Laboratory experiments on the thermal decarboxylation of solutions of acetic acid at 200°C and 300°C were carried out in hydrothermal equipment allowing for on-line sampling of both the gas and liquid phases for chemical and stable-carbon-isotope analyses. The solutions had ambient pH values between 2.5 and 7.1; pH values and the concentrations of the various acetate species at the conditions of the experiments were computed using a chemical model.
Results show that the concentrations of acetic acid, and not total acetate in solution, control the reaction rates which follow a first order equation based on decreasing concentrations of acetic acid with time. The decarboxylation rates at 200°C (1.81 × 10−8 per second) and 300°C (8.17 × 10−8 per second) and the extrapolated rates at lower temperatures are relatively high. The activation energy of decarboxylation is only 8.1 kcal/mole. These high decarboxylation rates, together with the distribution of short-chained aliphatic acid anions in formation waters, support the hypothesis that acid anions are precursors for an important portion of natural gas.
Results of the δ13C values of CO2, CH4, and total acetate show a reasonably constant fractionation factor of about 20 permil between CO2 and CH4 at 300°C. The δ13C values of CO2 and CH4 are initially low and become higher as decarboxylation increases.
","language":"English","publisher":"Elsevier","doi":"10.1016/0016-7037(83)90262-4","issn":"00167037","usgsCitation":"Kharaka, Y., Carothers, W., and Rosenbauer, R., 1983, Thermal decarboxylation of acetic acid: Implications for origin of natural gas: Geochimica et Cosmochimica Acta, v. 47, no. 3, p. 397-402, https://doi.org/10.1016/0016-7037(83)90262-4.","productDescription":"6 p.","startPage":"397","endPage":"402","numberOfPages":"6","costCenters":[],"links":[{"id":221747,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"47","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505bb21ce4b08c986b3255de","contributors":{"authors":[{"text":"Kharaka, Y.K.","contributorId":23568,"corporation":false,"usgs":true,"family":"Kharaka","given":"Y.K.","email":"","affiliations":[],"preferred":false,"id":360847,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Carothers, W.W.","contributorId":43803,"corporation":false,"usgs":true,"family":"Carothers","given":"W.W.","email":"","affiliations":[],"preferred":false,"id":360849,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Rosenbauer, R.J.","contributorId":37320,"corporation":false,"usgs":true,"family":"Rosenbauer","given":"R.J.","email":"","affiliations":[],"preferred":false,"id":360848,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":70011341,"text":"70011341 - 1983 - The role of digital cartographic data in the geosciences","interactions":[],"lastModifiedDate":"2013-01-21T15:49:53","indexId":"70011341","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":"The role of digital cartographic data in the geosciences","docAbstract":"The increasing demand of the Nation's natural resource developers for the manipulation, analysis, and display of large quantities of earth-science data has necessitated the use of computers and the building of geoscience information systems. These systems require, in digital form, the spatial data on map products. The basic cartographic data shown on quadrangle maps provide a foundation for the addition of geological and geophysical data. If geoscience information systems are to realize their full potential, large amounts of digital cartographic base data must be available. A major goal of the U.S. Geological Survey is to create, maintain, manage, and distribute a national cartographic and geographic digital database. This unified database will contain numerous categories (hydrography, hypsography, land use, etc.) that, through the use of standardized data-element definitions and formats, can be used easily and flexibly to prepare cartographic products and perform geoscience analysis. ?? 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)90032-8","issn":"00983004","usgsCitation":"Guptill, S., 1983, The role of digital cartographic data in the geosciences: Computers & Geosciences, v. 9, no. 1, p. 23-26, https://doi.org/10.1016/0098-3004(83)90032-8.","startPage":"23","endPage":"26","numberOfPages":"4","costCenters":[],"links":[{"id":266192,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1016/0098-3004(83)90032-8"},{"id":220832,"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":"505baf66e4b08c986b324772","contributors":{"authors":[{"text":"Guptill, S.C.","contributorId":84417,"corporation":false,"usgs":true,"family":"Guptill","given":"S.C.","email":"","affiliations":[],"preferred":false,"id":360878,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70011102,"text":"70011102 - 1983 - Geological setting of oil shales in the Permian phosphoria formation and some of the geochemistry of these rocks","interactions":[],"lastModifiedDate":"2012-03-12T17:18:35","indexId":"70011102","displayToPublicDate":"1983-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"Geological setting of oil shales in the Permian phosphoria formation and some of the geochemistry of these rocks","docAbstract":"Recent studies of the Meade Peak and the Retort Phosphatic Shale Members of the Phosphoria Formation have investigated the organic carbon content and some aspects of hydrocarbon generation from these rocks. Phosphorite has been mined from the Retort and Meade Peak members in southeastern Idaho, northern Utah, western Wyoming and southwestern Montana. Organic carbon-rich mudstone beds associated with the phosphorite in these two members also were natural sources of petroleum. These mudstone beds were differentially buried throughout the region so that heating of these rocks has been different from place to place. Most of the Phosphoria source beds have been deeply buried and naturally heated to catagenetically form hydrocarbons. Deepest burial was in eastern Idaho and throughout most of the northeastern Great Basin where high ambient temperatures have driven the catagenesis to its limit and beyond to degrade or to destroy the hydrocarbons. In southwest Montana, however, burial in some areas has been less than 2 km, ambient temperatures remained low and the kerogen has not produced hydrocarbons (2). In these areas in Montana, the kerogen in the carbonaceous mudstone has retained the potential for hydrocarbon generation and the carbon-rich Retort Member is an oil shale from which hydrocarbons can be synthetically extracted. The Phosphoria Formation was deposited in a foreland basin between the Cordilleran geosyncline and the North American craton. This foreland basin, which coincides with the area of deposition of the two organic carbon-rich mudstone members of the Phosphoria, has been named the Sublett basin (Maughan, 1979). The basin has a northwest-southeast trending axis and seems to have been deepest in central Idaho where deep-water sedimentary rocks equivalent to the Phosphoria Formation are exceptionally thick. The depth of the basin was increasingly shallower away from central Idaho toward the Milk River uplift - a land area in Montana, the ancestral Rocky Mountains. The basin is composed of land areas in Colorado, the Humboldt highland in northeastern Nevada and intervening carbonate shelves in Utah and Wyoming. The phosphorites and the carbonaceous mudstones were deposited on the foreslope between the carbonate and littoral sand