Diel changes of dissolved oxygen (DO) and pH were measured during 1981–1982 in Pool 1, a shallow reservoir in southeast Missouri. Diel changes in spring and fall were about half those of summer when extensive macrophyte biomass apparently had a strong influence on dynamics of DO and pH. During summer, daily pulses averaged 5.45 mg/L DO and 0.88 pH units, and extreme diel changes were 10–14 mg/L DO and 2–3 pH units. Ambient values of DO and pH were directly related to each other as was the magnitude of their daily changes because in the low alkalinity water of Pool 1, pH as well as DO responded to photosynthesis and respiration. Magnitudes of DO and pH changes at night were strongly related to fluctuations during the day, suggesting that community respiration was in a steady state relationship with photosynthesis over time.
No abstract available.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/coal94B","usgsCitation":"Sanchez, J., and Brown, T.L., 1987, Stratigraphic framework and coal resources of the Upper Cretaceous Blackhawk Formation in the Ferron Canyon and Rock Canyon areas of the Wasatch Plateau coal field, Manti 30' x 60' Quadrangle, Emery and Sanpete counties, Utah: U.S. Geological Survey Coal Map 94, 3 Plates: 55.50 x 39.77 inches or smaller, https://doi.org/10.3133/coal94B.","productDescription":"3 Plates: 55.50 x 39.77 inches or smaller","costCenters":[],"links":[{"id":185530,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/coal/094b/plate-1-thumb.jpg"},{"id":115342,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/coal/094b/plate-3.pdf","size":"5704","linkFileType":{"id":1,"text":"pdf"}},{"id":115341,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/coal/094b/plate-2.pdf","size":"6522","linkFileType":{"id":1,"text":"pdf"}},{"id":115340,"rank":399,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/coal/094b/plate-1.pdf","size":"10764","linkFileType":{"id":1,"text":"pdf"}}],"scale":"24000","country":"United States","state":"Utah","county":"Emery County, Sanpete County","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -111.36749999999999,39.1175 ], [ -111.36749999999999,39.25 ], [ -111.11749999999999,39.25 ], [ -111.11749999999999,39.1175 ], [ -111.36749999999999,39.1175 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b25e4b07f02db6af650","contributors":{"authors":[{"text":"Sanchez, J. D.","contributorId":35292,"corporation":false,"usgs":true,"family":"Sanchez","given":"J. D.","affiliations":[],"preferred":false,"id":279734,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Brown, Terrence L.","contributorId":88431,"corporation":false,"usgs":true,"family":"Brown","given":"Terrence","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":279735,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":1007766,"text":"1007766 - 1987 - Activity of the arboreal brown tree snake (Boiga irregularis) as determined by electrical outages","interactions":[],"lastModifiedDate":"2013-04-17T21:26:27","indexId":"1007766","displayToPublicDate":"1987-01-01T00:00:00","publicationYear":"1987","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3399,"text":"Snake","active":true,"publicationSubtype":{"id":10}},"title":"Activity of the arboreal brown tree snake (Boiga irregularis) as determined by electrical outages","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Snake","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","usgsCitation":"Fritts, T.H., Scott, N., and Savidge, J.A., 1987, Activity of the arboreal brown tree snake (Boiga irregularis) as determined by electrical outages: Snake, v. 19, p. 51-58.","productDescription":"p. 51-58","startPage":"51","endPage":"58","numberOfPages":"8","costCenters":[{"id":651,"text":"Western Ecological Research Center","active":true,"usgs":true}],"links":[{"id":130116,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"19","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b05e4b07f02db699ce0","contributors":{"authors":[{"text":"Fritts, T. H.","contributorId":40147,"corporation":false,"usgs":true,"family":"Fritts","given":"T.","middleInitial":"H.","affiliations":[],"preferred":false,"id":315996,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Scott, N.J. Jr.","contributorId":8407,"corporation":false,"usgs":true,"family":"Scott","given":"N.J.","suffix":"Jr.","email":"","affiliations":[],"preferred":false,"id":315994,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Savidge, J. A.","contributorId":36078,"corporation":false,"usgs":false,"family":"Savidge","given":"J.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":315995,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":70015124,"text":"70015124 - 1987 - A model for trace metal sorption processes at the calcite surface: Adsorption of Cd2+ and subsequent solid solution formation","interactions":[],"lastModifiedDate":"2020-03-05T19:46:45","indexId":"70015124","displayToPublicDate":"1987-01-01T00:00:00","publicationYear":"1987","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":"A model for trace metal sorption processes at the calcite surface: Adsorption of Cd2+ and subsequent solid solution formation","docAbstract":"The rate of Cd2+ sorption by calcite was determined as a function of pH and Mg2+ in aqueous solutions saturated with respect to calcite but undersaturated with respect to CdCO3. The sorption is characterized by two reaction steps, with the first reaching completion within 24 hours. The second step proceeded at a slow and nearly constant rate for at least 7 days. The rate of calcite recrystallization was also studied, using a Ca2+ isotopic exchange technique. Both the recrystallization rate of calcite and the rate of slow Cd2+ sorption decrease with increasing pH or with increasing Mg2+. The recrystallization rate could be predicted from the number of moles of Ca present in the hydrated surface layer. A model is presented which is consistent with the rates of Cd2+ sorption and Ca2+ isotopic exchange. In the model, the first step in Cd2+ sorption involves a fast adsorption reaction that is followed by diffusion of Cd2+ into a surface layer of hydrated CaCO3 that overlies crystalline calcite. Desorption of Cd2+ from the hydrated layer is slow. The second step is solid solution formation in new crystalline material, which grows from the disordered mixture of Cd and Ca carbonate in the hydrated surface layer. Calculated distribution coefficients for solid solutions formed at the surface are slightly greater than the ratio of equilibrium constants for dissolution of calcite and CdCO3, which is the value that would be expected for an ideal solid solution in equilibrium with the aqueous solution. ?? 