{"pageNumber":"7033","pageRowStart":"175800","pageSize":"25","recordCount":184617,"records":[{"id":70011109,"text":"70011109 - 1953 - Geochemical studies of clay minerals III. The determination of free silica and free alumina in montmorillonites","interactions":[],"lastModifiedDate":"2020-11-24T23:00:46.723064","indexId":"70011109","displayToPublicDate":"1953-01-01T00:00:00","publicationYear":"1953","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":"Geochemical studies of clay minerals III. The determination of free silica and free alumina in montmorillonites","docAbstract":"<p>Determination of free silica by the method proposed made possible the derivation of logical formulas for several specimens of montmorillonites for which the formulas could not be derived from the analyses alone. Other montmorillonites, for which logical formulas could be derived from their analyses, were found to contain small amounts of free silica or free alumina. Others were found to contain neither free silica nor free alumina.</p><p>The method consists of the following steps: (1) digestion of 1 g of the specimen with 0.5 N NaOH solution in a covered platinum crucible or dish on a steam bath for 4 hrs, stirring the mixture at 30-min intervals, (2) filtration of the undissolved material, followed by washing several times with 1% NaOH solution, (3) neutralization of the filtrate with HCl, addition of 5 ml HCl in excess and determination of SiO and Al<sub>2</sub>O<sub>3</sub><span>&nbsp;</span>in the usual way and (4) calculation of the amount of free SiO<sub>2</sub><span>&nbsp;</span>or free Al<sub>2</sub>O<sub>3</sub><span>&nbsp;</span>if any and the amount of attack of the clay structure by the treatment from the ratio of SiO<sub>2</sub><span>&nbsp;</span>to Al<sub>2</sub>O<sub>3</sub><span>&nbsp;</span>dissolved and the ratio of SiO<sub>2</sub><span>&nbsp;</span>to Al<sub>2</sub>O<sub>3</sub><span>&nbsp;</span>obtained on analysis.</p><p>Tests with 5% Na<sub>2</sub>CO<sub>3</sub><span>&nbsp;</span>solution, the reagent formerly used for the solution of free SiO<sub>2</sub><span>&nbsp;</span>in rocks and minerals, showed that solution of opal by this reagent is always fractional, never complete, no matter how small the amount present or how long the period of treatment. Re-treatment of the sample results in 90–95% solution if 10 mg or less of opal is present, but for larger amounts of opal the percentage dissolved decreases as the amount present increases.</p><p>On the other hand, 75 ml of 0.5 N NaOH completely dissolves as much as 400 mg of opal in 4 hrs digestion in a covered platinum crucible or dish, on a steam bath. However, a weaker solution or a shorter period of digestion does not effect complete solution. The same amount (75 ml) of 0.5 N NaOH also dissolves 90 mg of cristobalite and 57 mg of quartz having a grain size of less than 2 microns.</p><p>Use of NaOH also permits determination of the amount of alumina dissolved, and estimation of the extent to which the clay structure was attacked by the treatment.</p>","language":"English","publisher":"Elsevier","doi":"10.1016/0016-7037(53)90003-9","usgsCitation":"Foster, M., 1953, Geochemical studies of clay minerals III. The determination of free silica and free alumina in montmorillonites: Geochimica et Cosmochimica Acta, v. 3, no. 2-3, p. 143-154, https://doi.org/10.1016/0016-7037(53)90003-9.","productDescription":"12 p.","startPage":"143","endPage":"154","numberOfPages":"12","costCenters":[],"links":[{"id":221570,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"3","issue":"2-3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a16aee4b0c8380cd55220","contributors":{"authors":[{"text":"Foster, Margaret D.","contributorId":97958,"corporation":false,"usgs":true,"family":"Foster","given":"Margaret D.","affiliations":[],"preferred":false,"id":360299,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70011093,"text":"70011093 - 1953 - Water","interactions":[],"lastModifiedDate":"2012-03-12T17:18:27","indexId":"70011093","displayToPublicDate":"1953-01-01T00:00:00","publicationYear":"1953","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":"Water","docAbstract":"[No abstract available]","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Analytical Chemistry","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","issn":"00032700","usgsCitation":"Love, S.K., and Thatcher, L.L., 1953, Water: Analytical Chemistry, v. 25, no. 1, p. 65-74.","startPage":"65","endPage":"74","numberOfPages":"10","costCenters":[],"links":[{"id":221349,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"25","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505bc3fee4b08c986b32b44e","contributors":{"authors":[{"text":"Love, S. K.","contributorId":27419,"corporation":false,"usgs":true,"family":"Love","given":"S.","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":360265,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Thatcher, L. L.","contributorId":23271,"corporation":false,"usgs":true,"family":"Thatcher","given":"L.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":360264,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70011107,"text":"70011107 - 1953 - Separation of antimony by solvent extraction","interactions":[],"lastModifiedDate":"2012-03-12T17:19:08","indexId":"70011107","displayToPublicDate":"1953-01-01T00:00:00","publicationYear":"1953","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":"Separation of antimony by solvent extraction","docAbstract":"[No abstract available]","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Analytical Chemistry","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","issn":"00032700","usgsCitation":"White, C.E., and Rose, H., 1953, Separation of antimony by solvent extraction: Analytical Chemistry, v. 25, no. 2, p. 351-353.","startPage":"351","endPage":"353","numberOfPages":"3","costCenters":[],"links":[{"id":221568,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"25","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505b8d3fe4b08c986b3182f8","contributors":{"authors":[{"text":"White, C. E.","contributorId":24915,"corporation":false,"usgs":false,"family":"White","given":"C.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":360296,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Rose, H.J.","contributorId":67121,"corporation":false,"usgs":true,"family":"Rose","given":"H.J.","email":"","affiliations":[],"preferred":false,"id":360297,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70011089,"text":"70011089 - 1953 - Method for determination of small amounts of rare earths and thorium in phosphate rocks","interactions":[],"lastModifiedDate":"2012-03-12T17:18:28","indexId":"70011089","displayToPublicDate":"1953-01-01T00:00:00","publicationYear":"1953","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":"Method for determination of small amounts of rare earths and thorium in phosphate rocks","docAbstract":"In laboratory investigations, interest developed in the possible rare-earth content of phosphate samples from Florida and the northwestern United States. Because of the difficulty of making chemical determinations of traces of individual rare earths, a combined chemical-spectrographic method was investigated. After removal of iron by the extraction of the chloride with ether, the rare earths and thorium are concentrated by double oxalate precipitation, using calcium as a carrier. The rare earths are freed from calcium by an ammonium hydroxide precipitation with a fixed amount of aluminum as a carrier. The aluminum also serves as an internal standard in the final spectrographic analysis. The method will determine from 0.02 to 2 mg. of each rare earth with an error no greater than 10%. The investigation has resulted in a fairly rapid and precise procedure, involving no special spectrographic setup. The method could be applied to other types of geologic materials with the same expected accuracy.