{"pageNumber":"2145","pageRowStart":"53600","pageSize":"25","recordCount":68909,"records":[{"id":11121,"text":"ofr82363 - 1982 - Water-quality data for the American River basin, California, February-October 1979","interactions":[],"lastModifiedDate":"2023-03-17T21:00:48.271702","indexId":"ofr82363","displayToPublicDate":"1982-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"82-363","title":"Water-quality data for the American River basin, California, February-October 1979","docAbstract":"<p>Data were collected in the American River basin from February to October 1979 for use in assessing the water quality in the basin and developing land-use/water-quality relations. The basin covers 2,163 square miles of the western slope of the central Sierra Nevada. Basin headwaters are located primarily between Donner Summit and Echo Summit. Water-quality data were collected at 14 stream sites and at 3 sites on Folsom Lake and include selected measurements and analyses for physical, chemical, and biological properties and constituents.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr82363","usgsCitation":"Shay, J.M., 1982, Water-quality data for the American River basin, California, February-October 1979: U.S. Geological Survey Open-File Report 82-363, iv, 60 p., https://doi.org/10.3133/ofr82363.","productDescription":"iv, 60 p.","costCenters":[],"links":[{"id":38891,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0363/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":143648,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0363/report-thumb.jpg"},{"id":414365,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_13708.htm","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"California","otherGeospatial":"American River basin","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -119.977,\n              39.31\n            ],\n            [\n              -121.605,\n              39.31\n            ],\n            [\n              -121.605,\n              38.622\n            ],\n            [\n              -119.977,\n              38.622\n            ],\n            [\n              -119.977,\n              39.31\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e3e4b07f02db5e58fd","contributors":{"authors":[{"text":"Shay, J. M.","contributorId":98321,"corporation":false,"usgs":true,"family":"Shay","given":"J.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":162581,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70011814,"text":"70011814 - 1982 - Identification of the Holocene-Pleistocene boundary in the Bering Sea by diatoms.","interactions":[],"lastModifiedDate":"2012-03-12T17:18:27","indexId":"70011814","displayToPublicDate":"1982-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1068,"text":"Boreas","active":true,"publicationSubtype":{"id":10}},"title":"Identification of the Holocene-Pleistocene boundary in the Bering Sea by diatoms.","docAbstract":"The modern diatom flora from surface sediment of the Navarin Basin region of the Bering Sea is dominated by Denticulopsis seminae and Nitzschia oceanica. D. seminae, a north boreal species, is most abundant in the deeper waters of the slope-basin regions, whereas N. oceanica, an Arctic species associated with ice cover, dominates the shallow shelf water. Downcore studies show that these species alternate in dominance within the late Quaternary sediments suggest climatic fluctuations.-from Author","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Boreas","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","issn":"03009483","usgsCitation":"Baldauf, J., 1982, Identification of the Holocene-Pleistocene boundary in the Bering Sea by diatoms.: Boreas, v. 11, no. 1, p. 113-118.","startPage":"113","endPage":"118","numberOfPages":"6","costCenters":[],"links":[{"id":221199,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"11","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a383fe4b0c8380cd614cd","contributors":{"authors":[{"text":"Baldauf, J.G.","contributorId":67655,"corporation":false,"usgs":true,"family":"Baldauf","given":"J.G.","email":"","affiliations":[],"preferred":false,"id":362017,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70011859,"text":"70011859 - 1982 - Composition of estuarine colloidal material: Organic components","interactions":[],"lastModifiedDate":"2024-03-18T14:28:53.733867","indexId":"70011859","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":"Composition of estuarine colloidal material: Organic components","docAbstract":"<p><span>Colloidal material in the size range 1.2 nm to 0.4 μm was isolated by ultrafiltration from Chesapeake Bay and Patuxent River waters (U.S.A.). Temperature controlled, stepwise pyrolysis of the freeze-dried material, followed by gas chromatographic-mass spectrometric analyses of the volatile products indicates that the primary organic components of this polymer are carbohydrates and peptides. The major pyrolysis products at the 450°C step are acetic acid, furaldehydes, furoic acid, furanmethanol, diones and lactones characteristic of carbohydrate thermal decomposition. Pyrroles, pyridines, amides and indole (protein derivatives) become more prevalent and dominate the product yield at the 600°C pyrolysis step. Olefins and saturated hydrocarbons, originating from fatty acids, are present only in minor amounts. These results are consistent with the composition of Chesapeake phytoplankton (approximately 50% protein, 30% carbohydrate, 10% lipid and 10% nucleotides by dry weight). The pyrolysis of a cultured phytoplankton and natural particulate samples produced similar oxygen and nitrogencontaining compounds, although the proportions of some components differ relative to the colloidal fraction. There were no lignin derivatives indicative of terrestrial plant detritus in any of these samples. The data suggest that aquatic microorganisms, rather than terrestrial plants, are the dominant source of colloidal organic material in these river and estuarine surface waters.</span></p>","language":"English","publisher":"Elsevier","doi":"10.1016/0016-7037(82)90318-0","issn":"00167037","usgsCitation":"Sigleo, A., Hoering, T., and Helz, G., 1982, Composition of estuarine colloidal material: Organic components: Geochimica et Cosmochimica Acta, v. 46, no. 9, p. 1619-1626, https://doi.org/10.1016/0016-7037(82)90318-0.","productDescription":"8 p.","startPage":"1619","endPage":"1626","numberOfPages":"8","costCenters":[],"links":[{"id":220795,"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":"5059f928e4b0c8380cd4d47e","contributors":{"authors":[{"text":"Sigleo, A.C.","contributorId":20899,"corporation":false,"usgs":true,"family":"Sigleo","given":"A.C.","email":"","affiliations":[],"preferred":false,"id":362136,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hoering, T.C.","contributorId":101011,"corporation":false,"usgs":true,"family":"Hoering","given":"T.C.","email":"","affiliations":[],"preferred":false,"id":362138,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Helz, G.R.","contributorId":96823,"corporation":false,"usgs":true,"family":"Helz","given":"G.R.","email":"","affiliations":[],"preferred":false,"id":362137,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70011479,"text":"70011479 - 1982 - Determination of polar organic solutes in oil-shale retort water","interactions":[],"lastModifiedDate":"2023-10-19T18:10:52.882211","indexId":"70011479","displayToPublicDate":"1982-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1565,"text":"Environmental Science & Technology","onlineIssn":"1520-5851","printIssn":"0013-936X","active":true,"publicationSubtype":{"id":10}},"title":"Determination of polar organic solutes in oil-shale retort water","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"American Chemical Society","doi":"10.1021/es00104a015","issn":"0013936X","usgsCitation":"Leenheer, J., Noyes, T., and Stuber, H.A., 1982, Determination of polar organic