{"pageNumber":"2121","pageRowStart":"53000","pageSize":"25","recordCount":68919,"records":[{"id":8105,"text":"ofr82513 - 1982 - Evaluation of increases in dissolved solids in ground water, Stovepipe Wells Hotel, Death Valley National Monument, California","interactions":[],"lastModifiedDate":"2012-02-02T00:06:05","indexId":"ofr82513","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":"82-513","title":"Evaluation of increases in dissolved solids in ground water, Stovepipe Wells Hotel, Death Valley National Monument, California","docAbstract":"Increases in dissolved solids have been monitored in two observation wells near Stovepipe Wells Hotel, Death Valley National Monument, California. One of the hotel 's supply wells delivers water to a reverse-osmosis treatment plant that produces the area 's potable water supply. Should water with increased dissolved solids reach the supply well, the costs of production of potable water will increase. The reverse-osmosis plant supply well is located about 0.4 mile south of one of the wells where increases have been monitored, and 0.8 mile southwest of the well where the most significant increases have been monitored. The direction of local ground-water movement is eastward, which reduces the probability of the supply well being affected. Honey mesquite, a phreatophyte located about 1.5 miles downgradient from the well where the most significant increases have been monitored, might be adversely affected should water with increased dissolved solids extend that far. Available data and data collected during this investigation do not indicate the source of the dissolved-solids increases. Continued ground-water-quality monitoring of existing wells and the installation of additional wells for water-quality monitoring would be necessary before the area affected by the increases, and the source and direction of movement of the water with increased dissolved solids, can be determined. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr82513","usgsCitation":"Buono, A., and Packard, E., 1982, Evaluation of increases in dissolved solids in ground water, Stovepipe Wells Hotel, Death Valley National Monument, California: U.S. Geological Survey Open-File Report 82-513, iv, 23 p., ill., map ;28 cm., https://doi.org/10.3133/ofr82513.","productDescription":"iv, 23 p., ill., map ;28 cm.","costCenters":[],"links":[{"id":140607,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0513/report-thumb.jpg"},{"id":35703,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0513/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e499fe4b07f02db5bd1fa","contributors":{"authors":[{"text":"Buono, Anthony","contributorId":48175,"corporation":false,"usgs":true,"family":"Buono","given":"Anthony","email":"","affiliations":[],"preferred":false,"id":157157,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Packard, E.M.","contributorId":38552,"corporation":false,"usgs":true,"family":"Packard","given":"E.M.","email":"","affiliations":[],"preferred":false,"id":157156,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":7948,"text":"ofr82413 - 1982 - Surface and ground-water references index for the Navajo Indian Reservation, Arizona, New Mexico, and Utah","interactions":[],"lastModifiedDate":"2012-02-02T00:06:02","indexId":"ofr82413","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":"82-413","title":"Surface and ground-water references index for the Navajo Indian Reservation, Arizona, New Mexico, and Utah","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr82413","usgsCitation":"Bliss, J.D., 1982, Surface and ground-water references index for the Navajo Indian Reservation, Arizona, New Mexico, and Utah: U.S. Geological Survey Open-File Report 82-413, 17 p., 28 cm., https://doi.org/10.3133/ofr82413.","productDescription":"17 p., 28 cm.","costCenters":[],"links":[{"id":140884,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0413/report-thumb.jpg"},{"id":35519,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0413/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b00e4b07f02db6983ce","contributors":{"authors":[{"text":"Bliss, J. D.","contributorId":25564,"corporation":false,"usgs":true,"family":"Bliss","given":"J.","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":156876,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":7914,"text":"ofr82902 - 1982 - Directory of member organizations of the National Water Data Exchange","interactions":[{"subject":{"id":10527,"text":"ofr81497 - 1981 - Directory of member organizations of the National Water Data Exchange (NAWDEX)","indexId":"ofr81497","publicationYear":"1981","noYear":false,"title":"Directory of member organizations of the National Water Data Exchange (NAWDEX)"},"predicate":"SUPERSEDED_BY","object":{"id":7914,"text":"ofr82902 - 1982 - Directory of member organizations of the National Water Data Exchange","indexId":"ofr82902","publicationYear":"1982","noYear":false,"title":"Directory of member organizations of the National Water Data Exchange"},"id":1}],"lastModifiedDate":"2012-02-02T00:06:00","indexId":"ofr82902","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":"82-902","title":"Directory of member organizations of the National Water Data Exchange","docAbstract":"The National Water Data Exchange (NAWDEX) is a national confederation of water-oriented organizations working together to improve access to water data. It consists of member organizations from all sectors of the water-data community. This Directory provides the names, addresses, and telephone numbers of all NAWDEX member organizations and their designated NAWDEX representatives. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr82902","usgsCitation":"Blackwell, C.D., and Nokes, J.M., 1982, Directory of member organizations of the National Water Data Exchange: U.S. Geological Survey Open-File Report 82-902, viii, 74 p. ;28 cm., https://doi.org/10.3133/ofr82902.","productDescription":"viii, 74 p. ;28 cm.","costCenters":[],"links":[{"id":94839,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0902/report.pdf","size":"2681","linkFileType":{"id":1,"text":"pdf"}},{"id":140692,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0902/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b32e4b07f02db6b4667","contributors":{"authors":[{"text":"Blackwell, Cassandra D.","contributorId":25562,"corporation":false,"usgs":true,"family":"Blackwell","given":"Cassandra","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":156826,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Nokes, Janet M.","contributorId":103274,"corporation":false,"usgs":true,"family":"Nokes","given":"Janet","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":156827,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":7926,"text":"ofr82152 - 1982 - Water quality of the tidal Potomac River and estuary hydrologic data report, 1980 water year","interactions":[],"lastModifiedDate":"2012-02-02T00:06:00","indexId":"ofr82152","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":"82-152","title":"Water quality of the tidal Potomac River and estuary hydrologic data report, 1980 water year","docAbstract":"This report contains data on the physical and chemical properties measured in the Tidal Potomac River and Estuary during the 1980 Water Year. Data were collected routinely at five stations, and periodically at 17 stations including three stations near the mouth of the Potomac River in Chesapeake Bay. Each of the five stations represent a cross section through which the transport of selected dissolved and suspended materials can be computed. The remaining stations represent locations at which data were collected for special synoptic studies such as salt water migration, and dissolved oxygen dynamics. Routinely, samples were analyzed for silica, nitrogen, phosphorus, chlorophyll-a, pheophytin, and suspended sediment. Additional samples were analyzed for organic carbon, calcium, manganese, magnesium, sodium, alkalinity, sulfate, iron, potassium, chloride, fluoride, seston, algal growth potential, adenosine triphosphate, nitrifying bacteria and dissolved-solids residue. In addition, solar radiation measurements and in-situ measurements of dissolved oxygen, specific conductance, pH, temperature, and Secchi disk transparency are reported. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr82152","usgsCitation":"Blanchard, S., Coupe, R., and Woodward, J., 1982, Water quality of the tidal Potomac River and estuary hydrologic data report, 1980 water year: U.S. Geological Survey Open-File Report 82-152, i, 335 p. :ill., maps ;28 cm., https://doi.org/10.3133/ofr82152.","productDescription":"i, 335 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":140722,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0152/report-thumb.jpg"},{"id":35490,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0152/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a06e4b07f02db5f8882","contributors":{"authors":[{"text":"Blanchard, Stephen","contributorId":6852,"corporation":false,"usgs":true,"family":"Blanchard","given":"Stephen","affiliations":[],"preferred":false,"id":156845,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Coupe, R.H. Jr.","contributorId":84755,"corporation":false,"usgs":true,"family":"Coupe","given":"R.H.","suffix":"Jr.","email":"","affiliations":[],"preferred":false,"id":156847,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Woodward, J.C.","contributorId":62590,"corporation":false,"usgs":true,"family":"Woodward","given":"J.C.","email":"","affiliations":[],"preferred":false,"id":156846,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":7931,"text":"ofr82573 - 1982 - Water-level records for the northern High Plains of Colorado, 1978-82","interactions":[],"lastModifiedDate":"2012-02-02T00:06:02","indexId":"ofr82573","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":"82-573","title":"Water-level records for the northern High Plains of Colorado, 1978-82","docAbstract":"Water-level measurements were made in 674 wells during the winter of 1981-82 in the northern High Plains of Colorado. The water-level measurements for the winter of 1981-82 and the four preceding winters are given in a table. This table also contains the location, depth, land-surface elevation, and the aquifer of each well. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr82573","usgsCitation":"Blattner, J., and Rasmuson, B., 1982, Water-level records for the northern High Plains of Colorado, 1978-82: U.S. Geological Survey Open-File Report 82-573, 31 p., maps ;28 cm., https://doi.org/10.3133/ofr82573.","productDescription":"31 p., maps ;28 cm.","costCenters":[],"links":[{"id":140731,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0573/report-thumb.jpg"},{"id":35503,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0573/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e6e4b07f02db5e736a","contributors":{"authors":[{"text":"Blattner, J.L.","contributorId":44541,"corporation":false,"usgs":true,"family":"Blattner","given":"J.L.","affiliations":[],"preferred":false,"id":156858,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Rasmuson, B.D.","contributorId":32920,"corporation":false,"usgs":true,"family":"Rasmuson","given":"B.D.","affiliations":[],"preferred":false,"id":156857,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":4307,"text":"cir880 - 1982 - Goals and tasks of the landslide part of a ground-failure hazards reduction program","interactions":[],"lastModifiedDate":"2012-02-02T00:05:30","indexId":"cir880","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":"880","title":"Goals and tasks of the landslide part of a ground-failure hazards reduction program","language":"ENGLISH","publisher":"United States Dept. of the Interior, Geological Survey,","doi":"10.3133/cir880","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1982, Goals and tasks of the landslide part of a ground-failure hazards reduction program: U.S. Geological Survey Circular 880, v, 49 p. :ill., maps ;27 cm., https://doi.org/10.3133/cir880.","productDescription":"v, 49 p. :ill., maps ;27 cm.","costCenters":[],"links":[{"id":120880,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/circ/1982/0880/report-thumb.jpg"},{"id":31418,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/1982/0880/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4abde4b07f02db674221","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":528175,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":4257,"text":"cir878A - 1982 - A U.S. Geological Survey data standard: Codes for the identification of hydrologic units in the United States and the Caribbean outlying areas","interactions":[],"lastModifiedDate":"2012-02-02T00:05:38","indexId":"cir878A","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":"878","chapter":"A","title":"A U.S. Geological Survey data standard: Codes for the identification of hydrologic units in the United States and the Caribbean outlying areas","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/cir878A","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1982, A U.S. Geological Survey data standard: Codes for the identification of hydrologic units in the United States and the Caribbean outlying areas: U.S. Geological Survey Circular 878, iii, A1-A115 p. :map ;26 cm., https://doi.org/10.3133/cir878A.","productDescription":"iii, A1-A115 p. :map ;26 cm.","costCenters":[],"links":[{"id":120865,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/cir_878_A.bmp"},{"id":82,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/circ/circ878-A/","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53cd496de4b0b290850ef28c","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":528174,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":8035,"text":"ofr8299 - 1982 - Two-dimensional digital ground-water model of the Memphis Sand and equivalent units, Tennessee,Arkansas,Mississippi","interactions":[],"lastModifiedDate":"2012-02-02T00:06:04","indexId":"ofr8299","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":"82-99","title":"Two-dimensional digital ground-water model of the Memphis Sand and equivalent units, Tennessee,Arkansas,Mississippi","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr8299","usgsCitation":"Brahana, J., 1982, Two-dimensional digital ground-water model of the Memphis Sand and equivalent units, Tennessee,Arkansas,Mississippi: U.S. Geological Survey Open-File Report 82-99, 62 p., 1 over-size sheet, ill., maps ;28 cm., https://doi.org/10.3133/ofr8299.","productDescription":"62 p., 1 over-size sheet, ill., maps ;28 cm.","costCenters":[],"links":[{"id":140538,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0099/report-thumb.jpg"},{"id":35609,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/0099/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":35610,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0099/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a48e4b07f02db62395e","contributors":{"authors":[{"text":"Brahana, J. V.","contributorId":32926,"corporation":false,"usgs":true,"family":"Brahana","given":"J. V.","affiliations":[],"preferred":false,"id":157025,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":4421,"text":"cir875 - 1982 - U.S. Geological Survey activities, fiscal year 1981","interactions":[],"lastModifiedDate":"2012-02-02T00:05:28","indexId":"cir875","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":"875","title":"U.S. Geological Survey activities, fiscal year 1981","docAbstract":"This U.S. Geological Survey Activities report for fiscal year 1981 presents a summary of the work performed between October 1, 1980 and September 30, 1981. The main sections of this report are: (1) The Year in Review; a brief overview of the significant events of the Geological Survey during fiscal year 1980; (2) Perspectives; essays focusing on specific events (rather than scientific topics) and programs involving multi-Division participation; (3) Missions, Organization, and Budget; a description of the Geological Survey 's major duties and assignments and of the organizational structure that supports its missions; and (4) Division Chapters; a description of the significant accomplishments (rather than a comprehensive program by program discussion) of each of the eight operating Divisions and Offices. Also included are supplementary information regarding key personnel, cooperators, and selected summary budgetary tables. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/cir875","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1982, U.S. Geological Survey activities, fiscal year 1981: U.S. Geological Survey Circular 875, v, 161 p. :ill. ;26 cm., https://doi.org/10.3133/cir875.","productDescription":"v, 161 p. :ill. ;26 cm.","costCenters":[],"links":[{"id":117572,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/circ/1982/0875/report-thumb.jpg"},{"id":31526,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/1982/0875/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a53e4b07f02db62b40e","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":528221,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":6513,"text":"pp1044J - 1982 - Hydrology and geochemistry of thermal ground water in southwestern Idaho and north-central Nevada","interactions":[{"subject":{"id":53044,"text":"ofr802043 - 1980 - Hydrology and geochemistry of thermal ground water in southwestern Idaho and north-central Nevada","indexId":"ofr802043","publicationYear":"1980","noYear":false,"title":"Hydrology and geochemistry of thermal ground water in southwestern Idaho and north-central Nevada"},"predicate":"SUPERSEDED_BY","object":{"id":6513,"text":"pp1044J - 1982 - Hydrology and geochemistry of thermal ground water in southwestern Idaho and north-central Nevada","indexId":"pp1044J","publicationYear":"1982","noYear":false,"chapter":"J","title":"Hydrology and geochemistry of thermal ground water in southwestern Idaho and north-central Nevada"},"id":1}],"lastModifiedDate":"2025-04-17T17:04:29.694949","indexId":"pp1044J","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":331,"text":"Professional Paper","code":"PP","onlineIssn":"2330-7102","printIssn":"1044-9612","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"1044","chapter":"J","title":"Hydrology and geochemistry of thermal ground water in southwestern Idaho and north-central Nevada","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/pp1044J","usgsCitation":"Young, H., and Lewis, R., 1982, Hydrology and geochemistry of thermal ground water in southwestern Idaho and north-central Nevada: U.S. Geological Survey Professional Paper 1044, Report: 20 p.;  2 Plates: 20.50 x 25.00 inches and 21.00 x 25.00 inches, https://doi.org/10.3133/pp1044J.","productDescription":"Report: 20 p.;  2 Plates: 20.50 x 25.00 inches and 21.00 x 25.00 