{"pageNumber":"2667","pageRowStart":"66650","pageSize":"25","recordCount":68807,"records":[{"id":70217843,"text":"70217843 - 1951 - Discussion of “pedological relations of infiltration phenomena”","interactions":[],"lastModifiedDate":"2021-02-05T18:51:23.367092","indexId":"70217843","displayToPublicDate":"1951-04-01T12:48:32","publicationYear":"1951","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1578,"text":"Eos, Transactions, American Geophysical Union","onlineIssn":"2324-9250","printIssn":"0096-394","active":true,"publicationSubtype":{"id":10}},"title":"Discussion of “pedological relations of infiltration phenomena”","docAbstract":"<p>Smith provides an illuminating consideration of infiltration through soil in relation to the structure and texture of the soil its moisture content, and the variation of infiltration for A, B, and C soil zones. The organic nature of soil might also be stressed. Rotting rootlets provide passageways for water in addition to physical structure and texture.</p><p>The impression is gained that mechanical treatment, such as plowing and harrowing, general decreases the infiltration capacity of soil, through destruction of surface structure, and fragmentation. This appears true of the soil in the physical sense. Equally true, in a plowed soil, may be the formation of puddling colloids after a rain, through the breaking of natural granules into fragments. However, the surface infiltration is increased by plowing and harrowing through the turnover of the sod layer composed of grasses and weeds. Smith does not consider the sod layer as a soil zone, yet it is the first barrier that precipitation must pass before it enters the structural crevices and textural pores of the soil. Although a dense sod layer usually does not increase runoff because of its retentive nature, it increases interception, and hence evaporation, so unless the sod is economic, the water is lost anyway.</p>","language":"English","publisher":"American Geophysical Union","doi":"10.1029/TR032i002p00282","usgsCitation":"Rasmussen, W.C., and Smith, W.O., 1951, Discussion of “pedological relations of infiltration phenomena”: Eos, Transactions, American Geophysical Union, v. 32, no. 20, p. 282-283, https://doi.org/10.1029/TR032i002p00282.","productDescription":"2 p.","startPage":"282","endPage":"283","costCenters":[],"links":[{"id":383060,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"32","issue":"20","noUsgsAuthors":false,"publicationDate":"2014-08-18","publicationStatus":"PW","contributors":{"authors":[{"text":"Rasmussen, W. C.","contributorId":62201,"corporation":false,"usgs":true,"family":"Rasmussen","given":"W.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":809885,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Smith, W. O.","contributorId":53015,"corporation":false,"usgs":true,"family":"Smith","given":"W.","email":"","middleInitial":"O.","affiliations":[],"preferred":false,"id":809886,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":3858,"text":"cir104 - 1951 - Water resources of southeastern Bucks County, Pennsylvania","interactions":[],"lastModifiedDate":"2023-08-25T20:10:22.091338","indexId":"cir104","displayToPublicDate":"1951-04-01T00:00:00","publicationYear":"1951","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":307,"text":"Circular","code":"CIR","onlineIssn":"2330-5703","printIssn":"1067-084X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"104","title":"Water resources of southeastern Bucks County, Pennsylvania","docAbstract":"<p>This report has been prepared as a contribution to the development of southeastern Bucks County, Pa. It summarizes available information on the water resources of this 90-square mile area and evaluates current supplies. Future development of the area may change both the available quantity and the quality of the water supply. The effective development of the area demands a continuing knowledge of the water used and the potential quantity and quality of water available from both underground and surface sources. The area is strategically important to a great industrial section of the Bast. Its eastern boundary is a 26-mile segment of the Delaware River along the extreme southeastern border of Bucks County, Pa. (fig. 1). The present.population of the area is about 40,000, including 24,800 in Bristol Borough and Township and 6,770 in Morrisville. The area is traversed by both the Pennsylvania and the Reading Railroads and also by U.S. Highways 1 and 13. These are main transportation routes connecting the great market outlets of Philadelphia and New York. The Delaware River'is navigable from Morrisville to the sea. The area is only a short distance upstream from the Port of Philadelphia, which ranks second only to New York as the most important seaport in the United States. The area is mostly flat, open land 10 to 60 feet above mean sea level. It contains several large Industries, concentrated chiefly in the Bristol area (pi. 1). There are also scattered industries in the Morrisville, Langhorne, and Bensalem areas. However, Bucks County retains some of the characteristics of a farming region. Truck farming and gardening are still carried on to a considerable extent. Along Delaware River below Morrisville the mining of sand and gravel is an Important industry. The facts summarized in this report have been accumulated over a period of 25 years or more by Federal, State, and local agencies in connection with Investigations for other purposes. Most of the data used in this report have been obtained by the United States Geological Survey in cooperation with the Pennsylvania Department of Forests and Waters, the Pennsylvania Department of Internal Affairs, the Pennsylvania Department of Commerce, and State Planning Board, the City of Philadelphia, the Corps of Engineers, and the Interstate Commission on the Delaware River Basin. This report was prepared in the Water Resources Division of the U.S.Geological Survey by Jack B. Qraham, District Geologist; John W. Mangan, District Engineer; and Walter F. White, Jr., District Chemist, under the general direction of C. G. Paulsen, Chief Hydraulic Engineer. </p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/cir104","usgsCitation":"Graham, J., Mangan, J., and White, W.F., 1951, Water resources of southeastern Bucks County, Pennsylvania: U.S. Geological Survey Circular 104, Report: i, 21 p.; 1 Plate: 19.85 x 11.88 inches, https://doi.org/10.3133/cir104.","productDescription":"Report: i, 21 p.; 1 Plate: 19.85 x 11.88 inches","costCenters":[{"id":532,"text":"Pennsylvania Water Science Center","active":true,"usgs":true}],"links":[{"id":420173,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_23934.htm","linkFileType":{"id":5,"text":"html"}},{"id":30938,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/circ/1951/0104/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":117886,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/circ/1951/0104/report-thumb.jpg"},{"id":30939,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/1951/0104/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Pennsylvania","county":"Bucks County","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -74.667,\n              40.25\n            ],\n            [\n              -75,\n              40.25\n            ],\n            [\n              -75,\n              40.05\n            ],\n            [\n              -74.667,\n              40.05\n            ],\n            [\n              -74.667,\n              40.25\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a14e4b07f02db602ee0","contributors":{"authors":[{"text":"Graham, Jack B.","contributorId":15182,"corporation":false,"usgs":true,"family":"Graham","given":"Jack B.","affiliations":[],"preferred":false,"id":147735,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Mangan, John W.","contributorId":26677,"corporation":false,"usgs":true,"family":"Mangan","given":"John W.","affiliations":[],"preferred":false,"id":147736,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"White, Walter F.","contributorId":52159,"corporation":false,"usgs":true,"family":"White","given":"Walter","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":147737,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70175796,"text":"70175796 - 1951 - Surface-water supplies of the Mesabi Iron