{"pageNumber":"6827","pageRowStart":"170650","pageSize":"25","recordCount":184743,"records":[{"id":2001402,"text":"2001402 - 1960 - Microhematocrit as a tool in fishery research and management","interactions":[],"lastModifiedDate":"2012-02-02T00:15:02","indexId":"2001402","displayToPublicDate":"1960-01-01T02:00:00","publicationYear":"1960","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":1,"text":"Federal Government Series"},"seriesTitle":{"id":84,"text":"Special Scientific Report - Fisheries","active":false,"publicationSubtype":{"id":1}},"seriesNumber":"341","title":"Microhematocrit as a tool in fishery research and management","docAbstract":"No abstract available at this time","language":"English","publisher":"U.S. Fish and Wildlife Service","collaboration":"80/FH","usgsCitation":"Snieszko, S.F., Camper, J., Howard, F., and Pettijohn, L., 1960, Microhematocrit as a tool in fishery research and management: Special Scientific Report - Fisheries 341, 15 p.","productDescription":"15 p.","startPage":"0","endPage":"15","numberOfPages":"15","costCenters":[{"id":365,"text":"Leetown Science Center","active":true,"usgs":true}],"links":[{"id":198179,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a51e4b07f02db629d53","contributors":{"authors":[{"text":"Snieszko, S. F.","contributorId":13169,"corporation":false,"usgs":true,"family":"Snieszko","given":"S.","middleInitial":"F.","affiliations":[],"preferred":false,"id":325655,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Camper, J.","contributorId":70884,"corporation":false,"usgs":true,"family":"Camper","given":"J.","affiliations":[],"preferred":false,"id":325658,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Howard, F.","contributorId":20862,"corporation":false,"usgs":true,"family":"Howard","given":"F.","email":"","affiliations":[],"preferred":false,"id":325656,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Pettijohn, L.L.","contributorId":32878,"corporation":false,"usgs":true,"family":"Pettijohn","given":"L.L.","email":"","affiliations":[],"preferred":false,"id":325657,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":81355,"text":"81355 - 1960 - Surface currents in Lake Michigan, 1954 and 1955","interactions":[],"lastModifiedDate":"2016-03-10T13:43:24","indexId":"81355","displayToPublicDate":"1960-01-01T00:00:00","publicationYear":"1960","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":1,"text":"Federal Government Series"},"seriesTitle":{"id":84,"text":"Special Scientific Report - Fisheries","active":false,"publicationSubtype":{"id":1}},"seriesNumber":"338","title":"Surface currents in Lake Michigan, 1954 and 1955","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Fish and Wildlife Service","usgsCitation":"Johnson, J.H., 1960, Surface currents in Lake Michigan, 1954 and 1955: Special Scientific Report - Fisheries 338, 120 p.","productDescription":"120 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":324,"text":"Great Lakes Science Center","active":true,"usgs":true}],"links":[{"id":198914,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":101766,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://hdl.handle.net/2027/mdp.39015045826206?urlappend=%3Bseq=491"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4affe4b07f02db697e9a","contributors":{"authors":[{"text":"Johnson, James H. 0000-0002-5619-3871 jhjohnson@usgs.gov","orcid":"https://orcid.org/0000-0002-5619-3871","contributorId":389,"corporation":false,"usgs":true,"family":"Johnson","given":"James","email":"jhjohnson@usgs.gov","middleInitial":"H.","affiliations":[{"id":324,"text":"Great Lakes Science Center","active":true,"usgs":true}],"preferred":true,"id":295280,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70182052,"text":"70182052 - 1960 - A comparative study of the causative agent of a mycobacterial disease of salmonid fishes. I. A comparison of the staining characteristics of the fish disease with human tuberculosis in sections stained by the Fite-Faraco and Ziehl-Neelsen methods","interactions":[],"lastModifiedDate":"2017-02-15T14:23:58","indexId":"70182052","displayToPublicDate":"1960-01-01T00:00:00","publicationYear":"1960","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":5030,"text":"American Review of Respiratory Disease","active":true,"publicationSubtype":{"id":10}},"title":"A comparative study of the causative agent of a mycobacterial disease of salmonid fishes. I. A comparison of the staining characteristics of the fish disease with human tuberculosis in sections stained by the Fite-Faraco and Ziehl-Neelsen methods","docAbstract":"<p>No abstract available&nbsp;</p>","language":"English","publisher":"American Thoracic Society","usgsCitation":"Parisot, T., and Decker, A., 1960, A comparative study of the causative agent of a mycobacterial disease of salmonid fishes. I. A comparison of the staining characteristics of the fish disease with human tuberculosis in sections stained by the Fite-Faraco and Ziehl-Neelsen methods: American Review of Respiratory Disease, v. 82, no. 2, p. 212-222.","productDescription":"11 p.","startPage":"212","endPage":"222","costCenters":[{"id":654,"text":"Western Fisheries Research Center","active":true,"usgs":true}],"links":[{"id":335605,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":335604,"rank":1,"type":{"id":15,"text":"Index Page"},"url":"https://www.atsjournals.org/doi/abs/10.1164/arrd.1960.82.2.212?journalCode=arrd"}],"volume":"82","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"58a57710e4b057081a24eed9","contributors":{"authors":[{"text":"Parisot, T. J.","contributorId":43014,"corporation":false,"usgs":true,"family":"Parisot","given":"T. J.","affiliations":[],"preferred":false,"id":669402,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Decker, A.H.","contributorId":151173,"corporation":false,"usgs":false,"family":"Decker","given":"A.H.","email":"","affiliations":[],"preferred":false,"id":669403,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70161104,"text":"70161104 - 1960 - An illuminator for observing and photographing precipitin reactions in agar","interactions":[],"lastModifiedDate":"2016-06-17T11:28:47","indexId":"70161104","displayToPublicDate":"1960-01-01T00:00:00","publicationYear":"1960","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":5029,"text":"Journal of the Biological Photographic Association","active":true,"publicationSubtype":{"id":10}},"title":"An illuminator for observing and photographing precipitin reactions in agar","docAbstract":"<p>Abstract not available.