{"pageNumber":"6766","pageRowStart":"169125","pageSize":"25","recordCount":184617,"records":[{"id":70190791,"text":"70190791 - 1962 - Records of selected wells and springs, selected drillers' logs of wells, and chemical analyses of ground and surface waters, northern Utah Valley, Utah County, Utah","interactions":[],"lastModifiedDate":"2017-09-14T11:00:56","indexId":"70190791","displayToPublicDate":"1962-01-01T00:00:00","publicationYear":"1962","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":2,"text":"State or Local Government Series"},"seriesTitle":{"id":5497,"text":"Utah Basic-Data Report","active":false,"publicationSubtype":{"id":2}},"seriesNumber":"2","title":"Records of selected wells and springs, selected drillers' logs of wells, and chemical analyses of ground and surface waters, northern Utah Valley, Utah County, Utah","docAbstract":"<p>This report is intended to serve two purposes: (1) to make available to the public basic ground-water data useful in planning and studying development of water resources and (2) to supplement an interpretive report that will be published later.</p><p>Records were collected during the period 1956-59 by the U.S. Geological Survey in cooperation with the Utah State Engineer as a part of the investigation of the ground-water resources of northern Utah Walley in Utah County, Utah. Some earlier data and other information in the tables are from published reports on the ground-water resources of northern Utah Walley. The interpretive material will be published cooperatively by the U.S. Geological Survey and the Utah State Engineer in a companion report by Seymour Subitzky.</p><p>This report is most useful in predicting conditions likely to be found in areas that are being considered as well sites. The person considering the new well can spot the proposed site on plate 1 and examine the records of nearby wells as shown on the tables. From tables 1, 2, and h he can note the type of material that yields water to wells in the vicinity; from table 2 he can note (1) the depth and diameter of wells in the vicinity and the yield of some of those wells, and (2) the depth to water or the feet of water pressure in the vicinity; from table 3 and plate 1 he may note the location of springs and the conditions related to the occurrence of these springs; and from tables 5 and 6 he may note the chemical quality of the water from wells and from some surface sources, and the uses of these waters. If the reader decides from his examination that conditions are favorable, he may place an application to drill a well with the State Engineer. If the State Engineer believes unappropriated water is available, the application may be approved after minimum statutory requirements have been satisfied.</p><p>The report is also useful when planning large-scale developments of water supply. This and other uses of the report will be helped by use of the interpretive report upon its release.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Salt Lake City, UT","collaboration":"Prepared in cooperation with the Utah State Engineer","usgsCitation":"Subitsky, S., 1962, Records of selected wells and springs, selected drillers' logs of wells, and chemical analyses of ground and surface waters, northern Utah Valley, Utah County, Utah: Utah Basic-Data Report 2, 14 p.","productDescription":"14 p.","costCenters":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":345756,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":345754,"rank":1,"type":{"id":15,"text":"Index Page"},"url":"https://www.waterrights.utah.gov/cgi-bin/docview.exe?Folder=TP21-1-040&Title=Basic+Data+Report+2"}],"country":"United States","state":"Utah","county":"Utah County","otherGeospatial":"Utah Valley","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"59bb953ce4b091459a57823e","contributors":{"authors":[{"text":"Subitsky, Seymour","contributorId":77227,"corporation":false,"usgs":true,"family":"Subitsky","given":"Seymour","email":"","affiliations":[],"preferred":false,"id":710415,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70171158,"text":"70171158 - 1962 - An instance of upwelling along the east shore of Lake Michigan","interactions":[],"lastModifiedDate":"2016-05-24T10:29:24","indexId":"70171158","displayToPublicDate":"1962-01-01T00:00:00","publicationYear":"1962","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"An instance of upwelling along the east shore of Lake Michigan","docAbstract":"<p>No abstract available.</p>","largerWorkType":{"id":24,"text":"Conference Paper"},"largerWorkTitle":"Proceedings of the 5th Conference on Great Lakes Research","largerWorkSubtype":{"id":19,"text":"Conference Paper"},"conferenceTitle":"5th Conference on Great Lakes Research","conferenceDate":"April 9-10, 1962","conferenceLocation":"Toronto, Canada","language":"English","publisher":"University of Michigan","usgsCitation":"Moffett, J.W., 1962, An instance of upwelling along the east shore of Lake Michigan, <i>in</i> Proceedings of the 5th Conference on Great Lakes Research, Toronto, Canada, April 9-10, 1962.","productDescription":"1 p.","startPage":"126","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":324,"text":"Great Lakes Science Center","active":true,"usgs":true}],"links":[{"id":321596,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"574d643ce4b07e28b66834b8","contributors":{"authors":[{"text":"Moffett, James W.","contributorId":94245,"corporation":false,"usgs":true,"family":"Moffett","given":"James","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":630137,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70009799,"text":"70009799 - 1962 - Behaviour of calcium carbonate in sea water","interactions":[],"lastModifiedDate":"2020-09-09T13:46:35.413922","indexId":"70009799","displayToPublicDate":"1962-01-01T00:00:00","publicationYear":"1962","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":"Behaviour of calcium carbonate in sea water","docAbstract":"<div id=\"abstracts\" class=\"Abstracts u-font-serif\"><div id=\"aep-abstract-id4\" class=\"abstract author\"><div id=\"aep-abstract-sec-id5\"><p>Anomalies in the behaviour of calcium carbonate in natural solutions diminish when considered in context. Best values found by traditional oceanographie methods for the apparent solubility product constant<span>&nbsp;</span><i>K</i>'<sub><i>CaCO</i></sub><sub>3</sub><span>&nbsp;</span>in sea water at atmospheric pressure are consistent mineralogically—at 36 parts per thousand salinity and T-25°C,<span>&nbsp;</span><i>K</i>'<sub><i>aragonlte</i></sub><span>&nbsp;</span>is estimated as 1.12 × 10<sup>−6</sup><span>&nbsp;</span>and<span>&nbsp;</span><i>K</i>'<sub><i>calcite</i></sub><span>&nbsp;</span>as 0.61 × 10<sup>−6</sup>. At 30°C the corresponding values are 0.98 × 10<sup>−6</sup><span>&nbsp;</span>for aragonite and 0.53 × 10<sup>−6</sup><span>&nbsp;</span>for calcite. Because the<span>&nbsp;</span><i>K</i>' computations do not compensate for ionic activity, however, they cannot give thermodynamically satisfactory results. It is of interest, therefore, that approximate methods and information now available permit the estimation from the same basic data of an activity product constant<span>&nbsp;</span><i>K</i><sub><i>CaCO</i></sub><sub>3</sub><span>&nbsp;</span>close to that found in solutions to which Debye-Hückel theory applies. Such methods indicate approximate<span>&nbsp;</span><i>K</i><sub><i>aragonite</i></sub><span>&nbsp;</span>7.8 × 10<sup>−9</sup><span>&nbsp;</span>for surface sea water at 29°C;<span>&nbsp;</span><i>K</i><sub><i>calcite</i></sub><span>&nbsp;</span>would be proportionately lower.