{"pageNumber":"4254","pageRowStart":"106325","pageSize":"25","recordCount":184904,"records":[{"id":70017320,"text":"70017320 - 1992 - Types of phreatomagmatic volcanoes in the western Snake River Plain, Idaho, USA","interactions":[],"lastModifiedDate":"2012-03-12T17:18:50","indexId":"70017320","displayToPublicDate":"1992-01-01T00:00:00","publicationYear":"1992","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":"Types of phreatomagmatic volcanoes in the western Snake River Plain, Idaho, USA","docAbstract":"The western Snake River Plain graben in southwestern Idaho includes a large hydrovolcanic field which was produced in late Miocene to Pleistocene time by the interaction of rising basaltic magmas with the waters and water-saturated deposits of an enormous freshwater lake, Lake Idaho. The phreatomagmatic volcanoes in this field may be grouped into three types: emergent, subaqueous and subaerial. Emergent volcanoes, which began erupting under water and built up above the lake level, are relatively large and symmetrical, are dominated by bedded tuffs and late magmatic deposits, and are excellent indicators of water depth at the time of the eruption. Subaqueous volcanoes, which never built up above the lake level, are relatively small and asymmetrical, are dominated by basal massive deposits, and are potentially useful in discriminating between deep- and very-deep-water settings. Subaerial volcanoes, which were formed when magmas intercepted buried aquifers and interacted explosively with water, are small tuff rings and maars with variable shapes, are composed of subequal (although variable) proportions of basal massive deposits, bedded tuffs and late magmatic deposits, and are useful in determining the stratigraphic successions underlying them. ?? 1992.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Journal of Volcanology and Geothermal Research","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","issn":"03770273","usgsCitation":"Godchaux, M., Bonnichsen, B., and Jenks, M., 1992, Types of phreatomagmatic volcanoes in the western Snake River Plain, Idaho, USA: Journal of Volcanology and Geothermal Research, v. 52, no. 1-3, p. 1-25.","startPage":"1","endPage":"25","numberOfPages":"25","costCenters":[],"links":[{"id":224542,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"52","issue":"1-3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505bb9b3e4b08c986b327d54","contributors":{"authors":[{"text":"Godchaux, M.M.","contributorId":91638,"corporation":false,"usgs":true,"family":"Godchaux","given":"M.M.","affiliations":[],"preferred":false,"id":376121,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bonnichsen, B.","contributorId":19300,"corporation":false,"usgs":true,"family":"Bonnichsen","given":"B.","affiliations":[],"preferred":false,"id":376120,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Jenks, M.D.","contributorId":16885,"corporation":false,"usgs":true,"family":"Jenks","given":"M.D.","email":"","affiliations":[],"preferred":false,"id":376119,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70017150,"text":"70017150 - 1992 - Energy budgets and resistances to energy transport in sparsely vegetated rangeland","interactions":[],"lastModifiedDate":"2023-02-21T16:53:42.972072","indexId":"70017150","displayToPublicDate":"1992-01-01T00:00:00","publicationYear":"1992","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":681,"text":"Agricultural and Forest Meteorology","active":true,"publicationSubtype":{"id":10}},"title":"Energy budgets and resistances to energy transport in sparsely vegetated rangeland","docAbstract":"<p><span>Partitioning available energy between plants and bare soil in sparsely vegetated rangelands will allow hydrologists and others to gain a greater understanding of water use by native vegetation, especially phreatophytes. Standard methods of conducting energy budget studies result in measurements of latent and sensible heat fluxes above the plant canopy which therefore include the energy fluxes from both the canopy and the soil. One-dimensional theoretical numerical models have been proposed recently for the partitioning of energy in sparse crops. Bowen ratio and other micrometeorological data collected over phreatophytes growing in areas of shallow ground water in central Nevada were used to evaluate the feasibility of using these models, which are based on surface and within-canopy aerodynamic resistances, to determine heat and water vapor transport in sparsely vegetated rangelands. The models appear to provide reasonably good estimates of sensible heat flux from the soil and latent heat flux from the canopy. Estimates of latent heat flux from the soil were less satisfactory. Sensible heat flux from the canopy was not well predicted by the present resistance formulations. Also, estimates of total above-canopy fluxes were not satisfactory when using a single value for above-canopy bulk aerodynamic resistance.</span></p>","language":"English","publisher":"Elsevier","doi":"10.1016/0168-1923(92)90039-7","usgsCitation":"Nichols, W., 1992, Energy budgets and resistances to energy transport in sparsely vegetated rangeland: Agricultural and Forest Meteorology, v. 60, no. 3-4, p. 221-247, https://doi.org/10.1016/0168-1923(92)90039-7.","productDescription":"27 p.","startPage":"221","endPage":"247","numberOfPages":"27","costCenters":[],"links":[{"id":224822,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"60","issue":"3-4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a0946e4b0c8380cd51e53","contributors":{"authors":[{"text":"Nichols, William D.","contributorId":98296,"corporation":false,"usgs":true,"family":"Nichols","given":"William D.","affiliations":[],"preferred":false,"id":375564,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70182209,"text":"70182209 - 1992 - Changes in Alaskan soft-bottom prey communities along a gradient in sea otter predation","interactions":[],"lastModifiedDate":"2017-02-21T11:44:47","indexId":"70182209","displayToPublicDate":"1992-01-01T00:00:00","publicationYear":"1992","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1465,"text":"Ecology","active":true,"publicationSubtype":{"id":10}},"title":"Changes in Alaskan soft-bottom prey communities along a gradient in sea otter predation","docAbstract":"<p><span>Sea Otter (<i>Enhydra lutris</i>), well documented as \"keystone\" predators in rocky marine communities, were found to exert a strong influence on infaunal prey communities in soft-sediment habitats. Direct and indirect effects of sea otter predation on subtidal soft-bottom prey communities were evaluated along a temporal gradient of sea otter occupancy around the Kodiak Archipelago. The results indicate that Kodiak otters forage primarily on bivalve prey and dramatically reduce infaunal bivalve and green sea urchin (<i>Strongylocentrotus droebachiensis</i>) prey populations. Bivalve prey abundance, biomass, and size were inversely related to duration of sea otter occupancy. The relative conditions of shells discarded by otters in shallow (&lt;10 m) vs. deep (&gt; 20 m) water at the same sites indicate that otters first exploited <i>Saxidomus</i> in shallow-water feeding areas, and later switched to <i>Macoma</i> spp. in deeper water. Otter-cracked shells of the deep-burrowing clam <i>Tresus capax</i> were rarely found, even at otter foraging sites where the clam accounted for the majority of available prey biomass, suggesting that it has a partial depth refuge from otter predation. The indirect effects of otter predation included substratum disturbance and the facilitation of sea star predation on infaunal prey. Sea stars, <i>Pycnopodia helianthoides</i>, were attracted to experimentally dug excavations as well as natural sea otter foraging pits, where the sea stars foraged on smaller size classes of infaunal bivalves than those eaten by otters. Otters also discard clam shells on the sediment surface and expose old, buried shells during excavation. Surface shells were found to provide attachment sites for large anemones and kelp. Our study shows that sea otters can affect soft-sediment communities, not only through predation, as in rocky habitats, but also through disturbance, and thus retain a high degree of influence in two very different habitat types.</span></p>","language":"English","publisher":"Wiley","doi":"10.2307/1940749","usgsCitation":"Kvitek, R., Oliver, J., DeGange, A., and Anderson, B., 1992, Changes in Alaskan soft-bottom prey communities along a gradient in sea otter predation: Ecology, v. 73, no. 2, p. 413-428, https://doi.org/10.2307/1940749.","productDescription":"16 p.","startPage":"413","endPage":"428","costCenters":[{"id":114,"text":"Alaska Science Center","active":true,"usgs":true}],"links":[{"id":335873,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Alaska","otherGeospatial":"Kodiak Archipelago","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -151.19384765624997,\n              58.19966110122876\n            ],\n            [\n              -152.29248046875,\n              58.78528524510292\n            ],\n            [\n              -152.698974609375,\n              58.77959115030064\n            ],\n            [\n              -153.6767578125,\n              58.257507589081605\n            ],\n            [\n              -155.028076171875,\n              57.468589192089354\n            ],\n            [\n              -155.24780273437497,\n              56.23724470041031\n            ],\n            [\n              -154.2919921875,\n              56.15166933290848\n            ],\n            [\n              -151.951904296875,\n              57.33838126552897\n            ],\n            [\n              -151.19384765624997,\n              