{"pageNumber":"1654","pageRowStart":"41325","pageSize":"25","recordCount":68937,"records":[{"id":19787,"text":"ofr94353 - 1994 - Hydrologic Instrumentation Facility of the U.S. Geological Survey, annual report for fiscal year 1993","interactions":[],"lastModifiedDate":"2012-02-02T00:07:35","indexId":"ofr94353","displayToPublicDate":"1995-01-10T00:00:00","publicationYear":"1994","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"94-353","title":"Hydrologic Instrumentation Facility of the U.S. Geological Survey, annual report for fiscal year 1993","docAbstract":"The Hydrologic lnstrumentation Facility (HIF) of the U.S. Geological Survey (USGS) has nationwide responsibility for all aspects of hydrologic field instrumentation in support of Survey data-collection programs. Each year the HIF publishes a report to inform Water Resources Division (WRD) personnel of progress made by the HIF in fulfilling its mission to improve instrumentation services to the Division. The report for fiscal year 1993 (FY93) describes the activities of the HIF, including major accomplish- ments for the year; personnel actions; active projects (reported by section--Technical Services Section, Administrative Services Section, Field Coordination, Applications and Development Section, Test and Evaluation Section, Field Service and Supply Section); and planned activities for the coming year. Also presented in the appendixes are detailed listings of the memberships of the Instrumentation Committee and the Instrumentation Technical Advisory Subcommittee; district, sub- district, and field office visits by HIF personnel; professional and technical meetings attended by HIF personnel; vendor visits; and reports prepared by HIF personnel.","language":"ENGLISH","publisher":"U.S. Geological Survey :\r\nEarth Science Information Center, Open-File Reports Section [distributor],","doi":"10.3133/ofr94353","usgsCitation":"Latkovich, V., and Tracey, D.C., 1994, Hydrologic Instrumentation Facility of the U.S. Geological Survey, annual report for fiscal year 1993: U.S. Geological Survey Open-File Report 94-353, iv, 47 p. :ill. ;28 cm., https://doi.org/10.3133/ofr94353.","productDescription":"iv, 47 p. :ill. ;28 cm.","costCenters":[],"links":[{"id":152538,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1994/0353/report-thumb.jpg"},{"id":49263,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1994/0353/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a2de4b07f02db6145cd","contributors":{"authors":[{"text":"Latkovich, V.J.","contributorId":52576,"corporation":false,"usgs":true,"family":"Latkovich","given":"V.J.","email":"","affiliations":[],"preferred":false,"id":181510,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Tracey, Debra C.","contributorId":89157,"corporation":false,"usgs":true,"family":"Tracey","given":"Debra","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":181511,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":21440,"text":"ofr94320 - 1994 - Water levels through 1989 in bedrock aquifers in South Dakota","interactions":[],"lastModifiedDate":"2012-02-02T00:07:53","indexId":"ofr94320","displayToPublicDate":"1995-01-10T00:00:00","publicationYear":"1994","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"94-320","title":"Water levels through 1989 in bedrock aquifers in South Dakota","docAbstract":"The U.S. Geological Survey, in cooperation with the South Dakota Department of Environmental and Natural Resources, has collected water-level data for 237 wells completed in bedrock aquifers throughout South Dakota. The water levels are presented in hydrographs in the main body of the report and in tables in a Supplemental Information section at the end of the report. The data are organized by county, in alphabetical order.","language":"ENGLISH","publisher":"U.S. Geological Survey ;\r\nUSGS Earth Science Information Center, Open-File Reports Section [distributor],","doi":"10.3133/ofr94320","usgsCitation":"Winter, D.R., 1994, Water levels through 1989 in bedrock aquifers in South Dakota: U.S. Geological Survey Open-File Report 94-320, iv, 279 p. :ill., map ;28 cm., https://doi.org/10.3133/ofr94320.","productDescription":"iv, 279 p. :ill., map ;28 cm.","costCenters":[],"links":[{"id":154764,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1994/0320/report-thumb.jpg"},{"id":51008,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1994/0320/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a49e4b07f02db62403e","contributors":{"authors":[{"text":"Winter, Douglas R.","contributorId":28603,"corporation":false,"usgs":true,"family":"Winter","given":"Douglas","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":184432,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":18015,"text":"ofr93141 - 1994 - U.S. Geological Survey ground-water studies in Illinois","interactions":[],"lastModifiedDate":"2012-02-02T00:07:26","indexId":"ofr93141","displayToPublicDate":"1995-01-10T00:00:00","publicationYear":"1994","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"93-141","title":"U.S. Geological Survey ground-water studies in Illinois","docAbstract":"Ground water is an important source of water supply in Illinois. The largest amount of ground*water withdrawal is in the northern one-third of the State where aquifers to a depth of about 1,500 feet below land surface contain large quantities of potable water. Approximately 74 percent of the public water-supply systems in Illinois use ground water to supply potable water to more than 5.5 million people. Ground-water withdrawals account for almost 25 percent of the total water withdrawn for public water supplies in Illinois. Many public water-supply systems in the Chicago area have recently changed from using ground water pumped from wells to using water delivered from Lake Michigan. The major issues related to ground water in Illinois are: Water- quality degradation or contamination from point and nonpoint sources, and Water availability, because of the lowering of ground-water levels in the bedrock aquifers in northeastern Illinois and elsewhere in the State where pumpage has exceeded aquifer recharge and the susceptibility of the limited surface-water supplies in central and southern Illinois to drought.","language":"ENGLISH","publisher":"U.S. Geological Survey, U.S. Dept. of the Interior,","doi":"10.3133/ofr93141","usgsCitation":"Avery, C.F., 1994, U.S. Geological Survey ground-water studies in Illinois: U.S. Geological Survey Open-File Report 93-141, 2 p. :map ;28 cm., https://doi.org/10.3133/ofr93141.","productDescription":"2 p. :map ;28 cm.","costCenters":[],"links":[{"id":150686,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1993/0141/report-thumb.jpg"},{"id":21459,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1993/0141/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a2ae4b07f02db6129c9","contributors":{"authors":[{"text":"Avery, Charles F.","contributorId":28961,"corporation":false,"usgs":true,"family":"Avery","given":"Charles","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":178379,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":20508,"text":"ofr94364 - 1994 - Annual yield and selected hydrologic data for the Arkansas River Basin Compact Arkansas-Oklahoma 1993 water year","interactions":[],"lastModifiedDate":"2012-02-02T00:07:35","indexId":"ofr94364","displayToPublicDate":"1995-01-10T00:00:00","publicationYear":"1994","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"94-364","title":"Annual yield and selected hydrologic data for the Arkansas River Basin Compact Arkansas-Oklahoma 1993 water year","docAbstract":"The computed annual yield and deficiency of the subbasins as defined in the Arkansas River Basin Compact, Arkansas-Oklahoma, are given in tables for the 1993 water year. Actual runoff from the subbasins and depletion caused by major reservoirs in the compact area also are given in tabular form. Monthly maximum, minimum, and mean discharges are shown for the 14 streamflow stations used in computing annual yield. Water-quality data are shown for 12 water-quality stations sampled in the Arkansas River Basin.","language":"ENGLISH","publisher":"U.S. Geological Survey ;\r\nUSGS Earth Science Information Center, Open-File Reports Section [distributor],","doi":"10.3133/ofr94364","usgsCitation":"Porter, J., and Barks, C.S., 1994, Annual yield and selected hydrologic data for the Arkansas River Basin Compact Arkansas-Oklahoma 1993 water year: U.S. Geological Survey Open-File Report 94-364, iii, 61 p. :map ;28 cm., https://doi.org/10.3133/ofr94364.","productDescription":"iii, 61 p. :map ;28 cm.","costCenters":[],"links":[{"id":152673,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1994/0364/report-thumb.jpg"},{"id":50044,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1994/0364/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac8e4b07f02db67b777","contributors":{"authors":[{"text":"Porter, J.E.","contributorId":51779,"corporation":false,"usgs":true,"family":"Porter","given":"J.E.","email":"","affiliations":[],"preferred":false,"id":182773,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Barks, C. Shane csbarks@usgs.gov","contributorId":2088,"corporation":false,"usgs":true,"family":"Barks","given":"C.","email":"csbarks@usgs.gov","middleInitial":"Shane","affiliations":[],"preferred":true,"id":182772,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":20679,"text":"ofr93466 - 1994 - Geologic and hydrologic data collected at test hole NC-8, Vega Alta, Puerto Rico","interactions":[],"lastModifiedDate":"2012-02-02T00:07:46","indexId":"ofr93466","displayToPublicDate":"1995-01-10T00:00:00","publicationYear":"1994","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"93-466","title":"Geologic and hydrologic data collected at test