1987.","language":"English","publisher":"Elsevier","doi":"10.1016/0016-7037(87)90330-9","issn":"00167037","usgsCitation":"Davis, J., Fuller, C.C., and Cook, A., 1987, A model for trace metal sorption processes at the calcite surface: Adsorption of Cd2+ and subsequent solid solution formation: Geochimica et Cosmochimica Acta, v. 51, no. 6, p. 1477-1490, https://doi.org/10.1016/0016-7037(87)90330-9.","productDescription":"14 p.","startPage":"1477","endPage":"1490","numberOfPages":"14","costCenters":[{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":224289,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"51","issue":"6","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059e47de4b0c8380cd46671","contributors":{"authors":[{"text":"Davis, J.A.","contributorId":71694,"corporation":false,"usgs":true,"family":"Davis","given":"J.A.","email":"","affiliations":[],"preferred":false,"id":370136,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Fuller, C. C.","contributorId":29858,"corporation":false,"usgs":true,"family":"Fuller","given":"C.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":370134,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Cook, A.D.","contributorId":53530,"corporation":false,"usgs":true,"family":"Cook","given":"A.D.","email":"","affiliations":[],"preferred":false,"id":370135,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":70015229,"text":"70015229 - 1987 - NONHOMOGENEOUS TERMS IN THE UNSTEADY FLOW EQUATIONS: MODELING ASPECTS.","interactions":[],"lastModifiedDate":"2012-03-12T17:18:54","indexId":"70015229","displayToPublicDate":"1987-01-01T00:00:00","publicationYear":"1987","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"NONHOMOGENEOUS TERMS IN THE UNSTEADY FLOW EQUATIONS: MODELING ASPECTS.","docAbstract":"A study is in progress to identify the relative significance, effects, and benefits attributable to the use of one-dimensional, unsteady, open-channel, flow-simulation models employing a variety of nonhomogeneous terms in their equation formulations. Nonhomogeneous terms being analyzed include those representing bed slope, frictional resistance, nonprismatic channel geometry, lateral flow, and (surface) wind stress. After an initial theoretical discussion, the results of a set of numerical experiments are presented that demonstrate cause-and-effect relationships and intercomparisons achieved by neglect or improper treatment of important nonhomogeneous terms. Preliminary results of this study are discussed and presented in this paper, both in the form of qualitative considerations and quantitative tabular findings. These results are expected to yield a definitive set of guidelines and suggestions useful to model engineers.","conferenceTitle":"Hydraulic Engineering, Proceedings of the 1987 National Conference.","conferenceLocation":"Williamsburg, VA, USA","language":"English","publisher":"ASCE","publisherLocation":"New York, NY, USA","isbn":"0872626105","usgsCitation":"Lai, C., Schaffranek, R.W., and Baltzer, R.A., 1987, NONHOMOGENEOUS TERMS IN THE UNSTEADY FLOW EQUATIONS: MODELING ASPECTS., Hydraulic Engineering, Proceedings of the 1987 National Conference., Williamsburg, VA, USA, p. 351-358.","startPage":"351","endPage":"358","numberOfPages":"8","costCenters":[],"links":[{"id":224082,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a6169e4b0c8380cd71947","contributors":{"authors":[{"text":"Lai, Chintu","contributorId":16860,"corporation":false,"usgs":true,"family":"Lai","given":"Chintu","email":"","affiliations":[],"preferred":false,"id":370383,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Schaffranek, Raymond W.","contributorId":86314,"corporation":false,"usgs":true,"family":"Schaffranek","given":"Raymond","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":370385,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Baltzer, Robert A.","contributorId":34269,"corporation":false,"usgs":true,"family":"Baltzer","given":"Robert","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":370384,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":70015152,"text":"70015152 - 1987 - Geochemical evolution of Kohala Volcano, Hawaii","interactions":[],"lastModifiedDate":"2012-03-12T17:18:55","indexId":"70015152","displayToPublicDate":"1987-01-01T00:00:00","publicationYear":"1987","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1336,"text":"Contributions to Mineralogy and Petrology","active":true,"publicationSubtype":{"id":10}},"title":"Geochemical evolution of Kohala Volcano, Hawaii","docAbstract":"Kohala Volcano, the oldest of five shield volcanoes comprising the island of Hawaii, consists of a basalt shield dominated by tholeiitic basalt, Pololu Volcanics, overlain by alkalic lavas, Hawi Volcanics. In the upper Pololu Volcanics the lavas become more enriched in incompatible elements, and there is a transition from tholeiitic to alkalic basalt. In contrast, the Hawi volcanics consist of hawaiites, mugearites, and trachytes. 87Sr/86Sr ratios of 14 Pololu basalts and 5 Hawi lavas range from 0.70366 to 0.70392 and 0.70350 to 0.70355, respectively. This small but distinct difference in Sr isotopic composition of different lava types, especially the lower 87Sr/86Sr in the younger lavas with higher Rb/Sr, has been found at other Hawaiian volcanoes. Our data do not confirm previous data indicating Sr isotopic homogeneity among lavas from Kohala Volcano. Also some abundance trends, such as MgO-P2O5, are not consistent with a simple genetic relationship between Pololu and Hawi lavas. We conclude that all Kohala lavas were not produced by equilibrium partial melting of a compositionally homogeneous source. ?? 1987 Springer-Verlag.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Contributions to Mineralogy and Petrology","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisherLocation":"Springer-Verlag","doi":"10.1007/BF00518033","issn":"00107999","usgsCitation":"Lanphere, M.A., and Frey, F., 1987, Geochemical evolution of Kohala Volcano, Hawaii: Contributions to Mineralogy and Petrology, v. 95, no. 1, p. 100-113, https://doi.org/10.1007/BF00518033.","startPage":"100","endPage":"113","numberOfPages":"14","costCenters":[],"links":[{"id":205422,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1007/BF00518033"},{"id":223857,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"95","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a1636e4b0c8380cd550bd","contributors":{"authors":[{"text":"Lanphere, M. A.","contributorId":35298,"corporation":false,"usgs":true,"family":"Lanphere","given":"M.