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,{"id":70045438,"text":"70045438 - 1973 - Summary of ground-water data, Post Headquarters and adjacent areas, White Sands Missile Range","interactions":[],"lastModifiedDate":"2018-10-30T13:01:07","indexId":"70045438","displayToPublicDate":"1973-01-01T00:00:00","publicationYear":"1973","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"seriesTitle":{"id":375,"text":"Open-File Report","active":false,"publicationSubtype":{"id":6}},"title":"Summary of ground-water data, Post Headquarters and adjacent areas, White Sands Missile Range","docAbstract":"<p>Geohydrologic data have been obtained from more than 100 wells and test holes that have been drilled in the Post Headquarters and adjacent areas of White Sands Missile Range. Observation-well data show that, in general, a continuous decline of the water table has occurred in the vicinity of the well field since production began in 1949. Approximately 40,000 acre-feet of water has been produced from the aquifer to date (1972). </p><p>A series of maps are presented which show the changes that have occurred in the well field as the result of development.</p>","language":"English","publisher":"U.S Geological Survey","publisherLocation":"Albuquerque, NM","doi":"10.3133/70045438","collaboration":"Prepared in cooperation with White Sands Missile Range","usgsCitation":"Kelly, T.E., 1973, Summary of ground-water data, Post Headquarters and adjacent areas, White Sands Missile Range: Open-File Report, Report: 66 p.; 4 Plates: 28.47 x 46.17 inches or smaller, https://doi.org/10.3133/70045438.","productDescription":"Report: 66 p.; 4 Plates: 28.47 x 46.17 inches or smaller","numberOfPages":"68","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":272733,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/unnumbered/70045438/report.pdf"},{"id":270992,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/unnumbered/70045438/report-thumb.jpg"},{"id":358953,"rank":3,"type":{"id":29,"text":"Figure"},"url":"https://pubs.usgs.gov/unnumbered/70045438/figure-30.pdf","text":"Figure 30","linkFileType":{"id":1,"text":"pdf"}},{"id":358954,"rank":4,"type":{"id":29,"text":"Figure"},"url":"https://pubs.usgs.gov/unnumbered/70045438/figure-31.pdf","text":"Figure 31","linkFileType":{"id":1,"text":"pdf"}},{"id":358955,"rank":5,"type":{"id":29,"text":"Figure"},"url":"https://pubs.usgs.gov/unnumbered/70045438/figure-32.pdf","text":"Figure 32","linkFileType":{"id":1,"text":"pdf"}},{"id":358956,"rank":6,"type":{"id":29,"text":"Figure"},"url":"https://pubs.usgs.gov/unnumbered/70045438/figure-33.pdf","text":"Figure 33","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"New Mexico","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -106.61666667,\n              32.13333333\n            ],\n            [\n              -106.28333333,\n              32.13333333\n            ],\n            [\n              -106.28333333,\n              32.58333333\n            ],\n            [\n              -106.61666667,\n              32.58333333\n            ],\n            [\n              -106.61666667,\n              32.13333333\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"516e72efe4b00154e4368c48","contributors":{"authors":[{"text":"Kelly, T. E.","contributorId":63824,"corporation":false,"usgs":true,"family":"Kelly","given":"T.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":477500,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70175636,"text":"70175636 - 1973 - Ground water in selected areas in the Klamath Basin, Oregon","interactions":[],"lastModifiedDate":"2016-08-17T14:06:46","indexId":"70175636","displayToPublicDate":"1973-01-01T00:00:00","publicationYear":"1973","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":2,"text":"State or Local Government Series"},"seriesTitle":{"id":115,"text":"Ground Water Report","active":false,"publicationSubtype":{"id":2}},"title":"Ground water in selected areas in the Klamath Basin, Oregon","docAbstract":"<p><span class=\"EXLDetailsDisplayVal\">GROUNDWATER FEATURES OF SIX LOWLAND <span class=\"searchword\">AREAS</span> IN THE <span class=\"searchword\">KLAMATH</span> <span class=\"searchword\">BASIN</span> OF <span class=\"searchword\">OREGON</span>--<span class=\"searchword\">KLAMATH</span> MARSH AREA, AND SPRAGUE RIVER, SWAN LAKE, YONNA, POE, AND LANGELL VALLEYS--ARE DESCRIBED. RUGGED MOUNTAINS AND RIDGES SURROUND AND SEPARATE THESE LOWLANDS WHERE FLOORS RANGE IN ALTITUDE FROM 4,100 FEET IN POE VALLEY TO 4,600 FEET NORTH OF <span class=\"searchword\">KLAMATH</span> MARSH. THE SIX <span class=\"searchword\">AREAS</span> EXTEND OVER A NORTH-SOUTH DISTANCE OF 70 MILES, AN EAST-WEST DISTANCE OF 40 MILES, AND INCLUDE AN AREA OF APPROXIMATELY 600 SQUARE MILES. THE AREA IS SEMIARID AND RECEIVED ABOUT 14 TO 18 INCHES OF PRECIPITATION A YEAR. EXTINCT VOLCANOES AND THEIR EXTRUSIONS CHARACTERIZE THE AREA. MOST WELLS TAP PERMEABLE BASALT OR CINDERY RUBBLE BENEATH THE LACUSTRINE BEDS. THE DEPTHS OF WELLS RANGE FROM LESS THAN 50 TO NEARLY 2,000 FEET--MOST ARE BETWEEN 100 AND 1,000 FEET DEEP. FLOWING WELLS OCCUR IN ALL <span class=\"searchword\">AREAS</span> EXCEPT SWAN LAKE VALLEY. THE MOST EXTENSIVE AREA OF FLOWING WELLS IS IN THE SPRAGUE RIVER VALLEY, WHERE ABOUT 25 WELLS, SOME FLOWING MORE THAN 2,000 GPM, SUPPLY WATER FOR IRRIGATION. WATER LEVELS IN WELLS FLUCTUATE SEASONALLY FROM 1 TO 4 FEET. GROUNDWATER IN THE BASIN IS OF EXCELLENT QUALITY FOR DRINKING, IRRIGATION, AND MOST INDUSTRIAL USES. </span></p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","usgsCitation":"Leonard, A., and Harris, A., 1973, Ground water in selected areas in the Klamath Basin, Oregon: Ground Water Report.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":518,"text":"Oregon Water Science Center","active":true,"usgs":true}],"links":[{"id":326724,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Oregon","otherGeospatial":"Klamath Basin","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"57b58acfe4b03bcb0104bba9","contributors":{"authors":[{"text":"Leonard, A.R.","contributorId":101669,"corporation":false,"usgs":true,"family":"Leonard","given":"A.R.","email":"","affiliations":[],"preferred":false,"id":645901,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Harris, A.B.","contributorId":92290,"corporation":false,"usgs":true,"family":"Harris","given":"A.B.","email":"","affiliations":[],"preferred":false,"id":645902,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":17363,"text":"ofr7393 - 1973 - Mineral resources of the Alpine Lakes study area, Chelan, King, and Kittitas Counties, Washington, with a section on aeromagnetic interpretation","interactions":[],"lastModifiedDate":"2023-11-20T22:52:53.226768","indexId":"ofr7393","displayToPublicDate":"1973-01-01T00:00:00","publicationYear":"1973","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":"73-93","title":"Mineral resources of the Alpine Lakes study area, Chelan, King, and Kittitas Counties, Washington, with a section on aeromagnetic