{"pageNumber":"3569","pageRowStart":"89200","pageSize":"25","recordCount":184938,"records":[{"id":25477,"text":"wri974196 - 1997 - Environmental setting and implications for water quality in the Western Lake Michigan Drainages","interactions":[],"lastModifiedDate":"2018-10-22T19:25:01","indexId":"wri974196","displayToPublicDate":"1998-10-01T00:00:00","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":"97-4196","title":"Environmental setting and implications for water quality in the Western Lake Michigan Drainages","docAbstract":"<p>In 1991, the U.S. Geological Survey began to implement its National Water-Quality Assessment (NAWQA) program. The Western Lake Michigan Drainages was one of 20 study units selected for investigation to begin in 1991. The study-unit investigation will include an assessment of surface- and ground-water quality. The quality of water in a study unit is intrinsically related to the natural and anthropogenic features of the study unit. The natural features include geology, weather and climate, vegetation, and hydrology. The anthropogenic features of the basin include population distribution, land use and land cover, agricultural practices, and water use. This report describes the natural and anthropogenic features that constitute the environmental setting of the Western Lake Michigan Drainages as well as the implications of those features on the water quality.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri974196","usgsCitation":"1997, Environmental setting and implications for water quality in the Western Lake Michigan Drainages: U.S. Geological Survey Water-Resources Investigations Report 97-4196, ix, 79 p., https://doi.org/10.3133/wri974196.","productDescription":"ix, 79 p.","numberOfPages":"88","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":677,"text":"Wisconsin Water Science Center","active":true,"usgs":true}],"links":[{"id":54203,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1997/4196/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":118942,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1997/4196/report-thumb.jpg"}],"country":"United States","state":"Wisconsin","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -86.429443359375,\n              45.61403741135093\n            ],\n            [\n              -86.66015624999999,\n              46.40756396630067\n            ],\n            [\n              -87.099609375,\n              46.41513877649202\n            ],\n            [\n              -87.51708984375,\n              46.53619267489863\n            ],\n            [\n              -87.71484375,\n              46.626806395355175\n            ],\n            [\n              -88.033447265625,\n              46.7549166192819\n            ],\n            [\n              -88.13232421875,\n              46.7549166192819\n            ],\n            [\n              -88.39599609375,\n              46.76244305208004\n            ],\n            [\n              -88.934326171875,\n              46.604167162931844\n            ],\n            [\n              -89.176025390625,\n              46.52863469527167\n            ],\n            [\n              -89.296875,\n              46.32417161725694\n            ],\n            [\n              -89.84619140625,\n              45.4524242413431\n            ],\n            [\n              -90.142822265625,\n              44.56699093657141\n            ],\n            [\n              -90.274658203125,\n              43.667871610117494\n            ],\n            [\n              -89.84619140625,\n              43.068887774169625\n            ],\n            [\n              -89.47265625,\n              42.819580715795915\n            ],\n            [\n              -88.9013671875,\n              42.69858589169842\n            ],\n            [\n              -88.26416015625,\n              42.601619944327965\n            ],\n            [\n              -87.791748046875,\n              42.48019996901214\n            ],\n            [\n              -87.6708984375,\n              42.827638636242284\n            ],\n            [\n              -87.78076171875,\n              43.1811470593997\n            ],\n            [\n              -87.5390625,\n              44.07969327425713\n            ],\n            [\n              -87.308349609375,\n              44.55916341529184\n            ],\n            [\n              -86.8359375,\n              45.22848059584359\n            ],\n            [\n              -86.781005859375,\n              45.43700828867389\n            ],\n            [\n              -86.737060546875,\n              45.460130637921004\n            ],\n            [\n              -86.429443359375,\n              45.61403741135093\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a13e4b07f02db602287","contributors":{"editors":[{"text":"Peters, C.A.","contributorId":29794,"corporation":false,"usgs":true,"family":"Peters","given":"C.A.","email":"","affiliations":[],"preferred":false,"id":749314,"contributorType":{"id":2,"text":"Editors"},"rank":1}]}}
,{"id":32041,"text":"ofr97854A - 1997 - Digital and preliminary bedrock geologic map of the Chittenden quadrangle, Vermont","interactions":[],"lastModifiedDate":"2021-11-01T21:07:57.994284","indexId":"ofr97854A","displayToPublicDate":"1998-10-01T00:00:00","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":"97-854","chapter":"A","title":"Digital and preliminary bedrock geologic map of the Chittenden quadrangle, Vermont","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr97854A","usgsCitation":"Ratcliffe, N.M., 1997, Digital and preliminary bedrock geologic map of the Chittenden quadrangle, Vermont: U.S. Geological Survey Open-File Report 97-854, 1 Plate: 45.94 × 32.72 inches, https://doi.org/10.3133/ofr97854A.","productDescription":"1 Plate: 45.94 × 32.72 inches","costCenters":[],"links":[{"id":160977,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":109008,"rank":700,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_18867.htm","linkFileType":{"id":5,"text":"html"},"description":"18867"},{"id":60204,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1997/0854a/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"24000","country":"United States","state":"Vermont","otherGeospatial":"Chittenden quadrangle","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -73,\n              43.75\n            ],\n            [\n              -72.875,\n              43.75\n            ],\n            [\n              -72.875,\n              43.625\n            ],\n            [\n              -73,\n              43.625\n            ],\n            [\n              -73,\n              43.75\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a9ae4b07f02db65d5c0","contributors":{"authors":[{"text":"Ratcliffe, Nicholas M. 0000-0002-7922-5784 nratclif@usgs.gov","orcid":"https://orcid.org/0000-0002-7922-5784","contributorId":4167,"corporation":false,"usgs":true,"family":"Ratcliffe","given":"Nicholas","email":"nratclif@usgs.gov","middleInitial":"M.","affiliations":[],"preferred":true,"id":207511,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":30013,"text":"wri974063 - 1997 - Urbanization and recharge in the vicinity of East Meadow Brook, Nassau County, New York: Part 2 — Effect of urban runoff on the hydrology of the headwaters of East Meadow Brook, 1989-90","interactions":[],"lastModifiedDate":"2022-12-06T22:25:42.72833","indexId":"wri974063","displayToPublicDate":"1998-10-01T00:00:00","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":"97-4063","title":"Urbanization and recharge in the vicinity of East Meadow Brook, Nassau County, New York: Part 2 — Effect of urban runoff on the hydrology of the headwaters of East Meadow Brook, 1989-90","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri974063","usgsCitation":"Stumm, F., and Ku, H.F., 1997, Urbanization and recharge in the vicinity of East Meadow Brook, Nassau County, New York: Part 2 — Effect of urban runoff on the hydrology of the headwaters of East Meadow Brook, 1989-90: U.S. Geological Survey Water-Resources Investigations Report 97-4063, iv, 24 p., https://doi.org/10.3133/wri974063.","productDescription":"iv, 24 p.","costCenters":[{"id":474,"text":"New York Water Science Center","active":true,"usgs":true}],"links":[{"id":410127,"rank":2,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_48689.htm","linkFileType":{"id":5,"text":"html"}},{"id":58819,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1997/4063/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":160471,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1997/4063/report-thumb.jpg"}],"country":"United States","state":"New York","county":"Nassau County","otherGeospatial":"East Meadow Brook","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -73.5867,\n              40.7306\n            ],\n            [\n              -73.5867,\n              40.7167\n            ],\n            [\n              -73.5806,\n              40.7167\n            ],\n            [\n              -73.5806,\n              40.7306\n            ],\n            [\n              -73.5867,\n              40.7306\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adfe4b07f02db687799","contributors":{"authors":[{"text":"Stumm, Frederick 0000-0002-5388-8811 