Range","interactions":[],"lastModifiedDate":"2018-04-02T11:54:23","indexId":"70175796","displayToPublicDate":"1951-03-01T11:15:00","publicationYear":"1951","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":2,"text":"State or Local Government Series"},"seriesTitle":{"id":105,"text":"Bulletin","active":false,"publicationSubtype":{"id":2}},"seriesNumber":"5","title":"Surface-water supplies of the Mesabi Iron Range","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"Minnesota Department of Conservation, Division of Waters","publisherLocation":"St. Paul, MN","usgsCitation":"U.S. Geological Survey, 1951, Surface-water supplies of the Mesabi Iron Range: Bulletin 5, 117 p.","productDescription":"117 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":392,"text":"Minnesota Water Science Center","active":true,"usgs":true}],"links":[{"id":326921,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Minnesota","otherGeospatial":"Mesabi Iron Range","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"57b82debe4b03fd6b7da3a08","contributors":{"authors":[{"text":"U.S. Geological Survey","contributorId":152492,"corporation":true,"usgs":false,"organization":"U.S. Geological Survey","id":646368,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":72055,"text":"tem137 - 1951 - Preliminary statement of the analyses of ground water from the Morrison Formation, southwestern Colorado and southeastern Utah","interactions":[],"lastModifiedDate":"2014-02-28T13:54:13","indexId":"tem137","displayToPublicDate":"1951-01-01T14:50:00","publicationYear":"1951","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":338,"text":"Trace Elements Memorandum","code":"TEM","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"137","title":"Preliminary statement of the analyses of ground water from the Morrison Formation, southwestern Colorado and southeastern Utah","docAbstract":"As part of a study of the carnotite deposits of the Colorado Plateau,, samples of ground water from the Salt Wash sandstone and Brushy Basin shale members of the Morrison formation have been analyzed to determine their chemical character and metal content. The Salt Wash ground water is largely a bicarbonate solution with variable amounts of calcium and magnesium ions; that from the Brushy Basin is either a sulfate or bicarbonate solution with sodium, The ground water from the Salt Wash and Brushy Basin members is generally weakly alkaline In most samples, the metal ions of uranium, vanadium, copper, lead, and selenium are present in amounts of less than 1 part per million. It is concluded that if the ground water responsible for introduction of the uranium and vanadium metals into the Salt Wash was comparable to the recent ground water, it contained very small amounts of the metal ions.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/tem137","usgsCitation":"Phoenix, D.A., 1951, Preliminary statement of the analyses of ground water from the Morrison Formation, southwestern Colorado and southeastern Utah: U.S. Geological Survey Trace Elements Memorandum 137, Report: 12 p.; Plate 1: 22.10 inches x 27.51 inches; Plate 2: 21.48 inches x 25.29 inches, https://doi.org/10.3133/tem137.","productDescription":"Report: 12 p.; Plate 1: 22.10 inches x 27.51 inches; Plate 2: 21.48 inches x 25.29 inches","additionalOnlineFiles":"Y","costCenters":[],"links":[{"id":279202,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/tem/0137/report-thumb.jpg"},{"id":282982,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/tem/0137/plate-1.pdf"},{"id":282983,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/tem/0137/plate-2.pdf"},{"id":282981,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/tem/0137/report.pdf"}],"country":"United States","state":"Colorado;Utah","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -109.8248,37.5729 ], [ -109.8248,39.1428 ], [ -107.5644,39.1428 ], [ -107.5644,37.5729 ], [ -109.8248,37.5729 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"528c96b9e4b0c629af44ddf3","contributors":{"authors":[{"text":"Phoenix, David A.","contributorId":79156,"corporation":false,"usgs":true,"family":"Phoenix","given":"David","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":285052,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70221630,"text":"70221630 - 1951 - Ground water in alluvial deposits in Oklahoma","interactions":[],"lastModifiedDate":"2021-06-25T19:53:30.42827","indexId":"70221630","displayToPublicDate":"1951-01-01T14:46:03","publicationYear":"1951","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1472,"text":"Economic Geology","active":true,"publicationSubtype":{"id":10}},"title":"Ground water in alluvial deposits in Oklahoma","docAbstract":"<p><span>Alluvium along main streams&nbsp;</span>in<span>&nbsp;</span>Oklahoma<span>&nbsp;has long been recognized as a generally dependable aquifer. Pumping tests made&nbsp;</span>in<span>&nbsp;recent years afford a means of comparing one area with another. They indicate coefficients of transmissibility on the order of 70,000 gallons per day per foot&nbsp;</span>in<span>&nbsp;the Arkansas River alluvium near Fort Gibson, and 60,000&nbsp;</span>in<span>&nbsp;the North Canadian River alluvium near&nbsp;</span>Oklahoma<span>&nbsp;City and El Reno.</span></p>","language":"English","publisher":"Soicety of Economic Geologists","doi":"10.2113/gsecongeo.46.1.76","usgsCitation":"Schoff, S., and Reed, E., 1951, Ground water in alluvial deposits in Oklahoma: Economic Geology, v. 46, no. 1, p. 76-83, https://doi.org/10.2113/gsecongeo.46.1.76.","productDescription":"8 p.","startPage":"76","endPage":"83","costCenters":[],"links":[{"id":386753,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United  States","state":"Oklahoma","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -103.0078125,\n              37.020098201368114\n            ],\n            [\n              -103.02978515625,\n              36.500805317604794\n            ],\n            [\n              -99.97558593749999,\n              36.518465989675875\n            ],\n            [\n              -100.008544921875,\n              34.57895241036948\n            ],\n            [\n              -99.591064453125,\n              34.379712580462204\n            ],\n            [\n              -98.426513671875,\n              34.05265942137599\n            ],\n            [\n              -97.811279296875,\n              33.87953701355924\n            ],\n            [\n              -97.042236328125,\n              33.76088200086917\n            ],\n            [\n              -96.328125,\n              33.73347670599252\n            ],\n            [\n              -95.2294921875,\n              33.925129700072\n            ],\n            [\n              -94.482421875,\n              33.61461929233378\n            ],\n            [\n              -94.46044921875,\n              35.460669951495305\n            ],\n            [\n              -94.647216796875,\n              36.99377838872517\n            ],\n            [\n              -103.0078125,\n              37.020098201368114\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"46","issue":"1","noUsgsAuthors":false,"publicationDate":"1951-01-01","publicationStatus":"PW","contributors":{"authors":[{"text":"Schoff, S.L.","contributorId":107365,"corporation":false,"usgs":true,"family":"Schoff","given":"S.L.","email":"","affiliations":[],"preferred":false,"id":818286,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Reed, E.W.","contributorId":260643,"corporation":false,"usgs":false,"family":"Reed","given":"E.W.","email":"","affiliations":[],"preferred":false,"id":818287,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70094973,"text":"70094973 - 1951 - Preliminary report on the geology and ground-water supply of the Newark, New Jersey, area","interactions":[],"lastModifiedDate":"2014-06-26T11:57:25","indexId":"70094973","displayToPublicDate":"1951-01-01T09:47:00","publicationYear":"1951","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":2,"text":"State or Local Government Series"},"seriesTitle":{"id":136,"text":"Special Report (New Jersey Division of Water Policy and Supply)","active":false,"publicationSubtype":{"id":2}},"seriesNumber":"10","title":"Preliminary report on the geology and ground-water supply of the Newark, New Jersey, area","docAbstract":"<p>In the Newark area, ground water is used chiefly for industrial cooling, air-conditioning, general processing, and for sanitary purposes. A small amount is used in the manufacture of beverages. Total ground-water pumpage in Newark is estimated at not less than 20,000,000 gallons daily.