</p>","language":"English","publisher":"Biological Photographic Association","usgsCitation":"Klontz, G., Ridgway, G., and Wilson, G., 1960, An illuminator for observing and photographing precipitin reactions in agar: Journal of the Biological Photographic Association, v. 28, p. 11-14.","productDescription":"4 p.","startPage":"11","endPage":"14","numberOfPages":"4","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":654,"text":"Western Fisheries Research Center","active":true,"usgs":true}],"links":[{"id":313329,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"28","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"57651f30e4b07657d19c7880","contributors":{"authors":[{"text":"Klontz, G.W.","contributorId":113429,"corporation":false,"usgs":true,"family":"Klontz","given":"G.W.","email":"","affiliations":[],"preferred":false,"id":584720,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Ridgway, G.J.","contributorId":151203,"corporation":false,"usgs":false,"family":"Ridgway","given":"G.J.","email":"","affiliations":[],"preferred":false,"id":584721,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Wilson, G.P.","contributorId":151204,"corporation":false,"usgs":false,"family":"Wilson","given":"G.P.","email":"","affiliations":[],"preferred":false,"id":584722,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":81379,"text":"81379 - 1960 - The true pikes","interactions":[],"lastModifiedDate":"2023-04-05T16:50:30.945833","indexId":"81379","displayToPublicDate":"1960-01-01T00:00:00","publicationYear":"1960","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":1,"text":"Federal Government Series"},"seriesTitle":{"id":29,"text":"Fishery Leaflet","active":false,"publicationSubtype":{"id":1}},"seriesNumber":"496","title":"The true pikes","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Fish and Wildlife Service","usgsCitation":"Van Oosten, J., 1960, The true pikes: Fishery Leaflet 496, 9 p.","productDescription":"9 p.","costCenters":[{"id":324,"text":"Great Lakes Science Center","active":true,"usgs":true}],"links":[{"id":198182,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":415253,"rank":2,"type":{"id":15,"text":"Index Page"},"url":"https://spo.nmfs.noaa.gov/content/true-pikes","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0ee4b07f02db5fdb40","contributors":{"authors":[{"text":"Van Oosten, John","contributorId":23479,"corporation":false,"usgs":true,"family":"Van Oosten","given":"John","email":"","affiliations":[],"preferred":false,"id":295309,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70171162,"text":"70171162 - 1960 - Great Lakes limnological investigations","interactions":[],"lastModifiedDate":"2016-05-24T10:46:15","indexId":"70171162","displayToPublicDate":"1960-01-01T00:00:00","publicationYear":"1960","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"Great Lakes limnological investigations","docAbstract":"<p>No abstract available.</p>","largerWorkType":{"id":24,"text":"Conference Paper"},"largerWorkTitle":"Proceedings of the 3rd Conference on Great Lakes Research","largerWorkSubtype":{"id":19,"text":"Conference Paper"},"conferenceTitle":"3rd Conference on Great Lakes Research","conferenceDate":"May 6-7, 1959","language":"English","publisher":"University of Michigan","usgsCitation":"Beeton, A.M., 1960, Great Lakes limnological investigations, <i>in</i> Proceedings of the 3rd Conference on Great Lakes Research, May 6-7, 1959, p. 123-128.","productDescription":"6 p.","startPage":"123","endPage":"128","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":324,"text":"Great Lakes Science Center","active":true,"usgs":true}],"links":[{"id":321602,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"574d654be4b07e28b6684175","contributors":{"authors":[{"text":"Beeton, Alfred M.","contributorId":94247,"corporation":false,"usgs":true,"family":"Beeton","given":"Alfred","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":630143,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70010642,"text":"70010642 - 1960 - Potentiometric titration and equivalent weight of humic acid","interactions":[],"lastModifiedDate":"2024-03-07T15:38:40.812515","indexId":"70010642","displayToPublicDate":"1960-01-01T00:00:00","publicationYear":"1960","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":"Potentiometric titration and equivalent weight of humic acid","docAbstract":"<p><span>The “acid nature” of humic acid has been controversial for many years. Some investigators claim that humic acid is a true weak acid, while others feel that its behaviour during potentiometric titration can be accounted for by colloidal adsorption of hydrogen ions. The acid character of humic acid has been reinvestigated using newly-derived relationships for the titration of weak acids with strong base. Re-interpreting the potentiometric titration data published by&nbsp;</span><span class=\"small-caps\">Thiele</span><span>&nbsp;and&nbsp;</span><span class=\"small-caps\">Kettner</span><span>&nbsp;in 1953, it was found that Merck humic acid behaves as a weak polyelectrolytic acid having an equivalent weight of 150, a&nbsp;</span><i>pK</i><sub><i>a</i></sub><span>&nbsp;of 6.8 to 7.0, and a titration exponent of about 4.8. Interdretation of similar data pertaining to the titration of phenol-formaldehyde and pyrogallol-formaldehyde resins, considered to be analogs for humic acid by&nbsp;</span><span class=\"small-caps\">Thiele</span><span>&nbsp;and&nbsp;</span><span class=\"small-caps\">Kettner</span><span>, leads to the conclusion that it is not possible to differentiate between adsorption and acid-base reaction for these substances.</span></p>","language":"English","publisher":"Elsevier","doi":"10.1016/0016-7037(60)90136-8","issn":"00167037","usgsCitation":"Pommer, A., and Breger, I.A., 1960, Potentiometric titration and equivalent weight of humic acid: Geochimica et Cosmochimica Acta, v. 20, no. 1, p. 30-44, https://doi.org/10.1016/0016-7037(60)90136-8.","productDescription":"15 p.","startPage":"30","endPage":"44","numberOfPages":"15","costCenters":[],"links":[{"id":219312,"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":"505a8089e4b0c8380cd7b06e","contributors":{"authors":[{"text":"Pommer, A. M.","contributorId":20795,"corporation":false,"usgs":false,"family":"Pommer","given":"A. M.","affiliations":[],"preferred":false,"id":359337,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Breger, Irving A.","contributorId":65205,"corporation":false,"usgs":true,"family":"Breger","given":"Irving","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":359338,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70010845,"text":"70010845 - 1960 - Automatic measurements and computations for radiochemical analyses","interactions":[],"lastModifiedDate":"2020-11-16T16:53:29.248599","indexId":"70010845","displayToPublicDate":"1960-01-01T00:00:00","publicationYear":"1960","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":"Automatic measurements and computations for radiochemical analyses","docAbstract":"<p>In natural radioactive sources the most important radioactive daughter products useful for geochemical studies are protactinium-231, the alpha-emitting thorium isotopes, and the radium isotopes. To resolve the abundances of these thorium and radium isotopes by their characteristic decay and growth patterns, a large number of repeated alpha activity measurements on the two chemically separated elements were made over extended periods of time. Alpha scintillation counting with automatic measurements and sample changing is used to obtain the basic count data. Generation of the required theoretical decay and growth functions, varying with time, and the least squares solution of the overdetermined simultaneous count rate equations are done with a digital computer. Examples of the complex count rate equations which may be solved and results of a natural sample containing four alpha-emitting isotopes of thorium are illustrated. These methods facilitate the determination of the radioactive sources on the large scale required for many geochemical investigations.