologic-) data reports are free on request.
An index is included in this bibliography for ease of reference. Water-supply papers on the quantity and quality of ground and surface water in Utah that were published in a series are not listed separately in the index but are presented in tables 1 to 4.
","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Salt Lake City, UT","doi":"10.3133/ofr94309","usgsCitation":"1994, Bibliography of U.S. Geological Survey water-resources reports for Utah: U.S. Geological Survey Open-File Report 94-309, iv, 74 p., https://doi.org/10.3133/ofr94309.","productDescription":"iv, 74 p.","numberOfPages":"77","costCenters":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":46037,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1994/0309/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":149567,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1994/0309/report-thumb.jpg"}],"country":"United States","state":"Utah","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a51e4b07f02db6297fb","contributors":{"compilers":[{"text":"Hardy, Ellen E.","contributorId":79122,"corporation":false,"usgs":true,"family":"Hardy","given":"Ellen","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":709177,"contributorType":{"id":3,"text":"Compilers"},"rank":1},{"text":"Dragos, Stefanie L.","contributorId":107301,"corporation":false,"usgs":true,"family":"Dragos","given":"Stefanie","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":709178,"contributorType":{"id":3,"text":"Compilers"},"rank":2}]}} ,{"id":17239,"text":"ofr94384 - 1994 - Hydrologic and chemical data from an experiment to examine temporal variability in water samples from screened wells on Cape Cod, Massachusetts","interactions":[],"lastModifiedDate":"2019-12-08T14:18:12","indexId":"ofr94384","displayToPublicDate":"1995-02-01T00:00:00","publicationYear":"1994","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":"94-384","title":"Hydrologic and chemical data from an experiment to examine temporal variability in water samples from screened wells on Cape Cod, Massachusetts","docAbstract":"An experiment was designed to evaluate the changing chemical composition of the water pumped from a well screened in a physically and chemically heterogenous aquifer. Well F453-63, at the U.S. Geological Survey Toxic-Substances Hydrology research site located on Cape Cod, Massachusetts, was selected because it was known that the screen penetrated both the oxic and anoxic zones of the sewage plume from the Otis Air Base sewage-disposal sand beds. The experiment was conducted on August 12, 1992. Well F453-63 was sampled over time as it was pumped continuously, and three multilevel samplers were used to document the vertical distribution of selected chemicals in the ground water in the immediate vicinity of the well. All water samples obtained during the experiment were analyzed in the field for specific conductance and pH. The samples were subsequently analyzed for concentrations of ferrous iron (Fe+2), boron, calcium, chloride, iron (Fe total), phosphorus, potassium, magnesium, manganese, sodium, zinc, and nitrogen species, including nitrous oxide, ammonium, nitrite and nitrate. The results of these chemical analyses along with appropriate physical measurements of the site and aquifer material are documented in this data report.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr94384","usgsCitation":"Reilly, T.E., 1994, Hydrologic and chemical data from an experiment to examine temporal variability in water samples from screened wells on Cape Cod, Massachusetts: U.S. Geological Survey Open-File Report 94-384, vi, 34 p., https://doi.org/10.3133/ofr94384.","productDescription":"vi, 34 p.","costCenters":[{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":149335,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1994/0384/report-thumb.jpg"},{"id":46389,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1994/0384/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Massachusetts","otherGeospatial":"Cape Cod","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -70.9552001953125,\n 41.541477666790286\n ],\n [\n -69.840087890625,\n 41.541477666790286\n ],\n [\n -69.840087890625,\n 42.15933157601718\n ],\n [\n -70.9552001953125,\n 42.15933157601718\n ],\n [\n -70.9552001953125,\n 41.541477666790286\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a29e4b07f02db6118c8","contributors":{"authors":[{"text":"Reilly, Thomas E. tereilly@usgs.gov","contributorId":1660,"corporation":false,"usgs":true,"family":"Reilly","given":"Thomas","email":"tereilly@usgs.gov","middleInitial":"E.","affiliations":[{"id":493,"text":"Office of Ground Water","active":true,"usgs":true}],"preferred":true,"id":175554,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":18735,"text":"ofr94319 - 1994 - Compilation of selected hydrologic data, through water year 1992, Black Hills Hydrology Study, western South Dakota","interactions":[],"lastModifiedDate":"2012-02-02T00:07:24","indexId":"ofr94319","displayToPublicDate":"1995-01-10T00:00:00","publicationYear":"1994","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":"94-319","title":"Compilation of selected hydrologic data, through water year 1992, Black Hills Hydrology Study, western South Dakota","docAbstract":"This report presents water-level, water-quailty, and springflow data that have been collected or compiled, through water year 1992, for the Black Hills Hydrology Study. This study is a long-term cooperative effort between the U.S. Geological Survey, the South Dakota Department of Environmental and Natural Resources, and the West Dakota Water Development District (which represents various local and county cooperators). Water-level data are presented for 32 observation wells and 2 cave sites in the Black Hills area of western South Dakota. The wells are part of a network of observation wells maintained by the South Dakota Department of Environment and Natural Resources and are completed in various bedrock formations that are utilized as aquifers in the Black Hills area. Both cave sites are located within outcrops of the Madison Limestone. Data presented include site descriptions, hydrographs, and tabular data. Water- quality data are presented for 12 surface-water sites and 5 ground-water sites. Data presented include field parameters, bacteria counts, and concentrations of common ions, solids, nutrients, trace elements, radiometrics, cyanide, phenols, dissolved organic carbon, and suspended sediment. Spring data are presented for 83 springs and 21 stream reaches with significant springflow components. Data presented include site information, discharge, and field water-quality parameters including temperature, specific conductance, dissolved oxygen, and pH.","language":"ENGLISH","publisher":"U.S. Geological Survey ;\r\nUSGS Earth Science Information Center, Open-File Reports Section [distributor],","doi":"10.3133/ofr94319","usgsCitation":"Driscoll, D.G., and Bradford, W., 1994, Compilation of selected hydrologic data, through water year 1992, Black Hills Hydrology Study, western South Dakota: U.S. Geological Survey Open-File Report 94-319, vi, 158 p. :ill., maps ;28 cm., https://doi.org/10.3133/ofr94319.","productDescription":"vi, 158 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":151286,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1994/0319/report-thumb.jpg"},{"id":48096,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1994/0319/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1be4b07f02db6a8a50","contributors":{"authors":[{"text":"Driscoll, Daniel G. dgdrisco@usgs.gov","contributorId":1558,"corporation":false,"usgs":true,"family":"Driscoll","given":"Daniel","email":"dgdrisco@usgs.gov","middleInitial":"G.","affiliations":[{"id":562,"text":"South Dakota Water Science Center","active":true,"usgs":true}],"preferred":true,"id":179647,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bradford, Wendell","contributorId":52987,"corporation":false,"usgs":true,"family":"Bradford","given":"Wendell","affiliations":[],"preferred":false,"id":179648,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":17763,"text":"ofr94308 - 1994 - Surface-water-quality assessment of the Yakima River basin in Washington: major-and minor-element data for sediment, water, and aquatic biota, 1987-91","interactions":[],"lastModifiedDate":"2017-02-07T09:54:13","indexId":"ofr94308","displayToPublicDate":"1995-01-10T00:00:00","publicationYear":"1994","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":"94-308","title":"Surface-water-quality assessment of the Yakima River basin in Washington: major-and minor-element data for sediment, water, and aquatic biota, 1987-91","docAbstract":"Major- and minor-element concentrations are presented for streambed and suspended sediment, filtered- and unfiltered-water, and aquatic-biota samples collected during 1987-91 from the Yakima River Basin in south-central Washington. The samples were collected as part of the U.S. Geological Survey's National Water-quality Assessment (NAWQA) program which is designed to provide results that are useful in understanding and managing the Nation's water resources. This report includes the sampling approach, field collection and processing techniques, and methods of chemical analysis, as well as a compilation of chemical data, statistical summaries, and quality- control data. These data may be used by scientists and resource managers to describe (1) spatial distribution of selected major and minor elements in sediment, water, and aquatic biota of the Yakima River Basin; (2) temporal variation for element concentrations in filtered water and in suspended sediment at selected sites; (3) suita- bility of surface water for preservation of aquatic life and protection of human health; and (4) major natural and anthropogenic sources of major and minor elements in the Yakima River Basin that affect observed water-quality conditions.
\nStreambed-sediment samples were collected once from 27 sites in the basin during 1987-91. Suspended-sediment and filtered-water samples were collected monthly and during hydrologic events (including snowmelt and winter rainstorms) at seven sites, and filtered-water samples were collected at least once at an additional 37 sites during synoptic samplings. Unfiltered-water samples were collected at seven sites on a quarterly basis during 1987 only. Samples of aquatic plants were collected once in 1989, and aquatic insects, fish, and clams were collected from 34 sites three times during 1989-90.