</p><p>Field data and experimental results indicate that the mineralogy of precipitated CaCO<sub>3</sub><span>&nbsp;</span>depends primarily on degree of supersaturation, thus also on kinetic or biologic factors that facilitate or inhibit a high degree of supersaturation. The shallow, generally hypersaline bank waters west of Andros Island yield aragonitic sediments with<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>O</mtext><msup><mi></mi><mn>18</mn></msup><mtext>O</mtext><msup><mi></mi><mn>16</mn></msup></math>\"><span class=\"MJX_Assistive_MathML\">O18O16</span></span></span><span>&nbsp;</span>ratios that imply precipitation mainly during the warmer months, when the combination of a high rate of evaporation, increasing salinity (and ionic strength), maximal temperatures and photosynthetic removal of CO<sub>2</sub><span>&nbsp;</span>result in high apparent supersaturation. The usual precipitate from solutions of low ionic strength is calcite, except where the aragonite level of supersaturation is reached as a result of diffusion phenomena (<i>e.g.</i><span>&nbsp;</span>dripstones), gradual and marked evaporation, or biologic intervention. Published data also suggest the possibility of distinct chemical milieus for crystallographic variations in skeletal calcium carbonate. It appears that in nature aragonite precipitates from solutions that are supersaturated with respect to both calcite and aragonite and calcite between saturation levels for the two species. Such a relation is consistent with Ostwald's rule of successive reactions.</p><p>Aragonitc of marine origin persists in contact with supersaturated interstitial solutions at ordinary temperature and pressure. Conversion to calcite follows transfer to solutions undersaturated with respect to aragonite or upon exposure to the moist atmosphere.</p></div></div></div><ul id=\"issue-navigation\" class=\"issue-navigation u-margin-s-bottom u-bg-grey1\"></ul>","language":"English","publisher":"Elsevier","doi":"10.1016/0016-7037(62)90117-5","usgsCitation":"Cloud, P.E., 1962, Behaviour of calcium carbonate in sea water: Geochimica et Cosmochimica Acta, v. 26, no. 8, p. 867-884, https://doi.org/10.1016/0016-7037(62)90117-5.","productDescription":"19 p.","startPage":"867","endPage":"884","costCenters":[],"links":[{"id":218757,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"26","issue":"8","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059f0abe4b0c8380cd4a84d","contributors":{"authors":[{"text":"Cloud, P. E. Jr.","contributorId":6507,"corporation":false,"usgs":true,"family":"Cloud","given":"P.","suffix":"Jr.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":357173,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70195894,"text":"70195894 - 1962 - Ground water in the Hatton area, Traill and Steele Counties, North Dakota","interactions":[],"lastModifiedDate":"2018-03-07T13:25:46","indexId":"70195894","displayToPublicDate":"1962-01-01T00:00:00","publicationYear":"1962","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":2,"text":"State or Local Government Series"},"seriesTitle":{"id":5646,"text":"North Dakota Ground Water Studies","active":true,"publicationSubtype":{"id":2}},"seriesNumber":"39","title":"Ground water in the Hatton area, Traill and Steele Counties, North Dakota","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"North Dakota State Water Conservation Commission","usgsCitation":"Adolphson, D.G., 1962, Ground water in the Hatton area, Traill and Steele Counties, North Dakota: North Dakota Ground Water Studies 39, 23 p.","productDescription":"23 p.","costCenters":[{"id":478,"text":"North Dakota Water Science Center","active":true,"usgs":true},{"id":34685,"text":"Dakota Water Science Center","active":true,"usgs":true}],"links":[{"id":352288,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5aff6345e4b0da30c1bfdf08","contributors":{"authors":[{"text":"Adolphson, D. G.","contributorId":106081,"corporation":false,"usgs":true,"family":"Adolphson","given":"D.","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":730412,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70185627,"text":"70185627 - 1962 - Water","interactions":[],"lastModifiedDate":"2017-03-24T16:02:24","indexId":"70185627","displayToPublicDate":"1962-01-01T00:00:00","publicationYear":"1962","noYear":false,"publicationType":{"id":4,"text":"Book"},"publicationSubtype":{"id":15,"text":"Monograph"},"title":"Water","docAbstract":"<p>What do you use water for?</p><p>If someone asked you this question you would probably think right away of water for drinking. Then you would think of water for bathing, brushing teeth, flushing the toilet. Your list would get longer as you thought of water for cooking, washing the dishes, running the garbage grinder. Water for lawn watering, for play pools, for swimming pools, for washing the car and the dog. Water for washing machines and for air conditioning. You can hardly do without water for fun and pleasure—water for swimming, boating, fishing, water-skiing, and skin diving. In school or the public library, you need water to wash your hands, or to have a drink. If your home or school bursts into flames, quantities of water are needed to put it out.</p><p>In fact, life to Americans is unthinkable without large supplies of fresh, clean water. If you give the matter a little thought, you will realize that people in many countries, even in our own, may suffer from disease and dirt simply because their homes are not equipped with running water. Imagine your own town if for some reason - an explosion, perhaps - water service were cut off for a week or several weeks. You would have to drive or walk to a neighboring town and bring water back in pails. Certainly if people had to carry water themselves they might not be inclined to bathe very often; washing clothes would be a real chore.</p><p>Nothing can live without water. The earth is covered by water over three-fourths of its surface - water as a liquid in rivers, lakes and oceans, and water as ice and snow on the tops of high mountains and in the polar regions. Only one-quarter of our bodies is bone and muscle; the other three-fourths is made of water. We need water to live,&nbsp;and so do plants and animals. People and animals can live a long time without food, but without water they die in a few days. Without water, everything would die, and the world would turn into a huge desert. </p>","language":"English","publisher":"Saalfield Publishing Company","publisherLocation":"Akron, OH; New York, NY","usgsCitation":"Leopold, L.B., and Baldwin, H., 1962, Water, v. 1, no. 48, 48 p.","productDescription":"48 p.","numberOfPages":"50","costCenters":[],"links":[{"id":338328,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"1","issue":"48","publicComments":"Saalfield Science Series no. 5807","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"58d6304ce4b05ec799131145","contributors":{"authors":[{"text":"Leopold, Luna Bergere","contributorId":93884,"corporation":false,"usgs":true,"family":"Leopold","given":"Luna","email":"","middleInitial":"Bergere","affiliations":[],"preferred":false,"id":686154,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Baldwin, Helene L.","contributorId":34622,"corporation":false,"usgs":true,"family":"Baldwin","given":"Helene L.","affiliations":[],"preferred":false,"id":686155,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":1000071,"text":"1000071 - 1962 - Comparative toxicity of 3-trifluormethyl-4-nitrophenol (TFM) to larval lampreys and eleven species of fishes","interactions":[],"lastModifiedDate":"2016-03-07T12:11:42","indexId":"1000071","displayToPublicDate":"1962-01-01T00:00:00","publicationYear":"1962","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":"Comparative toxicity of 3-trifluormethyl-4-nitrophenol (TFM) to larval lampreys and eleven species of fishes","docAbstract":"<p><span>The tolerances of larval lampreys, rainbow trout, and 10 species of warmwater fishes to 3-trifluormethyl-4-nitrophenol (TFM), a selective lamprey larvicide, were determined in three dilution waters of different physical and chemical characteristics. Differential toxic effects of the chemical to larval lampreys and test fishes varied broadly with the species of fish. Smallmouth bass and other centrarchids were most tolerant of the chemical; walleye, yellow perch, bullheads, and white suckers were most susceptible. The toxicity of TFM to both lampreys and fishes diminished as the conductivity and alkalinity of the dilution water increased. The differential action of the chemical was retained in all waters, however.