{"pageNumber":"2144","pageRowStart":"53575","pageSize":"25","recordCount":68909,"records":[{"id":70011620,"text":"70011620 - 1982 - Estimating irrigation water use and withdrawal of ground water on the High Plains, U.S.A.","interactions":[],"lastModifiedDate":"2013-01-20T09:17:03","indexId":"70011620","displayToPublicDate":"1982-01-01T00:00:00","publicationYear":"1982","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":"Estimating irrigation water use and withdrawal of ground water on the High Plains, U.S.A.","docAbstract":"In four decades following the Dust Bowl days of the 1930's, extensive areas of dry farming and rangeland on the semi-arid U.S. High Plains were transformed into a vast region of irrigated oases, producing meat and grain for much of the world. The agricultural economy has experienced such rapid growth in part because of the availability of ground water and because of development of new irrigation technology to use that water for agriculture. However, more water is being used than is being replaced. To estimate both the volume of water withdrawn and the regional scope of the problem a technique has been developed that combines multispectral data from Earth-orbiting satellite with known pumpage data for the same growing season. The location and extent of irrigated cropland-some with different crops watered at different times-is inventoried using computer-assisted analysis of the data from Landsat. The amount of water used is estimated by multiplying and summing surface area of irrigated agriculture and the average measured pumpage from sampled sites. Published findings to date are cited in the Selected References. All suggest transferability of a promising technology to the study of land transformation processes elsewhere. ?? 1983.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Advances in Space Research","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"Elsevier","doi":"10.1016/0273-1177(82)90229-0","issn":"02731177","usgsCitation":"Wray, J.R., 1982, Estimating irrigation water use and withdrawal of ground water on the High Plains, U.S.A.: Advances in Space Research, v. 2, no. 8, p. 127-129, https://doi.org/10.1016/0273-1177(82)90229-0.","startPage":"127","endPage":"129","numberOfPages":"3","costCenters":[],"links":[{"id":220987,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":266023,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1016/0273-1177(82)90229-0"}],"volume":"2","issue":"8","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a0b24e4b0c8380cd525be","contributors":{"authors":[{"text":"Wray, J. R.","contributorId":51851,"corporation":false,"usgs":true,"family":"Wray","given":"J.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":361560,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70011680,"text":"70011680 - 1982 - Optimal dynamic management of groundwater pollutant sources","interactions":[],"lastModifiedDate":"2018-02-05T13:12:34","indexId":"70011680","displayToPublicDate":"1982-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3722,"text":"Water Resources Research","onlineIssn":"1944-7973","printIssn":"0043-1397","active":true,"publicationSubtype":{"id":10}},"title":"Optimal dynamic management of groundwater pollutant sources","docAbstract":"<p><span>The linear programing-superposition method is presented for managing multiple sources of groundwater pollution over time. The method uses any linear solute transport simulation model to generate a unit source-concentration response matrix that is incorporated into a management model. This series of constraints indicates local solute concentration histories that will result from any series of waste injection schedules. The linear program operates on the matrix to arrive at optimal disposal schedules. An example demonstrates application of the method to maximizing groundwater waste disposal while maintaining water quality of local water supplies within desired limits. Flow field variations associated with waste injection are ignored as an approximation. Parametric programing is shown to be an important tool in evaluating waste disposal trade-offs at various injection sites over time. Mixed-integer programing permits restrictions to be placed upon the number of injection wells which may operate during given management periods.</span></p>","language":"English","publisher":"American Geophysical Union","doi":"10.1029/WR018i001p00071","usgsCitation":"Gorelick, S.M., and Remson, I., 1982, Optimal dynamic management of groundwater pollutant sources: Water Resources Research, v. 18, no. 1, p. 71-76, https://doi.org/10.1029/WR018i001p00071.","productDescription":"6 p.","startPage":"71","endPage":"76","costCenters":[],"links":[{"id":220922,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"18","issue":"1","noUsgsAuthors":false,"publicationDate":"2010-07-09","publicationStatus":"PW","scienceBaseUri":"505a6edfe4b0c8380cd75844","contributors":{"authors":[{"text":"Gorelick, Steven M.","contributorId":8784,"corporation":false,"usgs":true,"family":"Gorelick","given":"Steven","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":361700,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Remson, Irwin","contributorId":89115,"corporation":false,"usgs":true,"family":"Remson","given":"Irwin","email":"","affiliations":[],"preferred":false,"id":361701,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70011679,"text":"70011679 - 1982 - Nuclear magnetic resonance studies of ancient buried wood-II. Observations on the origin of coal from lignite to bituminous coal","interactions":[],"lastModifiedDate":"2019-12-13T07:34:47","indexId":"70011679","displayToPublicDate":"1982-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2958,"text":"Organic Geochemistry","active":true,"publicationSubtype":{"id":10}},"title":"Nuclear magnetic resonance studies of ancient buried wood-II. Observations on the origin of coal from lignite to bituminous coal","docAbstract":"Coalified logs ranging in age from Late Pennsylvania to Miocene and in rank from lignite B to bituminous coal were analyzed by 13C nuclear magnetic resonance (NMR) utilizing the cross-polarization, magic-angle spinning technique, as well as by infrared spectroscopy. The results of this study indicate that at least three major stages of coalification can be observed as wood gradually undergoes transformation to bituminous coal. The first stage involves hydrolysis and loss of cellulose from wood with retention and differential concentration of the resistant lignin. The second stage involves conversion of the lignin residues directly to coalified wood of lignitic rank, during which the oxygen content of intermediate diagenetic products remains constant as the hydrogen content and the carbon content increases. These changes are thought to involve loss of methoxyl groups, water, and C3 side chains from the lignin. In the third major stage of coalification, the coalified wood increases in rank to subbituminous and bituminous coal; during this stage the oxygen content decreases, hydrogen remains constant, and the carbon content increases. These changes are thought to result from loss of soluble humic acids that are rich in oxygen and that are mobilized during compaction and dewatering. Relatively resistant resinous substances are differentially concentrated in the coal during this stage. The hypothesis that humic acids are formed as mobile by-products of the coalification of lignin and function only as vehicles for removal of oxygen represents a dramatic departure from commonly accepted views that they are relatively low-molecular-weight intermediates formed during the degradation of lignin that then condense to form high-molecular-weight coal structures. ?? 1982.","language":"English","publisher":"Elsevier","doi":"10.1016/0146-6380(82)90003-1","issn":"01466380","usgsCitation":"Hatcher, P.G., Breger, I.A., Szeverenyi, N., and Maciel, G., 1982, Nuclear magnetic resonance studies of ancient buried wood-II. Observations on the origin of coal from lignite to bituminous coal: Organic Geochemistry, v. 4, no. 1, p. 9-18, https://doi.org/10.1016/0146-6380(82)90003-1.","productDescription":"10 p. 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 \"}}]}","volume":"4","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a68c5e4b0c8380cd739bd","contributors":{"authors":[{"text":"Hatcher, Patrick G.","contributorId":93625,"corporation":false,"usgs":true,"family":"Hatcher","given":"Patrick","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":361699,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Breger, Irving A.","contributorId":65205,"corporation":false,"usgs":true,"family":"Breger","given":"Irving","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":361698,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Szeverenyi, Nikolaus","contributorId":47908,"corporation":false,"usgs":true,"family":"Szeverenyi","given":"Nikolaus","affiliations":[],"preferred":false,"id":361697,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Maciel, G.E.","contributorId":43910,"corporation":false,"usgs":true,"family":"Maciel","given":"G.E.","email":"","affiliations":[],"preferred":false,"id":361696,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70011432,"text":"70011432 - 1982 - Sediment deposition in a flood retention structure after two record floods in southwestern Wisconsin.","interactions":[],"lastModifiedDate":"2013-03-15T20:53:03","indexId":"70011432","displayToPublicDate":"1982-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2456,"text":"Journal of Soil and Water Conservation","active":true,"publicationSubtype":{"id":10}},"title":"Sediment deposition in a flood retention structure after two record floods in southwestern Wisconsin.","docAbstract":"Sediment deposited in a flood-control structure was measured after record floods in SW Wisconsin on June 17 and June 30-July 1, 1978. The structure is in the Driftless Area, where high relief, erodible soils, and land use contribute to high soil losses. The two floods deposited 4.1 acre-ft of sediment in the structure.