TCE (trichloroethylene) in concentrations that may be hazardous to health occurs in the water of an ice-contact largely sand and gravel aquifer (called the main aquifer) underlying much of the PAFB (Pease Air Force Base). In 1977 and 1978, the highest TCE concentration was found surrounding the most productive well, Haven well. Large quantities of TCE were used for degreasing between 1955 and 1965 and, so far as is known, TCE was used extensively up until 1973. Data on how, where, and when TCE got into the aquifer are lacking, but geochemical evidence and TCE analyses show a strong relation between the high TCE concentrations near Haven well and the extensive storm-drain system that underlies the parking apron and runway. The drains help recycle some of the TCE-contaminated ground water from the Haven well area.
Sources of TCE-free ground water on PAFB may exist in the northern parts and do exist in the southern parts of the main aquifer; however, in the southern part, either the ground water is probably already being used nearly to capacity (Smith and Harrison production wells) or further development might adversely affect off-base ground-water use. In the northern part, available subsurface data indicate that only relatively small yields are likely at any one site; thus, to get sustained yields comparable to that of the Haven well would probably require an unreasonable number of wells.
This study locates TCE contamination in the main PAFB aquifer and discusses three possible water-use alternatives: (I) Abandonment of Haven well, (2) treatment of Haven well water to remove TCE, and (3) treatment of a portion of Haven well water for domestic consumption and use of the remainder for nondomestic uses. Continued use of the Haven well, with treatment of all or part of its yield for TCE removal, is advantageous, both because the Haven well is a high-yield source of water and because cessation of pumping from it might allow TCE-contaminated ground water to move downgradient (southward), endangering the Smith and Harrison production wells. Continued study and monitoring of the TCE contamination would help in predicting when the contamination problem will no longer be threatening.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr80557","collaboration":"Prepared in cooperation with the U.S. Air Force","usgsCitation":"Bradley, E., 1982, Trichloroethylene in the ground-water supply of Pease Air Force Base, Portsmouth, New Hampshire: U.S. Geological Survey Open-File Report 80-557, Report: iv, 22 p.; 8 Plates: 12.40 x 10.18 inches or smaller, https://doi.org/10.3133/ofr80557.","productDescription":"Report: iv, 22 p.; 8 Plates: 12.40 x 10.18 inches or smaller","costCenters":[],"links":[{"id":427001,"rank":10,"type":{"id":29,"text":"Figure"},"url":"https://pubs.usgs.gov/of/1980/0557/figure-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":427000,"rank":9,"type":{"id":29,"text":"Figure"},"url":"https://pubs.usgs.gov/of/1980/0557/figure-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":426999,"rank":8,"type":{"id":29,"text":"Figure"},"url":"https://pubs.usgs.gov/of/1980/0557/figure-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":426998,"rank":7,"type":{"id":29,"text":"Figure"},"url":"https://pubs.usgs.gov/of/1980/0557/figure-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":426997,"rank":6,"type":{"id":29,"text":"Figure"},"url":"https://pubs.usgs.gov/of/1980/0557/figure-5.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":426996,"rank":5,"type":{"id":29,"text":"Figure"},"url":"https://pubs.usgs.gov/of/1980/0557/figure-6.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":426995,"rank":4,"type":{"id":29,"text":"Figure"},"url":"https://pubs.usgs.gov/of/1980/0557/figure-7.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":426994,"rank":3,"type":{"id":29,"text":"Figure"},"url":"https://pubs.usgs.gov/of/1980/0557/figure-8.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":426993,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1980/0557/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":141499,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1980/0557/report-thumb.jpg"}],"country":"United States","state":"New Hampshire","city":"Portsmouth","otherGeospatial":"Pease Air Force Base","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -70.82239490389902,\n 43.10272920652986\n ],\n [\n -70.82239490389902,\n 43.015435633341184\n ],\n [\n -70.69191552120652,\n 43.015435633341184\n ],\n [\n -70.69191552120652,\n 43.10272920652986\n ],\n [\n -70.82239490389902,\n 43.10272920652986\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a49e4b07f02db6247d5","contributors":{"authors":[{"text":"Bradley, Edward","contributorId":67071,"corporation":false,"usgs":true,"family":"Bradley","given":"Edward","email":"","affiliations":[],"preferred":false,"id":157011,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":26734,"text":"wri824009 - 1982 - Hydrology of coal-resource areas in the southern Wasatch Plateau, central Utah","interactions":[],"lastModifiedDate":"2012-02-02T00:08:37","indexId":"wri824009","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","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":"82-4009","title":"Hydrology of coal-resource areas in the southern Wasatch Plateau, central Utah","docAbstract":"The study defines the surface and groundwater hydrology of coal-resources areas in the Southern Wasatch Plateau in Central Utah and, where possible, predicts the hydrologic impacts of underground mining. Discharge data at four streamflow gaging stations indicated that from 5 to 29% of the average annual precipitation on a drainage runs off streams, mainly during the snowmelt period (spring and summer). Most of the base flow of streams originates as spring discharge in the higher altitudes of drainages. Peak flows, average 7-day flood flows, and flood depths were related to basin characteristics in order to develop flood equations for ungaged sites. Chemical quality of surface water was suitable for most uses. Dissolved-solids concentrations ranged from 97 to 835 milligrams per liter in 61 samples collected throughout the area. Data from wells and coal-test holes, and a comprehensive spring inventory indicate that groundwater occurs in all geologic units exposed in the study area. The coal-bearing Blackhawk Formation and underlying Star Point Sandstone are saturated in most areas. Some future mining operations would require dewatering of the Star Point-Blackhawk aquifer. Most of the springs issue from the Flagstaff Limestone and North Horn Formation above the Star Point-Blackhawk aquifer. It is not known whether water in the Flagstaff and North Horn is perched. Dissolved-solids concentrations in groundwater ranged from 105 to 1,080 milligrams per liter in 87 analyzed samples. Water levels in wells, the discharge of springs, benthic invertebrates in streams, and quantity and quality of mine effluents all need to be monitored in order to detect changes in the hydrologic system caused by coal mining. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri824009","usgsCitation":"Danielson, T.W., and Sylla, D., 1982, Hydrology of coal-resource areas in the southern Wasatch Plateau, central Utah: U.S. Geological Survey Water-Resources Investigations Report 82-4009, vi, 71 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri824009.","productDescription":"vi, 71 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":123766,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1982/4009/report-thumb.jpg"},{"id":55610,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1982/4009/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":55611,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1982/4009/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":55612,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1982/4009/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":55613,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1982/4009/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a13e4b07f02db601f43","contributors":{"authors":[{"text":"Danielson, T. W.","contributorId":48590,"corporation":false,"usgs":true,"family":"Danielson","given":"T.","middleInitial":"W.","affiliations":[],"preferred":false,"id":196908,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Sylla, D.A.","contributorId":26333,"corporation":false,"usgs":true,"family":"Sylla","given":"D.A.","email":"","affiliations":[],"preferred":false,"id":196907,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":28216,"text":"wri824048 - 1982 - Time of travel of selected Arkansas streams","interactions":[],"lastModifiedDate":"2012-02-02T00:08:52","indexId":"wri824048","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","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":"82-4048","title":"Time of travel of selected Arkansas streams","docAbstract":"Between 1971 and 1981, time-of-travel and dispersion measurements were made in 15 streams in Arkansas. Most of the streams studied were at or near base flow. Graphs are presented for predicting traveltime of solutes in segments of the streams studied. The relationship of time of passage and peak unit concentration to traveltime is presented for two of the streams. Examples of use and application of the data are given. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri824048","usgsCitation":"Lamb, T., 1982, Time of travel of selected Arkansas streams: U.S. Geological Survey Water-Resources Investigations Report 82-4048, v, 64 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri824048.","productDescription":"v, 64 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":159652,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1982/4048/report-thumb.jpg"},{"id":57050,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1982/4048/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b05e4b07f02db699c84","contributors":{"authors":[{"text":"Lamb, T.E.","contributorId":58272,"corporation":false,"usgs":true,"family":"Lamb","given":"T.E.","email":"","affiliations":[],"preferred":false,"id":199410,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":48795,"text":"ofr82694 - 1982 - Submersed aquatic vegetation in the tidal Potomac River and Estuary of Maryland, Virginia and the District of Columbia; Hydrologic data report, May, 1978 to November, 1981","interactions":[],"lastModifiedDate":"2012-02-02T00:10:22","indexId":"ofr82694","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":"82-694","title":"Submersed aquatic vegetation in the tidal Potomac River and Estuary of Maryland, Virginia and the District of Columbia; Hydrologic data report, May, 1978 to November, 1981","language":"ENGLISH","doi":"10.3133/ofr82694","usgsCitation":"Paschal, J.E., Miller, D.R., Bartow, N.C., and Carter, V., 1982, Submersed aquatic vegetation in the tidal Potomac River and Estuary of Maryland, Virginia and the District of Columbia; Hydrologic data report, May, 1978 to November, 1981: U.S. Geological Survey Open-File Report 82-694, 220 p., https://doi.org/10.3133/ofr82694.","productDescription":"220 p.","costCenters":[],"links":[{"id":169706,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0694/report-thumb.jpg"},{"id":85626,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0694/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b05e4b07f02db699b89","contributors":{"authors":[{"text":"Paschal, James E. Jr.","contributorId":45768,"corporation":false,"usgs":true,"family":"Paschal","given":"James","suffix":"Jr.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":238272,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Miller, Darin R.","contributorId":64713,"corporation":false,"usgs":true,"family":"Miller","given":"Darin","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":238274,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Bartow, Nancy C.","contributorId":56203,"corporation":false,"usgs":true,"family":"Bartow","given":"Nancy","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":238273,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Carter, Virginia","contributorId":12018,"corporation":false,"usgs":true,"family":"Carter","given":"Virginia","email":"","affiliations":[],"preferred":false,"id":238271,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":48794,"text":"ofr82292 - 1982 - Preliminary study of methods for upgrading USGS Antarctic seismological capability","interactions":[],"lastModifiedDate":"2018-07-23T10:26:25","indexId":"ofr82292","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":"82-292","title":"Preliminary study of methods for upgrading USGS Antarctic seismological capability","docAbstract":"The purpose of this study is to evaluate potential methods for obtaining higher quality seismic data from Antarctica. Currently, USGS-sponsored WWSSN stations are located at Scott Base, Sanae Base, and at South Pole Station. Scott and Sanae Stations are located near the coast; data obtained from coastal installations are normally degraded by noise generated by ocean wave action on the coast. Operations at South Pole are rather difficult because of the severe environmental characteristics and the extended logistics which are required to provide supplies and operating personnel to its remote location. Short-period data quality from Pole Station has been moderately high with a short-period magnification of 100K at 1Hz.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr82292","usgsCitation":"Holcomb, L.G., 1982, Preliminary study of methods for upgrading USGS Antarctic seismological capability: U.S. Geological Survey Open-File Report 82-292, 43 p., https://doi.org/10.3133/ofr82292.","productDescription":"43 p.","costCenters":[{"id":122,"text":"Albuquerque Seismological Laboratory","active":false,"usgs":true}],"links":[{"id":9710,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0292/ofr82-292.pdf","size":"2131","linkFileType":{"id":1,"text":"pdf"}},{"id":169705,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0292/coverthb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b07e4b07f02db69ade2","contributors":{"authors":[{"text":"Holcomb, L. Gary","contributorId":26308,"corporation":false,"usgs":true,"family":"Holcomb","given":"L.","email":"","middleInitial":"Gary","affiliations":[],"preferred":false,"id":238270,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":1719,"text":"wsp2079 - 1982 - An annotated key to the identification of commonly occurring and dominant genera of algae observed in the phytoplankton of the United States","interactions":[],"lastModifiedDate":"2012-02-02T00:05:15","indexId":"wsp2079","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":341,"text":"Water Supply Paper","code":"WSP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"2079","title":"An annotated key to the identification of commonly occurring and dominant genera of algae observed in the phytoplankton of the United States","docAbstract":"In early 1979, a retrieval was made for all phytoplankton data contained in the computerized data file of the U. S. Geological Survey. The retrieval revealed the analytical results of 17,959 samples collected and processed between October 1973 and October 1978. Of the approximately 500 genera of freshwater algae reported in the United States, the U.S. Geological Survey observed 321 genera in the phytoplankton. Fifty-two genera were considered to be commonly occurring and 42 genera were considered to be community dominants. The report lists, describes, and provides a detailed taxonomic key to the identification of 58 genera of algae considered either commonly occurring or dominant. Also included is a summary of environmental conditions under which each algal genus was observed, as well as a glossary and an extensive list of selected references.","language":"ENGLISH","publisher":"U.S. G.P.O.,","doi":"10.3133/wsp2079","usgsCitation":"Greeson, P.E., 1982, An annotated key to the identification of commonly occurring and dominant genera of algae observed in the phytoplankton of the United States: U.S. Geological Survey Water Supply Paper 2079, vi, 138 p. :ill. ;24 cm., https://doi.org/10.3133/wsp2079.","productDescription":"vi, 138 p. :ill. ;24 cm.","costCenters":[],"links":[{"id":136941,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/2079/report-thumb.jpg"},{"id":26807,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/2079/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adae4b07f02db685770","contributors":{"authors":[{"text":"Greeson, Phillip