</span></p>","language":"English","publisher":"Taylor & Francis","doi":"10.1577/1548-8659(1962)91[342:CTOTTT]2.0.CO;2","usgsCitation":"Applegate, V.C., and King, E.L., 1962, Comparative toxicity of 3-trifluormethyl-4-nitrophenol (TFM) to larval lampreys and eleven species of fishes: Transactions of the American Fisheries Society, v. 91, no. 4, p. 342-345, https://doi.org/10.1577/1548-8659(1962)91[342:CTOTTT]2.0.CO;2.","productDescription":"4 p.","startPage":"342","endPage":"345","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":324,"text":"Great Lakes Science Center","active":true,"usgs":true}],"links":[{"id":128996,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"91","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b24e4b07f02db6ae471","contributors":{"authors":[{"text":"Applegate, Vernon C.","contributorId":39317,"corporation":false,"usgs":true,"family":"Applegate","given":"Vernon","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":308029,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"King, Everett L.","contributorId":54922,"corporation":false,"usgs":true,"family":"King","given":"Everett","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":308030,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":2000020,"text":"2000020 - 1962 - A photoelectric amplifier as a dye detector","interactions":[],"lastModifiedDate":"2013-01-28T14:07:08","indexId":"2000020","displayToPublicDate":"1962-01-01T00:00:00","publicationYear":"1962","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":3,"text":"Organization Series"},"seriesTitle":{"id":222,"text":"Technical Report","active":false,"publicationSubtype":{"id":3}},"seriesNumber":"4","title":"A photoelectric amplifier as a dye detector","docAbstract":"A dye detector, based on a modified photoelectric amplifier, has been planned, built, and tested. It was designed to record automatically the time of arrival of fluorescein dye at predetermined points in a stream system. Laboratory tests and stream trials proved the instrument to be efficient. Small changes in color can be detected in turbid or clear water. The unit has been used successfully for timing intervals of more than 17 hours; significant savings of time and manpower have resulted. Replacement of the clock, included in the original device, with a recording milliammeter increases the efficiency of the unit by contin,!ously recording changes in turbidity. The addition of this component would increase the cost from $75 to approximately $105.","language":"English","publisher":"Great Lakes Fishery Commission","usgsCitation":"Ebel, W.J., 1962, A photoelectric amplifier as a dye detector: Technical Report 4, p. 19-26.","productDescription":"p. 19-26","startPage":"19","endPage":"26","numberOfPages":"8","costCenters":[{"id":324,"text":"Great Lakes Science Center","active":true,"usgs":true}],"links":[{"id":198043,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":92069,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://www.glfc.org/pubs/TechReports/Tr04.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1fe4b07f02db6ab801","contributors":{"authors":[{"text":"Ebel, Wesley J.","contributorId":88307,"corporation":false,"usgs":true,"family":"Ebel","given":"Wesley","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":324938,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":2000037,"text":"2000037 - 1962 - Estimation of the brook and sea lamprey ammocoete populations of three streams","interactions":[],"lastModifiedDate":"2023-04-07T15:33:11.106821","indexId":"2000037","displayToPublicDate":"1962-01-01T00:00:00","publicationYear":"1962","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":3,"text":"Organization Series"},"seriesTitle":{"id":222,"text":"Technical Report","active":false,"publicationSubtype":{"id":3}},"seriesNumber":"4","title":"Estimation of the brook and sea lamprey ammocoete populations of three streams","docAbstract":"<p>Marking experiments on three streams in the Upper Peninsula of Michigan yielded quantitative estimates of populations of larval and transforming lampreys. The estimates not only gave an idea as to the numbers of ammocetes in the streams, but also confirmed the judgments of abundance based on earlier surveys with electric-shocking equipment and provided valuable information on the movement of larvae during chemical treatment. The estimated numbers of ammocetes in the three streams were 4,300 in Furnace Creek, 30,600 in Snyder Creek, and 336,700 in the Ogontz River.</p>","language":"English","publisher":"Great Lakes Fishery Commission","usgsCitation":"Smith, B.R., and McLain, A.L., 1962, Estimation of the brook and sea lamprey ammocoete populations of three streams: Technical Report 4, 18 p.","productDescription":"18 p.","costCenters":[{"id":324,"text":"Great Lakes Science Center","active":true,"usgs":true}],"links":[{"id":198781,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":92071,"rank":2,"type":{"id":15,"text":"Index Page"},"url":"https://www.glfc.org/glfc-publications-reports.php","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Michigan","otherGeospatial":"Furnace Creek, Ogontz River, Snyder Creek, Upper Peninisula","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -86.9103521098381,\n              46.47603146409622\n            ],\n            [\n              -86.9103521098381,\n              45.750180380916646\n            ],\n            [\n              -86.25593446454421,\n              45.750180380916646\n            ],\n            [\n              -86.25593446454421,\n              46.47603146409622\n            ],\n            [\n              -86.9103521098381,\n              46.47603146409622\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0ae4b07f02db5fb1e2","contributors":{"authors":[{"text":"Smith, Bernard R.","contributorId":38924,"corporation":false,"usgs":true,"family":"Smith","given":"Bernard","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":324966,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"McLain, Alberton L.","contributorId":15561,"corporation":false,"usgs":true,"family":"McLain","given":"Alberton","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":324965,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":2000024,"text":"2000024 - 1962 - Collection and analysis of commercial fishery statistics in the Great Lakes","interactions":[],"lastModifiedDate":"2023-04-07T14:55:19.462398","indexId":"2000024","displayToPublicDate":"1962-01-01T00:00:00","publicationYear":"1962","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":3,"text":"Organization Series"},"seriesTitle":{"id":222,"text":"Technical Report","active":false,"publicationSubtype":{"id":3}},"seriesNumber":"5","title":"Collection and analysis of commercial fishery statistics in the Great Lakes","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"Great Lakes Fishery Commission","usgsCitation":"Hile, R., 1962, Collection and