{"pageNumber":"2584","pageRowStart":"64575","pageSize":"25","recordCount":68807,"records":[{"id":70045415,"text":"wdrCO621 - 1962 - Surface Water Records of Colorado","interactions":[],"lastModifiedDate":"2013-05-22T14:43:50","indexId":"wdrCO621","displayToPublicDate":"1962-01-01T00:00:00","publicationYear":"1962","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":340,"text":"Water Data Report","code":"WDR","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"CO-62-1","title":"Surface Water Records of Colorado","docAbstract":"The surface-water records for the 1962 water year for gaging stations and miscellaneous sites within the State of Colorado 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 J. W. Odell, district engineer, Surface Water Branch.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Denver, CO","doi":"10.3133/wdrCO621","collaboration":"Prepared in cooperation with Colorado Water Conservation Board, Office of the State Engineer, Southeastern Colorado Water Conservancy District, Arkansas River Compact Administration, Colorado Agricultural Experiment Station, Colorado River Water Conservation District, County of Boulder, Board of County Cotmnissioners, City and County of Denver Board of Water Conunissioners, City of ·Colorado Springs Department of Public Utilities, U.S. Army Corps of Engineers, U.S. Bureau of Reclamation, U.S. Soil Conservation Service","usgsCitation":"U.S. Geological Survey, W.R., 1962, Surface Water Records of Colorado: U.S. Geological Survey Water Data Report CO-62-1, xii, 335 p., https://doi.org/10.3133/wdrCO621.","productDescription":"xii, 335 p.","numberOfPages":"356","additionalOnlineFiles":"N","temporalStart":"1961-10-01","temporalEnd":"1962-09-30","costCenters":[],"links":[{"id":272538,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wdr/1962/co-62/report.pdf"},{"id":270918,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wdr/1962/co-62/report-thumb.jpg"}],"country":"United States","state":"Colorado","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -109.000,37.0000 ], [ -109.000,41.0000 ], [ -102.000,41.0000 ], [ -102.000,37.0000 ], [ -109.000,37.0000 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"516d216ce4b0411d430a8a31","contributors":{"authors":[{"text":"U.S. Geological Survey, Water Resources Division","contributorId":102359,"corporation":false,"usgs":true,"family":"U.S. Geological Survey","given":"Water","email":"","middleInitial":"Resources Division","affiliations":[],"preferred":false,"id":477467,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70010573,"text":"70010573 - 1962 - Concentration method for the spectrochemical determination of seventeen minor elements in natural water","interactions":[],"lastModifiedDate":"2020-11-19T17:30:23.631193","indexId":"70010573","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":"Concentration method for the spectrochemical determination of seventeen minor elements in natural water","docAbstract":"<p>A method for the quantitative spectrochemical determination of microgram amounts of 17 minor elements in water is given. The chelating reagents 8-quinolinol, tannic acid, and thionalide are utilized to concentrate traces (1 to 500 <span>μ</span>g.) of aluminum, cobalt, chromium, copper, iron, gallium, germanium, manganese, nickel, titanium, vanadium, bismuth, lead, molybdenum, cadmium, zinc, and beryllium. Indium is added as a buffer, and palladium is used as an internal standard. The ashed oxides of these 17 metals are subsequently subjected to direct current arcing conditions during spectrum analysis. The method can be used to analyze waters with dissolved solids ranging from less than 100 to more than 100,000 p.p.m. There is no limiting concentration range for the determination of the heavy metals since any volume of sample can be used that will contain a heavy metal concentration within the analytical range of the method. Both the chemical and spectrographic procedures are described, and precision and accuracy data are given.</p>","language":"English","publisher":"ACS Publications","doi":"10.1021/ac60187a021","usgsCitation":"Silvey, W., and Brennan, R., 1962, Concentration method for the spectrochemical determination of seventeen minor elements in natural water: Analytical Chemistry, v. 34, no. 7, p. 784-786, https://doi.org/10.1021/ac60187a021.","productDescription":"3 p.","startPage":"784","endPage":"786","numberOfPages":"3","costCenters":[],"links":[{"id":219021,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"34","issue":"7","noUsgsAuthors":false,"publicationDate":"2002-05-01","publicationStatus":"PW","scienceBaseUri":"5059f97ee4b0c8380cd4d62b","contributors":{"authors":[{"text":"Silvey, W. D.","contributorId":102914,"corporation":false,"usgs":true,"family":"Silvey","given":"W. D.","affiliations":[],"preferred":false,"id":359203,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Brennan, R.","contributorId":62572,"corporation":false,"usgs":true,"family":"Brennan","given":"R.","email":"","affiliations":[],"preferred":false,"id":359202,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70195893,"text":"70195893 - 1962 - Artesian water from glacial drift near Lehr, Logan and McIntosh Counties, North Dakota","interactions":[],"lastModifiedDate":"2018-03-08T09:28:58","indexId":"70195893","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":"38","title":"Artesian water from glacial drift near Lehr, Logan and McIntosh Counties, North Dakota","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"North Dakota State Water Conservation Commission","usgsCitation":"Adolphson, D.G., 1962, Artesian water from glacial drift near Lehr, Logan and McIntosh Counties, North Dakota: North Dakota Ground Water Studies 38, 22 p.","productDescription":"22 