E.","contributorId":25556,"corporation":false,"usgs":true,"family":"Greeson","given":"Phillip","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":144012,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":46847,"text":"ofr82631 - 1982 - Drainage divides, Massachusetts; Blackstone and Thames River basins","interactions":[],"lastModifiedDate":"2012-02-02T00:10:59","indexId":"ofr82631","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":"82-631","title":"Drainage divides, Massachusetts; Blackstone and Thames River basins","docAbstract":"Drainage boundaries for selected subbasins of the Blackstone and Thames River basins in eastern Hampden, eastern Hampshire, western Norfolk, southern Middlesex, and southern Worcester Counties, Massachusetts, are delineated on 12 topographic quadrangle maps at a scale of 1:24,000. Drainage basins are shown for all U.S. Geological Survey data-collection sites and for mouths of major rivers. Drainage basins are shown for the outlets of lakes or ponds and for streams where the drainage area is greater than 3 square miles. Successive sites along watercourses are indicated where the intervening area is at least 6 miles on tributary streams or 15 square miles along the Blackstone River, French River, or Quinebaug River. (USGS)","language":"ENGLISH","doi":"10.3133/ofr82631","usgsCitation":"Krejmas, B.E., and Wandle, S.W., 1982, Drainage divides, Massachusetts; Blackstone and Thames River basins: U.S. Geological Survey Open-File Report 82-631, 12 maps ;58 x 43 cm., https://doi.org/10.3133/ofr82631.","productDescription":"12 maps ;58 x 43 cm.","costCenters":[],"links":[{"id":168907,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a61e4b07f02db635df6","contributors":{"authors":[{"text":"Krejmas, Bruce E.","contributorId":102501,"corporation":false,"usgs":true,"family":"Krejmas","given":"Bruce","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":234188,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Wandle, S. William","contributorId":95862,"corporation":false,"usgs":true,"family":"Wandle","given":"S.","email":"","middleInitial":"William","affiliations":[],"preferred":false,"id":234187,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":48796,"text":"ofr82702 - 1982 - A note on transients in the SRO and ASRO long-period data","interactions":[],"lastModifiedDate":"2018-07-17T11:04:14","indexId":"ofr82702","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":"82-702","title":"A note on transients in the SRO and ASRO long-period data","docAbstract":"Data users have occasionally observed pulse-like transients in the long-period waveforms recorded at the Seismic Research Observatories (SRO) and at the Modified High-Gain Long-Period (ASRO) stations. In a recent paper, Dziewonski et al (1981) reported transients associated with earthquake signals record at some SRO stations, and the authors ascribed these transients to an unpredictable nonlinear system response. While some transients in the SRO and ASRO data are indeed generated by a nonlinear response (clipping), others are the result of linear processes. All event-associated transients are predictable in the sense that they are produced by large impulsive body-wave signals.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr82702","usgsCitation":"Peterson, J., 1982, A note on transients in the SRO and ASRO long-period data: U.S. Geological Survey Open-File Report 82-702, 20 p., https://doi.org/10.3133/ofr82702.","productDescription":"20 p.","costCenters":[{"id":122,"text":"Albuquerque Seismological Laboratory","active":false,"usgs":true}],"links":[{"id":169707,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0702/coverthb.jpg"},{"id":9712,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0702/ofr82-702.pdf","text":"Report","size":"584 kB","linkFileType":{"id":1,"text":"pdf"},"description":"OFR 1982-0702"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53cd495ee4b0b290850ef1bd","contributors":{"authors":[{"text":"Peterson, Jon","contributorId":67522,"corporation":false,"usgs":true,"family":"Peterson","given":"Jon","affiliations":[],"preferred":false,"id":238275,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":20415,"text":"ofr82696 - 1982 - Hydrologic data from Naval Oil Shale Reserves, Parachute Creek basin, northwestern Colorado, 1975-79","interactions":[],"lastModifiedDate":"2012-02-02T00:07:39","indexId":"ofr82696","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":"82-696","title":"Hydrologic data from Naval Oil Shale Reserves, Parachute Creek basin, northwestern Colorado, 1975-79","docAbstract":"This report summarizes data collected by the U.S. Geological Survey for the U.S. Department of Energy, Naval Petroleum, and Oil Shale Reserves in the Parachute Creek drainage basin of western Colorado. It includes data from five surface-water gages, two automatic sediment samplers and two water-quality monitors. Instantaneous streamflow measurements were made at 63 sites on Parachute Creek tributaries to determine gain or loss of flow. Thirteen springs and nine surface-water sites were sampled and chemical analyses of these sites are included. From 1975 to 1979, 88 spring sites were inventoried; conductivity, temperature, pH, and discharge were measured. Climate data include maximum, minimum, and total daily solar radiation. Daily total precipitation is reported for three stations and snow-course data is reported for one site.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr82696","usgsCitation":"Patt, R.O., Adams, D.B., and Collins, D.L., 1982, Hydrologic data from Naval Oil Shale Reserves, Parachute Creek basin, northwestern Colorado, 1975-79: U.S. Geological Survey Open-File Report 82-696, v, 134 p. :ill., maps ;28 cm., https://doi.org/10.3133/ofr82696.","productDescription":"v, 134 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":152090,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0696/report-thumb.jpg"},{"id":49957,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0696/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a1be4b07f02db6077cc","contributors":{"authors":[{"text":"Patt, Ralph O.","contributorId":61450,"corporation":false,"usgs":true,"family":"Patt","given":"Ralph","email":"","middleInitial":"O.","affiliations":[],"preferred":false,"id":182611,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Adams, D. Briane","contributorId":35707,"corporation":false,"usgs":true,"family":"Adams","given":"D.","email":"","middleInitial":"Briane","affiliations":[],"preferred":false,"id":182610,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Collins, Dannie L.","contributorId":77925,"corporation":false,"usgs":true,"family":"Collins","given":"Dannie","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":182612,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":60924,"text":"mf1482 - 1982 - Sections showing biostratigraphy and correlation of Tertiary rocks penetrated in wells drilled on the southern Oregon continental margin","interactions":[],"lastModifiedDate":"2016-08-23T09:35:23","indexId":"mf1482","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":325,"text":"Miscellaneous Field Studies Map","code":"MF","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1482","title":"Sections showing biostratigraphy and correlation of Tertiary rocks penetrated in wells drilled on the southern Oregon continental margin","docAbstract":"Geologic interpretation of seismic reflection profiles on the Continental Shelves of Oregon and Washington is measurably enhanced through the knowledge of Tertiary subsurface stratigraphy penetrated in 10 deep exploration wells drilled in the mid-1960's (Braislin and others, 1971; Snavely and others, 1977). These subsurface data make it possible to relate to the acoustic units differentiated on seismic-reflection profiles to time-stratigraphic units as determined from micropalentontological studies of samples collected from these wells. These biostratigraphic data also permit correlations between time-stratigraphic units in the offshore test wells and between those units and formations penetrated in onshore test wells, as well as strata that crop out in coastal Oregon and Washington.
