Radon measurement were made in several small, turbulent mountain streams in the Wasatch Mountains near Salt Lake City and Ogden, Utah, to determine the relationship between the distribution of radon and its geologic environment.
\nIn this area, the distribution of radon in streams can be sued to locate points where relatively large amounts of radon-bearing ground water enter the stream, although other evidence of spring activity may be lacking. These points of influence ground water are marked by abrupt increases (as much as two orders of magnitude within a distance of 50 feet) in the radon content of the stream waters.
\nThe excess radon in the stream water is then rapidly lost to the atmosphere through stream turbulence. The rate of radon dissipation is an exponential function, of different slopes, with respect to distance of streamflow, and depend upon the rate and volume of streamflow, and the gradient and nature of the stream channel.
\nThe higher radon concentration can be generally related to specific stratigraphic horizons in several different drainage area. Thus, lithologic units which act as the primary aquifers can be identifies. In one area, thrust faults were found to control he influx of ground water into the stream.
\nEstimates, based on radon concentration in stream and related spring waters, can also be made of the major increments of addition of ground water to streamflow where conventional methods such as stream gaging are not practical.
\nThe radon in the waters studied was found to be almost completely unsupported by radium in solution.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/tei619","collaboration":"This report concerns work done on behalf of the Division of Research of the U.S. Atomic Energy Commission","usgsCitation":"Rogers, A., 1956, The physical behavior and geologic control of radon in mountain streams: U.S. Geological Survey Trace Elements Investigations 619, 44 p., https://doi.org/10.3133/tei619.","productDescription":"44 p.","numberOfPages":"45","costCenters":[],"links":[{"id":290055,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":290054,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/tei/0619/report.pdf"}],"country":"United States","state":"Utah","city":"Ogden;Salt Lake City","otherGeospatial":"Wasatch Mountains","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -112.151,40.5021 ], [ -112.151,41.3868 ], [ -111.2973,41.3868 ], [ -111.2973,40.5021 ], [ -112.151,40.5021 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53a94c87e4b0f1f8e2fa8681","contributors":{"authors":[{"text":"Rogers, Allen S.","contributorId":66553,"corporation":false,"usgs":true,"family":"Rogers","given":"Allen S.","affiliations":[],"preferred":false,"id":284525,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":40011,"text":"b1033 - 1956 - Geophysical abstracts 160-163 January-December 1955","interactions":[{"subject":{"id":47354,"text":"b1033A - 1955 - Geophysical abstracts 160, January-March 1955","indexId":"b1033A","publicationYear":"1955","noYear":false,"chapter":"A","title":"Geophysical abstracts 160, January-March 1955"},"predicate":"IS_PART_OF","object":{"id":40011,"text":"b1033 - 1956 - Geophysical abstracts 160-163 January-December 1955","indexId":"b1033","publicationYear":"1956","noYear":false,"title":"Geophysical abstracts 160-163 January-December 1955"},"id":1},{"subject":{"id":47355,"text":"b1033B - 1955 - Geophysical abstracts 161, April-June 1955","indexId":"b1033B","publicationYear":"1955","noYear":false,"chapter":"B","title":"Geophysical abstracts 161, April-June 1955"},"predicate":"IS_PART_OF","object":{"id":40011,"text":"b1033 - 1956 - Geophysical abstracts 160-163 January-December 1955","indexId":"b1033","publicationYear":"1956","noYear":false,"title":"Geophysical abstracts 160-163 January-December 1955"},"id":2},{"subject":{"id":47356,"text":"b1033C - 1955 - Geophysical abstracts 162, July-September 1955","indexId":"b1033C","publicationYear":"1955","noYear":false,"chapter":"C","title":"Geophysical abstracts 162, July-September 1955"},"predicate":"IS_PART_OF","object":{"id":40011,"text":"b1033 - 1956 - Geophysical abstracts 160-163 January-December 1955","indexId":"b1033","publicationYear":"1956","noYear":false,"title":"Geophysical abstracts 160-163 January-December 1955"},"id":3},{"subject":{"id":47357,"text":"b1033D - 1956 - Geophysical abstracts 163, October-December 1955","indexId":"b1033D","publicationYear":"1956","noYear":false,"chapter":"D","title":"Geophysical abstracts 163, October-December 1955"},"predicate":"IS_PART_OF","object":{"id":40011,"text":"b1033 - 1956 - Geophysical abstracts 160-163 January-December 1955","indexId":"b1033","publicationYear":"1956","noYear":false,"title":"Geophysical abstracts 160-163 January-December 1955"},"id":4}],"lastModifiedDate":"2014-06-30T10:06:14","indexId":"b1033","displayToPublicDate":"1956-01-01T10:04:00","publicationYear":"1956","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":306,"text":"Bulletin","code":"B","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1033","title":"Geophysical abstracts 160-163 January-December 1955","docAbstract":"No abstract available.","language":"English","publisher":"U.S. Government Printing Office","publisherLocation":"Washington D.C.","doi":"10.3133/b1033","usgsCitation":"U.S. Government Printing Office, 1956, Geophysical abstracts 160-163 January-December 1955: U.S. Geological Survey Bulletin 1033, iii, 340 p., https://doi.org/10.3133/b1033.","productDescription":"iii, 340 p.","costCenters":[],"links":[{"id":289179,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53b286efe4b07b8813a554b3"} ,{"id":70098413,"text":"tei432 - 1956 - Geology and ore deposits of the Chicago Creek area, Clear Creek County, Colorado","interactions":[],"lastModifiedDate":"2014-06-11T14:37:34","indexId":"tei432","displayToPublicDate":"1956-01-01T09:56:00","publicationYear":"1956","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":"432","title":"Geology and ore deposits of the Chicago Creek area, Clear Creek County, Colorado","docAbstract":"The Chicago Creek area, Clear Creek County, Colo., forms part of the Front Range mineral belt, which is a northeast-trending belt of coextensive porphyry intrusive rocks and hydrothermal veins of Tertiary age. More than $4.5 million worth of gold, silver, copper, lead, zinc, and uranium was produced from the mines in the area between 1859 and 1954. This investigation was made by the Geological survey on behalf of the Division of Raw Materials of the U.S. Atomic Energy Commission.