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Analytical Chemistry","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","issn":"00032700","usgsCitation":"Waring, C.L., and Mela, H., 1953, Method for determination of small amounts of rare earths and thorium in phosphate rocks: Analytical Chemistry, v. 25, no. 3, p. 432-435.","startPage":"432","endPage":"435","numberOfPages":"4","costCenters":[],"links":[{"id":221275,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"25","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a554ee4b0c8380cd6d1a6","contributors":{"authors":[{"text":"Waring, C. L.","contributorId":96355,"corporation":false,"usgs":true,"family":"Waring","given":"C.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":360259,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Mela, H. Jr.","contributorId":68033,"corporation":false,"usgs":true,"family":"Mela","given":"H.","suffix":"Jr.","affiliations":[],"preferred":false,"id":360258,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70011072,"text":"70011072 - 1953 - The addition of iodine to tetramethylammonium iodide","interactions":[],"lastModifiedDate":"2020-11-23T17:56:36.40131","indexId":"70011072","displayToPublicDate":"1953-01-01T00:00:00","publicationYear":"1953","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2423,"text":"Journal of Physical Chemistry","active":true,"publicationSubtype":{"id":10}},"title":"The addition of iodine to tetramethylammonium iodide","docAbstract":"<p>The system tetramethylammonium iodide-iodine-toluene has been studied by the solubility method at 6 and at 25°. The compounds (CH<sub>3</sub>)<sub>4</sub>NI<sub>3</sub>, (CH<sub>3</sub>)<sub>4</sub>NI<sub>5</sub> and (CH<sub>3</sub>)<sub>4</sub>NI<sub>11</sub> were found to be stable phases at both temperatures. In addition, the compound (CH<sub>3</sub>)<sub>4</sub>NI<sub>10</sub> was found at 6° and the compound (CH<sub>3</sub>)<sub>4</sub>NI<sub>9</sub> at 25°. The dissociation pressures of the compounds at these temperatures were calculated from the solubility data.</p>","language":"English","publisher":"ACS Publications","doi":"10.1021/j150502a025","usgsCitation":"Foote, H.W., and Fleischer, M., 1953, The addition of iodine to tetramethylammonium iodide: Journal of Physical Chemistry, v. 57, no. 1, p. 122-125, https://doi.org/10.1021/j150502a025.","productDescription":"4 p.","startPage":"122","endPage":"125","numberOfPages":"4","costCenters":[],"links":[{"id":221087,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"57","issue":"1","noUsgsAuthors":false,"publicationDate":"2002-05-01","publicationStatus":"PW","scienceBaseUri":"505ba9a3e4b08c986b3223d7","contributors":{"authors":[{"text":"Foote, H. W.","contributorId":103006,"corporation":false,"usgs":true,"family":"Foote","given":"H.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":360221,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Fleischer, M.","contributorId":84069,"corporation":false,"usgs":true,"family":"Fleischer","given":"M.","email":"","affiliations":[],"preferred":false,"id":360220,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70011094,"text":"70011094 - 1953 - Quercetin as colorimetric reagent for determination of zirconium","interactions":[],"lastModifiedDate":"2020-11-24T22:53:27.504576","indexId":"70011094","displayToPublicDate":"1953-01-01T00:00:00","publicationYear":"1953","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":"Quercetin as colorimetric reagent for determination of zirconium","docAbstract":"<p>Methods described in the literature for the determination of zirconium are generally designed for relatively large amounts of this element. A good procedure using colorimetric reagent for the determination of trace amounts is desirable. Quercetin has been found to yield a sensitive color reaction with zirconium suitable for the determination of from 0.1 to 50 <sub><span class=\"mwe-math-element\"><img class=\"mwe-math-fallback-image-inline\" src=\"https://wikimedia.org/api/rest_v1/media/math/render/svg/a223c880b0ce3da8f64ee33c4f0010beee400b1a\" alt=\"\\gamma \" aria-hidden=\"true\" data-mce-src=\"https://wikimedia.org/api/rest_v1/media/math/render/svg/a223c880b0ce3da8f64ee33c4f0010beee400b1a\"></span></sub><span> </span>of zirconium dioxide. The procedure developed involves the separation of zirconium from interfering elements by precipitation with p-dimethylaminoazophenylarsonic acid prior to its estimation with quercetin. The quercetin reaction is carried out in 0.5N hydrochloric acid solution. Under the operating conditions it is indicated that quercetin forms a 2 to 1 complex with zirconium; however, a 2 to 1 and a 1 to 1 complex can coexist under special conditions. Approximate values for the equilibrium constants of the complexes are K<sub>1</sub> = 0.33 x 10<sup>-5</sup> and K<sub>2</sub> = 1.3 x 10<sup>-9</sup>. Seven Bureau of Standards samples of glass sands and refractories were analyzed with excellent results. The method described should find considerable application in the analysis of minerals and other materials for macro as well as micro amounts of zirconium.</p>","language":"English","publisher":"ACS Publications","doi":"10.1021/ac60084a026","usgsCitation":"Grimaldi, F.S., and White, C.E., 1953, Quercetin as colorimetric reagent for determination of zirconium: Analytical Chemistry, v. 25, no. 12, p. 1886-1890, https://doi.org/10.1021/ac60084a026.","productDescription":"5 p.","startPage":"1886","endPage":"1890","numberOfPages":"5","costCenters":[],"links":[{"id":221350,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"25","issue":"12","noUsgsAuthors":false,"publicationDate":"2002-05-01","publicationStatus":"PW","scienceBaseUri":"505a92e7e4b0c8380cd80aee","contributors":{"authors":[{"text":"Grimaldi, F. S.","contributorId":94286,"corporation":false,"usgs":true,"family":"Grimaldi","given":"F.","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":360267,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"White, C. E.","contributorId":24915,"corporation":false,"usgs":false,"family":"White","given":"C.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":360266,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70011108,"text":"70011108 - 1953 - Ultraviolet spectrophotometric determination of tantalum with pyrogallol","interactions":[],"lastModifiedDate":"2020-11-24T22:58:35.295691","indexId":"70011108","displayToPublicDate":"1953-01-01T00:00:00","publicationYear":"1953","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":"Ultraviolet spectrophotometric determination of tantalum with pyrogallol","docAbstract":"<p>In a search for a more rapid method for the determination of tantalum in rocks and minerals, an intensive study was made of the tantalum-pyrogallol reaction recommended by Platanov and Krivoshlikov, and a better modified spectrophotometric procedure is given. The improved method consists in measuring the absorbancy of the tantalum-pyrogallol complex at 325 m<i>μ</i> in 4<i>N</i> hydrochloric acid and a fixed concentration (0.0175<i>M</i>) of ammonium oxalate. Beer's law is followed for the concentration range up to 40 γ per ml. Sensitivity in terms of molar absorbancy index is 4775. Most interferences are additive in character and readily correctable. Separations or major corrections are required in the presence of significant amounts of molybdenum, tungsten, antimony, and uranium. The method has been successfully applied to three ores previously analyzed by gravimetric techniques. The method affords greater speed, sensitivity, and reproducibility in the determination of tantalum in rocks and minerals. A more reliable technique for preparing standard solutions of tantalum has been developed.