-from Authors","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Journal of Soil and Water Conservation","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"Soil and Water Conservation Society","usgsCitation":"Kammerer, P., and Batten, W.G., 1982, Sediment deposition in a flood retention structure after two record floods in southwestern Wisconsin.: Journal of Soil and Water Conservation, v. 37, no. 5, p. 302-304.","startPage":"302","endPage":"304","numberOfPages":"3","costCenters":[],"links":[{"id":221173,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":269420,"type":{"id":11,"text":"Document"},"url":"https://www.jswconline.org/content/37/5/302.abstract"}],"volume":"37","issue":"5","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505b8975e4b08c986b316de6","contributors":{"authors":[{"text":"Kammerer, P.A. Jr.","contributorId":39804,"corporation":false,"usgs":true,"family":"Kammerer","given":"P.A.","suffix":"Jr.","email":"","affiliations":[],"preferred":false,"id":361090,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Batten, W. G.","contributorId":89504,"corporation":false,"usgs":true,"family":"Batten","given":"W.","email":"","middleInitial":"G.","affiliations":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"preferred":false,"id":361091,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":1001440,"text":"1001440 - 1982 - Wetlands and deepwater habitats: a new classification","interactions":[],"lastModifiedDate":"2012-02-02T00:04:11","indexId":"1001440","displayToPublicDate":"1982-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2456,"text":"Journal of Soil and Water Conservation","active":true,"publicationSubtype":{"id":10}},"title":"Wetlands and deepwater habitats: a new classification","docAbstract":"Abstract has not been submitted","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Journal of Soil and Water Conservation","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","usgsCitation":"Cowardin, L., 1982, Wetlands and deepwater habitats: a new classification: Journal of Soil and Water Conservation, v. 37, no. 2, p. 83-85.","productDescription":"p. 83-85","startPage":"83","endPage":"85","numberOfPages":"2","costCenters":[],"links":[{"id":129014,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"37","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e2e4b07f02db5e49b4","contributors":{"authors":[{"text":"Cowardin, L.M.","contributorId":106435,"corporation":false,"usgs":true,"family":"Cowardin","given":"L.M.","email":"","affiliations":[],"preferred":false,"id":311030,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70011505,"text":"70011505 - 1982 - The effect of natural weathering on the chemical and isotopic compositions of biotites","interactions":[],"lastModifiedDate":"2024-03-18T14:40:15.488216","indexId":"70011505","displayToPublicDate":"1982-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1759,"text":"Geochimica et Cosmochimica Acta","active":true,"publicationSubtype":{"id":10}},"title":"The effect of natural weathering on the chemical and isotopic compositions of biotites","docAbstract":"<p>The effect of progressive natural weathering on the isotopic (Rb-Sr, K-Ar, δD,<span>&nbsp;</span><i>δ</i><sup>18</sup><i>O</i>) and chemical (REE, H<sub>2</sub>O<sup>+</sup>) compositions of biotite has been studied on a suite of migmatitic biotites from the Chad Republic. During the early stages of weathering the Rb-Sr system is strongly affected, the hydrogen and oxygen isotope compositions change markedly, the minerals are depleted in light REE, the water content increases by a factor of two, and the K-Ar system is relatively little disturbed. During intensive weathering the K-Ar system is more strongly disturbed than the Rb-Sr system.</p><p>Most of the isotopic and chemical modifications take place under nonequilibrium conditions and occur<span>&nbsp;</span><i>before</i><span>&nbsp;</span>newly formed kaolinite and/or smectite can be detected. These observations suggest that</p><ul class=\"list\"><li class=\"react-xocs-list-item\"><span class=\"list-label\">1.</span><p>(a) “protominerals” may form within the biotite structure during the initial period of weathering, and</p></li><li class=\"react-xocs-list-item\"><span class=\"list-label\">2.</span><p>(b) only when chemical equilibrium is approached in the weathering profile are new minerals able to form.</p></li></ul>","language":"English","publisher":"Elsevier","doi":"10.1016/0016-7037(82)90115-6","issn":"00167037","usgsCitation":"Clauer, N., O’Neil, J.R., and Bonnot-Courtois, C., 1982, The effect of natural weathering on the chemical and isotopic compositions of biotites: Geochimica et Cosmochimica Acta, v. 46, no. 10, p. 1755-1762, https://doi.org/10.1016/0016-7037(82)90115-6.","productDescription":"8 p.","startPage":"1755","endPage":"1762","numberOfPages":"8","costCenters":[],"links":[{"id":221292,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"46","issue":"10","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505bab39e4b08c986b322cdb","contributors":{"authors":[{"text":"Clauer, Norbert","contributorId":79664,"corporation":false,"usgs":false,"family":"Clauer","given":"Norbert","email":"","affiliations":[],"preferred":false,"id":361282,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"O’Neil, J. R.","contributorId":69633,"corporation":false,"usgs":true,"family":"O’Neil","given":"J.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":361281,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Bonnot-Courtois, C.","contributorId":90175,"corporation":false,"usgs":true,"family":"Bonnot-Courtois","given":"C.","email":"","affiliations":[],"preferred":false,"id":361283,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":1013898,"text":"1013898 - 1982 - Zooplankton production and manipulation in striped bass rearing ponds","interactions":[],"lastModifiedDate":"2023-08-09T14:57:14.512432","indexId":"1013898","displayToPublicDate":"1982-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":853,"text":"Aquaculture","active":true,"publicationSubtype":{"id":10}},"title":"Zooplankton production and manipulation in striped bass rearing ponds","docAbstract":"<div id=\"preview-section-abstract\"><div id=\"abstracts\" class=\"Abstracts u-font-gulliver text-s\"><div id=\"aep-abstract-id3\" class=\"abstract author\"><div id=\"aep-abstract-sec-id4\"><p>Zooplankton production and survival of striped bass fry (<i>Morone saxatilis</i>) were examined in ponds treated either with organic fertilizer (in 1980) or with a combination of organic and liquid inorganic fertilizers and inoculated with<span>&nbsp;</span><i>Daphnia pulex</i><span>&nbsp;</span>(in 1981). In 1980, there were significant differences in water quality variables and chlorophyll α levels among treatments in three series of three ponds fertilized only with different amounts of ground hay. Production of crustacean zooplankton was low, and rotifer populations increased as the number of crustaceans was reduced by predation. Electron transport system (ETS) activity was low in all treatments. Survival of striped bass differed greatly within and between treatments, ranging from 1 to 64% and averaging 17%. In 1981, water quality variation was less among treatments in four series of three ponds inoculated with<span>&nbsp;</span><i>Daphnia</i><span>&nbsp;</span>and fertilized either with chicken litter-chicken manure in combination with liquid ammonium nitrate and phosphoric acid, or with ground hay. Rotifer species were less abundant and numbers of crustacean zooplankton, total protein, and ETS activity were higher than in 1980. Survival of striped bass in 1981 ranged from 1 to 96% and averaged 45% in the ponds fertilized and inoculated with<span>&nbsp;</span><i>Daphnia</i>. Numbers of striped bass fingerlings produced per hectare and percent survival were significantly greater in 1981 (manure-fertilized ponds) than in 1980 (hay-fertilized ponds). Combinations of organic and liquid inorganic fertilizers and zooplankton inoculation are suggested to develop and maintain the zooplankton forage base in striped bass rearing ponds. Management effort (including the amounts and timing of organic and liquid inorganic fertilizers) should be shifted to maximize crustacean zooplankton foods during the period 2 weeks before and 2 weeks after the fish are stocked.</p></div></div></div></div>","language":"English","publisher":"Elsevier","doi":"10.1016/0044-8486(83)90105-9","usgsCitation":"Geiger, J.G., 1982, Zooplankton production and manipulation in striped bass rearing ponds: Aquaculture, v. 35, no. 4, p. 331-351, https://doi.org/10.1016/0044-8486(83)90105-9.","productDescription":"21 p.","startPage":"331","endPage":"351","numberOfPages":"21","costCenters":[{"id":365,"text":"Leetown Science Center","active":true,"usgs":true}],"links":[{"id":132017,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"35","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49afe4b07f02db5c88da","contributors":{"authors":[{"text":"Geiger, J. G.","contributorId":29340,"corporation":false,"usgs":true,"family":"Geiger","given":"J.","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":319412,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70011229,"text":"70011229 - 1982 - Obtaining maps and data from the U.S. Geological Survey","interactions":[],"lastModifiedDate":"2023-09-21T16:24:00.08603","indexId":"70011229","displayToPublicDate":"1982-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1317,"text":"Computers, Environment and Urban Systems","active":true,"publicationSubtype":{"id":10}},"title":"Obtaining maps and data from the U.S. Geological Survey","docAbstract":"<p><span>The U.S. Geological Survey produces a variety of resource information for the United States. This includes many data bases of particular interest to planners such as land use and terrain information prepared by the National Mapping Division, water quantity and quality data collected by Water Resources Division, and coal resource information gathered by the Geologic Division. These data are stored in various forms, and information on their availability can be obtained from appropriate offices in the U.S. Geological Survey as well as from USGS Circular 777. These data have been used for the management, development, and monitoring of our Nation's resources by Federal, State, and local agencies.