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":352287,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5aff6345e4b0da30c1bfdf0a","contributors":{"authors":[{"text":"Adolphson, D. G.","contributorId":106081,"corporation":false,"usgs":true,"family":"Adolphson","given":"D.","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":730411,"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":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":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":70010448,"text":"70010448 - 1962 - The solubility of quartz in water in the temperature interval from 25° to 300° C","interactions":[],"lastModifiedDate":"2015-06-22T09:01:28","indexId":"70010448","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":"The solubility of quartz in water in the temperature interval from 25° to 300° C","docAbstract":"<p id=\"\">The solubility of quartz in water was investigated by three sets of experiments</p>\n<ol>\n<li>at 1000 atm P<sub>H</sub><sub>2</sub>O and temperatures ranging from 45&deg; to 300&deg;C</li>\n<li>at water pressures appropriate for the coexistence of three phases, gaseous water, liquid, and quartz, at temperatures ranging from 69&deg; to 240&deg;C</li>\n<li>a long term study of the dissolution of quartz grains which were continuously tumbled in water at room temperature.</li>\n</ol>\n<p id=\"\">Saturated silica solutions in equilibrium with quartz were obtained in a few days at temperatures above 100&deg;C. Equilibrium is shown by reproducible results for runs of different durations and by the precipitation of quartz from initially supersaturated solutions. The differential heat of solution derived from the data obtained at 1000 atm pressure is 5.38 kcal/mole.</p>\n<p id=\"\">At room temperature and pressure, highly supersaturated silica solutions were obtained by continuously rotating quartz grains and water in plastic bottles at 75 rev/min. In one run the amount of silica in solution increased to a maximum value of 395 p.p.m. after 370 days. Another run reached 80 p.p.m. silica after 386 days and then dropped to 6 p.p.m. silica. It is concluded that quartz was precipitated at room temperature from this supersaturated solution and that 6 p.p.m. is essentially the true solubility of quartz at 25&deg;C.</p>\n<p id=\"\">In contrast to the runs rotated at 75 rev/min, quartz grains, and also silica glass grains, continuously rotated in water at<span id=\"mmlsi1\" class=\"mathmlsrc\"><img class=\"imgLazyJSB inlineImage\" title=\"\" src=\"http://ars.els-cdn.com/content/image/1-s2.0-0016703762900273-si1.gif\" alt=\"\" width=\"11\" height=\"35\" data-inlimgeid=\"1-s2.0-0016703762900273-si1.gif\" data-loaded=\"true\" /></span>&nbsp;rev/min, each contributed less than 1 p.p.m. colorimetric silica into solution after 1 year. Thus, vigorous agitation of the liquid is necessary to remove dissolved silica from the vicinity of surfaces of both quartz and glass.</p>\n<p id=\"\">Two significant factors that may have contributed to the formation of supersaturated silica solutions in the runs rotated at 75 rev/min at room temperature are</p>\n<ol>\n<li>stresses and structural irregularities at the surfaces of the crushed quartz grains, which contributed silica into solution more readily than well crystallized quartz</li>\n<li>the very slow rate at which dissolved silica polymerizes to species appropriate to act as nuclei for quartz growth. At the termination of the runs rotated at 75 rev/min, spikelike projections were present on many of the quartz grains. These are interpreted as indicating that abrasion was not the dominant cause for the great supersaturations which were obtained.</li>\n</ol>\n<p>&nbsp;</p>","language":"English","publisher":"Elsevier","doi":"10.1016/0016-7037(62)90027-3","issn":"00167037","usgsCitation":"Morey, G., Fournier, R., and Rowe, J., 1962, The solubility of quartz in water in the temperature interval from 25° to 300° C: Geochimica et Cosmochimica Acta, v. 26, no. 10, p. 1029-1040, https://doi.org/10.1016/0016-7037(62)90027-3.","productDescription":"12 p.","startPage":"1029","endPage":"1040","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":218798,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"26","issue":"10","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505bb043e4b08c986b324d40","contributors":{"authors":[{"text":"Morey, G.W.","contributorId":108155,"corporation":false,"usgs":true,"family":"Morey","given":"G.W.","email":"","affiliations":[],"preferred":false,"id":358950,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Fournier, R.O.","contributorId":73584,"corporation":false,"usgs":true,"family":"Fournier","given":"R.O.","email":"","affiliations":[],"preferred":false,"id":358949,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Rowe, J.J.","contributorId":29460,"corporation":false,"usgs":true,"family":"Rowe","given":"J.J.","affiliations":[],"preferred":false,"id":358948,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"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":70171141,"text":"70171141 - 1962 - Distribution and detoxication of toxaphene in Clayton Lake, New Mexico","interactions":[],"lastModifiedDate":"2016-05-23T17:23:31","indexId":"70171141","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":"Distribution and detoxication of toxaphene in Clayton Lake, New Mexico","docAbstract":"<p><span>The fate of toxaphene, applied in three treatments at a total calculated concentration of 0.05 p.p.m. to Clayton Lake, New Mexico, was followed over a 1.5-year period. A detailed description of the chromatographic method of analysis is given. Water concentrations of toxaphene were higher in leeshore samples than in windward samples for 2 weeks after the application; toxaphene levels then appeared to reach a constant value of about 0.001 p.p.m. for at least an additional 250 days. Total body concentrations of toxaphene were determined in trout and bullheads present in the lake during the poisoning and in trout placed in the lake in live-cars subsequently. Trout were more susceptible to toxaphene and accumulated lower body levels than bullheads. Bullheads which showed symptoms of toxaphene poisoning when collected had higher levels than did normal-appearing individuals. No difference in levels was observed in live-car trout collected dead as compared to survivors. Aquatic vegetation accumulated high concentrations of toxaphene; low concentrations were found in some sediment samples. The significance of these findings is discussed.