</p>","language":"English","publisher":"American Chemical Society","doi":"10.1021/ac60165a013","usgsCitation":"Rosholt, J.N., and Dooley, J.R., 1960, Automatic measurements and computations for radiochemical analyses: Analytical Chemistry, v. 32, no. 9, p. 1093-1098, https://doi.org/10.1021/ac60165a013.","productDescription":"6 p.","startPage":"1093","endPage":"1098","numberOfPages":"6","costCenters":[],"links":[{"id":219016,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"32","issue":"9","noUsgsAuthors":false,"publicationDate":"2002-05-01","publicationStatus":"PW","scienceBaseUri":"5059eef9e4b0c8380cd4a09b","contributors":{"authors":[{"text":"Rosholt, J. N.","contributorId":11325,"corporation":false,"usgs":true,"family":"Rosholt","given":"J.","email":"","middleInitial":"N.","affiliations":[],"preferred":false,"id":359775,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Dooley, J. R. Jr.","contributorId":8110,"corporation":false,"usgs":true,"family":"Dooley","given":"J.","suffix":"Jr.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":359774,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70010643,"text":"70010643 - 1960 - Diagenesis of metabolites and a discussion of the origin of petroleum hydrocarbons","interactions":[],"lastModifiedDate":"2019-12-13T07:44:31","indexId":"70010643","displayToPublicDate":"1960-01-01T00:00:00","publicationYear":"1960","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":"Diagenesis of metabolites and a discussion of the origin of petroleum hydrocarbons","docAbstract":"<p>Proteins and carbohydrates are rapidly degraded to compounds of no direct interest in the problem of the origin of petroleum. Lignin, if carried into marine basins in the form of humic substances, is probably the major progenitor of kerogen rather than the precursor of petroleum. Pigments are but minor contributors to petroleum. The fate of fatty acids in a marine environment is not completely understood. Although they may not be directly decarboxylated biochemically, it is shown how they can be converted into oxygenated or dehydrogenated acids more reactive than the parent compounds. Illustrations are also given for Diels-Alder reactions that could account for the formation from these compounds of the alicyclic and aromatic hydrocarbons in petroleum. It is most likely that crude oil is generated in sediments containing concentrations of lipids, the character of which governs the nature of the oil that is formed.</p>","language":"English","publisher":"Elsevier","doi":"10.1016/0016-7037(60)90036-3","issn":"00167037","usgsCitation":"Breger, I.A., 1960, Diagenesis of metabolites and a discussion of the origin of petroleum hydrocarbons: Geochimica et Cosmochimica Acta, v. 19, no. 4, p. 297-308, https://doi.org/10.1016/0016-7037(60)90036-3.","productDescription":"12 p. ","startPage":"297","endPage":"308","numberOfPages":"12","costCenters":[],"links":[{"id":219313,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"19","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a0097e4b0c8380cd4f7e8","contributors":{"authors":[{"text":"Breger, Irving A.","contributorId":65205,"corporation":false,"usgs":true,"family":"Breger","given":"Irving","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":359339,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70009817,"text":"70009817 - 1960 - Equivalent weight of humic acid from peat","interactions":[],"lastModifiedDate":"2020-11-16T16:50:27.572933","indexId":"70009817","displayToPublicDate":"1960-01-01T00:00:00","publicationYear":"1960","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":"Equivalent weight of humic acid from peat","docAbstract":"<p><span>By means of discontinuous titration, the equivalent weight of humic acid isolated from a peat was found to increase from 144 to 183 between the third and fifty-second day after the humic acid was dissolved. Infra-red studies showed that the material had probably condensed with loss of carbonyl groups.</span></p>","language":"English","publisher":"Elsevier","doi":"10.1016/0016-7037(60)90137-X","usgsCitation":"Pommer, A., and Breger, I.A., 1960, Equivalent weight of humic acid from peat: Geochimica et Cosmochimica Acta, v. 20, no. 1, p. 45-50, https://doi.org/10.1016/0016-7037(60)90137-X.","productDescription":"6 p.","startPage":"45","endPage":"50","numberOfPages":"6","costCenters":[],"links":[{"id":219034,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"20","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a0a2ee4b0c8380cd5222c","contributors":{"authors":[{"text":"Pommer, A. M.","contributorId":20795,"corporation":false,"usgs":false,"family":"Pommer","given":"A. M.","affiliations":[],"preferred":false,"id":357217,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Breger, Irving A.","contributorId":65205,"corporation":false,"usgs":true,"family":"Breger","given":"Irving","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":357218,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70010849,"text":"70010849 - 1960 - How volcanoes grow","interactions":[],"lastModifiedDate":"2020-03-24T14:31:05","indexId":"70010849","displayToPublicDate":"1960-01-01T00:00:00","publicationYear":"1960","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3338,"text":"Science","active":true,"publicationSubtype":{"id":10}},"title":"How volcanoes grow","docAbstract":"Geology, geochemistry, and geophysics disclose the constitution and eruption mechanism of Hawaiian volcanoes.","language":"English","publisher":"Elsevier","doi":"10.1126/science.132.3432.925","issn":"00368075","usgsCitation":"Eaton, J.P., and Murata, K.J., 1960, How volcanoes grow: Science, v. 132, no. 3432, p. 925-938, https://doi.org/10.1126/science.132.3432.925.","productDescription":"14 p.","startPage":"925","endPage":"938","numberOfPages":"14","costCenters":[],"links":[{"id":218809,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Hawaii","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -160.11474609375,\n              22.49225722008518\n            ],\n            [\n              -160.6640625,\n              21.596150576461426\n            ],\n            [\n              -159.697265625,\n              21.657428197370653\n            ],\n            [\n              -158.62060546875,\n              21.391704731036587\n            ],\n            [\n              -157.69775390625,\n              20.715015145512087\n            ],\n            [\n              -156.533203125,\n              19.84939395842279\n            ],\n            [\n              -156.24755859375,\n              19.16592425362802\n            ],\n            [\n              -155.89599609375,\n              18.70869162255995\n            ],\n            [\n              -154.3359375,\n              19.539084135509334\n            ],\n            [\n              -155.45654296875,\n              20.817741019786485\n            ],\n            [\n              -157.060546875,\n              21.514406720030294\n            ],\n            [\n              -158.26904296875,\n              22.167057857886153\n            ],\n            [\n              -160.11474609375,\n              22.49225722008518\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"132","issue":"3432","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a326be4b0c8380cd5e7af","contributors":{"authors":[{"text":"Eaton, J. P.","contributorId":105313,"corporation":false,"usgs":true,"family":"Eaton","given":"J.","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":359782,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Murata, K. J.","contributorId":18759,"corporation":false,"usgs":true,"family":"Murata","given":"K.