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,{"id":70006615,"text":"70006615 - 1982 - Freshwater aspects of anadromous salmonid enhancement","interactions":[],"lastModifiedDate":"2014-05-30T09:53:38","indexId":"70006615","displayToPublicDate":"1982-01-01T09:45:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":1,"text":"Federal Government Series"},"seriesTitle":{"id":49,"text":"NOAA Technical Report NMFS Circular","active":false,"publicationSubtype":{"id":1}},"seriesNumber":"447","title":"Freshwater aspects of anadromous salmonid enhancement","docAbstract":"<p>Freshwater enhancement of anadromous salmonid populations has been practiced in the United States and Canada since the late 1800's. Reduction of natural spawning habitat and increasing fishing pressure make artificial enhancement a possible alternative to declining populations.</p>\n<br>\n<p>Enhancement of anadromous salmonids involved improvement of the natural environment and reducing natural mortality. Methods of enhancement include fishways, spawning and rearing channels, stream rehabilitation, lake fertilization, environmental management, and artificial propagation techniques.</p>\n<br>\n<p>Five Pacific salmon species and steelhead trout are commonly enhanced, primarily in watershed entering the Pacific Ocean and Great Lakes. Enhancement efforts contribute heavily to a commercial and sport industry realizing over $1.5 billion.</p>","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Proceedings of the the eighth U.S.-Japan meeting on aquaculture at Bellingham, Washington, October 17-18, 1979","largerWorkSubtype":{"id":1,"text":"Federal Government Series"},"language":"English","publisher":"National Marine Fisheries Service","publisherLocation":"Silver Spring, MD","usgsCitation":"Gould, R.W., 1982, Freshwater aspects of anadromous salmonid enhancement: NOAA Technical Report NMFS Circular 447, 2 p.","productDescription":"2 p.","startPage":"21","endPage":"22","numberOfPages":"2","costCenters":[{"id":365,"text":"Leetown Science Center","active":true,"usgs":true}],"links":[{"id":287849,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53ae76cee4b0abf75cf2c026","contributors":{"authors":[{"text":"Gould, Rowan W.","contributorId":84271,"corporation":false,"usgs":true,"family":"Gould","given":"Rowan","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":354867,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":908,"text":"908 - 1982 - Water resources data: North Dakota","interactions":[],"lastModifiedDate":"2014-07-09T09:23:55","indexId":"908","displayToPublicDate":"1982-01-01T09:22:04","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"title":"Water resources data: North Dakota","docAbstract":"No abstract available.","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"U.S. Geological Survey water-supply paper","largerWorkSubtype":{"id":6,"text":"USGS Unnumbered Series"},"language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/908","collaboration":"Prepared in cooperation with the state of North Dakota","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1982, Water resources data: North Dakota, https://doi.org/10.3133/908.","costCenters":[],"links":[{"id":289585,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"country":"United States","state":"North Dakota","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -104.05,45.9351 ], [ -104.05,49.0007 ], [ -96.5545,49.0007 ], [ -96.5545,45.9351 ], [ -104.05,45.9351 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53be6491e4b0527d5d4097ef","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":527823,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70120392,"text":"70120392 - 1982 - Results of a modeling workshop concerning economic and environmental trends and concomitant resource management issues in the Mobile Bay area","interactions":[],"lastModifiedDate":"2014-08-14T09:36:52","indexId":"70120392","displayToPublicDate":"1982-01-01T09:19:54","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":9,"text":"Other Report"},"title":"Results of a modeling workshop concerning economic and environmental trends and concomitant resource management issues in the Mobile Bay area","docAbstract":"<p>During the past decade, the southern regions of the U.S. have experienced rapid change which is expected to continue into the foreseeable future.  Growth in population, industry, and resource development has been attributed to a variety of advantages such as an abundant and inexpensive labor force, a mild climate, and the availability of energy, water, land, and other natural resources.  While this growth has many benefits for the region, it also creates the potential for increased air, water, and solid waste pollution, and modification of natural habitats.</p>\n<br/>\n<p>A workshop was convened to consider the Mobile Bay area as a site-specific case of growth and its environmental consequences in the southern region.  The objectives of the modeling workshop were to: (1) identify major factors of economic development as they relate to growth in the area over the immediate and longer term; (2) identify major environmental and resource management issues associated with this expected growth; and (3) identify and characterize the complex interrelationships among economic and environmental factors.  This report summarizes the activities and results of a modeling workshop concerning economic growth and concomitant resource management issues in the Mobile Bay area.</p>\n<br/>\n<p>The workshop was organized around construction of a simulation model representing the relationships between a series of actions and indicators identified by participants.  The workshop model had five major components.  An Industry Submodel generated scenarios of growth in several industrial and transportation sectors.  A Human Population/Economy Submodel calculated human population and economic variables in response to employment opportunities.  A Land Use/Air Quality Submodel tabulated changes in land use, shoreline use, and air quality.  A Water Submodel calculated indicators of water quality and quantity for fresh surface water, ground water, and Mobile Bay based on discharge information provided by the Industry and Human Population/Economy Submodels.  Finally, a Fish Submodel calculated indicators of habitat quality for finfish and shellfish, utilizing information on water quality and wetlands acreage.</p>\n<br/>\n<p>The workshop was successful in identifying many of the critical interrelations between components of the Mobile area system.  Not all of those interactions, such as the feedback of air quality as a limitation on development, could be incorporated into the workshop model because of the model's broad spatial scale and because of uncertainties or data gaps.  Thus, the value of the modeling workshop was in the areas outlines below, rather than in the predictive power of the initial model developed at the workshop.</p>\n<br/>\n<p>First, participants developed a holistic perspective on the interactions which will determine future economic and environmental trends within the Mobile Bay area.  Potential environmental consequences and limitations to grown identified at the workshop included: shoreline and water access; water quality of Mobile Bay; finfish and shellfish habitat quality with respect to dissolved oxygen and coliforms; air quality; and acreage of critical wetland habitat.  Second, the model's requirements for specific, quantitative information stimulated supporting analyses, such as economic input-output calculations, which provide additional insight into the Mobile Bay area system.  Third, the perspective of the Mobile area as an interacting system was developed in an open, cooperative forum which my provide a foundation for conflict resolution based on common understanding.  Finally, the identification of model limitations and uncertainties should be useful in guiding the efficient allocation of future research effort.