deposits on the shelf and the dominantly cherty mudstone sediments in the axial part of the basin. Paleomagnetic evidence indicates that in the Permian the region would have been within the northern hemispheric trade wind belt; and wind-direction studies determined from studies of sand dunes, indicate that the prevailing winds from the Milk River uplift would have blown offshore across the Phosphoria sea. Offshore winds would have carried surface water away from the shore and generated upwelling in the sea in eastern Idaho and adjacent areas in Montana, Wyoming and Utah. Prior to deposition of the Phosphoria, the region was the site of extensive deposition of shallow-water carbonate sediments. Equivalent rocks in the northern part of the basin are dominantly sandstone derived from the adjacent Milk River uplift and similar sandstone strata in the southeastern sector were derived from the ancestral Rocky Mountains uplift. Tectonic subsidence of the Sublett basin in part of the region seems to have provided a sea-floor profile favorable for upwelling circulation and the shift in deposition from regional carbonates and local sandstone into a more complex depositional pattern that included the accumulation of the mudstone-chert-phosphorite facies that comprises the Phosphoria Formation. High biological productivity and the accumulation of sapropel on the sea floor is associated with contemporary coastal upwelling (1) and similar environmental and depositional conditions are attributed to the rich accumulations of organic matter in the Phosphoria Formation. Sapropelic mudstone and phosphorite composing the Meade Peak Member are approximately 60 m thick near the center of the Sublett basin. The Meade","largerWorkTitle":"Preprints Symposia","language":"English","issn":"05693799","usgsCitation":"Maughan, E.K., 1983, Geological setting of oil shales in the Permian phosphoria formation and some of the geochemistry of these rocks, in Preprints Symposia, v. 28, no. 1, p. 74-76.","startPage":"74","endPage":"76","numberOfPages":"3","costCenters":[],"links":[{"id":221503,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"28","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a227ee4b0c8380cd570ce","contributors":{"authors":[{"text":"Maughan, E. K.","contributorId":25568,"corporation":false,"usgs":true,"family":"Maughan","given":"E.","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":360287,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70011159,"text":"70011159 - 1983 - Geochemistry of the Chattanooga shale, Dekalb County, central Tennessee.","interactions":[],"lastModifiedDate":"2012-03-12T17:18:33","indexId":"70011159","displayToPublicDate":"1983-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3443,"text":"Southeastern Geology","active":true,"publicationSubtype":{"id":10}},"title":"Geochemistry of the Chattanooga shale, Dekalb County, central Tennessee.","docAbstract":"This Upper Devonian shale is of interest because of its unusual enrichment in trace elements, especially U; a new chemical analysis for major, minor and trace elements is presented. Stable isotopes of carbon (organic) show delta 13C approx -29per mille and for total sulphur show -21 to -27per mille delta 34S. The organic matter was found to range from dominantly marine (Dowelltown member) to dominantly terrestrial (Gassaway member) by extraction-column chromatography-GS and also by pyrolysis-GS of kerogen. Trace elements U, Mo, Co, Zn, Cu, Ni, V, As and Hg are enriched in the organic- and sulphide-rich units. This enrichment can be related to a euxinic depositional environment, to a very slow sedimentation rate (approx 2 mm/1000 years), to the type of organic matter that varied from mainly marine to terrestrial, and to the source of the metals, which shows abundance variations that originated, at least in part, from volcanic ash layers.-R.S.M.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Southeastern Geology","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","issn":"00383678","usgsCitation":"Leventhal, J., Briggs, P., and Baker, J., 1983, Geochemistry of the Chattanooga shale, Dekalb County, central Tennessee.: Southeastern Geology, v. 24, no. 3, p. 101-116.","startPage":"101","endPage":"116","numberOfPages":"16","costCenters":[],"links":[{"id":221025,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"24","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a171de4b0c8380cd553ab","contributors":{"authors":[{"text":"Leventhal, J.S.","contributorId":60640,"corporation":false,"usgs":true,"family":"Leventhal","given":"J.S.","email":"","affiliations":[],"preferred":false,"id":360423,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Briggs, Paul H.","contributorId":107691,"corporation":false,"usgs":true,"family":"Briggs","given":"Paul H.","affiliations":[],"preferred":false,"id":360424,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Baker, J.W.","contributorId":46525,"corporation":false,"usgs":true,"family":"Baker","given":"J.W.","email":"","affiliations":[],"preferred":false,"id":360422,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":70011410,"text":"70011410 - 1983 - USES OF MARKETING TECHNIQUES THE U. S. GEOLOGICAL SURVEY.","interactions":[],"lastModifiedDate":"2012-03-12T17:18:29","indexId":"70011410","displayToPublicDate":"1983-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"USES OF MARKETING TECHNIQUES THE U. S. GEOLOGICAL SURVEY.","docAbstract":"The use of marketing techniques by government agencies to provide more efficient and effective dissemination of their information is a fairly recent development. A recessive economy, and increased scrutiny of operations have become a powerful incentive to maximize revenues and minimize expenses wherever possible as long as the primary mission of public service is satisfactorily met.","largerWorkTitle":"Technical Papers of the American Congress of Surveying and Mapping","conferenceTitle":"Technical Papers of the 43rd Annual Meeting of the American Congress on Surveying and Mapping.","conferenceLocation":"Washington, DC, USA","language":"English","publisher":"American Congress on Surveying & Mapping","publisherLocation":"Falls Church, VA, USA","usgsCitation":"McDermott, M.P., 1983, USES OF MARKETING TECHNIQUES THE U. S. GEOLOGICAL SURVEY., in Technical Papers of the American Congress of Surveying and Mapping, Washington, DC, USA, p. 300-306.","startPage":"300","endPage":"306","numberOfPages":"7","costCenters":[],"links":[{"id":220772,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505bbb83e4b08c986b328686","contributors":{"authors":[{"text":"McDermott, Michael P. mmcdermo@usgs.gov","contributorId":259,"corporation":false,"usgs":true,"family":"McDermott","given":"Michael","email":"mmcdermo@usgs.gov","middleInitial":"P.","affiliations":[],"preferred":true,"id":361019,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":58581,"text":"mf1416B - 1983 - Mineral resource potential map of the Carson-Iceberg Roadless Areas, central Sierra Nevada, California","interactions":[],"lastModifiedDate":"2023-12-12T19:23:05.696626","indexId":"mf1416B","displayToPublicDate":"1983-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":325,"text":"Miscellaneous Field Studies Map","code":"MF","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1416","chapter":"B","title":"Mineral resource potential map of the Carson-Iceberg Roadless Areas, central Sierra Nevada, California","docAbstract":"No abstract available.