","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/mf1482","usgsCitation":"Snavely, P.D., Wagner, H.C., and Rau, W.W., 1982, Sections showing biostratigraphy and correlation of Tertiary rocks penetrated in wells drilled on the southern Oregon continental margin: U.S. Geological Survey Miscellaneous Field Studies Map 1482, 41.71 x 35.10 inches, https://doi.org/10.3133/mf1482.","productDescription":"41.71 x 35.10 inches","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":179829,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/mf1482.PNG"},{"id":327513,"rank":1,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mf/1482/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"20000","country":"United States","state":"Oregon","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -125,43 ], [ -125,45 ], [ -124,45 ], [ -124,43 ], [ -125,43 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0be4b07f02db5fc193","contributors":{"authors":[{"text":"Snavely, P. D. Jr.","contributorId":22770,"corporation":false,"usgs":true,"family":"Snavely","given":"P.","suffix":"Jr.","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":264626,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Wagner, H. C.","contributorId":95033,"corporation":false,"usgs":true,"family":"Wagner","given":"H.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":264628,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Rau, W. W.","contributorId":71963,"corporation":false,"usgs":true,"family":"Rau","given":"W.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":264627,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":56887,"text":"wdrMT812 - 1982 - Water resources data Montana, water year 1981; Volume 2, Columbia River basin","interactions":[],"lastModifiedDate":"2020-05-06T15:22:17.754884","indexId":"wdrMT812","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":340,"text":"Water Data Report","code":"WDR","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"MT-81-2","title":"Water resources data Montana, water year 1981; Volume 2, Columbia River basin","docAbstract":"No abstract available.
","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wdrMT812","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1982, Water resources data Montana, water year 1981; Volume 2, Columbia River basin: U.S. Geological Survey Water Data Report MT-81-2, viii, 174 p., https://doi.org/10.3133/wdrMT812.","productDescription":"viii, 174 p.","costCenters":[],"links":[{"id":184811,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"country":"United 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\"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a01e4b07f02db5f7ee2","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":532974,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":25398,"text":"wri8256 - 1982 - Aquatic biology in Nederlo Creek, southwestern Wisconsin","interactions":[],"lastModifiedDate":"2015-10-19T16:01:43","indexId":"wri8256","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","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":"82-56","title":"Aquatic biology in Nederlo Creek, southwestern Wisconsin","docAbstract":"This report presents the results of biologic investigations by the U.S. Geological Survey and the Wisconsin Department of Natural Resources during a study of hydrology and water quality in a small drainage basin in the \"Driftless Area\" of southwest Wisconsin. The investigation included aquatic macrophytes, periphytic and planktonic algae, benthic invertebrates, and trout population dynamics during 1967-78.
\nThe aquatic community is diverse and reasonably stable with little indication of environmental disturbance. Aquatic macrophyte population (dominated by Ranunculus aquatilis L., Veronica catenata Penn., and Nasturtium offlcinale) varies little from spring to fall. Periphytic and planktonic algae are predominantly diatoms, with the genus Achnanthes dominating both communities. Most genera of planktonic algae originate in the periphyton, but some true planktonic algae were identified. The benthic invertebrate population is dominated by Trichoptera and is a major food source for trout and forage fish. Biotic index values calculated from benthic invertebrate data indicate that water quality is very good to excellent. The trout population is low and represents only a small part of the total fish population both in biomass and numbers. Brown trout are usually stocked annually in the spring to enhance sport fishing, but by fall most trout are wild. The major environmental factors limiting trout population seem to be insufficient cover, insufficient pool depth and volume, and small spawning areas. The wild trout population is highly dependent on spawning success the previous fall.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri8256","collaboration":"Prepared in cooperation with the Wisconsin Department of Natural Resources","usgsCitation":"Kammerer, P.A., Lidwin, R., Mason, J., and Narf, R., 1982, Aquatic biology in Nederlo Creek, southwestern Wisconsin: U.S. Geological Survey Water-Resources Investigations Report 82-56, iv, 27 p., https://doi.org/10.3133/wri8256.","productDescription":"iv, 27 p.","numberOfPages":"31","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":677,"text":"Wisconsin Water Science Center","active":true,"usgs":true}],"links":[{"id":118755,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1982/0056/report-thumb.jpg"},{"id":54128,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1982/0056/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Wisconsin","county":"Crawford County","otherGeospatial":"Nederlo Creek","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -90.99460601806639,\n 43.320931654867984\n ],\n [\n -90.99460601806639,\n 43.44444442419639\n ],\n [\n -90.79238891601561,\n 43.44444442419639\n ],\n [\n -90.79238891601561,\n 43.320931654867984\n ],\n [\n -90.99460601806639,\n 43.320931654867984\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac5e4b07f02db67a083","contributors":{"authors":[{"text":"Kammerer, Phil A. Jr.","contributorId":85993,"corporation":false,"usgs":true,"family":"Kammerer","given":"Phil","suffix":"Jr.","email":"","middleInitial":"A.","affiliations":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"preferred":false,"id":193523,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Lidwin, R.A.","contributorId":33349,"corporation":false,"usgs":true,"family":"Lidwin","given":"R.A.","email":"","affiliations":[],"preferred":false,"id":193520,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Mason, J.W.","contributorId":79433,"corporation":false,"usgs":true,"family":"Mason","given":"J.W.","email":"","affiliations":[],"preferred":false,"id":193522,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Narf, R.P.","contributorId":48598,"corporation":false,"usgs":true,"family":"Narf","given":"R.P.","email":"","affiliations":[],"preferred":false,"id":193521,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":61250,"text":"mf1433 - 1982 - Seismic reflection study of Flathead Lake, Montana","interactions":[],"lastModifiedDate":"2016-08-23T10:19:15","indexId":"mf1433","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":325,"text":"Miscellaneous Field Studies Map","code":"MF","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1433","title":"Seismic reflection study of Flathead Lake, Montana","docAbstract":"A seismic reflection survey of Flathead Lake, Montana, was carried out in 1970 to study the geologic structure underlying the lake. Approximately 200 km of track lines were surveyed resulting in about 140 km of useable data (Fig. 1). A one cu. in. air gun was used as the energy source. Navigation was by a series of theodolite sitings of the boat from pairs of shore-based control points.
