{"pageNumber":"2114","pageRowStart":"52825","pageSize":"25","recordCount":68919,"records":[{"id":9454,"text":"ofr82699 - 1982 - A heat-pulse flowmeter for measuring minimal discharge rates in boreholes","interactions":[],"lastModifiedDate":"2012-02-02T00:06:17","indexId":"ofr82699","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","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":"82-699","title":"A heat-pulse flowmeter for measuring minimal discharge rates in boreholes","docAbstract":"The U.S. Geological Survey has tested a borehole-configured heat-pulse flowmeter which has good low-velocity flow-measuring sensitivity. The flowmeter was tested in the laboratory in 51-, 102-, and 152-millimeter-diameter columns using water velocities ranging from 0.35 to 250 millimeters per second. The heat-pulse flowmeter also was tested in a 15-meter-deep granite test pit with controlled water flow, and in a 58-meter-deep borehole in sedimentary materials. The flowmeter's capability to detect and measure naturally occurring, low-velocity, thermally induced convection currents in boreholes was demonstrated. Further improvements to the heat-pulse-flowmeter system are needed to increase its reliability and improve its response through four-conductor logging cable.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr82699","usgsCitation":"Hess, A., 1982, A heat-pulse flowmeter for measuring minimal discharge rates in boreholes: U.S. Geological Survey Open-File Report 82-699, iv, 44 p. ill. ;28 cm., https://doi.org/10.3133/ofr82699.","productDescription":"iv, 44 p. ill. ;28 cm.","costCenters":[],"links":[{"id":142763,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0699/report-thumb.jpg"},{"id":37159,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0699/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b24e4b07f02db6ae4ae","contributors":{"authors":[{"text":"Hess, A.E.","contributorId":71979,"corporation":false,"usgs":true,"family":"Hess","given":"A.E.","email":"","affiliations":[],"preferred":false,"id":159715,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":9484,"text":"ofr82404 - 1982 - Silver Plume Granite; possible source of uranium in sandstone uranium deposits, Tallahassee Creek and High Park areas, Fremont and Teller counties, Colorado","interactions":[],"lastModifiedDate":"2012-02-02T00:06:15","indexId":"ofr82404","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","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":"82-404","title":"Silver Plume Granite; possible source of uranium in sandstone uranium deposits, Tallahassee Creek and High Park areas, Fremont and Teller counties, Colorado","docAbstract":"Anomalously high concentrations of thorium and of the light rare earth elements lanthanum and cerium suggest that the actinides and light lanthanides were enriched to an abnormal degree by the magmatic processes that formed the Proterozoic Y Silver Plume Granite in areas adjoining Tallahassee Creek and High Park. However, no such enrichment is found in the Proterozoic X Boulder Creek Granodiorite. Although uranium presently does not appear to be significantly enriched in sampled outcrops of Silver Plume Granite, a large part of the original uranium content of Silver Plume may have been removed by oxidizing ground waters, leaving behind mainly the uranium bound in resistate minerals such as zircon and monazite. \r\n\r\nLead isotopic compositions of acid leachate from barren shale and sandstone associated with the Hansen uranium deposit (Tallahassee Creek area) indicate that (1) the predominant source of acid-soluble lead is 1410 m.y: old (Silver Plume age); (2) the source of the lead is characterized by Th/U around 1 (this ratio in the source may apply to soluble minerals only and may exclude thorium and uranium in resistate minerals), and the mean uranium content of this source may be as high as 30 ppm; and (3) at the time of sediment deposition, a paleohydrologic system existed that was capable of transporting Silver Plume lead and, therefore, Silver Plume uranium to the Hansen deposit. Although a significant contribution of uranium from Tertiary volcanic rocks cannot be ruled out and is even probable (Dickinson and Hills, 1982), it appears probable that some of the uranium in deposits of the Tallahassee Creek area was derived from Silver Plume Granite.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr82404","usgsCitation":"Hills, F., and Dickinson, K.A., 1982, Silver Plume Granite; possible source of uranium in sandstone uranium deposits, Tallahassee Creek and High Park areas, Fremont and Teller counties, Colorado: U.S. Geological Survey Open-File Report 82-404, ii, 26 p., maps ;28 cm., https://doi.org/10.3133/ofr82404.","productDescription":"ii, 26 p., maps ;28 cm.","costCenters":[],"links":[{"id":141908,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0404/report-thumb.jpg"},{"id":37192,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0404/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f9e4b07f02db5f3b7c","contributors":{"authors":[{"text":"Hills, F. A.","contributorId":22768,"corporation":false,"usgs":true,"family":"Hills","given":"F. A.","affiliations":[],"preferred":false,"id":159769,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Dickinson, K. A.","contributorId":77528,"corporation":false,"usgs":true,"family":"Dickinson","given":"K.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":159770,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":9508,"text":"ofr82733 - 1982 - A field study of large-scale oscillation ripples in a very coarse-grained, high-energy marine environment","interactions":[],"lastModifiedDate":"2012-02-02T00:06:11","indexId":"ofr82733","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","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":"82-733","title":"A field study of large-scale oscillation ripples in a very coarse-grained, high-energy marine environment","docAbstract":"Monastery Beach, Carmel, California is a pocket beach that sits within 200 m of the head of Carmel Submarine Canyon. Coarse to very coarse sand covers both the beach and adjacent shelf; in the latter area incoming waves have shaped the sand into large oscillation ripples. The accessibility of this area and a variable wave climate produce a unique opportunity to study large-scale coarse-grained ripples in a high-energy environment. These ripples, which only occur in very coarse sand, form under the intense, wave-generated currents that exist during storm conditions. Once formed, these ripples do not significantly change under lower energy waves. On three separate occasions scuba divers measured ripples and collected sand samples from ripple crests near fixed reference stakes along three transects. Ripple wavelength and grain size decreased with an increase in water depth. Sediment sorting was best closest to the surf zone and poorest at the rim of Carmel Canyon. Cobbles and gravel observed in ripple troughs represent lag deposits. \r\n\r\nCarmel Canyon refracts waves approaching Monastery Beach such that wave energy is focused towards the northern and southern portions of the beach, leaving the central part of the beach lower in energy. This energy distribution causes spatial variations in the ripples and grain sizes with the shortest wavelengths and smallest grain sizes being in the central part of the shelf.