{"pageNumber":"3845","pageRowStart":"96100","pageSize":"25","recordCount":185189,"records":[{"id":24034,"text":"ofr95324 - 1995 - Withdrawals of ground water and surface water in New Jersey, 1989-90","interactions":[],"lastModifiedDate":"2012-02-02T00:08:15","indexId":"ofr95324","displayToPublicDate":"1996-07-01T00:00:00","publicationYear":"1995","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"95-324","title":"Withdrawals of ground water and surface water in New Jersey, 1989-90","language":"ENGLISH","publisher":"U.S. Geological Survey ;\r\nEarth Science Information Center, Open-File Reports Section [distributor],","doi":"10.3133/ofr95324","issn":"0094-9140","usgsCitation":"Nawyn, J., and Clawges, R., 1995, Withdrawals of ground water and surface water in New Jersey, 1989-90: U.S. Geological Survey Open-File Report 95-324, v [i.e. vi], 52 p. :ill., maps ;28 cm., https://doi.org/10.3133/ofr95324.","productDescription":"v [i.e. vi], 52 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":156728,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1995/0324/report-thumb.jpg"},{"id":53204,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1995/0324/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49dae4b07f02db5e026b","contributors":{"authors":[{"text":"Nawyn, J. P.","contributorId":29016,"corporation":false,"usgs":true,"family":"Nawyn","given":"J. P.","affiliations":[],"preferred":false,"id":191193,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Clawges, R.M.","contributorId":24779,"corporation":false,"usgs":true,"family":"Clawges","given":"R.M.","affiliations":[],"preferred":false,"id":191192,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":24311,"text":"ofr95806 - 1995 - Description and calibration results of an in situ suspended matter sampler; the McLane Water Transfer System","interactions":[],"lastModifiedDate":"2012-02-02T00:08:10","indexId":"ofr95806","displayToPublicDate":"1996-07-01T00:00:00","publicationYear":"1995","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"95-806","title":"Description and calibration results of an in situ suspended matter sampler; the McLane Water Transfer System","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr95806","issn":"0094-9140","usgsCitation":"Rendigs, R., and Commeau, J., 1995, Description and calibration results of an in situ suspended matter sampler; the McLane Water Transfer System: U.S. Geological Survey Open-File Report 95-806, 32 p.  :ill., map ;28 cm., https://doi.org/10.3133/ofr95806.","productDescription":"32 p.  :ill., map ;28 cm.","costCenters":[],"links":[{"id":156253,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1995/0806/report-thumb.jpg"},{"id":53421,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1995/0806/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ab0e4b07f02db66ddc8","contributors":{"authors":[{"text":"Rendigs, R.R.","contributorId":50506,"corporation":false,"usgs":true,"family":"Rendigs","given":"R.R.","affiliations":[],"preferred":false,"id":191674,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Commeau, J.A.","contributorId":21549,"corporation":false,"usgs":true,"family":"Commeau","given":"J.A.","email":"","affiliations":[],"preferred":false,"id":191673,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":24259,"text":"ofr95741 - 1995 - Tritium and radioactive carbon (14C) analyses of gas collected from unsaturated sediments next to a low-level radioactive-waste burial site south of Beatty, Nevada, April 1994 and July 1995","interactions":[],"lastModifiedDate":"2019-12-07T10:54:14","indexId":"ofr95741","displayToPublicDate":"1996-07-01T00:00:00","publicationYear":"1995","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"95-741","displayTitle":"Tritium and radioactive carbon (<i>14</i>C) analyses of gas collected from unsaturated sediments next to a low-level radioactive-waste burial site south of Beatty, Nevada, April 1994 and July 1995","title":"Tritium and radioactive carbon (14C) analyses of gas collected from unsaturated sediments next to a low-level radioactive-waste burial site south of Beatty, Nevada, April 1994 and July 1995","docAbstract":"<p>Tritium activities in water vapor and radioactive carbon (<sup>14</sup>C) activities in carbon dioxide were determined in gas samples pumped from small-diameter air ports installed in a test hole within the unsaturated sediments next to a commercial burial site for low-level radioactive waste south of Beatty, Nevada. In April 1994, gas samples were collected from test hole UZB-2, which was drilled about 350 feet south of the southwest corner of the fence enclosing the burial site. The test hole is part of a study to determine the depth to which atmospheric air circulates through the unsaturated sediments at the desert site. Laboratory results completed in May 1995 show activities of tritium and <sup>14</sup>C were greater than expected, with measured tritium in the water vapor as high as 762 tritium units at a depth of 79 feet and measured <sup>14</sup>C in carbon dioxide as high as 1,700 percent modern carbon at a depth of 18 feet.</p><p>In July 1995, the uppermost five air ports in test hole UZB-2 were resampled. In addition, water vapor was collected for tritium analyses at a distant test hole, and water vapor for tritium analyses and carbon dioxide for <sup>14</sup>C analyses were collected from three depths at the research shaft about 200 feet north of test hole UZB-2, and at two shallow probes (depth of 5.5 feet) next to the fence enclosing the burial site. Analyses of samples collected in the upper 112 feet from test hole UZB-2 in July 1995 show the same distribution of tritium and<sup> 14</sup>C as analyses of samples collected in April 1994, except that activities were somewhat greater in July. The greatest activities of tritium and <sup>14</sup>C were measured from a shallow probe next to the fence with activities of 29,400 tritium units and 517,000 percent modern carbon, respectively.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Carson City, NV","doi":"10.3133/ofr95741","issn":"0094-9140","usgsCitation":"Prudic, D.E., and Striegl, R.G., 1995, Tritium and radioactive carbon (14C) analyses of gas collected from unsaturated sediments next to a low-level radioactive-waste burial site south of Beatty, Nevada, April 1994 and July 1995: U.S. Geological Survey Open-File Report 95-741, iii, 7 p., https://doi.org/10.3133/ofr95741.","productDescription":"iii, 7 p.","costCenters":[{"id":465,"text":"Nevada Water Science Center","active":true,"usgs":true},{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":155054,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1995/0741/report-thumb.jpg"},{"id":53386,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1995/0741/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Nevada","county":"Nye County","city":"Beatty","otherGeospatial":"Amargosa Desert Research Site","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"Polygon\",\"coordinates\":[[[-115.9082,39.1615],[-115.5191,38.9578],[-115.4725,38.9325],[-115.4433,38.9162],[-115.3694,38.8769],[-115.363,38.874],[-115.242,38.8093],[-115.0969,38.7309],[-115.0777,38.721],[-115.0604,38.7107],[-115.0291,38.6937],[-114.999,38.6777],[-114.9996,38.592],[-114.9997,38.4315],[-114.9994,38.3894],[-115.0004,38.0507],[-115.1185,38.0508],[-115.1436,38.0508],[-115.326,38.0515],[-115.3453,38.0514],[-115.4003,38.051],[-115.4587,38.0506],[-115.6394,38.0512],[-115.6581,38.051],[-115.8404,38.0504],[-115.8931,38.0507],[-115.8938,37.723],[-115.8969,37.5498],[-115.8975,37.2796],[-115.8982,37.1926],[-115.8942,36.8425],[-115.8941,36.686],[-115.8945,36.6702],[-115.8949,36.598],[-115.8949,36.5962],[-115.8946,36.5858],[-115.8947,36.5005],[-115.8945,36.4806],[-115.8949,36.462],[-115.8944,36.457],[-115.8948,36.3087],[-115.8945,36.2923],[-115.8943,36.1957],[-115.8945,36.1608],[-115.8948,36.1163],[-115.8948,36.0927],[-115.895,36.0015],[-115.9178,36.0192],[-115.9518,36.0457],[-115.9925,36.0773],[-116.049,36.1211],[-116.0624,36.1314],[-116.1039,36.1636],[-116.1287,36.1829],[-116.1702,36.2152],[-116.173,36.2174],[-116.2311,36.2626],[-116.2834,36.3028],[-116.2954,36.3122],[-116.3752,36.373],[-116.5107,36.4764],[-116.5247,36.4871],[-116.5589,36.5131],[-116.574,36.5245],[-116.5946,36.54],[-116.6556,36.5867],[-116.6583,36.5888],[-116.6764,36.6024],[-116.706,36.6248],[-116.7895,36.6877],[-116.8424,36.7276],[-116.8453,36.7298],[-116.8806,36.7568],[-116.8912,36.7648],[-116.9237,36.7891],[-116.9641,36.8193],[-116.9783,36.8299],[-116.981,36.8319],[-117.0046,36.8495],[-117.164,36.9688],[-117.1639,36.9698],[-117.1637,37.0182],[-117.164,37.0894],[-117.1642,37.171],[-117.1641,37.1909],[-117.1641,37.1936],[-117.1665,37.6995],[-117.1664,37.714],[-117.1663,37.7285],[-117.1663,37.7435],[-117.1662,37.7585],[-117.1657,38.0019],[-117.2198,38.0482],[-117.2397,38.0483],[-117.239,38.0641],[-117.2408,38.0705],[-117.2653,38.0932],[-117.6896,38.4731],[-118.0197,38.7599],[-118.197,38.9154],[-118.1972,38.9993],[-117.8559,39.0746],[-117.7748,39.092],[-117.7008,39.1058],[-117.6409,39.1149],[-117.5946,39.1231],[-117.4742,39.1431],[-117.3823,39.1562],[-117.3609,39.1585],[-117.3318,39.1629],[-117.3063,39.1634],[-117.2849,39.1633],[-117.1995,39.1632],[-117.0856,39.1628],[-117.0322,39.1626],[-117.0144,39.1626],[-116.9871,39.1625],[-116.9158,39.1631],[-116.7562,39.1622],[-116.7301,39.1625],[-116.5996,39.1616],[-116.5859,39.162],[-116.4815,39.1616],[-116.3497,39.1618],[-116.2358,39.1616],[-116.0548,39.1624],[-115.9082,39.1615]]]},\"properties\":{\"name\":\"Nye\",\"state\":\"NV\"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afee4b07f02db6979d6","contributors":{"authors":[{"text":"Prudic, David E. deprudic@usgs.gov","contributorId":3430,"corporation":false,"usgs":true,"family":"Prudic","given":"David","email":"deprudic@usgs.gov","middleInitial":"E.","affiliations":[{"id":465,"text":"Nevada Water Science Center","active":true,"usgs":true}],"preferred":true,"id":191582,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Striegl, Robert G. 0000-0002-8251-4659 rstriegl@usgs.gov","orcid":"https://orcid.org/0000-0002-8251-4659","contributorId":1630,"corporation":false,"usgs":true,"family":"Striegl","given":"Robert","email":"rstriegl@usgs.gov","middleInitial":"G.","affiliations":[{"id":200,"text":"Coop Res Unit Seattle","active":true,"usgs":true},{"id":5044,"text":"National