interpretation","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr7393","usgsCitation":"Gualtieri, J.L., Simmons, G.C., Thurber, H.K., Miller, M.S., and Davis, W., 1973, Mineral resources of the Alpine Lakes study area, Chelan, King, and Kittitas Counties, Washington, with a section on aeromagnetic interpretation: U.S. Geological Survey Open-File Report 73-93, Report: v, 132 p.; 2 Plates: 43.04 x 31.93 inches and 43.32 x 31.55 inches, https://doi.org/10.3133/ofr7393.","productDescription":"Report: v, 132 p.; 2 Plates: 43.04 x 31.93 inches and 43.32 x 31.55 inches","costCenters":[],"links":[{"id":422751,"rank":5,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_8840.htm","linkFileType":{"id":5,"text":"html"}},{"id":46499,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1973/0093/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":46498,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1973/0093/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":46500,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1973/0093/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":150844,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1973/0093/report-thumb.jpg"}],"country":"United States","state":"Washington","county":"Chelan County, King County, Kittitas County","otherGeospatial":"Alpine Lakes study area","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -121.4,\n              47.767\n            ],\n            [\n              -121.4,\n              47.4\n            ],\n            [\n              -120.683,\n              47.4\n            ],\n            [\n              -120.683,\n              47.767\n            ],\n            [\n              -121.4,\n              47.767\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a17e4b07f02db6046ad","contributors":{"authors":[{"text":"Gualtieri, James Louis","contributorId":46491,"corporation":false,"usgs":true,"family":"Gualtieri","given":"James","email":"","middleInitial":"Louis","affiliations":[],"preferred":false,"id":176088,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Simmons, G. C.","contributorId":82737,"corporation":false,"usgs":true,"family":"Simmons","given":"G.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":176092,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Thurber, H. K.","contributorId":59457,"corporation":false,"usgs":true,"family":"Thurber","given":"H.","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":176090,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Miller, M. S.","contributorId":69107,"corporation":false,"usgs":true,"family":"Miller","given":"M.","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":176091,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Davis, W. E.","contributorId":49228,"corporation":false,"usgs":true,"family":"Davis","given":"W. E.","affiliations":[],"preferred":false,"id":176089,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":1014153,"text":"1014153 - 1973 - Fish viruses: Buffers and methods for plaquing eight agents under normal atmosphere","interactions":[],"lastModifiedDate":"2023-09-13T14:05:39.414095","indexId":"1014153","displayToPublicDate":"1973-01-01T00:00:00","publicationYear":"1973","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":843,"text":"Applied Microbiology","active":true,"publicationSubtype":{"id":10}},"title":"Fish viruses: Buffers and methods for plaquing eight agents under normal atmosphere","docAbstract":"<p><span>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 (</span><i>Rhabdovirus carpio</i><span>), in dish cultures of various fish cells. Eagle minimal essential medium with sodium bicarbonate-CO</span><sub>2</sub><span>&nbsp;buffer (Earle’s salt solution) was compared with minimal essential medium buffered principally with tris (hydroxymethyl)aminomethane or&nbsp;</span><i>N</i><span>-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 CO</span><sub>2</sub><span>&nbsp;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 CO</span><sub>2</sub><span>&nbsp;incubators.</span></p>","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":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      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R.","contributorId":47520,"corporation":false,"usgs":true,"family":"Coleman","given":"R.","affiliations":[],"preferred":false,"id":360137,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Fleisher, R.L.","contributorId":59178,"corporation":false,"usgs":true,"family":"Fleisher","given":"R.L.","email":"","affiliations":[],"preferred":false,"id":360139,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Girdler, R.","contributorId":91626,"corporation":false,"usgs":true,"family":"Girdler","given":"R.","affiliations":[],"preferred":false,"id":360143,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Manheim, Frank T. 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, P.R.","contributorId":20072,"corporation":false,"usgs":true,"family":"Supko","given":"P.R.","email":"","affiliations":[],"preferred":false,"id":360135,"contributorType":{"id":1,"text":"Authors"},"rank":12}]}}
,{"id":1013621,"text":"1013621 - 1973 - Endrin uptake and release by fingerling channel catfish (Ictalurus punctatus)","interactions":[],"lastModifiedDate":"2025-03-04T16:42:42.889765","indexId":"1013621","displayToPublicDate":"1973-01-01T00:00:00","publicationYear":"1973","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2543,"text":"Journal of the Fisheries Research Board of Canada","active":true,"publicationSubtype":{"id":10}},"title":"Endrin uptake and release by fingerling channel catfish (Ictalurus punctatus)","docAbstract":"<p><span>Fingerling channel catfish (</span><i>Ictalurus punctatus</i><span>) 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.</span></p>","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":1014331,"text":"1014331 - 1973 - Practical farmer's guide to buffalo cross-breeding","interactions":[],"lastModifiedDate":"2012-02-02T00:04:26","indexId":"1014331","displayToPublicDate":"1973-01-01T00:00:00","publicationYear":"1973","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":716,"text":"American Fish Farmer and World Aquaculture News","active":true,"publicationSubtype":{"id":10}},"title":"Practical farmer's guide to buffalo cross-breeding","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"American Fish Farmer and World Aquaculture News","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","collaboration":"None/FF","usgsCitation":"Martin, M., 1973, Practical farmer's guide to buffalo cross-breeding: American Fish Farmer and World Aquaculture News, v. 4, no. 2, p. 6-8.","productDescription":"p. 6-8","startPage":"6","endPage":"8","numberOfPages":"3","costCenters":[{"id":365,"text":"Leetown Science Center","active":true,"usgs":true}],"links":[{"id":130678,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"4","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad3e4b07f02db681d47","contributors":{"authors":[{"text":"Martin, M.","contributorId":103217,"corporation":false,"usgs":true,"family":"Martin","given":"M.","affiliations":[],"preferred":false,"id":320214,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":7000078,"text":"7000078 - 1973 - Ferdinand Vandiveer Hayden and the founding of the Yellowstone National Park","interactions":[],"lastModifiedDate":"2016-09-07T12:55:03","indexId":"7000078","displayToPublicDate":"1973-01-01T00:00:00","publicationYear":"1973","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"seriesTitle":{"id":363,"text":"General Interest Publication","active":false,"publicationSubtype":{"id":6}},"title":"Ferdinand Vandiveer Hayden and the founding of the Yellowstone National Park","docAbstract":"<p>Following the Civil War, the United States intensified the exploration of her western frontiers to gain a measure of the vast lands and natural resources in the region now occupied by our Rocky Mountain States. As part of this effort, the U.S. Geological and Geographical Survey of the Territories was formed and staffed under the leadership of geologist Ferdinand Vandiveer Hayden. Originally organized under the U.S. Public Land Office in 1861, the Hayden Survey (as it was most often identified) was placed under the Secretary of the Interior in 1869 and later, under the newly created U.S. Geological Survey. Its records, maps, and photographs were then transferred to the latter agency. </p><p>In commemorating the centennial of Yellowstone National Park, the U.S. Geological Survey drew upon those items deposited by Hayden to describe the early exploration of the Yellowstone area and to recount events that led to the establishment of Yellowstone as the Nation's first national park.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/7000078","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1973, Ferdinand Vandiveer Hayden and the founding of the Yellowstone National Park (Revised and expanded): General Interest Publication, 45 p., https://doi.org/10.3133/7000078.","productDescription":"45 p.","costCenters":[],"links":[{"id":256842,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/gip/7000078/report-thumb.jpg"},{"id":256841,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/gip/7000078/report.pdf","text":"Report","size":"18.58 MB","linkFileType":{"id":1,"text":"pdf"},"description":"Report"}],"edition":"Revised and expanded","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a4be4b07f02db6258eb","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":535101,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":1001255,"text":"1001255 - 1973 - Waterfowl production on stock-watering ponds in the northern plains","interactions":[],"lastModifiedDate":"2025-02-27T17:44:09.339213","indexId":"1001255","displayToPublicDate":"1973-01-01T00:00:00","publicationYear":"1973","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2441,"text":"Journal of Range Management","active":true,"publicationSubtype":{"id":10}},"title":"Waterfowl production on stock-watering ponds in the northern plains","docAbstract":"In a 5-year study of stock-watering ponds in western North Dakota, pond size was found to be the major factor influencing duck use. As pond size increased, total pair and brood use per pond increased. Pairs used ponds as small as 0.1 acre in size, but broods were seldom seen on ponds of less than 1.0 surface acre. Dam-type ponds larger than 1.0 surface acre comprised only 29% of all man-made ponds on the study area but received 65% of the pair use and 87% of the brood use. Utilization of fenced ponds by pairs and broods was not significantly different from utilization of unfenced ponds. Grazing rates of 2 to 3 acres per AUM and lower rates permitted the development of grassy shoreline cover preferred by pairs and brushy and emergent shorelines preferred by broods. Duck pairs were significantly more numerous on older ponds and ponds with grassy shorelines but less numerous on ponds that had heavy deposits of sediment or were isolated from other wetlands. Broods were significantly more numerous on ponds with brushy shorelines and emergent vegetation than on those without. Broods were less numerous on turbid and newly constructed ponds. The most suitable stock-watering units for maximum waterfowl production were dam-type ponds of 1.5 surface acres, or larger, built in gentle to rolling terrain away from major sources of siltation.","language":"English","publisher":"Allen Press","doi":"10.2307/3896686","usgsCitation":"Lokemoen, J.T., 1973, Waterfowl production on stock-watering ponds in the northern plains: Journal of Range Management, v. 26, no. 3, p. 179-184, https://doi.org/10.2307/3896686.","productDescription":"6 p.","startPage":"179","endPage":"184","costCenters":[{"id":480,"text":"Northern Prairie Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":133802,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"26","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b28e4b07f02db6b1394","contributors":{"authors":[{"text":"Lokemoen, J. T.","contributorId":79049,"corporation":false,"usgs":true,"family":"Lokemoen","given":"J.","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":310755,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70009824,"text":"70009824 - 1973 - Thermal conductivity of carbonate rocks","interactions":[],"lastModifiedDate":"2020-12-29T19:59:08.591228","indexId":"70009824","displayToPublicDate":"1973-01-01T00:00:00","publicationYear":"1973","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1517,"text":"Engineering Geology","active":true,"publicationSubtype":{"id":10}},"title":"Thermal conductivity of carbonate rocks","docAbstract":"<p>The thermal conductivities of several well-defined carbonate rocks were determined near 40°C. Values range from 1.2 W<span>&nbsp;</span><i>m<sup>−1</sup>C<sup>−1</sup></i><span>&nbsp;</span>for a highly porous chalk to 5.1 W<span>&nbsp;</span><i>m<sup>−1</sup>C<sup>−1</sup></i><span>&nbsp;</span>for a dolomite. The thermal conductivity of magnesite (5.0) is at the high end of the range, and that for Iceland Spar Calcite (3.2) is near the middle. The values for limestones decrease linearly with increasing porosity. Dolomites of comparable porosity have greater thermal conductivities than limestones.</p><p>Water-sorbed samples have expected greater thermal conductivities than air-saturated (dry) samples of the same rock. An anomalously large increase in the thermal conductivity of a water-sorbed clayey dolomite over that of the same sample when dry is attributed to the clay fraction, which swells during water inhibition, causing more solid-to-solid contacts within the dolomite framework.</p><p>Measurements were made with a Colora Thermoconductometer. Chemical and mineralogical analyses were made and tabulated. Porosity of the rocks was determined by mercury porosimetry and also from density measurements. The Iceland Spar Calcite and magnesite were included for reference.