","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Portland, OR","doi":"10.3133/ofr94308","usgsCitation":"Fuhrer, G.J., Fluter, S.L., McKenzie, S.W., Rinella, J.F., Crawford, J.K., Cain, D.J., Hornberger, M.I., Bridges, J.L., and Skach, K.A., 1994, Surface-water-quality assessment of the Yakima River basin in Washington: major-and minor-element data for sediment, water, and aquatic biota, 1987-91: U.S. Geological Survey Open-File Report 94-308, vi, 222 p., https://doi.org/10.3133/ofr94308.","productDescription":"vi, 222 p.","onlineOnly":"N","additionalOnlineFiles":"N","temporalStart":"1987-01-01","temporalEnd":"1991-12-31","costCenters":[{"id":518,"text":"Oregon Water Science Center","active":true,"usgs":true}],"links":[{"id":46993,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1994/0308/report.pdf","text":"Report","size":"3.90 MB","linkFileType":{"id":1,"text":"pdf"},"description":"Report"},{"id":150597,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1994/0308/report-thumb.jpg"}],"country":"United States","state":"Washington","otherGeospatial":"Yakima River Basin","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -121.717529296875,\n 46.10561307998295\n ],\n [\n -121.717529296875,\n 47.42251265435723\n ],\n [\n -119.28955078124999,\n 47.42251265435723\n ],\n [\n -119.28955078124999,\n 46.10561307998295\n ],\n [\n -121.717529296875,\n 46.10561307998295\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae5e4b07f02db68a4d2","contributors":{"authors":[{"text":"Fuhrer, Gregory J. gjfuhrer@usgs.gov","contributorId":944,"corporation":false,"usgs":true,"family":"Fuhrer","given":"Gregory","email":"gjfuhrer@usgs.gov","middleInitial":"J.","affiliations":[],"preferred":true,"id":177724,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Fluter, Shelley L.","contributorId":36419,"corporation":false,"usgs":true,"family":"Fluter","given":"Shelley","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":177727,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"McKenzie, Stuart W.","contributorId":27841,"corporation":false,"usgs":true,"family":"McKenzie","given":"Stuart","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":177730,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Rinella, Joseph F. jrinella@usgs.gov","contributorId":1371,"corporation":false,"usgs":true,"family":"Rinella","given":"Joseph","email":"jrinella@usgs.gov","middleInitial":"F.","affiliations":[],"preferred":true,"id":177732,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Crawford, J. Kent","contributorId":54176,"corporation":false,"usgs":true,"family":"Crawford","given":"J.","email":"","middleInitial":"Kent","affiliations":[],"preferred":false,"id":177725,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Cain, Daniel J. 0000-0002-3443-0493 djcain@usgs.gov","orcid":"https://orcid.org/0000-0002-3443-0493","contributorId":1784,"corporation":false,"usgs":true,"family":"Cain","given":"Daniel","email":"djcain@usgs.gov","middleInitial":"J.","affiliations":[{"id":37277,"text":"WMA - Earth System Processes Division","active":true,"usgs":true},{"id":438,"text":"National Research Program - Western Branch","active":true,"usgs":true}],"preferred":true,"id":177731,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Hornberger, Michelle I. 0000-0002-7787-3446 mhornber@usgs.gov","orcid":"https://orcid.org/0000-0002-7787-3446","contributorId":1037,"corporation":false,"usgs":true,"family":"Hornberger","given":"Michelle","email":"mhornber@usgs.gov","middleInitial":"I.","affiliations":[{"id":37277,"text":"WMA - Earth System Processes Division","active":true,"usgs":true}],"preferred":true,"id":177726,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Bridges, Jennifer L.","contributorId":42480,"corporation":false,"usgs":true,"family":"Bridges","given":"Jennifer","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":177729,"contributorType":{"id":1,"text":"Authors"},"rank":8},{"text":"Skach, Kenneth A. kaskach@usgs.gov","contributorId":1894,"corporation":false,"usgs":true,"family":"Skach","given":"Kenneth","email":"kaskach@usgs.gov","middleInitial":"A.","affiliations":[],"preferred":true,"id":177728,"contributorType":{"id":1,"text":"Authors"},"rank":9}]}} ,{"id":19787,"text":"ofr94353 - 1994 - Hydrologic Instrumentation Facility of the U.S. Geological Survey, annual report for fiscal year 1993","interactions":[],"lastModifiedDate":"2012-02-02T00:07:35","indexId":"ofr94353","displayToPublicDate":"1995-01-10T00:00:00","publicationYear":"1994","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":"94-353","title":"Hydrologic Instrumentation Facility of the U.S. Geological Survey, annual report for fiscal year 1993","docAbstract":"The Hydrologic lnstrumentation Facility (HIF) of the U.S. Geological Survey (USGS) has nationwide responsibility for all aspects of hydrologic field instrumentation in support of Survey data-collection programs. Each year the HIF publishes a report to inform Water Resources Division (WRD) personnel of progress made by the HIF in fulfilling its mission to improve instrumentation services to the Division. The report for fiscal year 1993 (FY93) describes the activities of the HIF, including major accomplish- ments for the year; personnel actions; active projects (reported by section--Technical Services Section, Administrative Services Section, Field Coordination, Applications and Development Section, Test and Evaluation Section, Field Service and Supply Section); and planned activities for the coming year. Also presented in the appendixes are detailed listings of the memberships of the Instrumentation Committee and the Instrumentation Technical Advisory Subcommittee; district, sub- district, and field office visits by HIF personnel; professional and technical meetings attended by HIF personnel; vendor visits; and reports prepared by HIF personnel.","language":"ENGLISH","publisher":"U.S. Geological Survey :\r\nEarth Science Information Center, Open-File Reports Section [distributor],","doi":"10.3133/ofr94353","usgsCitation":"Latkovich, V., and Tracey, D.C., 1994, Hydrologic Instrumentation Facility of the U.S. Geological Survey, annual report for fiscal year 1993: U.S. Geological Survey Open-File Report 94-353, iv, 47 p. :ill. ;28 cm., https://doi.org/10.3133/ofr94353.","productDescription":"iv, 47 p. :ill. ;28 cm.","costCenters":[],"links":[{"id":152538,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1994/0353/report-thumb.jpg"},{"id":49263,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1994/0353/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a2de4b07f02db6145cd","contributors":{"authors":[{"text":"Latkovich, V.J.","contributorId":52576,"corporation":false,"usgs":true,"family":"Latkovich","given":"V.J.","email":"","affiliations":[],"preferred":false,"id":181510,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Tracey, Debra C.","contributorId":89157,"corporation":false,"usgs":true,"family":"Tracey","given":"Debra","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":181511,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":18273,"text":"ofr94329 - 1994 - Hydrogeologic and water-quality data from wells near the Hueco Bolson Recharge Project area, El Paso, Texas, 1990 and 1991","interactions":[],"lastModifiedDate":"2019-12-08T13:58:17","indexId":"ofr94329","displayToPublicDate":"1995-01-10T00:00:00","publicationYear":"1994","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":"94-329","title":"Hydrogeologic and water-quality data from wells near the Hueco Bolson Recharge Project area, El Paso, Texas, 1990 and 1991","docAbstract":"Tertiary-treated wastewater currently (1991) is being injected into the Hueco bolson aquifer at a site in northeastern El Paso, Texas, to supplement the quantity of available freshwater. Hydrologic data were compiled and water-quality and bacterial data were collected from existing wells near the Hueco Bolson Recharge Project (HBRP) in August and September 1990 and 1991.
\nBorehole tracer tests indicated upward ground-water flow in nearly all tested intervals of several observation wells. The cumulative volume of injected water was less than the volume produced from wells adjacent to the HBRP area. Water levels in three production wells, located more than 1.5 miles from the injection wells, declined at rates comparable to those observed before injection operations. Water levels in wells located within 0.75 mile of the injection-well pipeline declined at a slower rate after HBRP injection operations had begun. Between 1985 and 1991, water levels in observation wells located within 700 feet of an injection well either did not appreciably decline, or declined at smaller rates than water levels in more distant production wells.
\nTrihalomethane compounds were detected in water from 8 of the 16 observation and production wells sampled in 1990 and in 10 of the 17 wells sampled in 1991. Concentrations of trihalomethane compounds in these samples ranged from 0.05 to 1.9 |lg/L (micrograms per liter) in 1990 and from 0.05 to 1.4 |ig/L in 1991. Concentrations of trihalomethane compounds in samples of injected water from two wells were 27.8 and 34.6 |J,g/L respectively, in 1991. Dibromomethane and dichloromethane were detected in water from injection wells and from observation wells within about 700 feet of the injection wells.
\nAerobic bacteria were determined to be the only bacteria type present in ground water except for samples from two wells, which also contained denitrifying bacteria. The populations of aerobic bacteria determined in ground water ranged from 80 to more than 160,000 most probable number of organisms per milliliter of sample.
","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr94329","usgsCitation":"Brock, R.D., Buszka, P.M., and Godsy, E.M., 1994, Hydrogeologic and water-quality data from wells near the Hueco Bolson Recharge Project area, El Paso, Texas, 1990 and 1991: U.S. Geological Survey Open-File Report 94-329, v, 85 p., https://doi.org/10.3133/ofr94329.","productDescription":"v, 85 p.","numberOfPages":"90","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true},{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":151165,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1994/0329/report-thumb.jpg"},{"id":47626,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1994/0329/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Texas","city":"El Paso","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -106.64154052734374,\n 31.5668353078939\n ],\n [\n -106.15814208984374,\n 31.5668353078939\n ],\n [\n -106.15814208984374,\n 32.010404958190534\n ],\n [\n -106.64154052734374,\n 32.010404958190534\n ],\n [\n -106.64154052734374,\n 31.5668353078939\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a50e4b07f02db628c2d","contributors":{"authors":[{"text":"Brock, Robert D.","contributorId":27875,"corporation":false,"usgs":true,"family":"Brock","given":"Robert","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":178829,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Buszka, Paul M. 0000-0001-8218-826X pmbuszka@usgs.gov","orcid":"https://orcid.org/0000-0001-8218-826X","contributorId":1786,"corporation":false,"usgs":true,"family":"Buszka","given":"Paul","email":"pmbuszka@usgs.gov","middleInitial":"M.","affiliations":[{"id":27231,"text":"Indiana-Kentucky Water Science Center","active":true,"usgs":true},{"id":346,"text":"Indiana Water Science Center","active":true,"usgs":true}],"preferred":true,"id":178828,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Godsy, Edward M.","contributorId":66278,"corporation":false,"usgs":true,"family":"Godsy","given":"Edward","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":178830,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":20679,"text":"ofr93466 - 1994 - Geologic and hydrologic data collected at test hole NC-8, Vega Alta, Puerto Rico","interactions":[],"lastModifiedDate":"2012-02-02T00:07:46","indexId":"ofr93466","displayToPublicDate":"1995-01-10T00:00:00","publicationYear":"1994","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"93-466","title":"Geologic and hydrologic data collected at test hole NC-8, Vega Alta, Puerto Rico","docAbstract":"Test hole NC-8 was drilled in the municipality of Vega Alta as part of a study of the aquifers in the Northern Coastal Province of Puerto Rico. Test hole NC-8 was drilled to a depth of 1,736 feet below land surface. Geologic and hydrologic data collected during drilling included continuous core, water- quality samples, water-level measurements, and estimates of aquifer yields from the water-bearing zones. Test hole NC-8 penetrated five geologic formations of middle Tertiary age: the Aymamon Limestone, the Los Puertos Formation, the Cibao Formation, the Lares Limestone, and the San Sebastian Formation. Test hole NC-8 penetrated a water-table aquifer and seven artesian aquifers.","language":"ENGLISH","publisher":"U.S. Geological Survey ;\r\nUSGS Earth Science Information Center, Open-File Reports Section [distributor],","doi":"10.3133/ofr93466","usgsCitation":"Rodríguez-Martínez, J., and Scharlach, R.A., 1994, Geologic and hydrologic data collected at test hole NC-8, Vega Alta, Puerto Rico: U.S. Geological Survey Open-File Report 93-466, iv, 16 p. :ill., maps ;28 cm., https://doi.org/10.3133/ofr93466.","productDescription":"iv, 16 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":154012,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1993/0466/report-thumb.jpg"},{"id":50203,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1993/0466/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1ae4b07f02db6a8213","contributors":{"authors":[{"text":"Rodríguez-Martínez, Jesús","contributorId":48149,"corporation":false,"usgs":true,"family":"Rodríguez-Martínez","given":"Jesús","affiliations":[],"preferred":false,"id":183051,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Scharlach, Richard A.","contributorId":59475,"corporation":false,"usgs":true,"family":"Scharlach","given":"Richard","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":183052,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":20682,"text":"ofr93465 - 1994 - Geologic and hydrologic data collected at test holes NC-6 and NC-11, Hatillo and Isabela, northwestern Puerto Rico","interactions":[],"lastModifiedDate":"2012-02-02T00:07:46","indexId":"ofr93465","displayToPublicDate":"1995-01-10T00:00:00","publicationYear":"1994","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"93-465","title":"Geologic and hydrologic data collected at test holes NC-6 and NC-11, Hatillo and Isabela, northwestern Puerto Rico","docAbstract":"Test holes NC-6 and NC-11 were drilled in the municipalities of Hatillo and Isabela, respectively, as part of a study of the aquifers in the Northern Coastal Province of Puerto Rico. Test holes NC-6 and NC-11 were drilled to depths of 2,574 and 2,120 feet below land surface, respectively. Geologic and hydrologic data collected during drilling included continuous core, water-quality samples, water-level measurements, and estimates of aquifer yields from the water-bearing zones. Test hole NC-6 penetrated five formations ranging in age from late Oligocene to early Pliocene: the Lares Limestone, the Cibao Formation, the Los Puertos Formation, the Aymamon Limestone, and the Quebradillas Limestone. This test hole also penetrated a water-table aquifer and six artesian aquifer. Test hole NC-11 penetrated four formations ranging in age from late 01igocene to middle Miocene: the San Sebastian Formation, the Cibao Formation, the Los Puertos, and the Aymamon Limestone. A water-table aquifer and four artesian aquifers were penetrated by this well.","language":"ENGLISH","publisher":"U.S. Geological Survey ;\r\nUSGS Earth Science Information Center, Open-File Reports Section [distributor],","doi":"10.3133/ofr93465","usgsCitation":"Rodríguez-Martínez, J., and Hartley, J.L., 1994, Geologic and hydrologic data collected at test holes NC-6 and NC-11, Hatillo and Isabela, northwestern Puerto Rico: U.S. Geological Survey Open-File Report 93-465, iv, 39 p. :ill., maps ;28 cm., https://doi.org/10.3133/ofr93465.","productDescription":"iv, 39 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":154028,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1993/0465/report-thumb.jpg"},{"id":50205,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1993/0465/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1ae4b07f02db6a81e7","contributors":{"authors":[{"text":"Rodríguez-Martínez, Jesús","contributorId":48149,"corporation":false,"usgs":true,"family":"Rodríguez-Martínez","given":"Jesús","affiliations":[],"preferred":false,"id":183059,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hartley, John L.","contributorId":57095,"corporation":false,"usgs":true,"family":"Hartley","given":"John","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":183060,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":18106,"text":"ofr94301 - 1994 - Hydrogeologic and water-quality data for the main site, Naval Surface Warfare Center, Dahlgren Laboratory, Dahlgren, Virginia","interactions":[],"lastModifiedDate":"2012-02-02T00:07:15","indexId":"ofr94301","displayToPublicDate":"1995-01-10T00:00:00","publicationYear":"1994","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":"94-301","title":"Hydrogeologic and water-quality data for the main site, Naval Surface Warfare Center, Dahlgren Laboratory, Dahlgren, Virginia","docAbstract":"Hydrogeologic and water-quality data were collected at the Naval Surface Warfare Center, Dahlgren Laboratory at Dahlgren, Virginia, as part of a hydrogeologic assessment of the shallow aquifer system begun in 1992. The U.S. Geological Survey conducted this study to provide the Navy with hydrogeologic data to meet the requirements of a Spill Contingency Plan. This report describes the ground-water observation-well network, hydro- geologic, and water-quality data collected between August 1992 and September 1993. The report includes a description of the locations and con- struction of 35 observation wells on the Main Site. Hydrologic data include lithologic core samples, geophysical logs, and vertical hydraulic conductivity measurements of selected core intervals. Hydrologic data include synoptic and hourly measurements of ground-water levels, observation-well slug tests to determine horizontal hydraulic conductivity, and tide data. Water-quality data include analyses of major dissolved constituents in ground water and surface water.","language":"ENGLISH","publisher":"U.S. Geological Survey ;\r\nU.S. Geological Survey, Earth Science Information Center, Open-File Reports Section [distributor],","doi":"10.3133/ofr94301","usgsCitation":"Bell, C.F., Bolles, T.P., and Harlow, G., 1994, Hydrogeologic and water-quality data for the main site, Naval Surface Warfare Center, Dahlgren Laboratory, Dahlgren, Virginia: U.S. Geological Survey Open-File Report 94-301, iv, 81 p. :ill., maps ;28 cm., https://doi.org/10.3133/ofr94301.","productDescription":"iv, 81 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":149280,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1994/0301/report-thumb.jpg"},{"id":21589,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1994/0301/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":47462,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1994/0301/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a50e4b07f02db628c54","contributors":{"authors":[{"text":"Bell, Clifton F.","contributorId":79905,"corporation":false,"usgs":true,"family":"Bell","given":"Clifton","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":178560,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bolles, Thomas P.","contributorId":22374,"corporation":false,"usgs":true,"family":"Bolles","given":"Thomas","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":178559,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Harlow, George E. Jr. geharlow@usgs.gov","contributorId":383,"corporation":false,"usgs":true,"family":"Harlow","given":"George E.","suffix":"Jr.","email":"geharlow@usgs.gov","affiliations":[{"id":614,"text":"Virginia Water Science Center","active":true,"usgs":true}],"preferred":false,"id":178558,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":30522,"text":"wri924187 - 1994 - Hydrology and geochemistry of a surface coal mine in northwestern Colorado","interactions":[],"lastModifiedDate":"2012-02-02T00:08:57","indexId":"wri924187","displayToPublicDate":"1995-01-10T00:00:00","publicationYear":"1994","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"92-4187","title":"Hydrology and geochemistry of a surface coal mine in northwestern Colorado","docAbstract":"The hydrology and geochemistry of a reclaimed coal mine in northwestern Colorado were monitored during water years 1988 and 1989. Some data also were collected in water years 1987 and 1990. This report describes (1) the sources of hydrologic recharge to and discharge from reclaimed spoil, (2) the relative contributions of recharge to the reclaimed spoil aquifer from identified source waters and the rate of water movement from those sources to the reclaimed spoil, and (3) the geochemical reactions that control water quality in reclaimed spoil. The study area was at a dip-slope coal mine encompassing about 7 square miles with land slopes of varying aspect. The area was instrumented and monitored at five sites; two sites had unmined and reclaimed- spoil areas adjacent to each other and three sites were unmined. The mined areas had been reclaimed. Instrumentation at the study sites included 1 climate station, 3 rain gages, 19 soil-water access tubes, 2 lysimeters, 18 wells completed in bedrock, 7 wells completed in reclaimed spoil, and 2 surface- water gaging stations. The results of the study indicate that the reclaimed spoil is recharged from surface recharge and underburden aquifers. Discharge, as measured by lysimeters, was about 3 inches per year and occurred during and after snowmelt. Hydraulic-head measurements indicated a potential for ground-water movement from deeper to shallower aquifers. Water levels rose in the reclaimed-spoil aquifer and spring discharge at the toe of the spoil slopes increased rapidly in response to snowmelt. Water chemistry, stable isotopes, geochemical models, and mass-balance calculations indicate that surface recharge and the underburden aquifers each contribute about 50 percent of the water to the reclaimed-spoil aquifers. Geochemical information indicates that pyrite oxidation and dissolution of carbonate and efflorescent sulfate minerals control the water chemistry of the reclaimed-spoil aquifer.","language":"ENGLISH","publisher":"U.S. Dept. of the Interior, U.S. Geological Survey :\r\nEarth Science Information Center, Open-File Reports Section [distributor],","doi":"10.3133/wri924187","usgsCitation":"Williams, R., and Clark, G.M., 1994, Hydrology and geochemistry of a surface coal mine in northwestern Colorado: U.S. Geological Survey Water-Resources Investigations Report 92-4187, vi, 61 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri924187.","productDescription":"vi, 61 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":124119,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1992/4187/report-thumb.jpg"},{"id":59301,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1992/4187/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a18e4b07f02db604da8","contributors":{"authors":[{"text":"Williams, R.S. Jr.","contributorId":46102,"corporation":false,"usgs":true,"family":"Williams","given":"R.S.","suffix":"Jr.","email":"","affiliations":[],"preferred":false,"id":203394,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Clark, G. M.","contributorId":90325,"corporation":false,"usgs":true,"family":"Clark","given":"G.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":203395,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":29254,"text":"wri914183 - 1994 - Effects of changing irrigation practices on the ground-water hydrology of the Santa Isabel-Juana Díaz area, south central Puerto Rico","interactions":[],"lastModifiedDate":"2022-01-18T21:46:45.375419","indexId":"wri914183","displayToPublicDate":"1995-01-10T00:00:00","publicationYear":"1994","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"91-4183","title":"Effects of changing irrigation practices on the ground-water hydrology of the Santa Isabel-Juana Díaz area, south central Puerto Rico","docAbstract":"Prior to 1930, the principal source of water for irrigation in the Santa Isabel-Juana Diaz area was surface water from outside the study area, which was delivered by a complex channel-pond system. Recharge from water applied to the fields, estimated to be 18.7 million of gallons per day, and discharge by ground-water flow to sea, estimated to be 17 million of gallons per day, were the major water- budget components prior to intensive development of the ground-water resources. Development of the ground-water resources after 1930 resulted in a substantial increase in irrigation, primarily furrow irrigation. The surface water supplied by the complex channel-pond system continued to be used and ground-water withdrawals increased sub- stantially. By 1966-68, ground-water recharge from irrigation water applied to the fields, estimated to be 37 million of gallons per day, and discharge by pumpage for irrigation, estimated to be 77 million of gallons per day, were the two major components of the ground-water budget. By 1987, drip irrigation had become the principal method of irrigation in the study area, and surface-water irrigation had, for the most part, been discontinued. The estimated aquifer recharge from irrigation water in 1987 was about 6.6 million of gallons per day, which occurred primarily in the remaining fields where furrow irrigation was still practiced. Although aquifer recharge had been reduced as a result of the conversion from furrow to drip irrigation, water levels in the aquifer were higher in 1987 than in 1968 because of the large reduction in ground-water withdrawals and subsequent recovery of ground-water levels.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri914183","usgsCitation":"Ramos-Gines, O., 1994, Effects of changing irrigation practices on the ground-water hydrology of the Santa Isabel-Juana Díaz area, south central Puerto Rico: U.S. Geological Survey Water-Resources Investigations Report 91-4183, iv, 22 p., https://doi.org/10.3133/wri914183.","productDescription":"iv, 22 p.","costCenters":[],"links":[{"id":394477,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_47571.htm"},{"id":58104,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1991/4183/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":123542,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1991/4183/report-thumb.jpg"}],"country":"United States","state":"Puerto Rico","otherGeospatial":"Santa Isabel - Juana Diaz area","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -66.5064239501953,\n 17.93496881111123\n ],\n [\n -66.31553649902344,\n 17.93496881111123\n ],\n [\n -66.31553649902344,\n 18.0224865348244\n ],\n [\n -66.5064239501953,\n 18.0224865348244\n ],\n [\n -66.5064239501953,\n 17.93496881111123\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a4ae4b07f02db6248c7","contributors":{"authors":[{"text":"Ramos-Gines, Orlando","contributorId":98358,"corporation":false,"usgs":true,"family":"Ramos-Gines","given":"Orlando","affiliations":[],"preferred":false,"id":201227,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":44765,"text":"wri934096 - 1994 - Estimated withdrawals and use of freshwater in New Hampshire, 1990","interactions":[],"lastModifiedDate":"2012-02-02T00:05:00","indexId":"wri934096","displayToPublicDate":"1995-01-10T00:00:00","publicationYear":"1994","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"93-4096","title":"Estimated withdrawals and use of freshwater in New Hampshire, 1990","docAbstract":"Estimated freshwater withdrawals during 1990 in New Hampshire totaled about 422 million gallons per day from ground-water and surface-water sources. The largest withdrawals were for thermoelectric-power generation (60 percent), public supply (23 percent), and industrial use (9 percent). Most withdrawals, 358 million gallons