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":359781,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70010512,"text":"70010512 - 1960 - Effect of crystal thickness and geometry on the alpha-particle resolution of CsI (Tl)","interactions":[],"lastModifiedDate":"2020-11-16T17:06:19.631964","indexId":"70010512","displayToPublicDate":"1960-01-01T00:00:00","publicationYear":"1960","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3276,"text":"Review of Scientific Instruments","active":true,"publicationSubtype":{"id":10}},"title":"Effect of crystal thickness and geometry on the alpha-particle resolution of CsI (Tl)","docAbstract":"<p><span>The resolution of CsI(Tl) for Po</span><sup>210</sup><span>&nbsp;</span>alpha particles<span>&nbsp;has been measured as a function of crystal thickness. The best resolution of a ½‐in. diam cylindrical crystal was obtained for a thickness of 0.38 mm, and the effect of thickness on the resolution is discussed. Based on the proposed model, a conical crystal was designed, which yielded a line width of 1.8% for Po</span><sup>210</sup><span>&nbsp;</span>alpha particles<span>&nbsp;with a selected&nbsp;</span>photomultiplier tube.</p>","language":"English","publisher":"AIP Publishing","doi":"10.1063/1.1717121","usgsCitation":"Martinez, P., and Senftle, F.E., 1960, Effect of crystal thickness and geometry on the alpha-particle resolution of CsI (Tl): Review of Scientific Instruments, v. 31, no. 9, p. 974-977, https://doi.org/10.1063/1.1717121.","productDescription":"4 p.","startPage":"974","endPage":"977","numberOfPages":"4","costCenters":[],"links":[{"id":219463,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"31","issue":"9","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a05cde4b0c8380cd50f82","contributors":{"authors":[{"text":"Martinez, P.","contributorId":38706,"corporation":false,"usgs":true,"family":"Martinez","given":"P.","email":"","affiliations":[],"preferred":false,"id":359086,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Senftle, F. E.","contributorId":47788,"corporation":false,"usgs":true,"family":"Senftle","given":"F.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":359087,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70010621,"text":"70010621 - 1960 - The crystal structure of cesium biuranyl trisulphate, Cs2(UO2)2(SO4)3","interactions":[],"lastModifiedDate":"2020-11-16T16:58:18.35245","indexId":"70010621","displayToPublicDate":"1960-01-01T00:00:00","publicationYear":"1960","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2355,"text":"Journal of Inorganic and Nuclear Chemistry","active":true,"publicationSubtype":{"id":10}},"displayTitle":"The crystal structure of cesium biuranyl trisulphate, Cs<sub>2</sub>(UO<sub>2</sub>)<sub>2</sub>(SO<sub>4</sub>)<sub>3</sub>","title":"The crystal structure of cesium biuranyl trisulphate, Cs2(UO2)2(SO4)3","docAbstract":"<p>The crystal structure of the new compound Cs(UO<sub>2</sub>)<sub>2</sub>(SO<sub>4</sub>)<sub>3</sub><span>&nbsp;</span>has been determined by X-ray diffraction methods. The compound is tetragonal, space group<span>&nbsp;</span><span class=\"math\"><span id=\"MathJax-Element-1-Frame\" class=\"MathJax_SVG\" data-mathml=\"<math xmlns=&quot;http://www.w3.org/1998/Math/MathML&quot;><mtext>P</mtext><mtext>4</mtext><mtext>2</mtext><msub><mi></mi><mn>1</mn></msub><mtext>m</mtext></math>\"><span class=\"MJX_Assistive_MathML\">P42<sub>1</sub>m</span></span></span><span>&nbsp;</span>(<i>D</i><sub>2<i>d</i></sub><sup>3</sup>), with a = 9·62 ± 0·02,<span>&nbsp;</span><span class=\"math\"><span id=\"MathJax-Element-2-Frame\" class=\"MathJax_SVG\" data-mathml=\"<math xmlns=&quot;http://www.w3.org/1998/Math/MathML&quot;><mtext>c = 8&amp;#xB7;13 &amp;#xB1; 0&amp;#xB7;01</mtext><mtext>A</mtext><mtext>&amp;#x30A;</mtext></math>\"><span class=\"MJX_Assistive_MathML\">c = 8·13 ± 0·01Å</span></span></span>, and<span>&nbsp;</span><i>Z</i><span>&nbsp;</span>= 2; s.g. (calc.) = 4·80 ± 0·03, s.g. (obs.) = 4·74 ± 0·05. The compound forms plates parallel to (001) bounded by the form (110). Intensity data were obtained from Buerger precession photographs of the (<i>hk</i>0) and (0<i>kl</i>) reciprocal lattice nets. No corrections for absorption were made. The co-ordinates of the U and Cs atoms were obtained by interpretation of the Patterson projections normal to (001) and (100) and a plausible structure was derived from electron density projections. The final parameters of the structure were determined from subtraction electron density maps, least squares analysis of the structure factors, and spatial considerations.</p><p>The compound has a layer structure consisting of (UO<sub>2</sub>)<sub>2</sub>(SO<sub>4</sub>)<sub>3</sub>]<sub><i>n</i></sub><sup>2<i>n</i>−</sup><span>&nbsp;</span>sheets paralle to (001), tied together by cesium ions. The UO<sub>2</sub><sup>2+</sup><span>&nbsp;</span>group is co-ordinated by five sulphate oxygens which form a nearly plane pentagon approximately normal to the uranyl axis. The Cs<sub>2</sub><span>&nbsp;</span>atom is co-ordinated by twelve oxygen atoms and the Cs<sub>1</sub><span>&nbsp;</span>atom by eight oxygen atoms.</p><p>X-ray and optical data are also given for the compound Rb<sub>2</sub>UO<sub>2</sub>(SO<sub>4</sub>)<sub>2</sub>·2H<sub>2</sub>O.</p>","language":"English","publisher":"Elsevier","doi":"10.1016/0022-1902(60)80063-2","usgsCitation":"Ross, M., and Evans, H.T., 1960, The crystal structure of cesium biuranyl trisulphate, Cs2(UO2)2(SO4)3: Journal of Inorganic and Nuclear Chemistry, v. 15, no. 3-4, p. 338-351, https://doi.org/10.1016/0022-1902(60)80063-2.","productDescription":"14 p.","startPage":"338","endPage":"351","numberOfPages":"14","costCenters":[],"links":[{"id":219248,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"15","issue":"3-4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505baa74e4b08c986b322843","contributors":{"authors":[{"text":"Ross, M.","contributorId":8026,"corporation":false,"usgs":true,"family":"Ross","given":"M.","email":"","affiliations":[],"preferred":false,"id":359279,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Evans, H. T. Jr.","contributorId":41859,"corporation":false,"usgs":true,"family":"Evans","given":"H.","suffix":"Jr.","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":359280,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70010620,"text":"70010620 - 1960 - Determination of niobium in the parts per million range in rocks","interactions":[],"lastModifiedDate":"2020-08-31T16:04:51.909499","indexId":"70010620","displayToPublicDate":"1960-01-01T00:00:00","publicationYear":"1960","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 niobium in the parts per million range in rocks","docAbstract":"A modified niobium thiocyanate spectrophotometric procedure relatively insensitive to titanium interference is presented. Elements such as tungsten, molybdenum, vanadium, and rhenium, which seriously interfere in the