</span></p>","language":"English","publisher":"Taylor & Francis","doi":"10.1577/1548-8659(1962)91[14:DADOTI]2.0.CO;2","usgsCitation":"Kallman, B.J., Cope, O.B., and Navarre, R.J., 1962, Distribution and detoxication of toxaphene in Clayton Lake, New Mexico: Transactions of the American Fisheries Society, v. 91, no. 1, p. 14-22, https://doi.org/10.1577/1548-8659(1962)91[14:DADOTI]2.0.CO;2.","productDescription":"9 p.","startPage":"14","endPage":"22","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":192,"text":"Columbia Environmental Research Center","active":true,"usgs":true}],"links":[{"id":321555,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"New Mexico","otherGeospatial":"Clayton Lake","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -103.31233978271483,\n              36.58245213849012\n            ],\n            [\n              -103.31130981445312,\n              36.573216031837795\n            ],\n            [\n              -103.31062316894531,\n              36.57128595955732\n            ],\n            [\n              -103.29414367675781,\n              36.57004517333383\n            ],\n            [\n              -103.29465866088867,\n              36.58148722380944\n            ],\n            [\n              -103.2963752746582,\n              36.58617383928255\n            ],\n            [\n              -103.31216812133789,\n              36.586587350516545\n            ],\n            [\n              -103.31233978271483,\n              36.58245213849012\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"91","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"574d64a7e4b07e28b66839ef","contributors":{"authors":[{"text":"Kallman, Burton J.","contributorId":169580,"corporation":false,"usgs":false,"family":"Kallman","given":"Burton","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":630094,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Cope, Oliver B.","contributorId":13290,"corporation":false,"usgs":true,"family":"Cope","given":"Oliver","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":630095,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Navarre, Richard J.","contributorId":169581,"corporation":false,"usgs":false,"family":"Navarre","given":"Richard","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":630096,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70185611,"text":"70185611 - 1962 - The Vigil Network","interactions":[],"lastModifiedDate":"2017-03-24T14:24:10","indexId":"70185611","displayToPublicDate":"1962-01-01T00:00:00","publicationYear":"1962","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":"The Vigil Network","docAbstract":"<p>Those of us who seek to explain the variations in hydrologic phenomena such as may be observed in the occurrence of floods or in changes in the shape of river channels are painfully aware of the lack of adequate data. Our existing data, collected mainly to serve immediate practical needs for water-resources development, usually are deficient in providing information useful for many kinds of scientific inquiry. Hydrologic records are usually obtained on streams that are highly regulated or otherwise put to use, to the neglect of headwater streams better suited to studies of the details of hydrologic processes.</p>","language":"English","publisher":"Taylor & Francis","doi":"10.1080/02626666209493250","usgsCitation":"Leopold, L.B., 1962, The Vigil Network: International Association of Scientific Hydrology - Bulletin , v. 7, no. 2, p. 5-9, https://doi.org/10.1080/02626666209493250.","productDescription":"5 p.","startPage":"5","endPage":"9","costCenters":[],"links":[{"id":338317,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"7","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"58d6304ce4b05ec799131147","contributors":{"authors":[{"text":"Leopold, Luna Bergere","contributorId":93884,"corporation":false,"usgs":true,"family":"Leopold","given":"Luna","email":"","middleInitial":"Bergere","affiliations":[],"preferred":false,"id":686124,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"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":70171423,"text":"70171423 - 1962 - Glaciological investigations on South Cascade Glacier","interactions":[],"lastModifiedDate":"2016-06-20T10:58:57","indexId":"70171423","displayToPublicDate":"1962-01-01T00:00:00","publicationYear":"1962","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":5074,"text":"The Mountaineer","active":true,"publicationSubtype":{"id":10}},"title":"Glaciological investigations on South Cascade Glacier","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"The Mountaineers","usgsCitation":"Tangborn, W.V., 1962, Glaciological investigations on South Cascade Glacier: The Mountaineer, v. 55, no. 4.