Research Program - Central Branch","active":true,"usgs":true},{"id":37277,"text":"WMA - Earth System Processes Division","active":true,"usgs":true},{"id":36183,"text":"Hydro-Ecological Interactions Branch","active":true,"usgs":true}],"preferred":false,"id":191583,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":23230,"text":"ofr95835 - 1995 - Revised digital aeromagnetic data for areas in and adjacent to the National Petroleum Reserve Area (NPRA), North Slope, Alaska","interactions":[],"lastModifiedDate":"2022-09-30T21:03:36.02054","indexId":"ofr95835","displayToPublicDate":"1996-07-01T00:00:00","publicationYear":"1995","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"95-835","title":"Revised digital aeromagnetic data for areas in and adjacent to the National Petroleum Reserve Area (NPRA), North Slope, Alaska","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr95835","usgsCitation":"Grauch, V., and Castellanos, E., 1995, Revised digital aeromagnetic data for areas in and adjacent to the National Petroleum Reserve Area (NPRA), North Slope, Alaska: U.S. Geological Survey Open-File Report 95-835, 11 p., https://doi.org/10.3133/ofr95835.","productDescription":"11 p.","costCenters":[],"links":[{"id":407745,"rank":2,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_19168.htm","linkFileType":{"id":5,"text":"html"}},{"id":52530,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1995/0835/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":8084,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/1995/ofr-95-0835/","linkFileType":{"id":5,"text":"html"}},{"id":155354,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1995/0835/report-thumb.jpg"}],"country":"United States","state":"Alaska","otherGeospatial":"National Petroleum Reserve Area, North Slope","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -161.368,\n              68\n            ],\n            [\n              -146,\n              68\n            ],\n            [\n              -146,\n              71.5\n            ],\n            [\n              -161.368,\n              71.5\n            ],\n            [\n              -161.368,\n              68\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aafe4b07f02db66c88d","contributors":{"authors":[{"text":"Grauch, V.J. 0000-0002-0761-3489","orcid":"https://orcid.org/0000-0002-0761-3489","contributorId":70362,"corporation":false,"usgs":true,"family":"Grauch","given":"V.J.","affiliations":[],"preferred":false,"id":189685,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Castellanos, Esther","contributorId":21578,"corporation":false,"usgs":true,"family":"Castellanos","given":"Esther","affiliations":[],"preferred":false,"id":189684,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":25575,"text":"wri954139 - 1995 - Hydrogeology and water quality at the management systems evaluation area near Piketon, Ohio","interactions":[],"lastModifiedDate":"2023-01-09T22:03:28.347265","indexId":"wri954139","displayToPublicDate":"1996-07-01T00:00:00","publicationYear":"1995","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"95-4139","title":"Hydrogeology and water quality at the management systems evaluation area near Piketon, Ohio","docAbstract":"<p>This report presents the results of a study by the U.S. Geological Survey, The Ohio State University, and the U.S. Department of Agriculture to describe the hydrology, water quality, and geochemical factors controlling water quality at the Ohio Management Systems Evaluation Area (MSEA). The Ohio MSEA is located on a 650-acre farm in the Scioto River Valley in Pike County, south-central Ohio. The farm is underlain by an incised bedrock valley filled with about 70 feet of sand and gravel outwash deposits that are covered by a veneer of silty clay alluvium and silty loam and sandy loam soils. Outwash sediment are composed predominantly of dolomite, quartz, and calcite, and have a median organic carbon concentration of 0.39 weight percent. Horizontal hydraulic conductivity of the sediment based on results of multiple-well aquifer tests ranges from 400 to 560 feet per day. Ground-water flow is from east to west-southwest at an average velocity of 1.5 to 2.5 feet per day. Ground water and surface water at the site are highly interconnected. Big Beaver Creek recharges the outwash aquifer along the eastern edge of the study area, and ground water discharges to the Scioto River at the western edge of the study area. High-stage events on the Scioto River cause frequent flow reversals in the aquifer that allow streamwater to travel a maximum observed distance of 190 feet inland. A zone of oxidizing waters (characterized by high dissolved oxygen concentration and Eh) is found in shallow ground water for several hundred feet adjacent to Big Beaver Creek and the Scioto River. This zone of oxidizing ground water is caused by the periodic inflow of surface waters to the aquifer. A ground-water budget for the study area indicates that the aquifer received 17.7 inches of recharge during water year 1992; of this amount, 72 percent originated as infiltrating precipitation, 28 percent as infiltration of surface water from Big Beaver Creek, and 0.2 percent as leakage from bedrock. Areal variation in water quality is caused by areal differences in the relative importance of these three recharge sources. The effects of bedrock leakage are evident only in the northeast corner of the study area. Here, deep outwash waters are transitional in composition between the calcium magnesium bicarbonate waters found elsewhere in the outwash aquifer and the calcium sodium chloride waters of the bedrock aquifer. Mixing calculations indicate that these deep outwash waters are composed of as much as 26 percent bedrock water. In the southern part of the MSEA, ground water is diluted by surface water from Big Beaver Creek as it recharges the aquifer through a sand and gravel streambed. At the northeast corner of the MSEA, however, Big Beaver Creek flows across a shale streambed through which no infiltration occurs. Redox reactions in the outwash aquifer control variations in aquifer chemistry with depth. From the water table to about 40 feet below land surface, oxidizing conditions are characterized by the presence of dissolved oxygen and nitrates in ground water, Eh greater than 200 millivolts, ferrihydrite coatings on sediment grains, and the absence of dissolved iron and manganese. From about 40 feet below land surface to the base of the aquifer, reducing conditions are characterized by dissolved oxygen concentrations less than 2 mg/L, Eh less than 200 millivolts, and the presence of dissolved iron and manganese. Denitrification in the reducing zone naturally remediates anthropogenic nitrate contamination of the aquifer while oxidizing pyrite in the aquifer sediment.&nbsp;</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wri954139","usgsCitation":"Jagucki, M.L., Finton, C.D., Springer, A.E., and Bair, E., 1995, Hydrogeology and water quality at the management systems evaluation area near Piketon, Ohio: U.S. Geological Survey Water-Resources Investigations Report 95-4139, vii, 117 p., https://doi.org/10.3133/wri954139.","productDescription":"vii, 117 p.","costCenters":[{"id":513,"text":"Ohio Water Science Center","active":true,"usgs":true},{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":411594,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_48239.htm","linkFileType":{"id":5,"text":"html"}},{"id":124878,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1995/4139/report-thumb.jpg"},{"id":54294,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1995/4139/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Ohio","city":"Piketon","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -83.02476524225692,\n              39.05708700203755\n            ],\n            [\n              -83.06035253063361,\n              39.05708700203755\n            ],\n            [\n              -83.06035253063361,\n              39.01848388151214\n            ],\n            [\n              -83.02476524225692,\n              39.01848388151214\n            ],\n            [\n              -83.02476524225692,\n              39.05708700203755\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a4ae4b07f02db6251e5","contributors":{"authors":[{"text":"Jagucki, Martha L. 0000-0003-3798-8393 mjagucki@usgs.gov","orcid":"https://orcid.org/0000-0003-3798-8393","contributorId":1794,"corporation":false,"usgs":true,"family":"Jagucki","given":"Martha","email":"mjagucki@usgs.gov","middleInitial":"L.","affiliations":[{"id":513,"text":"Ohio Water Science Center","active":true,"usgs":true}],"preferred":true,"id":777020,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Finton, Christopher D.","contributorId":97145,"corporation":false,"usgs":true,"family":"Finton","given":"Christopher","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":194257,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Springer, Abraham E.","contributorId":76278,"corporation":false,"usgs":true,"family":"Springer","given":"Abraham","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":194256,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Bair, E. Scott","contributorId":73231,"corporation":false,"usgs":true,"family":"Bair","given":"E. Scott","affiliations":[],"preferred":false,"id":194255,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":26022,"text":"wri944144 - 1995 - Hydrochemistry of aquifer systems and relation to regional flow patterns in Cretaceous and older rocks underlying Kansas, Nebraska, and parts of Arkansas, Colorado, Missouri, New Mexico, Oklahoma, South Dakota, Texas, and Wyoming","interactions":[],"lastModifiedDate":"2017-09-20T15:58:35","indexId":"wri944144","displayToPublicDate":"1996-07-01T00:00:00","publicationYear":"1995","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"94-4144","title":"Hydrochemistry of aquifer systems and relation to regional flow patterns in Cretaceous and older rocks underlying Kansas, Nebraska, and parts of Arkansas, Colorado, Missouri, New Mexico, Oklahoma, South Dakota, Texas, and Wyoming","docAbstract":"Aquifer systems in Cretaceous and older rocks of the Central Midwest are divided on the basis of hydrochemistry and ground-water flow patterns in the Plains subregion, the