analysis of commercial fishery statistics in the Great Lakes: Technical Report 5, ii, 31 p.","productDescription":"ii, 31 p.","costCenters":[{"id":324,"text":"Great Lakes Science 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,{"id":61978,"text":"mr27 - 1962 - Magnesite and brucite in the United States, exclusive of Alaska and Hawaii","interactions":[{"subject":{"id":45985,"text":"ofr6156 - 1961 - Magnesite and brucite in the United States","indexId":"ofr6156","publicationYear":"1961","noYear":false,"title":"Magnesite and brucite in the United States"},"predicate":"SUPERSEDED_BY","object":{"id":61978,"text":"mr27 - 1962 - Magnesite and brucite in the United States, exclusive of Alaska and Hawaii","indexId":"mr27","publicationYear":"1962","noYear":false,"title":"Magnesite and brucite in the United States, exclusive of Alaska and Hawaii"},"id":1}],"lastModifiedDate":"2023-01-24T19:21:38.71232","indexId":"mr27","displayToPublicDate":"1962-01-01T00:00:00","publicationYear":"1962","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":324,"text":"Mineral Investigations Resource Map","code":"MR","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"27","title":"Magnesite and brucite in the United States, exclusive of Alaska and Hawaii","docAbstract":"<p>The important deposits of magnesite (MgCO<sub>3</sub>) and brucite (MgO.H<sub>2</sub>O) in the United States (exclusive of Alaska and Hawaii) are shown on the accompanying map. Single deposits and groups of deposits are shown by geometric symbols according to four size categories based on estimated production plus reserves. These categories are: less than 10,000 tons, 10,000 to 100,000 tons, 100,000 to 1,000,000 tons, and more than 1,000,000 tons. Occurrences of mineralogic interest only are not shown. All map locations are numbered consecutively in each State and keyed to the locality index. The geographical coordinates in the locality index represent the centers of the geometric symbols. Thus, the same coordinates are assigned to all deposits covered by a group symbol.</p><p>The map was compiled from published reports and data in the files of the United States Geological Survey. The names, geographic coordinates, and geologic types of deposits are given in the locality index. The principal published reports used in compiling the map are listed in the selected references.</p><p>The main types of commercial deposits of magnesite in the United States are: (1) replacement bodies in limestone and dolomite; (2) replacements and veins in serpentine; and (3) sedimentary beds. Other magnesite deposits of varied origin and less common occurrence include beds associated with talc, chlorite, and mica schists; and veins and lenses in altered tuffs.</p><p>Brucite is a relatively rare mineral of secondary origin which usually accompanies other magnesian minerals, particularly magnesite and hydromagnesite, and is associated with carbonate rocks and serpentine.</p><p>Magnesite was first mined in California in 1886, and the State was the only domestic producer until the development of the Washington deposits began in 1916. In recent years, the main production of magnesite has been from Stevens County, Washington, and Nye County, Nevada. Production in California has been intermittent since 1945. Magnesite deposits in Texas were mined during and immediately after World War II. At present (1961) the only brucite deposits being worked are those at Gabbs, Nye County, Nevada. They have been mined almost continuously since 1935.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/mr27","usgsCitation":"Gildersleeve, B., 1962, Magnesite and brucite in the United States, exclusive of Alaska and Hawaii: U.S. Geological Survey Mineral Investigations Resource Map 27, Report: 4 p.; 1 Plate: 63.55 x 40.06 inches, https://doi.org/10.3133/mr27.","productDescription":"Report: 4 p.; 1 Plate: 63.55 x 40.06 inches","costCenters":[],"links":[{"id":412282,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mr/27/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":412281,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/mr/27/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":179997,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/mr/27/report-thumb.jpg"}],"scale":"3168000","country":"United States","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -127.25,24.25 ], [ -127.25,49.25 ], [ -66.5,49.25 ], [ -66.5,24.25 ], [ -127.25,24.25 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a7fe4b07f02db64924b","contributors":{"authors":[{"text":"Gildersleeve, Benjamin","contributorId":14468,"corporation":false,"usgs":true,"family":"Gildersleeve","given":"Benjamin","email":"","affiliations":[],"preferred":false,"id":266643,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":39192,"text":"pp257C - 1962 - Lake Bonneville: Geology of southern Cache Valley, Utah","interactions":[],"lastModifiedDate":"2022-11-22T16:06:06.265107","indexId":"pp257C","displayToPublicDate":"1962-01-01T00:00:00","publicationYear":"1962","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":331,"text":"Professional Paper","code":"PP","onlineIssn":"2330-7102","printIssn":"1044-9612","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"257","chapter":"C","title":"Lake Bonneville: Geology of southern Cache Valley, Utah","docAbstract":"<p>This report, covering about 450 square miles in southern Cache Vally, Utah, is one of a series dealing with the geology of Pleistocene Lake Bonneville. The report summarizes in tabular form the Paleozoic formations that are exposed in the mountains adjacent to Cache Valley and describes briefly the Tertiary formations—the Wasatch and Salt Lake formations— which are exposed in the valley. Most of the report deals with the Quaternary deposits.</p><p>Fan gravel and landslides of pre-Lake Bonneville Quaternary age are exposed in a few places at the edges of the basin, and well logs indicate a deep fill of this age in the subsurface of the basin interior. The sediments of Lake Bonneville comprise the Lake Bonneville group. The oldest of the unconsolidated deposits are the Alpine and Bonneville formations, which were mostly mapped together in southern Cache Valley. These formations are composed mostly of silt, but they include some gravel in embankments and small deltas. Their thickness ranges from about 50 to 100 feet.</p><p>Overlying the Alpine and Bonneville formations is the Provo formation 50 to 75 feet thick. In Cache Valley, as elsewhere in the Lake Bonneville basin, the Provo includes extensive gravel deposits in bars, spits, and deltas. It is the surface formation in much of Cache Valley. Deposits younger than the Provo, mostly of Recent age, include alluvial flans, flood-plain alluvium, natural levee deposits along the Bear River, slope wash, eolian sand, and cones of spring tufa. Several faults, active in Tertiary time, are mapped.</p><p>Well logs indicate that the pre-Lake Bonneville deposits of Quaternary age are surprisingly thin in Cache Valley, suggesting that the valley had exterior drainage during most of Pleistocene time. The logs show two main aquifers of gravel and sand— the upper one between the Provo formation and the Alpine and Bonneville formations and the other directly beneath the Alpine and Bonneville deposits. These aquifers probably are alluvium deposited during interlake intervals.</p><p>The shore embankments and deltas of the Lake Bonneville group are abundant sources of gravel and sand for construction. Much of the gravel is suitable for concrete aggregate.