58.19966110122876\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"73","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"58ad5ff1e4b01ccd54f8b589","contributors":{"authors":[{"text":"Kvitek, R.G.","contributorId":36384,"corporation":false,"usgs":true,"family":"Kvitek","given":"R.G.","email":"","affiliations":[],"preferred":false,"id":669989,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Oliver, J.S.","contributorId":17073,"corporation":false,"usgs":true,"family":"Oliver","given":"J.S.","email":"","affiliations":[],"preferred":false,"id":669990,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"DeGange, A.R.","contributorId":52105,"corporation":false,"usgs":true,"family":"DeGange","given":"A.R.","email":"","affiliations":[],"preferred":false,"id":669991,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Anderson, B.S.","contributorId":181917,"corporation":false,"usgs":false,"family":"Anderson","given":"B.S.","email":"","affiliations":[],"preferred":false,"id":669992,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70017219,"text":"70017219 - 1992 - GIS-assisted regression analysis to identify sources of selenium in streams","interactions":[],"lastModifiedDate":"2019-03-19T07:47:56","indexId":"70017219","displayToPublicDate":"1992-01-01T00:00:00","publicationYear":"1992","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3718,"text":"Water Resources Bulletin","printIssn":"0043-1370","active":true,"publicationSubtype":{"id":10}},"title":"GIS-assisted regression analysis to identify sources of selenium in streams","docAbstract":"Using a geographic information system, a regression model has been developed to identify and to assess potential sources of selenium in the Kendrick Reclamation Project Area, Wyoming. A variety of spatially distributed factors was examined to determine which factors are most likely to affect selenium discharge in tributaries to the North Platte River. Areas of Upper Cretaceous Cody Shale and Quaternary alluvial deposits and irrigated land, length of irrigation canals, and boundaries of hydrologic subbasins of the major tributaries to the North Platte River were digitized and stored in a geographic information system. Selenium concentrations in samples of soil, plant material, ground water, and surface water were determined and evaluated. The location of all sampling sites was digitized and stored in the geographic information system, together with the selenium concentrations in samples. A regression model was developed using stepwise multiple regression of median selenium discharges on the physical and chemical characteristics of hydrologic subbasins. Results indicate that the intensity of irrigation in a hydrologic subbasin, as determined by area of irrigated land and length of irrigation delivery canals, accounts for the largest variation in median selenium discharges among subbasins. Tributaries draining hydrologic subbasins with greater intensity of irrigation result in greater selenium discharges to the North Platte River than do tributaries draining subbasins with lesser intensity of irrigation.","language":"English","publisher":"Wiley","doi":"10.1111/j.1752-1688.1992.tb03997.x","issn":"00431370","usgsCitation":"See, R.B., Naftz, D.L., and Qualls, C.L., 1992, GIS-assisted regression analysis to identify sources of selenium in streams: Water Resources Bulletin, v. 28, no. 2, p. 315-330, https://doi.org/10.1111/j.1752-1688.1992.tb03997.x.","productDescription":"16 p.","startPage":"315","endPage":"330","costCenters":[{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":225160,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":267706,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1111/j.1752-1688.1992.tb03997.x"}],"volume":"28","issue":"2","noUsgsAuthors":false,"publicationDate":"2007-06-08","publicationStatus":"PW","scienceBaseUri":"505a146be4b0c8380cd54a1a","contributors":{"authors":[{"text":"See, Randolph B. rsee@usgs.gov","contributorId":5632,"corporation":false,"usgs":true,"family":"See","given":"Randolph","email":"rsee@usgs.gov","middleInitial":"B.","affiliations":[],"preferred":true,"id":375780,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Naftz, David L. 0000-0003-1130-6892 dlnaftz@usgs.gov","orcid":"https://orcid.org/0000-0003-1130-6892","contributorId":1041,"corporation":false,"usgs":true,"family":"Naftz","given":"David","email":"dlnaftz@usgs.gov","middleInitial":"L.","affiliations":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true},{"id":5050,"text":"WY-MT Water Science Center","active":true,"usgs":true}],"preferred":true,"id":375779,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Qualls, Charles L.","contributorId":106394,"corporation":false,"usgs":true,"family":"Qualls","given":"Charles","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":375781,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70016904,"text":"70016904 - 1992 - Multispectral thermal infrared mapping of the 1 October 1988 Kupaianaha flow field, Kilauea volcano, Hawaii","interactions":[],"lastModifiedDate":"2012-03-12T17:18:53","indexId":"70016904","displayToPublicDate":"1992-01-01T00:00:00","publicationYear":"1992","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1109,"text":"Bulletin of Volcanology","active":true,"publicationSubtype":{"id":10}},"title":"Multispectral thermal infrared mapping of the 1 October 1988 Kupaianaha flow field, Kilauea volcano, Hawaii","docAbstract":"Multispectral thermal infrared radiance measurements of the Kupaianaha flow field were acquired with the NASA airborne Thermal Infrared Multispectral Scanner (TIMS) on the morning of 1 October 1988. The TIMS data were used to map both the temperature and emissivity of the surface of the flow field. The temperature map depicted the underground storage and transport of lava. The presence of molten lava in a tube or tumulus resulted in surface temperatures that were at least 10?? C above ambient. The temperature map also clearly defined the boundaries of hydrothermal plumes which resulted from the entry of lava into the ocean. The emissivity map revealed the boundaries between individual flow units within the Kupaianaha field. In general, the emissivity of the flows varied systematically with age but the relationship between age and emissivity was not unique. Distinct spectral anomalies, indicative of silica-rich surface materials, were mapped near fumaroles and ocean entry sites. This apparent enrichment in silica may have resulted from an acid-induced leaching of cations from the surfaces of glassy flows. Such incipient alteration may have been the cause for virtually all of the emissivity variations observed on the flow field, the spectral anomalies representing areas where the acid attack was most intense. ?? 1992 Springer-Verlag.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Bulletin of Volcanology","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisherLocation":"Springer-Verlag","doi":"10.1007/BF00301118","issn":"02588900","usgsCitation":"Realmuto, V., Hon, K., Kahle, A., Abbott, E., and Pieri, D., 1992, Multispectral thermal infrared mapping of the 1 October 1988 Kupaianaha flow field, Kilauea volcano, Hawaii: Bulletin of Volcanology, v. 55, no. 1-2, p. 33-44, https://doi.org/10.1007/BF00301118.","startPage":"33","endPage":"44","numberOfPages":"12","costCenters":[],"links":[{"id":205496,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1007/BF00301118"},{"id":224516,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"55","issue":"1-2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a60a8e4b0c8380cd715e9","contributors":{"authors":[{"text":"Realmuto, V.J.","contributorId":60779,"corporation":false,"usgs":true,"family":"Realmuto","given":"V.J.","email":"","affiliations":[],"preferred":false,"id":374814,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hon, K.","contributorId":20471,"corporation":false,"usgs":true,"family":"Hon","given":"K.","email":"","affiliations":[],"preferred":false,"id":374812,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Kahle, A.B.","contributorId":36928,"corporation":false,"usgs":true,"family":"Kahle","given":"A.B.","email":"","affiliations":[],"preferred":false,"id":374813,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Abbott, E.A.","contributorId":64814,"corporation":false,"usgs":true,"family":"Abbott","given":"E.A.","email":"","affiliations":[],"preferred":false,"id":374815,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Pieri, D.C.","contributorId":100547,"corporation":false,"usgs":true,"family":"Pieri","given":"D.C.","email":"","affiliations":[],"preferred":false,"id":374816,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":70017233,"text":"70017233 - 1992 - Use of geochemical biomarkers in bottom sediment to track oil from a spill, San Francisco Bay, California","interactions":[],"lastModifiedDate":"2019-03-14T05:23:15","indexId":"70017233","displayToPublicDate":"1992-01-01T00:00:00","publicationYear":"1992","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2676,"text":"Marine Pollution Bulletin","active":true,"publicationSubtype":{"id":10}},"title":"Use of geochemical biomarkers in bottom sediment to track oil from a spill, San Francisco Bay, California","docAbstract":"<p>In April 1988, approximately 1500 m3 of a San Joaquin Valley crude oil were accidentally released from a Shell Oil Co. refinery near Martinez, Californa. The oil flowed into Carquinez Strait and Suisun Bay in northern San Francisco Bay Sediment and oil samples were collected within a week and analysed for geochemical marker compounds in order to track the molecular signature of the oil spill in the bottom sediment. Identification of the spilled oil in the sediment was complicated by the degraded nature of the oil and the similarity of the remaining, chromatographically resolvable constituents to those already present in the sediments from anthropogenic petroleum contamination, pyrogenic sources, and urban drainage. Ratios of hopane and sterane biomarkers, and of polycyclic aromatic hydrocarbons and their alkylated derivatives best identified the oil impingement. They showed the oil impact at this early stage to be surficial only, and to be patchy even within an area of heavy oil exposure.