{"pageNumber":"5361","pageRowStart":"134000","pageSize":"25","recordCount":184769,"records":[{"id":70011455,"text":"70011455 - 1982 - Mineral identification from orbit: Initial results from the shuttle multispectral infrared radiometer","interactions":[],"lastModifiedDate":"2025-12-11T16:32:07.653191","indexId":"70011455","displayToPublicDate":"1982-12-03T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3338,"text":"Science","active":true,"publicationSubtype":{"id":10}},"title":"Mineral identification from orbit: Initial results from the shuttle multispectral infrared radiometer","docAbstract":"<p>A shuttle-borne radiometer containing ten channels in the reflective infrared has demonstrated that direct identification of carbonates and hydroxyl-bearing minerals is possible by remote measurement from Earth orbit.&nbsp;</p>","language":"English","publisher":"American Association for the Advancement of Science","doi":"10.1126/science.218.4576.1020","issn":"00368075","usgsCitation":"Goetz, A.F., Rowan, L.C., and Kingston, M., 1982, Mineral identification from orbit: Initial results from the shuttle multispectral infrared radiometer: Science, v. 218, no. 4576, p. 1020-1024, https://doi.org/10.1126/science.218.4576.1020.","productDescription":"5 p.","startPage":"1020","endPage":"1024","costCenters":[],"links":[{"id":221529,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"218","issue":"4576","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a578de4b0c8380cd6dd45","contributors":{"authors":[{"text":"Goetz, Alexander F.H.","contributorId":43747,"corporation":false,"usgs":true,"family":"Goetz","given":"Alexander","middleInitial":"F.H.","affiliations":[],"preferred":false,"id":361157,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Rowan, L. C.","contributorId":40584,"corporation":false,"usgs":true,"family":"Rowan","given":"L.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":361156,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Kingston, M.J.","contributorId":88768,"corporation":false,"usgs":true,"family":"Kingston","given":"M.J.","email":"","affiliations":[],"preferred":false,"id":361158,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70011673,"text":"70011673 - 1982 - Uranium in spring water and bryophytes at basin creek in central idaho","interactions":[],"lastModifiedDate":"2025-04-08T16:52:38.282389","indexId":"70011673","displayToPublicDate":"1982-12-03T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2302,"text":"Journal of Geochemical Exploration","active":true,"publicationSubtype":{"id":10}},"title":"Uranium in spring water and bryophytes at basin creek in central idaho","docAbstract":"<p><span>Arkosic sandstones and conglomerates of Tertiary age beneath the Challis Volcanics of Eocene age at Basin Creek, 10 km northeast of Stanley, Idaho, contain uranium-bearing vitrainized carbon fragments. The economic potential of these sandstones and conglomerates is currently being assessed. Springs abound at the contacts of rock units, and water from these springs supports abundant growths of bryophytes (mosses and liverworts). Water from 22 springs and associated bryophytes were sampled; two springs were found to contain apparently anomalous concentrations (normalized) of uranium — as much as 6.5 μg/L (ppb) in water and 1800 μg/g (ppm) in ash of mosses. Moss samples from both springs also contained anomalous concentrations of arsenic, and one contained highly anomalous amounts of beryllium. Water from a third spring contained slightly anomalous amounts of uranium, and two species of mosses at the spring contained anomalous uranium (400 and 700 μg/g) and high levels of both cadmium and lead. Water from a fourth spring was normal for uranium (0.18 μg/L), but the moss from the water contained a moderate uranium level and highly anomalous concentrations of lead, germanium, and thallium.</span></p><p><span>These results suggest that, in the Basin Creek area, moss sampling at springs may give a more reliable indication of uranium occurrence than would water sampling. The reason for this may be the ability of mosses to concentrate uranium and its associated pathfinder elements and to integrate uranium fluctuations that occur in the spring water over any period of time.</span></p>","language":"English","publisher":"Elsevier","doi":"10.1016/0375-6742(82)90004-8","usgsCitation":"Shacklette, H., and Erdman, J.A., 1982, Uranium in spring water and bryophytes at basin creek in central idaho: Journal of Geochemical Exploration, v. 17, no. 3, p. 221-236, https://doi.org/10.1016/0375-6742(82)90004-8.","productDescription":"16 p.","startPage":"221","endPage":"236","costCenters":[],"links":[{"id":220717,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Idaho","otherGeospatial":"central Idaho","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -117.11898816098233,\n              46.88064351215584\n            ],\n            [\n              -117.11898816098233,\n              43.52384377775087\n            ],\n            [\n              -112.3634806336367,\n              43.52384377775087\n            ],\n            [\n              -112.3634806336367,\n              46.88064351215584\n            ],\n            [\n              -117.11898816098233,\n              46.88064351215584\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","volume":"17","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505bbdb8e4b08c986b3291af","contributors":{"authors":[{"text":"Shacklette, H.T.","contributorId":61813,"corporation":false,"usgs":true,"family":"Shacklette","given":"H.T.","affiliations":[],"preferred":false,"id":361679,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Erdman, J. A.","contributorId":59786,"corporation":false,"usgs":true,"family":"Erdman","given":"J.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":361678,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70011668,"text":"70011668 - 1982 - Subsurface valleys and geoarcheology of the eastern Sahara revealed by shuttle radar","interactions":[],"lastModifiedDate":"2025-12-11T16:27:13.378662","indexId":"70011668","displayToPublicDate":"1982-12-03T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3338,"text":"Science","active":true,"publicationSubtype":{"id":10}},"title":"Subsurface valleys and geoarcheology of the eastern Sahara revealed by shuttle radar","docAbstract":"<p><span id=\"_mce_caret\" data-mce-bogus=\"1\" data-mce-type=\"format-caret\"><span>The shuttle imaging radar (SIR-A) carried on the space shuttle Columbia in November 1981 penetrated the extremely dry Selima Sand Sheet, dunes, and drift sand of the eastern Sahara, revealing previously unknown buried valleys, geologic structures, and possible Stone Age occupation sites. Radar responses from bedrock and gravel surfaces beneath windblown sand several centimeters to possibly meters thick delineate sand- and alluvium-filled valleys, some nearly as wide as the Nile Valley and perhaps as old as middle Tertiary. The now-vanished major river systems that carved these large valleys probably accomplished most of the erosional stripping of this extraordinarily flat, hyperarid region. Underfit and incised dry wadis, many superimposed on the large valleys, represent erosion by intermittent running water, probably during Quaternary pluvials. Stone Age artifacts associated with soils in the alluvium suggest that areas near the wadis may have been sites of early human occupation. The presence of old drainage networks beneath the sand sheet provides a geologic explanation for the locations of many playas and present-day oases which have been centers of episodic human habitation. Radar penetration of dry sand and soils varies with the wavelength of the incident signals (24 centimeters for the SIR-A system), incidence angle, and the electrical properties of the materials, which are largely determined by moisture content. The calculated depth of radar penetration of dry sand and granules, based on laboratory measurements of the electrical properties of samples from the Selima Sand Sheet, is at least 5 meters. Recent (September 1982) field studies in Egypt verified SIR-A signal penetration depths of at least 1 meter in the Selima Sand Sheet and in drift sand and 2 or more meters in sand dunes.