{"pageNumber":"5977","pageRowStart":"149400","pageSize":"25","recordCount":165846,"records":[{"id":68248,"text":"ha162 - 1965 - Availability of ground water in the Water Valley quadrangle, Kentucky-Tennessee","interactions":[],"lastModifiedDate":"2023-03-01T22:56:42.836243","indexId":"ha162","displayToPublicDate":"1965-01-01T00:00:00","publicationYear":"1965","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":318,"text":"Hydrologic Atlas","code":"HA","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"162","title":"Availability of ground water in the Water Valley quadrangle, Kentucky-Tennessee","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ha162","usgsCitation":"Lambert, T.W., 1965, Availability of ground water in the Water Valley quadrangle, Kentucky-Tennessee: U.S. Geological Survey Hydrologic Atlas 162, 1 Plate: 47.50 x 35.50 inches, https://doi.org/10.3133/ha162.","productDescription":"1 Plate: 47.50 x 35.50 inches","costCenters":[],"links":[{"id":189576,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":413588,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_15523.htm","linkFileType":{"id":5,"text":"html"}},{"id":89629,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/162/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"24000","country":"United States","state":"Kentucky, Tennessee","otherGeospatial":"Water Valley quadrangle","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -88.875,\n              36.5\n            ],\n            [\n              -88.875,\n              36.625\n            ],\n            [\n              -88.75,\n              36.625\n            ],\n            [\n              -88.75,\n              36.5\n            ],\n            [\n              -88.875,\n              36.5\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a9ae4b07f02db65d8db","contributors":{"authors":[{"text":"Lambert, T. William","contributorId":40574,"corporation":false,"usgs":true,"family":"Lambert","given":"T.","email":"","middleInitial":"William","affiliations":[],"preferred":false,"id":277905,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":68242,"text":"ha160 - 1965 - Availability of ground water in the Kentucky part of the Rushing Creek quadrangle, Kentucky-Tennessee","interactions":[],"lastModifiedDate":"2023-03-01T22:46:02.159683","indexId":"ha160","displayToPublicDate":"1965-01-01T00:00:00","publicationYear":"1965","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":318,"text":"Hydrologic Atlas","code":"HA","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"160","title":"Availability of ground water in the Kentucky part of the Rushing Creek quadrangle, Kentucky-Tennessee","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ha160","usgsCitation":"Lambert, T.W., 1965, Availability of ground water in the Kentucky part of the Rushing Creek quadrangle, Kentucky-Tennessee: U.S. Geological Survey Hydrologic Atlas 160, 1 Plate: 47.50 x 34.50 inches, https://doi.org/10.3133/ha160.","productDescription":"1 Plate: 47.50 x 34.50 inches","costCenters":[],"links":[{"id":189570,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":413585,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_15521.htm","linkFileType":{"id":5,"text":"html"}},{"id":89622,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/160/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"24000","country":"United States","state":"Kentucky, Tennessee","otherGeospatial":"Rushing Creek quadrangle","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -88.125,\n              36.625\n            ],\n            [\n              -88.125,\n              36.75\n            ],\n            [\n              -88,\n              36.75\n            ],\n            [\n              -88,\n              36.625\n            ],\n            [\n              -88.125,\n              36.625\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a9ee4b07f02db6608f4","contributors":{"authors":[{"text":"Lambert, T. William","contributorId":40574,"corporation":false,"usgs":true,"family":"Lambert","given":"T.","email":"","middleInitial":"William","affiliations":[],"preferred":false,"id":277899,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70185670,"text":"70185670 - 1965 - Vigil Network sites: A sample of data for permanent filing","interactions":[],"lastModifiedDate":"2017-03-27T13:03:24","indexId":"70185670","displayToPublicDate":"1965-01-01T00:00:00","publicationYear":"1965","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":5334,"text":"International Association of Scientific Hydrology - Bulletin ","onlineIssn":"2150-3435","printIssn":"0262-6667","active":false,"publicationSubtype":{"id":10}},"title":"Vigil Network sites: A sample of data for permanent filing","docAbstract":"<p>The Vigil Network consists of places where observations are made through time to record changes in landscape features over a long period. Resurveys will usually be made once each year or every few years and the period of observation, hopefully, will extend through and beyond the International Hydrological Decade.</p><p>Vigil Network sites will usually be chosen to represent some typical feature of a given landscape. In the example shown here, the feature is a small ephemeral channel in a basin of moderate relief underlain by silty sandstone typical of the surrounding area. Vigil sites are not protected from man's influence and indeed may be selected because of the possible or portending cultural influences. In this respect they differ from the Bench Mark Network whose purpose is to make precise observations of hydrologic factors in areas uninfluenced by and protected from man's use.</p><p>The factors which might be observed are many and varied. A few might be mentioned here, others are explained at length elsewhere (Miller and Leopold, 1963; Leopold, 1962). Streamchannel position, form, depth, and profile; vegetation in form of transects or quadrats; soil movement on slopes; rock movement on slopes or in channels. These and many more would yield valuable information on changes with time.</p><p>To assure permanence of initial field observations, including reference points, bench marks, and cross sections, brief descriptions, maps, and initial data should be filed identically in designated repositories where the data will be made available for inspection by any interested scientist. It is recommended that the designation of two such locations where records of the type here attached will be filed be taken up by the Coordinating Council of the International Hydrological Decade. In designating such repositories it should be recognized that there is no need for elaborate indexing. The main requirement is merely the maintenance of a simple file where the data are stored and can be inspected or copied by any scientist. There need be no special provision for lending or reproduction services.</p><p>The present document is an example showing what data, maps, and descriptions should be included in those permanent files at the two repositories. The material in these repositories should be sufficient to permit someone in the indefinite future to find and remeasure the same features described now. Thus the scientific value of the original surveys increases with time, - provided that the descriptions are sufficient to allow a person to find with assurance the original feature in the field.</p><p>It must be visualized that a permanent repository must economize in space. Thus, as the example here shows, the filed material is not all of the original field notes but a summary, brief but descriptive.</p>","language":"English","publisher":"Taylor & Francis","doi":"10.1080/02626666509493401","usgsCitation":"Leopold, L.B., and Emmett, W.W., 1965, Vigil Network sites: A sample of data for permanent filing: International Association of Scientific Hydrology - Bulletin , v. 10, no. 3, p. 12-21, https://doi.org/10.1080/02626666509493401.","productDescription":"10 p.","startPage":"12","endPage":"21","costCenters":[],"links":[{"id":480681,"rank":0,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1080/02626666509493401","text":"Publisher Index Page"},{"id":338379,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"10","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"58da253fe4b0543bf7fda87d","contributors":{"authors":[{"text":"Leopold, Luna Bergere","contributorId":93884,"corporation":false,"usgs":true,"family":"Leopold","given":"Luna","email":"","middleInitial":"Bergere","affiliations":[],"preferred":false,"id":686308,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Emmett, William W.","contributorId":68715,"corporation":false,"usgs":true,"family":"Emmett","given":"William","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":686309,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":5220427,"text":"5220427 - 1965 - Control of alligatorweed in South Carolina with granular silvex","interactions":[],"lastModifiedDate":"2026-03-18T16:29:09.803492","indexId":"5220427","displayToPublicDate":"1965-01-01T00:00:00","publicationYear":"1965","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3741,"text":"Weeds","active":true,"publicationSubtype":{"id":10}},"title":"Control of alligatorweed in South Carolina with granular silvex","docAbstract":"<p><span>Silvex, [2-(2,4,5-trichlorophenoxy)propionic acid], impregnated (20% ae) on clay granules, applied at a rate as low as 20 lb/A ae gave excellent control of well-rooted alligatorweed [</span><i><span class=\"italic\">Alternanthera philoxeroides</span></i><span>&nbsp;(Mart.) Grieb] growing in less than 18 inches of water. The 2-ethylhexyl ester of silvex was more effective than the potassium salt. Silvex was not effective on floating-mat alligatorweed or in water over 18 inches deep.