</p>\n<br/>\n<p>The Newark area is underlain by formations of Recent, Pleistocene and Triassic age, and the geology and hydrologic properties of these formations are discussed. Attention is called to the important influence of a buried valley in the rock floor beneath the Newark area on the yield of wells located within it. Data on the fluctuation of the water levels and the variation in pumpage are presented, and their significance discussed. The results of a pumping test made during the investigation were inconclusive. The beneficial results of artificially recharging the aquifers in one part of the area are described.</p>\n<br/>\n<p>The intrusion of salt water into certain parts of the ground-water body is described and graphically portrayed by a map showing the chloride concentration of the ground water in various parts of the City. Insofar as available data permit, the chemical quality of the ground water is discussed and records are given of the ground-water temperatures in various parts of the City.</p>\n<br/>\n<p>There has been marked lowering of the water table in the eastern part of the area, accompanied by salt water intrusion, indicating that the safe yield of the formations in this part of Newark has probably been exceeded. It is recommended that the study of the ground-water resources of this area be continued, and that artificial recharging of the aquifers be increased over as wide an area as possible.</p>","language":"English","publisher":"New Jersey Deptartment of Conservation and Economic Development, Division of Water Policy and Supply","collaboration":"Prepared in cooperation with the United States Department of the Interior Geological Survey","usgsCitation":"Herpers, H., and Barksdale, H.C., 1951, Preliminary report on the geology and ground-water supply of the Newark, New Jersey, area: Special Report (New Jersey Division of Water Policy and Supply) 10, 52 p.","productDescription":"52 p.","numberOfPages":"53","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":282811,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/70094973.jpg"},{"id":284824,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/unnumbered/70094973/report.pdf"}],"country":"United States","state":"New Jersey","city":"Newark","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -74.251324,40.673903 ], [ -74.251324,40.788139 ], [ -74.112787,40.788139 ], [ -74.112787,40.673903 ], [ -74.251324,40.673903 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53559529e4b0120853e8c156","contributors":{"authors":[{"text":"Herpers, Henry","contributorId":8378,"corporation":false,"usgs":true,"family":"Herpers","given":"Henry","email":"","affiliations":[],"preferred":false,"id":491013,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Barksdale, Henry C.","contributorId":11463,"corporation":false,"usgs":true,"family":"Barksdale","given":"Henry","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":491014,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":1000281,"text":"1000281 - 1951 - An aquarium experiment on the American eel as a predator on larval lampreys","interactions":[],"lastModifiedDate":"2013-02-04T15:56:34","indexId":"1000281","displayToPublicDate":"1951-01-01T00:00:00","publicationYear":"1951","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1337,"text":"Copeia","active":true,"publicationSubtype":{"id":10}},"title":"An aquarium experiment on the American eel as a predator on larval lampreys","docAbstract":"The parasitic sea lamprey, <i>Petromyzon  marinus</i>, has in recent years spread throughout Lakes Huron and Michigan and is now firmly established in these waters (Applegate, 1949, Mich. Cons., 18 (4):  13-15). Coincident with their spread, the abundance of  lake trout,  <i>Salvelinus  namaycush</i>,  has declined in both lakes (Hile, 1949, Trans. Amer. Fish.  Soc., 76 (1946): 121-147) and the  lake  trout  as  well  as  other species of fishes are showing  an increase in scarring from lamprey attacks.  For Lake Michigan the analysis of fishermen's questionnaires gave  an increase in  percentage by  weight of lamprey-scarred lake trout from 31 percent in 1947 to 41  percent in 1948. The sea lamprey is now spreading through Lake Superior, the last of the Great Lakes  containing a large population of lake trout.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Copeia","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"American Society of Ichthyologists and Herpetologists","publisherLocation":"Lawrence, KS","doi":"10.2307/1437556","collaboration":"Out-of-print","usgsCitation":"Perlmutter, A., 1951, An aquarium experiment on the American eel as a predator on larval lampreys: Copeia, v. 1951, no. 2, p. 173-174, https://doi.org/10.2307/1437556.","productDescription":"2 p.","startPage":"173","endPage":"174","numberOfPages":"2","costCenters":[{"id":324,"text":"Great Lakes Science Center","active":true,"usgs":true}],"links":[{"id":266965,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.2307/1437556"},{"id":128990,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"1951","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad9e4b07f02db6852b3","contributors":{"authors":[{"text":"Perlmutter, Alfred","contributorId":104431,"corporation":false,"usgs":true,"family":"Perlmutter","given":"Alfred","email":"","affiliations":[],"preferred":false,"id":308332,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70011170,"text":"70011170 - 1951 - Fluorometric determination of zirconium in minerals","interactions":[],"lastModifiedDate":"2012-03-12T17:18:30","indexId":"70011170","displayToPublicDate":"1951-01-01T00:00:00","publicationYear":"1951","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":"Fluorometric determination of zirconium in minerals","docAbstract":"The increasing use of zirconium in alloys and in the ceramics industry has created renewed interest in methods for its determination. It is a common constituent of many minerals, but is usually present in very small amounts. Published methods tend to be tedious, time-consuming, and uncertain as to accuracy. A new fluorometric procedure, which overcomes these objections to a large extent, is based on the blue fluorescence given by zirconium and flavonol in sulfuric acid solution. Hafnium is the only element that interferes. The sample is fused with borax glass and sodium carbonate and extracted with water. The residue is dissolved in sulfuric acid, made alkaline with sodium hydroxide to separate aluminum, and filtered. The precipitate is dissolved in sulfuric acid and electrolysed in a Melaven cell to remove iron. Flavonol is then added and the fluorescence intensity is measured with a photo-fluorometer. Analysis of seven standard mineral samples shows excellent results. The method is especially useful for minerals containing less than 0.25% zirconium oxide.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Analytical Chemistry","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","issn":"00032700","usgsCitation":"Alford, W., Shapiro, L., and White, C.E., 1951, Fluorometric determination of zirconium in minerals: Analytical Chemistry, v. 23, no. 8, p. 1149-1152.","startPage":"1149","endPage":"1152","numberOfPages":"4","costCenters":[],"links":[{"id":221153,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"23","issue":"8","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a1290e4b0c8380cd54363","contributors":{"authors":[{"text":"Alford, W.C.","contributorId":86487,"corporation":false,"usgs":true,"family":"Alford","given":"W.C.","email":"","affiliations":[],"preferred":false,"id":360450,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Shapiro, L.","contributorId":103408,"corporation":false,"usgs":true,"family":"Shapiro","given":"L.","email":"","affiliations":[],"preferred":false,"id":360451,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"White, C. E.","contributorId":24915,"corporation":false,"usgs":false,"family":"White","given":"C.