No abstract available.
","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr97151","issn":"0094-9140","usgsCitation":"Church, S.E., Kimball, B.A., Fey, D., Ferderer, D., Yager, T., and Vaughn, R.B., 1997, Source, transport, and partitioning of metals between water, colloids, and bed sediments of the Animas River, Colorado: U.S. Geological Survey Open-File Report 97-151, iii, 135 p., https://doi.org/10.3133/ofr97151.","productDescription":"iii, 135 p.","costCenters":[{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":155518,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1997/0151/report-thumb.jpg"},{"id":8098,"rank":100,"type":{"id":15,"text":"Index 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\"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4880e4b07f02db515e44","contributors":{"authors":[{"text":"Church, S. E.","contributorId":58260,"corporation":false,"usgs":true,"family":"Church","given":"S.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":187458,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Kimball, B. A.","contributorId":87583,"corporation":false,"usgs":false,"family":"Kimball","given":"B.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":187460,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Fey, D.L.","contributorId":44537,"corporation":false,"usgs":true,"family":"Fey","given":"D.L.","email":"","affiliations":[],"preferred":false,"id":187457,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Ferderer, D.A.","contributorId":65326,"corporation":false,"usgs":true,"family":"Ferderer","given":"D.A.","affiliations":[],"preferred":false,"id":187459,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Yager, T. J.","contributorId":33359,"corporation":false,"usgs":true,"family":"Yager","given":"T. J.","affiliations":[],"preferred":false,"id":187456,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Vaughn, R. B.","contributorId":27043,"corporation":false,"usgs":true,"family":"Vaughn","given":"R.","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":187455,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}} ,{"id":22038,"text":"ofr97219 - 1997 - Preliminary hydrogeologic assessment of a ground-water contamination area in Wolcott, Connecticut","interactions":[],"lastModifiedDate":"2012-02-02T00:07:50","indexId":"ofr97219","displayToPublicDate":"1997-09-01T00:00:00","publicationYear":"1997","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":"97-219","title":"Preliminary hydrogeologic assessment of a ground-water contamination area in Wolcott, Connecticut","docAbstract":"Contamination of ground water by volatile organic compounds and inorganic constituents has been identified at a number of industrial sites in the Town of Wolcott, Connecticut. Contamination is also present at a municipal landfill in the City of Waterbury that is upgradient from the industrial sites in the local ground-water-flow system. The study area, which lies in the Western Highlands of Connecticut, is in the Mad River Valley, a tributary to the Naugatuck River. Geohydrologic units (aquifer materials) include unconsolidated glacial sediments (surficial materials) and fractured crystalline (metamorphic) bedrock. Surficial materials include glacial till, coarse-grained andfine-grained glacial stratified deposits, and postglacial floodplain alluvium and swamp deposits. The ground-water-flow system in the surficial aquifer is complex because the hydraulic properties of the surficial materials are highly variable. In the bedrock aquifer, ground water moves exclusively through fractures. Hydrologic characteristics of the crystalline bedrock-degree of confinement, hydraulic conductivity, storativity, and porosity-are poorly defined in the study area. Further study is needed to adequately assess ground-water flow and contaminant migration under current or past hydrologic conditions. All known water-supply wells in the study area obtain water from the bedrock aquifer. Twenty households in a hillside residential area on Tosun Road currently obtain drinking water from private wells tapping the bedrock aquifer. The extent of contamination in the bedrock aquifer and the potential for future contamination from known sources of contamination in the surficial aquifer is of concern to regulatory agencies. Previous investigations have identified ground-water contamination by volatile organic compounds at the Nutmeg Valley Road site area. Contamination has been associated with on-site disposal of heavy metals, chlorinated and non-chlorinated volatile organic compounds, and cyanide. Concentrations of volatile organic compounds detected in water samples collected from bedrock wells during 1981-95 at the Nutmeg Valley Road site area show a general downward trend through time. Water samples collected from wells completed in surficial materials were not collected systematically, and a trend in concentration cannot be identified.","language":"ENGLISH","publisher":"U.S. Geological Survey ;\r\nInformation Services [distributor],","doi":"10.3133/ofr97219","issn":"0094-9140","usgsCitation":"Stone, J.R., Casey, G.D., Mondazzi, R., and Frick, T., 1997, Preliminary hydrogeologic assessment of a ground-water contamination area in Wolcott, Connecticut: U.S. Geological Survey Open-File Report 97-219, iv, 29 p. :ill. (some col.), maps (some col.) ;28 cm., https://doi.org/10.3133/ofr97219.","productDescription":"iv, 29 p. :ill. (some col.), maps (some col.) ;28 cm.","costCenters":[],"links":[{"id":258612,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1997/0219/report.pdf","size":"6509","linkFileType":{"id":1,"text":"pdf"}},{"id":258613,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1997/0219/report-thumb.jpg"},{"id":258604,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1997/0219/plate-1.pdf","size":"1117","linkFileType":{"id":1,"text":"pdf"}},{"id":258605,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1997/0219/plate-2.pdf","size":"5627","linkFileType":{"id":1,"text":"pdf"}},{"id":258606,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1997/0219/plate-3.pdf","size":"1002","linkFileType":{"id":1,"text":"pdf"}},{"id":258607,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1997/0219/plate-4.pdf","size":"1195","linkFileType":{"id":1,"text":"pdf"}},{"id":258608,"rank":404,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1997/0219/plate-5.pdf","size":"1388","linkFileType":{"id":1,"text":"pdf"}},{"id":258609,"rank":405,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1997/0219/plate-6.pdf","size":"909","linkFileType":{"id":1,"text":"pdf"}},{"id":258610,"rank":406,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1997/0219/plate-7.pdf","size":"1047","linkFileType":{"id":1,"text":"pdf"}},{"id":258611,"rank":407,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1997/0219/plate-8.pdf","size":"5021","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afee4b07f02db697396","contributors":{"authors":[{"text":"Stone, J. R.","contributorId":87964,"corporation":false,"usgs":true,"family":"Stone","given":"J.