","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/mf1416B","usgsCitation":"Keith, W.J., Chaffee, M.A., Plouff, D., and Miller, M.S., 1983, Mineral resource potential map of the Carson-Iceberg Roadless Areas, central Sierra Nevada, California: U.S. Geological Survey Miscellaneous Field Studies Map 1416, Report: 8 p.; 1 Plate: 39.50 x 55.00 inches, https://doi.org/10.3133/mf1416B.","productDescription":"Report: 8 p.; 1 Plate: 39.50 x 55.00 inches","costCenters":[],"links":[{"id":105839,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_7150.htm","linkFileType":{"id":5,"text":"html"},"description":"7150"},{"id":88426,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mf/1983/1416b/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":184064,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/mf/1983/1416b/report-thumb.jpg"},{"id":88427,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/mf/1983/1416b/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"62500","country":"United States","state":"California","otherGeospatial":"Carson-Iceberg Roadless Areas","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -120.0894812926488,\n 38.70031490776856\n ],\n [\n -120.05597990777807,\n 38.32560289425339\n ],\n [\n -119.7866774087454,\n 38.37749860650784\n ],\n [\n -119.63865263707217,\n 38.432946915403306\n ],\n [\n -119.69136307617298,\n 38.470800595639915\n ],\n [\n -119.96049704582668,\n 38.717870939406424\n ],\n [\n -120.0894812926488,\n 38.70031490776856\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b05e4b07f02db699f9f","contributors":{"authors":[{"text":"Keith, William J.","contributorId":21146,"corporation":false,"usgs":true,"family":"Keith","given":"William","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":259886,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Chaffee, Maurice A. mchaffee@usgs.gov","contributorId":4047,"corporation":false,"usgs":true,"family":"Chaffee","given":"Maurice","email":"mchaffee@usgs.gov","middleInitial":"A.","affiliations":[{"id":171,"text":"Central Mineral and Environmental Resources Science Center","active":true,"usgs":true}],"preferred":true,"id":890051,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Plouff, Donald","contributorId":94657,"corporation":false,"usgs":true,"family":"Plouff","given":"Donald","email":"","affiliations":[],"preferred":false,"id":259888,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Miller, Michael S.","contributorId":52588,"corporation":false,"usgs":true,"family":"Miller","given":"Michael","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":259887,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":70011218,"text":"70011218 - 1983 - Geoscience data management","interactions":[],"lastModifiedDate":"2013-01-21T15:48:49","indexId":"70011218","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":"Geoscience data management","docAbstract":"[No abstract available]","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)90029-8","issn":"00983004","usgsCitation":"Albert, T., 1983, Geoscience data management: Computers & Geosciences, v. 9, no. 1, p. 3-6, https://doi.org/10.1016/0098-3004(83)90029-8.","startPage":"3","endPage":"6","numberOfPages":"4","costCenters":[],"links":[{"id":266191,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1016/0098-3004(83)90029-8"},{"id":220824,"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":"505a28a1e4b0c8380cd5a287","contributors":{"authors":[{"text":"Albert, T.M.","contributorId":90469,"corporation":false,"usgs":true,"family":"Albert","given":"T.M.","email":"","affiliations":[],"preferred":false,"id":360590,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70011314,"text":"70011314 - 1983 - Gas-film coefficients for streams","interactions":[],"lastModifiedDate":"2020-01-26T09:43:34","indexId":"70011314","displayToPublicDate":"1983-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2255,"text":"Journal of Environmental Engineering","active":true,"publicationSubtype":{"id":10}},"title":"Gas-film coefficients for streams","docAbstract":"Equations for predicting the gas-film coefficient for the volatilization of organic solutes from streams are developed. The film coefficient is a function of windspeed and water temperature. The dependence of the coefficient on windspeed is determined from published information on the evaporation of water from a canal. The dependence of the coefficient on temperature is determined from laboratory studies on the evaporation of water. Procedures for adjusting the coefficients for different organic solutes are based on the molecular diffusion coefficient and the molecular weight. The molecular weight procedure is easiest to use because of the availability of molecular weights. However, the theoretical basis of the procedure is questionable. The diffusion coefficient procedure is supported by considerable data. Questions, however, remain regarding the exact dependence of the film coefficint on the diffusion coefficient. It is suggested that the diffusion coefficient procedure with a 0.68-power dependence be used when precise estimate of the gas-film coefficient are needed and that the molecular weight procedure be used when only approximate estimates are needed.","language":"English","publisher":"ASCE","doi":"10.1061/(ASCE)0733-9372(1983)109:5(1111)","usgsCitation":"Rathbun, R.E., and Tai, D.Y., 1983, Gas-film coefficients for streams: Journal of Environmental Engineering, v. 109, no. 5, p. 1111-1127, https://doi.org/10.1061/(ASCE)0733-9372(1983)109:5(1111).","productDescription":"17 p.","startPage":"1111","endPage":"1127","numberOfPages":"17","costCenters":[{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":221518,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"109","issue":"5","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a14dce4b0c8380cd54bd5","contributors":{"authors":[{"text":"Rathbun, R. E.","contributorId":61796,"corporation":false,"usgs":true,"family":"Rathbun","given":"R.