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr82733","usgsCitation":"Hirschaut, D., and Dingler, J., 1982, A field study of large-scale oscillation ripples in a very coarse-grained, high-energy marine environment: U.S. Geological Survey Open-File Report 82-733, 35 p., ill., maps ;28 cm., https://doi.org/10.3133/ofr82733.","productDescription":"35 p., ill., maps ;28 cm.","costCenters":[],"links":[{"id":140996,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0733/report-thumb.jpg"},{"id":37225,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0733/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b24e4b07f02db6aebb3","contributors":{"authors":[{"text":"Hirschaut, D.W.","contributorId":43761,"corporation":false,"usgs":true,"family":"Hirschaut","given":"D.W.","email":"","affiliations":[],"preferred":false,"id":159806,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Dingler, J.R.","contributorId":64247,"corporation":false,"usgs":true,"family":"Dingler","given":"J.R.","email":"","affiliations":[],"preferred":false,"id":159807,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":9550,"text":"ofr82514 - 1982 - Results of an aquifer test near Lynndyl, Utah","interactions":[],"lastModifiedDate":"2017-09-01T15:05:38","indexId":"ofr82514","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","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":"82-514","title":"Results of an aquifer test near Lynndyl, Utah","docAbstract":"<p>An aquifer test was conducted near Lynndyl, Utah, to determine the hydraulic characteristics of a deep artesian aquifer and its associated confining bed. A well completed in the aquifer was pulped continuously for 25 days and measurements of drawdown and recovery were made in 34 observation wells located within a 10-mile radius of the pumped well. Data from the tests were analyzed using the Hantush modified and Neuman and Witherspoon ratio methods for leaky confined aquifers in which the storage of water in the confining beds was taken into account.</p><p>The aquifer transmissivity was calculated to be 12,700 feet squared per day, and the storage coefficient was 6.4 x 10<sup>-5</sup>. Calculated average vertical hydraulic conductivity of the confining bed was about 6 x 10<sup>-3</sup> foot per day with the specific storage of the confining bed calculated to be 5.4 x 10<span id=\"_mce_caret\" data-mce-bogus=\"true\"><sup>-6</sup></span> per foot.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Salt Lake City, UT","doi":"10.3133/ofr82514","collaboration":"Prepared  in  cooperation  with  the Utah Department of Natural Resources and Energy, Division of Water Rights","usgsCitation":"Holmes, W.F., and Wilberg, D.E., 1982, Results of an aquifer test near Lynndyl, Utah: U.S. Geological Survey Open-File Report 82-514, Report: 17 p.; Plate: 12.96 in. x 14.24 in., https://doi.org/10.3133/ofr82514.","productDescription":"Report: 17 p.; Plate: 12.96 in. x 14.24 in.","numberOfPages":"15","costCenters":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":141683,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0514/report-thumb.jpg"},{"id":37279,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/0514/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":37280,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0514/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Utah","city":"Lynndyl","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a17e4b07f02db604828","contributors":{"authors":[{"text":"Holmes, Walter F.","contributorId":31737,"corporation":false,"usgs":true,"family":"Holmes","given":"Walter","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":159875,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Wilberg, Dale E.","contributorId":101275,"corporation":false,"usgs":true,"family":"Wilberg","given":"Dale","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":159876,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":9551,"text":"ofr811193 - 1982 - Low-flow characteristics of streams in the Lake Michigan basin, Wisconsin","interactions":[],"lastModifiedDate":"2023-12-14T22:04:15.454808","indexId":"ofr811193","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","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":"81-1193","title":"Low-flow characteristics of streams in the Lake Michigan basin, Wisconsin","docAbstract":"<p>Low-flow characteristics of streams in the Lake Michigan basin are presented. Included are estimates of low-flow frequency at 30 gaging stations, flow duration at 13 gaging stations, and selected low-flow frequency characteristics at 22 low-flow partial-record stations and 123 miscellaneous sites. Equations are provided to estimate low-flow characteristics at sites where one base-flow discharge measurement is available. The equations were determined from multiple-regression analyses that related low-flow characteristics at gaging stations and low-flow partial-record stations to basin characteristics. Drainage area and base-flow index were the most significant characteristics in explaining the variation in low flow for sites where one low base-flow measurement (flow durations greater than 80%) has been made. The equations and corresponding standard errors of estimate are computed. Low-flow characteristics are not well defined in the Lake Michigan basin. Standard errors for low-flow characteristics at gaging stations, low-flow partial-record stations, and miscellaneous sites are much higher than State averages. The standard errors for the regression equations are also very high. This is due in part to the flow of many streams in the basin approaching 0 ft/s during low base-flow periods. The graphical regression relation lines are steep for stations on these streams and the resulting standard errors are relatively high. (USGS).</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr811193","usgsCitation":"Holmstrom, B.K., 1982, Low-flow characteristics of streams in the Lake Michigan basin, Wisconsin: U.S. Geological Survey Open-File Report 81-1193, Report: v, 102 p.; 2 Plates: 12.50 x 29.00 inches, https://doi.org/10.3133/ofr811193.","productDescription":"Report: v, 102 p.; 2 Plates: 12.50 x 29.00 inches","numberOfPages":"114","onlineOnly":"N","additionalOnlineFiles":"Y","costCenters":[{"id":677,"text":"Wisconsin Water Science Center","active":true,"usgs":true}],"links":[{"id":37282,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1981/1193/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":37281,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1981/1193/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":37283,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1981/1193/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":141684,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1981/1193/report-thumb.jpg"},{"id":423592,"rank":5,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_11914.htm","linkFileType":{"id":5,"text":"html"}}],"scale":"500000","country":"United States","state":"Wisconsin","otherGeospatial":"Lake Michigan basin","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -86.956787109375,\n              45.506346901083425\n            ],\n            [\n              -87.374267578125,\n              45.27488643704894\n            ],\n            [\n              -87.64892578125,\n              44.879228141635274\n            ],\n            [\n              -87.890625,\n              44.67646564865964\n            ],\n            [\n              -88.06640625,\n              44.43377984606825\n            ],\n            [\n              -88.2861328125,\n              44.06390660801779\n            ],\n            [\n              -88.41796875,\n              43.73935207915473\n            ],\n            [\n              -88.516845703125,\n              43.50872101129684\n            ],\n            [\n              -88.494873046875,\n              43.43696596521823\n            ],\n            [\n              -88.4619140625,\n              43.03677585761058\n            ],\n            [\n              -88.29711914062499,\n              42.74701217318067\n            ],\n            [\n              -88.0224609375,\n              42.577354839557856\n            ],\n            [\n              -87.82470703125,\n              42.49640294093708\n            ],\n            [\n              -87.6708984375,\n              42.49640294093708\n            ],\n            [\n              -87.659912109375,\n              42.72280375732727\n            ],\n            [\n              -87.791748046875,\n              43.213183300738876\n            ],\n            [\n              -87.64892578125,\n              43.73935207915473\n            ],\n            [\n              -87.4951171875,\n              43.937461690316646\n            ],\n            [\n              -87.374267578125,\n              44.41808794374849\n            ],\n            [\n              -87.044677734375,\n              45.0502402697946\n            ],\n            [\n              -86.824951171875,\n              45.18978009667531\n            ],\n            [\n              -86.671142578125,\n              45.40616374516014\n            ],\n            [\n              -86.956787109375,\n              