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":360449,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70191232,"text":"70191232 - 1951 - Conservation: Where we stand: Review of <i>Water, land, and people</i>","interactions":[],"lastModifiedDate":"2017-10-01T14:11:08","indexId":"70191232","displayToPublicDate":"1951-01-01T00:00:00","publicationYear":"1951","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":5506,"text":"The Living Wilderness","active":false,"publicationSubtype":{"id":10}},"title":"Conservation: Where we stand: Review of <i>Water, land, and people</i>","docAbstract":"<p>A distinguished conservationist, just returned from more than a year in those Pacific islands held in trust by the United States, reports that representatives of the government there are nearly completely concerned with the maintenance of an administrative organization. Actual advances in matters of land use, of maintaining the material and mental welfare of the native population, and the preservation of the most interesting remnants of untouched habitat, are just never made.</p><p>Any such oversimplification is, of course, subject to error in detail, but it nevertheless stands as a touchstone to where we stand in conservation. In much more guarded phrases, and with considerable supporting data, Bernard Frank and Anthony Netboy say much the same thing about governmental conservation in the United States in their recently published <i>Water, Land, and People</i>.</p>","language":"English","publisher":"The Wilderness Society","usgsCitation":"Leopold, L.B., 1951, Conservation: Where we stand: Review of <i>Water, land, and people</i>: The Living Wilderness, v. 36, no. Spring 1951, 2 p.","productDescription":"2 p.","costCenters":[],"links":[{"id":346303,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"36","issue":"Spring 1951","publicComments":"Review of <i>Water, Land, and People,</i> by Bernard Frank and Anthony Netboy; New York, Alfred A. Knopf, 1950.","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"59d1fe97e4b05fe04cc23528","contributors":{"authors":[{"text":"Leopold, Luna Bergere","contributorId":93884,"corporation":false,"usgs":true,"family":"Leopold","given":"Luna","email":"","middleInitial":"Bergere","affiliations":[],"preferred":false,"id":711642,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":1000069,"text":"1000069 - 1951 - Downstream movement of recently transformed sea lampreys, Petromyzon marinus, in Carp Lake River, Michigan","interactions":[],"lastModifiedDate":"2016-02-18T10:43:59","indexId":"1000069","displayToPublicDate":"1951-01-01T00:00:00","publicationYear":"1951","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":"Downstream movement of recently transformed sea lampreys, Petromyzon marinus, in Carp Lake River, Michigan","docAbstract":"<div class=\"paragraph\">In order to obtain more precise information concerning the downstream movement of recently transformed sea lampreys, a trapping device was operated in the Carp Lake River, Emmet County, Michigan, from October, 1948, to July, 1951.</div>\n<div class=\"paragraph\">The period of downstream migration typically extends from the latter part of October to the middle of April. It varies, however, from year to year with climatic conditions. A few migrants usually appear every day during this period but a sudden increase in water level is characteristically accompanied by a surge in downstream movement of newly transformed sea lampreys. This phenomenon is realized principally during the spring floods and often concurrently with autumn rains and mid-winter thaws.</div>\n<div class=\"paragraph\">A total of 7,969 downstream migrants were taken in the 1948&ndash;49 season; 16,235 in 1949&ndash;50, and 15,103 in 1950&ndash;51. Measurements of representative samples from the total catch of sea lamprey migrants of the 1948&ndash;49 and 1949&ndash;50 seasons revealed a range in length of 95 to 190 millimeters and an average length of 145 millimeters (3.7 to 7.5 inches; mean &ndash;5.7 inches).</div>","language":"English","publisher":"Taylor & Francis","doi":"10.1577/1548-8659(1951)81[275:DMORTS]2.0.CO;2","usgsCitation":"Applegate, V.C., and Brynildson, C.L., 1951, Downstream movement of recently transformed sea lampreys, Petromyzon marinus, in Carp Lake River, Michigan: Transactions of the American Fisheries Society, v. 81, p. 275-290, https://doi.org/10.1577/1548-8659(1951)81[275:DMORTS]2.0.CO;2.","productDescription":"16 p.","startPage":"275","endPage":"290","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":324,"text":"Great Lakes Science Center","active":true,"usgs":true}],"links":[{"id":128994,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"81","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a61e4b07f02db635fd4","contributors":{"authors":[{"text":"Applegate, Vernon C.","contributorId":39317,"corporation":false,"usgs":true,"family":"Applegate","given":"Vernon","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":308024,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Brynildson, Clifford L.","contributorId":40550,"corporation":false,"usgs":true,"family":"Brynildson","given":"Clifford","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":308025,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":3019,"text":"wsp1000 - 1951 - Geology and ground-water resources of the Santa Maria Valley area, California, with a section on surface-water resources","interactions":[],"lastModifiedDate":"2023-04-11T18:26:31.999187","indexId":"wsp1000","displayToPublicDate":"1951-01-01T00:00:00","publicationYear":"1951","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":"1000","title":"Geology and ground-water resources of the Santa Maria Valley area, California, with a section on surface-water resources","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wsp1000","usgsCitation":"Worts, G., and Thomasson, H.G., 1951, Geology and ground-water resources of the Santa Maria Valley area, California, with a section on surface-water resources: U.S. Geological Survey Water Supply Paper 1000, Report: vi, 169 p.; 6 Plates: 34.50 x 56.50 inches or smaller, https://doi.org/10.3133/wsp1000.","productDescription":"Report: vi, 169 p.; 6 Plates: 34.50 x 56.50 inches or smaller","costCenters":[],"links":[{"id":415583,"rank":9,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_24193.htm","linkFileType":{"id":5,"text":"html"}},{"id":29848,"rank":8,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1000/plate-6.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":29847,"rank":7,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1000/plate-5.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":29846,"rank":6,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1000/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":29845,"rank":5,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1000/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":29844,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1000/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":29849,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1000/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":29843,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1000/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":139460,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1000/report-thumb.jpg"}],"country":"United States","state":"California","otherGeospatial":"Santa Maria Valley area","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -120.667,\n              35.047\n            ],\n            [\n              -120.667,\n              34.825\n            ],\n            [\n              -120.167,\n              34.825\n            ],\n            [\n              -120.167,\n              35.047\n            ],\n            [\n              -120.667,\n              35.047\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adae4b07f02db685527","contributors":{"authors":[{"text":"Worts, George Frank","contributorId":100830,"corporation":false,"usgs":true,"family":"Worts","given":"George Frank","affiliations":[],"preferred":false,"id":146157,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Thomasson, H. G. Jr.","contributorId":84343,"corporation":false,"usgs":true,"family":"Thomasson","given":"H.","suffix":"Jr.","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":146156,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70176807,"text":"70176807 - 1951 - Ground-water situation in Oregon","interactions":[],"lastModifiedDate":"2016-10-21T13:11:23","indexId":"70176807","displayToPublicDate":"1951-01-01T00:00:00","publicationYear":"1951","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"title":"Ground-water situation in Oregon","docAbstract":"<p>The water that occurs beneath the land surface follows definite and well-known rules of hydraulics, the same as water on the surface. However, ground water must be studied by methods, some of which are unique to that type of water occurrence, in order to evaluate the part it plays in the over-all water scheme.