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":360802,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Tai, D. Y.","contributorId":59778,"corporation":false,"usgs":true,"family":"Tai","given":"D.","email":"","middleInitial":"Y.","affiliations":[],"preferred":false,"id":360801,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70011245,"text":"70011245 - 1983 - Landslide risk assessment","interactions":[],"lastModifiedDate":"2012-03-12T17:18:28","indexId":"70011245","displayToPublicDate":"1983-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1539,"text":"Environmental Geology","active":true,"publicationSubtype":{"id":10}},"title":"Landslide risk assessment","docAbstract":"Landslide risk can be assessed by evaluating geological conditions associated with past events. A sample of 2,4 16 slides from urban areas in West Virginia, each with 12 associated geological factors, has been analyzed using SAS computer methods. In addition, selected data have been normalized to account for areal distribution of rock formations, soil series, and slope percents. Final calculations yield landslide risk assessments of <0.50=low risk, 0.50 to 1.50=moderate risk, and >1.50=high risk. The simplicity of the method provides for a rapid, initial assessment prior to financial investment. However, it does not replace on-site investigations, nor excuse poor construction. ?? 1983 Springer-Verlag New York Inc.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Environmental Geology","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisherLocation":"Springer-Verlag","doi":"10.1007/BF02381102","issn":"09430105","usgsCitation":"Lessing, P., Messina, C., and Fonner, R., 1983, Landslide risk assessment: Environmental Geology, v. 5, no. 2, p. 93-99, https://doi.org/10.1007/BF02381102.","startPage":"93","endPage":"99","numberOfPages":"7","costCenters":[],"links":[{"id":221436,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":205120,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1007/BF02381102"}],"volume":"5","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a4433e4b0c8380cd6693a","contributors":{"authors":[{"text":"Lessing, P.","contributorId":90038,"corporation":false,"usgs":true,"family":"Lessing","given":"P.","affiliations":[],"preferred":false,"id":360652,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Messina, C.P.","contributorId":35462,"corporation":false,"usgs":true,"family":"Messina","given":"C.P.","email":"","affiliations":[],"preferred":false,"id":360650,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Fonner, R.F.","contributorId":37069,"corporation":false,"usgs":true,"family":"Fonner","given":"R.F.","email":"","affiliations":[],"preferred":false,"id":360651,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":70011160,"text":"70011160 - 1983 - PROPOSED SPECIFICATIONS FOR INERTIAL SURVEYING.","interactions":[],"lastModifiedDate":"2012-03-12T17:18:34","indexId":"70011160","displayToPublicDate":"1983-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"PROPOSED SPECIFICATIONS FOR INERTIAL SURVEYING.","docAbstract":"The purpose of this paper is to continue the movement toward placing inertial surveying instruments in the toolbox of the geodetic surveyor. A set of specifications is proposed for performing horizontal geodetic surveys with inertial instruments that will meet the Federal Geodetic Control Committee (FGCC) second- and third-order standards. These specifications are tentative.","largerWorkTitle":"Technical Papers of the American Congress of Surveying and Mapping","conferenceTitle":"Technical Papers of the 43rd Annual Meeting of the American Congress on Surveying and Mapping.","conferenceLocation":"Washington, DC, USA","language":"English","publisher":"American Congress on Surveying & Mapping","publisherLocation":"Falls Church, VA, USA","usgsCitation":"Chapman, W.H., 1983, PROPOSED SPECIFICATIONS FOR INERTIAL SURVEYING., in Technical Papers of the American Congress of Surveying and Mapping, Washington, DC, USA, p. 287-293.","startPage":"287","endPage":"293","numberOfPages":"7","costCenters":[],"links":[{"id":221026,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a7381e4b0c8380cd7709e","contributors":{"authors":[{"text":"Chapman, William H.","contributorId":25163,"corporation":false,"usgs":true,"family":"Chapman","given":"William","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":360425,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":1004072,"text":"1004072 - 1983 - Neoplasms identified in free-flying birds","interactions":[],"lastModifiedDate":"2018-02-27T15:09:09","indexId":"1004072","displayToPublicDate":"1983-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":948,"text":"Avian Diseases","active":true,"publicationSubtype":{"id":10}},"title":"Neoplasms identified in free-flying birds","docAbstract":"Nine neoplasms were identified in carcasses of free-flying wild birds received at the National Wildlife Health Laboratory; gross and microscopic descriptions are reported herein. The prevalence of neoplasia in captive and free-flying birds is discussed, and lesions in the present cases are compared with those previously described in mammals and birds.
