Radiochemical data from the Amchitka Island study area were obtained from water samples collected by the U.S. Geological Survey during August 1973. Tritium determinations were made on 86 samples collected and gross alpha and gross beta/gamma determinations were made on 38 samples. The range of data for these samples was equal or less than the range of values obtained before the Cannikin event.
","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/70156956","usgsCitation":"Ballance, W.C., 1973, Biochemical monitoring of water after the Cannikin event, Amchitka Island, Alaska, August 1973, i, 20 p., https://doi.org/10.3133/70156956.","productDescription":"i, 20 p.","numberOfPages":"24","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":307872,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/OFR474205.JPG"},{"id":308550,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/unnumbered/70156956/report.pdf","text":"Report","size":"3,498 KB","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Alaska","otherGeospatial":"Amchitka Island, Aleutian Islands","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n 178.584136963,\n 51.63677159243599\n ],\n [\n 178.592376709,\n 51.61290019118336\n ],\n [\n 179.21585083,\n 51.3254629443313\n ],\n [\n 179.508361816,\n 51.37520943448463\n ],\n [\n 179.057922363,\n 51.587309751245456\n ],\n [\n 178.628082275,\n 51.67936786087718\n ],\n [\n 178.584136963,\n 51.63677159243599\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"55f7efb1e4b05d6c4e4fa968","contributors":{"authors":[{"text":"Ballance, Wilbur C.","contributorId":50436,"corporation":false,"usgs":true,"family":"Ballance","given":"Wilbur","email":"","middleInitial":"C.","affiliations":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"preferred":false,"id":571245,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":2001014,"text":"2001014 - 1973 - Residues of MS-222, benzocaine, and their metabolites in striped bass following anesthesia","interactions":[],"lastModifiedDate":"2012-02-02T00:14:58","indexId":"2001014","displayToPublicDate":"1973-01-01T00:00:00","publicationYear":"1973","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":1,"text":"Federal Government Series"},"seriesTitle":{"id":39,"text":"Investigations in Fish Control","active":false,"publicationSubtype":{"id":1}},"seriesNumber":"52","title":"Residues of MS-222, benzocaine, and their metabolites in striped bass following anesthesia","docAbstract":"Abstract not submitted to date","language":"English","publisher":"U.S. Fish and Wildlife Service","publisherLocation":"La Crosse, WI","usgsCitation":"Luhning, C., 1973, Residues of MS-222, benzocaine, and their metabolites in striped bass following anesthesia: Investigations in Fish Control 52, 11.","productDescription":"11","startPage":"0","endPage":"11","numberOfPages":"11","costCenters":[{"id":606,"text":"Upper Midwest Environmental Sciences Center","active":true,"usgs":true}],"links":[{"id":198720,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a53e4b07f02db62b517","contributors":{"authors":[{"text":"Luhning, C.W.","contributorId":76682,"corporation":false,"usgs":true,"family":"Luhning","given":"C.W.","affiliations":[],"preferred":false,"id":325292,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":1000351,"text":"1000351 - 1973 - Application of theory and research in fishery management of the Laurentian Great Lakes","interactions":[],"lastModifiedDate":"2013-02-05T11:27:32","indexId":"1000351","displayToPublicDate":"1973-01-01T00:00:00","publicationYear":"1973","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3624,"text":"Transactions of the American Fisheries Society","active":true,"publicationSubtype":{"id":10}},"title":"Application of theory and research in fishery management of the Laurentian Great Lakes","docAbstract":"The Great Lakes have a high potential for the conduct of research and useful application of research findings, but the history of the Great Lakes indicates that extensive research and intensive management have failed to prevent deterioration of the fisheries. At times the research was not done before a loss occurred, or did not provide the information needed to solve a problem, or was not interpreted to indicate a need for corrective action.\nThree examples are used to illustrate these problems: (1) Sea lamprey (Petromyzon marinus) research was not initiated until 50 years after the destructiveness of the sea lamprey was recognized, and control measures were not developed or applied until species most vulnerable to the lamprey had been greatly reduced or eliminated. (2) Most research on the alewife (Alosa pseudoharengus) has been directed toward determining why large numbers of alewives die during the spring and summer, but has not provided the information most urgently needed by management to use alewives to best advantage, or to reduce the biological or human problems that alewives cause. (3) After a study during 1926-30 to determine if pollution was affecting fish in Lake Erie, it was concluded that the detrimental effects of pollution in certain regions were offset by the benefits of enrichment in other areas, but managers were not warned that areas of pollution might expand, and eventually influence