fstumm@usgs.gov","orcid":"https://orcid.org/0000-0002-5388-8811","contributorId":1077,"corporation":false,"usgs":true,"family":"Stumm","given":"Frederick","email":"fstumm@usgs.gov","affiliations":[{"id":474,"text":"New York Water Science Center","active":true,"usgs":true}],"preferred":true,"id":202531,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Ku, Henry F. H.","contributorId":11258,"corporation":false,"usgs":true,"family":"Ku","given":"Henry","email":"","middleInitial":"F. H.","affiliations":[],"preferred":false,"id":202532,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":27109,"text":"wri974148 - 1997 - Results of quality-control sampling of water, bed sediment, and tissue in the Western Lake Michigan Drainages study unit of the National Water-Quality Assessment Program","interactions":[],"lastModifiedDate":"2015-10-22T11:09:08","indexId":"wri974148","displayToPublicDate":"1998-10-01T00:00:00","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":"97-4148","title":"Results of quality-control sampling of water, bed sediment, and tissue in the Western Lake Michigan Drainages study unit of the National Water-Quality Assessment Program","docAbstract":"<p>This report contains the quality control results of the Western Lake Michigan Drainages study unit of the National Water Quality Assessment Program. Quality control samples were collected in the same manner and contemporaneously with environmental samples during the first highintensity study phase in the unit (1992 through 1995) and amounted to approximately 15 percent of all samples collected. The accuracy and precision of hundreds of chemical analyses of surface and ground-water, bed sediment, and tissue was determined through the collection and analysis of field blanks, field replicates and splits, matrix spikes, and surrogates. Despite the several detections of analytes in the field blanks, the concentrations of most constituents in the environmental samples will likely be an order of magnitude or higher than those in the blanks. However, frequent detections, and high concentrations, of dissolved organic carbon (DOC) in several surface and ground-water blanks are probably significant with respect to commonly measured environmental concentrations, and the environmental data will have to be qualified accordingly. The precision of sampling of water on a percent basis, as determined from replicates and splits, was generally proportional to the concentration of the constituents, with constituents present in relatively high concentrations generally having less sampling variability than those with relatively low concentrations. In general, analytes with relatively high variability between replicates were present at concentrations near the reporting limit or were associated with relatively small absolute concentration differences, or both. Precision of replicates compared to that for splits in bed sediment samples was similar, thus eliminating sampling as a major source of variability in analyte concentrations. In the case the phthalates in bed sediment, contamination in either the field or laboratory could have caused the relatively large variability between replicate samples and between split samples.Variability of analyte concentrations in tissue samples was relatively low, being 29 percent or less for all constituents. Recoveries of most laboratory schedule 2001/2010 pesticide spike compounds in surfacewater samples were reasonably good. Low intrinsic method recovery resulted in relatively low recovery forp,p'-DDE, metribuzin, and propargite. In the case of propargite, decomposition with the environmental sample matrices was also indicated. Recoveries of two compounds, cyanazine and thiobencarb, might have been biased high due to interferences. The one laboratory schedule 2050/2051 field matrix pesticide spike indicated numerous operational problems with this method that biased recoveries either low or high. Recoveries of pesticides from both pesticide schedules in field spikes of ground-water samples generally were similar to those of field matrix spikes of surface- water samples. High maximum recoveries were noted for tebuthiuron, disulfoton, DCPA, and permethrin, which indicates the possible presence of interferents in the matrices for these compounds. Problems in the recoveries of pesticides on schedule 2050/2051 from ground-water samples generally were the same as those for surfacewater samples. Recoveries of VOCs in field matrix spikes were reasonable when consideration was given for the use of the micropipettor that delivered only about 80 percent on average of the nominal mass of spiked analytes. Finally, the recoveries of most surrogate compounds in surface and ground-water samples were reasonable. Problems in sample handling (for example, spillage) were likely not the cause of any of the low recoveries of spiked compounds.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri974148","usgsCitation":"Fitzgerald, S., 1997, Results of quality-control sampling of water, bed sediment, and tissue in the Western Lake Michigan Drainages study unit of the National Water-Quality Assessment Program: U.S. Geological Survey Water-Resources Investigations Report 97-4148, vii, 24 p., https://doi.org/10.3133/wri974148.","productDescription":"vii, 24 p.","numberOfPages":"31","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":677,"text":"Wisconsin Water Science Center","active":true,"usgs":true}],"links":[{"id":158993,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1997/4148/report-thumb.jpg"},{"id":55969,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1997/4148/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Michigan, Wisconsin","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -86.429443359375,\n              45.61403741135093\n            ],\n            [\n              -86.66015624999999,\n              46.40756396630067\n            ],\n            [\n              -87.099609375,\n              46.41513877649202\n            ],\n            [\n              -87.51708984375,\n              46.53619267489863\n            ],\n            [\n              -87.71484375,\n              46.626806395355175\n            ],\n            [\n              -88.033447265625,\n              46.7549166192819\n            ],\n            [\n              -88.13232421875,\n              46.7549166192819\n            ],\n            [\n              -88.39599609375,\n              46.76244305208004\n            ],\n            [\n              -88.934326171875,\n              46.604167162931844\n            ],\n            [\n              -89.176025390625,\n              46.52863469527167\n            ],\n            [\n              -89.296875,\n              46.32417161725694\n            ],\n            [\n              -89.84619140625,\n              45.4524242413431\n            ],\n            [\n              -90.142822265625,\n              44.56699093657141\n            ],\n            [\n              -90.274658203125,\n              43.667871610117494\n            ],\n            [\n              -89.84619140625,\n              43.068887774169625\n            ],\n            [\n              -89.47265625,\n              42.819580715795915\n            ],\n            [\n              -88.9013671875,\n              42.69858589169842\n            ],\n            [\n              -88.26416015625,\n              42.601619944327965\n            ],\n            [\n              -87.791748046875,\n              42.48019996901214\n            ],\n            [\n              -87.6708984375,\n              42.827638636242284\n            ],\n            [\n              -87.78076171875,\n              43.1811470593997\n            ],\n            [\n              -87.5390625,\n              44.07969327425713\n            ],\n            [\n              -87.308349609375,\n              44.55916341529184\n            ],\n            [\n              -86.8359375,\n              45.22848059584359\n            ],\n            [\n              -86.781005859375,\n              45.43700828867389\n            ],\n            [\n              -86.737060546875,\n              45.460130637921004\n            ],\n            [\n              -86.429443359375,\n              45.61403741135093\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a26e4b07f02db60fa32","contributors":{"authors":[{"text":"Fitzgerald, S.A.","contributorId":94348,"corporation":false,"usgs":true,"family":"Fitzgerald","given":"S.A.","email":"","affiliations":[],"preferred":false,"id":197565,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":23437,"text":"ofr97496 - 1997 - 4th International Symposium on Environmental Geochemistry; program with abstracts","interactions":[],"lastModifiedDate":"2018-10-25T18:49:00","indexId":"ofr97496","displayToPublicDate":"1998-10-01T00:00:00","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":"97-496","title":"4th International Symposium on Environmental Geochemistry; program with abstracts","language":"ENGLISH","publisher":"U.S. Geological Survey :\r\n[Branch of Information Services, distributor],","doi":"10.3133/ofr97496","issn":"0094-9140","usgsCitation":"Marsh, S., and Gough, L.P., 1997, 4th International Symposium on Environmental Geochemistry; program with abstracts: U.S. Geological Survey Open-File Report 97-496, xxvi, 106 p. :ill. ;28 