Western Interior Plains aquifer system contains sodium chloride type water with large concentrations of dissolved solids. Ion ratios suggest that the water was derived from seawater by concentration and by depletion of calcium and sulfate ions. In the overlying Western Interior Plains confining system, concentrations of depositional sea water and dissolution of extensive evaporite deposits have resulted in sodium chloride type water with large concentrations of dissolved solids and sodium. Overlying this confining system in the northwest part of the study area, the Great Plains aquifer system yields water that generally is less mineralized and more variable in water type than the underlying systems. Recharge of meteoric water, concentration of brackish water in which the rocks were deposited, and dissolution of underlying evaporite deposits have contributed to the observed water chemistry. The Great Plains confining system restricts the exchange of water between the underlying Great Plains aquifer system and the overlying unconfined aquifers. In the Ozark subregion, geological units equivalent to the Western Interior Plains aquifer system comprise the Ozark Plateaus aquifer system. Units of this aquifer system are exposed at the land surface, and fresh meteoric water moves rapidly through fractures and solution openings. Water chemistry in this system reflects primarily the dissolution of the predominately carbonate rocks.","language":"ENGLISH","publisher":"U.S. Geological Survey ;\r\nU.S. Geological Survey, Earth Science Information Center, Open-File Reports Section [distributor],","doi":"10.3133/wri944144","usgsCitation":"Baker, C.H., and Leonard, R., 1995, Hydrochemistry of aquifer systems and relation to regional flow patterns in Cretaceous and older rocks underlying Kansas, Nebraska, and parts of Arkansas, Colorado, Missouri, New Mexico, Oklahoma, South Dakota, Texas, and Wyoming: U.S. Geological Survey Water-Resources Investigations Report 94-4144, vi, 53 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri944144.","productDescription":"vi, 53 p. :ill., maps ;28 cm.","costCenters":[{"id":5050,"text":"WY-MT Water Science Center","active":true,"usgs":true}],"links":[{"id":123414,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1994/4144/report-thumb.jpg"},{"id":54800,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1994/4144/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afde4b07f02db696d20","contributors":{"authors":[{"text":"Baker, Claud H. Jr.","contributorId":53413,"corporation":false,"usgs":true,"family":"Baker","given":"Claud","suffix":"Jr.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":195658,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Leonard, Robert B.","contributorId":14407,"corporation":false,"usgs":true,"family":"Leonard","given":"Robert B.","affiliations":[],"preferred":false,"id":195657,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":23435,"text":"ofr95742 - 1995 - The strategy for improving water-quality monitoring in the United States; final report of the Intergovernmental Task Force on Monitoring Water Quality; technical appendices","interactions":[],"lastModifiedDate":"2012-02-02T00:08:10","indexId":"ofr95742","displayToPublicDate":"1996-07-01T00:00:00","publicationYear":"1995","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"95-742","title":"The strategy for improving water-quality monitoring in the United States; final report of the Intergovernmental Task Force on Monitoring Water Quality; technical appendices","docAbstract":"The Intergovernmental Task Force on Monitoring Water Quality (ITFM) prepared this report in collaboration with representatives of all levels of government and the private sector. The report recommends a strategy for nationwide water-quality monitoring and technical monitoring improvements to support sound water-quality decisionmaking. The strategy is intended to achieve a better return on public and private investments in monitoring, environmental protection, and natural resources management. It is also designed to expand the base of information useful to a variety of users at multiple geographic scales. Institutional and technical changes are needed to improve water-quality monitoring and to meet the full range of monitoring requirements. Monitoring must be incorporated as a critical element of program planning, implementation, and evaluation. The strategy includes recommendations in many key elements, such as the development of goal-oriented monitoring and indicators, institutional collaboration, and methods comparability. Initial actions have been taken to implement the strategy. Several Federal agencies have jointly purchased and shared remotely sensed land-cover information needed for water assessment. Major agency data systems are using common data-element names and reference tables that will ensure easy sharing of data. A number of States have held meetings with collectors of water information to initiate statewide monitoring strategies. New monitoring guidance has been developed for Federal water-quality grants to States. Many State offices have changed monitoring programs to place emphasis on priority watersheds and to improve assessment of water quality. As the competition increases for adequate supplies of clean water, concerns about public health and the environment escalate, and more demands are placed on the water information infrastructure. To meet these demands, the collaborative approach has already produced benefits, which will continue to grow as the recommendations are implemented","language":"ENGLISH","publisher":"U.S. Geological Survey, Office of Water Data Coordination,","doi":"10.3133/ofr95742","issn":"0094-9140","usgsCitation":"Intergovernmental Task Force on Monitoring Water Quality, 1995, The strategy for improving water-quality monitoring in the United States; final report of the Intergovernmental Task Force on Monitoring Water Quality; technical appendices: U.S. Geological Survey Open-File Report 95-742, iii, 146 p.  p. :ill., map ;28 cm. +Technical appendixes (iii, 117 p. : ill.), https://doi.org/10.3133/ofr95742.","productDescription":"iii, 146 p.  p. :ill., map ;28 cm. +Technical appendixes (iii, 117 p. : ill.)","costCenters":[],"links":[{"id":1765,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/ofr95742","linkFileType":{"id":5,"text":"html"}},{"id":156350,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1995/0742/report-thumb.jpg"},{"id":52757,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1995/0742/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b32e4b07f02db6b4947","contributors":{"authors":[{"text":"Intergovernmental Task Force on Monitoring Water Quality","contributorId":128116,"corporation":true,"usgs":false,"organization":"Intergovernmental Task Force on Monitoring Water Quality","id":529133,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":22028,"text":"ofr95831 - 1995 - Preliminary compilation of descriptive geoenvironmental mineral deposit models","interactions":[],"lastModifiedDate":"2019-12-07T11:12:19","indexId":"ofr95831","displayToPublicDate":"1996-07-01T00:00:00","publicationYear":"1995","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"95-831","title":"Preliminary compilation of descriptive geoenvironmental mineral deposit models","docAbstract":"Summary:  This book was released in paper form in June, 1996. After its release, it was converted to digital form as Adobe Acrobat (.pdf) files using Acrobat version 2.1. The Acrobat presentation you are accessing is a facsimile of the published book. A few minor editorial changes were made to the book to correct errors and some of the figures have been enhanced. The figures are the same as those in the book, but some have been reprocessed or redrafted and others converted from grayscale to color to make them more useable. In January 2004, the book was enhanced with the creation of a Navigation page, plus the addition of links, web links and bookmarks to improve ease of use.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr95831","issn":"0094-9140","usgsCitation":"du Bray, E.A., 1995, Preliminary compilation of descriptive geoenvironmental mineral deposit models: U.S. Geological Survey Open-File Report 95-831, ii, 272 p. , https://doi.org/10.3133/ofr95831.","productDescription":"ii, 272 p. ","costCenters":[{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":8083,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/1995/ofr-95-0831/","linkFileType":{"id":5,"text":"html"}},{"id":152994,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1995/0831/report-thumb.jpg"},{"id":51494,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1995/0831/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac9e4b07f02db67c727","contributors":{"authors":[{"text":"du Bray, Edward A. 0000-0002-4383-8394 edubray@usgs.gov","orcid":"https://orcid.org/0000-0002-4383-8394","contributorId":755,"corporation":false,"usgs":true,"family":"du Bray","given":"Edward","email":"edubray@usgs.gov","middleInitial":"A.","affiliations":[{"id":171,"text":"Central Mineral and Environmental Resources Science Center","active":true,"usgs":true},{"id":164,"text":"Central Energy Resources Science Center","active":true,"usgs":true}],"preferred":true,"id":186759,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":27185,"text":"wri954091 - 1995 - Geohydrology and simulation of ground-water flow near Los Alamos, north-central New Mexico","interactions":[],"lastModifiedDate":"2012-02-02T00:08:26","indexId":"wri954091","displayToPublicDate":"1996-07-01T00:00:00","publicationYear":"1995","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"95-4091","title":"Geohydrology and simulation of ground-water flow near Los Alamos, north-central New Mexico","docAbstract":"An existing model was modified in recognition of new \r\ngeohydrologic interpretations and adjusted to simulate \r\nhydrographs in well fields in the Los Alamos area. Hydraulic-head\r\ndrawdowns at the Buckman well field resulting from two projected\r\nground-water-withdrawal alternatives were estimated with the \r\nmodified model.