</p>","language":"English","publisher":"Elsevier","doi":"10.1016/0025-326X(92)90311-S","issn":"0025326X","usgsCitation":"Hostettler, F., Rapp, J.B., and Kvenvolden, K., 1992, Use of geochemical biomarkers in bottom sediment to track oil from a spill, San Francisco Bay, California: Marine Pollution Bulletin, v. 24, no. 1, p. 15-20, https://doi.org/10.1016/0025-326X(92)90311-S.","productDescription":"6 p.","startPage":"15","endPage":"20","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":154,"text":"California Water Science Center","active":true,"usgs":true},{"id":552,"text":"San Francisco Bay-Delta","active":false,"usgs":true},{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true},{"id":5079,"text":"Pacific Regional Director's Office","active":true,"usgs":true}],"links":[{"id":224731,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":205540,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1016/0025-326X(92)90311-S"}],"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              -122.82714843749999,\n              37.36579146999664\n            ],\n            [\n              -121.3604736328125,\n              37.36579146999664\n            ],\n            [\n              -121.3604736328125,\n              38.46864331036051\n            ],\n            [\n              -122.82714843749999,\n              38.46864331036051\n            ],\n            [\n              -122.82714843749999,\n              37.36579146999664\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"24","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505bbf16e4b08c986b329951","contributors":{"authors":[{"text":"Hostettler, F. D.","contributorId":99563,"corporation":false,"usgs":true,"family":"Hostettler","given":"F. D.","affiliations":[],"preferred":false,"id":375835,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Rapp, J. B.","contributorId":28987,"corporation":false,"usgs":true,"family":"Rapp","given":"J.","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":375833,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Kvenvolden, K.A.","contributorId":80674,"corporation":false,"usgs":true,"family":"Kvenvolden","given":"K.A.","email":"","affiliations":[],"preferred":false,"id":375834,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":1008505,"text":"1008505 - 1992 - Comparisons of salinity tolerances and osmotic regulatory capabilities in populations of Sailfin molly (Poecilia latipinna) from brackish and fresh waters","interactions":[],"lastModifiedDate":"2023-12-01T12:22:47.582679","indexId":"1008505","displayToPublicDate":"1992-01-01T00:00:00","publicationYear":"1992","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1337,"text":"Copeia","active":true,"publicationSubtype":{"id":10}},"title":"Comparisons of salinity tolerances and osmotic regulatory capabilities in populations of Sailfin molly (Poecilia latipinna) from brackish and fresh waters","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"American Society of Ichthyologists and Herpetologists","doi":"10.2307/1446150","usgsCitation":"Nordlie, F., Haney, D.C., and Walsh, S., 1992, Comparisons of salinity tolerances and osmotic regulatory capabilities in populations of Sailfin molly (Poecilia latipinna) from brackish and fresh waters: Copeia, v. 1992, no. 3, p. 741-746, https://doi.org/10.2307/1446150.","productDescription":"6 p.","startPage":"741","endPage":"746","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":131918,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"1992","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1ee4b07f02db6aa664","contributors":{"authors":[{"text":"Nordlie, F.G.","contributorId":71930,"corporation":false,"usgs":true,"family":"Nordlie","given":"F.G.","email":"","affiliations":[],"preferred":false,"id":317961,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Haney, D. C.","contributorId":97854,"corporation":false,"usgs":true,"family":"Haney","given":"D.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":317962,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Walsh, S. J. 0000-0002-1009-8537","orcid":"https://orcid.org/0000-0002-1009-8537","contributorId":62171,"corporation":false,"usgs":true,"family":"Walsh","given":"S. J.","affiliations":[],"preferred":false,"id":317960,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":1014852,"text":"1014852 - 1992 - Host defense mechanisms of Cephalopods","interactions":[],"lastModifiedDate":"2023-02-28T16:04:41.663908","indexId":"1014852","displayToPublicDate":"1992-01-01T00:00:00","publicationYear":"1992","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":810,"text":"Annual Review of Fish Diseases","active":true,"publicationSubtype":{"id":10}},"title":"Host defense mechanisms of Cephalopods","docAbstract":"<div id=\"preview-section-abstract\"><div id=\"abstracts\" class=\"Abstracts u-font-gulliver text-s\"><div id=\"aep-abstract-id2\" class=\"abstract author\"><div id=\"aep-abstract-sec-id3\"><p id=\"SP0005\">Humoral and cellular mechanisms of defense have been described for cephalopods, a relatively advanced group of mollusks. Typical of other mollusks, cephalopod agglutinins are the most documented component of humoral immunity. Lectins, which have agglutinating properties, have been described and characterized from octopuses. Agglutinins from cephalopod hemolymph have also been shown to agglutinate a variety of vertebrate red blood cells, as well as potential bacterial pathogens. Hemocytes are the primary component of cellular immunity. Although the hemocyte role in phagocytosis has been extensively studied in other mollusks, the mechanisms of phagocytosis have not been described extensively for cephalopods. Cephalopod hemocytes have phagocytic capabilities and may function in encapsulation and neutralization of foreign substances; however, the effects of environmental factors and the full extent of phagocytic capabilities of cephalopod hemocytes have not been reported. Hemocytes from cephalopods have a role in wound healing and inflammation which have been reported in detail by several investigators.</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":"Annual Reviews","doi":"10.1016/0959-8030(92)90054-2","usgsCitation":"Ford, L., 1992, Host defense mechanisms of Cephalopods: Annual Review of Fish Diseases, v. 2, p. 15-41, https://doi.org/10.1016/0959-8030(92)90054-2.","productDescription":"27 p.","startPage":"15","endPage":"41","numberOfPages":"27","costCenters":[{"id":365,"text":"Leetown Science Center","active":true,"usgs":true}],"links":[{"id":131662,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a54e4b07f02db62be07","contributors":{"authors":[{"text":"Ford, Larisa","contributorId":191025,"corporation":false,"usgs":false,"family":"Ford","given":"Larisa","email":"","affiliations":[],"preferred":false,"id":321364,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":1014903,"text":"1014903 - 1992 - Immunization of channel catfish with a crude, acid-extracted preparation of motile aeromonad S-layer protein Biomedical Letters","interactions":[],"lastModifiedDate":"2023-11-07T13:12:31.178449","indexId":"1014903","displayToPublicDate":"1992-01-01T00:00:00","publicationYear":"1992","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1036,"text":"Biomedical Letters","active":true,"publicationSubtype":{"id":10}},"title":"Immunization of channel catfish with a crude, acid-extracted preparation of motile aeromonad S-layer protein Biomedical Letters","docAbstract":"<p>No abstract available.&nbsp;</p>","language":"English","usgsCitation":"Ford, L., and Thune, R., 1992, Immunization of channel catfish with a crude, acid-extracted preparation of motile aeromonad S-layer protein Biomedical Letters: Biomedical Letters, v. 47, no. 188, p. 355-362.","productDescription":"8 p.","startPage":"355","endPage":"362","numberOfPages":"8","costCenters":[{"id":365,"text":"Leetown Science Center","active":true,"usgs":true}],"links":[{"id":130843,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"47","issue":"188","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac9e4b07f02db67c647","contributors":{"authors":[{"text":"Ford, L.A.","contributorId":25510,"corporation":false,"usgs":true,"family":"Ford","given":"L.A.","email":"","affiliations":[],"preferred":false,"id":321488,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Thune, R.L.","contributorId":100240,"corporation":false,"usgs":true,"family":"Thune","given":"R.L.","email":"","affiliations":[],"preferred":false,"id":321489,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":1014908,"text":"1014908 - 1992 - Recovery of infectious pancreatic necrosis virus from the faeces of wild piscivorous birds","interactions":[],"lastModifiedDate":"2023-08-08T15:10:41.019572","indexId":"1014908","displayToPublicDate":"1992-01-01T00:00:00","publicationYear":"1992","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":853,"text":"Aquaculture","active":true,"publicationSubtype":{"id":10}},"title":"Recovery of infectious pancreatic necrosis virus from the faeces of wild piscivorous birds","docAbstract":"<p><span>Faecal samples were collected from wild birds frequenting salmonid fish hatcheries to determine if birds excrete infectious pancreatic necrosis (IPN) virus in their faeces. Samples were collected from early June through early September. IPN virus was detected in faeces from herons, mallards, and other birds at titres similar to the titres found in the hatchery fish. Bird predation and virus prevalence in bird faeces was much reduced at a hatchery using electric fence barriers to deter birds and at a hatchery where the entire raceway area was enclosed by netting.</span></p>","language":"English","publisher":"Elsevier","doi":"10.1016/0044-8486(92)90254-I","usgsCitation":"McAllister, P.E., and Owens, W.J., 1992, Recovery of infectious pancreatic necrosis virus from the faeces of wild piscivorous birds: Aquaculture, v. 106, no. 3/4, p. 227-232, https://doi.org/10.1016/0044-8486(92)90254-I.","productDescription":"6 p.","startPage":"227","endPage":"232","numberOfPages":"6","costCenters":[{"id":365,"text":"Leetown Science Center","active":true,"usgs":true}],"links":[{"id":131983,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"106","issue":"3/4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a60e4b07f02db635455","contributors":{"authors":[{"text":"McAllister, P. E.","contributorId":71913,"corporation":false,"usgs":true,"family":"McAllister","given":"P.