</span></p>","language":"English","publisher":"Cambridge University Press","doi":"10.2307/4041102","usgsCitation":"McGilvrey, F., and Steenis, J., 1965, Control of alligatorweed in South Carolina with granular silvex: Weeds, v. 13, no. 1, p. 66-68, https://doi.org/10.2307/4041102.","productDescription":"3 p.","startPage":"66","endPage":"68","costCenters":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":194316,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"South 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,{"id":70009990,"text":"70009990 - 1965 - Glass electrode determination of sodium in closed basin waters","interactions":[],"lastModifiedDate":"2020-11-24T13:25:10.296594","indexId":"70009990","displayToPublicDate":"1965-01-01T00:00:00","publicationYear":"1965","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":"Glass electrode determination of sodium in closed basin waters","docAbstract":"<div id=\"abstracts\" class=\"Abstracts u-font-serif\"><div id=\"aep-abstract-id6\" class=\"abstract author\"><div id=\"aep-abstract-sec-id7\"><p>Because of its direct relation to total dissolved solids content, sodium concentration is the most useful single hydrochemical parameter of closed basin waters in the western United States. Therefore, it is advantageous to have a rapid method for sodium determination which could be readily adapted to field use. Accordingly, thirty waters of highly variable concentration and anionic composition from the western Great Basin have been analyzed with a sodium-sensitive glass electrode. Na<sup>+</sup><span>&nbsp;</span>values ranged from 10 to 130,000 ppm in waters containing from 102 to 401,000 ppm total dissolved solids. The electrode values were compared with conventional sodium determinations; results differed by as much as 11 per cent, although over two-thirds were within 5 per cent. No significant relation was found between the glass electrode and conventional method differences and the total dissolved solids or sodium concentration. The comparative accuracy of electrode and conventional procedures was checked, employing solutions of known sodium concentration. It was concluded that for the analysis of sodium in natural waters the glass electrode method offers results comparable in accuracy to those obtained by conventional methods, but with increased simplicity, and therefore the possibility of rapid, accurate field measurements.</p></div></div></div>","language":"English","publisher":"Elsevier","doi":"10.1016/0016-7037(65)90066-9","issn":"00167037","usgsCitation":"Truesdell, A., Jones, B., and Van Denburgh, A.S., 1965, Glass electrode determination of sodium in closed basin waters: Geochimica et Cosmochimica Acta, v. 29, no. 6, p. 725-736, https://doi.org/10.1016/0016-7037(65)90066-9.","productDescription":"12 p.","startPage":"725","endPage":"736","numberOfPages":"12","costCenters":[],"links":[{"id":218617,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"29","issue":"6","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a2928e4b0c8380cd5a6f4","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":357604,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Jones, B.F.","contributorId":52156,"corporation":false,"usgs":true,"family":"Jones","given":"B.F.","email":"","affiliations":[],"preferred":false,"id":357603,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Van Denburgh, A. S.","contributorId":23928,"corporation":false,"usgs":true,"family":"Van Denburgh","given":"A.","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":357602,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":68443,"text":"ha195 - 1965 - Hydrogeology of the glacial drift in the Skunk Creek-Lake Madison drainage basin, southeastern South Dakota","interactions":[],"lastModifiedDate":"2023-03-14T19:17:51.83257","indexId":"ha195","displayToPublicDate":"1965-01-01T00:00:00","publicationYear":"1965","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":318,"text":"Hydrologic Atlas","code":"HA","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"195","title":"Hydrogeology of the glacial drift in the Skunk Creek-Lake Madison drainage basin, southeastern South Dakota","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ha195","usgsCitation":"Ellis, M.J., and Adolphson, D.G., 1965, Hydrogeology of the glacial drift in the Skunk Creek-Lake Madison drainage basin, southeastern South Dakota: U.S. Geological Survey Hydrologic Atlas 195, 1 Plate: 52.00 x 34.50 inches, https://doi.org/10.3133/ha195.","productDescription":"1 Plate: 52.00 x 34.50 inches","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":414119,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_15559.htm","linkFileType":{"id":5,"text":"html"}},{"id":186219,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":89973,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/195/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"125000","country":"United States","state":"South Dakota","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -96.75,\n              43.478\n            ],\n            [\n              -96.75,\n              44.081\n            ],\n            [\n              -97.3,\n              44.081\n            ],\n            [\n              -97.3,\n              43.478\n            ],\n            [\n              -96.75,\n              43.478\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a2ee4b07f02db614eec","contributors":{"authors":[{"text":"Ellis, M. J.","contributorId":27840,"corporation":false,"usgs":true,"family":"Ellis","given":"M.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":278227,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Adolphson, D. G.","contributorId":106081,"corporation":false,"usgs":true,"family":"Adolphson","given":"D.","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":278228,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70009989,"text":"70009989 - 1965 - Alkali content of alpine ultramafic rocks","interactions":[],"lastModifiedDate":"2020-11-24T00:39:56.572868","indexId":"70009989","displayToPublicDate":"1965-01-01T00:00:00","publicationYear":"1965","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":"Alkali content of alpine ultramafic 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>The lower limit of abundance of sodium and potassium in ultramafic rocks is less than the threshold amount detectable by conventional analytical methods. By a dilutionaddition modification of the flame-spectrophotometric method, sodium and potassium have been determined in 40 specimens of alpine ultramafic rocks. Samples represent six regions in the United States and one in Australia, and include dunite, peridotite, pyroxenite, and their variably serpentinized and metamorphosed derivatives.</p><p>The median value found for Na<sub>2</sub>O is 0.004 per cent, and the range of Na<sub>2</sub>O is 0.001–0.19. The median value for K<sub>2</sub>O is 0.0034 per cent and the range is 0.001–0.031 per cent. Alkali concentrations are below 0.01 per cent Na<sub>2</sub>O in 28 samples and below 0.01 per cent K<sub>2</sub>O in 35.</p><p>Derivation of basalt magma from upper-mantle material similar to such ultramafic rocks, as has been postulated, is precluded by the relative amounts of sodium and potassium, which are from 200 to 600 times more abundant in basalt than in the ultramafic rocks. Similar factors apply to a number of other elements. No reasonable process could produce such concentrations in, for example, tens of thousands of cubic miles of uniform tholeiitic basalt. The ultramafic rocks might have originated either as magmatic crystal precipitates or as mantle residues left after fusion and removal of basaltic magma. Injection of ultramafic rocks to exposed positions is tectonic rather than magmatic.