</span></span></p>","language":"English","publisher":"American Association for the Advancement of Science","doi":"10.1126/science.218.4576.1004","issn":"00368075","usgsCitation":"McCauley, J., Schaber, G.G., Breed, C.S., Grolier, M., Haynes, C., Issawi, B., Elachi, C., and Blom, R., 1982, Subsurface valleys and geoarcheology of the eastern Sahara revealed by shuttle radar: Science, v. 218, no. 4576, p. 1004-1020, https://doi.org/10.1126/science.218.4576.1004.","productDescription":"17 p.","startPage":"1004","endPage":"1020","costCenters":[],"links":[{"id":221767,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"Egypt","otherGeospatial":"eastern Sahara","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              29.420206988982358,\n              26.493678313750593\n            ],\n            [\n              29.420206988982358,\n              23.313364774892932\n            ],\n            [\n              31.687518561025286,\n              23.313364774892932\n            ],\n            [\n              31.687518561025286,\n              26.493678313750593\n            ],\n            [\n              29.420206988982358,\n              26.493678313750593\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","volume":"218","issue":"4576","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505b9d94e4b08c986b31d91f","contributors":{"authors":[{"text":"McCauley, J.F.","contributorId":26310,"corporation":false,"usgs":true,"family":"McCauley","given":"J.F.","email":"","affiliations":[],"preferred":false,"id":361661,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Schaber, G. G.","contributorId":68300,"corporation":false,"usgs":true,"family":"Schaber","given":"G.","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":361666,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Breed, C. S.","contributorId":39809,"corporation":false,"usgs":true,"family":"Breed","given":"C.","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":361662,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Grolier, M. J.","contributorId":46946,"corporation":false,"usgs":true,"family":"Grolier","given":"M. J.","affiliations":[],"preferred":false,"id":361664,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Haynes, C.V.","contributorId":60381,"corporation":false,"usgs":true,"family":"Haynes","given":"C.V.","affiliations":[],"preferred":false,"id":361665,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Issawi, B.","contributorId":45458,"corporation":false,"usgs":true,"family":"Issawi","given":"B.","affiliations":[],"preferred":false,"id":361663,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Elachi, C.","contributorId":104606,"corporation":false,"usgs":false,"family":"Elachi","given":"C.","affiliations":[],"preferred":false,"id":361668,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Blom, R.","contributorId":90470,"corporation":false,"usgs":true,"family":"Blom","given":"R.","email":"","affiliations":[],"preferred":false,"id":361667,"contributorType":{"id":1,"text":"Authors"},"rank":8}]}}
,{"id":70011420,"text":"70011420 - 1982 - Shuttle imaging radar experiment","interactions":[],"lastModifiedDate":"2025-12-11T16:36:45.545052","indexId":"70011420","displayToPublicDate":"1982-12-03T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3338,"text":"Science","active":true,"publicationSubtype":{"id":10}},"title":"Shuttle imaging radar experiment","docAbstract":"<p><span id=\"_mce_caret\" data-mce-bogus=\"1\" data-mce-type=\"format-caret\"><span>The shuttle imaging radar (SIR-A) acquired images of a variety of the earth's geologic areas covering about 10 million square kilometers. Structural and geomorphic features such as faults, folds, outcrops, and dunes are clearly visible in both tropical and arid regions. The combination of SIR-A and Seasat images provides additional information about the surface physical properties: topography and roughness. Ocean features were also observed, including large internal waves in the Andaman Sea.</span></span></p>","language":"English","publisher":"American Association for the Advancement of Science","doi":"10.1126/science.218.4576.996","issn":"00368075","usgsCitation":"Elachi, C., Brown, W., Cimino, J., Dixon, T., Evans, D., Ford, J., Saunders, R., Breed, C., Masursky, H., McCauley, J., Schaber, G., Dellwig, L., England, A., MacDonald, H., Martin-Kaye, P., and Sabins, F., 1982, Shuttle imaging radar experiment: Science, v. 218, no. 4576, p. 996-1003, https://doi.org/10.1126/science.218.4576.996.","productDescription":"8 p.","startPage":"996","endPage":"1003","costCenters":[],"links":[{"id":220977,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"Myanmar, Thailand","otherGeospatial":"Andaman Sea, Indian Ocean","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n    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        ]\n        ]\n      }\n    }\n  ]\n}","volume":"218","issue":"4576","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505b8eebe4b08c986b318c15","contributors":{"authors":[{"text":"Elachi, C.","contributorId":104606,"corporation":false,"usgs":false,"family":"Elachi","given":"C.","affiliations":[],"preferred":false,"id":361056,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Brown, W.E.","contributorId":33447,"corporation":false,"usgs":true,"family":"Brown","given":"W.E.","affiliations":[],"preferred":false,"id":361050,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Cimino, J.B.","contributorId":51910,"corporation":false,"usgs":true,"family":"Cimino","given":"J.B.","email":"","affiliations":[],"preferred":false,"id":361054,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Dixon, T.","contributorId":14572,"corporation":false,"usgs":true,"family":"Dixon","given":"T.","email":"","affiliations":[],"preferred":false,"id":361045,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Evans, D.L.","contributorId":45663,"corporation":false,"usgs":true,"family":"Evans","given":"D.L.","email":"","affiliations":[],"preferred":false,"id":361052,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Ford, J.P.","contributorId":13746,"corporation":false,"usgs":true,"family":"Ford","given":"J.P.","email":"","affiliations":[],"preferred":false,"id":361043,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Saunders, R.S.","contributorId":14437,"corporation":false,"usgs":true,"family":"Saunders","given":"R.S.","email":"","affiliations":[],"preferred":false,"id":361044,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Breed, C.","contributorId":51454,"corporation":false,"usgs":true,"family":"Breed","given":"C.","affiliations":[],"preferred":false,"id":361053,"contributorType":{"id":1,"text":"Authors"},"rank":8},{"text":"Masursky, H.","contributorId":33823,"corporation":false,"usgs":true,"family":"Masursky","given":"H.","affiliations":[],"preferred":false,"id":361051,"contributorType":{"id":1,"text":"Authors"},"rank":9},{"text":"McCauley, J.F.","contributorId":26310,"corporation":false,"usgs":true,"family":"McCauley","given":"J.F.","email":"","affiliations":[],"preferred":false,"id":361048,"contributorType":{"id":1,"text":"Authors"},"rank":10},{"text":"Schaber, G.","contributorId":33053,"corporation":false,"usgs":true,"family":"Schaber","given":"G.","affiliations":[],"preferred":false,"id":361049,"contributorType":{"id":1,"text":"Authors"},"rank":11},{"text":"Dellwig, L.","contributorId":59945,"corporation":false,"usgs":true,"family":"Dellwig","given":"L.","affiliations":[],"preferred":false,"id":361055,"contributorType":{"id":1,"text":"Authors"},"rank":12},{"text":"England, A.","contributorId":6188,"corporation":false,"usgs":true,"family":"England","given":"A.","affiliations":[],"preferred":false,"id":361042,"contributorType":{"id":1,"text":"Authors"},"rank":13},{"text":"MacDonald, H.","contributorId":105046,"corporation":false,"usgs":true,"family":"MacDonald","given":"H.","email":"","affiliations":[],"preferred":false,"id":361057,"contributorType":{"id":1,"text":"Authors"},"rank":14},{"text":"Martin-Kaye, P.","contributorId":19706,"corporation":false,"usgs":true,"family":"Martin-Kaye","given":"P.","email":"","affiliations":[],"preferred":false,"id":361046,"contributorType":{"id":1,"text":"Authors"},"rank":15},{"text":"Sabins, F.","contributorId":22491,"corporation":false,"usgs":true,"family":"Sabins","given":"F.","email":"","affiliations":[],"preferred":false,"id":361047,"contributorType":{"id":1,"text":"Authors"},"rank":16}]}}
,{"id":70120261,"text":"70120261 - 1982 - Auditory evoked potentials in the West Indian Manatee (Sirenia: <i>Trichechus manatus</i>)","interactions":[],"lastModifiedDate":"2014-08-13T13:50:49","indexId":"70120261","displayToPublicDate":"1982-12-01T13:48:08","publicationYear":"1982","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2225,"text":"Journal of Comparative Physiology A","active":true,"publicationSubtype":{"id":10}},"title":"Auditory evoked potentials in the West Indian Manatee (Sirenia: <i>Trichechus manatus</i>)","docAbstract":"<p>Potentials evoked by clicks and tone pips were recorded by fine wires inserted extracranially in four West Indian manatees (<i>Trichechus manatus</i>) in air. Sounds were delivered via padded ear phones.</p>\n<br/>\n<p>Averaging a few thousand trials at 20/s reveals early peaks at N5.4 (‘vertex’ negativity to a frontal reference, at 5.4 ms), P7.6, N8.8, P9.5 — probably equivalent to waves IV and VII of the typical mammalian auditory brainstem response (ABR). Averaging 100 trials at <4/s suffices to reveal a complex sequence of later peaks including N25, P80, N150 and P190; consistent smaller peaks are visible when several hundred trials are averaged.</p>\n<br/>\n<p>Using tone pips with a rise and fall time of 2–5 ms the carrier frequency becomes important. Evoked potential wave forms are not the same at different frequencies, bringing out the fact that frequency is not a scalar that can be compensated for by intensity. Therefore the method was not used to obtain audiograms; however the largest EPs occur in the range of 1–1.5 kHz. EPs are found up to 35 kHz; almost no evoked potential is discernible at 40 kHz but the undistorted intensity available was limited. This is in reasonable agreement with the theoretical expectation for the upper limit of behavioral hearing from Heffner and Masterton based on head size and aquatic medium.</p.\n<br/>\n<p>Among several ear phone placements, that over the external auditory meatus was the most effective, but only slightly so. The external canal is presumably fluid or tissue filled and sound enters over a large area.</p>\n<br/>\n<p>Comparing data for two species on the most effective range of frequencies and the power spectra of their vocalizations, <i>T. manatus</i> is lower than <i>T. inunguis</i> in both respects.</p.\n<br/>\n<p>The results show the utility and limitations of the method of recording extracranial evoked potentials to sounds, especially for large and valuable animals under makeshift conditions.