</span></p>","language":"English","publisher":"Elsevier","doi":"10.1016/0198-9715(82)90016-3","usgsCitation":"Hallam, C.A., 1982, Obtaining maps and data from the U.S. Geological Survey: Computers, Environment and Urban Systems, v. 7, no. 4, p. 283-294, https://doi.org/10.1016/0198-9715(82)90016-3.","productDescription":"12 p.","startPage":"283","endPage":"294","numberOfPages":"12","costCenters":[],"links":[{"id":221032,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"7","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a6b0ee4b0c8380cd744c6","contributors":{"authors":[{"text":"Hallam, Cheryl A.","contributorId":59012,"corporation":false,"usgs":true,"family":"Hallam","given":"Cheryl","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":360619,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70011347,"text":"70011347 - 1982 - Notes. Characterization of plutonium in ground water near the idaho chemical processing plant","interactions":[],"lastModifiedDate":"2023-10-27T11:04:36.083216","indexId":"70011347","displayToPublicDate":"1982-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":5925,"text":"Environmental Science and Technology","active":true,"publicationSubtype":{"id":10}},"title":"Notes. Characterization of plutonium in ground water near the idaho chemical processing plant","docAbstract":"Plutonium is present in very low concentrations in ground water near the disposal well at the Idaho Chemical Processing Plant but was not detected in waters at greater distances. Because of the absence of strong complexing agents, the plutonium is present as an uncomplexed (perhaps hydrolyzed) tetravalent species, which is readily precipitated or sorbed by basalt or sediments along the ground-water flow path.","language":"English","publisher":"American Chemical Society","doi":"10.1021/es00101a014","usgsCitation":"Cleveland, J.M., and Rees, T.F., 1982, Notes. Characterization of plutonium in ground water near the idaho chemical processing plant: Environmental Science and Technology, v. 16, no. 7, p. 437-439, https://doi.org/10.1021/es00101a014.","productDescription":"3 p.","startPage":"437","endPage":"439","numberOfPages":"3","costCenters":[],"links":[{"id":220900,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Idaho","otherGeospatial":"Idaho Chemical Processing Plant area, Idaho National Engineering Laboratory","volume":"16","issue":"7","noUsgsAuthors":false,"publicationDate":"2002-05-01","publicationStatus":"PW","scienceBaseUri":"5059f4d5e4b0c8380cd4bf57","contributors":{"authors":[{"text":"Cleveland, Jess M.","contributorId":89661,"corporation":false,"usgs":true,"family":"Cleveland","given":"Jess","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":360886,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Rees, Terry F.","contributorId":9688,"corporation":false,"usgs":true,"family":"Rees","given":"Terry","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":886966,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70011606,"text":"70011606 - 1982 - Two-dimensional compressional wave velocity structure under San Francisco Volcanic Field, Arizona, from teleseismic P residual measurements","interactions":[],"lastModifiedDate":"2024-07-16T15:02:27.34143","indexId":"70011606","displayToPublicDate":"1982-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":6453,"text":"Journal of Geophysical Research Solid Earth","active":true,"publicationSubtype":{"id":10}},"title":"Two-dimensional compressional wave velocity structure under San Francisco Volcanic Field, Arizona, from teleseismic P residual measurements","docAbstract":"<p><span>A low compressional-wave velocity region in the midcrust below the San Francisco Mountain stratovolcano, Arizona, has been detected by the teleseismic&nbsp;</span><i>P</i><span>&nbsp;residual technique. This region is approximately 6 km wide, lies between elevations of 9 km and 34 km below sea level, and has a compressional velocity reduction of more than 6% with respect to the surrounding rocks. Several mechanisms are found to be quantitatively sufficient to produce such a feature. These include (1) a cool silicic pluton enclosed in a more mafic crust, (2) high temperature (near but below the solidus) in a quartz-bearing rock in the low-velocity region, (3) high density of water-filled cracks having pore pressures nearly equal to lithostatic pressure, and (4) the presence of melt, either in intergranular pores or in crystal-poor dikes.</span></p>","language":"English","publisher":"American Geophysical Union","doi":"10.1029/JB087iB07p05451","issn":"01480227","usgsCitation":"Stauber, D., 1982, Two-dimensional compressional wave velocity structure under San Francisco Volcanic Field, Arizona, from teleseismic P residual measurements: Journal of Geophysical Research Solid Earth, v. 87, no. B7, p. 5451-5459, https://doi.org/10.1029/JB087iB07p05451.","productDescription":"9 p.","startPage":"5451","endPage":"5459","numberOfPages":"9","costCenters":[],"links":[{"id":220782,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"87","issue":"B7","noUsgsAuthors":false,"publicationDate":"2012-09-20","publicationStatus":"PW","scienceBaseUri":"505bb992e4b08c986b327c84","contributors":{"authors":[{"text":"Stauber, D.A.","contributorId":52183,"corporation":false,"usgs":true,"family":"Stauber","given":"D.A.","email":"","affiliations":[],"preferred":false,"id":361528,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70011703,"text":"70011703 - 1982 - Paleoecological studies at Lake Patzcuaro on the west-central Mexican Plateau and at Chalco in the basin of Mexico","interactions":[],"lastModifiedDate":"2013-01-26T16:00:14","indexId":"70011703","displayToPublicDate":"1982-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3218,"text":"Quaternary Research","active":true,"publicationSubtype":{"id":10}},"title":"Paleoecological studies at Lake Patzcuaro on the west-central Mexican Plateau and at Chalco in the basin of Mexico","docAbstract":"A 1520-cm sediment core from Lake Patzcuaro, Michoacan, Mexico, is 44,000 yr old at the base. All parts of the core have abundant pollen of Pinus (pine), Alnus (alder), and Quercus (oak) with frequent Abies (fir). The interval dated from 44,000 to 11,000 yr ago has a homogeneous flora characterized by abundant Juniperus (juniper) pollen and frequent Artemisia (sagebrush). It is believed to represent an appreciably drier and colder climate than at present. The Holocene at Lake Patzcuaro is characterized by a moderate increase in Pinus pollen and the loss of Juniperus pollen, as the modern type of climate succeeded. Alnus was abundant until about 5000 yr ago; its abrupt decrease with the first appearance of herbaceous weed pollen may reflect the cutting of lake-shore and stream-course alder communities for agricultural purposes, or it may simply reflect a drying tendency in the climate. Pollen of Zea (corn) appears at Lake Patzcuaro along with low peaks of chenopod and grass pollen at 3500 yr B.P. apparently recording a human population large enough to modify the natural environment, as well as the beginning of agriculture. A rich aquatic flora in this phase suggests eutrophication of the lake by slope erosion. In the most recent period corn is absent from the sediments, perhaps reflecting a change in agricultural practices. The environment changes at Lake Patzcuaro are similar to and correlate with those in the Cuenca de Mexico, where diatom stratigraphy from the Chalco basin indicates fluctuations in lake levels and lake chemistry in response to variations in available moisture. Before 10,000 yr ago climates there were cool and dry, and the Chalco basin was occupied by a shallow freshwater marsh that drained north to Lake Texcoco, where saline water accumulated by evaporation. Increases in effective moisture and possible melting of glaciers during the Holocene caused lake levels to rise throughout the Cuenca de Mexico, and Lake Texcoco flooded the Chalco basin with brackish water. After 5000 yr ago such flooding decreased, and shallow freshwater ponds and marshes were restored in the Chalco basin. This environmental change coincides with the appearance of Zea pollen and suggests cultural control of lake levels and salinity. ?? 1982.