45.506346901083425\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a7ee4b07f02db64852d","contributors":{"authors":[{"text":"Holmstrom, B. K.","contributorId":90728,"corporation":false,"usgs":true,"family":"Holmstrom","given":"B.","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":159877,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":9558,"text":"ofr82866 - 1982 - Bedrock aquifers in the northern San Rafael Swell area, Utah, with special emphasis on the Navajo Sandstone","interactions":[{"subject":{"id":9558,"text":"ofr82866 - 1982 - Bedrock aquifers in the northern San Rafael Swell area, Utah, with special emphasis on the Navajo Sandstone","indexId":"ofr82866","publicationYear":"1982","noYear":false,"title":"Bedrock aquifers in the northern San Rafael Swell area, Utah, with special emphasis on the Navajo Sandstone"},"predicate":"SUPERSEDED_BY","object":{"id":70043865,"text":"70043865 - 1984 - Bedrock aquifers in the northern San Rafael Swell area, Utah, with special emphasis on the Navajo Sandstone","indexId":"70043865","publicationYear":"1984","noYear":false,"title":"Bedrock aquifers in the northern San Rafael Swell area, Utah, with special emphasis on the Navajo Sandstone"},"id":1}],"supersededBy":{"id":70043865,"text":"70043865 - 1984 - Bedrock aquifers in the northern San Rafael Swell area, Utah, with special emphasis on the Navajo Sandstone","indexId":"70043865","publicationYear":"1984","noYear":false,"title":"Bedrock aquifers in the northern San Rafael Swell area, Utah, with special emphasis on the Navajo Sandstone"},"lastModifiedDate":"2016-12-17T11:21:43","indexId":"ofr82866","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","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":"82-866","title":"Bedrock aquifers in the northern San Rafael Swell area, Utah, with special emphasis on the Navajo Sandstone","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr82866","usgsCitation":"Hood, J.W., and Patterson, D.J., 1982, Bedrock aquifers in the northern San Rafael Swell area, Utah, with special emphasis on the Navajo Sandstone: U.S. Geological Survey Open-File Report 82-866, https://doi.org/10.3133/ofr82866.","costCenters":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":141896,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"country":"United States","state":"Utah","county":"Carbon County, Emery County","otherGeospatial":"San Rafael Swell","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -110,\n              39.25\n            ],\n            [\n              -110,\n              38.5\n            ],\n            [\n              -110.5,\n              38.5\n            ],\n            [\n              -111,\n              38.95\n            ],\n            [\n              -110.7,\n              39.7\n            ],\n            [\n              -110,\n              39.25\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a6be4b07f02db63d8e3","contributors":{"authors":[{"text":"Hood, J. W.","contributorId":87908,"corporation":false,"usgs":true,"family":"Hood","given":"J.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":159888,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Patterson, Dale J.","contributorId":83122,"corporation":false,"usgs":true,"family":"Patterson","given":"Dale","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":159887,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":9598,"text":"ofr82109 - 1982 - Potential impacts of a proposed reservoir on hydrologic and water-quality conditions in Little Rush Creek watershed, Fairfield County, Ohio","interactions":[],"lastModifiedDate":"2012-02-02T00:06:14","indexId":"ofr82109","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","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":"82-109","title":"Potential impacts of a proposed reservoir on hydrologic and water-quality conditions in Little Rush Creek watershed, Fairfield County, Ohio","docAbstract":"Water-quality and discharge measurements were made at three sites on Indian Run and one site on Little Rush Creek between February and December, 1979. Indian Run was observed above and below the U.S. Soil Conservation Service Reservoir, VI-D. Little Rush Creek was observed 1.1 miles downstream from the proposed U.S. Soil Conservation Reservoir, VI-A, site. Data from the Indian Run sites were used to predict the potential water-quality conditions in and downstream from the proposed Little Rush Creek Reservoir. \r\n\r\nTemperatures measured in Indian Run at the reservoir outflow were as much as 4oc greater than those at the inflow. Dissolved-oxygen saturation ranged from 62 to 110 percent in the inflow and from 57 to 120 percent in the outflow. Indian Run and Little Push Creek are characterized by moderately hard to very hard calcium bicarbonate water. The concentration of dieldrin in water samples from both Little Rush Creek and the outflow from the reservoir on Indian Run was 0.01 micrograms per liter, and in reservoir-surface samples it was 0.02 micrograms per liter. Chlordane concentration in a bottom material sample from the reservoir was 26 micrograms per kilogram. Catfish taken from the reservoir contained 190 micrograms per kilogram chlordane. \r\n\r\nAll sites showed a good diversity in benthic invertebrate communities. Blue-green algal blooms occurred in the reservoir, indicating nutrient-enriched conditions. \r\n\r\nBecause of similarities in land use and watershed characteristics, water in the proposed reservoir VI-A is expected to be similar in quality to that of reservoir VI-D. The new reservoir will not significantly affect downstream water quality.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr82109","usgsCitation":"Hren, J., and Jones, R., 1982, Potential impacts of a proposed reservoir on hydrologic and water-quality conditions in Little Rush Creek watershed, Fairfield County, Ohio: U.S. Geological Survey Open-File Report 82-109, v, 67 p. :ill., map ;28 cm., https://doi.org/10.3133/ofr82109.","productDescription":"v, 67 p. :ill., map ;28 cm.","costCenters":[],"links":[{"id":142155,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0109/report-thumb.jpg"},{"id":37326,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/0109/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":37327,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/0109/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":37328,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/0109/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":37329,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0109/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac8e4b07f02db67c04f","contributors":{"authors":[{"text":"Hren, Janet","contributorId":69554,"corporation":false,"usgs":true,"family":"Hren","given":"Janet","email":"","affiliations":[],"preferred":false,"id":159977,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Jones, R.L.","contributorId":39785,"corporation":false,"usgs":true,"family":"Jones","given":"R.L.","email":"","affiliations":[],"preferred":false,"id":159976,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":9608,"text":"ofr82754 - 1982 - Ground-water data for Michigan, 1981","interactions":[],"lastModifiedDate":"2017-07-12T11:19:54","indexId":"ofr82754","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","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":"82-754","title":"Ground-water data for Michigan, 1981","docAbstract":"<p>This report summarizes data on water levels in 124 observation wells and provides information on well locations, depths, altitudes, and aquifers that they tap. Tabulated data include extremes of water levels for 1981 and for the period of record; pumpage of most major groundwater users in the State; and quality data on selected wells. The city of Lansing was the largest reported user of ground-water, pumping 8.6 billion gallons from the Saginaw Formation and glacial deposits.