{"pageNumber":"3928","pageRowStart":"98175","pageSize":"25","recordCount":185143,"records":[{"id":70018734,"text":"70018734 - 1995 - Roof-rock contamination of magma along the top of the reservoir for the Bishop Tuff","interactions":[],"lastModifiedDate":"2019-04-04T09:51:41","indexId":"70018734","displayToPublicDate":"1995-01-01T00:00:00","publicationYear":"1995","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":"Roof-rock contamination of magma along the top of the reservoir for the Bishop Tuff","docAbstract":"The Bishop Tuff, a Quaternary high-silica rhyolite in east-central California, is widely considered the type example of a vertically and monotonically zoned pyroclastic deposit that represents zoning in the source magma reservoir, inverted during the process of pyroclastic emplacement. However, the deposit of plinian pumice, which forms the base of the Bishop Tuff and represents the initial 10% or so of all magma erupted during the event that produced the Bishop Tuff, contains features at odds with monotonic zoning for the reservoir. Relative to overlying ignimbrite, the plinian deposit contains a reversal in trace-element zoning. The data have been previously interpreted as due to processes of chemical fractionation and evolution operating within a magma system closed to chemical interactions with its roof rocks. However, it is suggested here that the reversed zoning and other above-noted features can be explained equally well as consequences of minor assimilation of roof rocks into a magma reservoir that was erupted from the top down. -from Authors","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Journal of Volcanology and Geothermal Research","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"Elsevier","doi":"10.1016/0377-0273(95)00026-7","usgsCitation":"Duffield, W.A., Ruiz, J., and Webster, J., 1995, Roof-rock contamination of magma along the top of the reservoir for the Bishop Tuff: Journal of Volcanology and Geothermal Research, v. 69, no. 3-4, p. 187-195, https://doi.org/10.1016/0377-0273(95)00026-7.","startPage":"187","endPage":"195","numberOfPages":"9","costCenters":[{"id":615,"text":"Volcano Hazards Program","active":true,"usgs":true}],"links":[{"id":227444,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":269360,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1016/0377-0273(95)00026-7"}],"volume":"69","issue":"3-4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505aae81e4b0c8380cd870f7","contributors":{"authors":[{"text":"Duffield, W. A.","contributorId":71935,"corporation":false,"usgs":true,"family":"Duffield","given":"W.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":380586,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Ruiz, J.","contributorId":88886,"corporation":false,"usgs":true,"family":"Ruiz","given":"J.","email":"","affiliations":[],"preferred":false,"id":380587,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Webster, J.D.","contributorId":16582,"corporation":false,"usgs":true,"family":"Webster","given":"J.D.","email":"","affiliations":[],"preferred":false,"id":380585,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70019242,"text":"70019242 - 1995 - Precipitation depth-duration characteristics, Antelope Valley, California","interactions":[],"lastModifiedDate":"2012-03-12T17:19:16","indexId":"70019242","displayToPublicDate":"1995-01-01T00:00:00","publicationYear":"1995","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"Precipitation depth-duration characteristics, Antelope Valley, California","docAbstract":"To document the changes in runoff characteristics of basins subject to urbanization, streamflow and precipitation data were collected at eight small basins in Antelope Valley, California, for the period 1990-93. The data collected at U.S. Geological Survey stations were supplemented by data collected at 35 long-term precipitation stations. These data will be used to calibrate and verify rainfall-runoff models for the eight basins and for estimating basin runoff characteristics throughout Antelope Valley. Annual precipitation in Antelope Valley varies from more than 50 cm in the mountains to less than 10 cm on the valley floor. Most precipitation in the valley occurs during the winter months, December through March, but cyclonic storms in the fall and convectional storms in the summer sometimes occur.","largerWorkTitle":"International Water Resources Engineering Conference - Proceedings","conferenceTitle":"Proceedings of the 1st International Conference on Water Resources. Part 1 (of 2)","conferenceDate":"14 August 1995 through 18 August 1995","conferenceLocation":"San Antonio, TX, USA","language":"English","publisher":"ASCE","publisherLocation":"New York, NY, United States","usgsCitation":"Blodgett, J.C., and Nasseri, I., 1995, Precipitation depth-duration characteristics, Antelope Valley, California, <i>in</i> International Water Resources Engineering Conference - Proceedings, v. 1, San Antonio, TX, USA, 14 August 1995 through 18 August 1995, p. 274-278.","startPage":"274","endPage":"278","numberOfPages":"5","costCenters":[],"links":[{"id":226503,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a8116e4b0c8380cd7b367","contributors":{"editors":[{"text":"Espey William H.Combs Phil G.","contributorId":128391,"corporation":true,"usgs":false,"organization":"Espey William H.Combs Phil G.","id":536447,"contributorType":{"id":2,"text":"Editors"},"rank":1}],"authors":[{"text":"Blodgett, James C.","contributorId":82348,"corporation":false,"usgs":true,"family":"Blodgett","given":"James","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":382118,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Nasseri, Iraj","contributorId":85333,"corporation":false,"usgs":true,"family":"Nasseri","given":"Iraj","email":"","affiliations":[],"preferred":false,"id":382119,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70019691,"text":"70019691 - 1995 - Geoscience research databases for coastal Alabama ecosystem management","interactions":[],"lastModifiedDate":"2012-03-12T17:19:21","indexId":"70019691","displayToPublicDate":"1995-01-01T00:00:00","publicationYear":"1995","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"Geoscience research databases for coastal Alabama ecosystem management","docAbstract":"Effective management of complex coastal ecosystems necessitates access to scientific knowledge that can be acquired through a multidisciplinary approach involving Federal and State scientists that take advantage of agency expertise and resources for the benefit of all participants working toward a set of common research and management goals. Cooperative geostatic investigations have led toward building databases of fundamental scientific knowledge that can be utilized to manage coastal Alabama's natural and future development. These databases have been used to assess the occurrence and economic potential of hard mineral resources in the Alabama EFZ, and to support oil spill contingency planning and environmental analysis for coastal Alabama.","largerWorkTitle":"Coastal Zone: Proceedings of the Symposium on Coastal and Ocean Management","conferenceTitle":"Proceedings of the 9th 1995 Conference on Coastal Zone","conferenceDate":"16 July 1995 through 21 July 1995","conferenceLocation":"Tampa, FL, USA","language":"English","publisher":"ASCE","publisherLocation":"New York, NY, United States","usgsCitation":"Hummell, R.L., 1995, Geoscience research databases for coastal Alabama ecosystem management, <i>in</i> Coastal Zone: Proceedings of the Symposium on Coastal and Ocean Management, Tampa, FL, USA, 16 July 1995 through 21 July 1995, p. 578-579.","startPage":"578","endPage":"579","numberOfPages":"2","costCenters":[],"links":[{"id":227881,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a28a3e4b0c8380cd5a298","contributors":{"authors":[{"text":"Hummell, Richard L.","contributorId":68040,"corporation":false,"usgs":true,"family":"Hummell","given":"Richard","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":383603,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70018733,"text":"70018733 - 1995 - Preferential flow and segregation of porewater solutes in Wetland sediment","interactions":[],"lastModifiedDate":"2020-09-02T19:07:20.649052","indexId":"70018733","displayToPublicDate":"1995-01-01T00:00:00","publicationYear":"1995","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1583,"text":"Estuaries","active":true,"publicationSubtype":{"id":10}},"title":"Preferential flow and segregation of porewater solutes in Wetland sediment","docAbstract":"Sediment macropores (with effective diameters larger than 100 ??m) comprise 11% of the bulk sediment volume in a tidal freshwater wetland vegetated with Peltandra virginica. In order to determine effects of macroporous sediment structure on solute transport, we conducted a solute tracer experiment in the sediment. The effective transport volume (??eff, the volume of sediment through which solute was transported normalized to sediment bulk volume) was 0.15 cm3 cm-3, which is considerably smaller than the total pore space that is potentially available for transport (porosity of sediment is 0.63 cm3 cm-3). A mean transport time of 13 d was required to flush preferential flow paths in Peltandra hummocks; hydrologic turnover of the volumetrically dominant matrix pores (0.53 cm3 cm-3) was apparently much slower. Based on porewater sampler design and hydrological principles, we suggest that N2-purged tension solution samplers and diffusion equilibrators preferentially sample porewater from macropore and matrix domains, respectively. Dissolved ammonium and orthophosphate concentrations were three-fold higher in matrix pores compared to macropores, which is consistent with our finding that more rapid hydrological flushing occurred in macropores compared to matrix pores. Further evaluation of porewater sampler designs in macroporous sediment is needed to improve studies of hydrologic transport and biogeochemical cycling in wetlands. ?? 