the entire lake. The Great Lakes ecosystem is complex and in a state of rapid change. Thus, the outcome from the application of theory is uncertain at best and there can be no assurance that the desired results will be attained. The programs for sea lamprey control and salmonid restoration are a current example of difficulty in application of theory in management. Superficially the sea lamprey appears to be under control and salmonids have been restored. The postcontrol abundance of sea lampreys, however, is equal to the abundance that caused the initial collapse of the lake trout (Salvelinus namaycush), and there is evidence that the damage lampreys are inflicting on lake trout is as heavy as it was in the precontrol period. Also, in the presence of an abundance of hatchery-reared salmonids, the lamprey is reproducing and thriving as well as or better than it did during its initial population explosion, and indications are that it will increase rather than decrease under the present method and level of control. Successful application of theory and research to fishery management has always been impeded by lack of continued and close coordination among some 30-40 state, provincial, and federal governmental units that have varying degrees of influence on fishery programs of the Great Lakes. Frequently agreements that have been reached among conservation agencies were not sustained by legislative units, or were nullified by organizational changes. As a result, conflicting approaches were sometimes taken by management agencies with jurisdiction in different areas of the same lake. Sustained and compatible management objectives and practices can, however, contribute to greater stability, and optimum usefulness and productivity.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Transactions of the American Fisheries Society","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"Taylor & Francis","publisherLocation":"London, UK","doi":"10.1577/1548-8659(1973)102<156:AOTARI>2.0.CO;2","usgsCitation":"Smith, S.H., 1973, Application of theory and research in fishery management of the Laurentian Great Lakes: Transactions of the American Fisheries Society, v. 102, no. 1, p. 156-163, https://doi.org/10.1577/1548-8659(1973)102<156:AOTARI>2.0.CO;2.","productDescription":"8 p.","startPage":"156","endPage":"163","numberOfPages":"8","costCenters":[{"id":324,"text":"Great Lakes Science Center","active":true,"usgs":true}],"links":[{"id":132953,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":266987,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1577/1548-8659(1973)102<156:AOTARI>2.0.CO;2"}],"volume":"102","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac6e4b07f02db67a5ba","contributors":{"authors":[{"text":"Smith, Stanford H.","contributorId":86711,"corporation":false,"usgs":true,"family":"Smith","given":"Stanford","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":308438,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":37402,"text":"ssrw167 - 1973 - Sex determination of eagles, owls, and herons by analyzing plasma steroid hormones","interactions":[],"lastModifiedDate":"2020-03-20T06:57:58","indexId":"ssrw167","displayToPublicDate":"1973-01-01T00:00:00","publicationYear":"1973","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":1,"text":"Federal Government Series"},"seriesTitle":{"id":83,"text":"Special Scientific Report - Wildlife","active":false,"publicationSubtype":{"id":1}},"seriesNumber":"167","title":"Sex determination of eagles, owls, and herons by analyzing plasma steroid hormones","docAbstract":"No abstract available.
","language":"English","publisher":"U.S. Fish and Wildlife Service","usgsCitation":"Dieter, M.P., 1973, Sex determination of eagles, owls, and herons by analyzing plasma steroid hormones: Special Scientific Report - Wildlife 167, iv, 13 p.","productDescription":"iv, 13 p.","costCenters":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":166215,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49fbe4b07f02db5f4aa1","contributors":{"authors":[{"text":"Dieter, Michael P.","contributorId":80547,"corporation":false,"usgs":true,"family":"Dieter","given":"Michael","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":218010,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70159794,"text":"70159794 - 1973 - Determination of gold in phosphates by activation analysis using epithermal neutrons","interactions":[],"lastModifiedDate":"2015-11-23T11:56:49","indexId":"70159794","displayToPublicDate":"1973-01-01T00:00:00","publicationYear":"1973","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2446,"text":"Journal of Research of the U.S. Geological Survey","active":true,"publicationSubtype":{"id":10}},"title":"Determination of gold in phosphates by activation analysis using epithermal neutrons","docAbstract":"A simple method is described for determining gold in phosphates and phosphatic materials. Samples in a cadmium container are irradiated with epithermal neutrons to minimize the formation of 32 P, while permitting the formation of adequate amounts of 198 Au. Fire assay-radiochemical methods are used to separate the 198 Au. Concentrations as low as 0.1 ppb can be determined readily while maintaining low radiation levels.