</p>","language":"English","publisher":"Elsevier","doi":"10.1016/0013-7952(73)90003-3","issn":"00137952","usgsCitation":"Thomas, J., Frost, R., and Harvey, R., 1973, Thermal conductivity of carbonate rocks: Engineering Geology, v. 7, no. 1, p. 3-12, https://doi.org/10.1016/0013-7952(73)90003-3.","productDescription":"10 p.","startPage":"3","endPage":"12","numberOfPages":"10","costCenters":[],"links":[{"id":219333,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"7","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505bb216e4b08c986b3255bd","contributors":{"authors":[{"text":"Thomas, J. Jr.","contributorId":54727,"corporation":false,"usgs":true,"family":"Thomas","given":"J.","suffix":"Jr.","email":"","affiliations":[],"preferred":false,"id":357229,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Frost, R.R.","contributorId":87284,"corporation":false,"usgs":true,"family":"Frost","given":"R.R.","email":"","affiliations":[],"preferred":false,"id":357231,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Harvey, R.D.","contributorId":56371,"corporation":false,"usgs":true,"family":"Harvey","given":"R.D.","email":"","affiliations":[],"preferred":false,"id":357230,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70010264,"text":"70010264 - 1973 - Production of superheated steam from vapor-dominated geothermal reservoirs","interactions":[],"lastModifiedDate":"2020-12-29T14:15:38.320431","indexId":"70010264","displayToPublicDate":"1973-01-01T00:00:00","publicationYear":"1973","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1828,"text":"Geothermics","active":true,"publicationSubtype":{"id":10}},"title":"Production of superheated steam from vapor-dominated geothermal reservoirs","docAbstract":"<div id=\"abstracts\" class=\"Abstracts u-font-serif\"><div id=\"aep-abstract-id3\" class=\"abstract author\"><div id=\"aep-abstract-sec-id4\"><p>Vapor-dominated geothermal systems such as Larderello, Italy, The Geysers, California, and Matsukawa, Japan yield dry or superheated steam when exploited. Models for these systems are examined along with production data and the thermodynamic properties of water, steam and rock. It is concluded that these systems initially consist of a water and steam filled reservoir, a water-saturated cap rock, and a water or brine-saturated deep reservoir below a water table. Most liquid water in all parts of the system is relatively immobilized in small pores and crevices; steam dominates the large fractures and voids of the reservoir and is the continuous, pressure-controlling phase. With production, the pressure is lowered and the liquid water boils, causing massive transfer of heat from the rock and its eventual drying. Passage of steam through already dried rock produces superheating. After an initial vaporization of liquid water in the reservoir, the decrease in pressure produces increased boiling below the deep water table. With heavy exploitation, boiling extends deeper into hotter rock and the temperature of the steam increases. This model explains most features of the published production behavior of these systems and can be used to guide exploitation policies.</p></div></div></div><ul id=\"issue-navigation\" class=\"issue-navigation u-margin-s-bottom u-bg-grey1\"></ul>","language":"English","publisher":"Elsevier","doi":"10.1016/0375-6505(73)90022-9","issn":"03756505","usgsCitation":"Truesdell, A., and White, D., 1973, Production of superheated steam from vapor-dominated geothermal reservoirs: Geothermics, v. 2, no. 3-4, p. 154-173, https://doi.org/10.1016/0375-6505(73)90022-9.","productDescription":"20 p.","startPage":"154","endPage":"173","numberOfPages":"20","costCenters":[{"id":568,"text":"Southwest Biological Science Center","active":true,"usgs":true}],"links":[{"id":480661,"rank":1,"type":{"id":41,"text":"Open Access External Repository Page"},"url":"https://repositorio.unal.edu.co/handle/unal/79530","text":"External Repository"},{"id":218710,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"2","issue":"3-4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a8de7e4b0c8380cd7eed4","contributors":{"authors":[{"text":"Truesdell, A.H.","contributorId":52566,"corporation":false,"usgs":false,"family":"Truesdell","given":"A.H.","email":"","affiliations":[{"id":6672,"text":"former: USGS Southwest Biological Science Center, Colorado Plateau Research Station, Flagstaff, AZ. Current address:  TN-SCORE, Univ of Tennessee, Knoxville, TN, e-mail: jennen@gmail.com","active":true,"usgs":false}],"preferred":false,"id":358477,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"White, D. E.","contributorId":20729,"corporation":false,"usgs":false,"family":"White","given":"D. E.","affiliations":[{"id":6672,"text":"former: USGS Southwest Biological Science Center, Colorado Plateau Research Station, Flagstaff, AZ. Current address:  TN-SCORE, Univ of Tennessee, Knoxville, TN, e-mail: jennen@gmail.com","active":true,"usgs":false}],"preferred":false,"id":358476,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70009772,"text":"70009772 - 1973 - Ultrafiltration by a compacted clay membrane-I. Oxygen and hydrogen isotopic fractionation","interactions":[],"lastModifiedDate":"2020-12-29T19:56:46.436239","indexId":"70009772","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":"Ultrafiltration by a compacted clay membrane-I. Oxygen and hydrogen isotopic fractionation","docAbstract":"<div id=\"abstracts\" class=\"Abstracts u-font-serif\"><div id=\"aep-abstract-id7\" class=\"abstract author\"><div id=\"aep-abstract-sec-id8\"><p>Laboratory experiments were carried out to determine the magnitude of the isotopic fractionation of distilled water and of 0.01 N NaCl forced to flow at ambient temperature under a hydraulic pressure drop of 100 bars across a montmorillonite disc compacted to a porosity of 35 per cent by a pressure of 330 bars. The ultrafiltrates in both experiments were depleted in D by 2.5%. and in O<sup>18</sup><span>&nbsp;</span>by 0.8%. relative to the residual solution. No additional isotopic fractionation due to a salt filtering mechanism was observed at NaCl concentrations up to 0.01 N. Adsorption is most likely the principal mechanism which produces isotopic fractionation, but molecular diffusion may play a minor role.</p><p>The results suggest that oxygen and hydrogen isotopic fractionation of ground water during passage through compacted clayey sediments should be a common occurrence, in accord with published interpretations of isotopic data from the Illinois and Alberta basins.