per day, were made from surface- water sources, as compared to 63.7 million gallons per day from ground-water sources. The largest with- drawals were in the Merrimack river basin (322 million gallons per day). An additional 46,000 million gallons per day was used instream for hydroelectric-power generation, primarily in the Upper Androscoggin and Upper Connecticut River subbasins. Other information describing water-use patterns is shown in tables, bar graphs, pie charts, maps, and accompanying text. The data are aggregated by river basin (hydrologic cataloging unit), and all values are reported in million gallons per day.","language":"ENGLISH","doi":"10.3133/wri934096","usgsCitation":"Medalie, L., and Horn, M., 1994, Estimated withdrawals and use of freshwater in New Hampshire, 1990: U.S. Geological Survey Water-Resources Investigations Report 93-4096, 10 maps on 1 sheet : col. ; 20 x 10 cm. and 8 x 5 cm., sheet 86 x 102 cm., folded to 21 x 22 cm., https://doi.org/10.3133/wri934096.","productDescription":"10 maps on 1 sheet : col. ; 20 x 10 cm. and 8 x 5 cm., sheet 86 x 102 cm., folded to 21 x 22 cm.","costCenters":[],"links":[{"id":135757,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":82072,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1993/4096/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0ce4b07f02db5fcb91","contributors":{"authors":[{"text":"Medalie, Laura 0000-0002-2440-2149 lmedalie@usgs.gov","orcid":"https://orcid.org/0000-0002-2440-2149","contributorId":3657,"corporation":false,"usgs":true,"family":"Medalie","given":"Laura","email":"lmedalie@usgs.gov","affiliations":[{"id":466,"text":"New England Water Science Center","active":true,"usgs":true}],"preferred":true,"id":230387,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Horn, M.A.","contributorId":92223,"corporation":false,"usgs":true,"family":"Horn","given":"M.A.","email":"","affiliations":[],"preferred":false,"id":230388,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":20508,"text":"ofr94364 - 1994 - Annual yield and selected hydrologic data for the Arkansas River Basin Compact Arkansas-Oklahoma 1993 water year","interactions":[],"lastModifiedDate":"2012-02-02T00:07:35","indexId":"ofr94364","displayToPublicDate":"1995-01-10T00:00:00","publicationYear":"1994","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":"94-364","title":"Annual yield and selected hydrologic data for the Arkansas River Basin Compact Arkansas-Oklahoma 1993 water year","docAbstract":"The computed annual yield and deficiency of the subbasins as defined in the Arkansas River Basin Compact, Arkansas-Oklahoma, are given in tables for the 1993 water year. Actual runoff from the subbasins and depletion caused by major reservoirs in the compact area also are given in tabular form. Monthly maximum, minimum, and mean discharges are shown for the 14 streamflow stations used in computing annual yield. Water-quality data are shown for 12 water-quality stations sampled in the Arkansas River Basin.","language":"ENGLISH","publisher":"U.S. Geological Survey ;\r\nUSGS Earth Science Information Center, Open-File Reports Section [distributor],","doi":"10.3133/ofr94364","usgsCitation":"Porter, J., and Barks, C.S., 1994, Annual yield and selected hydrologic data for the Arkansas River Basin Compact Arkansas-Oklahoma 1993 water year: U.S. Geological Survey Open-File Report 94-364, iii, 61 p. :map ;28 cm., https://doi.org/10.3133/ofr94364.","productDescription":"iii, 61 p. :map ;28 cm.","costCenters":[],"links":[{"id":152673,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1994/0364/report-thumb.jpg"},{"id":50044,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1994/0364/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac8e4b07f02db67b777","contributors":{"authors":[{"text":"Porter, J.E.","contributorId":51779,"corporation":false,"usgs":true,"family":"Porter","given":"J.E.","email":"","affiliations":[],"preferred":false,"id":182773,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Barks, C. Shane csbarks@usgs.gov","contributorId":2088,"corporation":false,"usgs":true,"family":"Barks","given":"C.","email":"csbarks@usgs.gov","middleInitial":"Shane","affiliations":[],"preferred":true,"id":182772,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70205826,"text":"70205826 - 1994 - Ground-water contamination by petroleum hydrocarbons: Natural biodegradation in a dynamic hydrologic and geochemical system","interactions":[],"lastModifiedDate":"2019-10-07T12:52:49","indexId":"70205826","displayToPublicDate":"1994-12-31T12:47:06","publicationYear":"1994","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"title":"Ground-water contamination by petroleum hydrocarbons: Natural biodegradation in a dynamic hydrologic and geochemical system","docAbstract":"No abstract available.
","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Proceedings of the 208th ACS National Meeting","largerWorkSubtype":{"id":12,"text":"Conference publication"},"conferenceTitle":"208th American Chemical Society National Meeting","conferenceDate":"August 21-26, 1994","language":"English","publisher":"American Chemical Society","usgsCitation":"Cozzarelli, I.M., Baedecker, M.J., Fischer, J., and Phinney, C., 1994, Ground-water contamination by petroleum hydrocarbons: Natural biodegradation in a dynamic hydrologic and geochemical system, in Proceedings of the 208th ACS National Meeting, v. 34, August 21-26, 1994, p. 588-592.","productDescription":"5 p.","startPage":"588","endPage":"592","costCenters":[{"id":470,"text":"New Jersey Water Science Center","active":true,"usgs":true}],"links":[{"id":368054,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"34","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"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":49175,"text":"Geology, Energy & Minerals Science Center","active":true,"usgs":true},{"id":436,"text":"National Research Program - Eastern Branch","active":true,"usgs":true}],"preferred":true,"id":772508,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Baedecker, Mary Jo 0000-0002-4865-1043 mjbaedec@usgs.gov","orcid":"https://orcid.org/0000-0002-4865-1043","contributorId":197793,"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":true,"id":772509,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Fischer, Jeffrey 0000-0003-2996-9272 fischer@usgs.gov","orcid":"https://orcid.org/0000-0003-2996-9272","contributorId":187753,"corporation":false,"usgs":true,"family":"Fischer","given":"Jeffrey","email":"fischer@usgs.gov","affiliations":[],"preferred":true,"id":772510,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Phinney, C.S.","contributorId":50302,"corporation":false,"usgs":true,"family":"Phinney","given":"C.S.","email":"","affiliations":[],"preferred":false,"id":772511,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":70231437,"text":"70231437 - 1994 - Interstadial climatic cycles: A link between western North America and Greenland?","interactions":[],"lastModifiedDate":"2022-05-10T16:41:38.219254","indexId":"70231437","displayToPublicDate":"1994-12-01T11:33:25","publicationYear":"1994","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1796,"text":"Geology","active":true,"publicationSubtype":{"id":10}},"title":"Interstadial climatic cycles: A link between western North America and Greenland?","docAbstract":"During the interval 33.6 to 26.1 ka, Searles Lake in southeastern California went through six major cycles of expansion and contraction. A comparison of U/Th ages for these events with the chronologies for quasi-cyclic interstadial episodes in the ice core from Summit, Greenland, suggests that the episodes of low water at Searles Lake are synchronous with the interstadial episodes at Summit. The two phenomena may be linked by variations in the strength of the global hydrological cycle, driven by oscillations in the Atlantic Ocean thermohaline circulation.
","language":"English","publisher":"Geological Society of America","doi":"10.1130/0091-7613(1994)022%3C1115:ICCALB%3E2.3.CO;2","usgsCitation":"Phillips, F., Campbell, A.R., Smith, G., and Bischoff, J.L., 1994, Interstadial climatic cycles: A link between western North America and Greenland?: Geology, v. 22, no. 12, p. 1115-1118, https://doi.org/10.1130/0091-7613(1994)022%3C1115:ICCALB%3E2.3.CO;2.","productDescription":"4 p.","startPage":"1115","endPage":"1118","costCenters":[],"links":[{"id":400431,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"Greenland, United States","state":"California","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -118.5369873046875,\n 35.47632833265728\n ],\n [\n -116.92199707031249,\n 35.47632833265728\n ],\n [\n -116.92199707031249,\n 36.752089156946326\n ],\n [\n -118.5369873046875,\n 36.752089156946326\n ],\n [\n -118.5369873046875,\n 35.47632833265728\n ]\n ]\n ]\n }\n },\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -62.40234375,\n 75.73730278940474\n ],\n [\n -50.2734375,\n 75.73730278940474\n ],\n [\n -50.2734375,\n 78.31385955743478\n ],\n [\n -62.40234375,\n 78.31385955743478\n ],\n [\n -62.40234375,\n 75.73730278940474\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"22","issue":"12","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Phillips, Fred M.","contributorId":269402,"corporation":false,"usgs":false,"family":"Phillips","given":"Fred M.","affiliations":[{"id":34868,"text":"New Mexico Institute of Mining and Technology","active":true,"usgs":false}],"preferred":false,"id":842606,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Campbell, Andrew R.","contributorId":291589,"corporation":false,"usgs":false,"family":"Campbell","given":"Andrew","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":842607,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Smith, George I.","contributorId":57096,"corporation":false,"usgs":true,"family":"Smith","given":"George I.","affiliations":[],"preferred":false,"id":842608,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Bischoff, James L. jbischoff@usgs.gov","contributorId":1389,"corporation":false,"usgs":true,"family":"Bischoff","given":"James","email":"jbischoff@usgs.gov","middleInitial":"L.","affiliations":[],"preferred":true,"id":842609,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":70185734,"text":"70185734 - 1994 - Uranium retention by weathered schists-The role of iron minerals","interactions":[],"lastModifiedDate":"2019-03-01T07:00:36","indexId":"70185734","displayToPublicDate":"1994-12-01T00:00:00","publicationYear":"1994","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3226,"text":"Radiochimica Acta","active":true,"publicationSubtype":{"id":10}},"title":"Uranium retention by weathered schists-The role of iron minerals","docAbstract":"No abstract available.
","language":"English","publisher":"Walter de Gruyter GmbH","doi":"10.1524/ract.1994.6667.special-issue.297","usgsCitation":"Payne, T., Davis, J., and Waite, T., 1994, Uranium retention by weathered schists-The role of iron minerals: Radiochimica Acta, v. 66-67, no. s1, p. 297-303, https://doi.org/10.1524/ract.1994.6667.special-issue.297.","productDescription":"7 p.","startPage":"297","endPage":"303","costCenters":[{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":338476,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"66-67","issue":"s1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"58db7636e4b0ee37af29e4c8","contributors":{"authors":[{"text":"Payne, T.E.","contributorId":31916,"corporation":false,"usgs":true,"family":"Payne","given":"T.E.","email":"","affiliations":[],"preferred":false,"id":686575,"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":686576,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Waite, T.D.","contributorId":31116,"corporation":false,"usgs":true,"family":"Waite","given":"T.D.","email":"","affiliations":[],"preferred":false,"id":686577,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":70185710,"text":"70185710 - 1994 - Variability and prediction of freshwater and nitrate fluxes for the Louisiana-Texas shelf: Mississippi and Atchafalaya River source functions ","interactions":[],"lastModifiedDate":"2017-03-28T10:15:11","indexId":"70185710","displayToPublicDate":"1994-12-01T00:00:00","publicationYear":"1994","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1583,"text":"Estuaries","active":true,"publicationSubtype":{"id":10}},"title":"Variability and prediction of freshwater and nitrate fluxes for the Louisiana-Texas shelf: Mississippi and Atchafalaya River source functions ","docAbstract":"Time histories of riverine water discharge, nitrate concentration, and nitrate, flux have been analyzed for the Mississippi and Atchafalaya rivers. Results indicate that water discharge variability is dominated by the annual cycle and shorter-time-scale episodic events presumably associated with snowmelt runoff and spring or summer rains. Interannual variability in water discharge is relatively small compared to the above. In contrast, nitrate concentration exhibits strongest variability at decadal time scales. The interannual variability is not monotonic but more complicated in structure. Weak covariability between water discharge and nitrate concentration leads to a relatively “noisy” nitrate flux signal. Nitrate flux variations exhibit a low-amplitude, long-term modulation of a dominant annual cycle. Predictor-hindcastor analyses indicate that skilled forecasts of nitrate concentration and nitrate flux fields are feasible. Water discharge was the most reliably hindcast (on seasonal to interannual time scales) due to the fundamental strength of the annual hydrologic cycle. However, the forecasting effort for this variable was less successful than the hindcasting effort, mostly due to a phase shift in the annual cycle during our relatively short test period (18 mo). Nitrate concentration was more skillfully predicted (seasonal to interannual time scales) due to the relative dominance of the decadal-scale portion of the signal. Nitrate flux was also skillfully forecast even though historical analyses seemed to indicate that it should be more difficult to predict than either water discharge or nitrate concentration.