","language":"English","publisher":"American Association of Avian Pathologists","doi":"10.2307/1590375","usgsCitation":"Siegfried, L.M., 1983, Neoplasms identified in free-flying birds: Avian Diseases, v. 27, no. 1, p. 86-99, https://doi.org/10.2307/1590375.","productDescription":"14 p.","startPage":"86","endPage":"99","costCenters":[{"id":456,"text":"National Wildlife Health Center","active":true,"usgs":true}],"links":[{"id":131111,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"27","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49fbe4b07f02db5f4b32","contributors":{"authors":[{"text":"Siegfried, Lynne M.","contributorId":53732,"corporation":false,"usgs":true,"family":"Siegfried","given":"Lynne","email":"","middleInitial":"M.","affiliations":[{"id":456,"text":"National Wildlife Health Center","active":true,"usgs":true}],"preferred":false,"id":315098,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70195696,"text":"70195696 - 1983 - Chemical immobilization of North American mule deer","interactions":[],"lastModifiedDate":"2018-02-27T12:56:37","indexId":"70195696","displayToPublicDate":"1983-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"Chemical immobilization of North American mule deer","docAbstract":"The choice of agents for chemical immobilization of mule deer (Odocoileus hemionus) is a problem with a simple and effective solution, in my opinion. I recommend combinations of etorphine hydrochloride (M199©) and xylazine hydrochloride (Rompun©) administered intravenously and reversed intravenously. I have used this combination on hundreds of mule deer and have supervised its use on hundreds more. It is a forgiving combination in terms of safety to the deer. I have never seen a mortality in mule deer that I could blame on this combination of drugs, which, in my experience, has performed well under a wide variety of environmental, physiological and organizational conditions.
","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Proceedings of the North American Symposium: Chemical immobilization of North American wildlife","largerWorkSubtype":{"id":12,"text":"Conference publication"},"conferenceTitle":"Chemical immobilization of North American wildlife","conferenceDate":"April 4-6, 1982","conferenceLocation":"Milwaukee, WI","language":"English","publisher":"Wisconsin Humane Society","publisherLocation":"Milwaukee, WI","usgsCitation":"Lange, R., 1983, Chemical immobilization of North American mule deer, in Proceedings of the North American Symposium: Chemical immobilization of North American wildlife, Milwaukee, WI, April 4-6, 1982, p. 363-369.","productDescription":"7 p.","startPage":"363","endPage":"369","costCenters":[{"id":456,"text":"National Wildlife Health Center","active":true,"usgs":true}],"links":[{"id":352077,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5aff4004e4b0da30c1bfda88","contributors":{"editors":[{"text":"Nielsen, Leon","contributorId":171919,"corporation":false,"usgs":false,"family":"Nielsen","given":"Leon","email":"","affiliations":[],"preferred":false,"id":729744,"contributorType":{"id":2,"text":"Editors"},"rank":1},{"text":"Haigh, Jerry C.","contributorId":152537,"corporation":false,"usgs":false,"family":"Haigh","given":"Jerry","email":"","middleInitial":"C.","affiliations":[{"id":13248,"text":"University of Saskatchewan","active":true,"usgs":false}],"preferred":false,"id":729745,"contributorType":{"id":2,"text":"Editors"},"rank":2},{"text":"Fowler, Murray E.","contributorId":113762,"corporation":false,"usgs":false,"family":"Fowler","given":"Murray","email":"","middleInitial":"E.","affiliations":[{"id":7214,"text":"University of California, Davis","active":true,"usgs":false}],"preferred":false,"id":729746,"contributorType":{"id":2,"text":"Editors"},"rank":3}],"authors":[{"text":"Lange, Robert E.","contributorId":94262,"corporation":false,"usgs":true,"family":"Lange","given":"Robert E.","affiliations":[],"preferred":false,"id":729743,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70162502,"text":"70162502 - 1983 - Tangshan, six years later","interactions":[],"lastModifiedDate":"2024-05-21T15:00:13.758262","indexId":"70162502","displayToPublicDate":"1983-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1435,"text":"Earthquake Information Bulletin (USGS)","active":true,"publicationSubtype":{"id":10}},"title":"Tangshan, six years later","docAbstract":"At 3:42 a.m on July 28, 1976, the now infamous Tangshan earthquake struck that heavily industrialized city in eastern China killing, by official count, 240,000 people. During the first 2 years after the earthquake, estimates of casualties ranged from 650,000 to 800,000. Almost certainly the exact number will never be known. The earthquake was measured at magntiude 7.8, and intensities that registered XI on teh Modified Mercalli Intensity Scale occurred throughout the city of Tangshan.