spectrophotometric determination of niobium, are separated by simple sodium hydroxide fusion and leach; iron and magnesium are used as carriers for the niobium. Tolerance limits are given for 28 elements in the spectrophotometric method. Specific application is made to the determination of niobium in the parts per million range in rocks. The granite G-1 contains 0.0022% niobium and the diabase W-1 0.00096% niobium.","language":"English","publisher":"ACS Publications","doi":"10.1021/ac60157a035","usgsCitation":"Grimaldi, F.S., 1960, Determination of niobium in the parts per million range in rocks: Analytical Chemistry, v. 32, no. 1, p. 119-121, https://doi.org/10.1021/ac60157a035.","productDescription":"3 p.","startPage":"119","endPage":"121","numberOfPages":"3","costCenters":[],"links":[{"id":219247,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"32","issue":"1","noUsgsAuthors":false,"publicationDate":"2002-05-01","publicationStatus":"PW","scienceBaseUri":"5059ffb9e4b0c8380cd4f365","contributors":{"authors":[{"text":"Grimaldi, F. S.","contributorId":94286,"corporation":false,"usgs":true,"family":"Grimaldi","given":"F.","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":359278,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":1003293,"text":"1003293 - 1960 - An outbreak of columnaris disease in stonerollers","interactions":[],"lastModifiedDate":"2025-07-31T15:24:02.833925","indexId":"1003293","displayToPublicDate":"1960-01-01T00:00:00","publicationYear":"1960","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3196,"text":"Progressive Fish-Culturist","active":true,"publicationSubtype":{"id":10}},"title":"An outbreak of columnaris disease in stonerollers","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"Oxford Academic","doi":"10.1577/1548-8659(1960)22[102:AOOCDI]2.0.CO;2","usgsCitation":"Lennon, R.E., and Parker, P.S., 1960, An outbreak of columnaris disease in stonerollers: Progressive Fish-Culturist, v. 22, no. 3, https://doi.org/10.1577/1548-8659(1960)22[102:AOOCDI]2.0.CO;2.","productDescription":"1 p.","startPage":"102","costCenters":[{"id":606,"text":"Upper Midwest Environmental Sciences Center","active":true,"usgs":true}],"links":[{"id":129590,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"22","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad6e4b07f02db6841ec","contributors":{"authors":[{"text":"Lennon, R. E.","contributorId":37275,"corporation":false,"usgs":true,"family":"Lennon","given":"R.","middleInitial":"E.","affiliations":[],"preferred":false,"id":313080,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Parker, P. S.","contributorId":8043,"corporation":false,"usgs":true,"family":"Parker","given":"P.","middleInitial":"S.","affiliations":[],"preferred":false,"id":313079,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":1000164,"text":"1000164 - 1960 - Age and growth of the whitefish Coregonus clupeaformis, of Munising Bay, Lake Superior","interactions":[],"lastModifiedDate":"2013-02-04T11:43:10","indexId":"1000164","displayToPublicDate":"1960-01-01T00:00:00","publicationYear":"1960","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":"Age and growth of the whitefish Coregonus clupeaformis, of Munising Bay, Lake Superior","docAbstract":"This study is based on a sample of 415 whitefish collected in 1953 from an unexploited population in Munising Bay, Lake Superior.  Gill-net and trawl catches had different length-frequency distributions and age compositions, but estimates of growth from the two catches were very similar.  The body-scale relation is a straight line with an intercept of 1.5 inches.  Weight of Munising Bay whitefish captured in June increased as the 3.17 power of the length.  Growth in length and weight of Munising Bay whitefish was the slowest yet reported from Great Lakes waters.  Munising Bay whitefish required nearly 8 years to reach a length of 10 inches and a full 13 years to reach 15 inches.  Slightly more than 8 years were required to reach a weight of 8 ounces and a little less than 14 years to reach 1 pound.  The sex ratio of the Munising Bay whitefish exhibited no systematic change with an increase in age.  The entire sample for which ages were determined contained 52 percent males.  Munising Bay whitefish matured at much shorter lengths but at a greater age than reported for other Great Lakes whitefish populations.  The smallest mature males were in the 11.5- to 11.9-inch length interval (age-group VII) and all males longer than 14.4 inches (age-group XII) were mature.  The first mature females appeared at 12.0-12.4 inches (age-group X) and all females longer than 14.9 inches (age-group XII) were mature.  The more rapidly growing individuals matured earlier than the slow-growing ones.","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(1960)89[323:AAGOTW]2.0.CO;2","collaboration":"Out-of-print","usgsCitation":"Edsall, T.A., 1960, Age and growth of the whitefish Coregonus clupeaformis, of Munising Bay, Lake Superior: Transactions of the American Fisheries Society, v. 89, no. 4, p. 323-332, https://doi.org/10.1577/1548-8659(1960)89[323:AAGOTW]2.0.CO;2.","productDescription":"10 p.","startPage":"323","endPage":"332","costCenters":[{"id":324,"text":"Great Lakes Science Center","active":true,"usgs":true}],"links":[{"id":131718,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":266924,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1577/1548-8659(1960)89[323:AAGOTW]2.0.CO;2"}],"volume":"89","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae4e4b07f02db6899a5","contributors":{"authors":[{"text":"Edsall, Thomas A.","contributorId":84302,"corporation":false,"usgs":true,"family":"Edsall","given":"Thomas","email":"","middleInitial":"A.","affiliations":[{"id":324,"text":"Great Lakes Science Center","active":true,"usgs":true}],"preferred":false,"id":308172,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":1000104,"text":"1000104 - 1960 - The vertical migration of Mysis relicta in Lakes Huron and Michigan","interactions":[],"lastModifiedDate":"2016-03-10T13:48:20","indexId":"1000104","displayToPublicDate":"1960-01-01T00:00:00","publicationYear":"1960","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":"The vertical migration of Mysis relicta in Lakes Huron and Michigan","docAbstract":"<p><span>During the day&nbsp;</span><i>Mysis relicta</i><span>&nbsp;could be taken only near the bottom of Lakes Huron and Michigan. In the evening they migrated into the overlying strata as the surface light intensity decreased from 15 to 1 foot-candles. Frequently the mysids migrated through the metalimnion when first ascending, but later in the night the majority occurred in or immediately below this layer. As the length of day decreased following the summer solstice, the mysids ascended progressively earlier each evening and descended later each morning (they descended when the surface light intensity was increasing from 10</span><sup>&minus;3</sup><span>&nbsp;to 10</span><sup>&minus;2</sup><span>&nbsp;foot-candle). Moonlight and fog influenced the extent and time of vertical migration.The optimum light intensity for mysids is so low that they are concentrated near the bottom during the day. As the light decreases at sunset, they move upward rapidly; possibly because of a positive reaction to decreasing light. Their night-time distribution is determined by their response to the existing light and thermal conditions. Their dawn descent may be due to a photo-negative condition which originated during the night.