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":186795,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Casey, G. D.","contributorId":49819,"corporation":false,"usgs":true,"family":"Casey","given":"G.","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":186793,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Mondazzi, R.A.","contributorId":75563,"corporation":false,"usgs":true,"family":"Mondazzi","given":"R.A.","affiliations":[],"preferred":false,"id":186794,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Frick, T.W.","contributorId":90329,"corporation":false,"usgs":true,"family":"Frick","given":"T.W.","email":"","affiliations":[],"preferred":false,"id":186796,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":30321,"text":"wri964304 - 1997 - Changes in flow in the Beaver-North Canadian River basin upstream from Canton Lake, western Oklahoma","interactions":[],"lastModifiedDate":"2025-07-10T17:03:21.210183","indexId":"wri964304","displayToPublicDate":"1997-09-01T00:00:00","publicationYear":"1997","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":"96-4304","title":"Changes in flow in the Beaver-North Canadian River basin upstream from Canton Lake, western Oklahoma","docAbstract":"This report presents the results of an evaluation of hydrologic data for the Beaver-North Canadian River basin upstream from Canton Lake in western Oklahoma. It examines the climatic and hydrologic data for evidence of trends. The hydrologic data examined includes total annual flow, base flow, and annual peak discharges.\r\nThis study was conducted to determine if there is evidence of trends present in hydrologic and climatic data. All available streamflow-gaging station data, with at least 10 or more years of record, were examined for trends. In addition, the data were divided into an 'early' period (ending in 1971), representing conditions before ground-water levels had declined appreciably, and a 'recent' period (1978-1994), reflecting the condition of declining ground-water levels, including the effects of storage reservoirs.\r\n\r\nTests for trend, moving averages, and comparisons of median and average flows for an early period (ending in 1971) with those for the recent period (1978-1994) show that the total annual volume of flow and the magnitudes of instantaneous annual peak discharges measured at most gaging stations in the Beaver- North Canadian River basin have decreased in recent years. Precipitation records for the panhandle, however, show no corresponding changes.\r\n\r\nThe changes in flow are most pronounced in the headwaters upstream from Woodward, but also are evident at Woodward and near Seiling, which represents the inflow to Canton Lake. The average annual discharge decreased between the early period and the recent period by the following amounts: near Guymon, 18,000 acre-feet; at Beaver, 68,000 acre-feet; at Woodward, 72,000 acre-feet; and near Seiling, 63,000 acre-feet. These decreases, expressed as a percentage of the average flows for the early period, were 91 percent near Guymon, 82 percent at Beaver, 49 percent at Woodward, and 37 percent near Seiling. The medians of the annual peak discharges decreased from the early period to the recent period by the following amounts: near Guymon, 98 percent; at Beaver, 86 percent; at Woodward, 80 percent; and near Seiling, 53 percent. The Guymon gage is not affected by reservoirs; the other three mainstem gaging stations are influenced by reservoirs, but the decreases in annual peak discharges are greater than can be explained by storage in those reservoirs.\r\n\r\nBase flows have undergone substantial change, but unlike the annual volumes the base flows show some increases and some decreases. Flow duration analyses show a shift in the distribution of annual flows. Less contribution is coming from large floods that formerly added substantially to the yearly average flows. Near Seiling, for example, the magnitudes of the large flows that occur less than about 20 percent of the time were greatly reduced in the recent period.\r\n\r\nA primary mechanism producing these decreased streamflows appears to be the depletion of ground water in the High Plains aquifer that underlies more than 90 percent of the basin. Changes in farming and conservation practices and in water use also may be having an effect.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri964304","usgsCitation":"Wahl, K.L., and Tortorelli, R.L., 1997, Changes in flow in the Beaver-North Canadian River basin upstream from Canton Lake, western Oklahoma: U.S. Geological Survey Water-Resources Investigations Report 96-4304, vi, 58 p., https://doi.org/10.3133/wri964304.","productDescription":"vi, 58 p.","costCenters":[],"links":[{"id":2458,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/wri964304/pdf/wri96-4304.pdf","linkFileType":{"id":5,"text":"html"}},{"id":124820,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/wri_96_4304.jpg"}],"country":"United States","state":"Oklahoma","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -98.28223256564006,\n 36.366114435776524\n ],\n [\n -98.65668214895032,\n 36.55732225973237\n ],\n [\n -99.99994573352308,\n 36.98104291572069\n ],\n [\n -100.62402837237414,\n 36.91456402858782\n ],\n [\n -102.70430383520873,\n 36.890799658844145\n ],\n [\n -102.5735436632592,\n 36.54299803318963\n ],\n [\n -99.75625632216278,\n 36.50478711905258\n ],\n [\n -98.78149867672028,\n 35.659387111580685\n ],\n [\n -98.28223256564006,\n 36.366114435776524\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e2e4b07f02db5e4f0e","contributors":{"authors":[{"text":"Wahl, Kenneth L.","contributorId":61024,"corporation":false,"usgs":true,"family":"Wahl","given":"Kenneth","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":203052,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Tortorelli, Robert L.","contributorId":65071,"corporation":false,"usgs":true,"family":"Tortorelli","given":"Robert","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":203053,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":22260,"text":"ofr9722 - 1997 - Water-quality and hydrogeologic data used to evaluate the effects of farming systems on ground-water quality at the Management Systems Evaluation Area near Princeton, Minnesota, 1991-95","interactions":[],"lastModifiedDate":"2019-12-05T09:55:56","indexId":"ofr9722","displayToPublicDate":"1997-09-01T00:00:00","publicationYear":"1997","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":"97-22","title":"Water-quality and hydrogeologic data used to evaluate the effects of farming systems on ground-water quality at the Management Systems Evaluation Area near Princeton, Minnesota, 1991-95","docAbstract":"The Minnesota Management Systems Evaluation Area (MSEA) project was part of a multi-scale, inter-agency initiative to evaluate the effects of agricultural management systems on water quality in the midwest corn belt. The research area was located in the Anoka Sand Plain about 5 kilometers southwest of Princeton, Minnesota. The ground-water-quality monitoring network within and immediately surrounding the research area consisted of 73 observation wells and 25 multiport wells. The primary objectives of the ground-water monitoring program at the Minnesota MSEA were to: (1) determine the effects of three farming systems on ground-water quality, and (2) understand the processes and factors affecting the loading, transport, and fate of agricultural chemicals in ground water at the site. This report presents well construction, geologic, water-level, chemical application, water-quality, and quality-assurance data used to evaluate the effects of farming systems on ground-water quality during 1991-95.