</p>","language":"English","publisher":"ACS Publications","doi":"10.1021/ac60084a004","usgsCitation":"Dinnin, J., 1953, Ultraviolet spectrophotometric determination of tantalum with pyrogallol: Analytical Chemistry, v. 25, no. 12, p. 1803-1807, https://doi.org/10.1021/ac60084a004.","productDescription":"5 p.","startPage":"1803","endPage":"1807","numberOfPages":"5","costCenters":[],"links":[{"id":221569,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"25","issue":"12","noUsgsAuthors":false,"publicationDate":"2002-05-01","publicationStatus":"PW","scienceBaseUri":"505bbc0ee4b08c986b3289dd","contributors":{"authors":[{"text":"Dinnin, J. I.","contributorId":50886,"corporation":false,"usgs":true,"family":"Dinnin","given":"J. I.","affiliations":[],"preferred":false,"id":360298,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":39721,"text":"pp257A - 1953 - Lake Bonneville: Geology of northern Utah Valley, Utah","interactions":[{"subject":{"id":52055,"text":"ofr49117 - 1949 - Statement on the hydrology of pre-Pleistocene (?) aquifers, from a chapter on water resources to be included in a Geological Survey report on the geology of North Utah Valley","indexId":"ofr49117","publicationYear":"1949","noYear":false,"title":"Statement on the hydrology of pre-Pleistocene (?) aquifers, from a chapter on water resources to be included in a Geological Survey report on the geology of North Utah Valley"},"predicate":"SUPERSEDED_BY","object":{"id":39721,"text":"pp257A - 1953 - Lake Bonneville: Geology of northern Utah Valley, Utah","indexId":"pp257A","publicationYear":"1953","noYear":false,"chapter":"A","title":"Lake Bonneville: Geology of northern Utah Valley, Utah"},"id":1}],"lastModifiedDate":"2022-11-22T15:28:33.251107","indexId":"pp257A","displayToPublicDate":"1953-01-01T00:00:00","publicationYear":"1953","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":331,"text":"Professional Paper","code":"PP","onlineIssn":"2330-7102","printIssn":"1044-9612","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"257","chapter":"A","title":"Lake Bonneville: Geology of northern Utah Valley, Utah","docAbstract":"<p>Lake Bonneville was a vast Pleistocene lake that covered 20,000 square miles in northwestern Utah and had a maximum depth of about 1,000 feet. It was a body of water comparable in size to modern Lake Michigan.</p><p>Surveys of the unconsolidated deposits in the Lake Bonneville basin utilize the same methods used in studies of hard rocks, namely: separation of the deposits into mappable units and contacts between formations; observations of lateral and vertical changes in lithology; and plotting of these data on the map.</p>","language":"English","publisher":"U.S. Government Printing Office","publisherLocation":"Washington, D.C.","doi":"10.3133/pp257A","usgsCitation":"Hunt, C.B., Varnes, H., and Thomas, H.E., 1953, Lake Bonneville: Geology of northern Utah Valley, Utah: U.S. Geological Survey Professional Paper 257, Report: v, 99 p.; 4 Plates, https://doi.org/10.3133/pp257A.","productDescription":"Report: v, 99 p.; 4 Plates","numberOfPages":"109","costCenters":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":409532,"rank":6,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0257a/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":409531,"rank":5,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0257a/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":409530,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0257a/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":409529,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0257a/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":122291,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/0257a/report-thumb.jpg"},{"id":67485,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/0257a/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Utah","otherGeospatial":"Northern Utah Valley","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b32e4b07f02db6b42ff","contributors":{"authors":[{"text":"Hunt, C. B.","contributorId":42573,"corporation":false,"usgs":true,"family":"Hunt","given":"C.","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":222036,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Varnes, H.D.","contributorId":38631,"corporation":false,"usgs":true,"family":"Varnes","given":"H.D.","email":"","affiliations":[],"preferred":false,"id":222035,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Thomas, H. E.","contributorId":12829,"corporation":false,"usgs":true,"family":"Thomas","given":"H.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":222034,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70184457,"text":"70184457 - 1953 - Downstream change of velocity in rivers","interactions":[],"lastModifiedDate":"2017-03-09T12:02:51","indexId":"70184457","displayToPublicDate":"1953-01-01T00:00:00","publicationYear":"1953","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":732,"text":"American Journal of Science","active":true,"publicationSubtype":{"id":10}},"title":"Downstream change of velocity in rivers","docAbstract":"<p>Because river slope generally decreases in a downstream direction, it is generally supposed that velocity of flow also decreases downstream. Analysis of some of the large number of velocity measurements made at stream-gaging stations demonstrates that mean velocity generally tends to increase downstream. Although there are many reaches in nearly all rivers where mean velocity decreases downstream, the general tendency for conservation or for downstream increase was found in all data studied.</p><p>Computations of bed velocity indicate that this parameter also tends to increase downstream.</p><p>Near the streambed, shear in the vertical profile of velocity (rate of decrease of velocity with depth) tends to decrease downstream. This down-valley decrease of shear implies decreasing competence downstream.</p>","language":"English","publisher":"American Journal of Science","doi":"10.2475/ajs.251.8.606","usgsCitation":"Leopold, L.B., 1953, Downstream change of velocity in rivers: American Journal of Science, v. 251, no. 8, p. 606-624, https://doi.org/10.2475/ajs.251.8.606.","productDescription":"19 p.","startPage":"606","endPage":"624","costCenters":[],"links":[{"id":480434,"rank":0,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.2475/ajs.251.8.606","text":"Publisher Index Page"},{"id":337177,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"251","issue":"8","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"58c277fbe4b014cc3a3e771c","contributors":{"authors":[{"text":"Leopold, Luna Bergere","contributorId":93884,"corporation":false,"usgs":true,"family":"Leopold","given":"Luna","email":"","middleInitial":"Bergere","affiliations":[],"preferred":false,"id":681597,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":1285,"text":"wsp1190 - 1953 - Ground-water conditions in artesian aquifers in Brown County, Wisconsin","interactions":[],"lastModifiedDate":"2023-04-11T19:43:34.619708","indexId":"wsp1190","displayToPublicDate":"1953-01-01T00:00:00","publicationYear":"1953","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":"1190","title":"Ground-water conditions in artesian aquifers in Brown County, Wisconsin","docAbstract":"The principal water-bearing rocks underlying Brown County, Wis., are thick sandstone units of Cambrian and Ordovician age. Other aquifers include limestone and dolomite of Ordovician age, dolomite of Silurian age, and sands and gravel of Pleistocene and Recent age. Underlying the water-bearing formations are crystalline rocks of pre-Cambrian age which contain little or no water. \r\n\r\nGround water is the source of all public and most private and industrial supplies in. the county. Several of the large industries use large quantities of surface water also. Most of the water is pumped from wells that penetrate the Cambrian sandstones where the water occurs under artesian conditions. From 1886, when the first deep well was drilled, to 1949, the pumpage in the county increased to an average of about 5 million gallons a day (mgd) in 1939 and to about 10 mgd in 1949.