\n
\n
The bedrock in the area is Precambrian and consists of igneous rocks, some of which have been metamorphosed , and metasedimentary rocks. The metasedimentary rocks include biotite-quartz-plagioclase gneiss that is locally garnetiferous, sillimanitic biotite-quartz gneiss, amphibolite, and lime-silicate gneiss. Rocks that may be metasedimentary or meta-igneous are quartz monzonite gneiss and granite gneiss and pegmatite. The granite gneiss and pegmatite locally form a migmatite with the biotitic metasedimentary rocks. These older rocks have been intruded by granodiorite, quartz, and granite pegmatite. During Tertiary time the Precambrian rocks were invaded by dikes and plugs of quartz monzonite porphyry, alaskite porphyry, granite porphyry, monzonite porphyry, bostonite and garnetiferous bostonite porphyry, quartz bostonite porphyry, trachytic granite porphyry, and biotite-quartz latite-porphyry.
\nSolifluction debris of Wisconsin age forms sheets filling some of the high basins, covering some of the steep slopes, and filling parts of some of the valleys; talus and talus slides of Wisconsin age rest of or are mixed with solifluction debris in some of the high basins. Recent and/or Pleistocene alluvium is present along valley flats of the larger streams and gulches.
\nTwo periods of Precambrian folding can be recognized in the area. The older folding crumpled the metasedimentary rocks into a series of upright and overturned north-northeast plunging anticlines and synclines. Quartz monzonite gneiss, granite gneiss and pegmatite, granodiorite, and quartz diorite and associated hornblendite are metamorphosed during this period. The second period of folding appears to have been the reflection at depth of faulting nearer the surface; it resulted in crushing as well as some folding of the already folded rocks into terrace and monoclinal folds that plunge gently east-northeast. The biotite-muscovite granite, which is the youngest major Precambrian rock unit, is both concordant (phacolithic) and crosscutting along the older fold system and has been fractured by the younger fold system.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/tei432","collaboration":"This report concerns work done on behalf of the Division of Raw Materials of the U.S. Atomic Energy Commission","usgsCitation":"Harrison, J.E., and Wells, J.D., 1956, Geology and ore deposits of the Chicago Creek area, Clear Creek County, Colorado: U.S. Geological Survey Trace Elements Investigations 432, 6 p., https://doi.org/10.3133/tei432.","productDescription":"6 p.","numberOfPages":"7","costCenters":[],"links":[{"id":285841,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/tei/0432/report.pdf"},{"id":284139,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/tei432.jpg"}],"country":"United States","state":"Colorado","county":"Clear Creek County","otherGeospatial":"Chicago Creek","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -105.927057,39.564453 ], [ -105.927057,39.852061 ], [ -105.394554,39.852061 ], [ -105.394554,39.564453 ], [ -105.927057,39.564453 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5355946ee4b0120853e8bfd1","contributors":{"authors":[{"text":"Harrison, J. E.","contributorId":54532,"corporation":false,"usgs":true,"family":"Harrison","given":"J.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":491693,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Wells, J. D.","contributorId":58647,"corporation":false,"usgs":true,"family":"Wells","given":"J.","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":491694,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":71461,"text":"tei427 - 1956 - Preliminary study of radioactive limonite localities in Colorado, Utah, and Wyoming","interactions":[],"lastModifiedDate":"2014-06-11T14:18:06","indexId":"tei427","displayToPublicDate":"1956-01-01T09:40:00","publicationYear":"1956","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":"427","title":"Preliminary study of radioactive limonite localities in Colorado, Utah, and Wyoming","docAbstract":"Nine radioactive limonite localities of different types were sampled during the spring and fall of 1953 in an effort to establish criteria for differentiating limonite outcrops associated with uranium or thorium deposits from limonite outcrops not associated with such deposits. The samples were analyzed for uranium and thorium by standard chemical methods, for equivalent uranium by the radiometric method, and for a number of common metals by semiquantitative geochemical methods. Correlation coefficients were then calculated for each of the metals with respect to equivalent uranium, and to uranium where present, for all of the samples from each locality. The correlation coefficients may indicate a significant association between uranium or thorium and certain metals. Occurrences of specific that are interpreted as significant very considerably for different uranium localities but are more consistent for the thorium localities.