\r\n\r\n     The Chaquehui formation (informal usage) is the main new \r\nfeature of recent hydrologic interpretations for the Los Alamos \r\narea. The Chaquehui occupies a 'channel' that was eroded or \r\nfaulted into the Tesuque Formation, and the Chaquehui is more \r\npermeable than the Tesuque. The Chaquehui is a major producing \r\nzone in the Pajarito Mesa well field and to a lesser extent in\r\nthe Guaje well field.\r\n\r\n     Model modification included splitting the four layers of the\r\nMcAda-Wasiolek model (McAda, D.P., and Wasiolek, Maryann, 1988, \r\nSimulation of the regional geohydrology of the Tesuque aquifer \r\nsystem near Santa Fe, New Mexico: U.S. Geological Survey Water-\r\nResources Investigations Report 87-4056, 71 p.) into eight layers\r\nto better simulate vertical ground-water movement. Other model \r\nmodifications were limited as much as possible to the area of \r\ninterest near Los Alamos and consisted mainly of adjusting \r\nhydraulic-conductivity values representing the Tesuque Formation,\r\nChaquehui formation (informal usage), and Puye Formation, and \r\nadjusting simulated recharge along the Pajarito Fault Zone west \r\nof Los Alamos. Adjustments were based mainly on simulation of \r\nfluctuations in measured hydraulic heads near Los Alamos.\r\n\r\n     Two possible alternative plans for replacing Guaje well field \r\nproduction were suggested by Los Alamos National Laboratory. In \r\nthe first plan (Guaje alternative), the Guaje field would be \r\nrenewed with four new wells replacing the existing production \r\nwells in the Guaje field. In the second plan (Pajarito-Otowi \r\nalternative), the Guaje well field would be retired and its\r\nformer production would be made up by additional withdrawals from the \r\nPajarito Mesa and Otowi well fields. A projection for each of \r\nthese alternatives was made through 2012 using the new eight-\r\nlayer model. In the Guaje field, projected hydraulic heads at the\r\nend of 2012 were as much as 50 feet lower with the Guaje \r\nalternative; in the Pajarito Mesa field, hydraulic heads were as\r\nmuch as 12 feet higher with the Guaje alternative. At the western\r\nend of the Los Alamos well field, projected hydraulic heads were\r\nabout 20 feet higher with the Guaje alternative; at the eastern \r\nend of the Los Alamos field, the difference between alternatives\r\nwas much less. At the Buckman field, projected hydraulic heads \r\nwere about 2 feet higher with the Guaje alternative because the \r\nBuckman field is closer to the Pajarito Mesa field than to the \r\nGuaje field. \r\n\r\n     Ways of improving the understanding of the flow system \r\ninclude developing a more accurate representation of the \r\nstructure and extent of the Tesuque Formation, Chaquehui \r\nformation, and Puye Formation of the Santa Fe Group and obtaining\r\nmore detailed geologic and hydrologic data for the Chaquehui and\r\nPuye. Data that describe water chemistry, hydraulic head, and \r\ndegree of saturation would be valuable for determining the \r\nlocation and quantity of recharge on the Pajarito Plateau, \r\nespecially along the west side of the Plateau and in canyon \r\nbottoms. Chloride concentrations in soil at the top of the \r\nBandelier Tuff could be used to verify the concept that \r\nevapotranspiration accounts for nearly all precipitation over a \r\nlarge area of the plateau.","language":"ENGLISH","publisher":"U.S. Geological Survey, [Water Resources Division, New Mexico District] ;\r\nCan be purchased from U.S. Geological Survey, Earth Science Information Center, Open-File Reports Section,","doi":"10.3133/wri954091","usgsCitation":"Frenzel, P.F., 1995, Geohydrology and simulation of ground-water flow near Los Alamos, north-central New Mexico: U.S. Geological Survey Water-Resources Investigations Report 95-4091, vi, 92 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri954091.","productDescription":"vi, 92 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":124047,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1995/4091/report-thumb.jpg"},{"id":56059,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1995/4091/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1be4b07f02db6a8c49","contributors":{"authors":[{"text":"Frenzel, P. F.","contributorId":98726,"corporation":false,"usgs":true,"family":"Frenzel","given":"P.","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":197706,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":31889,"text":"ofr95513 - 1995 - Geologic map of the Belt Supergroup in north-central Idaho and western Montana","interactions":[],"lastModifiedDate":"2012-02-02T00:09:04","indexId":"ofr95513","displayToPublicDate":"1996-07-01T00:00:00","publicationYear":"1995","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"95-513","title":"Geologic map of the Belt Supergroup in north-central Idaho and western Montana","language":"ENGLISH","doi":"10.3133/ofr95513","usgsCitation":"Lewis, R.S., 1995, Geologic map of the Belt Supergroup in north-central Idaho and western Montana: U.S. Geological Survey Open-File Report 95-513, 1 over-size sheet, scale 1:500,000 (1 inch = about 8 miles). , https://doi.org/10.3133/ofr95513.","productDescription":"1 over-size sheet, scale 1:500,000 (1 inch = about 8 miles). ","costCenters":[],"links":[{"id":160242,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":19551,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1995/0513/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"500000","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b0ee4b07f02db69fc98","contributors":{"authors":[{"text":"Lewis, Reed S. (compiler)","contributorId":68357,"corporation":false,"usgs":true,"family":"Lewis","given":"Reed","suffix":"(compiler)","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":207170,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":31907,"text":"ofr9575I - 1995 - Oil and gas resource assessment areas-1995-Lower 48 states","interactions":[],"lastModifiedDate":"2021-10-13T20:18:29.925122","indexId":"ofr9575I","displayToPublicDate":"1996-07-01T00:00:00","publicationYear":"1995","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"95-75","chapter":"I","title":"Oil and gas resource assessment areas-1995-Lower 48 states","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr9575I","usgsCitation":"Dolton, G., Varnes, K., Gautier, D.L., and Barnet, D.L., 1995, Oil and gas resource assessment areas-1995-Lower 48 states: U.S. Geological Survey Open-File Report 95-75, 1 Plate: 42.00 × 30.00 inches, https://doi.org/10.3133/ofr9575I.","productDescription":"1 Plate: 42.00 × 30.00 inches","costCenters":[],"links":[{"id":390495,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_18388.htm"},{"id":19558,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1995/0075i/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":161195,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"scale":"500000","country":"United States","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"geometry\": {\n        \"type\": \"MultiPolygon\",\n        \"coordinates\": [\n          [\n            [\n              [\n                -94.81758,\n                49.38905\n              ],\n              [\n                -94.64,\n                48.84\n              ],\n              [\n                -94.32914,\n      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,{"id":31888,"text":"ofr95482 - 1995 - Preliminary bedrock geologic map of the Saxtons River 7.5 x 15-minute quadrangle, Windham and Windsor Counties, Vermont","interactions":[{"subject":{"id":31888,"text":"ofr95482 - 1995 - Preliminary bedrock geologic map of the Saxtons River 7.5 x 15-minute quadrangle, Windham and Windsor Counties, Vermont","indexId":"ofr95482","publicationYear":"1995","noYear":false,"title":"Preliminary bedrock geologic map of the Saxtons River 7.5 x 15-minute quadrangle, Windham and Windsor Counties, Vermont"},"predicate":"SUPERSEDED_BY","object":{"id":69563,"text":"i2636 - 2001 - Bedrock geologic map of the Saxtons River 7.5' x 15' quadrangle, Windham and Windsor counties, Vermont","indexId":"i2636","publicationYear":"2001","noYear":false,"title":"Bedrock geologic map of the Saxtons River 7.5' x 15' quadrangle, Windham and Windsor counties, Vermont"},"id":1}],"supersededBy":{"id":69563,"text":"i2636 - 2001 - Bedrock geologic map of the Saxtons River 7.5' x 15' quadrangle, Windham and Windsor counties, Vermont","indexId":"i2636","publicationYear":"2001","noYear":false,"title":"Bedrock geologic map of the Saxtons River 7.5' x 15' quadrangle, Windham and Windsor counties, Vermont"},"lastModifiedDate":"2022-07-21T18:12:20.297758","indexId":"ofr95482","displayToPublicDate":"1996-07-01T00:00:00","publicationYear":"1995","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"95-482","title":"Preliminary bedrock geologic map of the Saxtons River 7.5 x 15-minute quadrangle, Windham and Windsor Counties, Vermont","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr95482","usgsCitation":"Ratcliffe, N.M., and Armstrong, T.R., 1995, Preliminary bedrock geologic map of the Saxtons River 7.5 x 15-minute quadrangle, Windham and Windsor Counties, Vermont (Superceded by map I-2636): U.S. Geological Survey Open-File Report 95-482, 29 p., https://doi.org/10.3133/ofr95482.","productDescription":"29 p.","costCenters":[],"links":[{"id":397789,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_18485.htm"},{"id":160257,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1995/0482/report-thumb.jpg"},{"id":60074,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1995/0482/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"24000","country":"United States","state":"Vermont","county":"Windham County, Windsor County","otherGeospatial":"Saxtons River 7.5 x 15-minute quadrangle","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -72.75,\n              43.25\n            ],\n            [\n              -72.5,\n              43.25\n            ],\n            [\n              -72.5,\n              43.125\n            ],\n            [\n              -72.75,\n              43.125\n            ],\n            [\n              -72.75,\n              43.25\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","edition":"Superceded by map I-2636","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac9e4b07f02db67c900","contributors":{"authors":[{"text":"Ratcliffe, N. M.","contributorId":80691,"corporation":false,"usgs":true,"family":"Ratcliffe","given":"N.","middleInitial":"M.","affiliations":[],"preferred":false,"id":207168,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Armstrong, T. R.","contributorId":91528,"corporation":false,"usgs":true,"family":"Armstrong","given":"T.