hole NC-8, Vega Alta, Puerto Rico","docAbstract":"Test hole NC-8 was drilled in the municipality of Vega Alta as part of a study of the aquifers in the Northern Coastal Province of Puerto Rico. Test hole NC-8 was drilled to a depth of 1,736 feet below land surface. Geologic and hydrologic data collected during drilling included continuous core, water- quality samples, water-level measurements, and estimates of aquifer yields from the water-bearing zones. Test hole NC-8 penetrated five geologic formations of middle Tertiary age: the Aymamon Limestone, the Los Puertos Formation, the Cibao Formation, the Lares Limestone, and the San Sebastian Formation. Test hole NC-8 penetrated a water-table aquifer and seven artesian aquifers.","language":"ENGLISH","publisher":"U.S. Geological Survey ;\r\nUSGS Earth Science Information Center, Open-File Reports Section [distributor],","doi":"10.3133/ofr93466","usgsCitation":"Rodríguez-Martínez, J., and Scharlach, R.A., 1994, Geologic and hydrologic data collected at test hole NC-8, Vega Alta, Puerto Rico: U.S. Geological Survey Open-File Report 93-466, iv, 16 p. :ill., maps ;28 cm., https://doi.org/10.3133/ofr93466.","productDescription":"iv, 16 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":154012,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1993/0466/report-thumb.jpg"},{"id":50203,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1993/0466/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1ae4b07f02db6a8213","contributors":{"authors":[{"text":"Rodríguez-Martínez, Jesús","contributorId":48149,"corporation":false,"usgs":true,"family":"Rodríguez-Martínez","given":"Jesús","affiliations":[],"preferred":false,"id":183051,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Scharlach, Richard A.","contributorId":59475,"corporation":false,"usgs":true,"family":"Scharlach","given":"Richard","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":183052,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":20682,"text":"ofr93465 - 1994 - Geologic and hydrologic data collected at test holes NC-6 and NC-11, Hatillo and Isabela, northwestern Puerto Rico","interactions":[],"lastModifiedDate":"2012-02-02T00:07:46","indexId":"ofr93465","displayToPublicDate":"1995-01-10T00:00:00","publicationYear":"1994","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"93-465","title":"Geologic and hydrologic data collected at test holes NC-6 and NC-11, Hatillo and Isabela, northwestern Puerto Rico","docAbstract":"Test holes NC-6 and NC-11 were drilled in the municipalities of Hatillo and Isabela, respectively, as part of a study of the aquifers in the Northern Coastal Province of Puerto Rico. Test holes NC-6 and NC-11 were drilled to depths of 2,574 and 2,120 feet below land surface, respectively. Geologic and hydrologic data collected during drilling included continuous core, water-quality samples, water-level measurements, and estimates of aquifer yields from the water-bearing zones. Test hole NC-6 penetrated five formations ranging in age from late Oligocene to early Pliocene: the Lares Limestone, the Cibao Formation, the Los Puertos Formation, the Aymamon Limestone, and the Quebradillas Limestone. This test hole also penetrated a water-table aquifer and six artesian aquifer. Test hole NC-11 penetrated four formations ranging in age from late 01igocene to middle Miocene: the San Sebastian Formation, the Cibao Formation, the Los Puertos, and the Aymamon Limestone. A water-table aquifer and four artesian aquifers were penetrated by this well.","language":"ENGLISH","publisher":"U.S. Geological Survey ;\r\nUSGS Earth Science Information Center, Open-File Reports Section [distributor],","doi":"10.3133/ofr93465","usgsCitation":"Rodríguez-Martínez, J., and Hartley, J.L., 1994, Geologic and hydrologic data collected at test holes NC-6 and NC-11, Hatillo and Isabela, northwestern Puerto Rico: U.S. Geological Survey Open-File Report 93-465, iv, 39 p. :ill., maps ;28 cm., https://doi.org/10.3133/ofr93465.","productDescription":"iv, 39 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":154028,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1993/0465/report-thumb.jpg"},{"id":50205,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1993/0465/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1ae4b07f02db6a81e7","contributors":{"authors":[{"text":"Rodríguez-Martínez, Jesús","contributorId":48149,"corporation":false,"usgs":true,"family":"Rodríguez-Martínez","given":"Jesús","affiliations":[],"preferred":false,"id":183059,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hartley, John L.","contributorId":57095,"corporation":false,"usgs":true,"family":"Hartley","given":"John","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":183060,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":18374,"text":"ofr94378 - 1994 - Biomonitoring our streams","interactions":[],"lastModifiedDate":"2012-02-02T00:07:30","indexId":"ofr94378","displayToPublicDate":"1995-01-10T00:00:00","publicationYear":"1994","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"94-378","title":"Biomonitoring our streams","docAbstract":"Biomonitoring is often used to enhance or replace chemical monitoring when evaluating water quality in our streams. This report is intended to introduce the theories behind biomonitoring and some of the techniques used in a biomonitoring study. It also lists some of the advantages and limitations of biomonitoring.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr94378","usgsCitation":"Byl, T., and Smith, G.F., 1994, Biomonitoring our streams: U.S. Geological Survey Open-File Report 94-378, 1 sheet :ill. ;22 x 35 cm. folded to 22 x 9 cm., https://doi.org/10.3133/ofr94378.","productDescription":"1 sheet :ill. ;22 x 35 cm. folded to 22 x 9 cm.","costCenters":[],"links":[{"id":1097,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/ofr_94-378","linkFileType":{"id":5,"text":"html"}},{"id":151975,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a48e4b07f02db6230cc","contributors":{"authors":[{"text":"Byl, Thomas Duane","contributorId":65491,"corporation":false,"usgs":true,"family":"Byl","given":"Thomas Duane","affiliations":[],"preferred":false,"id":179004,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Smith, George F.","contributorId":87574,"corporation":false,"usgs":true,"family":"Smith","given":"George","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":179005,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":18273,"text":"ofr94329 - 1994 - Hydrogeologic and water-quality data from wells near the Hueco Bolson Recharge Project area, El Paso, Texas, 1990 and 1991","interactions":[],"lastModifiedDate":"2019-12-08T13:58:17","indexId":"ofr94329","displayToPublicDate":"1995-01-10T00:00:00","publicationYear":"1994","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"94-329","title":"Hydrogeologic and water-quality data from wells near the Hueco Bolson Recharge Project area, El Paso, Texas, 1990 and 1991","docAbstract":"<p>Tertiary-treated wastewater currently (1991) is being injected into the Hueco bolson aquifer at a site in northeastern El Paso, Texas, to supplement the quantity of available freshwater. Hydrologic data were compiled and water-quality and bacterial data were collected from existing wells near the Hueco Bolson Recharge Project (HBRP) in August and September 1990 and 1991.</p>\n<p>Borehole tracer tests indicated upward ground-water flow in nearly all tested intervals of several observation wells. The cumulative volume of injected water was less than the volume produced from wells adjacent to the HBRP area. Water levels in three production wells, located more than 1.5 miles from the injection wells, declined at rates comparable to those observed before injection operations. Water levels in wells located within 0.75 mile of the injection-well pipeline declined at a slower rate after HBRP injection operations had begun. Between 1985 and 1991, water levels in observation wells located within 700 feet of an injection well either did not appreciably decline, or declined at smaller rates than water levels in more distant production wells.</p>\n<p>Trihalomethane compounds were detected in water from 8 of the 16 observation and production wells sampled in 1990 and in 10 of the 17 wells sampled in 1991. Concentrations of trihalomethane compounds in these samples ranged from 0.05 to 1.9 |lg/L (micrograms per liter) in 1990 and from 0.05 to 1.4 |ig/L in 1991. Concentrations of trihalomethane compounds in samples of injected water from two wells were 27.8 and 34.6 |J,g/L respectively, in 1991. Dibromomethane and dichloromethane were detected in water from injection wells and from observation wells within about 700 feet of the injection wells.</p>\n<p>Aerobic bacteria were determined to be the only bacteria type present in ground water except for samples from two wells, which also contained denitrifying bacteria. The populations of aerobic bacteria determined in ground water ranged from 80 to more than 160,000 most probable number of organisms per milliliter of sample.