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Lansing, MI","doi":"10.3133/ofr82754","usgsCitation":"Huffman, G., 1982, Ground-water data for Michigan, 1981: U.S. Geological Survey Open-File Report 82-754, iv, 55 p., https://doi.org/10.3133/ofr82754.","productDescription":"iv, 55 p.","numberOfPages":"64","costCenters":[{"id":382,"text":"Michigan Water Science Center","active":true,"usgs":true}],"links":[{"id":141715,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0754/report-thumb.jpg"},{"id":343703,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0754/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United 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,{"id":9616,"text":"ofr82689 - 1982 - Data on subsurface storage of liquid waste near Pensacola, Florida, 1963-1980","interactions":[],"lastModifiedDate":"2012-02-02T00:06:15","indexId":"ofr82689","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","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":"82-689","title":"Data on subsurface storage of liquid waste near Pensacola, Florida, 1963-1980","docAbstract":"Since 1963, when industrial waste was first injected into the subsurface in northwest Florida, considerable data have been collected relating to the geochemistry of subsurface waste storage. This report presents hydrogeologic data on two subsurface waste storage. This report presents hydrogeologic data on two subsurface storage systems near Pensacola, Fla., which inject liquid industrial waste through deep wells into a saline aquifer. Injection sites are described giving a history of well construction, injection, and testing; geologic data from cores and grab samples; hydrographs of injection rates, volume, pressure, and water levels; and chemical and physical data from water-quality samples collected from injection and monitor wells. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr82689","usgsCitation":"Hull, R.W., and Martin, J., 1982, Data on subsurface storage of liquid waste near Pensacola, Florida, 1963-1980: U.S. Geological Survey Open-File Report 82-689, vii, 186 p., ill., maps ;28 cm., https://doi.org/10.3133/ofr82689.","productDescription":"vii, 186 p., ill., maps ;28 cm.","costCenters":[],"links":[{"id":141738,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0689/report-thumb.jpg"},{"id":37342,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0689/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac9e4b07f02db67c7d8","contributors":{"authors":[{"text":"Hull, R. W.","contributorId":66258,"corporation":false,"usgs":true,"family":"Hull","given":"R.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":160001,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Martin, J.B.","contributorId":32923,"corporation":false,"usgs":true,"family":"Martin","given":"J.B.","email":"","affiliations":[],"preferred":false,"id":160000,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":9624,"text":"ofr82554 - 1982 - Water resources program of the U.S. Geological Survey related to agriculture in Louisiana","interactions":[],"lastModifiedDate":"2012-02-02T00:06:15","indexId":"ofr82554","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","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":"82-554","title":"Water resources program of the U.S. Geological Survey related to agriculture in Louisiana","docAbstract":"Surveillance activities of the U.S. Geological Survey Louisiana District include long-term, hydrologic-data-collection sites that serve a current-purpose, management function and (or) that furnish a data base for interpretative studies. The proposed program for 1982 includes a network of 69 surface-water data sites (continuous gaging stations), 250 flood-data sites (crest-stage stations), 679 ground-water wells (water-level observation and water-quality monitor wells), and 138 water-quality sites. The geographic distribution of the data sites is shown in the report. Interpretive studies have objectives that are oriented toward a particular geographic area , to a particular set of hydrologic phenomena, or to obtain information for use in solving specific problems. Current studies of interest to agriculture include the following: (1) Flood hydraulics and hydrology, (2) Low-flow or base-flow of streams in Louisiana, (3) Hydrologic studies in southwestern Louisiana, (4) Hydrologic impacts of surface mining in northern Louisiana, (5) Sparta aquifer study, and (6) Limnology of freshwater lakes. A network of partial record sites is also maintained to monitor specific flows. Peak stages (crest stage) are only recorded at sites where flood information is of interest. At other sites, only the low-flow or base-flow recession is obtained for use in determining relations between ground water and surface water, to assess water supply, and for effluent studies. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr82554","usgsCitation":"Huntzinger, T., 1982, Water resources program of the U.S. Geological Survey related to agriculture in Louisiana: U.S. Geological Survey Open-File Report 82-554, iii, 22 p., ill., maps ;28 cm., https://doi.org/10.3133/ofr82554.","productDescription":"iii, 22 p., ill., maps ;28 cm.","costCenters":[],"links":[{"id":141762,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0554/report-thumb.jpg"},{"id":37355,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0554/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f3e4b07f02db5ef463","contributors":{"authors":[{"text":"Huntzinger, T.L.","contributorId":67503,"corporation":false,"usgs":true,"family":"Huntzinger","given":"T.L.","email":"","affiliations":[],"preferred":false,"id":160012,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":9663,"text":"ofr82570 - 1982 - Ground-water conditions in the eastern part of Michaud Flats, Fort Hall Indian Reservation, Idaho","interactions":[],"lastModifiedDate":"2012-02-02T00:06:09","indexId":"ofr82570","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","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":"82-570","title":"Ground-water conditions in the eastern part of Michaud Flats, Fort Hall Indian Reservation, Idaho","docAbstract":"The Michaud Flats study area occupies about 20 square miles on the Snake River Plain in southeastern Idaho: Ground-water resources are extensively developed for irrigation and industrial uses. The more productive wells are completed in the Pediment Gravel and the basalt flows of the Bighole Basalt and Starlight Formation and the sand and gravel of the Sunbeam Formation. A few shallow domestic wells are completed in the water-table aquifer in the Michaud Gravel. Historically, high levels of arsenic were observed in water from several wells completed in the shallow aquifer. In most wells and springs sampled during this study, levels of arsenic and other minor elements were within limits recommended by the U.S. Public Health Service. Heavy metal concentrations in one well completed in the shallow aquifer, and the concentration of arsenic exceeded the recommended limits. There is some evidence that arsenic, as well as several other minor elements, may occur in above-normal levels naturally in local ground water. Ground water used for irrigation generally has a low sodium-absorption ratio and can be used on almost all soils. All irrigation water sampled have a medium to high salinity hazard, and caution should be used when applying these waters on poorly drained soils. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr82570","usgsCitation":"Jacobson, N., 1982, Ground-water conditions in the eastern part of Michaud Flats, Fort Hall Indian Reservation, Idaho: U.S. Geological Survey Open-File Report 82-570, iv, 38 p., ill., maps ;28 cm., https://doi.org/10.3133/ofr82570.","productDescription":"iv, 38 p., ill., maps ;28 cm.","costCenters":[],"links":[{"id":140987,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0570/report-thumb.jpg"},{"id":37394,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0570/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aafe4b07f02db66d0fc","contributors":{"authors":[{"text":"Jacobson, N.D.","contributorId":105302,"corporation":false,"usgs":true,"family":"Jacobson","given":"N.D.","email":"","affiliations":[],"preferred":false,"id":160082,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":9693,"text":"ofr82262 - 1982 - Flood of October 8, 1977 in St. Croix, U.S. Virgin Islands","interactions":[],"lastModifiedDate":"2012-02-02T00:06:10","indexId":"ofr82262","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","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":"82-262","title":"Flood of October 8, 1977 in St. Croix, U.S. Virgin Islands","docAbstract":"Severe flooding throughout St. Croix, United States Virgin Islands occurred on October 8, 1977. A tropical storm moving across the island produced as much as 16 inches of precipitation. The most affected areas were near Frederiksted, Mon Bijou, and the Airport. The peak discharge of River Gut near the Airport was about 11,400 cubic feet per second. \r\n\r\nThe water depth in some urban areas exceeded 4.0 feet. Flood maps and flood profiles show the inundated areas near Frederiksted, Mon Bijou and the Airport.