solutes in oil-shale retort water: Environmental Science & Technology, v. 16, no. 10, p. 714-723, https://doi.org/10.1021/es00104a015.","productDescription":"10 p.","startPage":"714","endPage":"723","costCenters":[],"links":[{"id":220838,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Colorado","otherGeospatial":"Logan Wash","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -108.19497121932936,\n              39.40042581478241\n            ],\n            [\n              -108.18042492246276,\n              39.40084212255246\n            ],\n            [\n              -108.17584553270868,\n              39.40354806249445\n            ],\n            [\n              -108.17422927750103,\n              39.40667017043799\n            ],\n            [\n              -108.16507049799233,\n              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J.A.","contributorId":75123,"corporation":false,"usgs":true,"family":"Leenheer","given":"J.A.","affiliations":[],"preferred":false,"id":361210,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Noyes, T.I.","contributorId":54971,"corporation":false,"usgs":true,"family":"Noyes","given":"T.I.","email":"","affiliations":[],"preferred":false,"id":361209,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Stuber, H. A.","contributorId":52721,"corporation":false,"usgs":true,"family":"Stuber","given":"H.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":361208,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70011810,"text":"70011810 - 1982 - Holocene sedimentation in the shallow nearshore zone off Nauset Inlet, Cape Cod, Massachusetts","interactions":[],"lastModifiedDate":"2017-09-06T10:27:51","indexId":"70011810","displayToPublicDate":"1982-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2667,"text":"Marine Geology","active":true,"publicationSubtype":{"id":10}},"title":"Holocene sedimentation in the shallow nearshore zone off Nauset Inlet, Cape Cod, Massachusetts","docAbstract":"<p>Present conditions and sedimentary evolution of the shallow offshore region near Nauset Inlet on Cape Cod, Massachusetts were clarified using high-resolution seismic-reflection profiles, sidescan-sonar records, surface grab samples and current meter measurements. The study area contains three provinces: (1) a nearshore province (shallower than 18 m) with a relatively steep slope (0.6°) and a cover of medium sand; (2) a northern offshore province covered with coarse sand, gravel, and boulders, interpreted to be glacial drift; and (3) a southern offshore province with a gentle seaward-dipping slope (0.3°) and a surface sediment of coarse sand. The glacial drift exposed in the northern offshore province can be traced southward under the coarse sand province. The overlying fill is comprised of either outwash sediment derived from the Pleistocene South Channel ice lobe to the east or Holocene-aged marine sediments eroded from seacliffs to the north. Latest Holocene sediment appears to be limited to the zone shoreward of 18 m where the medium sand occurs.</p><p>Near-bottom mean flows (measured over two winter months in 10 m water depth) average 6 cm sec<sup>−1</sup><span>&nbsp;</span>to the south. Mean flows exceeded 20 cm sec<sup>−1</sup>approx. 23% of the time. Ninety percent of the flows exceeding 20 cm sec<sup>−1</sup>were directed to the south, reflecting the dominant atmospheric forcing during these winter months. Waves had an average variance of 650 cm<sup>2</sup><span>&nbsp;</span>with variance exceeding 5000 cm<sup>2</sup>, 3% of the time, indicating moderate wave activity.</p><p>Present processes are actively reshaping the nearshore province, which is characterized by many east to northeast-trending shore-oblique channels that do not extend seaward of the 18-m contour. Coarse sand in the floors of these channels suggests they may be erosional features, and the presence of megaripples oriented perpendicular to the channel axes indicates active transport in these channels. Megaripple orientation and the current and wave regime of the study area support a rip-current origin for these channels.</p>","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Marine Geology","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1016/0025-3227(82)90071-8","issn":"00253227","usgsCitation":"Aubrey, D., Twichell, D., and Pfirman, S., 1982, Holocene sedimentation in the shallow nearshore zone off Nauset Inlet, Cape Cod, Massachusetts: Marine Geology, v. 47, no. 3-4, p. 243-259, https://doi.org/10.1016/0025-3227(82)90071-8.","productDescription":"17 p.","startPage":"243","endPage":"259","costCenters":[{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"links":[{"id":221131,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Massachussetts","otherGeospatial":"Cape Cod, Nauset Inlet","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -70.68878173828125,\n              41.693424216151314\n            ],\n            [\n              -69.9224853515625,\n              41.693424216151314\n            ],\n            [\n              -69.9224853515625,\n              42.10229818948117\n            ],\n            [\n              -70.68878173828125,\n              42.10229818948117\n            ],\n            [\n              -70.68878173828125,\n              41.693424216151314\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"47","issue":"3-4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a31f4e4b0c8380cd5e3b3","contributors":{"authors":[{"text":"Aubrey, D.G.","contributorId":73336,"corporation":false,"usgs":true,"family":"Aubrey","given":"D.G.","email":"","affiliations":[],"preferred":false,"id":362010,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Twichell, D.C.","contributorId":84304,"corporation":false,"usgs":true,"family":"Twichell","given":"D.C.","affiliations":[],"preferred":false,"id":362011,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Pfirman, S.L.","contributorId":40281,"corporation":false,"usgs":true,"family":"Pfirman","given":"S.L.","affiliations":[],"preferred":false,"id":362009,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":38602,"text":"pp1217 - 1982 - Simulated effects of ground-water development on the potentiometric surface of the Floridan aquifer, west-central Florida","interactions":[{"subject":{"id":11698,"text":"ofr791271 - 1980 - Simulated effects of ground-water development on potentiometric surface of the Floridan Aquifer, west-central Florida","indexId":"ofr791271","publicationYear":"1980","noYear":false,"title":"Simulated effects of ground-water development on potentiometric surface of the Floridan Aquifer, west-central Florida"},"predicate":"SUPERSEDED_BY","object":{"id":38602,"text":"pp1217 - 1982 - Simulated effects of ground-water development on the potentiometric surface of the Floridan aquifer, west-central Florida","indexId":"pp1217","publicationYear":"1982","noYear":false,"title":"Simulated effects of ground-water development on the potentiometric surface of the Floridan aquifer, west-central Florida"},"id":1}],"lastModifiedDate":"2023-09-01T21:28:18.640478","indexId":"pp1217","displayToPublicDate":"1982-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":331,"text":"Professional Paper","code":"PP","onlineIssn":"2330-7102","printIssn":"1044-9612","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"1217","title":"Simulated effects of ground-water development on the potentiometric surface of the Floridan aquifer, west-central Florida","docAbstract":"A digital model of two-dimensional ground-water flow was used to predict changes in the potentiometric surface of the Floridan aquifer, 1976 to 2000, in a 5,938-square-mile area of west-central Florida. In 1975, ground water withdrawn from the Floridan aquifer for irrigation, phosphate mines, other industries, and municipal supplies averaged about 649 million gallons per day. Rates are projected to increase to about 840 million gallons per day by 2000. The