","language":"English","publisher":"Estuarine Research Federation","doi":"10.2307/1352746","usgsCitation":"Bratkovich, A., Dinnel, S., and Goolsby, D.A., 1994, Variability and prediction of freshwater and nitrate fluxes for the Louisiana-Texas shelf: Mississippi and Atchafalaya River source functions : Estuaries, v. 17, no. 4, p. 766-778, https://doi.org/10.2307/1352746.","productDescription":"13 p.","startPage":"766","endPage":"778","costCenters":[{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":338446,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"17","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"58db7636e4b0ee37af29e4cc","contributors":{"authors":[{"text":"Bratkovich, A.","contributorId":189926,"corporation":false,"usgs":false,"family":"Bratkovich","given":"A.","email":"","affiliations":[],"preferred":false,"id":686491,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Dinnel, S.P.","contributorId":189927,"corporation":false,"usgs":false,"family":"Dinnel","given":"S.P.","email":"","affiliations":[],"preferred":false,"id":686492,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Goolsby, D. A.","contributorId":50508,"corporation":false,"usgs":true,"family":"Goolsby","given":"D.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":686493,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":70185389,"text":"70185389 - 1994 - Influence of diurnal variations in stream temperature on streamflow loss and groundwater recharge","interactions":[],"lastModifiedDate":"2019-02-27T10:26:20","indexId":"70185389","displayToPublicDate":"1994-12-01T00:00:00","publicationYear":"1994","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":"Influence of diurnal variations in stream temperature on streamflow loss and groundwater recharge","docAbstract":"We demonstrate that for losing reaches with significant diurnal variations in stream temperature, the effect of stream temperature on streambed seepage is a major factor contributing to reduced afternoon streamflows. An explanation is based on the effect of stream temperature on the hydraulic conductivity of the streambed, which can be expected to double in the 0° to 25°C temperature range. Results are presented for field experiments in which stream discharge and temperature were continuously measured for several days over losing reaches at St. Kevin Gulch, Colorado, and Tijeras Arroyo, New Mexico. At St. Kevin Gulch in July 1991, the diurnal stream temperature in the 160-m study reach ranged from about 4° to 18°C, discharges ranged from 10 to 18 L/s, and streamflow loss in the study reach ranged from 2.7 to 3.7 L/s. On the basis of measured stream temperature variations, the predicted change in conductivity was about 38%; the measured change in stream loss was about 26%, suggesting that streambed temperature varied less than the stream temperature. At Tijeras Arroyo in May 1992, diurnal stream temperature in the 655-m study reach ranged from about 10° to 25°C and discharge ranged from 25 to 55 L/s. Streamflow loss was converted to infiltration rates by factoring in the changing stream reach surface area and streamflow losses due to evaporation rates as measured in a hemispherical evaporation chamber. Infiltration rates ranged from about 0.7 to 2.0 m/d, depending on time and location. Based on measured stream temperature variations, the predicted change in conductivity was 29%; the measured change in infiltration was also about 27%. This suggests that high infiltration rates cause rapid convection of heat to the streambed. Evapotranspiration losses were estimated for the reach and adjacent flood plain within the arroyo. On the basis of these estimates, only about 5% of flow loss was consumed via stream evaporation and stream-side evapotranspiration, indicating that 95% of the loss within the study reach represented groundwater recharge.
","language":"English","publisher":"American Geophysical Union","doi":"10.1029/94WR01968","usgsCitation":"Constantz, J., Thomas, C.L., and Zellweger, G.W., 1994, Influence of diurnal variations in stream temperature on streamflow loss and groundwater recharge: Water Resources Research, v. 30, no. 12, p. 3253-3264, https://doi.org/10.1029/94WR01968.","productDescription":"12 p.","startPage":"3253","endPage":"3264","costCenters":[{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":337953,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"30","issue":"12","noUsgsAuthors":false,"publicationDate":"2010-07-09","publicationStatus":"PW","scienceBaseUri":"58d23b96e4b0236b68f82956","contributors":{"authors":[{"text":"Constantz, Jim","contributorId":66338,"corporation":false,"usgs":true,"family":"Constantz","given":"Jim","affiliations":[],"preferred":false,"id":685417,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Thomas, Carole L.","contributorId":50938,"corporation":false,"usgs":true,"family":"Thomas","given":"Carole","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":685418,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Zellweger, Gary W.","contributorId":71171,"corporation":false,"usgs":true,"family":"Zellweger","given":"Gary","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":685419,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":70185724,"text":"70185724 - 1994 - Determination of atrazine in rainfall and surface water by enzyme immunoassay","interactions":[],"lastModifiedDate":"2019-02-25T10:52:14","indexId":"70185724","displayToPublicDate":"1994-12-01T00:00:00","publicationYear":"1994","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1564,"text":"Environmental Science and Pollution Research","active":true,"publicationSubtype":{"id":10}},"title":"Determination of atrazine in rainfall and surface water by enzyme immunoassay","docAbstract":"Rainwater and surface water from four sites in Germany (Bavaria and Lower Saxony) were analyzed for atrazine by enzyme immunoassay from June 1990 until October 1992. The limit of quantification of the immunoassay was 0.02 μg/L with a middle of the test at 0.2 μg/L. About 60 % of the samples contained measurable amounts of atrazine. Seasonal trends were observed, with the highest concentration in the summer months of up to 4 μg/L for rainwater and up to 15 μg/L for surface waters. The highest concentrations were found in agricultural areas, while in the investigated national parks up to 0.56 μg/L could be detected in rain water. This points to long-range atmospheric transport from agricultural areas to pristine national parks. Samples from forest stands usually showed higher atrazine concentrations than samples from open fields. Deposition rates of 10 – 50 μg/m2 · yr were observed in the national parks and 10–180 μg/m2 · yr at the agricultural sites. Comparison of results obtained by enzyme immunoassay and GC/MS showed a good correlation of r = 0.95.
","language":"English","publisher":"Ecomed Publishers","doi":"10.1007/BF02986530","usgsCitation":"Dankwardt, A., Wust, S., Elling, W., Thurman, E.M., and Hock, B., 1994, Determination of atrazine in rainfall and surface water by enzyme immunoassay: Environmental Science and Pollution Research, v. 1, no. 4, p. 196-204, https://doi.org/10.1007/BF02986530.","productDescription":"9 p. ","startPage":"196","endPage":"204","costCenters":[{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":338464,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"1","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"58db7636e4b0ee37af29e4ca","contributors":{"authors":[{"text":"Dankwardt, Andrea","contributorId":189943,"corporation":false,"usgs":false,"family":"Dankwardt","given":"Andrea","email":"","affiliations":[],"preferred":false,"id":686547,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Wust, Susanne","contributorId":189944,"corporation":false,"usgs":false,"family":"Wust","given":"Susanne","email":"","affiliations":[],"preferred":false,"id":686548,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Elling, Wolfram","contributorId":189945,"corporation":false,"usgs":false,"family":"Elling","given":"Wolfram","email":"","affiliations":[],"preferred":false,"id":686549,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Thurman, E. Michael","contributorId":9636,"corporation":false,"usgs":true,"family":"Thurman","given":"E.","email":"","middleInitial":"Michael","affiliations":[],"preferred":false,"id":686550,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Hock, Bertold","contributorId":189946,"corporation":false,"usgs":false,"family":"Hock","given":"Bertold","email":"","affiliations":[],"preferred":false,"id":686551,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}} ,{"id":70185431,"text":"70185431 - 1994 - Uranium(VI) adsorption to ferrihydrite: Application of a surface complexation model","interactions":[],"lastModifiedDate":"2020-01-07T14:56:48","indexId":"70185431","displayToPublicDate":"1994-12-01T00:00:00","publicationYear":"1994","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1759,"text":"Geochimica et Cosmochimica Acta","active":true,"publicationSubtype":{"id":10}},"title":"Uranium(VI) adsorption to ferrihydrite: Application of a surface complexation model","docAbstract":"A study of U(VI) adsorption by ferrihydrite was conducted over a wide range of U(VI) concentrations, pH, and at two partial pressures of carbon dioxide. A two-site (strong- and weak-affinity sites, FesOH and FewOH, respectively) surface complexation model was able to describe the experimental data well over a wide range of conditions, with only one species formed with each site type: an inner-sphere, mononuclear, bidentate complex of the type (FeO2)UO2. The existence of such a surface species was supported by results of uranium EXAFS spectroscopy performed on two samples with U(VI) adsorption density in the upper range observed in this study (10 and 18% occupancy of total surface sites). Adsorption data in the alkaline pH range suggested the existence of a second surface species, modeled as a ternary surface complex with UO2CO30 binding to a bidentate surface site. Previous surface complexation models for U(VI) adsorption have proposed surface species that are identical to the predominant aqueous species, e.g., multinuclear hydrolysis complexes or several U(VI)-carbonate complexes. The results demonstrate that the speciation of adsorbed U(VI) may be constrained by the coordination environment at the surface, giving rise to surface speciation for U(VI) that is significantly less complex than aqueous speciation.
","language":"English","publisher":"Elsevier","doi":"10.1016/0016-7037(94)90243-7","usgsCitation":"Waite, T., Davis, J., Payne, T., Waychunas, G., and Xu, N., 1994, Uranium(VI) adsorption to ferrihydrite: Application of a surface complexation model: Geochimica et Cosmochimica Acta, v. 58, no. 24, p. 5465-5478, https://doi.org/10.1016/0016-7037(94)90243-7.","productDescription":"14 p. ","startPage":"5465","endPage":"5478","costCenters":[{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":338018,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"58","issue":"24","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"58d38d3ce4b0236b68f98ef2","contributors":{"authors":[{"text":"Waite, T.D.","contributorId":31116,"corporation":false,"usgs":true,"family":"Waite","given":"T.D.","email":"","affiliations":[],"preferred":false,"id":685555,"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":685556,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Payne, T.E.","contributorId":31916,"corporation":false,"usgs":true,"family":"Payne","given":"T.E.","email":"","affiliations":[],"preferred":false,"id":685557,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Waychunas, G.A.","contributorId":90888,"corporation":false,"usgs":true,"family":"Waychunas","given":"G.A.","email":"","affiliations":[],"preferred":false,"id":685558,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Xu, N.","contributorId":105060,"corporation":false,"usgs":true,"family":"Xu","given":"N.","email":"","affiliations":[],"preferred":false,"id":685559,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}} ,{"id":70185417,"text":"70185417 - 1994 - Effects of land disposal of municipal sewage sludge on fate of nitrates in soil, streambed sediment, and water quality","interactions":[],"lastModifiedDate":"2019-02-27T10:21:57","indexId":"70185417","displayToPublicDate":"1994-12-01T00:00:00","publicationYear":"1994","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2342,"text":"Journal of Hydrology","active":true,"publicationSubtype":{"id":10}},"title":"Effects of land disposal of municipal sewage sludge on fate of nitrates in soil, streambed sediment, and water quality","docAbstract":"This study was undertaken to determine the effects of sewage-sludge disposal at the Lowry sewage-sludge-disposal area, near Denver, Colorado, on ground- and surface-water quality, to determine the fate of nitrates from sludge leachate, and to determine the source areas of leachate and the potential for additional leaching from the disposal area.