</p></div></div></div>","language":"English","publisher":"Elsevier","doi":"10.1016/0016-7037(65)90062-1","issn":"00167037","usgsCitation":"Hamilton, W., and Mountjoy, W., 1965, Alkali content of alpine ultramafic rocks: Geochimica et Cosmochimica Acta, v. 29, no. 6, p. 661-671, https://doi.org/10.1016/0016-7037(65)90062-1.","productDescription":"11 p.","startPage":"661","endPage":"671","numberOfPages":"11","costCenters":[],"links":[{"id":218616,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"29","issue":"6","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059e966e4b0c8380cd48251","contributors":{"authors":[{"text":"Hamilton, W.","contributorId":46683,"corporation":false,"usgs":true,"family":"Hamilton","given":"W.","email":"","affiliations":[],"preferred":false,"id":357600,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Mountjoy, W.","contributorId":65122,"corporation":false,"usgs":true,"family":"Mountjoy","given":"W.","email":"","affiliations":[],"preferred":false,"id":357601,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":2529,"text":"wsp1594C - 1965 - Artificial recharge in Oregon and Washington 1962","interactions":[{"subject":{"id":56108,"text":"ofr5845 - 1957 - Artificial recharge to ground water in Oregon and Washington","indexId":"ofr5845","publicationYear":"1957","noYear":false,"title":"Artificial recharge to ground water in Oregon and Washington"},"predicate":"SUPERSEDED_BY","object":{"id":2529,"text":"wsp1594C - 1965 - Artificial recharge in Oregon and Washington 1962","indexId":"wsp1594C","publicationYear":"1965","noYear":false,"chapter":"C","title":"Artificial recharge in Oregon and Washington 1962"},"id":1}],"lastModifiedDate":"2023-03-21T21:43:14.859497","indexId":"wsp1594C","displayToPublicDate":"1965-01-01T00:00:00","publicationYear":"1965","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":341,"text":"Water Supply Paper","code":"WSP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1594","chapter":"C","title":"Artificial recharge in Oregon and Washington 1962","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wsp1594C","usgsCitation":"Price, D., Hart, D.H., and Foxworthy, B., 1965, Artificial recharge in Oregon and Washington 1962: U.S. Geological Survey Water Supply Paper 1594, Report: iv, 65 p.; 2 Plates: 13.00 x 16.00 inches and 15.50 x 22.50 inches, https://doi.org/10.3133/wsp1594C.","productDescription":"Report: iv, 65 p.; 2 Plates: 13.00 x 16.00 inches and 15.50 x 22.50 inches","costCenters":[{"id":518,"text":"Oregon Water Science Center","active":true,"usgs":true}],"links":[{"id":414513,"rank":5,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_24780.htm","linkFileType":{"id":5,"text":"html"}},{"id":28750,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1594c/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":28751,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1594c/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":28752,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1594c/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":139101,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1594c/report-thumb.jpg"}],"country":"United States","state":"Oregon, Washington","city":"Richland","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -119.46350315641314,\n              46.4426973178723\n            ],\n            [\n              -119.46350315641314,\n              45.7221983183116\n            ],\n            [\n              -118.77099010172134,\n              45.7221983183116\n            ],\n            [\n              -118.77099010172134,\n              46.4426973178723\n            ],\n            [\n              -119.46350315641314,\n              46.4426973178723\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4abbe4b07f02db672c3e","contributors":{"authors":[{"text":"Price, Don","contributorId":30608,"corporation":false,"usgs":true,"family":"Price","given":"Don","email":"","affiliations":[],"preferred":false,"id":145352,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hart, D. H.","contributorId":16811,"corporation":false,"usgs":true,"family":"Hart","given":"D.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":145351,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Foxworthy, B. L.","contributorId":45686,"corporation":false,"usgs":true,"family":"Foxworthy","given":"B. L.","affiliations":[],"preferred":false,"id":145353,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":1013747,"text":"1013747 - 1965 - Eimeria aurati n. sp. (Protozoa:Eimeriidae) from goldfish (Carassius auratus) in North America","interactions":[],"lastModifiedDate":"2025-05-09T15:51:47.108634","indexId":"1013747","displayToPublicDate":"1965-01-01T00:00:00","publicationYear":"1965","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2434,"text":"Journal of Protozoology","active":true,"publicationSubtype":{"id":10}},"title":"Eimeria aurati n. sp. (Protozoa:Eimeriidae) from goldfish (Carassius auratus) in North America","docAbstract":"<p><i>Eimeria aurati</i><span>&nbsp;n. sp. is described from the intestine of the goldfish,&nbsp;</span><i>Carassius auratus</i><span>, from Pennsylvania, U.S.A. Oocysts were very numerous in long, whitish, opaque fecal casts. They were 16 to 24 by 14 to 17 μ (mean, 20.1 by 16.3) and were non-sporulated when passed but sporulated 2 to 5 days later.</span></p>","language":"English","publisher":"Wiley","doi":"10.1111/j.1550-7408.1965.tb01850.x","usgsCitation":"Hoffman, G.L., 1965, Eimeria aurati n. sp. (Protozoa:Eimeriidae) from goldfish (Carassius auratus) in North America: Journal of Protozoology, v. 12, no. 2, p. 273-275, https://doi.org/10.1111/j.1550-7408.1965.tb01850.x.","productDescription":"3 p.","startPage":"273","endPage":"275","numberOfPages":"3","costCenters":[{"id":365,"text":"Leetown Science Center","active":true,"usgs":true}],"links":[{"id":129473,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"12","issue":"2","noUsgsAuthors":false,"publicationDate":"2007-04-30","publicationStatus":"PW","scienceBaseUri":"4f4e4a25e4b07f02db60eec0","contributors":{"authors":[{"text":"Hoffman, G. L.","contributorId":70713,"corporation":false,"usgs":true,"family":"Hoffman","given":"G.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":319180,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":1014213,"text":"1014213 - 1965 - A review of advances in the study of diseases of fish: 1954-1964","interactions":[],"lastModifiedDate":"2016-01-06T11:28:55","indexId":"1014213","displayToPublicDate":"1965-01-01T00:00:00","publicationYear":"1965","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":"A review of advances in the study of diseases of fish: 1954-1964","docAbstract":"<p>STUDY OF DISEASE&nbsp;IN ANIMALS, INCLUDING MAN, has progressed rapidly in the past decade. Looking back, we find amazing success in the study of man's diseases and possibly only a little less success in studies of diseases of domesticated homeothermic animals. </p><p>We who are interested in the poikilothermic animals may feel at times that we have not advanced so rapidly in our field. The reason for this may be closely associated with economics. The market for drugs and therapeutic agents is greater for domestic livestock than for cultured fishes. A larger income is derived from rearing domestic livestock. Therefore, more public funds are available for study of diseases of man and domestic livestock, while such funds are limited for the study of diseases of fish. The Federal and State fish-cultural systems, as well as colleges and universities, have been most active in research on fish disease and probably will continue to be so.</p>","language":"English","publisher":" Bureau of Fisheries, U.S. Deptartment of Commerce","doi":"10.1577/1548-8640(1965)27[3:AROAIT]2.0.CO;2","usgsCitation":"Post, G., 1965, A review of advances in the study of diseases of fish: 1954-1964: Progressive Fish-Culturist, v. 27, no. 1, p. 3-12, https://doi.org/10.1577/1548-8640(1965)27[3:AROAIT]2.0.CO;2.","productDescription":"10 p.","startPage":"3","endPage":"12","numberOfPages":"10","costCenters":[{"id":365,"text":"Leetown Science Center","active":true,"usgs":true},{"id":654,"text":"Western Fisheries Research Center","active":true,"usgs":true}],"links":[{"id":132267,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"27","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1ae4b07f02db6a81c1","contributors":{"authors":[{"text":"Post, G.","contributorId":43699,"corporation":false,"usgs":true,"family":"Post","given":"G.","email":"","affiliations":[],"preferred":false,"id":319981,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70010658,"text":"70010658 - 1965 - Natural recharge and localization of fresh ground water in Kuwait","interactions":[],"lastModifiedDate":"2020-11-24T00:17:46.668516","indexId":"70010658","displayToPublicDate":"1965-01-01T00:00:00","publicationYear":"1965","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2342,"text":"Journal of Hydrology","active":true,"publicationSubtype":{"id":10}},"title":"Natural recharge and localization of fresh ground water in Kuwait","docAbstract":"<p>Fresh ground water (200 parts per million total dissolved solids and upwards) occurs in portions of Pleistocene sandstone aquifers beneath basins and wadis in north Kuwait where the mean rainfall is about five inches per year. The fresh water is surrounded and underlain by brackish water (&gt; 4000 ppm TDS). Drilling and testing show that fresh water saturation is restricted to wadis and basin areas; in Rawdatain basin it attains a maximum thickness of about 110 feet and a lateral extent of about seven miles.