","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, Va","usgsCitation":"Rowe, J., 1973, Determination of gold in phosphates by activation analysis using epithermal neutrons: Journal of Research of the U.S. Geological Survey, v. 1, no. 1, p. 79-80.","productDescription":"2 p.","startPage":"79","endPage":"80","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":311654,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":311653,"rank":1,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/journal/1973/vol1issue1/report.pdf","text":"Report","size":"22.2 MB","linkFileType":{"id":1,"text":"pdf"}}],"volume":"1","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"565446bde4b071e7ea53d4ab","contributors":{"authors":[{"text":"Rowe, Jack J.","contributorId":117455,"corporation":false,"usgs":true,"family":"Rowe","given":"Jack J.","affiliations":[],"preferred":false,"id":580484,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70010125,"text":"70010125 - 1973 - U-Th-Pb measurements of Luna 20 soil","interactions":[],"lastModifiedDate":"2021-01-06T14:22:44.31134","indexId":"70010125","displayToPublicDate":"1973-01-01T00:00:00","publicationYear":"1973","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":"U-Th-Pb measurements of Luna 20 soil","docAbstract":"The concentrations of uranium, thorium and lead and the lead isotopic composition of Luna 20 soil were determined. The data indicate that the Luna 20 soil is mainly a mixture of highland anorthosites and low-K basalt, but little KREEP basalt. The U-Th-Pb systematics are discussed in comparison with other lunar soils, especially with Apollo 16 soils which were collected from a ‘typical’ highland region. The data fit well in the Apollo 16 soil array on a U-Pb evolution diagram, and they exhibit excess lead relative to uranium. This relationship appears to be a characteristic of highland localities. Considering the previous observations of lunar samples, we infer that lead enrichment in the soil relative to uranium occurred between 3.2 and 3.9 b.y. ago and that the soil was disturbed by ‘third events’ about 2.0 b.y. ago. A lunar evolution model is discussed.
Water and gas samples from research wells in hydrothermal areas of Yellowstone National Park, U.S.A., have been mass spectrometrically analyzed for their rare gas contents and isotopic composition. In agreement with previous findings, the rare gases have been found to originate from infiltrating run-off water, saturated with air at 10 to 20°C. The atmospheric rare gas retention values found for the water varied between 3 and 87 per cent. The fine structure of the Ar, Kr and Xe abundance pattern in the water reveals fraotionational enrichment of the heavier gases due to partial outgassing of the waters. Radiogenic He and Ar have been detected. No positive evidence for magmatic water contribution has been found. Nevertheless, additions of magmatic waters free of rare gas can not be excluded, but if present the proportion is significantly less than 13 to 36 per cent.
Fingerling channel catfish (Ictalurus punctatus) offered diets containing 0.04–4.0 μg endrin/g food (dry weight) rapidly accumulated the pesticide. Amounts in the tissues were directly proportional to amounts in the food. Dietary endrin had no measurable effect on growth or mortality. After endrin was withdrawn from the diet, it rapidly disappeared and could not be detected after 41 days. In fish exposed to 0.5 μg endrin/liter of water, mortalities began at tissue levels of 0.7 μg endrin/g of wet whole fish and total mortality occurred at levels near 1.0 μg/g.