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr94329","usgsCitation":"Brock, R.D., Buszka, P.M., and Godsy, E.M., 1994, Hydrogeologic and water-quality data from wells near the Hueco Bolson Recharge Project area, El Paso, Texas, 1990 and 1991: U.S. Geological Survey Open-File Report 94-329, v, 85 p., https://doi.org/10.3133/ofr94329.","productDescription":"v, 85 p.","numberOfPages":"90","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true},{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":151165,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1994/0329/report-thumb.jpg"},{"id":47626,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1994/0329/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Texas","city":"El Paso","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -106.64154052734374,\n              31.5668353078939\n            ],\n            [\n              -106.15814208984374,\n              31.5668353078939\n            ],\n            [\n              -106.15814208984374,\n              32.010404958190534\n            ],\n            [\n              -106.64154052734374,\n              32.010404958190534\n            ],\n            [\n              -106.64154052734374,\n              31.5668353078939\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a50e4b07f02db628c2d","contributors":{"authors":[{"text":"Brock, Robert D.","contributorId":27875,"corporation":false,"usgs":true,"family":"Brock","given":"Robert","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":178829,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Buszka, Paul M. 0000-0001-8218-826X pmbuszka@usgs.gov","orcid":"https://orcid.org/0000-0001-8218-826X","contributorId":1786,"corporation":false,"usgs":true,"family":"Buszka","given":"Paul","email":"pmbuszka@usgs.gov","middleInitial":"M.","affiliations":[{"id":27231,"text":"Indiana-Kentucky Water Science Center","active":true,"usgs":true},{"id":346,"text":"Indiana Water Science Center","active":true,"usgs":true}],"preferred":true,"id":178828,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Godsy, Edward M.","contributorId":66278,"corporation":false,"usgs":true,"family":"Godsy","given":"Edward","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":178830,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":17763,"text":"ofr94308 - 1994 - Surface-water-quality assessment of the Yakima River basin in Washington: major-and minor-element data for sediment, water, and aquatic biota, 1987-91","interactions":[],"lastModifiedDate":"2017-02-07T09:54:13","indexId":"ofr94308","displayToPublicDate":"1995-01-10T00:00:00","publicationYear":"1994","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"94-308","title":"Surface-water-quality assessment of the Yakima River basin in Washington: major-and minor-element data for sediment, water, and aquatic biota, 1987-91","docAbstract":"<p>Major- and minor-element concentrations are presented for streambed and suspended sediment, filtered- and unfiltered-water, and aquatic-biota samples collected during 1987-91 from the Yakima River Basin in south-central Washington. The samples were collected as part of the U.S. Geological Survey's National Water-quality Assessment (NAWQA) program which is designed to provide results that are useful in understanding and managing the Nation's water resources. This report includes the sampling approach, field collection and processing techniques, and methods of chemical analysis, as well as a compilation of chemical data, statistical summaries, and quality- control data. These data may be used by scientists and resource managers to describe (1) spatial distribution of selected major and minor elements in sediment, water, and aquatic biota of the Yakima River Basin; (2) temporal variation for element concentrations in filtered water and in suspended sediment at selected sites; (3) suita- bility of surface water for preservation of aquatic life and protection of human health; and (4) major natural and anthropogenic sources of major and minor elements in the Yakima River Basin that affect observed water-quality conditions.</p>\n<p>Streambed-sediment samples were collected once from 27 sites in the basin during 1987-91. Suspended-sediment and filtered-water samples were collected monthly and during hydrologic events (including snowmelt and winter rainstorms) at seven sites, and filtered-water samples were collected at least once at an additional 37 sites during synoptic samplings. Unfiltered-water samples were collected at seven sites on a quarterly basis during 1987 only. Samples of aquatic plants were collected once in 1989, and aquatic insects, fish, and clams were collected from 34 sites three times during 1989-90.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Portland, OR","doi":"10.3133/ofr94308","usgsCitation":"Fuhrer, G.J., Fluter, S.L., McKenzie, S.W., Rinella, J.F., Crawford, J.K., Cain, D.J., Hornberger, M.I., Bridges, J.L., and Skach, K.A., 1994, Surface-water-quality assessment of the Yakima River basin in Washington: major-and minor-element data for sediment, water, and aquatic biota, 1987-91: U.S. Geological Survey Open-File Report 94-308, vi, 222 p., https://doi.org/10.3133/ofr94308.","productDescription":"vi, 222 p.","onlineOnly":"N","additionalOnlineFiles":"N","temporalStart":"1987-01-01","temporalEnd":"1991-12-31","costCenters":[{"id":518,"text":"Oregon Water Science Center","active":true,"usgs":true}],"links":[{"id":46993,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1994/0308/report.pdf","text":"Report","size":"3.90 MB","linkFileType":{"id":1,"text":"pdf"},"description":"Report"},{"id":150597,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1994/0308/report-thumb.jpg"}],"country":"United States","state":"Washington","otherGeospatial":"Yakima River Basin","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -121.717529296875,\n              46.10561307998295\n            ],\n            [\n              -121.717529296875,\n              47.42251265435723\n            ],\n            [\n              -119.28955078124999,\n              47.42251265435723\n            ],\n            [\n              -119.28955078124999,\n              46.10561307998295\n            ],\n            [\n              -121.717529296875,\n              46.10561307998295\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae5e4b07f02db68a4d2","contributors":{"authors":[{"text":"Fuhrer, Gregory J. gjfuhrer@usgs.gov","contributorId":944,"corporation":false,"usgs":true,"family":"Fuhrer","given":"Gregory","email":"gjfuhrer@usgs.gov","middleInitial":"J.","affiliations":[],"preferred":true,"id":177724,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Fluter, Shelley L.","contributorId":36419,"corporation":false,"usgs":true,"family":"Fluter","given":"Shelley","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":177727,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"McKenzie, Stuart W.","contributorId":27841,"corporation":false,"usgs":true,"family":"McKenzie","given":"Stuart","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":177730,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Rinella, Joseph F. jrinella@usgs.gov","contributorId":1371,"corporation":false,"usgs":true,"family":"Rinella","given":"Joseph","email":"jrinella@usgs.gov","middleInitial":"F.","affiliations":[],"preferred":true,"id":177732,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Crawford, J. Kent","contributorId":54176,"corporation":false,"usgs":true,"family":"Crawford","given":"J.","email":"","middleInitial":"Kent","affiliations":[],"preferred":false,"id":177725,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Cain, Daniel J. 0000-0002-3443-0493 djcain@usgs.gov","orcid":"https://orcid.org/0000-0002-3443-0493","contributorId":1784,"corporation":false,"usgs":true,"family":"Cain","given":"Daniel","email":"djcain@usgs.gov","middleInitial":"J.","affiliations":[{"id":438,"text":"National Research Program - Western Branch","active":true,"usgs":true},{"id":37277,"text":"WMA - Earth System Processes Division","active":true,"usgs":true}],"preferred":true,"id":177731,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Hornberger, Michelle I. 0000-0002-7787-3446 mhornber@usgs.gov","orcid":"https://orcid.org/0000-0002-7787-3446","contributorId":1037,"corporation":false,"usgs":true,"family":"Hornberger","given":"Michelle","email":"mhornber@usgs.gov","middleInitial":"I.","affiliations":[{"id":37277,"text":"WMA - Earth System Processes Division","active":true,"usgs":true}],"preferred":true,"id":177726,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Bridges, Jennifer L.","contributorId":42480,"corporation":false,"usgs":true,"family":"Bridges","given":"Jennifer","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":177729,"contributorType":{"id":1,"text":"Authors"},"rank":8},{"text":"Skach, Kenneth A. kaskach@usgs.gov","contributorId":1894,"corporation":false,"usgs":true,"family":"Skach","given":"Kenneth","email":"kaskach@usgs.gov","middleInitial":"A.","affiliations":[],"preferred":true,"id":177728,"contributorType":{"id":1,"text":"Authors"},"rank":9}]}}