\n
\n
Samples taken from radioactive outcrops in the vicinity of uranium or thorium deposits can be quickly analyzed by geochemical methods for various elements. Correlation coefficients can then be determined for the various elements with respect to uranium or thorium; if any significant correlations are obtained, the elements showing such correlation may be indicators of uranium or thorium. Soil samples of covered areas in the vicinity of the radioactive outcrop may then be analyzed for the indicator elements and any resulting anomalies used as a guide for prospecting where the depth of overburden is too great to allow the use of radiation-detecting instruments.
\nCorrelation coefficients of the associated indicator elements, used in conjunction with petrographic evidence, may also be useful in interpreting the origin and paragenesis of radioactive deposits.
\nChanges in color of limonite stains on the outcrop may also be a useful guide to ore in some areas.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/tei427","collaboration":"This report concerns work done on behalf of the Division of Raw Materials of the U.S. Atomic Energy Commission","usgsCitation":"Lovering, T., and Beroni, E., 1956, Preliminary study of radioactive limonite localities in Colorado, Utah, and Wyoming: U.S. Geological Survey Trace Elements Investigations 427, 61 p., https://doi.org/10.3133/tei427.","productDescription":"61 p.","numberOfPages":"62","costCenters":[],"links":[{"id":285831,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/tei/0427/report.pdf"},{"id":284136,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/tei427.PNG"}],"country":"United States","state":"Colorado;Utah;Wyoming","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -110.0,38.0 ], [ -110.0,43.0 ], [ -104.0,43.0 ], [ -104.0,38.0 ], [ -110.0,38.0 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5355952be4b0120853e8c15b","contributors":{"authors":[{"text":"Lovering, T.G.","contributorId":55014,"corporation":false,"usgs":true,"family":"Lovering","given":"T.G.","affiliations":[],"preferred":false,"id":284221,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Beroni, E.P.","contributorId":13222,"corporation":false,"usgs":true,"family":"Beroni","given":"E.P.","affiliations":[],"preferred":false,"id":284220,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":37793,"text":"37793 - 1956 - List of Fish and Wildlife Service informational leaflets on wildlife","interactions":[],"lastModifiedDate":"2014-07-24T08:52:30","indexId":"37793","displayToPublicDate":"1956-01-01T08:52:16","publicationYear":"1956","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":1,"text":"Federal Government Series"},"seriesTitle":{"id":98,"text":"Wildlife Leaflet","active":false,"publicationSubtype":{"id":1}},"seriesNumber":"378","title":"List of Fish and Wildlife Service informational leaflets on wildlife","docAbstract":"No abstract available.","language":"English","usgsCitation":"Bullard, C.O., 1956, List of Fish and Wildlife Service informational leaflets on wildlife (Supersedes Wildlife Leaflet 369 (1955).): Wildlife Leaflet 378, 2 p.","productDescription":"2 p.","numberOfPages":"2","costCenters":[],"links":[{"id":290849,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"edition":"Supersedes Wildlife Leaflet 369 (1955).","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"57ffd4a2e4b0824b2d17735b","contributors":{"authors":[{"text":"Bullard, Clifford O.","contributorId":107619,"corporation":false,"usgs":true,"family":"Bullard","given":"Clifford","email":"","middleInitial":"O.","affiliations":[],"preferred":false,"id":218564,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":2618,"text":"wsp1360B - 1956 - Ground water in northeastern Louisville, Kentucky with reference to induced infiltration","interactions":[],"lastModifiedDate":"2024-11-27T15:31:54.450981","indexId":"wsp1360B","displayToPublicDate":"1956-01-01T07:00:00","publicationYear":"1956","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":"1360","chapter":"B","title":"Ground water in northeastern Louisville, Kentucky with reference to induced infiltration","docAbstract":"In cooperation with the city of Louisville, Ky., the U. S. Geological Survey made a detailed investigation during the period February 1945 to March 1947 of the ground-water resources of a 3-square-mile area along the Ohio River north-east of Louisville. Test drilling shows that the principal aquifer consists of about 80 feet of glacial-outwash sands and gravels lying in an old river channel which was cut into rocks of Ordovician, Silurian, and Devonian age.
The total ground-water storage in the area is estimated as 7 billion gallons. The ground-water levels are affected by changes in river elevation, by rainfall, and by the effects of pumping in the downtown part of Louisville 3 miles to the southwest. In the northeastern part of the area the flow of ground water, as defined by contour maps, is toward the river, and in the southwestern part of the area it is from the river toward the downtown area of overpumping.
Ground water in the area has an average temperature of 56° F. The water, which is moderately hard, is suitable for domestic and industrial uses.
