Teleseismic data were recorded within the Sierra Nevada to look for lateral variations in the upper mantle. The data were collected at both temporary and permanent stations, and P wave residuals were computed. After correcting the P residual data for crustal and topographic effects, there is still a variation of as much as 0.5-0.6 s from the north end of the Sierra Nevada to Mono Lake, located east of the central part of the range. In addition, there are significant variations in travel time patterns, depending on the azimuth of wave arrivals. Two simple modeling approaches have been used to infer the upper mantle velocity structure from the observed variations in travel time. In the first, it is assumed that the velocity variations are distributed throughout a depth range of about 60–160 km. One model that fits the data indicates a north-to-south trend in upper mantle P velocities from about 7.9 km/s at the north end of the Sierra to 7.6 km/s near Mono Lake. Superimposed is a west-to-east trend from 7.85 km/s under the Sierra Nevada crest to 7.7 km/s east of Lake Tahoe. In the second modeling approach, a fixed velocity contrast is assumed between the lithosphere and asthenosphere with variations in travel time resulting from variations in lithospheric thickness. One model, consistent with the observations, indicates a thinning of the lithosphere from 110 km at the north end of the Sierra to 60 km near Mono Lake.
","language":"English","publisher":"American Geophysical Union","doi":"10.1029/JB088iB07p05874","issn":"01480227","usgsCitation":"Mavko, B., and Thompson, G.A., 1983, Crustal and upper mantle structure of the northern and central Sierra Nevada: Journal of Geophysical Research Solid Earth, v. 88, no. B7, p. 5874-5892, https://doi.org/10.1029/JB088iB07p05874.","productDescription":"19 p.","startPage":"5874","endPage":"5892","numberOfPages":"19","costCenters":[],"links":[{"id":220802,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"88","issue":"B7","noUsgsAuthors":false,"publicationDate":"2012-09-20","publicationStatus":"PW","scienceBaseUri":"5059fcd8e4b0c8380cd4e472","contributors":{"authors":[{"text":"Mavko, B.B.","contributorId":11331,"corporation":false,"usgs":true,"family":"Mavko","given":"B.B.","email":"","affiliations":[],"preferred":false,"id":362465,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Thompson, G. A.","contributorId":90332,"corporation":false,"usgs":true,"family":"Thompson","given":"G.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":362466,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70011995,"text":"70011995 - 1983 - The relationship of acquisition systems to automated stereo correlation.","interactions":[],"lastModifiedDate":"2012-03-12T17:18:34","indexId":"70011995","displayToPublicDate":"1983-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3052,"text":"Photogrammetric Engineering and Remote Sensing","active":true,"publicationSubtype":{"id":10}},"title":"The relationship of acquisition systems to automated stereo correlation.","docAbstract":"Today a concerted effort is being made to expedite the mapping process through automated correlation of stereo data. Stereo correlation involves the comparison of radiance (brightness) signals or patterns recorded by sensors. Conventionally, two-dimensional area correlation is utilized but this is a rather slow and cumbersome procedure. Digital correlation can be performed in only one dimension where suitable signal patterns exist, and the one-dimensional mode is much faster. Electro-optical (EO) systems, suitable for space use, also have much greater flexibility than film systems. Thus, an EO space system can be designed which will optimize one-dimensional stereo correlation and lead toward the automation of topographic mapping.-from Author","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Photogrammetric Engineering and Remote Sensing","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","usgsCitation":"Colvocoresses, A., 1983, The relationship of acquisition systems to automated stereo correlation.: Photogrammetric Engineering and Remote Sensing, v. 49, no. 4, p. 539-544.","startPage":"539","endPage":"544","numberOfPages":"6","costCenters":[],"links":[{"id":220804,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"49","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505baf21e4b08c986b324582","contributors":{"authors":[{"text":"Colvocoresses, A. P.","contributorId":82703,"corporation":false,"usgs":true,"family":"Colvocoresses","given":"A. P.","affiliations":[],"preferred":false,"id":362468,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70012009,"text":"70012009 - 1983 - Geotherm: the U.S. geological survey geothermal information system","interactions":[],"lastModifiedDate":"2013-01-21T15:50:49","indexId":"70012009","displayToPublicDate":"1983-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1315,"text":"Computers & Geosciences","printIssn":"0098-3004","active":true,"publicationSubtype":{"id":10}},"title":"Geotherm: the U.S. geological survey geothermal information system","docAbstract":"GEOTHERM is a comprehensive system of public databases and software used to store, locate, and evaluate information on the geology, geochemistry, and hydrology of geothermal systems. Three main databases address the general characteristics of geothermal wells and fields, and the chemical properties of geothermal fluids; the last database is currently the most active. System tasks are divided into four areas: (1) data acquisition and entry, involving data entry via word processors and magnetic tape; (2) quality assurance, including the criteria and standards handbook and front-end data-screening programs; (3) operation, involving database backups and information extraction; and (4) user assistance, preparation of such items as application programs, and a quarterly newsletter. The principal task of GEOTHERM is to provide information and research support for the conduct of national geothermal-resource assessments. The principal users of GEOTHERM are those involved with the Geothermal Research Program of the U.S. Geological Survey. Information in the system is available to the public on request. ?? 1983.