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":207169,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":31887,"text":"ofr95481 - 1995 - Preliminary bedrock geologic map of the Chester quadrangle, Windsor County, Vermont","interactions":[{"subject":{"id":31887,"text":"ofr95481 - 1995 - Preliminary bedrock geologic map of the Chester quadrangle, Windsor County, Vermont","indexId":"ofr95481","publicationYear":"1995","noYear":false,"title":"Preliminary bedrock geologic map of the Chester quadrangle, Windsor County, Vermont"},"predicate":"SUPERSEDED_BY","object":{"id":66888,"text":"i2598 - 2000 - Bedrock geologic map of the Chester Quadrangle, Windsor County, Vermont","indexId":"i2598","publicationYear":"2000","noYear":false,"title":"Bedrock geologic map of the Chester Quadrangle, Windsor County, Vermont"},"id":1}],"supersededBy":{"id":66888,"text":"i2598 - 2000 - Bedrock geologic map of the Chester Quadrangle, Windsor County, Vermont","indexId":"i2598","publicationYear":"2000","noYear":false,"title":"Bedrock geologic map of the Chester Quadrangle, Windsor County, Vermont"},"lastModifiedDate":"2022-03-29T18:33:27.005148","indexId":"ofr95481","displayToPublicDate":"1996-07-01T00:00:00","publicationYear":"1995","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"95-481","title":"Preliminary bedrock geologic map of the Chester quadrangle, Windsor County, Vermont","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr95481","usgsCitation":"Ratcliffe, N., 1995, Preliminary bedrock geologic map of the Chester quadrangle, Windsor County, Vermont (Superceded by Map I-2598): U.S. Geological Survey Open-File Report 95-481, 19 p., https://doi.org/10.3133/ofr95481.","productDescription":"19 p.","costCenters":[],"links":[{"id":397788,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_18484.htm"},{"id":60073,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1995/0481/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":160256,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1995/0481/report-thumb.jpg"}],"scale":"24000","projection":"Transverse Mercator","country":"United States","state":"Vermont","county":"Windsor County","otherGeospatial":"Chester quadrangle","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -72.625,\n              43.25\n            ],\n            [\n              -72.5,\n              43.25\n            ],\n            [\n              -72.5,\n              43.375\n            ],\n            [\n              -72.625,\n              43.375\n            ],\n            [\n              -72.625,\n              43.25\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","edition":"Superceded by Map I-2598","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac9e4b07f02db67c98e","contributors":{"authors":[{"text":"Ratcliffe, Nicholas Morley","contributorId":83169,"corporation":false,"usgs":true,"family":"Ratcliffe","given":"Nicholas Morley","affiliations":[],"preferred":false,"id":207167,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":28757,"text":"wri944182 - 1995 - Geohydrology and water quality of stratified-drift aquifers in the Saco and Ossipee River basins, east-central New Hampshire","interactions":[],"lastModifiedDate":"2012-02-02T00:08:46","indexId":"wri944182","displayToPublicDate":"1996-06-01T00:00:00","publicationYear":"1995","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"94-4182","title":"Geohydrology and water quality of stratified-drift aquifers in the Saco and Ossipee River basins, east-central New Hampshire","docAbstract":"Stratified-drift aquifers discontinuously underlie 152.5 square miles of the Saco and Ossipee River Basins, which have a total drainage area of 869.4 square miles. Saturated thicknesses of stratified drift in the study area are locally greater than 280 feet, but generally are less. Transmissivity locally exceeds 8,000 feet squared per day but are generally less. About 93.6 square miles, or 10.8 percent of the study area, are identified as having transmissivity greater than 1,000 feet squared per day. The stratified-drift aquifer in Ossipee, Freedom, Effingham, Madison, and Tamworth was analyzed for the availability of ground water by use of transient simulations and a two-dimensional, finite-difference ground-water-flow model. The numerical -model results indicate that potential available water amounts in this aquifer are 7.72 million gallons per day. Sample results of water- quality analyses obtained from 25 test wells and 4 springs indicated that water was generally suitable for drinking and other domestic purposes. Concen- trations of dissolved constituents in ground-water samples are less than or meet U.S. Environmental Protection Agency (USEPA)primary and secondary drinking-water regulations. Concentrations of inorganic constituents that exceeded the USEPA's secondary regulations were chloride and sodium, iron manganese, and fluoride.","language":"ENGLISH","publisher":"U.S. Geological Survey ;\r\nEarth Science Information Center, Open-File Reports Section [distributor],","doi":"10.3133/wri944182","usgsCitation":"Moore, R.B., and Medalie, L., 1995, Geohydrology and water quality of stratified-drift aquifers in the Saco and Ossipee River basins, east-central New Hampshire: U.S. Geological Survey Water-Resources Investigations Report 94-4182, vi, 234 p. :ill., col. maps ;28 cm., https://doi.org/10.3133/wri944182.","productDescription":"vi, 234 p. :ill., col. maps ;28 cm.","costCenters":[],"links":[{"id":123665,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1994/4182/report-thumb.jpg"},{"id":57621,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1994/4182/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":57622,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1994/4182/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":57623,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1994/4182/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":57624,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1994/4182/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":57625,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1994/4182/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1be4b07f02db6a8ba0","contributors":{"authors":[{"text":"Moore, R. B.","contributorId":98720,"corporation":false,"usgs":true,"family":"Moore","given":"R.","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":200349,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Medalie, Laura 0000-0002-2440-2149 lmedalie@usgs.gov","orcid":"https://orcid.org/0000-0002-2440-2149","contributorId":3657,"corporation":false,"usgs":true,"family":"Medalie","given":"Laura","email":"lmedalie@usgs.gov","affiliations":[{"id":466,"text":"New England Water Science Center","active":true,"usgs":true}],"preferred":true,"id":200348,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":23794,"text":"ofr94521 - 1995 - Water-use data by category, county, and water management district in Florida, 1950-90","interactions":[],"lastModifiedDate":"2012-02-02T00:08:16","indexId":"ofr94521","displayToPublicDate":"1996-06-01T00:00:00","publicationYear":"1995","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"94-521","title":"Water-use data by category, county, and water management district in Florida, 1950-90","docAbstract":"The population for Florida in 1990 was estimated at 12.94 million, an increase of nearly 10.17 million (370 percent) from the population of 2.77 million in 1950. Consequently, water use (fresh and saline) in Florida increased nearly 510 percent (15,175 million gallons per day) between 1950 and 1990. The resident population of the State is projected to surpass 20 million by the year 2020. Through the cooperation of the Florida Department of Environ- mental Protection and the U.S. Geologial Survey, water-use data for the period between 1950 and 1990 has been consolidated into one publication. This report aggregates and summarizes the quantities of water withdrawn annually for all water-use categories (public supply, self-supplied domestic, self-supplied commercial-industrial, agriculture, and thermoelectric power generation), by counties, and water management districts in Florida from 1950 through 1990. Total water withdrawn in Florida increased from 2,923 million gallons per day in 1950 to 17,898 million gallons per day in 1990. Surface- water withdrawals during 1950 totaled 2,333 million gallons per day but were not differentiated between fresh and saline, therefore, comparisons between fresh and saline water were made beginning with 1955 data. Freshwater withdrawals increased 245 percent between 1955 and 1990. Saline water withdrawals increased more than 1,500 percent between 1955 and 1990. In 1955, more than 47 percent of the fresh- water used was withdrawn from ground-water sources and 53 percent was withdrawn from surface-water sources. In 1990, nearly 62 percent of the fresh- water withdrawn was from ground-water sources, while 38 percent was withdrawn from surface-water sources. The steady increase in ground-water withdrawals since the 1950's primarily is a result of the ability to drill and pump water more economically from large, deep wells and the reliability of both the quality and quantity of water from these wells. Water withdrawn for public supply in Florida increased 1,030 percent between 1950 and 1990. The population served by public supply increased from 1.66 million in 1950 to 11.23 million in 1990, and the percentage of the population served by public supply increased from 60 percent in 1950 to nearly 88 percent in 1990. Freshwater withdrawn for self- supplied domestic use in Florida increased 1,010 percent, self-supplied commercial-industrial uses increased 170 percent, and agriculture increased 915 percent between 1950 and 1990. Freshwater with- drawals for thermoelectric power generation decreased 8 percent between 1955 and 1990, while saline water withdrawals increased nearly 1,540 percent between 1955 and 1990. Between 1965 and 1990, total freshwater withdrawals increased in 58 of the 67 counties in Florida. Fresh ground-water was withdrawn in all 67 counties in 1965 through 1990, and increased in 65 counties between 1965 and 1990. Fresh surface-water was withdrawn in 60 counties from 1965 to 1990, and increased in 42 counties between 1965 and 1990. The change in total freshwater withdrawals within the water management districts between 1975 and 1990 were as follows: Northwest Florida Water Management District increased 3 percent, St. Johns River Water Management District decreased 6 percent, South Florida Water Management District increased 37 percent, Southwest Florida Water Management District decreased 1 percent, and Suwannee River Water Management District increased 8 percent.