\r\n\r\nThe piezometric level, which was about 100 feet above the land surface in 1886, was about 300 feet below the land surface in 1949. About 200 feet of this decline took place after 1938. The water-level-measurement program begun in 1946 shows that yearly fluctuations of water levels in observation wells range from less than 1 foot to about 90 feet, the fluctuations being larger at the center of the heavily pumped area. The highest water levels occur in the winter or spring and the lowest in the summer near the end of the season of maximum withdrawal. Coefficients of transmissibility and storage for the sandstones were obtained by making controlled pumping tests at Green Bay and De Pere. The coefficients were verified by comparing computed water-level declines and rates of withdrawal with actual ones. The computed values were within I0 percent of the actual values. \r\n\r\nProbable declines of water levels by 1960 were computed, using the same coefficients of transmissibility and storage, and assuming three different conditions of pumping. The additional decline in water level will be 15 to 150 feet in the center of the pumped area, depending upon the amount of increased pumping and its distribution relative to the present pumped area and to the recharge area. \r\n\r\nThe water from the sandstones is a hard calcium magnesium bicarbonate water. Further work is needed to determine whether there is danger of contamination by salt water which occurs down the dip in the same formations. It is concluded that the rate of withdrawal from the area can be increased to 15 mgd by 1960 without dangerously lowering water levels, provided that new wells are properly spaced. In order to avoid expressive lowering of water levels, it is recommended that new wells be located west of Green Bay toward the recharge area. \r\n\r\nA detailed study has not been made of shallow aquifers in the county. Further work should be done to evaluate the possibilities of auxiliary supplies from the limestone of the Platteville formation or from the Niagara dolomite. \r\n\r\nConservation should be practice.4 by all users of ground water to avoid waste resulting in lower water levels and higher pumping costs.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wsp1190","usgsCitation":"Drescher, W.J., 1953, Ground-water conditions in artesian aquifers in Brown County, Wisconsin: U.S. Geological Survey Water Supply Paper 1190, Report: iv, 49 p.; 7 Plates: 20.00 x 9.00 inches or smaller, https://doi.org/10.3133/wsp1190.","productDescription":"Report: iv, 49 p.; 7 Plates: 20.00 x 9.00 inches or smaller","numberOfPages":"53","costCenters":[],"links":[{"id":415594,"rank":10,"type":{"id":36,"text":"NGMDB Index 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,{"id":70184458,"text":"70184458 - 1953 - Relation of suspended-sediment concentration to channel scour and fill","interactions":[],"lastModifiedDate":"2017-03-09T12:18:27","indexId":"70184458","displayToPublicDate":"1953-01-01T00:00:00","publicationYear":"1953","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"Relation of suspended-sediment concentration to channel scour and fill","docAbstract":"<p>It is known that during the passage of a flood the channel of an alluvial stream scours and fills with considerable rapidity. Though such changes may be random, it seems more likely that there is a definite pattern of channel change directly related both to discharge and to the sediment load provided to the river by the drainage basin.</p><p>In a study by the authors [1] an analysis was made of concurrent values of suspended sediment load and width, mean depth, mean velocity, and discharge at a number of gaging stations. From the data analyzed it appeared that fairly definite relations exist between these variables.</p>","largerWorkType":{"id":24,"text":"Conference Paper"},"largerWorkTitle":"Proceedings of the fifth Hydraulics Conference, June 9-11, 1952, arranged by the Iowa Institute of Hydraulic Research","largerWorkSubtype":{"id":19,"text":"Conference Paper"},"conferenceTitle":"Proceedings of the fifth Hydraulics Conference","conferenceDate":"June 9-11, 1952","conferenceLocation":"Iowa City, IA","language":"English","usgsCitation":"Leopold, L.B., and Maddock, T., 1953, Relation of suspended-sediment concentration to channel scour and fill, <i>in</i> Proceedings of the fifth Hydraulics Conference, June 9-11, 1952, arranged by the Iowa Institute of Hydraulic Research, Iowa City, IA, June 9-11, 1952, p. 159-178.","productDescription":"20 p.","startPage":"159","endPage":"178","costCenters":[],"links":[{"id":337178,"rank":1,"type":{"id":15,"text":"Index Page"},"url":"https://ir.uiowa.edu/uisie/34/","text":"Conference Proceedings"},{"id":337179,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"publicComments":"University of Iowa Studies in Engineering, 34","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"58c277fbe4b014cc3a3e771a","contributors":{"authors":[{"text":"Leopold, Luna Bergere","contributorId":93884,"corporation":false,"usgs":true,"family":"Leopold","given":"Luna","email":"","middleInitial":"Bergere","affiliations":[],"preferred":false,"id":681598,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Maddock, Thomas Jr.","contributorId":14402,"corporation":false,"usgs":true,"family":"Maddock","given":"Thomas","suffix":"Jr.","email":"","affiliations":[],"preferred":false,"id":681599,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":1000178,"text":"1000178 - 1953 - Fluctuations in the fisheries of State of Michigan waters of Green Bay","interactions":[],"lastModifiedDate":"2016-02-15T13:22:01","indexId":"1000178","displayToPublicDate":"1953-01-01T00:00:00","publicationYear":"1953","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1664,"text":"Fishery Bulletin of the U.S. Fish and Wildlife Service","active":true,"publicationSubtype":{"id":10}},"title":"Fluctuations in the fisheries of State of Michigan waters of Green Bay","docAbstract":"<p>Green Bay, traditionally a major center of production, has assumed in recent years a position of overwhelming dominance in the commercial fisheries of the State of Michigan waters of Lake Michigan. Within the 4-year period 1945-1948 the commercial take in State of Michigan waters of Green Bay increased from 3,317,000 pounds in 1945 to 7,909,000 pounds in 1948, and it was 7,782,000 poinds in 1949. At the same time the percentage contribution of Green Bay to the State total for Lake Michigan rose each year, increasing from 36.5 in 1945 to 65.4 in 1949. The tremendous upswing in commercial production in Green Bay can be attributed to the abnormally high abundance of three important species--the lake whitefish (Coregonus clupeaformis), the lake herring or shallowwater cisco (Coregonus [=Leucichthys] artedii), and the walleye or yellow pikeperch (Stizostedion v. vitreum)--and to a marked rise in fishing intensity.