inches","costCenters":[],"links":[{"id":33978,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/1044j/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":33977,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/1044j/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":33979,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/1044j/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":484685,"rank":5,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_4699.htm","linkFileType":{"id":5,"text":"html"}},{"id":118022,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/1044j/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a18e4b07f02db605128","contributors":{"authors":[{"text":"Young, H.W.","contributorId":68278,"corporation":false,"usgs":true,"family":"Young","given":"H.W.","email":"","affiliations":[],"preferred":false,"id":152850,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Lewis, R.E.","contributorId":31735,"corporation":false,"usgs":true,"family":"Lewis","given":"R.E.","email":"","affiliations":[],"preferred":false,"id":152849,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":8110,"text":"ofr82264 - 1982 - Availability and quality of water from the Dakota aquifer, northwest Iowa","interactions":[{"subject":{"id":8110,"text":"ofr82264 - 1982 - Availability and quality of water from the Dakota aquifer, northwest Iowa","indexId":"ofr82264","publicationYear":"1982","noYear":false,"title":"Availability and quality of water from the Dakota aquifer, northwest Iowa"},"predicate":"SUPERSEDED_BY","object":{"id":1089,"text":"wsp2215 - 1984 - Availability and quality of water from the Dakota aquifer, northwest Iowa","indexId":"wsp2215","publicationYear":"1984","noYear":false,"title":"Availability and quality of water from the Dakota aquifer, northwest Iowa"},"id":1}],"supersededBy":{"id":1089,"text":"wsp2215 - 1984 - Availability and quality of water from the Dakota aquifer, northwest Iowa","indexId":"wsp2215","publicationYear":"1984","noYear":false,"title":"Availability and quality of water from the Dakota aquifer, northwest Iowa"},"lastModifiedDate":"2022-11-18T20:38:04.864552","indexId":"ofr82264","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":"82-264","title":"Availability and quality of water from the Dakota aquifer, northwest Iowa","docAbstract":"<p>The Dakota aquifer in northwest Iowa consists of sandstones in the Dakota Formation. It underlies most of the study area and is the most extensive source of ground water in the area. Individual sandstone beds are from less than 10 to more than 150 feet thick. The cumulative thickness of sandstone is more than 200 feet throughout much of the area. The aquifer is confined by overlying Cretaceous limestone and shale, Quaternary glacial deposits and loess. The underlying confining material is shale of the Dakota Formation, undifferentiated Paleozoic age rocks, or Precambrian crystalline rock.</p><p>Water flows through the aquifer from the north-central part of the study area to the east, south and southwest. Recharge is dominantly by infiltration from the land surface through the confining materials. Discharge is to underlying Paleozoic aquifers and to the alluvium and glacial outwash deposits along the Missouri and Big Sioux Rivers in the southwest part of the area. Flow components toward bedrock valleys may reflect discharge to Quaternary sand and gravel deposits in these valleys.</p><p>Pumping tests conducted in the study area indicate a narrow range of hydraulic conductivities of the Dakota aquifer, from 37 to 50 feet per day. Consequently, an average hydraulic conductivity of 40 feet per day was used to estimate the potential yield to wells completed in the aquifer. Yields of more than 250 gallons per minute can be expected throughout much of the study area and more than 1000 gallons per minute could be produced in some areas.</p><p>The quality of water from the Dakota is a calcium, magnesium, sulfate type. It is generally suitable for irrigation purposes, based on comparisons of sodium adsorption ratios and electrical conductivities. In some areas the aquifer has water with high salinity hazard that may restrict its use to irrigation of only well drained types of soil. The concentration of radium226 and other radionuclides exceed recommended limits at several sites.</p><p>The quality of water pumped from the aquifer may be altered by induced leakage from the underlying aquifers in Paleozoic age rocks if withdrawals reverse the pattern of natural flow from the Dakota into the Paleozoic aquifers. Evidence for such a reversal exists in the area around the city of LeMars.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr82264","collaboration":"Prepared in cooperation with the Iowa Geological Survey","usgsCitation":"Burkart, M.R., 1982, Availability and quality of water from the Dakota aquifer, northwest Iowa: U.S. Geological Survey Open-File Report 82-264, Report: 83 p.; 8 Plates: 17.84 x 21.84 inches or smaller, https://doi.org/10.3133/ofr82264.","productDescription":"Report: 83 p.; 8 Plates: 17.84 x 21.84 inches or smaller","costCenters":[],"links":[{"id":409478,"rank":10,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/0264/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":409477,"rank":9,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/0264/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":409476,"rank":8,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/0264/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":409475,"rank":7,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/0264/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":409474,"rank":6,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/0264/plate-5.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":409473,"rank":5,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/0264/plate-6.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":409472,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/0264/plate-7.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":409471,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/0264/plate-8.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":409470,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0264/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":140626,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0264/report-thumb.jpg"}],"country":"United States","state":"Iowa","otherGeospatial":"northwest Iowa","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"Polygon\",\"coordinates\":[[[-91.217706,43.50055],[-91.216035,43.481142],[-91.233367,43.455168],[-91.200359,43.412701],[-91.198953,43.389835],[-91.21477,43.365874],[-91.20662,43.352524],[-91.132813,43.32803],[-91.107237,43.313645],[-91.07371,43.274746],[-91.071698,43.261014],[-91.058644,43.257679],[-91.066398,43.239293],[-91.12217,43.197255],[-91.1462,43.152405],[-91.1562,43.142945],[-91.175253,43.134665],[-91.179457,43.067427],[-91.156562,42.978226],[-91.14543,42.958211],[-91.14988,42.941955],[-91.1438,42.922877],[-91.146177,42.90985],[-91.100565,42.883078],[-91.097656,42.859871],[-91.091837,42.851225],[-91.09406,42.830813],[-91.078665,42.827678],[-91.069549,42.769628],[-91.060261,42.761847],[-91.065783,42.753387],[-91.056297,42.747341],[-91.051275,42.737001],[-91.035418,42.73734],[-91.026786,42.724228],[-91.000128,42.716189],[-90.977735,42.696816],[-90.949213,42.685573],[-90.923634,42.6855],[-90.88743,42.67247],[-90.731132,42.643437],[-90.706303,42.634169],[-90.692031,42.610366],[-90.686975,42.591774],[-90.661527,42.567999],[-90.654127,42.5499],[-90.643927,42.540401],[-90.636927,42.513202],[-90.655927,42.491703],[-90.654027,42.478503],[-90.624328,42.458904],[-90.567968,42.440389],[-90.560439,42.432897],[-90.555018,42.416138],[-90.477279,42.383794],[-90.462619,42.367253],[-90.443874,42.355218],[-90.416535,42.325109],[-90.430884,42.27823],[-90.419326,42.254467],[-90.400653,42.239293],[-90.391108,42.225473],[-90.356964,42.205445],[-90.328273,42.201047],[-90.282173,42.178846],[-90.234919,42.165431],[-90.209479,42.15268],[-90.197342,42.128163],[-90.167533,42.122475],[-90.161159,42.106372],[-90.168358,42.075779],[-90.164485,42.042105],[-90.151579,42.030633],[-90.140061,42.003252],[-90.146225,41.981329],[-90.164135,41.956178],[-90.163847,41.944934],[-90.152659,41.933058],[-90.153584,41.906614],[-90.181401,41.844647],[-90.181973,41.80707],[-90.278633,41.767358],[-90.310708,41.742214],[-90.317668,41.72269],[-90.313435,41.698082],[-90.334525,41.679559],[-90.343452,41.646959],[-90.339528,41.598633],[-90.343228,41.587833],[-90.41283,41.565333],[-90.461432,41.523533],[-90.500633,41.518033],[-90.540935,41.526133],[-90.591037,41.512832],[-90.602137,41.506032],[-90.605937,41.494232],[-90.655839,41.462132],[-90.750142,41.449632],[-90.846558,41.455141],[-90.930016,41.421404],[-90.979815,41.434321],[-91.027787,41.423603],[-91.043988,41.415897],[-91.05101,41.387556],[-91.06652,41.365246],[-91.074841,41.305578],[-91.092034,41.286911],[-91.114186,41.250029],[-91.113648,41.241401],[-91.07298,41.207151],[-91.041536,41.166138],[-91.027214,41.163373],[-91.007586,41.166183],[-90.99496,41.160624],[-90.946627,41.096632],[-90.949383,41.072711],[-90.942253,41.034702],[-90.945949,41.006495],[-90.958142,40.979767],[-90.952233,40.954047],[-90.965344,40.921633],[-91.009536,40.900565],[-91.021562,40.884021],[-91.044653,40.868356],[-91.05643,40.848387],[-91.092993,40.821079],[-91.097649,40.805575],[-91.091703,40.779708],[-91.110424,40.745528],[-91.115735,40.725168],[-91.11194,40.697018],[-91.123928,40.669152],[-91.185428,40.638071],[-91.253074,40.637962],[