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":321510,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Owens, W. J.","contributorId":15968,"corporation":false,"usgs":true,"family":"Owens","given":"W.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":321509,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70017266,"text":"70017266 - 1992 - Effects of acidic deposition on the erosion of carbonate stone - experimental results from the U.S. National Acid Precipitation Assessment Program (NAPAP)","interactions":[],"lastModifiedDate":"2012-03-12T17:18:53","indexId":"70017266","displayToPublicDate":"1992-01-01T00:00:00","publicationYear":"1992","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"Effects of acidic deposition on the erosion of carbonate stone - experimental results from the U.S. National Acid Precipitation Assessment Program (NAPAP)","docAbstract":"One of the goals of NAPAP-sponsored research on the effects of acidic deposition on carbonate stone has been to quantify the incremental effects of wet and dry deposition of hydrogen ion, sulfur dioxide and nitrogen oxides on stone erosion. Test briquettes and slabs of freshly quarried Indiana limestone and Vermont marble have been exposed to ambient environmental conditions in a long-term exposure program. Physical measurements of the recession of test stones exposed to ambient conditions at an angle of 30?? to horizontal at the five NAPAP materials exposure sites range from ~15 to ~30?? ??m yr-1 for marble, and from ~25 to ~45 ??m yr -1 for limestone, and are approximately double the recession estimates based on the observed calcium content of run-off solutions from test slabs. The difference between the physical and chemical recession measurements is attributed to the loss of mineral grains from the stone surfaces that are not measured in the run-off experiments. The erosion due to grain loss does not appear to be influenced by rainfall acidity, however, preliminary evidence suggests that grain loss may be influenced by dry deposition of sulfur dioxide between rainfall events. Chemical analyses of the run-off solutions and associated rainfall blanks suggest that ~30% of erosion by dissolution can be attributed to the wet deposition of hydrogen ion and the dry deposition of sulfur dioxide and nitric acid between rain events. The remaining ~70% of erosion by dissolution is accounted for by the solubility of carbonate stone in rain that is in equilibrium with atmospheric carbon dioxide ('clean rain'). These results are for marble and limestone slabs exposed at an angle of 30?? from horizontal. The relative contribution of sulfur dioxide to chemical erosion is significantly enhanced for stone slabs having an inclination of 60?? or 85??. The dry deposition of alkaline particulate material has a mitigating effect at the two urban field exposure sites at Washington, DC, and Steubenville, OH.","largerWorkTitle":"Atmospheric Environment - Part B Urban Atmosphere","language":"English","doi":"10.1016/0957-1272(92)90018-N","issn":"09571272","usgsCitation":"Baedecker, P.A., Reddy, M., Reimann, K., and Sciammarella, C., 1992, Effects of acidic deposition on the erosion of carbonate stone - experimental results from the U.S. National Acid Precipitation Assessment Program (NAPAP), <i>in</i> Atmospheric Environment - Part B Urban Atmosphere, v. 26, no. 2, p. 147-158, https://doi.org/10.1016/0957-1272(92)90018-N.","startPage":"147","endPage":"158","numberOfPages":"12","costCenters":[],"links":[{"id":205613,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1016/0957-1272(92)90018-N"},{"id":225211,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"26","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a0679e4b0c8380cd51272","contributors":{"authors":[{"text":"Baedecker, P. A.","contributorId":95444,"corporation":false,"usgs":true,"family":"Baedecker","given":"P.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":375935,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Reddy, M.M.","contributorId":24363,"corporation":false,"usgs":true,"family":"Reddy","given":"M.M.","email":"","affiliations":[],"preferred":false,"id":375933,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Reimann, K.J.","contributorId":19035,"corporation":false,"usgs":true,"family":"Reimann","given":"K.J.","email":"","affiliations":[],"preferred":false,"id":375932,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Sciammarella, C.A.","contributorId":62086,"corporation":false,"usgs":true,"family":"Sciammarella","given":"C.A.","email":"","affiliations":[],"preferred":false,"id":375934,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70017162,"text":"70017162 - 1992 - Effects of climatic change and climatic variability on the Thornthwaite moisture index in the Delaware River basin","interactions":[],"lastModifiedDate":"2012-03-12T17:18:52","indexId":"70017162","displayToPublicDate":"1992-01-01T00:00:00","publicationYear":"1992","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1252,"text":"Climatic Change","active":true,"publicationSubtype":{"id":10}},"title":"Effects of climatic change and climatic variability on the Thornthwaite moisture index in the Delaware River basin","docAbstract":"The Thornthwaite moisture index is useful as an indicator of the supply of water in an area relative to the demand under prevailing climatic conditions. This study examines the effects of long-term changes in climate (temperature and precipitation) on the Thornthwaite moisture index in the Delaware River basin. Temperature and precipitation estimates for doubled-CO2 conditions derived from three general circulation models (GCMs) are used to study the response of the moisture index for steady-state doubled-CO2 conditions and for gradual changes from present to doubled-CO2 conditions. Results of the study indicate that temperature and precipitation under doubled-CO2 conditions will cause the Thornthwaite moisture index to decrease, implying significantly drier conditions in the Delaware River basin than currently exist. The amount of decrease depends, however, on the GCM climatic-change scenario used. The results also indicate that future changes in the moisture index will be partly masked by natural year-to-year variability in temperature and precipitation. ?? 1992 Kluwer Academic Publishers.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Climatic Change","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisherLocation":"Kluwer Academic Publishers","doi":"10.1007/BF00154172","issn":"01650009","usgsCitation":"McCabe, G.J., and Wolock, D., 1992, Effects of climatic change and climatic variability on the Thornthwaite moisture index in the Delaware River basin: Climatic Change, v. 20, no. 2, p. 143-153, https://doi.org/10.1007/BF00154172.","startPage":"143","endPage":"153","numberOfPages":"11","costCenters":[],"links":[{"id":205586,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1007/BF00154172"},{"id":225007,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"20","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a06b0e4b0c8380cd51390","contributors":{"authors":[{"text":"McCabe, G. J. Jr.","contributorId":77551,"corporation":false,"usgs":true,"family":"McCabe","given":"G.","suffix":"Jr.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":375598,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Wolock, D.M. 0000-0002-6209-938X","orcid":"https://orcid.org/0000-0002-6209-938X","contributorId":36601,"corporation":false,"usgs":true,"family":"Wolock","given":"D.M.","affiliations":[],"preferred":false,"id":375597,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70017267,"text":"70017267 - 1992 - Analytical interferences of mercuric chloride preservative in environmental water samples: Determination of organic compounds isolated by continuous liquid-liquid extraction or closed-loop stripping","interactions":[],"lastModifiedDate":"2019-03-19T10:00:07","indexId":"70017267","displayToPublicDate":"1992-01-01T00:00:00","publicationYear":"1992","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1565,"text":"Environmental Science & Technology","onlineIssn":"1520-5851","printIssn":"0013-936X","active":true,"publicationSubtype":{"id":10}},"title":"Analytical interferences of mercuric chloride preservative in environmental water samples: Determination of organic compounds isolated by continuous liquid-liquid extraction or closed-loop stripping","docAbstract":"Analytical interferences were observed during the determination of organic compounds in groundwater samples preserved with mercuric chloride. The nature of the interference was different depending on the analytical isolation technique employed. (1) Water samples extracted with dichloromethane by continuous liquid-liquid extraction (CLLE) and analyzed by gas chromatography/mass spectrometry revealed a broad HgCl2 'peak' eluting over a 3-5-min span which interfered with the determination of coeluting organic analytes. Substitution of CLLE for separatory funnel extraction in EPA method 508 also resulted in analytical interferences from the use of HgCl2 preservative. (2) Mercuric chloride was purged, along with organic contaminants, during closed-loop stripping (CLS) of groundwater samples and absorbed onto the activated charcoal trap. Competitive sorption of the HgCl2 by the trap appeared to contribute to the observed poor recoveries for spiked organic contaminants. The HgCl2 was not displaced from the charcoal with the dichloromethane elution solvent and required strong nitric acid to achieve rapid, complete displacement. Similar competitive sorption mechanisms might also occur in other purge and trap methods when this preservative is used.","language":"English","publisher":"ACS","doi":"10.1021/es00031a004","issn":"0013936X","usgsCitation":"Foreman, W., Zaugg, S., Falres, L., Werner, M., Leiker, T., and Rogerson, P., 1992, Analytical interferences of mercuric chloride preservative in environmental water samples: Determination of organic compounds isolated by continuous liquid-liquid extraction or closed-loop stripping: Environmental Science & Technology, v. 26, no. 7, p. 1307-1312, https://doi.org/10.1021/es00031a004.","productDescription":"6 