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Computers and Geosciences","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"Elsevier","publisherLocation":"Amsterdam, Netherlands","doi":"10.1016/0098-3004(83)90034-1","issn":"00983004","usgsCitation":"Bliss, J.D., and Rapport, A., 1983, Geotherm: the U.S. geological survey geothermal information system: Computers & Geosciences, v. 9, no. 1, p. 35-39, https://doi.org/10.1016/0098-3004(83)90034-1.","startPage":"35","endPage":"39","numberOfPages":"5","costCenters":[],"links":[{"id":266193,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1016/0098-3004(83)90034-1"},{"id":222179,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"9","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a28c8e4b0c8380cd5a3e0","contributors":{"authors":[{"text":"Bliss, J. D.","contributorId":25564,"corporation":false,"usgs":true,"family":"Bliss","given":"J.","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":362509,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Rapport, A.","contributorId":97109,"corporation":false,"usgs":true,"family":"Rapport","given":"A.","email":"","affiliations":[],"preferred":false,"id":362510,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70011351,"text":"70011351 - 1983 - Can the earth be dated from decay of its magnetic field?.","interactions":[],"lastModifiedDate":"2024-05-07T16:38:26.184541","indexId":"70011351","displayToPublicDate":"1983-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2307,"text":"Journal of Geological Education","active":true,"publicationSubtype":{"id":10}},"title":"Can the earth be dated from decay of its magnetic field?.","docAbstract":"Thomas G. Barnes, Emeritus Professor of Physics at the University of Texas, El Paso, and a creationist, argues that the geomagnetic field was created by unknown processes at the time of creation of the earth and has been decaying irreversibly and exponentially, with a half-life of about 1400 years, since then. He calculates that the field would have been impossibly large in 8000 B.C. and concludes that the earth, therefore, is less than 10,000 years old. He denies that the earth's field has reversed polarity in the past, and attempts to refute the dynamo theory of the origin of the field. Barnes' arguments and conclusions are commonly cited in creationist literature as definitive proof that the earth is very young. Barnes is wrong, and has ignored or misrepresented much of the data on the earth's magnetic field.
Barnes calculations are based on observatory measurements showing that the earth's dipole field strength has decreased since 1835. But these same measurements also show a corresponding increase in the strength of the nondipole field so that the total field energy external to the core has remained about constant. Paleomagnetic evidence shows that the earth's field has existed for more than three billion years, and that the dipole field both fluctuates in strength and irregularly reverses polarity. The earth's field is generated by a fluid dynamo in the iron-nickel core; all of the elements necessary for a dynamo, including fluid motion and energy sources, are present. Contrary to Barnes' assertions, there are no theoretical reasons why a dynamo cannot exist in the earth.
There are no properties of the magnetid field that can be used to place an upper limit on the earth's age.
","language":"English","publisher":"Taylor & Francis","doi":"10.5408/0022-1368-31.2.124","issn":"00221368","usgsCitation":"Dalrymple, G.B., 1983, Can the earth be dated from decay of its magnetic field?.: Journal of Geological Education, v. 31, no. 2, p. 124-133, https://doi.org/10.5408/0022-1368-31.2.124.","productDescription":"10 p.","startPage":"124","endPage":"133","numberOfPages":"10","costCenters":[],"links":[{"id":480230,"rank":2,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.5408/0022-1368-31.2.124","text":"Publisher Index Page"},{"id":220974,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"31","issue":"2","noUsgsAuthors":false,"publicationDate":"2018-02-13","publicationStatus":"PW","scienceBaseUri":"5059f33be4b0c8380cd4b69b","contributors":{"authors":[{"text":"Dalrymple, G. B.","contributorId":10407,"corporation":false,"usgs":true,"family":"Dalrymple","given":"G.","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":360893,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70011197,"text":"70011197 - 1983 - Scoresum - A technique for displaying and evaluating multi-element geochemical information, with examples of its use in regional mineral assessment programs","interactions":[],"lastModifiedDate":"2025-03-07T16:52:51.250953","indexId":"70011197","displayToPublicDate":"1983-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2302,"text":"Journal of Geochemical Exploration","active":true,"publicationSubtype":{"id":10}},"title":"Scoresum - A technique for displaying and evaluating multi-element geochemical information, with examples of its use in regional mineral assessment programs","docAbstract":"Two contrasting models of the earthquake deformation cycle on strike slip faults predict significant temporal declines in shear strain rate near the fault, accompanied by a progressive broadening of the zone of deformation adjacent to it. In the thin lithosphere model, transient deformation results from flow in the asthenosphere due to stress relaxation following faulting through most or all of the lithosphere. For an earth model with a thick elastic lithosphere (plate thickness » depth of seismic slip), transient motions are due to postearthquake aseisrnic slip below the coseismic fault plane. Data from the San Andreas fault indicate a long-term temporal decrease in strain rate that persists for at least 30 years and may extend through the entire earthquake cycle. Observations support a cycle-long rate decrease and a temporal spreading of the deformation profile only if movement cycles on the northern and southern locked sections of the fault are basically similar. If so, the usually lower strain rates and broader deformation zone currently observed on the southern San Andreas represent a later evolutionary stage of the northern locked section, where a great earthquake is a more recent occurrence. Although the data allow some extreme models to be discarded, no sufficiently strong constraints exist to decide between the thin and thick lithosphere models. Regardless of the appropriate model the geodetic observations themselves indicate that strain buildup is sufficiently nonlinear to cause significant departures from recurrence estimates based on linear strain accumulation and the time-predictable model.