","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","usgsCitation":"Wallace, R.E., 1983, Tangshan, six years later: Earthquake Information Bulletin (USGS), v. 15, no. 3, p. 102-107.","productDescription":"6 p.","startPage":"102","endPage":"107","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":314827,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"China","otherGeospatial":"Tangshan","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n 117.92724609375,\n 39.11301365149975\n ],\n [\n 118.24584960937499,\n 38.77978137804918\n ],\n [\n 118.98193359375,\n 38.53097889440024\n ],\n [\n 119.37744140625,\n 38.976492485539396\n ],\n [\n 119.7509765625,\n 39.58875727696545\n ],\n [\n 119.761962890625,\n 40.371658891506094\n ],\n [\n 118.93798828125,\n 40.82212357516945\n ],\n [\n 118.311767578125,\n 41.02964338716638\n ],\n [\n 117.27905273437499,\n 40.75557964275589\n ],\n [\n 116.78466796875,\n 40.98819156349393\n ],\n [\n 117.103271484375,\n 39.605688178320804\n ],\n [\n 117.92724609375,\n 39.11301365149975\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"15","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"56a7556ce4b0b28f1184d88e","contributors":{"authors":[{"text":"Wallace, R. 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A.","contributorId":87531,"corporation":false,"usgs":true,"family":"Bailey","given":"R. A.","affiliations":[],"preferred":false,"id":627504,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":3192,"text":"wsp2195 - 1983 - Hydrology of the Ferron Sandstone aquifer and effects of proposed surface-coal mining in Castle Valley, Utah, with a section on stratigraphy and a section on leaching of overburden","interactions":[{"subject":{"id":23739,"text":"ofr81535 - 1981 - Hydrology of the Ferron sandstone aquifer and effects of proposed surface-coal mining in Castle Valley, Utah","indexId":"ofr81535","publicationYear":"1981","noYear":false,"title":"Hydrology of the Ferron sandstone aquifer and effects of proposed surface-coal mining in Castle Valley, Utah"},"predicate":"SUPERSEDED_BY","object":{"id":3192,"text":"wsp2195 - 1983 - Hydrology of the Ferron Sandstone aquifer and effects of proposed surface-coal mining in Castle Valley, Utah, with a section on stratigraphy and a section on leaching of overburden","indexId":"wsp2195","publicationYear":"1983","noYear":false,"title":"Hydrology of the Ferron Sandstone aquifer and effects of proposed surface-coal mining in Castle Valley, Utah, with a section on stratigraphy and a section on leaching of overburden"},"id":1}],"lastModifiedDate":"2023-11-29T22:45:01.092093","indexId":"wsp2195","displayToPublicDate":"1983-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":341,"text":"Water Supply Paper","code":"WSP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"2195","title":"Hydrology of the Ferron Sandstone aquifer and effects of proposed surface-coal mining in Castle Valley, Utah, with a section on stratigraphy and a section on leaching of overburden","docAbstract":"Coal in the Ferron Sandstone Member of the Mancos Shale of Cretaceous age has traditionally been mined by underground techniques in the Emery Coal Field in the southern end of Castle Valley in east-central Utah. However, approximately 99 million tons are recoverable by surface mining. Ground water in the Ferron is the sole source of supply for the town of Emery, but the aquifer is essentially untapped outside the Emery area.
The Ferron Sandstone Member crops out along the eastern edge of Castle Valley and generally dips 2 ? to 10 ? to the northwest. Sandstones in the Ferron are enclosed between relatively impermeable shale in the Tununk and Blue Gate Members of the Mancos Shale. Along the outcrop, the Ferron ranges in thickness from about 80 feet in the northern part of Castle Valley to 850 feet in the southern part. The Ferron also generally thickens in the subsurface downdip from the outcrop. Records from wells and test holes indicate that the full thickness of the Ferron is saturated with water in most areas downdip from the outcrop area.
Tests in the Emery area indicate that transmissivity of the Ferron sandstone aquifer ranges from about 200 to 700 feet squared per day where the Ferron is fully saturated. Aquifer transmissivity is greatest near the Paradise Valley-Joes Valley fault system where permeability has been increased by fracturing. Storage coefficient ranges from about 10 .6 to 10 -3 where the Ferron sandstone aquifer is confined and probably averages 5 x 10-2 where it is unconfined.
","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Washington, D.C.","doi":"10.3133/wsp2195","collaboration":"Prepared in cooperation with the United States Bureau of Land Management","usgsCitation":"Lines, G.C., Morrissey, D.J., Ryer, T.A., and Fuller, R.H., 1983, Hydrology of the Ferron Sandstone aquifer and effects of proposed surface-coal mining in Castle Valley, Utah, with a section on stratigraphy and a section on leaching of overburden: U.S. Geological Survey Water Supply Paper 2195, Report: vi, 40 p.; 3 Plates: 17.00 x 27.20 inches, https://doi.org/10.3133/wsp2195.","productDescription":"Report: vi, 40 p.; 3 Plates: 17.00 x 27.20 inches","numberOfPages":"46","costCenters":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":30174,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/2195/plate-1.pdf","text":"Plate 1","linkFileType":{"id":1,"text":"pdf"},"linkHelpText":"Map showing location of selected wells, springs, and test holes in and near Castle Valley, Utah, where ground-water information is available, 1980"},{"id":30175,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/2195/plate-2.pdf","text":"Plate 2","linkFileType":{"id":1,"text":"pdf"},"linkHelpText":"Map showing the thickness of the Ferron sandstone member of the Mancos shale in Castle Valley, Utah"},{"id":423046,"rank":6,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_25538.htm","linkFileType":{"id":5,"text":"html"}},{"id":138109,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/2195/report-thumb.jpg"},{"id":30177,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/2195/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":30176,"rank":5,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/2195/plate-3.pdf","text":"Plate 3","linkFileType":{"id":1,"text":"pdf"},"linkHelpText":"Map showing the altitude of the top of the Ferron Sandstone member of the Mancos Shale in Castle Valley, Utah"}],"country":"United States","state":"Utah","otherGeospatial":"Castle Valley","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -110.5,\n 39.75\n ],\n [\n -111.5,\n 39.75\n ],\n [\n -111.5,\n 38.5\n ],\n [\n -110.5,\n 38.5\n ],\n [\n -110.5,\n 39.75\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aa7e4b07f02db667150","contributors":{"authors":[{"text":"Lines, Gregory C.","contributorId":50502,"corporation":false,"usgs":true,"family":"Lines","given":"Gregory","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":146406,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Morrissey, Daniel J.","contributorId":89875,"corporation":false,"usgs":true,"family":"Morrissey","given":"Daniel","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":146408,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Ryer, Thomas A.","contributorId":100359,"corporation":false,"usgs":true,"family":"Ryer","given":"Thomas","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":146409,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Fuller, Richard H.","contributorId":66236,"corporation":false,"usgs":true,"family":"Fuller","given":"Richard","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":146407,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":70168593,"text":"70168593 - 1983 - Krakatau 1883","interactions":[],"lastModifiedDate":"2019-11-14T08:26:18","indexId":"70168593","displayToPublicDate":"1983-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1435,"text":"Earthquake Information Bulletin (USGS)","active":true,"publicationSubtype":{"id":10}},"title":"Krakatau 1883","docAbstract":"This year marks the 100th anniversary of the eruption of Krakatau, perhaps the most famous volcanic event in recorded history. During a 23-hour period on August 26 and 17, 1883, more than 4 cubic miles of volcanic debris exploded upward from Krakatau, resulting in the death of more than 36,000 people and producing catastrophic devastation. The 1883 events at Krakatau caused phenomena that were recorded around the world that lingered for several years after the main eruption.