model was calibrated under steady-state and transient conditions. Input parameters included transmissivity and storage coefficient of the Floridan aquifer; thickness, vertical hydraulic conductivity, and storage coefficient of the upper confining bed; altitudes of the water table and potentiometric surface; and ground-water withdrawals. Simulation of May 1976 to May 2000, using projected combined pumping rates for municipal supplies, irrigation, and industry (including existing and proposed phosphate mines), resulted in a rise in the potentiometric surface of about 10 feet in Polk County, and a decline of about 35 feet in parts of Manatee and Hardee Counties. The lowest predicted potentiometric level was about 30 feet below sea level. Predicted declines for November 1976 to October 2000 were generally 5 to 10 feet less than those for May 1976 to May 2000. (USGS)","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/pp1217","usgsCitation":"Wilson, W., and Gerhart, J.M., 1982, Simulated effects of ground-water development on the potentiometric surface of the Floridan aquifer, west-central Florida: U.S. Geological Survey Professional Paper 1217, Report: v, 83 p.; 2 Plates: 20.00 x 19.50 inches, https://doi.org/10.3133/pp1217.","productDescription":"Report: v, 83 p.; 2 Plates: 20.00 x 19.50 inches","costCenters":[],"links":[{"id":104573,"rank":5,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_4755.htm","linkFileType":{"id":5,"text":"html"},"description":"4755"},{"id":65417,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/1217/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":65419,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/1217/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":65418,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/1217/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":124267,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/1217/report-thumb.jpg"}],"country":"United States","state":"Florida","otherGeospatial":"Floridan aquifer","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -81.2817,\n              28.3244\n            ],\n            [\n              -81.4344,\n              28.3244\n            ],\n            [\n              -81.4344,\n              26.5183\n            ],\n            [\n              -81.2817,\n              26.5183\n            ],\n            [\n              -81.2817,\n              28.3244\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f9e4b07f02db5f36ac","contributors":{"authors":[{"text":"Wilson, W.E.","contributorId":100831,"corporation":false,"usgs":true,"family":"Wilson","given":"W.E.","email":"","affiliations":[],"preferred":false,"id":220147,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Gerhart, J. M.","contributorId":12855,"corporation":false,"usgs":true,"family":"Gerhart","given":"J.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":220146,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"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}]}}
,{"id":70011694,"text":"70011694 - 1982 - Siderite concretions: indicators of early diagenesis in the Gammon shale (Cretaceous).","interactions":[],"lastModifiedDate":"2012-03-12T17:18:27","indexId":"70011694","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":"Siderite concretions: indicators of early diagenesis in the Gammon shale (Cretaceous).","docAbstract":"The Gammon member of the Pierre shale of the northern Great Plains, USA, contains abundant siderite concretions. The relative depth and time of siderite precipitation can be inferred from the structure, mineralogy and isotopic composition of these concretions. Concretions that formed at shallow depths, early in the history of the sediment, contain a high percentage (75-85%) of carbonate, preserve uncompacted structures and have oxygen isotopic ratios similar to that of sea-water. In contrast, concretions that formed later and/or at greater depths have lower carbonate content and lower 18O/16O ratios. Concretions in rapidly deposited sediments formed at shallow depths (<10 m), and those in sediments that accumulated slowly formed at greater depths. These differences agree with the fossil evidence. Siderite did not form until nearly all the dissolved sulphur had been reduced and precipitated as pyrite; the excess organic matter produced methane at about the same time.-H.R.B.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Journal of Sedimentary Petrology","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","issn":"00224472","usgsCitation":"Gautier, D.L., 1982, Siderite concretions: indicators of early diagenesis in the Gammon shale (Cretaceous).: Journal of Sedimentary Petrology, v. 52, no. 3, p. 859-871.","startPage":"859","endPage":"871","numberOfPages":"13","costCenters":[],"links":[{"id":221127,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"52","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505b8ef2e4b08c986b318c3e","contributors":{"authors":[{"text":"Gautier, D. L.","contributorId":69996,"corporation":false,"usgs":true,"family":"Gautier","given":"D.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":361729,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70011824,"text":"70011824 - 1982 - Geochemistry of highly basic calcium hydroxide groundwater in Jordan","interactions":[],"lastModifiedDate":"2019-12-16T06:43:26","indexId":"70011824","displayToPublicDate":"1982-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1213,"text":"Chemical Geology","active":true,"publicationSubtype":{"id":10}},"title":"Geochemistry of highly basic calcium hydroxide groundwater in Jordan","docAbstract":"<div id=\"abstracts\" class=\"Abstracts u-font-serif\"><div id=\"aep-abstract-id6\" class=\"abstract author\"><div id=\"aep-abstract-sec-id7\"><p id=\"simple-para.0010\">Highly-alkaline (pH &gt; 12.5) meteoric waters of a Ca<sup>2+</sup>OH<sup>−</sup>-type issue from naturally calcined bituminous marl. The cold (16.5 ≤<span>&nbsp;</span><i>T</i>(°C) ≤ 19.1) waters are super-saturated with minerals thought to be of high-temperature origin.</p></div></div></div>","language":"English","publisher":"Elsevier","doi":"10.1016/0009-2541(82)90024-9","issn":"00092541","usgsCitation":"Barnes, I., Presser, T.S., Saines, M., Dickson, P., and Van Groos, A.F., 1982, Geochemistry of highly basic calcium hydroxide groundwater in Jordan: Chemical Geology, v. 35, no. 1-2, p. 147-154, https://doi.org/10.1016/0009-2541(82)90024-9.","productDescription":"8 p. ","startPage":"147","endPage":"154","numberOfPages":"8","costCenters":[],"links":[{"id":221316,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":266118,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1016/0009-2541(82)90024-9"}],"country":"Jordan ","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"Polygon\",\"coordinates\":[[[35.54567,32.39399],[35.71992,32.70919],[36.83406,32.31294],[38.79234,33.37869],[39.19547,32.16101],[39.00489,32.01022],[37.00217,31.50841],[37.99885,30.5085],[37.66812,30.33867],[37.50358,30.00378],[36.74053,29.86528],[36.50121,29.50525],[36.06894,29.19749],[34.95604,29.35655],[34.9226,29.50133],[35.42092,31.10007],[35.39756,31.48909],[35.54525,31.7825],[35.54567,32.39399]]]},\"properties\":{\"name\":\"Jordan\"}}]}","volume":"35","issue":"1-2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a16fce4b0c8380cd5533d","contributors":{"authors":[{"text":"Barnes, I.","contributorId":23678,"corporation":false,"usgs":true,"family":"Barnes","given":"I.","affiliations":[],"preferred":false,"id":362041,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Presser, T. S.","contributorId":93875,"corporation":false,"usgs":true,"family":"Presser","given":"T.","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":362044,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Saines, M.","contributorId":96827,"corporation":false,"usgs":true,"family":"Saines","given":"M.","email":"","affiliations":[],"preferred":false,"id":362045,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Dickson, P.","contributorId":75272,"corporation":false,"usgs":true,"family":"Dickson","given":"P.","email":"","affiliations":[],"preferred":false,"id":362043,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Van