</p><p>Water that falls on the land surface as rain or snow and water that rests upon the surface may in places pass laterally or downward through the pores of the earth materials. There it may take one or more of a variety of paths before again flowing out on the surface or being expelled to the atmosphere by evaporation and by the transpiration of plants. Water so diverted underground is delayed or diverted from its course toward the sea and that digression results in many services of prime importance to mankind. Underground, the water generally exceeds in total quantity the water present on the land surface at any one time.</p><p>The discussion of ground water can be clarified somewhat by a description of the major parts or phases of the normal path of water underground.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/70176807","collaboration":"Prepared in cooperation with the State Engineer of Oregon","usgsCitation":"Newcomb, R.C., 1951, Ground-water situation in Oregon, 19 p., https://doi.org/10.3133/70176807.","productDescription":"19 p.","numberOfPages":"26","costCenters":[{"id":518,"text":"Oregon Water Science Center","active":true,"usgs":true}],"links":[{"id":329384,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/70176807.jpg"},{"id":330318,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/unnumbered/70176807/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United 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,{"id":3905,"text":"cir151 - 1951 - Kansas-Missouri floods of July 1951","interactions":[],"lastModifiedDate":"2023-03-14T20:55:50.322038","indexId":"cir151","displayToPublicDate":"1951-01-01T00:00:00","publicationYear":"1951","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":307,"text":"Circular","code":"CIR","onlineIssn":"2330-5703","printIssn":"1067-084X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"151","title":"Kansas-Missouri floods of July 1951","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/cir151","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1951, Kansas-Missouri floods of July 1951: U.S. Geological Survey Circular 151, 69 p., https://doi.org/10.3133/cir151.","productDescription":"69 p.","costCenters":[],"links":[{"id":30992,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/1951/0151/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":117117,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/circ/1951/0151/report-thumb.jpg"},{"id":414137,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_23854.htm","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Kansas, Missouri","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -101,\n              40.5\n            ],\n            [\n              -101,\n              37\n            ],\n            [\n              -91,\n              37\n            ],\n            [\n              -91,\n              40.5\n            ],\n            [\n              -101,\n              40.5\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b32e4b07f02db6b4863","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":528153,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70184456,"text":"70184456 - 1951 - Vegetation of Southwestern watersheds in the nineteenth century","interactions":[],"lastModifiedDate":"2017-03-09T11:52:07","indexId":"70184456","displayToPublicDate":"1951-01-01T00:00:00","publicationYear":"1951","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1772,"text":"Geographical Review","active":true,"publicationSubtype":{"id":10}},"title":"Vegetation of Southwestern watersheds in the nineteenth century","docAbstract":"<p>The recollections of many old-timers who tell of grass “stirrup high” have given rise to the idea that vegetation in the Southwest was uniformly better in the middle of the last century than it is at present. The change is usually attributed to overgrazing, which timed if it did not cause extensive gullying of the alluvial valleys,<sup>I</sup> lowering the water table and decreasing the availability of water for plant use. This idea of an originally verdant vegetation, deteriorated as a result of man’s activities, has led to overoptimism concerning the possible results of reduced grazing. Obviously, any decrease in grazing pressure is a step in the right direction, but it is no exaggeration to say that recovery fo vegetation density on depleted ranges, even after protection for years, has been spotty and, in many places, disappointing. We may have allowed ourselves to be deluded by hopes of ‘restoring’ over large areas a level of vegetation density that was originally attained only in selected localities.</p><p>This conclusion is supported by the published diaries and field notes of members of early American exploring parties. They show that in certain places, particularly in south-central Arizona where grass is now meager, the alluvial valleys formerly supported large expanses of grassland. However, there were also many areas, even alluvial valleys, where grass was so poor that forage for a string of horses could hardly be obtained. Other areas, such as the Rio Puerco Valley, supported good grass in some places but only scattered shrubs, furnishing poor forage, in others, though until well past the middle of the nineteenth century extensive grazing had been prevented by frequent raids of hostile Indians.</p>","language":"English","publisher":"American Geographical Society","doi":"10.2307/211025","usgsCitation":"Leopold, L.B., 1951, Vegetation of Southwestern watersheds in the nineteenth century: Geographical Review, v. 41, no. 2, p. 295-316, https://doi.org/10.2307/211025.","productDescription":"22","startPage":"295","endPage":"316","costCenters":[],"links":[{"id":337174,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","otherGeospatial":"Southwest","volume":"41","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"58c277fbe4b014cc3a3e771e","contributors":{"authors":[{"text":"Leopold, Luna Bergere","contributorId":93884,"corporation":false,"usgs":true,"family":"Leopold","given":"Luna","email":"","middleInitial":"Bergere","affiliations":[],"preferred":false,"id":681595,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70221649,"text":"70221649 - 1951 - A state‐wide program of periodic measurements of ground‐water level In Nebraska","interactions":[],"lastModifiedDate":"2021-06-26T11:42:48.246322","indexId":"70221649","displayToPublicDate":"1935-08-01T06:38:48","publicationYear":"1951","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1578,"text":"Eos, Transactions, American Geophysical Union","onlineIssn":"2324-9250","printIssn":"0096-394","active":true,"publicationSubtype":{"id":10}},"title":"A state‐wide program of periodic measurements of ground‐water level In Nebraska","docAbstract":"<p><span>The precipitation&nbsp;</span>in<span>&nbsp;</span>Nebraska<span>&nbsp;has been considerably less than normal&nbsp;</span>in<span>&nbsp;the last four years, and&nbsp;</span>in<span>&nbsp;consequence the&nbsp;</span>ground<span>‐</span>water<span>&nbsp;</span>level<span>&nbsp;</span>in<span>&nbsp;many parts of the&nbsp;</span>State<span>&nbsp;has declined to&nbsp;</span>a<span>&nbsp;marked extent. Moreover,&nbsp;</span>in<span>&nbsp;some parts of&nbsp;</span>Nebraska<span>&nbsp;the&nbsp;</span>ground<span>‐</span>water<span>&nbsp;</span>level<span>&nbsp;has declined as the result of land‐drainage, and&nbsp;</span>in<span>&nbsp;other parts it has risen as the result of irrigation with&nbsp;</span>water<span>&nbsp;diverted from streams. These changes&nbsp;</span>in<span>&nbsp;</span>ground<span>‐</span>water<span>&nbsp;</span>level<span>&nbsp;produced by drainage, irrigation, and decreased precipitation have caused wells to fail, streams to cease flowing, lakes to become dry, and land to become&nbsp;</span>water<span>‐logged. Consequently, interest&nbsp;</span>in<span>&nbsp;fluctuations of&nbsp;</span>ground<span>‐</span>water<span>&nbsp;</span>level<span>&nbsp;has greatly increased, and the need of&nbsp;</span>a<span>&nbsp;systematic collection of base‐data for the future study of&nbsp;</span>ground<span>‐</span>water<span>&nbsp;problems has been recognized.