","language":"English","publisher":"U.S Geological Survey","publisherLocation":"Reston, VA","usgsCitation":"Simkin, T., and Fiske, R., 1983, Krakatau 1883: Earthquake Information Bulletin (USGS), v. 15, no. 4, p. 128-133.","productDescription":"6 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","language":"English","publisher":"University of Washington","publisherLocation":"Seattle, WA","usgsCitation":"Washington, P.M., 1983, An analysis of factors affecting the production of coho salmon in the Columbia River.","costCenters":[{"id":654,"text":"Western Fisheries Research Center","active":true,"usgs":true}],"links":[{"id":336090,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"publicComments":"Ph.D. Dissertation","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"58b002dce4b01ccd54fb281d","contributors":{"authors":[{"text":"Washington, P. M.","contributorId":29453,"corporation":false,"usgs":true,"family":"Washington","given":"P.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":671241,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70140556,"text":"70140556 - 1983 - Synthesis of geophysical data with space-acquired imagery: a review","interactions":[],"lastModifiedDate":"2017-12-14T16:41:05","indexId":"70140556","displayToPublicDate":"1983-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":661,"text":"Advances in Space Research","active":true,"publicationSubtype":{"id":10}},"title":"Synthesis of geophysical data with space-acquired imagery: a review","docAbstract":"Geophysical data obtained from ground and airborne platforms have been used in the development of regional geologic models for many years. Space-acquired data and imagery have a shorter but similar history of applications. All these data may be synthesized either manually or digitally. Manual synthesis methods consist of overlaying and comparing maps, whereas digital synthesis methods consist of computer storage and analysis of registered digital data sets.
\nA data base may include topographic, geologic, soils, aeromagnetic, gravity, radiometric, electromagnetic and geochemical data, and Landsat, Seasat, and Heat Capacity Mapping Mission (HCMM) images, all of which can be evaluated individually or compared in multiple layers (overlays).
\nStereographic models, useful in the correlation and interpretation of geophysical data, have been created from Landsat images by using aeromagnetic, gravity, geochemical, or topographic values to offset Landsat pixels, thus introducing parallax and permitting stereoscopic viewing.
\nStatistical correlation has been used to determine the applicability of specific data sets to the development of geologic or exploration models. Various arithmetic functions have proven useful in developing models from such data sets.
","language":"English","publisher":"Elsevier","doi":"10.1016/0273-1177(83)90116-3","usgsCitation":"Hastings, D.A., 1983, Synthesis of geophysical data with space-acquired imagery: a review: Advances in Space Research, v. 3, no. 2, p. 157-168, https://doi.org/10.1016/0273-1177(83)90116-3.","productDescription":"12 p.","startPage":"157","endPage":"168","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":222,"text":"Earth Resources Observation and Science (EROS) Center","active":true,"usgs":true}],"links":[{"id":297837,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"3","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"54dd2c67e4b08de9379b379a","contributors":{"authors":[{"text":"Hastings, David A.","contributorId":138985,"corporation":false,"usgs":true,"family":"Hastings","given":"David","email":"","middleInitial":"A.","affiliations":[{"id":223,"text":"Earth Resources Observation and Science (EROS) Center (Geography)","active":false,"usgs":true}],"preferred":false,"id":540071,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70010637,"text":"70010637 - 1983 - A Pleistocene diatomaceous clay and a pumiceous ash, Yolo County ( California).","interactions":[],"lastModifiedDate":"2012-03-12T17:18:22","indexId":"70010637","displayToPublicDate":"1983-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1154,"text":"California Geology","active":true,"publicationSubtype":{"id":10}},"title":"A Pleistocene diatomaceous clay and a pumiceous ash, Yolo County ( California).","docAbstract":"Discusses a diatomaceous clay of Pleistocene age, cored from 534-544ft, and a pumiceous ash found at a depth of 453ft in a test hole. Tests on the clay indicate that it is highly susceptible to compaction, and therefore, it could contribute, or perhaps has contributed, to land subsidence in the area of the test hole. The pumiceous ash is considered to be younger than about 450 000 yr. -from Authors","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"California Geology","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","issn":"00264555","usgsCitation":"Page, R.W., and Bertoldi, G., 1983, A Pleistocene diatomaceous clay and a pumiceous ash, Yolo County ( California).: California Geology, v. 36, no. 1, p. 14-20.","startPage":"14","endPage":"20","numberOfPages":"7","costCenters":[],"links":[{"id":219257,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"36","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059e2f6e4b0c8380cd45d5b","contributors":{"authors":[{"text":"Page, R. W.","contributorId":17215,"corporation":false,"usgs":true,"family":"Page","given":"R.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":359318,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bertoldi, G.L.","contributorId":11605,"corporation":false,"usgs":true,"family":"Bertoldi","given":"G.L.","affiliations":[],"preferred":false,"id":359317,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":30050,"text":"wri824100 - 1983 - Land application of wastewater and its effect on ground-water quality in the Livermore-Amador Valley, Alameda County, California","interactions":[],"lastModifiedDate":"2023-03-14T21:05:28.776892","indexId":"wri824100","displayToPublicDate":"1983-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"82-4100","title":"Land application of wastewater and its effect on ground-water quality in the Livermore-Amador Valley, Alameda County, California","docAbstract":"Ground-water quality, ground-water level, and rainfall data collected during the 1975 water year through the 1980 water year were analyzed to determine