","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Mounds View, MN","doi":"10.3133/ofr9722","issn":"0094-9140","collaboration":"Prepared in cooperation with the University of Minnesota Department of Soil, Water, and Climate, the U.S. Department of Agriculture, Agricultural Research Service, and the Minnesota Pollution Control Agency","usgsCitation":"Landon, M., Delin, G., Nelson, K., Regan, C., Lamb, J., Larson, S., Capel, P., Anderson, J.L., and Dowdy, R., 1997, Water-quality and hydrogeologic data used to evaluate the effects of farming systems on ground-water quality at the Management Systems Evaluation Area near Princeton, Minnesota, 1991-95: U.S. Geological Survey Open-File Report 97-22, vi, 25 p., https://doi.org/10.3133/ofr9722.","productDescription":"vi, 25 p.","onlineOnly":"N","additionalOnlineFiles":"N","temporalStart":"1991-01-01","temporalEnd":"1995-12-31","costCenters":[{"id":392,"text":"Minnesota Water Science Center","active":true,"usgs":true},{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":12221,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://mn.water.usgs.gov/publications/pubs/97-22.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":154430,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1997/0022/report-thumb.jpg"},{"id":51687,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1997/0022/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Minnesota","city":"Princeton","otherGeospatial":"Management Systems Evaluation Area","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -93.62385749816895, 45.52312701460922 ], [ -93.62385749816895, 45.530222474607434 ], [ -93.6140513420105, 45.530222474607434 ], [ -93.6140513420105, 45.52312701460922 ], [ -93.62385749816895, 45.52312701460922 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f1e4b07f02db5ee5e4","contributors":{"authors":[{"text":"Landon, M.K. 0000-0002-5766-0494","orcid":"https://orcid.org/0000-0002-5766-0494","contributorId":69572,"corporation":false,"usgs":true,"family":"Landon","given":"M.K.","affiliations":[],"preferred":false,"id":187831,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Delin, G. N.","contributorId":12834,"corporation":false,"usgs":true,"family":"Delin","given":"G. N.","affiliations":[],"preferred":false,"id":187827,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Nelson, K.J.","contributorId":36957,"corporation":false,"usgs":true,"family":"Nelson","given":"K.J.","email":"","affiliations":[],"preferred":false,"id":187829,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Regan, C.P.","contributorId":37364,"corporation":false,"usgs":true,"family":"Regan","given":"C.P.","email":"","affiliations":[],"preferred":false,"id":187830,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Lamb, J.A.","contributorId":95898,"corporation":false,"usgs":true,"family":"Lamb","given":"J.A.","email":"","affiliations":[],"preferred":false,"id":187834,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Larson, S.J.","contributorId":17641,"corporation":false,"usgs":true,"family":"Larson","given":"S.J.","email":"","affiliations":[],"preferred":false,"id":187828,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Capel, P. D. 0000-0003-1620-5185","orcid":"https://orcid.org/0000-0003-1620-5185","contributorId":95498,"corporation":false,"usgs":true,"family":"Capel","given":"P. D.","affiliations":[],"preferred":false,"id":187833,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Anderson, J. L.","contributorId":103240,"corporation":false,"usgs":true,"family":"Anderson","given":"J.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":187835,"contributorType":{"id":1,"text":"Authors"},"rank":8},{"text":"Dowdy, R.H.","contributorId":92275,"corporation":false,"usgs":true,"family":"Dowdy","given":"R.H.","email":"","affiliations":[],"preferred":false,"id":187832,"contributorType":{"id":1,"text":"Authors"},"rank":9}]}} ,{"id":35490,"text":"b2094A - 1997 - Regional diagenetic patterns in the St. Peter Sandstone; implications for brine migration in the Illinois Basin","interactions":[],"lastModifiedDate":"2012-02-02T00:09:47","indexId":"b2094A","displayToPublicDate":"1997-09-01T00:00:00","publicationYear":"1997","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":306,"text":"Bulletin","code":"B","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"2094","chapter":"A","title":"Regional diagenetic patterns in the St. Peter Sandstone; implications for brine migration in the Illinois Basin","docAbstract":"Diagenetic minerals and alteration patterns in the\r\nOrdovician St. Peter Sandstone, Illinois Basin, record varied\r\nhydrologic and chemical conditions during the basin?s long\r\nand complex geologic history. Major diagenetic events modifying\r\nthe St. Peter Sandstone include (1) mechanical compaction,\r\n(2) early K-feldspar overgrowth and dolospar\r\nprecipitation, (3) burial quartz, dolospar, anhydrite, and calcite\r\ncementation, and (4) carbonate-cement and K-feldspar\r\ngrain dissolution. Radiometric age dates of authigenic\r\nK-feldspar and illite in combination with the reconstructed\r\nburial history of the St. Peter reveal that early-diagenetic\r\nK-feldspar and dolospar precipitated at shallow to moderate\r\ndepths in the Devonian, whereas late-diagenetic quartz,\r\ndolospar, anhydrite, and calcite formed during deep burial in\r\nthe Late Pennsylvanian to Early Permian. Stable-isotope\r\ngeochemistry and fluid-inclusion paleothermometry suggest\r\nthat burial cements precipitated from saline fluids over a\r\nwide temperature range. In the southern part of the basin,\r\nburial cements preserve a record of diagenetic effects that\r\nwere in part controlled by fractures and hydrothermal-fluid\r\ncirculation. Baroque dolospar cementation is the most significant\r\nof these effects.","language":"ENGLISH","publisher":"U.S. G.P.O.,","doi":"10.3133/b2094A","usgsCitation":"Pitman, J.K., Goldhaber, M.B., and Spoetl, C., 1997, Regional diagenetic patterns in the St. Peter Sandstone; implications for brine migration in the Illinois Basin: U.S. Geological Survey Bulletin 2094, iii, p. A1-A17, ill., maps ;28 cm., https://doi.org/10.3133/b2094A.","productDescription":"iii, p. A1-A17, ill., maps ;28 cm.","costCenters":[],"links":[{"id":165406,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":3413,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/bul/b2094a/b2094a.html","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac9e4b07f02db67c5f5","contributors":{"authors":[{"text":"Pitman, Janet K. 0000-0002-0441-779X jpitman@usgs.gov","orcid":"https://orcid.org/0000-0002-0441-779X","contributorId":767,"corporation":false,"usgs":true,"family":"Pitman","given":"Janet","email":"jpitman@usgs.gov","middleInitial":"K.","affiliations":[{"id":241,"text":"Eastern Energy Resources Science Center","active":true,"usgs":true},{"id":164,"text":"Central Energy Resources Science Center","active":true,"usgs":true}],"preferred":true,"id":214734,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Goldhaber, Martin B. 0000-0002-1785-4243 mgold@usgs.gov","orcid":"https://orcid.org/0000-0002-1785-4243","contributorId":1339,"corporation":false,"usgs":true,"family":"Goldhaber","given":"Martin","email":"mgold@usgs.gov","middleInitial":"B.","affiliations":[{"id":171,"text":"Central Mineral and Environmental Resources Science Center","active":true,"usgs":true},{"id":211,"text":"Crustal Geophysics and Geochemistry Science Center","active":true,"usgs":true}],"preferred":true,"id":214735,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Spoetl, Christoph","contributorId":18043,"corporation":false,"usgs":true,"family":"Spoetl","given":"Christoph","email":"","affiliations":[],"preferred":false,"id":214736,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":70185299,"text":"70185299 - 1997 - A study of the temporal variability of atrazine in private well water. part ii: analysis of data","interactions":[],"lastModifiedDate":"2017-03-20T11:27:17","indexId":"70185299","displayToPublicDate":"1997-09-01T00:00:00","publicationYear":"1997","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1552,"text":"Environmental Monitoring and Assessment","onlineIssn":"1573-2959","printIssn":"0167-6369","active":true,"publicationSubtype":{"id":10}},"title":"A study of the temporal variability of atrazine in private well water. part ii: analysis of data","docAbstract":"In 1988, the Iowa Department of Natural Resources, along withthe University of Iowa, conducted the Statewide Rural WellWater Survey, commonly known as SWRL. A total of 686private rural drinking water wells was selected by use of aprobability sample and tested for pesticides and nitrate. A subsetof these wells, the 10% repeat wells, were additionally sampledin October, 1990 and June, 1991. Starting in November, 1991,the University of Iowa, with sponsorship from the United StatesEnvironmental Protection Agency, revisited the 10% repeat wellsto begin a study of the temporal variability of atrazine and nitratein wells. Other wells, which had originally tested positive foratrazine in SWRL but were not in the 10% population, wereadded to the study population. Temporal sampling for a year-long period began in February of 1992 and concluded in Januaryof 1993. All wells were sampled monthly, a subset was sampledweekly, and a second subset was sampled for 14 day consecutiveperiods. Of the 67 wells in the 10% population tested monthly,7 (10.4%) tested positive for atrazine at least once during theyear, and 3 (4%) were positive each of the 12 months. Theaverage concentration in the 7 wells was 0.10 µg/L. Fornitrate, 15 (22%) wells in the 10% repeat population monthlysampling were above the Maximum Contaminant Level of 10 mg/L at least once. This paper, the second of two papers on thisstudy, describes the analysis of data from the survey. The firstpaper (Lorber et al., 1997) reviews the study design, theanalytical methodologies, and development of the data base.