,{"id":18106,"text":"ofr94301 - 1994 - Hydrogeologic and water-quality data for the main site, Naval Surface Warfare Center, Dahlgren Laboratory, Dahlgren, Virginia","interactions":[],"lastModifiedDate":"2012-02-02T00:07:15","indexId":"ofr94301","displayToPublicDate":"1995-01-10T00:00:00","publicationYear":"1994","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"94-301","title":"Hydrogeologic and water-quality data for the main site, Naval Surface Warfare Center, Dahlgren Laboratory, Dahlgren, Virginia","docAbstract":"Hydrogeologic and water-quality data were collected at the Naval Surface Warfare Center, Dahlgren Laboratory at Dahlgren, Virginia, as part of a hydrogeologic assessment of the shallow aquifer system begun in 1992. The U.S. Geological Survey conducted this study to provide the Navy with hydrogeologic data to meet the requirements of a Spill Contingency Plan. This report describes the ground-water observation-well network, hydro- geologic, and water-quality data collected between August 1992 and September 1993. The report includes a description of the locations and con- struction of 35 observation wells on the Main Site. Hydrologic data include lithologic core samples, geophysical logs, and vertical hydraulic conductivity measurements of selected core intervals. Hydrologic data include synoptic and hourly measurements of ground-water levels, observation-well slug tests to determine horizontal hydraulic conductivity, and tide data. Water-quality data include analyses of major dissolved constituents in ground water and surface water.","language":"ENGLISH","publisher":"U.S. Geological Survey ;\r\nU.S. Geological Survey, Earth Science Information Center, Open-File Reports Section [distributor],","doi":"10.3133/ofr94301","usgsCitation":"Bell, C.F., Bolles, T.P., and Harlow, G., 1994, Hydrogeologic and water-quality data for the main site, Naval Surface Warfare Center, Dahlgren Laboratory, Dahlgren, Virginia: U.S. Geological Survey Open-File Report 94-301, iv, 81 p. :ill., maps ;28 cm., https://doi.org/10.3133/ofr94301.","productDescription":"iv, 81 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":149280,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1994/0301/report-thumb.jpg"},{"id":21589,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1994/0301/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":47462,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1994/0301/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a50e4b07f02db628c54","contributors":{"authors":[{"text":"Bell, Clifton F.","contributorId":79905,"corporation":false,"usgs":true,"family":"Bell","given":"Clifton","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":178560,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bolles, Thomas P.","contributorId":22374,"corporation":false,"usgs":true,"family":"Bolles","given":"Thomas","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":178559,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Harlow, George E. Jr. geharlow@usgs.gov","contributorId":383,"corporation":false,"usgs":true,"family":"Harlow","given":"George E.","suffix":"Jr.","email":"geharlow@usgs.gov","affiliations":[{"id":614,"text":"Virginia Water Science Center","active":true,"usgs":true}],"preferred":false,"id":178558,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":20581,"text":"ofr94349 - 1994 - Water-level data for the Albuquerque Basin, New Mexico, October 1, 1986, through September 30, 1990","interactions":[],"lastModifiedDate":"2012-02-02T00:07:43","indexId":"ofr94349","displayToPublicDate":"1995-01-10T00:00:00","publicationYear":"1994","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"94-349","title":"Water-level data for the Albuquerque Basin, New Mexico, October 1, 1986, through September 30, 1990","language":"ENGLISH","publisher":"U.S. Geological Survey ;\r\nUSGS Earth Science Information Center, Open-File Reports Section [distributor],","doi":"10.3133/ofr94349","usgsCitation":"Rankin, D.R., 1994, Water-level data for the Albuquerque Basin, New Mexico, October 1, 1986, through September 30, 1990: U.S. Geological Survey Open-File Report 94-349, v, 29 p. :ill., map ;28 cm., https://doi.org/10.3133/ofr94349.","productDescription":"v, 29 p. :ill., map ;28 cm.","costCenters":[],"links":[{"id":152951,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1994/0349/report-thumb.jpg"},{"id":50100,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1994/0349/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e6e4b07f02db5e7660","contributors":{"authors":[{"text":"Rankin, Dale R.","contributorId":50924,"corporation":false,"usgs":true,"family":"Rankin","given":"Dale","email":"","middleInitial":"R.","affiliations":[{"id":472,"text":"New Mexico Water Science Center","active":true,"usgs":true}],"preferred":false,"id":182885,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":21068,"text":"ofr94283 - 1994 - Preliminary geologic map of the Deadman Spring NE quadrangle, Lincoln County, Nevada","interactions":[],"lastModifiedDate":"2012-02-02T00:07:46","indexId":"ofr94283","displayToPublicDate":"1995-01-10T00:00:00","publicationYear":"1994","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"94-283","title":"Preliminary geologic map of the Deadman Spring NE quadrangle, Lincoln County, Nevada","docAbstract":"Pesticides are used extensively in the largely agricultural Red River of the North (Red River) Basin, but, unlike many other agricultural basins, only small amounts are routinely detected in samples from streams in the basin. The pesticides detected comprise less than 2 percent of the amount applied and usually are at concentrations far less than established drinking water standards. Most of the detected pesticides seem to come from sources near the headwaters in the southern part of the basin. Although low, concentrations are related to pesticide application and runoff. Flat slope, organic solids, pesticide management, and degra- dation all may reduce pesticide contamination of Red River streams.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr94283","usgsCitation":"Swadley, W.C., Page, W.R., and Scott, R.B., 1994, Preliminary geologic map of the Deadman Spring NE quadrangle, Lincoln County, Nevada: U.S. Geological Survey Open-File Report 94-283, 14 p. :ill., map ;28 cm., https://doi.org/10.3133/ofr94283.","productDescription":"14 p. :ill., map ;28 cm.","costCenters":[],"links":[{"id":108229,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_12495.htm","linkFileType":{"id":5,"text":"html"},"description":"12495"},{"id":152874,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1994/0283/report-thumb.jpg"},{"id":21585,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1994/0283/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":50659,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1994/0283/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac8e4b07f02db67ba51","contributors":{"authors":[{"text":"Swadley, W. C.","contributorId":46940,"corporation":false,"usgs":true,"family":"Swadley","given":"W.","middleInitial":"C.","affiliations":[],"preferred":false,"id":183786,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Page, William R. 0000-0002-0722-9911 rpage@usgs.gov","orcid":"https://orcid.org/0000-0002-0722-9911","contributorId":1628,"corporation":false,"usgs":true,"family":"Page","given":"William","email":"rpage@usgs.gov","middleInitial":"R.","affiliations":[{"id":318,"text":"Geosciences and Environmental Change Science Center","active":true,"usgs":true}],"preferred":true,"id":183785,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Scott, Robert B. rbscott@usgs.gov","contributorId":766,"corporation":false,"usgs":true,"family":"Scott","given":"Robert","email":"rbscott@usgs.gov","middleInitial":"B.","affiliations":[],"preferred":true,"id":183784,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":24217,"text":"ofr94463 - 1994 - Source code and ancillary data files for the MODPATH particles tracking package of the ground-water flow model MODFLOW","interactions":[],"lastModifiedDate":"2013-09-17T15:22:39","indexId":"ofr94463","displayToPublicDate":"1995-01-10T00:00:00","publicationYear":"1994","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"94-463","title":"Source code and ancillary data files for the MODPATH particles tracking package of the ground-water flow model MODFLOW","language":"ENGLISH","publisher":"U.S. Dept. of the Interior, U.S. Geological Survey ;Earth Science Information Center [distributor],","doi":"10.3133/ofr94463","issn":"0094-9140","collaboration":"The USGS does not support this software or technical questions for the software associated with the publication.","usgsCitation":"Pollock, D.W., 1994, Source code and ancillary data files for the MODPATH particles tracking package of the ground-water flow model MODFLOW (Version 3, Release 1.): U.S. Geological Survey Open-File Report 94-463, 2 computer disks ;3 1/2 in., https://doi.org/10.3133/ofr94463.","productDescription":"2 computer disks ;3 1/2 in.","costCenters":[],"links":[{"id":156578,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1994/0463/report-thumb.jpg"},{"id":53352,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1994/0463/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":277710,"type":{"id":4,"text":"Application Site"},"url":"https://pubs.usgs.gov/of/1994/0463/application.zip"}],"edition":"Version 3, Release 1.","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e6e4b07f02db5e775e","contributors":{"authors":[{"text":"Pollock, David W. dwpolloc@usgs.gov","contributorId":4248,"corporation":false,"usgs":true,"family":"Pollock","given":"David","email":"dwpolloc@usgs.gov","middleInitial":"W.","affiliations":[{"id":493,"text":"Office of Ground Water","active":true,"usgs":true}],"preferred":true,"id":191508,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":31779,"text":"ofr94373 - 1994 - Potentiometric surface of the lower Potomac Aquifer in Virginia, 1993","interactions":[],"lastModifiedDate":"2021-10-26T21:07:23.608316","indexId":"ofr94373","displayToPublicDate":"1995-01-10T00:00:00","publicationYear":"1994","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"94-373","title":"Potentiometric surface of the lower Potomac Aquifer in Virginia, 1993","docAbstract":"Ground-water level measurements from 17 wells in the lower Potomac aquifer in the Coastal Plain Physiographic Province of Virginia in 1993 were used to prepare a map of the potentiometric surface of the aquifer. The map shows the potentiometric surface of the lower Potomac aquifer indicating a regional trend toward the Chesapeake Bay and Atlantic Ocean. The potentiometric-surface data indicate that there are two cones of depression, one around well fields in Henrico County and the other around large well fields in Isle of Wight County and Franklin, Virginia. The highest ground-water-level measurement was 47 feet above sea level in southeast Southampton County, and the lowest ground-water-level measurement was 161 feet below sea level in the southeast area of Isle of Wight County near Franklin, Virginia.