</p>","language":"English","publisher":"U.S. Government Printing Office","doi":"10.3133/pp257C","usgsCitation":"Williams, J.S., 1962, Lake Bonneville: Geology of southern Cache Valley, Utah: U.S. Geological Survey Professional Paper 257, Report: p. 131-152; 2 Plates, https://doi.org/10.3133/pp257C.","productDescription":"Report: p. 131-152; 2 Plates","costCenters":[],"links":[{"id":409536,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0257c/plate-7.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":409537,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0257c/plate-6.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":66802,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/0257c/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":119656,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/0257c/report-thumb.jpg"}],"country":"United States","state":"Utah","otherGeospatial":"Cache Valley, Lake Bonneville","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b32e4b07f02db6b42dd","contributors":{"authors":[{"text":"Williams, J. S.","contributorId":65819,"corporation":false,"usgs":false,"family":"Williams","given":"J.","email":"","middleInitial":"S.","affiliations":[{"id":12682,"text":"Utah State University, Logan, UT","active":true,"usgs":false}],"preferred":false,"id":221111,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":1015409,"text":"1015409 - 1962 - Disease-protective symbiosis among fishes and other aquatic animals","interactions":[],"lastModifiedDate":"2012-10-03T17:16:15","indexId":"1015409","displayToPublicDate":"1962-01-01T00:00:00","publicationYear":"1962","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":"Disease-protective symbiosis among fishes and other aquatic animals","docAbstract":"There have been numerous observations of one species of animal removing parasites from another. These are, however, generally regarded as biological curiosities rather than as significant factors in the control of parasites or disease.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Progressive Fish-Culturist","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"Taylor & Francis","publisherLocation":"Philadelphia, PA","doi":"10.1577/1548-8659(1962)24[59:DSAFAO]2.0.CO;2","collaboration":"112/FH","usgsCitation":"Snieszko, S.F., 1962, Disease-protective symbiosis among fishes and other aquatic animals: Progressive Fish-Culturist, v. 24, no. 2, p. 59-59, https://doi.org/10.1577/1548-8659(1962)24[59:DSAFAO]2.0.CO;2.","productDescription":"1 p.","startPage":"59","endPage":"59","numberOfPages":"1","costCenters":[{"id":365,"text":"Leetown Science Center","active":true,"usgs":true}],"links":[{"id":132459,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":262273,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1577/1548-8659(1962)24[59:DSAFAO]2.0.CO;2","linkFileType":{"id":5,"text":"html"}}],"volume":"24","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a81e4b07f02db64a47e","contributors":{"authors":[{"text":"Snieszko, S. F.","contributorId":13169,"corporation":false,"usgs":true,"family":"Snieszko","given":"S.","middleInitial":"F.","affiliations":[],"preferred":false,"id":322980,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":1000283,"text":"1000283 - 1962 - Exposure of several developmental stages of the sea lamprey, Petromyzon marinus to selective larvicides","interactions":[],"lastModifiedDate":"2023-12-06T01:29:36.222042","indexId":"1000283","displayToPublicDate":"1962-01-01T00:00:00","publicationYear":"1962","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1337,"text":"Copeia","active":true,"publicationSubtype":{"id":10}},"title":"Exposure of several developmental stages of the sea lamprey, Petromyzon marinus to selective larvicides","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"American Society of Ichthyologists and Herpetologists (ASIH)","usgsCitation":"Piavis, G.W., 1962, Exposure of several developmental stages of the sea lamprey, Petromyzon marinus to selective larvicides: Copeia, v. 1962, no. 3, p. 652-653.","productDescription":"1 p.","startPage":"652","endPage":"653","numberOfPages":"1","costCenters":[{"id":324,"text":"Great Lakes Science Center","active":true,"usgs":true}],"links":[{"id":128992,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"1962","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a06e4b07f02db5f8b3d","contributors":{"authors":[{"text":"Piavis, George W.","contributorId":63755,"corporation":false,"usgs":true,"family":"Piavis","given":"George","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":308334,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":1007570,"text":"1007570 - 1962 - The Texas lyre snake, Trimorphodon vilkinsoni, in New Mexico","interactions":[],"lastModifiedDate":"2012-02-02T00:04:17","indexId":"1007570","displayToPublicDate":"1962-01-01T00:00:00","publicationYear":"1962","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1892,"text":"Herpetologica","active":true,"publicationSubtype":{"id":10}},"title":"The Texas lyre snake, Trimorphodon vilkinsoni, in New Mexico","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Herpetologica","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","usgsCitation":"Medica, P., 1962, The Texas lyre snake, Trimorphodon vilkinsoni, in New Mexico: Herpetologica, v. 18.","productDescription":"p. 65","startPage":"65","numberOfPages":"65","costCenters":[{"id":651,"text":"Western Ecological Research Center","active":true,"usgs":true}],"links":[{"id":130167,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"18","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4abce4b07f02db67369c","contributors":{"authors":[{"text":"Medica, P.A.","contributorId":77079,"corporation":false,"usgs":true,"family":"Medica","given":"P.A.","email":"","affiliations":[],"preferred":false,"id":315646,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":1003291,"text":"1003291 - 1962 - An annotated list of the fishes of Great Smoky Mountains National Park","interactions":[],"lastModifiedDate":"2012-02-02T00:04:09","indexId":"1003291","displayToPublicDate":"1962-01-01T00:00:00","publicationYear":"1962","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2570,"text":"Journal of the Tennessee Academy of Science","active":true,"publicationSubtype":{"id":10}},"title":"An annotated list of the fishes of Great Smoky Mountains National Park","docAbstract":"Abstract has not been submitted","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Journal of the Tennessee Academy of Science","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","usgsCitation":"Lennon, R.E., 1962, An annotated list of the fishes of Great Smoky Mountains National Park: Journal of the Tennessee Academy of Science, v. 37, no. 1, p. 5-7.","productDescription":"pp. 5-7","startPage":"5","endPage":"7","numberOfPages":"3","costCenters":[{"id":606,"text":"Upper Midwest Environmental Sciences Center","active":true,"usgs":true}],"links":[{"id":129588,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"37","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adae4b07f02db68579a","contributors":{"authors":[{"text":"Lennon, R. E.","contributorId":37275,"corporation":false,"usgs":true,"family":"Lennon","given":"R.","middleInitial":"E.","affiliations":[],"preferred":false,"id":313077,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":1000377,"text":"1000377 - 1962 - Lake Erie or Lake Eerie?","interactions":[],"lastModifiedDate":"2012-02-02T00:04:13","indexId":"1000377","displayToPublicDate":"1962-01-01T00:00:00","publicationYear":"1962","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2124,"text":"Izaak Walton Magazine","active":true,"publicationSubtype":{"id":10}},"title":"Lake Erie or Lake Eerie?","docAbstract":"Abstract has not been submitted","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Izaak Walton