Analysis of a pumping test made during the investigation proves that infiltration supplies can be developed. Studies to determine the degree of connection between the river and aquifer were made on the basis of chemical analyses, sections showing temperature distribution in the aquifer during the pumping test, shapes of water-level profiles in the test area, and shapes of time-drawdown curves for a number of observation wells. Quantitative studies to evaluate the hydrologic constants of the aquifer were made by both graphical and mathematical methods. The transmissibility was determined as 121,000 gpd/ft in the test area; the distance to the line source, 400 feet; and the coefficient of storage, 0.0003. A comparison of river-level fluctuations and water-level fluctuations in observation wells shows that conditions along the 6.4-mile reach of river are not greatly different from those at the site of the pumping test.
It is estimated that under adverse temperature and river-stage conditions infiltration supplies could be developed to the extent of 280 million gpd in the entire 6.4-mile reach investigated; at average river-water temperature (59° F) about 400 million gpd could be developed. Diagrams were drawn showing the estimated yield of wells of different radii, at various distances from the river, and at various spacings. In making the computations allowance was made for screen losses, dewatering of the aquifer, partial penetration of wells, location wells, eccentricity of large wells, and interference among wells.
","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Washington, D.C.","doi":"10.3133/wsp1360B","collaboration":"Prepared in cooperation with the city of Louisville","usgsCitation":"Rorabaugh, M.I., 1956, Ground water in northeastern Louisville, Kentucky with reference to induced infiltration: U.S. Geological Survey Water Supply Paper 1360, Report: v, 69 p.; 17 Plates: 8 x 23.81 inches or smaller, https://doi.org/10.3133/wsp1360B.","productDescription":"Report: v, 69 p.; 17 Plates: 8 x 23.81 inches or smaller","startPage":"101","endPage":"169","numberOfPages":"73","costCenters":[],"links":[{"id":416093,"rank":20,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_24337.htm","linkFileType":{"id":5,"text":"html"}},{"id":28927,"rank":19,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1360b/plate-17.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":28926,"rank":18,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1360b/plate-16.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":28925,"rank":17,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1360b/plate-15.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":28924,"rank":16,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1360b/plate-14.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":28923,"rank":15,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1360b/plate-13.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":138850,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1360b/report-thumb.jpg"},{"id":28917,"rank":9,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1360b/plate-07.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":28916,"rank":8,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1360b/plate-06.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":28914,"rank":6,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1360b/plate-04.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":28911,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1360b/plate-18.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":28920,"rank":12,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1360b/plate-10.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":279835,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1360b/report.pdf"},{"id":28912,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1360b/plate-02.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":28913,"rank":5,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1360b/plate-03.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":28915,"rank":7,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1360b/plate-05.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":28918,"rank":10,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1360b/plate-08.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":28919,"rank":11,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1360b/plate-09.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":28921,"rank":13,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1360b/plate-11.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":28922,"rank":14,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1360b/plate-12.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Kentucky","city":"Louisville","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -85.948441,37.9971 ], [ -85.948441,38.38051 ], [ -85.4051,38.38051 ], [ -85.4051,37.9971 ], [ -85.948441,37.9971 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ab0e4b07f02db66db38","contributors":{"authors":[{"text":"Rorabaugh, M. I.","contributorId":28221,"corporation":false,"usgs":true,"family":"Rorabaugh","given":"M.","email":"","middleInitial":"I.","affiliations":[],"preferred":false,"id":145505,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70185489,"text":"70185489 - 1956 - Land use and sediment yield","interactions":[],"lastModifiedDate":"2017-03-22T14:22:18","indexId":"70185489","displayToPublicDate":"1956-01-01T00:00:00","publicationYear":"1956","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"Land use and sediment yield","docAbstract":"When the vegetal cover is removed from a land surface, the rate of removal of the soil material, at least initially, increases rapidly. So well known is this principle that it hardly needs restatement.
If attention is focused on any individual drainage basin in its natural state, large or small, and inquiry is made as to the rate of denudation, a quantitative answer is not easily obtained. The possible error in any computation of rate of sediment production from any given drainage basin is considerable. Significant variations are found in sediment yields from closely adjacent watersheds which appear to be generally similar. To make a quantitative evaluation of the change in the rate of denudation when the natural vegetation is disturbed is, therefore, even more difficult. Considering the fact that \"soil conservation\" has been promoted to the status of a science, our lack of ability to answer what is apparently so simple a question may seem surprising. Let us look at some of the reasons.