</p>","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Journal of Comparative Physiology A","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"Springer Verlag","publisherLocation":"Berlin","doi":"10.1007/BF00619792","usgsCitation":"Bullock, T.H., O'Shea, T., and McClune, M.C., 1982, Auditory evoked potentials in the West Indian Manatee (Sirenia: <i>Trichechus manatus</i>): Journal of Comparative Physiology A, v. 148, no. 4, p. 547-554, https://doi.org/10.1007/BF00619792.","productDescription":"9 p.","startPage":"547","endPage":"554","numberOfPages":"9","costCenters":[],"links":[{"id":292104,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":292103,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1007/BF00619792"}],"volume":"148","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53ec7bc7e4b02bf5a7673ff3","contributors":{"authors":[{"text":"Bullock, Theodore H.","contributorId":56569,"corporation":false,"usgs":true,"family":"Bullock","given":"Theodore","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":498069,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"O'Shea, Thomas J. 0000-0002-0758-9730","orcid":"https://orcid.org/0000-0002-0758-9730","contributorId":78071,"corporation":false,"usgs":true,"family":"O'Shea","given":"Thomas J.","affiliations":[{"id":291,"text":"Fort Collins Science Center","active":true,"usgs":true}],"preferred":false,"id":498070,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"McClune, Michael C.","contributorId":104826,"corporation":false,"usgs":true,"family":"McClune","given":"Michael","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":498071,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70209670,"text":"70209670 - 1982 - U-Pb ages of uranium ores in the Churchrock uranium district, New Mexico","interactions":[],"lastModifiedDate":"2020-04-20T18:04:13.984093","indexId":"70209670","displayToPublicDate":"1982-12-01T12:58:56","publicationYear":"1982","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1472,"text":"Economic Geology","active":true,"publicationSubtype":{"id":10}},"title":"U-Pb ages of uranium ores in the Churchrock uranium district, New Mexico","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"Society of Economic Geologists","doi":"10.2113/gsecongeo.77.8.1942","usgsCitation":"Ludwig, K., Rubin, B., Fishman, N., and Reynolds, R.L., 1982, U-Pb ages of uranium ores in the Churchrock uranium district, New Mexico: Economic Geology, v. 77, no. 8, p. 1942-1945, https://doi.org/10.2113/gsecongeo.77.8.1942.","productDescription":"4 p.","startPage":"1942","endPage":"1945","costCenters":[{"id":318,"text":"Geosciences and Environmental Change Science Center","active":true,"usgs":true}],"links":[{"id":374126,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"New Mexico","otherGeospatial":"Church Rock uranium district","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -108.9404296875,\n              34.9805024453652\n            ],\n            [\n              -107.6275634765625,\n              34.9805024453652\n            ],\n            [\n              -107.6275634765625,\n              35.9157474194997\n            ],\n            [\n              -108.9404296875,\n              35.9157474194997\n            ],\n            [\n              -108.9404296875,\n              34.9805024453652\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"77","issue":"8","noUsgsAuthors":false,"publicationDate":"1982-12-01","publicationStatus":"PW","contributors":{"authors":[{"text":"Ludwig, K.R.","contributorId":97112,"corporation":false,"usgs":true,"family":"Ludwig","given":"K.R.","email":"","affiliations":[{"id":218,"text":"Denver Federal Center","active":false,"usgs":true}],"preferred":false,"id":787457,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Rubin, Bruce","contributorId":224221,"corporation":false,"usgs":false,"family":"Rubin","given":"Bruce","email":"","affiliations":[],"preferred":false,"id":787458,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Fishman, Neil","contributorId":145906,"corporation":false,"usgs":false,"family":"Fishman","given":"Neil","affiliations":[{"id":16290,"text":"Hess Corporation, Houston, Texas, USA","active":true,"usgs":false}],"preferred":false,"id":787459,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Reynolds, Richard L. 0000-0002-4572-2942 rreynolds@usgs.gov","orcid":"https://orcid.org/0000-0002-4572-2942","contributorId":139068,"corporation":false,"usgs":true,"family":"Reynolds","given":"Richard","email":"rreynolds@usgs.gov","middleInitial":"L.","affiliations":[{"id":318,"text":"Geosciences and Environmental Change Science Center","active":true,"usgs":true}],"preferred":true,"id":787460,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70226966,"text":"70226966 - 1982 - The United Kingdom-Caltech asteroid survey","interactions":[],"lastModifiedDate":"2021-12-22T16:16:22.952701","indexId":"70226966","displayToPublicDate":"1982-12-01T09:47:47","publicationYear":"1982","noYear":false,"publicationType":{"id":5,"text":"Book chapter"},"publicationSubtype":{"id":24,"text":"Book Chapter"},"title":"The United Kingdom-Caltech asteroid survey","docAbstract":"<p>No abstract available.</p>","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Reports of Planetary Programs, 1982","largerWorkSubtype":{"id":1,"text":"Federal Government Series"},"language":"English","publisher":"National Aeronautics and Space Administration","usgsCitation":"Bus, S.J., Helin, E.F., Dunbar, R.S., Shoemaker, E.M., Dawe, J., Barrow, J., Hartley, M., Morgan, D., Russell, K., and Savage, A., 1982, The United Kingdom-Caltech asteroid survey, chap. <i>of</i> Reports of Planetary Programs, 1982, p. 53-56.","productDescription":"NASA TM-85127, 4 p.","startPage":"53","endPage":"56","costCenters":[],"links":[{"id":393301,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Bus, S. J.","contributorId":270304,"corporation":false,"usgs":false,"family":"Bus","given":"S.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":828987,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Helin, E. F.","contributorId":73752,"corporation":false,"usgs":true,"family":"Helin","given":"E.","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":828988,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Dunbar, R. S.","contributorId":270305,"corporation":false,"usgs":false,"family":"Dunbar","given":"R.","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":828989,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Shoemaker, Eugene Merle","contributorId":20342,"corporation":false,"usgs":true,"family":"Shoemaker","given":"Eugene","email":"","middleInitial":"Merle","affiliations":[],"preferred":false,"id":828990,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Dawe, J.","contributorId":270306,"corporation":false,"usgs":false,"family":"Dawe","given":"J.","email":"","affiliations":[],"preferred":false,"id":828991,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Barrow, J.","contributorId":270307,"corporation":false,"usgs":false,"family":"Barrow","given":"J.","email":"","affiliations":[],"preferred":false,"id":828992,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Hartley, M.","contributorId":270308,"corporation":false,"usgs":false,"family":"Hartley","given":"M.","email":"","affiliations":[],"preferred":false,"id":828993,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Morgan, D.","contributorId":67413,"corporation":false,"usgs":true,"family":"Morgan","given":"D.","affiliations":[],"preferred":false,"id":828994,"contributorType":{"id":1,"text":"Authors"},"rank":8},{"text":"Russell, K.","contributorId":270309,"corporation":false,"usgs":false,"family":"Russell","given":"K.","email":"","affiliations":[],"preferred":false,"id":828995,"contributorType":{"id":1,"text":"Authors"},"rank":9},{"text":"Savage, A.","contributorId":270310,"corporation":false,"usgs":false,"family":"Savage","given":"A.","email":"","affiliations":[],"preferred":false,"id":828996,"contributorType":{"id":1,"text":"Authors"},"rank":10}]}}
,{"id":70260102,"text":"70260102 - 1982 - Status of Alaska sea otter populations and developing conflicts with fisheries","interactions":[],"lastModifiedDate":"2024-10-28T14:49:21.729595","indexId":"70260102","displayToPublicDate":"1982-12-01T09:42:26","publicationYear":"1982","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"Status of Alaska sea otter populations and developing conflicts with fisheries","docAbstract":"<p>No abstract available.