Movements and wetland selection by brood-rearing black ducks (Anas rubripes) were studied in Maine during 1977-80. Eight radio-marked hens moved their broods an average of 1.2 km from the nest to rearing pond, but only 1 hen initiated secondary brood movements. Half of the 85 broods reared in the study area used only 3 wetlands, and most rearing ponds contained active beaver (Castor canadensis) colonies. Brood-rearing hens preferred Emergent ponds over lakes and Evergreen Scrub-Shrub wetlands, and did not occupy Dead Scrub-Shrub, Unconsolidated Bottom, or Aquatic Bed wetlands. Rearing ponds were large and possessed extensive areas of flooded mountain alder (Alnus incana), willow (Salix spp.), and herbaceous vegetation. Wetlands avoided by brood-rearing hens were those with large areas of open water, submergent aquatics, or ericaceous shrub vegetation.
","language":"English","publisher":"Wiley","doi":"10.2307/3808551","usgsCitation":"Ringelman, J.K., and Longcore, J.R., 1982, Movements and wetland selection by brood-rearing black ducks: Journal of Wildlife Management, v. 46, no. 3, p. 615-621, https://doi.org/10.2307/3808551.","productDescription":"7 p.","startPage":"615","endPage":"621","costCenters":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":196926,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United 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\"}}]}","volume":"46","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b32e4b07f02db6b482a","contributors":{"authors":[{"text":"Ringelman, James K.","contributorId":202244,"corporation":false,"usgs":false,"family":"Ringelman","given":"James","email":"","middleInitial":"K.","affiliations":[{"id":36387,"text":"Ducks Unlimited, Inc., Retired, Menoken, ND 58558, USA","active":true,"usgs":false}],"preferred":false,"id":334586,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Longcore, Jerry R.","contributorId":45447,"corporation":false,"usgs":true,"family":"Longcore","given":"Jerry","email":"","middleInitial":"R.","affiliations":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"preferred":false,"id":334585,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":1003335,"text":"1003335 - 1982 - Effects of an aquatic plant and suspended clay on the activity of fish toxicants","interactions":[],"lastModifiedDate":"2025-04-01T16:16:56.565345","indexId":"1003335","displayToPublicDate":"1982-07-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2886,"text":"North American Journal of Fisheries Management","active":true,"publicationSubtype":{"id":10}},"title":"Effects of an aquatic plant and suspended clay on the activity of fish toxicants","docAbstract":"Rotenone, antimycin, permethrin, pydrin, and Salicylanilide I were tested for their toxicities against fathead minnows (Pimephales promelas) in the presence of Canadian waterweed (Elodea canadensis) or suspended clay. The plants had little effect on the activity of rotenone and antimycin but substantially reduced the activity of permethrin and pydrin (synthetic pyrethroids). Bentonite severely inhibited the activity of all chemicals tested. Salicylanilide I was affected least and pydrin most (27 times as much pydrin was required when I g/liter of bentonite was present in 96-hour tests). The efficacy of the registered fish toxicants rotenone and antimycin is probably not significantly affected by vegetation under field conditions, but is greatly reduced by suspended bentonite clay.
","language":"English","publisher":"Oxford Academic","doi":"10.1577/1548-8659(1982)2<301:EOAAPA>2.0.CO;2","usgsCitation":"Gilderhus, P., 1982, Effects of an aquatic plant and suspended clay on the activity of fish toxicants: North American Journal of Fisheries Management, v. 2, no. 3, p. 301-306, https://doi.org/10.1577/1548-8659(1982)2<301:EOAAPA>2.0.CO;2.","productDescription":"6 p.","startPage":"301","endPage":"306","costCenters":[{"id":606,"text":"Upper Midwest Environmental Sciences Center","active":true,"usgs":true}],"links":[{"id":129155,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"2","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a2fe4b07f02db615fb0","contributors":{"authors":[{"text":"Gilderhus, P.A.","contributorId":60156,"corporation":false,"usgs":true,"family":"Gilderhus","given":"P.A.","affiliations":[],"preferred":false,"id":313129,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70011526,"text":"70011526 - 1982 - Perched water tables on hillsides in western Oregon: II. Preferential downslope movement of water and anions","interactions":[],"lastModifiedDate":"2025-07-31T16:20:32.654541","indexId":"70011526","displayToPublicDate":"1982-07-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3420,"text":"Soil Science Society of America Journal","active":true,"publicationSubtype":{"id":10}},"title":"Perched water tables on hillsides in western Oregon: II. Preferential downslope movement of water and anions","docAbstract":"Perched water tables on hillsides in western Oregon potentially provide a means by which pollutants from agricultural and domestic sources may enter surface waters and consequently degrade the quality of these waters. This paper reports the results of experiments which were carried out to investigate the flow of solutes and water from buried line sources in and above perched water tables on three different hillsides in western Oregon. In the saturated soil and rock mantles of two hillsides, evidence suggests that water and solutes flow preferentially through large continuous voids. The evidence includes the very high maximum rate of anion movement downslope, the failure of pore velocities calculated from Darcy's Law to predict the rate and direction of anion movement, the short time before high levels of anions are detected downslope, and the spatial variability in the maximum rates of anion movement over the depth and width of sites. On the third hillside, tracer anion movement and soil water pressure measurements indicate that preferential flow occurs through large continuous pores during heavy rainfall while the surrounding soil and rock mantle remains unsaturated. Finally, experiments with Rodamine WT dye show that a variety of continuous voids of different origins and sizes conduct water and solutes preferentially in the soil and upper regions of rock on these hillsides.
","language":"English","publisher":"Wiley","doi":"10.2136/sssaj1982.03615995004600040031x","issn":"03615995","usgsCitation":"Hammermeister, D., Kling, G., and Vomocil, J., 1982, Perched water tables on hillsides in western Oregon: II. Preferential downslope movement of water and anions: Soil Science Society of America Journal, v. 46, no. 4, p. 819-826, https://doi.org/10.2136/sssaj1982.03615995004600040031x.","productDescription":"8 p.","startPage":"819","endPage":"826","costCenters":[],"links":[{"id":221675,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Oregon","otherGeospatial":"western Oregon","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -124.61982166251676,\n 46.091757176818106\n ],\n [\n -124.61982166251676,\n 42.0103125427612\n ],\n [\n -122.03666282827481,\n 42.0103125427612\n ],\n [\n -122.03666282827481,\n 46.091757176818106\n ],\n [\n -124.61982166251676,\n 46.091757176818106\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","volume":"46","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a7671e4b0c8380cd780f9","contributors":{"authors":[{"text":"Hammermeister, D.P.","contributorId":27066,"corporation":false,"usgs":true,"family":"Hammermeister","given":"D.P.","affiliations":[],"preferred":false,"id":361325,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Kling, G.F.","contributorId":23688,"corporation":false,"usgs":true,"family":"Kling","given":"G.F.","email":"","affiliations":[],"preferred":false,"id":361323,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Vomocil, J.A.","contributorId":25291,"corporation":false,"usgs":true,"family":"Vomocil","given":"J.A.","email":"","affiliations":[],"preferred":false,"id":361324,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":70011624,"text":"70011624 - 1982 - Perched water tables on hillsides in western Oregon: I. Some factors affecting their development and longevity","interactions":[],"lastModifiedDate":"2025-07-31T16:13:30.335497","indexId":"70011624","displayToPublicDate":"1982-07-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3420,"text":"Soil Science Society of America Journal","active":true,"publicationSubtype":{"id":10}},"title":"Perched water tables on hillsides in western Oregon: I. Some factors affecting their development and longevity","docAbstract":"Perched water tables on hillsides located on the western border of the Willamette Valley in Oregon in some cases have the potential to transport pollutants from either domestic or agricultural sources downslope to streams, ponds, or reservoirs, resulting in the deterioration of the quality of these waters. In this paper, some factors responsible for the development and longevity of these potentially problem-causing perched water tables on three hillsides were examined. Analyses of hydraulic conductivity data and the relationships between rainfall, soil water pressure potential, and time suggest that permeable rock below 110 cm rather than clayey B horizons is mainly responsible for the development of perched water tables on upper convex slope positions on two of these hillsides. The data also suggest that subsurface flow from the upper convex regions contributed significant amounts of water to the lower convex slope positions. Further, perched water tables developed more rapidly, to a greater extent, and lasted longer in upper horizons of a lower concave region of slope where a shallow perched water table was already present at the onset of rainfall. Finally, perched water tables did not develop in the upper horizons on a third hillside that had no impermeable regions in the soil or upper rock mantle.