","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Man’s role in changing the face of the Earth","largerWorkSubtype":{"id":12,"text":"Conference publication"},"conferenceTitle":"Man's role in changing the face of the Earth: Second annual Wenner-Gren Symposium","conferenceDate":"June 16-22, 1955","conferenceLocation":"Princeton, NJ","language":"English","publisher":"University of Chicago Press","publisherLocation":"Chicago, IL","usgsCitation":"Leopold, L.B., 1956, Land use and sediment yield, in Man’s role in changing the face of the Earth, Princeton, NJ, June 16-22, 1955, p. 639-647.","productDescription":"9 p.","startPage":"639","endPage":"647","costCenters":[],"links":[{"id":338086,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"58d38d66e4b0236b68f98f98","contributors":{"editors":[{"text":"Thomas, William L. Jr.","contributorId":189691,"corporation":false,"usgs":false,"family":"Thomas","given":"William","suffix":"Jr.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":685718,"contributorType":{"id":2,"text":"Editors"},"rank":1}],"authors":[{"text":"Leopold, Luna Bergere","contributorId":93884,"corporation":false,"usgs":true,"family":"Leopold","given":"Luna","email":"","middleInitial":"Bergere","affiliations":[],"preferred":false,"id":685717,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70185477,"text":"70185477 - 1956 - Floods in relation to the river channel","interactions":[],"lastModifiedDate":"2017-03-22T13:39:11","indexId":"70185477","displayToPublicDate":"1956-01-01T00:00:00","publicationYear":"1956","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":5272,"text":"Proceedings of the International Association of Hydrological Sciences","active":true,"publicationSubtype":{"id":10}},"title":"Floods in relation to the river channel","docAbstract":"Among the rivers studied by us two broad types may be distinguished. Channels in the semi-arid areas scour at high discharges so that the bed lowers nearly as much as the water surface rises. Detailed data on the middle reaches of the Rio Grande in New Mexico during the spring floods of 1948 and 1952 indicate that the bed aggrades to nearly its pre-flood level as the flood recedes. Channel banks may move rapidly by undercutting during periods of scour and levees are liable to failure not from overtopping but by undercutting.
In Connecticut, a sub-humid area, the repetitive processes of scour and fill in the semi-arid region were not demonstrated by the great floods of 1955. In a few reaches fresh sand was deposited over gravel beds subsequently to be removed by lower flows. Boulders four to six feet in diameter were moved in places over undisturbed beds of one-inch gravel. Channel widening occurred primarily in rivers in narrow valleys which confined the flow within the channel. Scour and deposition on flood plains adjacent to the rivers was irregular. Most deposits could be traced to local sources. In general, flood waters modified but did not vastly alter the prevailing configuration of the channel and structure of the flood plain.
","conferenceTitle":"Symposium Darcy: Floods","conferenceDate":"September 20-26, 1956","conferenceLocation":"Dijon, France","language":"English","publisher":"International Association of Hydrological Sciences","usgsCitation":"Leopold, L.B., and Wolman, M.G., 1956, Floods in relation to the river channel: Proceedings of the International Association of Hydrological Sciences, p. 85-98.","productDescription":"14 p.","startPage":"85","endPage":"98","costCenters":[],"links":[{"id":338073,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":338071,"rank":1,"type":{"id":15,"text":"Index Page"},"url":"https://iahs.info/Publications-News/","text":"Publisher's Website","linkHelpText":"Back issues of this publication are available using the search function"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"58d38d66e4b0236b68f98f9c","contributors":{"authors":[{"text":"Leopold, Luna Bergere","contributorId":93884,"corporation":false,"usgs":true,"family":"Leopold","given":"Luna","email":"","middleInitial":"Bergere","affiliations":[],"preferred":false,"id":685683,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Wolman, M. Gordon","contributorId":85163,"corporation":false,"usgs":true,"family":"Wolman","given":"M.","email":"","middleInitial":"Gordon","affiliations":[],"preferred":false,"id":685684,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":1000373,"text":"1000373 - 1956 - Research vessel Cisco operations in 1955","interactions":[],"lastModifiedDate":"2012-02-02T00:04:13","indexId":"1000373","displayToPublicDate":"1956-01-01T00:00:00","publicationYear":"1956","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1278,"text":"Commercial Fishing Review","active":true,"publicationSubtype":{"id":10}},"title":"Research vessel Cisco operations in 1955","docAbstract":"Abstract has not been submitted","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Commercial Fishing Review","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","collaboration":"Out-of-print","usgsCitation":"Smith, S.H., 1956, Research vessel Cisco operations in 1955: Commercial Fishing Review, v. 18, no. 5, p. 21-23.","productDescription":"p. 21-23","startPage":"21","endPage":"23","numberOfPages":"2","costCenters":[{"id":324,"text":"Great Lakes Science Center","active":true,"usgs":true}],"links":[{"id":129205,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"18","issue":"5","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad9e4b07f02db684eff","contributors":{"authors":[{"text":"Smith, Stanford