the effects of land application of effluent from wastewater treatment plants on ground-water quality in the Livermore-Amador Valley. Annual rainfall varied markedly during the study: 1976 and 1977 water years had less than one half the normal rainfall; 1978 and 1980 water years had greater than normal rainfall; and 1975 and 1979 water years had nearly normal rainfall. The direction ground-water movement in the valley was found to be generally that of surface water. Dissolved nitrate concentrations were generally much less in areas not receiving wastewater applications than in areas that do. Specific conductance, dissolved solids, dissolved chloride, and dissolved nitrate were substantially less in the lower aquifers than in the upper aquifer in the Livermore wastewater application areas. In the Castlewood, Pleasanton, Veterans Administration Hospital, and Livermore wastewater applications areas ground-water quality was similar to the quality of effluent from wastewater treatment plants in the valley. Rainfall, soil, and geology appeared to be the main determinants of ground-water quality in the Castlewood and Dublin-San Ramon and Camp Parks Military Reservation areas. Wastewater application appeared to be the main determinant of ground-water quality in Pleasanton, Veterans Administration Hospital, and Livermore Municipal Airport areas. Comparison of ground-water quality in wastewater application areas with proposed State water-quality objectives for ground water in the Livermore-Amador Valley showed impaired water quality in all areas.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri824100","usgsCitation":"Sylvester, M.A., 1983, Land application of wastewater and its effect on ground-water quality in the Livermore-Amador Valley, Alameda County, California: U.S. Geological Survey Water-Resources Investigations Report 82-4100, Report: vi, 53 p.; 2 Plates: 41.37 x 40.76 inches and 42.24 x 40.61 inches, https://doi.org/10.3133/wri824100.","productDescription":"Report: vi, 53 p.; 2 Plates: 41.37 x 40.76 inches and 42.24 x 40.61 inches","costCenters":[],"links":[{"id":110155,"rank":5,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_35608.htm","linkFileType":{"id":5,"text":"html"},"description":"35608"},{"id":58861,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1982/4100/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":58860,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1982/4100/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":58859,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1982/4100/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":124278,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1982/4100/report-thumb.jpg"}],"country":"United States","state":"California","county":"Alameda County","otherGeospatial":"Livermore-Amador Valley","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -122,\n 37.5\n ],\n [\n -121.625,\n 37.5\n ],\n [\n -121.625,\n 37.8333\n ],\n [\n -122,\n 37.8333\n ],\n [\n -122,\n 37.5\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b25e4b07f02db6aeeaa","contributors":{"authors":[{"text":"Sylvester, M. A.","contributorId":10838,"corporation":false,"usgs":true,"family":"Sylvester","given":"M.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":202595,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70168856,"text":"70168856 - 1983 - Earthquakes; September-October 1982","interactions":[],"lastModifiedDate":"2016-03-24T16:01:57","indexId":"70168856","displayToPublicDate":"1983-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1435,"text":"Earthquake Information Bulletin (USGS)","active":true,"publicationSubtype":{"id":10}},"title":"Earthquakes; September-October 1982","docAbstract":"Seismically speaking the months of September and October were very quiet. There were no major (magnitude 7.0-7.9) earthquakes. Guatemala was struck by a moderate earthquake on September 29 causing fatalities and considerable damage.
\nIn the United States, a number of earthquakes occurred, but only slight damage was reported.
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","language":"English","publisher":"Wiley","doi":"10.2307/3808066","usgsCitation":"Blus, L.J., Pattee, O.H., Henny, C.J., and Prouty, R.M., 1983, First records of chlordane-related mortality in wild birds: Journal of Wildlife Management, v. 47, no. 1, p. 196-198, https://doi.org/10.2307/3808066.","productDescription":"3 p.","startPage":"196","endPage":"198","costCenters":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":196599,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"47","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f9e4b07f02db5f3883","contributors":{"authors":[{"text":"Blus, Lawrence J.","contributorId":35199,"corporation":false,"usgs":true,"family":"Blus","given":"Lawrence","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":334926,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Pattee, Oliver H.","contributorId":45412,"corporation":false,"usgs":true,"family":"Pattee","given":"Oliver","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":334927,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Henny, Charles J.","contributorId":12578,"corporation":false,"usgs":true,"family":"Henny","given":"Charles","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":334924,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Prouty, Richard M.","contributorId":79121,"corporation":false,"usgs":false,"family":"Prouty","given":"Richard","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":334925,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":70168866,"text":"70168866 - 1983 - Earthquakes; July-August 1982","interactions":[],"lastModifiedDate":"2016-03-24T16:11:18","indexId":"70168866","displayToPublicDate":"1983-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1435,"text":"Earthquake Information Bulletin (USGS)","active":true,"publicationSubtype":{"id":10}},"title":"Earthquakes; July-August 1982","docAbstract":"During this reporting period, there were three major (7.0-7.9) earthquakes all in unpopulated areas. The quakes occurred north of Macquarie Island on July 7, in the Santa Cruz Islands on August 5, and south of Panama on August 19. In the United Stats, a number of earthquakes occurred, but no damage was reported.
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