","language":"English","publisher":"Wiley","doi":"10.2136/sssaj1982.03615995004600040030x","issn":"03615995","usgsCitation":"Hammermeister, D., Kling, G., and Vomocil, J., 1982, Perched water tables on hillsides in western Oregon: I. Some factors affecting their development and longevity: Soil Science Society of America Journal, v. 46, no. 4, p. 811-818, https://doi.org/10.2136/sssaj1982.03615995004600040030x.","productDescription":"8 p.","startPage":"811","endPage":"818","costCenters":[],"links":[{"id":221056,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Oregon","otherGeospatial":"western Oregon","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -124.61982166251676,\n 46.091757176818106\n ],\n [\n -124.61982166251676,\n 42.0103125427612\n ],\n [\n -122.03666282827481,\n 42.0103125427612\n ],\n [\n -122.03666282827481,\n 46.091757176818106\n ],\n [\n -124.61982166251676,\n 46.091757176818106\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","volume":"46","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a7670e4b0c8380cd780f3","contributors":{"authors":[{"text":"Hammermeister, D.P.","contributorId":27066,"corporation":false,"usgs":true,"family":"Hammermeister","given":"D.P.","affiliations":[],"preferred":false,"id":361568,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Kling, G.F.","contributorId":23688,"corporation":false,"usgs":true,"family":"Kling","given":"G.F.","email":"","affiliations":[],"preferred":false,"id":361566,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Vomocil, J.A.","contributorId":25291,"corporation":false,"usgs":true,"family":"Vomocil","given":"J.A.","email":"","affiliations":[],"preferred":false,"id":361567,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":70011672,"text":"70011672 - 1982 - Characterization of organic contaminants in environmental samples associated with Mount St. Helens 1980 volcanic eruption","interactions":[],"lastModifiedDate":"2023-10-27T11:04:06.170639","indexId":"70011672","displayToPublicDate":"1982-07-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":5925,"text":"Environmental Science and Technology","active":true,"publicationSubtype":{"id":10}},"title":"Characterization of organic contaminants in environmental samples associated with Mount St. Helens 1980 volcanic eruption","docAbstract":"Volcanic ash, surface-water, and bottom-material samples obtained in the vicinity of Mount St. Helens after the May 18, 1980, eruption were analyzed for organic contaminants by using capillary gas chromatography-mass spectrometry-computer techniques. Classes of compounds identified include n-alkanes, fatty acids, dicarboxylic acids, aromatic acids and aldehydes, phenols, resin acids, terpenes, and insect juvenile hormones. The most probable source of these compounds is from pyrolysis of plant and soil organic matter during and after the eruption. The toxicity of selected compounds and their environmental significance are discussed.
","language":"English","publisher":"American Chemical Society","doi":"10.1021/es00101a005","usgsCitation":"Pereira, W.E., Rostad, C.E., Taylor, H.E., and Klein, J.M., 1982, Characterization of organic contaminants in environmental samples associated with Mount St. Helens 1980 volcanic eruption: Environmental Science and Technology, v. 16, no. 7, p. 387-396, https://doi.org/10.1021/es00101a005.","productDescription":"10 p.","startPage":"387","endPage":"396","numberOfPages":"10","costCenters":[{"id":218,"text":"Denver Federal Center","active":false,"usgs":true}],"links":[{"id":220716,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Washinton","otherGeospatial":"Mount St. Helens","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -122.03984938696388,\n 46.368284173393704\n ],\n [\n -123.0098625343753,\n 46.368284173393704\n ],\n [\n -123.0098625343753,\n 45.98007368132036\n ],\n [\n -122.03984938696388,\n 45.98007368132036\n ],\n [\n -122.03984938696388,\n 46.368284173393704\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","volume":"16","issue":"7","noUsgsAuthors":false,"publicationDate":"2002-05-01","publicationStatus":"PW","scienceBaseUri":"5059f4d3e4b0c8380cd4bf4b","contributors":{"authors":[{"text":"Pereira, Wilfred E.","contributorId":95552,"corporation":false,"usgs":true,"family":"Pereira","given":"Wilfred","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":361677,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Rostad, Colleen E. cerostad@usgs.gov","contributorId":833,"corporation":false,"usgs":true,"family":"Rostad","given":"Colleen","email":"cerostad@usgs.gov","middleInitial":"E.","affiliations":[],"preferred":true,"id":886967,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Taylor, Howard E. hetaylor@usgs.gov","contributorId":1551,"corporation":false,"usgs":true,"family":"Taylor","given":"Howard","email":"hetaylor@usgs.gov","middleInitial":"E.","affiliations":[{"id":5044,"text":"National Research Program - Central Branch","active":true,"usgs":true}],"preferred":true,"id":886968,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Klein, John M.","contributorId":27036,"corporation":false,"usgs":true,"family":"Klein","given":"John","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":886969,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":5221801,"text":"5221801 - 1982 - Unweathered and weathered aviation kerosine: Chemical characterization and effects on hatching success of duck eggs","interactions":[],"lastModifiedDate":"2020-02-26T11:19:46","indexId":"5221801","displayToPublicDate":"1982-06-16T12:19:21","publicationYear":"1982","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1103,"text":"Bulletin of Environmental Contamination and Toxicology","active":true,"publicationSubtype":{"id":10}},"title":"Unweathered and weathered aviation kerosine: Chemical characterization and effects on hatching success of duck eggs","docAbstract":"Unweathered crude and refined oils are known to be very toxic to the embryos of aquatic birds (ALBERS 1977, 19781 SEARO et ale 1978, WHITE et al. 1979, McGILL & RICHMOND 1979, and others) but the toxicity of weathered petroleum is not as well established. The toxicity of Prudhoe Bay crude oil and No. 2 fuel oil to embryos of mallard ducks (Anas platyrhynchos) decreased only after 3 weeks and 2 weeks of weathering on a large container of fresh water (SZARO et al. 1980). Ten microliters (uL) of 4 week-old Libyan crude oil caused a significant increase in mortality among embryos of Louisiana herons (Hydranassa tricolor) but the same amount of fresh oil did not cause a significant increase in mortality. However, embryos of laughing gulls (Larus atricilla) were not significantly affected by I0 uL of 4 or 8 week-old weathered Libyan crude oil nor i0 UL of fresh oil (MACKO& KING 1980). Crude ell (i0 uL) recovered from the water surface (age unknown, but presumably slightly weathered) near the IXTOC-I oil spill site in the Gulf of Mexico did not significantly reduce the survival of mallard embryos by day 18 of incubation (D. HOFFMAN, unpublished data).