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":370209,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Frey, F.A.","contributorId":12618,"corporation":false,"usgs":true,"family":"Frey","given":"F.A.","email":"","affiliations":[],"preferred":false,"id":370208,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70015154,"text":"70015154 - 1987 - APPLICATIONS OF CATHODOLUMINESCENCE OF QUARTZ AND FELDSPAR TO SEDIMENTARY PETROLOGY.","interactions":[],"lastModifiedDate":"2012-03-12T17:18:55","indexId":"70015154","displayToPublicDate":"1987-01-01T00:00:00","publicationYear":"1987","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3336,"text":"Scanning Micros","active":true,"publicationSubtype":{"id":10}},"title":"APPLICATIONS OF CATHODOLUMINESCENCE OF QUARTZ AND FELDSPAR TO SEDIMENTARY PETROLOGY.","docAbstract":"Cathodoluminescence (CL), the emission of visible light during electron bombardment, was first used in sandstone petrology in the mid-1960's. CL techniques are especially useful for determining the origin and source of quartz and feldspar, two of the most common constituents in clastic rocks. CL properties of both minerals are dependent on their temperature of crystallization, duration of cooling, and/or history of deformation. Detrital quartz and feldspar are typically derived from igneous and metamorphic sources and luminesce in the visible range whereas authigenic quartz and feldspar form at low temperatures and do not luminesce. Quantification of luminescent and non-luminescent quartz and feldspar with the scanning electron microscope, electron microprobe, or a commercial CL device can allow for the determination of origin, diagenesis, and source of clastic rocks when used in conjunction with field and other petrographic analyses.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Scanning Micros","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","issn":"08917035","usgsCitation":"Ruppert, L.F., 1987, APPLICATIONS OF CATHODOLUMINESCENCE OF QUARTZ AND FELDSPAR TO SEDIMENTARY PETROLOGY.: Scanning Micros, v. 1, no. 1, p. 63-72.","startPage":"63","endPage":"72","numberOfPages":"10","costCenters":[],"links":[{"id":223859,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"1","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059e631e4b0c8380cd4722f","contributors":{"authors":[{"text":"Ruppert, Leslie F. 0000-0002-7453-1061 lruppert@usgs.gov","orcid":"https://orcid.org/0000-0002-7453-1061","contributorId":660,"corporation":false,"usgs":true,"family":"Ruppert","given":"Leslie","email":"lruppert@usgs.gov","middleInitial":"F.","affiliations":[{"id":245,"text":"Eastern Mineral and Environmental Resources Science Center","active":true,"usgs":true},{"id":241,"text":"Eastern Energy Resources Science Center","active":true,"usgs":true}],"preferred":true,"id":370212,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70015151,"text":"70015151 - 1987 - Analyzing numerical errors in domain heat transport models using the CVBEM","interactions":[],"lastModifiedDate":"2024-05-10T16:30:43.155146","indexId":"70015151","displayToPublicDate":"1987-01-01T00:00:00","publicationYear":"1987","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2406,"text":"Journal of Offshore Mechanics and Arctic Engineering","active":true,"publicationSubtype":{"id":10}},"title":"Analyzing numerical errors in domain heat transport models using the CVBEM","docAbstract":"Besides providing an exact solution for steady-state heat conduction processes (Laplace-Poisson equations), the CVBEM (complex variable boundary element method) can be used for the numerical error analysis of domain model solutions. For problems where soil-water phase change latent heat effects dominate the thermal regime, heat transport can be approximately modeled as a time-stepped steady-state condition in the thawed and frozen regions, respectively. The CVBEM provides an exact solution of the two-dimensional steady-state heat transport problem, and also provides the error in matching the prescribed boundary conditions by the development of a modeling error distribution or an approximate boundary generation. Consequently, this error evaluation can be used to develop highly accurate CVBEM models of the heat transport process, and the resulting model can be used as a test case for evaluating the precision of domain models based on finite elements or finite differences.
","language":"English","publisher":"ASME","doi":"10.1115/1.3257005","issn":"08927219","usgsCitation":"Hromadka, T., 1987, Analyzing numerical errors in domain heat transport models using the CVBEM: Journal of Offshore Mechanics and Arctic Engineering, v. 109, no. 2, p. 163-169, https://doi.org/10.1115/1.3257005.","productDescription":"7 p.","startPage":"163","endPage":"169","costCenters":[],"links":[{"id":223805,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"109","issue":"2","noUsgsAuthors":false,"publicationDate":"1987-05-01","publicationStatus":"PW","scienceBaseUri":"5059e62ee4b0c8380cd4720a","contributors":{"authors":[{"text":"Hromadka, T. V. II","contributorId":76464,"corporation":false,"usgs":true,"family":"Hromadka","given":"T. V.","suffix":"II","affiliations":[],"preferred":false,"id":370207,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70015123,"text":"70015123 - 1987 - Computer graphics for quality control in the INAA of geological samples","interactions":[],"lastModifiedDate":"2012-03-12T17:19:00","indexId":"70015123","displayToPublicDate":"1987-01-01T00:00:00","publicationYear":"1987","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2440,"text":"Journal of Radioanalytical and Nuclear Chemistry Articles","active":true,"publicationSubtype":{"id":10}},"title":"Computer graphics for quality control in the INAA of geological samples","docAbstract":"A data reduction system for the routine instrumental activation analysis of samples is described, with particular emphasis on interactive graphics capabilities for evaluating analytical quality. Graphics procedures have been developed to interactively control the analysis of selected photopeaks during spectral analysis, and to evaluate detector performance during a given counting cycle. Graphics algorithms are also used to compare the data on reference samples with accepted values, to prepare quality control charts to evaluate long term precision and to search for systematic variations in data on reference samples as a function of time. ?? 1987 Akade??miai Kiado??.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Journal of Radioanalytical and Nuclear Chemistry Articles","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisherLocation":"Kluwer Academic Publishers","doi":"10.1007/BF02036047","issn":"02365731","usgsCitation":"Grossman, J.N., and Baedecker, P.A., 1987, Computer graphics for quality control in the INAA of geological samples: Journal of Radioanalytical and Nuclear Chemistry Articles, v. 113, no. 1, p. 43-59, https://doi.org/10.1007/BF02036047.","startPage":"43","endPage":"59","numberOfPages":"17","costCenters":[],"links":[{"id":224239,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":205458,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1007/BF02036047"}],"volume":"113","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059f957e4b0c8380cd4d590","contributors":{"authors":[{"text":"Grossman, J. N.","contributorId":41840,"corporation":false,"usgs":true,"family":"Grossman","given":"J.","email":"","middleInitial":"N.","affiliations":[],"preferred":false,"id":370132,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Baedecker, P. A.","contributorId":95444,"corporation":false,"usgs":true,"family":"Baedecker","given":"P.