","language":"English","publisher":"Kluwer Academic Publishers","doi":"10.1023/A:1005704920640","usgsCitation":"Pinsky, P., Lorber, M., Johnson, K., Kross, B., Burmeister, L., Wilkins, A., and Hallberg, G., 1997, A study of the temporal variability of atrazine in private well water. part ii: analysis of data: Environmental Monitoring and Assessment, v. 47, no. 2, p. 197-221, https://doi.org/10.1023/A:1005704920640.","productDescription":"25 p. ","startPage":"197","endPage":"221","costCenters":[{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":337840,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"47","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"58d0ea1be4b0236b68f67379","contributors":{"authors":[{"text":"Pinsky, Paul","contributorId":189527,"corporation":false,"usgs":false,"family":"Pinsky","given":"Paul","email":"","affiliations":[],"preferred":false,"id":685072,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Lorber, Matthew","contributorId":189528,"corporation":false,"usgs":false,"family":"Lorber","given":"Matthew","email":"","affiliations":[],"preferred":false,"id":685073,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Johnson, Kent","contributorId":189529,"corporation":false,"usgs":false,"family":"Johnson","given":"Kent","email":"","affiliations":[],"preferred":false,"id":685074,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Kross, Burton","contributorId":189530,"corporation":false,"usgs":false,"family":"Kross","given":"Burton","email":"","affiliations":[],"preferred":false,"id":685075,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Burmeister, Leon","contributorId":189531,"corporation":false,"usgs":false,"family":"Burmeister","given":"Leon","email":"","affiliations":[],"preferred":false,"id":685076,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Wilkins, Amina","contributorId":189532,"corporation":false,"usgs":false,"family":"Wilkins","given":"Amina","email":"","affiliations":[],"preferred":false,"id":685077,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Hallberg, George","contributorId":16269,"corporation":false,"usgs":true,"family":"Hallberg","given":"George","affiliations":[],"preferred":false,"id":685078,"contributorType":{"id":1,"text":"Authors"},"rank":7}]}} ,{"id":24701,"text":"ofr97114 - 1997 - Status of ground-water resources at U.S. Navy Support Facility, Diego Garcia; summary of hydrologic and climatic data, January 1994 through December 1996","interactions":[],"lastModifiedDate":"2012-02-02T00:08:28","indexId":"ofr97114","displayToPublicDate":"1997-08-01T00:00:00","publicationYear":"1997","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":"97-114","title":"Status of ground-water resources at U.S. Navy Support Facility, Diego Garcia; summary of hydrologic and climatic data, January 1994 through December 1996","language":"ENGLISH","publisher":"U.S. Geological Survey ;\r\nBranch of Information Services [distributor],","doi":"10.3133/ofr97114","issn":"0094-9140","usgsCitation":"Torikai, J., 1997, Status of ground-water resources at U.S. Navy Support Facility, Diego Garcia; summary of hydrologic and climatic data, January 1994 through December 1996: U.S. Geological Survey Open-File Report 97-114, v, 43 p. :ill. ;28 cm., https://doi.org/10.3133/ofr97114.","productDescription":"v, 43 p. :ill. ;28 cm.","costCenters":[],"links":[{"id":157923,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1997/0114/report-thumb.jpg"},{"id":53734,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1997/0114/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49d7e4b07f02db5ded2c","contributors":{"authors":[{"text":"Torikai, J.D.","contributorId":93926,"corporation":false,"usgs":true,"family":"Torikai","given":"J.D.","affiliations":[],"preferred":false,"id":192404,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":44872,"text":"wri964184 - 1997 - Potentiometric surface and hydrologic conditions of the upper aquifer in the Manatí-Vega Baja area, north central Puerto Rico, March 1995","interactions":[],"lastModifiedDate":"2022-01-10T21:11:10.125226","indexId":"wri964184","displayToPublicDate":"1997-08-01T00:00:00","publicationYear":"1997","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":"96-4184","title":"Potentiometric surface and hydrologic conditions of the upper aquifer in the Manatí-Vega Baja area, north central Puerto Rico, March 1995","docAbstract":"No abstract available.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri964184","usgsCitation":"Conde-Costas, C., and Rodriguez-Rodriguez, G., 1997, Potentiometric surface and hydrologic conditions of the upper aquifer in the Manatí-Vega Baja area, north central Puerto Rico, March 1995: U.S. Geological Survey Water-Resources Investigations Report 96-4184, 1 Plate: 28.00 × 30.00 inches, https://doi.org/10.3133/wri964184.","productDescription":"1 Plate: 28.00 × 30.00 inches","costCenters":[],"links":[{"id":394141,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_48527.htm"},{"id":134694,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":82230,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1996/4184/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Puerto Rico","otherGeospatial":"Manatí-Vega Baja area","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -66.5,\n 18.4167\n ],\n [\n -66.375,\n 18.4167\n ],\n [\n -66.375,\n 18.475\n ],\n [\n -66.5,\n 18.475\n ],\n [\n -66.5,\n 18.4167\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e6e4b07f02db5e744e","contributors":{"authors":[{"text":"Conde-Costas, Carlos","contributorId":10768,"corporation":false,"usgs":true,"family":"Conde-Costas","given":"Carlos","email":"","affiliations":[],"preferred":false,"id":230587,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Rodriguez-Rodriguez, Gilberto","contributorId":101242,"corporation":false,"usgs":true,"family":"Rodriguez-Rodriguez","given":"Gilberto","email":"","affiliations":[],"preferred":false,"id":230588,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":5209,"text":"fs04197 - 1997 - Water quality of selected streams in Montgomery County, Indiana, 1996","interactions":[],"lastModifiedDate":"2019-04-22T09:51:34","indexId":"fs04197","displayToPublicDate":"1997-08-01T00:00:00","publicationYear":"1997","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":313,"text":"Fact Sheet","code":"FS","onlineIssn":"2327-6932","printIssn":"2327-6916","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"041-97","displayTitle":"Water Quality of Selected Streams in Montgomery County, Indiana, 1996","title":"Water quality of selected streams in Montgomery County, Indiana, 1996","docAbstract":"The USGS sampled streams in Montgomery County as part of a study done in cooperation with the Montgomery County Commissioners. The sampling program was designed by the Montgomery County Sanitarian and USGS hydrologists. The program focused on assessing general surface-water quality throughout the county and also targeted some specific areas of interest to county officials.