Groos, A. F. K.","contributorId":45457,"corporation":false,"usgs":true,"family":"Van Groos","given":"A.","email":"","middleInitial":"F. K.","affiliations":[],"preferred":false,"id":362042,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":70011792,"text":"70011792 - 1982 - The solubility of quartz in aqueous sodium chloride solution at 350°C and 180 to 500 bars","interactions":[],"lastModifiedDate":"2015-06-05T14:13:41","indexId":"70011792","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 solubility of quartz in aqueous sodium chloride solution at 350°C and 180 to 500 bars","docAbstract":"<p><span>The solubility of quartz in 2, 3, and 4 molal NaCl was measured at 350&deg;C and pressures ranging from 180 to 500 bars. The molal solubility in each of the salt solutions is greater than that in pure water throughout the measured pressure range, with the ratio of solubility in NaCl solution to solubility in pure water decreasing as pressure is increased. The measured solubilities are significantly higher than solubilities calculated using a simple model in which the water activity in NaCl solutions decreases either in proportion to decreasing vapor pressure of the solution as salinity is increased or in proportion to decreasing mole fraction of water in the solvent.</span></p>","language":"English","publisher":"Elsevier","doi":"10.1016/0016-7037(82)90136-3","issn":"00167037","usgsCitation":"Fournier, R.O., Rosenbauer, R.J., and Bischoff, J.L., 1982, The solubility of quartz in aqueous sodium chloride solution at 350°C and 180 to 500 bars: Geochimica et Cosmochimica Acta, v. 46, no. 10, p. 1975-1978, https://doi.org/10.1016/0016-7037(82)90136-3.","productDescription":"4 p.","startPage":"1975","endPage":"1978","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":220791,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"46","issue":"10","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505bb042e4b08c986b324d3a","contributors":{"authors":[{"text":"Fournier, Robert O.","contributorId":73202,"corporation":false,"usgs":true,"family":"Fournier","given":"Robert","email":"","middleInitial":"O.","affiliations":[],"preferred":false,"id":361969,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Rosenbauer, Robert J. brosenbauer@usgs.gov","contributorId":204,"corporation":false,"usgs":true,"family":"Rosenbauer","given":"Robert","email":"brosenbauer@usgs.gov","middleInitial":"J.","affiliations":[{"id":520,"text":"Pacific Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":true,"id":361968,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Bischoff, James L. jbischoff@usgs.gov","contributorId":1389,"corporation":false,"usgs":true,"family":"Bischoff","given":"James","email":"jbischoff@usgs.gov","middleInitial":"L.","affiliations":[],"preferred":true,"id":361967,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70010416,"text":"70010416 - 1982 - Gamma-emitting radionuclide measurements at the US geological survey national water quality laboratory, Denver, Colorado","interactions":[],"lastModifiedDate":"2012-03-12T17:18:17","indexId":"70010416","displayToPublicDate":"1982-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2906,"text":"Nuclear Instruments and Methods","active":true,"publicationSubtype":{"id":10}},"title":"Gamma-emitting radionuclide measurements at the US geological survey national water quality laboratory, Denver, Colorado","docAbstract":"Like sediment samples from Scofield Resevior in Utah were analyzed for 210Pb by the gamma-ray spectrometric method. The top 10 cm of surface sediment yielded excess 210Pb activity (excluding in situ 226Ra supported 210Pb) of 1.05 pCi/g dry weight and decreased to 0.25 pCi/g at a depth of 25 cm. Based on these data, sedimentation rate was approximately 0.49 cm/y for a total of 30 cm of lake sediment and a lake history of approximately 60 y. An alternative method of 210Pb measurements using wet chemical procedures followed by beta counting gave equivalent results. ?? 1982.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Nuclear Instruments and Methods","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","issn":"0029554X","usgsCitation":"In, C.Y., and Ambats, E., 1982, Gamma-emitting radionuclide measurements at the US geological survey national water quality laboratory, Denver, Colorado: Nuclear Instruments and Methods, v. 193, no. 1-2, p. 197-201.","startPage":"197","endPage":"201","numberOfPages":"5","costCenters":[],"links":[{"id":219374,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"193","issue":"1-2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a14b2e4b0c8380cd54b04","contributors":{"authors":[{"text":"In, Che Yang","contributorId":39934,"corporation":false,"usgs":true,"family":"In","given":"Che","email":"","middleInitial":"Yang","affiliations":[],"preferred":false,"id":358869,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Ambats, E.","contributorId":23270,"corporation":false,"usgs":true,"family":"Ambats","given":"E.","email":"","affiliations":[],"preferred":false,"id":358868,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70011788,"text":"70011788 - 1982 - The oxygen isotope composition of granitoid and sedimentary rocks of the southern Snake Range, Nevada","interactions":[],"lastModifiedDate":"2012-03-12T17:18:32","indexId":"70011788","displayToPublicDate":"1982-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1336,"text":"Contributions to Mineralogy and Petrology","active":true,"publicationSubtype":{"id":10}},"title":"The oxygen isotope composition of granitoid and sedimentary rocks of the southern Snake Range, Nevada","docAbstract":"Six diverse intrusive igneous types are exposed as discrete outcrops within an area of 900 km2 in the southern Snake Range, White Pine County, Nevada. The previously recognized variety among these igneous types is reflected in the wide range of ??18O values (-1.1 to 13.4 permil) found in these rocks. This range of ??18O values probably results from differences in source material and post-crystallization history of the different intrusive types. The Jurassic intrusive of the Snake Creek-Williams Canyon area represents the chemical equivalent of a large part of a differentiation sequence, with the entire range of composition (63-76 percent SiO2) exposed over a horizontal distance of about five km. The rather regular increase of ??18O values from the most mafic to the most felsic parts of this pluton, together with ??18O values determined for constituent minerals recovered from five of the samples, supports a fractional crystallization model. The high ??18O values found (10.2-12.2 permil) indicate that the magma likely was derived from or assimilated sedimentary materials. Nine samples of the Cretaceous two-mica granite of the Pole Canyon-Can Young Canyon area have ??18O values in the range 10.6-12.1 permil. These high ??18O values, an initial87Sr/86Sr ratio of 0.7165, and the presence of muscovite along with an accessory mineral suite limited to monazite, apatite, zircon, and an allanite-like mineral, characterize this intrusive mass as an S-type granite. It probably formed through anatexis of late Precambrian pelitic rocks. The granitoid rock exposed in the Young Canyon-Kious Basin area is Tertiary (32 m.y.). Most of this intrusive has been cataclastically deformed as a result of late (18 m.y.) movement on the overlying Snake Range decollement. The undeformed portion of this intrusive has ??18O values of 8.7-10.0 permil. However, the deformed portion of this intrusive has ??18O values as low as -1.1 permil, apparently resulting from isotopic exchange between this rock and ground water at the time of cataclasis. Although the igneous types exposed in the southern Snake Range differ petrologically and range in age from Jurassic to Tertiary, most have relatively high ??18O values compared with other granitoid rocks of the Basin-Range Province. ?? 