1995 Estuarine Research Federation.","language":"English","publisher":"Springer-Verlag","doi":"10.2307/1352377","issn":"15592723","usgsCitation":"Harvey, J., Chambers, R., and Hoelscher, J., 1995, Preferential flow and segregation of porewater solutes in Wetland sediment: Estuaries, v. 18, no. 4, p. 568-578, https://doi.org/10.2307/1352377.","startPage":"568","endPage":"578","numberOfPages":"11","costCenters":[],"links":[{"id":227443,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"18","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a821ce4b0c8380cd7b8f0","contributors":{"authors":[{"text":"Harvey, J. W. 0000-0002-2654-9873","orcid":"https://orcid.org/0000-0002-2654-9873","contributorId":39725,"corporation":false,"usgs":true,"family":"Harvey","given":"J. W.","affiliations":[],"preferred":false,"id":380583,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Chambers, R.M.","contributorId":31130,"corporation":false,"usgs":true,"family":"Chambers","given":"R.M.","email":"","affiliations":[],"preferred":false,"id":380582,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Hoelscher, J.R.","contributorId":57220,"corporation":false,"usgs":true,"family":"Hoelscher","given":"J.R.","email":"","affiliations":[],"preferred":false,"id":380584,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70019254,"text":"70019254 - 1995 - How wet is wet? Precipitation constraints on late Quaternary climate in the southern Arabian Peninsula","interactions":[],"lastModifiedDate":"2019-02-25T11:41:41","indexId":"70019254","displayToPublicDate":"1995-01-01T00:00:00","publicationYear":"1995","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2342,"text":"Journal of Hydrology","active":true,"publicationSubtype":{"id":10}},"title":"How wet is wet? Precipitation constraints on late Quaternary climate in the southern Arabian Peninsula","docAbstract":"<p><span>It is generally recognized that the southern Arabian Peninsula has had two wet periods in the late Quaternary. To quantify ‘wet’ a 28 000 year old capillary surface associated with a paleowater-table was mapped and used as a surrogate for the water table in a ground-water model. Analysis of this model suggests 1.4 mm year</span><sup>−1</sup><span>&nbsp;of recharge is necessary to support the water table at the mapped elevations during the wet period. Climatic relations between rainfall and recharge in arid areas infer that annual rainfall during this wet period was approximately 200 ± 50 mm year</span><sup>−1</sup><span>&nbsp;or approximately five times the present rate.</span></p>","language":"English","publisher":"Elsevier","doi":"10.1016/0022-1694(94)02551-L","issn":"00221694","usgsCitation":"Wood, W., and Imes, J.L., 1995, How wet is wet? Precipitation constraints on late Quaternary climate in the southern Arabian Peninsula: Journal of Hydrology, v. 164, no. 1-4, p. 263-268, https://doi.org/10.1016/0022-1694(94)02551-L.","productDescription":"6 p.","startPage":"263","endPage":"268","costCenters":[{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":226639,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"164","issue":"1-4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a326de4b0c8380cd5e7cc","contributors":{"authors":[{"text":"Wood, W.W.","contributorId":21974,"corporation":false,"usgs":true,"family":"Wood","given":"W.W.","email":"","affiliations":[],"preferred":false,"id":382144,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Imes, Jeffrey L. jimes@usgs.gov","contributorId":2983,"corporation":false,"usgs":true,"family":"Imes","given":"Jeffrey","email":"jimes@usgs.gov","middleInitial":"L.","affiliations":[],"preferred":true,"id":382145,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":44891,"text":"wri954146 - 1995 - Louisiana ground-water map no. 6: Potentiometric surface, 1990, and water-level changes, 1974-90, of the Mississippi River alluvial aquifer in northeastern Louisiana","interactions":[],"lastModifiedDate":"2023-04-17T19:01:49.115823","indexId":"wri954146","displayToPublicDate":"1995-01-01T00:00:00","publicationYear":"1995","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":"95-4146","title":"Louisiana ground-water map no. 6: Potentiometric surface, 1990, and water-level changes, 1974-90, of the Mississippi River alluvial aquifer in northeastern Louisiana","docAbstract":"The Mississippi River alluvial aquifer is the largest source of fresh ground water in northeastern Louisiana. In 1990, an average of 170 million gallons per day was withdrawn from the aquifer in 12 northeast Louisiana parishes. Additional knowledge about ground-water flow and the effects of withdrawals on the Mississippi River alluvial aquifer is needed for future ground-water development and protection of the resource. Generalized contours of the altitude of water levels in September 1990 and changes of water levels from 1974 to 1990 in the Mississippi River alluvial aquifer in northeastern Louisiana are shown on maps. Water-level trands in the aquifer are shown in hydrographs of selected wells.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri954146","usgsCitation":"Seanor, R.C., and Smoot, C.W., 1995, Louisiana ground-water map no. 6: Potentiometric surface, 1990, and water-level changes, 1974-90, of the Mississippi River alluvial aquifer in northeastern Louisiana: U.S. Geological Survey Water-Resources Investigations Report 95-4146, 2 Plates: 28.00 x 27.79 inches and 28.00 x 27.81 inches, https://doi.org/10.3133/wri954146.","productDescription":"2 Plates: 28.00 x 27.79 inches and 28.00 x 27.81 inches","costCenters":[],"links":[{"id":415858,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_49267.htm","linkFileType":{"id":5,"text":"html"}},{"id":82246,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1995/4146/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":82245,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1995/4146/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":169963,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"country":"United States","state":"Louisiana","otherGeospatial":"Mississippi River alluvial aquifer","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -92.2111,\n              33.0167\n            ],\n            [\n              -92.2111,\n              31.1306\n            ],\n            [\n              -91,\n              31.1306\n            ],\n            [\n              -91,\n              33.0167\n            ],\n            [\n              -92.2111,\n              33.0167\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a74e4b07f02db644605","contributors":{"authors":[{"text":"Seanor, Ronald C. 0000-0001-5735-5580 rcseanor@usgs.gov","orcid":"https://orcid.org/0000-0001-5735-5580","contributorId":3731,"corporation":false,"usgs":true,"family":"Seanor","given":"Ronald","email":"rcseanor@usgs.gov","middleInitial":"C.","affiliations":[],"preferred":true,"id":230625,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Smoot, Charles W.","contributorId":88398,"corporation":false,"usgs":true,"family":"Smoot","given":"Charles","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":230626,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70018741,"text":"70018741 - 1995 - Use of the euryhaline bivalve Potamocorbula amurensis as a biosentinel species to assess trace metal contamination in San Francisco Bay","interactions":[],"lastModifiedDate":"2020-01-07T14:14:56","indexId":"70018741","displayToPublicDate":"1995-01-01T00:00:00","publicationYear":"1995","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2663,"text":"Marine Ecology Progress Series","active":true,"publicationSubtype":{"id":10}},"title":"Use of the euryhaline bivalve Potamocorbula amurensis as a biosentinel species to assess trace metal contamination in San Francisco Bay","docAbstract":"<p class=\"abstract_block\"><i>Potamocorbula amurensis</i><span>&nbsp;</span>was assessed as a biosentinel species in San Francisco Bay, California, USA. Uptake of metal in both the laboratory and field showed that<span>&nbsp;</span><i>P. amurensis</i><span>&nbsp;</span>was sufficiently responsive to Ag, Cd, Cr, Ni and V to detect environmental differences in exposure. It was less suitable as an indicator of Cu and Zn contamination. Concentration factors for<span>&nbsp;</span><i>P. amurensis</i><span>&nbsp;</span>were: Ag, 386000; Cd, 50200; Cr, 36600; Cu, 12200; Ni, 5200; and Zn, 115500. Samples were collected from 6 stations throughout the bay at near-monthly intervals from January 1991 to March 1992. Variability within a collection was influenced by gut content and animal size. Other sources of variability were time [coefficient of variation (CV) = 10 to 21%], small-scale spatial variability (within 3 km, CV = 10 to 25%), and large-scale spatial variability (CV = 3.3 to 12.4%). Depuration for 48 h was necessary to mitigate bias from gut content. Precision was improved by analyzing large numbers of individuals (60 to 120) separated into several (5 to 14) composites at each collection and by determining, from regression, the mean and variance for samples with significant correlations between metal concentration and shell length. Repeated monthly sampling increased the accuracy of long-term site characterizations. Temporal variability was small because of drought. The grand means of the concentrations of Ag, Cd, Cr, Ni, and V in the tissues of<span>&nbsp;</span><i>P. amurensis</i><span>&nbsp;</span>at each station for the 15 mo period revealed persistent contamination from industrialized Suisun Bay to the mouth of San Francisco Bay. Demonstration of responsiveness, precision and accuracy should be a prerequisite for the optimal use of biosentinels.</p>","language":"English","publisher":"Inter-Research","doi":"10.3354/meps124129","issn":"01718630","usgsCitation":"Brown, C.L., and Luoma, S., 1995, Use of the euryhaline bivalve Potamocorbula amurensis as a biosentinel species to assess trace metal contamination in San Francisco Bay: Marine Ecology Progress Series, v. 124, no. 1-3, p. 129-142, https://doi.org/10.3354/meps124129.","productDescription":"14 p.","startPage":"129","endPage":"142","numberOfPages":"14","costCenters":[{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":480195,"rank":1,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.3354/meps124129","text":"Publisher Index Page"},{"id":227535,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"California","otherGeospatial":"San Francisco Bay","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -123.134765625,\n              37.3002752813443\n            ],\n            [\n              -121.83837890625,\n              37.3002752813443\n            ],\n            [\n              -121.83837890625,\n              38.298559092254344\n            ],\n            [\n              -123.134765625,\n              38.298559092254344\n            ],\n            [\n              -123.134765625,\n              37.3002752813443\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"124","issue":"1-3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505bbf9de4b08c986b329c74","contributors":{"authors":[{"text":"Brown, C. L.","contributorId":35678,"corporation":false,"usgs":true,"family":"Brown","given":"C.