</p></div></div></div>","language":"English","publisher":"Elsevier","doi":"10.1016/0016-7037(73)90105-1","issn":"00167037","usgsCitation":"Coplen, T., and Hanshaw, B., 1973, Ultrafiltration by a compacted clay membrane-I. Oxygen and hydrogen isotopic fractionation: Geochimica et Cosmochimica Acta, v. 37, no. 10, p. 2295-2310, https://doi.org/10.1016/0016-7037(73)90105-1.","productDescription":"16 p.","startPage":"2295","endPage":"2310","numberOfPages":"16","costCenters":[],"links":[{"id":219490,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"37","issue":"10","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505bbbfee4b08c986b328969","contributors":{"authors":[{"text":"Coplen, T.B.","contributorId":34147,"corporation":false,"usgs":true,"family":"Coplen","given":"T.B.","affiliations":[],"preferred":false,"id":357106,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hanshaw, B.B.","contributorId":25928,"corporation":false,"usgs":true,"family":"Hanshaw","given":"B.B.","email":"","affiliations":[],"preferred":false,"id":357105,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70009823,"text":"70009823 - 1973 - Uranium concentration and distribution in six peridotite inclusions of probable mantle origin","interactions":[],"lastModifiedDate":"2023-12-14T00:54:14.7955","indexId":"70009823","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":"Uranium concentration and distribution in six peridotite inclusions of probable mantle origin","docAbstract":"<div id=\"abstracts\" class=\"Abstracts u-font-serif\"><div id=\"ab1\" class=\"abstract author\" lang=\"en\"><div id=\"aep-abstract-sec-id5\"><p>Fission-track activation was used to investigate uranium concentration and distribution in peridotite inclusions in alkali basalt from six localities. Whole-rock uranium concentrations range from 24 to 82 ng/g (1ng= 10<sup>−9</sup>g). Most of the uranium is uniformly distributed in the major silicate phases — olivine, orthopyroxene, and clinopyroxene. Chromian spinels may be classified into two groups on the basis of their uranium content, having either less than 10 ng/g or 100–150 ng/g U. In one sample accessory hydrous phases, phlogopite and hornblende, contain 130 and 300 ng/g U, respectively. The contact between the inclusion and the host basalt is usually quite sharp. Glassy or microcrystalline veinlets found in some samples contain more than 1μg/g(1 μg= 10<sup>−6</sup>g). Very little uranium is associated with microcrystals of apatite. Our results agree with some earlier investigators, who have concluded that suboceanic peridotites contain too little uranium to account for normal oceanic heat flow by conduction alone.</p></div></div></div>","language":"English","publisher":"Elsevier","doi":"10.1016/0012-821X(73)90138-6","issn":"0012821X","usgsCitation":"Haines, E., and Zartman, R., 1973, Uranium concentration and distribution in six peridotite inclusions of probable mantle origin: Earth and Planetary Science Letters, v. 20, no. 1, p. 45-53, https://doi.org/10.1016/0012-821X(73)90138-6.","productDescription":"9 p.","startPage":"45","endPage":"53","numberOfPages":"9","costCenters":[],"links":[{"id":219111,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"20","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505bbd9ae4b08c986b329103","contributors":{"authors":[{"text":"Haines, E.L.","contributorId":70107,"corporation":false,"usgs":true,"family":"Haines","given":"E.L.","email":"","affiliations":[],"preferred":false,"id":357228,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Zartman, R. E.","contributorId":15632,"corporation":false,"usgs":true,"family":"Zartman","given":"R. E.","affiliations":[],"preferred":false,"id":357227,"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":"<div id=\"abstracts\" class=\"Abstracts u-font-serif\"><div id=\"aep-abstract-id8\" class=\"abstract author\"><div id=\"aep-abstract-sec-id9\"><p>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 Fe<sup>2+</sup><span>&nbsp;</span>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.</p></div></div></div><ul id=\"issue-navigation\" class=\"issue-navigation u-margin-s-bottom u-bg-grey1\"></ul>","language":"English","publisher":"Elsevier","doi":"10.1016/0016-7037(73)90199-3","issn":"00167037","usgsCitation":"Senftle, F.E., Thorpe, A.N., Alexander, C., and Briggs, C., 1973, Comparison of the magnetic properties of glass from Luna 20 with similar properties of glass from the Apollo missions: Geochimica et Cosmochimica Acta, v. 37, no. 4, p. 1053-1062, https://doi.org/10.1016/0016-7037(73)90199-3.","productDescription":"10 p.","startPage":"1053","endPage":"1062","numberOfPages":"10","costCenters":[],"links":[{"id":219649,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"37","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059f8aee4b0c8380cd4d212","contributors":{"authors":[{"text":"Senftle, F. E.","contributorId":47788,"corporation":false,"usgs":true,"family":"Senftle","given":"F.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":357234,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Thorpe, A. N.","contributorId":53504,"corporation":false,"usgs":true,"family":"Thorpe","given":"A.","email":"","middleInitial":"N.","affiliations":[],"preferred":false,"id":357235,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Alexander, C.C.","contributorId":34256,"corporation":false,"usgs":true,"family":"Alexander","given":"C.C.","email":"","affiliations":[],"preferred":false,"id":357233,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Briggs, C.L.","contributorId":33048,"corporation":false,"usgs":true,"family":"Briggs","given":"C.L.","email":"","affiliations":[],"preferred":false,"id":357232,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70009771,"text":"70009771 - 1973 - Determination of indium in rocks by substoichiometric radioisotope dilution analysis","interactions":[],"lastModifiedDate":"2020-12-29T19:51:06.802233","indexId":"70009771","displayToPublicDate":"1973-01-01T00:00:00","publicationYear":"1973","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":760,"text":"Analytica Chimica Acta","active":true,"publicationSubtype":{"id":10}},"title":"Determination of indium in rocks by substoichiometric radioisotope dilution analysis","docAbstract":"<div id=\"aep-abstract-id4\" class=\"abstract author\"><div id=\"aep-abstract-sec-id5\"><p id=\"simple-para.0010\">Rocks containing 10–140 ng of indium per g are decomposed with hydrofluoric and nitric acids in the presence of<span>&nbsp;</span><sup>114</sup>In. Indium is separated from other constituents by sequential extractions of the bromide, cupferronate, and acetylacetonate, and is then reacted with a substoichiometric amont of EDTA. Excess of indium is removed by acetylacetone extraction and the specific activity of the complexed fraction is determined by counting<span>&nbsp;</span><sup>114</sup>In. Analyses of the U.S.G.S. standard rocks are reported. These show good agreement with previous neutron activation analyses. Repetitive rock analyses indicated an analytical precision of ±4–7%.