1982 Springer-Verlag.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Contributions to Mineralogy and Petrology","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisherLocation":"Springer-Verlag","doi":"10.1007/BF01132884","issn":"00107999","usgsCitation":"Lee, D.E., Friedman, I., and Gleason, J., 1982, The oxygen isotope composition of granitoid and sedimentary rocks of the southern Snake Range, Nevada: Contributions to Mineralogy and Petrology, v. 79, no. 2, p. 150-158, https://doi.org/10.1007/BF01132884.","startPage":"150","endPage":"158","numberOfPages":"9","costCenters":[],"links":[{"id":205059,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1007/BF01132884"},{"id":220721,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"79","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505bae78e4b08c986b324104","contributors":{"authors":[{"text":"Lee, D. E.","contributorId":96705,"corporation":false,"usgs":true,"family":"Lee","given":"D.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":361962,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Friedman, I.","contributorId":95596,"corporation":false,"usgs":true,"family":"Friedman","given":"I.","email":"","affiliations":[],"preferred":false,"id":361961,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Gleason, J.D.","contributorId":27072,"corporation":false,"usgs":true,"family":"Gleason","given":"J.D.","email":"","affiliations":[],"preferred":false,"id":361960,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70011243,"text":"70011243 - 1982 - An analysis of input errors in precipitation-runoff models using regression with errors in the independent variables","interactions":[],"lastModifiedDate":"2018-02-05T12:39:08","indexId":"70011243","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":"An analysis of input errors in precipitation-runoff models using regression with errors in the independent variables","docAbstract":"<p><span>Errors in runoff prediction caused by input data errors are analyzed by treating precipitation-runoff models as regression (conditional expectation) models. Independent variables of the regression consist of precipitation and other input measurements; the dependent variable is runoff. In models using erroneous input data, prediction errors are inflated and estimates of expected storm runoff for given observed input variables are biased. This bias in expected runoff estimation results in biased parameter estimates if these parameter estimates are obtained by a least squares fit of predicted to observed runoff values. The problems of error inflation and bias are examined in detail for a simple linear regression of runoff on rainfall and for a nonlinear U.S. Geological Survey precipitation-runoff model. Some implications for flood frequency analysis are considered. A case study using a set of data from Turtle Creek near Dallas, Texas illustrates the problems of model input errors.</span></p>","language":"English","publisher":"American Geophysical Union","doi":"10.1029/WR018i004p00947","usgsCitation":"Troutman, B.M., 1982, An analysis of input errors in precipitation-runoff models using regression with errors in the independent variables: Water Resources Research, v. 18, no. 4, p. 947-964, https://doi.org/10.1029/WR018i004p00947.","productDescription":"18 p.","startPage":"947","endPage":"964","costCenters":[],"links":[{"id":221434,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Texas","city":"Dallas","otherGeospatial":"Turtle Creek","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -96.81529998779297,\n              32.79275826977453\n            ],\n            [\n              -96.78749084472655,\n              32.79275826977453\n            ],\n            [\n              -96.78749084472655,\n              32.85132662142229\n            ],\n            [\n              -96.81529998779297,\n              32.85132662142229\n            ],\n            [\n              -96.81529998779297,\n              32.79275826977453\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"18","issue":"4","noUsgsAuthors":false,"publicationDate":"2010-07-09","publicationStatus":"PW","scienceBaseUri":"5059e9f0e4b0c8380cd4853d","contributors":{"authors":[{"text":"Troutman, Brent M.","contributorId":195329,"corporation":false,"usgs":false,"family":"Troutman","given":"Brent","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":360648,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":1014037,"text":"1014037 - 1982 - Survival of duck plaque virus in water from Lake Andes National Wildlife Refuge, South Dakota","interactions":[],"lastModifiedDate":"2024-07-23T00:00:45.52039","indexId":"1014037","displayToPublicDate":"1982-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2507,"text":"Journal of Wildlife Diseases","active":true,"publicationSubtype":{"id":10}},"title":"Survival of duck plaque virus in water from Lake Andes National Wildlife Refuge, South Dakota","docAbstract":"<div id=\"9831238\" class=\"article-section-wrapper js-article-section js-content-section  \" data-section-parent-id=\"0\"><p>An isolant of duck plague herpesvirus from the Lake Andes Refuge outbreak was seeded in raw and filter-decontaminated water from two locations on the refuge, held at 4 C, and assayed for infectivity intermittently over a period of 2 mo. From an initial level of about 10<sup>5</sup><span>&nbsp;</span>PFU per ml, infectivity in the filtered samples uniformly dropped to about 10<sup>4</sup><span>&nbsp;</span>PFU per ml. Infectivity in the raw samples declined much more rapidly; infectious virus remaining at the end of 2 mo (ca. 10<sup>1</sup><span>&nbsp;</span>PFU per ml) was only about 0.01% of that originally seeded.</p></div>","language":"English","publisher":"Wildlife Disease Association","doi":"10.7589/0090-3558-18.4.437","usgsCitation":"Wolf, K., and Burke, C., 1982, Survival of duck plaque virus in water from Lake Andes National Wildlife Refuge, South Dakota: Journal of Wildlife Diseases, v. 18, no. 4, p. 437-440, https://doi.org/10.7589/0090-3558-18.4.437.","productDescription":"4 p.","startPage":"437","endPage":"440","numberOfPages":"4","costCenters":[{"id":365,"text":"Leetown Science Center","active":true,"usgs":true}],"links":[{"id":480259,"rank":2,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.7589/0090-3558-18.4.437","text":"Publisher Index Page"},{"id":129491,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"18","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae0e4b07f02db688185","contributors":{"authors":[{"text":"Wolf, K.","contributorId":16344,"corporation":false,"usgs":true,"family":"Wolf","given":"K.","email":"","affiliations":[],"preferred":false,"id":319660,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Burke, C.N.","contributorId":96213,"corporation":false,"usgs":true,"family":"Burke","given":"C.N.","email":"","affiliations":[],"preferred":false,"id":319661,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"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":70011764,"text":"70011764 - 1982 - Geochemical indices of fine sediment transport, northwest Gulf of Mexico","interactions":[],"lastModifiedDate":"2024-05-21T23:46:01.539707","indexId":"70011764","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":"Geochemical indices of fine sediment transport, northwest Gulf of Mexico","docAbstract":"<div><div id=\"12458437\" class=\"article-section-wrapper js-article-section js-content-section  \" data-section-parent-id=\"0\"><p>The<span>&nbsp;</span><sup>210</sup><span>&nbsp;</span>Pb distribution, the clay mineralogy distribution, and the distribution of three trace metals, barium, lead, and manganese, in the sediments of the south Texas shelf are related to the dynamics of the sedimentary transport process.