","language":"English","publisher":"American Geophysical Union","doi":"10.1029/JB088iB07p05893","issn":"01480227","usgsCitation":"Thatcher, W., 1983, Nonlinear strain buildup and the earthquake cycle on the San Andreas fault: Journal of Geophysical Research Solid Earth, v. 88, no. B7, p. 5893-5902, https://doi.org/10.1029/JB088iB07p05893.","productDescription":"10 p.","startPage":"5893","endPage":"5902","numberOfPages":"10","costCenters":[],"links":[{"id":222288,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"88","issue":"B7","noUsgsAuthors":false,"publicationDate":"2012-09-20","publicationStatus":"PW","scienceBaseUri":"505a6793e4b0c8380cd733d0","contributors":{"authors":[{"text":"Thatcher, W.","contributorId":32669,"corporation":false,"usgs":true,"family":"Thatcher","given":"W.","email":"","affiliations":[],"preferred":false,"id":362795,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70010326,"text":"70010326 - 1983 - Maps for the nation: The current federal mapping establishment","interactions":[],"lastModifiedDate":"2023-11-29T16:43:32.147923","indexId":"70010326","displayToPublicDate":"1983-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1851,"text":"Government Publications Review","active":true,"publicationSubtype":{"id":10}},"title":"Maps for the nation: The current federal mapping establishment","docAbstract":"The U.S. Government annually produces an estimated 53,000 new maps and charts and distributes about 160 million copies. A large number of these maps are produced under the national mapping program, a decentralized Federal/State cooperative approach to mapping the country at standard scales. Circular A-16, issued by the Office of Management and Budget in 1953 and revised in 1967, delegates the mapping responsibilities to various federal agencies. The U.S. Department of the Interior's Geological Survey is the principal federal agency responsible for implementing the national mapping program. Other major federal map producing agencies include the Departments of Agriculture, Commerce, Defense, Housing and Urban Development, and Transportation, and the Tennessee Valley Authority. To make maps and mapping information more readily available, the National Cartographic Information Center was established in 1974 and an expanded National Map Library Depository Program in 1981. The most recent of many technological advances made under the mapping program are in the areas of digital cartography and video disc and optical disc information storage systems. Future trends and changes in the federal mapping program will involve expanded information and customer service operations, further developments in the production and use of digital cartographic data, and consideration of a Federal Mapping Agency.
","language":"English","publisher":"Elsevier","doi":"10.1016/0277-9390(83)90075-4","usgsCitation":"North, G.W., 1983, Maps for the nation: The current federal mapping establishment: Government Publications Review, v. 10, no. 4, p. 345-360, https://doi.org/10.1016/0277-9390(83)90075-4.","productDescription":"16 p.","startPage":"345","endPage":"360","numberOfPages":"16","costCenters":[{"id":430,"text":"National Mapping Program","active":false,"usgs":true}],"links":[{"id":218714,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -130.67138671875,\n 54.686534234529695\n ],\n [\n -129.9462890625,\n 55.36662484928637\n ],\n [\n -130.1220703125,\n 56.145549500679074\n ],\n [\n -131.9677734375,\n 56.9449741808516\n 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}\n }\n ]\n}","volume":"10","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a50ace4b0c8380cd6b84f","contributors":{"authors":[{"text":"North, Gary W.","contributorId":28587,"corporation":false,"usgs":true,"family":"North","given":"Gary","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":358648,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70011366,"text":"70011366 - 1983 - Objective procedures for lineament enhancement and extraction","interactions":[],"lastModifiedDate":"2017-01-18T14:43:51","indexId":"70011366","displayToPublicDate":"1983-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3052,"text":"Photogrammetric Engineering and Remote Sensing","active":true,"publicationSubtype":{"id":10}},"title":"Objective procedures for lineament enhancement and extraction","docAbstract":"A longterm research goal at EROS Data Center is to develop automated, objective procedures for lineament mapping. In support of this goal, a five-step digital convolution procedure has been used to produce directionally enhanced images, which contain few artifacts and little noise. The main limitation of this procedure is that little enhancement of lineaments occurs in dissected terrain, in shadowed areas, and in flat areas with a uniform land cover. The directional enhancement procedure can be modified to extract edge and line segments from an image. Any of various decision rules can then be used to connect the line segments and to produce a final lineament map. The result is an interpretive map, but one that is based on an objective extraction of lineament components by digital processing. -from Authors","language":"English","usgsCitation":"Moore, G.K., and Waltz, F., 1983, Objective procedures for lineament enhancement and extraction: Photogrammetric Engineering and Remote Sensing, v. 49, no. 5, p. 641-647.","productDescription":"7 p.","startPage":"641","endPage":"647","numberOfPages":"7","costCenters":[{"id":222,"text":"Earth Resources Observation and Science (EROS) Center","active":true,"usgs":true}],"links":[{"id":221230,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"49","issue":"5","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a6a27e4b0c8380cd7401b","contributors":{"authors":[{"text":"Moore, G. K.","contributorId":67550,"corporation":false,"usgs":true,"family":"Moore","given":"G.","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":360928,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Waltz, F. A.","contributorId":44034,"corporation":false,"usgs":true,"family":"Waltz","given":"F. A.","affiliations":[],"preferred":false,"id":360927,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":30342,"text":"wri8159 - 1982 - Effects of land use on surface-water quality in the East Everglades, Dade County, Florida","interactions":[],"lastModifiedDate":"2021-12-13T12:29:37.561555","indexId":"wri8159","displayToPublicDate":"2021-12-12T20:45:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"81-59","title":"Effects of land use on surface-water quality in the East Everglades, Dade County, Florida","docAbstract":"Water-quality characteristics were determined at five developed areas in the East Everglades, Dade County, Florida, during the 1978 wet season (June through October). These areas are designated as: Coopertown; Chekika Hammock State Park; residential area; rock-plowed tomato field; and Cracker Jack Slough agricultural area. Data from the developed areas were compared with data from four baseline sites in undeveloped areas to determine the effects of land use on the surface-water quality. The rock-plowed tomato field was the only area where surface-water quality was affected. Water quality at this field is affected by agricultural activities and chemical applications as indicated by increased concentrations of orthophosphate, organic nitrogen, organic carbon, copper, manganese, mercury, and potassium. The remaining four areas of land use had water-quality characteristics typical of baseline sites in nearby Northeast Shark River Slough or Taylor Slough. Chemical analyses of soil indicated chlorinated-hydrocarbon insecticide residues at Coopertown and the two agricultural areas, Cracker Jack Slough and the rock-plowed tomato field. Trace elements in concentrations greater than base level occurred at both agricultural areas (manganese), Chekika Hammock State Park (manganese), and at Coopertown (lead and zinc). (USGS)","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wri8159","collaboration":"Prepared in cooperation with the Metropolitan Dade County Planning Department","usgsCitation":"Waller, B.G., 1982, Effects of land use on surface-water quality in the East Everglades, Dade County, Florida: U.S. Geological Survey Water-Resources Investigations Report 81-59, Report: v, 37 p.; 2 Plates: 32.88 x 30.00 inches or smaller, https://doi.org/10.3133/wri8159.","productDescription":"Report: v, 37 p.; 2 Plates: 32.88 x 30.00 inches or smaller","costCenters":[{"id":27821,"text":"Caribbean-Florida Water Science Center","active":true,"usgs":true}],"links":[{"id":159305,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1981/0059/coverthb.jpg"},{"id":59135,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1981/0059/wri8159_plate1.pdf","text":"Plate 1","size":"4.17 MB","linkFileType":{"id":1,"text":"pdf"}},{"id":59136,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1981/0059/wri8159_plate2.pdf","text":"Plate 2","size":"3.94 MB","linkFileType":{"id":1,"text":"pdf"}},{"id":2480,"rank":100,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1981/0059/wri8159.pdf","text":"Report","size":"1.56 MB","linkFileType":{"id":1,"text":"pdf"},"description":"WRI 81-59"}],"country":"United States","state":"Florida","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -80.66162109375,\n 25.18505888358067\n ],\n [\n -79.98046875,\n 25.18505888358067\n ],\n [\n -79.98046875,\n 25.997549919572112\n ],\n [\n -80.66162109375,\n 25.997549919572112\n ],\n [\n -80.66162109375,\n 25.18505888358067\n ]\n ]\n ]\n }\n }\n ]\n}","contact":"Caribbean-Florida Water Science Center
U.S. Geological Survey
3321 College Avenue
Davie, FL 33314
Caribbean-Florida Water Science Center
U.S. Geological Survey
3321 College Avenue
Davie, FL 33314
No abstract available.
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\"}}]}","contact":"","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49fbe4b07f02db5f4636","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":532960,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70180227,"text":"70180227 - 1982 - Reconnaissance geochemical studies in the Bristol Bay, Ugashik, and Karluk quadrangles, Alaska: A section in The United States Geological Survey in Alaska: Accomplishments during 1980","interactions":[{"subject":{"id":70180227,"text":"70180227 - 1982 - Reconnaissance geochemical studies in the Bristol Bay, Ugashik, and Karluk quadrangles, Alaska: A section in The United States Geological Survey in Alaska: Accomplishments during 1980","indexId":"70180227","publicationYear":"1982","noYear":false,"title":"Reconnaissance geochemical studies in the Bristol Bay, Ugashik, and Karluk quadrangles, Alaska: A section in The United States Geological Survey in Alaska: Accomplishments during 1980"},"predicate":"IS_PART_OF","object":{"id":4434,"text":"cir844 - 1982 - The United States Geological Survey in Alaska: Accomplishments during 1980","indexId":"cir844","publicationYear":"1982","noYear":false,"title":"The United States Geological Survey in Alaska: Accomplishments during 1980"},"id":1}],"isPartOf":{"id":4434,"text":"cir844 - 1982 - The United States Geological Survey in Alaska: Accomplishments during 1980","indexId":"cir844","publicationYear":"1982","noYear":false,"title":"The United States Geological Survey in Alaska: Accomplishments during 1980"},"lastModifiedDate":"2017-01-27T11:13:10","indexId":"70180227","displayToPublicDate":"2017-01-01T00:00:00","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":"844","title":"Reconnaissance geochemical studies in the Bristol Bay, Ugashik, and Karluk quadrangles, Alaska: A section in The United States Geological Survey in Alaska: Accomplishments during 1980","docAbstract":"Geochemical reconnaissance studies in the Bristol Bay, Ugashik, and Karluk quadrangles were completed with collection and analyses of more than 1,200 stream-sediment and heavy mineral-concentrate samples during 1979 and 1980. At least two areas of possible metallic mineral occurrence have been delineated by results of the analyses, geologic fieldwork, and data provided by Bear Creek Mining Company.