</p>","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Fishery Bulletin of the U.S. Fish and Wildlife Service","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"U.S. Fish and Wildlife Service","usgsCitation":"Hile, R., Lunger, G.F., and Buettner, H.J., 1953, Fluctuations in the fisheries of State of Michigan waters of Green Bay: Fishery Bulletin of the U.S. Fish and Wildlife Service, v. 54, no. 75, p. 1-34.","productDescription":"p. 1-34","startPage":"1","endPage":"34","numberOfPages":"33","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":324,"text":"Great Lakes Science Center","active":true,"usgs":true}],"links":[{"id":131765,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"54","issue":"75","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b25e4b07f02db6aed3d","contributors":{"authors":[{"text":"Hile, Ralph","contributorId":48510,"corporation":false,"usgs":true,"family":"Hile","given":"Ralph","email":"","affiliations":[],"preferred":false,"id":308196,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Lunger, George F.","contributorId":11550,"corporation":false,"usgs":true,"family":"Lunger","given":"George","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":308195,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Buettner, Howard J.","contributorId":82247,"corporation":false,"usgs":true,"family":"Buettner","given":"Howard","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":308197,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":1000145,"text":"1000145 - 1953 - The effect of ether anesthesia on fin-clipping rate","interactions":[],"lastModifiedDate":"2016-02-15T13:56:55","indexId":"1000145","displayToPublicDate":"1953-01-01T00:00:00","publicationYear":"1953","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":"The effect of ether anesthesia on fin-clipping rate","docAbstract":"<p>As part of an experimental program to learn the effects of stocking lake trout (Salvelinus namaycush) in Lake Superior, 141, 392 fingerlings were marked at the Charlevoix (Michigan) Station of the U.S. Fish and Wildlife Service in October 1952. The adipose fin was removed from all fish, the right pelvic from the remainder. A random sample of 2, 417 of the fish showed an average total length of 4.0 inches (range, 2.7 to 5.4). The mean weight of all fish marked was slightly less than one-third ounce (49 fish per pound). The local women, none of whom had previous experience in the work, were employed to mark the fish. Bone-cutting forceps were used for excision of the fins, and each worker wore a bobbinet glove to facilitate handling of the fish. On alternate days the fish were anesthetized with ether before marking, to determine the effect of its use on the fin-clipping rate.</p>","language":"English","publisher":"Taylor & Francis","doi":"10.1577/1548-8640(1953)15[80:TEOEAO]2.0.CO;2","usgsCitation":"Eschmeyer, P.H., 1953, The effect of ether anesthesia on fin-clipping rate: Progressive Fish-Culturist, v. 15, no. 2, p. 80-82, https://doi.org/10.1577/1548-8640(1953)15[80:TEOEAO]2.0.CO;2.","productDescription":"3 p.","startPage":"80","endPage":"82","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":324,"text":"Great Lakes Science Center","active":true,"usgs":true}],"links":[{"id":133229,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"15","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a80e4b07f02db649641","contributors":{"authors":[{"text":"Eschmeyer, Paul H.","contributorId":86719,"corporation":false,"usgs":true,"family":"Eschmeyer","given":"Paul","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":308142,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":1000296,"text":"1000296 - 1953 - Lake fisheries need lamprey control and research","interactions":[],"lastModifiedDate":"2012-02-02T00:04:05","indexId":"1000296","displayToPublicDate":"1953-01-01T00:00:00","publicationYear":"1953","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3560,"text":"The Fisherman","active":true,"publicationSubtype":{"id":10}},"title":"Lake fisheries need lamprey control and research","docAbstract":"Since 1921, when the first sea lamprey was recorded from Lake Erie, concern about this parasite in the Great Lakes above Niagara Falls, where previously it had never occurred, grew successively.  At first, the concern was shared only in scientific circles, but as the parasite continued its persistent and rapid spread throughout the upper Great Lakes this concern was voiced by state conservation departments, the U.S. Fish and Wildlife Service, and interested fishermen.  Catches of lake trout especially, and other species secondarily, began to fall below anything representing normal fluctuations in abundance.  The fishing industry on Lake Huron and Lake Michigan became extremely concerned due to the fact that income was diminishing greatly.  Producers on Lake Superior were fearful that the same decline in production would soon characterize their fishery.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"The Fisherman","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","usgsCitation":"Moffett, J.W., 1953, Lake fisheries need lamprey control and research: The Fisherman, v. 21, no. 4, p. 10-11.","productDescription":"p. 10-11,14","startPage":"10","endPage":"11","numberOfPages":"1","costCenters":[{"id":324,"text":"Great Lakes Science Center","active":true,"usgs":true}],"links":[{"id":128655,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"21","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b28e4b07f02db6b12b5","contributors":{"authors":[{"text":"Moffett, James W.","contributorId":94245,"corporation":false,"usgs":true,"family":"Moffett","given":"James","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":308353,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":81350,"text":"81350 - 1953 - Sea lamprey spawning: Wisconsin and Minnesota streams of Lake Superior","interactions":[],"lastModifiedDate":"2023-04-04T15:32:23.205022","indexId":"81350","displayToPublicDate":"1953-01-01T00:00:00","publicationYear":"1953","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":"97","title":"Sea lamprey spawning: Wisconsin and Minnesota streams of Lake Superior","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Fish and Wildlife Service","usgsCitation":"Loeb, H.A., 1953, Sea lamprey spawning: Wisconsin and Minnesota streams of Lake Superior: Special Scientific Report - Fisheries 97, 36 p.","productDescription":"36 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":324,"text":"Great Lakes Science Center","active":true,"usgs":true}],"links":[{"id":198426,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":101780,"rank":2,"type":{"id":15,"text":"Index Page"},"url":"https://spo.nmfs.noaa.gov/content/sea-lamprey-spawning-wisconsin-and-minnesota-streams-lake-superior"}],"country":"United States","state":"Minnesota, Wisconsin","otherGeospatial":"Lake Superior","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -90.2932442060535,\n              46.53801849599847\n            ],\n            [\n              -89.50894716491341,\n              48.02282639866175\n            ],\n            [\n              -91.15711887978152,\n              48.20234741183825\n            ],\n            [\n              -91.7057408913751,\n              48.15833881302618\n            ],\n            [\n              -92.48213634605524,\n              48.40319670473866\n            ],\n            [\n              -93.32900490043916,\n              46.61093869529458\n            ],\n            [\n              -93.55261656462791,\n              45.75903028146064\n            ],\n            [\n              -89.53197557881144,\n              45.82436185574744\n            ],\n            [\n              -90.2932442060535,\n              46.53801849599847\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0ce4b07f02db5fc5e3","contributors":{"authors":[{"text":"Loeb, Howard A.","contributorId":63505,"corporation":false,"usgs":true,"family":"Loeb","given":"Howard","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":295272,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":1000448,"text":"1000448 - 1953 - A modification in the technique of computing average lengths from the scales of fishes","interactions":[],"lastModifiedDate":"2013-01-28T13:36:23","indexId":"1000448","displayToPublicDate":"1953-01-01T00:00:00","publicationYear":"1953","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3196,"text":"Progressive Fish-Culturist","active":true,"publicationSubtype":{"id":10}},"title":"A modification in the technique of computing average lengths from the scales of fishes","docAbstract":"In virtually all the studies that employ scales, otollths, or bony structures to obtain the growth history of fishes, it has been the custom to compute lengths for each individual fish and from these data obtain the average growth rates for any particular group. This method involves a considerable amount of mathematical manipulation, time, and effort. Theoretically it should be possible to obtain the same information simply by averaging the scale measurements for each year of life and the length of the fish employed and computing the average lengths from these data. This method would eliminate all calculations for individual fish. Although Van Oosten (1929: 338) pointed out many years ago the validity of this method of computation, his statements apparently have been overlooked by subsequent investigators.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Progressive Fish-Culturist","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"Taylor & Francis","publisherLocation":"London, UK","doi":"10.1577/1548-8640(1953)15[85:AMITTO]2.0.CO;2","collaboration":"Out-of-print","usgsCitation":"Van Oosten, J., 1953, A modification in the technique of computing average lengths from the scales of fishes: Progressive Fish-Culturist, v. 15, no. 2, p. 85-86, https://doi.org/10.1577/1548-8640(1953)15[85:AMITTO]2.0.CO;2.","productDescription":"p. 85-86","startPage":"85","endPage":"86","numberOfPages":"1","costCenters":[{"id":324,"text":"Great Lakes Science Center","active":true,"usgs":true}],"links":[{"id":130584,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":266617,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1577/1548-8640(1953)15[85:AMITTO]2.0.CO;2"}],"volume":"15","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b23e4b07f02db6adeed","contributors":{"authors":[{"text":"Van Oosten, John","contributorId":23479,"corporation":false,"usgs":true,"family":"Van Oosten","given":"John","email":"","affiliations":[],"preferred":false,"id":308561,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":39176,"text":"pp248F - 1953 - Mica deposits of the southeastern Piedmont, Part 9, Thomaston-Barnesville district, Georgia; Part 10, Outlying deposits in Georgia","interactions":[{"subject":{"id":55364,"text":"ofr4468 - 1944 - Georgia mica mines","indexId":"ofr4468","publicationYear":"1944","noYear":false,"title":"Georgia mica mines"},"predicate":"SUPERSEDED_BY","object":{"id":39176,"text":"pp248F - 1953 - Mica deposits of the southeastern Piedmont, Part 9, Thomaston-Barnesville district, Georgia; Part 10, Outlying deposits in Georgia","indexId":"pp248F","publicationYear":"1953","noYear":false,"chapter":"F","title":"Mica deposits of the southeastern Piedmont, Part 9, Thomaston-Barnesville district, Georgia; Part 10, Outlying deposits in Georgia"},"id":1},{"subject":{"id":55366,"text":"ofr4467 - 1944 - Map of the Mitchell Creek mine, Upson County, Georgia","indexId":"ofr4467","publicationYear":"1944","noYear":false,"title":"Map of the Mitchell Creek mine, Upson County, 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,{"id":70189740,"text":"70189740 - 1953 - The use of soils and paleosols for interpreting geomorphic and climatic history of arid regions","interactions":[],"lastModifiedDate":"2017-07-22T13:01:12","indexId":"70189740","displayToPublicDate":"1953-01-01T00:00:00","publicationYear":"1953","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"seriesTitle":{"id":5468,"text":"Research Council of Israel Special Publication","active":false,"publicationSubtype":{"id":19}},"seriesNumber":"2","title":"The use of soils and paleosols for interpreting geomorphic and climatic history of arid regions","docAbstract":"<p>The study of modern surface soils, and ancient weathering zones, which occur either buried or as surface relicts, has contributed materially to understanding the complex events of the glacial and post-glacial period both in glaciated areas and in regions not influenced by glaciation. Most work of this kind in the United States has been done by geologists.</p><p>Numerous Pleistocene geologists have noted weathered zones between sheets of glacial drift or loess in the middle western United States. These include Condra, et al<sup>5</sup>; Frye<sup>7</sup>; Frye and Leonard<sup>8</sup>; Kay and Pearce<sup>13</sup>; Leighton and MacClintock<sup>15</sup>; Leverett<sup>16</sup>,<sup>17</sup>,<sup>18</sup>; Lugn<sup>19</sup>; Peltier<sup>23</sup>; Schultz and Stout<sup>26</sup>; Schultz, et al<sup>27</sup>; and Simonson<sup>28</sup>. Kay and Pearce<sup>13</sup> interpreted the weathered zones between sheets of glacial drift as profiles of ancient soils which they referred to as gumbotil. Hseung, Marshall and Krusekopf<sup>10</sup> have recently questioned the pedogenic character of gumbotil, but have failed to offer a satisfactory alternative explanation. Thorp, and coworkers<sup>30</sup>, in a general review of buried soils, apparently consider gumbotil a product of ancient soil-forming processes.</p>","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Desert research: Proceedings (Research Council of Israel Special Publication No. 2)","largerWorkSubtype":{"id":12,"text":"Conference publication"},"conferenceTitle":"Desert Research","conferenceDate":"May 7-14, 1952","conferenceLocation":"Jerusalem, Israel","language":"English","publisher":"Research Council of Israel","publisherLocation":"Jerusalem, Israel","usgsCitation":"Miller, J., and Leopold, L.B., 1953, The use of soils and paleosols for interpreting geomorphic and climatic history of arid regions, <i>in</i> Desert research: Proceedings (Research Council of Israel Special Publication No. 2), Jerusalem, Israel, May 7-14, 1952, p. 453-462.","productDescription":"10 p.","startPage":"453","endPage":"462","costCenters":[],"links":[{"id":344223,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"59746421e4b0ec1a48878495","contributors":{"authors":[{"text":"Miller, John","contributorId":190242,"corporation":false,"usgs":false,"family":"Miller","given":"John","email":"","affiliations":[],"preferred":false,"id":706049,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Leopold, Luna Bergere","contributorId":93884,"corporation":false,"usgs":true,"family":"Leopold","given":"Luna","email":"","middleInitial":"Bergere","affiliations":[],"preferred":false,"id":706050,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70184460,"text":"70184460 - 1953 - River meanders and vorticity theorem","interactions":[],"lastModifiedDate":"2017-03-09T12:33:42","indexId":"70184460","displayToPublicDate":"1953-01-01T00:00:00","publicationYear":"1953","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3879,"text":"Eos, Earth and Space Science News","active":true,"publicationSubtype":{"id":10}},"title":"River meanders and vorticity theorem","docAbstract":"<p>T<span>he serpentine windings of rivers, which in certain reaches attain a remarkable symmetry and are then called meanders, must represent one aspect of the tendency for establishment of quasi-equilibrium in natural streams. With the increase in knowledge of the interaction of forces operating in rivers, this tendency toward equilibrium has assumed a greater significance.