{"pageNumber":"1870","pageRowStart":"46725","pageSize":"25","recordCount":68927,"records":[{"id":70015410,"text":"70015410 - 1989 - Moderate-temperature zeolitic alteration in a cooling pyroclastic deposit","interactions":[],"lastModifiedDate":"2013-01-20T20:47:48","indexId":"70015410","displayToPublicDate":"1989-01-01T00:00:00","publicationYear":"1989","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":"Moderate-temperature zeolitic alteration in a cooling pyroclastic deposit","docAbstract":"The locally zeolitized Topopah Spring Member of the Paintbrush Tuff (13 Myr.), Yucca Mountain, Nevada, U.S.A., is part of a thick sequence of zeolitized pyroclastic units. Most of the zeolitized units are nonwelded tuffs that were altered during low-temperature diagenesis, but the distribution and textural setting of zeolite (heulandite-clinoptilolite) and smectite in the densely welded Topopah Spring tuff suggest that these hydrous minerals formed while the tuff was still cooling after pyroclastic emplacement and welding. The hydrous minerals are concentrated within a transition zone between devitrified tuff in the central part of the unit and underlying vitrophyre. Movement of liquid and convected heat along fractures from the devitrified tuff to the ritrophyre caused local devitrification and hydrous mineral crystallization. Oxygen isotope geothermometry of cogenetic quartz confirms the nondiagenetic moderate temperature origin of the hydrous minerals at temperatures of ??? 40-100??C, assuming a meteoric water source. The Topopah Spring tuff is under consideration for emplacement of a high-level nuclear waste repository. The natural rock alteration of the cooling pyroclastic deposit may be a good natural analog for repository-induced hydrothermal alteration. As a result of repository thermal loading, temperatures in the Topopah Spring vitrophyre may rise sufficiently to duplicate the inferred temperatures of natural zeolitic alteration. Heated water moving downward from the repository into the vitrophyre may contribute to new zeolitic alteration. ?? 1989.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Chemical Geology","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"Elsevier","doi":"10.1016/0009-2541(89)90100-9","issn":"00092541","usgsCitation":"Levy, S.S., and O’Neil, J.R., 1989, Moderate-temperature zeolitic alteration in a cooling pyroclastic deposit: Chemical Geology, v. 76, no. 3-4, p. 321-326, https://doi.org/10.1016/0009-2541(89)90100-9.","startPage":"321","endPage":"326","numberOfPages":"6","costCenters":[],"links":[{"id":266086,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1016/0009-2541(89)90100-9"},{"id":224310,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"76","issue":"3-4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a5c86e4b0c8380cd6fd6e","contributors":{"authors":[{"text":"Levy, S. S.","contributorId":18630,"corporation":false,"usgs":true,"family":"Levy","given":"S.","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":370876,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"O’Neil, J. R.","contributorId":69633,"corporation":false,"usgs":true,"family":"O’Neil","given":"J.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":370877,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70015233,"text":"70015233 - 1989 - The influence of formation material properties on the response of water levels in wells to Earth tides and atmospheric loading","interactions":[],"lastModifiedDate":"2024-05-30T16:08:40.566375","indexId":"70015233","displayToPublicDate":"1989-01-01T00:00:00","publicationYear":"1989","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":"The influence of formation material properties on the response of water levels in wells to Earth tides and atmospheric loading","docAbstract":"<p><span>The water level in an open well can change in response to deformation of the surrounding material, either because of applied strains (tidal or tectonic) or surface loading by atmospheric pressure changes. Under conditions of no vertical fluid flow and negligible well bore storage (static-confined conditions), the sensitivities to these effects depend on the elastic properties and porosity which characterize the surrounding medium. For a poroelastic medium, high sensitivity to applied areal strains occurs for low porosity, while high sensitivity to atmospheric loading occurs for high porosity; both increase with decreasing compressibility of the solid matrix. These material properties also influence vertical fluid flow induced by areally extensive deformation and can be used to define two types of hydraulic diffusivity which govern pressure diffusion, one for applied strain and one for surface loading. The hydraulic diffusivity which governs pressure diffusion in response to surface loading is slightly smaller than that which governs fluid flow in response to applied strain. Given the static-confined response of a water well to atmospheric loading and Earth tides, the in situ drained matrix compressibility and porosity (and hence the one-dimensional specific storage) can be estimated. Analysis of the static-confined response of five wells to atmospheric loading and Earth tides gives generally reasonable estimates for material properties.</span></p>","language":"English","publisher":"American Geophysical Union","doi":"10.1029/JB094iB09p12403","issn":"01480227","usgsCitation":"Rojstaczer, S., and Agnew, D., 1989, The influence of formation material properties on the response of water levels in wells to Earth tides and atmospheric loading: Journal of Geophysical Research Solid Earth, v. 94, no. B9, p. 12403-12411, https://doi.org/10.1029/JB094iB09p12403.","productDescription":"9 p.","startPage":"12403","endPage":"12411","costCenters":[],"links":[{"id":224192,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"94","issue":"B9","noUsgsAuthors":false,"publicationDate":"2012-09-20","publicationStatus":"PW","scienceBaseUri":"505bad22e4b08c986b3239d7","contributors":{"authors":[{"text":"Rojstaczer, S.","contributorId":92709,"corporation":false,"usgs":true,"family":"Rojstaczer","given":"S.","email":"","affiliations":[],"preferred":false,"id":370400,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Agnew, D.C.","contributorId":32186,"corporation":false,"usgs":true,"family":"Agnew","given":"D.C.","email":"","affiliations":[],"preferred":false,"id":370399,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":1003828,"text":"1003828 - 1989 - Presumed drowning of Aleutian Canada geese on the Pacific coast of California and Oregon","interactions":[],"lastModifiedDate":"2017-09-19T11:37:35","indexId":"1003828","displayToPublicDate":"1989-01-01T00:00:00","publicationYear":"1989","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":"Presumed drowning of Aleutian Canada geese on the Pacific coast of California and Oregon","docAbstract":"<p><span>Carcasses of 42 and 17 Aleutian Canada geese (</span><i>Branta canadensis leucopareia</i><span>), a federally listed endangered species, were found on ocean beaches near Crescent City, California, and near Pacific City, Oregon, respectively, following severe storms. Necropsies and other information suggest that the birds were flushed during the storms and somehow entered the water where they were washed into the surf and drowned.</span></p>","language":"English","publisher":"Wildlife Disease Association","doi":"10.7589/0090-3558-25.2.276","usgsCitation":"Springer, P.F., Lowe, R.W., Stroud, R.K., and Gullett, P.A., 1989, Presumed drowning of Aleutian Canada geese on the Pacific coast of California and Oregon: Journal of Wildlife Diseases, v. 25, no. 2, p. 276-279, https://doi.org/10.7589/0090-3558-25.2.276.","productDescription":"4 p.","startPage":"276","endPage":"279","numberOfPages":"4","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":456,"text":"National Wildlife Health Center","active":true,"usgs":true}],"links":[{"id":486829,"rank":1,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.7589/0090-3558-25.2.276","text":"Publisher Index Page"},{"id":131134,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"California, Oregon","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -124.24919128417967,\n              41.777456667491066\n            ],\n            [\n              -124.22859191894531,\n              41.801006999656636\n            ],\n            [\n              -124.21520233154297,\n              41.8242928385401\n            ],\n            [\n              -124.20490264892578,\n              41.84859319874276\n            ],\n            [\n              -124.19700622558594,\n              41.86981648734634\n            ],\n            [\n              -124.19528961181639,\n              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F.","contributorId":70445,"corporation":false,"usgs":true,"family":"Springer","given":"Paul","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":314406,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Lowe, Roy W.","contributorId":50847,"corporation":false,"usgs":false,"family":"Lowe","given":"Roy","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":314405,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Stroud, Richard K.","contributorId":102837,"corporation":false,"usgs":true,"family":"Stroud","given":"Richard","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":314404,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Gullett, Patricia A.","contributorId":65428,"corporation":false,"usgs":true,"family":"Gullett","given":"Patricia","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":314407,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70140597,"text":"70140597 - 1989 - Terrain, vegetation, and landscape evolution of the R4D research site, Brooks Range Foothills, Alaska","interactions":[],"lastModifiedDate":"2019-12-10T15:09:08","indexId":"70140597","displayToPublicDate":"1989-01-01T00:00:00","publicationYear":"1989","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3869,"text":"Holarctic Ecology","active":true,"publicationSubtype":{"id":10}},"title":"Terrain, vegetation, and landscape evolution of the R4D research site, Brooks Range Foothills, Alaska","docAbstract":"<p>Maps of the vegetation and terrain of a 22 km2 area centered on the Department of Energy (DOE) R4D (Response, Resistance, Resilience to and Recovery from Disturbance in Arctic Ecosystems) study site in the Southern Foothills Physiographic Province of Alaska were made using integrated geobotanical mapping procedures and a geographic-information system. Typical land forms and surface f orms include hillslope water tracks, Sagavanirktok-age till deposits, nonsorted stone stripes, and colluvial-basin deposits. Thirty-two plant communities are described; the dominant vegetation (51% of the mapped area) is moist tussock-sedge, dwarf-shrub tundra dominated by Eriophorum vaginatum or Carex bigelowii. Much of the spatial variation in the mapped geobotanical characters reflects different-aged glaciated surfaces. Shannon-Wienerin dices indicate that the more mature landscapes, represented by retransported hillslope deposits and basin colluvium, are less heterogeneous than newer landscapes such as surficial till deposits and floodplains. A typical toposequence on a mid-Pleistocene-age surface is discussed with respect to evolution of the landscape. Thick Sphagnum moss layers occur on lower hillslopes, and the patterns of moss-layer development, heat flux, active layer thickness, and ground-ice are seen as keys to developing thermokarst-susceptibility maps.