","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/mf1433","usgsCitation":"Wold, R.J., 1982, Seismic reflection study of Flathead Lake, Montana: U.S. Geological Survey Miscellaneous Field Studies Map 1433, 34.49 x 36.91 inches, https://doi.org/10.3133/mf1433.","productDescription":"34.49 x 36.91 inches","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":186906,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/mf1433.PNG"},{"id":327575,"rank":1,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mf/1433/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Montana","otherGeospatial":"Flathead Lake","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -114.3621826171875,\n 47.68110753158711\n ],\n [\n -114.3621826171875,\n 48.098260411732674\n ],\n [\n -113.99139404296875,\n 48.098260411732674\n ],\n [\n -113.99139404296875,\n 47.68110753158711\n ],\n [\n -114.3621826171875,\n 47.68110753158711\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0ae4b07f02db5fb6eb","contributors":{"authors":[{"text":"Wold, Richard J.","contributorId":105338,"corporation":false,"usgs":true,"family":"Wold","given":"Richard","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":265257,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":26187,"text":"wri8226 - 1982 - Streamflow and water-quality conditions, Wilsons Creek and James River, Springfield area, Missouri","interactions":[],"lastModifiedDate":"2017-12-06T12:52:13","indexId":"wri8226","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","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":"82-26","title":"Streamflow and water-quality conditions, Wilsons Creek and James River, Springfield area, Missouri","docAbstract":"A network of water-quality-monitoring stations was established upstream and downstream from the Southwest Wastewater-Treatment Plant on Wilsons Creek to monitor the effects of sewage effluent on water quality. Data indicate that 82 percent of the time the flow in Wilsons Creek upstream from the wastewater-treatment plant is less than the effluent discharged from the plant. On October 15, 1977, an advanced wastewater-treatment facility was put into operation. Of the four water-quality indicators measured at the monitoring stations (specific conductance, dissolved oxygen, pH, and water temperature), only dissolved oxygen showed improvement downstream from the plant. During urban runoff, the specific conductance momentarily increased and dissolved-oxygen concentration momentarily decreased in Wilsons Creek upstream from the plant. Urban runoff was found to have no long-term effects on specific conductance and dissolved oxygen downstream from the plant before or after the addition of the advanced wastewater-treatment facility. Data collected monthly from the James River showed that the dissolved-oxygen concentrations and the total nitrite plus nitrate nitrogen concentrations increased, whereas the dissolved-manganese concentrations decreased after the advanced wastewater-treatment facility became operational.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri8226","usgsCitation":"Berkas, W.R., 1982, Streamflow and water-quality conditions, Wilsons Creek and James River, Springfield area, Missouri: U.S. Geological Survey Water-Resources Investigations Report 82-26, v, 38 p., https://doi.org/10.3133/wri8226.","productDescription":"v, 38 p.","numberOfPages":"49","costCenters":[],"links":[{"id":157616,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1982/0026/report-thumb.jpg"},{"id":349774,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1982/0026/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Missouri","city":"Springfield","otherGeospatial":"James River, Wilsons Creek","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -93.49983215332031,\n 36.99322996239362\n ],\n [\n -93.27529907226562,\n 36.99322996239362\n ],\n [\n -93.27529907226562,\n 37.20462845803212\n ],\n [\n -93.49983215332031,\n 37.20462845803212\n ],\n [\n -93.49983215332031,\n 36.99322996239362\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b15e4b07f02db6a4e9b","contributors":{"authors":[{"text":"Berkas, Wayne R. wrberkas@usgs.gov","contributorId":425,"corporation":false,"usgs":true,"family":"Berkas","given":"Wayne","email":"wrberkas@usgs.gov","middleInitial":"R.","affiliations":[{"id":5050,"text":"WY-MT Water Science Center","active":true,"usgs":true}],"preferred":true,"id":195957,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":57279,"text":"wdrND811 - 1982 - Water resources data, North Dakota, water year 1981, Volume 1. Hudson Bay Basin","interactions":[],"lastModifiedDate":"2020-10-27T17:42:08.268637","indexId":"wdrND811","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":340,"text":"Water Data Report","code":"WDR","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"ND-81-1","title":"Water resources data, North Dakota, water year 1981, Volume 1. Hudson Bay Basin","docAbstract":"No abstract available.
","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wdrND811","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1982, Water resources data, North Dakota, water year 1981, Volume 1. 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Dakota\",\"nation\":\"USA \"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a09e4b07f02db5fb008","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":533051,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":61163,"text":"mf1432 - 1982 - Map of erosion potential and sediment sources in the Navajo Mine area, San Juan County, New Mexico","interactions":[],"lastModifiedDate":"2016-08-23T10:08:22","indexId":"mf1432","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":325,"text":"Miscellaneous Field Studies Map","code":"MF","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1432","title":"Map of erosion potential and sediment sources in the Navajo Mine area, San Juan County, New Mexico","docAbstract":"This map shows estimated erosion and sediment yields of an area designated for extensive surface mining, in San Juan County, New Mexico. The results of this study are important for the planning of future mining operations and will aid in developing suitable reclamation procedures. In addition, these data will serve as a base line from which a long-term program for determining rates of erosion and deposition could be developed. Such measurements are essential to understanding the impact of surface mining on geomorphic processes affected by extraction of resources form arid lands. The area chosen for the study lies within for 7-1/2-minute quadrangles (The Hogback South, Kirtland SW, Newcomb NE, and The Pillar NW) in the northwest San Juan Basin (figs. 1,2). The area includes five drainage basins covering approximately 200 mi2 (520 km2) that flow west into the Chaco River (fig. 1). Approximately 41 mi2 (106 km2) of this area is scheduled for surface mining during the next several years as part of the southern extension of the Navajo Mine.
","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/mf1432","usgsCitation":"Weide, D.L., 1982, Map of erosion potential and sediment sources in the Navajo Mine area, San Juan County, New Mexico: U.S. Geological Survey Miscellaneous Field Studies Map 1432, 48.93 x 34.10 inches, https://doi.org/10.3133/mf1432.","productDescription":"48.93 x 34.10 inches","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":183472,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/mf1432.PNG"},{"id":327556,"rank":1,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mf/1432/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"50000","country":"United States","state":"New Mexico","county":"San Juan","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -108.61749999999999,36.3675 ], [ -108.61749999999999,36.6175 ], [ -108.36749999999999,36.6175 ], [ -108.36749999999999,36.3675 ], [ -108.61749999999999,36.3675 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a91e4b07f02db656dc8","contributors":{"authors":[{"text":"Weide, David L.","contributorId":48537,"corporation":false,"usgs":true,"family":"Weide","given":"David","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":265104,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":57280,"text":"wdrND812 - 1982 - Water resources data, North Dakota, water year 1981. Volume 2. Missouri River Basin","interactions":[],"lastModifiedDate":"2020-10-28T19:28:38.907593","indexId":"wdrND812","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":340,"text":"Water Data Report","code":"WDR","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"ND-81-2","title":"Water resources data, North Dakota, water year 1981. Volume 2. Missouri River Basin","docAbstract":"No abstract available.