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":380607,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Luoma, S. N.","contributorId":86353,"corporation":false,"usgs":true,"family":"Luoma","given":"S. N.","affiliations":[],"preferred":false,"id":380608,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70019664,"text":"70019664 - 1995 - Reservoir model for Hillsboro gas storage field management","interactions":[],"lastModifiedDate":"2012-03-12T17:19:19","indexId":"70019664","displayToPublicDate":"1995-01-01T00:00:00","publicationYear":"1995","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"Reservoir model for Hillsboro gas storage field management","docAbstract":"A 3-dimensional reservoir model is used to understand the behavior of the Hillsboro Gas Storage Field and to investigate the field's performance under various future development. Twenty-two years of the gas storage reservoir history, comprising the initial gas bubble development and seasonal gas injection and production cycles, are examined with a full-field, gas water, reservoir simulation model. The results suggest that the gas-water front is already in the vicinity of the west observation well that increasing the field's total gas-in-place volume would cause gas to migrate beyond the east, north and west observation well. They also suggest that storage enlargement through gas injection into the lower layers may not prevent gas migration. Moreover, the results suggest that the addition of strategically-located new wells would boost the simulated gas deliverabilities.","largerWorkTitle":"Proceedings - SPE Eastern Regional Conference and Exhibition","conferenceTitle":"Proceedings of the 1995 Eastern Regional Conference","conferenceDate":"18 September 1995 through 20 September 1995","conferenceLocation":"Morgantown, WV, USA","language":"English","publisher":"Society of Petroleum Engineers (SPE)","publisherLocation":"Richardson, TX, United States","usgsCitation":"Udegbunam, E.O., Kemppainen, C., and Morgan, J., 1995, Reservoir model for Hillsboro gas storage field management, <i>in</i> Proceedings - SPE Eastern Regional Conference and Exhibition, Morgantown, WV, USA, 18 September 1995 through 20 September 1995, p. 163-180.","startPage":"163","endPage":"180","numberOfPages":"18","costCenters":[],"links":[{"id":228088,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505aa962e4b0c8380cd85d82","contributors":{"editors":[{"text":"Anon","contributorId":128316,"corporation":true,"usgs":false,"organization":"Anon","id":536458,"contributorType":{"id":2,"text":"Editors"},"rank":1}],"authors":[{"text":"Udegbunam, Emmanuel O.","contributorId":48331,"corporation":false,"usgs":true,"family":"Udegbunam","given":"Emmanuel","email":"","middleInitial":"O.","affiliations":[],"preferred":false,"id":383487,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Kemppainen, Curt","contributorId":46239,"corporation":false,"usgs":true,"family":"Kemppainen","given":"Curt","email":"","affiliations":[],"preferred":false,"id":383486,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Morgan, Jim","contributorId":107447,"corporation":false,"usgs":true,"family":"Morgan","given":"Jim","email":"","affiliations":[],"preferred":false,"id":383488,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":1014706,"text":"1014706 - 1995 - Influence of tank design and hydraulic loading on the behavior, growth, and metabolism of rainbow trout (Oncorhynchus mykiss)","interactions":[],"lastModifiedDate":"2023-08-09T15:29:40.078799","indexId":"1014706","displayToPublicDate":"1995-01-01T00:00:00","publicationYear":"1995","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":852,"text":"Aquacultural Engineering","active":true,"publicationSubtype":{"id":10}},"displayTitle":"Influence of tank design and hydraulic loading on the behavior, growth, and metabolism of rainbow trout (<i>Oncorhynchus mykiss</i>)","title":"Influence of tank design and hydraulic loading on the behavior, growth, and metabolism of rainbow trout (Oncorhynchus mykiss)","docAbstract":"<p>Subadult rainbow trout (<i>Oncorhynchus mykiss</i>) stocked at 48 kg/m<sup>3</sup><span>&nbsp;</span>(3 lb/ft<sup>3</sup>) were subjected to treatments of tank design (rectangular plug flow, circular, and cylindrical cross flow) and water exchange rate (1·5 and 2·5 exchanges/h) to determine their effects on fish behavior, growth, and metabolism. Ambient light levels and current velocities were also measured in each of three tank sectors (upstream, middle, and downstream) to determine their relative contributions to behavioral effects. Tank design significantly affected fish orientation to current, contact time with tank surfaces, and frequency of agonistic encounters, though aggression levels were relatively low overall. Gradients in fish distribution by sector were greatest in plug-flow tanks. Effects were either modified or eliminated by increasing the water exchange rate from 1·5 to 2·5/h. Multiple-regression analysis showed the following hieararchy of independent-variable effects on fish distribution: tank type &gt; exchange rate &gt; aggression level &gt; current velocity &gt; light level.</p><p>Significant effects of tank design were also observed on fish growth in terms of biomass gain (cross flow &gt; plug flow &gt; circular). These results were matched in metabolic studies, where both oxygen consumption and ammonia excretion were highest in circular and lowest in cross-flow tanks. Reduction (cross-flow compared with circular tanks) in oxygen consumption averaged 13·6%, ammonia excretion 17·5%. These results were also modified by an increase in water exchange rate. Tank-design effects on fish metabolism and growth may be mediated, at least partly, through changes in fish behavior.</p>","language":"English","publisher":"Elsevier","doi":"10.1016/0144-8609(94)P4425-B","usgsCitation":"Ross, R.M., Watten, B.J., Krise, W.F., DiLauro, M.N., and Soderberg, R.W., 1995, Influence of tank design and hydraulic loading on the behavior, growth, and metabolism of rainbow trout (Oncorhynchus mykiss): Aquacultural Engineering, v. 14, no. 1, p. 29-47, https://doi.org/10.1016/0144-8609(94)P4425-B.","productDescription":"19 p.","startPage":"29","endPage":"47","numberOfPages":"19","costCenters":[{"id":365,"text":"Leetown Science Center","active":true,"usgs":true}],"links":[{"id":129433,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"14","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f1e4b07f02db5ee63f","contributors":{"authors":[{"text":"Ross, Robert M.","contributorId":62562,"corporation":false,"usgs":true,"family":"Ross","given":"Robert","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":320967,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Watten, Barnaby J. 0000-0002-2227-8623 bwatten@usgs.gov","orcid":"https://orcid.org/0000-0002-2227-8623","contributorId":2002,"corporation":false,"usgs":true,"family":"Watten","given":"Barnaby","email":"bwatten@usgs.gov","middleInitial":"J.","affiliations":[{"id":365,"text":"Leetown Science Center","active":true,"usgs":true}],"preferred":true,"id":320966,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Krise, W. F.","contributorId":50842,"corporation":false,"usgs":true,"family":"Krise","given":"W.","middleInitial":"F.","affiliations":[],"preferred":false,"id":320968,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"DiLauro, M. N.","contributorId":75475,"corporation":false,"usgs":true,"family":"DiLauro","given":"M.","email":"","middleInitial":"N.","affiliations":[],"preferred":false,"id":320969,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Soderberg, R. W.","contributorId":93855,"corporation":false,"usgs":false,"family":"Soderberg","given":"R.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":320970,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":70019040,"text":"70019040 - 1995 - Adjusting stream-sediment geochemical maps in the Austrian Bohemian Massif by analysis of variance","interactions":[],"lastModifiedDate":"2012-03-12T17:19:35","indexId":"70019040","displayToPublicDate":"1995-01-01T00:00:00","publicationYear":"1995","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2700,"text":"Mathematical Geology","active":true,"publicationSubtype":{"id":10}},"title":"Adjusting stream-sediment geochemical maps in the Austrian Bohemian Massif by analysis of variance","docAbstract":"The Austrian portion of the Bohemian Massif is a Precambrian terrane composed mostly of highly metamorphosed rocks intruded by a series of granitoids that are petrographically similar. Rocks are exposed poorly and the subtle variations in rock type are difficult to map in the field. A detailed geochemical survey of stream sediments in this region has been conducted and included as part of the Geochemischer Atlas der Republik O??sterreich, and the variations in stream sediment composition may help refine the geological interpretation. In an earlier study, multivariate analysis of variance (MANOVA) was applied to the stream-sediment data in order to minimize unwanted sampling variation and emphasize relationships between stream sediments and rock types in sample catchment areas. The estimated coefficients were used successfully to correct for the sampling effects throughout most of the region, but also introduced an overcorrection in some areas that seems to result from consistent but subtle differences in composition of specific rock types. By expanding the model to include an additional factor reflecting the presence of a major tectonic unit, the Rohrbach block, the overcorrection is removed. This iterative process simultaneously refines both the geochemical map by removing extraneous variation and the geological map by suggesting a more detailed classification of rock types. ?? 1995 International Association for Mathematical Geology.