H.","contributorId":86711,"corporation":false,"usgs":true,"family":"Smith","given":"Stanford","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":308477,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":53563,"text":"53563 - 1956 - Biology of the sea lamprey in its parasitic phase","interactions":[],"lastModifiedDate":"2013-02-11T14:44:56","indexId":"53563","displayToPublicDate":"1956-01-01T00:00:00","publicationYear":"1956","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":1,"text":"Federal Government Series"},"seriesTitle":{"id":74,"text":"Research Report","active":false,"publicationSubtype":{"id":1}},"seriesNumber":"44","title":"Biology of the sea lamprey in its parasitic phase","docAbstract":"The investigations conducted on sea lampreys in aquariums were concerned with the duration of the parasitic phase of life, feeding, growth, and the interrelations between predator and host fish. Observations on lampreys reared from metamorphosis to maturity were made at the Fish and Wildlife Service Laboratory at Hammond Bay, Michigan. Most of the experimental lampreys were mature and ripe after 14 to 18 months of parasitic life. They exhibited signs of irreversible physical degeneration which precedes death. Three specimens were immature after 14, 18, and 26 months in aquariums, thus indicating that under certain conditions, lampreys may extend their parasitic phase. The feeding activity, growth, and shrinkage in size of aquarium specimens were considered typical of lampreys in the Great Lakes, although the wild lampreys achieve greater average size. Female lampreys made more attacks, fed more, killed more fish, and grew larger than males. They also shrank proportionately more in length and weight as they approached sexual maturity, but their terminal average size was slightly larger than that of males. It is estimated that the average fish-kill by a wild lamprey exceeds, and could be approximately double, the 18.5 pounds of fish killed by a laboratory lamprey. The rate and extent of fish destruction depended on the size, sex, and stage in the parasitic phase of the lampreys, and on the species and size of the fish. There was an increase in the number of fish killed as the lampreys grew, and the fish were killed more quickly. Attacks made by experimental lampreys at any stage of their parasitic phase up to full maturity, and on any part of a prey fish except fins, usually resulted in death to the host. Some fish which survived lamprey attacks succumbed to fungus infections of the wounds. A small number of trout recovered from attacks, and their wounds healed.","language":"English","publisher":"U.S. Fish and Wildlife Service","collaboration":"Fishery Bulletin of the U. S. Fish and Wildlife Service, v. 57, Out-of-print","usgsCitation":"Parker, P.S., and Lennon, R.E., 1956, Biology of the sea lamprey in its parasitic phase: Research Report 44, 32 p.","productDescription":"32 p.","startPage":"0","endPage":"32","numberOfPages":"32","costCenters":[{"id":324,"text":"Great Lakes Science Center","active":true,"usgs":true}],"links":[{"id":178232,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":267222,"type":{"id":11,"text":"Document"},"url":"https://hdl.handle.net/2027/mdp.39015086578658"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a48e4b07f02db62311f","contributors":{"authors":[{"text":"Parker, Phillip S.","contributorId":74450,"corporation":false,"usgs":true,"family":"Parker","given":"Phillip","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":247813,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Lennon, Robert E.","contributorId":14341,"corporation":false,"usgs":true,"family":"Lennon","given":"Robert","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":247812,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70010479,"text":"70010479 - 1956 - Multiple-unit fusion rack","interactions":[],"lastModifiedDate":"2023-03-20T16:55:05.147334","indexId":"70010479","displayToPublicDate":"1956-01-01T00:00:00","publicationYear":"1956","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":"Multiple-unit fusion rack","docAbstract":"No abstract available.
","language":"English","publisher":"ACS Publications","doi":"10.1021/ac60110a048","usgsCitation":"Marranzino, A., and Wood, W.H., 1956, Multiple-unit fusion rack: Analytical Chemistry, v. 28, no. 2, p. 273-274, https://doi.org/10.1021/ac60110a048.","productDescription":"2 p.","startPage":"273","endPage":"274","numberOfPages":"2","costCenters":[],"links":[{"id":219148,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"28","issue":"2","noUsgsAuthors":false,"publicationDate":"2002-05-01","publicationStatus":"PW","scienceBaseUri":"505a608fe4b0c8380cd71541","contributors":{"authors":[{"text":"Marranzino, A. P.","contributorId":61798,"corporation":false,"usgs":true,"family":"Marranzino","given":"A. P.","affiliations":[],"preferred":false,"id":359017,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Wood, W. H.","contributorId":77294,"corporation":false,"usgs":true,"family":"Wood","given":"W.