</p><p>The fresh ground water represents recharge localized, during infrequent, torrential rain storms, in areas of concentrated runoff where sediments in the vadose zone are moderately permeable and depth to the water table is generally less than a hundred feet. Concentration of runoff appears to be the primary control in the localization of recharge. The fresh water percolates downward to the ground-water reservoir following rare storms, then flows in the direction of hydraulic gradient and gradually becomes brackish.</p><p>Theoretical delineation of the recharge area and ground-water flow pattern in Rawdatain was confirmed by tritium and C<sub>14</sub><span>&nbsp;</span>dating of the water.</p><p>Brackish ground-water conditions prevail from water table downward in areas where rainfall infiltrates essentially where it falls, permeability of sediments in the vadose zone is low, or the water table is several hundred feet below land surface. In these areas, rainfall is retained and lost within the soil zone or becomes mineralized during deep percolation.</p>","language":"English","publisher":"Elsevier","doi":"10.1016/0022-1694(65)90038-7","issn":"00221694","usgsCitation":"Bergstrom, R., and Aten, R., 1965, Natural recharge and localization of fresh ground water in Kuwait: Journal of Hydrology, v. 2, no. 3, p. 213-231, https://doi.org/10.1016/0022-1694(65)90038-7.","productDescription":"19 p.","startPage":"213","endPage":"231","numberOfPages":"19","costCenters":[],"links":[{"id":219390,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"Kuwait","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"Polygon\",\"coordinates\":[[[47.97452,29.97582],[48.18319,29.53448],[48.09394,29.3063],[48.41609,28.552],[47.70885,28.52606],[47.45982,29.00252],[46.56871,29.09903],[47.30262,30.05907],[47.97452,29.97582]]]},\"properties\":{\"name\":\"Kuwait\"}}]}","volume":"2","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a6351e4b0c8380cd7241c","contributors":{"authors":[{"text":"Bergstrom, R.E.","contributorId":66413,"corporation":false,"usgs":true,"family":"Bergstrom","given":"R.E.","email":"","affiliations":[],"preferred":false,"id":359369,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Aten, R.E.","contributorId":18105,"corporation":false,"usgs":true,"family":"Aten","given":"R.E.","email":"","affiliations":[],"preferred":false,"id":359368,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70010681,"text":"70010681 - 1965 - Geochemistry of Birch Creek, Inyo County, California a travertine depositing creek in an arid climate","interactions":[],"lastModifiedDate":"2020-11-24T00:16:31.13398","indexId":"70010681","displayToPublicDate":"1965-01-01T00:00:00","publicationYear":"1965","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":"Geochemistry of Birch Creek, Inyo County, California a travertine depositing creek in an arid climate","docAbstract":"<div id=\"abstracts\" class=\"Abstracts u-font-serif\"><div id=\"aep-abstract-id4\" class=\"abstract author\"><div id=\"aep-abstract-sec-id5\"><p>A small stream in eastern California was studied in detail to determine the causes of travertine deposition from the stream. Although the ground water feeding the stream is slightly supersaturated to just saturated with calcite, the ground water is supersaturated with CO<sub>2</sub><span>&nbsp;</span>with respect to the overlying air. The water becomes increasingly supersaturated with calcite in a downstream direction as CO<sub>2</sub><span>&nbsp;</span>loss to the air and by photosynthesis exceeds the rate of precipitation of calcite. Water loss by evaporation was below detection and does not play an important role in calcite deposition in this case. The water loss is by seepage through the stream bed. Observations showed variations in HCO<sup>−</sup><sub>3</sub>, pH, discharge, Ca<sup>+2</sup>, relative humidity, water and air temperatures, and dissolved CO<sub>2</sub>. Comparisons of observed and equilibrium states are given for five sampling stations along the stream.</p></div></div></div>","language":"English","publisher":"Elsevier","doi":"10.1016/0016-7037(65)90119-5","issn":"00167037","usgsCitation":"Barnes, I., 1965, Geochemistry of Birch Creek, Inyo County, California a travertine depositing creek in an arid climate: Geochimica et Cosmochimica Acta, v. 29, no. 2, p. 85-112, https://doi.org/10.1016/0016-7037(65)90119-5.","productDescription":"28 p.","startPage":"85","endPage":"112","numberOfPages":"28","costCenters":[],"links":[{"id":219470,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"California","county":"Inyo County","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"Polygon\",\"coordinates\":[[[-117.8357,37.4655],[-117.8339,37.4655],[-117.7506,37.4045],[-117.7398,37.3966],[-117.684,37.3555],[-117.6414,37.3244],[-117.5857,37.2832],[-117.5789,37.2781],[-117.5715,37.2726],[-117.5108,37.2281],[-117.5046,37.2234],[-117.3489,37.1078],[-117.293,37.066],[-117.284,37.0595],[-117.275,37.053],[-117.253,37.0363],[-117.2394,37.0265],[-117.1639,36.9698],[-117.164,36.9688],[-117.0046,36.8495],[-116.981,36.8319],[-116.9783,36.8299],[-116.9641,36.8193],[-116.9237,36.7891],[-116.8912,36.7648],[-116.8806,36.7568],[-116.8453,36.7298],[-116.8424,36.7276],[-116.7895,36.6877],[-116.706,36.6248],[-116.6764,36.6024],[-116.6583,36.5888],[-116.6556,36.5867],[-116.5946,36.54],[-116.574,36.5245],[-116.5589,36.5131],[-116.5247,36.4871],[-116.5107,36.4764],[-116.3752,36.373],[-116.2954,36.3122],[-116.2834,36.3028],[-116.2311,36.2626],[-116.173,36.2174],[-116.1702,36.2152],[-116.1287,36.1829],[-116.1039,36.1636],[-116.0624,36.1314],[-116.049,36.1211],[-115.9925,36.0773],[-115.9518,36.0457],[-115.9178,36.0192],[-115.895,36.0015],[-115.6884,35.8402],[-115.6513,35.8111],[-115.7013,35.8114],[-115.7359,35.8116],[-115.7362,35.7953],[-115.7532,35.7953],[-115.7975,35.7949],[-115.8423,35.7954],[-115.8605,35.7951],[-115.8786,35.7952],[-115.8968,35.7952],[-116.0353,35.7953],[-116.0619,35.7952],[-116.0795,35.7952],[-116.1221,35.7946],[-116.1766,35.7939],[-116.1891,35.7938],[-116.2095,35.7934],[-116.2549,35.7933],[-116.2765,35.793],[-116.2952,35.793],[-116.3389,35.7929],[-116.3474,35.7931],[-116.3588,35.7929],[-116.4444,35.7943],[-116.5068,35.7954],[-116.5346,35.7956],[-116.6021,35.7964],[-116.6071,35.7965],[-116.9232,35.7961],[-116.9357,35.7959],[-116.9453,35.7957],[-117.0917,35.7946],[-117.259,35.7947],[-117.3504,35.7946],[-117.3685,35.7945],[-117.3844,35.7948],[-117.4031,35.7946],[-117.4162,35.7944],[-117.4224,35.7945],[-117.6362,35.7958],[-117.8523,35.7985],[-117.8738,35.7988],[-117.9005,35.7983],[-117.9249,35.7986],[-117.9234,35.7863],[-118.009,35.7861],[-118.0133,35.7993],[-118.0131,35.8093],[-118.009,35.8174],[-118.0015,35.8218],[-117.9975,35.8232],[-118.0065,35.8278],[-118.007,35.8337],[-118.0068,35.8441],[-118.0094,35.8555],[-118.007,35.8627],[-118.0012,35.8663],[-117.9955,35.8699],[-117.9905,35.8648],[-117.9836,35.8661],[-117.9852,35.8738],[-117.9891,35.8793],[-117.9901,35.8861],[-117.9842,35.8929],[-117.9886,35.9029],[-117.9906,35.9129],[-117.9905,35.9197],[-117.9858,35.9255],[-117.9858,35.9301],[-117.9868,35.9342],[-117.9906,35.9424],[-117.9991,35.9461],[-118.0093,35.9449],[-118.0154,35.9541],[-118.0193,35.9609],[-118.014,35.969],[-118.0139,35.974],[-118.0053,35.9784],[-118.0046,35.9811],[-118.0057,35.9839],[-118.0074,35.9875],[-118.0124,35.9935],[-118.0162,35.9985],[-118.0196,36.0013],[-118.0252,36.0045],[-118.0332,36.0051],[-118.0381,36.0151],[-118.0385,36.0265],[-118.0423,36.0329],[-118.0467,36.0415],[-118.046,36.0461],[-118.0488,36.0534],[-118.0537,36.0611],[-118.0529,36.0729],[-118.0539,36.0829],[-118.0572,36.087],[-118.06,36.0921],[-118.0668,36.0899],[-118.069,36.0963],[-118.0677,36.1062],[-118.068,36.1194],[-118.0735,36.1308],[-118.0751,36.1344],[-118.0756,36.1403],[-118.0721,36.1435],[-118.0646,36.1475],[-118.0616,36.1551],[-118.0626,36.1647],[-118.0618,36.1751],[-118.0657,36.1783],[-118.0708,36.1811],[-118.0774,36.1953],[-118.0881,36.2008],[-118.0949,36.2045],[-118.0994,36.2073],[-118.1067,36.216],[-118.1099,36.2247],[-118.1086,36.2328],[-118.1119,36.241],[-118.118,36.2515],[-118.1185,36.2533],[-118.1189,36.2624],[-118.1194,36.2656],[-118.1216,36.2729],[-118.1266,36.2793],[-118.1253,36.2888],[-118.1228,36.2979],[-118.1215,36.3069],[-118.1169,36.31],[-118.114,36.3145],[-118.115,36.3191],[-118.1018,36.3262],[-118.1005,36.3325],[-118.1021,36.338],[-118.1031,36.3434],[-118.1065,36.3476],[-118.1162,36.3481],[-118.1219,36.3486],[-118.1242,36.3505],[-118.1302,36.3628],[-118.1336,36.3674],[-118.1404,36.3693],[-118.146,36.3743],[-118.1517,36.378],[-118.1562,36.3817],[-118.1601,36.3876],[-118.1623,36.3913],[-118.1594,36.394],[-118.149,36.397],[-118.145,36.3997],[-118.1414,36.4056],[-118.1402,36.4142],[-118.1424,36.4187],[-118.1486,36.4229],[-118.1548,36.4266],[-118.1599,36.4298],[-118.165,36.4294],[-118.1748,36.4268],[-118.1823,36.426],[-118.192,36.4265],[-118.2028,36.4298],[-118.2131,36.4308],[-118.2153,36.434],[-118.2129,36.4408],[-118.2151,36.4477],[-118.2173,36.4531],[-118.2223,36.4595],[-118.2331,36.4651],[-118.238,36.4769],[-118.2483,36.4802],[-118.2516,36.4843],[-118.2447,36.4911],[-118.2395,36.4915],[-118.2394,36.4955],[-118.2411,36.5001],[-118.2409,36.5101],[-118.2413,36.5187],[-118.2458,36.5237],[-118.2498,36.5265],[-118.2513,36.5369],[-118.2587,36.5447],[-118.2666,36.5489],[-118.2774,36.5531],[-118.2894,36.5586],[-118.2938,36.5659],[-118.296,36.5755],[-118.2924,36.5836],[-118.2871,36.5899],[-118.2819,36.5957],[-118.2806,36.6021],[-118.2892,36.604],[-118.2977,36.6104],[-11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I.","contributorId":23678,"corporation":false,"usgs":true,"family":"Barnes","given":"I.","affiliations":[],"preferred":false,"id":359417,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":1013643,"text":"1013643 - 1965 - Characteristics and identification of oxidative Pseudomonads isolated from diseased fish","interactions":[],"lastModifiedDate":"2025-02-05T16:18:27.467682","indexId":"1013643","displayToPublicDate":"1965-01-01T00:00:00","publicationYear":"1965","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2300,"text":"Journal of General Microbiology","active":true,"publicationSubtype":{"id":10}},"title":"Characteristics and identification of oxidative Pseudomonads isolated from diseased fish","docAbstract":"<p><span>Several characteristics of 20 strains of oxidative pseudomonads, all but one of which were isolated from freshwater fish, were determined. All strains oxidized glucose and gluconate, produced NH</span><sub><span class=\"jp-sub\">3</span></sub><span>&nbsp;from 1 % peptone, grew at 6, 12, 20 and 30° and produced cytochrome oxidase. Lipase was produced by 17 of the strains, while 15 produced gelatinase, and 16 produced fluorescent pigment. These and other characteristics used to identify fish-spoilage pseudomonads are also useful for identification of fish-pathogenic pseudomonads. Species determinations from the present data were not attempted. However, from previously published data on speciation of&nbsp;</span><i><span class=\"jp-italic\">Pseudomonas</span></i><span>, most of the 20 strains appeared to be closely related to or identical with <i>P.&nbsp;</i></span><i><span class=\"jp-italic\">fluorescens</span></i><span>.</span></p>","language":"English","publisher":"Microbiology Society","doi":"10.1099/00221287-38-1-1","usgsCitation":"Bullock, G.L., Snieszko, S.F., and Dunbar, C.E., 1965, Characteristics and identification of oxidative Pseudomonads isolated from diseased fish: Journal of General Microbiology, v. 38, p. 1-7, https://doi.org/10.1099/00221287-38-1-1.","productDescription":"7 p.","startPage":"1","endPage":"7","numberOfPages":"7","costCenters":[{"id":365,"text":"Leetown Science Center","active":true,"usgs":true}],"links":[{"id":486903,"rank":2,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1099/00221287-38-1-1","text":"Publisher Index Page"},{"id":131914,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"38","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e3e4b07f02db5e539f","contributors":{"authors":[{"text":"Bullock, G. L.","contributorId":69498,"corporation":false,"usgs":true,"family":"Bullock","given":"G.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":318949,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Snieszko, S. F.","contributorId":13169,"corporation":false,"usgs":true,"family":"Snieszko","given":"S.","middleInitial":"F.","affiliations":[],"preferred":false,"id":318948,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Dunbar, C. E.","contributorId":96623,"corporation":false,"usgs":true,"family":"Dunbar","given":"C.","middleInitial":"E.","affiliations":[],"preferred":false,"id":318950,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70010682,"text":"70010682 - 1965 - The binary system K2SO4CaSO4","interactions":[],"lastModifiedDate":"2020-11-24T00:13:45.438175","indexId":"70010682","displayToPublicDate":"1965-01-01T00:00:00","publicationYear":"1965","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 binary system K<sub>2</sub>SO<sub>4</sub>CaSO<sub>4</sub>","title":"The binary system K2SO4CaSO4","docAbstract":"<div id=\"abstracts\" class=\"Abstracts u-font-serif\"><div id=\"aep-abstract-id6\" class=\"abstract author\"><div id=\"aep-abstract-sec-id7\"><p>The binary system K<sub>2</sub>SO<sub>4</sub>CaSO<sub>4</sub><span>&nbsp;</span>was studied by means of heating-cooling curves, differential thermal analysis, high-temperature quenching technique and by means of a heating stage mounted on an X-ray diffractometer. Compositions and quench products were identified optically and by X-ray. Limited solid solution of CaSO<sub>4</sub><span>&nbsp;</span>in K<sub>2</sub>SO<sub>4</sub><span>&nbsp;</span>was found. There is a eutectic at 875°C and 34 wt. per cent CaSO<sub>4</sub>. Calcium langbeinite melts incongruently at 1011°C. The melting-point of CaSO<sub>4</sub><span>&nbsp;</span>(1462°C) was determined by the quenching technique using sealed platinum tubes. The only intermediate crystalline phase found in the system is K<sub>2</sub>SO<sub>4</sub>·2CaSO<sub>4</sub><span>&nbsp;</span>(calcium langbeinite).</p></div></div></div>","language":"English","publisher":"Elsevier","doi":"10.1016/0022-1902(65)80189-0","issn":"00221902","usgsCitation":"Rowe, J., Morey, G., and Hansen, I., 1965, The binary system K2SO4CaSO4: Journal of Inorganic and Nuclear Chemistry, v. 27, no. 1, p. 53-58, https://doi.org/10.1016/0022-1902(65)80189-0.","productDescription":"6 p.","startPage":"53","endPage":"58","numberOfPages":"6","costCenters":[],"links":[{"id":219402,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"27","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505ba9e7e4b08c986b3225c2","contributors":{"authors":[{"text":"Rowe, J.J.","contributorId":29460,"corporation":false,"usgs":true,"family":"Rowe","given":"J.J.","affiliations":[],"preferred":false,"id":359418,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Morey, G.W.","contributorId":108155,"corporation":false,"usgs":true,"family":"Morey","given":"G.W.","email":"","affiliations":[],"preferred":false,"id":359420,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Hansen, I.D.","contributorId":81630,"corporation":false,"usgs":true,"family":"Hansen","given":"I.D.","email":"","affiliations":[],"preferred":false,"id":359419,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70176114,"text":"70176114 - 1965 - Surface water records of Texas, 1964","interactions":[],"lastModifiedDate":"2017-04-19T10:37:54","indexId":"70176114","displayToPublicDate":"1965-01-01T00:00:00","publicationYear":"1965","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"seriesTitle":{"id":5196,"text":"Water Data Report","active":true,"publicationSubtype":{"id":6}},"title":"Surface water records of Texas, 1964","docAbstract":"<p>The surface-water records for the 1964 water year for gaging stations, partial-record stations, miscellaneous sites, and base-flow studies within the State of Texas are given in this report. For convenience there are also included records for a few pertinent gaging stations in bordering States. The records were collected and computed by the Water Resources Division of the U. S. Geological Survey, under the direction of Trigg Twichell, district chief, Water Resources Division. </p><p>Through September 30, 1960, the records of discharge and stage of streams and contents and stage of lakes or reservoirs were published in an annual series of U.S. Geological Survey water supply papers, entitled \"Surface Water Supply of the United States.\" Since 1951 there have been 20 volumes in the series; each volume covered an area whose boundaries coincided with those of certain natural drainage areas. The records in Texas were contained in Parts 7 and 8 of that series. </p><p>Beginning with the 1961 water year, streamflow records and related data have been released by the Geological Survey in annual reports on a State-boundary basis. Distribution of these basic-data reports is limited and primarily for local needs. Records will be published in Geological Survey water-supply papers at 5-year intervals.