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":622,"text":"Washington Water Science Center","active":true,"usgs":true}],"links":[{"id":323972,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"55","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"576913c6e4b07657d19ff0c5","contributors":{"authors":[{"text":"Tangborn, Wendell V.","contributorId":32152,"corporation":false,"usgs":true,"family":"Tangborn","given":"Wendell","email":"","middleInitial":"V.","affiliations":[],"preferred":false,"id":630948,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70185586,"text":"70185586 - 1962 - Water and the arid zone of the United States","interactions":[],"lastModifiedDate":"2017-03-24T10:27:03","indexId":"70185586","displayToPublicDate":"0002-01-01T00:00:00","publicationYear":"1962","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"Water and the arid zone of the United States","docAbstract":"<p>In a pluvial period associated with Wisconsin glaciation the closed basin of the Estancia Valley in New Mexico held a lake which, at its maximum extent, was 150 feet deep and had a surface area of 450 square miles. This basin, with a mean elevation of about 6,000 feet, has at present an annual precipitation of about 14 inches.</p><p>Estimates have been made of the Pleistocene precipitation necessary to maintain this pluvial lake. Instead of the present annual average of 14 inches it has been variously estimated that the precipitation must have been between 20 and 24 inches. Lakes existed during Pleistocene time in many places in the western United States that are now true deserts - with a precipitation of less than 4 inches - and there is abundant evidence that early man lived on the shores of these lakes. He must have adapted himself to the increasing aridity; this adaptation can be seen even at present in the form of floodwater farming practices, which have been highly developed by the Hopi Indians, particularly in northeastern Arizona.</p><p>A gradually changing climate is only one, and not the most important, of the changing conditions to which man must gradually adjust in his particular relation to the use of water. The changes in his own culture in conjunction with changes in population density are usually even more important determinants of man’s use of and attitude toward his water supplies. In a desert area of Central Arizona, near Florence, the remains of irrigation systems developed by the aborigines to irrigate the alluvial valley floor with water diverted from the Gila River, which was at that time perennial, have been mapped and partially excavated. Irrigated agriculture was not practised nearly so extensively in the arid portions of the United States as in Persia, India, and many Mediterranean countries, nor was the general culture of indigenous American tribes so highly developed. Even in the simple cultures of the American Indians patterns of adjustment to a changing climate and to a changing culture and population level can be discerned. These patterns include, however crudely, the development of irrigated agriculture, floodwater farming, water storage for both stock and community use, spring development, and even efforts at rain-making through the offices of prayers, rattles, and dances. These same patterns, more complex to be sure, can be seen to have characterized the adjustment of modern culture to the limited water supplies of the arid climates, even including the prayers and rattles.</p><p>An aspect of the development of American culture in the arid areas is probably typical and may have a counterpart in certain of the underdeveloped areas in other parts of the world at the present time. The local civilization of the arid climate usually does not develop to a very high level in situ. The indigenous cultures are usually transfused with new bursts of energy and knowledge by the incursion of other cultures which have developed in other climes. The cultural advances in the Fertile Crescent of Mesopotamia were gradually influenced by the barbarian invasion, which added much to, as well as detracted from, the locally developing society. Similarly the spurt of civilization which has characterized the arid parts of the United States since 1846 was determined by the superposition of a culture from the eastern United States on the essentially Spanish culture which had been developing since the initial exploration of the southwestern desert in 1630. </p>","conferenceTitle":"Arid Zone Research - XVIII: The Problems of the Arid Zone, Proceedings of the Paris Symposium","conferenceDate":"May 11-18, 1960","conferenceLocation":"Paris, France","language":"English","publisher":"UNESCO","publisherLocation":"Paris, France","usgsCitation":"Leopold, L.B., 1962, Water and the arid zone of the United States, Arid Zone Research - XVIII: The Problems of the Arid Zone, Proceedings of the Paris Symposium, Paris, France, May 11-18, 1960, p. 395-399.","productDescription":"5 p.","startPage":"395","endPage":"399","costCenters":[],"links":[{"id":338260,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":338258,"rank":1,"type":{"id":15,"text":"Index Page"},"url":"https://www.unesco.org/ulis/cgi-bin/ulis.pl?catno=148747&set=0058D53A53_2_317&gp=1&lin=1&ll=1"}],"country":"United States","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"58d6304ce4b05ec799131149","contributors":{"authors":[{"text":"Leopold, Luna Bergere","contributorId":93884,"corporation":false,"usgs":true,"family":"Leopold","given":"Luna","email":"","middleInitial":"Bergere","affiliations":[],"preferred":false,"id":686037,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70217326,"text":"wdrMDDE61 - 1961 - Surface water records of Maryland and Delaware, water year 1961","interactions":[],"lastModifiedDate":"2021-01-22T19:12:04.621675","indexId":"wdrMDDE61","displayToPublicDate":"2021-01-22T14:45:00","publicationYear":"1961","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":340,"text":"Water Data Report","code":"WDR","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"MD-DE-61","displayTitle":"Surface Water Records of Maryland and Delaware, Water Year 1961","title":"Surface water records of Maryland and Delaware, water year 