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":370133,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":57334,"text":"wdrWV851 - 1987 - Water Resources Data for West Virginia, Water Year 1985","interactions":[],"lastModifiedDate":"2025-01-14T22:08:28.391371","indexId":"wdrWV851","displayToPublicDate":"1987-01-01T00:00:00","publicationYear":"1987","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":340,"text":"Water Data Report","code":"WDR","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"WV-85-1","title":"Water Resources Data for West Virginia, Water Year 1985","docAbstract":"Water resources data for the 1985 water year for West Virginia consist of records of stage, discharge, and water quality of streams; contents of reservoirs; and water levels and water quality of observation wells. This report contains discharge records for 75 streamflow-gaging stations; stage only records for 12 gaging stations, and 2 crest-stage partial-record stations; (2) contents for 2 reservoirs, and change in contents for 1 reservoir; (3) water-quality records for 24 streamflow-gaging stations; (4) water-level records for 33 observation wells; and (5) water-quality records for 17 observation wells. Locations of these sites are shown on figures 4 and 5. Additional water data were collected at various sites, not involved in the systematic data collection program, and are published as miscellaneous measurements. These data represent that part of the National Water Data System collected by the U.S. Geological Survey and cooperating State and Federal agencies in West Virginia.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wdrWV851","collaboration":"Prepared in cooperation with the State of West Virginia and with other agencies","usgsCitation":"Embree, W., Friel, E., and Taylor, F., 1987, Water Resources Data for West Virginia, Water Year 1985: U.S. Geological Survey Water Data Report WV-85-1, viii, 224 p., https://doi.org/10.3133/wdrWV851.","productDescription":"viii, 224 p.","costCenters":[],"links":[{"id":466319,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wdr/1985/wv-85-1/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":184497,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wdr/1985/wv-85-1/report-thumb.jpg"}],"country":"United States","state":"West 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Although the area was sparsely populated,the earthquakes, generally referred to as the New Madrid earthquakes, were felt throughout a wide area if the Central and Eastern United States. Consequently, they were widely reported in newspapers and in other written accounts.
","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","usgsCitation":"U.S. Geological Survey, 1987, Accounts describing the Mississippi Valley Earthquakes of 1811-12: Earthquakes & Volcanoes (USGS), v. 19, no. 6, p. 212-217.","productDescription":"6 p.","startPage":"212","endPage":"217","temporalStart":"1811-12-16","temporalEnd":"1812-02-29","costCenters":[],"links":[{"id":328503,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -92.26184550019639,\n 39.28013441672701\n ],\n [\n -88.77768557664305,\n 34.81154911352175\n ],\n [\n -80.2738141638751,\n 33.13776512800938\n ],\n [\n -75.08433556275008,\n 36.98197959860714\n ],\n [\n -71.1888303263107,\n 42.181366039517314\n ],\n [\n -76.24500676233586,\n 45.07094044357041\n ],\n [\n -77.79425636048583,\n 43.009793273505665\n ],\n [\n -83.12431998271089,\n 41.647322192326044\n ],\n [\n -91.81052049958322,\n 40.11009539133286\n ],\n [\n -92.26184550019639,\n 39.28013441672701\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","volume":"19","issue":"6","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"57d7d1ade4b090824ff98cce"} ,{"id":70015215,"text":"70015215 - 1987 - The hydrothermal system of the Calabozos caldera, central Chilean Andes","interactions":[],"lastModifiedDate":"2012-03-12T17:18:55","indexId":"70015215","displayToPublicDate":"1987-01-01T00:00:00","publicationYear":"1987","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2499,"text":"Journal of Volcanology and Geothermal Research","active":true,"publicationSubtype":{"id":10}},"title":"The hydrothermal system of the Calabozos caldera, central Chilean Andes","docAbstract":"Active thermal springs associated with the late Pleistocene Calabozos caldera complex occur in two groups: the Colorado group which issues along structures related to caldera collapse and resurgence, and the Puesto Calabozos group, a nearby cluster that is chemically distinct and probably unrelated to the Colorado springs. Most of the Colorado group can be related to a hypothetical parent water containing ???400 ppm Cl at ???250??C by dilution with ???50% of cold meteoric water. The thermal springs in the most deeply eroded part of the caldera were derived from the same parent water by boiling. The hydrothermal system has probably been active for at least as long as 300,000 years, based on geologic evidence and calculations of paleo-heat flow. There is no evidence for economic mineralization at shallow depth. The Calabozos hydrothermal system would be an attractive geothermal prospect were its location not so remote. ?? 1987.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Journal of Volcanology and Geothermal Research","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","issn":"03770273","usgsCitation":"Grunder, A., Thompson, J., and Hildreth, W., 1987, The hydrothermal system of the Calabozos caldera, central Chilean Andes: Journal of Volcanology and Geothermal Research, v. 32, no. 4, p. 287-298.","startPage":"287","endPage":"298","numberOfPages":"12","costCenters":[],"links":[{"id":223862,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"32","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505bacd1e4b08c986b32376f","contributors":{"authors":[{"text":"Grunder, A.L.","contributorId":71314,"corporation":false,"usgs":true,"family":"Grunder","given":"A.L.","affiliations":[],"preferred":false,"id":370341,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Thompson, J. 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Self-reproducing stocks of lake trout (Salvelinus namaycush) have been reestablished in many inshore areas, although they have not yet reached pre-sea lamprey abundance; offshore lake trout are probably at or near pre-sea lamprey abundance. Stocks of lake whitefish (Coregonus clupeaformis) appear to have fully recovered; commercial catches are at or above historical levels. Lake herring (Coregonus artedii) are recovering rapidly in U.S. waters and are abundant in western Canadian waters. The population of rainbow smelt (Osmerus mordax), which declined in the 1970s, is recovering. Pacific salmon (Oncorhynchus) are becoming more abundant as a result of increased stocking in U.S. waters and are reproducing in most suitable tributaries; they have become significant in anglers' creels.