","language":"English","publisher":"Canadian Science Publishing","doi":"10.1139/f73-278","usgsCitation":"Argyle, R., Williams, G., and Dupree, H., 1973, Endrin uptake and release by fingerling channel catfish (Ictalurus punctatus): Journal of the Fisheries Research Board of Canada, v. 30, no. 11, p. 1743-1744, https://doi.org/10.1139/f73-278.","productDescription":"2 p.","startPage":"1743","endPage":"1744","numberOfPages":"2","costCenters":[{"id":365,"text":"Leetown Science Center","active":true,"usgs":true}],"links":[{"id":131975,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"30","issue":"11","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a14e4b07f02db6028f0","contributors":{"authors":[{"text":"Argyle, R.L.","contributorId":103614,"corporation":false,"usgs":true,"family":"Argyle","given":"R.L.","affiliations":[],"preferred":false,"id":318887,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Williams, G.C.","contributorId":36901,"corporation":false,"usgs":true,"family":"Williams","given":"G.C.","email":"","affiliations":[],"preferred":false,"id":318886,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Dupree, H.K.","contributorId":6785,"corporation":false,"usgs":true,"family":"Dupree","given":"H.K.","email":"","affiliations":[],"preferred":false,"id":318885,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":70010228,"text":"70010228 - 1973 - Inorganic chemical investigation by x-ray fluorescence analysis: The Viking Mars Lander","interactions":[],"lastModifiedDate":"2025-02-28T16:52:00.529379","indexId":"70010228","displayToPublicDate":"1973-01-01T00:00:00","publicationYear":"1973","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1963,"text":"Icarus","active":true,"publicationSubtype":{"id":10}},"title":"Inorganic chemical investigation by x-ray fluorescence analysis: The Viking Mars Lander","docAbstract":"The sialic basement of New Caledonia is a Permian-Jurassic greywacke sequence which was folded and metamorphosed to prehnite-pumpellyite or low-grade greenschist facies by the Late Jurassic. Succeeding Cretaceous-Eocene sediments unconformably overlie this basement and extend outwards onto oceanic crust. Tertiary tectonism occurred in three distinct phases.
At the present time, the tectonics of the southwest Pacific are related to a series of opposite facing subduction (Benioff) zones connected by transform faults extending from New Britain-Solomon Islands south through the New Hebrides to New Zealand and marking the boundary between the Australian and Pacific plates. Available geologic data from this region suggest that a similar geometry existed during the Tertiary and that the microcontinents of New Guinea, New Caledonia and New Zealand all lay along the former plate boundary which has since migrated north and east by a complex process of sea-floor spreading behind the active island arcs.
","language":"English","publisher":"Elsevier","doi":"10.1016/0040-1951(73)90046-2","issn":"00401951","usgsCitation":"Brothers, R., and Blake, M., 1973, Tertiary plate tectonics and high-pressure metamorphism in New Caledonia: Tectonophysics, v. 17, no. 4, p. 337-358, https://doi.org/10.1016/0040-1951(73)90046-2.","productDescription":"22 p.","startPage":"337","endPage":"358","costCenters":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"links":[{"id":218927,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"17","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505ba57fe4b08c986b320ab3","contributors":{"authors":[{"text":"Brothers, R.N.","contributorId":90866,"corporation":false,"usgs":true,"family":"Brothers","given":"R.N.","email":"","affiliations":[],"preferred":false,"id":358020,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Blake, M.C. Jr.","contributorId":27094,"corporation":false,"usgs":true,"family":"Blake","given":"M.C.","suffix":"Jr.","affiliations":[],"preferred":false,"id":358019,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70010113,"text":"70010113 - 1973 - Isotopic composition of oil-field brines from Kettleman North Dome, California, and their geologic implications","interactions":[],"lastModifiedDate":"2020-12-30T15:25:29.654987","indexId":"70010113","displayToPublicDate":"1973-01-01T00:00:00","publicationYear":"1973","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":"Isotopic composition of oil-field brines from Kettleman North Dome, California, and their geologic implications","docAbstract":"Deuterium and O18 analyses were made on 25 formation-water samples from Miocene (Temblor Formation) and Eocene (McAdams Formation) reservoir rocks at Kettleman North Dome oil field, California, and on three surface water samples from Reef Ridge located about three miles to the west of the field. The δO18 values obtained generally increase with depth and most probably are due to temperature controlled exchange reactions with carbonate cement and dissolved carbonate species. The δD values obtained seem to be controlled primarily by the membrane behavior of shales modifying the assumed original values. The contribution of isotopic exchange between water and clays cannot be evaluated at present.
The isotopic data support the conclusions based on a detailed study of geology, hydrodynamics, and formation water geochemistry (Kharaka, 1971) which indicate that:
1. The Temblor Formation waters are probably meteoric in origin concentrated chemically and isotopically by shale membranes, and 2. The McAdams Formation waters were most probably obtained by squeezing the original interstitial marine connate waters of deposition from the underlying Mesozoic sediments.