cm., https://doi.org/10.3133/ofr97496.","productDescription":"xxvi, 106 p. :ill. ;28 cm.","costCenters":[],"links":[{"id":156367,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1997/0496/report-thumb.jpg"},{"id":52759,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1997/0496/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53cd4934e4b0b290850eefa0","contributors":{"editors":[{"text":"Wanty, R.B. 0000-0002-2063-6423","orcid":"https://orcid.org/0000-0002-2063-6423","contributorId":96298,"corporation":false,"usgs":true,"family":"Wanty","given":"R.B.","affiliations":[],"preferred":false,"id":749913,"contributorType":{"id":2,"text":"Editors"},"rank":1}],"authors":[{"text":"Marsh, S.P.","contributorId":32913,"corporation":false,"usgs":true,"family":"Marsh","given":"S.P.","email":"","affiliations":[],"preferred":false,"id":190101,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Gough, L. P.","contributorId":64198,"corporation":false,"usgs":true,"family":"Gough","given":"L.","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":190102,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":26947,"text":"wri974272 - 1997 - Mesocosm experiments to assess factors affecting phosphorus retention and release in an extended Wisconsin wetland","interactions":[],"lastModifiedDate":"2015-10-27T15:54:54","indexId":"wri974272","displayToPublicDate":"1998-10-01T00:00:00","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":"97-4272","title":"Mesocosm experiments to assess factors affecting phosphorus retention and release in an extended Wisconsin wetland","docAbstract":"<p>Phosphorus retention by wetland sediments and vegetation was investigated in Jackson Creek wetland, an extension of an existing prairie marsh in southeastern Wisconsin. The extended wetland construction was undertaken in 1992-93 to help reduce the phosphorus loading to a downstream eutrophic lake. Two approaches were used to study potential and actual phosphorus retention in the system. Mesocosm experiments of 20-40 days duration indicated that retention of total and dissolved reactive phosphorus in mesocosm cells containing macrophytes and/or sediments was reduced by factors of 2-20 relative to cells containing only water or a copper algicide to suppress metabolic activity. In contrast to the nutrient trapping function, these results show a potential for net phosphorus release that can be associated with increased biological richness. Measurements of water flow and nutrient loads at the wetland's inflow and outflow points demonstrated 9-39% net uptake of phosphorus on an annual scale but frequent occurrences of net phosphorus release over shorter (one-month) time scales. These episodes of release are most likely during the summer months. Thus, the wetland role in phosphorus cycling is not one of a true source or sink, although the annual budget data alone suggest substantial net retention. Effective management of the wetland for its nutrient trapping potential can be hindered by this oversimplification. The system is instead subject to relatively short-term alternation between net import and export. The periodic phosphorus export, although representing a small fraction of net annual import, could be critical for growth of macrophyte and algal communities downstream.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri974272","collaboration":"Prepared in cooperation with the Wisconsin Department of Natural Resources","usgsCitation":"Elder, J.F., Manion, B., and Goddard, G.L., 1997, Mesocosm experiments to assess factors affecting phosphorus retention and release in an extended Wisconsin wetland: U.S. Geological Survey Water-Resources Investigations Report 97-4272, vi, 14 p., https://doi.org/10.3133/wri974272.","productDescription":"vi, 14 p.","numberOfPages":"19","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":677,"text":"Wisconsin Water Science Center","active":true,"usgs":true}],"links":[{"id":119103,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1997/4272/report-thumb.jpg"},{"id":55835,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1997/4272/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Wisconsin","county":"Walworth County","otherGeospatial":"Delevan Lake, Jackson Creek","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -88.57383728027344,\n              42.717759147911806\n            ],\n            [\n              -88.76884460449219,\n              42.62385465855651\n            ],\n            [\n              -88.8079833984375,\n              42.583422001323584\n            ],\n            [\n              -88.76335144042969,\n              42.55763248666914\n            ],\n            [\n              -88.69606018066406,\n              42.54498667313236\n            ],\n            [\n              -88.6164093017578,\n              42.552574468712514\n            ],\n            [\n              -88.56559753417969,\n              42.56623017635374\n            ],\n            [\n              -88.48663330078125,\n              42.628401690377316\n            ],\n            [\n              -88.45848083496094,\n              42.64204079304428\n            ],\n            [\n              -88.44131469726562,\n              42.66325123326261\n            ],\n            [\n              -88.43376159667969,\n              42.68344492725026\n            ],\n            [\n              -88.41316223144531,\n              42.705145830019895\n            ],\n            [\n              -88.4674072265625,\n              42.72835235396481\n            ],\n            [\n              -88.57383728027344,\n              42.717759147911806\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a4ae4b07f02db624f47","contributors":{"authors":[{"text":"Elder, J. 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,{"id":4947,"text":"fs16497 - 1997 - Variability of nutrients in streams in part of the Upper Mississippi River Basin, Minnesota and Wisconsin","interactions":[],"lastModifiedDate":"2018-03-12T12:41:05","indexId":"fs16497","displayToPublicDate":"1998-09-01T00:00:00","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":"164-97","title":"Variability of nutrients in streams in part of the Upper Mississippi River Basin, Minnesota and Wisconsin","docAbstract":"<p>Physical conditions differ among the Mississippi River and its major tributaries in Minnesota and Wisconsin. Analysis of the environmental framework of the basin and analysis of historical water-quality information by the National Water-Quality Assessment (NAWQA) Program shows that nutrients (nitrogen and phosphorus) in streams in the Upper Mississippi River Basin are influenced primarily by land use. In the Mississippi River, nutrient concentrations were greater downstream of the Minnesota River and major wastewater discharge points in the Twin Cities Metropolitan Area (TCMA). Stream loads of nutrients (the amount of the constituent carried past a point on a stream during a given period of time) also increased downstream of the Minnesota River and major wastewater discharge points in the TCMA.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Mounds View, MN","doi":"10.3133/fs16497","usgsCitation":"Kroening, S.E., and Stark, J.R., 1997, Variability of nutrients in streams in part of the Upper Mississippi River Basin, Minnesota and Wisconsin: U.S. Geological Survey Fact Sheet 164-97, 5 p., https://doi.org/10.3133/fs16497.","productDescription":"5 p.","onlineOnly":"Y","additionalOnlineFiles":"Y","costCenters":[{"id":392,"text":"Minnesota Water Science Center","active":true,"usgs":true}],"links":[{"id":31808,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/fs/1997/0164/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":12197,"rank":100,"type":{"id":15,"text":"Index 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,{"id":27928,"text":"wri974047 - 1997 - Integrity of production wells and confining unit at the Naval Weapons Industrial Reserve Plant, Dallas, Texas, 1995","interactions":[],"lastModifiedDate":"2023-04-13T21:02:23.847588","indexId":"wri974047","displayToPublicDate":"1998-09-01T00:00:00","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":"97-4047","title":"Integrity of production wells and confining unit at the Naval Weapons Industrial Reserve Plant, Dallas, Texas, 1995","docAbstract":"<p>Ground water in the shallow alluvial aquifer is contaminated at the Naval Weapons Industrial Reserve Plant, Dallas, Texas. Five production wells at the site are cased through the alluvial aquifer and underlying units and are screened in either the Paluxy or Twin Mountains aquifers. Three abandoned wells, originally completed in the Twin Mountains aquifer but filled with drilling mud in 1958, also penetrate the alluvial aquifer. The Paluxy and Twin Mountains aquifers are used for drinking-water supplies in and around the Dallas-Fort Worth metroplex.</p>\n<p>Trichloroethylene and its degradation products, dichloroethylene and vinyl chloride, and the metal chromium previously have been detected in the shallow alluvial aquifer. Current (1995) analyses of water-quality samples taken from the static water column of the five production wells and one of the abandoned wells indicate no trichloroethylene, dichloroethylene, or vinyl chloride in the water column of these wells. Chromium was detected in all samples, but concentrations were less than the practical quantitation limit, which is the regulatory action level for this site.