p.","startPage":"1307","endPage":"1312","costCenters":[{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":225212,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":205614,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1021/es00031a004"}],"volume":"26","issue":"7","noUsgsAuthors":false,"publicationDate":"2002-05-01","publicationStatus":"PW","scienceBaseUri":"5059eb68e4b0c8380cd48da8","contributors":{"authors":[{"text":"Foreman, W.T.","contributorId":94684,"corporation":false,"usgs":true,"family":"Foreman","given":"W.T.","email":"","affiliations":[],"preferred":false,"id":375940,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Zaugg, S.D.","contributorId":82811,"corporation":false,"usgs":true,"family":"Zaugg","given":"S.D.","email":"","affiliations":[],"preferred":false,"id":375938,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Falres, L.M.","contributorId":34661,"corporation":false,"usgs":true,"family":"Falres","given":"L.M.","email":"","affiliations":[],"preferred":false,"id":375936,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Werner, M.G.","contributorId":47400,"corporation":false,"usgs":true,"family":"Werner","given":"M.G.","email":"","affiliations":[],"preferred":false,"id":375937,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Leiker, T.J.","contributorId":96719,"corporation":false,"usgs":true,"family":"Leiker","given":"T.J.","email":"","affiliations":[],"preferred":false,"id":375941,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Rogerson, P.F.","contributorId":84087,"corporation":false,"usgs":true,"family":"Rogerson","given":"P.F.","email":"","affiliations":[],"preferred":false,"id":375939,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}}
,{"id":70017025,"text":"70017025 - 1992 - The effect of membrane filtration artifacts on dissolved trace element concentrations","interactions":[],"lastModifiedDate":"2012-03-12T17:18:52","indexId":"70017025","displayToPublicDate":"1992-01-01T00:00:00","publicationYear":"1992","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3716,"text":"Water Research","onlineIssn":"1879-2448","printIssn":"0043-1354","active":true,"publicationSubtype":{"id":10}},"title":"The effect of membrane filtration artifacts on dissolved trace element concentrations","docAbstract":"Among environment scientists, the current and almost universally accepted definition of dissolved constituents is an operational one only those materials which pass through a 0.45-??m membrane filter are considered to be dissolved. Detailed laboratory and field studies on Fe and Al indicate that a number of factors associated with filtration, other than just pore size, can substantially alter 'dissolved' trace element concentrations; these include: filter type, filter diameter, filtration method, volume of sample processed, suspended sediment concentration, suspended sediment grain-size distribution, concentration of colloids and colloidally-associated trace elements and concentration of organic matter. As such, reported filtered-water concentrations employing the same pore size filter may not be equal. Filtration artifacts may lead to the production of chemical data that indicate seasonal or annual 'dissolved' chemical trends which do not reflect actual environmental conditions. Further, the development of worldwide averages for various dissolved chemical constituents, the quantification of geochemical cycles, and the determination of short- or long-term environmental chemical trends may be subject to substantial errors, due to filtration artifacts, when data from the same or multiple sources are combined. Finally, filtration effects could have a substantial impact on various regulatory requirements.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Water Research","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1016/0043-1354(92)90006-P","issn":"00431354","usgsCitation":"Horowitz, A.J., Elrick, K.A., and Colberg, M., 1992, The effect of membrane filtration artifacts on dissolved trace element concentrations: Water Research, v. 26, no. 6, p. 753-763, https://doi.org/10.1016/0043-1354(92)90006-P.","startPage":"753","endPage":"763","numberOfPages":"11","costCenters":[],"links":[{"id":205562,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1016/0043-1354(92)90006-P"},{"id":224863,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"26","issue":"6","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505bab33e4b08c986b322cb7","contributors":{"authors":[{"text":"Horowitz, A. J.","contributorId":102066,"corporation":false,"usgs":true,"family":"Horowitz","given":"A.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":375183,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Elrick, K. A.","contributorId":98731,"corporation":false,"usgs":true,"family":"Elrick","given":"K.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":375182,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Colberg, M.R.","contributorId":88497,"corporation":false,"usgs":true,"family":"Colberg","given":"M.R.","affiliations":[],"preferred":false,"id":375181,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70017161,"text":"70017161 - 1992 - Mass transfer constraints on the chemical evolution of an active hydrothermal system, Valles caldera, New Mexico","interactions":[],"lastModifiedDate":"2012-03-12T17:18:53","indexId":"70017161","displayToPublicDate":"1992-01-01T00:00:00","publicationYear":"1992","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":"Mass transfer constraints on the chemical evolution of an active hydrothermal system, Valles caldera, New Mexico","docAbstract":"Partial equilibrium conditions occur between fluids and secondary minerals in the Valles hydrothermal system, contained principally in the Tertiary rhyolitic Bandelier Tuff. The mass transfer processes are governed by reactive phase compositions, surface areas, water-rock ratios, reaction rates, and fluid residence times. Experimental dissolution of the vitric phase of the tuff was congruent with respect to Cl in the solid and produced reaction rates which obeyed a general Arrhenius release rate between 250 and 300??C. The 18O differences between reacted and unreacted rock and fluids, and mass balances calculations involving Cl in the glass phase, produced comparable water-rock ratios of unity, confirming the importance of irreversible reaction of the vitric tuff. A fluid residence time of approximately 2 ?? 103 years, determined from fluid reservoir volume and discharge rates, is less than 0.2% of the total age of the hydrothermal system and denotes a geochemically and isotopically open system. Mass transfer calculations generally replicated observed reservoir pH, Pco2, and PO2 conditions, cation concentrations, and the secondary mineral assemblage between 250 and 300??C. The only extraneous component required to maintain observed calcite saturation and high Pco2 pressures was carbon presumably derived from underlying Paleozoic limestones. Phase rule constraints indicate that Cl was the only incompatible aqueous component not controlled by mineral equilibrium. Concentrations of Cl in the reservoir directly reflect mass transport rates as evidenced by correlations between anomalously high Cl concentrations in the fluids and tuff in the Valles caldera relative to other hydrothermal systems in rhyolitic rocks. ?? 1992.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Journal of Volcanology and Geothermal Research","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","issn":"03770273","usgsCitation":"White, A.F., Chuma, N., and Goff, F., 1992, Mass transfer constraints on the chemical evolution of an active hydrothermal system, Valles caldera, New Mexico: Journal of Volcanology and Geothermal Research, v. 49, no. 3-4, p. 233-253.","startPage":"233","endPage":"253","numberOfPages":"21","costCenters":[],"links":[{"id":224965,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"49","issue":"3-4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a5259e4b0c8380cd6c347","contributors":{"authors":[{"text":"White, A. F.","contributorId":36546,"corporation":false,"usgs":true,"family":"White","given":"A.","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":375594,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Chuma, N.J.","contributorId":48319,"corporation":false,"usgs":true,"family":"Chuma","given":"N.J.","email":"","affiliations":[],"preferred":false,"id":375595,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Goff, F.","contributorId":53408,"corporation":false,"usgs":true,"family":"Goff","given":"F.","email":"","affiliations":[],"preferred":false,"id":375596,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70017159,"text":"70017159 - 1992 - Garnet/high-silica rhyolite trace element partition coefficients measured by ion microprobe","interactions":[],"lastModifiedDate":"2018-10-25T11:02:20","indexId":"70017159","displayToPublicDate":"1992-01-01T00:00:00","publicationYear":"1992","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":"Garnet/high-silica rhyolite trace element partition coefficients measured by ion microprobe","docAbstract":"<p>Garnet/liquid trace element partition coefficients have been measured in situ by ion microprobe in a rhyolite from Monache Mountain, California. Partition coefficients are reported for La, Ce, Nd, Sm, Dy, Er, Yb, Sc, Ti, V, Cr, Sr, Y, and Zr. The in situ analyses avoid the problem of contamination of the garnet phase by trace element-rich accessory minerals encountered in traditional bulk phenocryst/matrix partitioning studies. The partitioning pattern for the rare earth elements (REEs, excluding Eu) is smooth and rises steeply from the light to the heavy REEs with no sharp kinks or changes in slope, unlike patterns for garnet /silicic liquid REE partitioning determined by bulk methods. This difference suggests that the previous determinations by bulk methods are in error, having suffered from contamination of the phenocryst separates.