</p>","language":"English","publisher":"U.S. Fish and Wildlife Service, Western Energy and Land Use Team","publisherLocation":"Fort Collins, CO","usgsCitation":"Hamilton, D.B., Andrews, A.K., Auble, G.T., Ellison, R.A., Johnson, R.A., Roelle, J.E., and Staley, M.J., 1982, Results of a modeling workshop concerning economic and environmental trends and concomitant resource management issues in the Mobile Bay area, 84 p.","productDescription":"84 p.","numberOfPages":"84","costCenters":[],"links":[{"id":292147,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Alabama","otherGeospatial":"Mobile Bay","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -88.109396,30.26461 ], [ -88.109396,30.673552 ], [ -87.91553,30.673552 ], [ -87.91553,30.26461 ], [ -88.109396,30.26461 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53edcd4fe4b0f61b386d2453","contributors":{"authors":[{"text":"Hamilton, David B. hamiltond@usgs.gov","contributorId":193,"corporation":false,"usgs":true,"family":"Hamilton","given":"David","email":"hamiltond@usgs.gov","middleInitial":"B.","affiliations":[],"preferred":true,"id":498128,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Andrews, Austin K.","contributorId":85516,"corporation":false,"usgs":true,"family":"Andrews","given":"Austin","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":498134,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Auble, Gregor T. 0000-0002-0843-2751 aubleg@usgs.gov","orcid":"https://orcid.org/0000-0002-0843-2751","contributorId":2187,"corporation":false,"usgs":true,"family":"Auble","given":"Gregor","email":"aubleg@usgs.gov","middleInitial":"T.","affiliations":[{"id":291,"text":"Fort Collins Science Center","active":true,"usgs":true}],"preferred":true,"id":498129,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Ellison, Richard A.","contributorId":19087,"corporation":false,"usgs":true,"family":"Ellison","given":"Richard","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":498131,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Johnson, Richard A.","contributorId":81420,"corporation":false,"usgs":true,"family":"Johnson","given":"Richard","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":498133,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"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":498130,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Staley, Michael J.","contributorId":77859,"corporation":false,"usgs":true,"family":"Staley","given":"Michael","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":498132,"contributorType":{"id":1,"text":"Authors"},"rank":7}]}}
,{"id":905,"text":"905 - 1982 - Water resources data: New Mexico","interactions":[],"lastModifiedDate":"2014-07-09T09:00:51","indexId":"905","displayToPublicDate":"1982-01-01T08:59:12","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"title":"Water resources data: New Mexico","docAbstract":"No abstract available.","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"U.S. Geological Survey water-supply paper","largerWorkSubtype":{"id":6,"text":"USGS Unnumbered Series"},"language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/905","issn":"0364-4065","collaboration":"Prepared in cooperation with the state of New Mexico and with other agencies","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1982, Water resources data: New Mexico, https://doi.org/10.3133/905.","costCenters":[],"links":[{"id":289580,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"country":"United States","state":"New Mexico","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -109.0502,31.3322 ], [ -109.0502,37.0003 ], [ -103.002,37.0003 ], [ -103.002,31.3322 ], [ -109.0502,31.3322 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53be6490e4b0527d5d4097e9","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":527820,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":903,"text":"903 - 1982 - Water resources data: New Hampshire and Vermont","interactions":[],"lastModifiedDate":"2014-07-09T08:47:00","indexId":"903","displayToPublicDate":"1982-01-01T08:44:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"title":"Water resources data: New Hampshire and Vermont","docAbstract":"No abstract available.","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"U.s. Geological Survey water-supply paper","largerWorkSubtype":{"id":6,"text":"USGS Unnumbered Series"},"language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/903","collaboration":"Prepared in cooperation with states of New Hampshire and Vermont and with other agencies","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1982, Water resources data: New Hampshire and Vermont, https://doi.org/10.3133/903.","costCenters":[],"links":[{"id":289577,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"country":"United States","state":"New Hampshire;Vermont","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -73.4636,42.7454 ], [ -73.4636,45.3055 ], [ -70.6027,45.3055 ], [ -70.6027,42.7454 ], [ -73.4636,42.7454 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53be648ee4b0527d5d4097e5","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":527818,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70120387,"text":"70120387 - 1982 - HEP as a planning tool: an application to waterfowl enhancement","interactions":[],"lastModifiedDate":"2014-08-14T08:43:06","indexId":"70120387","displayToPublicDate":"1982-01-01T08:41:31","publicationYear":"1982","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3638,"text":"Transactions of the North American Wildlife and Natural Resources Conference","active":true,"publicationSubtype":{"id":10}},"title":"HEP as a planning tool: an application to waterfowl enhancement","docAbstract":"To many, the principal role of wildlife agencies in public and private resource development has been that of impact mitigation. With known or pending habitat damage, biologists have to develop mitigation or compensation plans. Unfortunately, once in a mitigation framework, they are in a no-win situation, seeking remedial action at best. Yet, the potential exists for cooperative project planning, thereby facilitating mitigation of impacts before they occur, and enhancement of environmental amenities through project development. In fact, such planning is mandated by federal legislation (e.g., National Environmental Policy Act, Fish and Wildlife Coordination Act, Outdoor Recreation Act, etc.).","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Transactions of the North American Wildlife and Natural Resources Conference","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"Wildlife Management Institute","publisherLocation":"Washington, D.C.","usgsCitation":"Matulich, S.C., Hanson, J.E., Lines, I., and Farmer, A., 1982, HEP as a planning tool: an application to waterfowl enhancement: Transactions of the North American Wildlife and Natural Resources Conference, v. 47, 1 p.","productDescription":"1 p.","numberOfPages":"1","costCenters":[],"links":[{"id":292135,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"47","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53edcd4ce4b0f61b386d2415","contributors":{"authors":[{"text":"Matulich, Scott C.","contributorId":25479,"corporation":false,"usgs":true,"family":"Matulich","given":"Scott","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":498113,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hanson, Jeffrey E.","contributorId":80593,"corporation":false,"usgs":true,"family":"Hanson","given":"Jeffrey","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":498116,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Lines, Ivan","contributorId":61757,"corporation":false,"usgs":true,"family":"Lines","given":"Ivan","email":"","affiliations":[],"preferred":false,"id":498115,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Farmer, Adrian","contributorId":51211,"corporation":false,"usgs":true,"family":"Farmer","given":"Adrian","affiliations":[],"preferred":false,"id":498114,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70094968,"text":"70094968 - 1982 - Compilation of hydrologic data for the Edwards Aquifer, San Antonio area, Texas, 1934-80","interactions":[],"lastModifiedDate":"2016-08-24T10:31:02","indexId":"70094968","displayToPublicDate":"1982-01-01T08:33:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":2,"text":"State or Local Government Series"},"seriesTitle":{"id":5177,"text":"Edwards Underground Water District Bulletin","active":true,"publicationSubtype":{"id":2}},"seriesNumber":"40","title":"Compilation of hydrologic data for the Edwards Aquifer, San Antonio area, Texas, 1934-80","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"Edwards Underground Water District","publisherLocation":"San Antonia, TX","collaboration":"Prepared in cooperation with the U.S. Geological Survey  and the Texas Department of Water