Sewage-sludge disposal began in 1969. Two methods were used to apply the sludge: burial and plowing. Also, the sludge was applied both in liquid and cake forms. Data in this report represent the chemical composition of soil and streambed sediment from seven soil- and four streambed-sampling sites in 1986, chemical and bacterial composition of ground water from 28 wells from 1981 to 1987, and surface-water runoff from seven water-sampling sites from 1984 to 1987. Ground water samples were obtained from alluvial and bedrock aquifers. Samples of soil, streambed sediment, ground water and surface water were obtained for onsite measurement and chemical analysis. Measurements included determination of nitrogen compounds and major cations and anions, fecal-coliform and -streptococcus bacteria, specific conductance, and pH.
Thirteen wells in the alluvial aquifer in Region 3 of the study area contain water that was probably affected by sewage-sludge leachate. The plots of concentration of nitrate with time show seasonal trends and trends caused by precipitation. In addition to yearly fluctuation, there were noticeable increases in ground-water concentrations of nitrate that coincided with increased precipitation. After 3 years of annual ground-water-quality monitoring and 4 years of a quarterly sampling program, it has been determined that leachate from the sewage-sludge-disposal area caused increased nitrite plus nitrate (as nitrogen) concentration in the alluvial ground water at the site. Soil analyses from the disposal area indicate that organic nitrogen was the dominant form of nitrogen in the soil.
As a result of investigations at the research site, it has been determined that a potentially large source of contamination exists in the soils of the study area owing to increased concentrations of nitrogen, sodium, calcium, magnesium, sulfate, bicarbonate, and chloride because of sewage disposal. Continued monitoring of surface and ground water for nitrogen and the other ions previously mentioned is required to assess long-term effects of municipal sludge disposal on water quality.
","language":"English","publisher":"Elsevier","doi":"10.1016/0022-1694(94)90027-2","usgsCitation":"Tindall, J.A., Lull, K.J., and Gaggiani, N.G., 1994, Effects of land disposal of municipal sewage sludge on fate of nitrates in soil, streambed sediment, and water quality: Journal of Hydrology, v. 163, no. 1-2, p. 147-185, https://doi.org/10.1016/0022-1694(94)90027-2.","productDescription":"39 p. ","startPage":"147","endPage":"185","costCenters":[{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":337994,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"163","issue":"1-2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"58d23b96e4b0236b68f82953","contributors":{"authors":[{"text":"Tindall, James A. 0000-0002-0940-1586 jtindall@usgs.gov","orcid":"https://orcid.org/0000-0002-0940-1586","contributorId":2529,"corporation":false,"usgs":true,"family":"Tindall","given":"James","email":"jtindall@usgs.gov","middleInitial":"A.","affiliations":[{"id":5044,"text":"National Research Program - Central Branch","active":true,"usgs":true}],"preferred":true,"id":685513,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Lull, Kenneth J.","contributorId":189642,"corporation":false,"usgs":false,"family":"Lull","given":"Kenneth","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":685514,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Gaggiani, Neville G. gaggiani@usgs.gov","contributorId":3280,"corporation":false,"usgs":true,"family":"Gaggiani","given":"Neville","email":"gaggiani@usgs.gov","middleInitial":"G.","affiliations":[],"preferred":true,"id":685515,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":70216590,"text":"70216590 - 1994 - Simulation of long-term thermal characteristics of three Estonian lakes","interactions":[],"lastModifiedDate":"2020-11-27T18:27:55.131014","indexId":"70216590","displayToPublicDate":"1994-11-25T13:40:23","publicationYear":"1994","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2342,"text":"Journal of Hydrology","active":true,"publicationSubtype":{"id":10}},"title":"Simulation of long-term thermal characteristics of three Estonian lakes","docAbstract":"A one-dimensional surface energy-balance lake model, coupled to a thermodynamic model of lake ice, is used to simulate variations in the temperature of and evaporation from three Estonian lakes: Karujärv, Viljandi and Kirjaku. The model is driven by daily climate data, derived by cubic-spline interpolation from monthly mean data, and was run for periods of 8 years (Kirjaku) up to 30 years (Viljandi). Simulated surface water temperature is in good agreement with observations: mean differences between simulated and observed temperatures are from −0.8°C to +0.1°C. The simulated duration of snow and ice cover is comparable with observed. However, the model generally underpredicts ice thickness and overpredicts snow depth. Sensitivity analyses suggest that the model results are robust across a wide range (0.1–2.0 m −1) of lake extinction coefficient: surface temperature differs by less than 0.5°C between extreme values of the extinction coefficient. The model results are more sensitive to snow and ice albedos. However, changing the snow (0.2–0.9) and ice (0.15–0.55) albedos within realistic ranges does not improve the simulations of snow depth and ice thickness. The underestimation of ice thickness is correlated with the overestimation of snow cover, since a thick snow layer insulates the ice and limits ice formation. The overestimation of snow cover results from the assumption that all the simulated winter precipitation occurs as snow, a direct consequence of using daily climate data derived by interpolation from mean monthly data.
","language":"English","publisher":"Elsevier","doi":"10.1016/0022-1694(94)90025-6","usgsCitation":"Vassiljev, J., Harrison, S., Hostetler, S.W., and Bartlein, P.J., 1994, Simulation of long-term thermal characteristics of three Estonian lakes: Journal of Hydrology, v. 163, no. 1, p. 107-123, https://doi.org/10.1016/0022-1694(94)90025-6.","productDescription":"17 p.","startPage":"107","endPage":"123","costCenters":[{"id":200,"text":"Coop Res Unit Seattle","active":true,"usgs":true},{"id":481,"text":"Northern Rocky Mountain Science Center","active":true,"usgs":true}],"links":[{"id":380816,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"Estonia","otherGeospatial":"Karujärv, Kirjaku, Viljandi","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"Polygon\",\"coordinates\":[[[24.31286,57.79342],[24.42893,58.38341],[24.0612,58.25737],[23.42656,58.61275],[23.3398,59.18724],[24.60421,59.46585],[25.86419,59.61109],[26.94914,59.4458],[27.98111,59.47539],[28.1317,59.30083],[27.42017,58.72458],[27.71669,57.7919],[27.28818,57.47453],[26.46353,57.47639],[25.60281,57.84753],[25.16459,57.97016],[24.31286,57.79342]]]},\"properties\":{\"name\":\"Estonia\"}}]}","volume":"163","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Vassiljev, J.","contributorId":21458,"corporation":false,"usgs":true,"family":"Vassiljev","given":"J.","email":"","affiliations":[],"preferred":false,"id":805689,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Harrison, S.P.","contributorId":245247,"corporation":false,"usgs":false,"family":"Harrison","given":"S.P.","email":"","affiliations":[],"preferred":false,"id":805690,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Hostetler, Steven W. 0000-0003-2272-8302 swhostet@usgs.gov","orcid":"https://orcid.org/0000-0003-2272-8302","contributorId":3249,"corporation":false,"usgs":true,"family":"Hostetler","given":"Steven","email":"swhostet@usgs.gov","middleInitial":"W.","affiliations":[{"id":200,"text":"Coop Res Unit Seattle","active":true,"usgs":true},{"id":438,"text":"National Research Program - Western Branch","active":true,"usgs":true}],"preferred":true,"id":805691,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Bartlein, Patrick J","contributorId":194325,"corporation":false,"usgs":false,"family":"Bartlein","given":"Patrick","email":"","middleInitial":"J","affiliations":[],"preferred":false,"id":805692,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":70216580,"text":"70216580 - 1994 - Stable isotopes of oxygen and hydrogen in the Truckee River–Pyramid Lake surface‐water system. 2. A predictive model of δ18O and 182H in Pyramid Lake","interactions":[],"lastModifiedDate":"2020-11-27T18:23:17.063545","indexId":"70216580","displayToPublicDate":"1994-11-25T13:12:29","publicationYear":"1994","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}},"displayTitle":"Stable isotopes of oxygen and hydrogen in the Truckee River–Pyramid Lake surface‐water system. 2. A predictive model of δ18O and 182H in Pyramid Lake","title":"Stable isotopes of oxygen and hydrogen in the Truckee River–Pyramid Lake surface‐water system. 2. A predictive model of δ18O and 182H in Pyramid Lake","docAbstract":"A physically based model of variations in δ18O and δ2H in Pyramid Lake is presented. For inputs, the model uses measurements of liquid water inflows and outflows and their associated isotopic compositions and a set of meteorological data (radiative fluxes, air temperature, relative humidity, and windspeed). The model simulates change of lake volume, thermal and isotopic stratification, evaporation, and the isotopic composition of evaporation. A validation of the model for 1987–1989 and 1991 indicates that it can reproduce measured intra‐ and interannual variations of δ18O and δ2H. Three applications of the model demonstrate its ability to simulate longer term responses of δ18O to change in the hydrologic balance and hydrologic characteristics (opening and closing) of the lake.
","language":"English","publisher":"Association for the Sciences of Limnology and Oceanography","doi":"10.4319/lo.1994.39.2.0356","usgsCitation":"Hostetler, S.W., and Benson, L.V., 1994, Stable isotopes of oxygen and hydrogen in the Truckee River–Pyramid Lake surface‐water system. 2. A predictive model of δ18O and 182H in Pyramid Lake: Limnology and Oceanography, v. 39, no. 2, p. 356-364, https://doi.org/10.4319/lo.1994.39.2.0356.","productDescription":"9 p.","startPage":"356","endPage":"364","costCenters":[{"id":481,"text":"Northern Rocky Mountain Science Center","active":true,"usgs":true}],"links":[{"id":380808,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Nevada","otherGeospatial":"Pyramid Lake","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -119.7784423828125,\n 39.8401771327549\n ],\n [\n -119.3939208984375,\n 39.8401771327549\n ],\n [\n -119.3939208984375,\n 40.212440718286466\n ],\n [\n -119.7784423828125,\n 40.212440718286466\n ],\n [\n -119.7784423828125,\n 39.8401771327549\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"39","issue":"2","noUsgsAuthors":false,"publicationDate":"2003-12-22","publicationStatus":"PW","contributors":{"authors":[{"text":"Hostetler, S. W. 0000-0003-2272-8302","orcid":"https://orcid.org/0000-0003-2272-8302","contributorId":42911,"corporation":false,"usgs":true,"family":"Hostetler","given":"S.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":805683,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Benson, L. V.","contributorId":50159,"corporation":false,"usgs":true,"family":"Benson","given":"L.","email":"","middleInitial":"V.","affiliations":[],"preferred":false,"id":805684,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70216573,"text":"70216573 - 1994 - Analysis of the surface hydrology in a regional climate model","interactions":[],"lastModifiedDate":"2020-11-27T18:20:00.191634","indexId":"70216573","displayToPublicDate":"1994-11-25T12:35:13","publicationYear":"1994","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":7443,"text":"Quarterly Journal of the Royal Meteorological Society","active":true,"publicationSubtype":{"id":10}},"title":"Analysis of the surface hydrology in a regional climate model","docAbstract":"This paper discusses the surface hydrology of a multi‐year simulation of present day climate over the United States (US) conducted with a regional climate model (RegCM) nested within a general circulation model (GCM). The RegCM, which is run with a 60 km gridpoint spacing is interactively coupled with a state‐of‐the‐art surface physics package that includes full surface hydrology calculations (the Biosphere‐Atmosphere Transfer Scheme or BATS). The hydrologic budgets of ten regional drainage basins in the US are analysed. Model results are compared with available observations and with results from previous modelling experiments to evaluate the feasibility of using nested RegCM/GCM models for hydrology studies. In our experiment, the model captures the basic seasonality of the basin hydrologic budgets, although the simulated precipitation amounts are too high over the western US and too low over the eastern US. As a result, runoff, snow cover and soil water content are underestimated over the eastern US basins, while evaporation and runoff are overestimated in some of the western US basins. Topographically induced characteristics of precipitation, snow cover and runoff are well simulated over the mountainous western regions. Also well captured is the inter‐basin variation of hydrologic budgets which occurs in response to different climatic settings. The springtime snowmelt and peak runoff season generally occurs in the model earlier in the year than is observed. Although our work indicates that the coupled regional modelling system can be useful in applications to hydrological studies, results from this experiment indicate that better accuracy in the simulation of regional climatic variables and more detailed representation of some hydrologic processes would be required before the coupled modelling system could be used to provide accurate assessments of hydrologic responses to climate change.