</p>","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Geochimica et Cosmochimica Acta","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1016/0016-7037(92)90336-H","issn":"00167037","usgsCitation":"Sisson, T.W., and Bacon, C.R., 1992, Garnet/high-silica rhyolite trace element partition coefficients measured by ion microprobe: Geochimica et Cosmochimica Acta, v. 56, no. 5, p. 2133-2136, https://doi.org/10.1016/0016-7037(92)90336-H.","productDescription":"4 p.","startPage":"2133","endPage":"2136","numberOfPages":"4","costCenters":[{"id":617,"text":"Volcano Science Center","active":true,"usgs":true}],"links":[{"id":224963,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"56","issue":"5","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a14bbe4b0c8380cd54b38","contributors":{"authors":[{"text":"Sisson, Thomas W. 0000-0003-3380-6425 tsisson@usgs.gov","orcid":"https://orcid.org/0000-0003-3380-6425","contributorId":2341,"corporation":false,"usgs":true,"family":"Sisson","given":"Thomas","email":"tsisson@usgs.gov","middleInitial":"W.","affiliations":[{"id":617,"text":"Volcano Science Center","active":true,"usgs":true}],"preferred":true,"id":375589,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bacon, Charles R. 0000-0002-2165-5618 cbacon@usgs.gov","orcid":"https://orcid.org/0000-0002-2165-5618","contributorId":2909,"corporation":false,"usgs":true,"family":"Bacon","given":"Charles","email":"cbacon@usgs.gov","middleInitial":"R.","affiliations":[{"id":617,"text":"Volcano Science Center","active":true,"usgs":true}],"preferred":true,"id":375588,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70017009,"text":"70017009 - 1992 - Recorded seismic response of Pacific Park Plaza. II. System identification","interactions":[],"lastModifiedDate":"2013-03-15T20:13:32","indexId":"70017009","displayToPublicDate":"1992-01-01T00:00:00","publicationYear":"1992","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2467,"text":"Journal of Structural Engineering","active":true,"publicationSubtype":{"id":10}},"title":"Recorded seismic response of Pacific Park Plaza. II. System identification","docAbstract":"This is the second of two companion papers on the recorded seismic response of the Pacific Park Plaza building, in Emeryville, Calif., during the October 17, 1989, Ms = 7.1 (surface-wave magnitude) Loma Prieta earthquake. In this second part, the recorded data are analyzed in more detail by using system-identification techniques. The three-dimensional behavior and the coupled modes of the building are determined, and the effects of soil-structure interaction are investigated. The study shows that the response of the building is nonlinear at the beginning, and becomes linear after 17 sec into the earthquake. The dominant motion of the building follows an elliptical path oriented in the southeast-northwest direction. Some of the modes are complex, with nonproportional damping, and there are phase differences among modal response components. The fundamental mode of the building is a translation in the southeast-northwest direction at 0.4 Hz, with 13% damping. The wing displacements relative to the center core are large, about 50% of the center core displacements, and indicate significant torsion in the center core. The soil-structure interaction is characterized by a vibration at 0.7 Hz. This is believed to be the fundamental frequency of the surrounding soil medium. The rocking motions of the building are negligible.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Journal of Structural Engineering","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"ASCE","doi":"10.1061/(ASCE)0733-9445(1992)118:6(1566)","issn":"07339445","usgsCitation":"Safak, F., and Çelebi, M., 1992, Recorded seismic response of Pacific Park Plaza. II. System identification: Journal of Structural Engineering, v. 118, no. 6, p. 1566-1589, https://doi.org/10.1061/(ASCE)0733-9445(1992)118:6(1566).","startPage":"1566","endPage":"1589","numberOfPages":"24","costCenters":[],"links":[{"id":224625,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":269411,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1061/(ASCE)0733-9445(1992)118:6(1566)"}],"volume":"118","issue":"6","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"50e4a285e4b0e8fec6cdb631","contributors":{"authors":[{"text":"Safak, F.","contributorId":89286,"corporation":false,"usgs":true,"family":"Safak","given":"F.","email":"","affiliations":[],"preferred":false,"id":375135,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Çelebi, M.","contributorId":36946,"corporation":false,"usgs":true,"family":"Çelebi","given":"M.","affiliations":[],"preferred":false,"id":375134,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70017158,"text":"70017158 - 1992 - Redistribution of soil nitrogen, carbon and organic matter by mechanical disturbance during whole-tree harvesting in northern hardwoods","interactions":[],"lastModifiedDate":"2019-09-19T10:23:57","indexId":"70017158","displayToPublicDate":"1992-01-01T00:00:00","publicationYear":"1992","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1687,"text":"Forest Ecology and Management","active":true,"publicationSubtype":{"id":10}},"title":"Redistribution of soil nitrogen, carbon and organic matter by mechanical disturbance during whole-tree harvesting in northern hardwoods","docAbstract":"<p><span>To investigate whether mechanical mixing during harvesting could account for losses observed from forest floor, we measured surface disturbance on a 22 ha watershed that was whole-tree harvested. Surface soil on each 10 cm interval along 81, randomly placed transects was classified immediately after harvesting as mineral or organic, and as undisturbed, depressed, rutted, mounded, scarified, or scalped (forest floor scraped away). We quantitatively sampled these surface categories to collect soil in which preharvest forest floor might reside after harvest. Mechanically mixed mineral and organic soil horizons were readily identified. Buried forest floor under mixed mineral soil occurred in 57% of mounds with mineral surface soil. Harvesting disturbed 65% of the watershed surface and removed forest floor from 25% of the area. Mechanically mixed soil under ruts with organic or mineral surface soil, and mounds with mineral surface soil contained organic carbon and nitrogen pools significantly greater than undisturbed forest floor. Mechanical mixing into underlying mineral soil could account for the loss of forest floor observed between the preharvest condition and the second growing season after whole-tree harvesting.</span></p>","language":"English","doi":"10.1016/0378-1127(92)90162-3","issn":"03781127","usgsCitation":"Ryan, D., Huntington, T.G., and Wayne, M.C., 1992, Redistribution of soil nitrogen, carbon and organic matter by mechanical disturbance during whole-tree harvesting in northern hardwoods: Forest Ecology and Management, v. 49, no. 1-2, p. 87-99, https://doi.org/10.1016/0378-1127(92)90162-3.","productDescription":"13 p.","startPage":"87","endPage":"99","numberOfPages":"13","costCenters":[{"id":466,"text":"New England Water Science Center","active":true,"usgs":true}],"links":[{"id":488052,"rank":1,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1016/0378-1127(92)90162-3","text":"Publisher Index Page"},{"id":224920,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"New Hampshire","otherGeospatial":" Hubbard Brook Experimental Forest","volume":"49","issue":"1-2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"50e4a3bae4b0e8fec6cdb948","contributors":{"authors":[{"text":"Ryan, D.F.","contributorId":43626,"corporation":false,"usgs":true,"family":"Ryan","given":"D.F.","email":"","affiliations":[],"preferred":false,"id":375585,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Huntington, Thomas G. 0000-0002-9427-3530 thunting@usgs.gov","orcid":"https://orcid.org/0000-0002-9427-3530","contributorId":117440,"corporation":false,"usgs":true,"family":"Huntington","given":"Thomas","email":"thunting@usgs.gov","middleInitial":"G.","affiliations":[{"id":466,"text":"New England Water Science Center","active":true,"usgs":true}],"preferred":true,"id":375586,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Wayne, Martin C.","contributorId":84634,"corporation":false,"usgs":true,"family":"Wayne","given":"Martin","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":375587,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70017095,"text":"70017095 - 1992 - Paleoecology of late-glacial peats from the bering land bridge, Chukchi Sea shelf region, northwestern Alaska","interactions":[],"lastModifiedDate":"2013-01-25T13:54:44","indexId":"70017095","displayToPublicDate":"1992-01-01T00:00:00","publicationYear":"1992","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3218,"text":"Quaternary Research","active":true,"publicationSubtype":{"id":10}},"title":"Paleoecology of late-glacial peats from the bering land bridge, Chukchi Sea shelf region, northwestern Alaska","docAbstract":"Insect fossils and pollen from late Pleistocene nonmarine peat layers were recovered from cores from the shelf region of the Chukchi Sea at depths of about 50 m below sea level. The peats date to 11,300-11,000 yr B.P. and provide a limiting age for the regional Pleistocene-Holocene marine transgression. The insect fossils are indicative of arctic coastal habitats like those of the Mackenzie Delta region (mean July temperatures = 10.6-14??C) suggesting that 11,000 yr ago the exposed Chukchi Sea shelf had a climate substantially warmer than modern coastal regions of the Alaskan north slope. The pollen spectra are consistent with the age assignment to the Birch Interval (14,000-9000 yr B.P.). The data suggest a meadow-like graminoid tundra with birch shrubs and some willow shrubs growing in sheltered areas. ?? 1992.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Quaternary Research","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"Elsevier","publisherLocation":"Amsterdam, Netherlands","doi":"10.1016/0033-5894(92)90045-K","issn":"00335894","usgsCitation":"Elias, S.A., Short, S.K., and Phillips, R., 1992, Paleoecology of late-glacial peats from the bering land bridge, Chukchi Sea shelf region, northwestern Alaska: Quaternary Research, v. 38, no. 3, p. 371-378, https://doi.org/10.1016/0033-5894(92)90045-K.","startPage":"371","endPage":"378","numberOfPages":"8","costCenters":[],"links":[{"id":224630,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":266479,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1016/0033-5894(92)90045-K"}],"volume":"38","issue":"3","noUsgsAuthors":false,"publicationDate":"2017-01-20","publicationStatus":"PW","scienceBaseUri":"505a73dae4b0c8380cd772af","contributors":{"authors":[{"text":"Elias, S. A.","contributorId":65996,"corporation":false,"usgs":false,"family":"Elias","given":"S.