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Quaternary Research","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"Elsevier","publisherLocation":"Amsterdam, Netherlands","doi":"10.1016/0033-5894(82)90045-X","issn":"00335894","usgsCitation":"Watts, W., and Bradbury, J., 1982, Paleoecological studies at Lake Patzcuaro on the west-central Mexican Plateau and at Chalco in the basin of Mexico: Quaternary Research, v. 17, no. 1, p. 56-70, https://doi.org/10.1016/0033-5894(82)90045-X.","startPage":"56","endPage":"70","numberOfPages":"15","costCenters":[],"links":[{"id":266567,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1016/0033-5894(82)90045-X"},{"id":221307,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"17","issue":"1","noUsgsAuthors":false,"publicationDate":"2017-01-20","publicationStatus":"PW","scienceBaseUri":"505a73d7e4b0c8380cd772a2","contributors":{"authors":[{"text":"Watts, W.A.","contributorId":95616,"corporation":false,"usgs":true,"family":"Watts","given":"W.A.","email":"","affiliations":[],"preferred":false,"id":361763,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bradbury, J.P.","contributorId":14431,"corporation":false,"usgs":true,"family":"Bradbury","given":"J.P.","email":"","affiliations":[],"preferred":false,"id":361762,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":44522,"text":"wri824043 - 1982 - Map showing cumulative thickness of sandstone in the Fox Hills-Lower Hell Creek aquifer, Montana","interactions":[],"lastModifiedDate":"2023-03-15T18:32:18.234504","indexId":"wri824043","displayToPublicDate":"1982-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"82-4043","title":"Map showing cumulative thickness of sandstone in the Fox Hills-Lower Hell Creek aquifer, Montana","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri824043","usgsCitation":"Feltis, R.D., 1982, Map showing cumulative thickness of sandstone in the Fox Hills-Lower Hell Creek aquifer, Montana: U.S. Geological Survey Water-Resources Investigations Report 82-4043, 1 Plate: 35.48 x 22.48 inches, https://doi.org/10.3133/wri824043.","productDescription":"1 Plate: 35.48 x 22.48 inches","costCenters":[],"links":[{"id":162410,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":414244,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_35567.htm","linkFileType":{"id":5,"text":"html"}},{"id":81904,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1982/4043/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Montana","otherGeospatial":"Fox Hills-Lower Hell Creek aquifer","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -104.054,\n              49\n            ],\n            [\n              -110,\n              49\n            ],\n            [\n              -110,\n              45\n            ],\n            [\n              -104.054,\n              45\n            ],\n            [\n              -104.054,\n              49\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a94e4b07f02db659150","contributors":{"authors":[{"text":"Feltis, Richard D.","contributorId":98773,"corporation":false,"usgs":true,"family":"Feltis","given":"Richard","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":229927,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70011587,"text":"70011587 - 1982 - Depositional setting and diagenetic evolution of some Tertiary unconventional reservoir rocks, Uinta Basin, Utah","interactions":[],"lastModifiedDate":"2023-01-10T17:56:03.888123","indexId":"70011587","displayToPublicDate":"1982-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":701,"text":"American Association of Petroleum Geologists Bulletin","active":true,"publicationSubtype":{"id":10}},"title":"Depositional setting and diagenetic evolution of some Tertiary unconventional reservoir rocks, Uinta Basin, Utah","docAbstract":"<p>The Douglas Creek Member of the Tertiary Green River Formation underlies much of the Uinta basin, Utah, and contains large volumes of oil and gas trapped in a complex of fractured low-permeability sandstone reservoirs. In the southeastern part of the basin at Pariette Bench, the Eocene Douglas Creek Member is a thick sequence of fine-grained alluvial sandstone complexly intercalated with lacustrine claystone and carbonate rock. Sediments were deposited in a subsiding intermontane basin along the shallow fluctuating margin of ancient Lake Uinta. Although the Uinta basin has undergone postdepositional uplift and erosion, the deepest cored rocks at Pariette Bench have never been buried more than 9,800 ft (3,000 m).</p><p>The sandstones, dominantly lithic arkoses and feldspathic litharenites, were derived from source terranes south of the Uinta basin. Secondary silica and several generations of authigenic calcite [Ca<sub>1.8-1.9</sub>(Mg<sub>0.02-0.06</sub>Fe<sub>0.02-0.06</sub>)(CO<sub>3</sub>)<sub>2</sub>], dolomite [Ca<sub>1.3-1.4</sub>(Mg<sub>0.6-0.7</sub>Fe<sub>0.02-0.04</sub>)(CO<sub>3</sub>)<sub>2</sub>], and ankerite [Ca<sub>1.2-1.3</sub>(Mg<sub>0.2-0.3</sub>Fe<sub>0.4-0.6</sub>)(CO<sub>3</sub>)<sub>2</sub>] form a replacive cement in the sandstones. Commonly, syntaxial overgrowths of late iron-bearing carbonate occur on detrital grains and preexisting relicts of iron-free carbonate cement. In sandstone where carbonate has been partly dissolved, abundant authigenic illite, partly ordered mixed- ayer illite-smectite, and small amounts of chlorite partly to completely fill secondary pores. Isotopic composition of carbonate cement and grain-supported rock range from -0.39 to -6.18 ^pmil for ^dgr<sup>13</sup>C and -7.80 to -13.98 ^pmil for ^dgr<sup>18</sup>O, indicating that authigenic carbonate formed at low temperatures in the presence of meteoric waters by a process of solution-precipitation. Enrichment of carbon and oxygen in early diagenetic calcite and fossiliferous rock relative to late diagenetic ankerite indicates a trend toward lighter isotopic carbonate compositions with increasing diagenesis.</p><p>Kerogenous rocks at Pariette Bench are thermochemically immature and therefore are not the source of oil produced in the field. Hydrocarbons are compositionally similar to some of the oils produced from the Green River Formation in the Bluebell-Altamont field and are interpreted to have migrated from mature Green River source rocks through a network of open fractures. The occurrence of small amounts of hydrocarbon in secondary pores indicates that its emplacement postdated carbonate dissolution.</p>","language":"English","publisher":"American Association of Petroleum Geologists","doi":"10.1306/03B5A98F-16D1-11D7-8645000102C1865D","usgsCitation":"Pitman, J.K., Fouch, T.D., and Goldhaber, M., 1982, Depositional setting and diagenetic evolution of some Tertiary unconventional reservoir rocks, Uinta Basin, Utah: American Association of Petroleum Geologists Bulletin, v. 66, no. 10, p. 1581-1596, https://doi.org/10.1306/03B5A98F-16D1-11D7-8645000102C1865D.","productDescription":"16 p.","startPage":"1581","endPage":"1596","numberOfPages":"16","costCenters":[{"id":241,"text":"Eastern Energy Resources Science Center","active":true,"usgs":true}],"links":[{"id":221598,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Utah","otherGeospatial":"Uinta Basin","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -111.0225857789739,\n              40.63348012338835\n            ],\n            [\n              -111.0225857789739,\n              39.27696875971418\n            ],\n            [\n              -108.75245518662385,\n              39.27696875971418\n            ],\n            [\n              -108.75245518662385,\n              40.63348012338835\n            ],\n            [\n              -111.0225857789739,\n              40.63348012338835\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","volume":"66","issue":"10","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059fec8e4b0c8380cd4ef16","contributors":{"authors":[{"text":"Pitman, Janet K. 0000-0002-0441-779X jpitman@usgs.gov","orcid":"https://orcid.org/0000-0002-0441-779X","contributorId":767,"corporation":false,"usgs":true,"family":"Pitman","given":"Janet","email":"jpitman@usgs.gov","middleInitial":"K.","affiliations":[{"id":241,"text":"Eastern Energy Resources Science Center","active":true,"usgs":true},{"id":164,"text":"Central Energy Resources Science Center","active":true,"usgs":true}],"preferred":true,"id":361472,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Fouch, T. D.","contributorId":68333,"corporation":false,"usgs":true,"family":"Fouch","given":"T.","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":361471,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Goldhaber, M. B. 0000-0002-1785-4243","orcid":"https://orcid.org/0000-0002-1785-4243","contributorId":103280,"corporation":false,"usgs":true,"family":"Goldhaber","given":"M. B.","affiliations":[],"preferred":false,"id":361473,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70011451,"text":"70011451 - 1982 - Fate of acetone in water","interactions":[],"lastModifiedDate":"2020-01-26T09:59:06","indexId":"70011451","displayToPublicDate":"1982-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1226,"text":"Chemosphere","active":true,"publicationSubtype":{"id":10}},"title":"Fate of acetone in water","docAbstract":"<p>The physical, chemical, and biological processes that might affect the concentration of acetone in water were investigated in laboratory studies. Processes considered included volatilization, adsorption by sediments, photodecomposition, bacterial degradation, and absorption by algae and molds. It was concluded that volatilization and bacterial degradation were the dominant processes determining the fate of acetone in streams and rivers.</p>","language":"English","publisher":"Elsevier","doi":"10.1016/0045-6535(82)90114-X","issn":"00456535","usgsCitation":"Rathbun, R.E., Stephens, D.W., and Shultz, D., 1982, Fate of acetone in water: Chemosphere, v. 11, no. 11, p. 1097-1114, https://doi.org/10.1016/0045-6535(82)90114-X.","productDescription":"18 p.","startPage":"1097","endPage":"1114","numberOfPages":"18","costCenters":[{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":221525,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"11","issue":"11","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a0f10e4b0c8380cd53741","contributors":{"authors":[{"text":"Rathbun, R. E.","contributorId":61796,"corporation":false,"usgs":true,"family":"Rathbun","given":"R.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":361147,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Stephens, D. W.","contributorId":68335,"corporation":false,"usgs":true,"family":"Stephens","given":"D.