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/70176114","collaboration":"Prepared in cooperation with the Texas Water Commission, Pecos River Commission, Sabine River Compact Administration, City of Dallas, City of Houston, U.S. Army Corps of Engineers, U.S. Soil Conservation Service, U.S. Public Health Service, and U.S. Bureau of Reclamation","usgsCitation":"U.S. Geological Survey, 1965, Surface water records of Texas, 1964: Water Data Report, xiv, 479 p., https://doi.org/10.3133/70176114.","productDescription":"xiv, 479 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":583,"text":"Texas Water Science 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,{"id":1718,"text":"wsp1809I - 1965 - Ground-water pumpage and water-level changes in the Milwaukee-Waukesha area, Wisconsin, 1950-61","interactions":[],"lastModifiedDate":"2023-03-13T20:10:12.868331","indexId":"wsp1809I","displayToPublicDate":"1965-01-01T00:00:00","publicationYear":"1965","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":341,"text":"Water Supply Paper","code":"WSP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1809","chapter":"I","title":"Ground-water pumpage and water-level changes in the Milwaukee-Waukesha area, Wisconsin, 1950-61","docAbstract":"<p>Artesian water pressure in the deep sandstone aquifer continued to decline throughout most of the Milwaukee-Waukesha area, Wisconsin between 1950 and 1961. Areas of greatest water-level decline were in northeast Waukesha County and in northwest Milwaukee County. The chief cause of the decline was continued heavy pumpage. The major aquifers of southeastern Wisconsin are the Niagara aquifer, which is primarily Niagara Dolomite of Silurian age, and the sandstone aquifer, which consists of sandstones of Cambrian and Ordovician ages. Locally, the glacial sands and gravels ,of Pleistocene age also are important aquifers. In the Milwaukee-Waukesha area, the sandstone aquifer is completely artesian, confined above by the Maquoketa Shale. The Niagara aquifer is generally unconfined. Pumpage from the sandstone aquifer in the Milwaukee-Waukesha area de- creased from about 23.3 million gallons per day in 1950 to about 20.9 million gallons per day in 1961. The principal reason for decreased pumpage was sub- stitution of surface-water supply from Lake Michigan. Between 1950 and 1961, the water-level changes in wells in the sandstone aquifer ranged from plus 10 feet at Town of Lake to minus 98 feet in northwest Milwaukee. Except for a small area near Town of Lake, water levels in wells in the Milwaukee-Waukesha area were lower in 1961 than in 1950. Water-level changes were directly related to the pumpage pattern and pump- age changes. Increased pumpage at Waukesha and in northwest Milwaukee and continued heavy pumpage at Wauwatosa caused widespread water-level declines in northeast Waukesha County and in northwest Milwaukee County. Locally, decreased pumpage at West Milwaukee allowed limited recovery of water levels since 1957. Estimates of pumpage through the year 1975 indicate a pumpage decrease in the middle 1960's, followed by an increase in the late 1960's and early 1970's. Additional conversion to surface-water supply in Milwaukee County will account for most pumpage decreases. Increased pumpage is most likely in Waukesha County where the population is expanding rapidly and an adequate surface-water supply is not readily accessible. The westward shift of the pumpage pattern may cause an additional water-level decline of about 50 feet at Waukesha but will permit water levels to recover about 100 feet at West Allis by 1975. Partial or complete conversion to surface-water supplies by municipalities that depend entirely on water from the sandstone aquifer would allow greater use of the sandstone aquifer by isolated suburban developments and industries.</p>","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Contributions to the hydrology of the United States","largerWorkSubtype":{"id":5,"text":"USGS Numbered Series"},"language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wsp1809I","collaboration":"Prepared in cooperation with the University of Wisconsin, Geological and Natural History Survey","usgsCitation":"Green, J.H., and Hutchinson, R.D., 1965, Ground-water pumpage and water-level changes in the Milwaukee-Waukesha area, Wisconsin, 1950-61: U.S. Geological Survey Water Supply Paper 1809, Report: iii, 19 p. ; 2 Plates: 19.50 x 24.00 inches and 18.50 x 24.00 inches, https://doi.org/10.3133/wsp1809I.","productDescription":"Report: iii, 19 p. ; 2 Plates: 19.50 x 24.00 inches and 18.50 x 24.00 inches","numberOfPages":"23","onlineOnly":"N","additionalOnlineFiles":"Y","costCenters":[{"id":677,"text":"Wisconsin Water Science Center","active":true,"usgs":true}],"links":[{"id":26806,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1809i/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":136940,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1809i/report-thumb.jpg"},{"id":26805,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1809i/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":26804,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1809i/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":414041,"rank":5,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_25008.htm","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Wisconsin","city":"Milwaukee, Waukesha","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -88.82011978710044,\n              43.6048598948214\n            ],\n            [\n              -88.82011978710044,\n              42.619688745253114\n            ],\n            [\n              -87.76500461016991,\n              42.619688745253114\n            ],\n            [\n              -87.76500461016991,\n              43.6048598948214\n            ],\n            [\n              -88.82011978710044,\n              43.6048598948214\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aa8e4b07f02db6673ff","contributors":{"authors":[{"text":"Green, J. H.","contributorId":43312,"corporation":false,"usgs":true,"family":"Green","given":"J.","email":"","middleInitial":"H.","affiliations":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"preferred":false,"id":144010,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hutchinson, R. D.","contributorId":99112,"corporation":false,"usgs":true,"family":"Hutchinson","given":"R.","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":144011,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70185700,"text":"70185700 - 1965 - Water supply and management concepts","interactions":[],"lastModifiedDate":"2017-03-27T16:57:44","indexId":"70185700","displayToPublicDate":"1965-01-01T00:00:00","publicationYear":"1965","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":5342,"text":"Industrial Water Engineering","active":false,"publicationSubtype":{"id":10}},"title":"Water supply and management concepts","docAbstract":"<p>If I had to cite one fact about water in the United States which would be not only the most important but also the most informative, the one I would choose would k this: Over 50 percent of all the water presently being used in the United States is used by industry, and nearly all of that is used for cooling.</p><p>The large amount of attention recently being given to water shortage and the expected rapid increase in demand for water is probably to some extent clouded because there are certain simple facts about water availability and water use which, though readily available, are not generally either known or understood.</p><p>Probably most people react to information in the public press about present and possible future water shortages with the thought that it is going to be more difficult in the future to supply the ordinary household with water for drinking, washing, and tbe culinary arts. As a matter of fact that may be true to some extent, but it is not the salient aspect.</p>","language":"English","usgsCitation":"Leopold, L.B., 1965, Water supply and management concepts: Industrial Water Engineering, v. 2, no. 1, p. 10-22.","productDescription":"5 p.","startPage":"10","endPage":"22","costCenters":[],"links":[{"id":338432,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"2","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"58da253fe4b0543bf7fda87b","contributors":{"authors":[{"text":"Leopold, Luna Bergere","contributorId":93884,"corporation":false,"usgs":true,"family":"Leopold","given":"Luna","email":"","middleInitial":"Bergere","affiliations":[],"preferred":false,"id":686444,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70174082,"text":"70174082 - 1965 - The water story in Central Iowa","interactions":[],"lastModifiedDate":"2016-06-27T14:45:29","indexId":"70174082","displayToPublicDate":"1965-01-01T00:00:00","publicationYear":"1965","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":2,"text":"State or Local Government Series"},"seriesTitle":{"id":5106,"text":"Iowa Geological Survey Water Atlas","active":true,"publicationSubtype":{"id":2}},"seriesNumber":"1","title":"The water story in Central Iowa","docAbstract":"<p>\"The general welfare of the people of the state of Iowa requires that the water resources of the state be put to beneficial use to the fullest extent of which they are capable.\" &nbsp;This can be achieved only by a knowledge and understanding of the water resources - their use, their source, their quality, their availability, and the demands place upon them. &nbsp;To provide such knowledge and understanding, the United States Geological Survey in cooperation with the Iowa Geological Survey produced this report on the utilization and availability of water in central Iowa.</p>\n<p>This report contains information on the past, present, and future statues of central Iowa;s water; information that can be used by the regional developer, the resource planner and manager, and other informed persons whose opinions and sound judgements are required in making decisions toward efficient development, management, use, and conservation of water. &nbsp;It gives an over-all view of the area's water resources and is aimed at guiding the people of central Iowa to the best available sources of water.