</p></div></div>","language":"English","publisher":"Elsevierr","doi":"10.1016/S0003-2670(01)80230-0","issn":"00032670","usgsCitation":"Greenland, L.P., and Campbell, E., 1973, Determination of indium in rocks by substoichiometric radioisotope dilution analysis: Analytica Chimica Acta, v. 67, no. 1, p. 29-36, https://doi.org/10.1016/S0003-2670(01)80230-0.","productDescription":"8p.","startPage":"29","endPage":"36","numberOfPages":"8","costCenters":[],"links":[{"id":219489,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"67","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059ffade4b0c8380cd4f312","contributors":{"authors":[{"text":"Greenland, L. Paul","contributorId":22488,"corporation":false,"usgs":true,"family":"Greenland","given":"L.","email":"","middleInitial":"Paul","affiliations":[],"preferred":false,"id":357103,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Campbell, E.Y.","contributorId":59803,"corporation":false,"usgs":true,"family":"Campbell","given":"E.Y.","email":"","affiliations":[],"preferred":false,"id":357104,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":1007637,"text":"1007637 - 1973 - Effects of radiation on a fenced population of horned lizards (Phrynosoma platyrhinos) in southern Nevada","interactions":[],"lastModifiedDate":"2012-02-02T00:04:19","indexId":"1007637","displayToPublicDate":"1973-01-01T00:00:00","publicationYear":"1973","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2334,"text":"Journal of Herpetology","active":true,"publicationSubtype":{"id":10}},"title":"Effects of radiation on a fenced population of horned lizards (Phrynosoma platyrhinos) in southern Nevada","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Journal of Herpetology","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","usgsCitation":"Medica, P., Turner, F., and Smith, D., 1973, Effects of radiation on a fenced population of horned lizards (Phrynosoma platyrhinos) in southern Nevada: Journal of Herpetology, v. 7, p. 79-85.","productDescription":"p. 79-85","startPage":"79","endPage":"85","numberOfPages":"7","costCenters":[{"id":651,"text":"Western Ecological Research Center","active":true,"usgs":true}],"links":[{"id":130215,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"7","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a29e4b07f02db611a06","contributors":{"authors":[{"text":"Medica, P.A.","contributorId":77079,"corporation":false,"usgs":true,"family":"Medica","given":"P.A.","email":"","affiliations":[],"preferred":false,"id":315763,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Turner, F.B.","contributorId":95414,"corporation":false,"usgs":true,"family":"Turner","given":"F.B.","email":"","affiliations":[],"preferred":false,"id":315765,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Smith, D.D.","contributorId":85539,"corporation":false,"usgs":true,"family":"Smith","given":"D.D.","email":"","affiliations":[],"preferred":false,"id":315764,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70045441,"text":"70045441 - 1973 - Annual compilation and analysis of hydrologic data for urban studies  in the Austin, Texas Metropolitan Area, 1971","interactions":[],"lastModifiedDate":"2016-08-23T14:00:15","indexId":"70045441","displayToPublicDate":"1973-01-01T00:00:00","publicationYear":"1973","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":2,"text":"State or Local Government Series"},"seriesTitle":{"id":128,"text":"Open-File Report","active":false,"publicationSubtype":{"id":2}},"title":"Annual compilation and analysis of hydrologic data for urban studies  in the Austin, Texas Metropolitan Area, 1971","docAbstract":"<p>The U.S. Geological Survey, in cooperation with the Texas Water Development Board, began hydrologic studies in the Austin urban area in 1954. The objectives of this project are as follows: </p><p style=\"padding-left: 30px;\" data-mce-style=\"padding-left: 30px;\">1. To determine the effects of progressive urbanization on infiltration, rates of peak discharge, and rainfall-runoff relations in the Waller Creek watershed. </p><p style=\"padding-left: 30px;\" data-mce-style=\"padding-left: 30px;\">2. To provide rainfall-and-runoff data from the rural Wilbarger Creek watershed to be used for comparative purposes in determining the effects of existing and progressive urbanization in the Waller Creek watershed. </p><p style=\"padding-left: 30px;\" data-mce-style=\"padding-left: 30px;\">3. To provide applied research facilities for studies at the University of Texas at Austin. </p><p style=\"padding-left: 30px;\" data-mce-style=\"padding-left: 30px;\">The purpose of this report is to present rainfall-and-runoff data for the Waller Creek and Wilbarger Creek study areas for the 1971 water year (October 1, 1970, to September 30, 1971). </p><p style=\"padding-left: 30px;\" data-mce-style=\"padding-left: 30px;\">To facilitate the publication and distribution of this report at the earliest feasible time, certain material has been included that does not conform to the formal publication standards of the U.S. Geological Survey. </p>","language":"English","publisher":"U.S. Gelogical Survey, Water Resources Division","publisherLocation":"Reston, VA","collaboration":"Prepared in cooperation with the Texas Water Development Board","usgsCitation":"Tovar, F., 1973, Annual compilation and analysis of hydrologic data for urban studies  in the Austin, Texas Metropolitan Area, 1971: Open-File Report, iv, 73 p.","productDescription":"iv, 73 p.","numberOfPages":"77","additionalOnlineFiles":"N","temporalStart":"1970-10-01","temporalEnd":"1971-09-30","costCenters":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"links":[{"id":271000,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/unnumbered/70045441/report-thumb.jpg"},{"id":272734,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/unnumbered/70045441/report.pdf"}],"country":"United States","state":"Texas","city":"Austin","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"516e72dee4b00154e4368b7f","contributors":{"authors":[{"text":"Tovar, F.H.","contributorId":42116,"corporation":false,"usgs":true,"family":"Tovar","given":"F.H.","email":"","affiliations":[],"preferred":false,"id":477505,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70159880,"text":"70159880 - 1973 - The Great Tunisian Flood","interactions":[],"lastModifiedDate":"2015-12-02T13:44:27","indexId":"70159880","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":"The Great Tunisian Flood","docAbstract":"<p>In the autumn of 1969, unusual meteorological conditions&nbsp;over Europe and northern Africa caused an enormous persistent desert&nbsp;storm in Tunisia and eastern Algeria. Poorly developed drainage&nbsp;patterns and gypsum-encrusted surfaces of these desert regions intensified&nbsp;effects of the storm and contributed to the heavy loss of life and&nbsp;property. Destruction of Roman bridges suggests that such storms may&nbsp;have recurrence probabilities of several thousands of years. The event&nbsp;also suggests that, although desert storms are less frequent than those of&nbsp;temperate regions, they can be similar in magnitude.