Magazine","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","collaboration":"Out-of-print","usgsCitation":"Smith, S.H., 1962, Lake Erie or Lake Eerie?: Izaak Walton Magazine, v. 27, no. 4, p. 4-5.","productDescription":"p. 4-5","startPage":"4","endPage":"5","numberOfPages":"1","costCenters":[{"id":324,"text":"Great Lakes Science Center","active":true,"usgs":true}],"links":[{"id":129209,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"27","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b2fe4b07f02db6b4064","contributors":{"authors":[{"text":"Smith, Stanford H.","contributorId":86711,"corporation":false,"usgs":true,"family":"Smith","given":"Stanford","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":308481,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70010571,"text":"70010571 - 1962 - Temperature dependence of decay time and intensity of alpha pulses in pure and thallium-activated cesium iodide","interactions":[],"lastModifiedDate":"2020-11-19T17:46:33.453266","indexId":"70010571","displayToPublicDate":"1962-01-01T00:00:00","publicationYear":"1962","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":"Temperature dependence of decay time and intensity of alpha pulses in pure and thallium-activated cesium iodide","docAbstract":"<p><span>The intensity and decay time of Po</span><sup>210</sup><span>&nbsp;</span>alpha particle<span>&nbsp;scintillations produced in pure and thallium‐activated cesium iodide have been measured with a fast electronic system as a function of temperature down to 77°K. Three modes of decay due to alpha excitation have been observed for CsI(Tl), and two for CsI. Other than the 7‐ and 0.55‐μsec modes (at room temperature) reported in the literature for CsI(Tl), an additional temperature‐independent mode of about 1.3 μsec has been detected between 77 and 150°K. In CsI a fast temperature‐dependent mode of decay (≈100 nsec) was observed between 100–200°K in addition to the known principal mode.</span></p>","language":"English","publisher":"AIP Publishing","doi":"10.1063/1.1717979","usgsCitation":"Senftle, F.E., Martinez, P., and Alekna, V.P., 1962, Temperature dependence of decay time and intensity of alpha pulses in pure and thallium-activated cesium iodide: Review of Scientific Instruments, v. 33, no. 8, p. 819-822, https://doi.org/10.1063/1.1717979.","productDescription":"4 p.","startPage":"819","endPage":"822","numberOfPages":"4","costCenters":[],"links":[{"id":219019,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"33","issue":"8","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505ba4c1e4b08c986b320570","contributors":{"authors":[{"text":"Senftle, F. E.","contributorId":47788,"corporation":false,"usgs":true,"family":"Senftle","given":"F.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":359199,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Martinez, P.","contributorId":38706,"corporation":false,"usgs":true,"family":"Martinez","given":"P.","email":"","affiliations":[],"preferred":false,"id":359198,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Alekna, V. P.","contributorId":35459,"corporation":false,"usgs":true,"family":"Alekna","given":"V.","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":359197,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70010794,"text":"70010794 - 1962 - Aromatic fluorine compounds. X. The 2,3- and 2,6-difluoropyridines","interactions":[],"lastModifiedDate":"2020-11-19T17:43:15.215708","indexId":"70010794","displayToPublicDate":"1962-01-01T00:00:00","publicationYear":"1962","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2408,"text":"Journal of Organic Chemistry","active":true,"publicationSubtype":{"id":10}},"title":"Aromatic fluorine compounds. X. The 2,3- and 2,6-difluoropyridines","docAbstract":"<p>The preparation of difluoropyridines by the Schiemann reaction was investigated. 2-Amino-6-fluoropyridine (IIIa), necessary for the synthesis of 2,6-difluoropyridine (IVa) by the Schiemann reaction, was conveniently prepared by the Curtius degradation of 6-fluoropicolinic hydrazide (IIa) and by the Hofmann reaction on 6-fluoropicolinamide (IId). Since an <span>α</span>-fluorine on a pyridine nucleus is preferentially replaced by hydrazine when it is either adjacent to or opposite a carbomethoxy group, the hydrazides necessary for the synthesis of 3-amino-2- and 6-fluoropyridine could not be prepared. These amines were prepared from the appropriate 2-fluoropyridinecarboxamide by the Hofmann reaction. The preparation of difluoropyridines was successful with two of the aminofluoropyridines and led to the following new compounds: 2,3-difluoro(IVb) and 2,6-difluoropyridine (IVa).</p>","language":"English","publisher":"American Chemical Society","doi":"10.1021/jo01058a050","usgsCitation":"Finger, G.C., Starr, L.D., Roe, A., and Link, W.J., 1962, Aromatic fluorine compounds. X. The 2,3- and 2,6-difluoropyridines: Journal of Organic Chemistry, v. 27, no. 11, p. 3965-3968, https://doi.org/10.1021/jo01058a050.","productDescription":"4 p.","startPage":"3965","endPage":"3968","numberOfPages":"4","costCenters":[],"links":[{"id":218734,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"27","issue":"11","noUsgsAuthors":false,"publicationDate":"2002-05-01","publicationStatus":"PW","scienceBaseUri":"5059ed81e4b0c8380cd49851","contributors":{"authors":[{"text":"Finger, G. C.","contributorId":89277,"corporation":false,"usgs":true,"family":"Finger","given":"G.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":359662,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Starr, L. D.","contributorId":74872,"corporation":false,"usgs":true,"family":"Starr","given":"L.","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":359660,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Roe, A.","contributorId":67214,"corporation":false,"usgs":true,"family":"Roe","given":"A.","email":"","affiliations":[],"preferred":false,"id":359659,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Link, W. J.","contributorId":76877,"corporation":false,"usgs":true,"family":"Link","given":"W.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":359661,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70010793,"text":"70010793 - 1962 - Spectrophotometric catalytic determination of small amounts of rhenium in mineralized rocks and molybdenite","interactions":[],"lastModifiedDate":"2020-11-19T17:21:51.495943","indexId":"70010793","displayToPublicDate":"1962-01-01T00:00:00","publicationYear":"1962","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":"Spectrophotometric catalytic determination of small amounts of rhenium in mineralized rocks and molybdenite","docAbstract":"<p>Rhenium is determined by spectrophotometry of the tellurium sol formed by the reduction of tellurate by stannous chloride under the catalytic influence of rhenium. A detailed investigation of the conditions for high sensitivity and stability at lowest concentration levels of rhenium is presented as well as the behavior of 26 ions. The method is applied to the determination of some tenths of 1 p.p.m. or more of rhenium in a 1-mg. aliquot of mineralized rocks, mixtures of molybdenite and rocks, and molybdenite concentrates. The practical quantity limit of detection is 2x<sup>-10</sup> gram of rhenium. Samples are decomposed with a mixture of CaO, CaCl<sub>2</sub>, and MgO. On leaching, most constituents of the sample are precipitated either as calcium salts or hydroxides, except for rhenium and a small amount of molybdenum which pass into the filtrate. Residual molybdenum is removed by extraction with 8-quinolinol in chloroform. Better than 95% recoveries are obtained with two fusions with flux.