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr82262","usgsCitation":"Johnson, K.G., Carrasquillo, R., and Gonzalez, R., 1982, Flood of October 8, 1977 in St. Croix, U.S. Virgin Islands: U.S. Geological Survey Open-File Report 82-262, iv, 21 p. :ill., maps ;28 cm., https://doi.org/10.3133/ofr82262.","productDescription":"iv, 21 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":141013,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0262/report-thumb.jpg"},{"id":37412,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0262/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49efe4b07f02db5edb01","contributors":{"authors":[{"text":"Johnson, Karl G.","contributorId":7680,"corporation":false,"usgs":true,"family":"Johnson","given":"Karl","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":160137,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Carrasquillo, Ramon A.","contributorId":100815,"corporation":false,"usgs":true,"family":"Carrasquillo","given":"Ramon A.","affiliations":[],"preferred":false,"id":160139,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Gonzalez, Ralph","contributorId":82700,"corporation":false,"usgs":true,"family":"Gonzalez","given":"Ralph","email":"","affiliations":[],"preferred":false,"id":160138,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":9704,"text":"ofr82765 - 1982 - Mineralogy of fine-grained alluvium from borehole U11g, expl. 1, northern Frenchman Flat area, Nevada Test Site","interactions":[],"lastModifiedDate":"2012-02-02T00:06:21","indexId":"ofr82765","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","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":"82-765","title":"Mineralogy of fine-grained alluvium from borehole U11g, expl. 1, northern Frenchman Flat area, Nevada Test Site","docAbstract":"The mineralogy of matrix fines in alluvium from borehole Ullg, expl. 1, north of Frenchman Flat, Nevada Test Site, has been examined for evidence of past variations in water table elevation. Although greater abundance of zeolite and slightly more expanded basal spacings in smectite clays suggest effects of increased hydration of material up to 50 m above the present water table, these differences might also be related to provenance of environment of deposition. The relative uniformity of clay hydration properties in the 50 meters above the current water table suggest long-term stability near the present level. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr82765","usgsCitation":"Jones, B., 1982, Mineralogy of fine-grained alluvium from borehole U11g, expl. 1, northern Frenchman Flat area, Nevada Test Site: U.S. Geological Survey Open-File Report 82-765, iii, 13 p. :ill. ;28 cm., https://doi.org/10.3133/ofr82765.","productDescription":"iii, 13 p. :ill. ;28 cm.","costCenters":[],"links":[{"id":142354,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0765/report-thumb.jpg"},{"id":37417,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0765/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b05e4b07f02db699e24","contributors":{"authors":[{"text":"Jones, B.F.","contributorId":52156,"corporation":false,"usgs":true,"family":"Jones","given":"B.F.","email":"","affiliations":[],"preferred":false,"id":160157,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":9718,"text":"ofr82925 - 1982 - Directory of assistance centers of the National Water Data Exchange (NAWDEX)","interactions":[],"lastModifiedDate":"2012-02-02T00:06:22","indexId":"ofr82925","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","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":"82-925","title":"Directory of assistance centers of the National Water Data Exchange (NAWDEX)","docAbstract":"The National Water Data Exchange (NAWDEX), managed by the U.S. Geological Survey, has established a network of Assistance Centers throughout the United States and Puerto Rico to assist users of water data in identifying and locating the data they need. This Directory provides the information needed to contact any of the established Centers. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr82925","usgsCitation":"Josefson, B.M., and Blackwell, C.D., 1982, Directory of assistance centers of the National Water Data Exchange (NAWDEX): U.S. Geological Survey Open-File Report 82-925, iv, 35 p. ;28 cm., https://doi.org/10.3133/ofr82925.","productDescription":"iv, 35 p. ;28 cm.","costCenters":[],"links":[{"id":142330,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0925/report-thumb.jpg"},{"id":37463,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0925/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b32e4b07f02db6b462c","contributors":{"authors":[{"text":"Josefson, Beverly M.","contributorId":94306,"corporation":false,"usgs":true,"family":"Josefson","given":"Beverly","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":160178,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Blackwell, Cassandra D.","contributorId":25562,"corporation":false,"usgs":true,"family":"Blackwell","given":"Cassandra","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":160177,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":9732,"text":"ofr82373 - 1982 - Quality of water in Luxapallia Creek at Columbus, Mississippi","interactions":[],"lastModifiedDate":"2022-08-23T20:06:49.956171","indexId":"ofr82373","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","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":"82-373","title":"Quality of water in Luxapallia Creek at Columbus, Mississippi","docAbstract":"<p>A quality-of-water study was conducted on September 9-12, 1979, on Luxapallila Creek and its tributaries, Magby and McCrary Creeks. The short term study indicated that the water in Luxapallila, Magby, and McCrary Creeks is suitable for many purposes.</p><p>The dissolved-oxygen concentration, temperature, and pH of the water in Luxapallila Creek changed little downstream from site 1 to site 5. The mean specific conductance increased from 25 micromhos per centimeter at site 1 to 46 micromhos per centimeter at site 5. The concentrations of nitrogen and phosphorus species, densities of fecal bacteria and 5-day biochemical-oxygen-demand load in Luxapallila Creek also increased downstream.</p><p>The maximum BOD<sub>5</sub> increased from 0.7 mg/L at the upstream site to 2.6 mg/L at the most downstream site. The maximum total nitrogen concentration increased from 0.71 mg/L to 2.0 mg/L. The maximum ammonia nitrogen concentration increased from 0.08 mg/L to 0.50 mg/L. Maximum nitrate plus nitrite concentrations increased from 0.13 mg/L to 0.15 mg/L and the maximum organic nitrogen concentrations increased from 0.53 mg/L to 1.6 mg/L.</p><p>Maximum total phosphorus concentrations increased from 0.04 mg/L at the upstream site to 0.30 mg/L at the downstream site.</p><p>The fecal coliform to fecal streptococcus ratio of three of five samples collected at site 5 was greater than 4.0 strongly suggesting the presence of human wastes at the downstream sites during the study.