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":359018,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70010563,"text":"70010563 - 1956 - Aromatic fluorine compounds. VII. Replacement of aromatic -Cl and -NO2 groups by -F","interactions":[],"lastModifiedDate":"2025-01-28T16:15:44.192574","indexId":"70010563","displayToPublicDate":"1956-01-01T00:00:00","publicationYear":"1956","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2519,"text":"Journal of the American Chemical Society","active":true,"publicationSubtype":{"id":10}},"title":"Aromatic fluorine compounds. VII. Replacement of aromatic -Cl and -NO2 groups by -F","docAbstract":"Replacement of -Cl by -F in aryl chlorides with potassium fluoride has been extended from 2,4-dinitrochlorobenzene to less activated halides by the use of non-aqueous solvents, especially dimethylformamide (DMF) and dimethyl sulfoxide (DMSO). Also replacement of -NO2 by -F in substituted nitrobenzenes was studied in DMF. As a direct result of this study, many aromatic fluorine compounds can now be obtained by a relatively simple synthetic route.","language":"English","publisher":"American Chemical Society","doi":"10.1021/ja01604a022","issn":"00027863","usgsCitation":"Finger, G.C., and Kruse, C., 1956, Aromatic fluorine compounds. VII. Replacement of aromatic -Cl and -NO2 groups by -F: Journal of the American Chemical Society, v. 78, no. 23, p. 6034-6037, https://doi.org/10.1021/ja01604a022.","productDescription":"4 p.","startPage":"6034","endPage":"6037","numberOfPages":"4","costCenters":[],"links":[{"id":219083,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"78","issue":"23","noUsgsAuthors":false,"publicationDate":"2002-05-01","publicationStatus":"PW","scienceBaseUri":"5059ed81e4b0c8380cd4984b","contributors":{"authors":[{"text":"Finger, G. C.","contributorId":89277,"corporation":false,"usgs":true,"family":"Finger","given":"G.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":359177,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Kruse, C.W.","contributorId":52333,"corporation":false,"usgs":true,"family":"Kruse","given":"C.W.","email":"","affiliations":[],"preferred":false,"id":359176,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70010584,"text":"70010584 - 1956 - Spectrophotometric study of the thorium-morin mixed-color system","interactions":[],"lastModifiedDate":"2020-11-27T22:28:04.522118","indexId":"70010584","displayToPublicDate":"1956-01-01T00:00:00","publicationYear":"1956","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":761,"text":"Analytical Chemistry","active":true,"publicationSubtype":{"id":10}},"title":"Spectrophotometric study of the thorium-morin mixed-color system","docAbstract":"A spectrophotometric study was made of the thoriummorin reaction to evaluate the suitability of morin as a reagent for the determination of trace amounts of thorium. At pH 2, the equilibrium constant for the reaction is 1 x 106, and a single complex having a thorium-morin ratio of 1 to 2 is formed. The complex shows maximum absorbance at a wave length of 410 mμ, and its absorbance obeys Beer's law. The absorbance readings are highly reproducible, and the sensitivity is relatively high, an absorbance difference of 0.001 being equivalent to 0.007 γ of ThO2 per sq. cm. The effects of acid, alcohol, and morin concentration, time, temperature, and age of the morin reagent as well as the behavior of morin with zirconium(IV), iron(III), aluminum(III), ytterbium(III), yttrium(III), uranium(VI), praseodymium(III), lead(II), lanthanum(III), and calcium(II) ions are discussed. A method is presented for the determination of thorium in pure solutions. Appropriate separations for the isolation of thorium may extend the usefulness of the method and permit the determination of trace amounts of thorium in complex materials.
","language":"English","publisher":"ACS Publications","doi":"10.1021/ac60117a014","usgsCitation":"Fletcher, M.H., and Milkey, R., 1956, Spectrophotometric study of the thorium-morin mixed-color system: Analytical Chemistry, v. 28, no. 9, p. 1402-1407, https://doi.org/10.1021/ac60117a014.","productDescription":"6 p.","startPage":"1402","endPage":"1407","numberOfPages":"6","costCenters":[],"links":[{"id":480419,"rank":1,"type":{"id":41,"text":"Open Access External Repository Page"},"url":"https://digital.library.unt.edu/ark:/67531/metadc1050200/","text":"External Repository"},{"id":219090,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"28","issue":"9","noUsgsAuthors":false,"publicationDate":"2002-05-01","publicationStatus":"PW","scienceBaseUri":"505b95ade4b08c986b31b059","contributors":{"authors":[{"text":"Fletcher, M. H.","contributorId":53438,"corporation":false,"usgs":true,"family":"Fletcher","given":"M.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":359216,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Milkey, R.G.","contributorId":89125,"corporation":false,"usgs":true,"family":"Milkey","given":"R.G.","affiliations":[],"preferred":false,"id":359217,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70010583,"text":"70010583 - 1956 - Thoron-tartaric acid systems for spectrophotometric determination of thorium","interactions":[],"lastModifiedDate":"2023-03-20T16:56:54.126962","indexId":"70010583","displayToPublicDate":"1956-01-01T00:00:00","publicationYear":"1956","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":"Thoron-tartaric acid systems for spectrophotometric determination of thorium","docAbstract":"Thoron is commonly used for the spectrophotometric determination of thorium. An undesirable feature of its use is its high sensitivity to zirconium. This study describes the use of tartaric acid as a masking reagent for zirconium. Three tartaric acid-thoron systems, developed for the determination of thorium, differ with respect to the concentrations of thoron and tartaric acid. Mesotartaric acid, used in one of the systems, is most effective in masking zirconium. The behavior of rarer elements, usually associated with thorium ores, is determined in two systems, and a dilution method is described for the direct determination of thorium in monazite concentrates.","language":"English","publisher":"ACS