","language":"English","publisher":"Springer","doi":"10.1007/bf01607706","usgsCitation":"Albers, P., and Gay, M.L., 1982, Unweathered and weathered aviation kerosine: Chemical characterization and effects on hatching success of duck eggs: Bulletin of Environmental Contamination and Toxicology, v. 28, no. 4, p. 430-434, https://doi.org/10.1007/bf01607706.","productDescription":"5 p.","startPage":"430","endPage":"434","numberOfPages":"5","costCenters":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":196578,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"28","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49dfe4b07f02db5e37ad","contributors":{"authors":[{"text":"Albers, P.H.","contributorId":26646,"corporation":false,"usgs":true,"family":"Albers","given":"P.H.","email":"","affiliations":[],"preferred":false,"id":334712,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Gay, M. L.","contributorId":91191,"corporation":false,"usgs":true,"family":"Gay","given":"M.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":334713,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":5221792,"text":"5221792 - 1982 - Parathion accumulation in cricket frogs and its effect on American kestrels","interactions":[],"lastModifiedDate":"2020-03-27T07:15:21","indexId":"5221792","displayToPublicDate":"1982-06-16T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2480,"text":"Journal of Toxicology and Environmental Health","active":true,"publicationSubtype":{"id":10}},"title":"Parathion accumulation in cricket frogs and its effect on American kestrels","docAbstract":"Adult cricket frogs (Acris crepitans) were held individually for 96 h in static systems containing initial concentrations of either 0, 0.1, 1.0, or 10 ppm parathion in 10 ml water. Mortality of cricket frogs was directly related to the parathion concentration in the water. Frogs from the 1.0- and 10-ppm groups accumulated 0.08 and 4.6 ppm parathion, respectively. One of four American kestrels (Falco sparverius) fed frogs from the 10-ppm group died from organophosphate poisoning less than 3 h after consuming five frogs. Mortality did not occur in kestrels fed frogs from the other treatment groups, which represented more environmentally realistic levels of exposure.","language":"English","publisher":"Taylor and Francis","doi":"10.1080/15287398209530306","usgsCitation":"Fleming, W.J., de Chacin, H., Pattee, O.H., and Lamont, T.G., 1982, Parathion accumulation in cricket frogs and its effect on American kestrels: Journal of Toxicology and Environmental Health, v. 10, no. 6, p. 921-927, https://doi.org/10.1080/15287398209530306.","productDescription":"7 p.","startPage":"921","endPage":"927","numberOfPages":"7","costCenters":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":193463,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"10","issue":"6","noUsgsAuthors":false,"publicationDate":"2009-10-20","publicationStatus":"PW","scienceBaseUri":"4f4e4b1be4b07f02db6a88e4","contributors":{"authors":[{"text":"Fleming, W. James","contributorId":85279,"corporation":false,"usgs":true,"family":"Fleming","given":"W.","email":"","middleInitial":"James","affiliations":[],"preferred":false,"id":334695,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"de Chacin, H.","contributorId":27960,"corporation":false,"usgs":true,"family":"de Chacin","given":"H.","email":"","affiliations":[],"preferred":false,"id":334692,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Pattee, O. H.","contributorId":46459,"corporation":false,"usgs":true,"family":"Pattee","given":"O.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":334693,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Lamont, T. G.","contributorId":51252,"corporation":false,"usgs":true,"family":"Lamont","given":"T.","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":334694,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":70011231,"text":"70011231 - 1982 - Deep oxygenated ground water: Anomaly or common occurrence?","interactions":[],"lastModifiedDate":"2025-12-22T16:17:48.139798","indexId":"70011231","displayToPublicDate":"1982-06-11T00:00:00","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":"Deep oxygenated ground water: Anomaly or common occurrence?","docAbstract":"Contrary to the prevailing notion that oxygen-depleting reactions in the soil zone and in the aquifer rapidly reduce the dissolved oxygen content of recharge water to detection limits, 2 to 8 milligrams per liter of dissolved oxygen is present in water from a variety of deep (100 to 1000 meters) aquifers in Nevada, Arizona, and the hot springs of the folded Appalachians and Arkansas. Most of the waters sampled are several thousand to more than 10,000 years old, and some are 80 kilometers from their point of recharge.
","language":"English","publisher":"American Association for the Advancement of Science","doi":"10.1126/science.216.4551.1227","issn":"00368075","usgsCitation":"Winograd, I., and Robertson, F.N., 1982, Deep oxygenated ground water: Anomaly or common occurrence?: Science, v. 216, no. 4551, p. 1227-1230, https://doi.org/10.1126/science.216.4551.1227.","productDescription":"4 p.","startPage":"1227","endPage":"1230","costCenters":[],"links":[{"id":221034,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"216","issue":"4551","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059fe27e4b0c8380cd4eb59","contributors":{"authors":[{"text":"Winograd, I.J.","contributorId":10408,"corporation":false,"usgs":true,"family":"Winograd","given":"I.J.","affiliations":[],"preferred":false,"id":360621,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Robertson, F. N.","contributorId":66737,"corporation":false,"usgs":true,"family":"Robertson","given":"F.","email":"","middleInitial":"N.","affiliations":[],"preferred":false,"id":360622,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70011708,"text":"70011708 - 1982 - Uraniferous opal, Virgin Valley, Nevada: Conditions of formation and implications for uranium exploration","interactions":[],"lastModifiedDate":"2025-04-08T17:10:15.793994","indexId":"70011708","displayToPublicDate":"1982-06-04T00:00:00","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":"Uraniferous opal, Virgin Valley, Nevada: Conditions of formation and implications for uranium exploration","docAbstract":"Uraniferous, fluorescent opal, which occurs in tuffaceous sedimentary rocks at Virgin Valley, Nevada, records the temperature and composition of uranium-rich solutions as well as the time of uranium-silica coprecipitation. Results are integrated with previous geologic and geochronologic data for the area to produce a model for uranium mobility that may be used to explore for uranium deposits in similar geologic settings.
Uraniferous opal occurs as replacements of diatomite, or silicic air-fall ash layers in tuffaceous lakebeds of the Virgin Valley Formation (Miocene) of Merriam (1907). Fission-track radiography shows uranium to be homogeneously dispersed throughout the opal structure, suggesting coprecipitation of dissolved uranium and silica gel. Fluid inclusions preserved within opal replacements of diatomite have homogenization temperatures in the epithermal range and are of low salinity. Four samples of opal from one locality all have U-Pb apparent ages which suggest uraniferous opal precipitation in late Pliocene time. These ages correspond to a period of local, normal faulting, and highangle faults may have served as vertical conduits for transport of deep, thermalized ground water to shallower levels. Lateral migration of rising solutions occurred at intersections of faults with permeable strata. Silica and some uranium were dissolved from silica-rich host strata of 5–20 ppm original uranium content and reprecipitated as the solutions cooled. The model predicts that in similar geologic settings, ore-grade concentrations of uranium will occur in permeable strata that intersect high-angle faults and that contain uranium source rocks as well as efficient reductant traps for uranium. In the absence of sufficient quantities of reductant materials, uranium will be flushed from the system or will accumulate in low-grade disseminated hosts such as uraniferous opal.
","language":"English","publisher":"Elsevier","doi":"10.1016/0375-6742(82)90010-3","usgsCitation":"Zielinski, R.A., 1982, Uraniferous opal, Virgin Valley, Nevada: Conditions of formation and implications for uranium exploration: Journal of Geochemical Exploration, v. 16, no. 3, p. 197-216, https://doi.org/10.1016/0375-6742(82)90010-3.","productDescription":"20 p.","startPage":"197","endPage":"216","costCenters":[],"links":[{"id":221384,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Nevada","county":"Humboldt County","otherGeospatial":"Virgin 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R. A. 0000-0002-4047-5129","orcid":"https://orcid.org/0000-0002-4047-5129","contributorId":106930,"corporation":false,"usgs":true,"family":"Zielinski","given":"R.","email":"","middleInitial":"A.","affiliations":[{"id":164,"text":"Central Energy Resources Science Center","active":true,"usgs":true}],"preferred":false,"id":361778,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70011860,"text":"70011860 - 1982 - Hydrogeochemical prospecting for porphyry copper deposits in the tropical-marine climate of Puerto Rico","interactions":[],"lastModifiedDate":"2025-04-09T15:02:15.596022","indexId":"70011860","displayToPublicDate":"1982-06-04T00:00:00","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":"Hydrogeochemical prospecting for porphyry copper deposits in the tropical-marine climate of Puerto Rico","docAbstract":"A hydrogeochemical survey utilizing waters from streams and springs was conducted in the area of two known porphyry copper deposits in the tropical-marine climate of westcentral Puerto Rico. The most important pathfinder for regional hydrogeochemical surveys is sulfate which reflects the associated pyrite mineralization. Because of increased mobility due to intense chemical weathering and the low pH environment, dissolved copper can also be used as a pathfinder for regional surveys and has the advantage of distinguishing barren pyrite from pyrite associated with copper mineralization. For follow-up surveys, the most important pathfinders are copper, sulfate, pH, zinc, and fluoride. High concentrations of dissolved copper and moderate concentrations of sulfate is a diagnostic indication of nearby sources of copper minerals.