</p>","language":"English","publisher":"Nordic Society Oikos","usgsCitation":"Walker, D., Binnian, E.F., Evans, B.M., Lederer, N., Nordstrand, E., and Webber, P., 1989, Terrain, vegetation, and landscape evolution of the R4D research site, Brooks Range Foothills, Alaska: Holarctic Ecology, v. 12, no. 3, p. 238-261.","productDescription":"24 p.","startPage":"238","endPage":"261","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":114,"text":"Alaska Science Center","active":true,"usgs":true},{"id":222,"text":"Earth Resources Observation and Science (EROS) Center","active":true,"usgs":true}],"links":[{"id":297881,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":336825,"rank":2,"type":{"id":15,"text":"Index Page"},"url":"https://www.jstor.org/stable/3682732"}],"country":"United States","state":"Alaska","otherGeospatial":"Brooks Range","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -159.345703125,\n              66.79190947341796\n            ],\n            [\n              -140.712890625,\n              66.79190947341796\n            ],\n            [\n              -140.712890625,\n              69.51914693717981\n            ],\n            [\n              -159.345703125,\n              69.51914693717981\n            ],\n            [\n              -159.345703125,\n              66.79190947341796\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"12","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"54dd2c68e4b08de9379b37a5","contributors":{"authors":[{"text":"Walker, D.A.","contributorId":82484,"corporation":false,"usgs":false,"family":"Walker","given":"D.A.","email":"","affiliations":[],"preferred":false,"id":540218,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Binnian, Emily F.","contributorId":34090,"corporation":false,"usgs":true,"family":"Binnian","given":"Emily","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":540219,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Evans, B. M.","contributorId":107872,"corporation":false,"usgs":false,"family":"Evans","given":"B.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":540220,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Lederer, N.D.","contributorId":139151,"corporation":false,"usgs":false,"family":"Lederer","given":"N.D.","email":"","affiliations":[],"preferred":false,"id":540221,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Nordstrand, E.A.","contributorId":139152,"corporation":false,"usgs":false,"family":"Nordstrand","given":"E.A.","email":"","affiliations":[],"preferred":false,"id":540222,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Webber, P.J.","contributorId":25351,"corporation":false,"usgs":false,"family":"Webber","given":"P.J.","email":"","affiliations":[],"preferred":false,"id":540223,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}}
,{"id":70015417,"text":"70015417 - 1989 - Non-energy minerals and surficial geology of the continental margin of Maryland","interactions":[],"lastModifiedDate":"2024-10-09T11:10:37.6228","indexId":"70015417","displayToPublicDate":"1989-01-01T00:00:00","publicationYear":"1989","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2667,"text":"Marine Geology","active":true,"publicationSubtype":{"id":10}},"title":"Non-energy minerals and surficial geology of the continental margin of Maryland","docAbstract":"<div id=\"preview-section-abstract\"><div id=\"abstracts\" class=\"Abstracts u-font-serif\"><div id=\"aep-abstract-id3\" class=\"abstract author\"><div id=\"aep-abstract-sec-id4\"><div class=\"u-margin-s-bottom\">The surficial sediments have been mapped and the shallow geologic framework outlined of the Maryland inner continental shelf. The initial study encompassed a small area offshore of Assateague Island but was extended northward to include the Ocean City area and eastward across several linear shoals.</div><div class=\"u-margin-s-bottom\"><br data-mce-bogus=\"1\"></div><div class=\"u-margin-s-bottom\">The surficial sediments are predominantly sand with mean grain sizes ranging from 0.40 to 2.89∅. Mud and gravel are the mappable components of the surficial sediments. Muds are distributed along a N-S-trending band seaward of the shoreface. Gravels are mapped farther offshore in 18–22 m of water.</div><div class=\"u-margin-s-bottom\"><br data-mce-bogus=\"1\"></div><div class=\"u-margin-s-bottom\">Four distinct seismic units are identified from seismic reflection profiles. The lowermost unit, T1, exhibits high-angle clinoforms truncated at the top by a locally prominent near-horizontal reflector. Above this reflector are concordant strata with parallel to subparallel bedding designated as Q2. Incised into Q2 is an extensive channel, Q3, that trends both coast-parallel and coast-normal. The upper unit, Q4, overlaps portions of units Q2 and Q3 along the eastward edges of the study area and is represented in the nearshore by (Holocene inlet?) channeling adjacent to the shoreface. Note that this excludes the modern shelf and “sheet”.</div></div></div></div></div><div id=\"preview-section-introduction\"><br></div>","language":"English","publisher":"Elsevier","doi":"10.1016/0025-3227(89)90118-7","issn":"00253227","usgsCitation":"Kerhin, R., 1989, Non-energy minerals and surficial geology of the continental margin of Maryland: Marine Geology, v. 90, no. 1-2, p. 95-102, https://doi.org/10.1016/0025-3227(89)90118-7.","productDescription":"8 p.","startPage":"95","endPage":"102","numberOfPages":"8","costCenters":[],"links":[{"id":223600,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"90","issue":"1-2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a6741e4b0c8380cd7324b","contributors":{"authors":[{"text":"Kerhin, R.T.","contributorId":38189,"corporation":false,"usgs":true,"family":"Kerhin","given":"R.T.","email":"","affiliations":[],"preferred":false,"id":370890,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70016119,"text":"70016119 - 1989 - Data-collection program for Pamlico River Estuary model calibration and validation","interactions":[],"lastModifiedDate":"2012-03-12T17:18:47","indexId":"70016119","displayToPublicDate":"1989-01-01T00:00:00","publicationYear":"1989","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"Data-collection program for Pamlico River Estuary model calibration and validation","docAbstract":"An investigation is being conducted to collect and interpret continuous records relating to the flow characteristics of the Pamlico River Estuary, North Carolina, and to calibrate and validate a numerical model of estuarine hydrodynamics. The study reach is 50 kilometers long and ranges in width from 330 meters at the upstream boundary to 6.4 kilometers at the downstream end. Water levels are recorded at 6 locations along the estuary; daily water-level range is typically greater at the head of the estuary than at the mouth, most likely due to upstream narrowing of the channel. Water-quality data are recorded at 14 locations. These data indicate that saline waters with low dissolved oxygen concentrations move upstream along the bottom of the estuary. Point velocities were monitored for 3 weeks at 7 locations; vertical profiles of horizontal velocity were made at the boundaries of the study reach for about 32 hours. Local tributary inflows and wind speed and direction are also being determined.","conferenceTitle":"Estuarine and Coastal Modeling - Proceedings of the Conference","conferenceDate":"15 November 1989 through 17 November 1989","conferenceLocation":"Newport, RI, USA","language":"English","publisher":"Publ by ASCE","publisherLocation":"Boston, MA, United States","isbn":"0872627586","usgsCitation":"Bales, J.D., 1989, Data-collection program for Pamlico River Estuary model calibration and validation, Estuarine and Coastal Modeling - Proceedings of the Conference, Newport, RI, USA, 15 November 1989 through 17 November 1989, p. 492-501.","startPage":"492","endPage":"501","numberOfPages":"10","costCenters":[],"links":[{"id":223349,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059fdd1e4b0c8380cd4e961","contributors":{"authors":[{"text":"Bales, Jerad D. 0000-0001-8398-6984 jdbales@usgs.gov","orcid":"https://orcid.org/0000-0001-8398-6984","contributorId":683,"corporation":false,"usgs":true,"family":"Bales","given":"Jerad","email":"jdbales@usgs.gov","middleInitial":"D.","affiliations":[{"id":436,"text":"National Research Program - Eastern Branch","active":true,"usgs":true},{"id":5058,"text":"Office of the Chief Scientist for Water","active":true,"usgs":true}],"preferred":true,"id":372598,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70015013,"text":"70015013 - 1989 - 100 years of sedimentation study by the USGS","interactions":[],"lastModifiedDate":"2012-03-12T17:18:51","indexId":"70015013","displayToPublicDate":"1989-01-01T00:00:00","publicationYear":"1989","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"100 years of sedimentation study by the USGS","docAbstract":"On January 15, 1889, the U.S. Geological Survey began collecting sediment data on the Rio Grande at Embudo, New Mexico. During the past 100 years the U.S. Geological Survey's Water Resources Division (WRD) has collected daily sediment data at more than 1,200 sites. Projects have addressed the problems associated with reservoir construction, agricultural irrigation projects, energy production, and transport and deposition of pollutants sorbed to sediments. The Survey has been active as a charter member of the Federal Interagency Sediment Project and currently has three full-time hydrologists working on