Resources","usgsCitation":"Reeves, R., Maclay, R., and Davis, M., 1982, Compilation of hydrologic data for the Edwards Aquifer, San Antonio area, Texas, 1934-80: Edwards Underground Water District Bulletin 40, 128 p.","productDescription":"128 p.","numberOfPages":"134","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"links":[{"id":282804,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/70094968.JPG"},{"id":284821,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/unnumbered/70094968/report.pdf"}],"country":"United States","state":"Texas","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -100.7971,29.0834 ], [ -100.7971,30.2330 ], [ -97.7105,30.2330 ], [ -97.7105,29.0834 ], [ -100.7971,29.0834 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"57c6aef0e4b0f2f0cebe460a","contributors":{"authors":[{"text":"Reeves, R.D.","contributorId":95043,"corporation":false,"usgs":true,"family":"Reeves","given":"R.D.","email":"","affiliations":[],"preferred":false,"id":491008,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Maclay, R.W.","contributorId":72804,"corporation":false,"usgs":true,"family":"Maclay","given":"R.W.","affiliations":[],"preferred":false,"id":491006,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Davis, M.F.","contributorId":79400,"corporation":false,"usgs":true,"family":"Davis","given":"M.F.","email":"","affiliations":[],"preferred":false,"id":491007,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":1001440,"text":"1001440 - 1982 - Wetlands and deepwater habitats: a new classification","interactions":[],"lastModifiedDate":"2012-02-02T00:04:11","indexId":"1001440","displayToPublicDate":"1982-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2456,"text":"Journal of Soil and Water Conservation","active":true,"publicationSubtype":{"id":10}},"title":"Wetlands and deepwater habitats: a new classification","docAbstract":"Abstract has not been submitted","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Journal of Soil and Water Conservation","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","usgsCitation":"Cowardin, L., 1982, Wetlands and deepwater habitats: a new classification: Journal of Soil and Water Conservation, v. 37, no. 2, p. 83-85.","productDescription":"p. 83-85","startPage":"83","endPage":"85","numberOfPages":"2","costCenters":[],"links":[{"id":129014,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"37","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e2e4b07f02db5e49b4","contributors":{"authors":[{"text":"Cowardin, L.M.","contributorId":106435,"corporation":false,"usgs":true,"family":"Cowardin","given":"L.M.","email":"","affiliations":[],"preferred":false,"id":311030,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70142169,"text":"70142169 - 1982 - Evaluating depth to shallow groundwater using Heat Capacity Mapping Mission (HCMM) data","interactions":[],"lastModifiedDate":"2017-01-18T14:51:34","indexId":"70142169","displayToPublicDate":"1982-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3052,"text":"Photogrammetric Engineering and Remote Sensing","active":true,"publicationSubtype":{"id":10}},"title":"Evaluating depth to shallow groundwater using Heat Capacity Mapping Mission (HCMM) data","docAbstract":"<p>Four dates of Heat Capacity Mapping Mission (HCMM) data were analyzed to evaluate the utility of HCMM thermal data for evaluating depth to shallow groundwater. During the summer, shallow water tables can create lower soil temperatures throughout the diurnal temperature cycle. Because of large spatial and temporal ground cover variations, HCMM daytime radiometric temperatures alone did not correlate with water table depth. The radiometric temperatures consisted of radiance contributions from different crop canopies and their respective soil backgrounds. However, when surface soil temperatures were empirically estimated from HCMM temperatures and percent cover of each pixel, significant correlations were obtained between estimated soil temperatures and water table depth. Correlations increased as the season progressed and temperature gradients within the soil profile increased. However, estimated soil temperatures were also correlated with near-surface soil moisture since during the daytime, increasing soil moisture reduced surface soil temperature. Complementary effects of shallow water tables and soil moisture on daytime temperatures cannot be separated.</p>","language":"English","publisher":"American Society for Photogrammetry and Remote Sensing","usgsCitation":"Heilman, J.L., and Moore, D.G., 1982, Evaluating depth to shallow groundwater using Heat Capacity Mapping Mission (HCMM) data: Photogrammetric Engineering and Remote Sensing, v. 48, no. 12, p. 1903-1906.","productDescription":"4 p.","startPage":"1903","endPage":"1906","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":222,"text":"Earth Resources Observation and Science (EROS) Center","active":true,"usgs":true}],"links":[{"id":298206,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"48","issue":"12","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"54f597c7e4b02419550d2f42","contributors":{"authors":[{"text":"Heilman, J. L.","contributorId":85723,"corporation":false,"usgs":true,"family":"Heilman","given":"J.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":541655,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Moore, Donald G.","contributorId":41146,"corporation":false,"usgs":true,"family":"Moore","given":"Donald","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":541656,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70011474,"text":"70011474 - 1982 - Nutrient exchange across the sediment-water interface in the Potomac River estuary","interactions":[],"lastModifiedDate":"2023-10-12T16:48:54.757023","indexId":"70011474","displayToPublicDate":"1982-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1587,"text":"Estuarine, Coastal and Shelf Science","active":true,"publicationSubtype":{"id":10}},"title":"Nutrient exchange across the sediment-water interface in the Potomac River estuary","docAbstract":"<p>The flux of ammonia, phosphate, silica and radon-222 from Potomac tidal river and estuary sediments is controlled by processes occurring at the sediment-water interface and within surficial sediment. Calculated diffusive fluxes range between 0·6 and 6·5 mmol m<sup>−2</sup><span>&nbsp;</span>day<sup>−1</sup><span>&nbsp;</span>for ammonia, 0·020 and 0·30 mmol m<sup>−2</sup><span>&nbsp;</span>day<sup>−1</sup><span>&nbsp;</span>for phosphate, and 1·3 and 3·8 mmol m<sup>−2</sup><span>&nbsp;</span>day<sup>−1</sup><span>&nbsp;</span>for silica. Measured<span>&nbsp;</span><i>in situ</i><span>&nbsp;</span>fluxes range between 1 and 21 mmol m<sup>−2</sup><span>&nbsp;</span>day<sup>−1</sup><span>&nbsp;</span>for ammonia, 0·1 and 2·0 mmol m<sup>−2</sup><span>&nbsp;</span>day<sup>−1</sup><span>&nbsp;</span>for phosphate, and 2 and 19 mmol m<sup>−2</sup><span>&nbsp;</span>day<sup>−1</sup><span>&nbsp;</span>for silica. The ratio of<span>&nbsp;</span><i>in situ</i><span>&nbsp;</span>fluxes to diffusive fluxes (flux enhancement) varied between 1·6 and 5·2 in the tidal river, between 2·0 and 20 in the transition zone, and from 1·3 to 5·1 in the lower estuary. The large flux enhancements from transition zone sediments are attributed to macrofaunal irrigation. Nutrient flux enhancements are correlated with radon flux enhancements, suggesting that fluxes may originate from a common region and that nutrients are regenerated within the upper 10–20 cm of the sediment column.</p><p>The low fluxes of phosphate from tidal viver sediments reflect the control benthic sediment exerts on phosphorus through sorption by sedimentary iron oxyhydroxides. In the tidal river, benthic fluxes of ammonia and phosphate equal one-half and one-third of the nutrient input of the Blue Plains sewage treatment plant. In the tidal Potomac River, benthic sediment regeneration supplies a significant fraction of the nutrients utilized by primary producers in the water column during the summer months.