","language":"English","publisher":"NRC Research Press","doi":"10.1139/f87-306","usgsCitation":"MacCallum, W.R., and Selgeby, J.H., 1987, Lake Superior revisited 1984: Canadian Journal of Fisheries and Aquatic Sciences, v. 44, no. Suppl. 2, p. 23-36, https://doi.org/10.1139/f87-306.","productDescription":"14 p.","startPage":"23","endPage":"36","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":324,"text":"Great Lakes Science Center","active":true,"usgs":true}],"links":[{"id":128700,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"44","issue":"Suppl. 2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b32e4b07f02db6b4269","contributors":{"authors":[{"text":"MacCallum, Wayne R.","contributorId":53727,"corporation":false,"usgs":true,"family":"MacCallum","given":"Wayne","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":308768,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Selgeby, James H.","contributorId":89828,"corporation":false,"usgs":true,"family":"Selgeby","given":"James","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":308769,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":1000555,"text":"1000555 - 1987 - Predicting Great Lakes fish yields: tools and constraints","interactions":[],"lastModifiedDate":"2016-03-25T10:29:19","indexId":"1000555","displayToPublicDate":"1987-01-01T00:00:00","publicationYear":"1987","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1169,"text":"Canadian Journal of Fisheries and Aquatic Sciences","active":true,"publicationSubtype":{"id":10}},"title":"Predicting Great Lakes fish yields: tools and constraints","docAbstract":"Prediction of yield is a critical component of fisheries management. The development of sound yield prediction methodology and the application of the results of yield prediction are central to the evolution of strategies to achieve stated goals for Great Lakes fisheries and to the measurement of progress toward those goals. Despite general availability of species yield models, yield prediction for many Great Lakes fisheries has been poor due to the instability of the fish communities and the inadequacy of available data. A host of biological, institutional, and societal factors constrain both the development of sound predictions and their application to management. Improved predictive capability requires increased stability of Great Lakes fisheries through rehabilitation of well-integrated communities, improvement of data collection, data standardization and information-sharing mechanisms, and further development of the methodology for yield prediction. Most important is the creation of a better-informed public that will in turn establish the political will to do what is required.
","language":"English","publisher":"NRC Research Press","doi":"10.1139/f87-342","usgsCitation":"Lewis, C., Schupp, D., Taylor, W., Collins, J., and Hatch, R.W., 1987, Predicting Great Lakes fish yields: tools and constraints: Canadian Journal of Fisheries and Aquatic Sciences, v. 44, no. Suppl. 2, p. 411-416, https://doi.org/10.1139/f87-342.","productDescription":"6 p.","startPage":"411","endPage":"416","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":324,"text":"Great Lakes Science Center","active":true,"usgs":true}],"links":[{"id":133141,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"44","issue":"Suppl. 2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b08e4b07f02db69b2d8","contributors":{"authors":[{"text":"Lewis, C.A.","contributorId":85927,"corporation":false,"usgs":true,"family":"Lewis","given":"C.A.","email":"","affiliations":[],"preferred":false,"id":308760,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Schupp, D.H.","contributorId":99943,"corporation":false,"usgs":true,"family":"Schupp","given":"D.H.","email":"","affiliations":[],"preferred":false,"id":308761,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Taylor, W.W.","contributorId":61002,"corporation":false,"usgs":true,"family":"Taylor","given":"W.W.","email":"","affiliations":[],"preferred":false,"id":308757,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Collins, J.J.","contributorId":67844,"corporation":false,"usgs":true,"family":"Collins","given":"J.J.","email":"","affiliations":[],"preferred":false,"id":308758,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Hatch, Richard W.","contributorId":82245,"corporation":false,"usgs":true,"family":"Hatch","given":"Richard","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":308759,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}} ,{"id":1000572,"text":"1000572 - 1987 - Unusual larval habitats and life history of chironomid (Diptera) genera","interactions":[],"lastModifiedDate":"2012-02-02T00:04:39","indexId":"1000572","displayToPublicDate":"1987-01-01T00:00:00","publicationYear":"1987","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1519,"text":"Entomologica Scandinavica Supplements","active":true,"publicationSubtype":{"id":10}},"title":"Unusual larval habitats and life history of chironomid (Diptera) genera","docAbstract":"Ninety-three genera, representing all subfamilies of Chironomidae, are organized into 9 categories of unusual habitats or life history including hygropetric, riparian (bank, floodplain, upland), hyporheic, symbiotic, and intertidal; others live in water held in plants or mine into unusual substrates. In riparian zones precise location of optimum habitat is difficult to determine as is definition of habitat within the continuum from shoreline to upland areas. The ecological importance of the riparian group appears to lie in its processing of coarse particulate matter along the floodplain of streams and rivers. All riparian genera are zoogeographically useful and can be used in reconstructing evolutionary dispersal pathways because they are adapted to unique habits that have remained largely undisturbed by human activities.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Entomologica Scandinavica Supplements","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","usgsCitation":"Hudson, P.L., 1987, Unusual larval habitats and life history of chironomid (Diptera) genera: Entomologica Scandinavica Supplements, v. 29, p. 369-373.","productDescription":"p. 369-373","startPage":"369","endPage":"373","numberOfPages":"4","costCenters":[{"id":324,"text":"Great Lakes Science Center","active":true,"usgs":true}],"links":[{"id":133395,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"29","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49dfe4b07f02db5e3b5d","contributors":{"authors":[{"text":"Hudson, Patrick L. 0000-0002-7646-443X phudson@usgs.gov","orcid":"https://orcid.org/0000-0002-7646-443X","contributorId":5616,"corporation":false,"usgs":true,"family":"Hudson","given":"Patrick","email":"phudson@usgs.gov","middleInitial":"L.","affiliations":[{"id":324,"text":"Great Lakes Science Center","active":true,"usgs":true}],"preferred":true,"id":308803,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70180805,"text":"70180805 - 1987 - Life history and ecology requirements of the Moapa dace (Moapa coracea)","interactions":[],"lastModifiedDate":"2017-02-03T13:04:06","indexId":"70180805","displayToPublicDate":"1987-01-01T00:00:00","publicationYear":"1987","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":1,"text":"Federal Government Series"},"title":"Life history and ecology requirements of the Moapa dace (Moapa coracea)","docAbstract":"No abstract available