</p>","language":"English","publisher":"ACS Publications","doi":"10.1021/ac60191a003","usgsCitation":"Simon, F., and Grimaldi, F.S., 1962, Spectrophotometric catalytic determination of small amounts of rhenium in mineralized rocks and molybdenite: Analytical Chemistry, v. 34, no. 11, p. 1361-1364, https://doi.org/10.1021/ac60191a003.","productDescription":"4 p.","startPage":"1361","endPage":"1364","numberOfPages":"4","costCenters":[],"links":[{"id":218733,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"34","issue":"11","noUsgsAuthors":false,"publicationDate":"2002-05-01","publicationStatus":"PW","scienceBaseUri":"505b95a6e4b08c986b31b030","contributors":{"authors":[{"text":"Simon, F.O.","contributorId":41808,"corporation":false,"usgs":true,"family":"Simon","given":"F.O.","email":"","affiliations":[],"preferred":false,"id":359657,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Grimaldi, F. S.","contributorId":94286,"corporation":false,"usgs":true,"family":"Grimaldi","given":"F.","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":359658,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70175632,"text":"70175632 - 1962 - Chemical analysis of water from observation wells in the Edwards and associated limestones, San Antonio area, Texas","interactions":[],"lastModifiedDate":"2016-08-17T13:58:13","indexId":"70175632","displayToPublicDate":"1962-01-01T00:00:00","publicationYear":"1962","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":"1","title":"Chemical analysis of water from observation wells in the Edwards and associated limestones, San Antonio area, Texas","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"Edwards Underground Water District","usgsCitation":"Garza, S., 1962, Chemical analysis of water from observation wells in the Edwards and associated limestones, San Antonio area, Texas: Edwards Underground Water District Bulletin 1, 56 p.","productDescription":"56 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"links":[{"id":326718,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"57b58ac0e4b03bcb0104bb6e","contributors":{"authors":[{"text":"Garza, Sergio","contributorId":88713,"corporation":false,"usgs":true,"family":"Garza","given":"Sergio","email":"","affiliations":[],"preferred":false,"id":645896,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":2015,"text":"wsp1539N - 1962 - Ground-water resources of Hamilton County, Nebraska, with a section on the chemical quality of the water","interactions":[],"lastModifiedDate":"2023-11-01T21:52:29.473357","indexId":"wsp1539N","displayToPublicDate":"1962-01-01T00:00:00","publicationYear":"1962","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":"1539","chapter":"N","title":"Ground-water resources of Hamilton County, Nebraska, with a section on the chemical quality of the water","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wsp1539N","usgsCitation":"Keech, C.F., and Rosene, P.G., 1962, Ground-water resources of Hamilton County, Nebraska, with a section on the chemical quality of the water: U.S. Geological Survey Water Supply Paper 1539, Report: v, 64 p.; 2 Plates: 14.76 x 23.80 inches and 27.00 x 38.440 inches, https://doi.org/10.3133/wsp1539N.","productDescription":"Report: v, 64 p.; 2 Plates: 14.76 x 23.80 inches and 27.00 x 38.440 inches","costCenters":[],"links":[{"id":109981,"rank":5,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_24736.htm","linkFileType":{"id":5,"text":"html"},"description":"24736"},{"id":27481,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1539n/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":27480,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1539n/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":27479,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1539n/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":137583,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1539n/report-thumb.jpg"}],"country":"United States","state":"Nebraska","county":"Hamilton County","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"Polygon\",\"coordinates\":[[[-97.8283,41.1733],[-97.8276,41.0467],[-97.8245,40.6985],[-97.9385,40.6981],[-98.278,40.6987],[-98.2829,40.6992],[-98.2829,40.8725],[-98.2443,40.9044],[-98.2187,40.9308],[-98.192,40.9444],[-98.1707,40.9588],[-98.1318,40.9964],[-98.1109,41.0068],[-98.1082,41.0031],[-98.1,41.0075],[-98.0856,41.0114],[-98.0647,41.0307],[-98.0384,41.0469],[-98.0404,41.0486],[-98.0189,41.066],[-97.9781,41.0895],[-97.9745,41.0851],[-97.9638,41.0866],[-97.9366,41.095],[-97.9299,41.0992],[-97.9309,41.1007],[-97.9116,41.1047],[-97.8916,41.1118],[-97.8633,41.134],[-97.8367,41.1618],[-97.8283,41.1733]]]},\"properties\":{\"name\":\"Hamilton\",\"state\":\"NE\"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a9ae4b07f02db65d71c","contributors":{"authors":[{"text":"Keech, Charles Franklin","contributorId":44123,"corporation":false,"usgs":true,"family":"Keech","given":"Charles","email":"","middleInitial":"Franklin","affiliations":[],"preferred":false,"id":144533,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Rosene, P. G.","contributorId":22192,"corporation":false,"usgs":true,"family":"Rosene","given":"P.","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":144532,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":1015410,"text":"1015410 - 1962 - [Book review] Taschenbuch der Fischkrankheiten fuur Fischereibiologen Tierarzte Fischzuchter und Aquarianer (Pocketbook of fish diseases for fishery biologists, veterinarians, fish culturists, and aquarium fanciers), by Erwin Amlacher","interactions":[],"lastModifiedDate":"2023-12-06T01:28:30.437862","indexId":"1015410","displayToPublicDate":"1962-01-01T00:00:00","publicationYear":"1962","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1337,"text":"Copeia","active":true,"publicationSubtype":{"id":10}},"title":"[Book review] Taschenbuch der Fischkrankheiten fuur Fischereibiologen Tierarzte Fischzuchter und Aquarianer (Pocketbook of fish diseases for fishery biologists, veterinarians, fish culturists, and aquarium fanciers), by Erwin Amlacher","docAbstract":"Review of: Taschenbuch der Fischkrankheiten, fu?r Fischereibiologen, Tiera?rzte, Fischzu?chter und Aquarianer. Erwin Amlacher. Jena, Fischer, 1961. xi, 286 p. illus.","language":"English","publisher":"American Society of Ichthyologists and Herpetologists (ASIH)","doi":"10.2307/1441217","usgsCitation":"Snieszko, S.F., 1962, [Book review] Taschenbuch der Fischkrankheiten fuur Fischereibiologen Tierarzte Fischzuchter und Aquarianer (Pocketbook of fish diseases for fishery biologists, veterinarians, fish culturists, and aquarium fanciers), by Erwin Amlacher: Copeia, v. 3, p. 670-671, https://doi.org/10.2307/1441217.","productDescription":"2 p.","startPage":"670","endPage":"671","numberOfPages":"2","costCenters":[{"id":365,"text":"Leetown Science Center","active":true,"usgs":true}],"links":[{"id":132460,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad9e4b07f02db684c97","contributors":{"authors":[{"text":"Snieszko, S. F.","contributorId":13169,"corporation":false,"usgs":true,"family":"Snieszko","given":"S.","middleInitial":"F.","affiliations":[],"preferred":false,"id":322981,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70010569,"text":"70010569 - 1962 - Study of natural glasses through their behaviour as membrane electrodes","interactions":[],"lastModifiedDate":"2020-11-19T17:49:37.931207","indexId":"70010569","displayToPublicDate":"1962-01-01T00:00:00","publicationYear":"1962","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2840,"text":"Nature","active":true,"publicationSubtype":{"id":10}},"title":"Study of natural glasses through their behaviour as membrane electrodes","docAbstract":"<p><span>THE low-temperature chemical alteration of natural glass occurs in two stages: an initial stage in which it remains glassy but absorbs as much as 6 per cent water</span><sup>1</sup><span>, and a final stage in which devitrification to clay minerals, with release of silica, occurs</span><sup>2,3</sup><span>. During the first stage the composition of the glass may change, with gain of K</span><sub>2</sub><span>O and water and loss of Na</span><sub>2</sub><span>O (Smith, R. L., personal communication). This change is due to ion exchange.