</p>","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Transactions of the 47th North American wildlife and national resources conference","largerWorkSubtype":{"id":12,"text":"Conference publication"},"language":"English","publisher":"Wildlife Management Institute","usgsCitation":"Wildlife Management Institute, 1982, Status of Alaska sea otter populations and developing conflicts with fisheries, <i>in</i> Transactions of the 47th North American wildlife and national resources conference, p. 293-299.","productDescription":"7 p.","startPage":"293","endPage":"299","costCenters":[],"links":[{"id":463248,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Alaska","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -140.81229080608082,\n              69.55730901161931\n            ],\n            [\n              -141.17441986325167,\n              71.10856340711914\n            ],\n            [\n              -155.70833863026414,\n              72.53941384045936\n            ],\n            [\n              -170.17927840370044,\n              68.81931647024456\n            ],\n            [\n              -168.70155581561633,\n              65.12829916084013\n            ],\n            [\n              -171.36549073152332,\n              63.558064621323894\n            ],\n            [\n              -176.32823785170464,\n              50.69829011552713\n            ],\n            [\n              -159.01370701646405,\n              53.525823556965435\n            ],\n            [\n              -145.6523491137187,\n              59.07901510679412\n            ],\n            [\n              -140.95548113785986,\n              59.238797708351996\n            ],\n            [\n              -134.50250409495405,\n              54.621671404502365\n            ],\n            [\n              -130.1473646462728,\n              54.692795018182494\n            ],\n            [\n              -130.29209444399325,\n              56.289631420496505\n            ],\n            [\n              -135.27963077823088,\n              59.349873309070176\n            ],\n            [\n              -137.38132737746545,\n              59.07354994844752\n            ],\n            [\n              -141.0693249810899,\n              60.326013526222\n            ],\n            [\n              -149.99643314166477,\n              62.216732511242526\n            ],\n            [\n              -154.0923498951266,\n              59.78939498063829\n            ],\n            [\n              -155.5004844678802,\n              58.57738144974863\n            ],\n            [\n              -158.3685285415279,\n              59.406499244851545\n            ],\n            [\n              -163.40238049135712,\n              60.86346733831388\n            ],\n            [\n              -160.38200775753907,\n              63.02366087600697\n            ],\n            [\n              -160.20851237350166,\n              65.21298091103421\n            ],\n            [\n              -165.19954541371303,\n              65.22168270874386\n            ],\n            [\n              -161.07871252827428,\n              65.68632604298915\n            ],\n            [\n              -159.4105438215461,\n              66.52856012151437\n            ],\n            [\n              -164.68866250028753,\n              68.35664914496184\n            ],\n            [\n              -156.27704196581317,\n              70.55410064968143\n            ],\n            [\n              -140.81229080608082,\n              69.55730901161931\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW"}
,{"id":70120391,"text":"70120391 - 1982 - Use and interpretation of statistics in wildlife journals","interactions":[],"lastModifiedDate":"2014-08-14T09:15:58","indexId":"70120391","displayToPublicDate":"1982-12-01T09:10:44","publicationYear":"1982","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3779,"text":"Wildlife Society Bulletin","onlineIssn":"1938-5463","printIssn":"0091-7648","active":true,"publicationSubtype":{"id":10}},"title":"Use and interpretation of statistics in wildlife journals","docAbstract":"Use and interpretation of statistics in wildlife journals are reviewed, and suggestions for improvement are offered.  Populations from which inferences are to be drawn should be clearly defined, and conclusions should be limited to the range of the data analyzed.  Authors should be careful to avoid improper methods of plotting data and should clearly define the use of estimates of variance, standard deviation, standard error, or confidence intervals.  Biological and statistical significant are often confused by authors and readers.  Statistical hypothesis testing is a tool, and not every question should be answered by hypothesis testing.  Meeting assumptions of hypothesis tests is the responsibility of authors, and assumptions should be reviewed before a test is employed.  The use of statistical tools should be considered carefully both before and after gathering data.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Wildlife Society Bulletin","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"Wildlife Society","publisherLocation":"Bethesda, MD","usgsCitation":"Tacha, T.C., Warde, W.D., and Burnham, K.P., 1982, Use and interpretation of statistics in wildlife journals: Wildlife Society Bulletin, v. 10, no. 4, p. 355-362.","productDescription":"8 p.","startPage":"355","endPage":"362","numberOfPages":"8","costCenters":[],"links":[{"id":292145,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"10","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53edcd56e4b0f61b386d24b9","contributors":{"authors":[{"text":"Tacha, Thomas C.","contributorId":97434,"corporation":false,"usgs":true,"family":"Tacha","given":"Thomas","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":498127,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Warde, William D.","contributorId":84669,"corporation":false,"usgs":true,"family":"Warde","given":"William","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":498125,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Burnham, Kenneth P.","contributorId":95025,"corporation":false,"usgs":true,"family":"Burnham","given":"Kenneth","email":"","middleInitial":"P.","affiliations":[{"id":189,"text":"Colorado Cooperative Fish and Wildlife Research Unit","active":false,"usgs":true}],"preferred":false,"id":498126,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70226985,"text":"70226985 - 1982 - Volcanism in ice on Europa","interactions":[],"lastModifiedDate":"2021-12-23T15:16:26.615893","indexId":"70226985","displayToPublicDate":"1982-12-01T08:49:18","publicationYear":"1982","noYear":false,"publicationType":{"id":5,"text":"Book chapter"},"publicationSubtype":{"id":24,"text":"Book Chapter"},"title":"Volcanism in ice on Europa","docAbstract":"<p>No abstract available.</p>","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Reports of Planetary Programs, 1982","largerWorkSubtype":{"id":1,"text":"Federal Government Series"},"language":"English","publisher":"National Aeronautics and Space Administration","usgsCitation":"Cook, A.F., Shoemaker, E.M., Soderblom, L.A., Mullins, K.F., and Fiedler, R., 1982, Volcanism in ice on Europa, chap. <i>of</i> Reports of Planetary Programs, 1982, p. 415-416.","productDescription":"NASA TM-85127, 2 p.","startPage":"415","endPage":"416","costCenters":[],"links":[{"id":393358,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"otherGeospatial":"Europa","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Cook, A. F.","contributorId":82848,"corporation":false,"usgs":true,"family":"Cook","given":"A.","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":829080,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Shoemaker, Eugene Merle","contributorId":20342,"corporation":false,"usgs":true,"family":"Shoemaker","given":"Eugene","email":"","middleInitial":"Merle","affiliations":[],"preferred":false,"id":829081,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Soderblom, L. A.","contributorId":106689,"corporation":false,"usgs":true,"family":"Soderblom","given":"L.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":829082,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Mullins, K. F.","contributorId":104702,"corporation":false,"usgs":true,"family":"Mullins","given":"K.","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":829083,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Fiedler, R.","contributorId":270341,"corporation":false,"usgs":false,"family":"Fiedler","given":"R.","email":"","affiliations":[],"preferred":false,"id":829084,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":70179053,"text":"70179053 - 1982 - Magnitude > or = 6.0 earthquakes","interactions":[],"lastModifiedDate":"2024-03-13T19:04:24.435467","indexId":"70179053","displayToPublicDate":"1982-12-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1435,"text":"Earthquake Information Bulletin (USGS)","active":true,"publicationSubtype":{"id":10}},"title":"Magnitude > or = 6.0 earthquakes","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","usgsCitation":"1982, Magnitude > or = 6.0 earthquakes: Earthquake Information Bulletin (USGS), v. 14, no. 5, p. 192-195.","productDescription":"4 p.","startPage":"192","endPage":"195","numberOfPages":"4","costCenters":[],"links":[{"id":332107,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.er.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"14","issue":"5","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"58526900e4b0e2663625ecac","contributors":{"editors":[{"text":"Spall, Henry","contributorId":77933,"corporation":false,"usgs":true,"family":"Spall","given":"Henry","email":"","affiliations":[],"preferred":false,"id":655880,"contributorType":{"id":2,"text":"Editors"},"rank":1}]}}