</p>","language":"English","publisher":"Elsevier","doi":"10.1016/0272-7714(82)90050-6","issn":"02727714","usgsCitation":"Callender, E., and Hammond, D.E., 1982, Nutrient exchange across the sediment-water interface in the Potomac River estuary: Estuarine, Coastal and Shelf Science, v. 15, no. 4, p. 395-413, https://doi.org/10.1016/0272-7714(82)90050-6.","productDescription":"19 p.","startPage":"395","endPage":"413","costCenters":[],"links":[{"id":220710,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Maryland, Virginia","otherGeospatial":"Potomac River Estuary","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      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Douglas E.","contributorId":67878,"corporation":false,"usgs":true,"family":"Hammond","given":"Douglas","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":361197,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70011408,"text":"70011408 - 1982 - A comparison of four streamflow record extension techniques","interactions":[],"lastModifiedDate":"2018-02-05T13:24:20","indexId":"70011408","displayToPublicDate":"1982-01-01T00:00:00","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":"A comparison of four streamflow record extension techniques","docAbstract":"<p><span>One approach to developing time series of streamflow, which may be used for simulation and optimization studies of water resources development activities, is to extend an existing gage record in time by exploiting the interstation correlation between the station of interest and some nearby (long-term) base station. Four methods of extension are described, and their properties are explored. The methods are regression (REG), regression plus noise (RPN), and two new methods, maintenance of variance extension types 1 and 2 (MOVE.l, MOVE.2). MOVE.l is equivalent to a method which is widely used in psychology, biometrics, and geomorphology and which has been called by various names, e.g., ‘line of organic correlation,’ ‘reduced major axis,’ ‘unique solution,’ and ‘equivalence line.’ The methods are examined for bias and standard error of estimate of moments and order statistics, and an empirical examination is made of the preservation of historic low-flow characteristics using 50-year-long monthly records from seven streams. The REG and RPN methods are shown to have serious deficiencies as record extension techniques. MOVE.2 is shown to be marginally better than MOVE.l, according to the various comparisons of bias and accuracy.</span></p>","language":"English","publisher":"American Geophysical Union","doi":"10.1029/WR018i004p01081","usgsCitation":"Hirsch, R.M., 1982, A comparison of four streamflow record extension techniques: Water Resources Research, v. 18, no. 4, p. 1081-1088, https://doi.org/10.1029/WR018i004p01081.","productDescription":"8 p.","startPage":"1081","endPage":"1088","costCenters":[],"links":[{"id":220770,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"18","issue":"4","noUsgsAuthors":false,"publicationDate":"2010-07-09","publicationStatus":"PW","scienceBaseUri":"5059e35be4b0c8380cd45fbe","contributors":{"authors":[{"text":"Hirsch, Robert M. 0000-0002-4534-075X rhirsch@usgs.gov","orcid":"https://orcid.org/0000-0002-4534-075X","contributorId":2005,"corporation":false,"usgs":true,"family":"Hirsch","given":"Robert","email":"rhirsch@usgs.gov","middleInitial":"M.","affiliations":[{"id":502,"text":"Office of Surface Water","active":true,"usgs":true},{"id":436,"text":"National Research Program - Eastern Branch","active":true,"usgs":true},{"id":37778,"text":"WMA - Integrated Modeling and Prediction Division","active":true,"usgs":true},{"id":37316,"text":"WMA - Integrated Information Dissemination Division","active":true,"usgs":true}],"preferred":true,"id":361017,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70011792,"text":"70011792 - 1982 - The solubility of quartz in aqueous sodium chloride solution at 350°C and 180 to 500 bars","interactions":[],"lastModifiedDate":"2015-06-05T14:13:41","indexId":"70011792","displayToPublicDate":"1982-01-01T00:00:00","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":"The solubility of quartz in aqueous sodium chloride solution at 350°C and 180 to 500 bars","docAbstract":"<p><span>The solubility of quartz in 2, 3, and 4 molal NaCl was measured at 350&deg;C and pressures ranging from 180 to 500 bars. The molal solubility in each of the salt solutions is greater than that in pure water throughout the measured pressure range, with the ratio of solubility in NaCl solution to solubility in pure water decreasing as pressure is increased. The measured solubilities are significantly higher than solubilities calculated using a simple model in which the water activity in NaCl solutions decreases either in proportion to decreasing vapor pressure of the solution as salinity is increased or in proportion to decreasing mole fraction of water in the solvent.</span></p>","language":"English","publisher":"Elsevier","doi":"10.1016/0016-7037(82)90136-3","issn":"00167037","usgsCitation":"Fournier, R.O., Rosenbauer, R.J., and Bischoff, J.L., 1982, The solubility of quartz in aqueous sodium chloride solution at 350°C and 180 to 500 bars: Geochimica et Cosmochimica Acta, v. 46, no. 10, p. 1975-1978, https://doi.org/10.1016/0016-7037(82)90136-3.","productDescription":"4 p.","startPage":"1975","endPage":"1978","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":220791,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"46","issue":"10","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505bb042e4b08c986b324d3a","contributors":{"authors":[{"text":"Fournier, Robert O.","contributorId":73202,"corporation":false,"usgs":true,"family":"Fournier","given":"Robert","email":"","middleInitial":"O.","affiliations":[],"preferred":false,"id":361969,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Rosenbauer, Robert J. brosenbauer@usgs.gov","contributorId":204,"corporation":false,"usgs":true,"family":"Rosenbauer","given":"Robert","email":"brosenbauer@usgs.gov","middleInitial":"J.","affiliations":[{"id":520,"text":"Pacific Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":true,"id":361968,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Bischoff, James L. jbischoff@usgs.gov","contributorId":1389,"corporation":false,"usgs":true,"family":"Bischoff","given":"James","email":"jbischoff@usgs.gov","middleInitial":"L.","affiliations":[],"preferred":true,"id":361967,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70011811,"text":"70011811 - 1982 - Seasonal growth in the bivalve Macoma balthica near the southern limit of its range","interactions":[],"lastModifiedDate":"2020-09-02T17:41:34.917836","indexId":"70011811","displayToPublicDate":"1982-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1583,"text":"Estuaries","active":true,"publicationSubtype":{"id":10}},"title":"Seasonal growth in the bivalve Macoma balthica near the southern limit of its range","docAbstract":"<p>Shell-length growth in Macoma balthica from San Francisco Bay, California, as measured on living animals in situ, is highly seasonal despite a mild Mediterranean climate: a long period of near non-growth from May to the following February is followed by a short period of rapid growth between March and May. The rapid-growth period follows the spawning period during January/February and ends as water temperature rises above about 15??C. Despite the shortness of the growth period, M. balthica grows larger at a given age in San Francisco Bay than is recorded elsewhere in the world. Application of a model, developed elsewhere from these same field measurements, shows that (1) measurable growth occurs during the summer/autumn/early winter \"nongrowth\" period, (2) there is an autumn recruitment, and (3) both spring and autumn recruits combine to form a single \"one-year-old\" size grouping. None of these features is detectable through growth-ring analysis of field samples, apparently because of indistinct climatic seasons, or through size-frequency histogram analysis because of the combined effects of slow growth and intermittent recruitment. ?? 1982 Estuarine Research Federation.