1961","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wdrMDDE61","usgsCitation":"U.S. Geological Survey, 1961, Surface water records of Maryland and Delaware, water year 1961: U.S. Geological Survey Water Data Report MD-DE-61, 102 p., 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,{"id":70198519,"text":"70198519 - 1961 - Stratigraphy of Onesquethaw stage of Devonian in West Virginia and bordering States","interactions":[],"lastModifiedDate":"2018-08-06T15:41:17","indexId":"70198519","displayToPublicDate":"2018-01-01T15:39:17","publicationYear":"1961","noYear":false,"publicationType":{"id":4,"text":"Book"},"title":"Stratigraphy of Onesquethaw stage of Devonian in West Virginia and bordering States","largerWorkTitle":"West Virginia Geological Survey Bulletin","publisher":"West Virginia Geological Survey","publisherLocation":"Morgantown, WV","usgsCitation":"Dennison, J., 1961, Stratigraphy of Onesquethaw stage of Devonian in West Virginia and bordering States, v. 22, 87 p.","productDescription":"87 p.","costCenters":[{"id":37280,"text":"Virginia and West Virginia Water Science Center ","active":true,"usgs":true}],"links":[{"id":356214,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"West Virginia","otherGeospatial":"Appalachian Mountains","volume":"22","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Dennison, J.M.","contributorId":58724,"corporation":false,"usgs":true,"family":"Dennison","given":"J.M.","email":"","affiliations":[],"preferred":false,"id":741765,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70198470,"text":"70198470 - 1961 - Ground-water features of Berkeley and Jefferson Counties","interactions":[],"lastModifiedDate":"2018-08-03T13:44:57","indexId":"70198470","displayToPublicDate":"2018-01-01T13:44:34","publicationYear":"1961","noYear":false,"publicationType":{"id":4,"text":"Book"},"title":"Ground-water features of Berkeley and Jefferson Counties","largerWorkTitle":"West Virginia Geological and Economic Survey Bulletin","publisherLocation":"Morgantown, WV","usgsCitation":"Bieber, P.P., 1961, Ground-water features of Berkeley and Jefferson Counties, v. 21, 81 p.","productDescription":"81 p.","costCenters":[{"id":37280,"text":"Virginia and West Virginia Water Science Center ","active":true,"usgs":true}],"links":[{"id":356146,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"West Virginia","county":"Berkeley County, Jefferson County","volume":"21","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Bieber, Paul Peter","contributorId":119609,"corporation":false,"usgs":true,"family":"Bieber","given":"Paul","email":"","middleInitial":"Peter","affiliations":[],"preferred":false,"id":741544,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70179899,"text":"70179899 - 1961 - Developing ground water in the central Sevier Valley, Utah","interactions":[],"lastModifiedDate":"2017-01-19T17:31:49","indexId":"70179899","displayToPublicDate":"2016-12-01T00:00:00","publicationYear":"1961","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":2,"text":"State or Local Government Series"},"seriesTitle":{"id":5271,"text":"Utah State Engineer Information Bulletin","active":false,"publicationSubtype":{"id":2}},"seriesNumber":"5","title":"Developing ground water in the central Sevier Valley, Utah","docAbstract":"<p>This report presents a summary of conclusions reached from the recently completed State Engineer-United States Geological Survey cooperative investigation of the geology and ground water resources of the central Sevier River Valley. The detailed report will be published as a United States Geological Survey water supply paper and will be available to the public.</p>","language":"English","publisher":"Utah State Engineer's Office","publisherLocation":"Salt Lake City, UT","collaboration":"Prepared in cooperation with the Utah State Engineer","usgsCitation":"Young, R.A., and Carpenter, C.H., 1961, Developing ground water in the central Sevier Valley, Utah: Utah State Engineer Information Bulletin 5, 6 p.","productDescription":"6 p.","numberOfPages":"10","costCenters":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":333512,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":333511,"rank":1,"type":{"id":15,"text":"Index Page"},"url":"https://www.waterrights.utah.gov/cgi-bin/libview.exe?Modinfo=Viewpub&LIBNUM=21-4-100"}],"country":"United States","state":"Utah","otherGeospatial":"Sevier River, Sevier Valley","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5881defae4b01192927da001","contributors":{"authors":[{"text":"Young, Richard A.","contributorId":38975,"corporation":false,"usgs":true,"family":"Young","given":"Richard","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":659141,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Carpenter, Carl H.","contributorId":46074,"corporation":false,"usgs":true,"family":"Carpenter","given":"Carl","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":659142,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70179900,"text":"70179900 - 1961 - Relation of the deep and shallow artesian aquifers near Lynndyl, Utah","interactions":[],"lastModifiedDate":"2017-01-19T17:40:00","indexId":"70179900","displayToPublicDate":"2016-12-01T00:00:00","publicationYear":"1961","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":2,"text":"State or Local Government Series"},"seriesTitle":{"id":5271,"text":"Utah State Engineer Information Bulletin","active":false,"publicationSubtype":{"id":2}},"seriesNumber":"7","title":"Relation of the deep and shallow artesian aquifers near Lynndyl, Utah","docAbstract":"<p>Ground water occurs in several aquifers in the vicinity of Lynndyl, Utah. There are one shallow perched water-table aquifer and at least two artisan aquifers. The perched aquifer is not related to the artisan aquifers and, because it is relatively unimportant, is not discussed here. Pumping tests made during the investigation show also that the artesian aquifers are not connected hydraulically.