","language":"English","publisher":"Elsevier","doi":"10.1016/0016-7037(73)90148-8","issn":"00167037","usgsCitation":"Kharaka, Y., Berry, F., and Friedman, I., 1973, Isotopic composition of oil-field brines from Kettleman North Dome, California, and their geologic implications: Geochimica et Cosmochimica Acta, v. 37, no. 8, p. 1899-1908, https://doi.org/10.1016/0016-7037(73)90148-8.","productDescription":"10 p.","startPage":"1899","endPage":"1908","numberOfPages":"10","costCenters":[],"links":[{"id":381758,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"California","otherGeospatial":"Kettleman North Dome","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -119.58892822265626,\n 35.980228800645676\n ],\n [\n -119.41177368164061,\n 35.980228800645676\n ],\n [\n -119.41177368164061,\n 36.094609063015085\n ],\n [\n -119.58892822265626,\n 36.094609063015085\n ],\n [\n -119.58892822265626,\n 35.980228800645676\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"37","issue":"8","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a3fa3e4b0c8380cd646aa","contributors":{"authors":[{"text":"Kharaka, Y.K.","contributorId":23568,"corporation":false,"usgs":true,"family":"Kharaka","given":"Y.K.","email":"","affiliations":[],"preferred":false,"id":357954,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Berry, F.A.F.","contributorId":15755,"corporation":false,"usgs":true,"family":"Berry","given":"F.A.F.","email":"","affiliations":[],"preferred":false,"id":357953,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Friedman, I.","contributorId":95596,"corporation":false,"usgs":true,"family":"Friedman","given":"I.","email":"","affiliations":[],"preferred":false,"id":357955,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":70010111,"text":"70010111 - 1973 - Can American oil refineries yield vanadium?","interactions":[],"lastModifiedDate":"2012-03-12T17:18:23","indexId":"70010111","displayToPublicDate":"1973-01-01T00:00:00","publicationYear":"1973","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"Can American oil refineries yield vanadium?","docAbstract":"[No abstract available]","largerWorkTitle":"Preprints","language":"English","issn":"05693799","usgsCitation":"Fischer, R.P., 1973, Can American oil refineries yield vanadium?, in Preprints, v. 18, no. 4, p. 620-622.","startPage":"620","endPage":"622","numberOfPages":"3","costCenters":[],"links":[{"id":218704,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"18","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059f331e4b0c8380cd4b654","contributors":{"authors":[{"text":"Fischer, R. P.","contributorId":89958,"corporation":false,"usgs":true,"family":"Fischer","given":"R.","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":357941,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70010022,"text":"70010022 - 1973 - Absolute stress measurements at the rangely anticline, Northwestern Colorado. Discussion of R. V. De La Cruz and C. B. Raleigh's","interactions":[],"lastModifiedDate":"2013-01-18T13:36:33","indexId":"70010022","displayToPublicDate":"1973-01-01T00:00:00","publicationYear":"1973","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":"Absolute stress measurements at the rangely anticline, Northwestern Colorado. Discussion of R. V. De La Cruz and C. B. Raleigh's","docAbstract":"[No abstract available]","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(73)90018-1","issn":"01489062","usgsCitation":"Nichols, T.C., and Farrow, R., 1973, Absolute stress measurements at the rangely anticline, Northwestern Colorado. Discussion of R. V. De La Cruz and C. B. Raleigh's: International Journal of Rock Mechanics and Mining Sciences & Geomechanics Abstracts, v. 10, no. 6, p. 751-755, https://doi.org/10.1016/0148-9062(73)90018-1.","productDescription":"p.751-755","startPage":"751","endPage":"755","numberOfPages":"5","costCenters":[],"links":[{"id":265956,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1016/0148-9062(73)90018-1"},{"id":219345,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"10","issue":"6","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059e64ce4b0c8380cd4731a","contributors":{"authors":[{"text":"Nichols, T. C. Jr.","contributorId":95482,"corporation":false,"usgs":true,"family":"Nichols","given":"T.","suffix":"Jr.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":357709,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Farrow, R.A.","contributorId":60636,"corporation":false,"usgs":true,"family":"Farrow","given":"R.A.","affiliations":[],"preferred":false,"id":357708,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70010146,"text":"70010146 - 1973 - Solubility and occurrence of lead in surface water","interactions":[],"lastModifiedDate":"2025-01-07T16:11:33.867111","indexId":"70010146","displayToPublicDate":"1973-01-01T00:00:00","publicationYear":"1973","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2136,"text":"Journal - American Water Works Association","active":true,"publicationSubtype":{"id":10}},"title":"Solubility and occurrence of lead in surface water","docAbstract":"The data in this article suggest methods of reducing the lead content of drinking water at the water-treatment plant.