-91.306524,40.626231],[-91.339719,40.613488],[-91.359873,40.601805],[-91.379752,40.57445],[-91.401482,40.559458],[-91.406373,40.551831],[-91.404125,40.539127],[-91.384531,40.530948],[-91.369059,40.512532],[-91.364211,40.500043],[-91.364915,40.484168],[-91.381769,40.442555],[-91.372554,40.4012],[-91.381958,40.387632],[-91.419422,40.378264],[-91.441243,40.386255],[-91.452458,40.375501],[-91.463895,40.375659],[-91.465116,40.385257],[-91.484507,40.3839],[-91.490977,40.393484],[-91.487829,40.403866],[-91.498093,40.401926],[-91.522333,40.409648],[-91.527057,40.416689],[-91.519012,40.431298],[-91.529132,40.434272],[-91.533548,40.440804],[-91.523271,40.450061],[-91.526155,40.458625],[-91.552691,40.458769],[-91.574746,40.465664],[-91.590817,40.492292],[-91.621353,40.510072],[-91.618028,40.53403],[-91.6219,40.542292],[-91.6887,40.55739],[-91.691557,40.564867],[-91.686357,40.580875],[-91.716769,40.59853],[-91.729115,40.61364],[-92.686693,40.589809],[-94.294813,40.571341],[-94.632032,40.571186],[-95.765645,40.585208],[-95.753148,40.59284],[-95.748626,40.603355],[-95.768926,40.621264],[-95.776251,40.647463],[-95.795489,40.662384],[-95.822913,40.66724],[-95.842801,40.677496],[-95.852615,40.702262],[-95.883178,40.717579],[-95.888907,40.731855],[-95.879027,40.753081],[-95.84662,40.768619],[-95.835232,40.779151],[-95.834523,40.787778],[-95.845342,40.811324],[-95.837186,40.835347],[-95.847084,40.854174],[-95.847785,40.864328],[-95.838735,40.872191],[-95.815933,40.879846],[-95.809474,40.891228],[-95.813458,40.901693],[-95.836438,40.921642],[-95.839743,40.93278],[-95.829074,40.975688],[-95.838908,40.986484],[-95.867286,41.001599],[-95.869486,41.009399],[-95.859918,41.025403],[-95.859654,41.035695],[-95.882415,41.060411],[-95.862587,41.088399],[-95.865888,41.117898],[-95.882088,41.143998],[-95.883489,41.154898],[-95.871912,41.168122],[-95.846188,41.166698],[-95.841288,41.174998],[-95.856788,41.187098],[-95.90969,41.184398],[-95.91829,41.186698],[-95.92599,41.195698],[-95.924891,41.211198],[-95.910891,41.231798],[-95.921891,41.264598],[-95.913991,41.271398],[-95.928691,41.281398],[-95.927491,41.298397],[-95.90589,41.300897],[-95.90429,41.293497],[-95.912491,41.279498],[-95.90249,41.273398],[-95.87689,41.285097],[-95.871489,41.295797],[-95.883089,41.316697],[-95.92569,41.322197],[-95.946891,41.334096],[-95.956691,41.345496],[-95.954891,41.351796],[-95.93549,41.360596],[-95.92879,41.370096],[-95.93689,41.396387],[-95.929721,41.411331],[-95.933169,41.42943],[-95.919865,41.447922],[-95.922529,41.455766],[-95.936801,41.46519],[-95.962329,41.46281],[-96.011757,41.476212],[-96.019542,41.486617],[-95.997903,41.504789],[-95.992599,41.514174],[-95.999529,41.538679],[-96.005079,41.544004],[-96.019686,41.545743],[-96.027289,41.541081],[-96.034305,41.512853],[-96.040701,41.507076],[-96.05369,41.508859],[-96.07307,41.525052],[-96.08822,41.530595],[-96.09409,41.539265],[-96.093613,41.558271],[-96.081152,41.577289],[-96.085771,41.585746],[-96.109387,41.596871],[-96.117558,41.609999],[-96.116233,41.621574],[-96.100701,41.635507],[-96.095046,41.647365],[-96.099837,41.66103],[-96.120983,41.677861],[-96.121401,41.688522],[-96.111968,41.697773],[-96.082429,41.698159],[-96.073063,41.705004],[-96.079682,41.717962],[-96.10261,41.728016],[-96.106425,41.73789],[-96.102772,41.746339],[-96.079915,41.757895],[-96.077543,41.777824],[-96.064537,41.793002],[-96.075548,41.807811],[-96.107592,41.820685],[-96.110246,41.84885],[-96.142045,41.868865],[-96.148826,41.888132],[-96.161756,41.90182],[-96.160767,41.908044],[-96.136743,41.920826],[-96.144583,41.941544],[-96.133318,41.955732],[-96.1289,41.969727],[-96.141228,41.978063],[-96.156538,41.980137],[-96.184243,41.976696],[-96.192141,41.984461],[-96.183568,41.999987],[-96.194556,42.008662],[-96.215225,42.006701],[-96.223896,41.995456],[-96.236487,41.996428],[-96.241932,42.006965],[-96.223611,42.022652],[-96.223822,42.033346],[-96.238392,42.041088],[-96.261132,42.038974],[-96.271427,42.044988],[-96.279342,42.07028],[-96.267636,42.096177],[-96.2689,42.11359],[-96.279203,42.12348],[-96.310085,42.132523],[-96.319528,42.146647],[-96.342395,42.160491],[-96.349688,42.172043],[-96.348066,42.194747],[-96.35987,42.210545],[-96.358141,42.214088],[-96.336323,42.218922],[-96.323723,42.229887],[-96.330004,42.240224],[-96.328905,42.254734],[-96.336003,42.264806],[-96.365792,42.285875],[-96.369212,42.308344],[-96.375307,42.318339],[-96.407998,42.337408],[-96.417786,42.351449],[-96.417093,42.361443],[-96.408436,42.376092],[-96.41498,42.393442],[-96.413609,42.407894],[-96.387608,42.432494],[-96.380707,42.446394],[-96.385407,42.473094],[-96.396107,42.484095],[-96.409408,42.487595],[-96.474409,42.491895],[-96.476909,42.497795],[-96.473339,42.503537],[-96.477454,42.509589],[-96.490089,42.512441],[-96.49297,42.517282],[-96.479909,42.524195],[-96.476952,42.556079],[-96.498041,42.558153],[-96.498709,42.57087],[-96.489328,42.5708],[-96.485796,42.575001],[-96.49545,42.579474],[-96.494777,42.585741],[-96.499885,42.588539],[-96.509468,42.61273],[-96.517048,42.615343],[-96.525671,42.609312],[-96.531604,42.615148],[-96.518542,42.62035],[-96.516338,42.630435],[-96.537881,42.646446],[-96.542366,42.660736],[-96.559281,42.657903],[-96.556461,42.663939],[-96.566684,42.675942],[-96.576381,42.671302],[-96.575299,42.682665],[-96.596405,42.688514],[-96.59908,42.697296],[-96.61017,42.694568],[-96.629625,42.705102],[-96.624446,42.714294],[-96.624704,42.725497],[-96.631931,42.725086],[-96.638621,42.734921],[-96.630485,42.750378],[-96.620548,42.753534],[-96.620272,42.757124],[-96.632212,42.761512],[-96.633168,42.768325],[-96.61949,42.784034],[-96.604559,42.783034],[-96.595283,42.792982],[-96.590757,42.808255],[-96.596008,42.815044],[-96.585699,42.818041],[-96.577937,42.827645],[-96.581604,42.837521],[-96.571353,42.837155],[-96.565605,42.830434],[-96.560572,42.839373],[-96.552092,42.836057],[-96.549513,42.839143],[-96.554709,42.846142],[-96.545502,42.849956],[-96.54146,42.857682],[-96.550439,42.863171],[-96.549659,42.870281],[-96.537851,42.878475],[-96.540396,42.888877],[-96.526563,42.893755],[-96.542847,42.903737],[-96.537354,42.908791],[-96.541689,42.922576],[-96.525536,42.935511],[-96.516203,42.933769],[-96.52012,42.938183],[-96.500308,42.959391],[-96.505028,42.970844],[-96.515922,42.972886],[-96.520773,42.980385],[-96.512237,42.985937],[-96.509986,42.995126],[-96.49782,42.998143],[-96.49167,43.009707],[-96.499187,43.019213],[-96.510995,43.024701],[-96.509146,43.03668],[-96.518431,43.042068],[-96.510256,43.049917],[-96.490365,43.050789],[-96.476905,43.062383],[-96.463094,43.062981],[-96.458201,43.067554],[-96.454188,43.083379],[-96.462636,43.089614],[-96.460516,43.09494],[-96.436589,43.120842],[-96.450361,43.142237],[-96.458854,43.143356],[-96.466537,43.150281],[-96.464896,43.182034],[-96.473834,43.189804],[-96.470781,43.205099],[-96.475571,43.221054],[-96.496454,43.223652],[-96.519273,43.21769],[-96.535741,43.22764],[-96.56044,43.224219],[-96.568505,43.231554],[-96.571194,43.238961],[-96.552963,43.247281],[-96.552591,43.257769],[-96.582904,43.26769],[-96.586317,43.274319],[-96.577588,43.2788],[-96.580346,43.298204],[-96.553087,43.29286],[-96.530392,43.300034],[-96.526004,43.309999],[-96.534913,43.336473],[-96.524289,43.347214],[-96.527345,43.368109],[-96.521323,43.374607],[-96.521572,43.38564],[-96.524044,43.394762],[-96.529152,43.397735],[-96.537116,43.395063],[-96.573579,43.419228],[-96.569628,43.427527],[-96.575181,43.431756],[-96.592905,43.43317],[-96.602608,43.449649],[-96.600039,43.45708],[-96.584603,43.46961],[-96.586364,43.478251],[-96.580997,43.481384],[-96.590452,43.494298],[-96.598396,43.495074],[-96.598929,43.500441],[-91.217706,43.50055]]]},\"properties\":{\"name\":\"Iowa\",\"nation\":\"USA  \"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a9be4b07f02db65dd34","contributors":{"authors":[{"text":"Burkart, M. R.","contributorId":42190,"corporation":false,"usgs":true,"family":"Burkart","given":"M.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":157165,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":4657,"text":"twri03A9_1982 - 1982 - Measurement of time of travel and dispersion in streams by dye tracing","interactions":[],"lastModifiedDate":"2012-02-02T00:05:38","indexId":"twri03A9_1982","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":336,"text":"Techniques of Water-Resources Investigations","code":"TWRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"03-A9","title":"Measurement of time of travel and dispersion in streams by dye tracing","docAbstract":"The use of fluorescent dyes and tracing techniques provides\r\na means for measuring the time-of-travel and dispersion\r\ncharacteristics of steady and gradually varied flow in\r\nstreams. Measurements of the dispersion and concentration\r\nof dyes give insight into the behavior of soluble contaminants\r\nthat may be introduced into a stream.\r\nThis manual describes methods of measuring time of\r\ntravel of water and waterborne solutes by dye tracing. The\r\nfluorescent dyes, measuring equipment used, and the field\r\nand laboratory procedures are also described.