","language":"English","publisher":"U.S. Fish and Wildlife Service","usgsCitation":"Scoppettone, G., 1987, Life history and ecology requirements of the Moapa dace (Moapa coracea).","costCenters":[{"id":654,"text":"Western Fisheries Research Center","active":true,"usgs":true}],"links":[{"id":334680,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5895a4d5e4b0fa1e59bc1eae","contributors":{"authors":[{"text":"Scoppettone, G.G.","contributorId":22793,"corporation":false,"usgs":true,"family":"Scoppettone","given":"G.G.","email":"","affiliations":[],"preferred":false,"id":662474,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":1000562,"text":"1000562 - 1987 - Effects of freezing in and out of water on length and weight of Lake Michigan bloaters","interactions":[],"lastModifiedDate":"2016-03-25T10:37:11","indexId":"1000562","displayToPublicDate":"1987-01-01T00:00:00","publicationYear":"1987","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2886,"text":"North American Journal of Fisheries Management","active":true,"publicationSubtype":{"id":10}},"title":"Effects of freezing in and out of water on length and weight of Lake Michigan bloaters","docAbstract":"The purpose of this study was to determine if freezing significantly alters the length or weight of bloaters Coregonus hoyi. Bloaters were collected from southern Lake Michigan and were frozen for periods of 2-200 d. Freezing in water caused a significant decrease in length and a significant increase in weight. These changes did not vary predictably with time. The mean change in weight was greater for adults than for juveniles, but the mean change in length was not significantly different between juveniles and adults. Regressions for weight or length after freezing versus weight or length before freezing were highly significant and can be used as correction equations for estimating the original lengths and weights of fresh specimens after fish have been frozen. Test fish that were subsequently refrozen in air shrank more than those refrozen in water.
","language":"English","publisher":"Taylor & Francis","doi":"10.1577/1548-8659(1987)7<299:EOFIAO>2.0.CO;2","usgsCitation":"Sayers, R., 1987, Effects of freezing in and out of water on length and weight of Lake Michigan bloaters: North American Journal of Fisheries Management, v. 7, no. 2, p. 299-301, https://doi.org/10.1577/1548-8659(1987)7<299:EOFIAO>2.0.CO;2.","productDescription":"3 p.","startPage":"299","endPage":"301","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":324,"text":"Great Lakes Science Center","active":true,"usgs":true}],"links":[{"id":128701,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"7","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a2ee4b07f02db6153d3","contributors":{"authors":[{"text":"Sayers, Richard E.","contributorId":56592,"corporation":false,"usgs":true,"family":"Sayers","given":"Richard E.","affiliations":[],"preferred":false,"id":308778,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70180798,"text":"70180798 - 1987 - Effects of dietary selenium on smolting in Chinook salmon","interactions":[],"lastModifiedDate":"2017-02-03T12:46:40","indexId":"70180798","displayToPublicDate":"1987-01-01T00:00:00","publicationYear":"1987","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"Effects of dietary selenium on smolting in Chinook salmon","docAbstract":"No abstract available
","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Proceedings of the fourth Selenium symposium, Selenium and agricultural drainage: Implications for San Francisco Bay and the California environment","largerWorkSubtype":{"id":12,"text":"Conference publication"},"language":"English","usgsCitation":"Palmisano, A., 1987, Effects of dietary selenium on smolting in Chinook salmon, in Proceedings of the fourth Selenium symposium, Selenium and agricultural drainage: Implications for San Francisco Bay and the California environment.","costCenters":[{"id":654,"text":"Western Fisheries Research Center","active":true,"usgs":true}],"links":[{"id":334677,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5895a4d5e4b0fa1e59bc1eb5","contributors":{"authors":[{"text":"Palmisano, A.N.","contributorId":152185,"corporation":false,"usgs":false,"family":"Palmisano","given":"A.N.","email":"","affiliations":[],"preferred":false,"id":662462,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":1000559,"text":"1000559 - 1987 - Horizontal ichthyoplankton tow-net system with unobstructed net opening","interactions":[],"lastModifiedDate":"2016-03-25T09:14:34","indexId":"1000559","displayToPublicDate":"1987-01-01T00:00:00","publicationYear":"1987","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2886,"text":"North American Journal of Fisheries Management","active":true,"publicationSubtype":{"id":10}},"title":"Horizontal ichthyoplankton tow-net system with unobstructed net opening","docAbstract":"No abstract available
","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Proceedings of the reservoir mortality workshop","largerWorkSubtype":{"id":12,"text":"Conference publication"},"language":"English","publisher":"Columbia Basin Fish and Wildlife Authority","publisherLocation":"Portland, OR","usgsCitation":"Poe, T., 1987, Predation as a component of reservoir mortality: information needs, in Proceedings of the reservoir mortality workshop, 38 p. .","productDescription":"38 p. ","costCenters":[{"id":654,"text":"Western Fisheries Research Center","active":true,"usgs":true}],"links":[{"id":334678,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5895a4d5e4b0fa1e59bc1eb3","contributors":{"authors":[{"text":"Poe, T.P.","contributorId":51687,"corporation":false,"usgs":true,"family":"Poe","given":"T.P.","email":"","affiliations":[],"preferred":false,"id":662463,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":1000558,"text":"1000558 - 1987 - Acid rain stimulation of Lake Michigan phytoplankton growth","interactions":[],"lastModifiedDate":"2016-03-25T09:16:44","indexId":"1000558","displayToPublicDate":"1987-01-01T00:00:00","publicationYear":"1987","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2330,"text":"Journal of Great Lakes Research","active":true,"publicationSubtype":{"id":10}},"title":"Acid rain stimulation of Lake Michigan phytoplankton growth","docAbstract":"Three laboratory experiments demonstrated that additions of rainwater to epilimnetic lake water collected in southeastern Lake Michigan stimulated chlorophyll a production more than did additions of reagent-grade water during incubations of 12 to 20 d. Chlorophyll a production did not begin until 3–5 d after the rain and lake water were mixed. The stimulation caused by additions of rain acidified to pH 3.0 was greater than that caused by additions of untreated rain (pH 4.0–4.5). Our results support the following hypotheses: (1) Acid rain stimulates the growth of phytoplankton in lake water; (2) phosphorus in rain appears to be the factor causing this stimulation. We conclude that acid rain may accelerate the growth of epilimnetic phytoplankton in Lake Michigan (and other similar lakes) during stratification when other sources of bioavailable phosphorus to the epilimnion are limited