","language":"English","publisher":"American Water Works Association","doi":"10.1002/j.1551-8833.1973.tb01896.x","issn":"0003150X","usgsCitation":"Hem, J., and Durum, W.H., 1973, Solubility and occurrence of lead in surface water: Journal - American Water Works Association, v. 65, no. 8, p. 562-568, https://doi.org/10.1002/j.1551-8833.1973.tb01896.x.","productDescription":"7 p.","startPage":"562","endPage":"568","numberOfPages":"7","costCenters":[],"links":[{"id":219352,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"65","issue":"8","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505b9241e4b08c986b319db7","contributors":{"authors":[{"text":"Hem, J.D.","contributorId":54576,"corporation":false,"usgs":true,"family":"Hem","given":"J.D.","affiliations":[],"preferred":false,"id":358117,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Durum, W. H.","contributorId":78311,"corporation":false,"usgs":true,"family":"Durum","given":"W.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":358118,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70011041,"text":"70011041 - 1973 - Red sea drillings","interactions":[],"lastModifiedDate":"2019-12-19T15:16:44","indexId":"70011041","displayToPublicDate":"1973-01-01T00:00:00","publicationYear":"1973","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3338,"text":"Science","active":true,"publicationSubtype":{"id":10}},"title":"Red sea drillings","docAbstract":"Recent drilling in the Red Sea has shown that much of the basin is underlain by evaporites of a similar age to that of evaporites found in the Mediterranean Sea. These evaporites and their structural positions indicate that other brine areas are present - and, indeed, several others have been discovered.","language":"English","publisher":"AAAS","doi":"10.1126/science.179.4071.377","issn":"00368075","usgsCitation":"Ross, D., Whitmarsh, R., Ali, S., Boudreaux, J., Coleman, R., Fleisher, R., Girdler, R., Manheim, F.T., Matter, A., Nigrini, C., Stoffers, P., and Supko, P., 1973, Red sea drillings: Science, v. 179, no. 4071, p. 377-380, https://doi.org/10.1126/science.179.4071.377.","productDescription":"4 p.","startPage":"377","endPage":"380","numberOfPages":"4","costCenters":[{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"links":[{"id":220684,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"otherGeospatial":"Red Sea","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n 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0000-0003-4005-4524","orcid":"https://orcid.org/0000-0003-4005-4524","contributorId":20770,"corporation":false,"usgs":true,"family":"Manheim","given":"Frank","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":360138,"contributorType":{"id":1,"text":"Authors"},"rank":8},{"text":"Matter, A.","contributorId":68879,"corporation":false,"usgs":true,"family":"Matter","given":"A.","email":"","affiliations":[],"preferred":false,"id":360140,"contributorType":{"id":1,"text":"Authors"},"rank":9},{"text":"Nigrini, C.","contributorId":30753,"corporation":false,"usgs":true,"family":"Nigrini","given":"C.","email":"","affiliations":[],"preferred":false,"id":360136,"contributorType":{"id":1,"text":"Authors"},"rank":10},{"text":"Stoffers, P.","contributorId":81634,"corporation":false,"usgs":true,"family":"Stoffers","given":"P.","email":"","affiliations":[],"preferred":false,"id":360141,"contributorType":{"id":1,"text":"Authors"},"rank":11},{"text":"Supko, 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It extracts and simultaneously concentrates organic solutes from water. Any immiscible solvent can be used in this apparatus if the solute will partition between the solvent and water. A concentration factor of up to 105 is obtained with this technique. The dipole moment difference between the solute and solvent is demonstrated to be an index of the extraction efficiency. Optimum extraction of a given molecular species may be obtained by use of this index.