</span></p>","language":"English","publisher":"Nature Publications","doi":"10.1038/194077b0","usgsCitation":"Truesdell, A., 1962, Study of natural glasses through their behaviour as membrane electrodes: Nature, v. 194, no. 4823, p. 77-79, https://doi.org/10.1038/194077b0.","productDescription":"3 p.","startPage":"77","endPage":"79","numberOfPages":"3","costCenters":[],"links":[{"id":218971,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"194","issue":"4823","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505b9cd8e4b08c986b31d4e3","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":359192,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70010718,"text":"70010718 - 1962 - Oxygen adsorption and the magnetic susceptibility of ice at low temperatures","interactions":[],"lastModifiedDate":"2020-11-19T17:48:20.117143","indexId":"70010718","displayToPublicDate":"1962-01-01T00:00:00","publicationYear":"1962","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2840,"text":"Nature","active":true,"publicationSubtype":{"id":10}},"title":"Oxygen adsorption and the magnetic susceptibility of ice at low temperatures","docAbstract":"<p><span>WHEN dealing with the magnetic susceptibility of tumour tissue</span><sup>1</sup><span>, we reported the magnetic susceptibility of ice at various temperatures from 273° K. down to 77° K. Since this publication, the authors have made many susceptibility measurements of ice, using the same equipment, and have obtained similar results, that is, a relatively large increase in diamagnetism below 150° K. Normal diamagnetism is not dependent on temperature, and hence further experiments were made of the magnetic susceptibility of ice at low temperatures in an attempt to determine some extraneous cause of the increased diamagnetism.</span></p>","language":"English","publisher":"Nature Publications","doi":"10.1038/194673a0","usgsCitation":"Senftle, F.E., and Thorpe, A., 1962, Oxygen adsorption and the magnetic susceptibility of ice at low temperatures: Nature, v. 194, no. 4829, p. 673-674, https://doi.org/10.1038/194673a0.","productDescription":"2 p.","startPage":"673","endPage":"674","numberOfPages":"2","costCenters":[],"links":[{"id":219552,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"194","issue":"4829","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a7277e4b0c8380cd76af6","contributors":{"authors":[{"text":"Senftle, F. E.","contributorId":47788,"corporation":false,"usgs":true,"family":"Senftle","given":"F.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":359484,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Thorpe, A.","contributorId":70534,"corporation":false,"usgs":true,"family":"Thorpe","given":"A.","affiliations":[],"preferred":false,"id":359485,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":6308,"text":"pp342 - 1962 - Geology and ore deposits of the Globe-Miami district, Arizona","interactions":[{"subject":{"id":51373,"text":"ofr53216 - 1953 - Geologic map of a portion of the Inspiration quadrangle, Arizona","indexId":"ofr53216","publicationYear":"1953","noYear":false,"title":"Geologic map of a portion of the Inspiration quadrangle, Arizona"},"predicate":"SUPERSEDED_BY","object":{"id":6308,"text":"pp342 - 1962 - Geology and ore deposits of the Globe-Miami district, Arizona","indexId":"pp342","publicationYear":"1962","noYear":false,"title":"Geology and ore deposits of the Globe-Miami district, Arizona"},"id":1}],"lastModifiedDate":"2023-11-07T19:34:14.377195","indexId":"pp342","displayToPublicDate":"1962-01-01T00:00:00","publicationYear":"1962","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":331,"text":"Professional Paper","code":"PP","onlineIssn":"2330-7102","printIssn":"1044-9612","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"342","title":"Geology and ore deposits of the Globe-Miami district, Arizona","docAbstract":"The rocks of the Globe-Miami district range from lower Precambrian to Recent. The oldest formation, the Pinal schist, comprises several varieties of schist formed by dynamic and thermal metamorphism of shale and feldspathic sandstone during the early Precambrian Mazatzal revolution. During the later stages of this revolution, the schist was intruded by a complex of dioritic rocks and by plutons of granite and quartz monzonite. There were extensive intrusions of a biotite-quartz diorite, known as the Madera diorite, mainly south of the district. In the northern part of the mapped area, the schist was invaded by an extensive mass, the Ruin granite, which is a coarse-grained rock most commonly of quartz monzonitic composition. There are also smaller sill-like masses of slightly gneissic muscovite granite.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/pp342","usgsCitation":"Peterson, N.P., 1962, Geology and ore deposits of the Globe-Miami district, Arizona: U.S. Geological Survey Professional Paper 342, Report: vi, 151 p.; 8 Plates: 44.79 x 30.92 inches or smaller, https://doi.org/10.3133/pp342.","productDescription":"Report: vi, 151 p.; 8 Plates: 44.79 x 30.92 inches or smaller","numberOfPages":"157","costCenters":[],"links":[{"id":271114,"rank":9,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0342/plate-6.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":271113,"rank":7,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0342/plate-5.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":271111,"rank":6,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0342/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":271112,"rank":5,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0342/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":275837,"rank":10,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0342/plate-8.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":271109,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0342/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":422430,"rank":11,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_4334.htm","linkFileType":{"id":5,"text":"html"}},{"id":271115,"rank":8,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0342/plate-7.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":271110,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0342/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":139786,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/0342/report-thumb.jpg"},{"id":268960,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/0342/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Arizona","county":"Pinal County","otherGeospatial":"Globe-Miami district","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -111,\n              33.5\n            ],\n            [\n              -111,\n              33.25\n            ],\n            [\n              -110.875,\n              33.25\n            ],\n            [\n              -110.875,\n              33.375\n            ],\n            [\n              -110.75,\n              33.375\n            ],\n            [\n              -110.75,\n              33.5\n            ],\n            [\n              -111,\n              33.5\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad7e4b07f02db68449a","contributors":{"authors":[{"text":"Peterson, N. 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