</p>","language":"English","publisher":"Utah State Engineer's Office","publisherLocation":"Salt Lake City, UT","usgsCitation":"Mower, R.W., 1961, Relation of the deep and shallow artesian aquifers near Lynndyl, Utah: Utah State Engineer Information Bulletin 7, 4 p.","productDescription":"4 p.","numberOfPages":"11","costCenters":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":333514,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":333513,"rank":1,"type":{"id":15,"text":"Index Page"},"url":"https://www.waterrights.utah.gov/cgi-bin/libview.exe?Modinfo=Viewpub&LIBNUM=21-4-140"}],"country":"United States","state":"Utah","city":"Lynndyl","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5881defae4b01192927d9fff","contributors":{"authors":[{"text":"Mower, R. W.","contributorId":34898,"corporation":false,"usgs":true,"family":"Mower","given":"R.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":659146,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70176020,"text":"70176020 - 1961 -  Ground-water levels in observation wells in Kansas, 1960","interactions":[],"lastModifiedDate":"2016-08-23T14:49:24","indexId":"70176020","displayToPublicDate":"2015-11-23T00:00:00","publicationYear":"1961","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2579,"text":"Kansas Geological Survey Bulletin","active":true,"publicationSubtype":{"id":10}},"title":" Ground-water levels in observation wells in Kansas, 1960","language":"English","publisher":"University of Kansas","publisherLocation":" Lawrence, KS","usgsCitation":"Broeker, M., and Fishel, V., 1961,  Ground-water levels in observation wells in Kansas, 1960: Kansas Geological Survey Bulletin, v. 153, 183 p. .","productDescription":"183 p. ","costCenters":[{"id":353,"text":"Kansas Water Science Center","active":false,"usgs":true}],"links":[{"id":327741,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":327740,"rank":1,"type":{"id":15,"text":"Index Page"},"url":"https://www.kgs.ku.edu/General/geologyBulls.html"}],"volume":"153","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"57bd73abe4b03fd6b7df2c52","contributors":{"authors":[{"text":"Broeker, M.E.","contributorId":173983,"corporation":false,"usgs":false,"family":"Broeker","given":"M.E.","email":"","affiliations":[],"preferred":false,"id":646807,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Fishel, V.C.","contributorId":6126,"corporation":false,"usgs":true,"family":"Fishel","given":"V.C.","email":"","affiliations":[],"preferred":false,"id":646808,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70176018,"text":"70176018 - 1961 - Geology and ground-water resources of Sumner County, Kansas","interactions":[],"lastModifiedDate":"2018-09-27T11:55:07","indexId":"70176018","displayToPublicDate":"2015-11-16T00:00:00","publicationYear":"1961","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2579,"text":"Kansas Geological Survey Bulletin","active":true,"publicationSubtype":{"id":10}},"title":"Geology and ground-water resources of Sumner County, Kansas","docAbstract":"<p>This report describes the geography, geology, and ground-water resources of Sumner County in south-central Kansas. The hydrologic and geologic data upon which this report is based were obtained in the field during the summers of 1955 and 1956. Records of 300 wells and 2 springs, chemical analyses of 219 water samples from wells and test holes and of 15 from streams, and logs of 362 wells and test holes are included in tables.</p><p>Sumner County has an area of 1,183 square miles and lies in the Wellington Lowland and Arkansas River Lowlands of the Central Lowland physiographic province. It is drained by Arkansas River, Ninnescah River, and Chikaskia River and their tributaries. The land surface in general is a southeastward-sloping, gently rolling plain. The average annual precipitation at Wellington is about 31 inches. Wheat fanning is the principal industry of the county, and oil is the chief natural resource.</p><p>The Wellington Formation, of Permian age, crops out in the eastern two-thirds of the county except where it is covered by Pleistocene deposits. The Ninnescah Shale (Permian) overlies the Wellington Formation and crops out in parts of the western third of the county. The Permian rocks yield small quantities of hard water to wells. Pleistocene sand and gravel deposits of Nebraskan age are present in the northwestern corner of the county and yield moderate quantities of good water to wells. Discontinuous deposits of Kansan or Illinoisan age, locally mantled by colluvium, forms terraces in southern and eastern Sumner County, and may yield moderate quantities of water. Wisconsinan terrace deposits and Recent alluvium along the major streams yield large quantities of water. Colluvium and dune sand are unimportant as sources of water but may facilitate recharge.</p><p>Maps of Sumner County included in this report show the outcrop areas of the formations, geologic cross sections, the shape and slope of the water table, the locations of wells and test holes for which records are given, and the distribution of chloride in water samples.</p><p>The ground-water reservoir is recharged principally from rain and snow that fall within the county, by percolation from streams and other surface bodies of water, and by underflow from adjacent areas. Water is discharged from the ground-water reservoir by seepage into streams, by transpiration and evaporation, by movement into adjacent areas, and by wells. Water is pumped from wells for domestic, stock, municipal, industrial, and irrigation use. Irrigation from wells is most extensive in the valley of Arkansas River, in which area further development is most probable.