","language":"English","publisher":"ACS Publications","doi":"10.1021/ac60323a020","usgsCitation":"Goldberg, M.C., DeLong, L.L., and Sinclair, M., 1973, Extraction and concentration of organic solutes from water: Analytical Chemistry, v. 45, no. 1, p. 89-93, https://doi.org/10.1021/ac60323a020.","productDescription":"5 p.","startPage":"89","endPage":"93","numberOfPages":"5","costCenters":[],"links":[{"id":219434,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"45","issue":"1","noUsgsAuthors":false,"publicationDate":"2002-05-01","publicationStatus":"PW","scienceBaseUri":"505a0e5ce4b0c8380cd533f2","contributors":{"authors":[{"text":"Goldberg, Marvin C.","contributorId":26066,"corporation":false,"usgs":true,"family":"Goldberg","given":"Marvin","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":358152,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"DeLong, Lewis L.","contributorId":91146,"corporation":false,"usgs":true,"family":"DeLong","given":"Lewis","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":358150,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Sinclair, Mark","contributorId":91027,"corporation":false,"usgs":true,"family":"Sinclair","given":"Mark","email":"","affiliations":[],"preferred":false,"id":358151,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":70010160,"text":"70010160 - 1973 - Polyphenyl fluorides","interactions":[],"lastModifiedDate":"2013-03-14T12:51:04","indexId":"70010160","displayToPublicDate":"1973-01-01T00:00:00","publicationYear":"1973","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2292,"text":"Journal of Fluorine Chemistry","active":true,"publicationSubtype":{"id":10}},"title":"Polyphenyl fluorides","docAbstract":"Studies related to the chemistry of aromatic fluorine compounds have been carried out at the Illinois State Geological Survey since 1933. In our reference collection we have several compounds that have not previously been described. This communication records data on 18 biphenyl, three terphenyl and some benzene fluorinated derivatives that were obtained as by-products and/or by specific synthesis. ?? 1973.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Journal of Fluorine Chemistry","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"Elsevier","doi":"10.1016/S0022-1139(00)82864-X","issn":"00221139","usgsCitation":"Dickerson, D.R., Finger, G.C., and Shiley, R., 1973, Polyphenyl fluorides: Journal of Fluorine Chemistry, v. 3, no. 1, p. 113-116, https://doi.org/10.1016/S0022-1139(00)82864-X.","startPage":"113","endPage":"116","numberOfPages":"4","costCenters":[],"links":[{"id":269323,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1016/S0022-1139(00)82864-X"},{"id":219511,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"3","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a7d09e4b0c8380cd79cff","contributors":{"authors":[{"text":"Dickerson, D. R.","contributorId":66837,"corporation":false,"usgs":true,"family":"Dickerson","given":"D.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":358159,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Finger, G. C.","contributorId":89277,"corporation":false,"usgs":true,"family":"Finger","given":"G.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":358160,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Shiley, R.H.","contributorId":44282,"corporation":false,"usgs":true,"family":"Shiley","given":"R.H.","email":"","affiliations":[],"preferred":false,"id":358158,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":70010293,"text":"70010293 - 1973 - Effect of sea water interaction on strontium isotope composition of deep-sea basalts","interactions":[],"lastModifiedDate":"2020-12-29T15:14:13.871125","indexId":"70010293","displayToPublicDate":"1973-01-01T00:00:00","publicationYear":"1973","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":"Effect of sea water interaction on strontium isotope composition of deep-sea basalts","docAbstract":"Analyses of rim-to-interior samples of fresh tholeiitic pillow basalts, deuterically altered holocrystalline basalts, and older, weathered tholeiitic basalts from the deep sea indicate that 87Sr/86Sr ratios of the older basalts are raised by low temperature interaction with strontium dissolved in sea water. 87Sr/86Sr correlates positively with H2O in these basalts; however, there is little detectable modification of the strontium isotope composition in rocks with H2O contents less than 1%. The isotope changes appear to be a function of relatively long-term, low-temperature weathering, rather than high-temperature or deuteric alteration. Strontium abundance and isotopic data for these rocks suggest that strontium content is only slightly modified by interaction with sea water, and it is a relatively insensitive indicator of marine alteration. Average Rb-Sr parameters for samples of apparently unaltered basalt are: Rb= 1.11ppm; Sr= 132ppm; 87Sr/86Sr= 0.70247.
A universal procedure was sought for plaque assay of eight fish viruses (bluegill myxovirus, channel catfish virus, eel virus, Egtved virus, infectious hematopoietic necrosis virus, infectious pancreatic necrosis virus, lymphocystis virus, and the agent of spring viremia of carp (Rhabdovirus carpio), in dish cultures of various fish cells. Eagle minimal essential medium with sodium bicarbonate-CO2 buffer (Earle’s salt solution) was compared with minimal essential medium buffered principally with tris (hydroxymethyl)aminomethane or N-2-hydroxyethylpiperazine-N′-2′-ethanesulfonic acid at a pH or in the range of 7.6 to 8.0 depending upon temperature. Five fish cell lines collectively capable of replicating all fish viruses thus far isolated were tested and quantitatively found to grow comparably well in the three media. Two-phase (gel-liquid) media incorporating the various buffer systems allowed plaquing at 15 to 33 C either in partial pressures of CO2 or in normal atmosphere, but greater efficiency and sensitivity were obtained with the organic buffers, and, overall, the best results were obtained with tris(hydroxymethyl)aminomethane. Epizootiological data, specific fish cell line response, and plaque morphology permit presumptive identification of most of the agents. At proper pH, use of organic buffers obviates the need for CO2 incubators.