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\"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"587f3df8e4b0d96de256459b","contributors":{"authors":[{"text":"Hooper, David","contributorId":14121,"corporation":false,"usgs":true,"family":"Hooper","given":"David","affiliations":[],"preferred":false,"id":658712,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Schwarting, Richard","contributorId":178399,"corporation":false,"usgs":false,"family":"Schwarting","given":"Richard","email":"","affiliations":[],"preferred":false,"id":658713,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70162190,"text":"70162190 - 1982 - Gasometer: An inexpensive device for continuous monitoring of dissolved gases and supersaturation","interactions":[],"lastModifiedDate":"2016-01-14T16:12:12","indexId":"70162190","displayToPublicDate":"2015-09-08T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3624,"text":"Transactions of the American Fisheries Society","active":true,"publicationSubtype":{"id":10}},"title":" Gasometer: An inexpensive device for continuous monitoring of dissolved gases and supersaturation","docAbstract":"The “gasometer” is a device that measures differential dissolved-gas pressures (δP) in water relative to barometric pressure (as does the “Weiss saturometer”), but operates continuously without human attention. The gasometer can be plumbed into a water-supply system and requires 8 liters/minute of water or more at 60 kilopascals. The gasometer's surfaces are nontoxic, and flow-through water can be used for fish culture. The gasometer may be connected to a small submersible pump and operated as a portable unit. The gasometer can activate an alarm system and thus protect fish from hyperbaric (supersaturation) or hypobaric gas pressures (usually due to low dissolved oxygen). Instructions are included for calculating and reporting data including the pressure and saturation of individual gases. Construction and performance standards are given for the gasometer. Occasional cleaning is required to remove biofouling from the gas-permeable tubing.
","language":"English","publisher":"American Fisheries Society","doi":"10.1577/1548-8659(1982)111<505:G>2.0.CO;2","usgsCitation":"Bouck, G., 1982, Gasometer: An inexpensive device for continuous monitoring of dissolved gases and supersaturation: Transactions of the American Fisheries Society, v. 111, no. 4, p. 505-516, https://doi.org/10.1577/1548-8659(1982)111<505:G>2.0.CO;2.","productDescription":"12 p.","startPage":"505","endPage":"516","numberOfPages":"12","costCenters":[],"links":[{"id":314400,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"111","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5698d4b8e4b0fbd3f7fa4bf4","contributors":{"authors":[{"text":"Bouck, G.R.","contributorId":152274,"corporation":false,"usgs":false,"family":"Bouck","given":"G.R.","email":"","affiliations":[],"preferred":false,"id":588799,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70047700,"text":"70047700 - 1982 - Developing a state water plan: Ground-water conditions in Utah, spring of 1982","interactions":[{"subject":{"id":51038,"text":"ofr51139 - 1951 - Discharge of wells in East Shore area, Utah","indexId":"ofr51139","publicationYear":"1951","noYear":false,"title":"Discharge of wells in East Shore area, Utah"},"predicate":"SUPERSEDED_BY","object":{"id":70047700,"text":"70047700 - 1982 - Developing a state water plan: Ground-water conditions in Utah, spring of 1982","indexId":"70047700","publicationYear":"1982","noYear":false,"title":"Developing a state water plan: Ground-water conditions in Utah, spring of 1982"},"id":1},{"subject":{"id":51791,"text":"ofr54325 - 1954 - Inventory of ground-water pumpage in three irrigation districts in southern Utah","indexId":"ofr54325","publicationYear":"1954","noYear":false,"title":"Inventory of ground-water pumpage in three irrigation districts in southern Utah"},"predicate":"SUPERSEDED_BY","object":{"id":70047700,"text":"70047700 - 1982 - Developing a state water plan: Ground-water conditions in Utah, spring of 1982","indexId":"70047700","publicationYear":"1982","noYear":false,"title":"Developing a state water plan: Ground-water conditions in Utah, spring of 1982"},"id":2}],"lastModifiedDate":"2017-01-20T17:57:36","indexId":"70047700","displayToPublicDate":"2013-01-01T15:15:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":2,"text":"State or Local Government Series"},"seriesTitle":{"id":110,"text":"Cooperative Investigations Report","active":true,"publicationSubtype":{"id":2}},"seriesNumber":"22","title":"Developing a state water plan: Ground-water conditions in Utah, spring of 1982","docAbstract":"This is the nineteenth in a series of annual reports that describe ground-water conditions in Utah. Reports in this series, published cooperatively by the U.S. Geological Survey and the Utah Division of Water Resources, provide data to enable interested parties to keep abreast of changing ground-water conditions.
This report, like the others in the series, contains information on well construction, ground-water withdrawals from wells, water-level changes, and related changes in precipitation and streamflow. Supplementary data such as graphs showing chemical quality of water and maps showing ground-water level contours are included in reports of this series only for those years or areas for which applicable data are available and are important to a discussion of changing ground-water conditions.
This report includes individual discussions of selected major areas of ground-water development in the State for the calendar year 1981. Water-level fluctuations, however, are described for the periiod spring 1981 to spring 1982. Much of the data used in this report were collected by the U.S. Geological Survey in cooperation with the Division of Water Rights, Utah Department of Natural Resources.