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":361148,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Shultz, D.J.","contributorId":60246,"corporation":false,"usgs":true,"family":"Shultz","given":"D.J.","email":"","affiliations":[],"preferred":false,"id":361146,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70011589,"text":"70011589 - 1982 - Rapid intrusion of magma into wet rock: Groundwater flow due to pore pressure increases","interactions":[],"lastModifiedDate":"2024-07-16T15:04:29.069009","indexId":"70011589","displayToPublicDate":"1982-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":6453,"text":"Journal of Geophysical Research Solid Earth","active":true,"publicationSubtype":{"id":10}},"title":"Rapid intrusion of magma into wet rock: Groundwater flow due to pore pressure increases","docAbstract":"<p><span>Analytical and numerical solutions are developed to simulate the pressurization, expansion, and flow of groundwater contained within saturated, intact host rocks subject to sudden heating from the planar surface of an igneous intrusion. For most rocks, water diffuses more rapidly than heat, assuring that groundwater is not heated along a constant-volume pressure path and that thermal expansion and pressurization adjacent to the intrusion drives a flow that extends well beyond the heated region. The forcing parameter for pressurization and flow is α Δ</span><i>T</i><span>, where α is a thermal expansion coefficient reflecting the overall expansion of water heated through the temperature difference Δ</span><i>T</i><span>&nbsp;between the initial ambient and intrusive values. Pore pressure increases due to heating are greatest when the intrusion is emplaced rapidly and where the intrusive contact is impervious to groundwater contained in stiff, impermeable rocks with high thermal diffusivities and porosities. The maximum velocity of water flowing in pores decays with the inverse square root of time and is insensitive to hydraulic properties of the host rocks. Pressures are lessened and flow directions are reversed with the onset of hydrothermal convection. This occurs at times ranging from hours to weeks after onset of intrusion. As magma rises into near-surface rocks, steam can be generated. Solutions indicate that pressure increases and velocities are sensitive to the overall amount of expansion rather than the behavior of the water-steam transition. Both the overall thermal expansion coefficient α and the temperature difference Δ</span><i>T</i><span>&nbsp;are greater in shallow (&lt;1 km) environments than in deep (∼5 km) ones. Thus, for rocks with similar transport properties, pressure increases due to heating are greatest in shallow environments. Although solutions can be applied to rocks with a wide variety of properties, pressure increases are calculated for compliant quartz-rich sedimentary rocks with a porosities between 1 and 20% and permeabilities between 1 darcy and 1 μdarcy, subject to temperature increases of 500 and 1000 K at depths ranging from 0.1 to 5 km in a region of hydrostatic pressures and normal geothermal gradient. Such rocks, with porosities greater than 5%, permeabilities less than a 0.1 mdarcy, and drained hydrostatic compressibilities of 10</span><sup>−4</sup><span>/MPa, undergo pressure increases greater than 10 MPa (100 bars)for conditions typical of water table depths of 2.5 km and heating to 500 K above ambient. Similar rocks, but with permeabilities less than 1 mdarcy, undergo pressure increases of 10 MPa for conditions typical of 1 km water table depth. Rocks commonly considered to be good aquifers undergo pressure increases of less than 1 MPa, primarily because of their high permeability. Although these estimates neglect the effects of fracturing and brecciation that may accompany such pressure increases, calculations indicate that pressure increases due to heating of cool groundwater can lead to failure of host rocks by a phreatic mechanism.</span></p>","language":"English","publisher":"American Geophysical Union","doi":"10.1029/JB087iB09p07739","issn":"01480227","usgsCitation":"Delaney, P., 1982, Rapid intrusion of magma into wet rock: Groundwater flow due to pore pressure increases: Journal of Geophysical Research Solid Earth, v. 87, no. B9, p. 7739-7756, https://doi.org/10.1029/JB087iB09p07739.","productDescription":"18 p.","startPage":"7739","endPage":"7756","numberOfPages":"18","costCenters":[],"links":[{"id":221600,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"87","issue":"B9","noUsgsAuthors":false,"publicationDate":"2012-09-20","publicationStatus":"PW","scienceBaseUri":"505a94ebe4b0c8380cd816d2","contributors":{"authors":[{"text":"Delaney, P.T.","contributorId":69980,"corporation":false,"usgs":true,"family":"Delaney","given":"P.T.","email":"","affiliations":[],"preferred":false,"id":361478,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":1004127,"text":"1004127 - 1982 - Chlamydiosis in 2 biologists investigating disease occurrences in wild waterfowl","interactions":[],"lastModifiedDate":"2018-02-27T16:52:57","indexId":"1004127","displayToPublicDate":"1982-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3779,"text":"Wildlife Society Bulletin","onlineIssn":"1938-5463","printIssn":"0091-7648","active":true,"publicationSubtype":{"id":10}},"title":"Chlamydiosis in 2 biologists investigating disease occurrences in wild waterfowl","docAbstract":"<p>Chlamydiosis (ornithosis, psittacosis) is an infectious disease of birds that can be transmitted to humans. Human infections are probably acquired by inhalation of aerosols containing elementary bodies of the causative agent <i>Chlamydia psittaci</i>, from bird droppings, or from tissues. Infected birds do not have to be ill to transmit the organism (Schachter and Dawson 1978). The disease in humans is considered an occupational risk for people working with pet birds (particularly psittacine species) and poultry, but all avian species can be considered as potential reservoirs (Schachter and Dawson 1978). Burkhart and Page (1971) listed &gt;130 species of wild birds as being infected.</p><p>The purpose of this report is to draw the disease to the attention of those working with wild birds by describing 2 cases acquired from wild waterfowl and by reviewing other information on human infections associated with wild birds. We do this because the disease can be serious if not treated properly, and because the disease is not usually associated with wild birds the diagnosis may not be considered by physicians without some prompting from the patient.</p>","language":"English","publisher":"Wiley","usgsCitation":"Wobeser, G., and Brand, C.J., 1982, Chlamydiosis in 2 biologists investigating disease occurrences in wild waterfowl: Wildlife Society Bulletin, v. 10, no. 2, p. 170-172.","productDescription":"3 p.","startPage":"170","endPage":"172","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":456,"text":"National Wildlife Health Center","active":true,"usgs":true}],"links":[{"id":135723,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":15346,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://www.jstor.org/stable/3781740","linkFileType":{"id":5,"text":"html"},"description":"3554.000000000000000"}],"country":"Canada, United States of America","state":"California, Manitoba, Saskatchewan, Texas, Wisconsin","otherGeospatial":"Aransas National Wildlife 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 \"}}]}","volume":"10","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49c2e4b07f02db5d3cf0","contributors":{"authors":[{"text":"Wobeser, Gary","contributorId":120268,"corporation":false,"usgs":false,"family":"Wobeser","given":"Gary","email":"","affiliations":[{"id":13248,"text":"University of Saskatchewan","active":true,"usgs":false}],"preferred":false,"id":315230,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Brand, Christopher J. cbrand@usgs.gov","contributorId":1186,"corporation":false,"usgs":true,"family":"Brand","given":"Christopher","email":"cbrand@usgs.gov","middleInitial":"J.","affiliations":[{"id":456,"text":"National Wildlife Health Center","active":true,"usgs":true}],"preferred":true,"id":315231,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70045309,"text":"70045309 - 1982 - Notes on sedimentation activities calendar year 1981","interactions":[],"lastModifiedDate":"2013-05-23T11:22:13","indexId":"70045309","displayToPublicDate":"1982-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":1,"text":"Federal Government Series"},"title":"Notes on sedimentation activities calendar year 1981","docAbstract":"This report is a digest of information furnished by those Federal agencies conducting sedimentation investigations. It includes descriptions of work in progress or planned, important findings, new methods, new publications, laboratory and other research activities, and other pertinent information. The material has been organized by major drainage regions in the conterminous United States, Alaska, Hawaii, Puerto Rico, and foreign. There is also a section on Research and Other Activities.","language":"English","publisher":"U.S. Geological Survey, Office of Water Data Coordination","publisherLocation":"Reston, VA","usgsCitation":"U.S. Interagency Advisory Committee on Water Data- Subcommittee on Sedimentation, 1982, Notes on sedimentation activities calendar year 1981, xx, 287 p.","productDescription":"xx, 287 p.","numberOfPages":"310","temporalStart":"1981-01-01","temporalEnd":"1981-12-31","costCenters":[],"links":[{"id":270685,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/unnumbered/70045309/report-thumb.jpg"},{"id":272708,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/unnumbered/70045309/report.pdf"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5165386ee4b077fa94dadfd9","contributors":{"authors":[{"text":"U.S. Interagency Advisory Committee on Water Data- Subcommittee on Sedimentation","contributorId":127893,"corporation":true,"usgs":false,"organization":"U.S. Interagency Advisory Committee on Water Data- Subcommittee on Sedimentation","id":535468,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":1001252,"text":"1001252 - 1982 - Electric fences to reduce mammalian predation on waterfowl nests","interactions":[],"lastModifiedDate":"2018-01-02T13:20:25","indexId":"1001252","displayToPublicDate":"1982-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3779,"text":"Wildlife Society Bulletin","onlineIssn":"1938-5463","printIssn":"0091-7648","active":true,"publicationSubtype":{"id":10}},"title":"Electric fences to reduce mammalian predation on waterfowl nests","docAbstract":"We evaluated electric fences as predator barriers to reduce high losses of waterfowl nests to mammalian predation at Waterfowl Production Areas (WPAs). The work was done in 1978-81 on 3 paired sites in central North Dakota and western Minnesota. Resident mammalian predators were trapped from inside the exclosures. All 3 fences operated during the study period with few major maintenance problems. Nest success in the exclosures was 65% in North Dakota and 55% in Minnesota vs. 45 and 12% in the respective controls. Cover inside the electric fence produced 7.8 more young/ha than cover in control plots in North Dakota during the 3 years. Cover inside the 2 electric fences in Minnesota yielded 9.5 and 4.3 more young/ha than cover in control plots during the 3 years. Using construction costs only we estimated that each additional duckling produced in cover protected by electric fencing cost $0.65 in North Dakota and $0.87 in Minnesota.