&nbsp;</span></p>","language":"English","publisher":"American Geophysical Union","doi":"10.1029/TR016i002p00495","usgsCitation":"Wenzel, L., 1951, A state‐wide program of periodic measurements of ground‐water level In Nebraska: Eos, Transactions, American Geophysical Union, v. 16, no. 2, p. 495-498, https://doi.org/10.1029/TR016i002p00495.","productDescription":"4 p.","startPage":"495","endPage":"498","costCenters":[],"links":[{"id":386772,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United  States","state":"Nebraska","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -96.6796875,\n              42.74701217318067\n            ],\n            [\n              -98.37158203125,\n              43.004647127794435\n            ],\n            [\n              -104.0625,\n              43.004647127794435\n            ],\n            [\n              -104.04052734375,\n              40.9964840143779\n            ],\n            [\n              -102.01904296874999,\n              41.04621681452063\n            ],\n            [\n              -102.0849609375,\n              40.01078714046552\n            ],\n            [\n              -95.38330078125,\n              40.04443758460856\n            ],\n            [\n              -95.91064453125,\n              41.47566020027821\n            ],\n            [\n              -96.6796875,\n              42.74701217318067\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"16","issue":"2","noUsgsAuthors":false,"publicationDate":"2014-08-18","publicationStatus":"PW","contributors":{"authors":[{"text":"Wenzel, L.K.","contributorId":18733,"corporation":false,"usgs":true,"family":"Wenzel","given":"L.K.","email":"","affiliations":[],"preferred":false,"id":818352,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70178711,"text":"70178711 - 1950 - Ground water in the Escalante Valley, Beaver, Iron, and Washington Counties, Utah","interactions":[],"lastModifiedDate":"2017-01-24T16:42:09","indexId":"70178711","displayToPublicDate":"2016-11-01T00:00:00","publicationYear":"1950","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":4,"text":"Other Government Series"},"seriesTitle":{"id":294,"text":"Technical Publication","active":false,"publicationSubtype":{"id":4}},"seriesNumber":"6","title":"Ground water in the Escalante Valley, Beaver, Iron, and Washington Counties, Utah","docAbstract":"<p>Escalante Valley in southwestern Utah is one of the largest and most important ground-water areas of the State, with 1,300 square miles of arid land and an additional 1,500 square miles in its tributary drainage basin. Ground water is obtained from gravel and sand beds in the unconsolidated valley fill. In 1950 more irrigation wells were pumped than in any other basin of Utah, and their total pumpage exceeded 80,000 acre-feet. Farming is done chiefly in the Beryl-Enterprise district at the south (upper) end of the valley, where it depends almost entirely upon ground water, and in the Milford and Minersville districts in the northeast-central part of the valley. This progress report concerns chiefly the Beryl-Enterprise and Milford districts.</p>","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Twenty-seventh biennial report of the State Engineer to the Governor of Utah: 1948-1950","largerWorkSubtype":{"id":2,"text":"State or Local Government Series"},"language":"English","publisher":"Utah Department of Natural Resources, Division of Water Rights","publisherLocation":"Salt Lake City, UT","usgsCitation":"Fix, P., Nelson, W., Lofgren, B.E., and Butler, R., 1950, Ground water in the Escalante Valley, Beaver, Iron, and Washington Counties, Utah: Technical Publication 6, 102 p.","productDescription":"102 p.","startPage":"109","endPage":"210","numberOfPages":"122","costCenters":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":331491,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":333873,"rank":4,"type":{"id":22,"text":"Related Work"},"url":"https://www.waterrights.utah.gov/cgi-bin/libview.exe?Modinfo=Viewpub&LIBNUM=50-1-401","text":"Utah State Engineer's 27th Biennial Report (larger work)"},{"id":331490,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://waterrights.utah.gov/docSys/v920/w920/w9200085.pdf"},{"id":331489,"rank":1,"type":{"id":15,"text":"Index Page"},"url":"https://www.waterrights.utah.gov/cgi-bin/libview.exe?Modinfo=Viewpub&LIBNUM=20-4-150"}],"country":"United States","state":"Utah","county":"Beaver County, Iron County, Washington County","otherGeospatial":"Escalante Valley","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -114.04907226562499,\n              37.43997405227057\n            ],\n            [\n              -112.9998779296875,\n              37.80544394934271\n            ],\n            [\n              -112.7197265625,\n              38.40194908237822\n            ],\n            [\n              -112.8570556640625,\n              38.634036452919226\n            ],\n            [\n              -113.30749511718749,\n              38.67264490154078\n            ],\n            [\n              -113.88427734374999,\n              38.23386541556985\n            ],\n            [\n              -114.0985107421875,\n              37.82280243352756\n            ],\n            [\n              -114.04907226562499,\n              37.43997405227057\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"58468aefe4b04fc80e5236db","contributors":{"authors":[{"text":"Fix, Philip F.","contributorId":21649,"corporation":false,"usgs":true,"family":"Fix","given":"Philip F.","affiliations":[],"preferred":false,"id":654896,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Nelson, W.B.","contributorId":30282,"corporation":false,"usgs":true,"family":"Nelson","given":"W.B.","email":"","affiliations":[],"preferred":false,"id":654897,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Lofgren, B. E.","contributorId":42579,"corporation":false,"usgs":true,"family":"Lofgren","given":"B.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":654898,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Butler, R.G.","contributorId":60706,"corporation":false,"usgs":true,"family":"Butler","given":"R.G.","email":"","affiliations":[],"preferred":false,"id":654899,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70175888,"text":"70175888 - 1950 - Subsurface reconnaissance of glacial deposits in northeastern Kansas","interactions":[],"lastModifiedDate":"2016-08-19T14:09:06","indexId":"70175888","displayToPublicDate":"2016-01-12T00:00:00","publicationYear":"1950","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":"Subsurface reconnaissance of glacial deposits in northeastern Kansas","language":"English","publisher":"University of Kansas","publisherLocation":"Lawrence, KS","usgsCitation":"Frye, J., and Walters, K., 1950, Subsurface reconnaissance of glacial deposits in northeastern Kansas: Kansas Geological Survey Bulletin, v. 86, no. 6, p. 141-158.","productDescription":"17 p.","startPage":"141","endPage":"158","costCenters":[{"id":353,"text":"Kansas Water Science Center","active":false,"usgs":true}],"links":[{"id":327086,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":327085,"rank":1,"type":{"id":15,"text":"Index Page"},"url":"https://www.kgs.ku.edu/General/geologyBulls.html"}],"volume":"86","issue":"6","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"57b82deae4b03fd6b7da3a03","contributors":{"authors":[{"text":"Frye, J.C.","contributorId":35067,"corporation":false,"usgs":true,"family":"Frye","given":"J.C.","email":"","affiliations":[],"preferred":false,"id":646499,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Walters, K.L.","contributorId":105765,"corporation":false,"usgs":true,"family":"Walters","given":"K.L.","affiliations":[],"preferred":false,"id":646500,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70160630,"text":"70160630 - 1950 - Pollution in the lower Columbia Basin in 1948 with particular reference to the Willamette River","interactions":[],"lastModifiedDate":"2015-12-28T10:19:13","indexId":"70160630","displayToPublicDate":"2015-09-07T00:00:00","publicationYear":"1950","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":1,"text":"Federal Government Series"},"seriesTitle":{"id":84,"text":"Special Scientific Report - Fisheries","active":false,"publicationSubtype":{"id":1}},"seriesNumber":"30","title":"Pollution in the lower Columbia Basin in 1948 with particular reference to the Willamette River","docAbstract":"<p>Development of the salmon resources of the lower Columbia River Basin appears as sound insurance against the threat of a serious reduction in the runs to the upper river areas through the multiple-purpose programs of water development now under way by the Corps of Engineers, the Bureau of Reclamation, and private interests. Any comprehensive plan for the full development of the fisheries resources in the lower Columbia Basin must be predicated upon accurate knowledge of the waters therein polluted to a degree affecting fish life. Pollution surveys have been made in the lower Columbia Basin at various times in the past -- the most intensive studies having been made in the Willamette Valley.