(USGS)","language":"ENGLISH","publisher":"U.S. Dept. of the Interior, U.S. Geological Survey ;\r\nEarth Science Information Center, Open-File Reports Section [distributor],","doi":"10.3133/ofr94521","issn":"0094-9140","usgsCitation":"Marella, R., 1995, Water-use data by category, county, and water management district in Florida, 1950-90: U.S. Geological Survey Open-File Report 94-521, x, 114 p. :ill., maps ;28 cm., https://doi.org/10.3133/ofr94521.","productDescription":"x, 114 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":156862,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1994/0521/report-thumb.jpg"},{"id":53016,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1994/0521/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac7e4b07f02db67ad8e","contributors":{"authors":[{"text":"Marella, R. L.","contributorId":34164,"corporation":false,"usgs":true,"family":"Marella","given":"R. L.","affiliations":[],"preferred":false,"id":190737,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":22435,"text":"ofr95460 - 1995 - Reference manual for data base on Nevada well logs","interactions":[],"lastModifiedDate":"2012-02-02T00:08:07","indexId":"ofr95460","displayToPublicDate":"1996-06-01T00:00:00","publicationYear":"1995","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"95-460","title":"Reference manual for data base on Nevada well logs","docAbstract":"The U.S. Geological Survey and Nevada Division of Water Resources are cooperatively using a data base for are cooperatively using a data base for managing well-log information for the State of Nevada. The Well-Log Data Base is part of an integrated system of computer data bases using the Ingres Relational Data-Base Management System, which allows efficient storage and access to water information from the State Engineer's office. The data base contains a main table, two ancillary tables, and nine lookup tables, as well as a menu-driven system for entering, updating, and reporting on the data. This reference guide outlines the general functions of the system and provides a brief description of data tables and data-entry screens.","language":"ENGLISH","publisher":"U.S. Geological Survey ;","doi":"10.3133/ofr95460","issn":"0094-9140","usgsCitation":"Bauer, E., and Cartier, K.D., 1995, Reference manual for data base on Nevada well logs: U.S. Geological Survey Open-File Report 95-460, iv, 29 p. :ill. ;28 cm., https://doi.org/10.3133/ofr95460.","productDescription":"iv, 29 p. :ill. ;28 cm.","costCenters":[],"links":[{"id":155627,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1995/0460/report-thumb.jpg"},{"id":51972,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1995/0460/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a60e4b07f02db635220","contributors":{"authors":[{"text":"Bauer, E.M.","contributorId":49816,"corporation":false,"usgs":true,"family":"Bauer","given":"E.M.","email":"","affiliations":[],"preferred":false,"id":188248,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Cartier, K. D.","contributorId":9236,"corporation":false,"usgs":true,"family":"Cartier","given":"K.","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":188247,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":54113,"text":"ofr95210_V2 - 1995 - National Earthquake Hazards Reduction Program, annual project summaries, XXXVI; Volume 2","interactions":[],"lastModifiedDate":"2012-02-02T00:11:38","indexId":"ofr95210_V2","displayToPublicDate":"1996-06-01T00:00:00","publicationYear":"1995","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"95-210","title":"National Earthquake Hazards Reduction Program, annual project summaries, XXXVI; Volume 2","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"National Earthquake Hazards Reduction Program, annual project summaries, XXXVI","largerWorkSubtype":{"id":5,"text":"USGS Numbered Series"},"language":"ENGLISH","publisher":"Geological Survey (U.S.)","doi":"10.3133/ofr95210_V2","issn":"0094-9140","usgsCitation":"Jacobson, M.L., 1995, National Earthquake Hazards Reduction Program, annual project summaries, XXXVI; Volume 2 (Volume 2): U.S. Geological Survey Open-File Report 95-210, Volume 2 - Total: 549 p.; Report: Pages 575-1101; Index: I1-I13, https://doi.org/10.3133/ofr95210_V2.","productDescription":"Volume 2 - Total: 549 p.; Report: Pages 575-1101; Index: I1-I13","costCenters":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"links":[{"id":178192,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1995/0210-v2/report-thumb.jpg"},{"id":87853,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1995/0210-v2/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"edition":"Volume 2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b01e4b07f02db698854","contributors":{"authors":[{"text":"Jacobson, Muriel L. (compiler)","contributorId":42965,"corporation":false,"usgs":true,"family":"Jacobson","given":"Muriel","suffix":"(compiler)","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":249232,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":22277,"text":"ofr95429 - 1995 - Water-quality, bed-sediment, and biological data (October 1993 through September 1994) and statistical summaries of data for streams in the Upper Clark Fork basin, Montana","interactions":[],"lastModifiedDate":"2012-02-02T00:08:02","indexId":"ofr95429","displayToPublicDate":"1996-06-01T00:00:00","publicationYear":"1995","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"95-429","title":"Water-quality, bed-sediment, and biological data (October 1993 through September 1994) and statistical summaries of data for streams in the Upper Clark Fork basin, Montana","docAbstract":"Water, bed sediment, and biota were sampled in streams from Butte to below Missoula as part of a program to characterize aquatic resources in the upper Clark Fork basin of western Montana. Water- quality data were obtained periodically at 16 stations during October 1993 through September 1994 (water year 1994); daily suspended-sediment data were obtained at six of these stations. Bed-sediment and biological data were obtained at 11 stations in August 1994. Sampling stations were located on the Clark Fork and major tributaries. The primary constituents analyzed were trace elements associated with mine tailings from historical mining and smelting activities. Water-quality data include concentrations of major ions, trace elements, and suspended sediment in samples collected periodically during water year 1994. Daily values of streamflow, suspended-sediment concentration, and suspended- sediment discharge are given for six stations. Bed- sediment data include trace-element concentrations in the fine and bulk fractions. Biological data include trace-element concentrations in whole-body tissue of aquatic benthic insects. Quality-assurance data are reported for analytical results of water, bed sediment, and biota. Statistical summaries of bed sediment, and biological data are provided for the period of record at each station since 1985.","language":"ENGLISH","publisher":"U.S. Geological Survey ;\r\nEarth Science Information Center, Open-File Reports Section [distributor],","doi":"10.3133/ofr95429","issn":"0094-9140","usgsCitation":"Lambing, J., Hornberger, M.I., Axtmann, E., and Dodge, K.A., 1995, Water-quality, bed-sediment, and biological data (October 1993 through September 1994) and statistical summaries of data for streams in the Upper Clark Fork basin, Montana: U.S. Geological Survey Open-File Report 95-429, iv, 104 p. :map ;28 cm., https://doi.org/10.3133/ofr95429.","productDescription":"iv, 104 p. :map ;28 cm.","costCenters":[],"links":[{"id":155793,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1995/0429/report-thumb.jpg"},{"id":51699,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1995/0429/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e48cbe4b07f02db54397d","contributors":{"authors":[{"text":"Lambing, J. H.","contributorId":100860,"corporation":false,"usgs":true,"family":"Lambing","given":"J. H.","affiliations":[],"preferred":false,"id":187911,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hornberger, Michelle I. 0000-0002-7787-3446","orcid":"https://orcid.org/0000-0002-7787-3446","contributorId":23574,"corporation":false,"usgs":true,"family":"Hornberger","given":"Michelle","email":"","middleInitial":"I.","affiliations":[],"preferred":false,"id":187908,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Axtmann, E.V.","contributorId":30652,"corporation":false,"usgs":true,"family":"Axtmann","given":"E.V.","email":"","affiliations":[],"preferred":false,"id":187909,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Dodge, K. A.","contributorId":40615,"corporation":false,"usgs":true,"family":"Dodge","given":"K.