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Dakota\",\"nation\":\"USA \"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a09e4b07f02db5fb011","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":533052,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":60640,"text":"mf1321 - 1982 - Maps showing locations and descriptions of radiocarbon-dated samples from central and northern California","interactions":[],"lastModifiedDate":"2015-09-24T12:16:16","indexId":"mf1321","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":325,"text":"Miscellaneous Field Studies Map","code":"MF","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1321","title":"Maps showing locations and descriptions of radiocarbon-dated samples from central and northern California","docAbstract":"This compilation includes radiocarbon dates and other pertinent information about samples from northern and central California, principally north of latitude 36°, drawn largely from Radiocarbon, Science, unpublished data of U.S. Geological Survey geologists, and other published and unpublished data brought to the author's attention as of January 1981. It includes a location map, several tables, and two lists of sources that contain further information about the samples. This compilation is intended as a progress report rather than a complete survey of the literature.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/mf1321","usgsCitation":"Price, C.A., 1982, Maps showing locations and descriptions of radiocarbon-dated samples from central and northern California: U.S. Geological Survey Miscellaneous Field Studies Map 1321, Report: 38 p.; 2 Plates: 41.56 x 39.49 inches and 41.56 x 50.80 inches, https://doi.org/10.3133/mf1321.","productDescription":"Report: 38 p.; 2 Plates: 41.56 x 39.49 inches and 41.56 x 50.80 inches","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":180524,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/mf1321.PNG"},{"id":308506,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mf/1321/plate-1.pdf","text":"Plate 1","size":"38,293 KB","linkFileType":{"id":1,"text":"pdf"}},{"id":308507,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mf/1321/plate-2.pdf","text":"Plate 2","size":"26,533 KB","linkFileType":{"id":1,"text":"pdf"}},{"id":308505,"rank":1,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/mf/1321/report.pdf","text":"Report","size":"15,800 KB","linkFileType":{"id":1,"text":"pdf"}}],"scale":"0","country":"United States","state":"California","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -124,34 ], [ -124,42 ], [ -117,42 ], [ -117,34 ], [ -124,34 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a19e4b07f02db605b76","contributors":{"authors":[{"text":"Price, Carol A.","contributorId":51377,"corporation":false,"usgs":true,"family":"Price","given":"Carol","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":264122,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":9180,"text":"ofr82644 - 1982 - Subsurface information from eight wells drilled at the Idaho National Engineering Laboratory, southeastern Idaho","interactions":[],"lastModifiedDate":"2012-02-02T00:06:16","indexId":"ofr82644","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":"82-644","title":"Subsurface information from eight wells drilled at the Idaho National Engineering Laboratory, southeastern Idaho","docAbstract":"The Idaho National Engineering Laboratory (INEL) covers about 890 square miles of the eastern Snake River Plain, in southeastern Idaho. The eastern Snake River Plain is a structural basin which has been filled with thin basaltic lava flows, rhyolitic deposits, and interbedded sediments. These rocks form an extensive ground-water reservoir known as the Snake River Plain aquifer. \r\n\r\nSix wells were drilled and two existing wells were deepened at the INEL from 1969 through 1974. Interpretation of data from the drilling program confirms that the subsurface is dominated by basalt flows interbedded with layers of sediment, cinders, and silicic volcanic rocks. \r\n\r\nWater levels in the wells show cyclic seasonal fluctuations of maximum water levels in winter and minimum water levels in mid-summer. Water levels in three wells near the Big Lost River respond to changes in recharge to the Snake River Plain aquifer from the Big Lost River. Measured water levels in multiple piezometers in one well indicate increasing pressure heads with depth. A marked decline in water levels in the wells since 1977 is attributed to a lack of recharge to the Snake River Plain aquifer.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr82644","usgsCitation":"Goldstein, F., and Weight, W., 1982, Subsurface information from eight wells drilled at the Idaho National Engineering Laboratory, southeastern Idaho: U.S. Geological Survey Open-File Report 82-644, v, 34 p., ill., maps ;28 cm., https://doi.org/10.3133/ofr82644.","productDescription":"v, 34 p., ill., maps ;28 cm.","costCenters":[],"links":[{"id":141609,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0644/report-thumb.jpg"},{"id":36794,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0644/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b05e4b07f02db6997a8","contributors":{"authors":[{"text":"Goldstein, F.J.","contributorId":71975,"corporation":false,"usgs":true,"family":"Goldstein","given":"F.J.","email":"","affiliations":[],"preferred":false,"id":159233,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Weight, W.D.","contributorId":81906,"corporation":false,"usgs":true,"family":"Weight","given":"W.D.","email":"","affiliations":[],"preferred":false,"id":159234,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":11594,"text":"ofr82704 - 1982 - Interpretation of Schlumberger DC resistivity data from Gibson Dome-Lockhart Basin study area, San Juan County, Utah","interactions":[],"lastModifiedDate":"2012-02-02T00:06:49","indexId":"ofr82704","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":"82-704","title":"Interpretation of Schlumberger DC resistivity data from Gibson Dome-Lockhart Basin study area, San Juan County, Utah","docAbstract":"A Schlumberger dc resistivity survey of the Gibson Dome-Lockhart Basin area, San Juan County, Utah, has revealed the following electrical characteristics of the area: (1) the area between the northern part of Davis Canyon and Gibson Dome is electrically quite uniform and resistive at the depth of the Pennsylvanian evaporite deposits, (2) there is a deep conductive anomaly at Horsehead Rock, and (3) there are several shallow and deep electrical anomalies in the vicinity of the Lockhart fault system. No adverse indicators were found for nuclear waste repository siting south of Indian Creek, but additional soundings should be made to increase data density and to extend the survey area southward. The Lockhart fault system appears to have triggered salt dissolution or flow outside the limits of Lockhart Basin; further geophysical work and drilling will be required to understand the origin of the Lockhart Basin structure and its present state of activity. This problem is important because geologic processes that lead to enlargement of the Lockhart Basin structure or to development of similar structures would threaten the integrity of a repository in the Gibson Dome area.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr82704","usgsCitation":"Watts, R., 1982, Interpretation of Schlumberger DC resistivity data from Gibson Dome-Lockhart Basin study area, San Juan County, Utah: U.S. Geological Survey Open-File Report 82-704, 21 p., ill., maps ;28 cm., https://doi.org/10.3133/ofr82704.","productDescription":"21 p., ill., maps ;28 cm.","costCenters":[],"links":[{"id":145911,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0704/report-thumb.jpg"},{"id":39453,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0704/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aa7e4b07f02db667072","contributors":{"authors":[{"text":"Watts, R.D.","contributorId":94666,"corporation":false,"usgs":true,"family":"Watts","given":"R.D.","email":"","affiliations":[],"preferred":false,"id":163412,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":25963,"text":"wri8247 - 1982 - Ground-water resources of the White River basin, Delaware County, Indiana","interactions":[],"lastModifiedDate":"2020-11-05T21:15:00.164788","indexId":"wri8247","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","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":"82-47","title":"Ground-water resources of the White River basin, Delaware County, Indiana","docAbstract":"The ground-water resources of the White River basin in and near Delaware County, Indiana, were investigated by mapping the aquifers, calculating their hydraulic properties, determining the distribution of potentiometric head, and determining some of the components of the ground-water budget from data collected in the field. This information was used to construct and calibrate a seven-layer, digital ground-water-flow model. The model, constructed and calibrated to water-level and seepage data collected during the study, simulates conditions for the autumn of 1977. The model was used to assess ground-water potential in terms of yield, drawdown, and streamflow depletion.
Drift covers nearly the entire area and generally ranges in thickness from 0 to 500 feet. Beneath the drift lie Silurian and Ordovician limestone, dolomite, and shale. A bedrock valley trends east-west through the center of the area. Bedrock surface relief is about 400 feet.
Six confined sand and gravel aquifers interbedded in the drift, a bedrock aquifer, and an unconfined outwash aquifer are the three major aquifer systems. The nearly horizontal, areally discontinuous, confined sand and gravel aquifers generally range in thickness from 5 to 40 feet and have an average hydraulic conductivity estimated to be 433 feet per day. The bedrock aquifer underlying all of Delaware County has a permeable thickness estimated to be 150 feet and an average transmissivity of 1,000 square feet per day.