An understanding of the geochemical processes taking place in the streambeds and the weathering environment, such as the precipitation of secondary copper minerals, contributes to the interpretation of the geochemical data and the selection of the most favorable areas for further exploration.
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The relatively slight degree of scatter of the points defining the isochron is probably due to initial Pb isotope inhomogeneity, and the resulting inferred persistence of closed system behavior for U and Pb is probably the result of the long-term presence of U- and Pb-immobilizing H 2 S. 206 Pb/ 238 U systematics are badly scattered owing to long-term migration of radioactive daughters of 238 U. Beta- and gamma-activity systematics of the ores consistently identify those with grossly anomalous Pb isotope systematics, however, and proved highly useful in identifying ores that have gained gross amounts of uranium daughters.FeS 2 minerals in the altered tongue of the host sandstone are characterized by abundant postore pyrite and heavy delta 34 S values, whereas FeS 2 minerals in mineralized and unaltered, barren rock are characterized by abundant ore-stage marcasite and by light delta 34 S values. The delta 34 S values of FeS 2 minerals in the altered tongue are similar to those defined for sour gas from the underlying Edwards Limestone of Cretaceous age, indicating the probable source for the sulfur of an inferred resulfidization event. The 5.07-m.y. isochron age probably reflects the end of roll-front development; we believe that the end was due to the resulfidization and does not preclude significant earlier periods of mineralization. Modern ground water in the area is also sulfide bearing (thus helping preserve the deposit), but with delta 34 S values distinct from those of sulfides in the resulfidized zone of the host rock.
","language":"English","publisher":"Society of Economic Geologists","doi":"10.2113/gsecongeo.77.3.557","usgsCitation":"Ludwig, K., Goldhaber, M.B., Reynolds, R.L., and Simmons, K., 1982, Uranium-lead isochron age and preliminary sulfur isotope systematics of the Felder uranium deposit, south Texas: Economic Geology, v. 77, no. 3, p. 557-563, https://doi.org/10.2113/gsecongeo.77.3.557.","productDescription":"8 p.","startPage":"557","endPage":"563","costCenters":[{"id":318,"text":"Geosciences and Environmental Change Science Center","active":true,"usgs":true}],"links":[{"id":374165,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Texas","county":"Live Oak County","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"Polygon\",\"coordinates\":[[[-98.0037,28.6896],[-98.0894,28.6599],[-98.0167,28.5323],[-97.8084,28.1788],[-97.8136,28.1757],[-97.8896,28.1253],[-97.8991,28.1185],[-97.9007,28.1167],[-97.9018,28.1135],[-97.9008,28.1108],[-97.9009,28.1071],[-97.902,28.1048],[-97.9047,28.0998],[-97.9059,28.0934],[-97.9041,28.0846],[-97.9021,28.079],[-97.9013,28.0726],[-97.8988,28.0684],[-97.8963,28.0646],[-97.8943,28.0609],[-97.8923,28.0595],[-98.2338,28.0607],[-98.3343,28.06],[-98.3358,28.4775],[-98.336,28.4982],[-98.3363,28.6117],[-98.099,28.7882],[-98.0037,28.6896]]]},\"properties\":{\"name\":\"Live Oak\",\"state\":\"TX\"}}]}","volume":"77","issue":"3","noUsgsAuthors":false,"publicationDate":"1982-05-01","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":787598,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Goldhaber, Martin B. 0000-0002-1785-4243 mgold@usgs.gov","orcid":"https://orcid.org/0000-0002-1785-4243","contributorId":1339,"corporation":false,"usgs":true,"family":"Goldhaber","given":"Martin","email":"mgold@usgs.gov","middleInitial":"B.","affiliations":[{"id":171,"text":"Central Mineral and Environmental Resources Science Center","active":true,"usgs":true},{"id":211,"text":"Crustal Geophysics and Geochemistry Science Center","active":true,"usgs":true}],"preferred":true,"id":787599,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"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":787600,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Simmons, Kathleen R. ksimmons@usgs.gov","contributorId":140955,"corporation":false,"usgs":true,"family":"Simmons","given":"Kathleen R.","email":"ksimmons@usgs.gov","affiliations":[{"id":318,"text":"Geosciences and Environmental Change Science Center","active":true,"usgs":true}],"preferred":false,"id":787601,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":70011634,"text":"70011634 - 1982 - Temperature dependence of unsaturated hydraulic conductivity of two soils","interactions":[],"lastModifiedDate":"2025-07-31T16:09:17.289365","indexId":"70011634","displayToPublicDate":"1982-05-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3420,"text":"Soil Science Society of America Journal","active":true,"publicationSubtype":{"id":10}},"title":"Temperature dependence of unsaturated hydraulic conductivity of two soils","docAbstract":"Packed columns of Oakley sand (mixed, mesic Typic Paleudalfs) and Hanford sandy loam (mixed, nonacid, thermic Typic Xerorthents) were used to develop isothermal steady-state fluxes. Soil matric potentials were measured and unsaturated hydraulic conductivities were calculated over a range of matric potentials at 2°, 25°, and 45° ± 0.5°C. In addition, water retention characteristics (to −100 kPa) were measured at these same temperatures for both soils. In this paper, the calculated results are compared to an equation that relates unsaturated conductivity to the intrinsic permeability, the relative permeability, and the viscosity of water. The equation considers viscosity to be the only parameter that changes with temperature. The results show a much greater temperature dependence in the unsaturated conductivity than would be predicted by this equation. The results indicate that the relative permeability may be a function of temperature. The temperature dependence of the soil water matric potential, surface tension, and diffuse double-layer thickness are discussed in terms of their possible interaction with the unsaturated conductivity values obtained. A case is presented for further study to isolate these temperature-sensitive parameters as well as additional parameters related to fluid flow path changes with temperature.
","language":"English","publisher":"Wiley","doi":"10.2136/sssaj1982.03615995004600030005x","issn":"03615995","usgsCitation":"Constantz, J., 1982, Temperature dependence of unsaturated hydraulic conductivity of two soils: Soil Science Society of America Journal, v. 46, no. 3, p. 466-470, https://doi.org/10.2136/sssaj1982.03615995004600030005x.","productDescription":"5 p.","startPage":"466","endPage":"470","costCenters":[],"links":[{"id":221189,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"46","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505ba4c3e4b08c986b32057c","contributors":{"authors":[{"text":"Constantz, Jim","contributorId":66338,"corporation":false,"usgs":true,"family":"Constantz","given":"Jim","affiliations":[],"preferred":false,"id":361583,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":1003330,"text":"1003330 - 1982 - Acute and chronic toxicity studies with monochlorobenzene in rainbow trout","interactions":[],"lastModifiedDate":"2023-03-03T19:32:28.301109","indexId":"1003330","displayToPublicDate":"1982-05-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":874,"text":"Aquatic Toxicology","active":true,"publicationSubtype":{"id":10}},"title":"Acute and chronic toxicity studies with monochlorobenzene in rainbow trout","docAbstract":"The toxicity of monochlorobenzene (CB) was investigated in rainbow trout following acute intraperitoneal (i.p.) administration and chronic exposure via the water in a continuously flowing system for 15 or 30 days.