</p>","language":"English","publisher":"Iowa Geological Survey","usgsCitation":"Twenter, F.R., and Coble, R.W., 1965, The water story in Central Iowa: Iowa Geological Survey Water Atlas 1, viii, 89 p.","productDescription":"viii, 89 p.","numberOfPages":"95","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":351,"text":"Iowa Water Science Center","active":true,"usgs":true}],"links":[{"id":324446,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":324445,"rank":1,"type":{"id":15,"text":"Index Page"},"url":"https://s-iihr34.iihr.uiowa.edu/publications/publications?category=Water-Supply-Bulletins"}],"country":"United States","state":"Iowa","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"Polygon\",\"coordinates\":[[[-93.972,42.5566],[-93.8563,42.557],[-93.7367,42.5568],[-93.6191,42.5565],[-93.5002,42.557],[-93.3819,42.557],[-93.2637,42.5564],[-93.1473,42.5561],[-93.0284,42.5562],[-92.9101,42.5557],[-92.7925,42.556],[-92.6755,42.5558],[-92.5553,42.555],[-92.5552,42.4695],[-92.5353,42.4694],[-92.5353,42.2972],[-92.6531,42.2971],[-92.7697,42.2964],[-92.7687,42.2101],[-92.7672,42.1234],[-92.7662,42.0348],[-92.7671,41.9494],[-92.7674,41.8618],[-92.7683,41.776],[-92.768,41.6879],[-92.7683,41.6007],[-92.7567,41.6011],[-92.7564,41.509],[-92.8729,41.5082],[-92.9894,41.5083],[-93.1047,41.5078],[-93.2181,41.5076],[-93.3304,41.5074],[-93.3304,41.4906],[-93.3347,41.4888],[-93.339,41.4833],[-93.3414,41.481],[-93.3445,41.481],[-93.347,41.4815],[-93.3488,41.4833],[-93.3531,41.4947],[-93.3561,41.4965],[-93.3586,41.4965],[-93.3598,41.4947],[-93.3611,41.4879],[-93.3641,41.4861],[-93.3703,41.4852],[-93.3733,41.4856],[-93.3745,41.4874],[-93.3764,41.4902],[-93.3776,41.492],[-93.3801,41.4929],[-93.3862,41.4929],[-93.3893,41.492],[-93.3935,41.4879],[-93.3978,41.4856],[-93.4021,41.4856],[-93.4052,41.4866],[-93.4058,41.4884],[-93.4052,41.4897],[-93.4015,41.492],[-93.3991,41.4938],[-93.3991,41.4961],[-93.4003,41.4988],[-93.4027,41.5002],[-93.407,41.4993],[-93.4113,41.4943],[-93.4162,41.4916],[-93.4199,41.4911],[-93.423,41.4925],[-93.4236,41.4943],[-93.4224,41.4961],[-93.4174,41.4997],[-93.4162,41.502],[-93.4162,41.5047],[-93.4174,41.507],[-93.4217,41.5084],[-93.426,41.5075],[-93.4346,41.502],[-93.4407,41.5025],[-93.4432,41.5038],[-93.4414,41.5061],[-93.4456,41.5061],[-93.5615,41.5102],[-93.6774,41.511],[-93.7927,41.5108],[-93.8773,41.5024],[-93.9006,41.5014],[-94.0159,41.5019],[-94.1299,41.5028],[-94.2427,41.5031],[-94.2419,41.5993],[-94.2812,41.6],[-94.281,41.6871],[-94.2813,41.7757],[-94.2811,41.8624],[-94.1671,41.8626],[-94.1652,41.8626],[-94.166,41.9493],[-94.1656,42.0347],[-94.1665,42.1228],[-94.1649,42.1519],[-94.1673,42.2091],[-94.2843,42.2089],[-94.3989,42.2086],[-94.3982,42.2954],[-94.3975,42.3835],[-94.3974,42.4721],[-94.4434,42.4718],[-94.4445,42.5572],[-94.4457,42.644],[-94.3279,42.6435],[-94.2101,42.6437],[-94.0942,42.6438],[-93.9714,42.6434],[-93.972,42.5566]]]},\"properties\":{\"name\":\"Boone\",\"state\":\"IA\"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"57724e36e4b07657d1a819df","contributors":{"authors":[{"text":"Twenter, F. R.","contributorId":81080,"corporation":false,"usgs":true,"family":"Twenter","given":"F.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":640835,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Coble, R. W.","contributorId":49380,"corporation":false,"usgs":true,"family":"Coble","given":"R.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":640836,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":81356,"text":"81356 - 1965 - Distribution of fishes in U. S. streams tributary to Lake Superior","interactions":[],"lastModifiedDate":"2016-02-25T10:52:08","indexId":"81356","displayToPublicDate":"1965-01-01T00:00:00","publicationYear":"1965","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":"516","title":"Distribution of fishes in U. S. streams tributary to Lake Superior","docAbstract":"<p>Experimental sea lamprey control by the Bureau of Commercial Fisheries on Lake Superior streams provided many new distributional records of the fish fauna. Seventy-one species were recorded from 175 streams. Specimens were collected at the electromechanical barriers, with electric shockers, with fyke nets, and during chemical treatment of streams. Maps showing stream records of each species are presented.</p>","language":"English","publisher":"U.S. Fish and Wildlife Service","usgsCitation":"Moore, H.H., and Braem, R.A., 1965, Distribution of fishes in U. S. streams tributary to Lake Superior: Special Scientific Report - Fisheries 516, 61 p.","productDescription":"61 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":324,"text":"Great Lakes Science Center","active":true,"usgs":true}],"links":[{"id":198915,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":101759,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://hdl.handle.net/2027/mdp.39015045826339?urlappend=%3Bseq=193"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a69e4b07f02db63bfbf","contributors":{"authors":[{"text":"Moore, Harry H.","contributorId":48670,"corporation":false,"usgs":true,"family":"Moore","given":"Harry","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":295282,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Braem, Robert A.","contributorId":34858,"corporation":false,"usgs":true,"family":"Braem","given":"Robert","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":295281,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70175644,"text":"70175644 - 1965 - Ground-water discharge from the Edwards and associated limestones, San Antonio area, Texas, 1964","interactions":[],"lastModifiedDate":"2016-08-17T14:16:52","indexId":"70175644","displayToPublicDate":"1965-01-01T00:00:00","publicationYear":"1965","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":2,"text":"State or Local Government Series"},"seriesTitle":{"id":5177,"text":"Edwards Underground Water District Bulletin","active":true,"publicationSubtype":{"id":2}},"seriesNumber":"8","title":"Ground-water discharge from the Edwards and associated limestones, San Antonio area, Texas, 1964","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"Edwards Underground Water District","usgsCitation":"Rettman, P., 1965, Ground-water discharge from the Edwards and associated limestones, San Antonio area, Texas, 1964: Edwards Underground Water District Bulletin 8, 4 p.","productDescription":"4 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"links":[{"id":326734,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"57b58ad0e4b03bcb0104bbbc","contributors":{"authors":[{"text":"Rettman, Paul","contributorId":68699,"corporation":false,"usgs":true,"family":"Rettman","given":"Paul","affiliations":[],"preferred":false,"id":645914,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70175643,"text":"70175643 - 1965 - Chemical analyses of water from observation wells in the Edwards and associated limestones, San Antonio area, Texas, 1964","interactions":[],"lastModifiedDate":"2016-08-17T14:15:05","indexId":"70175643","displayToPublicDate":"1965-01-01T00:00:00","publicationYear":"1965","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":2,"text":"State or Local Government Series"},"seriesTitle":{"id":5177,"text":"Edwards Underground Water District Bulletin","active":true,"publicationSubtype":{"id":2}},"seriesNumber":"7","title":"Chemical analyses of water from observation wells in the Edwards and associated limestones, San Antonio area, Texas, 1964","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"Edwards Underground Water District","usgsCitation":"Garza, S., 1965, Chemical analyses of water from observation wells in the Edwards and associated limestones, San Antonio area, Texas, 1964: Edwards Underground Water District Bulletin 7, 12 p.","productDescription":"12 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"links":[{"id":326731,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"57b58ac0e4b03bcb0104bb66","contributors":{"authors":[{"text":"Garza, Sergio","contributorId":88713,"corporation":false,"usgs":true,"family":"Garza","given":"Sergio","email":"","affiliations":[],"preferred":false,"id":645913,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70176115,"text":"70176115 - 1965 - Water quality records in Texas, 1964","interactions":[],"lastModifiedDate":"2016-08-26T10:16:39","indexId":"70176115","displayToPublicDate":"1965-01-01T00:00:00","publicationYear":"1965","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"seriesTitle":{"id":5196,"text":"Water Data Report","active":true,"publicationSubtype":{"id":6}},"title":"Water quality records in Texas, 1964","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/70176115","usgsCitation":"U.S. Geological Survey, 1965, Water quality records in Texas, 1964: Water Data Report, 199 p., https://doi.org/10.3133/70176115.","productDescription":"199 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"links":[{"id":327890,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"57c16841e4b0f2f0ceb90899","contributors":{"authors":[{"text":"U.S. Geological