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr82373","collaboration":"Prepared in cooperation with the Mississippi Department of Natural Resources Bureau of Pollution Control","usgsCitation":"Kalkhoff, S.J., 1982, Quality of water in Luxapallia Creek at Columbus, Mississippi: U.S. Geological Survey Open-File Report 82-373, v, 38 p., https://doi.org/10.3133/ofr82373.","productDescription":"v, 38 p.","costCenters":[],"links":[{"id":405490,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0373/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":143058,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0373/report-thumb.jpg"}],"country":"United States","state":"Mississippi","city":"Columbus","otherGeospatial":"Luxapallia Creek","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -88.44131469726562,\n              33.47154465603414\n            ],\n            [\n              -88.37127685546875,\n              33.47154465603414\n            ],\n            [\n              -88.37127685546875,\n              33.529947711130646\n            ],\n            [\n              -88.44131469726562,\n              33.529947711130646\n            ],\n            [\n              -88.44131469726562,\n              33.47154465603414\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a8be4b07f02db6516cb","contributors":{"authors":[{"text":"Kalkhoff, Stephen J. 0000-0003-4110-1716 sjkalkho@usgs.gov","orcid":"https://orcid.org/0000-0003-4110-1716","contributorId":1731,"corporation":false,"usgs":true,"family":"Kalkhoff","given":"Stephen","email":"sjkalkho@usgs.gov","middleInitial":"J.","affiliations":[{"id":35680,"text":"Illinois-Iowa-Missouri Water Science Center","active":true,"usgs":true},{"id":36532,"text":"Central Midwest Water Science Center","active":true,"usgs":true},{"id":351,"text":"Iowa Water Science Center","active":true,"usgs":true}],"preferred":true,"id":160202,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":9734,"text":"ofr82353 - 1982 - Specific conductance and dissolved chloride concentrations of freshwater aquifers and streams in petroleum producing areas in Mississippi","interactions":[],"lastModifiedDate":"2012-02-02T00:06:25","indexId":"ofr82353","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","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":"82-353","title":"Specific conductance and dissolved chloride concentrations of freshwater aquifers and streams in petroleum producing areas in Mississippi","docAbstract":"Specific conductance and dissolved chloride reconnasissance sampling was conducted in six oil-producing areas of Mississippi during periods of low streamflow in 1980 and 1981. Water samples were collected at 224 ground-water and 190 suface-water sites. Samples from 55 surface-water and 17 ground-water sites contained dissolved chloride concentrations in excess of 100 milligrams per liter. All data collected are presented in tables without interpretation. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr82353","usgsCitation":"Kalkhoff, S., 1982, Specific conductance and dissolved chloride concentrations of freshwater aquifers and streams in petroleum producing areas in Mississippi: U.S. Geological Survey Open-File Report 82-353, iv, 37 p. :maps ;28 cm., https://doi.org/10.3133/ofr82353.","productDescription":"iv, 37 p. :maps ;28 cm.","costCenters":[],"links":[{"id":143077,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0353/report-thumb.jpg"},{"id":37476,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0353/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a60e4b07f02db634dd0","contributors":{"authors":[{"text":"Kalkhoff, S. J.","contributorId":28967,"corporation":false,"usgs":true,"family":"Kalkhoff","given":"S. J.","affiliations":[],"preferred":false,"id":160204,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":9746,"text":"ofr811200 - 1982 - Analysis and characterization of urban storm-water runoff for selected basins in the Baltimore, Maryland, metropolitan area; a project plan","interactions":[],"lastModifiedDate":"2012-02-02T00:06:06","indexId":"ofr811200","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","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":"81-1200","title":"Analysis and characterization of urban storm-water runoff for selected basins in the Baltimore, Maryland, metropolitan area; a project plan","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr811200","usgsCitation":"Katz, B., and Fisher, G.T., 1982, Analysis and characterization of urban storm-water runoff for selected basins in the Baltimore, Maryland, metropolitan area; a project plan: U.S. Geological Survey Open-File Report 81-1200, iv, 58 p. ill., maps ;28 cm., https://doi.org/10.3133/ofr811200.","productDescription":"iv, 58 p. ill., maps ;28 cm.","costCenters":[],"links":[{"id":141587,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1981/1200/report-thumb.jpg"},{"id":37492,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1981/1200/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad0e4b07f02db680c5a","contributors":{"authors":[{"text":"Katz, B. G.","contributorId":82702,"corporation":false,"usgs":true,"family":"Katz","given":"B. G.","affiliations":[],"preferred":false,"id":160224,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Fisher, G. T.","contributorId":49359,"corporation":false,"usgs":true,"family":"Fisher","given":"G.","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":160223,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":9801,"text":"ofr81499 - 1982 - Ground-water pumpage in Nassau County, Long Island, New York, 1920-77: Introduction and user's guide to the data compilation","interactions":[],"lastModifiedDate":"2022-12-06T20:24:52.205511","indexId":"ofr81499","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","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":"81-499","title":"Ground-water pumpage in Nassau County, Long Island, New York, 1920-77: Introduction and user's guide to the data compilation","docAbstract":"<p>Pumpage data from about 2,100 wells used for public and nonpublic water-supply in Nassau County from 1920-77 have been collected and are available for public inspection at the U.S. Geological Survey office in Syosset, Nassau County. Except for wells in use before 1920, these data constitute the entire record available through 1977. The data are divided into two categories--pumpage from wells used for public supply, and pumpage from wells used mainly for industrial and commercial uses, designated as nonpublic water supply. Pumpage is tabulated by well or well field and is given by month or year with an annual total. The report serves as an introduction and user 's manual to the data, which are available for inspection but are not included in the report because they fill several hundred pages. The report describes the method of reporting pumpage on Long Island and how pumpage values were derived from the records. It also includes well-completion data and two maps showing the location of all wells.&nbsp;</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr81499","usgsCitation":"Kilburn, C., 1982, Ground-water pumpage in Nassau County, Long Island, New York, 1920-77: Introduction and user's guide to the data compilation: U.S. Geological Survey Open-File Report 81-499, Report: iii, 67 p.; 2 Plates: 27.15 × 38.08 inches and 27.15 × 37.65 inches, https://doi.org/10.3133/ofr81499.","productDescription":"Report: iii, 67 p.; 2 Plates: 27.15 × 38.08 inches and 27.15 × 37.65 inches","costCenters":[],"links":[{"id":410112,"rank":5,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_75499.htm","linkFileType":{"id":5,"text":"html"}},{"id":37576,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1981/0499/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":37575,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1981/0499/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":37574,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1981/0499/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":141786,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1981/0499/report-thumb.jpg"}],"country":"United States","state":"New York","county":"Nassau County","otherGeospatial":"Long Island","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -73.4167,\n              40.9167\n            ],\n            [\n              -73.7667,\n              40.9167\n            ],\n            [\n              -73.7667,\n              40.5833\n            ],\n            [\n              -73.4167,\n              40.5833\n            ],\n            [\n              -73.4167,\n              40.9167\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aa8e4b07f02db6673e5","contributors":{"authors":[{"text":"Kilburn, Chabot","contributorId":83499,"corporation":false,"usgs":true,"family":"Kilburn","given":"Chabot","email":"","affiliations":[],"preferred":false,"id":160321,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":9808,"text":"ofr82860 - 1982 - Geohydrologic reconnaissance of drainage wells in Florida; an interim report","interactions":[],"lastModifiedDate":"2012-02-02T00:06:15","indexId":"ofr82860","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","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":"82-860","title":"Geohydrologic reconnaissance of drainage wells in Florida; an interim report","docAbstract":"Drainage wells are used to inject surface waters directly into an aquifer, or shallow ground waters directly into a deeper aquifer, primarily by gravity. Such wells in Florida may be grouped into two broad types: (1) Surface-water injection wells, and (2) interaquifer connector wells. Surface-water injection wells are commonly used to supplement drainage for urban areas in karst terranes of central and north Florida. Data are available for 25 wells in the Ocala, Live Oak, and Orlando areas that allow comparison of the quality of water samples from these Floridan aquifer drainage wells with allowable contaminant levels. Comparison indicates that maximum contaminant levels for turbidity, color, and iron, manganese, and lead concentrations are equaled or exceeded in some drainage-well samples, and relatively high counts for coliform bacteria are present in most wells. Interaquifer connector wells are used in the phosphate mining areas of Polk and Hillsborough Counties, to drain mining operations and recharge the Floridan aquifer. Water-quality data available from 13 connector wells indicate that samples from most of these wells exceed standards values for iron concentration and turbidity. One well yielded a highly mineralized water, and samples from 6 of the other 12 wells exceed standards values for gross alpha concentrations. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr82860","usgsCitation":"Kimrey, J.O., and Fayard, L.D., 1982, Geohydrologic reconnaissance of drainage wells in Florida; an interim report: U.S. Geological Survey Open-File Report 82-860, iv, 63 p. :ill., maps ;28 cm., https://doi.org/10.3133/ofr82860.","productDescription":"iv, 63 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":141825,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0860/report-thumb.jpg"},{"id":37594,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0860/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1be4b07f02db6a8e28","contributors":{"authors":[{"text":"Kimrey, Joel O.","contributorId":96262,"corporation":false,"usgs":true,"family":"Kimrey","given":"Joel","email":"","middleInitial":"O.","affiliations":[],"preferred":false,"id":160335,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Fayard, Larry D.","contributorId":78326,"corporation":false,"usgs":true,"family":"Fayard","given":"Larry","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":160334,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":9846,"text":"ofr82556 - 1982 - Full-time equivalency tracking system","interactions":[],"lastModifiedDate":"2012-02-02T00:06:16","indexId":"ofr82556","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","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":"82-556","title":"Full-time equivalency tracking system","docAbstract":"To help meet the goals of the Surface-Mining Control and Reclamation Act of 1977, the U.S. Geological Survey is assessing the physical, chemical, and biological characteristics of surface water within the coal-mining region of southwestern Indiana. This report discussed benthic-invertebrate and periphytic-algal communities in streams draining homogeneous agricultural, forested, active/reclaimed-mine, and unreclaimed mine watersheds, and relates the biological communities to the physical and chemical characteristics of the streams. Alkalinity and pH were lower and the concentrations of dissolved solids, calcium, magnesium, sodium, potassium, sulfate, iron, manganese, aluminum, and zinc were higher in unreclaimed-mine watersheds than in the other land-use watersheds. Numbers and community diversity of benthic invertebrates were less at sites affected by mining than at agricultural or forested sites, owing to (1) synergistic effects of pH, metals, and unsuitable habitat and (2) lack of colonizing drift organisms because of the small drainage area upstream from the mined area. Only a few organisms , such as the caddisflies Cheumatopsyche and Hydrosyche and the chironomids Chironomus and Cricotopus were found in streams draining mine areas. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr82556","usgsCitation":"Klesert, S., 1982, Full-time equivalency tracking system: U.S. Geological Survey Open-File Report 82-556, 69 p, https://doi.org/10.3133/ofr82556.","productDescription":"69 p","costCenters":[],"links":[{"id":141909,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0556/report-thumb.jpg"},{"id":37633,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0556/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b32e4b07f02db6b4397","contributors":{"authors":[{"text":"Klesert, Stephen","contributorId":31769,"corporation":false,"usgs":true,"family":"Klesert","given":"Stephen","email":"","affiliations":[],"preferred":false,"id":160400,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":9881,"text":"ofr82307 - 1982 - Hydrotectonics; principles and relevance","interactions":[],"lastModifiedDate":"2012-02-02T00:06:10","indexId":"ofr82307","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","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":"82-307","title":"Hydrotectonics; principles and relevance","docAbstract":"Hydrotectonics combines the principles of hydraulics and rock mechanics. The hypothesis assumes that: (1) no faults are truly planar, (2) opposing noncongruent wavy wallrock surfaces form chambers and bottlenecks along the fault, and (3) most thrusting occurs beneath the water table. These physical constraints permit the following dynamics. \r\n\r\nShear displacement accompanying faulting must constantly change the volume of each chamber. Addition of ground water liquefies dry fault breccia to a heavy incompressible viscous muddy breccia I call fault slurry. When the volume of a chamber along a thrust fault decreases faster than its fault slurry can escape laterally, overpressurized slurry is hydraulically injected into the base of near-vertical fractures in the otherwise impervious overriding plate. Breccia pipes commonly form where such fissures intersect. \r\n\r\nAlternating decrease and increase in volume of the chamber subjects this injection slurry to reversible surges that not only raft and abrade huge clasts sporadically spalled from the walls of the conduit but also act as a forceful hydraulic ram which periodically widens the conduit and extends its top. If the pipe perforates a petroleum reservoir, leaking hydrocarbons float to its top. \r\n\r\nSudden faulting may generate a powerful water hammer that can be amplified at some distal narrow ends of the anastomosing plumbing system, where the shock may produce shatter cones. If vented on the Earth's surface, the muddy breccia, now called extrusion slurry, forms a mud volcano. \r\n\r\nThis hypothesis suggests that many highly disturbed features presently attributed to such catastrophic processes as subsurface explosions or meteorite impacts are due to the rheology of tectonic slurry in an intermittently reactivated pressure-relief tube rooted in a powerful reciprocating hydrotectonic pump activated by a long-lived deep-seated thrust fault.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr82307","usgsCitation":"Kopf, R.W., 1982, Hydrotectonics; principles and relevance: U.S. Geological Survey Open-File Report 82-307, 30 p., ill. ;28 cm., https://doi.org/10.3133/ofr82307.","productDescription":"30 p., ill. ;28 cm.","costCenters":[],"links":[{"id":140947,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0307/report-thumb.jpg"},{"id":37669,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0307/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac9e4b07f02db67c928","contributors":{"authors":[{"text":"Kopf, R. W.","contributorId":69544,"corporation":false,"usgs":true,"family":"Kopf","given":"R.