","language":"English","publisher":"Elsevier","doi":"10.1016/S0380-1330(87)71644-X","usgsCitation":"Manny, B.A., Fahnenstiel, G., and Gardner, W., 1987, Acid rain stimulation of Lake Michigan phytoplankton growth: Journal of Great Lakes Research, v. 13, no. 2, p. 218-223, https://doi.org/10.1016/S0380-1330(87)71644-X.","productDescription":"6 p.","startPage":"218","endPage":"223","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":324,"text":"Great Lakes Science Center","active":true,"usgs":true}],"links":[{"id":133322,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"13","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b12e4b07f02db6a2760","contributors":{"authors":[{"text":"Manny, Bruce A. 0000-0002-4074-9329 bmanny@usgs.gov","orcid":"https://orcid.org/0000-0002-4074-9329","contributorId":3699,"corporation":false,"usgs":true,"family":"Manny","given":"Bruce","email":"bmanny@usgs.gov","middleInitial":"A.","affiliations":[{"id":324,"text":"Great Lakes Science Center","active":true,"usgs":true}],"preferred":true,"id":308770,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Fahnenstiel, G.L.","contributorId":85554,"corporation":false,"usgs":true,"family":"Fahnenstiel","given":"G.L.","affiliations":[],"preferred":false,"id":308772,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Gardner, W.S.","contributorId":46910,"corporation":false,"usgs":true,"family":"Gardner","given":"W.S.","email":"","affiliations":[],"preferred":false,"id":308771,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":1000556,"text":"1000556 - 1987 - Partitioning potential fish yields from the Great Lakes","interactions":[],"lastModifiedDate":"2016-03-25T10:33:29","indexId":"1000556","displayToPublicDate":"1987-01-01T00:00:00","publicationYear":"1987","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1169,"text":"Canadian Journal of Fisheries and Aquatic Sciences","active":true,"publicationSubtype":{"id":10}},"title":"Partitioning potential fish yields from the Great Lakes","docAbstract":"We proposed and implemented procedures for partitioning future fish yields from the Great Lakes into taxonomic components. These projections are intended as guidelines for Great Lakes resource managers and scientists. Attainment of projected yields depends on restoration of stable fish communities containing some large piscivores that will use prey efficiently, continuation of control of the sea lamprey (Petromyzon marinus), and restoration of high-quality fish habitat. Because Great Lakes fish communities were harmonic before their collapse, we used their historic yield properties as part of the basis for projecting potential yields of rehabilitated communities. This use is qualified, however, because of possible inaccuracies in the wholly commercial yield data, the presence now of greatly expanded sport fisheries that affect yield composition and magnitude, and some possibly irreversible changes since the 1950s in the various fish communities themselves. We predict that total yields from Lakes Superior, Huron, and Ontario will be increased through rehabilitation, while those from Lakes Michigan and Erie will decline. Salmonines and coregonines will dominate future yields from the upper lakes. The Lake Erie fishery will continue to yield mostly rainbow smelt (Osmerus mordax), but the relative importance of percids, especially of walleye (Stizostedion vitreum vitreum) will increase. In Lake Ontario, yields of salmonines will be increased. Managers will have to apply the most rigorous management strictures to major predator species.
","language":"English","publisher":"NRC Research Press","doi":"10.1139/f87-343","usgsCitation":"Loftus, D., Olver, C., Brown, E., Colby, P., Hartman, W.L., and Schupp, D., 1987, Partitioning potential fish yields from the Great Lakes: Canadian Journal of Fisheries and Aquatic Sciences, v. 44, no. Suppl. 2, p. 417-424, https://doi.org/10.1139/f87-343.","productDescription":"8 p.","startPage":"417","endPage":"424","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":324,"text":"Great Lakes Science Center","active":true,"usgs":true}],"links":[{"id":133321,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"44","issue":"Suppl. 2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae2e4b07f02db688ea2","contributors":{"authors":[{"text":"Loftus, D.H.","contributorId":25117,"corporation":false,"usgs":true,"family":"Loftus","given":"D.H.","email":"","affiliations":[],"preferred":false,"id":308764,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Olver, C.H.","contributorId":13936,"corporation":false,"usgs":true,"family":"Olver","given":"C.H.","affiliations":[],"preferred":false,"id":308762,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Brown, Edward H.","contributorId":49732,"corporation":false,"usgs":true,"family":"Brown","given":"Edward H.","affiliations":[],"preferred":false,"id":308765,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Colby, P.J.","contributorId":101233,"corporation":false,"usgs":true,"family":"Colby","given":"P.J.","email":"","affiliations":[],"preferred":false,"id":308767,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Hartman, Wilbur L.","contributorId":14763,"corporation":false,"usgs":true,"family":"Hartman","given":"Wilbur","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":308763,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Schupp, D.H.","contributorId":99943,"corporation":false,"usgs":true,"family":"Schupp","given":"D.H.","email":"","affiliations":[],"preferred":false,"id":308766,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}} ,{"id":70014883,"text":"70014883 - 1987 - Structural analysis of geochemical samples by solid-state nuclear magnetic resonance spectrometry. Role of paramagnetic material","interactions":[],"lastModifiedDate":"2023-03-09T17:49:54.994759","indexId":"70014883","displayToPublicDate":"1987-01-01T00:00:00","publicationYear":"1987","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":761,"text":"Analytical Chemistry","active":true,"publicationSubtype":{"id":10}},"title":"Structural analysis of geochemical samples by solid-state nuclear magnetic resonance spectrometry. Role of paramagnetic material","docAbstract":"An examination of coals, coal tars, a fulvic acid, and soil fractions by solid-state 13C NMR spectrometry has demonstrated widely differing behavior regarding quantitative representation in the spectrum. Spin counting experiments on coal tars and the fulvic acid show that almost all the sample carbon is observed in both solution and solid-state NMR spectra. Similar experiments on two coals (a lignite and a bituminous coal) show that most (70-97%) of the carbon is observed; however, when the lignite is ion exchanged with 3% (w/w) Fe3+, the fraction of carbon observed drops to below 10%. In additional experiments signal intensity from soil samples is enhanced by a simple dithionite treatment. This is illustrated by 13C, 27Al, and 29Si solid-state NMR experiments on soil fractions.