</p>","language":"English","publisher":"Springer-Verlag","doi":"10.2307/1352108","issn":"15592723","usgsCitation":"Nichols, F., and Thompson, J., 1982, Seasonal growth in the bivalve Macoma balthica near the southern limit of its range: Estuaries, v. 5, no. 2, p. 110-120, https://doi.org/10.2307/1352108.","startPage":"110","endPage":"120","numberOfPages":"11","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":552,"text":"San Francisco Bay-Delta","active":false,"usgs":true},{"id":5079,"text":"Pacific Regional Director's Office","active":true,"usgs":true}],"links":[{"id":221132,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"5","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505b88ace4b08c986b316ac9","contributors":{"authors":[{"text":"Nichols, F.H.","contributorId":88020,"corporation":false,"usgs":true,"family":"Nichols","given":"F.H.","affiliations":[],"preferred":false,"id":362012,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Thompson, J.K.","contributorId":103300,"corporation":false,"usgs":true,"family":"Thompson","given":"J.K.","email":"","affiliations":[],"preferred":false,"id":362013,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70006531,"text":"70006531 - 1982 - Alewives and rainbow smelt in Lake Huron: midwater and bottom aggregations and estimates of standing stocks","interactions":[],"lastModifiedDate":"2013-02-04T14:24:53","indexId":"70006531","displayToPublicDate":"1982-01-01T00:00:00","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":"Alewives and rainbow smelt in Lake Huron: midwater and bottom aggregations and estimates of standing stocks","docAbstract":"The continued availability of adequate amounts of forage fish, primarily alewives <i>Alosa pseudoharengus</i> and rainbow smelt <i>Osmerus mordax</i>, is critical to the success of ongoing programs aimed at rebuilding lake trout <i>Salvelinus namaycush</i> populations and maintaining other salmonid stocks in Lake Huron. These forage species are distributed at middepths as well as on or near the bottom. Acoustic methods were integrated with midwater and bottom trawling to characterize the population and estimate the biomass of the forage stocks. The average sizes of alewives and rainbow smelt caught at middepths were smaller than those caught in bottom trawls; however, most size ranges in the bottom trawl catches were also present in the midwater catches. Subadult and adult fish (both species) were rarely caught concurrently in midwater and when they were caught together the fish were invariably large subadults and small adults. Biomass estimates for the pelagic component were determined from trawl catches and echogram counts. The regression of echogram counts (<i>X</i>) on trawl catches (<i>Y</i>) was <i>Y</i> = -2.69 + 0.983<i>X</i> (r<sup>2</sup> = 0.766) at the fish densities investigated. The pelagic biomasses of alewives and rainbow smelt in United States waters of Lake Huron were estimated at 17,200 t in July 1974, 22,000 t in July 1975, and 19,000 t in August 1976. Biomass estimates of the stocks in midwater were usually larger in spring than in fall, probably due to seasonal differences in distribution rather than in abundance. Estimates for the demersal component of the combined alewife-rainbow smelt forage stock, calculated from stratified random sampling of the spring bottom trawl catches for 1973 through 1980 went from 35,000 t in 1973, to a high of 83,000 t in 1975, and to 72,000 t in 1980; the estimates in fall went from 31,000 t in 1973, to a high of 56,000 t in 1977, and to 43,000 t in 1980. Biomass estimates calculated from spring catch data were usually larger than those calculated from fall data. Estimates of the midwater stocks, coinciding with the spring and fall bottom trawl surveys, indicated that between 20 and 30% of the total biomass was in midwater.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Transactions of the American Fisheries Society","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"Taylor & Francis","publisherLocation":"London, UK","doi":"10.1577/1548-8659(1982)111<267:AARSIL>2.0.CO;2","collaboration":"Abstract has subscript/superscript to be fixed","usgsCitation":"Argyle, R.L., 1982, Alewives and rainbow smelt in Lake Huron: midwater and bottom aggregations and estimates of standing stocks: Transactions of the American Fisheries Society, v. 111, no. 3, p. 267-285, https://doi.org/10.1577/1548-8659(1982)111<267:AARSIL>2.0.CO;2.","productDescription":"19 p.","startPage":"267","endPage":"285","numberOfPages":"18","costCenters":[{"id":324,"text":"Great Lakes Science Center","active":true,"usgs":true}],"links":[{"id":258398,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1577/1548-8659(1982)111<267:AARSIL>2.0.CO;2","linkFileType":{"id":5,"text":"html"}},{"id":258409,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","otherGeospatial":"Lake Huron","volume":"111","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059e959e4b0c8380cd48206","contributors":{"authors":[{"text":"Argyle, Ray L.","contributorId":9993,"corporation":false,"usgs":true,"family":"Argyle","given":"Ray","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":354690,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70011481,"text":"70011481 - 1982 - Permafrost, heat flow, and the geothermal regime at Prudhoe Bay, Alaska","interactions":[],"lastModifiedDate":"2024-07-16T15:11:03.279817","indexId":"70011481","displayToPublicDate":"1982-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":6453,"text":"Journal of Geophysical Research Solid Earth","active":true,"publicationSubtype":{"id":10}},"title":"Permafrost, heat flow, and the geothermal regime at Prudhoe Bay, Alaska","docAbstract":"<p><span>Temperature measurements through permafrost in the oil field at Prudhoe Bay, Alaska, combined with laboratory measurements of the thermal conductivity of drill cuttings permit an evaluation of in situ thermal properties and an understanding of the general factors that control the geothermal regime. A sharp contrast in temperature gradient at ∼600 m represents a contrast in thermal conductivity caused by the downward change from interstitial ice to interstitial water at the base of permafrost under near steady state conditions. Interpretation of the gradient contrast in terms of a simple model for the conductivity of an aggregate yields the mean ice content (∼39%), and thermal conductivities for the frozen and thawed sections (8.1 and 4.7 mcal/cm s °C, respectively). These results yield a heat flow of ∼1.3 HFU, which is similar to other values on the Alaskan Arctic Coast; the anomalously deep permafrost is a result of the anomalously high conductivity of the siliceous ice-rich sediments. Curvature in the upper 160 m of the temperature profiles represents a warming of ∼1.8°C of the mean surface temperature and a net accumulation of 5–6 kcal/cm</span><sup>2</sup><span>&nbsp;by the solid earth surface during the last 100 years or so. Rising sea level and thawing of ice-rich sea cliffs probably caused the shoreline to retreat tens of kilometers in the last 20,000 years, inundating a portion of the continental shelf that is presently the target of intensive oil exploration. A simple conduction model suggests that this recently inundated region is underlain by near-melting ice-rich permafrost to depths of 300–500 m; its presence is important to seismic interpretations in oil exploration and to engineering considerations in oil production. With confirmation of the permafrost configuration by offshore drilling, heat conduction models can yield reliable new information on the chronology of arctic shorelines.</span></p>","language":"English","publisher":"American Geophysical Union","doi":"10.1029/JB087iB11p09301","issn":"01480227","usgsCitation":"Lachenbruch, A., Sass, J., Marshall, B., and Moses, T.H., 1982, Permafrost, heat flow, and the geothermal regime at Prudhoe Bay, Alaska: Journal of Geophysical Research Solid Earth, v. 87, no. B11, p. 9301-9316, https://doi.org/10.1029/JB087iB11p09301.","productDescription":"16 p.","startPage":"9301","endPage":"9316","numberOfPages":"16","costCenters":[],"links":[{"id":220840,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"87","issue":"B11","noUsgsAuthors":false,"publicationDate":"2012-09-20","publicationStatus":"PW","scienceBaseUri":"505a76a3e4b0c8380cd78223","contributors":{"authors":[{"text":"Lachenbruch, A.H.","contributorId":76737,"corporation":false,"usgs":true,"family":"Lachenbruch","given":"A.H.","affiliations":[],"preferred":false,"id":361216,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Sass, J.H.","contributorId":70749,"corporation":false,"usgs":true,"family":"Sass","given":"J.H.","email":"","affiliations":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"preferred":false,"id":361214,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Marshall, B.V.","contributorId":72375,"corporation":false,"usgs":true,"family":"Marshall","given":"B.V.","affiliations":[],"preferred":false,"id":361215,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Moses, T. H. Jr.","contributorId":70385,"corporation":false,"usgs":true,"family":"Moses","given":"T.","suffix":"Jr.