</p>\n<p>The results of borehole geophysical log analysis indicate that two of the production wells could have vertically connected intervals where cement bonding in the well annulus is poor. The other production wells have overall good bonding. Temperature logs do not indicate flow behind casing except in the screened interval of one well. Geophysical logs show the Eagle Ford Shale ranges from 147 to 185 feet thick at the site. The Eagle Ford Shale has low permeability and a high plasticity index. These physical characteristics make the Eagle Ford Shale an excellent confining unit.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Austin, TX","doi":"10.3133/wri974047","collaboration":"Prepared in cooperation with the Southern Division Naval Facilities Engineering Command","usgsCitation":"Jones, S.A., and Paillet, F.L., 1997, Integrity of production wells and confining unit at the Naval Weapons Industrial Reserve Plant, Dallas, Texas, 1995: U.S. Geological Survey Water-Resources Investigations Report 97-4047, iv, 30 p., https://doi.org/10.3133/wri974047.","productDescription":"iv, 30 p.","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":122662,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/wri_97_4047.jpg"},{"id":415738,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_48677.htm","linkFileType":{"id":5,"text":"html"}},{"id":2195,"rank":2,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/wri97-4047/","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Texas","county":"Dallas","otherGeospatial":"Naval Weapons Industrial Reserve Plant","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -96.97206974029541,\n              32.745630348985976\n            ],\n            [\n              -96.97224140167236,\n              32.738013925875606\n            ],\n            [\n              -96.97473049163818,\n              32.737977827533605\n            ],\n            [\n              -96.97704792022705,\n              32.73844710483917\n            ],\n            [\n              -96.97696208953857,\n              32.73689487047408\n            ],\n            [\n              -96.97751998901367,\n              32.73700316677224\n            ],\n            [\n              -96.97794914245605,\n              32.736389486009415\n            ],\n            [\n              -96.9792366027832,\n              32.73570360250915\n            ],\n            [\n              -96.97992324829102,\n              32.734801116177394\n            ],\n            [\n              -96.98571681976318,\n              32.73476501653406\n            ],\n            [\n              -96.98588848114014,\n              32.735631403938896\n            ],\n            [\n              -96.98627471923828,\n              32.736281188965556\n            ],\n            [\n              -96.98661804199219,\n              32.73667827748301\n            ],\n            [\n              -96.98726177215576,\n              32.73696706802081\n            ],\n            [\n              -96.98773384094237,\n              32.738013925875606\n            ],\n            [\n              -96.9873046875,\n              32.7450889186024\n            ],\n            [\n              -96.97206974029541,\n              32.745630348985976\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ab0e4b07f02db66d630","contributors":{"authors":[{"text":"Jones, Sonya A. 0000-0002-7462-8576 sajones@usgs.gov","orcid":"https://orcid.org/0000-0002-7462-8576","contributorId":1690,"corporation":false,"usgs":true,"family":"Jones","given":"Sonya","email":"sajones@usgs.gov","middleInitial":"A.","affiliations":[],"preferred":true,"id":198917,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Paillet, Frederick L.","contributorId":38191,"corporation":false,"usgs":true,"family":"Paillet","given":"Frederick","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":198918,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":4989,"text":"fs12397 - 1997 - Flood of January 1997 in Truckee River Basin, Western Nevada","interactions":[],"lastModifiedDate":"2012-02-02T00:05:30","indexId":"fs12397","displayToPublicDate":"1998-09-01T00:00:00","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":"123-97","title":"Flood of January 1997 in Truckee River Basin, Western Nevada","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/fs12397","usgsCitation":"Hess, G.W., and Williams, R.P., 1997, Flood of January 1997 in Truckee River Basin, Western Nevada: U.S. Geological Survey Fact Sheet 123-97, 1 sheet : col. ill., col. map ; 28 cm. col. ill., col. map ;, https://doi.org/10.3133/fs12397.","productDescription":"1 sheet : col. ill., col. map ; 28 cm. col. ill., col. map ;","costCenters":[],"links":[{"id":125256,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/fs/1997/0123/report-thumb.jpg"},{"id":31829,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/fs/1997/0123/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f2e4b07f02db5eee25","contributors":{"authors":[{"text":"Hess, Glen W.","contributorId":19136,"corporation":false,"usgs":true,"family":"Hess","given":"Glen","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":150248,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Williams, Rhea P.","contributorId":87114,"corporation":false,"usgs":true,"family":"Williams","given":"Rhea","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":150249,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":27927,"text":"wri974078 - 1997 - Chemical evolution and estimated flow velocity of water in the Trinity Aquifer, south-central Texas","interactions":[],"lastModifiedDate":"2016-08-19T13:21:32","indexId":"wri974078","displayToPublicDate":"1998-09-01T00:00:00","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":"97-4078","title":"Chemical evolution and estimated flow velocity of water in the Trinity Aquifer, south-central Texas","docAbstract":"<p>Three permeable zones with varying lithology and water chemistry compose the Trinity aquifer, a principal source of water in the 5,500- square-mile study area in south-central Texas. The upper permeable zone locally yields small quantities of water to wells and was not included in this study. The middle permeable zone primarily is composed of limestone with minor amounts of dolostone. Terrigenous sand and marine limestone, with minor amounts of dolostone, are the principal lithologic units in the lower permeable zone. Dissolved solids concentrations range from 329 to 1,820 milligrams per liter in water samples from the middle permeable zone and from 518 to 3,030 milligrams per liter in water samples from the lower permeable zone. Principal hydrochemical facies in the middle permeable zone are calcium magnesium bicarbonate and calcium magnesium sulfate. Hydrochemical facies in ground-water samples from the lower permeable zone vary. Tritium concentrations as large as 5.3 tritium units in the southeastern part of the study area are indicative of relatively recent recharge. Results of a geochemical mass balance simulation along a flowpath in the middle permeable zone indicate a mass transfer of 4.25 millimoles per liter of dolomite dissolved, 5.74 millimoles per liter of gypsum dissolved, 0.46 millimole per liter of sodium chloride dissolved, 8.07 millimoles per liter of calcite precipitated, and 0.67 millimole per liter of calcium-for-sodium cation exchange between solid and aqueous phases. These results support dedolomitization as a principal chemical process in the middle permeable zone of the Trinity aquifer. Results of a simulation along a flowpath in the lower permeable zone indicate a mass transfer of 0.41 millimole per liter of dolomite dissolved, 0.001 millimole per liter of gypsum dissolved, 9.58 millimoles per liter of sodium chloride dissolved, 1.09 millimoles per liter of calcite precipitated, and 1.11 millimoles per liter of sodium-forcalcium cation exchange between solid and aqueous phases. Lower permeable zone processes indicate sodium chloride dissolution, dedolomitization, and cation exchange. Ground-water-flow velocities determined from adjusted carbon-14 ages, calculated using NETPATH, for selected flowpaths in the middle and lower permeable zones were about 1.7 feet per year and less than about 4.4 feet per year, respectively.