","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/fs04197","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1997, Water quality of selected streams in Montgomery County, Indiana, 1996: U.S. Geological Survey Fact Sheet 041-97, 1 sheet 2 p. : col. ill., col. map ; 28 cm. col. ill., col. map ;, https://doi.org/10.3133/fs04197.","productDescription":"1 sheet 2 p. : col. ill., col. map ; 28 cm. col. ill., col. map ;","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":346,"text":"Indiana Water Science Center","active":true,"usgs":true}],"links":[{"id":118336,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/fs_041_97.jpg"},{"id":358747,"rank":2,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/fs/1997/0041/","linkFileType":{"id":5,"text":"html"},"description":"FS 1997-041"}],"country":"United States","state":"Indiana","county":"Montgomery","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"Polygon\",\"coordinates\":[[[-86.6957,40.2144],[-86.6962,40.1785],[-86.6961,40.1282],[-86.6946,40.0402],[-86.6938,39.9528],[-86.6937,39.9228],[-86.6929,39.8643],[-86.7918,39.8651],[-86.8056,39.865],[-86.8967,39.8666],[-86.9182,39.8674],[-87.0087,39.8685],[-87.0333,39.8683],[-87.0914,39.8685],[-87.0909,39.9538],[-87.0919,40.2172],[-87.0353,40.2165],[-86.9221,40.2161],[-86.8095,40.2146],[-86.6957,40.2144]]]},\"properties\":{\"name\":\"Montgomery\",\"state\":\"IN\"}}]}","contact":"Director, Ohio-Kentucky-Indiana Water Science Center
U.S. Geological Survey
64640 Busch Blvd, Suite 100
Columbus, OH 43229
No abstract available.
","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/fs00597","usgsCitation":"Brown, J.G., Brew, R., and Harvey, J.W., 1997, Research on acidic metal contaminants in Pinal Creek Basin near Globe, Arizona: U.S. Geological Survey Fact Sheet 005-97, 4 p., https://doi.org/10.3133/fs00597.","productDescription":"4 p.","costCenters":[{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":117231,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/fs_005_97.bmp"},{"id":634,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/FS/FS-005-97","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Arizona","otherGeospatial":"Pinal Creek Basin","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -111.99462890625,\n 32.37996146435729\n ],\n [\n -110.36865234374999,\n 32.37996146435729\n ],\n [\n -110.36865234374999,\n 33.578014746143985\n ],\n [\n -111.99462890625,\n 33.578014746143985\n ],\n [\n -111.99462890625,\n 32.37996146435729\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a55e4b07f02db62c63e","contributors":{"authors":[{"text":"Brown, James G.","contributorId":81094,"corporation":false,"usgs":true,"family":"Brown","given":"James","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":150589,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Brew, Robert","contributorId":65842,"corporation":false,"usgs":true,"family":"Brew","given":"Robert","affiliations":[],"preferred":false,"id":150588,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Harvey, Judson W. 0000-0002-2654-9873 jwharvey@usgs.gov","orcid":"https://orcid.org/0000-0002-2654-9873","contributorId":1796,"corporation":false,"usgs":true,"family":"Harvey","given":"Judson","email":"jwharvey@usgs.gov","middleInitial":"W.","affiliations":[{"id":436,"text":"National Research Program - Eastern Branch","active":true,"usgs":true}],"preferred":true,"id":150587,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":5096,"text":"fs24596 - 1997 - Use of tracer injections and synoptic sampling to measure metal loading from acid mine drainage","interactions":[],"lastModifiedDate":"2019-10-09T15:05:29","indexId":"fs24596","displayToPublicDate":"1997-08-01T00:00:00","publicationYear":"1997","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":313,"text":"Fact Sheet","code":"FS","onlineIssn":"2327-6932","printIssn":"2327-6916","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"245-96","title":"Use of tracer injections and synoptic sampling to measure metal loading from acid mine drainage","docAbstract":"Thousands of abandoned and inactive mines are located in environmentally sensitive mountain watersheds. Cost-effective remediation of the effects of metals from mining in these watersheds requires knowledge of the most significant sources of metals. The significance of a given source depends on the toxicity of a particular metal, how much of the metal enters the stream, and whether or not the metal remains in the stream in a toxic form. This discussion deals with accounting for how much metal enters the stream and whether it stays in the stream. The amount of metal entering the stream is called the mass loading and is calculated as the product of metal concentration and stream discharge. The overall effect of high metal concentrations on streams and aquatic organisms is unclear without discharge measurements.
A traditional discharge measurement is obtained by dividing a stream into small sections and measuring the cross-sectional area and the average water velocity in each section. Summing the measurements of all the sections gives the discharge of the entire stream. This method works well where the channel bottom and banks are smooth. In mountain streams, however, the stream bottom typically is covered with cobbles, allowing much of the water to flow through the cobbles of the streambed where it cannot be measured by a flow meter (fig. 1). Thus, accurate discharge measurements are difficult to obtain in mountain streams, even under the best of conditions.
A method for analyzing and interpreting travel times of solutes in heterogeneous aquifers is presented based on the peak concentration arrival times as measured at various samplers in the aquifer. The method allows separation of the effects of pore-scale dispersion from the effects of the large-scale aquifer heterogeneity. An analysis of data from the Cape Cod field experiment is presented, and we found that the values of the hydrogeological parameters inferred from the travel times match very well the values obtained from direct interpretation of cores. Analysis of the spatial correlations of the travel times also allows inference of spatial covariances of the log conductivity and the anisotropy ratio of the correlation lengths. Separate analyses of the travel times carried over planes at different travel distances show that the variance of the log conductivity increases with travel distance.