</span></p>","language":"English","publisher":"AGU Publications","doi":"10.1029/TR034i006p00955","usgsCitation":"Leopold, L.B., 1953, River meanders and vorticity theorem: Eos, Earth and Space Science News, v. 34, no. 6, p. 955-959, https://doi.org/10.1029/TR034i006p00955.","productDescription":"5 p.","startPage":"955","endPage":"959","costCenters":[],"links":[{"id":337183,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"34","issue":"6","noUsgsAuthors":false,"publicationDate":"2014-08-18","publicationStatus":"PW","scienceBaseUri":"58c277fbe4b014cc3a3e7718","contributors":{"authors":[{"text":"Leopold, Luna Bergere","contributorId":93884,"corporation":false,"usgs":true,"family":"Leopold","given":"Luna","email":"","middleInitial":"Bergere","affiliations":[],"preferred":false,"id":681605,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70178712,"text":"70178712 - 1952 - Status of development of selected ground-water basins in Utah","interactions":[],"lastModifiedDate":"2016-12-09T11:28:53","indexId":"70178712","displayToPublicDate":"2016-11-01T00:00:00","publicationYear":"1952","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":"7","title":"Status of development of selected ground-water basins in Utah","docAbstract":"<p>This technical publication consists essentially of abstracts of more detailed reports which have been published. 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,{"id":70160626,"text":"70160626 - 1952 -  An interim report on gill disease","interactions":[],"lastModifiedDate":"2016-01-04T09:20:00","indexId":"70160626","displayToPublicDate":"2015-12-28T00:00:00","publicationYear":"1952","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3196,"text":"Progressive Fish-Culturist","active":true,"publicationSubtype":{"id":10}},"title":" An interim report on gill disease","docAbstract":"<p><span><strong>GILL DISEASE among fish, a disease which is characterized by a proliferation of the gill epithelium, has been attributed to a number of different causes. Generally, there are two recognized types: the eastern or bacterial type, in which long filamentous bacteria can always be demonstrated; and the western type, in which, by definition, bacteria cannot be demonstrated.</strong></span></p>","language":"English","publisher":"Department of Commerce, Bureau of Fisheries","doi":"10.1577/1548-8640(1952)14[10:AIROGD]2.0.CO;2","usgsCitation":"Rucker, R., Johnson, H., and Kaydas, G., 1952,  An interim report on gill disease: Progressive Fish-Culturist, v. 14, no. 1, p. 10-14, https://doi.org/10.1577/1548-8640(1952)14[10:AIROGD]2.0.CO;2.","productDescription":"5 p.","startPage":"10","endPage":"14","numberOfPages":"5","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":654,"text":"Western Fisheries Research Center","active":true,"usgs":true}],"links":[{"id":312873,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"14","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"56825d27e4b0a04ef4925af1","contributors":{"authors":[{"text":"Rucker, R.R.","contributorId":104000,"corporation":false,"usgs":true,"family":"Rucker","given":"R.R.","email":"","affiliations":[],"preferred":false,"id":583372,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Johnson, H.E.","contributorId":56757,"corporation":false,"usgs":true,"family":"Johnson","given":"H.E.","email":"","affiliations":[],"preferred":false,"id":583373,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Kaydas, G.M.","contributorId":150875,"corporation":false,"usgs":false,"family":"Kaydas","given":"G.M.","email":"","affiliations":[],"preferred":false,"id":583374,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70175968,"text":"70175968 - 1952 - Geology and ground-water resources of Lincoln County, Kansas, with a chapter on The chemical quality of ground water, by W.H. Durum","interactions":[],"lastModifiedDate":"2016-08-23T09:02:48","indexId":"70175968","displayToPublicDate":"2015-10-20T00:00:00","publicationYear":"1952","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 Lincoln County, Kansas, with a chapter on The chemical quality of ground water, by W.H. Durum","language":"English","publisher":"University of Kansas","publisherLocation":"Lawrence, KS","usgsCitation":"Berry, D., and Durum, W.H., 1952, Geology and ground-water resources of Lincoln County, Kansas, with a chapter on The chemical quality of ground water, by W.H. Durum: Kansas Geological Survey Bulletin, v. 95, 96 p. .","productDescription":"96 p. ","costCenters":[{"id":353,"text":"Kansas Water Science Center","active":false,"usgs":true}],"links":[{"id":327430,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":327429,"rank":1,"type":{"id":15,"text":"Index Page"},"url":"https://www.kgs.ku.edu/General/geologyBulls.html"}],"volume":"95","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"57bd73dbe4b03fd6b7df2cd9","contributors":{"authors":[{"text":"Berry, D.W.","contributorId":24842,"corporation":false,"usgs":true,"family":"Berry","given":"D.W.","email":"","affiliations":[],"preferred":false,"id":646719,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Durum, W. H.","contributorId":78311,"corporation":false,"usgs":true,"family":"Durum","given":"W.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":646720,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70175967,"text":"70175967 - 1952 - Geology and ground-water resources of the Kansas River Valley between Lawrence and Topeka, Kansas","interactions":[],"lastModifiedDate":"2016-08-23T09:00:14","indexId":"70175967","displayToPublicDate":"2015-08-12T00:00:00","publicationYear":"1952","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 the Kansas River Valley between Lawrence and Topeka, Kansas","language":"English","publisher":"University of Kansas","publisherLocation":"Lawrence, KS","usgsCitation":"Davis, S., and Carlson, W.A., 1952, Geology and ground-water resources of the Kansas River Valley between Lawrence and Topeka, Kansas: Kansas Geological Survey Bulletin, v. 96, no. 5, p. 201-276.","productDescription":"75 p. ","startPage":"201","endPage":"276","costCenters":[{"id":353,"text":"Kansas Water Science Center","active":false,"usgs":true}],"links":[{"id":327424,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":327423,"rank":1,"type":{"id":15,"text":"Index Page"},"url":"https://www.kgs.ku.edu/General/geologyBulls.html"}],"volume":"96","issue":"5","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"57bd73dce4b03fd6b7df2ced","contributors":{"authors":[{"text":"Davis, S.N.","contributorId":51918,"corporation":false,"usgs":true,"family":"Davis","given":"S.N.","email":"","affiliations":[],"preferred":false,"id":646717,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Carlson, W. A.","contributorId":173967,"corporation":false,"usgs":false,"family":"Carlson","given":"W.