</p><p>Chemical analyses of samples of water from Sumner County indicate that the quality varies greatly from place to place. Sulfate is common in water from the Wellington Formation and Ninnescah Shale. Water from Pleistocene deposits is generally suitable for most uses except in local areas where it contains excessive chloride.</p>","language":"English","publisher":"University of Kansas","publisherLocation":"Lawrence, KS","usgsCitation":"Walters, K., 1961, Geology and ground-water resources of Sumner County, Kansas: Kansas Geological Survey Bulletin, v. 151, 198 p. .","productDescription":"198 p. ","costCenters":[{"id":353,"text":"Kansas Water Science Center","active":false,"usgs":true}],"links":[{"id":327735,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":327734,"rank":1,"type":{"id":15,"text":"Index Page"},"url":"https://www.kgs.ku.edu/General/Geology/Sumner/index.html"}],"volume":"151","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"57bd73dbe4b03fd6b7df2ce7","contributors":{"authors":[{"text":"Walters, K.L.","contributorId":105765,"corporation":false,"usgs":true,"family":"Walters","given":"K.L.","affiliations":[],"preferred":false,"id":646804,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70176019,"text":"70176019 - 1961 - Geology and ground-water resources of southern Ellis County and parts of Trego and Rush Counties, Kansas","interactions":[],"lastModifiedDate":"2016-08-23T14:47:11","indexId":"70176019","displayToPublicDate":"2015-10-12T00:00:00","publicationYear":"1961","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2579,"text":"Kansas Geological Survey Bulletin","active":true,"publicationSubtype":{"id":10}},"title":"Geology and ground-water resources of southern Ellis County and parts of Trego and Rush Counties, Kansas","language":"English","publisher":"University of Kansas","publisherLocation":"Lawrence, KS","usgsCitation":"Leonard, A., and Berry, D., 1961, Geology and ground-water resources of southern Ellis County and parts of Trego and Rush Counties, Kansas: Kansas Geological Survey Bulletin, v. 149, 156 p. .","productDescription":"156 p. ","costCenters":[{"id":353,"text":"Kansas Water Science Center","active":false,"usgs":true}],"links":[{"id":327738,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":327737,"rank":1,"type":{"id":15,"text":"Index Page"},"url":"https://www.kgs.ku.edu/General/geologyBulls.html"}],"volume":"149","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"57bd73dbe4b03fd6b7df2ceb","contributors":{"authors":[{"text":"Leonard, A.R.","contributorId":101669,"corporation":false,"usgs":true,"family":"Leonard","given":"A.R.","email":"","affiliations":[],"preferred":false,"id":646805,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Berry, D.W.","contributorId":24842,"corporation":false,"usgs":true,"family":"Berry","given":"D.W.","email":"","affiliations":[],"preferred":false,"id":646806,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70160911,"text":"70160911 - 1961 - Trout hepatoma--a preliminary report","interactions":[],"lastModifiedDate":"2016-08-15T21:33:39","indexId":"70160911","displayToPublicDate":"2015-09-14T08:30:00","publicationYear":"1961","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":"Trout hepatoma--a preliminary report","docAbstract":"<p>Fish pathology and its role in fish culture were brought into prominence in the spring of 1960 by the disclosure of a high incidence of hepatomas in hatchery-reared rainbow trout. The current problem came to light as the result of a routine inspection of live trout shipments at a California border fish-disease checking station. This service is performed by personnel of the California Department of Fish and Game to preclude the introduction or further spread of communicable fish diseases into California watersheds. Collaborative studies which followed revealed the nationwide distribution of the disease. This unusual disease soon attracted the attention of the Bureau of Sport Fisheries and Wildlife, the Food and Drug Administration, Public Health Service, and several western State health and conservation agencies.</p>","language":"English","publisher":"Bureau of Fisheries, U.S. Department of Commerce","doi":"10.1577/1548-8659(1961)23[3:THAPR]2.0.CO;2","usgsCitation":"Rucker, R., Yasutake, W.T., and Wolf, H., 1961, Trout hepatoma--a preliminary report: Progressive Fish-Culturist, v. 23, no. 1, p. 3-7, https://doi.org/10.1577/1548-8659(1961)23[3:THAPR]2.0.CO;2.","productDescription":"5 p.","startPage":"3","endPage":"7","numberOfPages":"5","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":654,"text":"Western Fisheries Research Center","active":true,"usgs":true}],"links":[{"id":313265,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"23","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"568ba5e4e4b0e7594ee776d9","contributors":{"authors":[{"text":"Rucker, R.R.","contributorId":104000,"corporation":false,"usgs":true,"family":"Rucker","given":"R.R.","email":"","affiliations":[],"preferred":false,"id":584221,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Yasutake, W. T.","contributorId":103222,"corporation":false,"usgs":true,"family":"Yasutake","given":"W.","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":584222,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Wolf, H.","contributorId":151062,"corporation":false,"usgs":false,"family":"Wolf","given":"H.","email":"","affiliations":[],"preferred":false,"id":584223,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":276,"text":"276 - 1961 - Surface water records of Missouri","interactions":[],"lastModifiedDate":"2014-08-05T09:20:54","indexId":"276","displayToPublicDate":"2015-08-30T09:19:23","publicationYear":"1961","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"title":"Surface water records of Missouri","docAbstract":"No abstract available.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Rolla, MO","doi":"10.3133/276","issn":"0565-5986","collaboration":"Prepared in cooperation with the State of Missouri and other agencies, 1960/61-1963/64.","usgsCitation":"U.S. Geological Survey, 1961, Surface water records of Missouri, 4 p., https://doi.org/10.3133/276.","productDescription":"4 p.","numberOfPages":"4","costCenters":[],"links":[{"id":291650,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"country":"United States","state":"Missouri","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -95.7747,35.9957 ], [ -95.7747,40.6136 ], [ -89.1045,40.6136 ], [ -89.1045,35.9957 ], [ -95.7747,35.9957 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"57ffd0a3e4b0824b2d17645b"}