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Mathematical Geology","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisherLocation":"Kluwer Academic Publishers-Plenum Publishers","doi":"10.1007/BF02083215","issn":"08828121","usgsCitation":"Davis, J., Hausberger, G., Schermann, O., and Bohling, G., 1995, Adjusting stream-sediment geochemical maps in the Austrian Bohemian Massif by analysis of variance: Mathematical Geology, v. 27, no. 2, p. 279-299, https://doi.org/10.1007/BF02083215.","startPage":"279","endPage":"299","numberOfPages":"21","costCenters":[],"links":[{"id":205697,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1007/BF02083215"},{"id":226272,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"27","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059e6f6e4b0c8380cd47757","contributors":{"authors":[{"text":"Davis, J.C.","contributorId":72121,"corporation":false,"usgs":true,"family":"Davis","given":"J.C.","email":"","affiliations":[],"preferred":false,"id":381494,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hausberger, G.","contributorId":86907,"corporation":false,"usgs":true,"family":"Hausberger","given":"G.","email":"","affiliations":[],"preferred":false,"id":381495,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Schermann, O.","contributorId":63178,"corporation":false,"usgs":true,"family":"Schermann","given":"O.","email":"","affiliations":[],"preferred":false,"id":381493,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Bohling, G.","contributorId":60789,"corporation":false,"usgs":true,"family":"Bohling","given":"G.","email":"","affiliations":[],"preferred":false,"id":381492,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70019047,"text":"70019047 - 1995 - The role of palynology in paleoecological analyses of Tertiary coals","interactions":[],"lastModifiedDate":"2024-02-21T13:13:47.34068","indexId":"70019047","displayToPublicDate":"1995-01-01T00:00:00","publicationYear":"1995","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2033,"text":"International Journal of Coal Geology","active":true,"publicationSubtype":{"id":10}},"title":"The role of palynology in paleoecological analyses of Tertiary coals","docAbstract":"<div id=\"preview-section-abstract\"><div id=\"abstracts\" class=\"Abstracts u-font-serif text-s\"><div id=\"aep-abstract-id3\" class=\"abstract author\"><div id=\"aep-abstract-sec-id4\"><p>Pollen, spores, and other plant microfossils are important constituents of Tertiary coals, both as petrographic components (the maceral sporinite) and as distinctive indicators of the nature of the depositional environment in which the coal-forming peat accumulated. Palynological analyses, which have been conducted on Tertiary coals since the 1930's, play an increasingly important role in modern paleoecological analyses of coals.</p><p>Among the most important factors controlling the petrographic composition and facies characteristics of coal deposits are the types and relative abundances of plants that composed the peat. At present, wetland environments in which peat accumulates (mires) range from marshes and bogs to forested swamps; each is inhabited by distinctive plant communities. These plant communities are associated with varied conditions of climate, water depth, chemistry, and nutrient supply, and the floras can be indicative of these conditions. In the Tertiary Period, plant communities of mires were also highly diverse and specialized (especially as compared with those of the Carboniferous). The dominant species in some Paleocene mire floras were gymnosperms, but continuing a trend begun in Late Cretaceous time, angiosperms became increasingly prominent through the Tertiary. The diverse: angiosperm-dominated mire floras produced coals that vary significantly in facies and hence in quality. Such contrasts are evident in contemporaneous coals from different paleolatitudes, as well as among, coals of different ages within the Tertiary, as exemplified by selected deposits in the western United. States. The palynofloras of these coals reflect the floristic composition of the plant communities of the ancient mires.</p></div></div></div></div><div id=\"preview-section-introduction\"><br></div><div id=\"preview-section-snippets\"><br></div><div id=\"preview-section-references\"><br></div>","language":"English","publisher":"Elsevier","doi":"10.1016/0166-5162(95)00017-8","issn":"01665162","usgsCitation":"Nichols, D.J., 1995, The role of palynology in paleoecological analyses of Tertiary coals: International Journal of Coal Geology, v. 28, no. 2-4, p. 139-159, https://doi.org/10.1016/0166-5162(95)00017-8.","productDescription":"21 p.","startPage":"139","endPage":"159","numberOfPages":"21","costCenters":[],"links":[{"id":226360,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"28","issue":"2-4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505baf8de4b08c986b3248a4","contributors":{"authors":[{"text":"Nichols, D. J.","contributorId":55466,"corporation":false,"usgs":true,"family":"Nichols","given":"D.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":381514,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70018757,"text":"70018757 - 1995 - Can magma-injection and groundwater forces cause massive landslides on Hawaiian volcanoes?","interactions":[],"lastModifiedDate":"2019-06-06T13:05:39","indexId":"70018757","displayToPublicDate":"1995-01-01T00:00:00","publicationYear":"1995","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":"Can magma-injection and groundwater forces cause massive landslides on Hawaiian volcanoes?","docAbstract":"<p><span>Landslides with volumes exceeding 1000 km</span><sup>3</sup><span>&nbsp;have occurred on the flanks of Hawaiian volcanoes. Because the flanks typically slope seaward no more than 12 °, the mechanics of slope failure are problematic. Limit-equilibrium analyses of wedge-shaped slices of the volcano flanks show that magma injection at prospective headscarps might trigger the landslides, but only under very restrictive conditions. If static magma weight is the sole source of magma pressure, hypothetical flank failures can have any size, but can occur only if slip-surface friction angles are less than about 16 °. If slip surfaces have friction angles more typical of fragmented or intact rocks (30–40 °), flank failures can occur only if mean magma pressures exceed static equilibrium pressures. Landslide length then scales with the excess magma pressure divided by the buoyant unit weight of the volcano flank. For typical excess magma pressures, buoyant unit weights and rock friction angles, the largest landslides that might be triggered in this manner have lengths of only several kilometers. This is at least an order of magnitude too small to explain the occurrence of giant Hawaiian landslides. The growing mass of active Hawaiian volcanoes can compress the edifice and substrate rocks and consequently produce groundwater head gradients that might destabilize larger sectors of the volcano flanks. However, calculations show that volcano growth at an estimated long-term vertical rate of 0.02 m/yr can generate significant head gradients only if an areally extensive, buried clay layer exists that has a great thickness (~ 200 m) or very low hydraulic diffusivity (~ 10</span><sup>−11</sup><span>&nbsp;m</span><sup>2</sup><span>/s). Additional calculations show that groundwater head gradients associated with topographically induced flow and sea-level change are less likely to be important. Thus a simple, quantitative explanation for failure of Hawaiian volcano flanks remains elusive, and more complex scenarios may merit investigation.</span></p>","language":"English","publisher":"Elsevier","doi":"10.1016/0377-0273(94)00064-N","usgsCitation":"Iverson, R., 1995, Can magma-injection and groundwater forces cause massive landslides on Hawaiian volcanoes?: Journal of Volcanology and Geothermal Research, v. 66, no. 1-4, p. 295-308, https://doi.org/10.1016/0377-0273(94)00064-N.","productDescription":"14 p.","startPage":"295","endPage":"308","costCenters":[{"id":615,"text":"Volcano Hazards Program","active":true,"usgs":true}],"links":[{"id":227087,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":269361,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1016/0377-0273(94)00064-N"}],"volume":"66","issue":"1-4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059f336e4b0c8380cd4b679","contributors":{"authors":[{"text":"Iverson, R.M. 0000-0002-7369-3819","orcid":"https://orcid.org/0000-0002-7369-3819","contributorId":16435,"corporation":false,"usgs":true,"family":"Iverson","given":"R.M.","affiliations":[],"preferred":false,"id":380668,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":1014718,"text":"1014718 - 1995 - Association of Cytophaga psychrophila with mortality among eyed eggs of Atlantic salmon (Salmo salar)","interactions":[],"lastModifiedDate":"2024-07-09T23:55:33.353205","indexId":"1014718","displayToPublicDate":"1995-01-01T00:00:00","publicationYear":"1995","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":"Association of Cytophaga psychrophila with mortality among eyed eggs of Atlantic salmon (Salmo salar)","docAbstract":"<div id=\"9840087\" class=\"article-section-wrapper js-article-section js-content-section  \" data-section-parent-id=\"0\"><p>Although<span>&nbsp;</span><i>Pseudomonas fluorescens</i><span>&nbsp;</span>was the predominant bacterium associated with Atlantic salmon (<i>Salmo salar</i>) eggs incubated at the White River National Fish Hatchery (Bethel, Vermont) during January 1992, the fish pathogen<span>&nbsp;</span><i>Cytophaga psychrophila</i><span>&nbsp;</span>was isolated only from specific lots of eggs that displayed poor survival (35% eye-up).</p></div>","language":"English","publisher":"Allen Press","doi":"10.7589/0090-3558-31.2.166","usgsCitation":"Cipriano, R.C., Ford, L., and Teska, J., 1995, Association of Cytophaga psychrophila with mortality among eyed eggs of Atlantic salmon (Salmo salar): Journal of Wildlife Diseases, v. 31, no. 2, p. 166-171, https://doi.org/10.7589/0090-3558-31.2.166.","productDescription":"6 p.","startPage":"166","endPage":"171","numberOfPages":"6","costCenters":[{"id":365,"text":"Leetown Science Center","active":true,"usgs":true}],"links":[{"id":129537,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"31","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aafe4b07f02db66ce35","contributors":{"authors":[{"text":"Cipriano, R. C.","contributorId":12400,"corporation":false,"usgs":true,"family":"Cipriano","given":"R.","middleInitial":"C.","affiliations":[],"preferred":false,"id":321010,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Ford, L.A.","contributorId":25510,"corporation":false,"usgs":true,"family":"Ford","given":"L.A.","email":"","affiliations":[],"preferred":false,"id":321012,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Teska, J.D.","contributorId":15961,"corporation":false,"usgs":true,"family":"Teska","given":"J.D.","email":"","affiliations":[],"preferred":false,"id":321011,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70019623,"text":"70019623 - 1995 - Depth to pre-Cenozoic basement in Southwest Nevada","interactions":[],"lastModifiedDate":"2012-03-12T17:19:19","indexId":"70019623","displayToPublicDate":"1995-01-01T00:00:00","publicationYear":"1995","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"Depth to pre-Cenozoic basement in Southwest Nevada","docAbstract":"An iterative procedure based on gravity data, surface geology, and an estimated density-depth function was used to estimate the depth to pre-Cenozoic basement at Yucca Mountain and vicinity.","largerWorkTitle":"High Level Radioactive Waste