In the acute study overt toxicity and hepatotoxicity were monitored over a 96-h time period. Variables measured to assess toxicity included weight changes, liver weight to body weight ratios, behavioral changes, alanine aminotransferase activity (GPT), sulfobromophthalein (BSP) retention, total plasma protein concentration and liver histopathology. In the chronic study the same measures of toxicity were followed as well as food consumption and alkaline phosphatase (AP) activity.
Upon acute i.p. exposure the toxicant (9.8 mmol/kg) caused behavioral changes in the fish which were consistent with the known anesthetic properties of CB in mammals. Elevations in BSP retention and GPT activity, and histopathology indicated that CB was hepatotoxic in fish.
The LC50 of CB in trout exposed via the water for 96 h was 4.7 mg/l. Chronic exposure of trout to 2 or 3 mg/l CB resulted in similar behavioral changes as seen in the acute study. Liver toxicity was evident from elevations in GPT activity. BSP retention and AP activity appeared to be affected by the nutritional status of the trout as much as by the CB treatment. After 30 days of exposure to 3 mg/l CB, trout appeared to have developed some tolerance to the toxic effects.
","language":"English","publisher":"Elsevier","doi":"10.1016/0166-445X(82)90011-X","usgsCitation":"Dalich, G.M., Larson, R.E., and Gingerich, W.H., 1982, Acute and chronic toxicity studies with monochlorobenzene in rainbow trout: Aquatic Toxicology, v. 2, p. 127-142, https://doi.org/10.1016/0166-445X(82)90011-X.","productDescription":"16 p.","startPage":"127","endPage":"142","numberOfPages":"16","costCenters":[{"id":606,"text":"Upper Midwest Environmental Sciences Center","active":true,"usgs":true}],"links":[{"id":134228,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b05e4b07f02db699bf1","contributors":{"authors":[{"text":"Dalich, George M.","contributorId":302873,"corporation":false,"usgs":false,"family":"Dalich","given":"George","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":313120,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Larson, R. E.","contributorId":15583,"corporation":false,"usgs":false,"family":"Larson","given":"R.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":313118,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Gingerich, William H.","contributorId":36086,"corporation":false,"usgs":true,"family":"Gingerich","given":"William","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":313119,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":70180852,"text":"70180852 - 1982 - Lakes and lake-like waters of the Hawaiian Archipelago","interactions":[],"lastModifiedDate":"2017-02-03T15:24:38","indexId":"70180852","displayToPublicDate":"1982-04-30T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":5287,"text":"Occasional Papers Bernice P. Bishop Museum","active":true,"publicationSubtype":{"id":10}},"title":"Lakes and lake-like waters of the Hawaiian Archipelago","docAbstract":"This summary of Hawaiian lacustrine limnology is based on 12 years of field and literature surveys of archipelagic inland waters. Lakes here are distinguished from other standing waters by limits on surface oceanic area (> 0.1 ha) and depth (> 2 m), and by the absence of flatural surface oceanic connection. A variety of extinct and existing water bodies, sometimes referred to as lakes, are noted. Six lakes are described. Five of them are in crater basins, 3 are freshwater, and 2 are elevated (highest = 3969 m). The scarcity of elevated lakes results from general permeability of the substrata. Among the 6 lakes, surface areas range from 0.22 to 88 ha and maximum depths from 3 to 248 m. Naturally occurring aquatic biota generally is low in species diversity except for phytoplankton; fishes and submersed vascular plants are absent. Two lowland lakes, freshwater Green (Wai a Pele) and saline Kauhak6, are described for the first time. Profundal Kauhak6, 248 m deep, has a surface area of only 0.35 ha, which results in an extraordinary relative depth of 370%. It is permanently stratified, a condition apparently due primarily to the unique morphometry of its basin.
No abstract available.
","language":"English","publisher":"Federal Inter-Agency Sedimentation Project","usgsCitation":"Skinner, J.V., 1982, A fluid density gage for measuring suspended-sediment concentration, Part A. Gage response to steady-state and transient conditions: Report X, 125 p.","productDescription":"125 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":392,"text":"Minnesota Water Science Center","active":true,"usgs":true}],"links":[{"id":327054,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"57b82dabe4b03fd6b7da3600","contributors":{"authors":[{"text":"Skinner, J. V.","contributorId":32504,"corporation":false,"usgs":true,"family":"Skinner","given":"J.","email":"","middleInitial":"V.","affiliations":[],"preferred":false,"id":646467,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70175873,"text":"70175873 - 1982 - Services provided by the Federal Inter-Agency Sedimentation Project","interactions":[],"lastModifiedDate":"2018-04-02T10:47:37","indexId":"70175873","displayToPublicDate":"1982-04-02T14:15:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":1,"text":"Federal Government Series"},"title":"Services provided by the Federal Inter-Agency Sedimentation Project","docAbstract":"No abstract available.
","language":"English","publisher":"Federal Inter-Agency Sedimentation Project","usgsCitation":"Skinner, J.V., and Benson, D., 1982, Services provided by the Federal Inter-Agency Sedimentation Project, 2 p.","productDescription":"2 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":392,"text":"Minnesota Water Science Center","active":true,"usgs":true}],"links":[{"id":327061,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"57b82de5e4b03fd6b7da39b4","contributors":{"authors":[{"text":"Skinner, J. V.","contributorId":32504,"corporation":false,"usgs":true,"family":"Skinner","given":"J.","email":"","middleInitial":"V.","affiliations":[],"preferred":false,"id":646476,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Benson, D.A.","contributorId":173876,"corporation":false,"usgs":false,"family":"Benson","given":"D.A.","email":"","affiliations":[],"preferred":false,"id":646477,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70170908,"text":"70170908 - 1982 - Status of water-resources projects in Minnesota, fiscal year 1982","interactions":[],"lastModifiedDate":"2018-03-12T11:53:15","indexId":"70170908","displayToPublicDate":"1982-04-01T11:45:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"title":"Status of water-resources projects in Minnesota, fiscal year 1982","docAbstract":"No abstract available.
","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"St. Paul, MN","doi":"10.3133/70170908","usgsCitation":"Hein, M., 1982, Status of water-resources projects in Minnesota, fiscal year 1982, 61 p., https://doi.org/10.3133/70170908.","productDescription":"61 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":392,"text":"Minnesota Water Science Center","active":true,"usgs":true}],"links":[{"id":321083,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"country":"United 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\"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"57330636e4b0dae0d5dcd224","contributors":{"authors":[{"text":"Hein, M.D.","contributorId":169239,"corporation":false,"usgs":false,"family":"Hein","given":"M.D.","email":"","affiliations":[],"preferred":false,"id":629046,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70185626,"text":"70185626 - 1982 - On conducting the modified ‘Slug’ test in tight formations","interactions":[],"lastModifiedDate":"2020-03-09T19:49:29","indexId":"70185626","displayToPublicDate":"1982-04-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3722,"text":"Water Resources Research","onlineIssn":"1944-7973","printIssn":"0043-1397","active":true,"publicationSubtype":{"id":10}},"title":"On conducting the modified ‘Slug’ test in tight formations","docAbstract":"The method introduced by Bredehoeft and Papadopulos (1980) for conducting a modified ‘slug’ test in tight formations does not assure the condition of approximate equilibrium necessary at the start of the test. In addition, compressibility in the shut-in well can be significantly larger than the compressibility of water, which Bredehoeft and Papadopulos indicate should be used in the calculations. Errors that may result from using the original test procedure are discussed, and a modified procedure and testing arrangement are presented.