","language":"English","publisher":"American Geophysical Union","doi":"10.1029/96WR00016","usgsCitation":"Rubin, Y., and Ezzedine, S., 1997, The travel times of solutes at the Cape Cod Tracer Experiment: Data analysis, modeling, and structural parameters inference: Water Resources Research, v. 33, no. 7, p. 1537-1547, https://doi.org/10.1029/96WR00016.","productDescription":"11 p. ","startPage":"1537","endPage":"1547","costCenters":[{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":479917,"rank":0,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1029/96wr00016","text":"Publisher Index Page"},{"id":337842,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Massachusetts","otherGeospatial":"Cape Cod","volume":"33","issue":"7","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"58d0ea1ce4b0236b68f6737b","contributors":{"authors":[{"text":"Rubin, Yoram","contributorId":189432,"corporation":false,"usgs":false,"family":"Rubin","given":"Yoram","email":"","affiliations":[],"preferred":false,"id":685081,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Ezzedine, Souheil","contributorId":189491,"corporation":false,"usgs":false,"family":"Ezzedine","given":"Souheil","email":"","affiliations":[],"preferred":false,"id":685082,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":6754,"text":"fs04797 - 1997 - The U.S. Geological Survey Drinking Water Initiative","interactions":[],"lastModifiedDate":"2012-02-02T00:06:01","indexId":"fs04797","displayToPublicDate":"1997-07-01T00:00:00","publicationYear":"1997","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":313,"text":"Fact Sheet","code":"FS","onlineIssn":"2327-6932","printIssn":"2327-6916","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"047-97","title":"The U.S. Geological Survey Drinking Water Initiative","docAbstract":"Safe drinking-water supplies are critical to maintaining and preserving public health. Although the Nation's drinking water is generally safe, natural and introduced contaminants in water supplies throughout the country have adversely affected human health. This new U.S. Geological Survey (USGS) initiative will provide information on the vulnerability of water supplies to be used by water-supply and regulatory agencies who must balance water-supply protection with the wise use of public funds. Using the results of the initiative, they will be better able to focus on the supplies most at risk and the variability of contaminants of most concern, and so address the mandates of the Safe Drinking Water Act. With its store of geologic, hydrologic, and land use and land cover data and its network of information in every State, the USGS can help to identify potential sources of contamination, delineate source areas, determine the vulnerability of waters to potential contamination, and evaluate strategies being used to protect source waters in light of the scientific information available. Many recent and ongoing studies by the USGS concern drinking-water issues. This fact sheet highlights four particular studies begun under the Drinking Water Initiative.","language":"ENGLISH","publisher":"Geological Survey (U.S.)","doi":"10.3133/fs04797","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1997, The U.S. Geological Survey Drinking Water Initiative: U.S. Geological Survey Fact Sheet 047-97, 2 p., https://doi.org/10.3133/fs04797.","productDescription":"2 p.","costCenters":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"links":[{"id":125753,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/fs_047_97.bmp"},{"id":776,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/FS/FS-047-97","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4abce4b07f02db673545","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":528775,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":5436,"text":"fs00397 - 1997 - USGS research on saline waters co-produced with energy resources","interactions":[],"lastModifiedDate":"2019-12-05T10:23:22","indexId":"fs00397","displayToPublicDate":"1997-07-01T00:00:00","publicationYear":"1997","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":313,"text":"Fact Sheet","code":"FS","onlineIssn":"2327-6932","printIssn":"2327-6916","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"003-97","title":"USGS research on saline waters co-produced with energy resources","docAbstract":"The United States energy industry faces the challenge of satisfying our expanding thirst for energy while protecting the environment. This challenge is magnified by the increasing volumes of saline water produced with oil and gas in the Nation's aging petroleum fields. Ultimately, energy-producing companies are responsible for disposing of these waters. USGS research provides basic information, for use by regulators, industry, and the public, about the chemistry of co-produced waters and environmentally acceptable ways of handling them.
","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/fs00397","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1997, USGS research on saline waters co-produced with energy resources: U.S. Geological Survey Fact Sheet 003-97, HTML, https://doi.org/10.3133/fs00397.","productDescription":"HTML","costCenters":[{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":117619,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/fs_003_97.jpg"},{"id":584,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/fs/1997/fs003-97/FS-003-97.html","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a28e4b07f02db6115ba","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":528578,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70207765,"text":"70207765 - 1997 - Effect of hydrologic management on marsh surface sediment deposition in coastal Louisiana","interactions":[],"lastModifiedDate":"2020-01-09T15:24:46","indexId":"70207765","displayToPublicDate":"1997-06-01T15:04:25","publicationYear":"1997","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1583,"text":"Estuaries","active":true,"publicationSubtype":{"id":10}},"title":"Effect of hydrologic management on marsh surface sediment deposition in coastal Louisiana","docAbstract":"High rates of coastal land loss in Louisiana have prompted efforts to maintain or restore coastal wetland habitats, and structural management of marsh hydrology is one of a number of approaches that has been adopted. The aim of this study was to determine the effect of hydrologic management measures on marsh-surface sediment deposition in the Mississippi deltaic plain. Four impoundments, ranging in size from 50 ha to 177 ha and similarly sized control sites were included in the study. At each site, marsh-surface sediment traps were collected approximately biweekly for 3.5 yr to measure changes in sediment deposition. There was no significant difference in sediment deposition between any of the impoundment and control sites during the premanagement period. The results show no significant difference in marsh-surface sediment deposition between management year 1992–1993 and management year 1994–1995, but management year 1993–1994 had significantly lower sediment deposition than either the first or the last year of the study. Management year 1992–1993 showed the highest sediment deposition when it was assessed across all basins, areas, and sites, and this high rate of deposition is accounted for by the impact of Hurricane Andrew. For all management years there were significant differences between impoundment and control sites, with control sites showing higher rates of marsh surface sediment deposition than impoundments. No clear pattern was identified concerning the influence of various types of hydrologic management on rates of sediment deposition. This reduction in sediment deposition indicated that the areas under management in this study are receiving insufficient inorganic sediment deposition to keep pace with sea-level rise.