Management - Proceedings of the Annual International Conference","conferenceTitle":"Proceedings of the 6th Annual International Conference on High Level Radioactive Waste Management","conferenceDate":"30 April 1995 through 5 May 1995","conferenceLocation":"Las Vegas, NV, USA","language":"English","publisher":"ASCE","publisherLocation":"New York, NY, United States","usgsCitation":"Langenheim, V., and Ponce, D., 1995, Depth to pre-Cenozoic basement in Southwest Nevada, <i>in</i> High Level Radioactive Waste Management - Proceedings of the Annual International Conference, Las Vegas, NV, USA, 30 April 1995 through 5 May 1995, p. 129-131.","startPage":"129","endPage":"131","numberOfPages":"3","costCenters":[],"links":[{"id":228084,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059fed6e4b0c8380cd4ef57","contributors":{"editors":[{"text":"Hughes Howard R.","contributorId":128387,"corporation":true,"usgs":false,"organization":"Hughes Howard R.","id":536455,"contributorType":{"id":2,"text":"Editors"},"rank":1}],"authors":[{"text":"Langenheim, V.E. 0000-0003-2170-5213","orcid":"https://orcid.org/0000-0003-2170-5213","contributorId":54956,"corporation":false,"usgs":true,"family":"Langenheim","given":"V.E.","affiliations":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"preferred":false,"id":383355,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Ponce, D. A. 0000-0003-4785-7354","orcid":"https://orcid.org/0000-0003-4785-7354","contributorId":104019,"corporation":false,"usgs":true,"family":"Ponce","given":"D. A.","affiliations":[],"preferred":false,"id":383356,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70018745,"text":"70018745 - 1995 - Basement and cover-rock deformation during Laramide contraction in the northern Madison Range (Montana) and its influence on Cenozoic basin formation","interactions":[],"lastModifiedDate":"2023-01-20T17:10:20.209986","indexId":"70018745","displayToPublicDate":"1995-01-01T00:00:00","publicationYear":"1995","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":701,"text":"American Association of Petroleum Geologists Bulletin","active":true,"publicationSubtype":{"id":10}},"title":"Basement and cover-rock deformation during Laramide contraction in the northern Madison Range (Montana) and its influence on Cenozoic basin formation","docAbstract":"<p>Two major Laramide fault systems converge in the northwestern Madison Range: the northwest-striking, southwest-vergent Spanish Peaks reverse fault and the north-striking, east-vergent Hilgard thrust system. Analysis of foliation attitudes in basement gneiss north and south of the Spanish Peaks fault indicates that the basement in thrusted blocks of the Hilgard thrust system has been rotated by an amount similar to that of the basement-cover contact. Steeply dipping, north-striking breccia zones enclosing domains of relatively undeformed basement may have permitted domino-style rotation of basement blocks during simple shear between pairs of thrusts.</p><p>In most places along the Hilgard thrust system, a large basement overhang, produced by thrusting of Archean blocks above rocks as young as Late Cretaceous, overlies a tight footwall syncline. This tight folding is largely concentric and was accommodated by flexural slip, resulting in severe crowding in synclinal hinges that resulted in observed or inferred features such as bedding-plane slip, imbricate and out-of-syncline thrusting, and hinge collapse.</p><p>The north-striking Madison normal fault system, a zone of Tertiary and Quaternary valley-forming normal faults, is approximately parallel to the Hilgard thrust system. In some places, normal faults are reactivated thrusts on which large basement overhangs of the Hilgard thrust system were dropped back into the Madison Valley and covered by Tertiary basin-fill deposits, leaving only the rocks of the footwall synclines exposed. In other places, both the thrusted Archean blocks and the near-isoclinal footwall synclines are well preserved.</p><p>This paired fault system (the Madison normal fault system and the Hilgard thrust system) of the northern Madison Range is strikingly similar to other paired systems in southwestern Montana along and adjacent to the western margins of the Ruby Range, Snowcrest Range, Greenhorn Range, Tobacco Root Mountains, and Bridger Range. Such systems may be the result of collapse of the crestal zones of large Laramide basement uplifts (arches) during Tertiary extension.</p><p>No hydrocarbon discoveries have been made in this unique structural province. However, petroleum exploration here has focused on basement-cored anticlines, both surface and subthrust, related to the two major Laramide fault systems and on the fault-bounded blocks of Tertiary rocks within the post-Laramide extensional basins. The interplay of the two Laramide fault systems during both Laramide shortening and Tertiary extension has produced a variety of possible structural traps in the Madison Range that have not yet been thoroughly investigated.</p>","language":"English","publisher":"American Association of Petroleum Geologists","doi":"10.1306/8D2B21F5-171E-11D7-8645000102C1865D","usgsCitation":"Kellogg, K., Schmidt, C.J., and Young, S.W., 1995, Basement and cover-rock deformation during Laramide contraction in the northern Madison Range (Montana) and its influence on Cenozoic basin formation: American Association of Petroleum Geologists Bulletin, v. 79, no. 8, p. 1117-1137, https://doi.org/10.1306/8D2B21F5-171E-11D7-8645000102C1865D.","productDescription":"21 p.","startPage":"1117","endPage":"1137","numberOfPages":"21","costCenters":[],"links":[{"id":227582,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Montana","otherGeospatial":"Madison Range","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -110.96298275085888,\n              45.93551953311629\n            ],\n            [\n              -113.14612178278776,\n              45.93551953311629\n            ],\n            [\n              -113.14612178278776,\n              44.48642248439407\n            ],\n            [\n              -110.96298275085888,\n              44.48642248439407\n            ],\n            [\n              -110.96298275085888,\n              45.93551953311629\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","volume":"79","issue":"8","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059efdee4b0c8380cd4a4c1","contributors":{"authors":[{"text":"Kellogg, Karl S.","contributorId":89896,"corporation":false,"usgs":true,"family":"Kellogg","given":"Karl S.","affiliations":[],"preferred":false,"id":380633,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Schmidt, C. J.","contributorId":45066,"corporation":false,"usgs":true,"family":"Schmidt","given":"C.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":380632,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Young, S. W.","contributorId":19722,"corporation":false,"usgs":true,"family":"Young","given":"S.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":380631,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70018942,"text":"70018942 - 1995 - Scour measurements at bridge sites during 1993 Upper Mississippi River Basin flood","interactions":[],"lastModifiedDate":"2016-03-16T15:08:58","indexId":"70018942","displayToPublicDate":"1995-01-01T00:00:00","publicationYear":"1995","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3647,"text":"Transportation Research Record","active":true,"publicationSubtype":{"id":10}},"title":"Scour measurements at bridge sites during 1993 Upper Mississippi River Basin flood","docAbstract":"<p>The record flood on the upper Mississippi River basin during the summer of 1993 provided a rare opportunity for collection of data on streambed scour at bridges and for testing of scour data collection equipment under extreme hydraulic conditions. Real-time scour measurements at bridges are categorized into one of three classes according to their objective: inspection measurements, limited-detail measurements, and detailed measurements. All three types of measurements were made during the 1993 flood. Recent advances in technology and improved application of existing technology allow hydraulic and channel bathymetry data to be collected more accurately, in greater detail, and more efficiently than previously possible. Two limited-detail and two detailed data sets are presented. The observed depths of scour are consistently less than the depths of pier scour estimated by use of recommended procedures. Additional data processing, analysis, and visualization are required to characterize and understand complex processes measured by use of state-of-the-art instrumentation.</p>","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Transportation Research Record","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"National Research Council","publisherLocation":"Washington, DC, United States","issn":"03611981","usgsCitation":"Mueller, D.S., Landers, M.N., and Fischer, E.E., 1995, Scour measurements at bridge sites during 1993 Upper Mississippi River Basin flood: Transportation Research Record, no. 1483, p. 47-55.","startPage":"47","endPage":"55","numberOfPages":"9","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":351,"text":"Iowa Water Science Center","active":true,"usgs":true}],"links":[{"id":226761,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","otherGeospatial":"Upper Mississippi River basin","issue":"1483","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505b87abe4b08c986b3165d7","contributors":{"authors":[{"text":"Mueller, David S. dmueller@usgs.gov","contributorId":1499,"corporation":false,"usgs":true,"family":"Mueller","given":"David","email":"dmueller@usgs.gov","middleInitial":"S.","affiliations":[{"id":502,"text":"Office of Surface Water","active":true,"usgs":true}],"preferred":true,"id":381159,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Landers, Mark N. 0000-0002-3014-0480 landers@usgs.gov","orcid":"https://orcid.org/0000-0002-3014-0480","contributorId":1103,"corporation":false,"usgs":true,"family":"Landers","given":"Mark","email":"landers@usgs.gov","middleInitial":"N.","affiliations":[{"id":502,"text":"Office of Surface Water","active":true,"usgs":true}],"preferred":true,"id":381158,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Fischer, Edward E. edf@usgs.gov","contributorId":1063,"corporation":false,"usgs":true,"family":"Fischer","given":"Edward","email":"edf@usgs.gov","middleInitial":"E.","affiliations":[],"preferred":true,"id":381157,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70018951,"text":"70018951 - 1995 - How much velocity information is necessary to predict sediment suspension in the surf