,{"id":70157476,"text":"70157476 - 1961 - A preliminary study of the distribution of saline water in the bedrock aquifers of eastern Wisconsin","interactions":[],"lastModifiedDate":"2018-01-08T19:47:43","indexId":"70157476","displayToPublicDate":"2014-12-08T08:00:00","publicationYear":"1961","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":2,"text":"State or Local Government Series"},"seriesTitle":{"id":5596,"text":"Wisconsin Geological & Natural History Survey Information Circular","active":true,"publicationSubtype":{"id":2}},"seriesNumber":"5","title":"A preliminary study of the distribution of saline water in the bedrock aquifers of eastern Wisconsin","docAbstract":"<p>The occurrence of saline water in the bedrock aquifers of eastern Wisconsin has been known for many years. Because of the ready availability of fresh water from other sources, little has been known of the extent of the saline-water area. Saline ground water is a potential source of contamination to wells if it moves into fresh-water zones.</p>","language":"English","publisher":"Wisconsin Geological & Natural History Survey","publisherLocation":"Madison, WI","collaboration":"Prepared by United States Geological Survey in cooperation with the Wisconsin Geological and Natural History Survey","usgsCitation":"Ryling, R.W., 1961, A preliminary study of the distribution of saline water in the bedrock aquifers of eastern Wisconsin: Wisconsin Geological & Natural History Survey Information Circular 5, iv, 23 p.","productDescription":"iv, 23 p.","numberOfPages":"28","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":308493,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":350400,"rank":2,"type":{"id":15,"text":"Index Page"},"url":"https://wgnhs.uwex.edu/pubs/download_ic05/"}],"country":"United States","state":"Wisconsin","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -86.68212890625,\n              45.38301927899065\n            ],\n            [\n              -88.52783203125,\n              45.390735154248894\n            ],\n            [\n              -89.23095703125,\n              44.15068115978091\n            ],\n            [\n              -89.417724609375,\n              43.644025847699496\n            ],\n            [\n              -89.45068359374999,\n              42.88401467044253\n            ],\n            [\n              -89.373779296875,\n              42.48019996901214\n            ],\n            [\n              -88.11035156249999,\n              42.512601715736665\n            ],\n            [\n              -87.747802734375,\n              42.512601715736665\n            ],\n            [\n              -87.56103515625,\n              42.50450285299051\n            ],\n            [\n              -87.637939453125,\n              43.26920624914964\n            ],\n            [\n              -87.593994140625,\n              43.89789239125797\n            ],\n            [\n              -87.38525390624999,\n              44.465151013519616\n            ],\n            [\n              -87.25341796875,\n              44.77013681219717\n            ],\n            [\n              -86.68212890625,\n              45.38301927899065\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"56051eb0e4b058f706e512a6","contributors":{"authors":[{"text":"Ryling, Roy W.","contributorId":147926,"corporation":false,"usgs":true,"family":"Ryling","given":"Roy","email":"","middleInitial":"W.","affiliations":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"preferred":false,"id":573268,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":71764,"text":"tei810 - 1961 - Potential effects of Project Chariot on local water supplies","interactions":[],"lastModifiedDate":"2014-07-16T10:59:31","indexId":"tei810","displayToPublicDate":"2013-07-16T10:55:00","publicationYear":"1961","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":337,"text":"Trace Elements Investigations","code":"TEI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"810","title":"Potential effects of Project Chariot on local water supplies","docAbstract":"No abstract available.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Washington, D.C.","doi":"10.3133/tei810","collaboration":"Prepared on behalf of the San Francisco Operations Office, U.S. Atomic Energy Commission.","usgsCitation":"Piper, A.M., 1961, Potential effects of Project Chariot on local water supplies: U.S. Geological Survey Trace Elements Investigations 810, Report: 76 p.; 2 Maps; 3 Illustrations; 15 Tables, https://doi.org/10.3133/tei810.","productDescription":"Report: 76 p.; 2 Maps; 3 Illustrations; 15 Tables","costCenters":[],"links":[{"id":290267,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53c79f0de4b0194841642487","contributors":{"authors":[{"text":"Piper, Arthur Maine","contributorId":46427,"corporation":false,"usgs":true,"family":"Piper","given":"Arthur","email":"","middleInitial":"Maine","affiliations":[],"preferred":false,"id":284726,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
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