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Austin, TX","doi":"10.3133/wri974078","usgsCitation":"Jones, S.A., Lee, R.W., and Busby, J., 1997, Chemical evolution and estimated flow velocity of water in the Trinity Aquifer, south-central Texas: U.S. Geological Survey Water-Resources Investigations Report 97-4078, iv, 22 p., https://doi.org/10.3133/wri974078.","productDescription":"iv, 22 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"links":[{"id":124327,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/wri_97_4078.jpg"},{"id":2194,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/wri97-4078/","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Texas","otherGeospatial":"Trinity Aquifer","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e478fe4b07f02db48a003","contributors":{"authors":[{"text":"Jones, Sonya A. 0000-0002-7462-8576 sajones@usgs.gov","orcid":"https://orcid.org/0000-0002-7462-8576","contributorId":1690,"corporation":false,"usgs":true,"family":"Jones","given":"Sonya","email":"sajones@usgs.gov","middleInitial":"A.","affiliations":[],"preferred":true,"id":198914,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Lee, Roger W.","contributorId":105273,"corporation":false,"usgs":true,"family":"Lee","given":"Roger","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":198916,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Busby, John F.","contributorId":42186,"corporation":false,"usgs":true,"family":"Busby","given":"John F.","affiliations":[],"preferred":false,"id":198915,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":25604,"text":"wri974193 - 1997 - Hydrology and water quality of the Beaver Dam Wash area, Washington County, Utah, Lincoln County, Nevada, and Mohave County, Arizona","interactions":[],"lastModifiedDate":"2012-02-02T00:08:24","indexId":"wri974193","displayToPublicDate":"1998-09-01T00:00:00","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":"97-4193","title":"Hydrology and water quality of the Beaver Dam Wash area, Washington County, Utah, Lincoln County, Nevada, and Mohave County, Arizona","language":"ENGLISH","publisher":"U.S. Geological Survey ;\r\nBranch of Information Services [distributor],","doi":"10.3133/wri974193","usgsCitation":"Holmes, W., Pyper, G., Gates, J.S., Schaefer, D.H., and Waddell, K., 1997, Hydrology and water quality of the Beaver Dam Wash area, Washington County, Utah, Lincoln County, Nevada, and Mohave County, Arizona: U.S. Geological Survey Water-Resources Investigations Report 97-4193, vi, 71 p. :ill. (some col.), maps (some col.) ;28 cm., https://doi.org/10.3133/wri974193.","productDescription":"vi, 71 p. :ill. (some col.), maps (some col.) ;28 cm.","costCenters":[],"links":[{"id":121884,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1997/4193/report-thumb.jpg"},{"id":54347,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1997/4193/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a18e4b07f02db604c62","contributors":{"authors":[{"text":"Holmes, W. F.","contributorId":7277,"corporation":false,"usgs":true,"family":"Holmes","given":"W. F.","affiliations":[],"preferred":false,"id":194371,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Pyper, G. E.","contributorId":35337,"corporation":false,"usgs":true,"family":"Pyper","given":"G. E.","affiliations":[],"preferred":false,"id":194372,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Gates, J. S.","contributorId":99553,"corporation":false,"usgs":true,"family":"Gates","given":"J.","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":194375,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Schaefer, D. H.","contributorId":84763,"corporation":false,"usgs":true,"family":"Schaefer","given":"D.","middleInitial":"H.","affiliations":[],"preferred":false,"id":194374,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Waddell, K.M.","contributorId":59009,"corporation":false,"usgs":true,"family":"Waddell","given":"K.M.","email":"","affiliations":[],"preferred":false,"id":194373,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":22005,"text":"ofr97736 - 1997 - Paleontological data from Mud Creek Core 1, southern Florida","interactions":[],"lastModifiedDate":"2012-02-02T00:07:50","indexId":"ofr97736","displayToPublicDate":"1998-09-01T00:00:00","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":"97-736","title":"Paleontological data from Mud Creek Core 1, southern Florida","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr97736","issn":"0094-9140","usgsCitation":"Willard, D., Brewster-Wingard, G., Fellman, C., and Ishman, S., 1997, Paleontological data from Mud Creek Core 1, southern Florida: U.S. Geological Survey Open-File Report 97-736, 13 p. :ill., map ;28 cm., https://doi.org/10.3133/ofr97736.","productDescription":"13 p. :ill., map ;28 cm.","costCenters":[],"links":[{"id":153750,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":1179,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/pdf/of/ofr97736.html","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae4e4b07f02db689c60","contributors":{"authors":[{"text":"Willard, Debra  A. 0000-0003-4878-0942","orcid":"https://orcid.org/0000-0003-4878-0942","contributorId":85982,"corporation":false,"usgs":true,"family":"Willard","given":"Debra  A.","affiliations":[],"preferred":false,"id":186639,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Brewster-Wingard, G. L.","contributorId":102508,"corporation":false,"usgs":true,"family":"Brewster-Wingard","given":"G. L.","affiliations":[],"preferred":false,"id":186640,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Fellman, Claire","contributorId":50929,"corporation":false,"usgs":true,"family":"Fellman","given":"Claire","email":"","affiliations":[],"preferred":false,"id":186638,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Ishman, S. E.","contributorId":20346,"corporation":false,"usgs":true,"family":"Ishman","given":"S. E.","affiliations":[],"preferred":false,"id":186637,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":25567,"text":"wri974228 - 1997 - Hydrogeologic framework and simulation of ground-water flow and travel time in the shallow aquifer system in the area of Naval Support Activity Memphis, Millington, Tennessee","interactions":[],"lastModifiedDate":"2012-02-02T00:08:23","indexId":"wri974228","displayToPublicDate":"1998-09-01T00:00:00","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":"97-4228","title":"Hydrogeologic framework and simulation of ground-water flow and travel time in the shallow aquifer system in the area of Naval Support Activity Memphis, Millington, Tennessee","docAbstract":"Naval Support Activity (NSA) Memphis is a Department of the Navy facility located at the City of Millington, Tennessee, about 5 miles north of Memphis. Contaminants have been detected in surface-water, sediment, and ground-water samples collected at the facility. As part of the Installation Restoration Program, the Navy is considering remedial-action options to prevent or lessen the effect of ground-water contamination at the facility and to control the movement and discharge of contaminants. A numerical model of the ground-water-flow system in the area of NSA Memphis was constructed and calibrated so that quantifiable estimates could be made of ground-water-flow rates, direction, and time-of-travel.  The sediments beneath NSA Memphis, to a depth of about 200 feet, form a shallow aquifer system. From youngest to oldest, the stratigraphic units that form the shallow aquifer system are alluvium, loess, fluvial deposits, and the Cockfield and Cook Mountain Formations. The shallow aquifer system is organized into five hydrogeologic units: (1) a confining unit composed of the relatively low permeability sediments of the upper alluvium and the loess; (2) the A1 aquifer comprising sand and gravel of the lower alluvium and the fluvial deposits, and sand lenses in the upper part of the preserved section of the Cockfield Formation; (3) a confining unit composed of clay and silt within the upper part of the Cockfield Formation; (4) the Cockfield aquifer comprising sand lenses within the lower part of the preserved section of the Cockfield Formation; and (5) a confining unit formed by low permeability sediments of the Cook Mountain Formation that composes the upper confining unit for the Memphis aquifer. Thicknesses of individual units vary considerably across the facility. Structural and depositional features that affect the occurrence of ground water in the shallow aquifer system include faulting, an erosional scarp, and 'windows' in the confining units. Underlying the shallow aquifer system is the Memphis aquifer, the primary source of water for NSA Memphis and the City of Memphis, Tennessee. Analyses of sediment cores, aquifer and well specific-capacity tests, and numerical modeling were used to estimate the hydraulic characteristics of units of the shallow aquifer system. The vertical hydraulic conductivity of core samples of the alluvium-loess confining unit ranged from about 8.5 x 10-5 to 1.6 x 10-2 feet per day, and the total porosity of the samples ranged from about 35 to 48 percent. The results of the aquifer test were used to estimate a horizontal hydraulic conductivity of about 5 feet per day for the alluvial-fluvial deposits aquifer. The total porosity of core samples of the alluvial-fluvial deposits aquifer ranged from about 22 to 39 percent. The vertical hydraulic conductivity of core samples of the Cockfield confining unit ranged from about 4.5 x 10-5 to 2.5 x 10-3 feet per day, and the total porosity ranged from about 41 to 55 percent. Well specific-capacity tests indicate that the horizontal hydraulic conductivity of sand units that compose the Cockfield aquifer range from about 0.5 to 3 feet per day. The vertical hydraulic conductivity of core samples of the Cook Mountain confining unit ranged from about 5.0 x 10-6 to 9.9 x 10-4 feet per day. Total porosity of core samples of the Cook Mountain confining unit ranged from about 30 to 42 percent. Ground-water flow and time-of-travel in the shallow aquifer system were simulated using the MODFLOW finite-difference model and the -particle-tracking program MODPATH. A three-layer, steady-state model of the shallow aquifer system was constructed and calibrated to the potentiometric