zone?","interactions":[],"lastModifiedDate":"2012-03-12T17:19:14","indexId":"70018951","displayToPublicDate":"1995-01-01T00:00:00","publicationYear":"1995","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"How much velocity information is necessary to predict sediment suspension in the surf zone?","docAbstract":"Instantaneous horizontal water velocity, or velocity to a power, does not contain enough information to predict suspension in the surf zone. Unlike steady uniform flow, more one than one velocity is necessary to parameterize pick-up and mixing of sediment into the water column. Using a velocity history improves predictions of suspension by more carefully specifying flow conditions (including accelerations and changes in accelerations) responsible for suspension. Suspension in the future is better predicted than suspension at the same instant as velocity measurements. Incorporating such a lag between velocity and concentration improved predictions, with optimum lag time increasing with elevation above the sea bed. These lags are largely due to the time for an observed flow event to effect the bed and mix sediment upward.","largerWorkTitle":"Proceedings of the Coastal Engineering Conference","conferenceTitle":"Proceedings of the 24th International Conference on Coastal Engineering. Part 1 (of 3)","conferenceDate":"23 October 1994 through 28 October 1994","conferenceLocation":"Kobe, Jpn","language":"English","publisher":"ASCE","publisherLocation":"New York, NY, United States","issn":"08938717","usgsCitation":"Jaffe, B.E., Rubin, D.M., and Sallenger, A., 1995, How much velocity information is necessary to predict sediment suspension in the surf zone?, <i>in</i> Proceedings of the Coastal Engineering Conference, v. 2, Kobe, Jpn, 23 October 1994 through 28 October 1994, p. 2085-2099.","startPage":"2085","endPage":"2099","numberOfPages":"15","costCenters":[],"links":[{"id":226854,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a3251e4b0c8380cd5e6f0","contributors":{"authors":[{"text":"Jaffe, Bruce E. 0000-0002-8816-5920 bjaffe@usgs.gov","orcid":"https://orcid.org/0000-0002-8816-5920","contributorId":2049,"corporation":false,"usgs":true,"family":"Jaffe","given":"Bruce","email":"bjaffe@usgs.gov","middleInitial":"E.","affiliations":[{"id":520,"text":"Pacific Coastal and Marine Science Center","active":true,"usgs":true},{"id":186,"text":"Coastal and Marine Geology Program","active":true,"usgs":true}],"preferred":true,"id":381177,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Rubin, David M. 0000-0003-1169-1452 drubin@usgs.gov","orcid":"https://orcid.org/0000-0003-1169-1452","contributorId":3159,"corporation":false,"usgs":true,"family":"Rubin","given":"David","email":"drubin@usgs.gov","middleInitial":"M.","affiliations":[{"id":520,"text":"Pacific Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":true,"id":381178,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Sallenger, Asbury Jr.","contributorId":90479,"corporation":false,"usgs":true,"family":"Sallenger","given":"Asbury","suffix":"Jr.","email":"","affiliations":[],"preferred":false,"id":381179,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":5222617,"text":"5222617 - 1995 - Quantitative assessment of pair formation behavior in captive whooping cranes (Grus americana)","interactions":[],"lastModifiedDate":"2026-04-29T16:06:40.607779","indexId":"5222617","displayToPublicDate":"1995-01-01T00:00:00","publicationYear":"1995","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3807,"text":"Zoo Biology","active":true,"publicationSubtype":{"id":10}},"displayTitle":"Quantitative assessment of pair formation behavior in captive whooping cranes (<i>Grus americana</i>)","title":"Quantitative assessment of pair formation behavior in captive whooping cranes (Grus americana)","docAbstract":"<p><span>Instantaneous scan sampling for mean distance and synchronous action patterns and all-occurrence sampling for unison call, dance, strut, and hoover-up behaviors were conducted for five potential whooping crane pairs at Patuxent Environmental Science Center, Laurel, Maryland. Dance, strut, and hoover-up differed among pairs, as did total frequency of social behaviors. It was unclear whether or not total frequency of social behaviors during pair formation can be used as an index for potential breeding success. The relative importance of different action patterns should be used as indices of pair compatibility in captive whooping cranes.</span></p>","language":"English","publisher":"Wiley","doi":"10.1002/zoo.1430140204","usgsCitation":"Nelson, J., Small, C., and Ellis, D.H., 1995, Quantitative assessment of pair formation behavior in captive whooping cranes (Grus americana): Zoo Biology, v. 14, no. 2, p. 107-114, https://doi.org/10.1002/zoo.1430140204.","productDescription":"8 p.","startPage":"107","endPage":"114","costCenters":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":503799,"rank":2,"type":{"id":41,"text":"Open Access External Repository Page"},"url":"https://stars.library.ucf.edu/scopus1990/1693","text":"External Repository"},{"id":199543,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"14","issue":"2","noUsgsAuthors":false,"publicationDate":"2005-05-13","publicationStatus":"PW","scienceBaseUri":"4f4e4a87e4b07f02db64e886","contributors":{"authors":[{"text":"Nelson, J.T.","contributorId":91052,"corporation":false,"usgs":true,"family":"Nelson","given":"J.T.","email":"","affiliations":[],"preferred":false,"id":336691,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Small, C.R.","contributorId":6970,"corporation":false,"usgs":true,"family":"Small","given":"C.R.","email":"","affiliations":[],"preferred":false,"id":336689,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Ellis, D. H.","contributorId":79830,"corporation":false,"usgs":true,"family":"Ellis","given":"D.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":336690,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70018728,"text":"70018728 - 1995 - Petrography, geochemistry, and depositional setting of the San Pedro and Santo Tomas coal zones: Anomalous algae-rich coals in the middle part of the Claiborne Group (Eocene) of Webb County, Texas","interactions":[],"lastModifiedDate":"2018-02-01T12:50:23","indexId":"70018728","displayToPublicDate":"1995-01-01T00:00:00","publicationYear":"1995","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2033,"text":"International Journal of Coal Geology","active":true,"publicationSubtype":{"id":10}},"title":"Petrography, geochemistry, and depositional setting of the San Pedro and Santo Tomas coal zones: Anomalous algae-rich coals in the middle part of the Claiborne Group (Eocene) of Webb County, Texas","docAbstract":"<p>Two coal zones, the San Pedro and the overlying Santo Tomas, are present for nearly 35 km in outcrop, surface and underground mines, and shallow drill holes along the strike of the middle part of the Claiborne Group (Eocene) in Webb County, Texas. A sandstone-dominated interval of 25 to 35 m separates the two coal zones, which range up to 3 m in thickness. Each coal zone contains carbonaceous shales, thin (&lt;0.75 m) impure coal beds, and thin (&lt;0.85 m) but commercially significant nonbanded coal beds. The nonbanded coals are different from other Tertiary coals of the Gulf of Mexico Coastal Plain: unlike lignites that are typical of the older Wilcox Group (Paleocene-Eocene) and younger Jackson Group (Eocene), nonbanded coals of the Claiborne Group have high vitrinite-reflectance values (0.53<span>&nbsp;</span><i>R</i><sub>max</sub>) and high calorific yields (average 6670 kcal/kg or 12,000 Btu, dry basis). The coals are weakly agglomerating (free-swelling index is 1.5–2.0) and have an apparent rank of high-volatile bituminous.</p><p>The coal-bearing portion of the middle Claiborne Group in the Rio Grande area represents a fining-upward transition from sandstone-dominated, marine-influenced, lower delta plain depositional environments to more inland, mudstone-rich, predominantly freshwater deltaic settings. Discontinuities within the San Pedro coal zone are attributed mainly to the influence of contemporaneous deposition of distributary mouth-bar sand bodies. The less variable nature of the Santo Tomas coal zone reflects its origin in the upper part of an interlobe basin that received only minor clastic influx.</p><p>Petrographic attributes of the nonbanded coals indicate that they formed subaqueously in fresh to possibly brackish waters. A highly degraded groundmass composed of eugelinite is the main petrographic component (approximately 71%, mineral-matter-free basis). An enriched liptinite fraction (approximately 23%) probably accounts for unusually high calorific values. There is negligible inertinite. Petrographic study of polished blocks indicates that approximately 10 percent of the nonbanded coal from both coal zones is composed of green algae fructifications, which also occur in clastic rocks of the coal-bearing interval. Such algal material cannot be identified or quantified by conventional coal petrographic techniques that utilize particle pellets or by palynological analyses that include acid preparation.