","language":"English","publisher":"American Geophysical Union","doi":"10.1029/WR018i002p00439","usgsCitation":"Neuzil, C., 1982, On conducting the modified ‘Slug’ test in tight formations: Water Resources Research, v. 18, no. 2, p. 439-441, https://doi.org/10.1029/WR018i002p00439.","productDescription":"3 p. ","startPage":"439","endPage":"441","costCenters":[{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":338327,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"18","issue":"2","noUsgsAuthors":false,"publicationDate":"2010-07-09","publicationStatus":"PW","scienceBaseUri":"58d63042e4b05ec799131125","contributors":{"authors":[{"text":"Neuzil, C.E. 0000-0003-2022-4055","orcid":"https://orcid.org/0000-0003-2022-4055","contributorId":60401,"corporation":false,"usgs":true,"family":"Neuzil","given":"C.E.","email":"","affiliations":[],"preferred":false,"id":686153,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70185630,"text":"70185630 - 1982 - Volatilization of ketones from water","interactions":[],"lastModifiedDate":"2020-01-26T09:56:15","indexId":"70185630","displayToPublicDate":"1982-04-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3728,"text":"Water, Air, & Soil Pollution","onlineIssn":"1573-2932","printIssn":"0049-6979","active":true,"publicationSubtype":{"id":10}},"title":"Volatilization of ketones from water","docAbstract":"The overall mass-transfer coefficients for the volatilization from water of acetone, 2-butanone, 2-pentanone, 3-pentanone, 4-methyl-2-pentanone, 2-heptanone, and 2-octanone were measured simultaneously with the oxygen-absorption coefficient in a laboratory stirred water bath. The liquid-film and gas-film coefficients of the two-film model were determined for the ketones from the overall coefficients, and both film resistances were important for volatilization of the ketones.
The liquid-film coefficients for the ketones varied with the 0.719 power of the molecular-diffusion coefficient, in agreement with the literature. The liquid-film coefficients showed a variable dependence on molecular weight, with the dependence ranging from the −0.263 power for acetone to the −0.378 power for 2-octanone. This is in contrast with the literature where a constant −0.500 power dependence on the molecular weight is assumed.
The gas-film coefficients for the ketones showed no dependence on molecular weight, in contrast with the literature where a −0.500 power is assumed.
","language":"English","publisher":"D. Reidel Publishing Co","doi":"10.1007/BF00283158","usgsCitation":"Rathbun, R.E., and Tai, D.Y., 1982, Volatilization of ketones from water: Water, Air, & Soil Pollution, v. 17, no. 3, p. 281-293, https://doi.org/10.1007/BF00283158.","productDescription":"13 p.","startPage":"281","endPage":"293","costCenters":[{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":338331,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"17","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"58d63041e4b05ec799131123","contributors":{"authors":[{"text":"Rathbun, R. E.","contributorId":61796,"corporation":false,"usgs":true,"family":"Rathbun","given":"R.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":686162,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Tai, D. Y.","contributorId":59778,"corporation":false,"usgs":true,"family":"Tai","given":"D.","email":"","middleInitial":"Y.","affiliations":[],"preferred":false,"id":686163,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70230870,"text":"70230870 - 1982 - California's Central Valley wintering waterfowl: Concerns and challenges","interactions":[],"lastModifiedDate":"2022-04-27T14:00:43.950118","indexId":"70230870","displayToPublicDate":"1982-03-26T08:47:02","publicationYear":"1982","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"seriesTitle":{"id":5322,"text":"Transactions of the North American Wildlife and Natural Resources Conference","printIssn":"0078-1355","active":true,"publicationSubtype":{"id":19}},"title":"California's Central Valley wintering waterfowl: Concerns and challenges","docAbstract":"No abstract available.
","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Transactions of the 47th North American Wildlife and Natural Resources Conference","largerWorkSubtype":{"id":12,"text":"Conference publication"},"conferenceTitle":"47th North American Wildlife and Natural Resources Conference","conferenceDate":"March 26-31, 1982","conferenceLocation":"Portland, Oregon, United States","language":"English","publisher":"Wildlife Management Institute","publisherLocation":"Washington, D. C.","usgsCitation":"Gilmer, D.S., Miller, M.R., Bauer, R.D., and LeDonne, J.R., 1982, California's Central Valley wintering waterfowl: Concerns and challenges, in Transactions of the 47th North American Wildlife and Natural Resources Conference, Portland, Oregon, United States, March 26-31, 1982, p. 441-452.","productDescription":"12 p.","startPage":"441","endPage":"452","costCenters":[],"links":[{"id":399741,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":399740,"rank":1,"type":{"id":15,"text":"Index Page"},"url":"https://wildlifemanagement.institute/store/product/37"}],"country":"United States","state":"California","otherGeospatial":"Central Valley, Delta & Suisun Marsh, Sacramento Valley, San Joaquin Valley","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -121.84936523437499,\n 40.81380923056958\n ],\n [\n -122.508544921875,\n 40.78054143186033\n ],\n [\n -122.64038085937499,\n 40.522150985623796\n ],\n [\n -122.991943359375,\n 40.36328834091583\n ],\n [\n -122.684326171875,\n 39.96870074491696\n ],\n [\n -122.71728515624999,\n 39.825413103424786\n ],\n [\n -122.618408203125,\n 39.757879992021756\n ],\n [\n -122.76123046875,\n 39.26628442213066\n ],\n [\n -122.607421875,\n 39.13006024213511\n ],\n [\n -122.37670898437499,\n 38.839707613545144\n ],\n [\n -122.06909179687501,\n 38.565347844885466\n ],\n [\n -122.135009765625,\n 38.35888785866677\n ],\n [\n -122.54150390625,\n 38.18638677411551\n ],\n [\n -122.45361328124999,\n 37.82280243352756\n ],\n [\n -122.025146484375,\n 37.57070524233116\n ],\n [\n -121.56372070312499,\n 37.64903402157866\n ],\n [\n -121.22314453124999,\n 37.23032838760387\n ],\n [\n -120.80566406250001,\n 36.80928470205937\n ],\n [\n -120.4541015625,\n 36.36822190085111\n ],\n [\n -120.44311523437499,\n 36.05798104702501\n ],\n [\n -120.16845703125,\n 35.82672127366604\n ],\n [\n -119.44335937499999,\n 34.94899072578227\n ],\n [\n -119.0478515625,\n 34.95799531086792\n ],\n [\n -118.85009765625,\n 34.84085858477277\n ],\n [\n -118.49853515625,\n 35.02099970111467\n ],\n [\n -118.67431640625,\n 35.12889434101051\n ],\n [\n -118.564453125,\n 35.290468565908775\n ],\n [\n -118.68530273437501,\n 35.44277092585766\n ],\n [\n -118.68530273437501,\n 36.00467348670187\n ],\n [\n -119.080810546875,\n 36.527294814546245\n ],\n [\n -119.278564453125,\n 36.83566824724438\n ],\n [\n -119.564208984375,\n 37.15156050223665\n ],\n [\n -119.66308593749999,\n 37.42252593456307\n ],\n [\n -120.0146484375,\n 37.59682400108367\n ],\n [\n -120.25634765624999,\n 37.97884504049713\n ],\n [\n -120.56396484375,\n 38.324420427006544\n ],\n [\n -120.92651367187499,\n 38.92522904714054\n ],\n [\n -121.19018554687499,\n 39.138581990583525\n ],\n [\n -121.40991210937499,\n 39.740986355883564\n ],\n [\n -121.86035156249999,\n 40.204050425113294\n ],\n [\n -121.728515625,\n 40.47202439692057\n ],\n [\n -121.84936523437499,\n 40.81380923056958\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Gilmer, David S.","contributorId":59508,"corporation":false,"usgs":true,"family":"Gilmer","given":"David","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":841521,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Miller, Michael R.","contributorId":45796,"corporation":false,"usgs":false,"family":"Miller","given":"Michael","email":"","middleInitial":"R.","affiliations":[{"id":12709,"text":"Department of Animal Science, University of California, Davis, One Shields Avenue, Davis, CA 95616, USA","active":true,"usgs":false}],"preferred":false,"id":841522,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Bauer, Richard D.","contributorId":290672,"corporation":false,"usgs":false,"family":"Bauer","given":"Richard","email":"","middleInitial":"D.","affiliations":[{"id":6987,"text":"U.S. Fish and Wildlife Sevice","active":true,"usgs":false}],"preferred":false,"id":841523,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"LeDonne, John R.","contributorId":290673,"corporation":false,"usgs":false,"family":"LeDonne","given":"John","email":"","middleInitial":"R.","affiliations":[{"id":12939,"text":"California Department of Fish and Game","active":true,"usgs":false}],"preferred":false,"id":841524,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":1007586,"text":"1007586 - 1982 - Lumber spill in central California waters: Implications for oil spills and sea otters","interactions":[],"lastModifiedDate":"2025-12-22T16:51:02.150891","indexId":"1007586","displayToPublicDate":"1982-03-19T00:00:00","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":"Lumber spill in central California waters: Implications for oil spills and sea otters","docAbstract":"A large quantity of lumber was spilled in the ocean off central California during the winter of 1978, and it spread through most of the range of the threatened California sea otter population within 4 weeks. The movement rates of lumber were similar to those of oil slicks observed elsewhere. These observations indicate that a major oil spill could expose significant numbers of California sea otters to oil contamination.