surface of the A1 aquifer. Results of numerical modeling support the proposed conceptual hydrogeologic model of the shallow aquifer system. Ground-water time-of-travel in the A1 aquifer was simulated using an assumed effective porosity of 25 percent. Typical ground-water-flow velocities were on the or","language":"ENGLISH","publisher":"U.S. Geological Survey ;\r\nBranch of Information Services [distributor],","doi":"10.3133/wri974228","usgsCitation":"Robinson, J.L., Carmichael, J.K., Halford, K.J., and Ladd, D.E., 1997, Hydrogeologic framework and simulation of ground-water flow and travel time in the shallow aquifer system in the area of Naval Support Activity Memphis, Millington, Tennessee: U.S. Geological Survey Water-Resources Investigations Report 97-4228, vi, 56 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri974228.","productDescription":"vi, 56 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":118760,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1997/4228/report-thumb.jpg"},{"id":1909,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/wri974228","linkFileType":{"id":5,"text":"html"}},{"id":54288,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1997/4228/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a4ee4b07f02db627dc7","contributors":{"authors":[{"text":"Robinson, James L.","contributorId":82284,"corporation":false,"usgs":true,"family":"Robinson","given":"James","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":194230,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Carmichael, John K. 0000-0003-1099-841X jkcarmic@usgs.gov","orcid":"https://orcid.org/0000-0003-1099-841X","contributorId":4554,"corporation":false,"usgs":true,"family":"Carmichael","given":"John","email":"jkcarmic@usgs.gov","middleInitial":"K.","affiliations":[{"id":24708,"text":"Lower Mississippi-Gulf Water Science Center","active":true,"usgs":true}],"preferred":true,"id":194229,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Halford, Keith J. 0000-0002-7322-1846 khalford@usgs.gov","orcid":"https://orcid.org/0000-0002-7322-1846","contributorId":1374,"corporation":false,"usgs":true,"family":"Halford","given":"Keith","email":"khalford@usgs.gov","middleInitial":"J.","affiliations":[{"id":465,"text":"Nevada Water Science Center","active":true,"usgs":true}],"preferred":true,"id":194227,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Ladd, David E. 0000-0002-9247-7839 deladd@usgs.gov","orcid":"https://orcid.org/0000-0002-9247-7839","contributorId":1646,"corporation":false,"usgs":true,"family":"Ladd","given":"David","email":"deladd@usgs.gov","middleInitial":"E.","affiliations":[{"id":581,"text":"Tennessee Water Science Center","active":true,"usgs":true}],"preferred":true,"id":194228,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":24872,"text":"ofr97865 - 1997 - Data related to contaminant distribution at the Beatty, Nevada and Richland, Washington low-level radioactive waste disposal sites","interactions":[],"lastModifiedDate":"2012-02-02T00:08:24","indexId":"ofr97865","displayToPublicDate":"1998-09-01T00:00:00","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":"97-865","title":"Data related to contaminant distribution at the Beatty, Nevada and Richland, Washington low-level radioactive waste disposal sites","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr97865","issn":"0094-9140","usgsCitation":"Wilshire, H.G., and Friedman, I., 1997, Data related to contaminant distribution at the Beatty, Nevada and Richland, Washington low-level radioactive waste disposal sites: U.S. Geological Survey Open-File Report 97-865, 30 p. :ill., maps ;28 cm., https://doi.org/10.3133/ofr97865.","productDescription":"30 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":157564,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1997/0865/report-thumb.jpg"},{"id":53864,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1997/0865/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac7e4b07f02db67b562","contributors":{"authors":[{"text":"Wilshire, H. G.","contributorId":36125,"corporation":false,"usgs":false,"family":"Wilshire","given":"H.","middleInitial":"G.","affiliations":[],"preferred":false,"id":192718,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Friedman, Irving","contributorId":90664,"corporation":false,"usgs":true,"family":"Friedman","given":"Irving","email":"","affiliations":[],"preferred":false,"id":192719,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
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,{"id":6624,"text":"fs03797 - 1997 - Flood-control effects of Truckee River Basin Reservoirs, December 31, 1996, through January 4, 1997, California and Nevada","interactions":[],"lastModifiedDate":"2018-08-20T17:46:48","indexId":"fs03797","displayToPublicDate":"1998-09-01T00:00:00","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":"037-97","title":"Flood-control effects of Truckee River Basin Reservoirs, December 31, 1996, through January 4, 1997, California and Nevada","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/fs03797","usgsCitation":"Berris, S.N., Hess, G., Taylor, R.L., and Bohman, L.R., 1997, Flood-control effects of Truckee River Basin Reservoirs, December 31, 1996, through January 4, 1997, California and Nevada: U.S. Geological Survey Fact Sheet 037-97, 1 sheet : col. ill., col. map ; 43 x 28 cm. by 22 x 28 cm. col. ill., col. map ;, https://doi.org/10.3133/fs03797.","productDescription":"1 sheet : col. ill., col. map ; 43 x 28 cm. by 22 x 28 cm. col. ill., col. map ;","costCenters":[],"links":[{"id":34062,"rank":299,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/fs/1997/0037/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":118134,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/fs/1997/0037/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f1e4b07f02db5eeab5","contributors":{"authors":[{"text":"Berris, Steven N. snberris@usgs.gov","contributorId":1736,"corporation":false,"usgs":true,"family":"Berris","given":"Steven","email":"snberris@usgs.gov","middleInitial":"N.","affiliations":[],"preferred":true,"id":153050,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hess, Glen gwhess@usgs.gov","contributorId":4619,"corporation":false,"usgs":true,"family":"Hess","given":"Glen","email":"gwhess@usgs.gov","affiliations":[{"id":518,"text":"Oregon Water Science Center","active":true,"usgs":true}],"preferred":true,"id":153052,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Taylor, R. Lynn","contributorId":85616,"corporation":false,"usgs":true,"family":"Taylor","given":"R.","email":"","middleInitial":"Lynn","affiliations":[],"preferred":false,"id":153051,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Bohman, Larry R. lrbohman@usgs.gov","contributorId":4769,"corporation":false,"usgs":true,"family":"Bohman","given":"Larry","email":"lrbohman@usgs.gov","middleInitial":"R.","affiliations":[],"preferred":true,"id":153053,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":5122,"text":"fs22996 - 1997 - The \"100-Year Flood\"","interactions":[],"lastModifiedDate":"2018-06-20T13:38:03","indexId":"fs22996","displayToPublicDate":"1998-09-01T00:00:00","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":"229-96","title":"The \"100-Year Flood\"","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/fs22996","usgsCitation":"Dinicola, K., 1997, The \"100-Year Flood\": U.S. Geological Survey Fact Sheet 229-96, 2 p., https://doi.org/10.3133/fs22996.","productDescription":"2 p.","costCenters":[],"links":[{"id":117079,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/fs_229_96.jpg"},{"id":513,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/FS/FS-229-96/","linkFileType":{"id":5,"text":"html"}},{"id":355213,"rank":3,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/fs/FS-229-96/pdf/FS_229-96.pdf","text":"Report","size":"586 KB","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad5e4b07f02db6836cc","contributors":{"authors":[{"text":"Dinicola, Karen","contributorId":87918,"corporation":false,"usgs":true,"family":"Dinicola","given":"Karen","email":"","affiliations":[],"preferred":false,"id":150454,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":23772,"text":"ofr97569 - 1997 - Ground-water flow in the Saginaw aquifer in the vicinity of the north Lansing well field, Lansing Michigan — Part 1, simulations with a regional model","interactions":[],"lastModifiedDate":"2022-09-27T19:06:06.200532","indexId":"ofr97569","displayToPublicDate":"1998-09-01T00:00:00","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":"97-569","title":"Ground-water flow in the Saginaw aquifer in the vicinity of the north Lansing well field, Lansing Michigan — Part 1, simulations with a regional model","docAbstract":"<p>Vinyl chloride has been detected in water from the Saginaw aquifer near Lansing Board of Water and Light wells in the north Lansing well field. These public-supply wells have the potential to withdraw contaminated ground water. Groundwater-flow simulations and particle-tracking analyses with a regional model were used to investigate local ground-water movement. The effectiveness of hypothetical purge wells to remove ground water containing vinyl chloride was also evaluated. Five pumping scenarios were developed to assess effects of existing groundwater pumping conditions and alternative