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr94373","usgsCitation":"Hammond, E.C., McFarland, E.R., and Focazio, M., 1994, Potentiometric surface of the lower Potomac Aquifer in Virginia, 1993: U.S. Geological Survey Open-File Report 94-373, 1 p., https://doi.org/10.3133/ofr94373.","productDescription":"1 p.","costCenters":[],"links":[{"id":390986,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_12513.htm"},{"id":59994,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1994/0373/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":160997,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1994/0373/report-thumb.jpg"}],"country":"United States","state":"Virginia","otherGeospatial":"lower Potomac Aquifer","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -78,\n              36.48\n            ],\n            [\n              -75.119,\n              36.48\n            ],\n            [\n              -75.119,\n              39\n            ],\n            [\n              -78,\n              39\n            ],\n            [\n              -78,\n              36.48\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad4e4b07f02db682e2a","contributors":{"authors":[{"text":"Hammond, E. C.","contributorId":34544,"corporation":false,"usgs":true,"family":"Hammond","given":"E.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":206942,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"McFarland, E. R.","contributorId":65109,"corporation":false,"usgs":true,"family":"McFarland","given":"E.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":206944,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Focazio, M. J.","contributorId":62997,"corporation":false,"usgs":true,"family":"Focazio","given":"M. J.","affiliations":[],"preferred":false,"id":206943,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":31778,"text":"ofr94372 - 1994 - Potentiometric surface of the middle Potomac Aquifer in Virginia, 1993","interactions":[],"lastModifiedDate":"2021-10-26T21:10:19.789663","indexId":"ofr94372","displayToPublicDate":"1995-01-10T00:00:00","publicationYear":"1994","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"94-372","title":"Potentiometric surface of the middle Potomac Aquifer in Virginia, 1993","docAbstract":"Ground-water level measurements from 50 wells in the middle Potomac aquifer in the Coastal Plain Physiographic Province of Virginia in 1993 were used to prepare a map of the potentiometric surface of the aquifer. The map shows the potentiometric surface of the middle Potomac aquifer sharply declining eastward from nearly 100 feet above sear level near the western boundary of the aquifer to 20 feet below sea level, and continues declining gradually toward the Chesapeake Bay and Atlantic Ocean. A cone of depression is apparent around well fields in Franklin, Virginia. The potentiometric surface also appears to be affected by pumping in the area of Henrico County and Hanover County, Virginia. The highest ground-water-level measurement was 89 feet above sea level in Chesterfield County near Richmond, and the lowest ground-water-level measurement was 179 feet below sea level in southeastern Isle of Wight County, Virginia.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr94372","usgsCitation":"Hammond, E.C., McFarland, E.R., and Focazio, M., 1994, Potentiometric surface of the middle Potomac Aquifer in Virginia, 1993: U.S. Geological Survey Open-File Report 94-372, 1 p., https://doi.org/10.3133/ofr94372.","productDescription":"1 p.","costCenters":[],"links":[{"id":59993,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1994/0372/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":390987,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_12512.htm"},{"id":160996,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1994/0372/report-thumb.jpg"}],"country":"United States","state":"Virginia","otherGeospatial":"middle Potomac Aquifer","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -78,\n              36.48\n            ],\n            [\n              -75.119,\n              36.48\n            ],\n            [\n              -75.119,\n              39\n            ],\n            [\n              -78,\n              39\n            ],\n            [\n              -78,\n              36.48\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad4e4b07f02db682e36","contributors":{"authors":[{"text":"Hammond, E. C.","contributorId":34544,"corporation":false,"usgs":true,"family":"Hammond","given":"E.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":206939,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"McFarland, E. R.","contributorId":65109,"corporation":false,"usgs":true,"family":"McFarland","given":"E.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":206941,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Focazio, M. J.","contributorId":62997,"corporation":false,"usgs":true,"family":"Focazio","given":"M. J.","affiliations":[],"preferred":false,"id":206940,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":31777,"text":"ofr94370 - 1994 - Potentiometric surface of the Brightseat-upper Potomac Aquifer in Virginia, 1993","interactions":[],"lastModifiedDate":"2021-10-26T21:03:08.324949","indexId":"ofr94370","displayToPublicDate":"1995-01-10T00:00:00","publicationYear":"1994","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"94-370","title":"Potentiometric surface of the Brightseat-upper Potomac Aquifer in Virginia, 1993","docAbstract":"<p>Ground-water level measurements from 30 wells in the Brightseat-upper Potomac aquifer in the Coastal Plain Physiographic Province of Virginia in 1993 were used to prepare a map of the potentiometric surface of the aquifer. The map shows the potentiometric surface of the Brightseat-upper Potomac aquifer indicating a regional trend toward the Chesapeake Bay and Atlantic Ocean. The potentiometric-surface data indicate that cones of depression are apparent around West Point and in southeastern Isle of Wight County near Franklin, Virginia. The highest ground-water-level measurement was 4 feet above sea level in northern Accomack County, and the lowest ground-water-level measurement was 117 feet below sea level in Franklin, Virginia.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr94370","usgsCitation":"Hammond, E.C., McFarland, E.R., and Focazio, M., 1994, Potentiometric surface of the Brightseat-upper Potomac Aquifer in Virginia, 1993: U.S. Geological Survey Open-File Report 94-370, 1 p., https://doi.org/10.3133/ofr94370.","productDescription":"1 p.","costCenters":[],"links":[{"id":160995,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1994/0370/report-thumb.jpg"},{"id":390985,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_12510.htm"},{"id":59992,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1994/0370/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Virginia","otherGeospatial":"Brightseat-upper Potomac aquifer","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -78,\n              36.48\n            ],\n            [\n              -75.119,\n              36.48\n            ],\n            [\n              -75.119,\n              39\n            ],\n            [\n              -78,\n              39\n            ],\n            [\n              -78,\n              36.48\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad4e4b07f02db683061","contributors":{"authors":[{"text":"Hammond, E. C.","contributorId":34544,"corporation":false,"usgs":true,"family":"Hammond","given":"E.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":206936,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"McFarland, E. R.","contributorId":65109,"corporation":false,"usgs":true,"family":"McFarland","given":"E.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":206938,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Focazio, M. J.","contributorId":62997,"corporation":false,"usgs":true,"family":"Focazio","given":"M. J.","affiliations":[],"preferred":false,"id":206937,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":31781,"text":"ofr94391 - 1994 - Potentiometric surface of the Magothy Aquifer in southern Maryland, September 1993","interactions":[],"lastModifiedDate":"2022-08-02T18:47:50.257102","indexId":"ofr94391","displayToPublicDate":"1995-01-10T00:00:00","publicationYear":"1994","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"94-391","title":"Potentiometric surface of the Magothy Aquifer in southern Maryland, September 1993","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr94391","usgsCitation":"Curtin, S.E., Mack, F., and Andreasen, D.C., 1994, Potentiometric surface of the Magothy Aquifer in southern Maryland, September 1993: U.S. Geological Survey Open-File Report 94-391, 1 p., https://doi.org/10.3133/ofr94391.","productDescription":"1 p.","costCenters":[{"id":374,"text":"Maryland Water Science Center","active":true,"usgs":true}],"links":[{"id":404692,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_12519.htm","linkFileType":{"id":5,"text":"html"}},{"id":59996,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1994/0391/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":160999,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1994/0391/report-thumb.jpg"}],"country":"United States","state":"Maryland, Virginia","otherGeospatial":"Magothy Aquifer","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -77.333,\n              38\n            ],\n            [\n              -76,\n              38\n            ],\n            [\n              -76,\n              39.25\n            ],\n            [\n              -77.333,\n              39.25\n            ],\n            [\n              -77.333,\n              38\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad4e4b07f02db682f58","contributors":{"authors":[{"text":"Curtin, Stephen E. securtin@usgs.gov","contributorId":3703,"corporation":false,"usgs":true,"family":"Curtin","given":"Stephen","email":"securtin@usgs.gov","middleInitial":"E.","affiliations":[{"id":374,"text":"Maryland Water Science Center","active":true,"usgs":true}],"preferred":true,"id":206948,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Mack, Frederick K.","contributorId":95858,"corporation":false,"usgs":true,"family":"Mack","given":"Frederick K.","affiliations":[],"preferred":false,"id":206950,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Andreasen, D. C.","contributorId":32565,"corporation":false,"usgs":true,"family":"Andreasen","given":"D.