,{"id":70200532,"text":"70200532 - 1982 - Ice sculpture in the Martian outflow channels","interactions":[],"lastModifiedDate":"2018-10-23T10:38:47","indexId":"70200532","displayToPublicDate":"1982-11-30T10:37:42","publicationYear":"1982","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2314,"text":"Journal of Geophysical Research B: Solid Earth","active":true,"publicationSubtype":{"id":10}},"title":"Ice sculpture in the Martian outflow channels","docAbstract":"<p><span>Many landforms in Martian outflow channels have characteristics that suggest sculpture by glaciers, ice streams, or ice sheets. Viking Orbiter and terrestrial satellite images were examined at similar resolution to compare features of the Martian outflow channels to features produced by the movement of ice on earth. Many resemblances were found. They include the anastomoses, sinuosities, and U‐shaped cross profiles of valleys; hanging valleys; and linear scour marks on valley walls, grooves and ridges on valley floors, and streamlining of bedrock highs. The question of whether ice could have moved in the Martian environment is investigated. Since gradients on Martian channel floors are extremely low or even reversed, a certain thickness of ice is required to initiate glacial motion. If ice filled the Martian channels to the level of interior plateaus, flow could have occurred, even under present climatic conditions, although warmer climates in the past would have been more favorable. Additionally, if the channel fluids were brines, ice might have been wet based and would have moved readily by slipping over the ground. It is envisioned that springs or small catastrophic outbursts discharged fluids from structural outlets or chaotic terrains. The fluids built icings that may have grown into substantial masses and eventually flowed like glaciers down preexisting valleys. Alternatively, the fluids may have formed rivers or floods that formed ice jams and consolidated into icy masses in places where obstacles blocked their flow. These masses of ice or slush were probably episodic and temporary, but where they occurred within the channels, they may have produced landforms that are characteristic of glacial sculpture on earth.</span></p>","language":"English","publisher":"American Geophysical Union","doi":"10.1029/JB087iB12p09951","usgsCitation":"Lucchitta, B.K., 1982, Ice sculpture in the Martian outflow channels: Journal of Geophysical Research B: Solid Earth, v. 87, no. B12, p. 9951-9973, https://doi.org/10.1029/JB087iB12p09951.","productDescription":"23 p.","startPage":"9951","endPage":"9973","costCenters":[{"id":131,"text":"Astrogeology Science Center","active":true,"usgs":true}],"links":[{"id":358664,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"87","issue":"B12","noUsgsAuthors":false,"publicationDate":"2012-09-20","publicationStatus":"PW","contributors":{"authors":[{"text":"Lucchitta, Baerbel K. blucchitta@usgs.gov","contributorId":3649,"corporation":false,"usgs":true,"family":"Lucchitta","given":"Baerbel","email":"blucchitta@usgs.gov","middleInitial":"K.","affiliations":[],"preferred":true,"id":749388,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70010368,"text":"70010368 - 1982 - Reply to comments of S.M. Johnson","interactions":[],"lastModifiedDate":"2025-04-08T16:55:43.506798","indexId":"70010368","displayToPublicDate":"1982-11-05T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2302,"text":"Journal of Geochemical Exploration","active":true,"publicationSubtype":{"id":10}},"title":"Reply to comments of S.M. Johnson","docAbstract":"<p>No abstract available.&nbsp;</p>","language":"English","publisher":"Elsevier","doi":"10.1016/0375-6742(82)90032-2","usgsCitation":"Theobald, P.K., 1982, Reply to comments of S.M. Johnson: Journal of Geochemical Exploration, v. 17, no. 2, p. 163-164, https://doi.org/10.1016/0375-6742(82)90032-2.","productDescription":"2 p.","startPage":"163","endPage":"164","costCenters":[],"links":[{"id":219685,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"17","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505aa76be4b0c8380cd853e6","contributors":{"authors":[{"text":"Theobald, P. K. Jr.","contributorId":70398,"corporation":false,"usgs":true,"family":"Theobald","given":"P.","suffix":"Jr.","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":358755,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70011491,"text":"70011491 - 1982 - Natural groundwater recharge in an upland area of central North Dakota, U.S.A.","interactions":[],"lastModifiedDate":"2025-04-10T23:18:52.172669","indexId":"70011491","displayToPublicDate":"1982-11-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2342,"text":"Journal of Hydrology","active":true,"publicationSubtype":{"id":10}},"title":"Natural groundwater recharge in an upland area of central North Dakota, U.S.A.","docAbstract":"<p><span>The magnitude of groundwater recharge to coal aquifers in a 150-km</span><sup>2</sup><span>&nbsp;area in west-central North Dakota was determined using three separate approaches: (1) the net water level rise in water-table wells; (2) calculations of the fluid flux between nested piezometers, using the Darcy equation and measured values of hydraulic conductivity and vertical gradients; and (3) evaluation of the inputs to and outputs from the coal aquifer, using a steady-state control volume approach in which the aquifer was divided into semi-rectangular cells bounded by equipotential lines and flow lines. Measurements of potential gradients and hydraulic conductivity permitted indirect determination of all components of flow into and out of the cell except the recharge input, which was determined by difference.</span></p><p><span>All methods yielded consistent results on the order of 0.04-0.01 m yr.<sup>−1</sup>&nbsp;These values, which represent 2–9% of the annual precipitation, are consistent with results of other studies on recharge throughout the prairies of North America.</span></p><p><span>Evaluation of site hydrology and stable-isotope data indicates that recharge is restricted in both time and place. Most recharge occurs in late spring and in the fall following heavy rainfall events. During these seasons the ground is not frozen and vegetation is not transpiring large amounts of water. Some recharge may occur during very heavy localized summer storms, but it is not considered volumetrically significant. Major permanent depressions on the site are a source of significant recharge. In addition, the extensive area of ephemeral standing water bodies that result from snowmelt can produce significant amounts of infiltration over the entire site.</span></p>","language":"English","publisher":"Elsevier","doi":"10.1016/0022-1694(82)90093-2","issn":"00221694","usgsCitation":"Rehm, B., Moran, S., and Groenewold, G., 1982, Natural groundwater recharge in an upland area of central North Dakota, U.S.A.: Journal of Hydrology, v. 59, no. 3-4, p. 293-314, https://doi.org/10.1016/0022-1694(82)90093-2.","productDescription":"22 p.","startPage":"293","endPage":"314","costCenters":[],"links":[{"id":221048,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","otherGeospatial":"central North Dakota","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -102.60876813870183,\n              49.012008277756365\n            ],\n            [\n              -102.60876813870183,\n              45.988974212508225\n            ],\n            [\n              -99.24442932052045,\n              45.988974212508225\n            ],\n            [\n              -99.24442932052045,\n              49.012008277756365\n            ],\n            [\n              -102.60876813870183,\n              49.012008277756365\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","volume":"59","issue":"3-4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a630be4b0c8380cd7227b","contributors":{"authors":[{"text":"Rehm, B.W.","contributorId":73748,"corporation":false,"usgs":true,"family":"Rehm","given":"B.W.","email":"","affiliations":[],"preferred":false,"id":361247,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Moran, S.R.","contributorId":20888,"corporation":false,"usgs":true,"family":"Moran","given":"S.R.","email":"","affiliations":[],"preferred":false,"id":361246,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Groenewold, G.H.","contributorId":14113,"corporation":false,"usgs":true,"family":"Groenewold","given":"G.H.","email":"","affiliations":[],"preferred":false,"id":361245,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":1003189,"text":"1003189 - 1982 - Growth and condition of bluegills in Wisconsin lakes: Effects of population density and lake pH","interactions":[],"lastModifiedDate":"2026-04-13T16:37:03.021677","indexId":"1003189","displayToPublicDate":"1982-11-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3624,"text":"Transactions of the American Fisheries Society","active":true,"publicationSubtype":{"id":10}},"title":"Growth and condition of bluegills in Wisconsin lakes: Effects of population density and lake pH","docAbstract":"<p><span>Growth and condition of bluegills Lepomis macrochirus from five acidic lakes (pH 5.1–6.0) and six circumueutral lakes (pH 6.7–7.5) in northern Wisconsin were compared. Although mean condition factors and mean back‐calculated total lengths at ages 1 to 4 varied significantly among lakes, the differences were not related to lake pH. Rather, the ranks of mean condition factors and back‐calculated lengths at ages 2, 3, and 4 were negatively correlated with relative density of bluegills among the lakes. Because of the dominating effect of density, growth rates and condition factors are not useful as indicators of chronic, pH‐related stress on bluegill populations.