","language":"English","publisher":"Utah Department of Natural Resources and Energy, Division of Water Resources","publisherLocation":"Salt Lake City, UT","collaboration":"Prepared by the United States Geological Survey in cooperation with the State of Utah","usgsCitation":"Holmes, W.F., Herbert, L.R., Bischoff, D., Smith, M.E., Seiler, R.L., Steiger, J.I., Appel, C.L., Jensen, V., Enright, M., Emett, D.C., Burden, C.B., Beard, R., Sultz, L., Eckenwiler, M., and Sandberg, G.W., 1982, Developing a state water plan: Ground-water conditions in Utah, spring of 1982: Cooperative Investigations Report 22, viii, 85 p.","productDescription":"viii, 85 p.","numberOfPages":"96","costCenters":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":276778,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":333661,"rank":2,"type":{"id":15,"text":"Index Page"},"url":"https://www.waterrights.utah.gov/cgi-bin/libview.exe?Modinfo=Viewpub&LIBNUM=50-1-183"}],"country":"United States","state":"Utah","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"52136e34e4b0b08f446198e2","contributors":{"authors":[{"text":"Holmes, Walter F.","contributorId":31737,"corporation":false,"usgs":true,"family":"Holmes","given":"Walter","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":482760,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Herbert, L. R.","contributorId":39865,"corporation":false,"usgs":true,"family":"Herbert","given":"L.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":482762,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Bischoff, D.A.","contributorId":58548,"corporation":false,"usgs":true,"family":"Bischoff","given":"D.A.","email":"","affiliations":[],"preferred":false,"id":482764,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Smith, Melanie E.","contributorId":101977,"corporation":false,"usgs":true,"family":"Smith","given":"Melanie","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":482769,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Seiler, R. L.","contributorId":87546,"corporation":false,"usgs":true,"family":"Seiler","given":"R.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":482766,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Steiger, Judy I. jsteiger@usgs.gov","contributorId":3689,"corporation":false,"usgs":true,"family":"Steiger","given":"Judy","email":"jsteiger@usgs.gov","middleInitial":"I.","affiliations":[],"preferred":true,"id":482756,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Appel, Cynthia L.","contributorId":34509,"corporation":false,"usgs":true,"family":"Appel","given":"Cynthia","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":482761,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Jensen, V.L.","contributorId":99034,"corporation":false,"usgs":true,"family":"Jensen","given":"V.L.","email":"","affiliations":[],"preferred":false,"id":482767,"contributorType":{"id":1,"text":"Authors"},"rank":8},{"text":"Enright, Michael","contributorId":99979,"corporation":false,"usgs":true,"family":"Enright","given":"Michael","email":"","affiliations":[],"preferred":false,"id":482768,"contributorType":{"id":1,"text":"Authors"},"rank":9},{"text":"Emett, D. C.","contributorId":21213,"corporation":false,"usgs":true,"family":"Emett","given":"D.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":482759,"contributorType":{"id":1,"text":"Authors"},"rank":10},{"text":"Burden, Carole B. cburden@usgs.gov","contributorId":852,"corporation":false,"usgs":true,"family":"Burden","given":"Carole","email":"cburden@usgs.gov","middleInitial":"B.","affiliations":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"preferred":true,"id":482755,"contributorType":{"id":1,"text":"Authors"},"rank":11},{"text":"Beard, R.C.","contributorId":16310,"corporation":false,"usgs":true,"family":"Beard","given":"R.C.","email":"","affiliations":[],"preferred":false,"id":482758,"contributorType":{"id":1,"text":"Authors"},"rank":12},{"text":"Sultz, L.G.","contributorId":61736,"corporation":false,"usgs":true,"family":"Sultz","given":"L.G.","email":"","affiliations":[],"preferred":false,"id":482765,"contributorType":{"id":1,"text":"Authors"},"rank":13},{"text":"Eckenwiler, M.R.","contributorId":9674,"corporation":false,"usgs":true,"family":"Eckenwiler","given":"M.R.","email":"","affiliations":[],"preferred":false,"id":482757,"contributorType":{"id":1,"text":"Authors"},"rank":14},{"text":"Sandberg, G. W.","contributorId":55426,"corporation":false,"usgs":true,"family":"Sandberg","given":"G.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":482763,"contributorType":{"id":1,"text":"Authors"},"rank":15}]}} ,{"id":70043399,"text":"70043399 - 1982 - Hydrology of the Beryl-Enterprise area, Escalante Desert, Utah, with emphasis on ground water; With a section on surface water","interactions":[{"subject":{"id":10426,"text":"ofr81533 - 1981 - Hydrology of the Beryl-Enterprise area, Escalante Desert, Utah, with emphasis on ground water","indexId":"ofr81533","publicationYear":"1981","noYear":false,"title":"Hydrology of the Beryl-Enterprise area, Escalante Desert, Utah, with emphasis on ground water"},"predicate":"SUPERSEDED_BY","object":{"id":70043399,"text":"70043399 - 1982 - Hydrology of the Beryl-Enterprise area, Escalante Desert, Utah, with emphasis on ground water; With a section on surface water","indexId":"70043399","publicationYear":"1982","noYear":false,"title":"Hydrology of the Beryl-Enterprise area, Escalante Desert, Utah, with emphasis on ground water; With a section on surface water"},"id":1}],"lastModifiedDate":"2016-12-17T12:48:26","indexId":"70043399","displayToPublicDate":"2013-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":4,"text":"Other Government Series"},"seriesTitle":{"id":294,"text":"Technical Publication","active":false,"publicationSubtype":{"id":4}},"seriesNumber":"73","title":"Hydrology of the Beryl-Enterprise area, Escalante Desert, Utah, with emphasis on ground water; With a section on surface water","docAbstract":"An investigation of the water resources of the Beryl-Enterprise area, Escalante Desert, Utah (pl. 1), was made during 1976-78 as part of a cooperative program with the Utah Department of Natural Resources, Division of Water Rights. Wells were the most important source of water for all purposes in the Beryl-Enterprise area during 1978, but it has not always been so. For nearly a century after the first settlers arrived in about 1860, streams supplied most of the irrigation water and springs supplied much of the water for domestic and stock use. A few shallow wells were dug by the early settlers for domestic and stock water, but the widespread use of ground water did not start until the 1920's when shallow wells were first dug to supply irrigation water. Ground-water withdrawals from wells, principally for irrigation, have increased nearly every year since the 1920's. The quantity withdrawn from wells surpassed that diverted from surface sources during the mid-1940's and was about eight times that amount during the 1970's. As a result, water levels have declined measurably throughout the area resulting in administrative water-rights problems.