</p>","language":"English","publisher":"U.S. Department of the Interior, Fish and Wildlife Service","usgsCitation":"Fish, F.F., and Rucker, R., 1950, Pollution in the lower Columbia Basin in 1948 with particular reference to the Willamette River: Special Scientific Report - Fisheries 30, 32 p.","productDescription":"32 p.","numberOfPages":"32","costCenters":[{"id":654,"text":"Western Fisheries Research Center","active":true,"usgs":true}],"links":[{"id":312882,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":312880,"rank":1,"type":{"id":11,"text":"Document"},"url":"https://spo.nmfs.noaa.gov/SSRF/SSRF30.pdf","text":"pdf"}],"country":"United States","state":"Oregon","otherGeospatial":"Columbia River, Willamette River","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -123.96972656249999,\n              46.2102496001872\n            ],\n            [\n              -123.96972656249999,\n              45.47554027158593\n            ],\n            [\n              -124.23339843749999,\n              43.46886761482925\n            ],\n            [\n              -124.56298828125001,\n              42.85985981506279\n            ],\n            [\n              -124.43115234375,\n              42.45588764197166\n            ],\n            [\n              -124.16748046874999,\n              42.00032514831621\n            ],\n            [\n              -123.72802734375,\n              41.983994270935625\n            ],\n            [\n              -122.25585937500001,\n              41.96765920367816\n            ],\n            [\n              -118.828125,\n              41.983994270935625\n            ],\n            [\n              -116.93847656250001,\n              42.114523952464246\n            ],\n            [\n              -117.04833984375001,\n              44.5435052132082\n            ],\n            [\n              -116.82861328125001,\n              45.583289756006316\n            ],\n            [\n              -117.02636718749999,\n              45.96642454131025\n            ],\n            [\n              -118.828125,\n              46.027481852486645\n            ],\n            [\n              -120.25634765624999,\n              45.73685954736049\n            ],\n            [\n              -121.37695312499999,\n              45.69083283645816\n            ],\n            [\n              -122.23388671874999,\n              45.72152152227954\n            ],\n            [\n              -122.62939453125001,\n              46.01222384063236\n            ],\n            [\n              -122.93701171874999,\n              46.30140615437332\n            ],\n            [\n              -123.33251953125,\n              46.392411189814645\n            ],\n            [\n              -123.68408203124999,\n              46.34692761055676\n            ],\n            [\n              -123.96972656249999,\n              46.2102496001872\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"56826b47e4b0a04ef4925b90","contributors":{"authors":[{"text":"Fish, F. F.","contributorId":82572,"corporation":false,"usgs":true,"family":"Fish","given":"F.","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":583398,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Rucker, R.R.","contributorId":104000,"corporation":false,"usgs":true,"family":"Rucker","given":"R.R.","email":"","affiliations":[],"preferred":false,"id":583399,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70175889,"text":"70175889 - 1950 - Geology and ground-water resources of Rice County, Kansas:","interactions":[],"lastModifiedDate":"2016-08-19T14:12:11","indexId":"70175889","displayToPublicDate":"2015-06-24T00:00:00","publicationYear":"1950","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 Rice County, Kansas:","language":"English","publisher":"University of Kansas","publisherLocation":"Lawrence, KS","usgsCitation":"Fent, O.S., 1950, Geology and ground-water resources of Rice County, Kansas:: Kansas Geological Survey Bulletin, v. 85, 142.","productDescription":"142","costCenters":[{"id":353,"text":"Kansas Water Science Center","active":false,"usgs":true}],"links":[{"id":327091,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":327090,"rank":1,"type":{"id":15,"text":"Index Page"},"url":"https://www.kgs.ku.edu/General/geologyBulls.html"}],"volume":"85","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"57b82dbde4b03fd6b7da3703","contributors":{"authors":[{"text":"Fent, O. S.","contributorId":173880,"corporation":false,"usgs":false,"family":"Fent","given":"O.","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":646501,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70175887,"text":"70175887 - 1950 - Subsurface reconnaissance of glacial deposits in northeastern Kansas","interactions":[],"lastModifiedDate":"2016-08-19T14:09:31","indexId":"70175887","displayToPublicDate":"2015-01-06T00:00:00","publicationYear":"1950","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":"Subsurface reconnaissance of glacial deposits in northeastern Kansas","language":"English","publisher":"University of Kansas","publisherLocation":"Lawrence, KS","usgsCitation":"Frye, J., and Walters, K., 1950, Subsurface reconnaissance of glacial deposits in northeastern Kansas: Kansas Geological Survey Bulletin, v. 86, no. 6, p. 141-158.","productDescription":"17 p.","startPage":"141","endPage":"158","costCenters":[{"id":353,"text":"Kansas Water Science Center","active":false,"usgs":true}],"links":[{"id":327087,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":327084,"rank":1,"type":{"id":15,"text":"Index Page"},"url":"https://www.kgs.ku.edu/General/geologyBulls.html"}],"volume":"86","issue":"6","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"57b82deae4b03fd6b7da39fd","contributors":{"authors":[{"text":"Frye, J.C.","contributorId":35067,"corporation":false,"usgs":true,"family":"Frye","given":"J.C.","email":"","affiliations":[],"preferred":false,"id":646497,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Walters, K.L.","contributorId":105765,"corporation":false,"usgs":true,"family":"Walters","given":"K.L.","affiliations":[],"preferred":false,"id":646498,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70047775,"text":"70047775 - 1950 - Preliminary report on the ground-water resources of southwestern Skagit County, Washington","interactions":[{"subject":{"id":70047775,"text":"70047775 - 1950 - Preliminary report on the ground-water resources of southwestern Skagit County, Washington","indexId":"70047775","publicationYear":"1950","noYear":false,"title":"Preliminary report on the ground-water resources of southwestern Skagit County, Washington"},"predicate":"SUPERSEDED_BY","object":{"id":51045,"text":"ofr5136 - 1951 - Preliminary report on the ground-water resources of southwestern Skagit County, Washington","indexId":"ofr5136","publicationYear":"1951","noYear":false,"title":"Preliminary report on the ground-water resources of southwestern Skagit County, Washington"},"id":1}],"supersededBy":{"id":51045,"text":"ofr5136 - 1951 - Preliminary report on the ground-water resources of southwestern Skagit County, Washington","indexId":"ofr5136","publicationYear":"1951","noYear":false,"title":"Preliminary report on the ground-water resources of southwestern Skagit County, Washington"},"lastModifiedDate":"2013-08-22T16:19:57","indexId":"70047775","displayToPublicDate":"2013-01-01T16:12:39","publicationYear":"1950","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":2,"text":"State or Local Government Series"},"seriesTitle":{"id":116,"text":"Ground-water Report","active":false,"publicationSubtype":{"id":2}},"seriesNumber":"1","title":"Preliminary