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":187910,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":25750,"text":"wri944174 - 1995 - Relation of nitrate concentrations in ground water to well depth, well use, and land use in Franklin Township, Gloucester County, New Jersey, 1970-85","interactions":[],"lastModifiedDate":"2022-10-04T21:27:53.31422","indexId":"wri944174","displayToPublicDate":"1996-06-01T00:00:00","publicationYear":"1995","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"94-4174","title":"Relation of nitrate concentrations in ground water to well depth, well use, and land use in Franklin Township, Gloucester County, New Jersey, 1970-85","docAbstract":"A water-quality data base was developed to permit the investigation of the relation of concentrations of nitrate (as nitrogen) in ground water to well depth, well use, and land use (agricultural, residential, urban nonresidential, and undeveloped) in Franklin Township. Nitrate concentrations in water from 868 wells tended to decrease with depth. A rank-order regression model of nitrate concen- trations and land-use percentages was fitted to data from 98 shallow domestic wells. The model, which explains about 25 percent of the variance in the data, indicated that nitrate concentration increased with the percentage of developed land in a well's buffer zone. Further stratification of the data based on well use (commercial, domestic, or agricultural/irrigation) indicated that elevated nitrate concentrations were more common in water from agricultural/irrigation wells than in water from domestic or commercial wells. Concentrations of nitrate were indicative of human activities in water from about one-third of the wells sampled but exceeded the U.S. Environmental Protection Agency's maximum contaminant level of 10 milligrams per liter in water from only 1 percent of the wells. A sampling strategy in which water from wells of different depths located within areas in each of the four land-use categories is sampled yearly and analyzed for nitrate and other constituents would facilitate determination of the effects of human activities on ground-water quality.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri944174","usgsCitation":"MacLeod, C.L., Barringer, T.H., Vowinkel, E., and Price, C.V., 1995, Relation of nitrate concentrations in ground water to well depth, well use, and land use in Franklin Township, Gloucester County, New Jersey, 1970-85: U.S. Geological Survey Water-Resources Investigations Report 94-4174, v, 29 p., https://doi.org/10.3133/wri944174.","productDescription":"v, 29 p.","costCenters":[],"links":[{"id":54512,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1994/4174/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":156191,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1994/4174/report-thumb.jpg"},{"id":407920,"rank":2,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_48049.htm","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"New Jersey","county":"Gloucester County","otherGeospatial":"Franklin Township","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -75.1833,\n              39.5333\n            ],\n            [\n              -74.75,\n              39.5333\n            ],\n            [\n              -74.75,\n              39.6611\n            ],\n            [\n              -75.1833,\n              39.6611\n            ],\n            [\n              -75.1833,\n              39.5333\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e499ee4b07f02db5bcbe4","contributors":{"authors":[{"text":"MacLeod, Cecilia Louise","contributorId":22799,"corporation":false,"usgs":true,"family":"MacLeod","given":"Cecilia","email":"","middleInitial":"Louise","affiliations":[],"preferred":false,"id":194917,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Barringer, T. H.","contributorId":29468,"corporation":false,"usgs":true,"family":"Barringer","given":"T.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":194918,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Vowinkel, E. F.","contributorId":90737,"corporation":false,"usgs":true,"family":"Vowinkel","given":"E. F.","affiliations":[],"preferred":false,"id":194919,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Price, C. V.","contributorId":19190,"corporation":false,"usgs":true,"family":"Price","given":"C.","email":"","middleInitial":"V.","affiliations":[],"preferred":false,"id":194916,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":29711,"text":"wri954032 - 1995 - Water use in Kentucky, 1990","interactions":[],"lastModifiedDate":"2012-02-02T00:08:56","indexId":"wri954032","displayToPublicDate":"1996-06-01T00:00:00","publicationYear":"1995","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"95-4032","title":"Water use in Kentucky, 1990","docAbstract":"Water-use information for 1990 was collected and reported, by county, for eight major categories of use. Seven of the categories were offstream uses, which included public supply, commercial, domestic, industrial, mining, thermoelectric, and agricultural uses. The agricultural category was subdivided into irrigation and livestock water use. Instream water- use data also were collected for hydroelectric-power generation. Estimated average water use in Kentucky exceeded 4,300 million gallons per day during 1990 for all offstream uses. About 94 percent of this amount was from surface-water sources, and about 6 percent was from ground-water sources. Per capita use for all offstream uses was almost 1,200 gallons per day. Estimated average consumptive use was 309 million gallons per day. Estimated average instream water use for hydroelectric-power generation was 83,000 million gallons per day. Ninety-seven percent of the offstream water withdrawals during 1990 were withdrawn for thermoelectric, public supply, and industrial use. Cooling water used in the production of thermoelectric power accounted for about 80 percent of the total offstream water use during 1990. Water withdrawn for public supplies was second largest at almost 10 percent of the total, and industrial water withdrawals were about 7 percent of the total. Thermoelectric, domestic, and livestock uses accounted for almost 90 percent of the consumptive use during 1990. The thermoelectric category accounted for almost two-thirds of the total consumptive use in the State for all uses.","language":"ENGLISH","publisher":"U.S. Dept. of the Interior, U.S. Geological Survey ;\r\nEarth Science Information Center, Open-File Reports Section [distributor],","doi":"10.3133/wri954032","usgsCitation":"Sholar, C., and Wood, P., 1995, Water use in Kentucky, 1990: U.S. Geological Survey Water-Resources Investigations Report 95-4032, iv, 51 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri954032.","productDescription":"iv, 51 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":123864,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1995/4032/report-thumb.jpg"},{"id":58529,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1995/4032/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f4e4b07f02db5f006a","contributors":{"authors":[{"text":"Sholar, C.J.","contributorId":44186,"corporation":false,"usgs":true,"family":"Sholar","given":"C.J.","affiliations":[],"preferred":false,"id":201990,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Wood, P.A.","contributorId":106540,"corporation":false,"usgs":true,"family":"Wood","given":"P.A.","email":"","affiliations":[],"preferred":false,"id":201991,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":5066,"text":"fs10795 - 1995 - Selected herbicides in major streams in the Potomic River Basin upstream from Washington, D.C.","interactions":[],"lastModifiedDate":"2012-02-02T00:05:51","indexId":"fs10795","displayToPublicDate":"1996-06-01T00:00:00","publicationYear":"1995","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":313,"text":"Fact Sheet","code":"FS","onlineIssn":"2327-6932","printIssn":"2327-6916","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"107-95","title":"Selected herbicides in major streams in the Potomic River Basin upstream from Washington, D.C.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/fs10795","usgsCitation":"Fisher, G.T., 1995, Selected herbicides in major streams in the Potomic River Basin upstream from Washington, D.C.: U.S. Geological Survey Fact Sheet 107-95, 4 p. : maps (some col.) ; 28 cm. maps (some col.), https://doi.org/10.3133/fs10795.","productDescription":"4 p. : maps (some col.) ; 28 cm. maps (some col.)","costCenters":[],"links":[{"id":398,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://ca.water.usgs.gov/pnsp/rep/fs95107/","linkFileType":{"id":5,"text":"html"}},{"id":121631,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/fs/1995/0107/report-thumb.jpg"},{"id":31873,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/fs/1995/0107/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a07e4b07f02db5f9507","contributors":{"authors":[{"text":"Fisher, Gary T. gtfisher@usgs.gov","contributorId":4931,"corporation":false,"usgs":true,"family":"Fisher","given":"Gary","email":"gtfisher@usgs.gov","middleInitial":"T.","affiliations":[],"preferred":true,"id":150362,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":27150,"text":"wri954135 - 1995 - Characteristics, transport, and yield of sediment in Juday Creek, St. Joseph County, Indiana, 1993-94","interactions":[],"lastModifiedDate":"2016-05-16T13:06:53","indexId":"wri954135","displayToPublicDate":"1996-06-01T00:00:00","publicationYear":"1995","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"95-4135","title":"Characteristics, transport, and yield of sediment in Juday Creek, St. Joseph County, Indiana, 1993-94","docAbstract":"<p>Juday Creek is a tributary of the St. Joseph River in St. Joseph County, north-central Indiana. The creek has been identified as one of the few streams in the State that can support a naturally reproducing brown trout population. A recent study of benthic invertebrates shows a decline in the production rate of insect species and suggests that this decline may be caused by increased sedimen- tation. This report presents the results of a study of the sediment conditions in Juday Creek from April 1993 through June 1994. Measurements of streamflow, suspended sediment, and bedload were made at six sampling sites during three storms and a period of low flow. A total of 11 samples were collected during storms, and 1 sample was collected during low flow at each site. Bed-material samples were collected at the six sites. Sediment cores were collected from the delta of an instream pond and at a sediment trap near the mouth of the stream. Scour and fill at the six sites were monitored by means of scour chains and surveyed cross sections. The instream pond was surveyed twice, and the volume weight of the sediment was determined to estimate the yield of sediment for the upper reach of Juday Creek.</p>\n<p>Particle-size distributions indicate that the bed material is predominantly sand and gravel and that very little of the bed material is silt or finer (less than 0.062 millimeter). Analysis of sediment cores showed that most of the sediment deposited in the sediment trap and instream pond was sand.