</span></p>","language":"English","publisher":"NRC Research Press","doi":"10.1139/f60-037","usgsCitation":"Beeton, A.M., 1960, The vertical migration of Mysis relicta in Lakes Huron and Michigan: Journal of the Fisheries Research Board of Canada, v. 17, no. 4, p. 517-539, https://doi.org/10.1139/f60-037.","productDescription":"23 p.","startPage":"517","endPage":"539","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":324,"text":"Great Lakes Science Center","active":true,"usgs":true}],"links":[{"id":128472,"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":"4f4e4a09e4b07f02db5faae1","contributors":{"authors":[{"text":"Beeton, Alfred M.","contributorId":94247,"corporation":false,"usgs":true,"family":"Beeton","given":"Alfred","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":308084,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70185557,"text":"70185557 - 1960 - River meanders","interactions":[],"lastModifiedDate":"2017-03-23T16:07:37","indexId":"70185557","displayToPublicDate":"1960-01-01T00:00:00","publicationYear":"1960","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1786,"text":"Geological Society of America Bulletin","active":true,"publicationSubtype":{"id":10}},"title":"River meanders","docAbstract":"<p id=\"p-3\">Most river curves have nearly the same value of the ratio of curvature radius to channel width, in the range of 2 to 3. Meanders formed by meltwater on the surface of glaciers, and by the main current of the Gulf Stream, have a relation of meander length to channel width similar to rivers. Because such meanders carry no sediment, the shapes of curves in rivers are evidently determined primarily by the dynamics of flow rather than by relation to debris load.</p><p id=\"p-4\">Velocity distributions along river curves provide a generalized picture of flow characteristics. Evidence on flow resistance in curved channels suggests that a basic aspect of meander mechanics may be related to the distribution of energy loss provided by a particular configuration or curvature. No general theory of meanders is as yet satisfactory, however; in fact, present evidence suggests that no single theory will explain the formation and characteristics of all meanders and that few of the physical principles involved have yet been clearly identified.</p>","language":"English","publisher":"Geological Society of America","doi":"10.1130/0016-7606(1960)71[769:RM]2.0.CO;2","usgsCitation":"Leopold, L.B., and Wolman, M.G., 1960, River meanders: Geological Society of America Bulletin, v. 71, no. 6, p. 769-793, https://doi.org/10.1130/0016-7606(1960)71[769:RM]2.0.CO;2.","productDescription":"25 p.","startPage":"769","endPage":"793","costCenters":[],"links":[{"id":338229,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"71","issue":"6","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"58d4df19e4b05ec79911d20d","contributors":{"authors":[{"text":"Leopold, Luna Bergere","contributorId":93884,"corporation":false,"usgs":true,"family":"Leopold","given":"Luna","email":"","middleInitial":"Bergere","affiliations":[],"preferred":false,"id":685949,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Wolman, M. Gordon","contributorId":85163,"corporation":false,"usgs":true,"family":"Wolman","given":"M.","email":"","middleInitial":"Gordon","affiliations":[],"preferred":false,"id":685950,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70171139,"text":"70171139 - 1960 - Collection and preservation of fish and other materials exposed to pesticides","interactions":[],"lastModifiedDate":"2016-05-23T17:07:30","indexId":"70171139","displayToPublicDate":"1960-01-01T00:00:00","publicationYear":"1960","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3196,"text":"Progressive Fish-Culturist","active":true,"publicationSubtype":{"id":10}},"title":"Collection and preservation of fish and other materials exposed to pesticides","docAbstract":"<p><span>The effects of pesticides on fish have become improtant to fish conservation since World War II, when DDT first came into common use. With the development of other potent insecticides and the increasing use of massive dosages in more recent years, the threat to fish and fish foods has increased. Fishery biologists have conducted some studies on the effects of insecticides, but it has been impossible for fishery science to keep pace with chemistry and agriculture.</span></p>","language":"English","publisher":"Taylor & Francis","doi":"10.1577/1548-8659(1960)22[103:CAPOFA]2.0.CO;2","usgsCitation":"Cope, O.B., 1960, Collection and preservation of fish and other materials exposed to pesticides: Progressive Fish-Culturist, v. 22, no. 3, p. 103-108, https://doi.org/10.1577/1548-8659(1960)22[103:CAPOFA]2.0.CO;2.","productDescription":"6 p.","startPage":"103","endPage":"108","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":192,"text":"Columbia Environmental Research Center","active":true,"usgs":true}],"links":[{"id":321551,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"22","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"574d645be4b07e28b668366e","contributors":{"authors":[{"text":"Cope, Oliver B.","contributorId":13290,"corporation":false,"usgs":true,"family":"Cope","given":"Oliver","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":630092,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":7000045,"text":"7000045 - 1960 - A primer on water","interactions":[],"lastModifiedDate":"2017-03-23T15:30:33","indexId":"7000045","displayToPublicDate":"1960-01-01T00:00:00","publicationYear":"1960","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":"A primer on water","docAbstract":"<p>When you open the faucet you expect water to flow. And you expect it to flow night or day, summer or winter, whether you want to fill a glass or water the lawn. It should be clean and pure, without any odor.</p><p>You have seen or read about places where the water doesn't have these qualities. You may have lived in a city where you were allowed to water the lawn only during a few hours of certain days. We know a large town where the water turns brown after every big rainstorm.</p><p>Beginning shortly after World War II, large areas in the Southwestern United States had a 10-year drought, and newspapers published a lot of information about its effects. Some people say that the growing demand for water will cause serious shortages over much of the country in the next 10 to 40 years. But it has always been true that while water wells and springs dry up in some places, floods may be occurring in other places at the same time.</p><p>Nearly every month news stories are published describing floods somewhere in the country. In fact, every year, on the average, 75,000 persons are forced from their homes by floods. In some years, as in 1951 when the lower Kansas River experienced a great flood, half a million people are affected. To understand the reasons for such recurring distress, it is necessary to know something about rivers and about the flat land or flood plain that borders the river.