report on the ground-water resources of southwestern Skagit County, Washington","language":"English","publisher":"Washington Department of Natural Resources","publisherLocation":"Olympia, WA","collaboration":"Prepared in cooperation with State of Washington, Department of Conservation and Development, Division of Hydraulics","usgsCitation":"Sceva, J.E., 1950, Preliminary report on the ground-water resources of southwestern Skagit County, Washington: Ground-water Report 1, ii, 40 p.; Maps: 2 Sheets.","productDescription":"ii, 40 p.; Maps: 2 Sheets","costCenters":[],"links":[{"id":276924,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Washington","county":"Skagit County","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -122.7596,48.2951 ], [ -122.7596,48.6598 ], [ -120.6854,48.6598 ], [ -120.6854,48.2951 ], [ -122.7596,48.2951 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"521732e7e4b043bae8d2e607","contributors":{"authors":[{"text":"Sceva, Jack E.","contributorId":79086,"corporation":false,"usgs":true,"family":"Sceva","given":"Jack","email":"","middleInitial":"E.","affiliations":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"preferred":false,"id":482942,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70040288,"text":"70040288 - 1950 - The ground-water resources of Montgomery County, New York","interactions":[],"lastModifiedDate":"2012-10-12T17:16:08","indexId":"70040288","displayToPublicDate":"2012-01-01T10:19:43","publicationYear":"1950","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":4,"text":"Other Government Series"},"seriesTitle":{"id":242,"text":"Bulletin","active":false,"publicationSubtype":{"id":4}},"seriesNumber":"GW-23","title":"The ground-water resources of Montgomery County, New York","language":"English","publisher":"New York State Water Power and Control Commission","publisherLocation":"Albany, NY","usgsCitation":"Jeffords, R., 1950, The ground-water resources of Montgomery County, New York: Bulletin GW-23, 63 p., 2 Plates.","productDescription":"63 p., 2 Plates","numberOfPages":"63","costCenters":[{"id":474,"text":"New York Water Science Center","active":true,"usgs":true}],"links":[{"id":262553,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"New York","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -79.76,40.48 ], [ -79.76,45.02 ], [ -71.86,45.02 ], [ -71.86,40.48 ], [ -79.76,40.48 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"50e50731e4b0e8fec6ce9f03","contributors":{"authors":[{"text":"Jeffords, R.M.","contributorId":70233,"corporation":false,"usgs":true,"family":"Jeffords","given":"R.M.","email":"","affiliations":[],"preferred":false,"id":468001,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70040287,"text":"70040287 - 1950 - The ground-water resources of Schoharie County, New York","interactions":[],"lastModifiedDate":"2012-10-12T17:16:08","indexId":"70040287","displayToPublicDate":"2012-01-01T10:12:47","publicationYear":"1950","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":4,"text":"Other Government Series"},"seriesTitle":{"id":242,"text":"Bulletin","active":false,"publicationSubtype":{"id":4}},"seriesNumber":"GW-22","title":"The ground-water resources of Schoharie County, New York","language":"English","publisher":"New York State Water Power and Control Commission","publisherLocation":"Albany, NY","usgsCitation":"Berdan, J., 1950, The ground-water resources of Schoharie County, New York: Bulletin GW-22, 61 p., 2 Plates.","productDescription":"61 p., 2 Plates","numberOfPages":"61","costCenters":[{"id":474,"text":"New York Water Science Center","active":true,"usgs":true}],"links":[{"id":262551,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"New York","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -79.76,40.48 ], [ -79.76,45.02 ], [ -71.86,45.02 ], [ -71.86,40.48 ], [ -79.76,40.48 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"50e50737e4b0e8fec6ce9f16","contributors":{"authors":[{"text":"Berdan, J.M.","contributorId":27913,"corporation":false,"usgs":true,"family":"Berdan","given":"J.M.","affiliations":[],"preferred":false,"id":468000,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70040286,"text":"70040286 - 1950 - The ground-water resources of Rensselaer County, New York","interactions":[],"lastModifiedDate":"2012-10-12T17:16:08","indexId":"70040286","displayToPublicDate":"2012-01-01T10:06:03","publicationYear":"1950","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":4,"text":"Other Government Series"},"seriesTitle":{"id":242,"text":"Bulletin","active":false,"publicationSubtype":{"id":4}},"seriesNumber":"GW-21","title":"The ground-water resources of Rensselaer County, New York","language":"English","publisher":"New York State Water Power and Control Commission","publisherLocation":"Albany, NY","usgsCitation":"Cushman, R., 1950, The ground-water resources of Rensselaer County, New York: Bulletin GW-21, 56 p., 3 Plates.","productDescription":"56 p., 3 Plates","numberOfPages":"56","costCenters":[{"id":474,"text":"New York Water Science Center","active":true,"usgs":true}],"links":[{"id":262552,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"New York","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -79.76,40.48 ], [ -79.76,45.02 ], [ -71.86,45.02 ], [ -71.86,40.48 ], [ -79.76,40.48 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"50e50735e4b0e8fec6ce9f0e","contributors":{"authors":[{"text":"Cushman, R.V.","contributorId":28220,"corporation":false,"usgs":true,"family":"Cushman","given":"R.V.","email":"","affiliations":[],"preferred":false,"id":467999,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":5220061,"text":"5220061 - 1950 - Toxicity and repellency to rats of actidione","interactions":[],"lastModifiedDate":"2025-02-27T18:10:54.981849","indexId":"5220061","displayToPublicDate":"2010-06-16T12:18:19","publicationYear":"1950","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2524,"text":"Journal of the American Pharmaceutical Association, Scientific Edition","active":true,"publicationSubtype":{"id":10}},"title":"Toxicity and repellency to rats of actidione","docAbstract":"<p><span>The antibiotic actidione was found to be highly repellent to laboratory rats and to significantly reduce gnawing attacks upon treated paperboards. Rats refused to accept food or water containing this material even under conditions of acute starvation and died of starvation and thirst rather than accept water containing 1.0</span><span>&nbsp;</span><span>mg. of actidione per liter. The compound is highly toxic to rats with the minimum lethal dose by oral administration being approximately 1.0 mg./Kg. body weight. Paperboard treated with the compound resisted gnawing attacks by specially trained and motivated rats for periods of two hundred hours, although similar untreated boards were pierced within thirty to sixty minutes.</span></p>","language":"English","publisher":"Elsevier","doi":"10.1002/jps.3030391006","usgsCitation":"Traub, R., DeWitt, J., Welch, J., and Newman, D., 1950, Toxicity and repellency to rats of actidione: Journal of the American Pharmaceutical Association, Scientific Edition, v. 39, no. 10, p. 552-555, https://doi.org/10.1002/jps.3030391006.","productDescription":"4 p.","startPage":"552","endPage":"555","numberOfPages":"4","costCenters":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":196170,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"39","issue":"10","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a4ee4b07f02db6280d0","contributors":{"authors":[{"text":"Traub, R.","contributorId":73303,"corporation":false,"usgs":true,"family":"Traub","given":"R.","email":"","affiliations":[],"preferred":false,"id":331273,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"DeWitt, J.B.","contributorId":89080,"corporation":false,"usgs":true,"family":"DeWitt","given":"J.B.","email":"","affiliations":[],"preferred":false,"id":331274,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Welch, J.F.","contributorId":21241,"corporation":false,"usgs":true,"family":"Welch","given":"J.F.","email":"","affiliations":[],"preferred":false,"id":331272,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Newman, D.","contributorId":104588,"corporation":false,"usgs":true,"family":"Newman","given":"D.","email":"","affiliations":[],"preferred":false,"id":331275,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
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