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":206949,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":28553,"text":"wri944053 - 1994 - Iodine-129 in the Snake River Plain aquifer at and near the Idaho National Engineering Laboratory, Idaho, 1990-91","interactions":[],"lastModifiedDate":"2012-02-02T00:08:46","indexId":"wri944053","displayToPublicDate":"1995-01-10T00:00:00","publicationYear":"1994","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"94-4053","title":"Iodine-129 in the Snake River Plain aquifer at and near the Idaho National Engineering Laboratory, Idaho, 1990-91","docAbstract":"From 1953 to 1990, an estimated 0.56 to 1.18 curies of iodine-129 were contained in wastewater generated by the Idaho Chemical Processing Plant (ICPP) at the Idaho National Engineering Laboratory. The waste- water was discharged directly to the Snake River Plain aquifer through a deep disposal well prior to February 1984 and through unlined disposal ponds in 1984-90. The wastewater did not contain measurable concentrations of iodine-129 in 1989-90. Samples were collected from 51 wells that obtain water from the Snake River Plain aquifer and 1 well that obtains water from a perched ground-water zone. The samples were analyzed for iodine-129 using an accelerator mass spectrometer which is two to six orders of magnitude more sensitive than neutron- activation methods. Therefore, iodine-129 was detectable in samples from a larger number of wells distributed over a larger area than previously was possible. Ground-water flow velocities calculated using iodine-129 data are estimated to be at least 6 feet per day. These velocities compare favorably with those of 4 to 10 feet per day calculated from tritium data and tracer studies at wells down- gradient from the ICPP. In 1990-91, concentrations of iodine-129 in water samples from wells that obtain water from the Snake River Plain aquifer ranged from less than 0.0000006+0.0000002 to 3.82.+0.19 picocuries per liter (pCi/L). The mean concentration in water from 18 wells was 0.81+0.19 pCi/L as compared with 1.30+0.26 pCi/L in 1986. The decrease in the iodine-l29 concentrations from 1986 to 1990-91 chiefly was the result of a decrease in the amount of iodine-129 disposed of annually, and changes in disposal techniques.","language":"ENGLISH","publisher":"U.S. Geological Survey ;\r\nUSGS Earth Science Information Center, Open-File Reports Section [distributor],","doi":"10.3133/wri944053","usgsCitation":"Mann, L., and Beasley, T., 1994, Iodine-129 in the Snake River Plain aquifer at and near the Idaho National Engineering Laboratory, Idaho, 1990-91: U.S. Geological Survey Water-Resources Investigations Report 94-4053, iv, 27 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri944053.","productDescription":"iv, 27 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":122980,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1994/4053/report-thumb.jpg"},{"id":57382,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1994/4053/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aa8e4b07f02db667300","contributors":{"authors":[{"text":"Mann, L. J.","contributorId":39392,"corporation":false,"usgs":true,"family":"Mann","given":"L. J.","affiliations":[],"preferred":false,"id":200014,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Beasley, T.M.","contributorId":74788,"corporation":false,"usgs":true,"family":"Beasley","given":"T.M.","email":"","affiliations":[],"preferred":false,"id":200015,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":44765,"text":"wri934096 - 1994 - Estimated withdrawals and use of freshwater in New Hampshire, 1990","interactions":[],"lastModifiedDate":"2012-02-02T00:05:00","indexId":"wri934096","displayToPublicDate":"1995-01-10T00:00:00","publicationYear":"1994","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"93-4096","title":"Estimated withdrawals and use of freshwater in New Hampshire, 1990","docAbstract":"Estimated freshwater withdrawals during 1990 in New Hampshire totaled about 422 million gallons per day from ground-water and surface-water sources. The largest withdrawals were for thermoelectric-power generation (60 percent), public supply (23 percent), and industrial use (9 percent). Most withdrawals, 358 million gallons per day, were made from surface- water sources, as compared to 63.7 million gallons per day from ground-water sources. The largest with- drawals were in the Merrimack river basin (322 million gallons per day). An additional 46,000 million gallons per day was used instream for hydroelectric-power generation, primarily in the Upper Androscoggin and Upper Connecticut River subbasins. Other information describing water-use patterns is shown in tables, bar graphs, pie charts, maps, and accompanying text. The data are aggregated by river basin (hydrologic cataloging unit), and all values are reported in million gallons per day.","language":"ENGLISH","doi":"10.3133/wri934096","usgsCitation":"Medalie, L., and Horn, M., 1994, Estimated withdrawals and use of freshwater in New Hampshire, 1990: U.S. Geological Survey Water-Resources Investigations Report 93-4096, 10 maps on 1 sheet : col. ; 20 x 10 cm. and 8 x 5 cm., sheet 86 x 102 cm., folded to 21 x 22 cm., https://doi.org/10.3133/wri934096.","productDescription":"10 maps on 1 sheet : col. ; 20 x 10 cm. and 8 x 5 cm., sheet 86 x 102 cm., folded to 21 x 22 cm.","costCenters":[],"links":[{"id":135757,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":82072,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1993/4096/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0ce4b07f02db5fcb91","contributors":{"authors":[{"text":"Medalie, Laura 0000-0002-2440-2149 lmedalie@usgs.gov","orcid":"https://orcid.org/0000-0002-2440-2149","contributorId":3657,"corporation":false,"usgs":true,"family":"Medalie","given":"Laura","email":"lmedalie@usgs.gov","affiliations":[{"id":466,"text":"New England Water Science Center","active":true,"usgs":true}],"preferred":true,"id":230387,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Horn, M.A.","contributorId":92223,"corporation":false,"usgs":true,"family":"Horn","given":"M.A.","email":"","affiliations":[],"preferred":false,"id":230388,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":44728,"text":"wri944088 - 1994 - Permeability of soils in Mississippi","interactions":[],"lastModifiedDate":"2012-02-10T00:10:09","indexId":"wri944088","displayToPublicDate":"1995-01-10T00:00:00","publicationYear":"1994","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"94-4088","title":"Permeability of soils in Mississippi","docAbstract":"The permeability of soils in Mississippi was determined and mapped using a geographic information system (GIS). Soil permeabilities in Mississippi were determined to range in value from nearly 0.0 to values exceeding 5.0 inches per hour. The U.S. Soil Conservation Service's State Soil Geographic Data Base (STATSGO) was used as the primary source of data for the determination of area-weighted soil permeability. STATSGO provides soil layer properties that are spatially referenced to mapped areas. These mapped areas are referred to as polygons in the GIS. The polygons arc boundaries of soils mapped as a group and are given unique Map Unit Identifiers (MUIDs). The data describing the physical characteristics of the soils within each polygon are stored in a tabular data base format and are referred to as attributes. The U.S. Soil Conservation Service developed STATSGO to be primarily used as a guide for regional resource planning, management, and monitoring. STATSGO was designed so that soil information could be extracted from properties tables at the layer level, combined by component, and statistically expanded to cover the entire map unit. The results of this study provide a mapped value for permeability which is representative of the vertical permeability of soils in that area. The resultant permeability map provides a representative vertical soil permeability for a given area sufficient for county, multi- county, and area planning, and will be used as the soil permeability data component in the evaluation of the susceptibility of major aquifers to contami- nation in Mississippi.","language":"ENGLISH","doi":"10.3133/wri944088","usgsCitation":"O'Hara, C., 1994, Permeability of soils in Mississippi: U.S. Geological Survey Water-Resources Investigations Report 94-4088, 1 map : col. ; 114 x 87 cm., folded in envelope 30 x 24 cm., https://doi.org/10.3133/wri944088.","productDescription":"1 map : col. ; 114 x 87 cm., folded in envelope 30 x 24 cm.","costCenters":[],"links":[{"id":161624,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":82030,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1994/4088/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"500000","projection":"Lambert conformal conic","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -91.63333333333334,30 ], [ -91.63333333333334,35 ], [ -88.11666666666666,35 ], [ -88.11666666666666,30 ], [ -91.63333333333334,30 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b32e4b07f02db6b4772","contributors":{"authors":[{"text":"O'Hara, Charles