","language":"English","publisher":"ACS Publications","doi":"10.1021/ac00131a005","usgsCitation":"Vassallo, A.M., Wilson, M.A., Collin, P.J., Oades, J.M., Waters, A.G., and Malcolm, R.L., 1987, Structural analysis of geochemical samples by solid-state nuclear magnetic resonance spectrometry. Role of paramagnetic material: Analytical Chemistry, v. 59, no. 4, p. 558-562, https://doi.org/10.1021/ac00131a005.","productDescription":"5 p.","startPage":"558","endPage":"562","numberOfPages":"5","costCenters":[],"links":[{"id":226114,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"59","issue":"4","noUsgsAuthors":false,"publicationDate":"2002-05-01","publicationStatus":"PW","scienceBaseUri":"505b9bbee4b08c986b31d070","contributors":{"authors":[{"text":"Vassallo, A. M.","contributorId":62345,"corporation":false,"usgs":false,"family":"Vassallo","given":"A.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":369518,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Wilson, M. A.","contributorId":107649,"corporation":false,"usgs":false,"family":"Wilson","given":"M.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":369520,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Collin, P. J.","contributorId":45062,"corporation":false,"usgs":false,"family":"Collin","given":"P.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":369515,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Oades, J. M.","contributorId":71325,"corporation":false,"usgs":false,"family":"Oades","given":"J.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":369519,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Waters, A. G.","contributorId":54351,"corporation":false,"usgs":false,"family":"Waters","given":"A.","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":369517,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Malcolm, Ronald L.","contributorId":97500,"corporation":false,"usgs":true,"family":"Malcolm","given":"Ronald","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":369516,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}} ,{"id":70014874,"text":"70014874 - 1987 - Examples of transient sounding from groundwater exploration in sedimentary aquifers","interactions":[],"lastModifiedDate":"2024-03-20T22:38:47.424001","indexId":"70014874","displayToPublicDate":"1987-01-01T00:00:00","publicationYear":"1987","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3825,"text":"Groundwater","active":true,"publicationSubtype":{"id":10}},"title":"Examples of transient sounding from groundwater exploration in sedimentary aquifers","docAbstract":"Examples of the use of transient electromagnetic soundings for three ground-water exploration problems in sedimentary aquifers are given. The examples include: (1) estimating depths to water table and bedrock in an alluvium-filled basin, (2) mapping a confined fresh-water aquifer in bedrock sediments, and (3) locating a freshwater/salt-water interface in a glacial-outwash aquifer. The technique works quite well for these problems within the limitations imposed by the problem of equivalence. For thin conductive targets (S-equivalence) such as a salt-water lens, the ratio of the layer thickness to its resistivity can be determined, but not the individual layer parameters. The thickness of thin resistive zones (H-equivalence) can be resolved, but the resistivity of such layers is not well determined. The problem of H-equivalence is more severe than the S-equivalence. Equivalence imposes restrictions on the transient sounding method for some ground-water exploration problems. Model studies prior to field work can be used to assess the usefulness of the technique for a particular exploration objective.
Aquatic humic- and fulvic-acid standards of the International Humic Substances Society were characterized, with emphasis on carbonyl-group nature and content, by carbon-13 nuclear-magnetic-resonance spectroscopy, proton nuclear-magnetic-resonance spectroscopy, and infrared spectroscopy. After comparing spectral results of underivatized humic and fulvic acids with spectral results of chemically modified derivatives, that allow improved observation of the carbonyl group, the data clearly indicated that aromatic ketone groups comprised the majority of the carbonyl-group content. About one ketone group per monocyclic aromatic ring was determined for both humic and fulvic acids. Aromatic-ketone groups were hypothesized to form by photolytic rearrangements and oxidation of phenolic ester and hydrocarbon precursors; these groups have potential significance regarding haloform formation in water, reactivity resulting from active hydrogen of the methyl and methylene adjacent to the ketone groups, and formation of hemiketal and lactol structures. Aromatic-ketone groups also may be the point of attachment between aliphatic and aromatic moieties of aquatic humic-substance structure.
","language":"English","publisher":"Elsevier","doi":"10.1016/0146-6380(87)90038-6","usgsCitation":"Leenheer, J., Wilson, M.A., and Malcolm, R., 1987, Presence and potential significance of aromatic-ketone groups in aquatic humic substances: Organic Geochemistry, v. 11, no. 4, p. 273-280, https://doi.org/10.1016/0146-6380(87)90038-6.","productDescription":"8 p.","startPage":"273","endPage":"280","costCenters":[],"links":[{"id":226253,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Georgia","city":"Fargo","otherGeospatial":"Suwannee River","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -82.55719563644614,\n 30.73718669262388\n ],\n [\n -82.70468259143186,\n 30.595406491784985\n ],\n [\n -82.62660258515855,\n 30.599762786732207\n ],\n [\n -82.52104350470628,\n 30.666323175534032\n ],\n [\n -82.33092442455035,\n 30.827183395185997\n ],\n [\n -82.35189154748764,\n 30.855175569793232\n ],\n [\n -82.55719563644614,\n 30.73718669262388\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","volume":"11","issue":"4","noUsgsAuthors":false,"plainLanguageSummary":"