\r\nMethods of analysis and presentation to illustrate time-oftravel\r\nand dispersion characteristics of streams are provided.","language":"ENGLISH","publisher":"U.S. G.P.O.,","doi":"10.3133/twri03A9_1982","usgsCitation":"Hubbard, E., Kilpatrick, F.A., Martens, L., and Wilson, J.F., 1982, Measurement of time of travel and dispersion in streams by dye tracing (1982): U.S. Geological Survey Techniques of Water-Resources Investigations 03-A9, ix, 44 p. :ill., maps ;26 cm., https://doi.org/10.3133/twri03A9_1982.","productDescription":"ix, 44 p. :ill., maps ;26 cm.","costCenters":[],"links":[{"id":139327,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":156,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/twri/twri3-a9/pdf/twri_3-a9_ver1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"edition":"1982","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a28e4b07f02db611238","contributors":{"authors":[{"text":"Hubbard, E. F.","contributorId":66666,"corporation":false,"usgs":true,"family":"Hubbard","given":"E. F.","affiliations":[],"preferred":false,"id":149567,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Kilpatrick, F. A.","contributorId":22319,"corporation":false,"usgs":true,"family":"Kilpatrick","given":"F.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":149565,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Martens, L.A.","contributorId":52166,"corporation":false,"usgs":true,"family":"Martens","given":"L.A.","email":"","affiliations":[],"preferred":false,"id":149566,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Wilson, J. F. Jr.","contributorId":99541,"corporation":false,"usgs":true,"family":"Wilson","given":"J.","suffix":"Jr.","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":149568,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":4682,"text":"twri05A6 - 1982 - Quality assurance practices for the chemical and biological analyses of water and fluvial sediments","interactions":[],"lastModifiedDate":"2013-11-21T11:01:11","indexId":"twri05A6","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":336,"text":"Techniques of Water-Resources Investigations","code":"TWRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"05-A6","title":"Quality assurance practices for the chemical and biological analyses of water and fluvial sediments","docAbstract":"This chapter contains practices used by the U.S. Geological Survey to assure the quality of analytical data for water, fluvial sediment, and aquatic organisms. These practices are directed primarily toward personnel making water quality measurements. Some detail specific quality control techniques, others document quality assurance procedures being used by the Central Laboratories System of the U.S. Geological Survey, and still others describe various statistical techniques and give examples of their use in evaluating and assuring the quality of analytical data. The practices are arranged into eight sections: Analytical Methods Development Procedures, Standard Quantitative Analysis Techniques, Instrumental Techniques, Reference Material, Laboratory Quality Control; Quality Assurance Monitoring; Documentation, Summary, and Evaluation of Data, Materials Evaluation. Each section is preceded by a brief description of the material covered. Similarly within each section, each practice is preceded by a description of its application or scope.","language":"English","publisher":"U.S. Government Printing Office","doi":"10.3133/twri05A6","usgsCitation":"Friedman, L., and Erdmann, D.E., 1982, Quality assurance practices for the chemical and biological analyses of water and fluvial sediments: U.S. Geological Survey Techniques of Water-Resources Investigations 05-A6, ix, 181 p., https://doi.org/10.3133/twri05A6.","productDescription":"ix, 181 p.","numberOfPages":"164","costCenters":[{"id":343,"text":"Idaho Water Science Center","active":true,"usgs":true}],"links":[{"id":243,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/twri/twri5a6/","linkFileType":{"id":5,"text":"html"}},{"id":139154,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/twri/05a06/report-thumb.jpg"},{"id":31714,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/twri/05a06/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a8fe4b07f02db655218","contributors":{"authors":[{"text":"Friedman, Linda C.","contributorId":98702,"corporation":false,"usgs":true,"family":"Friedman","given":"Linda C.","affiliations":[],"preferred":false,"id":149617,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Erdmann, David E.","contributorId":62991,"corporation":false,"usgs":true,"family":"Erdmann","given":"David","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":149616,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":3869,"text":"cir863 - 1982 - Water-data program of the U.S. Geological Survey","interactions":[],"lastModifiedDate":"2012-02-02T00:05:36","indexId":"cir863","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":"863","title":"Water-data program of the U.S. Geological Survey","docAbstract":"The U.S. Geological Survey is the principal Federal agency responsible for the collection of hydrologic data needed for the planning, development, use, and management of the Nation 's water resources. These data are the foundation necessary for conducting analytical and interpretive appraisals describing the occurrence and availability of surface and ground waters, and their physical, chemical, and biological characteristics. The data are likewise required for basic and problem-oriented research in hydraulics, hydrology, and related fields. Hydrologic data collection by the Geological Survey began in 1894. Current operations include about 17,000 stations for collection of river, lake, and reservoir data; about 27,000 wells for collection of ground-water data; and almost 17,000 stations for collection of water-quality information. These activities are described as well as the means by which the data are made available, and how the program is coordinated with other agencies. (USGS)","language":"ENGLISH","publisher":"U.S. Dept. of the Interior, Geological Survey,","doi":"10.3133/cir863","usgsCitation":"Gilbert, B.K., and Buchanan, T.J., 1982, Water-data program of the U.S. Geological Survey: U.S. Geological Survey Circular 863, iii, 16 p. :ill., maps ;27 cm., https://doi.org/10.3133/cir863.","productDescription":"iii, 16 p. :ill., maps ;27 cm.","costCenters":[],"links":[{"id":126650,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/circ/1982/0863/report-thumb.jpg"},{"id":30961,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/1982/0863/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f1e4b07f02db5ee2c2","contributors":{"authors":[{"text":"Gilbert, Bruce K.","contributorId":60198,"corporation":false,"usgs":true,"family":"Gilbert","given":"Bruce","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":147761,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Buchanan, Thomas J.","contributorId":6842,"corporation":false,"usgs":true,"family":"Buchanan","given":"Thomas","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":147760,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":8080,"text":"ofr811197 - 1982 - Effects of effluent spray irrigation on ground water at a test site near Tarpon Springs, Florida","interactions":[],"lastModifiedDate":"2012-02-02T00:06:07","indexId":"ofr811197","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":"81-1197","title":"Effects of effluent spray irrigation on ground water at a test site near Tarpon Springs, Florida","docAbstract":"Secondary-treated effluent was applied to a 7.2-acre test site near Tarpon Springs, Fla., for about 1 year at an average rate of 0.06 million gallons per day and 3 years at 0.11 million gallons per day. Chemical fertilizer was applied periodically to the test site and adjacent areas. Periodic mounding of the water table occurred due to effluent irrigation, inducing radial flow from the test site. Physical, geochemical, biochemical processes effectively reduced total nitrogen concentration 90% and total phosphorous concentration more than 95% in the ground water of the surficial aquifer about 300 feet downgradient from the test site from that of the applied effluent. Downgradient, total nitrogen averaged 2.4 milligrams per liter and total phosphorus averaged 0.17 milligrams per liter. Substantial increases in total phosphorus were observed when the pH of the ground water increased. Total coliform bacteria in the ground water of the surficial aquifer were generally less than 100 colonies per 100 milliliters. Fecal coliform bacteria were generally less than 25 colonies per 100 milliliters at the test site and were not detected downgradient or near the test site. Fecal streptococcal bacteria were generally less than 100 colonies per 100 milliliters at the test site, but were detected on three occasions near the test site. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr811197","usgsCitation":"Brown, D., 1982, Effects of effluent spray irrigation on ground water at a test site near Tarpon Springs, Florida: U.S. Geological Survey Open-File Report 81-1197, iv, 40 p. ill., map ;28 cm., https://doi.org/10.3133/ofr811197.","productDescription":"iv, 40 p. ill., map ;28 cm.","costCenters":[],"links":[{"id":141464,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1981/1197/report-thumb.jpg"},{"id":35685,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1981/1197/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a2ee4b07f02db615a95","contributors":{"authors":[{"text":"Brown, D.P.","contributorId":95881,"corporation":false,"usgs":true,"family":"Brown","given":"D.P.","email":"","affiliations":[],"preferred":false,"id":157109,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":3648,"text":"cir856 - 1982 - Storage and retrieval of ground-water data at the U.S. Geological Survey","interactions":[],"lastModifiedDate":"2012-02-02T00:05:21","indexId":"cir856","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":"856","title":"Storage and retrieval of ground-water data at the U.S. Geological Survey","docAbstract":"The U.S. Geological Survey maintains a computerized Ground-Water Site-Inventory (GWSI) file that contains information about wells and springs at sites from all States of the United States. This file contains data collected by U.S. Geological Survey personnel and personnel of cooperating State, local and Federal agencies. The file is easily accessible to members or users of the National Water Data Exchange. Since the establishment of the GWSI file in 1974, the data base has grown 19% per year and contains information on about 770,000 sites as of February 1981. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/cir856","usgsCitation":"Mercer, M.W., and Morgan, C.O., 1982, Storage and retrieval of ground-water data at the U.S. Geological Survey: U.S. Geological Survey Circular 856, iii, 9 p. :ill., maps ;26 cm., https://doi.org/10.3133/cir856.","productDescription":"iii, 9 p. :ill., maps ;26 cm.","costCenters":[],"links":[{"id":123186,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/circ/1982/0856/report-thumb.jpg"},{"id":30690,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/1982/0856/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b31e4b07f02db6b41b9","contributors":{"authors":[{"text":"Mercer, Maria W.","contributorId":57828,"corporation":false,"usgs":true,"family":"Mercer","given":"Maria","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":147327,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Morgan, Charles O.","contributorId":66238,"corporation":false,"usgs":true,"family":"Morgan","given":"Charles","email":"","middleInitial":"O.","affiliations":[],"preferred":false,"id":147328,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":8027,"text":"ofr80557 - 1982 - Trichloroethylene in the ground-water supply of Pease Air Force Base, Portsmouth, New Hampshire","interactions":[],"lastModifiedDate":"2024-03-25T18:21:18.752437","indexId":"ofr80557","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":"80-557","title":"Trichloroethylene in the ground-water supply of Pease Air Force Base, Portsmouth, New Hampshire","docAbstract":"<p>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.</p><p>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.</p><p>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.</p>","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":7013,"text":"ofr82714 - 1982 - Assessment of the petroleum, coal, and geothermal resources of the Economic Community of West African States (ECOWAS) region","interactions":[],"lastModifiedDate":"2012-02-02T00:05:46","indexId":"ofr82714","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":"82-714","title":"Assessment of the petroleum, coal, and geothermal resources of the Economic Community of West African States (ECOWAS) region","docAbstract":"Approximately 85 percent of the land area of the ECOWAS (Economic Community of West African States) region is covered by basement rocks (igneous and highly metamorphosed rocks) or relatively thin layers of Paleozoic, Upper Precambrian, and 'Continental Intercalaire? sedimentary rocks. These areas have little or no petroleum potential. \r\n\r\nAreas of the ECOWAS region that have potential for petroleum production or potential for increased petroleum production include the narrow belt of sedimentary rocks that stretches along the continental margin from Mauritania to Nigeria and the Niger Delta and the Benue depression. The Senegal Basin, located on the continental margin of Mauritania, Senegal, Gambia, Guinea Bissau, and Guinea, has been intensely explored by the oil industry and most of the larger structures onshore and on the shelf probably have been tested by drilling with little or no resulting commercial production. Unless basic ideas pertaining to the petroleum geology of the Senegal Basin are revised, future discoveries are expected to be limited to small fields overlooked by industry at a time when petroleum prices were low. On the continental shelf of Sierra Leone and the continental shelf of northeast and central Liberia, the sedimentary rocks are relatively thin, and industry has shown little interest in the area. On the continental rise of these countries, however, the sedimentary section, deposited in a complex fault-block system, increases in thickness. A renewal of industry interest in this deep-water area will probably follow further development of deep-water production technology. A recent oil discovery on the continental slope off the Ivory Coast is expected to spur further exploration offshore of southeastern Liberia, Ivory Coast, Ghana, Togo, and Benin. This relatively unexplored area in the Gulf of Guinea has good possibilities .for the discovery of giant oil fields. \r\n\r\nNigeria's oil development from the Niger Delta may have peaked, as 13 of 14 giant oil fields were discovered prior to 1969 and the greatest number of fields were discovered in the period 1965 through 1967. Like delta regions in other parts of the world, individual oil fields of the Niger Delta are small to medium by world standards and future discoveries, therefore, are likely to reflect this reality. The natural gas resources of the Niger Delta, unlike its oil resources, are comparatively underdeveloped. \r\n\r\nParts of the Benue depression in Nigeria and Niger could contain significant deposits of petroleum. The lower Benue depression, immediately north of the Niger Delta, has been extensively explored by drilling. Except for noncommercial discoveries of oil and gas and traces of oil and gas on the ground surface, the results of exploration in the lower Benue depression were negative. However, in the Lake Chad area of Chad and in southern Chad near the Central African Republic boundary, oil and gas discoveries were made just prior to the cessation of all drilling and exploration activity in early 1979. It is rumored that these discoveries may be large although little information is available. The relation between the two areas in Chad and their overall relation to the Benue depression is poorly understood; however, the possibility of thick sedimentary sections containing Cretaceous marine source rock and Tertiary reservoir beds-all contained within grabens in a highly faulted failed-arm system subjected to high heat flow--is attractive. Of the ECOWAS countries, only Nigeria and Niger produce coal commercially. \r\n\r\nNigeria produces subbituminous coal from Paleocene-Maestrichtian and Maestrichtian (Late Cretaceous) age rocks of the Niger Delta region; reserves are estimated, on the basis of extensive drilling, to be 350 million tons (standard coal equivalent). In addition, lignite deposits of the Niger Delta appear to be large but have not been developed. Niger produces small amounts of coal used locally by uranium mine and mill operations from C","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr82714","usgsCitation":"Mattick, R., 1982, Assessment of the petroleum, coal, and geothermal resources of the Economic Community of West African States (ECOWAS) region: U.S. Geological Survey Open-File Report 82-714, 87 p., ill., maps ;28 cm., https://doi.org/10.3133/ofr82714.","productDescription":"87 p., ill., maps ;28 cm.","costCenters":[],"links":[{"id":139548,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0714/report-thumb.jpg"},{"id":34306,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0714/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4abae4b07f02db671d16","contributors":{"authors":[{"text":"Mattick, R. E. (compiler)","contributorId":65459,"corporation":false,"usgs":true,"family":"Mattick","given":"R. E.","suffix":"(compiler)","affiliations":[],"preferred":false,"id":153911,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":7020,"text":"ofr82235 - 1982 - Before the well runs dry; a workshop on how to design a local water conservation plan","interactions":[],"lastModifiedDate":"2012-02-02T00:05:46","indexId":"ofr82235","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":"82-235","title":"Before the well runs dry; a workshop on how to design a local water conservation plan","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr82235","usgsCitation":"Water Resources Division, U.S. Geological Survey, and Missouri River Basin Commission, 1982, Before the well runs dry; a workshop on how to design a local water conservation plan: U.S. Geological Survey Open-File Report 82-235, 141 leaves in various foliations :ill. ;28 cm., https://doi.org/10.3133/ofr82235.","productDescription":"141 leaves in various foliations :ill. ;28 cm.","costCenters":[],"links":[{"id":139558,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0235/report-thumb.jpg"},{"id":34311,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/0235/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":34312,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0235/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a54e4b07f02db62c380","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":528808,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Missouri River Basin Commission","contributorId":127915,"corporation":true,"usgs":false,"organization":"Missouri River Basin Commission","id":528807,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":4530,"text":"cir884 - 1982 - Annual