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":361213,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70011798,"text":"70011798 - 1982 - The mobility of uranium and other elements during alteration of rhyolite ash to montmorillonite: A case study in the Troublesome Formation, Colorado, U.S.A.","interactions":[],"lastModifiedDate":"2013-01-21T09:33:28","indexId":"70011798","displayToPublicDate":"1982-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1213,"text":"Chemical Geology","active":true,"publicationSubtype":{"id":10}},"title":"The mobility of uranium and other elements during alteration of rhyolite ash to montmorillonite: A case study in the Troublesome Formation, Colorado, U.S.A.","docAbstract":"An unusual occurrence of juxtaposed glassy and clay-altered ash was sampled to estimate the degree and type of element mobility during alteration of glass to montmorillonite. The results are particularly interesting in that major mobilization of uranium is indicated. Closely spaced samples of glassy and montmorillonitic ash were collected from the same 20-50 cm thick stratigraphic horizon in the Troublesome Formation (Miocene) of northwestern Colorado. Sharp contacts exist between glassy ash and underlying pink montmorillonite and indicate that water-saturated conditions were restricted to basal ash layers. Formation of montmorillonite instead of zeolites suggests that the water was not highly saline or alkaline. Isotopic and chemical analyses of glassy and clay-altered samples indicate the following: 1. (1) Montmorillonite has U concentrations which are only 10-15% of the concentrations in coexisting glass. Similarly depleted elements include Cs, Rb, Na and K. Much smaller depletions of these elements in some glassy samples serve as sensitive indicators of incipient alteration of glass to montmorillonite. 2. (2) Abundances of relatively insoluble elements such as Th, Ta, Hf and Al are slightly higher (5-50%) in clay-altered ash and serve as indicators of the maximum levels of enrichment in residual material. Greater enrichment of elements such as Ca, Mg, Sr, Sc, P, Cr and Co indicate structural incorporation, adsorption, or ion-exchange uptake by clay or secondary hydrous oxides of Fe and Mn. 3. (3) The rare-earth-element patterns and abundances in glass are sufficiently mimicked by detritus-free montmorillonite to document the compositional equivalency of the two. 4. (4) Radioactive equilibrium exists between 238U and its decay products 234U and 230Th. This documents minimal open-system mobility of U within the last ??? 0.3 Ma. ?? 1982.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Chemical Geology","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"Elsevier","doi":"10.1016/0009-2541(82)90001-8","issn":"00092541","usgsCitation":"Zielinski, R.A., 1982, The mobility of uranium and other elements during alteration of rhyolite ash to montmorillonite: A case study in the Troublesome Formation, Colorado, U.S.A.: Chemical Geology, v. 35, no. 3-4, p. 185-204, https://doi.org/10.1016/0009-2541(82)90001-8.","startPage":"185","endPage":"204","numberOfPages":"20","costCenters":[],"links":[{"id":266117,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1016/0009-2541(82)90001-8"},{"id":220933,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"35","issue":"3-4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505baddde4b08c986b323e2f","contributors":{"authors":[{"text":"Zielinski, 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":361980,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70011824,"text":"70011824 - 1982 - Geochemistry of highly basic calcium hydroxide groundwater in Jordan","interactions":[],"lastModifiedDate":"2019-12-16T06:43:26","indexId":"70011824","displayToPublicDate":"1982-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1213,"text":"Chemical Geology","active":true,"publicationSubtype":{"id":10}},"title":"Geochemistry of highly basic calcium hydroxide groundwater in Jordan","docAbstract":"<div id=\"abstracts\" class=\"Abstracts u-font-serif\"><div id=\"aep-abstract-id6\" class=\"abstract author\"><div id=\"aep-abstract-sec-id7\"><p id=\"simple-para.0010\">Highly-alkaline (pH &gt; 12.5) meteoric waters of a Ca<sup>2+</sup>OH<sup>−</sup>-type issue from naturally calcined bituminous marl. The cold (16.5 ≤<span>&nbsp;</span><i>T</i>(°C) ≤ 19.1) waters are super-saturated with minerals thought to be of high-temperature origin.</p></div></div></div>","language":"English","publisher":"Elsevier","doi":"10.1016/0009-2541(82)90024-9","issn":"00092541","usgsCitation":"Barnes, I., Presser, T.S., Saines, M., Dickson, P., and Van Groos, A.F., 1982, Geochemistry of highly basic calcium hydroxide groundwater in Jordan: Chemical Geology, v. 35, no. 1-2, p. 147-154, https://doi.org/10.1016/0009-2541(82)90024-9.","productDescription":"8 p. ","startPage":"147","endPage":"154","numberOfPages":"8","costCenters":[],"links":[{"id":221316,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":266118,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1016/0009-2541(82)90024-9"}],"country":"Jordan ","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"Polygon\",\"coordinates\":[[[35.54567,32.39399],[35.71992,32.70919],[36.83406,32.31294],[38.79234,33.37869],[39.19547,32.16101],[39.00489,32.01022],[37.00217,31.50841],[37.99885,30.5085],[37.66812,30.33867],[37.50358,30.00378],[36.74053,29.86528],[36.50121,29.50525],[36.06894,29.19749],[34.95604,29.35655],[34.9226,29.50133],[35.42092,31.10007],[35.39756,31.48909],[35.54525,31.7825],[35.54567,32.39399]]]},\"properties\":{\"name\":\"Jordan\"}}]}","volume":"35","issue":"1-2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a16fce4b0c8380cd5533d","contributors":{"authors":[{"text":"Barnes, I.","contributorId":23678,"corporation":false,"usgs":true,"family":"Barnes","given":"I.","affiliations":[],"preferred":false,"id":362041,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Presser, T. S.","contributorId":93875,"corporation":false,"usgs":true,"family":"Presser","given":"T.","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":362044,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Saines, M.","contributorId":96827,"corporation":false,"usgs":true,"family":"Saines","given":"M.","email":"","affiliations":[],"preferred":false,"id":362045,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Dickson, P.","contributorId":75272,"corporation":false,"usgs":true,"family":"Dickson","given":"P.","email":"","affiliations":[],"preferred":false,"id":362043,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Van Groos, A. F. K.","contributorId":45457,"corporation":false,"usgs":true,"family":"Van Groos","given":"A.","email":"","middleInitial":"F. K.","affiliations":[],"preferred":false,"id":362042,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":44522,"text":"wri824043 - 1982 - Map showing cumulative thickness of sandstone in the Fox Hills-Lower Hell Creek aquifer, Montana","interactions":[],"lastModifiedDate":"2023-03-15T18:32:18.234504","indexId":"wri824043","displayToPublicDate":"1982-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"82-4043","title":"Map showing cumulative thickness of sandstone in the Fox Hills-Lower Hell Creek aquifer, Montana","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri824043","usgsCitation":"Feltis, R.D., 1982, Map showing cumulative thickness of sandstone in the Fox Hills-Lower Hell Creek aquifer, Montana: U.S. Geological Survey Water-Resources Investigations Report 82-4043, 1 Plate: 35.48 x 22.48 inches, https://doi.org/10.3133/wri824043.","productDescription":"1 Plate: 35.48 x 22.48 inches","costCenters":[],"links":[{"id":162410,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":414244,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_35567.htm","linkFileType":{"id":5,"text":"html"}},{"id":81904,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1982/4043/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Montana","otherGeospatial":"Fox Hills-Lower Hell Creek aquifer","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -104.054,\n              49\n            ],\n            [\n              -110,\n              49\n            ],\n            [\n              -110,\n              45\n            ],\n            [\n              -104.054,\n              