","language":"English","publisher":"American Association for the Advancement of Science","doi":"10.1126/science.215.4539.1503","usgsCitation":"VanBlaricom, G., and Jameson, R., 1982, Lumber spill in central California waters: Implications for oil spills and sea otters: Science, v. 215, no. 4539, p. 1503-1505, https://doi.org/10.1126/science.215.4539.1503.","productDescription":"3 p.","startPage":"1503","endPage":"1505","costCenters":[{"id":651,"text":"Western Ecological Research Center","active":true,"usgs":true}],"links":[{"id":129872,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"California","otherGeospatial":"central California","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -125.01453001470827,\n 39.194787155092456\n ],\n [\n -120.48460325212284,\n 33.48450467089073\n ],\n [\n -118.28209449425341,\n 34.280736888845524\n ],\n [\n -121.64372529379582,\n 39.398525519817156\n ],\n [\n -125.01453001470827,\n 39.194787155092456\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","volume":"215","issue":"4539","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a7fe4b07f02db6489e2","contributors":{"authors":[{"text":"VanBlaricom, G.R.","contributorId":94239,"corporation":false,"usgs":true,"family":"VanBlaricom","given":"G.R.","email":"","affiliations":[],"preferred":false,"id":315671,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Jameson, R.J.","contributorId":56581,"corporation":false,"usgs":true,"family":"Jameson","given":"R.J.","email":"","affiliations":[],"preferred":false,"id":315670,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70011801,"text":"70011801 - 1982 - Molecular size of aquatic humic substances","interactions":[],"lastModifiedDate":"2025-03-19T15:47:43.144793","indexId":"70011801","displayToPublicDate":"1982-03-05T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2958,"text":"Organic Geochemistry","active":true,"publicationSubtype":{"id":10}},"title":"Molecular size of aquatic humic substances","docAbstract":"Aquatic humic substances, which account for 30 to 50% of the organic carbon in water, are a principal component of aquatic organic matter. The molecular size of aquatic humic substances, determined by small-angle X-ray scattering, varies from 4.7 to 33 Å in their radius of gyration, corresponding to a molecular weight range of 500 to greater than 10,000. The aquatic fulvic acid fraction contains substances with molecular weights ranging from 500 to 2000 and is monodisperse, whereas the aquatic humic acid fraction contains substances with molecular weights ranging from 1000 to greater than 10,000 and is generally polydisperse.
","language":"English","publisher":"Elsevier","doi":"10.1016/0146-6380(82)90005-5","usgsCitation":"Thurman, E., Wershaw, R., Malcolm, R., and Pinckney, D., 1982, Molecular size of aquatic humic substances: Organic Geochemistry, v. 4, no. 1, p. 27-35, https://doi.org/10.1016/0146-6380(82)90005-5.","productDescription":"9 p.","startPage":"27","endPage":"35","costCenters":[],"links":[{"id":220994,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Arizona, Colorado, Hawaii, Florida, Massachusetts, Minnesota, North Dakota, South Dakota, Wyoming","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"MultiPolygon\",\"coordinates\":[[[[-112.538593,37.000674],[-109.045223,36.999084],[-109.050044,31.332502],[-111.125646,31.348978],[-114.813613,32.494277],[-114.463127,32.901884],[-114.701165,33.086368],[-114.722872,33.398779],[-114.542011,33.542481],[-114.52868,33.947817],[-114.163122,34.255187],[-114.630682,34.866352],[-114.569238,35.18348],[-114.755618,36.087166],[-114.114531,36.095217],[-113.965907,37.000025],[-112.538593,37.000674]]],[[[-104.053249,41.001406],[-102.124972,41.002338],[-102.04192,37.035083],[-109.045223,36.999084],[-109.050076,41.000659],[-111.046723,40.997959],[-111.055199,45.001321],[-104.057698,44.997431],[-103.992467,48.999567],[-95.153711,48.998903],[-95.153314,49.384358],[-94.878454,49.333193],[-94.640803,48.741171],[-93.818375,48.534442],[-92.984963,48.623731],[-92.634931,48.542873],[-92.698824,48.494892],[-92.341207,48.23248],[-92.066269,48.359602],[-91.542512,48.053268],[-90.88548,48.245784],[-90.703702,48.096009],[-89.489226,48.014528],[-90.735927,47.624343],[-92.058888,46.809938],[-92.025789,46.710839],[-92.189091,46.717541],[-92.291976,46.503997],[-92.33859,46.050111],[-92.869193,45.717568],[-92.646602,45.441635],[-92.807362,44.758909],[-91.410555,43.970892],[-91.244135,43.774667],[-91.243183,43.540309],[-96.591213,43.500514],[-96.439335,43.113916],[-96.630311,42.770885],[-96.483592,42.510345],[-97.302075,42.86566],[-98.035034,42.764205],[-98.568936,42.998537],[-104.053127,43.000585],[-104.053249,41.001406]]],[[[-81.582923,24.658732],[-81.451267,24.747464],[-81.298028,24.656774],[-81.765993,24.552103],[-81.582923,24.658732]]],[[[-84.777208,29.707398],[-84.696726,29.76993],[-85.036219,29.588919],[-84.777208,29.707398]]],[[[-82.255777,26.703437],[-82.038403,26.456907],[-82.186441,26.489221],[-82.255777,26.703437]]],[[[-80.250581,25.34193],[-80.611693,24.93842],[-80.192336,25.473331],[-80.250581,25.34193]]],[[[-83.309455,30.634417],[-82.287343,30.573458],[-82.101416,30.366556],[-81.962739,30.813636],[-81.472597,30.713312],[-81.256711,29.784693],[-80.567361,28.562353],[-80.566432,28.09563],[-80.031362,26.796339],[-80.152896,25.702855],[-80.229107,25.732509],[-80.495341,25.199463],[-81.079859,25.118797],[-81.362272,25.824401],[-81.727086,25.907207],[-81.868983,26.378648],[-82.094748,26.48393],[-82.076349,26.958263],[-82.147068,26.789803],[-82.301736,26.841588],[-82.714521,27.500415],[-82.393383,27.837519],[-82.716522,27.958398],[-82.566819,27.858002],[-82.721622,27.663908],[-82.851126,27.8863],[-82.674787,28.441956],[-82.702618,28.932955],[-83.679219,29.918513],[-84.245668,30.093021],[-84.335953,29.912962],[-85.343619,29.672004],[-85.405052,29.938487],[-86.222561,30.343585],[-87.518324,30.280435],[-87.395941,30.643968],[-87.626228,30.857127],[-87.548543,30.997927],[-85.057534,31.000585],[-84.887522,30.741791],[-83.309455,30.634417]]],[[[-155.778234,20.245743],[-155.149215,19.922872],[-154.838545,19.463642],[-155.505281,19.137908],[-155.658486,18.924835],[-155.88155,19.036644],[-156.051652,19.703649],[-155.835312,19.976078],[-155.901452,20.235787],[-155.778234,20.245743]]],[[[-159.431707,22.220015],[-159.295271,22.13039],[-159.408284,21.897781],[-159.788139,22.018411],[-159.699978,22.165252],[-159.431707,22.220015]]],[[[-157.014553,21.185503],[-156.742231,21.176214],[-156.865795,21.057801],[-157.254061,21.090601],[-157.185553,21.205602],[-157.014553,21.185503]]],[[[-156.612012,21.02477],[-155.991534,20.713654],[-156.444242,20.607941],[-156.464043,20.781667],[-156.688969,20.888673],[-156.612012,21.02477]]],[[[-157.010001,20.929757],[-156.838321,20.764575],[-156.949009,20.738997],[-157.010001,20.929757]]],[[[-158.044485,21.306011],[-158.250671,21.557373],[-158.018127,21.699955],[-157.6619,21.3131],[-158.044485,21.306011]]],[[[-70.59628,41.471905],[-70.450431,41.420703],[-70.496162,41.346452],[-70.802083,41.314207],[-70.59628,41.471905]]],[[[-70.092142,41.297741],[-69.960277,41.278731],[-70.256164,41.288123],[-70.092142,41.297741]]],[[[-73.022903,42.741133],[-71.351874,42.698154],[-70.886136,42.88261],[-70.595474,42.660336],[-70.996097,42.271222],[-70.754488,42.228673],[-70.471552,41.761563],[-70.008462,41.800786],[-70.169781,42.059736],[-70.082624,42.054657],[-69.928261,41.6917],[-70.902763,41.421061],[-70.658659,41.543385],[-70.623652,41.707398],[-71.12057,41.497448],[-71.458104,42.017762],[-73.508142,42.086257],[-73.264957,42.74594],[-73.022903,42.741133]]]]},\"properties\":{\"name\":\"Arizona\",\"nation\":\"USA \"}}]}","volume":"4","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a5d12e4b0c8380cd70137","contributors":{"authors":[{"text":"Thurman, E.M.","contributorId":102864,"corporation":false,"usgs":true,"family":"Thurman","given":"E.M.","affiliations":[],"preferred":false,"id":361988,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Wershaw, R.L.","contributorId":62223,"corporation":false,"usgs":true,"family":"Wershaw","given":"R.L.","affiliations":[],"preferred":false,"id":361987,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Malcolm, Ronald L.","contributorId":46075,"corporation":false,"usgs":true,"family":"Malcolm","given":"Ronald L.","affiliations":[],"preferred":false,"id":361986,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Pinckney, D.J.","contributorId":23175,"corporation":false,"usgs":true,"family":"Pinckney","given":"D.J.","affiliations":[],"preferred":false,"id":361985,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":5221736,"text":"5221736 - 1982 - Accumulation of 14C-naphthalene in the tissues of redhead ducks fed oil-contaminated crayfish","interactions":[],"lastModifiedDate":"2023-12-12T17:38:13.870888","indexId":"5221736","displayToPublicDate":"1982-03-01T12:19:29","publicationYear":"1982","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":887,"text":"Archives of Environmental Contamination and Toxicology","active":true,"publicationSubtype":{"id":10}},"displayTitle":"Accumulation of 14C-naphthalene in the tissues of redhead ducks fed oil-contaminated crayfish","title":"Accumulation of 14C-naphthalene in the tissues of redhead ducks fed oil-contaminated crayfish","docAbstract":"Crayfish, artificially contaminated with14C-naphthalene-5% water-soluble fraction of No. 2 fuel oil, were force-fed to one-year-old redhead ducks to determine the accumulation of petroleum hydrocarbons. The relative distribution of carbon-14 activity in the gall bladder containing bile, and fat were similar, and significantly greater (P < 0.05) than the activity in the blood, brain, liver, and kidney. There was a significant increase (P < 0.05) in the disintegrations per minute per gram (dpm/g) in the blood, brain, kidney, and liver between days 1 and 3 of feeding, indicating a progressive accumulation of carbon-14 activity (naphthalene and presumably its metabolites). There was no significant effect of sex or the interaction of the duration of feeding and sex on carbon-14 activity in any of the tissues. The low daily dose of petroleum hydrocarbons (a total of approximately 1.25 mg/day) received by the ducks from the crayfish and the relatively short feeding regimen did not cause any overt signs of toxicity in the ducks.
","language":"English","publisher":"Springer","doi":"10.1007/BF01054891","usgsCitation":"Tarshis, I., and Rattner, B., 1982, Accumulation of 14C-naphthalene in the tissues of redhead ducks fed oil-contaminated crayfish: Archives of Environmental Contamination and Toxicology, v. 11, no. 2, p. 155-159, https://doi.org/10.1007/BF01054891.","productDescription":"5 p.","startPage":"155","endPage":"159","numberOfPages":"5","costCenters":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":196673,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"11","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b13e4b07f02db6a35dc","contributors":{"authors":[{"text":"Tarshis, I. Barry","contributorId":82378,"corporation":false,"usgs":true,"family":"Tarshis","given":"I. Barry","affiliations":[],"preferred":false,"id":334560,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Rattner, Barnett A. 0000-0003-3676-2843","orcid":"https://orcid.org/0000-0003-3676-2843","contributorId":95843,"corporation":false,"usgs":true,"family":"Rattner","given":"Barnett A.","affiliations":[{"id":50464,"text":"Eastern Ecological Science Center","active":true,"usgs":true}],"preferred":true,"id":334561,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70208505,"text":"70208505 - 1982 - Survival of duck plague virus in water from Lake Andes National Wildlife Refuge, South Dakota","interactions":[],"lastModifiedDate":"2020-03-11T09:52:25","indexId":"70208505","displayToPublicDate":"1982-02-12T10:54:12","publicationYear":"1982","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2507,"text":"Journal of Wildlife Diseases","active":true,"publicationSubtype":{"id":10}},"title":"Survival of duck plague virus in water from Lake Andes National Wildlife Refuge, South Dakota","docAbstract":"An isolant of duck plague herpesvirus from the Lake Andes Refuge outbreak was seeded in raw and filter-decontaminated water from two locations on the refuge, held at 4 C, and assayed for infectivity intermittently over a period of 2 mo. From an initial level of about 105 PFU per ml, infectivity in the filtered samples uniformly dropped to about 104 PFU per ml. Infectivity in the raw samples declined much more rapidly; infectious virus remaining at the end of 2 mo (ca. 101 PFU per ml) was only about 0.01% of that originally seeded.
","language":"English","publisher":"BioOne","doi":"10.7589/0090-3558-18.4.437","usgsCitation":"Wolf, K., and Burke, C., 1982, Survival of duck plague virus in water from Lake Andes National Wildlife Refuge, South Dakota: Journal of Wildlife Diseases, v. 18, no. 4, p. 437-440, https://doi.org/10.7589/0090-3558-18.4.437.","productDescription":"4 p.","startPage":"437","endPage":"440","costCenters":[{"id":365,"text":"Leetown Science Center","active":true,"usgs":true}],"links":[{"id":480256,"rank":0,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.7589/0090-3558-18.4.437","text":"Publisher Index Page"},{"id":372276,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"South Dakota","county":"Charles Mix County","otherGeospatial":"Lake Andes National Wildlife 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