</span></p>","language":"English","publisher":"American Fisheries Society","doi":"10.1577/1548-8659(1982)111<761:GACOBI>2.0.CO;2","usgsCitation":"Wiener, J., and Hanneman, W., 1982, Growth and condition of bluegills in Wisconsin lakes: Effects of population density and lake pH: Transactions of the American Fisheries Society, v. 111, no. 6, p. 761-767, https://doi.org/10.1577/1548-8659(1982)111<761:GACOBI>2.0.CO;2.","productDescription":"7 p.","startPage":"761","endPage":"767","costCenters":[{"id":606,"text":"Upper Midwest Environmental Sciences Center","active":true,"usgs":true}],"links":[{"id":179590,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"111","issue":"6","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afbe4b07f02db69613e","contributors":{"authors":[{"text":"Wiener, J.G.","contributorId":44107,"corporation":false,"usgs":true,"family":"Wiener","given":"J.G.","email":"","affiliations":[],"preferred":false,"id":312903,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hanneman, W.R.","contributorId":94380,"corporation":false,"usgs":true,"family":"Hanneman","given":"W.R.","email":"","affiliations":[],"preferred":false,"id":312904,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70185624,"text":"70185624 - 1982 - Adsorption of natural dissolved organic matter at the oxide/water interface","interactions":[],"lastModifiedDate":"2020-01-26T09:52:30","indexId":"70185624","displayToPublicDate":"1982-11-01T00:00:00","publicationYear":"1982","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":"Adsorption of natural dissolved organic matter at the oxide/water interface","docAbstract":"<p><span>Natural organic matter is readily adsorbed by alumina and kaolinite in the pH range of natural waters. Adsorption occurs by complex formation between surface hydroxyls and the acidic functional groups of the organic matter. Oxides with relatively acidic surface hydroxyls, </span><i>e.g.</i><span> silica, do not react strongly with the organic matter. Under conditions typical for natural waters, almost complete surface coverage by adsorbed organic matter may be expected for alumina, hydrous iron oxides and the edge sites of aluminosilicates. Potentiometric titration and electrophoresis indicate that most of the acidic functional groups of the adsorbed organic matter are neutralized by protons from solution. The organic coating is expected to have a great influence on subsequent adsorption of inorganic cations and anions.</span></p>","language":"English","publisher":"Elsevier","doi":"10.1016/0016-7037(82)90209-5","usgsCitation":"Davis, J., 1982, Adsorption of natural dissolved organic matter at the oxide/water interface: Geochimica et Cosmochimica Acta, v. 46, no. 11, p. 2381-2393, https://doi.org/10.1016/0016-7037(82)90209-5.","productDescription":"13 p. ","startPage":"2381","endPage":"2393","costCenters":[{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":338325,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"46","issue":"11","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"58d63041e4b05ec79913111f","contributors":{"authors":[{"text":"Davis, James A.","contributorId":69289,"corporation":false,"usgs":true,"family":"Davis","given":"James A.","affiliations":[],"preferred":false,"id":686151,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70011472,"text":"70011472 - 1982 - Active geologic processes in Barrow Canyon, northeast Chukchi Sea","interactions":[],"lastModifiedDate":"2024-10-11T17:33:36.143825","indexId":"70011472","displayToPublicDate":"1982-11-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2667,"text":"Marine Geology","active":true,"publicationSubtype":{"id":10}},"title":"Active geologic processes in Barrow Canyon, northeast Chukchi Sea","docAbstract":"<p><span>Circulation patterns on the shelf and at the shelf break appear to dominate the Barrow Canyon system. The canyon's shelf portion underlies and is maintained by the Alaska Coastal Current (A.C.C.), which flows northeastward along the coast toward the northeast corner of the broad Chukchi Sea. Offshelf and onshelf advective processes are indicated by oceanographic measurements of other workers. These advective processes may play an important role in the production of bedforms that are found near the canyon head as well as in processes of erosion or non-deposition in the deeper canyon itself. Coarse sediments recovered from the canyon axis at 400 to 570 m indicate that there is presently significant flow along the canyon. The canyon hooks left at a point north of Point Barrow where the A.C.C. loses its coastal constriction. The left hook, as well as preferential west-wall erosion, continues down to the abyssal plain of the Canada Basin at 3800 m. A possible explanation for the preferential west-wall erosion along the canyon, at least for the upper few hundred meters, is that the occasional upwelling events, which cause nutrient-rich water to flow along the west wall would in turn cause larger populations of burrowing organisms to live there than on the east wall, and that these organisms cause high rates of bioerosion. This hypothesis assumes that the dominant factor in the canyon's erosion is biological activity, not current velocity. Sedimentary bedforms consisting of waves and furrows are formed in soft mud in a region on the shelf west of the canyon head; their presence there perhaps reflects: (a) the supply of fine suspended sediments delivered by the A.C.C. from sources to the south, probably the Yukon and other rivers draining northwestern Alaska; and (b) the westward transport of these suspended sediments by the prevailing Beaufort Gyre which flows along the outer shelf.</span></p>","language":"English","publisher":"Elsevier","doi":"10.1016/0025-3227(82)90061-5","usgsCitation":"Eittreim, S., Grantz, A., and Greenberg, J., 1982, Active geologic processes in Barrow Canyon, northeast Chukchi Sea: Marine Geology, v. 50, no. 1-2, p. 61-76, https://doi.org/10.1016/0025-3227(82)90061-5.","productDescription":"16 p.","startPage":"61","endPage":"76","costCenters":[],"links":[{"id":220708,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Alaska","otherGeospatial":"Barrow Canyon, northeast Chukchi Sea","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -164.9782036874746,\n              72.59817606230985\n            ],\n            [\n              -164.9782036874746,\n              70.87893177138113\n            ],\n            [\n              -153.0605673497228,\n              70.87893177138113\n            ],\n            [\n              -153.0605673497228,\n              72.59817606230985\n            ],\n            [\n              -164.9782036874746,\n              72.59817606230985\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","volume":"50","issue":"1-2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059e6abe4b0c8380cd47592","contributors":{"authors":[{"text":"Eittreim, Stephen","contributorId":102553,"corporation":false,"usgs":true,"family":"Eittreim","given":"Stephen","email":"","affiliations":[],"preferred":false,"id":361193,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Grantz, Arthur agrantz@usgs.gov","contributorId":2585,"corporation":false,"usgs":true,"family":"Grantz","given":"Arthur","email":"agrantz@usgs.gov","affiliations":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"preferred":true,"id":361192,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Greenberg, Jonathan","contributorId":9627,"corporation":false,"usgs":true,"family":"Greenberg","given":"Jonathan","affiliations":[],"preferred":false,"id":361194,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":1007548,"text":"1007548 - 1982 - Gas exchange characteristics of the submerged aquatic Crassulacean acid metabolism plant, Isoetes howellii","interactions":[],"lastModifiedDate":"2025-06-24T15:37:44.93782","indexId":"1007548","displayToPublicDate":"1982-11-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3088,"text":"Plant Physiology","active":true,"publicationSubtype":{"id":10}},"title":"Gas exchange characteristics of the submerged aquatic Crassulacean acid metabolism plant, Isoetes howellii","docAbstract":"<p><span>The submerged aquatic plant&nbsp;</span><i>Isoetes howellii</i><span>&nbsp;Engelmann possesses Crassulacean acid metabolism (CAM) comparable to that known from terrestrial CAM plants. Infrared gas analysis of submerged leaves showed&nbsp;</span><i>Isoetes</i><span>&nbsp;was capable of net CO</span><sub>2</sub><span>&nbsp;uptake in both light and dark. CO</span><sub>2</sub><span>&nbsp;uptake rates were a function of CO</span><sub>2</sub><span>&nbsp;levels in the medium. At 2,500 microliters CO</span><sub>2</sub><span>&nbsp;per liter (gas phase, equivalent to 1.79 milligrams per liter aqueous phase),&nbsp;</span><i>Isoetes</i><span>&nbsp;leaves showed continuous uptake in both the light and dark. At this CO</span><sub>2</sub><span>&nbsp;level, photosynthetic rates were light saturated at about 10% full sunlight and were about 3-fold greater than dark CO</span><sub>2</sub><span>&nbsp;uptake rates. In the dark, CO</span><sub>2</sub><span>&nbsp;uptake rates were also a function of length of time in the night period. Measurements of dark CO</span><sub>2</sub><span>&nbsp;uptake showed that, at both 2,500 and 500 microliters CO</span><sub>2</sub><span>&nbsp;per liter, rates declined during the night period. At the higher CO</span><sub>2</sub><span>&nbsp;level, dark CO</span><sub>2</sub><span>&nbsp;uptake rates at 0600 h were 75% less than at 1800 h. At 500 microliters CO</span><sub>2</sub><span>&nbsp;per liter, net CO</span><sub>2</sub><span>&nbsp;uptake in the dark at 1800 h was replaced by net CO</span><sub>2</sub><span>&nbsp;evolution in the dark at 0600 h. At both CO</span><sub>2</sub><span>&nbsp;levels, the overnight decline in net CO</span><sub>2</sub><span>&nbsp;uptake was marked by periodic bursts of accelerated CO</span><sub>2</sub><span>&nbsp;uptake. CO</span><sub>2</sub><span>&nbsp;uptake in the light was similar at 1% and 21% O</span><sub>2</sub><span>, and this held for leaves intact as well as leaves split longitudinally. Estimating the contribution of light&nbsp;</span><i>versus</i><span>&nbsp;dark CO</span><sub>2</sub><span>&nbsp;uptake to the total carbon gain is complicated by the diurnal flux in CO</span><sub>2</sub><span>&nbsp;availability under field conditions.