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":160450,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":9892,"text":"ofr82173 - 1982 - Digital model evaluation of the predevelopment flow system of the Tertiary limestone aquifer, Southeast Georgia, Northeast Florida, and South South Carolina","interactions":[],"lastModifiedDate":"2016-12-14T12:25:00","indexId":"ofr82173","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","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":"82-173","title":"Digital model evaluation of the predevelopment flow system of the Tertiary limestone aquifer, Southeast Georgia, Northeast Florida, and South South Carolina","docAbstract":"A computer model using finite-difference techniques was used successfully to simulate the predevelopment flow regime within the multilayered Tertiary limestone aquifer system in Southeastern Georgia, Northeastern Florida, and Southern South Carolina as part of the U.S. Geological Survey 's Tertiary Limestone Regional Aquifer System analysis. The aquifer, of early Eocene to Miocene age, ranges from thin interbedded clastics and marl in the updip area to massive limestone and dolomite 1,500 feet thick in the downdip area. The aquifer is confined above by Miocene clay beds, and terminates at depth in low-permeability rocks or the saltwater interface. Model-simulated transmissivity of the upper permeable zone ranged from about 1 x 10 super 3 foot squared per day in the updip area and within parts of the Gulf Trough (a series of alinement basins filled by fine clastic in material) to about 1 x 10 super 6 foot squared per day in South Georgia, and area having large secondarily developed solution channels. The model results indicate that only about 540 cubic feet per second of water flowed through the predeveloped system, from the updip highland area of high altitude and in the areas north of Valdosta and southwest of Jacksonville, to discharge along streams in the updip area and diffuse upward leakage in the downdip area near the coast and offshore. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr82173","usgsCitation":"Krause, R.E., 1982, Digital model evaluation of the predevelopment flow system of the Tertiary limestone aquifer, Southeast Georgia, Northeast Florida, and South South Carolina: U.S. Geological Survey Open-File Report 82-173, 27 p, https://doi.org/10.3133/ofr82173.","productDescription":"27 p","costCenters":[{"id":13634,"text":"South Atlantic Water Science Center","active":true,"usgs":true}],"links":[{"id":141192,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"country":"United States","state":"Florida, Georgia, South 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 \"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a96e4b07f02db65aa0f","contributors":{"authors":[{"text":"Krause, Richard E.","contributorId":40185,"corporation":false,"usgs":true,"family":"Krause","given":"Richard","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":160470,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":9906,"text":"ofr82121 - 1982 - Statistical summaries of water-quality data for two coal areas of Jackson County, Colorado","interactions":[],"lastModifiedDate":"2012-02-02T00:06:18","indexId":"ofr82121","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","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":"82-121","title":"Statistical summaries of water-quality data for two coal areas of Jackson County, Colorado","docAbstract":"Statistical summaries of water-quality data are compiled for eight streams in two separate coal areas of Jackson County, Colo. The quality-of-water data were collected from October 1976 to September 1980. For inorganic constituents, the maximum, minimum, and mean concentrations, as well as other statistics are presented; for minor elements, only the maximum, minimum, and mean values are included. Least-squares equations (regressions) are also given relating specific conductance of the streams to the concentration of the major ions. The observed range of specific conductance was 85 to 1,150 micromhos per centimeter for the eight sites. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr82121","usgsCitation":"Kuhn, G., 1982, Statistical summaries of water-quality data for two coal areas of Jackson County, Colorado: U.S. Geological Survey Open-File Report 82-121, iv, 27 p. :maps ;28 cm., https://doi.org/10.3133/ofr82121.","productDescription":"iv, 27 p. :maps ;28 cm.","costCenters":[],"links":[{"id":142914,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0121/report-thumb.jpg"},{"id":37698,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0121/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49dce4b07f02db5e132f","contributors":{"authors":[{"text":"Kuhn, Gerhard","contributorId":102080,"corporation":false,"usgs":true,"family":"Kuhn","given":"Gerhard","email":"","affiliations":[],"preferred":false,"id":160491,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":9908,"text":"ofr82260 - 1982 - Quality of surface waters in Wilton, Connecticut","interactions":[],"lastModifiedDate":"2012-02-02T00:06:19","indexId":"ofr82260","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","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":"82-260","title":"Quality of surface waters in Wilton, Connecticut","docAbstract":"Water, bed material, and biological samples were collected and analyzed at 10 surface-water gaging sites on six streams in the town of Wilton, Connecticut over a 2-year period. The data indicate fair to excellent water quality. Fecal coliform bacteria, pH, alkalinity, iron, and manganese are the parameters that most often exceed recommended limits established by either the U. S. Environmental Protection Agency or the Connecticut Department of Environmental Protection. Data from sites on the Norwalk and East Branch Silvermine Rivers indicate little if any undesirable changes in water quality take place as they flow through the study area. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr82260","usgsCitation":"Kulp, K., 1982, Quality of surface waters in Wilton, Connecticut: U.S. Geological Survey Open-File Report 82-260, iv, 55 p. :maps ;28 cm., https://doi.org/10.3133/ofr82260.","productDescription":"iv, 55 p. :maps ;28 cm.","costCenters":[],"links":[{"id":142697,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0260/report-thumb.jpg"},{"id":37700,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0260/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adce4b07f02db686837","contributors":{"authors":[{"text":"Kulp, K.P.","contributorId":49791,"corporation":false,"usgs":true,"family":"Kulp","given":"K.P.","email":"","affiliations":[],"preferred":false,"id":160493,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":9909,"text":"ofr82868 - 1982 - Geohydrologic data from sandstone aquifers in southwestern Kansas","interactions":[],"lastModifiedDate":"2012-02-02T00:06:19","indexId":"ofr82868","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","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":"82-868","title":"Geohydrologic data from sandstone aquifers in southwestern Kansas","docAbstract":"Data collected during a reconnaissance investigation of the geology and hydrology of sandstone aquifers provide useful information in the study of, and planning for, water-resources development in a 17,400 square-mile area in 26 counties of southwestern Kansas. The aquifers consist chiefly of saturated sandstones that occur in Upper Permian, Upper Jurassic, and Lower and Upper Cretaceous rocks. In parts of southwestern Kansas, the sandstone aquifers already serve as the principal or secondary source of ground water for irrigation and other uses. Data indicate that water may be available for development in sandstone aquifers in other parts of the study area. In still other areas, water from wells in sandstone aquifers may not be of a suitable quality for some purposes. The data provided include records of selected wells, lithologic logs of test holes and wells, selected formation surfaces and sandstone thicknesses , chemical analyses of water from selected wells, and water levels in observation wells. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr82868","usgsCitation":"Kume, J., and Spinazola, J.M., 1982, Geohydrologic data from sandstone aquifers in southwestern Kansas: U.S. Geological Survey Open-File Report 82-868, iii, 116 p. :ill., maps ;28 cm., https://doi.org/10.3133/ofr82868.","productDescription":"iii, 116 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":142698,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0868/report-thumb.jpg"},{"id":37701,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0868/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae1e4b07f02db688814","contributors":{"authors":[{"text":"Kume, Jack","contributorId":100843,"corporation":false,"usgs":true,"family":"Kume","given":"Jack","email":"","affiliations":[],"preferred":false,"id":160494,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Spinazola, Joseph M.","contributorId":102044,"corporation":false,"usgs":true,"family":"Spinazola","given":"Joseph","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":160495,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
]}