the project. The WRD's sediment-research projects have covered a wide variety of subjects from the fundamental theories of resistance to flow and sediment transport in alluvial channels to lunar erosion mechanisms.","conferenceTitle":"Sediment Transport Modeling: Proceedings of the International Symposium","conferenceDate":"14 August 1989 through 18 August 1989","conferenceLocation":"New Orleans, LA, USA","language":"English","publisher":"Publ by ASCE","publisherLocation":"New York, NY, United States","isbn":"0872627187","usgsCitation":"Glysson, G.D., 1989, 100 years of sedimentation study by the USGS, Sediment Transport Modeling: Proceedings of the International Symposium, New Orleans, LA, USA, 14 August 1989 through 18 August 1989, p. 260-265.","startPage":"260","endPage":"265","numberOfPages":"6","costCenters":[],"links":[{"id":224452,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059e221e4b0c8380cd4599f","contributors":{"authors":[{"text":"Glysson, G. Douglas","contributorId":13607,"corporation":false,"usgs":true,"family":"Glysson","given":"G.","email":"","middleInitial":"Douglas","affiliations":[],"preferred":false,"id":369855,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70015011,"text":"70015011 - 1989 - Estimating urban flood-frequency characteristics","interactions":[],"lastModifiedDate":"2012-03-12T17:18:51","indexId":"70015011","displayToPublicDate":"1989-01-01T00:00:00","publicationYear":"1989","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"Estimating urban flood-frequency characteristics","docAbstract":"Methods in use by the U.S. Geological Survey to estimate flood-frequency characteristics for urban watersheds are compared with estimates based on the Soil Conservation Service TR-55 model. Data from four small urban watersheds in Georgia are used in the flood-peak and hydrograph comparisons.","conferenceTitle":"Proceedings of the 1989 National Conference on Hydraulic Engineering","conferenceDate":"14 August 1989 through 18 August 1989","conferenceLocation":"New Orleans, LA, USA","language":"English","publisher":"Publ by ASCE","publisherLocation":"New York, NY, United States","isbn":"0872627195","usgsCitation":"Jennings, M., Atkins, J., and Inman, E.J., 1989, Estimating urban flood-frequency characteristics, Proceedings of the 1989 National Conference on Hydraulic Engineering, New Orleans, LA, USA, 14 August 1989 through 18 August 1989, p. 516-521.","startPage":"516","endPage":"521","numberOfPages":"6","costCenters":[],"links":[{"id":224450,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a0b6be4b0c8380cd526fa","contributors":{"authors":[{"text":"Jennings, M.E.","contributorId":76775,"corporation":false,"usgs":true,"family":"Jennings","given":"M.E.","email":"","affiliations":[],"preferred":false,"id":369852,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Atkins, J.B.","contributorId":63842,"corporation":false,"usgs":true,"family":"Atkins","given":"J.B.","email":"","affiliations":[],"preferred":false,"id":369851,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Inman, E. J.","contributorId":44193,"corporation":false,"usgs":true,"family":"Inman","given":"E.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":369850,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70015770,"text":"70015770 - 1989 - Oxygen-isotope composition of ground water and secondary minerals in Columbia Plateau basalts: Implications for the paleohydrology of the Pasco Basin","interactions":[],"lastModifiedDate":"2024-01-24T01:40:58.508164","indexId":"70015770","displayToPublicDate":"1989-01-01T00:00:00","publicationYear":"1989","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1796,"text":"Geology","active":true,"publicationSubtype":{"id":10}},"title":"Oxygen-isotope composition of ground water and secondary minerals in Columbia Plateau basalts: Implications for the paleohydrology of the Pasco Basin","docAbstract":"<div id=\"15572336\" class=\"article-section-wrapper js-article-section js-content-section  \" data-section-parent-id=\"0\"><p>Concentrations of<span>&nbsp;</span><sup>18</sup>O and deuterium in ground waters beneath the Hanford Reservation, Washington State, suggest that the meteoric waters recharging the basalt aquifers have been progressively depleted in these isotopes since at least Pleistocene time. This conclusion is supported by oxygen-isotope analyses of low-temperature secondary minerals filling vugs and fractures in the basalts, which are used to approximate the<span>&nbsp;</span><sup>18</sup>O content of ground water at the time the mineral assemblage formed. A fossil profile of δ<sup>18</sup>O values projected for ground water in a 1500 m vertical section beneath the reservation suggests that the vertical mixing of shallow and deep ground water indicated by present-day hydrochemical data was also occurring during Neogene time. These data also suggest that a unidirectional depletion of<span>&nbsp;</span><sup>18</sup>O and deuterium recorded in Pleistocene ground waters may have extended considerably further back in time. This shift is tentatively attributed to the orographic depletion of<span>&nbsp;</span><sup>18</sup>O associated with the progressive uplift of the Cascade Range since the middle Miocene.</p></div>","language":"English","publisher":"Geological Society of America","doi":"10.1130/0091-7613(1989)017<0606:OICOGW>2.3.CO;2","issn":"00917613","usgsCitation":"Hearn, P., Steinkampf, W., Horton, D.G., Solomon, G., White, L.D., and Evans, J., 1989, Oxygen-isotope composition of ground water and secondary minerals in Columbia Plateau basalts: Implications for the paleohydrology of the Pasco Basin: Geology, v. 17, no. 7, p. 606-610, https://doi.org/10.1130/0091-7613(1989)017<0606:OICOGW>2.3.CO;2.","productDescription":"5 p.","startPage":"606","endPage":"610","numberOfPages":"5","costCenters":[],"links":[{"id":224391,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"17","issue":"7","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a72bfe4b0c8380cd76c9d","contributors":{"authors":[{"text":"Hearn, P.P. Jr.","contributorId":76763,"corporation":false,"usgs":true,"family":"Hearn","given":"P.P.","suffix":"Jr.","email":"","affiliations":[],"preferred":false,"id":371731,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Steinkampf, W.C.","contributorId":8137,"corporation":false,"usgs":true,"family":"Steinkampf","given":"W.C.","affiliations":[],"preferred":false,"id":371726,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Horton, D. G.","contributorId":17375,"corporation":false,"usgs":true,"family":"Horton","given":"D.","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":371728,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Solomon, G.C.","contributorId":20473,"corporation":false,"usgs":true,"family":"Solomon","given":"G.C.","email":"","affiliations":[],"preferred":false,"id":371729,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"White, L. D.","contributorId":14330,"corporation":false,"usgs":true,"family":"White","given":"L.","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":371727,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Evans, J.R.","contributorId":50526,"corporation":false,"usgs":true,"family":"Evans","given":"J.R.","email":"","affiliations":[],"preferred":false,"id":371730,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}}
,{"id":70015532,"text":"70015532 - 1989 - Recharge of the early atmosphere of Mars by impact-induced release of CO2","interactions":[],"lastModifiedDate":"2013-10-29T15:18:09","indexId":"70015532","displayToPublicDate":"1989-01-01T00:00:00","publicationYear":"1989","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1963,"text":"Icarus","active":true,"publicationSubtype":{"id":10}},"title":"Recharge of the early atmosphere of Mars by impact-induced release of CO2","docAbstract":"Channels on the Martian surface suggest that Mars had an early, relatively thick atmosphere. If the atmosphere was thick enough for water to be stable at the surface, CO<sub>2</sub> in the atmosphere would have been fixed as carbonates on a relatively short time scale, previously estimated to be 1 bar every 10<sup>7</sup> years. This loss must have been offset by some replenishment mechanism to account for the numerous valley networks in the oldest surviving terrains. Impacts could have released CO<sub>2</sub> into the atmosphere by burial, by shock-induced release during impact events, and by addition of carbon to Mars from the impacting bolides. Depending on the relationship between the transient cavity diameter and the diameter of the resulting crater, burial rates as a result of impact gardening at the end of heavy bombardment are estimated to range from 20 to 45 m/10<sup>6</sup> years, on the assumption that cratering rates in Mars were similar to those of the Nectarian Period on the Moon. At these rates 0.1-0.2 bar of CO<sub>2</sub> could have been released every 107 years as a result of burial to depths where dissociation temperatures of carbonates were reached. Modeling of large impacts suggests that an additional 0.01 to 0.02 bar of CO<sub>2</sub> could have been released every 10<sup>7</sup> years during the actual impacts. In the unlikely event that all the impacting material was composed of carbonaceous chondrites, a further 0.3 bar of CO<sub>2</sub> could have been added to the atmosphere every 10<sup>7</sup> years by oxidation of meteoritic carbon. Even when supplemented by the volcanically induced release of CO<sub>2</sub>, these release rates are barely sufficient to sustain an early atmosphere if water were continuously present at the surface. The results suggest that water may have been only intermittently present on the surface early in the planet's history.