</span></p>","language":"English","publisher":"Oxford Academic","doi":"10.1104/pp.70.5.1455","usgsCitation":"Keeley, J., and Bowes, G., 1982, Gas exchange characteristics of the submerged aquatic Crassulacean acid metabolism plant, Isoetes howellii: Plant Physiology, v. 70, no. 5, p. 1455-1458, https://doi.org/10.1104/pp.70.5.1455.","productDescription":"4 p.","startPage":"1455","endPage":"1458","costCenters":[{"id":651,"text":"Western Ecological Research Center","active":true,"usgs":true}],"links":[{"id":491478,"rank":2,"type":{"id":41,"text":"Open Access External Repository Page"},"url":"https://www.ncbi.nlm.nih.gov/pmc/articles/1065905","text":"External Repository"},{"id":131590,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"70","issue":"5","noUsgsAuthors":false,"publicationDate":"1982-11-01","publicationStatus":"PW","scienceBaseUri":"4f4e4b28e4b07f02db6b1303","contributors":{"authors":[{"text":"Keeley, Jon E. 0000-0002-4564-6521","orcid":"https://orcid.org/0000-0002-4564-6521","contributorId":69082,"corporation":false,"usgs":true,"family":"Keeley","given":"Jon E.","affiliations":[],"preferred":false,"id":315601,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bowes, G.","contributorId":39232,"corporation":false,"usgs":true,"family":"Bowes","given":"G.","email":"","affiliations":[],"preferred":false,"id":315600,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70186204,"text":"70186204 - 1982 - Geophysics, tectonics and mineral deposits of Africa—Preface","interactions":[],"lastModifiedDate":"2017-03-31T13:32:53","indexId":"70186204","displayToPublicDate":"1982-11-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1761,"text":"Geoexploration","active":true,"publicationSubtype":{"id":10}},"title":"Geophysics, tectonics and mineral deposits of Africa—Preface","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"Elsevier","doi":"10.1016/0016-7142(82)90016-3","usgsCitation":"Hastings, D.A., 1982, Geophysics, tectonics and mineral deposits of Africa—Preface: Geoexploration, v. 20, no. 3-4, p. 198-199, https://doi.org/10.1016/0016-7142(82)90016-3.","productDescription":"2 p.","startPage":"198","endPage":"199","costCenters":[{"id":222,"text":"Earth Resources Observation and Science (EROS) Center","active":true,"usgs":true}],"links":[{"id":338967,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"20","issue":"3-4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"58df6acfe4b02ff32c6aeaa9","contributors":{"authors":[{"text":"Hastings, David A.","contributorId":138985,"corporation":false,"usgs":true,"family":"Hastings","given":"David","email":"","middleInitial":"A.","affiliations":[{"id":223,"text":"Earth Resources Observation and Science (EROS) Center (Geography)","active":false,"usgs":true}],"preferred":false,"id":687874,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70120255,"text":"70120255 - 1982 - Susitna Hydroelectric Project: terrestrial environmental workshop and preliminary simulation model","interactions":[],"lastModifiedDate":"2014-08-13T13:41:01","indexId":"70120255","displayToPublicDate":"1982-10-22T13:39:28","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":9,"text":"Other Report"},"title":"Susitna Hydroelectric Project: terrestrial environmental workshop and preliminary simulation model","docAbstract":"<p>The technical feasibility, economic viability, and environmental impacts of a hydroelectric development project in the Susitna River Basin are being studied by Acres American, Inc. on behalf of the Alaska Power Authority. As part of these studies, Acres American recently contracted LGL Alaska Research Associates, Inc. to coordinate the terrestrial environmental studies being performed by the Alaska Department of Fish and Game and, as subcontractors to LGL, several University of Alaska research groups. LGL is responsible for further quantifying the potential impacts of the project on terrestrial wildlife and vegetation, and for developing a plan to mitigate adverse impacts on the terrestrial environment. The impact assessment and mitigation plan will be included as part of a license application to the Federal Energy Regulatory Commission (FERC) scheduled for the first quarter of 1983.</p>\n<br/>\n<p>The quantification of impacts, mitigation planning, and design of future research is being organized using a computer simulation modelling approach. Through a series of workshops attended by researchers, resource managers, and policy-makers, a computer model is being developed and refined for use in the quantification of impacts on terrestrial wildlife and vegetation, and for evaluating different mitigation measures such as habitat enhancement and the designation of replacement lands to be managed by wildlife habitat. This report describes the preliminary model developed at the first workshop held August 23 -27, 1982 in Anchorage.</p>","language":"English","publisher":"Enviromental and Social Systems Analysts","publisherLocation":"Vancouver, British Columbia, Canada","usgsCitation":"Everitt, R.R., Sonntag, N.C., Auble, G.T., Roelle, J.E., and Gazey, W., 1982, Susitna Hydroelectric Project: terrestrial environmental workshop and preliminary simulation model, 123 p.","productDescription":"123 p.","numberOfPages":"123","costCenters":[],"links":[{"id":292100,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53ec7bd3e4b02bf5a76740b6","contributors":{"authors":[{"text":"Everitt, Robert R.","contributorId":34837,"corporation":false,"usgs":true,"family":"Everitt","given":"Robert","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":498063,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Sonntag, Nicholas C.","contributorId":85894,"corporation":false,"usgs":true,"family":"Sonntag","given":"Nicholas","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":498065,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Auble, Gregory T.","contributorId":23456,"corporation":false,"usgs":true,"family":"Auble","given":"Gregory","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":498062,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Roelle, James E. roelleb@usgs.gov","contributorId":2330,"corporation":false,"usgs":true,"family":"Roelle","given":"James","email":"roelleb@usgs.gov","middleInitial":"E.","affiliations":[{"id":291,"text":"Fort Collins Science Center","active":true,"usgs":true}],"preferred":true,"id":498061,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Gazey, William","contributorId":78653,"corporation":false,"usgs":true,"family":"Gazey","given":"William","email":"","affiliations":[],"preferred":false,"id":498064,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":70199907,"text":"70199907 - 1982 - Aqueous pyrite oxidation and the consequent formation of secondary iron minerals","interactions":[],"lastModifiedDate":"2018-10-03T09:17:49","indexId":"70199907","displayToPublicDate":"1982-10-03T09:16:04","publicationYear":"1982","noYear":false,"publicationType":{"id":5,"text":"Book chapter"},"publicationSubtype":{"id":24,"text":"Book Chapter"},"title":"Aqueous pyrite oxidation and the consequent formation of secondary iron minerals","docAbstract":"<p>No abstract available.&nbsp;</p>","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Acid sulfate weathering","language":"English","publisher":"Soil Science Society of America","usgsCitation":"Nordstrom, D.K., 1982, Aqueous pyrite oxidation and the consequent formation of secondary iron minerals, chap. <i>of</i> Acid sulfate weathering, p. 37-56.","productDescription":"20 p.","startPage":"37","endPage":"56","costCenters":[{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":358082,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"editors":[{"text":"Kittrick, J.A.","contributorId":20893,"corporation":false,"usgs":true,"family":"Kittrick","given":"J.A.","email":"","affiliations":[],"preferred":false,"id":747243,"contributorType":{"id":2,"text":"Editors"},"rank":1},{"text":"Fanning, D.A.","contributorId":208433,"corporation":false,"usgs":false,"family":"Fanning","given":"D.A.","email":"","affiliations":[],"preferred":false,"id":747244,"contributorType":{"id":2,"text":"Editors"},"rank":2},{"text":"Hossner, L.R.","contributorId":208434,"corporation":false,"usgs":false,"family":"Hossner","given":"L.R.","email":"","affiliations":[],"preferred":false,"id":747245,"contributorType":{"id":2,"text":"Editors"},"rank":3}],"authors":[{"text":"Nordstrom, D. Kirk 0000-0003-3283-5136 dkn@usgs.gov","orcid":"https://orcid.org/0000-0003-3283-5136","contributorId":749,"corporation":false,"usgs":true,"family":"Nordstrom","given":"D.","email":"dkn@usgs.gov","middleInitial":"Kirk","affiliations":[{"id":5044,"text":"National Research Program - Central Branch","active":true,"usgs":true},{"id":37277,"text":"WMA - Earth System Processes Division","active":true,"usgs":true}],"preferred":false,"id":747242,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70170881,"text":"70170881 - 1982 - Degradation of phenolic contaminants in ground water by anaerobic bacteria: St. Louis Park, Minnesota","interactions":[],"lastModifiedDate":"2020-01-26T09:51:54","indexId":"70170881","displayToPublicDate":"1982-10-01T17:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1861,"text":"Ground Water","active":true,"publicationSubtype":{"id":10}},"title":"Degradation of phenolic contaminants in ground water by anaerobic bacteria: St. Louis Park, Minnesota","docAbstract":"<p><span>Coal-tar derivatives from a coal-tar distillation and wood-treating plant that operated from 1918 to 1972 at St. Louis Park, Minnesota contaminated the near-surface ground water. Solutions of phenolic compounds and a water-immiscible mixture of polynuclear aromatic compounds accumulated in wetlands near the plant site and entered the aquifer. The concentration of phenolic compounds in the aqueous phase under the wetlands is about 30 mg/1 but decreases to less than 0.2 mg/1 at a distance of 430 m immediately downgradient from the source. Concentrations of naphthalene (the predominant polynuclear compound in the ground water) and sodium (selected as a conservative tracer) range from about 20 mg/1 and 430 mg/1 in the aqueous phase at the source to about 2 mg/1 and 120 mg/1 at 430 m downgradient, respectively. Phenolic compounds and naphthalene are disappearing faster than expected if only dilution were occurring. Sorption of phenolic compounds on aquifer sediments is negligible but naphthalene is slightly sorbed. Anaerobic biodegradation of phenolic compounds is primarily responsible for the observed attenuation. Methane was found only in water samples from the contaminated zone (2-20 mg/1). Methane-producing bacteria were found only in water from the contaminated zone. Methane was produced in laboratory cultures of contaminated water inoculated with bacteria from the contaminated zone. Evidence for anaerobic biodegradation of naphthalene under either field or laboratory conditions was not obtained.