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","usgsCitation":"Clarke, F., 1973, The Great Tunisian Flood: Journal of Research of the U.S. Geological Survey, v. 1, no. 1, p. 121-124.","productDescription":"4 p.","startPage":"121","endPage":"124","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":311794,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":311793,"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"}}],"country":"Algeria, Tunisia","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -4.658203125,\n              35.92464453144099\n            ],\n            [\n              5.4931640625,\n              38.856820134743636\n            ],\n            [\n              11.865234375,\n              37.71859032558816\n            ],\n            [\n              14.809570312499998,\n              32.62087018318113\n            ],\n            [\n              12.6123046875,\n              20.879342971957897\n            ],\n            [\n              0.263671875,\n              17.476432197195532\n            ],\n            [\n              -11.3818359375,\n              26.745610382199022\n            ],\n            [\n              -4.658203125,\n              35.92464453144099\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"1","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"56602440e4b071e7ea544cb6","contributors":{"authors":[{"text":"Clarke, Frank Eldridge","contributorId":107255,"corporation":false,"usgs":true,"family":"Clarke","given":"Frank Eldridge","affiliations":[],"preferred":false,"id":580867,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70010934,"text":"70010934 - 1973 - Determination of lead, uranium, thorium, and thallium in silicate glass standard materials by isotope dilution mass spectrometry","interactions":[],"lastModifiedDate":"2023-03-17T16:48:17.539084","indexId":"70010934","displayToPublicDate":"1973-01-01T00:00:00","publicationYear":"1973","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":761,"text":"Analytical Chemistry","active":true,"publicationSubtype":{"id":10}},"title":"Determination of lead, uranium, thorium, and thallium in silicate glass standard materials by isotope dilution mass spectrometry","docAbstract":"A set of four standard glasses has been prepared which have been doped with 61 different elements at the 500-, 50-, 1-, and 0.02-ppm level. The concentrations of lead, uranium, thorium, and thallium have been determined by isotope dilution mass spectrometry at a number of points in each of the glasses. The results obtained from independent determinations in two laboratories demonstrate the homogeneity of the samples and that precision of the order of 0.5% (95% L.E.) may be obtained by the method even at the 20-ppb level for these elements. The chemical and mass spectrometric procedures necessary are presented.","language":"English","publisher":"ACS Publications","doi":"10.1021/ac60328a005","usgsCitation":"Barnes, I.L., Garner, E.L., Gramlich, J.W., Moore, L.J., Murphy, T.J., Machlan, L.A., Shields, W.R., Tatsumoto, M., and Knight, R.J., 1973, Determination of lead, uranium, thorium, and thallium in silicate glass standard materials by isotope dilution mass spectrometry: Analytical Chemistry, v. 45, no. 6, p. 880-885, https://doi.org/10.1021/ac60328a005.","productDescription":"6 p.","startPage":"880","endPage":"885","numberOfPages":"6","costCenters":[],"links":[{"id":220736,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"45","issue":"6","noUsgsAuthors":false,"publicationDate":"2002-05-01","publicationStatus":"PW","scienceBaseUri":"5059ffb1e4b0c8380cd4f332","contributors":{"authors":[{"text":"Barnes, I. L.","contributorId":8342,"corporation":false,"usgs":false,"family":"Barnes","given":"I.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":359921,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Garner, E. L.","contributorId":52322,"corporation":false,"usgs":false,"family":"Garner","given":"E.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":359922,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Gramlich, J. W.","contributorId":69967,"corporation":false,"usgs":false,"family":"Gramlich","given":"J.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":359924,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Moore, L. J.","contributorId":53132,"corporation":false,"usgs":false,"family":"Moore","given":"L.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":359923,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Murphy, T. J.","contributorId":90982,"corporation":false,"usgs":false,"family":"Murphy","given":"T.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":359926,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Machlan, L. A.","contributorId":90983,"corporation":false,"usgs":false,"family":"Machlan","given":"L.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":359927,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Shields, W. R.","contributorId":7412,"corporation":false,"usgs":false,"family":"Shields","given":"W.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":359920,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Tatsumoto, Mitsunobu","contributorId":10444,"corporation":false,"usgs":true,"family":"Tatsumoto","given":"Mitsunobu","email":"","affiliations":[],"preferred":false,"id":359925,"contributorType":{"id":1,"text":"Authors"},"rank":8},{"text":"Knight, R. J.","contributorId":96255,"corporation":false,"usgs":true,"family":"Knight","given":"R.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":359928,"contributorType":{"id":1,"text":"Authors"},"rank":9}]}}
,{"id":1001622,"text":"1001622 - 1973 - Red-winged blackbirds nesting near Great Slave Lake, N.W.T","interactions":[],"lastModifiedDate":"2023-09-21T14:44:27.787391","indexId":"1001622","displayToPublicDate":"1973-01-01T00:00:00","publicationYear":"1973","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1063,"text":"Blue Jay","active":true,"publicationSubtype":{"id":10}},"title":"Red-winged blackbirds nesting near Great Slave Lake, N.W.T","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"Nature Saskatchewan","doi":"10.29173/bluejay4157","usgsCitation":"Krapu, G., 1973, Red-winged blackbirds nesting near Great Slave Lake, N.W.T: Blue Jay, v. 31, no. 3, p. 147-149, https://doi.org/10.29173/bluejay4157.","productDescription":"3 p.","startPage":"147","endPage":"149","costCenters":[{"id":480,"text":"Northern Prairie Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":480664,"rank":2,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.29173/bluejay4157","text":"Publisher Index Page"},{"id":130526,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"Canada","state":"Northwest Territories","otherGeospatial":"Great Slave Lake","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -108.46634810500355,\n              63.13976004970118\n            ],\n            [\n              -118.08698043345574,\n              63.13976004970118\n            ],\n            [\n              -118.08698043345574,\n              60.61830047095037\n            ],\n            [\n              -108.46634810500355,\n              60.61830047095037\n            ],\n            [\n              -108.46634810500355,\n              63.13976004970118\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","volume":"31","issue":"3","noUsgsAuthors":false,"publicationDate":"1970-01-01","publicationStatus":"PW","scienceBaseUri":"4f4e4a60e4b07f02db635327","contributors":{"authors":[{"text":"Krapu, Gary 0000-0001-8482-6130 gkrapu@usgs.gov","orcid":"https://orcid.org/0000-0001-8482-6130","contributorId":168791,"corporation":false,"usgs":true,"family":"Krapu","given":"Gary","email":"gkrapu@usgs.gov","affiliations":[{"id":480,"text":"Northern Prairie Wildlife Research