</p>","language":"English","publisher":"Elsevier","doi":"10.1016/0166-5162(95)00022-4","usgsCitation":"Warwick, P.D., and Hook, R.W., 1995, Petrography, geochemistry, and depositional setting of the San Pedro and Santo Tomas coal zones: Anomalous algae-rich coals in the middle part of the Claiborne Group (Eocene) of Webb County, Texas: International Journal of Coal Geology, v. 28, no. 2-4, p. 303-342, https://doi.org/10.1016/0166-5162(95)00022-4.","productDescription":"40 p.","startPage":"303","endPage":"342","costCenters":[],"links":[{"id":227398,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"28","issue":"2-4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a77b2e4b0c8380cd78562","contributors":{"authors":[{"text":"Warwick, Peter D. 0000-0002-3152-7783 pwarwick@usgs.gov","orcid":"https://orcid.org/0000-0002-3152-7783","contributorId":762,"corporation":false,"usgs":true,"family":"Warwick","given":"Peter","email":"pwarwick@usgs.gov","middleInitial":"D.","affiliations":[{"id":241,"text":"Eastern Energy Resources Science Center","active":true,"usgs":true}],"preferred":false,"id":380566,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hook, Robert W.","contributorId":26006,"corporation":false,"usgs":true,"family":"Hook","given":"Robert","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":380567,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70018729,"text":"70018729 - 1995 - Pb2+ and Zn2+ adsorption by a natural aluminum- and iron-bearing surface coating on an aquifer sand","interactions":[],"lastModifiedDate":"2019-02-25T07:41:42","indexId":"70018729","displayToPublicDate":"1995-01-01T00:00:00","publicationYear":"1995","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":"Pb2+ and Zn2+ adsorption by a natural aluminum- and iron-bearing surface coating on an aquifer sand","docAbstract":"<div id=\"abstracts\" class=\"Abstracts u-font-serif\"><div id=\"aep-abstract-id5\" class=\"abstract author\"><div id=\"aep-abstract-sec-id6\"><p>Pb<sup>2+</sup><span>&nbsp;</span>and Zn<sup>2+</sup><span>&nbsp;</span>adsorption was studied in batch experiments with material collected from a shallow, unconfined aquifer of glacial outwash sand and gravel in Falmouth, Massachusetts, USA. The aquifer solids contain primarily quartz (95% w/w), with minor amounts of alkali feldspars and ferromagnetic minerals. Pb<sup>2+</sup><span>&nbsp;</span>and Zn<sup>2+</sup><span>&nbsp;</span>adsorption experiments with various grain size and mineral fractions of the aquifer solids showed that (1) Zn<sup>2+</sup><span>&nbsp;</span>adsorption was independent of grain size, but Pb<sup>2+</sup><span>&nbsp;</span>was preferentially adsorbed by the &lt;64 μm size fraction and (2) Pb<sup>2+</sup>adsorption decreased after removal of the paramagnetic, Fe-bearing mineral fraction, but Zn<sup>2+</sup><span>&nbsp;</span>adsorption was unaffected. Pb<sup>2+</sup><span>&nbsp;</span>and Zn<sup>2+</sup>adsorption on mineral separates from the aquifer material compared with metal adsorption on a purified quartz powder indicated that adsorption of both metal ions was dominated by coatings on the quartz fraction of the sediment. Characterization of the coatings by AES, SEM-EDS, and TOF-SIMS demonstrated that the natural quartz grains were extensively coated with Al- and Fe-bearing minerals of variable composition. Thin sections of quartz grains examined by TEM showed that the coatings contained both polycrystalline regions and single mineral crystals. The coating thickness varied from &lt;10 nm up to 30 μm. The coatings were mostly resistant to dissolution by an extraction protocol designed to dissolve noncrystalline phases. The effect on metal adsorption of dissolving surface coatings from the sediment by chemical extraction was also measured. A hydroxylamine-HC] extraction designed to dissolve crystalline Fe oxide phases decreased Pb<sup>2+</sup><span>&nbsp;</span>and Zn<sup>2+</sup>adsorption relative to untreated sediment (extracted Fe/Al ∼ 1), but Pb<sup>2+</sup>and Zn<sup>2+</sup><span>&nbsp;</span>adsorption were not appreciably changed after sediment was extracted with dithionite-citrate (extracted Fe/Al ∼ 5). Overall, the results suggest that Pb<sup>2+</sup><span>&nbsp;</span>preferred to form complexes with iron hydroxyl sites, while aluminol sites were more important for Zn<sup>2+</sup><span>&nbsp;</span>adsorption. However, a definitive understanding of adsorption reactions in groundwaters will require detailed studies of the extensive coatings formed at mineral-water interfaces by chemical weathering processes.</p></div></div></div>","language":"English","publisher":"Elsevier","doi":"10.1016/0016-7037(95)00231-N","issn":"00167037","usgsCitation":"Coston, J., Fuller, C.C., and Davis, J., 1995, Pb2+ and Zn2+ adsorption by a natural aluminum- and iron-bearing surface coating on an aquifer sand: Geochimica et Cosmochimica Acta, v. 59, no. 17, p. 3535-3547, https://doi.org/10.1016/0016-7037(95)00231-N.","productDescription":"13 p.","startPage":"3535","endPage":"3547","costCenters":[{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":227399,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":205909,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1016/0016-7037(95)00231-N"}],"volume":"59","issue":"17","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a7602e4b0c8380cd77e8e","contributors":{"authors":[{"text":"Coston, J.A.","contributorId":59572,"corporation":false,"usgs":true,"family":"Coston","given":"J.A.","email":"","affiliations":[],"preferred":false,"id":380569,"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":380568,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Davis, J.A.","contributorId":71694,"corporation":false,"usgs":true,"family":"Davis","given":"J.A.","email":"","affiliations":[],"preferred":false,"id":380570,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":1014713,"text":"1014713 - 1995 - Can otolith microchemistry chart patterns of migration and habitat utilization in anadromous fishes?","interactions":[],"lastModifiedDate":"2024-04-30T14:53:26.234633","indexId":"1014713","displayToPublicDate":"1995-01-01T00:00:00","publicationYear":"1995","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2277,"text":"Journal of Experimental Marine Biology and Ecology","active":true,"publicationSubtype":{"id":10}},"title":"Can otolith microchemistry chart patterns of migration and habitat utilization in anadromous fishes?","docAbstract":"<div id=\"preview-section-abstract\"><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>Seasonal and ontogenetic patterns in estuarine and coastal migrations of anadromous fish species have important consequences to their survival, growth, recruitment, and reproduction. We tested the hypothesis that otolith (sagitta) microchemistry can document the environmental history of individual fish across an estuarine salinity gradient. Juvenile striped bass,<span>&nbsp;</span><i>Morone saxatilis</i><span>&nbsp;</span>(Walbaum), (80 days posthatch) were reared for 3 wk in aquaria at two temperatures and six salinities. The ratio of strontium/calcium (<span class=\"math\"><span id=\"MathJax-Element-1-Frame\" class=\"MathJax_SVG\" data-mathml=\"<math xmlns=&quot;http://www.w3.org/1998/Math/MathML&quot;><mtext>Sr</mtext><mtext>Ca</mtext></math>\"><span class=\"MJX_Assistive_MathML\">SrCa</span></span></span>) deposited in the sagittal otoliths of reared juveniles was positively related to salinity. Temperature and growth rate had relatively minor, but significant effects on the<span>&nbsp;</span><span class=\"math\"><span id=\"MathJax-Element-2-Frame\" class=\"MathJax_SVG\" data-mathml=\"<math xmlns=&quot;http://www.w3.org/1998/Math/MathML&quot;><mtext>Sr</mtext><mtext>Ca</mtext></math>\"><span class=\"MJX_Assistive_MathML\">SrCa</span></span></span><span>&nbsp;</span>ratio. In a second experiment, juveniles (80 days posthatch) were exposed to increasing salinity (0 ppt to 25 ppt) and then decreasing salinity (25 ppt to 0 ppt) over a 20-wk period. Electron microprobe examination of the otoliths from these juveniles showed a gradual rise and decline in<span>&nbsp;</span><span class=\"math\"><span id=\"MathJax-Element-3-Frame\" class=\"MathJax_SVG\" data-mathml=\"<math xmlns=&quot;http://www.w3.org/1998/Math/MathML&quot;><mtext>Sr</mtext><mtext>Ca</mtext></math>\"><span class=\"MJX_Assistive_MathML\">SrCa</span></span></span><span>&nbsp;</span>during the experimental period which corresponded directly with experimental changes in salinity. Field data on subadult and adult striped bass corroborated the laboratory analyses and indicated a logistic relationship between ambient salinity and otolith<span>&nbsp;</span><span class=\"math\"><span id=\"MathJax-Element-4-Frame\" class=\"MathJax_SVG\" data-mathml=\"<math xmlns=&quot;http://www.w3.org/1998/Math/MathML&quot;><mtext>Sr</mtext><mtext>Ca</mtext></math>\"><span class=\"MJX_Assistive_MathML\">SrCa</span></span></span><span>&nbsp;</span>ratio. Verification studies support the use of otolith microchemistry to measure migratory schedules and habitat utilization patterns in anadromous striped bass populations.</p></div></div></div></div>","language":"English","publisher":"Elsevier","doi":"10.1016/0022-0981(95)00054-U","usgsCitation":"Secor, D., Henderson-Arzapalo, A., and Piccoli, P., 1995, Can otolith microchemistry chart patterns of migration and habitat utilization in anadromous fishes?: Journal of Experimental Marine Biology and Ecology, v. 192, p. 15-33, https://doi.org/10.1016/0022-0981(95)00054-U.","productDescription":"19 p.","startPage":"15","endPage":"33","numberOfPages":"19","costCenters":[{"id":365,"text":"Leetown Science Center","active":true,"usgs":true}],"links":[{"id":129439,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"192","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49ffe4b07f02db5f797a","contributors":{"authors":[{"text":"Secor, D.H.","contributorId":99495,"corporation":false,"usgs":true,"family":"Secor","given":"D.H.","email":"","affiliations":[],"preferred":false,"id":320990,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Henderson-Arzapalo, A.","contributorId":92607,"corporation":false,"usgs":true,"family":"Henderson-Arzapalo","given":"A.","email":"","affiliations":[],"preferred":false,"id":320989,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Piccoli, P.M.","contributorId":19504,"corporation":false,"usgs":true,"family":"Piccoli","given":"P.M.","email":"","affiliations":[],"preferred":false,"id":320988,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70018732,"text":"70018732 - 1995 - The Uwekahuna Ash Member of the Puna Basalt: product of violent phreatomagmatic eruptions at Kilauea volcano, Hawaii, between 2800 and 2100 14C years ago","interactions":[],"lastModifiedDate":"2013-03-14T19:12:01","indexId":"70018732","displayToPublicDate":"1995-01-01T00:00:00","publicationYear":"1995","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 Uwekahuna Ash Member of the Puna Basalt: product of violent phreatomagmatic eruptions at Kilauea volcano, Hawaii, between 2800 and 2100 14C years ago","docAbstract":"Kilauea volcano's reputation for relatively gentle effusive eruptions belies a violent geologic past, including several large phreatic and phreatomagmatic eruptions that are recorded by Holocene pyroclastic deposits which mantle Kilauea's summit area and the southeast flank of adjacent Mauna Loa volcano. The most widespread of these deposits is the Uwekahuna Ash Member, a basaltic surge and fall deposit emplaced during two or more eruptive episodes separated by a few decades to several centuries. It is infered that the eruptions which produced the Uwekahuna were driven by water interacting with a fluctuating magma column. The volume, extent and character of the Uwekahuna deposits underscore the hazards posed by relatively infrequent but potentially devastating explosive eruptions at Kilauea, as well as at other basaltic volcanoes. -from Authors","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Journal of Volcanology and Geothermal Research","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"Elsevier","doi":"10.1016/0377-0273(94)00062-L","usgsCitation":"Dzurisin, D., Lockwood, J.P., Casadevall, T.J., and Rubin, M., 1995, The Uwekahuna Ash Member of the Puna Basalt: product of violent phreatomagmatic eruptions at Kilauea volcano, Hawaii, between 2800 and 2100 14C years ago: Journal of Volcanology and Geothermal Research, v. 66, no. 1-4, p. 163-184, https://doi.org/10.1016/0377-0273(94)00062-L.","startPage":"163","endPage":"184","numberOfPages":"22","costCenters":[],"links":[{"id":227442,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":269359,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1016/0377-0273(94)00062-L"}],"volume":"66","issue":"1-4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505ba970e4b08c986b32228b","contributors":{"authors":[{"text":"Dzurisin, D.","contributorId":76067,"corporation":false,"usgs":true,"family":"Dzurisin","given":"D.","email":"","affiliations":[],"preferred":false,"id":380578,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Lockwood, J. P.","contributorId":104473,"corporation":false,"usgs":true,"family":"Lockwood","given":"J.","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":380581,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Casadevall, T. J.","contributorId":96680,"corporation":false,"usgs":true,"family":"Casadevall","given":"T.