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Icarus","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"Elsevier","doi":"10.1016/0019-1035(89)90080-8","issn":"00191035","usgsCitation":"Carr, M.H., 1989, Recharge of the early atmosphere of Mars by impact-induced release of CO2: Icarus, v. 79, no. 2, p. 311-327, https://doi.org/10.1016/0019-1035(89)90080-8.","startPage":"311","endPage":"327","numberOfPages":"17","costCenters":[],"links":[{"id":223827,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":278565,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1016/0019-1035(89)90080-8"}],"volume":"79","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a9665e4b0c8380cd81f7e","contributors":{"authors":[{"text":"Carr, Michael H.","contributorId":61894,"corporation":false,"usgs":true,"family":"Carr","given":"Michael","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":371167,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70015899,"text":"70015899 - 1989 - Interrelationships among hydrologic-budget components of a northern Wisconsin seepage lake and implications for acid-deposition modeling","interactions":[],"lastModifiedDate":"2023-12-12T15:19:57.286534","indexId":"70015899","displayToPublicDate":"1989-01-01T00:00:00","publicationYear":"1989","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}},"title":"Interrelationships among hydrologic-budget components of a northern Wisconsin seepage lake and implications for acid-deposition modeling","docAbstract":"<p><span>Components of the hydrologic budget for a northern Wisconsin seepage lake were analyzed by applying correlation and regression techniques to monthly data. Analyses for the 1981–83 water years revealed a statistically significant, direct relationship between storage change and precipitation-evaporation balance. Ground-water outflow was negatively correlated with ground-water inflow, and this relationship was influenced by similar relationships for both hydraulic gradients and cross-sectional areas in outflow versus inflow regions of the lake. Neither ground-water outflow nor inflow was significantly related to precipitation, evaporation, storage change, or lake stage; this may reflect a lag in response time of the ground-water system compared to the lake. The results (1) emphasize the complexity of factors that influence ground-water interactions with seepage lakes and (2) suggest the importance of completing detailed hydrologic studies of these systems before mechanistic models, such as those developed to predict effects of acid deposition, are applied.</span></p>","language":"English","publisher":"Springer","doi":"10.1007/BF01056199","usgsCitation":"Wentz, D.A., and Rose, W., 1989, Interrelationships among hydrologic-budget components of a northern Wisconsin seepage lake and implications for acid-deposition modeling: Archives of Environmental Contamination and Toxicology, v. 18, no. 1-2, p. 147-155, https://doi.org/10.1007/BF01056199.","productDescription":"9 p.","startPage":"147","endPage":"155","numberOfPages":"9","costCenters":[],"links":[{"id":223032,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Wisconsin","county":"Vilas County","otherGeospatial":"Vandercook Lake","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -89.69120679416645,\n              45.9894661436733\n            ],\n            [\n              -89.69120679416645,\n              45.97500382959842\n            ],\n            [\n              -89.67867191017365,\n              45.97500382959842\n            ],\n            [\n              -89.67867191017365,\n              45.9894661436733\n            ],\n            [\n              -89.69120679416645,\n              45.9894661436733\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","volume":"18","issue":"1-2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a3da4e4b0c8380cd63709","contributors":{"authors":[{"text":"Wentz, Dennis A. dawentz@usgs.gov","contributorId":1838,"corporation":false,"usgs":true,"family":"Wentz","given":"Dennis","email":"dawentz@usgs.gov","middleInitial":"A.","affiliations":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"preferred":false,"id":372033,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Rose, William J. wjrose@usgs.gov","contributorId":2182,"corporation":false,"usgs":true,"family":"Rose","given":"William J.","email":"wjrose@usgs.gov","affiliations":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"preferred":false,"id":372032,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70015460,"text":"70015460 - 1989 - Water balance at a low-level radioactive-waste disposal site","interactions":[],"lastModifiedDate":"2013-02-19T14:25:51","indexId":"70015460","displayToPublicDate":"1989-01-01T00:00:00","publicationYear":"1989","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3718,"text":"Water Resources Bulletin","printIssn":"0043-1370","active":true,"publicationSubtype":{"id":10}},"title":"Water balance at a low-level radioactive-waste disposal site","docAbstract":"The water balance at a low-level radioactive-waste disposal site in northwestern Illinois was studied from July 1982 through June 1984. Continuous data collection allowed estimates to be made for each component of the water-balance equation independent of other components. The average annual precipitation was 948 millimeters. Average annual evapotranspiration was estimated at 637 millimeters, runoff was 160 millimeters, change in water storage in a waste-trench cover was 24 millimeters, and deep percolation was 208 millimeters. The magnitude of the difference between precipitation and all other components (81 millimeters per year) indicates that, in a similar environment, the water-budget method would be useful in estimating evapotranspiration, but questionable for estimation of other components. Precipitation depth and temporal distribution had a very strong effect on all other components of the water-balance equation. Due to the variability of precipitation from year to year, it appears that two years of data are inadequate for characterization of the long-term average water balance at the site.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Water Resources Bulletin","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"American Water Resources Association","doi":"10.1111/j.1752-1688.1989.tb03075.x","issn":"00431370","usgsCitation":"Healy, R.W., Gray, J.R., De Vries, G.M., and Mills, P., 1989, Water balance at a low-level radioactive-waste disposal site: Water Resources Bulletin, v. 25, no. 2, p. 381-390, https://doi.org/10.1111/j.1752-1688.1989.tb03075.x.","startPage":"381","endPage":"390","numberOfPages":"10","costCenters":[],"links":[{"id":267749,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1111/j.1752-1688.1989.tb03075.x"},{"id":224422,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"25","issue":"2","noUsgsAuthors":false,"publicationDate":"2007-06-08","publicationStatus":"PW","scienceBaseUri":"505bc7c1e4b08c986b32c5ec","contributors":{"authors":[{"text":"Healy, R. W.","contributorId":89872,"corporation":false,"usgs":true,"family":"Healy","given":"R.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":371003,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Gray, J. R.","contributorId":63372,"corporation":false,"usgs":true,"family":"Gray","given":"J.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":371000,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"De Vries, G. M.","contributorId":65612,"corporation":false,"usgs":true,"family":"De Vries","given":"G.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":371001,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Mills, P. C.","contributorId":69117,"corporation":false,"usgs":true,"family":"Mills","given":"P. C.","affiliations":[],"preferred":false,"id":371002,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70015387,"text":"70015387 - 1989 - Mass conservation: 1-D open channel flow equations","interactions":[],"lastModifiedDate":"2024-12-12T17:01:40.420247","indexId":"70015387","displayToPublicDate":"1989-01-01T00:00:00","publicationYear":"1989","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2338,"text":"Journal of Hydraulic Engineering","active":true,"publicationSubtype":{"id":10}},"title":"Mass conservation: 1-D open channel flow equations","docAbstract":"<p><span>Unsteady flow simulation in natural rivers is often complicated by meandering channels of compound section. Hydraulic properties and the length of the wetted channel may vary significantly as a meandering river inundates its adjacent floodplain. The one-dimensional, unsteady, open-channel flow equations can be extended to simulate floods in channels of compound section if it is assumed that the lateral velocities are negligible, the water surface is level across the section, and the effects of turbulence and friction may be adequately described by resistance laws used for uniform flow. It is shown that the equations derived from the addition of differential equations individually describing flow in main and overbank channels do not conserve mass when overbank and main channels are of different lengths. Equations derived through the use of appropriate integral relations, however, do conserve mass and momentum in the general case and are not limited to the specification of one main and two overbank channels.</span></p>","language":"English","publisher":"ASCE","doi":"10.1061/(ASCE)0733-9429(1989)115:2(263)","issn":"07339429","usgsCitation":"DeLong, L.L., 1989, Mass conservation: 1-D open channel flow equations: Journal of Hydraulic Engineering, v. 115, no. 2, p. 263-269, https://doi.org/10.1061/(ASCE)0733-9429(1989)115:2(263).","productDescription":"7 p.","startPage":"263","endPage":"269","numberOfPages":"7","costCenters":[],"links":[{"id":223983,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"115","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a524ce4b0c8380cd6c2eb","contributors":{"authors":[{"text":"DeLong, Lewis L.","contributorId":91146,"corporation":false,"usgs":true,"family":"DeLong","given":"Lewis","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":370822,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70015615,"text":"70015615 - 1989 - Simulation of calcite dissolution and porosity changes in saltwater mixing zones in coastal aquifers","interactions":[],"lastModifiedDate":"2020-01-12T11:17:53","indexId":"70015615","displayToPublicDate":"1989-01-01T00:00:00","publicationYear":"1989","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":"Simulation of calcite dissolution and porosity changes in saltwater mixing zones in coastal aquifers","docAbstract":"<p><span>Thermodynamic models of aqueous solutions have indicated that the mixing of seawater and calcite-saturated fresh groundwater can produce a water that is undersaturated with respect to calcite. Mixing of such waters in coastal carbonate aquifers could lead to significant amounts of limestone dissolution. The potential for such dissolution in coastal saltwater mixing zones is analyzed by coupling the results from a reaction simulation model (PHREEQE) with a variable density groundwater flow and solute transport model. Idealized cross sections of coastal carbonate aquifers are simulated to estimate the potential for calcite dissolution under a variety of hydrologic and geochemical conditions. Results show that limestone dissolution in mixing zones is strongly dependent on groundwater flux and nearly independent of the dissolution kinetics of calcite. The amount of dissolution varies within a mixing zone, depending on the properties, physical dimensions, and boundary conditions of the aquifer system. Nearly all of the dissolution occurs in the fresher side of the mixing zone, with the maximum dissolution occurring in water that is fresher than that predicted solely by geochemical reaction models. The greatest porosity and permeability development occur at the toe and at the top of the mixing zone. If permeability increases as porosity increases, asymmetry in the dissolution causes the mixing zone to migrate landward over time. Dissolution rates indicated by the model show that this mechanism can produce significant increases in porosity and permeability over time spans on the order of tens of thousands of years. Given the comparatively long span of geologic time, this process may be largely responsible for porosity and permeability development observed in those carbonate rocks through which a freshwater-saltwater mixing zone had at one time migrated.