","language":"English","publisher":"Springer","doi":"10.2307/1352345","usgsCitation":"Reed, D., De Luca, N., and Foote, A.L., 1997, Effect of hydrologic management on marsh surface sediment deposition in coastal Louisiana: Estuaries, v. 20, no. 2, p. 301-311, https://doi.org/10.2307/1352345.","productDescription":"11 p.","startPage":"301","endPage":"311","costCenters":[{"id":455,"text":"National Wetlands Research Center","active":true,"usgs":true},{"id":17705,"text":"Wetland and Aquatic Research Center","active":true,"usgs":true}],"links":[{"id":371124,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Louisiana","otherGeospatial":"Barataria Basin, Terrebonne Basin","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -89.14306640625,\n 29.964452850852005\n ],\n [\n -90.615234375,\n 30.32547125932808\n ],\n [\n -91.60400390625,\n 30.90222470517144\n ],\n [\n -92.362060546875,\n 31.924192605327708\n ],\n [\n -92.64770507812499,\n 32.11980111179328\n ],\n [\n -92.98828125,\n 31.774877618507386\n ],\n [\n -92.28515625,\n 30.230594564932193\n ],\n [\n -92.26318359375,\n 29.76437737516313\n ],\n [\n -91.12060546875,\n 29.200123477644983\n ],\n [\n -90.15380859375,\n 29.065772888415406\n ],\n [\n -89.05517578125,\n 29.0273547804184\n ],\n [\n -89.14306640625,\n 29.964452850852005\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"20","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Reed, D.J.","contributorId":40949,"corporation":false,"usgs":true,"family":"Reed","given":"D.J.","email":"","affiliations":[],"preferred":false,"id":779235,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"De Luca, Nina","contributorId":221627,"corporation":false,"usgs":false,"family":"De Luca","given":"Nina","email":"","affiliations":[],"preferred":false,"id":779236,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Foote, A. Lee","contributorId":216145,"corporation":false,"usgs":false,"family":"Foote","given":"A.","email":"","middleInitial":"Lee","affiliations":[],"preferred":false,"id":779237,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":2224,"text":"wsp2482 - 1997 - Use of particle tracking to improve numerical model calibration and to analyze ground-water flow and contaminant migration, Massachusetts Military Reservation, western Cape Cod, Massachusetts","interactions":[{"subject":{"id":23811,"text":"ofr96214 - 1996 - Use of particle tracking to improve numerical model calibration and to analyze ground-water flow and contaminant migration, Massachusetts Military Reservation, western Cape Cod, Massachusetts","indexId":"ofr96214","publicationYear":"1996","noYear":false,"title":"Use of particle tracking to improve numerical model calibration and to analyze ground-water flow and contaminant migration, Massachusetts Military Reservation, western Cape Cod, Massachusetts"},"predicate":"SUPERSEDED_BY","object":{"id":2224,"text":"wsp2482 - 1997 - Use of particle tracking to improve numerical model calibration and to analyze ground-water flow and contaminant migration, Massachusetts Military Reservation, western Cape Cod, Massachusetts","indexId":"wsp2482","publicationYear":"1997","noYear":false,"title":"Use of particle tracking to improve numerical model calibration and to analyze ground-water flow and contaminant migration, Massachusetts Military Reservation, western Cape Cod, Massachusetts"},"id":1}],"lastModifiedDate":"2018-05-17T14:12:06","indexId":"wsp2482","displayToPublicDate":"1997-06-01T00:00:00","publicationYear":"1997","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":341,"text":"Water Supply Paper","code":"WSP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"2482","title":"Use of particle tracking to improve numerical model calibration and to analyze ground-water flow and contaminant migration, Massachusetts Military Reservation, western Cape Cod, Massachusetts","docAbstract":"A steady-state, three-dimensional flow model coupled with a particle-tracking algorithm was developed to assess the complex interaction of hydrogeologic conditions affecting ground-water flow and contaminant transport--including aquifer heterogeneities, hydrologic boundaries such as ponds and streams, ground-water withdrawals, and aquifer recharge to characterize the migration of contaminants emanating from beneath the Massachusetts Military Reservation, Cape Cod, Massachusetts. The known extent of contaminant plumes were used to assess the effects of changes in model input parameters on model-calculated water-table and pond altitudes, streamflow, and water-particle pathlines. Although changes in selected simulated hydrogeologic conditions resulted in minor changes in model-calculated water-table altitudes, pond altitudes, and streamflow, these changes had significant effects on the projection of model-calculated water-particle pathlines.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wsp2482","usgsCitation":"Masterson, J., Walter, D.A., and Savoie, J., 1997, Use of particle tracking to improve numerical model calibration and to analyze ground-water flow and contaminant migration, Massachusetts Military Reservation, western Cape Cod, Massachusetts: U.S. Geological Survey Water Supply Paper 2482, v, 50 p. :ill., maps ;28 cm., https://doi.org/10.3133/wsp2482.","productDescription":"v, 50 p. :ill., maps ;28 cm.","costCenters":[{"id":466,"text":"New England Water Science Center","active":true,"usgs":true}],"links":[{"id":137695,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/2482/report-thumb.jpg"},{"id":27973,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/2482/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a17e4b07f02db60441e","contributors":{"authors":[{"text":"Masterson, John P. 0000-0003-3202-4413 jpmaster@usgs.gov","orcid":"https://orcid.org/0000-0003-3202-4413","contributorId":1865,"corporation":false,"usgs":true,"family":"Masterson","given":"John P.","email":"jpmaster@usgs.gov","affiliations":[{"id":466,"text":"New England Water Science Center","active":true,"usgs":true}],"preferred":false,"id":144848,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Walter, Donald A. 0000-0003-0879-4477 dawalter@usgs.gov","orcid":"https://orcid.org/0000-0003-0879-4477","contributorId":1101,"corporation":false,"usgs":true,"family":"Walter","given":"Donald","email":"dawalter@usgs.gov","middleInitial":"A.","affiliations":[{"id":466,"text":"New England Water Science Center","active":true,"usgs":true}],"preferred":true,"id":144846,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Savoie, Jennifer G. jsavoie@usgs.gov","contributorId":1691,"corporation":false,"usgs":true,"family":"Savoie","given":"Jennifer G.","email":"jsavoie@usgs.gov","affiliations":[{"id":466,"text":"New England Water Science Center","active":true,"usgs":true}],"preferred":false,"id":144847,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":24298,"text":"ofr9723 - 1997 - Digital atlas of Oklahoma","interactions":[],"lastModifiedDate":"2012-02-02T00:08:01","indexId":"ofr9723","displayToPublicDate":"1997-06-01T00:00:00","publicationYear":"1997","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":"97-23","title":"Digital atlas of Oklahoma","docAbstract":"This compact disc contains 25 digital map data sets covering the State of Oklahoma that may be of interest to the general public, private industry, schools, and government agencies. Fourteen data sets are statewide. These data sets include: administrative boundaries; 104th U.S. Congressional district boundaries; county boundaries; latitudinal lines; longitudinal lines; geographic names; indexes of U.S. Geological Survey 1:100,000, and 1:250,000-scale topographic quadrangles; a shaded-relief image; Oklahoma State House of Representatives district boundaries; Oklahoma State Senate district boundaries; locations of U.S. Geological Survey stream gages; watershed boundaries and hydrologic cataloging unit numbers; and locations of weather stations. Eleven data sets are divided by county and are located in 77 county subdirectories. These data sets include: census block group boundaries with selected demographic data; city and major highways text; geographic names; land surface elevation contours; elevation points; an index of U.S. Geological Survey 1:24,000-scale topographic quadrangles; roads, streets and address ranges; highway text; school district boundaries; streams, river and lakes; and the public land survey system.