45\n            ],\n            [\n              -104.054,\n              49\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a94e4b07f02db659150","contributors":{"authors":[{"text":"Feltis, Richard D.","contributorId":98773,"corporation":false,"usgs":true,"family":"Feltis","given":"Richard","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":229927,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70011663,"text":"70011663 - 1982 - Water-soluble material on aerosols collected within volcanic eruption clouds","interactions":[],"lastModifiedDate":"2024-07-16T15:00:42.55983","indexId":"70011663","displayToPublicDate":"1982-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":9107,"text":"Journal of Geophysical Research - Oceans","active":true,"publicationSubtype":{"id":10}},"title":"Water-soluble material on aerosols collected within volcanic eruption clouds","docAbstract":"<p><span>In February and March of 1978, filter samplers mounted on an aircraft were used to collect the aerosol fraction of the eruption clouds from three active Guatemalan volcanoes (Fuego, Pacaya, and Santiaguito). The samples were collected on Teflon (Fluoropore) filters with a nominal pore diameter of 0.5μm. The mass of air sampled by the filters ranged from 0.15 to 6.6 kg. The particulate material collected consisted of fragments of angular silicate ash and droplets of what is interpreted as dilute H</span><sub>2</sub><span>SO</span><sub>4</sub><span>&nbsp;and HCl. After collection of the samples, each filter was rinsed with 60 ml of distilled-deionized water. Splits of each extract were centrifuged to remove particles greater than or equal to 0.1 μm in diameter, acidified, and analyzed for B, Ba, Be, Ca, Cd, Co, Cu, Fe, Li, Mg, Mn, Mo, Na, Pb, Si, Sr, V, and Zn by inductively coupled plasma—optical emission spectroscopy. Separate splits were analyzed for F and Cl by specific-ion-electrode methods and for U by a fission track technique. The elements dissolved in the aqueous extracts represent components of water-soluble material either formed directly in the eruption cloud or derived from interaction of ash particles and aerosol components of the plume. Calculations of enrichment factors, based upon concentration ratios, showed the elements most enriched in the extracts relative to bulk ash composition were Cd, Cu, V, F, Cl, Zn, and Pb. These elements represent a subset (with the addition of Cl and F) of elements previously reported enriched in atmospheric aerosols in remote regions as well as in volcanic areas. This suggests that some of the enriched elements were widely dispersed as volatile halides emitted from a volcanic source.</span></p>","language":"English","publisher":"American Geophysical Union","doi":"10.1029/JC087iC07p04963","issn":"01480227","usgsCitation":"Smith, D.B., Zielinski, R.A., Rose, W., and Huebert, B., 1982, Water-soluble material on aerosols collected within volcanic eruption clouds: Journal of Geophysical Research - Oceans, v. 87, no. C7, p. 4963-4972, https://doi.org/10.1029/JC087iC07p04963.","productDescription":"10 p.","startPage":"4963","endPage":"4972","numberOfPages":"10","costCenters":[{"id":164,"text":"Central Energy Resources Science Center","active":true,"usgs":true}],"links":[{"id":221606,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"87","issue":"C7","noUsgsAuthors":false,"publicationDate":"2012-09-20","publicationStatus":"PW","scienceBaseUri":"505bcef3e4b08c986b32e64e","contributors":{"authors":[{"text":"Smith, D. B. davidsmith@usgs.gov","contributorId":12840,"corporation":false,"usgs":true,"family":"Smith","given":"D.","email":"davidsmith@usgs.gov","middleInitial":"B.","affiliations":[],"preferred":false,"id":361652,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Zielinski, 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":361654,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Rose, W.I. Jr.","contributorId":25275,"corporation":false,"usgs":true,"family":"Rose","given":"W.I.","suffix":"Jr.","email":"","affiliations":[],"preferred":false,"id":361653,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Huebert, B.J.","contributorId":6189,"corporation":false,"usgs":true,"family":"Huebert","given":"B.J.","email":"","affiliations":[],"preferred":false,"id":361651,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70011650,"text":"70011650 - 1982 - U.S. Geological Survey Federal-State Program","interactions":[],"lastModifiedDate":"2024-05-23T14:46:03.094881","indexId":"70011650","displayToPublicDate":"1982-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2501,"text":"Journal of Water Resources Planning and Management","active":true,"publicationSubtype":{"id":10}},"title":"U.S. Geological Survey Federal-State Program","docAbstract":"<p><span>The U.S. Geological Survey Federal-State Cooperative Water Resource Program is a partnership between the Geological Survey and State and local agencies for the collection of the hydrologic information needed for the continuing determination and evaluation of the quantity, quality, and use of the Nation's water resources. The first Cooperative Program was started in 1895; the Congress gave formal recognition to the partnership in 1928 and authorized Federal funding of not more than 50 percent for cooperative programs with the Geological Survey, with total funding over $80 million. The process of project selection in the Cooperative Water Resource Program is a mutual effort in which Geological Survey represents national interests, including the needs of other Federal agencies, and the cooperator represents State and local interests. The result is a balanced program that involves careful evaluation of needs, priorities, and resources. A number of typical examples of projects within the Cooperative Program are presented.</span></p>","language":"English","publisher":"ASCE","doi":"10.1061/JWRDDC.0000246","usgsCitation":"Buchanan, T., and Gilbert, B., 1982, U.S. Geological Survey Federal-State Program: Journal of Water Resources Planning and Management, v. 108, no. WR1, p. 37-45, https://doi.org/10.1061/JWRDDC.0000246.","productDescription":"9 p.","startPage":"37","endPage":"45","numberOfPages":"9","costCenters":[],"links":[{"id":221454,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"108","issue":"WR1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505bba66e4b08c986b328157","contributors":{"authors":[{"text":"Buchanan, T.J.","contributorId":38559,"corporation":false,"usgs":true,"family":"Buchanan","given":"T.J.","email":"","affiliations":[],"preferred":false,"id":361621,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Gilbert, B.K.","contributorId":32167,"corporation":false,"usgs":true,"family":"Gilbert","given":"B.K.","email":"","affiliations":[],"preferred":false,"id":361620,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70006377,"text":"70006377 - 1982 - Detection of diethylnitrosamine in nitrate-rich water following treatment with Rhodamine flow tracers","interactions":[],"lastModifiedDate":"2026-03-16T16:16:12.072498","indexId":"70006377","displayToPublicDate":"1982-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3716,"text":"Water Research","onlineIssn":"1879-2448","printIssn":"0043-1354","active":true,"publicationSubtype":{"id":10}},"title":"Detection of diethylnitrosamine in nitrate-rich water following treatment with Rhodamine flow tracers","docAbstract":"<p><span>Extremely carcinogenic diethylnitrosamine (DENA) was found to form in up to 75% yield from the reaction of nitrite with the two commonly used water tracing dyes. Rhodamine B and Rhodamine WT, DENA was detected at trace levels (0.13–7.02 μg&nbsp;</span><sup>−1</sup><span>) in river water samples after treatment with the dye and nitrite. Analysis of these chemically treated environmental water samples required extensive separation techniques prior to acquisition of reliable analytical data using highly sensitive instruments for detection. The occurrence of DENA in nitrite-rich water treated with Rhodamines may pose a health hazard to general populations.