</span></p>","language":"English","publisher":"American Geophysical Union","doi":"10.1029/WR025i004p00655","usgsCitation":"Sanford, W.E., and Konikow, L.F., 1989, Simulation of calcite dissolution and porosity changes in saltwater mixing zones in coastal aquifers: Water Resources Research, v. 25, no. 4, p. 655-667, https://doi.org/10.1029/WR025i004p00655.","productDescription":"13 p.","startPage":"655","endPage":"667","costCenters":[{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":224434,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"25","issue":"4","noUsgsAuthors":false,"publicationDate":"2010-07-09","publicationStatus":"PW","scienceBaseUri":"505b9015e4b08c986b3192f1","contributors":{"authors":[{"text":"Sanford, Ward E. 0000-0002-6624-0280 wsanford@usgs.gov","orcid":"https://orcid.org/0000-0002-6624-0280","contributorId":2268,"corporation":false,"usgs":true,"family":"Sanford","given":"Ward","email":"wsanford@usgs.gov","middleInitial":"E.","affiliations":[{"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}],"preferred":true,"id":371373,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Konikow, Leonard F. 0000-0002-0940-3856 lkonikow@usgs.gov","orcid":"https://orcid.org/0000-0002-0940-3856","contributorId":158,"corporation":false,"usgs":true,"family":"Konikow","given":"Leonard","email":"lkonikow@usgs.gov","middleInitial":"F.","affiliations":[{"id":436,"text":"National Research Program - Eastern Branch","active":true,"usgs":true}],"preferred":true,"id":371372,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70015931,"text":"70015931 - 1989 - Extracting spectral contrast in Landsat Thematic Mapper image data using selective principal component analysis","interactions":[],"lastModifiedDate":"2012-03-12T17:18:44","indexId":"70015931","displayToPublicDate":"1989-01-01T00:00:00","publicationYear":"1989","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":"Extracting spectral contrast in Landsat Thematic Mapper image data using selective principal component analysis","docAbstract":"A challenge encountered with Landsat Thematic Mapper (TM) data, which includes data from size reflective spectral bands, is displaying as much information as possible in a three-image set for color compositing or digital analysis. Principal component analysis (PCA) applied to the six TM bands simultaneously is often used to address this problem. However, two problems that can be encountered using the PCA method are that information of interest might be mathematically mapped to one of the unused components and that a color composite can be difficult to interpret. \"Selective' PCA can be used to minimize both of these problems. The spectral contrast among several spectral regions was mapped for a northern Arizona site using Landsat TM data. Field investigations determined that most of the spectral contrast seen in this area was due to one of the following: the amount of iron and hematite in the soils and rocks, vegetation differences, standing and running water, or the presence of gypsum, which has a higher moisture retention capability than do the surrounding soils and rocks. -from Authors","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Photogrammetric Engineering and Remote Sensing","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","usgsCitation":"Chavez, P., and Kwarteng, A.Y., 1989, Extracting spectral contrast in Landsat Thematic Mapper image data using selective principal component analysis: Photogrammetric Engineering and Remote Sensing, v. 55, no. 3, p. 339-348.","startPage":"339","endPage":"348","numberOfPages":"10","costCenters":[],"links":[{"id":223441,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"55","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a0e5ae4b0c8380cd533e8","contributors":{"authors":[{"text":"Chavez, P.S. Jr.","contributorId":75147,"corporation":false,"usgs":true,"family":"Chavez","given":"P.S.","suffix":"Jr.","email":"","affiliations":[],"preferred":false,"id":372109,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Kwarteng, Andy Y.","contributorId":7423,"corporation":false,"usgs":true,"family":"Kwarteng","given":"Andy","email":"","middleInitial":"Y.","affiliations":[],"preferred":false,"id":372108,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70015951,"text":"70015951 - 1989 - Organic geochemistry and brine composition in Great Salt, Mono, and Walker Lakes","interactions":[],"lastModifiedDate":"2024-04-11T16:27:30.476731","indexId":"70015951","displayToPublicDate":"1989-01-01T00:00:00","publicationYear":"1989","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":"Organic geochemistry and brine composition in Great Salt, Mono, and Walker Lakes","docAbstract":"<div id=\"abstracts\" class=\"Abstracts u-font-serif text-s\"><div id=\"aep-abstract-id4\" class=\"abstract author\"><div id=\"aep-abstract-sec-id5\"><p>Samples of Recent sediments, representing up to 1000 years of accumulation, were collected from three closed basin lakes (Mono Lake, CA, Walker Lake, NV, and Great Salt Lake, UT) to assess the effects of brine composition on the accumulation of total organic carbon, the concentration of dissolved organic carbon, humic acid structure and diagenesis, and trace metal complexation.</p><p>The Great Salt Lake water column is a stratified Na-Mg-Cl-SO<sub>4</sub><span>&nbsp;</span>brine with low alkalinity. Algal debris is entrained in the high density (1.132–1.190 g/cc) bottom brines, and in this region maximum organic matter decomposition occurs by anaerobic processes, with sulfate ion as the terminal electron acceptor. Organic matter, below 5 cm of the sediment-water interface, degrades at a very slow rate in spite of very high pore-fluid sulfate levels. The organic carbon concentration stabilizes at 1.1 wt%. Mono Lake is an alkaline (Na-CO<sub>3</sub>-Cl-SO<sub>4</sub>) system. The water column is stratified, but the bottom brines are of lower density relative to the Great Salt Lake, and sedimentation of algal debris is rapid. Depletion of pore-fluid sulfate, near l m of core, results in a much higher accumulation of organic carbon, approximately 6 wt%. Walker Lake is also an alkaline system. The water column is not stratified, and decomposition of organic matter occurs by aerobic processes at the sediment-water interface and by anaerobic processes below. Total organic carbon and dissolved organic carbon concentrations in Walker Lake sediments vary with location and depth due to changes in input and pore-fluid sulfate concentrations.</p><p>Nuclear magnetic resonance studies (<sup>13</sup>C) of humic substances and dissolved organic carbon provide information on the source of the Recent sedimentary organic carbon (aquatic vs. terrestrial), its relative state of decomposition, and its chemical structure. The spectra suggest an algal origin with little terrestrial signature at all three lakes. This is indicated by the ratio of aliphatic to aromatic carbon and the absence of chemical structures indicative of the lignin of vascular plants. The dissolved organic carbon of the Mono Lake pore fluids is structurally related to humic acid and is also related to carbohydrate metabolism. The alkaline pore fluids, due to high pH, solubilize high molecular weight organic matter from the sediments. This hydrophilic material is a metal complexing agent.</p><p>Despite very high algal productivities, organic carbon accumulation can be low in stratified lakes if the anoxic bottom waters are hypersaline with high concentrations of sulfate ion. Labile organic matter is recycled to the water column and the sedimentary organic matter is relatively nonsusceptible to bacterial metabolism. As a result, pore-fluid dissolved organic carbon and metal-organic complexation are low.</p></div></div></div><ul id=\"issue-navigation\" class=\"issue-navigation u-margin-s-bottom u-bg-grey1\"></ul>","language":"English","publisher":"Elsevier","doi":"10.1016/0016-7037(89)90163-4","issn":"00167037","usgsCitation":"Domagalski, J.L., Orem, W., and Eugster, H., 1989, Organic geochemistry and brine composition in Great Salt, Mono, and Walker Lakes: Geochimica et Cosmochimica Acta, v. 53, no. 11, p. 2857-2872, https://doi.org/10.1016/0016-7037(89)90163-4.","productDescription":"16 p.","startPage":"2857","endPage":"2872","numberOfPages":"16","costCenters":[{"id":154,"text":"California Water Science Center","active":true,"usgs":true}],"links":[{"id":480530,"rank":2,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1016/0016-7037(89)90163-4","text":"Publisher Index Page"},{"id":222980,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"53","issue":"11","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a6fb7e4b0c8380cd75c14","contributors":{"authors":[{"text":"Domagalski, Joseph L. 0000-0002-6032-757X joed@usgs.gov","orcid":"https://orcid.org/0000-0002-6032-757X","contributorId":1330,"corporation":false,"usgs":true,"family":"Domagalski","given":"Joseph","email":"joed@usgs.gov","middleInitial":"L.","affiliations":[{"id":154,"text":"California Water Science Center","active":true,"usgs":true}],"preferred":true,"id":372163,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Orem, W. H. 