groundwater management options on the movement of the vinyl chloride plume in the Saginaw aquifer. Results indicate that under 1995 average pumping conditions, four public-supply wells in the north Lansing well field will remove water that originates in a portion of the Saginaw aquifer known to be contaminated with vinyl chloride. When pumping rates by wells in the north Lansing well field are reduced to simulate winter withdrawals, four public-supply wells to the west and south of the north Lansing well field remove water that originates in a portion of the Saginaw aquifer known to be contaminated with vinyl chloride. Simulation results indicate that purge wells can be used to capture most contaminated water and prevent interception of contaminated water by supply wells. However, further analysis is needed to determine the full extent of the vinyl chloride plume and the potential impact on Lansing Board of Water and Light public-supply wells. </p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Lansing, MI","doi":"10.3133/ofr97569","collaboration":"Prepared in cooperation with Lansing Board of Water and Light","usgsCitation":"Luukkonen, C.L., Grannemann, N., and Holtschlag, D., 1997, Ground-water flow in the Saginaw aquifer in the vicinity of the north Lansing well field, Lansing Michigan — Part 1, simulations with a regional model: U.S. Geological Survey Open-File Report 97-569, v, 13 p., https://doi.org/10.3133/ofr97569.","productDescription":"v, 13 p.","costCenters":[{"id":382,"text":"Michigan Water Science Center","active":true,"usgs":true}],"links":[{"id":407467,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_18814.htm","linkFileType":{"id":5,"text":"html"}},{"id":157453,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1997/0569/report-thumb.jpg"},{"id":52999,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1997/0569/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Michigan","city":"Lansing","otherGeospatial":"Saginaw aquifer","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -84.514,\n              42.724\n            ],\n            [\n              -84.573,\n              42.724\n            ],\n            [\n              -84.573,\n              42.768\n            ],\n            [\n              -84.514,\n              42.768\n            ],\n            [\n              -84.514,\n              42.724\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aafe4b07f02db66cd7b","contributors":{"authors":[{"text":"Luukkonen, C. L.","contributorId":28962,"corporation":false,"usgs":true,"family":"Luukkonen","given":"C.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":190694,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Grannemann, N.G.","contributorId":11221,"corporation":false,"usgs":true,"family":"Grannemann","given":"N.G.","affiliations":[],"preferred":false,"id":190693,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Holtschlag, D. J. 0000-0001-5185-4928","orcid":"https://orcid.org/0000-0001-5185-4928","contributorId":102493,"corporation":false,"usgs":true,"family":"Holtschlag","given":"D. J.","affiliations":[],"preferred":false,"id":190695,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":23773,"text":"ofr97570 - 1997 - Ground-water flow in the Saginaw aquifer in the vicinity of the north Lansing well field, Lansing Michigan — Part 2, simulations with a regional model using a reduced cell size","interactions":[],"lastModifiedDate":"2022-09-27T19:09:44.590801","indexId":"ofr97570","displayToPublicDate":"1998-09-01T00:00:00","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":"97-570","title":"Ground-water flow in the Saginaw aquifer in the vicinity of the north Lansing well field, Lansing Michigan — Part 2, simulations with a regional model using a reduced cell size","docAbstract":"<p>Vinyl chloride has been detected in water from the Saginaw aquifer near Lansing Board of Water and Light wells in the north Lansing well field. These public-supply wells have the potential to withdraw contaminated ground water. The effects of reduced grid spacing for the existing TriCounty regional ground-water-flow model on local ground-water movement were investigated. This refinement of the grid eliminated multiple wells in a cell and reduced the number of wells represented as weak sinks. Two pumping scenarios were developed to investigate the effects of pumping conditions, plume size, and hypothetical purge well locations on the movement of the vinyl chloride plume in the Saginaw aquifer. </p><p>Under 1995 pumping conditions, water that originates in the central portion of the Saginaw aquifer known to be contaminated with vinyl chloride is prevented from reaching Lansing Board of Water and Light supply wells when hypothetical purge wells located west of the plume are simulated as pumping either 100 gallons per minute or 200 gallons per minute. Purge wells located north of the plume are effective at preventing contamination from reaching Lansing Board of Water and Light supply wells when simulated as pumping 200 gallons per minute. Water that originates within and surrounding the area known to be contaminated with vinyl chloride is not prevented from reaching Lansing Board of Water and Light supply wells under 1995 conditions using either purge well location or pumping rate. </p><p>Under 1997 pumping conditions, water that originates in the central portion of the Saginaw aquifer known to be contaminated with vinyl chloride is prevented from reaching Lansing Board of Water and Light supply wells when hypothetical purge wells located either west or north of the plume are simulated as pumping 200 gallons per minute. Water that originates within and surrounding the area known to be contaminated with vinyl chloride is not prevented from reaching Lansing Board of Water and Light supply wells under 1997 conditions using either purge well location or pumping rate.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Lansing, MI","doi":"10.3133/ofr97570","collaboration":"Prepared in cooperation with Lansing Board of Water and Light","usgsCitation":"Luukkonen, C.L., Grannemann, N., and Holtschlag, D., 1997, Ground-water flow in the Saginaw aquifer in the vicinity of the north Lansing well field, Lansing Michigan — Part 2, simulations with a regional model using a reduced cell size: U.S. Geological Survey Open-File Report 97-570, vi, 25 p., https://doi.org/10.3133/ofr97570.","productDescription":"vi, 25 p.","costCenters":[{"id":382,"text":"Michigan Water Science Center","active":true,"usgs":true}],"links":[{"id":53000,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1997/0570/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":407468,"rank":2,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_18815.htm","linkFileType":{"id":5,"text":"html"}},{"id":157454,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1997/0570/report-thumb.jpg"}],"country":"United States","state":"Michigan","city":"Lansing","otherGeospatial":"Saginaw aquifer","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -84.514,\n              42.724\n            ],\n            [\n              -84.573,\n              42.724\n            ],\n            [\n              -84.573,\n              42.768\n            ],\n            [\n              -84.514,\n              42.768\n            ],\n            [\n              -84.514,\n              42.724\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aafe4b07f02db66cd88","contributors":{"authors":[{"text":"Luukkonen, C. 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,{"id":31639,"text":"ofr97481 - 1997 - Geologic map of the West Fall Butte quadrangle, Malheur County, Oregon","interactions":[],"lastModifiedDate":"2022-08-09T19:06:36.86901","indexId":"ofr97481","displayToPublicDate":"1998-09-01T00:00:00","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":"97-481","title":"Geologic map of the West Fall Butte quadrangle, Malheur County, Oregon","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr97481","usgsCitation":"Evans, J.G., and Binger, G.B., 1997, Geologic map of the West Fall Butte quadrangle, Malheur County, Oregon: U.S. Geological Survey Open-File Report 97-481, Report: 11 p.; 1 Plate: 40.71 × 31.12 inches, https://doi.org/10.3133/ofr97481.","productDescription":"Report: 11 p.; 1 Plate: 40.71 × 31.12 inches","costCenters":[],"links":[{"id":108995,"rank":700,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_18789.htm","linkFileType":{"id":5,"text":"html"},"description":"18789"},{"id":59853,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1997/0481/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":59852,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1997/0481/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":161472,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1997/0481/report-thumb.jpg"}],"scale":"24000","country":"United States","state":"Oregon","county":"Malheur County","otherGeospatial":"Westfall Butte 7 1/2' quadrangle","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -118,\n              43.875\n            ],\n            [\n              -117.875,\n              43.875\n            ],\n            [\n              -117.875,\n              44\n            ],\n            [\n              -118,\n              44\n            ],\n            [\n              -118,\n              