</span></p>","language":"English","publisher":"Elsevier","doi":"10.1016/0043-1354(82)90111-7","usgsCitation":"Abidi, S.L., 1982, Detection of diethylnitrosamine in nitrate-rich water following treatment with Rhodamine flow tracers: Water Research, v. 16, no. 2, p. 199-204, https://doi.org/10.1016/0043-1354(82)90111-7.","productDescription":"6 p.","startPage":"199","endPage":"204","costCenters":[{"id":606,"text":"Upper Midwest Environmental Sciences Center","active":true,"usgs":true}],"links":[{"id":258232,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"16","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059ff73e4b0c8380cd4f1c6","contributors":{"authors":[{"text":"Abidi, S. L.","contributorId":19898,"corporation":false,"usgs":true,"family":"Abidi","given":"S.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":354414,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70011479,"text":"70011479 - 1982 - Determination of polar organic solutes in oil-shale retort water","interactions":[],"lastModifiedDate":"2023-10-19T18:10:52.882211","indexId":"70011479","displayToPublicDate":"1982-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1565,"text":"Environmental Science & Technology","onlineIssn":"1520-5851","printIssn":"0013-936X","active":true,"publicationSubtype":{"id":10}},"title":"Determination of polar organic solutes in oil-shale retort water","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"American Chemical Society","doi":"10.1021/es00104a015","issn":"0013936X","usgsCitation":"Leenheer, J., Noyes, T., and Stuber, H.A., 1982, Determination of polar organic solutes in oil-shale retort water: Environmental Science & Technology, v. 16, no. 10, p. 714-723, https://doi.org/10.1021/es00104a015.","productDescription":"10 p.","startPage":"714","endPage":"723","costCenters":[],"links":[{"id":220838,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Colorado","otherGeospatial":"Logan Wash","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -108.19497121932936,\n              39.40042581478241\n            ],\n            [\n              -108.18042492246276,\n              39.40084212255246\n            ],\n            [\n              -108.17584553270868,\n              39.40354806249445\n            ],\n            [\n              -108.17422927750103,\n              39.40667017043799\n            ],\n            [\n              -108.16507049799233,\n              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   39.40708644093658\n            ],\n            [\n              -108.23079820976037,\n              39.41104088674359\n            ],\n            [\n              -108.22379443719481,\n              39.40729457525447\n            ],\n            [\n              -108.21786816810086,\n              39.406878305998276\n            ],\n            [\n              -108.20466875057411,\n              39.403964351628986\n            ],\n            [\n              -108.19497121932936,\n              39.40042581478241\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","volume":"16","issue":"10","noUsgsAuthors":false,"publicationDate":"2002-05-01","publicationStatus":"PW","scienceBaseUri":"5059ffbee4b0c8380cd4f38c","contributors":{"authors":[{"text":"Leenheer, J.A.","contributorId":75123,"corporation":false,"usgs":true,"family":"Leenheer","given":"J.A.","affiliations":[],"preferred":false,"id":361210,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Noyes, T.I.","contributorId":54971,"corporation":false,"usgs":true,"family":"Noyes","given":"T.I.","email":"","affiliations":[],"preferred":false,"id":361209,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Stuber, H. A.","contributorId":52721,"corporation":false,"usgs":true,"family":"Stuber","given":"H.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":361208,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70011859,"text":"70011859 - 1982 - Composition of estuarine colloidal material: Organic components","interactions":[],"lastModifiedDate":"2024-03-18T14:28:53.733867","indexId":"70011859","displayToPublicDate":"1982-01-01T00:00:00","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":"Composition of estuarine colloidal material: Organic components","docAbstract":"<p><span>Colloidal material in the size range 1.2 nm to 0.4 μm was isolated by ultrafiltration from Chesapeake Bay and Patuxent River waters (U.S.A.). Temperature controlled, stepwise pyrolysis of the freeze-dried material, followed by gas chromatographic-mass spectrometric analyses of the volatile products indicates that the primary organic components of this polymer are carbohydrates and peptides. The major pyrolysis products at the 450°C step are acetic acid, furaldehydes, furoic acid, furanmethanol, diones and lactones characteristic of carbohydrate thermal decomposition. Pyrroles, pyridines, amides and indole (protein derivatives) become more prevalent and dominate the product yield at the 600°C pyrolysis step. Olefins and saturated hydrocarbons, originating from fatty acids, are present only in minor amounts. These results are consistent with the composition of Chesapeake phytoplankton (approximately 50% protein, 30% carbohydrate, 10% lipid and 10% nucleotides by dry weight). The pyrolysis of a cultured phytoplankton and natural particulate samples produced similar oxygen and nitrogencontaining compounds, although the proportions of some components differ relative to the colloidal fraction. There were no lignin derivatives indicative of terrestrial plant detritus in any of these samples. The data suggest that aquatic microorganisms, rather than terrestrial plants, are the dominant source of colloidal organic material in these river and estuarine surface waters.</span></p>","language":"English","publisher":"Elsevier","doi":"10.1016/0016-7037(82)90318-0","issn":"00167037","usgsCitation":"Sigleo, A., Hoering, T., and Helz, G., 1982, Composition of estuarine colloidal material: Organic components: Geochimica et Cosmochimica Acta, v. 46, no. 9, p. 1619-1626, https://doi.org/10.1016/0016-7037(82)90318-0.","productDescription":"8 p.","startPage":"1619","endPage":"1626","numberOfPages":"8","costCenters":[],"links":[{"id":220795,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"46","issue":"9","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059f928e4b0c8380cd4d47e","contributors":{"authors":[{"text":"Sigleo, A.C.","contributorId":20899,"corporation":false,"usgs":true,"family":"Sigleo","given":"A.C.","email":"","affiliations":[],"preferred":false,"id":362136,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hoering, T.C.","contributorId":101011,"corporation":false,"usgs":true,"family":"Hoering","given":"T.C.","email":"","affiliations":[],"preferred":false,"id":362138,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Helz, G.R.","contributorId":96823,"corporation":false,"usgs":true,"family":"Helz","given":"G.R.","email":"","affiliations":[],"preferred":false,"id":362137,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70011814,"text":"70011814 - 1982 - Identification of the Holocene-Pleistocene boundary in the Bering Sea by diatoms.","interactions":[],"lastModifiedDate":"2012-03-12T17:18:27","indexId":"70011814","displayToPublicDate":"1982-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1068,"text":"Boreas","active":true,"publicationSubtype":{"id":10}},"title":"Identification of the Holocene-Pleistocene boundary in the Bering Sea by diatoms.","docAbstract":"The modern diatom flora from surface sediment of the Navarin Basin region of the Bering Sea is dominated by Denticulopsis seminae and Nitzschia oceanica. D. seminae, a north boreal species, is most abundant in the deeper waters of the slope-basin regions, whereas N. oceanica, an Arctic species associated with ice cover, dominates the shallow shelf water. Downcore studies show that these species alternate in dominance within the late Quaternary sediments suggest climatic fluctuations.-from Author","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Boreas","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","issn":"03009483","usgsCitation":"Baldauf, J., 1982, Identification of the Holocene-Pleistocene boundary in the Bering Sea by diatoms.: Boreas, v. 11, no. 1, p. 113-118.","startPage":"113","endPage":"118","numberOfPages":"6","costCenters":[],"links":[{"id":221199,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"11","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a383fe4b0c8380cd614cd","contributors":{"authors":[{"text":"Baldauf, J.G.","contributorId":67655,"corporation":false,"usgs":true,"family":"Baldauf","given":"J.G.","email":"","affiliations":[],"preferred":false,"id":362017,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
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