0000-0003-4990-0539","orcid":"https://orcid.org/0000-0003-4990-0539","contributorId":93084,"corporation":false,"usgs":true,"family":"Orem","given":"W. H.","affiliations":[],"preferred":false,"id":372164,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Eugster, H.P.","contributorId":99992,"corporation":false,"usgs":true,"family":"Eugster","given":"H.P.","email":"","affiliations":[],"preferred":false,"id":372165,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":2000127,"text":"2000127 - 1989 - Prairie basin wetlands of the Dakotas: a community profile","interactions":[],"lastModifiedDate":"2017-12-29T12:50:38","indexId":"2000127","displayToPublicDate":"1989-01-01T00:00:00","publicationYear":"1989","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":1,"text":"Federal Government Series"},"seriesTitle":{"id":8,"text":"Biological Report","active":false,"publicationSubtype":{"id":1}},"seriesNumber":"85(7.28)","title":"Prairie basin wetlands of the Dakotas: a community profile","docAbstract":"This description of prairie basin wetlands of the Dakotas is part of a series of community profiles on ecologically important wetlands of national significance. The shallow wetlands of the Dakotas form the bulk of the portion of the Prairie Pothole Region lying within the United States. This region is famous as the producer of at least half of North America's waterfowl and an unknown, but large, proportion of other prairie-dwelling marsh and aquatic birds.The wetlands described here lie in relatively small, shallow basins that vary greatly in their ability to maintain surface water, and in their water chemistry, which varies from fresh to hypersaline. These wetlands occur in a wide variety of hydrological settings, in an area where annual and seasonal precipitation varies greatly in form and amount. Thus the presence of surface water in these wetlands is largely unpredictable. Superimposed on these phenomena are the effects of a variety of land uses, including pasture, cultivation, mechanical forage removal, idle conditions and burning. All those factors greatly affect the plant and animal communities found in these basins.This profile covers lacustrine and palustrine basins with temporarily flooded, seasonally flooded, and semipermanently flooded water regimes. Basins with these water regimes compose about 90% of the basins in the Prairie Pothole Region of the Dakotas. This profile outlines the wetland subsystems, classes and subclasses that occur in these basins, and provides a useful reference to their geologic, climatic, hydrologic, and pedologic setting.Detailed information on the biotic environment of the wetlands dealt with in this profile will be useful to scientists and resource managers. Special recognition is paid to the macrophyte and invertebrate communities, which have dynamic qualities found in few other of the world's wetland ecosystems.The most noteworthy animal inhabitants of these basins are waterfowl, which are a resource of international concern. Because of the importance of this resource, much research on the habitat use and feeding ecology of breeding waterfowl has been conducted in the region. These topics receive special attention in this profile.The Prairie Pothole Region is a major world supplier of cereal grains. Consequently, wetlands in the region are often drained for crop production or otherwise cropped when water conditions permit. These practices degrade the value of wetlands for most species of wildlife and conflict with the aims of conservationists. The subject of human uses and impacts to prairie wetlands is thus an important part of this profile.","language":"English","publisher":"U.S. Fish and Wildlife Service","publisherLocation":"Washington, DC","usgsCitation":"Kantrud, H., Krapu, G., and Swanson, G., 1989, Prairie basin wetlands of the Dakotas: a community profile: Biological Report 85(7.28), 111 p.","productDescription":"111 p.","costCenters":[{"id":480,"text":"Northern Prairie Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":198739,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad2e4b07f02db681c4a","contributors":{"authors":[{"text":"Kantrud, H.A.","contributorId":28553,"corporation":false,"usgs":true,"family":"Kantrud","given":"H.A.","email":"","affiliations":[],"preferred":false,"id":325136,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Krapu, Gary L.","contributorId":56994,"corporation":false,"usgs":true,"family":"Krapu","given":"Gary L.","affiliations":[],"preferred":false,"id":325138,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Swanson, G.A.","contributorId":49299,"corporation":false,"usgs":true,"family":"Swanson","given":"G.A.","email":"","affiliations":[],"preferred":false,"id":325137,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":1007480,"text":"1007480 - 1989 - Contaminants in foods of aquatic birds at Kesterson Reservoir, California, 1985","interactions":[],"lastModifiedDate":"2023-12-12T15:32:08.868998","indexId":"1007480","displayToPublicDate":"1989-01-01T00:00:00","publicationYear":"1989","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}},"title":"Contaminants in foods of aquatic birds at Kesterson Reservoir, California, 1985","docAbstract":"<p><span>Plants, aquatic insects, and mosquitofish (</span><i>Gambusia affinis</i><span>) were collected from Kesterson Reservoir, Merced County, California, and a nearby reference site (Volta Wildlife Area) to compare concentrations of three contaminants found in 1985 with those reported in 1983 and 1984. Mean selenium concentrations in food-chain organisms from sites at Kesterson in 1985 ranged from 26.0 μg/g (dry wt) in water boatman (Corixidae) to 119 μg/g in mosquitofish. All mean selenium concentrations at Kesterson were significantly higher than those from Volta and were sufficient to have caused the impaired avian reproduction observed at Kesterson. Boron concentrations were also significantly higher at Kesterson, and, at one pond, the mean concentration in widgeongrass (</span><i>Ruppia mari-tima</i><span>) (1,630 μg/g) was high enough to impair avian reproduction. There were no differences in arsenic concentrations between locations, and concentrations in all food-chain organisms (&lt;1.9 μg/g) were lower than those reported to cause adverse effects in wildlife. Within-location differences were observed for all three contaminants at Kesterson and for selenium at Volta, but there was no consistent pattern to these differences. Between-year comparisons showed that selenium concentrations in mosquitofish generally decreased at Kesterson, but remained about the same at Volta over the 3 years. Selenium concentrations in insects from 1985 were lower at Kesterson than 1983, but were similar to 1984. Concentrations in plants were generally higher in 1983 and lower in 1984 compared with 1985. Boron concentrations in plants were generally higher in 1985, but in mosquitofish and insects, boron concentrations remained about the same all 3 years. Most arsenic concentrations did not change significantly between years.</span></p>","language":"English","publisher":"Springer","doi":"10.1007/BF01160291","usgsCitation":"Hothem, R.L., and Ohlendorf, H.M., 1989, Contaminants in foods of aquatic birds at Kesterson Reservoir, California, 1985: Archives of Environmental Contamination and Toxicology, v. 18, p. 773-786, https://doi.org/10.1007/BF01160291.","productDescription":"14 p.","startPage":"773","endPage":"786","numberOfPages":"14","costCenters":[{"id":651,"text":"Western Ecological Research Center","active":true,"usgs":true}],"links":[{"id":130205,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"California","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -120.8613045068121,\n              37.32762574572922\n            ],\n            [\n              -121.02112001477681,\n              37.32762574572922\n            ],\n            [\n              -121.02112001477681,\n              37.102990953108474\n            ],\n            [\n              -120.8613045068121,\n              37.102990953108474\n            ],\n            [\n              -120.8613045068121,\n              37.32762574572922\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","volume":"18","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b05e4b07f02db6997ba","contributors":{"authors":[{"text":"Hothem, R. L.","contributorId":82633,"corporation":false,"usgs":true,"family":"Hothem","given":"R.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":315443,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Ohlendorf, H. M.","contributorId":28194,"corporation":false,"usgs":true,"family":"Ohlendorf","given":"H.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":315442,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":16021,"text":"ofr87217 - 1989 - Selected ground-water data, Chester County, Pennsylvania","interactions":[],"lastModifiedDate":"2023-04-04T18:30:02.633611","indexId":"ofr87217","displayToPublicDate":"1989-01-01T00:00:00","publicationYear":"1989","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"87-217","title":"Selected ground-water data, Chester County, Pennsylvania","docAbstract":"Hydrologic data for Chester County, Pennsylvania are given for 3,010 wells and 32 springs. Water levels are given for 48 observation wells measured monthly during 1936-86. Chemical analyses of ground water are given for major ions, physical properties, nutrients, metals and other trace constituents, volatile organic compounds, acid organic compounds, base-neutral organic compounds, organochlorine insecticides, polychlorinated biphenyls, polychlorinated napthalenes, organophosphorous insecticides, organic acid herbicides, triazine herbicides, other organic compounds, and radionuclides.