","language":"English","publisher":"Wiley","doi":"10.1002/qj.49712051510","usgsCitation":"Giorgi, F., Hostetler, S.W., and Shields Brodeur, C., 1994, Analysis of the surface hydrology in a regional climate model: Quarterly Journal of the Royal Meteorological Society, v. 120, no. 515, p. 161-183, https://doi.org/10.1002/qj.49712051510.","productDescription":"23 p","startPage":"161","endPage":"183","costCenters":[{"id":200,"text":"Coop Res Unit Seattle","active":true,"usgs":true},{"id":481,"text":"Northern Rocky Mountain Science Center","active":true,"usgs":true}],"links":[{"id":380803,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"MultiPolygon\",\"coordinates\":[[[[-66.28243,18.51476],[-65.7713,18.42668],[-65.591,18.22803],[-65.84716,17.97591],[-66.59993,17.98182],[-67.18416,17.94655],[-67.24243,18.37446],[-67.10068,18.5206],[-66.28243,18.51476]]],[[[-155.54211,19.08348],[-155.68817,18.91619],[-155.93665,19.05939],[-155.90806,19.33888],[-156.07347,19.70294],[-156.02368,19.81422],[-155.85008,19.97729],[-155.91907,20.17395],[-155.86108,20.26721],[-155.78505,20.2487],[-155.40214,20.07975],[-155.22452,19.99302],[-155.06226,19.8591],[-154.80741,19.50871],[-154.83147,19.45328],[-155.22217,19.23972],[-155.54211,19.08348]]],[[[-156.07926,20.64397],[-156.41445,20.57241],[-156.58673,20.783],[-156.70167,20.8643],[-156.71055,20.92676],[-156.61258,21.01249],[-156.25711,20.91745],[-155.99566,20.76404],[-156.07926,20.64397]]],[[[-156.75824,21.17684],[-156.78933,21.06873],[-157.32521,21.09777],[-157.25027,21.21958],[-156.75824,21.17684]]],[[[-157.65283,21.32217],[-157.70703,21.26442],[-157.7786,21.27729],[-158.12667,21.31244],[-158.2538,21.53919],[-158.29265,21.57912],[-158.0252,21.71696],[-157.94161,21.65272],[-157.65283,21.32217]]],[[[-159.34512,21.982],[-159.46372,21.88299],[-159.80051,22.06533],[-159.74877,22.1382],[-159.5962,22.23618],[-159.36569,22.21494],[-159.34512,21.982]]],[[[-94.81758,49.38905],[-94.64,48.84],[-94.32914,48.67074],[-93.63087,48.60926],[-92.61,48.45],[-91.64,48.14],[-90.83,48.27],[-89.6,48.01],[-89.27292,48.01981],[-88.37811,48.30292],[-87.43979,47.94],[-86.46199,47.55334],[-85.65236,47.22022],[-84.87608,46.90008],[-84.77924,46.6371],[-84.54375,46.53868],[-84.6049,46.4396],[-84.3367,46.40877],[-84.14212,46.51223],[-84.09185,46.27542],[-83.89077,46.11693],[-83.61613,46.11693],[-83.46955,45.99469],[-83.59285,45.81689],[-82.55092,45.34752],[-82.33776,44.44],[-82.13764,43.57109],[-82.43,42.98],[-82.9,42.43],[-83.12,42.08],[-83.142,41.97568],[-83.02981,41.8328],[-82.69009,41.67511],[-82.43928,41.67511],[-81.27775,42.20903],[-80.24745,42.3662],[-78.93936,42.86361],[-78.92,42.965],[-79.01,43.27],[-79.17167,43.46634],[-78.72028,43.62509],[-77.73789,43.62906],[-76.82003,43.62878],[-76.5,44.01846],[-76.375,44.09631],[-75.31821,44.81645],[-74.867,45.00048],[-73.34783,45.00738],[-71.50506,45.0082],[-71.405,45.255],[-71.08482,45.30524],[-70.66,45.46],[-70.305,45.915],[-69.99997,46.69307],[-69.23722,47.44778],[-68.905,47.185],[-68.23444,47.35486],[-67.79046,47.06636],[-67.79134,45.70281],[-67.13741,45.13753],[-66.96466,44.8097],[-68.03252,44.3252],[-69.06,43.98],[-70.11617,43.68405],[-70.64548,43.09024],[-70.81489,42.8653],[-70.825,42.335],[-70.495,41.805],[-70.08,41.78],[-70.185,42.145],[-69.88497,41.92283],[-69.96503,41.63717],[-70.64,41.475],[-71.12039,41.49445],[-71.86,41.32],[-72.295,41.27],[-72.87643,41.22065],[-73.71,40.9311],[-72.24126,41.11948],[-71.945,40.93],[-73.345,40.63],[-73.982,40.628],[-73.95232,40.75075],[-74.25671,40.47351],[-73.96244,40.42763],[-74.17838,39.70926],[-74.90604,38.93954],[-74.98041,39.1964],[-75.20002,39.24845],[-75.52805,39.4985],[-75.32,38.96],[-75.07183,38.78203],[-75.05673,38.40412],[-75.37747,38.01551],[-75.94023,37.21689],[-76.03127,37.2566],[-75.72205,37.93705],[-76.23287,38.31921],[-76.35,39.15],[-76.54272,38.71762],[-76.32933,38.08326],[-76.99,38.23999],[-76.30162,37.91794],[-76.25874,36.9664],[-75.9718,36.89726],[-75.86804,36.55125],[-75.72749,35.55074],[-76.36318,34.80854],[-77.39763,34.51201],[-78.05496,33.92547],[-78.55435,33.86133],[-79.06067,33.49395],[-79.20357,33.15839],[-80.30132,32.50935],[-80.86498,32.0333],[-81.33629,31.44049],[-81.49042,30.72999],[-81.31371,30.03552],[-80.98,29.18],[-80.53558,28.47213],[-80.53,28.04],[-80.05654,26.88],[-80.08801,26.20576],[-80.13156,25.81677],[-80.38103,25.20616],[-80.68,25.08],[-81.17213,25.20126],[-81.33,25.64],[-81.71,25.87],[-82.24,26.73],[-82.70515,27.49504],[-82.85526,27.88624],[-82.65,28.55],[-82.93,29.1],[-83.70959,29.93656],[-84.1,30.09],[-85.10882,29.63615],[-85.28784,29.68612],[-85.7731,30.15261],[-86.4,30.4],[-87.53036,30.27433],[-88.41782,30.3849],[-89.18049,30.31598],[-89.59383,30.15999],[-89.41373,29.89419],[-89.43,29.48864],[-89.21767,29.29108],[-89.40823,29.15961],[-89.77928,29.30714],[-90.15463,29.11743],[-90.88022,29.14854],[-91.62678,29.677],[-92.49906,29.5523],[-93.22637,29.78375],[-93.84842,29.71363],[-94.69,29.48],[-95.60026,28.73863],[-96.59404,28.30748],[-97.14,27.83],[-97.37,27.38],[-97.38,26.69],[-97.33,26.21],[-97.14,25.87],[-97.53,25.84],[-98.24,26.06],[-99.02,26.37],[-99.3,26.84],[-99.52,27.54],[-100.11,28.11],[-100.45584,28.69612],[-100.9576,29.38071],[-101.6624,29.7793],[-102.48,29.76],[-103.11,28.97],[-103.94,29.27],[-104.45697,29.57196],[-104.70575,30.12173],[-105.03737,30.64402],[-105.63159,31.08383],[-106.1429,31.39995],[-106.50759,31.75452],[-108.24,31.75485],[-108.24194,31.34222],[-109.035,31.34194],[-111.02361,31.33472],[-113.30498,32.03914],[-114.815,32.52528],[-114.72139,32.72083],[-115.99135,32.61239],[-117.12776,32.53534],[-117.29594,33.04622],[-117.944,33.62124],[-118.4106,33.74091],[-118.51989,34.02778],[-119.081,34.078],[-119.43884,34.34848],[-120.36778,34.44711],[-120.62286,34.60855],[-120.74433,35.15686],[-121.71457,36.16153],[-122.54747,37.55176],[-122.51201,37.78339],[-122.95319,38.11371],[-123.7272,38.95166],[-123.86517,39.76699],[-124.39807,40.3132],[-124.17886,41.14202],[-124.2137,41.99964],[-124.53284,42.76599],[-124.14214,43.70838],[-124.02053,44.6159],[-123.89893,45.52341],[-124.07963,46.86475],[-124.39567,47.72017],[-124.68721,48.18443],[-124.5661,48.37971],[-123.12,48.04],[-122.58736,47.096],[-122.34,47.36],[-122.5,48.18],[-122.84,49],[-120,49],[-117.03121,49],[-116.04818,49],[-113,49],[-110.05,49],[-107.05,49],[-104.04826,48.99986],[-100.65,49],[-97.22872,49.0007],[-95.15907,49],[-95.15609,49.38425],[-94.81758,49.38905]]],[[[-153.00631,57.11584],[-154.00509,56.73468],[-154.5164,56.99275],[-154.67099,57.4612],[-153.76278,57.81657],[-153.22873,57.96897],[-152.56479,57.90143],[-152.14115,57.59106],[-153.00631,57.11584]]],[[[-165.57916,59.90999],[-166.19277,59.75444],[-166.84834,59.94141],[-167.45528,60.21307],[-166.46779,60.38417],[-165.67443,60.29361],[-165.57916,59.90999]]],[[[-171.73166,63.78252],[-171.11443,63.59219],[-170.49111,63.69498],[-169.68251,63.43112],[-168.68944,63.29751],[-168.77194,63.1886],[-169.52944,62.97693],[-170.29056,63.19444],[-170.67139,63.37582],[-171.55306,63.31779],[-171.79111,63.40585],[-171.73166,63.78252]]],[[[-155.06779,71.14778],[-154.34417,70.69641],[-153.90001,70.88999],[-152.21001,70.82999],[-152.27,70.60001],[-150.73999,70.43002],[-149.72,70.53001],[-147.61336,70.21403],[-145.68999,70.12001],[-144.92001,69.98999],[-143.58945,70.15251],[-142.07251,69.85194],[-140.98599,69.712],[-140.9925,66.00003],[-140.99777,60.3064],[-140.013,60.27684],[-139.039,60.00001],[-138.34089,59.56211],[-137.4525,58.905],[-136.47972,59.46389],[-135.47583,59.78778],[-134.945,59.27056],[-134.27111,58.86111],[-133.35555,58.41029],[-132.73042,57.69289],[-131.70781,56.55212],[-130.00778,55.91583],[-129.97999,55.285],[-130.53611,54.80275],[-131.08582,55.17891],[-131.96721,55.49778],[-132.25001,56.37],[-133.53918,57.17889],[-134.07806,58.12307],[-135.03821,58.18771],[-136.62806,58.21221],[-137.80001,58.5],[-139.86779,59.53776],[-140.82527,59.72752],[-142.57444,60.08445],[-143.95888,59.99918],[-145.92556,60.45861],[-147.11437,60.88466],[-148.22431,60.67299],[-148.01807,59.97833],[-148.57082,59.91417],[-149.72786,59.70566],[-150.60824,59.36821],[-151.71639,59.15582],[-151.85943,59.74498],[-151.40972,60.7258],[-150.34694,61.03359],[-150.62111,61.28442],[-151.89584,60.7272],[-152.57833,60.06166],[-154.01917,59.35028],[-153.28751,58.86473],[-154.23249,58.14637],[-155.30749,57.72779],[-156.30833,57.42277],[-156.5561,56.97998],[-158.11722,56.46361],[-158.43332,55.99415],[-159.60333,55.56669],[-160.28972,55.64358],[-161.22305,55.36473],[-162.23777,55.02419],[-163.06945,54.68974],[-164.78557,54.40417],[-164.94223,54.57222],[-163.84834,55.03943],[-162.87,55.34804],[-161.80417,55.89499],[-160.5636,56.00805],[-160.07056,56.41806],[-158.68444,57.01668],[-158.4611,57.21692],[-157.72277,57.57],[-157.55027,58.32833],[-157.04167,58.91888],[-158.19473,58.6158],[-158.51722,58.78778],[-159.05861,58.42419],[-159.71167,58.93139],[-159.98129,58.57255],[-160.35527,59.07112],[-161.355,58.67084],[-161.96889,58.67166],[-162.05499,59.26693],[-161.87417,59.63362],[-162.51806,59.98972],[-163.81834,59.79806],[-164.66222,60.26748],[-165.34639,60.5075],[-165.35083,61.0739],[-166.12138,61.50002],[-165.73445,62.075],[-164.91918,62.63308],[-164.56251,63.14638],[-163.75333,63.21945],[-163.06722,63.05946],[-162.26056,63.54194],[-161.53445,63.45582],[-160.77251,63.76611],[-160.95834,64.2228],[-161.51807,64.40279],[-160.77778,64.7886],[-161.39193,64.77724],[-162.45305,64.55944],[-162.75779,64.33861],[-163.54639,64.55916],[-164.96083,64.44695],[-166.42529,64.68667],[-166.845,65.0889],[-168.11056,65.67],[-166.70527,66.08832],[-164.47471,66.57666],[-163.65251,66.57666],[-163.7886,66.07721],[-161.67777,66.11612],[-162.48971,66.73557],[-163.71972,67.11639],[-164.43099,67.61634],[-165.39029,68.04277],[-166.76444,68.35888],[-166.20471,68.88303],[-164.43081,68.91554],[-163.16861,69.37111],[-162.93057,69.85806],[-161.9089,70.33333],[-160.9348,70.44769],[-159.03918,70.89164],[-158.11972,70.82472],[-156.58082,71.35776],[-155.06779,71.14778]]]]},\"properties\":{\"name\":\"United