The primary purpose of this report is to describe the water resources with emphasis on ground water. The surface-water resources are evaluated only as they pertain to the understanding of the ground-water resources. A secondary purpose is to discuss the extent and effects of the development of ground water in order to provide the hydrologic information needed for the orderly and optimum development of the resource and for the effective administration and adjudication of water rights in the area. The hydrologic data on which this report is based are given in a companion report by Mower (1981).
","language":"English","publisher":"Utah Department of Natural Resources, Division of Water Rights","publisherLocation":"Salt Lake City, Utah","collaboration":"Prepared by the United State Geological Survey in cooperation with the Utah Department of Natural Resources Division of Water Rights","usgsCitation":"Mower, R.W., and Sandberg, G.W., 1982, Hydrology of the Beryl-Enterprise area, Escalante Desert, Utah, with emphasis on ground water; With a section on surface water: Technical Publication 73, vi, 66 p.","productDescription":"vi, 66 p.","numberOfPages":"86","costCenters":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":267297,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":331998,"rank":3,"type":{"id":11,"text":"Document"},"url":"https://waterrights.utah.gov/docSys/v920/w920/w920009y.pdf"},{"id":331997,"rank":2,"type":{"id":15,"text":"Index Page"},"url":"https://www.waterrights.utah.gov/cgi-bin/libview.exe?Modinfo=Viewpub&LIBNUM=20-5-730"}],"country":"United States","state":"Utah","otherGeospatial":"Escalante Desert","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -114.1,\n 37.6\n ],\n [\n -114.1,\n 38.3\n ],\n [\n -113,\n 38.3\n ],\n [\n -113,\n 37.6\n ],\n [\n -114.1,\n 37.6\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"511b7282e4b0e3ef7b6f1e3c","contributors":{"authors":[{"text":"Mower, Reed W.","contributorId":32503,"corporation":false,"usgs":true,"family":"Mower","given":"Reed","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":473505,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Sandberg, George Woodard","contributorId":87434,"corporation":false,"usgs":true,"family":"Sandberg","given":"George","email":"","middleInitial":"Woodard","affiliations":[],"preferred":false,"id":473506,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70043690,"text":"70043690 - 1982 - Reconnaissance of the quality of surface water in the San Rafael River basin, Utah","interactions":[{"subject":{"id":24003,"text":"ofr80574 - 1980 - Reconnaissance of the quality of surface water in the San Rafael River basin, Utah","indexId":"ofr80574","publicationYear":"1980","noYear":false,"title":"Reconnaissance of the quality of surface water in the San Rafael River basin, Utah"},"predicate":"SUPERSEDED_BY","object":{"id":70043690,"text":"70043690 - 1982 - Reconnaissance of the quality of surface water in the San Rafael River basin, Utah","indexId":"70043690","publicationYear":"1982","noYear":false,"title":"Reconnaissance of the quality of surface water in the San Rafael River basin, Utah"},"id":1}],"lastModifiedDate":"2016-12-12T16:11:37","indexId":"70043690","displayToPublicDate":"2013-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":4,"text":"Other Government Series"},"seriesTitle":{"id":294,"text":"Technical Publication","active":false,"publicationSubtype":{"id":4}},"seriesNumber":"72","title":"Reconnaissance of the quality of surface water in the San Rafael River basin, Utah","docAbstract":"The water-quality reconnaissance of the San Rafael River basin, Utah, encompassed an area of about 2,300 square miles (5,960 square kilometers). Data were obtained by the U.S. Geological Survey one or more times at 116 sites from June 1977 to September 1978. At 19 other sites visited during the same period, the streams were dry. Precipitation and stream discharge were significantly less than normal during 1977 and ranged from less than to more than normal during 1978. Exposed rocks in the San Rafael River basin range in age from Permian to Holocene. The Carmel Formation of Jurassic age and various members of the Mancos Shale of Cretaceous age are major contributors of dissolved solids to streams in the basin. There are eight major reservoirs having a total usable capacity of 115, 000 acre-feet (142 cubic hectometers); seven are mainly for irrigation supply; one, having a usable capacity of 30,530 acre-feet (38 cubic hectometers), is for power plant water supply. From about April to November, major diversions from Huntington, Cottonwood, and Ferron Creeks nearly deplete the flow downstream; during such periods, downstream flow in these streams and in the San Rafael River is mainly irrigation-return flow and some ground-water seepage. The water at the points of major diversion on Huntington, Cottonwood, and Ferron Creeks is of excellent quality for irrigation; salinity hazard is low to medium, and sodium hazard is low. Dissolved-solids concentrations are less than 500 milligrams per liter. The water at the mouths of Huntington, Cottonwood, and Ferron Creeks has markedly larger dissolved-solids concentrations than does the water upstream from major diversions. The changes in the chemical quality occur in stream reaches that cross a belt of land 10 to 15 miles (16 to 24 kilometers) wide where the Mancos Shale is widely exposed. This also is the area where nearly all the intensive irrigation in the San Rafael River basin is practiced. There are no perennial tributaries to the San Rafael River downstream from Ferron Creek. Except during infrequent short periods of runoff from