Survey","contributorId":128240,"corporation":true,"usgs":false,"organization":"U.S. Geological Survey","id":647151,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":1000291,"text":"1000291 - 1965 - Movements of hatchery-reared lake trout in Lake Superior","interactions":[],"lastModifiedDate":"2016-02-25T10:45:56","indexId":"1000291","displayToPublicDate":"1965-01-01T00:00:00","publicationYear":"1965","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":"Movements of hatchery-reared lake trout in Lake Superior","docAbstract":"<p>The history of stocking of lake trout (Salvelinus namaycush) in the Great Lakes is reviewed. The study of movements is based on capture of 24,275 fin-clipped lake trout taken in experimental gill nets and trawls and commercial gill nets. Yearling lake trout planted from shore dispersed to 15-fath (27-m) depths in 3A? hr. Most fish remained within 2 miles (3.2 km) of the planting site 2 months, but within 4 months some fish had moved as much as 17 miles (27 km). The highest abundance of planted lake trout was in areas 2-4 miles (3.2-6.4 km) from the planting site even 3 years after release. Distance moved and size of fish were not correlated. Dispersal of lake trout begins at planting and probably continues until the fish are mature. Most movement was eastward in southern Lake Superior and followed the counterclockwise surface currents. Movement is most rapid in areas of strong currents and slowest in areas of weak currents or eddies. Movement to areas west of the Keweenaw Peninsula was insignificant from plantings in Keweenaw Bay and nil from other plantings farther east. Lake trout planted in the eastern third of the lake dispersed more randomly than those planted farther west. Few fish moved farther offshore than the 50-fath (91-m) contour. Lake trout planted in Canadian waters made insignificant contributions to populations in US waters.</p>","language":"English","publisher":"NRC Research Press","doi":"10.1139/f65-093","usgsCitation":"Pycha, R.L., Dryer, W.R., and King, G.R., 1965, Movements of hatchery-reared lake trout in Lake Superior: Journal of the Fisheries Research Board of Canada, v. 22, no. 4, p. 999-1024, https://doi.org/10.1139/f65-093.","productDescription":"26 p.","startPage":"999","endPage":"1024","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":324,"text":"Great Lakes Science Center","active":true,"usgs":true}],"links":[{"id":132878,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"22","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a6de4b07f02db63ee14","contributors":{"authors":[{"text":"Pycha, Richard L.","contributorId":17175,"corporation":false,"usgs":true,"family":"Pycha","given":"Richard","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":308346,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Dryer, William R.","contributorId":71921,"corporation":false,"usgs":true,"family":"Dryer","given":"William","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":308347,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"King, George R.","contributorId":74721,"corporation":false,"usgs":true,"family":"King","given":"George","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":308348,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70010445,"text":"70010445 - 1965 - Potassium, rubidium, strontium, thorium, uranium, and the ratio of strontium-87 to strontium-86 in oceanic tholeiitic basalt","interactions":[],"lastModifiedDate":"2020-11-24T00:31:09.499823","indexId":"70010445","displayToPublicDate":"1965-01-01T00:00:00","publicationYear":"1965","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3338,"text":"Science","active":true,"publicationSubtype":{"id":10}},"title":"Potassium, rubidium, strontium, thorium, uranium, and the ratio of strontium-87 to strontium-86 in oceanic tholeiitic basalt","docAbstract":"<div class=\"panel-pane pane-highwire-panel-tabs-container article__body\"><div class=\"pane-content\"><div id=\"panels-ajax-tab-container-highwire_article_tabs\" class=\"panels-ajax-tab-container\" data-panels-ajax-tab-preloaded=\"jnl_sci_tab_art\"><div class=\"panels-ajax-tab-wrap-jnl_sci_tab_art\"><div class=\"panel-display panel-1col clearfix\"><div class=\"panel-panel panel-col\"><div><div class=\"panel-pane pane-highwire-markup\"><div class=\"pane-content\"><div class=\"highwire-markup\"><div id=\"content-block-markup\" data-highwire-cite-ref-tooltip-instance=\"highwire_reflinks_tooltip\" data-highwire-glossary-tooltip-instance=\"highwire_reflinks_tooltip\"><div class=\"article abstract-view \"><div id=\"abstract-1\" class=\"section abstract\"><p id=\"p-1\">The average concentrations of potassium, rubidium, strontium, thorium, and uranium in oceanic tholeiitic basalt are (in parts per million) K, 1400; Rb, 1.2; Sr, 120; Th, 0.2; and U, 0.1. The ratio Sr<sup>87</sup><span>&nbsp;</span>to Sr<sup>86</sup><span>&nbsp;</span>is about 0.702, that of K to U is 1.4 x 10<sup>4</sup>, and of Th to U is 1.8. These amounts of K, Th, U, and radiogenic Sr<sup>87</sup><span>&nbsp;</span>are less than in other common igneous rocks. The ratios of Th to U and Sr<sup>87</sup><span>&nbsp;</span>to Sr<sup>86</sup><span>&nbsp;</span>suggest that the source region of the oceanic tholeiites was differentiated from the original mantle material some time in the geologic past.</p></div></div><span id=\"related-urls\"></span></div></div></div></div></div></div></div></div></div></div></div>","language":"English","publisher":"AAAP","doi":"10.1126/science.150.3698.886","issn":"00368075","usgsCitation":"Tatsumoto, M., Hedge, C., and Engel, A., 1965, Potassium, rubidium, strontium, thorium, uranium, and the ratio of strontium-87 to strontium-86 in oceanic tholeiitic basalt: Science, v. 150, no. 3698, p. 886-888, https://doi.org/10.1126/science.150.3698.886.","productDescription":"3 p.","startPage":"886","endPage":"888","numberOfPages":"3","costCenters":[],"links":[{"id":218724,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"150","issue":"3698","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a7eaae4b0c8380cd7a68c","contributors":{"authors":[{"text":"Tatsumoto, M.","contributorId":76798,"corporation":false,"usgs":true,"family":"Tatsumoto","given":"M.","email":"","affiliations":[],"preferred":false,"id":358943,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hedge, C. E.","contributorId":73611,"corporation":false,"usgs":true,"family":"Hedge","given":"C. E.","affiliations":[],"preferred":false,"id":358942,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Engel, A.E.J.","contributorId":52246,"corporation":false,"usgs":true,"family":"Engel","given":"A.E.J.","email":"","affiliations":[],"preferred":false,"id":358941,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70010523,"text":"70010523 - 1965 - Vacuum-jacketed hydrofluoric acid solution calorimeter","interactions":[],"lastModifiedDate":"2020-11-24T00:24:12.732825","indexId":"70010523","displayToPublicDate":"1965-01-01T00:00:00","publicationYear":"1965","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":"Vacuum-jacketed hydrofluoric acid solution calorimeter","docAbstract":"<div class=\"hlFld-Abstract\"><div class=\"NLM_paragraph\">A vacuum‐jacketed metal<span>&nbsp;</span>calorimeter<span>&nbsp;</span>for determining heats of solution in aqueous HF was constructed. The reaction vessel was made of<span>&nbsp;</span>copper<span>&nbsp;</span>and was heavily<span>&nbsp;</span>gold<span>&nbsp;</span>plated. The<span>&nbsp;</span>calorimeter<span>&nbsp;</span>has a cooling constant of 0.6 cal‐deg<sup>−1</sup>‐min<sup>−1</sup>, approximately ¼ that of the air‐jacketed<span>&nbsp;</span>calorimeters<span>&nbsp;</span>most commonly used with HF. It reaches equilibrium within 10 min after turning off the<span>&nbsp;</span>heater<span>&nbsp;</span>current. Measurements of the heat of solution of reagent grade KCl(−100 mesh dried 2 h at 200°C) at a mole ratio of 1 KCl to 200 H<sub>2</sub>O gave Δ<i>H</i><span>&nbsp;</span>= 4198±11 cal at 25°C.</div></div><div class=\"article-paragraphs\"><div class=\"sectionInfo\"><h4 class=\"refHeading\"><a name=\"_i1\" class=\"mce-item-anchor\"></a></h4></div></div>","language":"English","publisher":"AIP","doi":"10.1063/1.1719605","issn":"00346748","usgsCitation":"Robie, R.A., 1965, Vacuum-jacketed hydrofluoric acid solution calorimeter: Review of Scientific Instruments, v. 36, no. 4, p. 484-486, https://doi.org/10.1063/1.1719605.","productDescription":"3 p.","startPage":"484","endPage":"486","numberOfPages":"3","costCenters":[],"links":[{"id":480358,"rank":1,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1063/1.1719605","text":"Publisher Index Page"},{"id":219618,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"36","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505bc0f6e4b08c986b32a3d8","contributors":{"authors":[{"text":"Robie, R. A.","contributorId":71237,"corporation":false,"usgs":true,"family":"Robie","given":"R.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":359108,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
]}