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Wildlife Society Bulletin","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"U.S. Fish and Wildlife Service","usgsCitation":"Lokemoen, J.T., Doty, H.A., Sharp, D., and Neaville, J., 1982, Electric fences to reduce mammalian predation on waterfowl nests: Wildlife Society Bulletin, v. 10, no. 4, p. 318-323.","productDescription":"6 p.","startPage":"318","endPage":"323","costCenters":[{"id":480,"text":"Northern Prairie Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":133772,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"10","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a25e4b07f02db60ed66","contributors":{"authors":[{"text":"Lokemoen, J. T.","contributorId":79049,"corporation":false,"usgs":true,"family":"Lokemoen","given":"J.","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":310752,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Doty, Harold A.","contributorId":17565,"corporation":false,"usgs":true,"family":"Doty","given":"Harold","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":310749,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Sharp, D.E.","contributorId":34460,"corporation":false,"usgs":true,"family":"Sharp","given":"D.E.","email":"","affiliations":[],"preferred":false,"id":310751,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Neaville, J.E.","contributorId":30200,"corporation":false,"usgs":true,"family":"Neaville","given":"J.E.","email":"","affiliations":[],"preferred":false,"id":310750,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70174408,"text":"70174408 - 1982 - Removing tidal-period variations from time-series data using low-pass digital filters","interactions":[],"lastModifiedDate":"2016-07-27T15:44:58","indexId":"70174408","displayToPublicDate":"1982-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2426,"text":"Journal of Physical Oceanography","active":true,"publicationSubtype":{"id":10}},"title":"Removing tidal-period variations from time-series data using low-pass digital filters","docAbstract":"<p><span>Several low-pass, digital filters are examined for their ability to remove tidal Period Variations from a time-series of water surface elevation for San Francisco Bay. The most efficient filter is the one which is applied to the Fourier coefficients of the transformed data, and the filtered data recovered through an inverse transform. The ability of the filters to remove the tidal components increased in the following order: 1) cosine-Lanczos filter, 2) cosine-Lanczos squared filter; 3) Godin filter; and 4) a transform fitter. The Godin fitter is not sufficiently sharp to prevent severe attenuation of 2&ndash;3 day variations in surface elevation resulting from weather events.</span></p>","language":"English","publisher":"American Meteorological Society","doi":"10.1175/1520-0485(1982)012<0112:RTPVFT>2.0.CO;2","usgsCitation":"Walters, R.A., and Heston, C., 1982, Removing tidal-period variations from time-series data using low-pass digital filters: Journal of Physical Oceanography, v. 12, p. 112-115, https://doi.org/10.1175/1520-0485(1982)012<0112:RTPVFT>2.0.CO;2.","productDescription":"4 p.","startPage":"112","endPage":"115","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":552,"text":"San Francisco Bay-Delta","active":false,"usgs":true},{"id":5079,"text":"Pacific Regional Director's Office","active":true,"usgs":true}],"links":[{"id":480556,"rank":0,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1175/1520-0485(1982)012<0112:rtpvft>2.0.co;2","text":"Publisher Index Page"},{"id":325054,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"12","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5784c343e4b0e02680be59cf","contributors":{"authors":[{"text":"Walters, Roy A.","contributorId":74877,"corporation":false,"usgs":true,"family":"Walters","given":"Roy","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":642142,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Heston, Cynthia","contributorId":172808,"corporation":false,"usgs":false,"family":"Heston","given":"Cynthia","email":"","affiliations":[],"preferred":false,"id":642143,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":47662,"text":"wri824037 - 1982 - Map showing total thickness of the \"Dakota Sandstone,\" Montana","interactions":[],"lastModifiedDate":"2023-03-21T18:29:27.496972","indexId":"wri824037","displayToPublicDate":"1982-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"82-4037","title":"Map showing total thickness of the \"Dakota Sandstone,\" Montana","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri824037","usgsCitation":"Feltis, R.D., 1982, Map showing total thickness of the \"Dakota Sandstone,\" Montana: U.S. Geological Survey Water-Resources Investigations Report 82-4037, 1 Plate: 35.48 x 22.21 inches, https://doi.org/10.3133/wri824037.","productDescription":"1 Plate: 35.48 x 22.21 inches","costCenters":[],"links":[{"id":170514,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":414466,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_35561.htm","linkFileType":{"id":5,"text":"html"}},{"id":84574,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1982/4037/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Montana","otherGeospatial":"Dakota Sandstone","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -104.054,\n              49\n            ],\n            [\n              -113,\n              49\n            ],\n            [\n              -113,\n              45\n            ],\n            [\n              -104.054,\n              45\n            ],\n            [\n              -104.054,\n              49\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a9fe4b07f02db660e8a","contributors":{"authors":[{"text":"Feltis, Richard D.","contributorId":98773,"corporation":false,"usgs":true,"family":"Feltis","given":"Richard","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":235973,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70011812,"text":"70011812 - 1982 - The effect of sulfate on aluminum concentrations in natural waters: some stability relations in the system Al2O3-SO3-H2O at 298 K","interactions":[],"lastModifiedDate":"2020-03-09T19:51:33","indexId":"70011812","displayToPublicDate":"1982-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1759,"text":"Geochimica et Cosmochimica Acta","active":true,"publicationSubtype":{"id":10}},"title":"The effect of sulfate on aluminum concentrations in natural waters: some stability relations in the system Al2O3-SO3-H2O at 298 K","docAbstract":"<p>While gibbsite and kaolinite solubilities usually regulate aluminum concentrations in natural waters, the presence of sulfate can dramatically alter these solubilities under acidic conditions, where other, less soluble minerals can control the aqueous geochemistry of aluminum. The likely candidates include alunogen, Al<sub>2</sub>(SO<sub>4</sub>)<sub>3</sub><span>&nbsp;</span>· 17H<sub>2</sub>O, alunite, KAl<sub>3</sub>(SO<sub>4</sub>)<sub>2</sub>(OH)<sub>6</sub>, jurbanite, Al(SO<sub>4</sub>)(OH) · 5H<sub>2</sub>O, and basaluminite, Al<sub>4</sub>(SO<sub>4</sub>)(OH)<sub>10</sub><span>&nbsp;</span>· 5H<sub>2</sub>O. An examination of literature values shows that the log<span>&nbsp;</span><span class=\"math\"><span id=\"MathJax-Element-1-Frame\" class=\"MathJax_SVG\" data-mathml=\"<math xmlns=&quot;http://www.w3.org/1998/Math/MathML&quot;><mtext>K</mtext><msub><mi></mi><mn>sp</mn></msub><mtext>= &amp;#x2212;85.4</mtext></math>\"><span class=\"MJX_Assistive_MathML\">Ksp= −85.4</span></span></span><span>&nbsp;</span>for alunite and log<span>&nbsp;</span><span class=\"math\"><span id=\"MathJax-Element-2-Frame\" class=\"MathJax_SVG\" data-mathml=\"<math xmlns=&quot;http://www.w3.org/1998/Math/MathML&quot;><mtext>K</mtext><msub><mi></mi><mn>sp</mn></msub><mtext>= &amp;#x2212;117.7</mtext></math>\"><span class=\"MJX_Assistive_MathML\">Ksp= −117.7</span></span></span><span>&nbsp;</span>for basaluminite. In this report the log<span>&nbsp;</span><span class=\"math\"><span id=\"MathJax-Element-3-Frame\" class=\"MathJax_SVG\" data-mathml=\"<math xmlns=&quot;http://www.w3.org/1998/Math/MathML&quot;><mtext>K</mtext><msub><mi></mi><mn>sp</mn></msub><mtext>= &amp;#x2212;7.0</mtext></math>\"><span class=\"MJX_Assistive_MathML\">Ksp= −7.0</span></span></span><span>&nbsp;</span>is estimated for alunogen and log<span>&nbsp;</span><span class=\"math\"><span id=\"MathJax-Element-4-Frame\" class=\"MathJax_SVG\" data-mathml=\"<math xmlns=&quot;http://www.w3.org/1998/Math/MathML&quot;><mtext>K</mtext><msub><mi></mi><mn>sp</mn></msub><mtext>= &amp;#x2212;17.8</mtext></math>\"><span class=\"MJX_Assistive_MathML\">Ksp= −17.8</span></span></span><span>&nbsp;</span>is estimated for jurbanite. The solubility and stability relations among these four minerals and gibbsite are plotted as a function of pH and sulfate activity at 298 K. Alunogen is stable only at pH values too low for any natural waters (&lt;0) and probably only forms as efflorescences from capillary films. Jurbanite is stable from<span>&nbsp;</span><span class=\"math\"><span id=\"MathJax-Element-5-Frame\" class=\"MathJax_SVG\" data-mathml=\"<math xmlns=&quot;http://www.w3.org/1998/Math/MathML&quot;><mtext>pH &amp;lt; 0</mtext></math>\"><span class=\"MJX_Assistive_MathML\">pH &lt; 0</span></span></span><span>&nbsp;</span>up to the range of 3–5 depending on sulfate activity. Alunite is stable at higher pH values than jurbanite, up to 4–7 depending on sulfate activity. Above these pH limits gibbsite is the most stable phase. Basaluminite, although kinetically favored to precipitate, is metastable for all values of pH and sulfate activity. These equilibrium calculations predict that both sulfate and aluminum can be immobilized in acid waters by the precipitation of aluminum hydroxysulfate minerals.