</span></p>","language":"English","publisher":"Wiley","doi":"10.1111/j.1745-6584.1982.tb01390.x","usgsCitation":"Ehrlich, G.G., Goerlitz, D., Godsy, E., and Hult, M.F., 1982, Degradation of phenolic contaminants in ground water by anaerobic bacteria: St. Louis Park, Minnesota: Ground Water, v. 20, no. 6, p. 703-710, https://doi.org/10.1111/j.1745-6584.1982.tb01390.x.","productDescription":"8 p.","startPage":"703","endPage":"710","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":392,"text":"Minnesota Water Science Center","active":true,"usgs":true},{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":321034,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Minnesota","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -93.394775390625,\n              44.91965873229824\n            ],\n            [\n              -93.394775390625,\n              44.95769222787594\n            ],\n            [\n              -93.3354663848877,\n              44.95769222787594\n            ],\n            [\n              -93.3354663848877,\n              44.91965873229824\n            ],\n            [\n              -93.394775390625,\n              44.91965873229824\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"20","issue":"6","noUsgsAuthors":false,"publicationDate":"2006-03-21","publicationStatus":"PW","scienceBaseUri":"572dc02fe4b0dae0d5d8f06f","contributors":{"authors":[{"text":"Ehrlich, G. G.","contributorId":89126,"corporation":false,"usgs":true,"family":"Ehrlich","given":"G.","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":628905,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Goerlitz, D.F.","contributorId":8445,"corporation":false,"usgs":true,"family":"Goerlitz","given":"D.F.","affiliations":[],"preferred":false,"id":628906,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Godsy, E.M.","contributorId":56685,"corporation":false,"usgs":true,"family":"Godsy","given":"E.M.","email":"","affiliations":[],"preferred":false,"id":628907,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Hult, M. F.","contributorId":29817,"corporation":false,"usgs":true,"family":"Hult","given":"M.","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":628908,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70227030,"text":"70227030 - 1982 - Technical manual for estimating low-flow characteristics of Pennsylvania streams","interactions":[],"lastModifiedDate":"2021-12-27T18:25:13.56775","indexId":"70227030","displayToPublicDate":"1982-10-01T12:16:39","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":2,"text":"State or Local Government Series"},"seriesTitle":{"id":144,"text":"Water Resources Bulletin","active":false,"publicationSubtype":{"id":2}},"seriesNumber":"15","title":"Technical manual for estimating low-flow characteristics of Pennsylvania streams","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"Pennsylvania Department of Environmental Resources","collaboration":"U.S. Geological Survey","usgsCitation":"Flippo, H.N., 1982, Technical manual for estimating low-flow characteristics of Pennsylvania streams: Water Resources Bulletin 15, 100 p.","productDescription":"100 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Jr.","contributorId":36597,"corporation":false,"usgs":true,"family":"Flippo","given":"Herbert","suffix":"Jr.","email":"","middleInitial":"N.","affiliations":[],"preferred":false,"id":829282,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":1001268,"text":"1001268 - 1982 - Age-class determination of canvasbacks","interactions":[],"lastModifiedDate":"2024-10-30T16:44:00.467245","indexId":"1001268","displayToPublicDate":"1982-10-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2508,"text":"Journal of Wildlife Management","active":true,"publicationSubtype":{"id":10}},"title":"Age-class determination of canvasbacks","docAbstract":"<p>A technique was developed to distinguish yearling from adult canvasbacks (<i>Aythya valisineria</i>) in the field during spring on the basis of white flecking on the distal ends of selected wing feathers. Covert feathers from adults had well-defined vermiculation patterns whereas feathers from yearlings lacked such markings. These age-related characters were confirmed by paired comparisons of feathers from the same captive birds in consecutive years and by discriminant analysis of feathers using densitometric measurements from known-age wild birds. Reflective densitometric measurements of greater secondary coverts for females and males were significantly different between 1- and 2-year-old and between 2- and 3-year-old canvasbacks. Greater secondary coverts were the best feathers for recognizing age-classes of males and females. Densitometric values indicate low variability among different observers and within samples.</p>","language":"English","publisher":"Wiley","doi":"10.2307/3808222","usgsCitation":"Serie, J.R., Trauger, D.L., Doty, H.A., and Sharp, D., 1982, Age-class determination of canvasbacks: Journal of Wildlife Management, v. 46, no. 4, p. 894-904, https://doi.org/10.2307/3808222.","productDescription":"11 p.","startPage":"894","endPage":"904","costCenters":[{"id":480,"text":"Northern Prairie Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":134338,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"46","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afbe4b07f02db6960a7","contributors":{"authors":[{"text":"Serie, Jerome R.","contributorId":174564,"corporation":false,"usgs":false,"family":"Serie","given":"Jerome","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":310773,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Trauger, David L.","contributorId":107682,"corporation":false,"usgs":true,"family":"Trauger","given":"David","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":310774,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Doty, Harold A.","contributorId":17565,"corporation":false,"usgs":true,"family":"Doty","given":"Harold","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":310771,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Sharp, David E.","contributorId":12592,"corporation":false,"usgs":true,"family":"Sharp","given":"David E.","affiliations":[],"preferred":false,"id":310772,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":1001315,"text":"1001315 - 1982 - Behavioral interactions of penned red and arctic foxes","interactions":[],"lastModifiedDate":"2024-10-30T16:49:46.625057","indexId":"1001315","displayToPublicDate":"1982-10-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2508,"text":"Journal of Wildlife Management","active":true,"publicationSubtype":{"id":10}},"title":"Behavioral interactions of penned red and arctic foxes","docAbstract":"<p>Expansion of the geographical distribution of red foxes (<i>Vulpes vulpes</i>) into the far north tundra region may lead to competition between arctic (<i>Alopex lagopus</i>) and red foxes for space and resources. Behavioral interactions between red and arctic foxes were evaluated during 9 trials conducted in a 4.05-ha enclosure near Woodworth, North Dakota. Each trial consisted of introducing a male-female pair of arctic foxes into the enclosure and allowing them to acclimate for approximately a week before releasing a female red fox into the enclosure, followed by her mate a few days later. In 8 of 9 trials, red foxes were dominant over arctic foxes during encounters. Activity of the arctic foxes decreased upon addition of red foxes. Arctic foxes tried unsuccessfully to defend preferred den, resting, and feeding areas. Even though the outcome of competition between red and arctic foxes in the Arctic is uncertain, the more aggressive red fox can dominate arctic foxes in direct competition for den sites and other limited resources.</p>","language":"English","publisher":"Wiley","doi":"10.2307/3808220","usgsCitation":"Rudzinski, D., Graves, H., Sargeant, A., and Storm, G., 1982, Behavioral interactions of penned red and arctic foxes: Journal of Wildlife Management, v. 46, no. 4, p. 877-884, https://doi.org/10.2307/3808220.","productDescription":"8 p.","startPage":"877","endPage":"884","costCenters":[{"id":480,"text":"Northern Prairie Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":133803,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"North 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