Observation-well records indicate that water-level fluctuation is seasonal and has no long-term trends. Municipal and industrial ground-water pumpage for 1976 was 3.1 million gallons per day (4.8 cubic feet per second). On October 29, 1977, when the flow duration in the White River at Muncie was 80 percent, ground-water seepage to streams was 81 cubic feet per second. The water budget simulated in the model indicated that the rate of inflow to the ground-water system in the modeled area is 102 cubic feet per second: 80 percent from effective areal recharge of precipitation and 20 percent from ground-water flow across the area boundaries. Two percent of the ground-water discharge is pump-age, 66 percent is seepage to streams, and the remaining 32 percent is flow across the area boundaries.
Simulations of seven pumping plans provide a general assessment of the water-yielding potential of the three major aquifer systems. Model results indicate that as much as 3 million gallons per day can be developed from well fields where the average drawdown is 20 feet. Model simulations also indicate that 7 million gallons per day is available from a potential well field around Muncie.
","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wri8247","collaboration":"Prepared in cooperation with the Indiana Department of Natural Resources","usgsCitation":"Arihood, L.D., and Lapham, W.W., 1982, Ground-water resources of the White River basin, Delaware County, Indiana: U.S. Geological Survey Water-Resources Investigations Report 82-47, vi, 69 p., https://doi.org/10.3133/wri8247.","productDescription":"vi, 69 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":346,"text":"Indiana Water Science Center","active":true,"usgs":true}],"links":[{"id":380218,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1982/0047/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":157571,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1982/0047/report-thumb.jpg"}],"country":"United States","state":"Indiana","county":"Delaware County","otherGeospatial":"White River basin","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"Polygon\",\"coordinates\":[[[-85.4451,40.3792],[-85.2205,40.379],[-85.2182,40.3073],[-85.2168,40.2198],[-85.2165,40.135],[-85.2157,40.0765],[-85.5763,40.0769],[-85.5784,40.3794],[-85.4451,40.3792]]]},\"properties\":{\"name\":\"Delaware\",\"state\":\"IN\"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afde4b07f02db696a92","contributors":{"authors":[{"text":"Arihood, Leslie D. 0000-0001-5792-3699 larihood@usgs.gov","orcid":"https://orcid.org/0000-0001-5792-3699","contributorId":2357,"corporation":false,"usgs":true,"family":"Arihood","given":"Leslie","email":"larihood@usgs.gov","middleInitial":"D.","affiliations":[{"id":346,"text":"Indiana Water Science Center","active":true,"usgs":true},{"id":35860,"text":"Ohio-Kentucky-Indiana Water Science Center","active":true,"usgs":true}],"preferred":true,"id":195554,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Lapham, Wayne W.","contributorId":74734,"corporation":false,"usgs":true,"family":"Lapham","given":"Wayne","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":195555,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":3188,"text":"wsp2185B - 1982 - Water-quality characteristics of streams in forested and rural areas of North Carolina","interactions":[],"lastModifiedDate":"2012-02-02T00:05:25","indexId":"wsp2185B","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":341,"text":"Water Supply Paper","code":"WSP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"2185","chapter":"B","title":"Water-quality characteristics of streams in forested and rural areas of North Carolina","docAbstract":"Data collected in North Carolina during 1973-78 from a statewide network of 39 rural sampling sites were used to define unpolluted or baseline stream quality. The basins were 90 to 100 percent forested and, except for the unknown effects of air pollution, were relatively unaffected by man 's activities. Five distinct geochemical zones were delineated across the State. The chemical characteristics of surface waters in each zone are similar. Mean and other statistical values for major dissolved constituents, nutrients, and minor elements in base runoff and storm runoff were determined. Twenty additional rural sites were located in basins where farming activities ranged from 15 to 55 percent of basins' land area. Data from these 20 sites were used for comparison with data from the 39 unpolluted sites to determine the increase in constituent levels caused by man. For basins where farming activities accounted for 20 or more percent of total land use, phosphorus levels were 2 to 13 times greater than those from the forested basins and several major constituents were 2 to 3 times greater. Concentrations of minor elements were essentially the same in both developed and undeveloped basins.","language":"ENGLISH","publisher":"U.S. G.P.O.,","doi":"10.3133/wsp2185B","usgsCitation":"Simmons, C.E., and Heath, R., 1982, Water-quality characteristics of streams in forested and rural areas of North Carolina: U.S. Geological Survey Water Supply Paper 2185, 1 v. (various pagings) : ill., maps ; 28 cm. ;33 p., https://doi.org/10.3133/wsp2185B.","productDescription":"1 v. (various pagings) : ill., maps ; 28 cm. ;33 p.","costCenters":[],"links":[{"id":138302,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/2185a/report-thumb.jpg"},{"id":91271,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/2185a/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aa8e4b07f02db667579","contributors":{"authors":[{"text":"Simmons, Clyde E.","contributorId":71528,"corporation":false,"usgs":true,"family":"Simmons","given":"Clyde","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":146400,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Heath, Ralph C.","contributorId":53359,"corporation":false,"usgs":true,"family":"Heath","given":"Ralph C.","affiliations":[],"preferred":false,"id":146399,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":25964,"text":"wri8248 - 1982 - Ground-water resources of the White River basin, Hamilton and Tipton Counties, Indiana","interactions":[],"lastModifiedDate":"2020-11-05T21:13:59.692849","indexId":"wri8248","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","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":"82-48","title":"Ground-water resources of the White River basin, Hamilton and Tipton Counties, Indiana","docAbstract":"An analysis of the ground-water resources of the Hamilton and Tipton Counties was based on data from about 1,900 well logs, 125 water levels in 125 wells, streamflow measurements at 57 sites, and municipal- and industrial-pumpage records. These data were used to map the flow system and construct a three-dimensional model of the study area and a more detailed two-dimensional model of the outwash deposits along the White River. The models were used to determine the pumpage from several pumping plans and the effect of these pump-ages on streamflow and ground-water levels.
Model results indicate that 39 million gallons per day could be obtained from the outwash aquifer. This quantity of pumping in areas of high transmissivity near and parallel to the White River would reduce the saturated thick-ness of the aquifers at the wells by half. The models also indicated that 0.18 to 6.7 million gallons per day could be pumped from the confined sand and gravel and the bedrock aquifers that have high transmissivities and are near favor-able discharge areas.
Drift covers most of the study area and ranges in thickness from 0 to about 400 feet. The drift consists mainly of till and outwash deposits. Beneath the drift lie Silurian and Devonian limestone, dolomite, and shale having a surface relief of about 300 feet.
The study area contains five discontinuous, confined sand and gravel aquifers within the till, an outwash aquifer associated with the White River, and a bedrock aquifer. Of these aquifers, the south half of the outwash aquifer, having a saturated thickness averaging 70 feet and a width ranging from 2 to 3 miles, has the greatest potential for water supply. The general ranges of measurements for the aquifers are: thin and discontinuous confined aquifer, thickness from 5 to 20 feet and transmissivity from 1,000 to 20,000 square feet per day; outwash, transmissivity from 1,000 to 28,000 square feet per day; and bedrock, transmissivity from 500 to 10,000 square feet per day. Vertical hydraulic conductivity of the confining beds between the confined aquifers ranges from 7 x 10-4 to 7 x 10-2 feet per day and averages near 7 x 10-3 feet per day.