cloudbursts or snowmelt, the flow in the San Rafael River is composed of the flow that reaches the mouths of Huntington, Cottonwood, and Ferron Creeks. The quality of water in the mainstem of the San Rafael River is largely determined by the major consumptive use of water for irrigation in upstream areas and by the poor quality of irrigation-return flow. During the data-collection periods for this study, dissolved-solids concentrations in the San Rafael River were more than 2,000 milligrams per liter except during snowmelt runoff in June 1978 and during a major flood in August 1977. The concentrations of trace elements, with the exception of strontium, were relatively small; strontium concentrations exceeded 1,500 micrograms per liter at seven sites. Most of the suspended-sediment discharge of the San Rafael River probably occurs during a few days each year and results mainly from cloudburst runoff.","language":"English","publisher":"Utah Department of Natural Resources, Division of Water Rights","publisherLocation":"Salt Lake City, UT","collaboration":"Prepared by the United States Geological Survey in cooperation with The Utah Department of Natural Resources and Energy Division of Water Rights","usgsCitation":"Mundorff, J.C., and Thompson, K.R., 1982, Reconnaissance of the quality of surface water in the San Rafael River basin, Utah: Technical Publication 72, vi, 53 p.","productDescription":"vi, 53 p.","numberOfPages":"64","costCenters":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":267618,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":331994,"rank":0,"type":{"id":15,"text":"Index Page"},"url":"https://www.waterrights.utah.gov/cgi-bin/libview.exe?Modinfo=Viewpub&LIBNUM=20-5-720"},{"id":267617,"type":{"id":11,"text":"Document"},"url":"https://waterrights.utah.gov/docSys/v920/w920/w920009x.pdf"}],"country":"United States","state":"Utah","otherGeospatial":"San Rafael River","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -111.5,\n 38.4\n ],\n [\n -111.5,\n 39.75\n ],\n [\n -110,\n 39.75\n ],\n [\n -110,\n 38.4\n ],\n [\n -111.5,\n 38.4\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"51235b85e4b0c9f2bfcf8d47","contributors":{"authors":[{"text":"Mundorff, J. C.","contributorId":63374,"corporation":false,"usgs":true,"family":"Mundorff","given":"J.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":474085,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Thompson, Kendall R.","contributorId":100854,"corporation":false,"usgs":true,"family":"Thompson","given":"Kendall","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":474086,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70006788,"text":"70006788 - 1982 - A rapid high-performance liquid-chromatographic method for simultaneously determining the concentrations of TFM and Bayer 73 in water during lampricide treatments","interactions":[],"lastModifiedDate":"2012-07-12T01:01:45","indexId":"70006788","displayToPublicDate":"2012-01-01T19:55:17","publicationYear":"1982","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1169,"text":"Canadian Journal of Fisheries and Aquatic Sciences","active":true,"publicationSubtype":{"id":10}},"title":"A rapid high-performance liquid-chromatographic method for simultaneously determining the concentrations of TFM and Bayer 73 in water during lampricide treatments","docAbstract":"The high-performance liquid-chromatography (HPLC) procedure requires only minutes per sample, is specific, and is relatively sensitive (limit of detection < 0.005 mg/L for both chemicals). A combined buffer (pH 4) and internal standard (3-chlorodiphenylamine) reagent is added to the water sample, which is injected through a Sep Pak C18 disposable cartridge. The cartridge adsorbs and retains both the lampricides and the internal standard. The quantitative elution of the three chemicals from the cartridge with a small volume of methanol effectively concentrates the sample and provides sample cleanup. The methanol extract is then analyzed directly by HPLC on an MCH 10 reverse phase column by using a methanol:0.01 mol/L acetate buffer (87:13, v:v) as the mobile phase at 2 mL/min and detected by ultraviolet spectrophotometry at 330 (or 254) nm. A microprocessor data system further facilitates the procedure by quantifying off-scale peaks and yielding results directly in units of concentration (mg/L).","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Canadian Journal of Fisheries and Aquatic Sciences","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"NRC Research Press","publisherLocation":"Ottawa, Ontario","doi":"10.1139/f82-105","collaboration":"None","usgsCitation":"Dawson, V.K., 1982, A rapid high-performance liquid-chromatographic method for simultaneously determining the concentrations of TFM and Bayer 73 in water during lampricide treatments: Canadian Journal of Fisheries and Aquatic Sciences, v. 39, no. 5, p. 778-782, https://doi.org/10.1139/f82-105.","productDescription":"5 p.","startPage":"778","endPage":"782","numberOfPages":"5","costCenters":[{"id":606,"text":"Upper Midwest Environmental Sciences Center","active":true,"usgs":true}],"links":[{"id":258390,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":258377,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1139/f82-105","linkFileType":{"id":5,"text":"html"}}],"volume":"39","issue":"5","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059e52be4b0c8380cd46b9f","contributors":{"authors":[{"text":"Dawson, V. K.","contributorId":48900,"corporation":false,"usgs":true,"family":"Dawson","given":"V.","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":355230,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ]}