","language":"English","publisher":"American Society for Microbiology","doi":"10.1128/am.25.4.659-664.1973","usgsCitation":"Wolf, K., and Quimby, M.C., 1973, Fish viruses: Buffers and methods for plaquing eight agents under normal atmosphere: Applied Microbiology, v. 25, no. 4, p. 659-664, https://doi.org/10.1128/am.25.4.659-664.1973.","productDescription":"6 p.","startPage":"659","endPage":"664","costCenters":[{"id":365,"text":"Leetown Science Center","active":true,"usgs":true}],"links":[{"id":480662,"rank":2,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1128/am.25.4.659-664.1973","text":"Publisher Index Page"},{"id":197561,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"25","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f3e4b07f02db5ef553","contributors":{"authors":[{"text":"Wolf, K.","contributorId":16344,"corporation":false,"usgs":true,"family":"Wolf","given":"K.","email":"","affiliations":[],"preferred":false,"id":319870,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Quimby, M. C.","contributorId":14334,"corporation":false,"usgs":true,"family":"Quimby","given":"M.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":319869,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70009825,"text":"70009825 - 1973 - Comparison of the magnetic properties of glass from Luna 20 with similar properties of glass from the Apollo missions","interactions":[],"lastModifiedDate":"2020-12-29T20:02:02.886089","indexId":"70009825","displayToPublicDate":"1973-01-01T00:00:00","publicationYear":"1973","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":"Comparison of the magnetic properties of glass from Luna 20 with similar properties of glass from the Apollo missions","docAbstract":"Magnetic susceptibility measurements have been made on four glass spherules and fragments from the Luna 20 fines; two at 300°K and two from 300°K to 4°K. From these data the magnetic susceptibility extrapolated to infinite field, the magnetization at low fields and also the saturation magnetization at high fields, the Curie constant, the Weiss temperature, and the temperature-independent susceptibility were determined. Using a model previously proposed for the Apollo specimens, the Curie constant of the antiferromagnetic inclusions and a zero field splitting parameter were calculated for the same specimens. The data show the relatively low concentration of iron in all forms in these specimens. In addition, the Weiss temperature is lower than that measured for the Apollo specimens, and can be attributed almost entirely to the ligand field distortion about the Fe2+ ions in the glassy phase. The data further suggest that the Luna 20 specimens cooled more slowly than those of the Apollo missions, and that some of the antiferromagnetic inclusions in the glass may have crystallized from the glass during cooling.
Electron microprobe analyses of green hornblende and coexisting cummingtonite from garnet amphibolite show identical Fe/Mg ratios ( = 0.9). Cummingtonite is iron-magnesium silicate with very little calcium and aluminum and practically no alkalies. In contrast, the hornblende has 1.5 tetrahedral Al, 0.9 octahedral Al and a considerable amount of Ca and alkalies. Comparison with the hornblendes from the Sierra Nevada shows a higher relative amount of tschemakite molecule in the hornblendes from Idaho where pressures during the recrystallization were higher.
The sorption of silver by poorly crystallized manganese oxides was studied using synthesized samples of three members of the manganous manganite (birnessite) group, of different chemical composition and crystallinity, and a poorly organized γ-MnO2. All four oxides sorbed significant quantities of silver. The manganous manganites showed the greatest sorption (up to 0.5 moles silver/mole MnOx at pH 7) while the γ-MnO2 showed the least (0.3 moles silver/ mole MnOx at pH 7). Sorption of silver was adequately described by the Langmuir equation over a considerable concentration range. The relationship failed at low pH values and high equilibrium silver concentrations. The sorption capacity showed a direct relationship with pH. However, the rate of increase of sorption capacity decreased at the higher pH values.
Silver sorption maxima. were not directly related to surface area but appeared to vary with the amount of occluded sodium and potassium present in the manganese oxide. The important processes involved in the uptake of silver by the four poorly crystallized manganese oxides ara considered to be surface exchange for manganese, potassium and sodium as well as exchange for structural manganese, potassium and sodium.
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