report on Alaska's mineral resources","interactions":[],"lastModifiedDate":"2012-02-02T00:05:43","indexId":"cir884","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":"884","title":"Annual report on Alaska's mineral resources","language":"ENGLISH","publisher":"U.S. Dept. of the Interior, [Geological Survey,","doi":"10.3133/cir884","isbn":"0607887206 (pbk.)","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1982, Annual report on Alaska's mineral resources: U.S. Geological Survey Circular 884, v. 59 p. maps ;26 cm., https://doi.org/10.3133/cir884.","productDescription":"v. 59 p. maps ;26 cm.","costCenters":[],"links":[{"id":118454,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/circ/1982/0884/report-thumb.jpg"},{"id":31588,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/1982/0884/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac8e4b07f02db67b90d","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":528230,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":7087,"text":"ofr821039 - 1982 - Depth and temperature of permafrost on the Alaskan Arctic Slope; preliminary results","interactions":[],"lastModifiedDate":"2012-02-02T00:06:07","indexId":"ofr821039","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":"82-1039","title":"Depth and temperature of permafrost on the Alaskan Arctic Slope; preliminary results","docAbstract":"As permafrost is defined by its temperature, the only way to determine its depth is to monitor the return to equilibrium of temperatures in boreholes that penetrate permafrost. Such measurements are under way in 25 wells on the Alaskan Arctic Slope; 21 are in Naval Petroleum Reserve Alaska (NPRA), and 4 are in the foothills to the east. Near-equilibrium results indicate that permafrost thickness in NPRA generally ranges between 200 and 400 m (compared to 600+ m at Prudhoe Bay); there are large local variations and no conspicuous regional trends. By contrast the long-term mean temperature of the ground surface (one factor determining permafrost depth) varies systematically from north to south in a pattern modified by the regional topography. The observed variation in permafrost temperature and depth cannot result primarily from effects of surface bodies of water or regional variations in heat flow; they are consistent, however, with expectable variations in the thermal conductivity of the sediments. It remains to be determined (with conductivity measurements) whether certain sites with anomalously high local gradients have anomalously high heat flow; if they do, they might indicate upwelling of interstitial fluids in the underlying basin sediments.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr821039","usgsCitation":"Lachenbruch, A.H., Sass, J., Lawver, L., Brewer, M., and Moses, T., 1982, Depth and temperature of permafrost on the Alaskan Arctic Slope; preliminary results: U.S. Geological Survey Open-File Report 82-1039, 30 p. :ill., map ;28 cm., https://doi.org/10.3133/ofr821039.","productDescription":"30 p. :ill., map ;28 cm.","costCenters":[],"links":[{"id":141344,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/1039/report-thumb.jpg"},{"id":34414,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/1039/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aa8e4b07f02db667a77","contributors":{"authors":[{"text":"Lachenbruch, Arthur H.","contributorId":27850,"corporation":false,"usgs":true,"family":"Lachenbruch","given":"Arthur","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":154243,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Sass, J.H.","contributorId":70749,"corporation":false,"usgs":true,"family":"Sass","given":"J.H.","email":"","affiliations":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"preferred":false,"id":154245,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Lawver, L.A.","contributorId":73599,"corporation":false,"usgs":true,"family":"Lawver","given":"L.A.","email":"","affiliations":[],"preferred":false,"id":154246,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Brewer, M.C.","contributorId":54994,"corporation":false,"usgs":true,"family":"Brewer","given":"M.C.","email":"","affiliations":[],"preferred":false,"id":154244,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Moses, T.H.","contributorId":24344,"corporation":false,"usgs":true,"family":"Moses","given":"T.H.","email":"","affiliations":[],"preferred":false,"id":154242,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":7127,"text":"ofr811115 - 1982 - An evaluation of water-quality monitoring in the Brandywine Creek basin, Pennsylvania, 1973-78","interactions":[],"lastModifiedDate":"2017-06-20T10:02:13","indexId":"ofr811115","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":"81-1115","title":"An evaluation of water-quality monitoring in the Brandywine Creek basin, Pennsylvania, 1973-78","docAbstract":"Data recorded from 1973 through 1978 by monitors on West Branch Brandywine Creek at Modena, East Branch Brandywine Creek below Downingtown, and Brandywine Creek at Chadds Ford were analyzed to evaluate the effectiveness of the monitors in describing water-quality conditions. The data show that the stream at Modena and below Downingtown had periods of low dissolved oxygen, and that the stream below Downingtown had a particularly severe dissolved-oxygen deficiency from May through September 1974. The pH at all three sites exceeded 9.0 at times and the pH below Downingtown occasionally dropped below 6.0. The most critical period in the basin was from March to November when pH was most likely to exceed water-quality standards and dissolved oxygen was most likely to fall below the standards. Without the monitors, the extent and magnitude of these problems would not have been detected.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Harrisburg, PA","doi":"10.3133/ofr811115","usgsCitation":"Murphy, J., Ritter, J., Brown, A., and Chiarella, J., 1982, An evaluation of water-quality monitoring in the Brandywine Creek basin, Pennsylvania, 1973-78: U.S. Geological Survey Open-File Report 81-1115, iv, 28 p., https://doi.org/10.3133/ofr811115.","productDescription":"iv, 28 p.","additionalOnlineFiles":"N","costCenters":[{"id":532,"text":"Pennsylvania Water Science Center","active":true,"usgs":true}],"links":[{"id":141561,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1981/1115/report-thumb.jpg"},{"id":277911,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1981/1115/report.pdf"}],"country":"United States","state":"Pennsylvania","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -76.0000,39.7283 ], [ -76.0000,40.1250 ], [ -75.2563,40.1250 ], [ -75.2563,39.7283 ], [ -76.0000,39.7283 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad8e4b07f02db68484c","contributors":{"authors":[{"text":"Murphy, J.J.","contributorId":69144,"corporation":false,"usgs":true,"family":"Murphy","given":"J.J.","email":"","affiliations":[],"preferred":false,"id":154391,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Ritter, J.R.","contributorId":22350,"corporation":false,"usgs":true,"family":"Ritter","given":"J.R.","email":"","affiliations":[],"preferred":false,"id":154389,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Brown, A.E.","contributorId":48557,"corporation":false,"usgs":true,"family":"Brown","given":"A.E.","email":"","affiliations":[],"preferred":false,"id":154390,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Chiarella, J.P.","contributorId":17603,"corporation":false,"usgs":true,"family":"Chiarella","given":"J.P.","email":"","affiliations":[],"preferred":false,"id":154388,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":7139,"text":"ofr82537 - 1982 - A field study of littoral processes in Estero Bay, California","interactions":[],"lastModifiedDate":"2012-02-02T00:06:08","indexId":"ofr82537","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":"82-537","title":"A field study of littoral processes in Estero Bay, California","docAbstract":"Estero Bay, which lies on the central California coast, has rocky headlands at both ends and sandy beaches within it. The shoreline of the bay has adjusted to be in equilibrium with the predominant wave climate, which is from the northwest. Because of its present shoreline configuration, the net southward littoral transport found along much of the California coast does not occur within Estero Bay. Instead, the sand primarily moves on- and offshore with a reversing longshore component. This sand transport pattern produces a littoral cell within Estero Bay even though there is no submarine canyon in the area. The primary sand sinks for this cell appear to be the sand spit south of Morro Rock and the entrance to Morro Bay itself, although this opinion was not experimentally verified. \r\n\r\nField work during one summer (1978) and the following winter (1979) produced baseline data on the profile of and grain-size distribution across the littoral zone. In the offshore part of the littoral zone we also studied ripple size and type, internal structure, depth of erosion, and mineralogy. Although these data, which were collected along nine transects spaced 2 km apart, are inadequate to yield transport and energy rates, they indicate a northward decrease in wave energy within Estero Bay and a mixing of the sediments in the offshore. Box core and rod height data from grid points in seven meters of water showed that on the order of a meter of erosion occurred in the central part of the bay between the two sampling periods. Offshore, the data were incomplete, but at one station, in 17 m of water, at least 20 cm of erosion occurred.