States\"}}]}","volume":"120","issue":"515","noUsgsAuthors":false,"publicationDate":"2006-12-15","publicationStatus":"PW","contributors":{"authors":[{"text":"Giorgi, F.","contributorId":24924,"corporation":false,"usgs":false,"family":"Giorgi","given":"F.","affiliations":[],"preferred":false,"id":805680,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hostetler, Steven W. 0000-0003-2272-8302 swhostet@usgs.gov","orcid":"https://orcid.org/0000-0003-2272-8302","contributorId":3249,"corporation":false,"usgs":true,"family":"Hostetler","given":"Steven","email":"swhostet@usgs.gov","middleInitial":"W.","affiliations":[{"id":200,"text":"Coop Res Unit Seattle","active":true,"usgs":true},{"id":438,"text":"National Research Program - Western Branch","active":true,"usgs":true}],"preferred":true,"id":805681,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Shields Brodeur, Christine","contributorId":245246,"corporation":false,"usgs":false,"family":"Shields Brodeur","given":"Christine","email":"","affiliations":[],"preferred":false,"id":805682,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":70169054,"text":"70169054 - 1994 - Suspended sediment and stream discharge in Bloody Run and Sny Magill watershed, water year 1992","interactions":[],"lastModifiedDate":"2025-07-29T20:50:36.059065","indexId":"70169054","displayToPublicDate":"1994-11-01T14:45:00","publicationYear":"1994","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":2,"text":"State or Local Government Series"},"seriesTitle":{"id":5107,"text":"Iowa Geological Survey Bureau Technical Information Series","active":true,"publicationSubtype":{"id":2}},"seriesNumber":"32","title":"Suspended sediment and stream discharge in Bloody Run and Sny Magill watershed, water year 1992","docAbstract":"Hydrologic data were collected in the Bloody Run and Sny Magill watersheds in Clayton County, Iowa during the 1992 Water Year (October 1, 1991 to September 30, 1992) to provide data on suspended sediment and stream discharge from these watersheds. Suspended-sediment samples were collected daily during normal flow and several times during rainstorms. Stream stage was recorded continuously and stream-discharge measurements were made monthly to develop a stage-discharge relation. Data on drainage-basin morphology and precipitation were quantified to help understand the variability in sediment and stream discharge. The total suspended-sediment discharge for Water Year 1992 was 2,720 tons at site BR1 on Bloody Run and 1,940 tons at site SN1 on Sny Magill Creek The daily median suspended-sediment discharge was 1.1 tons at both sites BR1 and SN1. The maximum daily mean stream discharge (205 cubic feet per second) at site BR1 on Bloody Run occurred on November 1, 1991. The median daily discharge at BR1 for the 1992 Water year was 24 cubic feet per second or 0.70 cubic feet per second per square mile (ft3/s/mi2). The maximum daily mean stream discharge at site SN1 on Sny Magill Creek was 90 cubic feet per second which occurred on April 20, 1992. The median daily discharge at site SN1 for the 1992 Water Year was 15 cubic feet per second or 0.54 ft3/s/mi2.
","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Sny Magill water shed monitoring project, baseline data","largerWorkSubtype":{"id":2,"text":"State or Local Government Series"},"language":"English","publisher":"Iowa Department of Natural Resources","publisherLocation":"Iowa City, IA","usgsCitation":"Kalkhoff, S.J., and Eash, D.A., 1994, Suspended sediment and stream discharge in Bloody Run and Sny Magill watershed, water year 1992: Iowa Geological Survey Bureau Technical Information Series 32, 17 p.","productDescription":"17 p.","startPage":"73","endPage":"89","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":351,"text":"Iowa Water Science Center","active":true,"usgs":true}],"links":[{"id":493154,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/unnumbered/70169054/IADNR_techinfo32.pdf","text":"Report","size":"1.62","linkFileType":{"id":1,"text":"pdf"}},{"id":318850,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Iowa","otherGeospatial":"Bloody Run Creek, Sny Magill Creek","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -91.17210388183594,\n 43.03426640603482\n ],\n [\n -91.17691040039062,\n 43.04982335155646\n ],\n [\n -91.17759704589844,\n 43.05785119934999\n ],\n [\n -91.18927001953124,\n 43.061363052307875\n ],\n [\n -91.20506286621092,\n 43.06437305188956\n ],\n [\n -91.21673583984375,\n 43.063369735115884\n ],\n [\n -91.22222900390625,\n 43.062868070571454\n ],\n [\n -91.23870849609375,\n 43.058854606434494\n ],\n [\n -91.27098083496094,\n 43.060359686273614\n ],\n [\n -91.29707336425781,\n 43.07340216393554\n ],\n [\n -91.31217956542969,\n 43.07641157238099\n ],\n [\n -91.33827209472655,\n 43.074906886631524\n ],\n [\n -91.34925842285156,\n 43.06236640192197\n ],\n [\n -91.36917114257811,\n 43.05634605793571\n ],\n [\n -91.40007019042967,\n 43.04982335155646\n ],\n [\n -91.42547607421875,\n 43.041794452901534\n ],\n [\n -91.4227294921875,\n 43.03276068583203\n ],\n [\n -91.41998291015625,\n 43.02171760887777\n ],\n [\n -91.40625,\n 43.004647127794435\n ],\n [\n -91.40625,\n 42.98907873036066\n ],\n [\n -91.38839721679688,\n 42.981041885223775\n ],\n [\n -91.36917114257811,\n 42.979032509768984\n ],\n [\n -91.34307861328125,\n 42.974511174899156\n ],\n [\n -91.32591247558594,\n 42.96596996868038\n ],\n [\n -91.33209228515625,\n 42.94385780966297\n ],\n [\n -91.33277893066406,\n 42.9257601336102\n ],\n [\n -91.31561279296875,\n 42.91821786558452\n ],\n [\n -91.30462646484375,\n 42.900615649573275\n ],\n [\n -91.28952026367188,\n 42.873951296240556\n ],\n [\n -91.29501342773438,\n 42.858853157602105\n ],\n [\n -91.29501342773438,\n 42.845261675587544\n ],\n [\n -91.26274108886719,\n 42.835191982798925\n ],\n [\n -91.22016906738281,\n 42.82663145362289\n ],\n [\n -91.17759704589844,\n 42.80900310137467\n ],\n [\n -91.16661071777342,\n 42.793385221161735\n ],\n [\n -91.13296508789062,\n 42.78985805744296\n ],\n [\n -91.12197875976562,\n 42.80396550624671\n ],\n [\n -91.12815856933594,\n 42.81051429991596\n ],\n [\n -91.15150451660156,\n 42.839220056847175\n ],\n [\n -91.15219116210938,\n 42.84979250192644\n ],\n [\n -91.15974426269531,\n 42.8694222423884\n ],\n [\n -91.16111755371094,\n 42.894579446909525\n ],\n [\n -91.16798400878906,\n 42.92073205751725\n ],\n [\n -91.17210388183594,\n 42.93631775765237\n ],\n [\n -91.1700439453125,\n 42.96195016710802\n ],\n [\n -91.18240356445311,\n 42.96647242540857\n ],\n [\n -91.20025634765625,\n 42.96948707959155\n ],\n [\n -91.21261596679686,\n 42.968984647487986\n ],\n [\n -91.22360229492188,\n 42.982548873720326\n ],\n [\n -91.22634887695312,\n 43.00012767681193\n ],\n [\n -91.22634887695312,\n 43.014689161895184\n ],\n [\n -91.175537109375,\n 43.034768304559556\n ],\n [\n -91.17210388183594,\n 43.03426640603482\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"56e7e0c7e4b0f59b85d6ab24","contributors":{"authors":[{"text":"Kalkhoff, Stephen J. 0000-0003-4110-1716 sjkalkho@usgs.gov","orcid":"https://orcid.org/0000-0003-4110-1716","contributorId":1731,"corporation":false,"usgs":true,"family":"Kalkhoff","given":"Stephen","email":"sjkalkho@usgs.gov","middleInitial":"J.","affiliations":[{"id":35680,"text":"Illinois-Iowa-Missouri Water Science Center","active":true,"usgs":true},{"id":36532,"text":"Central Midwest Water Science Center","active":true,"usgs":true},{"id":351,"text":"Iowa Water Science Center","active":true,"usgs":true}],"preferred":true,"id":622694,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Eash, David A. 0000-0002-2749-8959 daeash@usgs.gov","orcid":"https://orcid.org/0000-0002-2749-8959","contributorId":1887,"corporation":false,"usgs":true,"family":"Eash","given":"David","email":"daeash@usgs.gov","middleInitial":"A.","affiliations":[{"id":351,"text":"Iowa Water Science Center","active":true,"usgs":true}],"preferred":true,"id":622695,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ]}