</p><p>Considerable evidence supports the conclusion that the formation of insoluble aluminum hydroxy-sulfate minerals may be the cause of sulfate retention in soils and sediments, as suggested by Adams and Rawajfih (1977), instead of adsorption.</p>","language":"English","publisher":"Elsevier","doi":"10.1016/0016-7037(82)90168-5","issn":"00167037","usgsCitation":"Nordstrom, D.K., 1982, The effect of sulfate on aluminum concentrations in natural waters: some stability relations in the system Al2O3-SO3-H2O at 298 K: Geochimica et Cosmochimica Acta, v. 46, no. 4, p. 681-692, https://doi.org/10.1016/0016-7037(82)90168-5.","productDescription":"12 p.","startPage":"681","endPage":"692","numberOfPages":"12","costCenters":[{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":221133,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"46","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505bab50e4b08c986b322d6e","contributors":{"authors":[{"text":"Nordstrom, D. Kirk 0000-0003-3283-5136 dkn@usgs.gov","orcid":"https://orcid.org/0000-0003-3283-5136","contributorId":749,"corporation":false,"usgs":true,"family":"Nordstrom","given":"D.","email":"dkn@usgs.gov","middleInitial":"Kirk","affiliations":[{"id":37277,"text":"WMA - Earth System Processes Division","active":true,"usgs":true},{"id":5044,"text":"National Research Program - Central Branch","active":true,"usgs":true}],"preferred":false,"id":362014,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70011496,"text":"70011496 - 1982 - Chemical and light-stable isotope characteristics of waters from the Raft River geothermal area and environs, Cassia County, Idaho; Box Elder County, Utah","interactions":[],"lastModifiedDate":"2024-04-19T18:34:09.022151","indexId":"70011496","displayToPublicDate":"1982-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1828,"text":"Geothermics","active":true,"publicationSubtype":{"id":10}},"title":"Chemical and light-stable isotope characteristics of waters from the Raft River geothermal area and environs, Cassia County, Idaho; Box Elder County, Utah","docAbstract":"<p><span>Chemical and light-stable isotope data are presented for water samples from the Raft River geothermal area and environs. On the basis of chemical character, as defined by a trilinear plot of per cent milliequivalents, and light-stable isotope data, the waters in the geothermal area can be divided into waters that have and have not mixed with cold water. The non-mixed waters have essentially a constant value of light-stable isotopes but show a large variation in chloride content. The variation of chloride composition is not the usual pattern for deep geothermal waters, where it is normally assumed that the deep water has a single chloride composition. Different mixed waters also have hot-water sources of varying chloride composition. Plots of chloride values on cross-sections show that water circulation patterns are confused, with non-mixed waters having different chloride concentrations located in close proximity. Three models can explain the characteristics of the deep geothermal water: (1) in addition to near-surface mixing of cold and hot water, there is deep mixing of two hot waters with the same enthalpy and isotopic composition but differing chloride concentrations to produce the range of chloride concentrations found in the deep geothermal water; (2) there is a single deep hot water, and the range of chloride concentrations is produced by the water passing through a zone of highly soluble materials (most likely in the sedimentary section above the basement) in which waters have different residence times or slightly different circulation paths; (3) the varying chloride concentrations in space have been caused by varying chloride concentrations in the deep feed water through time. Some of this older water has not been flushed from the system by the natural discharge. Although one model may seem more plausible than the others, the available data do not rule out any of them. Data for water samples from the Raft River and Jim Sage Mountains show that water from these areas is probably the source for the cold mixing water determined from end-members on mixing lines. Data for water samples in the Upper Raft River Valley show that the thermal anomaly found at Almo 1 is probably not related to the Raft River geothermal area. The water is different in type as shown by its placement on a trilinear plot, and the isotopes are different enough to show that it is probably a different water. Isotopic compositions of samples from a wide area around the Raft River geothermal system indicate that the likely source of the recharge water is the southern Albion Mountains and western Raft River Mountains. The recharge area is at one end of the Narrows zone, and the geothermal area is along the Narrows zone; thus it is likely that the Narrows zone defines the circulation path.</span></p>","language":"English","publisher":"Elsevier","doi":"10.1016/0375-6505(82)90030-X","issn":"03756505","usgsCitation":"Nathenson, M., Nehring, N., Crosthwaite, E., Harmon, R., Janik, C., and Borthwick, J., 1982, Chemical and light-stable isotope characteristics of waters from the Raft River geothermal area and environs, Cassia County, Idaho; Box Elder County, Utah: Geothermics, v. 11, no. 4, p. 215-237, https://doi.org/10.1016/0375-6505(82)90030-X.","productDescription":"23 p.","startPage":"215","endPage":"237","numberOfPages":"23","costCenters":[],"links":[{"id":221117,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"11","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059f547e4b0c8380cd4c157","contributors":{"authors":[{"text":"Nathenson, M.","contributorId":46632,"corporation":false,"usgs":true,"family":"Nathenson","given":"M.","email":"","affiliations":[],"preferred":false,"id":361260,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Nehring, N.L.","contributorId":21157,"corporation":false,"usgs":true,"family":"Nehring","given":"N.L.","email":"","affiliations":[],"preferred":false,"id":361259,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Crosthwaite, E. G.","contributorId":83098,"corporation":false,"usgs":true,"family":"Crosthwaite","given":"E. G.","affiliations":[],"preferred":false,"id":361262,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Harmon, R.S.","contributorId":6585,"corporation":false,"usgs":true,"family":"Harmon","given":"R.S.","email":"","affiliations":[],"preferred":false,"id":361257,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Janik, C.","contributorId":82458,"corporation":false,"usgs":true,"family":"Janik","given":"C.","affiliations":[],"preferred":false,"id":361261,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Borthwick, J.","contributorId":18905,"corporation":false,"usgs":true,"family":"Borthwick","given":"J.","email":"","affiliations":[],"preferred":false,"id":361258,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}}
,{"id":70011633,"text":"70011633 - 1982 - Modern shallow-water graded sand layers from storm surges, Bering Shelf: a mimic of Bouma sequences and turbidite systems","interactions":[],"lastModifiedDate":"2024-05-21T23:50:16.941879","indexId":"70011633","displayToPublicDate":"1982-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2450,"text":"Journal of Sedimentary Petrology","active":true,"publicationSubtype":{"id":10}},"title":"Modern shallow-water graded sand layers from storm surges, Bering Shelf: a mimic of Bouma sequences and turbidite systems","docAbstract":"<div><div id=\"12458278\" class=\"article-section-wrapper js-article-section js-content-section  \" data-section-parent-id=\"0\"><p>A sequence of graded sand layers, interbedded with mud, extends offshore over 100 km from the Yukon Delta shoreline across the flat, shallow (&lt;20 m depth) epicontinental shelf of the northern Bering Sea, Alaska. Proximal graded sand beds on the delta-front platform near the shoreline are coarser (2-3phi ), thicker (10 to 20 cm), and contain more complete vertical sequences of sedimentary structures than distal beds. The inshore graded vertical sequence of structures from the base to the top of individual sand layers includes plane-parallel lamination (S<span>&nbsp;</span><sub>b</sub><span>&nbsp;</span>), cross lamination (S<span>&nbsp;</span><sub>c</sub><span>&nbsp;</span>), plane-parallel lamination (S<span>&nbsp;</span><sub>d</sub><span>&nbsp;</span>), and mud (S<span>&nbsp;</span><sub>e</sub><span>&nbsp;</span>) analogous to the Bouma T (sub a-e) turbidite sequence. Structures vary between interchannel platform deposits with complete S<span>&nbsp;</span><sub>b</sub><span>&nbsp;</span>-S<span>&nbsp;</span><sub>e</sub><span>&nbsp;</span>sequences and channel-floor sands that are all trough cross-laminated. Distally, storm-sand layers change to thin (1 to 5 cm) silt beds that contain flat and ripple-drift lamination (S (sub c-e,de) ), are commonly bioturbated, and are associated with shell and pebble lags from storm-wave reworking. The sequence of graded sands appears to be related to the major storm surges that occur every several years. The major storms increase the average 10-m water depth in southern Norton Sound as much as 5 m and cause fluctuations in pore pressure from wave cyclic loading that may liquefy the upper 2 to 3 m of sediment. Storm-associated bottom currents, possibly dominated by rapidly waning ebb flow, transport the liquefied inshore sand far offshore (&gt; 100 kin). Such shallow-water graded layers off lobate deltas may be distinguished from similar deep-water turbidites by: 1) the predominance of trough cross-lamination, perhaps resulting from wave oscillation effects, in the proximal part of the system, and 2) gradation to common shallow marine fossils, bioturbation, and storm lag layers in distal areas.