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr87217","usgsCitation":"Sloto, R.A., 1989, Selected ground-water data, Chester County, Pennsylvania: U.S. Geological Survey Open-File Report 87-217, Report: iv, 198 p.; 2 Plates: 46.88 x 29.11 inches and 57.39 x 32.02 inches, https://doi.org/10.3133/ofr87217.","productDescription":"Report: iv, 198 p.; 2 Plates: 46.88 x 29.11 inches and 57.39 x 32.02 inches","costCenters":[{"id":532,"text":"Pennsylvania Water Science 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Ronald A. rasloto@usgs.gov","contributorId":424,"corporation":false,"usgs":true,"family":"Sloto","given":"Ronald","email":"rasloto@usgs.gov","middleInitial":"A.","affiliations":[{"id":532,"text":"Pennsylvania Water Science Center","active":true,"usgs":true}],"preferred":true,"id":172107,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70177025,"text":"70177025 - 1989 - A system for reconstituting special water qualities for use in chronic toxicity studies","interactions":[],"lastModifiedDate":"2016-10-14T14:59:09","indexId":"70177025","displayToPublicDate":"1989-01-01T00:00:00","publicationYear":"1989","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":"A system for reconstituting special water qualities for use in chronic toxicity studies","docAbstract":"<p><span>A water treatment system and procedure are described that are designed for preparing large quantities of reconstituted water with specific chemical and physical characteristics for use in chronic toxicity studies with fish and invertebrates. Water treatment units produce high-purity water in large quantities for storage in high-density cross-linked polyethylene tanks, where it is combined with various salts to reconstitute an appropriate experimental water quality that simulates potential environmental conditions for use as the test medium in an intermittent-flow proportional diluter. Several water quality characteristics for the source water and the receiving water, and respective flow rates must be considered when one calculates the chemical constituents that must be added to closely simulate the water in a potential environmental situation. The water treatment system and procedure have been used to produce four differently reconstituted experimental waters that were used in 60- to 90-day early life stage chronic toxicity studies with fish. Of the ten water quality characteristics measured in the experimental waters during the studies, eight had a coefficient of variation of &lt;5%-indicating that the various physiochemical characteristics could be precisely reproduced throughout long-term exposure studies.</span></p>","language":"English","publisher":"Elsevier","doi":"10.1016/0043-1354(89)90039-0","usgsCitation":"Hamilton, S., Faerber, N.L., and Buhl, K.J., 1989, A system for reconstituting special water qualities for use in chronic toxicity studies: Water Research, v. 23, no. 2, p. 159-165, https://doi.org/10.1016/0043-1354(89)90039-0.","productDescription":"7 p.","startPage":"159","endPage":"165","costCenters":[{"id":192,"text":"Columbia Environmental Research Center","active":true,"usgs":true}],"links":[{"id":329616,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"23","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5801eec0e4b0824b2d18c443","contributors":{"authors":[{"text":"Hamilton, Steven J.","contributorId":174108,"corporation":false,"usgs":false,"family":"Hamilton","given":"Steven J.","affiliations":[],"preferred":false,"id":651029,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Faerber, Neil L.","contributorId":175406,"corporation":false,"usgs":false,"family":"Faerber","given":"Neil","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":651030,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Buhl, Kevin J. 0000-0002-9963-2352 kevin_buhl@usgs.gov","orcid":"https://orcid.org/0000-0002-9963-2352","contributorId":1396,"corporation":false,"usgs":true,"family":"Buhl","given":"Kevin","email":"kevin_buhl@usgs.gov","middleInitial":"J.","affiliations":[{"id":192,"text":"Columbia Environmental Research Center","active":true,"usgs":true}],"preferred":true,"id":651031,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70178426,"text":"70178426 - 1989 - Distribution and bioaccumulation of selenium in aquatic microcosms","interactions":[],"lastModifiedDate":"2016-11-17T15:58:45","indexId":"70178426","displayToPublicDate":"1989-01-01T00:00:00","publicationYear":"1989","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1555,"text":"Environmental Pollution","active":true,"publicationSubtype":{"id":10}},"title":"Distribution and bioaccumulation of selenium in aquatic microcosms","docAbstract":"<p><span>Closed-system microcosms were used to study factors affecting the fate of selenium (Se) in aquatic systems. Distribution and bioaccumulation of Se varied among sediment types and Se species. A mixture of dissolved </span><sup>75</sup><span>Se species (selenate, selenite and selenomethionine) was sorbed more rapidly to fine-textured, highly organic pond sediments than to sandy riverine sediments. Sulfate did not affect the distribution and bioaccumulation of </span><sup>75</sup><span>Se over the range 80–180 mg SO</span><sub>4</sub><span> liter</span><sup>−1</sup><span>. When each Se species was labeled separately, selenomethionine was lost from the water column more rapidly than selenate or selenite. Selenium lost from the water column accumulated primarily in sediments, but volatilization was also an important pathway for loss of Se added as selenomethionine. Loss rates of dissolved Se residues were more rapid than rates reported from mesocosm and field studies, suggesting that sediment: water interactions are more important in microcosms than in larger test systems. Daphnids accumulated highest concentrations of Se, followed by periphyton and macrophytes. Selenium added as selenomethionine was bioaccumulated preferentially compared to that added as selenite or selenate. Organoselenium compounds such as selenomethione may thus contribute disproportionately to Se bioaccumulation and toxicity in aquatic organisms.</span></p>","language":"English","publisher":"Elsevier","doi":"10.1016/0269-7491(89)90091-2","usgsCitation":"Besser, J.M., Huckins, J.N., Little, E.E., and La Point, T.W., 1989, Distribution and bioaccumulation of selenium in aquatic microcosms: Environmental Pollution, v. 62, no. 1, p. 1-12, https://doi.org/10.1016/0269-7491(89)90091-2.","productDescription":"12 p.","startPage":"1","endPage":"12","costCenters":[{"id":192,"text":"Columbia Environmental Research Center","active":true,"usgs":true}],"links":[{"id":331123,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"62","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"582ecff5e4b04d580bd43554","contributors":{"authors":[{"text":"Besser, John M. 0000-0002-9464-2244 jbesser@usgs.gov","orcid":"https://orcid.org/0000-0002-9464-2244","contributorId":2073,"corporation":false,"usgs":true,"family":"Besser","given":"John","email":"jbesser@usgs.gov","middleInitial":"M.","affiliations":[{"id":192,"text":"Columbia Environmental Research Center","active":true,"usgs":true}],"preferred":true,"id":654067,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Huckins, James N.","contributorId":83454,"corporation":false,"usgs":true,"family":"Huckins","given":"James","email":"","middleInitial":"N.","affiliations":[{"id":192,"text":"Columbia Environmental Research Center","active":true,"usgs":true}],"preferred":false,"id":654068,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Little, Edward E. 0000-0003-0034-3639 elittle@usgs.gov","orcid":"https://orcid.org/0000-0003-0034-3639","contributorId":1746,"corporation":false,"usgs":true,"family":"Little","given":"Edward","email":"elittle@usgs.gov","middleInitial":"E.","affiliations":[{"id":192,"text":"Columbia Environmental Research Center","active":true,"usgs":true}],"preferred":true,"id":654069,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"La Point, Thomas W.","contributorId":114142,"corporation":false,"usgs":true,"family":"La Point","given":"Thomas","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":654070,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70015132,"text":"70015132 - 1989 - Effect of climate change on watershed runoff","interactions":[],"lastModifiedDate":"2012-03-12T17:18:56","indexId":"70015132","displayToPublicDate":"1989-01-01T00:00:00","publicationYear":"1989","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"Effect of climate change on watershed runoff","docAbstract":"This paper examines forecasts of changes in watershed runoff in the Delaware River basin that result from a range of predicted effects of increased atmospheric carbon dioxide (CO2) on future precipitation, temperature, and stomatal resistance of plants. A deterministic hydrologic model, TOPMODEL, was driven with stochastic inputs of temperature and precipitation to derive the forecasts. Results indicate that the direction and magnitude of the changes in watershed runoff are dependent on the relative magnitudes of the induced changes in precipitation, temperature, and stomatal resistance. Natural variability in temperature and precipitation obscured the changes in watershed runoff even when the simulated changes in precipitation, temperature, and stomatal resistance were substantial.","conferenceTitle":"Proceedings of the 1989 National Conference on Hydraulic Engineering","conferenceDate":"14 August 1989 through 18 August 1989","conferenceLocation":"New Orleans, LA, USA","language":"English","publisher":"Publ by ASCE","publisherLocation":"New York, NY, United States","isbn":"0872627195","usgsCitation":"Wolock, D., Ayers, M.A., Hay, L., and McCabe, G.J., 1989, Effect of climate change on watershed runoff, Proceedings of the 1989 National Conference on Hydraulic Engineering, New Orleans, LA, USA, 14 August 1989 through 18 August 1989, p. 673-678.","startPage":"673","endPage":"678","numberOfPages":"6","costCenters":[],"links":[{"id":223581,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a05cae4b0c8380cd50f6e","contributors":{"authors":[{"text":"Wolock, D.M. 0000-0002-6209-938X","orcid":"https://orcid.org/0000-0002-6209-938X","contributorId":36601,"corporation":false,"usgs":true,"family":"Wolock","given":"D.M.","affiliations":[],"preferred":false,"id":370161,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Ayers, M. A.","contributorId":41417,"corporation":false,"usgs":true,"family":"Ayers","given":"M.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":370162,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Hay, L.E.","contributorId":54253,"corporation":false,"usgs":true,"family":"Hay","given":"L.E.","email":"","affiliations":[],"preferred":false,"id":370163,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"McCabe, G. J. Jr.","contributorId":77551,"corporation":false,"usgs":true,"family":"McCabe","given":"G.","suffix":"Jr.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":370164,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":47725,"text":"wri874236 - 1989 - Potentiometric surface of the Peedee aquifer in the central coastal plain of North Carolina, December 1986","interactions":[],"lastModifiedDate":"2023-03-31T19:30:05.086041","indexId":"wri874236","displayToPublicDate":"1989-01-01T00:00:00","publicationYear":"1989","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":"87-4236","title":"Potentiometric surface of the Peedee aquifer in the central coastal plain of North Carolina, December 1986","docAbstract":"Water level measurements were made in 37 wells open to the Peedee aquifer at the end of 1986 to determine the configuration of its potentiometric surface over an area of about 4,100 square miles in the central Coastal Plain of North Carolina. The potentiometric surface of the Peedee slopes southeastward from an altitude of more than 100 ft above sea level along the western limits of the aquifer to less than 20 ft near the coastline. Several cones of depression have formed in response to the effects of groundwater pumpage. The largest cone occurs near the City of Jacksonville in Onslow County where the potentiometric surface is nearly 70 ft below sea level.