G.","contributorId":83911,"corporation":false,"usgs":true,"family":"O'Hara","given":"Charles G.","affiliations":[],"preferred":false,"id":230329,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":28756,"text":"wri924013 - 1994 - Geohydrology and water quality of stratified-drift aquifers in the lower Connecticut River basin, southwestern New Hampshire","interactions":[],"lastModifiedDate":"2012-02-02T00:08:46","indexId":"wri924013","displayToPublicDate":"1995-01-10T00:00:00","publicationYear":"1994","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"92-4013","title":"Geohydrology and water quality of stratified-drift aquifers in the lower Connecticut River basin, southwestern New Hampshire","docAbstract":"Stratified-drift aquifers discontinuously underlie 116 square miles of the Lower Connecticut River basin in southwestern New Hampshire, which has a total drainage area of 1,163 square miles. Saturated thicknesses of stratified drift within the study area are locally greater than 400 feet but generally are less. Transmissivities 1ocally exceeds 4,000 feet squared per day but are generally much less. The 20.8 square mile, or 1.8 percent, of the study area identified as having transmissivity greater than 1,000 feet squared per day represents a valuable resource. The geohydrology of stratified- drift aquifers was investigated by focusing on basic aquifer properties, including aquifer boundaries; recharge, discharge, and direction of ground-water flow; saturated thickness and storage; and transmissivity. Surficial geologic mapping assisted in the determination of aquifer boundaries. Data from more than 2,300 wells, test borings, and springs were used to produce maps of water-table altitude, saturated thickness, and transmissivity of-stratified drift. Seismic-refraction profiles were completed at 29 locations in the study area. These profiles aided in the construction of the water-table and saturated-thickness maps. Seismic- reflection data were also collected along 60 miles of the Connecticut River. A stratified-drift aquifer in southern Croydon and northern Newport was analyzed for aquifer yield using transient simulations and a two-dimensional, finite-difference ground-water-flow model. The objective was to estimate the yield after a 180-day period of pumping. Two hypothetical wells were pumped at 1.0 Mgal/d and 0.5 Mgal/d for 180 days respectively. The amount of water available for infiltration was the limiting factor. Results of analysis of water samples from 22 wells and 8 spring show that, with some exceptions, water in the stratified-drift aquifer generally meets the U.S. Environmental Protection Agency's primary and secondary drinking-water regulations.","language":"ENGLISH","publisher":"U.S. Dept. of the Interior, U.S. Geological Survey ;\r\nUSGS Earth Science Information Center, Open-File Reports Section [distributor],","doi":"10.3133/wri924013","usgsCitation":"Moore, R.B., Johnson, C., and Douglas, E., 1994, Geohydrology and water quality of stratified-drift aquifers in the lower Connecticut River basin, southwestern New Hampshire: U.S. Geological Survey Water-Resources Investigations Report 92-4013, 1 v. (various paging) :ill., maps (some col.) ;28 cm. [PGS - 325 p.], https://doi.org/10.3133/wri924013.","productDescription":"1 v. (various paging) :ill., maps (some col.) ;28 cm. [PGS - 325 p.]","costCenters":[],"links":[{"id":123676,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1992/4013/report-thumb.jpg"},{"id":57616,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1992/4013/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":57617,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1992/4013/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":57618,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1992/4013/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":57619,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1992/4013/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":57620,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1992/4013/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae0e4b07f02db6880d5","contributors":{"authors":[{"text":"Moore, R. B.","contributorId":98720,"corporation":false,"usgs":true,"family":"Moore","given":"R.","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":200347,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Johnson, C. D.","contributorId":8120,"corporation":false,"usgs":true,"family":"Johnson","given":"C. D.","affiliations":[],"preferred":false,"id":200345,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Douglas, E.M.","contributorId":60685,"corporation":false,"usgs":true,"family":"Douglas","given":"E.M.","email":"","affiliations":[],"preferred":false,"id":200346,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":29284,"text":"wri934233 - 1994 - Use of landsat thematic mapper data to identify crop types and estimate irrigated acreage, Uvalde and Medina counties, Texas, 1991","interactions":[],"lastModifiedDate":"2016-08-16T13:58:33","indexId":"wri934233","displayToPublicDate":"1995-01-10T00:00:00","publicationYear":"1994","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"93-4233","title":"Use of landsat thematic mapper data to identify crop types and estimate irrigated acreage, Uvalde and Medina counties, Texas, 1991","docAbstract":"<p>Landsat Thematic Mapper (TM) data were used to estimate that about 51,000 acres of crops were irrigated with water pumped from the Edwards aquifer in Uvalde and Medina Counties, Texas in 1991. Bands 2, 3,4, and 5 from a TM image for August 10,1991, were classified using the maximum-likelihood, unsupervised-classification procedure to identify the areas of crops irrigated in the two counties. Detailed vegetation distribution maps of two calibration sites in the study area, and boundaries of the areas probably irrigated in 1991, were used to interpret the results and to separate probable irrigated areas by county from the rest of the image.</p>\n<p>Areas calculated for irrigated crops were 31,000 acres for Uvalde County, about 35 percent less than the area calculated using Landsat multispectral scanner (MSS) data in 1989, and 20,000 acres for Medina County, about 13 percent less than in 1989, a total decrease of about 28 percent for the two counties. Quantities of water pumped from the Edwards aquifer to irrigate crops in 1991 were estimated as 65,000 acre-feet for Uvalde County and 18,000 acre-feet for Medina County, a total decrease of about 56 percent from the value calculated using crop acreages from MSS data for 1989. Differences were attributed primarily to greater precipitation in 1991 than in 1989, resulting in smaller irrigation water requirements and less supplemental irrigation in 1991. Differences between results from 1989 and 1991, and between results from Uvalde and Medina Counties in 1991, were attributed primarily to greater precipitation in 1991, particularly in Medina County.</p>\n<p>The total number of acres of irrigated crops estimated using Landsat TM data was about 9 percent lower in Uvalde County and about 13 percent lower in Medina County than the number of acres calculated from data reported by the U.S. Department of Agriculture, Agricultural Stabilization and Conservation Service (ASCS). The total quantity of water pumped from the Edwards aquifer for irrigation in the two counties in 1991, about 83,000 acre-feet, was about 5 percent greater than the quantity calculated from data reported by the ASCS.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Austin, TX","doi":"10.3133/wri934233","collaboration":"Prepared in cooperation with the Edwards Underground Water District","usgsCitation":"Raymond, L., and McFarlane, S., 1994, Use of landsat thematic mapper data to identify crop types and estimate irrigated acreage, Uvalde and Medina counties, Texas, 1991: U.S. Geological Survey Water-Resources Investigations Report 93-4233, iii, 19 p., https://doi.org/10.3133/wri934233.","productDescription":"iii, 19 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"links":[{"id":58129,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1993/4233/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":158896,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1993/4233/report-thumb.jpg"}],"country":"United States","state":"Texas","county":"Medina County, Uvalde County","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"Polygon\",\"coordinates\":[[[-98.8056,29.6968],[-98.8042,29.2513],[-98.8039,29.0884],[-99.4107,29.087],[-99.6813,29.0872],[-100.1119,29.0844],[-100.1112,29.3486],[-100.111,29.6236],[-100.0145,29.6237],[-99.6173,29.6257],[-99.6033,29.6257],[-99.4132,29.6253],[-99.0103,29.6187],[-98.9909,29.6185],[-98.982,29.6148],[-98.9794,29.6129],[-98.9789,29.6102],[-98.9779,29.606],[-98.9801,29.5983],[-98.9818,29.5909],[-98.9819,29.5804],[-98.9836,29.5717],[-98.9837,29.5671],[-98.9832,29.5625],[-98.9811,29.5589],[-98.978,29.5556],[-98.9765,29.5547],[-98.9712,29.5533],[-98.9676,29.5546],[-98.9633,29.5578],[-98.9607,29.5578],[-98.9513,29.5581],[-98.9429,29.5585],[-98.9318,29.5588],[-98.9282,29.5593],[-98.9245,29.562],[-98.9213,29.5665],[-98.8056,29.6968]]]},\"properties\":{\"name\":\"Medina\",\"state\":\"TX\"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adae4b07f02db6858c5","contributors":{"authors":[{"text":"Raymond, L.H.","contributorId":23151,"corporation":false,"usgs":true,"family":"Raymond","given":"L.H.","email":"","affiliations":[],"preferred":false,"id":201279,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"McFarlane, S.I.","contributorId":57504,"corporation":false,"usgs":true,"family":"McFarlane","given":"S.I.","email":"","affiliations":[],"preferred":false,"id":201280,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":29254,"text":"wri914183 - 1994 - Effects of changing irrigation practices on the ground-water hydrology of the Santa Isabel-Juana Díaz area, south central Puerto Rico","interactions":[],"lastModifiedDate":"2022-01-18T21:46:45.375419","indexId":"wri914183","displayToPublicDate":"1995-01-10T00:00:00","publicationYear":"1994","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"91-4183","title":"Effects of changing irrigation practices on the ground-water hydrology of the Santa Isabel-Juana Díaz area, south central Puerto Rico","docAbstract":"Prior to 1930, the principal source of water for irrigation in the Santa Isabel-Juana Diaz area was surface water from outside the study area, which was delivered by a complex channel-pond system. Recharge from water applied to the fields, estimated to be 18.7 million of gallons per day, and discharge by ground-water flow to sea, estimated to be 17 million of gallons per day, were the major water- budget components prior to intensive development of the ground-water resources. Development of the ground-water resources after 1930 resulted in a substantial increase in irrigation, primarily furrow irrigation. The surface water supplied by the complex channel-pond system continued to be used and ground-water withdrawals increased sub- stantially. By 1966-68, ground-water recharge from irrigation water applied to the fields, estimated to be 37 million of gallons per day, and discharge by pumpage for irrigation, estimated to be 77 million of gallons per day, were the two major components of the ground-water budget. By 1987, drip irrigation had become the principal method of irrigation in the study area, and surface-water irrigation had, for the most part, been discontinued. The estimated aquifer recharge from irrigation water in 1987 was about 6.6 million of gallons per day, which occurred primarily in the remaining fields where furrow irrigation was still practiced. Although aquifer recharge had been reduced as a result of the conversion from furrow to drip irrigation, water levels in the aquifer were higher in 1987 than in 1968 because of the large reduction in ground-water withdrawals and subsequent recovery of ground-water levels.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri914183","usgsCitation":"Ramos-Gines, O., 1994, Effects of changing irrigation practices on the ground-water hydrology of the Santa Isabel-Juana Díaz area, south central Puerto Rico: U.S. Geological Survey Water-Resources Investigations Report 91-4183, iv, 22 p., https://doi.org/10.3133/wri914183.","productDescription":"iv, 22 p.","costCenters":[],"links":[{"id":394477,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_47571.htm"},{"id":58104,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1991/4183/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":123542,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1991/4183/report-thumb.jpg"}],"country":"United States","state":"Puerto Rico","otherGeospatial":"Santa Isabel - Juana Diaz area","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -66.5064239501953,\n              17.93496881111123\n            ],\n            [\n              -66.31553649902344,\n              17.93496881111123\n            ],\n            [\n              -66.31553649902344,\n              18.0224865348244\n            ],\n            [\n              -66.5064239501953,\n              18.0224865348244\n            ],\n            [\n              -66.5064239501953,\n              17.93496881111123\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a4ae4b07f02db6248c7","contributors":{"authors":[{"text":"Ramos-Gines, Orlando","contributorId":98358,"corporation":false,"usgs":true,"family":"Ramos-Gines","given":"Orlando","affiliations":[],"preferred":false,"id":201227,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":30522,"text":"wri924187 - 1994 - Hydrology and geochemistry of a surface coal mine in northwestern Colorado","interactions":[],"lastModifiedDate":"2012-02-02T00:08:57","indexId":"wri924187","displayToPublicDate":"1995-01-10T00:00:00","publicationYear":"1994","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"92-4187","title":"Hydrology and geochemistry of a surface coal mine in northwestern Colorado","docAbstract":"The hydrology and geochemistry of a reclaimed coal mine in northwestern Colorado were monitored during water years 1988 and 1989. Some data also were collected in water years 1987 and 1990. This report describes (1) the sources of hydrologic recharge to and discharge from reclaimed spoil, (2) the relative contributions of recharge to the reclaimed spoil aquifer from identified source waters and the rate of water movement from those sources to the reclaimed spoil, and (3) the geochemical reactions that control water quality in reclaimed spoil. The study area was at a dip-slope coal mine encompassing about 7 square miles with land slopes of varying aspect. The area was instrumented and monitored at five sites; two sites had unmined and reclaimed- spoil areas adjacent to each other and three sites were unmined. The mined areas had been reclaimed. Instrumentation at the study sites included 1 climate station, 3 rain gages, 19 soil-water access tubes, 2 lysimeters, 18 wells completed in bedrock, 7 wells completed in reclaimed spoil, and 2 surface- water gaging stations. The results of the study indicate that the reclaimed spoil is recharged from surface recharge and underburden aquifers. Discharge, as measured by lysimeters, was about 3 inches per year and occurred during and after snowmelt. Hydraulic-head measurements indicated a potential for ground-water movement from deeper to shallower aquifers. Water levels rose in the reclaimed-spoil aquifer and spring discharge at the toe of the spoil slopes increased rapidly in response to snowmelt. Water chemistry, stable isotopes, geochemical models, and mass-balance calculations indicate that surface recharge and the underburden aquifers each contribute about 50 percent of the water to the reclaimed-spoil aquifers. Geochemical information indicates that pyrite oxidation and dissolution of carbonate and efflorescent sulfate minerals control the water chemistry of the reclaimed-spoil aquifer.","language":"ENGLISH","publisher":"U.S. Dept. of the Interior, U.S. Geological Survey :\r\nEarth Science Information Center, Open-File Reports Section [distributor],","doi":"10.3133/wri924187","usgsCitation":"Williams, R., and Clark, G.M., 1994, Hydrology and geochemistry of a surface coal mine in northwestern Colorado: U.S. Geological Survey Water-Resources Investigations Report 92-4187, vi, 61 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri924187.","productDescription":"vi, 61 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":124119,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1992/4187/report-thumb.jpg"},{"id":59301,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1992/4187/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a18e4b07f02db604da8","contributors":{"authors":[{"text":"Williams, R.S. Jr.","contributorId":46102,"corporation":false,"usgs":true,"family":"Williams","given":"R.S.","suffix":"Jr.","email":"","affiliations":[],"preferred":false,"id":203394,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Clark, G. M.","contributorId":90325,"corporation":false,"usgs":true,"family":"Clark","given":"G.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":203395,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":30353,"text":"wri944071 - 1994 - Traveltime and reaeration characteristics for a reach of the Rio Grande, Albuquerque, New Mexico, October 1991","interactions":[],"lastModifiedDate":"2012-02-02T00:08:56","indexId":"wri944071","displayToPublicDate":"1995-01-10T00:00:00","publicationYear":"1994","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"94-4071","title":"Traveltime and reaeration characteristics for a reach of the Rio Grande, Albuquerque, New Mexico, October 1991","docAbstract":"Traveltime characteristics were determined using stream-velocity data and tracer-dye data for a reach of the Rio Grande. Traveltimes determined by the stream-velocity method were virtually the same as those determined by the tracer-dye and tracer-gas technique. The mean velocity of the stream was 1.12 miles per hour at a flow of about 300 cubic feet per second. Reaeration characteristics were determined using a propane tracer gas and a tracer-dye (rhodamine WT). Reaeration coefficients were adjusted for water temperature and the effects of wind movement on the water surface. The peak method-adjusted reaeration-coefficient mean value for the reach was 7.0 per day and ranged from 4.6 to 8.3 per day. The area method-adjusted reaeration- coefficient mean value for the reach was 7.7 per day and ranged from 5.5 to 10.4 per day.","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/wri944071","usgsCitation":"Waltemeyer, S., 1994, Traveltime and reaeration characteristics for a reach of the Rio Grande, Albuquerque, New Mexico, October 1991: U.S. Geological Survey Water-Resources Investigations Report 94-4071, iv, 19 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri944071.","productDescription":"iv, 19 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":159849,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1994/4071/report-thumb.jpg"},{"id":59143,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1994/4071/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a4ce4b07f02db626a1f","contributors":{"authors":[{"text":"Waltemeyer, S. D.","contributorId":65857,"corporation":false,"usgs":true,"family":"Waltemeyer","given":"S. D.","affiliations":[],"preferred":false,"id":203104,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
]}