<span>&nbsp;</span><sup>210</sup><span>&nbsp;</span>Pb, whose concentration is time dependent, defines three loci of recent sediment accumulations. In addition, the variation of<span>&nbsp;</span><sup>210</sup><span>&nbsp;</span>Pb activity at the sediment-water interface delineates areas of terrestrial sedimentation from hemipelagic sedimentation. The clay mineralogy composition of the bottom and suspended sediments assists in defining the origin of the persistent nepheloid layer and bottom sediment. Barium, a major element used in drilling mud, tags sediment movement from areas of hydrocarbon exploration. Lead concentrations, anthropogenically introduced from urban areas, tag the sediment derived from the metropolitan complexes of coastal Texas. Manganese, because of diagenic mobilization, is concentrated in areas of very slow sediment accumulation. The distribution of these geochemical properties of the sediment are in direct response to the sediment regime of the shelf. Based on this data, a model of sediment transport and deposition which relates currents, wind, tides, sediment flux, and precipitation has been formulated. This model differs from the \"advective\" transport or convergent current schemes previously proposed for this shelf.</p></div></div>","language":"English","publisher":"SEPM","doi":"10.1306/212F7F3B-2B24-11D7-8648000102C1865D","issn":"00224472","usgsCitation":"Holmes, C.W., 1982, Geochemical indices of fine sediment transport, northwest Gulf of Mexico: Journal of Sedimentary Petrology, v. 52, no. 1, p. 307-321, https://doi.org/10.1306/212F7F3B-2B24-11D7-8648000102C1865D.","productDescription":"15 p.","startPage":"307","endPage":"321","numberOfPages":"15","costCenters":[],"links":[{"id":221390,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"52","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a1644e4b0c8380cd550f5","contributors":{"authors":[{"text":"Holmes, C. W.","contributorId":36076,"corporation":false,"usgs":true,"family":"Holmes","given":"C.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":361908,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70011861,"text":"70011861 - 1982 - Benthic phosphorus regeneration in the Potomac River Estuary","interactions":[],"lastModifiedDate":"2012-03-12T17:18:33","indexId":"70011861","displayToPublicDate":"1982-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1919,"text":"Hydrobiologia","onlineIssn":"1573-5117","printIssn":"0018-8158","active":true,"publicationSubtype":{"id":10}},"title":"Benthic phosphorus regeneration in the Potomac River Estuary","docAbstract":"The flux of dissolved reactive phosphate from Potomac riverine and estuarine sediments is controlled by processes occurring at the water-sediment interface and within surficial sediment. In situ benthic fluxes (0.1 to 2.0 mmoles m-2 day-1) are generally five to ten times higher than calculated diffusive fluxes (0.020 to 0.30 mmoles m-2 day-1). The discrepancy between the two flux estimates is greatest in the transition zone (river mile 50 to 70) and is attributd to macrofaunal irrigation. Both in situ and diffusive fluxes of dissolved reactive phosphate from Potomac tidal river sediments are low while those from anoxic lower estuarine sediments are high. The net accumulation rate of phosphorus in benthic sediment exhibits an inverse pattern. Thus a large fraction of phosphorus is retained by Potomac tidal river sediments, which contain a surficial oxidized layer and oligochaete worms tolerant of low oxygen conditions, and a large fraction of phosphorus is released from anoxic lower estuary sediments. Tidal river sediment pore waters are in equilibrium with amorphous Fe (OH)3 while lower estuary pore waters are significantly undersaturated with respect to this phase. Benthic regeneration of dissolved reactive phosphorus is sufficient to supply all the phosphorus requirements for net primary production in the lower tidal river and transition-zone waters of the Potomac River Estuary. Benthic regeneration supplies approximately 25% as much phosphorus as inputs from sewage treatment plants and 10% of all phosphorus inputs to the tidal Potomac River. When all available point source phosphorus data are put into a steady-state conservation of mass model and reasonable coefficients for uptake of dissolved phosphorus, remineralization of particulate phosphorus, and sedimentation of particulate phosphorus are used in the model, a reasonably accurate simulation of dissolved and particulate phosphorus in the water column is obtained for the summer of 1980. ?? 1982 Dr W. Junk Publishers.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Hydrobiologia","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisherLocation":"Kluwer Academic Publishers","doi":"10.1007/BF00000042","issn":"00188158","usgsCitation":"Callender, E., 1982, Benthic phosphorus regeneration in the Potomac River Estuary: Hydrobiologia, v. 91-92, no. 0, p. 431-446, https://doi.org/10.1007/BF00000042.","startPage":"431","endPage":"446","numberOfPages":"16","costCenters":[],"links":[{"id":205067,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1007/BF00000042"},{"id":220862,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"91-92","issue":"0","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059f0c2e4b0c8380cd4a8ce","contributors":{"authors":[{"text":"Callender, E.","contributorId":72528,"corporation":false,"usgs":true,"family":"Callender","given":"E.","email":"","affiliations":[],"preferred":false,"id":362142,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":1013977,"text":"1013977 - 1982 - Furunculosis in brook trout: Infection by contact exposure","interactions":[],"lastModifiedDate":"2025-08-13T14:57:54.660105","indexId":"1013977","displayToPublicDate":"1982-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3196,"text":"Progressive Fish-Culturist","active":true,"publicationSubtype":{"id":10}},"title":"Furunculosis in brook trout: Infection by contact exposure","docAbstract":"<p><span>In juvenile brook trout (Salvelinus fontinalis) challenged by applying about 10</span><sup>9</sup><span>&nbsp;virulent Aeromonas salmonicida cells to an abraded area along the lateral line, or held in aquarium water containing about 10</span><sup>5</sup><span>&nbsp;cells per milliliter, mortalities were 50 and 60%, respectively, within 7 days after exposure. Neither feeding the bacterium to the fish nor applying it directly to the gills caused systemic bacterial infection. Two consistent experimental challenges were developed for inducing furunculosis in juvenile brook trout: (1) 15‐min contact (bath) exposures of trout to about 10</span><sup>6</sup><span>&nbsp;A. salmonicida cells per milliliter of spring water, and (2) 60‐s dip exposures of the fish to 10</span><sup>9</sup><span>&nbsp;A. salmonicida cells per milliliter. These challenge procedures produced 70‐100% and 74‐88% mortality, respectively, within 14 days after exposure. Results obtained with a strain of brook trout from Owhi Lake, Washington, by the dip exposure method were affected by neither the age of the fish (up to 1 year) nor the source of the population. The challenge was also effective for Atlantic salmon (Salmo salar) but not for rainbow trout (S. gairdneri).