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":646718,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70159230,"text":"tei138 - 1952 - Geology of the Quartz Creek Pegmatite District, Gunnison County Colorado","interactions":[],"lastModifiedDate":"2015-10-30T10:48:25","indexId":"tei138","displayToPublicDate":"2015-07-06T08:00:00","publicationYear":"1952","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":"138","title":"Geology of the Quartz Creek Pegmatite District, Gunnison County Colorado","docAbstract":"<p>The Quartz Creek pegmatite district includes an area about 29 square miles in the vicinity of Quartz Creek in Gunnison County,. Colo. This area contains 1,803 pegmatites that are intruded into pre-Cambrian rocks.</p>\n<p>The rocks exposed in the district range in age from pre-Cambrian to Recent. The oldest pre-Cambrian rocks are chiefly quartzites interbedded with a few arkoses and conglomerates. These rocks are surrounded by more abundant hornblende gneiss and tonalite. A small body of biotite tonalite was intruded and two thin layers of dacitic pillow lava were extruded into this series. The hornblende gneiss and tonalite have the same composition and differ only in texture. The older material (hornblende gneiss) has a well-marked lineation, whereas the younger (tonalite) is equigranular. Subsequently, a large body of quartz monzonite was intruded along the northern boundary of the mapped area. Later, coarse-grained granite was intruded into the southern part of the area. Dikes of fine-grained granite cut the coarse-grained variety.&nbsp; The last period of intrusive activity in pre-Cambrian time is marked by a large number of pegmatites.</p>\n<p>The pre-Cambrian rocks were tilted and eroded, and the flatlying&nbsp; Jurassic Morrison formation was deposited on the irregular surface. This formation is conformably overlain by the Cretaceous Dakota sandstone. Faulting produced a vertical offset of 410 feet in the Mesozoic sediments along the only large fault in the area. At the end of Mesozoic time there was another period of erosion. Tertiary (?) tuff is exposed in small, scattered areas in the southern part of the district. It overlies both the Dakota sandstone and pre-Cambrian formations. Glacial till occurs along the edges of Quartz Creek and Wood Gulch. Quaternary alluvium fills the valley bottoms.</p>\n<p>&nbsp;Although the composition of the country rock has little effect on the shape of the pegmatites, the foliation imposed on this rock has a localizing effect and in part controls the ultimate shape of pegmatites.&nbsp; &nbsp;Zoned and related internal structures are not well developed in the pegmatites of this region. &nbsp;Many of the pegmatites are homogeneous and those that are zoned usually contain a large wall zone and small discontinuous cores. In addition to the more common homogeneous and zoned pegmatites, 7 percent of the pegmatites show a layered structure of textural and mineralogical units not repeated on the opposite side of the pegmatite. Other internal structural units include pegmatites which vary in composition along strike, multiple or &ldquo;line-rock pegmatites&rdquo; and fracture fillings.</p>\n<p>The mineralogy of the pegmatites is described in detail. &nbsp;Specific attention was given to most of the 27 observed minerals. A study of the index of refraction of 439 specimens of plagioclase showed that the variation from zone to zone and layer to layer is minor and that there is no systematic variation in respect to the entire district. No correlation could be found between the refractive index of plagioclase in the pegmatites and the type country rock, or the presence of various accessory minerals.</p>\n<p>Index of refraction determinations on 95 specimens of muscovite showed no constant variation from wall zone to core or from layer to layer. &nbsp;Curved muscovite has identical optical properties with the flat variety. The index of refraction was determined for 189 beryl specimens. The beryl in the pegmatites containing only a wall zone and a core showed no difference between zones, but in pegmatites that have intermediate zones, the indices of refraction of the beryl showed an inward increase in the alkali content from the contact. Beryl occurs with almost all of the pegmatite minerals and is not restricted in its mineral associations.</p>\n<p>Tourmaline, except the black variety, is associated with lepidolite. Dark green and blue tourmaline is found in the outer zones of pegmatites containing lepidolite, and the pink and light green varieties are found in direct contact with lepidolite.</p>\n<p>Lepidolite occurs in aggregates of fine grains, in flat plates, and in curved plates; the three varieties are optically identical. The lighter-colored varieties have higher indices of refraction and contain less lithia than the darker varieties.</p>\n<p>In addition, the occurrence of the following minerals is described in detail: perthite, quartz, martite, biotite, garnet, columbite-tantalite, monazite, microlite, topaz, gahnite, allanite, and an unidentified mineral.</p>\n<p>The lack of alteration in the wall rocks adjacent to the pegmatites is interpreted as indicating that the original pegmatite&nbsp; magma did not have an excess of materials such as B, OH-, and P that are needed to form alteration minerals. Because of their low concentration, the above materials were available only in the pegmatitic magma during its crystallization. Pegmatites that contain the rare minerals such as beryl, tourmaline, curved muscovite, biotite, magnetite, monazite, columbite-tantalite, cleavelandite, topaz, lepidolite, and microlite show a grouping in clusters within the district.</p>\n<p>Beryl-bearing pegmatites occur most abundantly in hornblende gneiss and are only rarely found in either granite or quartz monzonite. The types of minerals that form in a pegmatite appear to be determined by the character of the material segregated from the original magma and the period in which it segregated. The elements escape at one period and may be from only-a specific pocket in the magma. These liquids tend to form groups of pegmatites in which the later bodies contain a high proportion of volatiles.</p>\n<p>&nbsp;</p>\n<p>&nbsp;</p>\n<p>Inferred reserves of the district are estimated for beryl, scrap mica, both hand-cobbing and milling feldspar, lepidolite, columbite-tantalite, topaz, monazite, and microlite. No sheet mica was found. Reserves are small and transportation costs are high so substantial production of low-priced feldspar and scrap mica will depend on the adoption of economica milling techniques for recovering the large quantities of feldspar available.&nbsp; Beryl is irregularly distributed and its recovery as a byproduct will depend on the establishment of a stable market for feldspar and scrap mica.&nbsp; Lepidolite reserves are small low grade.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/tei138","usgsCitation":"Staatz, M.H., and Trites, A., 1952, Geology of the Quartz Creek Pegmatite District, Gunnison County Colorado: U.S. Geological Survey Trace Elements Investigations 138, Report: 288 p.; 11 Plates: 29.61 x 46.75 inches or smaller, https://doi.org/10.3133/tei138.","productDescription":"Report: 288 p.; 11 Plates: 29.61 x 46.75 inches or 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