</p>\n<p>Sediment sampling during a period of low flow detected only minimal concentrations of suspended sediment; the maximum concentration was 6 milligrams per liter, equivalent to a daily load of 0.32 ton. Bedload ranged from 5.2 to 76.7 grams per cross- channel sampling, equivalent to 0.11 to 1.70 tons per day.</p>\n<p>Sediment sampling during the storms indicates that bedload discharge is the primary mode of sediment transport. Suspended-sediment concentration ranged from 4 to 67 milligrams per liter; the median was 17 milligrams per liter. Bedload ranged from 3.4 to 862 grams per cross- channel sampling; the median was 109 grams. Only 15 percent of the samples were less than 50 grams.</p>\n<p>Scour chains and surveyed cross sections documented some scour and fill at most of the sites.Scour and fill tended to balance out; after a 1-year period, the net change in the streambed altitude was minimal. Some infilling was the net result at most of the sites.</p>\n<p>Surveys of the instream pond determined that the volume of sediment delivered to the pond from April 1993 to April 1994 was approximately 26,500 cubic feet. The average volume weight of the sediment was determined to be 102 pounds per cubic foot. The sediment yield for the upper reach of Juday Creek from April 1993 to April 1994 was estimated to be 48 tons per square mile.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Indianapolis, IN","doi":"10.3133/wri954135","collaboration":"Prepared in cooperation with the Indiana Department of Natural Resources, Division of Water, and the St. Joseph County Drainage Board","usgsCitation":"Fowler, K.K., and Wilson, J., 1995, Characteristics, transport, and yield of sediment in Juday Creek, St. Joseph County, Indiana, 1993-94: U.S. Geological Survey Water-Resources Investigations Report 95-4135, v, 47 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri954135.","productDescription":"v, 47 p. :ill., maps ;28 cm.","startPage":"1","endPage":"47","numberOfPages":"52","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":346,"text":"Indiana Water Science Center","active":true,"usgs":true}],"links":[{"id":123954,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1995/4135/report-thumb.jpg"},{"id":56031,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1995/4135/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Indiana","county":"Saint Joseph","otherGeospatial":"Juday Creek","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {\n        \"stroke\": \"#555555\",\n        \"stroke-width\": 2,\n        \"stroke-opacity\": 1,\n        \"fill\": \"#555555\",\n        \"fill-opacity\": 0.5\n      },\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -86.19426727294922,\n              41.668808555620586\n            ],\n            [\n              -86.29262924194336,\n              41.66906501728199\n            ],\n            [\n              -86.29262924194336,\n              41.73225164878485\n            ],\n            [\n              -86.10071182250977,\n              41.73276406529474\n            ],\n            [\n              -86.09933853149414,\n              41.67034731026393\n            ],\n            [\n              -86.19426727294922,\n              41.668808555620586\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e2e4b07f02db5e4ea6","contributors":{"authors":[{"text":"Fowler, K. K. 0000-0002-0107-3848","orcid":"https://orcid.org/0000-0002-0107-3848","contributorId":40633,"corporation":false,"usgs":true,"family":"Fowler","given":"K.","middleInitial":"K.","affiliations":[],"preferred":false,"id":197642,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Wilson, J.T.","contributorId":97489,"corporation":false,"usgs":true,"family":"Wilson","given":"J.T.","affiliations":[],"preferred":false,"id":197643,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":23949,"text":"ofr95358 - 1995 - Estimated water use in Puerto Rico, 1986-87","interactions":[],"lastModifiedDate":"2012-02-02T00:08:00","indexId":"ofr95358","displayToPublicDate":"1996-06-01T00:00:00","publicationYear":"1995","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"95-358","title":"Estimated water use in Puerto Rico, 1986-87","language":"ENGLISH","publisher":"U.S. Geological Survey ;\r\nU.S. Geological Survey, Earth Science Information Center, Open-File Reports Section [distributor],","doi":"10.3133/ofr95358","issn":"0094-9140","usgsCitation":"Molina-Rivera, W., and Dopazo, T., 1995, Estimated water use in Puerto Rico, 1986-87: U.S. Geological Survey Open-File Report 95-358, v, 31 p. :ill., maps ;28 cm., https://doi.org/10.3133/ofr95358.","productDescription":"v, 31 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":154949,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1995/0358/report-thumb.jpg"},{"id":53148,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1995/0358/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0ce4b07f02db5fcc1e","contributors":{"authors":[{"text":"Molina-Rivera, W. L.","contributorId":84790,"corporation":false,"usgs":true,"family":"Molina-Rivera","given":"W. L.","affiliations":[],"preferred":false,"id":191029,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Dopazo, Teresa","contributorId":42246,"corporation":false,"usgs":true,"family":"Dopazo","given":"Teresa","affiliations":[],"preferred":false,"id":191028,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":21715,"text":"ofr95469 - 1995 - Data on selected herbicides and two triazine metabolites in precipitation of the Midwestern and Northeastern United States, 1990-91","interactions":[],"lastModifiedDate":"2019-12-07T10:40:44","indexId":"ofr95469","displayToPublicDate":"1996-06-01T00:00:00","publicationYear":"1995","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"95-469","title":"Data on selected herbicides and two triazine metabolites in precipitation of the Midwestern and Northeastern United States, 1990-91","docAbstract":"Weekly precipitation (rain and snow) samples were collected from 81 National Atmospheric Deposition Program/National Trends Network sites in the Midwestern and Northeastern United States for the analysis of herbicides. In addition, five high- elevation background sites along the Rocky Mountains and in Alaska were sampled to provide data on herbicides in precipitation at sites far from the study area. The study began in March 1990 and continued through September 1991. The precipitation samples were shipped to the Central Analytical Laboratory operated by the Illinois State Water Survey for analyses of inorganic compounds. Subsamples of the precipitation were shipped to the U.S. Geological Survey laboratory in Lawrence, Kansas, for the analysis of 11 herbicides and 2 triazines metabolites. This report provides descriptions of the study area, sample-collection methods, laboratory methods, and quality assurance. The report also includes a compilation of herbicide concentration data from both enzyme-linked immunosorbent assay and gas chromatography/mass spectrometry methods. Laboratory analyses consisted of 6,230 samples that were analyzed by enzyme-linked immunosorbent assay using alachlor and atrazine microtiter plates and 2,341 samples that were confirmed by gas chromatography/mass spectrometry analysis. Graphical and statistical comparisons of the two analytical methods are given in this report. Data from this study have been useful in determining the spatial and temporal distribution of herbicide concentrations and deposition in precipitation of over a 26-State area of the Midwestern and Northeastern United States. The data also provide evidence of long-range atmospheric transport of herbicides and triazine metabolites.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr95469","issn":"0566-8174","usgsCitation":"Goolsby, D.A., Scribner, E., Thurman, E., Pomes, M., and Meyer, M.T., 1995, Data on selected herbicides and two triazine metabolites in precipitation of the Midwestern and Northeastern United States, 1990-91: U.S. Geological Survey Open-File Report 95-469, iv, 341 p., https://doi.org/10.3133/ofr95469.","productDescription":"iv, 341 p.","costCenters":[{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":154557,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1995/0469/report-thumb.jpg"},{"id":51242,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1995/0469/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -104.150390625,\n              48.80686346108517\n            ],\n            [\n              -101.865234375,\n              36.527294814546245\n            ],\n            [\n              -81.298828125,\n              35.02999636902566\n            ],\n            [\n              -67.587890625,\n              45.213003555993964\n            ],\n            [\n              -68.64257812499999,\n              47.39834920035926\n            ],\n            [\n              -82.353515625,\n              41.96765920367816\n            ],\n            [\n              -83.49609375,\n              46.13417004624326\n            ],\n            [\n              -88.330078125,\n              48.3416461723746\n            ],\n            [\n              -104.150390625,\n              48.80686346108517\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac8e4b07f02db67bdbc","contributors":{"authors":[{"text":"Goolsby, D. A.","contributorId":50508,"corporation":false,"usgs":true,"family":"Goolsby","given":"D.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":185386,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Scribner, E.A.","contributorId":50925,"corporation":false,"usgs":true,"family":"Scribner","given":"E.A.","email":"","affiliations":[],"preferred":false,"id":185387,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Thurman, E.M.","contributorId":102864,"corporation":false,"usgs":true,"family":"Thurman","given":"E.M.","affiliations":[],"preferred":false,"id":185390,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Pomes, M.L.","contributorId":84393,"corporation":false,"usgs":true,"family":"Pomes","given":"M.L.","affiliations":[],"preferred":false,"id":185388,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Meyer, M. T.","contributorId":92279,"corporation":false,"usgs":true,"family":"Meyer","given":"M.","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":185389,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
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