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri874236","usgsCitation":"Brockman, A., Lyke, W.L., and Winner, M.D., 1989, Potentiometric surface of the Peedee aquifer in the central coastal plain of North Carolina, December 1986: U.S. Geological Survey Water-Resources Investigations Report 87-4236, 1 Plate: 11.54 x 13.77 inches, https://doi.org/10.3133/wri874236.","productDescription":"1 Plate: 11.54 x 13.77 inches","costCenters":[{"id":13634,"text":"South Atlantic Water Science Center","active":true,"usgs":true}],"links":[{"id":161985,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":415028,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_46889.htm","linkFileType":{"id":5,"text":"html"}},{"id":84632,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1987/4236/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"North Carolina","otherGeospatial":"Coastal Plain, Peedee aquifer","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -77.89306640625,\n              34.08906131584994\n            ],\n            [\n              -77.77221679687499,\n              34.252676117101515\n            ],\n            [\n              -77.62939453125,\n              34.379712580462176\n            ],\n            [\n              -77.2998046875,\n              34.56085936708384\n            ],\n            [\n              -77.574462890625,\n              34.93097858831627\n            ],\n            [\n              -77.28881835937499,\n              35.27701633139884\n            ],\n            [\n              -77.27783203124999,\n              35.98689628443789\n            ],\n            [\n              -78.36547851562499,\n              36.37706783983682\n            ],\n            [\n              -79.07958984375,\n              35.862343734896484\n            ],\n            [\n              -78.99169921875,\n              35.36217605914681\n            ],\n            [\n              -78.60717773437499,\n              35.31736632923788\n            ],\n            [\n              -78.25561523437499,\n              35.01200204316073\n            ],\n            [\n              -78.44238281249999,\n              34.50655662164561\n            ],\n            [\n              -77.89306640625,\n              34.08906131584994\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad4e4b07f02db682f24","contributors":{"authors":[{"text":"Brockman, Allen R.","contributorId":91828,"corporation":false,"usgs":true,"family":"Brockman","given":"Allen R.","affiliations":[],"preferred":false,"id":236091,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Lyke, William L.","contributorId":38616,"corporation":false,"usgs":true,"family":"Lyke","given":"William","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":236089,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Winner, M. D. Jr.","contributorId":51766,"corporation":false,"usgs":true,"family":"Winner","given":"M.","suffix":"Jr.","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":236090,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70015197,"text":"70015197 - 1989 - Water solubility enhancements of DDT and trichlorobenzene by some surfactants below and above the critical micelle concentration","interactions":[],"lastModifiedDate":"2020-01-12T10:12:36","indexId":"70015197","displayToPublicDate":"1989-01-01T00:00:00","publicationYear":"1989","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1414,"text":"ES and T Contents","active":true,"publicationSubtype":{"id":10}},"title":"Water solubility enhancements of DDT and trichlorobenzene by some surfactants below and above the critical micelle concentration","docAbstract":"Water solubility enhancements of 1,1-bis(p-chlorophenyl)-2,2,2-trichloroethane (DDT) and 1,2,3-trichlorobenzene (TCB) by aqueous surfactants below and above their critical micelle concentrations (CMCs) have been studied at room temperature with the following surfactants: Triton X-100, Triton X-114, Triton X-405, Brij 35, sodium dodecyl sulfate, and cetyltrimethylammonium bromide. While the solubilities of DDT and TCB are greatly enhanced by all surfactants above the measured CMC, DDT also exhibits significant solubility enhancements below the CMC of the molecularly nonhomogeneous surfactants (the Triton series and Brij 35). The plot of the apparent DDT solubility against the concentration of Triton and Brij surfactants shows an uprising curve below the nominal CMC, which is attributed to the successive micellization of the heterogeneous monomer species. Above the CMC, the enhancement effect with the nonionic surfactants is closely proportional to the nonpolar chain content of the surfactant, whereas the effect with the ionic surfactants is less accountable in terms of their nonpolar chain contents. The solubilization power of a micelle relative to a bulk solvent is evaluated by a comparison of the observed micelle-water and solvent-water partition coefficients.","language":"English","publisher":"ACS","doi":"10.1021/es00065a012","issn":"0013936X","usgsCitation":"Kile, D.E., and Chiou, C.T., 1989, Water solubility enhancements of DDT and trichlorobenzene by some surfactants below and above the critical micelle concentration: ES and T Contents, v. 23, no. 7, p. 832-838, https://doi.org/10.1021/es00065a012.","productDescription":"7 p.","startPage":"832","endPage":"838","numberOfPages":"7","costCenters":[{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":223588,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"23","issue":"7","noUsgsAuthors":false,"publicationDate":"2002-05-01","publicationStatus":"PW","scienceBaseUri":"505bcc73e4b08c986b32db5a","contributors":{"authors":[{"text":"Kile, D. E.","contributorId":22758,"corporation":false,"usgs":true,"family":"Kile","given":"D.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":370302,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Chiou, C. T.","contributorId":97080,"corporation":false,"usgs":true,"family":"Chiou","given":"C.","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":370303,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70015119,"text":"70015119 - 1989 - Hydrologic effects on water level changes associated with episodic fault creep near Parkfield, California","interactions":[],"lastModifiedDate":"2024-05-30T16:11:39.849828","indexId":"70015119","displayToPublicDate":"1989-01-01T00:00:00","publicationYear":"1989","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":"Hydrologic effects on water level changes associated with episodic fault creep near Parkfield, California","docAbstract":"<p><span>As part of the Parkfield, California, earthquake prediction experiment, water level is monitored in a well 460 m from the main trace of the San Andreas fault on Middle Mountain, in the preparation zone of the anticipated Parkfield earthquake. The well configuration allows water level to be monitored in two fluid reservoirs at depths of 85 and 250 m below land surface. During 1987, water level changes were recorded during 12 of the 18 episodes of accelerated fault creep detected by a creep meter spanning the fault trace 750 m northwest of the well. The creep-related water level changes in the shallow reservoir have durations of less than 1 day, whereas in the deeper reservoir the changes persist for as long as 2 months. These data suggest that the transient nature of the water level changes in the shallow interval is due to vertical flow to the water table and is not evidence that creep events propagate past the well. Phase leads of earth tidal constituents in the water level data from the shallow interval relative to the same constituents in the local volume strain tide support the interpretation of significant flow to the water table at periods of 1 day or less. The form of the water level changes in the deep interval is affected by horizontal flow to the well bore. This effect can be removed from the water level records using a theoretical response curve constrained by the phases of earth tidal constituents in the deep interval relative to the local volume strain tide. For the events where the signal in the shallow interval has been large enough to measure, the sizes of the simultaneous water level changes in the two reservoirs are consistent with the same amounts of volume strain occurring at both depths.</span></p>","language":"English","publisher":"American Geophysical Union","doi":"10.1029/JB094iB09p12387","issn":"01480227","usgsCitation":"Roeloffs, E., Burford, S., Riley, F.S., and Records, A., 1989, Hydrologic effects on water level changes associated with episodic fault creep near Parkfield, California: Journal of Geophysical Research Solid Earth, v. 94, no. B9, p. 12387-12402, https://doi.org/10.1029/JB094iB09p12387.","productDescription":"16 p.","startPage":"12387","endPage":"12402","costCenters":[],"links":[{"id":224235,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"94","issue":"B9","noUsgsAuthors":false,"publicationDate":"2012-09-20","publicationStatus":"PW","scienceBaseUri":"505a3622e4b0c8380cd6048b","contributors":{"authors":[{"text":"Roeloffs, E.A.","contributorId":88742,"corporation":false,"usgs":true,"family":"Roeloffs","given":"E.A.","email":"","affiliations":[],"preferred":false,"id":370127,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Burford, S.S.","contributorId":85335,"corporation":false,"usgs":true,"family":"Burford","given":"S.S.","email":"","affiliations":[],"preferred":false,"id":370126,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Riley, F. S.","contributorId":7701,"corporation":false,"usgs":true,"family":"Riley","given":"F.","middleInitial":"S.","affiliations":[],"preferred":false,"id":370125,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Records, A.W.","contributorId":107860,"corporation":false,"usgs":true,"family":"Records","given":"A.W.","email":"","affiliations":[],"preferred":false,"id":370128,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
]}