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr82537","usgsCitation":"Dingler, J., Anima, R.J., Molzan, D., Luepke, G., and Peterson, C., 1982, A field study of littoral processes in Estero Bay, California: U.S. Geological Survey Open-File Report 82-537, 41 p., ill., maps ;28 cm., https://doi.org/10.3133/ofr82537.","productDescription":"41 p., ill., maps ;28 cm.","costCenters":[],"links":[{"id":141541,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0537/report-thumb.jpg"},{"id":34445,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0537/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b24e4b07f02db6aeb7a","contributors":{"authors":[{"text":"Dingler, J.R.","contributorId":64247,"corporation":false,"usgs":true,"family":"Dingler","given":"J.R.","email":"","affiliations":[],"preferred":false,"id":154444,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Anima, R. J.","contributorId":106115,"corporation":false,"usgs":true,"family":"Anima","given":"R.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":154446,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Molzan, D.E.","contributorId":54995,"corporation":false,"usgs":true,"family":"Molzan","given":"D.E.","affiliations":[],"preferred":false,"id":154443,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Luepke, Gretchen","contributorId":91827,"corporation":false,"usgs":true,"family":"Luepke","given":"Gretchen","email":"","affiliations":[],"preferred":false,"id":154445,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Peterson, C.L.","contributorId":30986,"corporation":false,"usgs":true,"family":"Peterson","given":"C.L.","email":"","affiliations":[],"preferred":false,"id":154442,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":7175,"text":"ofr82299 - 1982 - Geologic reconnaissance and geochemical sampling survey of molybdenum mineralization near Schiestler Peak, Temple Peak Quadrangle, Sublette County, Wyoming","interactions":[],"lastModifiedDate":"2012-02-02T00:06:12","indexId":"ofr82299","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":"82-299","title":"Geologic reconnaissance and geochemical sampling survey of molybdenum mineralization near Schiestler Peak, Temple Peak Quadrangle, Sublette County, Wyoming","docAbstract":"A brief geologic reconnaissance and geochemical survey of molybdenum mineralization near Schiestler Peak, Sublette County, Wyo., indicates that molybdenite occurs in this area as disseminations and blebs in granitic or quartz monzonitic rocks intruded by felsic dikes of similar composition. Samples of stream sediments, panned concentrates from stream sediments, soils, rocks, and water were collected in the geochemical survey. Analytical results show that in reconnaissance, panned concentrates are the best of the sample types used in this study to detect molybdenum mineralization. More detailed analysis of the distribution of the molybdenum is best achieved through the collection of rock samples. Hydrothermal alteration is generally not conspicuous in the study area; however, rock samples that contain molybdenite are usually slightly enriched in silver, copper, lead, and in several instances, gold. Conversely, there appear to be negative associations between molybdenum and zinc and between molybdenum and several of the rare-earth elements. Mo concentrations in the rock samples with no visible molybdenite range from undetectable at a sensitivity of 5 parts per million (ppm) to 700 ppm. Mo content in rock samples containing visible molybdenite ranges from 10 ppm to greater than 2,000 ppm. Stream-sediment values range from undetected to 15 ppm; panned concentrates from undetected to 15 ppm; soils from undetected to 20 ppm. Analyses of the water samples indicate Mo concentrations from 0.8 parts per billion (ppb) to 4.8 ppb. As currently understood, this deposit is not extensive or continuous, but drilling to provide information on the vertical extent of mineralization may alter this opinion.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr82299","usgsCitation":"Lee, G.K., Antweiler, J., Love, J.D., and Benedict, J., 1982, Geologic reconnaissance and geochemical sampling survey of molybdenum mineralization near Schiestler Peak, Temple Peak Quadrangle, Sublette County, Wyoming: U.S. Geological Survey Open-File Report 82-299, 205 p., 4 over-size sheets, map ;28 cm., https://doi.org/10.3133/ofr82299.","productDescription":"205 p., 4 over-size sheets, map ;28 cm.","costCenters":[],"links":[{"id":141953,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0299/report-thumb.jpg"},{"id":34517,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/0299/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":34518,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/0299/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":34519,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/0299/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":34520,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/0299/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":34521,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0299/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae0e4b07f02db688442","contributors":{"authors":[{"text":"Lee, G. K.","contributorId":76722,"corporation":false,"usgs":true,"family":"Lee","given":"G.","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":154626,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Antweiler, J.C.","contributorId":35722,"corporation":false,"usgs":true,"family":"Antweiler","given":"J.C.","email":"","affiliations":[],"preferred":false,"id":154623,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Love, J. D.","contributorId":64620,"corporation":false,"usgs":true,"family":"Love","given":"J.","middleInitial":"D.","affiliations":[],"preferred":false,"id":154624,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Benedict, J.F.","contributorId":66688,"corporation":false,"usgs":true,"family":"Benedict","given":"J.F.","email":"","affiliations":[],"preferred":false,"id":154625,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":7204,"text":"ofr82279 - 1982 - Geotechnical properties of ash deposits near Hilo, Hawaii","interactions":[],"lastModifiedDate":"2012-02-02T00:06:00","indexId":"ofr82279","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":"82-279","title":"Geotechnical properties of ash deposits near Hilo, Hawaii","docAbstract":"Two holes were hand augered and sampled in ash deposits near Hilo, Hawaii. Color, water content and sensitivity of the ash were measured in the field. The ash alternated between reddish brown and dark reddish brown in color and had water contents as high as 392%. A downhole vane shear device measured sensitivities as high as 6.9. A series of laboratory tests including grain size distribution, Atterberg limits, X-ray diffraction analysis, total carbon determination, vane shear, direct shear and triaxial tests were performed to determine the composition and geotechnical properties of the ash. The ash is very fine grained, highly plastic and composed mostly of gibbsite and amorphous material presumably allophane. The ash has a high angle of internal friction ranging from 40-43? and is classified as medium to very sensitive. \r\n\r\nA series of different ash layers was distinguished on the basis of plasticity and other geotechnical properties. Sensitivity may be due to a metastable fabric, cementation, leaching, high organic content, and thixotropy. The sensitivity of the volcanic ash deposits near Hilo is consistent with documented slope instability during earthquakes in Hawaii. The high angles of internal friction and cementation permit very steep slopes under static conditions. However, because of high sensitivity of the ash, these slopes are particularly susceptible to seismically-induced landsliding.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr82279","usgsCitation":"Wieczorek, G.F., Jibson, R., Wilson, R.C., and Buchanan-Banks, J., 1982, Geotechnical properties of ash deposits near Hilo, Hawaii: U.S. Geological Survey Open-File Report 82-279, 20 p., ill., maps ;28 cm., https://doi.org/10.3133/ofr82279.","productDescription":"20 p., ill., maps ;28 cm.","costCenters":[],"links":[{"id":140189,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0279/report-thumb.jpg"},{"id":34603,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0279/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac7e4b07f02db67b085","contributors":{"authors":[{"text":"Wieczorek, G. F.","contributorId":50143,"corporation":false,"usgs":true,"family":"Wieczorek","given":"G.","middleInitial":"F.","affiliations":[],"preferred":false,"id":154753,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Jibson, R.W.","contributorId":8467,"corporation":false,"usgs":true,"family":"Jibson","given":"R.W.","email":"","affiliations":[],"preferred":false,"id":154751,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Wilson, R. C.","contributorId":50889,"corporation":false,"usgs":true,"family":"Wilson","given":"R.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":154754,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Buchanan-Banks, J.M.","contributorId":32918,"corporation":false,"usgs":true,"family":"Buchanan-Banks","given":"J.M.","affiliations":[],"preferred":false,"id":154752,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
]}