</p><p>Interest in water and related problems is growing as our population increases and as the use of water becomes steadily greater. To help meet this heightened interest in general information about water and its use and control is the reason this primer was written. The primer is in two parts. The first part tells about hydrology, or the science that concerns the relation of water to our earth, and the second part describes the development of water supplies and the use of water. The Geological Survey is publishing this primer in nontechnical language in the hope that it will enable the general reader to understand the facts about water as a part of nature, and that by having this understanding the people can solve their water problems.</p><p>We, as representatives of the Geological Survey, acknowledge with thanks the helpful suggestions made on an early draft by Marion Loizeaux, Maria Lord Converse, Constance Foley, Laura R. Langbein, and Bruce C. Leopold. We are also indebted to various geologists and engineers of the Survey for their discerning critical reviews.</p>","language":"English","publisher":"U.S. Government Printing Office","publisherLocation":"Washington, D.C.","doi":"10.3133/7000045","usgsCitation":"Leopold, L.B., and Langbein, W.B., 1960, A primer on water: General Interest Publication, iv, 50 p., https://doi.org/10.3133/7000045.","productDescription":"iv, 50 p.","numberOfPages":"57","costCenters":[],"links":[{"id":261217,"rank":800,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/gip/7000045/report.pdf"},{"id":261218,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/gip/7000045/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1be4b07f02db6a8fa7","contributors":{"authors":[{"text":"Leopold, Luna Bergere","contributorId":93884,"corporation":false,"usgs":true,"family":"Leopold","given":"Luna","email":"","middleInitial":"Bergere","affiliations":[],"preferred":false,"id":344013,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Langbein, Walter Basil","contributorId":40581,"corporation":false,"usgs":true,"family":"Langbein","given":"Walter","email":"","middleInitial":"Basil","affiliations":[],"preferred":false,"id":344014,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70010850,"text":"70010850 - 1960 - Isotopic composition and temperature of formation of antarctic snows","interactions":[],"lastModifiedDate":"2012-03-12T17:18:17","indexId":"70010850","displayToPublicDate":"1960-01-01T00:00:00","publicationYear":"1960","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2840,"text":"Nature","active":true,"publicationSubtype":{"id":10}},"title":"Isotopic composition and temperature of formation of antarctic snows","docAbstract":"[No abstract available]","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Nature","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1038/187857a0","issn":"00280836","usgsCitation":"Picciotto, E., De Maere, X., and Friedman, I., 1960, Isotopic composition and temperature of formation of antarctic snows: Nature, v. 187, no. 4740, p. 857-859, https://doi.org/10.1038/187857a0.","startPage":"857","endPage":"859","numberOfPages":"3","costCenters":[],"links":[{"id":480392,"rank":10000,"type":{"id":41,"text":"Open Access External Repository Page"},"url":"http://hdl.handle.net/2013/ULB-DIPOT:oai:dipot.ulb.ac.be:2013/182133","text":"External Repository"},{"id":204888,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1038/187857a0"},{"id":218810,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"187","issue":"4740","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a3f9ce4b0c8380cd64667","contributors":{"authors":[{"text":"Picciotto, E.","contributorId":34648,"corporation":false,"usgs":true,"family":"Picciotto","given":"E.","email":"","affiliations":[],"preferred":false,"id":359783,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"De Maere, X.","contributorId":100114,"corporation":false,"usgs":true,"family":"De Maere","given":"X.","email":"","affiliations":[],"preferred":false,"id":359785,"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":359784,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70010539,"text":"70010539 - 1960 - Magnetic susceptibility of tetragonal titanium dioxide","interactions":[],"lastModifiedDate":"2020-11-16T17:02:08.583509","indexId":"70010539","displayToPublicDate":"1960-01-01T00:00:00","publicationYear":"1960","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3060,"text":"Physical Review","active":true,"publicationSubtype":{"id":10}},"title":"Magnetic susceptibility of tetragonal titanium dioxide","docAbstract":"<p><span>Careful measurements have been made of the magnetic susceptibility of the rutile and anatase crystalline forms of titanium dioxide. The magnetic susceptibility of a single crystal of high-purity rutile was found to be (0.067±0.0015)×</span><span class=\"aps-inline-formula\"><span id=\"MathJax-Element-1-Frame\" class=\"mjx-chtml MathJax_CHTML\"><span id=\"MJXc-Node-1\" class=\"mjx-math\"><span id=\"MJXc-Node-2\" class=\"mjx-mrow\"><span id=\"MJXc-Node-3\" class=\"mjx-mrow\"><span id=\"MJXc-Node-4\" class=\"mjx-msup\"><span class=\"mjx-base\"><span id=\"MJXc-Node-5\" class=\"mjx-mrow\"><span id=\"MJXc-Node-6\" class=\"mjx-mn\"><span class=\"mjx-char MJXc-TeX-main-R\">10</span></span></span></span><span class=\"mjx-sup\"><span id=\"MJXc-Node-7\" class=\"mjx-mrow\"><sup><span id=\"MJXc-Node-8\" class=\"mjx-mo\"><span class=\"mjx-char MJXc-TeX-main-R\">−</span></span><span id=\"MJXc-Node-9\" class=\"mjx-mn\"><span class=\"mjx-char MJXc-TeX-main-R\">6</span></span></sup><span id=\"MJXc-Node-10\" class=\"mjx-mn\"></span></span></span></span></span></span></span></span></span><span>&nbsp;emu per gram, and was temperature-independent from 55° to 372°K. Difficulty was encountered in obtaining a good value of the magnetic susceptibility of anatase because of impurities. However, a value of 0.02×</span><span class=\"aps-inline-formula\"><span id=\"MathJax-Element-2-Frame\" class=\"mjx-chtml MathJax_CHTML\"><span id=\"MJXc-Node-11\" class=\"mjx-math\"><span id=\"MJXc-Node-12\" class=\"mjx-mrow\"><span id=\"MJXc-Node-13\" class=\"mjx-mrow\"><span id=\"MJXc-Node-14\" class=\"mjx-msup\"><span class=\"mjx-base\"><span id=\"MJXc-Node-15\" class=\"mjx-mrow\"><span id=\"MJXc-Node-16\" class=\"mjx-mn\"><span class=\"mjx-char MJXc-TeX-main-R\">10</span></span></span></span><span class=\"mjx-sup\"><span id=\"MJXc-Node-17\" class=\"mjx-mrow\"><sup><span id=\"MJXc-Node-18\" class=\"mjx-mo\"><span class=\"mjx-char MJXc-TeX-main-R\">−</span></span><span id=\"MJXc-Node-19\" class=\"mjx-mn\"><span class=\"mjx-char MJXc-TeX-main-R\">6</span></span></sup><span id=\"MJXc-Node-20\" class=\"mjx-mn\"></span></span></span></span></span></span></span></span></span><span>&nbsp;emu per gram was obtained as a maximum value for anatase powder. A discussion is given for the different values obtained for anatase and rutile.</span></p>","language":"English","publisher":"American Physical Society","doi":"10.1103/PhysRev.120.820","usgsCitation":"Senftle, F.E., Pankey, T., and Grant, F.A., 1960, Magnetic susceptibility of tetragonal titanium dioxide: Physical Review, v. 120, no. 3, p. 820-825, https://doi.org/10.1103/PhysRev.120.820.","productDescription":"6 p.","startPage":"820","endPage":"825","numberOfPages":"6","costCenters":[],"links":[{"id":219763,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"120","issue":"3","noUsgsAuthors":false,"publicationDate":"1960-11-01","publicationStatus":"PW","scienceBaseUri":"505a4b91e4b0c8380cd6963f","contributors":{"authors":[{"text":"Senftle, F. E.","contributorId":47788,"corporation":false,"usgs":true,"family":"Senftle","given":"F.