\r\nAll data sets are provided in a readily accessible format. Most data sets are provided in Digital Line Graph (DLG) format. The attributes for many of the DLG files are stored in related dBASE(R)-format files and may be joined to the data set polygon attribute or arc attribute tables using dBASE(R)-compatible software. (Any use of trade names in this publication is for descriptive purposes only and does not imply endorsement by the U.S. Government.) Point attribute tables are provided in dBASE(R) format only, and include the X and Y map coordinates of each point. Annotation (text plotted in map coordinates) are provided in AutoCAD Drawing Exchange format (DXF) files. The shaded-relief image is provided in TIFF format. All data sets except the shaded-relief image also are provided in ARC/INFO export-file format.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr9723","issn":"0094-9140","usgsCitation":"Rea, A.H., and Becker, C., 1997, Digital atlas of Oklahoma: U.S. Geological Survey Open-File Report 97-23, 1 computer laser optical disk ;4 3/4 in., https://doi.org/10.3133/ofr9723.","productDescription":"1 computer laser optical disk ;4 3/4 in.","costCenters":[],"links":[{"id":1673,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://ok.water.usgs.gov/gis/digatlas/","linkFileType":{"id":5,"text":"html"}},{"id":155066,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b32e4b07f02db6b4609","contributors":{"authors":[{"text":"Rea, A. H.","contributorId":58301,"corporation":false,"usgs":true,"family":"Rea","given":"A.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":191650,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Becker, C.J.","contributorId":64269,"corporation":false,"usgs":true,"family":"Becker","given":"C.J.","email":"","affiliations":[],"preferred":false,"id":191651,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":6411,"text":"pp1572 - 1997 - Numerical simulation of ground-water flow through glacial deposits and crystalline bedrock in the Mirror Lake area, Grafton County, New Hampshire","interactions":[],"lastModifiedDate":"2019-10-10T09:03:24","indexId":"pp1572","displayToPublicDate":"1997-06-01T00:00:00","publicationYear":"1997","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":331,"text":"Professional Paper","code":"PP","onlineIssn":"2330-7102","printIssn":"1044-9612","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"1572","title":"Numerical simulation of ground-water flow through glacial deposits and crystalline bedrock in the Mirror Lake area, Grafton County, New Hampshire","docAbstract":"This report documents the development of a computer model to simulate steady-state (long-term average) flow of ground water in the vicinity of Mirror Lake, which lies at the eastern end of the Hubbard Brook valley in central New Hampshire. The 10-km2 study area includes Mirror Lake, the three streams that flow into Mirror Lake, Leeman's Brook, Paradise Brook, and parts of Hubbard Brook and the Pemigewasset River. The topography of the area is characterized by steep hillsides and relatively flat valleys. Major hydrogeologic units include glacial deposits, composed of till containing pockets of sand and gravel, and fractured crystalline bedrock, composed of schist intruded by granite, pegmatite, and lamprophyre. Ground water occurs in both the glacial deposits and bedrock. Precipitation and snowmelt infiltrate to the water table on the hillsides, flow downslope through the saturated glacial deposits and fractured bedrock, and discharge to streams and to Mirror Lake. \r\n\r\n The model domain includes the glacial deposits, the uppermost 150m of bedrock, Mirror Lake, the layer of organic sediments on the lake bottom, and streams and rivers within the study area. A streamflow routing package was included in the model to simulate baseflow in streams and interaction between streams and ground water. Recharge from precipitation is assumed to be areally uniform, and riparian evapotranspiration along stream banks is assumed negligible. The spatial distribution of hydraulic conductivity is represented by dividing the model domain into several zones, each having uniform hydraulic properties. Local variations in recharge and hydraulic conductivities are ignored; therefore, the simulation results characterize the general ground-water system, not local details of ground-water movement. \r\n\r\n The model was calibrated using a nonlinear regression method to match hydraulic heads measured in piezometers and wells, and baseflow in three inlet streams to Mirror Lake. Model calibration indicates that recharge from precipitation to the water table is 26 to 28 cm/year. Hydraulic conductivities are 1.7 x 10-6 to 2.7 x 10-6 m/s for glacial deposits, about 3 x 10-7 m/s for bedrock beneath lower hillsides and valleys, and about 6x10-8 m/s for bedrock beneath upper hillsides and hilltops. Analysis of parameter uncertainty indicates that the above values are well constrained, at least within the context of regression analysis. In the regression, several attributes of the ground-water flow model are assumed perfectly known. The hydraulic conductivity for bedrock beneath upper hillsides and hilltops was determined from few data, and additional data are needed to further confirm this result. Model fit was not improved by introducing a 10-to-1 ration of horizontal-to-vertical anisotropy in the hydraulic conductivity of the glacial deposits, or by varying hydraulic conductivity with depth in the modeled part (uppermost 150m) of the bedrock. \r\n\r\n The calibrated model was used to delineate the Mirror Lake ground-water basin, defined as the volumes of subsurface through which ground water flows from the water table to Mirror Lake or its inlet streams. Results indicate that Mirror Lake and its inlet streams drain an area of ground-water recharge that is about 1.5 times the area of the surface-water basin. The ground-water basin extends far up the hillside on the northwestern part of the study area. Ground water from this area flows at depth under Norris Brook to discharge into Mirror Lake or its inlet streams. As a result, the Mirror Lake ground-water basin extends beneath the adjacent ground-water basin that drains into Norris Brook. \r\n\r\n Model simulation indicates that approximately 300,000 m3/year of precipitation recharges the Mirror Lake ground-water basin. About half the recharge enters the basin in areas where the simulated water table lies in glacial deposits; the other half enters the basin in areas where the simulated water table lies in be","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/pp1572","usgsCitation":"Tiedeman, C.R., Goode, D., and Hsieh, P.A., 1997, Numerical simulation of ground-water flow through glacial deposits and crystalline bedrock in the Mirror Lake area, Grafton County, New Hampshire: U.S. Geological Survey Professional Paper 1572, 50 p., https://doi.org/10.3133/pp1572.","productDescription":"50 p.","costCenters":[{"id":532,"text":"Pennsylvania Water Science Center","active":true,"usgs":true},{"id":589,"text":"Toxic Substances Hydrology 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