</span></p>","language":"English","publisher":"Oxford Academic","doi":"10.1577/1548-8659(1982)44[12:FIBT]2.0.CO;2","usgsCitation":"Cipriano, R.C., 1982, Furunculosis in brook trout: Infection by contact exposure: Progressive Fish-Culturist, v. 44, no. 1, p. 12-14, https://doi.org/10.1577/1548-8659(1982)44[12:FIBT]2.0.CO;2.","productDescription":"3 p.","startPage":"12","endPage":"14","numberOfPages":"3","costCenters":[{"id":365,"text":"Leetown Science Center","active":true,"usgs":true}],"links":[{"id":131620,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"44","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b32e4b07f02db6b4303","contributors":{"authors":[{"text":"Cipriano, R. C.","contributorId":12400,"corporation":false,"usgs":true,"family":"Cipriano","given":"R.","middleInitial":"C.","affiliations":[],"preferred":false,"id":319550,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70011825,"text":"70011825 - 1982 - Mineralogy and stable isotope geochemistry of hydrothermally altered oceanic rocks","interactions":[],"lastModifiedDate":"2023-12-12T12:26:55.364294","indexId":"70011825","displayToPublicDate":"1982-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1427,"text":"Earth and Planetary Science Letters","active":true,"publicationSubtype":{"id":10}},"title":"Mineralogy and stable isotope geochemistry of hydrothermally altered oceanic rocks","docAbstract":"<p>Mineralogical and isotopic variations observed in altered glassy and crystalline rocksfrom the East Pacific Rise and the Mid-Atlantic Ridge provide information about the temperatures of alteration and seawater/rock ratios for various hydrothermal regimes within the oceanic crust. A systematic increase in alteration temperature is evident for the glassy rocksin the sequence: (1) nontronite and celadonite vesicle fillings (35°C), (2) saponite-rich pillow breccias ( 130–170°C), (3) calcite-rich greenstone breccias and epidote-rich greenstone (200–350°C). Theseresults include the highest temperatures thus far reported for saponite formation.</p><p>The “seawater-dominated” hydrothermal alteration process that formed the saponite-rich pillow breccias is characterized by high water/rock ratios (&gt;0:1), low to moderate temperatures, a seawater origin of most of the carbon in vein calcites (δ<sup>13</sup>C≈0) and the predominance of Fe-rich saponite and calcite as secondary phases. Greenstones (chlorite-quartz-epidote) and greenstone breccias (chlorite-quartz-albite-calcite) are altered in a “rock-dominated” system with lower water/rock ratios (50:1 to &lt; 1:1), higher temperatures, and vein calcites with carbon that is principally of magmatic origin (δ<sup>13</sup>C≈−4). The crystalline rocks (diabase, gabbro, and metagabbro) are affected to varying degrees by pervasive high-temperature seawater interactions that commence soon after solidification, producing varying proportions of fine-grained secondary minerals including talc, smectite, chlorite, vermiculite, actinolite, and sodicplagioclase. Hydrothermal solutions, derived from alteration of the crystalline rocks, are of the appropriate temperature and isotopic composition to alter the overlying glassy rocks to the observed mineralogies as well as being the source of metal-rich deposits associated with the oceanic spreading centers.</p>","language":"English","publisher":"Elsevier","doi":"10.1016/0012-821X(82)90151-0","issn":"0012821X","usgsCitation":"Stakes, D., and O’Neil, J.R., 1982, Mineralogy and stable isotope geochemistry of hydrothermally altered oceanic rocks: Earth and Planetary Science Letters, v. 57, no. 2, p. 285-304, https://doi.org/10.1016/0012-821X(82)90151-0.","productDescription":"20 p.","startPage":"285","endPage":"304","numberOfPages":"20","costCenters":[],"links":[{"id":221317,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"57","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a5ac8e4b0c8380cd6f117","contributors":{"authors":[{"text":"Stakes, D.S.","contributorId":103792,"corporation":false,"usgs":true,"family":"Stakes","given":"D.S.","email":"","affiliations":[],"preferred":false,"id":362047,"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":362046,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"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":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":70011749,"text":"70011749 - 1982 - Accumulation rates of Th-230, Pa-231, and some transition metals on the Bermuda Rise","interactions":[],"lastModifiedDate":"2024-03-18T14:15:55.23402","indexId":"70011749","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":"Accumulation rates of Th-230, Pa-231, and some transition metals on the Bermuda Rise","docAbstract":"<p><span>Measurements of&nbsp;</span><sup>238</sup><span>U,&nbsp;</span><sup>234</sup><span>U,&nbsp;</span><sup>230</sup><span>Th,&nbsp;</span><sup>232</sup><span>Th,&nbsp;</span><sup>231</sup><span>Pa, Mn, Fe, Co, Ni, Cu, and Zn were made on 23 samples from core GPC-5, a 29-m giant piston core from a water depth of 4583 m on the northeastern Bermuda Rise (33°41.2′N, 57°36.9′W). This area is characterized by rapid deposition of sediment transported by abyssal currents. Unsupported&nbsp;</span><sup>230</sup><span>Th and&nbsp;</span><sup>231</sup><span>Pa are present throughout the core but, because of large variations in the sedimentation rate, show marked departures from exponential decay with depth. The trend with depth of the&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;><msup><mi></mi><mn>231</mn></msup><mtext>Pa</mtext><msub><mi></mi><mn>ex</mn></msub><msup><mi></mi><mn>230</mn></msup><mtext>Th</mtext><msub><mi></mi><mn>ex</mn></msub></math>\"><span class=\"MJX_Assistive_MathML\"><sup>231</sup>Pa<sub>ex</sub><sup>230</sup>Th<sub>ex</sub></span></span></span><span>&nbsp;ratio is consistent with the average accumulation rate of 36 cm/1000 y reported earlier on the basis of radiocarbon dating and CaCO</span><sub>3</sub><span>&nbsp;stratigraphy. When expressed on a carbonate-free basis, concentrations of Mn, Co, Ni, Cu, Zn,&nbsp;</span><sup>230</sup><span>Th</span><sub>ex</sub><span>, and&nbsp;</span><sup>231</sup><span>Pa</span><sub>ex</sub><span>&nbsp;all show cyclic variations positively correlated with those of CaCO</span><sub>3</sub><span>. The correlations can be explained by a model in which all of these constituents, including CaCO</span><sub>3</sub><span>, are supplied to the sediments from the water column at a constant rate. Concentration variations are controlled mainly by varying inputs of terrigenous detritus, with low inputs occurring during interglacials and high inputs during glacials. Relationships between the metal and&nbsp;</span><sup>230</sup><span>Th</span><sub>ex</sub><span>&nbsp;concentrations permit estimates of the rates at which the metals are removed to the sediment by scavenging from the water column. The results, in μg/cm</span><sup>2</sup><span>-1000 y, are: 4300 ± 1100 for Mn, 46 ± 16 for Ni and 76 ± 26 for Cu. These rates are somewhat larger than ocean-wide averages estimated by other methods, and the absolute rate of&nbsp;</span><sup>230</sup><span>Th accumulation in GPC-5 averages about nine times higher than production in the overlying water column. This part of the Bermuda Rise and similar bottom-current deposits may act as important accumulators of elements scavenged from seawater.</span></p>","language":"English","publisher":"Elsevier","doi":"10.1016/0016-7037(82)90166-1","issn":"00167037","usgsCitation":"Bacon, M., and Rosholt, J., 1982, Accumulation rates of Th-230, Pa-231, and some transition metals on the Bermuda Rise: Geochimica et Cosmochimica Acta, v. 46, no. 4, p. 651-666, https://doi.org/10.1016/0016-7037(82)90166-1.","productDescription":"16 p.","startPage":"651","endPage":"666","numberOfPages":"16","costCenters":[],"links":[{"id":221194,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"46","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059e685e4b0c8380cd4747d","contributors":{"authors":[{"text":"Bacon, M.P.","contributorId":76069,"corporation":false,"usgs":false,"family":"Bacon","given":"M.P.","email":"","affiliations":[{"id":6706,"text":"Woods Hole Oceanographic Institution,","active":true,"usgs":false}],"preferred":false,"id":361869,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Rosholt, J.N.","contributorId":37749,"corporation":false,"usgs":true,"family":"Rosholt","given":"J.N.","email":"","affiliations":[],"preferred":false,"id":361868,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70011751,"text":"70011751 - 1982 - Variation in sand body types on the eastern Bering Sea epicontinental shelf.","interactions":[],"lastModifiedDate":"2012-03-12T17:18:27","indexId":"70011751","displayToPublicDate":"1982-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1794,"text":"Geologie en Mijnbouw","active":true,"publicationSubtype":{"id":10}},"title":"Variation in sand body types on the eastern Bering Sea epicontinental shelf.","docAbstract":"The eastern epicontinental shelf of the Bering Sea is characterized by variations in river and glacial sediment supply, wave energy, tidal range (microtidal to mesotidal), and tidal, geostrophic, and storm-induced currents. These factors, combined with the effect of the Holocene rise in sea level, have resulted in the formation of a complex assemblage of generally linear sand bodies of similar morphology anad lithology, but different origins. The sand bodies are large features found from the present shoreline to tens of kilometers offshore, in water depths up to 50m. -from Authors","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Geologie en Mijnbouw","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","usgsCitation":"Nelson, C., Dupre, W., Field, M., and Howard, J., 1982, Variation in sand body types on the eastern Bering Sea epicontinental shelf.: Geologie en Mijnbouw, v. 61, no. 1, p. 37-48.","startPage":"37","endPage":"48","numberOfPages":"12","costCenters":[],"links":[{"id":221196,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"61","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505bc164e4b08c986b32a555","contributors":{"authors":[{"text":"Nelson, C.H.","contributorId":88346,"corporation":false,"usgs":true,"family":"Nelson","given":"C.H.","email":"","affiliations":[],"preferred":false,"id":361876,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Dupre, W.R.","contributorId":57540,"corporation":false,"usgs":true,"family":"Dupre","given":"W.R.","email":"","affiliations":[],"preferred":false,"id":361875,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Field, M.E.","contributorId":27052,"corporation":false,"usgs":true,"family":"Field","given":"M.E.","affiliations":[],"preferred":false,"id":361874,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Howard, J.D.","contributorId":103413,"corporation":false,"usgs":true,"family":"Howard","given":"J.D.","email":"","affiliations":[],"preferred":false,"id":361877,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70011842,"text":"70011842 - 1982 - Mineral paragenesis in the talc-water experimental hydrothermal system.","interactions":[],"lastModifiedDate":"2013-02-14T09:54:18","indexId":"70011842","displayToPublicDate":"1982-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":738,"text":"American Mineralogist","active":true,"publicationSubtype":{"id":10}},"title":"Mineral paragenesis in the talc-water experimental hydrothermal system.","docAbstract":"The talc-like gel was treated between 300o and 550oC at 1 kbar for 7, 30, 50, 120 and 200 days. The trends suggest that stevensite and/or corrensite are the stable minerals at <450oC. At 500o- 550oC, talc is stable.-K.A.R.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"American Mineralogist","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"Mineralogical Society of America","issn":"0003004X","usgsCitation":"Whitney, G., and Eberl, D.D., 1982, Mineral paragenesis in the talc-water experimental hydrothermal system.: American Mineralogist, v. 67, no. 9-10, p. 944-949.","startPage":"944","endPage":"949","numberOfPages":"6","costCenters":[],"links":[{"id":221551,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":267369,"type":{"id":11,"text":"Document"},"url":"https://www.minsocam.org/ammin/AM67/AM67_944.pdf"}],"volume":"67","issue":"9-10","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a57a2e4b0c8380cd6ddd9","contributors":{"authors":[{"text":"Whitney, G.","contributorId":32678,"corporation":false,"usgs":true,"family":"Whitney","given":"G.","email":"","affiliations":[],"preferred":false,"id":362090,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Eberl, D. D.","contributorId":66282,"corporation":false,"usgs":true,"family":"Eberl","given":"D.","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":362091,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70011750,"text":"70011750 - 1982 - Laboratory measurements of reservoir rock from the Geysers geothermal field, California","interactions":[],"lastModifiedDate":"2013-01-18T13:20:42","indexId":"70011750","displayToPublicDate":"1982-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2071,"text":"International Journal of Rock Mechanics and Mining Sciences & Geomechanics Abstracts","active":true,"publicationSubtype":{"id":10}},"title":"Laboratory measurements of reservoir rock from the Geysers geothermal field, California","docAbstract":"Rock samples taken from two outcrops, as well as rare cores from three well bores at the Geysers geothermal field, California, were tested at temperatures and pressures similar to those found in the geothermal field. Both intact and 30?? sawcut cylinders were deformed at confining pressures of 200-1000 bars, pore pressure of 30 bars and temperatures of 150?? and 240??C. Thin-section and X-ray analysis revealed that some borehole samples had undergone extensive alteration and recrystallization. Constant strain rate tests of 10-4 and 10-6 per sec gave a coefficient of friction of 0.68. Due to the highly fractured nature of the rocks taken from the production zone, intact samples were rarely 50% stronger than the frictional strength. This result suggests that the Geysers reservoir can support shear stresses only as large as its frictional shear strength. Velocity of p-waves (6.2 km/sec) was measured on one sample. Acoustic emission and sliding on a sawcut were related to changes in pore pressure. b-values computed from the acoustic emissions generated during fluid injection were typically about 0.55. An unusually high b-value (approximately 1.3) observed during sudden injection of water into the sample may have been related to thermal cracking. ?? 1982.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"International Journal of Rock Mechanics and Mining Sciences & Geomechanics Abstracts","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"Elsevier","doi":"10.1016/0148-9062(82)91632-1","issn":"01489062","usgsCitation":"Lockner, D., Summers, R., Moore, D., and Byerlee, J., 1982, Laboratory measurements of reservoir rock from the Geysers geothermal field, California: International Journal of Rock Mechanics and Mining Sciences & Geomechanics Abstracts, v. 19, no. 2, p. 65-80, https://doi.org/10.1016/0148-9062(82)91632-1.","productDescription":"p.65-80","startPage":"65","endPage":"80","numberOfPages":"16","costCenters":[],"links":[{"id":265944,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1016/0148-9062(82)91632-1"},{"id":221195,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"19","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a4112e4b0c8380cd65289","contributors":{"authors":[{"text":"Lockner, D.A. 0000-0001-8630-6833","orcid":"https://orcid.org/0000-0001-8630-6833","contributorId":85603,"corporation":false,"usgs":true,"family":"Lockner","given":"D.A.","affiliations":[],"preferred":false,"id":361872,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Summers, R.","contributorId":65483,"corporation":false,"usgs":true,"family":"Summers","given":"R.","email":"","affiliations":[],"preferred":false,"id":361870,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Moore, D.","contributorId":105307,"corporation":false,"usgs":true,"family":"Moore","given":"D.","affiliations":[],"preferred":false,"id":361873,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Byerlee, J.D.","contributorId":69982,"corporation":false,"usgs":true,"family":"Byerlee","given":"J.D.","affiliations":[],"preferred":false,"id":361871,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
]}