","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wri8248","collaboration":"Prepared in cooperation with the Indiana Department of Natural Resources","usgsCitation":"Arihood, L.D., 1982, Ground-water resources of the White River basin, Hamilton and Tipton Counties, Indiana: U.S. Geological Survey Water-Resources Investigations Report 82-48, vi, 69 p., https://doi.org/10.3133/wri8248.","productDescription":"vi, 69 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":346,"text":"Indiana Water Science Center","active":true,"usgs":true}],"links":[{"id":157573,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1982/0048/report-thumb.jpg"},{"id":380217,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1982/0048/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Indiana","county":"Hamilton County, Tipton County","otherGeospatial":"White River basin","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -86.45690917968749,\n 39.829631721333726\n ],\n [\n -86.45690917968749,\n 40.46784549077257\n ],\n [\n -85.58349609375,\n 40.46784549077257\n ],\n [\n -85.58349609375,\n 39.829631721333726\n ],\n [\n -86.45690917968749,\n 39.829631721333726\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a96e4b07f02db65a69d","contributors":{"authors":[{"text":"Arihood, Leslie D. 0000-0001-5792-3699 larihood@usgs.gov","orcid":"https://orcid.org/0000-0001-5792-3699","contributorId":2357,"corporation":false,"usgs":true,"family":"Arihood","given":"Leslie","email":"larihood@usgs.gov","middleInitial":"D.","affiliations":[{"id":35860,"text":"Ohio-Kentucky-Indiana Water Science Center","active":true,"usgs":true},{"id":346,"text":"Indiana Water Science Center","active":true,"usgs":true}],"preferred":true,"id":195556,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":11593,"text":"ofr82831 - 1982 - Fortran '77 programs for computing data fitting functions based on a principle of minimum integrated squared curvature","interactions":[],"lastModifiedDate":"2012-02-02T00:06:49","indexId":"ofr82831","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":"82-831","title":"Fortran '77 programs for computing data fitting functions based on a principle of minimum integrated squared curvature","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr82831","usgsCitation":"Watts, R., 1982, Fortran '77 programs for computing data fitting functions based on a principle of minimum integrated squared curvature: U.S. Geological Survey Open-File Report 82-831, 42 p., 28 cm., https://doi.org/10.3133/ofr82831.","productDescription":"42 p., 28 cm.","costCenters":[],"links":[{"id":145910,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0831/report-thumb.jpg"},{"id":39452,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0831/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49d5e4b07f02db5dd9b8","contributors":{"authors":[{"text":"Watts, R.D.","contributorId":94666,"corporation":false,"usgs":true,"family":"Watts","given":"R.D.","email":"","affiliations":[],"preferred":false,"id":163411,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":3239,"text":"cir859 - 1982 - Bibliography of U.S. Geological Survey studies of lakes and reservoirs; the first 100 years","interactions":[],"lastModifiedDate":"2018-03-13T11:45:06","indexId":"cir859","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":307,"text":"Circular","code":"CIR","onlineIssn":"2330-5703","printIssn":"1067-084X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"859","title":"Bibliography of U.S. Geological Survey studies of lakes and reservoirs; the first 100 years","docAbstract":"For more than 100 years, the U.S. Geological Survey has pursued its mission of assessing and mapping the earth resources of the United States, including assessment of the Nation's water resources. Although the Survey has never been a water-management or development agency, it has assisted agencies that are responsible for such developments, and commonly provides data and information for such purposes. Because reservoirs are an intergral part of most water-development projects, the Survey has been involved in reservoir-related studies since the 1880's. The largest and longest involvement has centered on providing information on streamflows and sediment transport related to existing and proposed reservoirs. During the late 1940's, the Survey greatly expanded its activities in evaporation research. More recently, ground water, including bank storage, has gained increased attention. Most of these studies were related primarily to questions of water quantity, and the Survey continues to be involved in studies of physical hydrology. In addition, in response to the increased concern with environmental quality during the past 20 years, the number of Survey studies of the chemical and biological aspects of lakes and reservoirs have increased considerably.
Prompted by the recent Centennial (1879-1979) of the U.S. Geological Survey, it is appropriate to assess the Survey's contributions to the hydrology of lakes and reservoirs. Both natural lakes and manmade reservoirs are included in this report. 1 This report includes studies in which lakes or reservoirs are the principal topics. It does not include reports of general water resources of an area in which lakes are discussed as part of that area. This report also does not include data reports in which the data are merely tabulated. The types of reports listed herein include studies of existing or proposed water bodies and associated fluxes of water to and from these water bodies.
This report does not include geological or paleobiological studies of ancient lakes. This report does, however, include geological studies of proposed reservoir sites.
This bibliography has three parts. The first part is an alphabetical listing that gives complete references to the given reports. Part 2 is a listing by topics, and only the authors, date of publication, and cross-reference to the State are given. Six general categories are considered: Lake hydrology; interaction of lakes and streamflow, including geological studies of reservoir sites; interaction of lakes and atmospheric water; interaction of lakes. and ground water; chemical and biological limnology; and sediment studies. The first four consist of studies of physical characteristics of lakes, and the last two of water-quality characteristics. The category of lake hydrology includes general studies of lakes that are not easily grouped into one of the more specific categories of physical characteristics. For example, it includes water-budget studies where all aspects of hydrology are discussed. It also includes studies of hydrodynamics of lakes as well as studies of lake-level fluctuations.
The category of interaction of lakes and streamflow includes preimpoundment studies of streamflow discharge for reservoir design, and studies of the effects of existing reservoirs on streamflow and channel characteristics. Also included in this category are geological studies of river valleys for proposed reservoir sites. The category of interaction of lakes and atmospheric water includes primarily studies of evaporation. The interaction of lakes and ground water includes studies of bank storage. The category of chemical and biological studies was not subdivided into more specific types because of the virtually inseparable relation between chemistry and biology in most studies.
This bibliography provided much of the information for two papers that discuss the history of U.S. Geological Survey studies of lakes and reservoirs. (See Winter, 1981b; and Hadley, 1981).
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/cir859","usgsCitation":"Winter, T.C., 1982, Bibliography of U.S. Geological Survey studies of lakes and reservoirs; the first 100 years: U.S. Geological Survey Circular 859, 35 p., https://doi.org/10.3133/cir859.","productDescription":"35 p.","costCenters":[{"id":478,"text":"North Dakota Water Science Center","active":true,"usgs":true},{"id":34685,"text":"Dakota Water Science Center","active":true,"usgs":true}],"links":[{"id":122598,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/circ/1982/0859/report-thumb.jpg"},{"id":30235,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/1982/0859/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a51e4b07f02db629788","contributors":{"authors":[{"text":"Winter, Thomas C.","contributorId":84736,"corporation":false,"usgs":true,"family":"Winter","given":"Thomas","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":146492,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ]}