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":375375,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Short, S. K.","contributorId":6596,"corporation":false,"usgs":true,"family":"Short","given":"S.","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":375374,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Phillips, R. L.","contributorId":98289,"corporation":false,"usgs":true,"family":"Phillips","given":"R. L.","affiliations":[],"preferred":false,"id":375376,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70017154,"text":"70017154 - 1992 - The influence of pH on biotite dissolution and alteration kinetics at low temperature","interactions":[],"lastModifiedDate":"2024-04-12T16:03:48.576753","indexId":"70017154","displayToPublicDate":"1992-01-01T00:00:00","publicationYear":"1992","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1759,"text":"Geochimica et Cosmochimica Acta","active":true,"publicationSubtype":{"id":10}},"title":"The influence of pH on biotite dissolution and alteration kinetics at low temperature","docAbstract":"<p>Biotite dissolution rates in acidic solutions were determined in fluidized-bed reactors and flowthrough columns. Biotite dissolution rates increased inversely as a linear function of pH in the pH range 3–7, where the rate order<span>&nbsp;</span><i>n</i><span>&nbsp;</span>= −0.34. Biotite dissolved incongruently over this pH range, with preferential release of magnesium and iron from the octahedral layer. Release of tetrahedral silicon was much greater at pH 3 than at higher pH. Iron release was significantly enhanced by low pH conditions.</p><p>Solution compositions from a continuous exposure flow-through column of biotite indicated biotite dissolves incongruently at pH 4, consistent with alteration to a vermiculite-type product. Solution compositions from a second intermittent-flow column exhibited elevated cation release rates upon the initiation of each exposure to solution.</p><p>The presence of strong oxidizing agents, the mineral surface area, and sample preparation methodology also influenced the dissolution or alteration kinetics of biotite.</p>","language":"English","publisher":"Elsevier","doi":"10.1016/0016-7037(92)90290-Y","issn":"00167037","usgsCitation":"Acker, J.G., and Bricker, O., 1992, The influence of pH on biotite dissolution and alteration kinetics at low temperature: Geochimica et Cosmochimica Acta, v. 56, no. 8, p. 3073-3092, https://doi.org/10.1016/0016-7037(92)90290-Y.","productDescription":"20 p.","startPage":"3073","endPage":"3092","numberOfPages":"20","costCenters":[],"links":[{"id":224871,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.er.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"56","issue":"8","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505bad31e4b08c986b323a48","contributors":{"authors":[{"text":"Acker, James G.","contributorId":52334,"corporation":false,"usgs":true,"family":"Acker","given":"James","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":375577,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bricker, O.P.","contributorId":33717,"corporation":false,"usgs":true,"family":"Bricker","given":"O.P.","affiliations":[],"preferred":false,"id":375576,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70017270,"text":"70017270 - 1992 - Geochemical effects of deep-well injection of the Paradox Valley brine into Paleozoic carbonate rocks, Colorado, U.S.A.","interactions":[],"lastModifiedDate":"2023-02-14T13:16:50.666082","indexId":"70017270","displayToPublicDate":"1992-01-01T00:00:00","publicationYear":"1992","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":835,"text":"Applied Geochemistry","active":true,"publicationSubtype":{"id":10}},"title":"Geochemical effects of deep-well injection of the Paradox Valley brine into Paleozoic carbonate rocks, Colorado, U.S.A.","docAbstract":"<div id=\"abstracts\" class=\"Abstracts u-font-gulliver text-s\"><div id=\"ab1\" class=\"abstract author\" lang=\"en\"><div id=\"aep-abstract-sec-id5\"><p>Brine seepage into the Dolores River from ground water in Paradox Valley, Colorado constitutes a major source of salt to the Colorado River. Plants are enderway to remove this source of salt by drawing down the Paradox Valley brine (PVB) and forcibly injecting it into a deep disposal well (4.8 km). Experiments were conducted to determine the effects of deep-well injection of PVB. The results show that PVB is near saturation with anhydrite at 25°C, and that heating results in anhydrite precipitation. The amount and the rate at which anhydrite forms is temperature, pressure, and substrate dependent. Paradox Valley brine heated in the presence of Precambrian rocks from the drill core produces the same amount of anhydrite as PVB heated alone, but at a greatly accelerated rate. A 30% dilution of PVB with Dolores River water completely eliminates anhydrite precipitation when the fluid is heated with the Precambrian rocks. Interaction of PVB and Leadville Limestone is characterized by dolomitization of calcite by brine Mg which releases Ca to solution. This added Ca reacts with SO<sub>4</sub><span>&nbsp;</span>to form increased amounts of anhydrite. A 20% dilution of PVB by Dolores River water has no effect on dolomitization and reduces the amount of anhydrite only slightly. A 65% dilution of PVB by Dolores River water still does not prevent dolomitization but does suppress anhydrite formation. Computer modeling of PVB by programs utilizing the Pitzer ion-interaction parameters is in general agreement with the experimental results. Ion-activity products calculated by both SOLMINEQ and PHRQPITZ are close to equilibrium with both anhydrite and dolomite whenever these phases are present experimentally, although the calculations over-estimate by a factor of 2 the degree of saturation. Some discrepancies in the calculated results between the two programs are due largely to differences in mineral solubility data.</p></div></div></div>","language":"English","publisher":"Elsevier","doi":"10.1016/0883-2927(92)90043-3","issn":"08832927","usgsCitation":"Rosenbauer, R., Bischoff, J.L., and Kharaka, Y., 1992, Geochemical effects of deep-well injection of the Paradox Valley brine into Paleozoic carbonate rocks, Colorado, U.S.A.: Applied Geochemistry, v. 7, no. 3, p. 273-286, https://doi.org/10.1016/0883-2927(92)90043-3.","productDescription":"14 p.","startPage":"273","endPage":"286","numberOfPages":"14","costCenters":[{"id":34983,"text":"Contaminant Biology Program","active":true,"usgs":true}],"links":[{"id":224493,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Colorado","county":"Montrose County","otherGeospatial":"Paradox Valley","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -109.9072265625,\n              37.50972584293751\n            ],\n            [\n              -106.973876953125,\n              37.50972584293751\n            ],\n            [\n              -106.973876953125,\n              39.13006024213511\n            ],\n            [\n              -109.9072265625,\n              39.13006024213511\n            ],\n            [\n              -109.9072265625,\n              37.50972584293751\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"7","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a1624e4b0c8380cd5506c","contributors":{"authors":[{"text":"Rosenbauer, R.J.","contributorId":37320,"corporation":false,"usgs":true,"family":"Rosenbauer","given":"R.J.","email":"","affiliations":[],"preferred":false,"id":375950,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bischoff, J. L.","contributorId":28969,"corporation":false,"usgs":true,"family":"Bischoff","given":"J.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":375949,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Kharaka, Y.K.","contributorId":23568,"corporation":false,"usgs":true,"family":"Kharaka","given":"Y.K.","email":"","affiliations":[],"preferred":false,"id":375948,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70017214,"text":"70017214 - 1992 - Synthetic organic agrochemicals in the lower Mississippi River and its major tributaries: Distribution, transport and fate","interactions":[],"lastModifiedDate":"2012-03-12T17:18:53","indexId":"70017214","displayToPublicDate":"1992-01-01T00:00:00","publicationYear":"1992","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"Synthetic organic agrochemicals in the lower Mississippi River and its major tributaries: Distribution, transport and fate","docAbstract":"The Mississippi River and its major tributaries transport herbicides and their degradation products from agricultural areas in the mid-western U.S.A. These compounds include atrazine and its degradation products (desethyl- and desisopropylatrazine), simazine, cyanazine, metolachlor, and alachlor and its degradation products (2-chloro-2',6'-diethylacetanilide, 2-hydroxy-2',6'-diethylacetanilide and 2,6-diethylaniline). These compounds were identified and confirmed by gas chromatography-ion trap mass spectrometry. Loads of these compounds were determined during five sampling trips in 1987-1989. Stream loads of these compounds indicated that atrazine and metolachlor were relatively conservative in downstream transport. Alachlor and its degradation products were generated from point and non-point sources. Seasonal variations and hydrologic conditions controlled the loads of these compounds in the Mississippi River. Cross-channel mixing was slow downstream from major river confluences, possibly requiring several hundred kilometers of downriver transit for completion. The annual transport of these compounds into the Gulf of Mexico was estimated to be < 2% of the annual application of each herbicide in the Midwest.The Mississippi River and its major tributaries transport herbicides and their degradation products from agricultural areas in the mid-western U.S.A. These compounds include atrazine and its degradation products (desethyl- and desisopropylatrazine), simazine, cyanazine, metolachlor, and alachlor and its degradation products (2-chloro-2???,6???