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":359132,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Pankey, T.","contributorId":58773,"corporation":false,"usgs":true,"family":"Pankey","given":"T.","affiliations":[],"preferred":false,"id":359133,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Grant, F. A.","contributorId":77659,"corporation":false,"usgs":true,"family":"Grant","given":"F.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":359134,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70010540,"text":"70010540 - 1960 - Releasing effects in flame photometry. Determination of calcium","interactions":[],"lastModifiedDate":"2023-03-20T16:11:42.727677","indexId":"70010540","displayToPublicDate":"1960-01-01T00:00:00","publicationYear":"1960","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":"Releasing effects in flame photometry. Determination of calcium","docAbstract":"Strontium, lanthanum, neodymium, samarium, and yttrium completely release the flame emission of calcium from the depressive effects of sulfate, phosphate, and aluminate. Magnesium, beryllium, barium, and scandium release most of the calcium emission. These cations, when present in high concentration, preferentially form compounds with the depressing anions when the solution is evaporated rapidly in the flame. The mechanism of the interference and releasing effects is explained on the basis of the chemical equilibria in the evaporating droplets of solution and is shown to depend upon the nature of the compounds present in the aqueous phase of the solution. The need for background correction techniques is stressed. The releasing effect is used in the determination of calcium in silicate rocks without the need for separations.","language":"English","publisher":"ACS Publications","doi":"10.1021/ac60167a029","usgsCitation":"Dinnin, J., 1960, Releasing effects in flame photometry. Determination of calcium: Analytical Chemistry, v. 32, no. 11, p. 1475-1480, https://doi.org/10.1021/ac60167a029.","productDescription":"6 p.","startPage":"1475","endPage":"1480","numberOfPages":"6","costCenters":[],"links":[{"id":219764,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"32","issue":"11","noUsgsAuthors":false,"publicationDate":"2002-05-01","publicationStatus":"PW","scienceBaseUri":"505aa6b2e4b0c8380cd84fd0","contributors":{"authors":[{"text":"Dinnin, J. I.","contributorId":50886,"corporation":false,"usgs":true,"family":"Dinnin","given":"J. I.","affiliations":[],"preferred":false,"id":359135,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70009816,"text":"70009816 - 1960 - Data of rock analyses-VII. Bibliography and index of rock analyses in the periodical and serial literature of the Republic of Ireland and of Northern Ireland","interactions":[],"lastModifiedDate":"2024-03-07T15:45:26.430497","indexId":"70009816","displayToPublicDate":"1960-01-01T00:00:00","publicationYear":"1960","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":"Data of rock analyses-VII. Bibliography and index of rock analyses in the periodical and serial literature of the Republic of Ireland and of Northern Ireland","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"Elsevier","doi":"10.1016/0016-7037(60)90057-0","issn":"00167037","usgsCitation":"Woodland, M., 1960, Data of rock analyses-VII. Bibliography and index of rock analyses in the periodical and serial literature of the Republic of Ireland and of Northern Ireland: Geochimica et Cosmochimica Acta, v. 20, no. 2, p. 149-153, https://doi.org/10.1016/0016-7037(60)90057-0.","productDescription":"5 p.","startPage":"149","endPage":"153","numberOfPages":"5","costCenters":[],"links":[{"id":219033,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"20","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059fd8de4b0c8380cd4e89d","contributors":{"authors":[{"text":"Woodland, M.V.","contributorId":35065,"corporation":false,"usgs":true,"family":"Woodland","given":"M.V.","email":"","affiliations":[],"preferred":false,"id":357216,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70010537,"text":"70010537 - 1960 - Anisotropy of the magnetic susceptibility of gallium","interactions":[],"lastModifiedDate":"2020-11-16T17:04:42.468012","indexId":"70010537","displayToPublicDate":"1960-01-01T00:00:00","publicationYear":"1960","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2171,"text":"Journal of Applied Physics","active":true,"publicationSubtype":{"id":10}},"title":"Anisotropy of the magnetic susceptibility of gallium","docAbstract":"<p><span>The bulk&nbsp;</span>magnetic susceptibilities<span>&nbsp;of single&nbsp;</span>gallium<span>&nbsp;crystals and&nbsp;</span>polycrystalline<span>&nbsp;</span>gallium<span>&nbsp;spheres were&nbsp;</span>measured<span>&nbsp;at 25°C. The following&nbsp;</span>anisotropic<span>&nbsp;</span>diamagnetic<span>&nbsp;</span>susceptibilities<span>&nbsp;were found:&nbsp;</span><i>a</i><span>&nbsp;axis (−0.119±0.001)×10</span><sup>−6</sup><span>&nbsp;emu/g,&nbsp;</span><i>b</i><span>&nbsp;axis (−0.416±0.002)×10</span><sup>−6</sup><span>&nbsp;emu/g, and&nbsp;</span><i>c</i><span>&nbsp;axis (−0.229±0.001) emu/g. The&nbsp;</span>susceptibility<span>&nbsp;of the&nbsp;</span>polycrystalline<span>&nbsp;spheres, assumed to be the average value for the bulk&nbsp;</span>susceptibility<span>&nbsp;of&nbsp;</span>gallium,<span>&nbsp;was (−0.257±0.003)×10</span><sup>−6</sup><span>&nbsp;emu/g at 25°C, and (−0.299±0.003)×10</span><sup>−6</sup><span>&nbsp;emu/g at −196°C. The&nbsp;</span>susceptibility<span>&nbsp;of liquid&nbsp;</span>gallium<span>&nbsp;was (0.0031±0.001)×10</span><sup>−6</sup><span>&nbsp;emu/g at 30°C and 100°C. Rotational diagrams of the&nbsp;</span>susceptibilities<span>&nbsp;in the three orthogonal planes of the unit cell were not sinusoidal. The&nbsp;</span>anisotropy<span>&nbsp;in the&nbsp;</span>single crystals<span>&nbsp;was presumably caused by the partial overlap of&nbsp;</span>Brillouin<span>&nbsp;zone boundaries by the Fermi‐energy&nbsp;</span>surface.<span>&nbsp;The large change in&nbsp;</span>susceptibility<span>&nbsp;associated with the change in state was attributed to the absence of effective mass influence in the liquid state.</span></p>","language":"English","publisher":"AIP Publishing","doi":"10.1063/1.1735451","usgsCitation":"Pankey, T., 1960, Anisotropy of the magnetic susceptibility of gallium: Journal of Applied Physics, v. 31, no. 10, p. 1802-1804, https://doi.org/10.1063/1.1735451.","productDescription":"3 p.","startPage":"1802","endPage":"1804","numberOfPages":"3","costCenters":[],"links":[{"id":219761,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"31","issue":"10","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059ec00e4b0c8380cd4901c","contributors":{"authors":[{"text":"Pankey, T. Jr.","contributorId":99833,"corporation":false,"usgs":true,"family":"Pankey","given":"T.","suffix":"Jr.","email":"","affiliations":[],"preferred":false,"id":359128,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
]}