Center","active":true,"usgs":true}],"preferred":true,"id":311364,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70174173,"text":"70174173 - 1973 - Floods in Iowa: Technical manual for estimating their magnitude and frequency","interactions":[],"lastModifiedDate":"2025-07-29T18:14:39.097091","indexId":"70174173","displayToPublicDate":"1973-01-01T00:00:00","publicationYear":"1973","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":2,"text":"State or Local Government Series"},"seriesTitle":{"id":5108,"text":"Iowa Natural Resources Council Bulletin","active":true,"publicationSubtype":{"id":2}},"seriesNumber":"11","title":"Floods in Iowa: Technical manual for estimating their magnitude and frequency","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"Iowa Natural Resources Council","usgsCitation":"Lara, O.G., 1973, Floods in Iowa: Technical manual for estimating their magnitude and frequency: Iowa Natural Resources Council Bulletin 11, 56 p.","productDescription":"56 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":351,"text":"Iowa Water Science Center","active":true,"usgs":true}],"links":[{"id":493122,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/unnumbered/70174173/IA-NRC_bull11.pdf","text":"Report","size":"3.9 MB","linkFileType":{"id":1,"text":"pdf"}},{"id":324498,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"57739fb0e4b07657d1a90cc8","contributors":{"authors":[{"text":"Lara, Oscar G.","contributorId":19555,"corporation":false,"usgs":true,"family":"Lara","given":"Oscar","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":641028,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70009773,"text":"70009773 - 1973 - Point of zero charge of weathered forsterite","interactions":[],"lastModifiedDate":"2020-12-29T19:44:51.597727","indexId":"70009773","displayToPublicDate":"1973-01-01T00:00:00","publicationYear":"1973","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":"Point of zero charge of weathered forsterite","docAbstract":"<div id=\"abstracts\" class=\"Abstracts u-font-serif\"><div id=\"aep-abstract-id4\" class=\"abstract author\"><div id=\"aep-abstract-sec-id5\"><p id=\"simple-para.0010\">The point of zero charge of forsterite shifts from an estimated 8.9 for the unaltered mineral to 8.4 and 8.0, respectively, after being weathered artificially for 1 h and 4 h. These results corroborate the presence of magnesium-deficient surfaces on the weathered minerals, also indicated by chemical analyses of the solutions. H<sup>+</sup><span>&nbsp;</span>and OH<sup>−</sup><span>&nbsp;</span>are shown to be potential-determining ions in this system</p></div></div></div><ul id=\"issue-navigation\" class=\"issue-navigation u-margin-s-bottom u-bg-grey1\"></ul>","language":"English","publisher":"Elsevier","doi":"10.1016/0009-2541(73)90112-5","issn":"00092541","usgsCitation":"Luce, R., and Parks, G.A., 1973, Point of zero charge of weathered forsterite: Chemical Geology, v. 12, no. 2, p. 147-153, https://doi.org/10.1016/0009-2541(73)90112-5.","productDescription":"7 p.","startPage":"147","endPage":"153","numberOfPages":"7","costCenters":[],"links":[{"id":219491,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"12","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a7cb3e4b0c8380cd79b24","contributors":{"authors":[{"text":"Luce, R.W.","contributorId":39862,"corporation":false,"usgs":true,"family":"Luce","given":"R.W.","email":"","affiliations":[],"preferred":false,"id":357107,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Parks, George A.","contributorId":41433,"corporation":false,"usgs":true,"family":"Parks","given":"George","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":357108,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70009774,"text":"70009774 - 1973 - The selenium content of U.S.G.S. standard rocks","interactions":[],"lastModifiedDate":"2020-12-29T19:47:52.513022","indexId":"70009774","displayToPublicDate":"1973-01-01T00:00:00","publicationYear":"1973","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":"The selenium content of U.S.G.S. standard rocks","docAbstract":"<div id=\"abstracts\" class=\"Abstracts u-font-serif\"><div id=\"aep-abstract-id5\" class=\"abstract author\"><div id=\"aep-abstract-sec-id6\"><p id=\"simple-para.0010\">Selenium was determined in duplicate portions from three bottles of six U.S.G.S. standard rocks by a spect rofluorimetric procedure. The following averages, as p.p.m. Se, were obtained: PCC-1, 0.031; GSP-1, 0.088; BCR-1, 0.12; SCo-1, 0.91; MAG-1, 1.3; and SGR-1, 3.7. One-way analysis of variance of the several sets of data showed no significant differences in the selenium content among bottles of any specific rock; these samples may be accepted as homogeneous for their selenium contents by this analytical method.</p></div></div></div><ul id=\"issue-navigation\" class=\"issue-navigation u-margin-s-bottom u-bg-grey1\"></ul>","language":"English","publisher":"Elsevier","doi":"10.1016/0009-2541(73)90030-2","issn":"00092541","usgsCitation":"Schnepfe, M., and Flanagan, F., 1973, The selenium content of U.S.G.S. standard rocks: Chemical Geology, v. 12, no. 1, p. 77-80, https://doi.org/10.1016/0009-2541(73)90030-2.","productDescription":"4 p.","startPage":"77","endPage":"80","numberOfPages":"4","costCenters":[],"links":[{"id":219567,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"12","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505bb00be4b08c986b324bbf","contributors":{"authors":[{"text":"Schnepfe, M. M.","contributorId":93622,"corporation":false,"usgs":true,"family":"Schnepfe","given":"M. M.","affiliations":[],"preferred":false,"id":357110,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Flanagan, F.J.","contributorId":50139,"corporation":false,"usgs":true,"family":"Flanagan","given":"F.J.","email":"","affiliations":[],"preferred":false,"id":357109,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70182491,"text":"70182491 - 1973 - Pathophysiology of IHN virus in rainbow trout","interactions":[],"lastModifiedDate":"2017-02-23T12:38:29","indexId":"70182491","displayToPublicDate":"1973-01-01T00:00:00","publicationYear":"1973","noYear":false,"publicationType":{"id":21,"text":"Thesis"},"publicationSubtype":{"id":28,"text":"Thesis"},"title":"Pathophysiology of IHN virus in rainbow trout","docAbstract":"<p>No abstract available&nbsp;</p>","language":"English","publisher":"University of Washington","usgsCitation":"Amend, D., 1973, Pathophysiology of IHN virus in rainbow trout, 102 p. .","productDescription":"102 p. ","costCenters":[{"id":654,"text":"Western Fisheries Research Center","active":true,"usgs":true}],"links":[{"id":336103,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"publicComments":"Ph.D. Dissertation","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"58b002dfe4b01ccd54fb283f","contributors":{"authors":[{"text":"Amend, D.F.","contributorId":63082,"corporation":false,"usgs":true,"family":"Amend","given":"D.F.","email":"","affiliations":[],"preferred":false,"id":671251,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
]}