</p></div></div>","language":"English","publisher":"SEPM","doi":"10.1306/212F7F9A-2B24-11D7-8648000102C1865D","issn":"00224472","usgsCitation":"Nelson, C., 1982, Modern shallow-water graded sand layers from storm surges, Bering Shelf: a mimic of Bouma sequences and turbidite systems: Journal of Sedimentary Petrology, v. 52, no. 2, p. 537-545, https://doi.org/10.1306/212F7F9A-2B24-11D7-8648000102C1865D.","productDescription":"9 p.","startPage":"537","endPage":"545","numberOfPages":"9","costCenters":[],"links":[{"id":221188,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"52","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a5ca1e4b0c8380cd6fe37","contributors":{"authors":[{"text":"Nelson, C.H.","contributorId":88346,"corporation":false,"usgs":true,"family":"Nelson","given":"C.H.","email":"","affiliations":[],"preferred":false,"id":361582,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70011793,"text":"70011793 - 1982 - Extreme fractionation of  234U 238U and  230Th 234U in spring waters, sediments, and fossils at the Pomme de Terre Valley, southwestern Missouri","interactions":[],"lastModifiedDate":"2024-03-18T14:38:18.446104","indexId":"70011793","displayToPublicDate":"1982-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1759,"text":"Geochimica et Cosmochimica Acta","active":true,"publicationSubtype":{"id":10}},"displayTitle":"Extreme fractionation of  <sup>234</sup>U <sup>238</sup>U and  <sup>230</sup>Th <sup>234</sup>U in spring waters, sediments, and fossils at the Pomme de Terre Valley, southwestern Missouri","title":"Extreme fractionation of  234U 238U and  230Th 234U in spring waters, sediments, and fossils at the Pomme de Terre Valley, southwestern Missouri","docAbstract":"<p><span>Isotopic fractionation as great as 1600% exists between&nbsp;</span><sup>234</sup><span>U and&nbsp;</span><sup>238</sup><span>U in spring waters, sediments, and fossils in the Pomme de Terre Valley, southwestern Missouri. The activity ratios of&nbsp;</span><span class=\"math\"><span id=\"MathJax-Element-3-Frame\" class=\"MathJax_SVG\" data-mathml=\"<math xmlns=&quot;http://www.w3.org/1998/Math/MathML&quot;><msup><mi></mi><mn>234</mn></msup><mtext>U</mtext><msup><mi></mi><mn>238</mn></msup><mtext>U</mtext></math>\"><span class=\"MJX_Assistive_MathML\">234U238U</span></span></span><span>&nbsp;in five springs range from 7.2 to 16 in water which has been discharged for at least the past 30,000 years. The anomalies in&nbsp;</span><span class=\"math\"><span id=\"MathJax-Element-4-Frame\" class=\"MathJax_SVG\" data-mathml=\"<math xmlns=&quot;http://www.w3.org/1998/Math/MathML&quot;><msup><mi></mi><mn>234</mn></msup><mtext>U</mtext><msup><mi></mi><mn>238</mn></msup><mtext>U</mtext></math>\"><span class=\"MJX_Assistive_MathML\">234U238U</span></span></span><span>&nbsp;ratio in deep water have potential usefulness in hydrologic investigations in southern Missouri. Clayey units overlying the spring bog sediments of Trolinger Spring are enriched in&nbsp;</span><sup>230</sup><span>Th relative to their parent&nbsp;</span><sup>234</sup><span>U by as much as 720%. The results indicate that both preferential displacement&nbsp;</span><i>via</i><span>&nbsp;alpha recoil ejection and the preferential emplacement&nbsp;</span><i>via</i><span>&nbsp;recoiling and physical entrapment are significant processes that are occurring in the geologic environment.</span></p>","language":"English","publisher":"Elsevier","doi":"10.1016/0016-7037(82)90323-4","issn":"00167037","usgsCitation":"Szabo, B.J., 1982, Extreme fractionation of  234U 238U and  230Th 234U in spring waters, sediments, and fossils at the Pomme de Terre Valley, southwestern Missouri: Geochimica et Cosmochimica Acta, v. 46, no. 9, p. 1675-1679, https://doi.org/10.1016/0016-7037(82)90323-4.","productDescription":"5 p.","startPage":"1675","endPage":"1679","numberOfPages":"5","costCenters":[],"links":[{"id":220792,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"46","issue":"9","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a0e68e4b0c8380cd5343a","contributors":{"authors":[{"text":"Szabo, Barney J.","contributorId":6848,"corporation":false,"usgs":true,"family":"Szabo","given":"Barney","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":361970,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70011897,"text":"70011897 - 1982 - Leachability of uranium and other elements from freshly erupted volcanic ash","interactions":[{"subject":{"id":11218,"text":"ofr81118 - 1981 - Leachability of uranium and other elements from freshly erupted volcanic ash","indexId":"ofr81118","publicationYear":"1981","noYear":false,"title":"Leachability of uranium and other elements from freshly erupted volcanic ash"},"predicate":"SUPERSEDED_BY","object":{"id":70011897,"text":"70011897 - 1982 - Leachability of uranium and other elements from freshly erupted volcanic ash","indexId":"70011897","publicationYear":"1982","noYear":false,"title":"Leachability of uranium and other elements from freshly erupted volcanic ash"},"id":1}],"lastModifiedDate":"2013-02-12T16:05:41","indexId":"70011897","displayToPublicDate":"1982-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2499,"text":"Journal of Volcanology and Geothermal Research","active":true,"publicationSubtype":{"id":10}},"title":"Leachability of uranium and other elements from freshly erupted volcanic ash","docAbstract":"A study of leaching of freshly erupted basaltic and dacitic air-fall ash and bomb fragment samples, unaffected by rain, shows that glass dissolution is the dominant process by which uranium is initially mobilized from air-fall volcanic ash. Si, Li, and V are also preferentially mobilized by glass dissolution. Gaseous transfer followed by fixation of soluble uranium species on volcanic-ash particles is not an important process affecting uranium mobility. Gaseous transfer, however, may be important in forming water-soluble phases, adsorbed to ash surfaces, enriched in the economically and environmentally important elements Zn, Cu, Cd, Pb, B, F, and Ba. Quick removal of these adsorbed elements by the first exposure of freshly erupted ash to rain and surface water may pose short-term hazards to certain forms of aquatic and terrestrial life. Such rapid release of material may also represent the first step in transportation of economically important elements to environments favorable for precipitation into deposits of commercial interest. Ash samples collected from the active Guatemalan volcanoes Fuego and Pacaya (high-Al basalts) and Santiaguito (hornblende-hypersthene dacite); bomb fragments from Augustine volcano (andesite-dacite), Alaska, and Heimaey (basalt), Vestmann Islands, Iceland; and fragments of \"rhyolitic\" pumice from various historic eruptions were subjected to three successive leaches with a constant water-to-ash weight ratio of 4:1. The volcanic material was successively leached by: (1) distilled-deionized water (pH = 5.0-5.5) at room temperature for 24 h, which removes water-soluble gases and salts adsorbed on ash surfaces during eruption; (2) dilute HCl solution (pH = 3.5-4.0) at room temperature for 24 h, which continues the attack initiated by the water and also attacks acid-soluble sulfides and oxides; (3) a solution 0.05 M in both Na,CO, and NaHCO, (pH = 9.9) at 80&deg;C for one week, which preferentially dissolves volcanic glass. The first two leaches mimic interaction of ash with rain produced in the vicinity of an active eruption. The third leach accelerates the effect of prolonged contact of volcanic ash with alkaline ground water present during ash diagenesis.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Journal of Volcanology and Geothermal Research","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"Elsevier","publisherLocation":"Amsterdam, Netherlands","doi":"10.1016/0377-0273(82)90017-8","issn":"03770273","usgsCitation":"Smith, D.B., Zielinski, R.A., and Rose, W., 1982, Leachability of uranium and other elements from freshly erupted volcanic ash: Journal of Volcanology and Geothermal Research, v. 13, no. 1-2, p. 1-30, https://doi.org/10.1016/0377-0273(82)90017-8.","productDescription":"30 p.","startPage":"1","endPage":"30","costCenters":[],"links":[{"id":221397,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":267294,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1016/0377-0273(82)90017-8"}],"volume":"13","issue":"1-2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a4597e4b0c8380cd6742e","contributors":{"authors":[{"text":"Smith, D. B. davidsmith@usgs.gov","contributorId":12840,"corporation":false,"usgs":true,"family":"Smith","given":"D.","email":"davidsmith@usgs.gov","middleInitial":"B.","affiliations":[],"preferred":false,"id":362239,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Zielinski, R. A. 0000-0002-4047-5129","orcid":"https://orcid.org/0000-0002-4047-5129","contributorId":106930,"corporation":false,"usgs":true,"family":"Zielinski","given":"R.","email":"","middleInitial":"A.","affiliations":[{"id":164,"text":"Central Energy Resources Science Center","active":true,"usgs":true}],"preferred":false,"id":362241,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Rose, W.I. Jr.","contributorId":25275,"corporation":false,"usgs":true,"family":"Rose","given":"W.I.","suffix":"Jr.","email":"","affiliations":[],"preferred":false,"id":362240,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
]}