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":380580,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Rubin, M.","contributorId":88079,"corporation":false,"usgs":true,"family":"Rubin","given":"M.","email":"","affiliations":[],"preferred":false,"id":380579,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":1014703,"text":"1014703 - 1995 - Seasonal and annual changes in the diet of double-crested cormorants: implications for Lake Ontario's fishery","interactions":[],"lastModifiedDate":"2012-02-02T00:04:21","indexId":"1014703","displayToPublicDate":"1995-01-01T00:00:00","publicationYear":"1995","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1858,"text":"Great Lakes Research Review","active":true,"publicationSubtype":{"id":10}},"title":"Seasonal and annual changes in the diet of double-crested cormorants: implications for Lake Ontario's fishery","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Great Lakes Research Review","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","collaboration":"96-020/PY96/NF/TL","usgsCitation":"Ross, R.M., and Johnson, J.H., 1995, Seasonal and annual changes in the diet of double-crested cormorants: implications for Lake Ontario's fishery: Great Lakes Research Review, v. 2, no. 1, p. 1-9.","productDescription":"p. 1-9","startPage":"1","endPage":"9","numberOfPages":"9","costCenters":[{"id":365,"text":"Leetown Science Center","active":true,"usgs":true}],"links":[{"id":131343,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"2","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0ce4b07f02db5fc4df","contributors":{"authors":[{"text":"Ross, R. M.","contributorId":39311,"corporation":false,"usgs":true,"family":"Ross","given":"R.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":320958,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Johnson, J. H.","contributorId":54914,"corporation":false,"usgs":true,"family":"Johnson","given":"J.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":320959,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70182478,"text":"70182478 - 1995 - Migratory behavior of Heterosigma carterae, implications for bloom development","interactions":[],"lastModifiedDate":"2017-02-23T12:11:07","indexId":"70182478","displayToPublicDate":"1995-01-01T00:00:00","publicationYear":"1995","noYear":false,"publicationType":{"id":21,"text":"Thesis"},"publicationSubtype":{"id":28,"text":"Thesis"},"title":"Migratory behavior of Heterosigma carterae, implications for bloom development","docAbstract":"<p>No abstract available&nbsp;</p>","language":"English","publisher":"University of Washington","publisherLocation":"Seattle, WA","usgsCitation":"Hershberger, P., 1995, Migratory behavior of Heterosigma carterae, implications for bloom development.","costCenters":[{"id":654,"text":"Western Fisheries Research Center","active":true,"usgs":true}],"links":[{"id":336087,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"publicComments":"M.S. Thesis","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"58b002d9e4b01ccd54fb2801","contributors":{"authors":[{"text":"Hershberger, P.K. 0000-0002-2261-7760","orcid":"https://orcid.org/0000-0002-2261-7760","contributorId":58818,"corporation":false,"usgs":true,"family":"Hershberger","given":"P.K.","affiliations":[],"preferred":false,"id":671238,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70182707,"text":"70182707 - 1995 - Brood amalgamation in the Bristle-thighed Curlew <i>Numenius tahitiensis</i>: process and function","interactions":[],"lastModifiedDate":"2018-08-21T14:38:16","indexId":"70182707","displayToPublicDate":"1995-01-01T00:00:00","publicationYear":"1995","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1961,"text":"Ibis","active":true,"publicationSubtype":{"id":10}},"title":"Brood amalgamation in the Bristle-thighed Curlew <i>Numenius tahitiensis</i>: process and function","docAbstract":"<p><span>Alloparental care in birds generally involves nonbreeding adults that help at nests or breeding adults that help raise young in communal nests. A less often reported form involves the amalgamation of broods, where one or more adults care for young that are not their own. We observed this phenomenon among Bristle-thighed Curlew </span><i>Numenius tahitiensis</i><span> broods in western Alaska during 1990–1992. Amalgamation of broods generally involved the formation of temporary and extended associations. Temporary associations were formed by the incidental convergence of broods soon after they left their nests. During this period, parents defended distinct brood-rearing areas, were antagonistic to conspecifics and remained together for less than 3 days. Extended associations formed when chicks were 1–2 weeks old. Here, parents and their broods occupied distinct, but adjacent, brood-rearing areas and moved around as a unit. Whether a brood participated in either temporary or extended associations or remained solitary appeared to depend on brood density in the immediate area and on hatching date. When chicks were 3–4 weeks old, aggregations of up to ten broods formed wherein young mixed and parents defended a common brood-rearing area. All broods </span><i>(n =</i><span> 48) that survived to fledging joined such aggregations. Alloparental care involved only antipredator defence and was not associated with activities such as feeding and brooding. Most female parents abandoned their broods shortly after the young could fly and when aggregations were forming. The female parent of a pair always deserted its young before or on the same day as the male parent and, in every aggregation, one or two males continued to tend young for about 5 days longer than other male parents. In most cases, adults deserted the young 2–6 days before the young departed the area when about 38 days old. Bristle-thighed Curlews also formed temporary associations with American and Pacific Golden Plover </span><i>Pluvialis dominica</i><span> and </span><i>Pluvialis fulva,</i><span> Whimbrel </span><i>Numenius phaeopus,</i><span> Bar-tailed Godwit </span><i>Limosa lapponica,</i><span> Western Sandpiper </span><i>Cal-idris mauri</i><span> and Long-tailed Skua </span><i>Stercorarius longicaudus.</i><span> Curlews and other larger bodied species commonly attack-mobbed predators together, whereas smaller bodied species generally gave alarm calls and circled the predators. For all species, the intensity of antipredator defence by attending adults gradually decreased as young became older and aggregations formed. We suggest that amalgamation of broods among Bristle-thighed Curlew enhances predator defence, aids in the process of flock formation for migrating young, and allows females and some males to desert their young earlier.</span></p>","language":"English","publisher":"Wiley","doi":"10.1111/j.1474-919X.1995.tb03267.x","usgsCitation":"Lanctot, R.B., Gill, R., Tibbitts, T.L., and Handel, C.M., 1995, Brood amalgamation in the Bristle-thighed Curlew <i>Numenius tahitiensis</i>: process and function: Ibis, v. 137, no. 4, p. 559-569, https://doi.org/10.1111/j.1474-919X.1995.tb03267.x.","productDescription":"9 p.","startPage":"559","endPage":"569","costCenters":[{"id":114,"text":"Alaska Science Center","active":true,"usgs":true}],"links":[{"id":336238,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Alaska","otherGeospatial":"Kougarok River drainage","volume":"137","issue":"4","noUsgsAuthors":false,"publicationDate":"2008-04-03","publicationStatus":"PW","scienceBaseUri":"58b2a59de4b01ccd54fca165","contributors":{"authors":[{"text":"Lanctot, Richard B.","contributorId":31894,"corporation":false,"usgs":true,"family":"Lanctot","given":"Richard","email":"","middleInitial":"B.","affiliations":[{"id":17786,"text":"Carleton University","active":true,"usgs":false},{"id":7029,"text":"Queen's University, Kingston, Ontario, Canada","active":true,"usgs":false},{"id":135,"text":"Biological Resources Division","active":false,"usgs":true},{"id":6987,"text":"U.S. Fish and Wildlife Sevice","active":true,"usgs":false}],"preferred":false,"id":673379,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Gill, Robert E. Jr. 0000-0002-6385-4500 rgill@usgs.gov","orcid":"https://orcid.org/0000-0002-6385-4500","contributorId":171747,"corporation":false,"usgs":true,"family":"Gill","given":"Robert E.","suffix":"Jr.","email":"rgill@usgs.gov","affiliations":[{"id":117,"text":"Alaska Science Center Biology WTEB","active":true,"usgs":true}],"preferred":true,"id":673380,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Tibbitts, T. Lee 0000-0002-0290-7592 ltibbitts@usgs.gov","orcid":"https://orcid.org/0000-0002-0290-7592","contributorId":140455,"corporation":false,"usgs":true,"family":"Tibbitts","given":"T.","email":"ltibbitts@usgs.gov","middleInitial":"Lee","affiliations":[{"id":114,"text":"Alaska Science Center","active":true,"usgs":true},{"id":117,"text":"Alaska Science Center Biology WTEB","active":true,"usgs":true}],"preferred":false,"id":673381,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Handel, Colleen M. 0000-0002-0267-7408 cmhandel@usgs.gov","orcid":"https://orcid.org/0000-0002-0267-7408","contributorId":3067,"corporation":false,"usgs":true,"family":"Handel","given":"Colleen","email":"cmhandel@usgs.gov","middleInitial":"M.","affiliations":[{"id":117,"text":"Alaska Science Center Biology WTEB","active":true,"usgs":true}],"preferred":true,"id":673382,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
]}