43.875\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a13e4b07f02db601f11","contributors":{"authors":[{"text":"Evans, James George","contributorId":73578,"corporation":false,"usgs":true,"family":"Evans","given":"James","email":"","middleInitial":"George","affiliations":[],"preferred":false,"id":206613,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Binger, G. Benjamin","contributorId":86820,"corporation":false,"usgs":true,"family":"Binger","given":"G.","email":"","middleInitial":"Benjamin","affiliations":[],"preferred":false,"id":206614,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":30155,"text":"wri974207 - 1997 - Evaluation of nitrate sources using nitrogen-isotope techniques in shallow ground water within selected lake basins in the Central Lakes District, Polk and Highlands Counties, Florida","interactions":[],"lastModifiedDate":"2023-04-07T21:55:54.190215","indexId":"wri974207","displayToPublicDate":"1998-09-01T00:00:00","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":"97-4207","title":"Evaluation of nitrate sources using nitrogen-isotope techniques in shallow ground water within selected lake basins in the Central Lakes District, Polk and Highlands Counties, Florida","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri974207","usgsCitation":"Tihansky, A., and Sacks, L.A., 1997, Evaluation of nitrate sources using nitrogen-isotope techniques in shallow ground water within selected lake basins in the Central Lakes District, Polk and Highlands Counties, Florida: U.S. Geological Survey Water-Resources Investigations Report 97-4207, iv, 28 p., https://doi.org/10.3133/wri974207.","productDescription":"iv, 28 p.","costCenters":[],"links":[{"id":415483,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_48816.htm","linkFileType":{"id":5,"text":"html"}},{"id":119682,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1997/4207/report-thumb.jpg"},{"id":58960,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1997/4207/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Florida","county":"Highlands County, Polk County","otherGeospatial":"Central Lakes District","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -81.3167,\n              28.1611\n            ],\n            [\n              -82,\n              28.1611\n            ],\n            [\n              -82,\n              27.2\n            ],\n            [\n              -81.3167,\n              27.2\n            ],\n            [\n              -81.3167,\n              28.1611\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a09e4b07f02db5facb6","contributors":{"authors":[{"text":"Tihansky, A. B. 0000-0003-1681-1601","orcid":"https://orcid.org/0000-0003-1681-1601","contributorId":77956,"corporation":false,"usgs":true,"family":"Tihansky","given":"A. B.","affiliations":[],"preferred":false,"id":202779,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Sacks, L. A.","contributorId":83092,"corporation":false,"usgs":true,"family":"Sacks","given":"L.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":202780,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":24274,"text":"ofr97402 - 1997 - Characterization of stormwater runoff from the Naval Air Station and Naval Wepons Industrial Reserve Plant, Dallas, Texas, 1994-96","interactions":[],"lastModifiedDate":"2016-08-22T15:41:38","indexId":"ofr97402","displayToPublicDate":"1998-09-01T00:00:00","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":"97-402","title":"Characterization of stormwater runoff from the Naval Air Station and Naval Wepons Industrial Reserve Plant, Dallas, Texas, 1994-96","docAbstract":"<p>The characterization of stormwater runoff from the Naval Air Station (NAS) and the Naval Weapons Industrial Reserve Plant (NWIRP), Dallas, Texas, is necessary to determine if runoff from the facilities is contributing to off-site contamination of surface waters, A network of five fixed sites and four grab sites was established to collect stormwater-runoff samples from a substantial part of the drainage area of each facility. Fixed sites were instrumented to measure and store precipitation, stage, discharge, and runoff-volume data and to collect flow-weighted composite samples during a storm. Grab and composite samples were collected for six storms at each of the five fixed sites from October 1994 to March 1996. The grab samples were analyzed for about 100 properties and constituents including specific conductance, pH, water temperature, bacteria, trace elements, oil and grease, total phenols, and volatile organic compounds. The composite samples were analyzed for about 220 properties and constituents including specific conductance, pH, chemical oxygen demand, biochemical oxygen demand, major ions, suspended and dissolved solids, nutrients, trace elements, total organic carbon, volatile organic compounds, semivolatile organic compounds, and organochlorine and organophosphorus pesticides. Grab samples were collected for two storms (September 18,1995, and October 2,1995) at each of the four grab sites. The grab samples were analyzed for about 80 constituents including specific conductance, pH, water temperature, trace elements, and volatile organic compounds. Composite samples were collected for two of the six storms sampled at the fixed sites and analyzed for aquatic toxicity. Fathead minnow growth and survival toxicity tests and water flea reproduction and survival toxicity tests were done.</p>\n<p>Median event-mean concentrations computed for 12 selected constituents in samples from NAS and NWIRP fixed sites were compared to median event-mean concentrations for residential, commercial, industrial, and highway land uses within the Dallas-Fort Worth area computed from data collected for the National Pollutant Discharge Elimination System program. NAS and NWIRP median event-mean concentrations also were compared to those for residential and commercial land uses from the Nationwide Urban Runoff Program.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr97402","issn":"0094-9140","usgsCitation":"Raines, T.H., Baldys, S., and Lizarraga, J., 1997, Characterization of stormwater runoff from the Naval Air Station and Naval Wepons Industrial Reserve Plant, Dallas, Texas, 1994-96: U.S. Geological Survey Open-File Report 97-402, iv, 80 p., https://doi.org/10.3133/ofr97402.","productDescription":"iv, 80 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"links":[{"id":155029,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1997/0402/report-thumb.jpg"},{"id":53396,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1997/0402/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e2e4b07f02db5e4d1e","contributors":{"authors":[{"text":"Raines, T. H.","contributorId":88389,"corporation":false,"usgs":true,"family":"Raines","given":"T.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":191616,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Baldys, Stanley sbaldys@usgs.gov","contributorId":3366,"corporation":false,"usgs":true,"family":"Baldys","given":"Stanley","email":"sbaldys@usgs.gov","affiliations":[],"preferred":true,"id":191614,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Lizarraga, J.S.","contributorId":17875,"corporation":false,"usgs":true,"family":"Lizarraga","given":"J.S.","affiliations":[],"preferred":false,"id":191615,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":27718,"text":"wri974189 - 1997 - Flood of October 1996 in southern Maine","interactions":[],"lastModifiedDate":"2025-01-10T20:55:16.430132","indexId":"wri974189","displayToPublicDate":"1998-09-01T00:00:00","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":"97-4189","title":"Flood of October 1996 in southern Maine","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri974189","usgsCitation":"Hodgkins, G., and Stewart, G., 1997, Flood of October 1996 in southern Maine: U.S. Geological Survey Water-Resources Investigations Report 97-4189, iv, 28 p., https://doi.org/10.3133/wri974189.","productDescription":"iv, 28 p.","costCenters":[],"links":[{"id":119791,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1997/4189/report-thumb.jpg"},{"id":56562,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1997/4189/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":466052,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_48800.htm"}],"country":"United States","state":"Maine","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -70.8,\n              44\n            ],\n            [\n              -70.8,\n              43.17229047615379\n            ],\n            [\n              -70.25,\n              43.17229047615379\n            ],\n            [\n              -70.25,\n              44\n            ],\n            [\n              -70.8,\n              44\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f2e4b07f02db5eec8b","contributors":{"authors":[{"text":"Hodgkins, Glenn","contributorId":29481,"corporation":false,"usgs":true,"family":"Hodgkins","given":"Glenn","affiliations":[],"preferred":false,"id":198583,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Stewart, G.J.","contributorId":62246,"corporation":false,"usgs":true,"family":"Stewart","given":"G.J.","email":"","affiliations":[],"preferred":false,"id":198584,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
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