Publications","doi":"10.1021/ac60113a011","usgsCitation":"Grimaldi, F.S., and Fletcher, M., 1956, Thoron-tartaric acid systems for spectrophotometric determination of thorium: Analytical Chemistry, v. 28, no. 5, p. 812-816, https://doi.org/10.1021/ac60113a011.","productDescription":"5 p.","startPage":"812","endPage":"816","numberOfPages":"5","costCenters":[],"links":[{"id":480420,"rank":2,"type":{"id":41,"text":"Open Access External Repository Page"},"url":"https://digital.library.unt.edu/ark:/67531/metadc1050370/","text":"External Repository"},{"id":219089,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"28","issue":"5","noUsgsAuthors":false,"publicationDate":"2002-05-01","publicationStatus":"PW","scienceBaseUri":"505bb2ebe4b08c986b325aa0","contributors":{"authors":[{"text":"Grimaldi, F. S.","contributorId":94286,"corporation":false,"usgs":true,"family":"Grimaldi","given":"F.","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":359215,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Fletcher, Mary H.","contributorId":52954,"corporation":false,"usgs":true,"family":"Fletcher","given":"Mary H.","affiliations":[],"preferred":false,"id":359214,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70010818,"text":"70010818 - 1956 - Aromatic fluorine compounds. VI. Displacement of aryl fluorine in diazonium salts","interactions":[],"lastModifiedDate":"2025-01-28T16:16:52.333872","indexId":"70010818","displayToPublicDate":"1956-01-01T00:00:00","publicationYear":"1956","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2519,"text":"Journal of the American Chemical Society","active":true,"publicationSubtype":{"id":10}},"title":"Aromatic fluorine compounds. VI. Displacement of aryl fluorine in diazonium salts","docAbstract":"Several chlorofluorobenzenes have been isolated from the Schiemann synthesis of fluorobenzenes. These have been shown to be the products of two side reactions occurring during thermal decomposition of the dry benzenediazonium fluoborate salt containing coprecipitated sodium chloride, an unavoidable contaminant in large preparations involving the use of hydrochloric acid and sodium fluoborate. The major side reaction and its chloro product were unexpected; a unique displacement of fluorine ortho to the diazonium group was observed. Replacement of the diazo group with chlorine was the predicted side reaction which proved to be minor. Conditions causing the side reactions and the isolation and identification of the products are described.","language":"English","publisher":"American Chemical Society","doi":"10.1021/ja01592a073","issn":"00027863","usgsCitation":"Finger, G.C., and Oesterling, R., 1956, Aromatic fluorine compounds. VI. Displacement of aryl fluorine in diazonium salts: Journal of the American Chemical Society, v. 78, no. 11, p. 2593-2596, https://doi.org/10.1021/ja01592a073.","productDescription":"4 p.","startPage":"2593","endPage":"2596","numberOfPages":"4","costCenters":[],"links":[{"id":218745,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"78","issue":"11","noUsgsAuthors":false,"publicationDate":"2002-05-01","publicationStatus":"PW","scienceBaseUri":"5059ed80e4b0c8380cd49848","contributors":{"authors":[{"text":"Finger, G. C.","contributorId":89277,"corporation":false,"usgs":true,"family":"Finger","given":"G.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":359719,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Oesterling, R.E.","contributorId":25282,"corporation":false,"usgs":true,"family":"Oesterling","given":"R.E.","affiliations":[],"preferred":false,"id":359718,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70010587,"text":"70010587 - 1956 - Variation in content of abstracts according to use","interactions":[],"lastModifiedDate":"2025-01-07T16:59:48.480616","indexId":"70010587","displayToPublicDate":"1956-01-01T00:00:00","publicationYear":"1956","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2206,"text":"Journal of Chemical Education","active":true,"publicationSubtype":{"id":10}},"title":"Variation in content of abstracts according to use","docAbstract":"No abstract available.
","language":"English","publisher":"ACS Publications","doi":"10.1021/ed033p27","issn":"00219584","usgsCitation":"Fleischer, M., and Hooker, M., 1956, Variation in content of abstracts according to use: Journal of Chemical Education, v. 33, no. 1, p. 27-32, https://doi.org/10.1021/ed033p27.","productDescription":"6 p.","startPage":"27","endPage":"32","numberOfPages":"6","costCenters":[],"links":[{"id":219150,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"33","issue":"1","noUsgsAuthors":false,"publicationDate":"1956-01-01","publicationStatus":"PW","scienceBaseUri":"505bc155e4b08c986b32a516","contributors":{"authors":[{"text":"Fleischer, M.","contributorId":84069,"corporation":false,"usgs":true,"family":"Fleischer","given":"M.","email":"","affiliations":[],"preferred":false,"id":359222,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hooker, M.","contributorId":47903,"corporation":false,"usgs":true,"family":"Hooker","given":"M.","email":"","affiliations":[],"preferred":false,"id":359221,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":81344,"text":"81344 - 1956 - Sea lamprey control on the Great Lakes 1953 and 1954","interactions":[],"lastModifiedDate":"2023-04-04T15:13:17.730294","indexId":"81344","displayToPublicDate":"1956-01-01T00:00:00","publicationYear":"1956","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":"175","title":"Sea lamprey control on the Great Lakes 1953 and 1954","docAbstract":"No abstract available.
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