-diethylacetanilide, 2-hydroxy-2???,6???-diethylacetanilide and 2,6-diethylaniline). These compounds were identified and confirmed by gas chromatography-ion trap mass spectrometry. Loads of these compounds were determined during five sampling trips in 1987-1989. Stream loads of these compounds indicated that atrazine and metolachlor were relatively conservative in downstream transport. Alachlor and its degradation products were generated from point and non-point sources. Seasonal variations and hydrologic conditions controlled the loads of these compounds in the Mississippi River. Cross-channel mixing was slow downstream from major river confluences, possibly requiring several hundred kilometers of downriver transit for completion. The annual transport of these compounds into the Gulf of Mexico was estimated to be <2% of the annual application of each herbicide in the Midwest.","largerWorkTitle":"Journal of Contaminant Hydrology","conferenceTitle":"Pacifichem '89","conferenceDate":"17 December 1989 through 22 December 1989","conferenceLocation":"Honolulu, HI, USA","language":"English","issn":"01697722","usgsCitation":"Pereira, W.E., Rostad, C., and Leiker, T., 1992, Synthetic organic agrochemicals in the lower Mississippi River and its major tributaries: Distribution, transport and fate, <i>in</i> Journal of Contaminant Hydrology, v. 9, no. 1-2, Honolulu, HI, USA, 17 December 1989 through 22 December 1989, p. 175-188.","startPage":"175","endPage":"188","numberOfPages":"14","costCenters":[],"links":[{"id":225058,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"9","issue":"1-2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505ba35fe4b08c986b31fc9e","contributors":{"editors":[{"text":"McCalady Donald L.","contributorId":128410,"corporation":true,"usgs":false,"organization":"McCalady Donald L.","id":536360,"contributorType":{"id":2,"text":"Editors"},"rank":1}],"authors":[{"text":"Pereira, W. E.","contributorId":46981,"corporation":false,"usgs":true,"family":"Pereira","given":"W.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":375763,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Rostad, C.E.","contributorId":50939,"corporation":false,"usgs":true,"family":"Rostad","given":"C.E.","email":"","affiliations":[],"preferred":false,"id":375764,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Leiker, T.J.","contributorId":96719,"corporation":false,"usgs":true,"family":"Leiker","given":"T.J.","email":"","affiliations":[],"preferred":false,"id":375765,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70017271,"text":"70017271 - 1992 - Surface chemistry associated with the cooling and subaerial weathering of recent basalt flows","interactions":[],"lastModifiedDate":"2024-04-12T16:10:09.975718","indexId":"70017271","displayToPublicDate":"1992-01-01T00:00:00","publicationYear":"1992","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":"Surface chemistry associated with the cooling and subaerial weathering of recent basalt flows","docAbstract":"<p>The surface chemistry of fresh and weathered historical basalt flows was characterized using surface-sensitive X-ray photoelectron spectroscopy (XPS). Surfaces of unweathered 1987–1990 flows from the Kilauea Volcano, Hawaii, exhibited variable enrichment in Al, Mg, Ca, and F due to the formation of refractory fluoride compounds and pronounced depletion in Si and Fe from the volatilization of SiF<sub>4</sub><span>&nbsp;</span>and FeF<sub>3</sub><span>&nbsp;</span>during cooling. These reactions, as predicted from shifts in thermodynamic equilibrium with temperature, are induced by diffusion of HF from the flow interiors to the cooling surface. The lack of Si loss and solid fluoride formation for recent basalts from the Krafla Volcano, Iceland, suggest HF degassing at higher temperatures.</p><p>Subsequent short-term subaerial weathering reactions are strongly influenced by the initial surface composition of the flow and therefore its cooling history. Successive samples collected from the 1987 Kilauea flow demonstrated that the fluoridated flow surfaces leached to a predominantly SiO<sub>2</sub><span>&nbsp;</span>composition by natural weathering within one year. These chemically depleted surfaces were also observed on Hawaiian basalt flows dating back to 1801 AD. Solubility and kinetic models, based on thermodynamic and kinetic data for crystalline AlF<sub>3</sub>, MgF<sub>2</sub>, and CaF<sub>2</sub>, support observed elemental depletion rates due to chemical weathering. Additional loss of alkalis from the Hawaiian basalt occurs from incongruent dissolution of the basalt glass substrate during weathering.</p>","language":"English","publisher":"Elsevier","doi":"10.1016/0016-7037(92)90164-E","issn":"00167037","usgsCitation":"White, A.F., and Hochella, M., 1992, Surface chemistry associated with the cooling and subaerial weathering of recent basalt flows: Geochimica et Cosmochimica Acta, v. 56, no. 10, p. 3711-3721, https://doi.org/10.1016/0016-7037(92)90164-E.","productDescription":"11 p.","startPage":"3711","endPage":"3721","numberOfPages":"11","costCenters":[],"links":[{"id":224538,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"56","issue":"10","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505b9f97e4b08c986b31e6c6","contributors":{"authors":[{"text":"White, A. F.","contributorId":36546,"corporation":false,"usgs":true,"family":"White","given":"A.","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":375952,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hochella, M.F. Jr.","contributorId":30765,"corporation":false,"usgs":true,"family":"Hochella","given":"M.F.","suffix":"Jr.","affiliations":[],"preferred":false,"id":375951,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70017213,"text":"70017213 - 1992 - Associations of free-living bacteria and dissolved organic compounds in a plume of contaminated groundwater","interactions":[],"lastModifiedDate":"2012-03-12T17:18:53","indexId":"70017213","displayToPublicDate":"1992-01-01T00:00:00","publicationYear":"1992","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"Associations of free-living bacteria and dissolved organic compounds in a plume of contaminated groundwater","docAbstract":"Associations of free-living bacteria (FLB) and dissolved organic contaminants in a 4-km-long plume of sewage-contaminated groundwater were investigated. Abundance of FLB in the core of the plume (as delineated by maximum specific conductance) steadily decreased in the direction of flow from a point 0.25 km downgradient from the source to the toe of the plume. At 0.25 km downgradient, FLB comprised up to 31% of the total bacterial population, but constituted < 7% of the population at 2 km downgradient. Abundance of FLB correlated strongly (r = 0.80 n = 23) with total dissolved organic carbon (DOC) in contaminated groundwater between 0.64 and 2.1 km downgradient, although distributions of individual contaminants such as di-, tri- and tetrachloroethene were highly variable, and their association with FLB less clear. Numbers of FLB in the downgradient portion of the plume which is contaminated with branched-chain alkylbenzenesulfonate (ABS) surfactants were low (< 5??108/L) in spite of relatively high levels of DOC (up to 4 mg/L). However, abundance of FLB correlated strongly with non-surfactant DOC along vertical transects through the plume. The ratio of FLB to DOC and the ratio of FLB to attached bacteria generally decreased in the direction of flow and, consequently, with the age of the organic contaminants.","largerWorkTitle":"Journal of Contaminant Hydrology","conferenceTitle":"Pacifichem '89","conferenceDate":"17 December 1989 through 22 December 1989","conferenceLocation":"Honolulu, HI, USA","language":"English","issn":"01697722","usgsCitation":"Harvey, R., and Barber, L., 1992, Associations of free-living bacteria and dissolved organic compounds in a plume of contaminated groundwater, <i>in</i> Journal of Contaminant Hydrology, v. 9, no. 1-2, Honolulu, HI, USA, 17 December 1989 through 22 December 1989, p. 91-103.","startPage":"91","endPage":"103","numberOfPages":"13","costCenters":[],"links":[{"id":225057,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"9","issue":"1-2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059ee95e4b0c8380cd49e41","contributors":{"editors":[{"text":"McCalady Donald L.","contributorId":128410,"corporation":true,"usgs":false,"organization":"McCalady Donald L.","id":536359,"contributorType":{"id":2,"text":"Editors"},"rank":1}],"authors":[{"text":"Harvey, R.W. 0000-0002-2791-8503","orcid":"https://orcid.org/0000-0002-2791-8503","contributorId":11757,"corporation":false,"usgs":true,"family":"Harvey","given":"R.W.","affiliations":[],"preferred":false,"id":375762,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Barber, L.B. II","contributorId":6097,"corporation":false,"usgs":true,"family":"Barber","given":"L.B.","suffix":"II","affiliations":[],"preferred":false,"id":375761,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70017268,"text":"70017268 - 1992 - Mineralogy and geothermometry of high-temperature rhyolites from the central and western Snake River Plain","interactions":[],"lastModifiedDate":"2012-03-12T17:18:49","indexId":"70017268","displayToPublicDate":"1992-01-01T00:00:00","publicationYear":"1992","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1109,"text":"Bulletin of Volcanology","active":true,"publicationSubtype":{"id":10}},"title":"Mineralogy and geothermometry of high-temperature rhyolites from the central and western Snake River Plain","docAbstract":"Voluminous mid-Miocene rhyolitic ash-flow tuffs and lava flows are exposed along the northern and southern margins of the central and western Snake River Plain. These rhyolites are essentially anhydrous with the general mineral assemblage of plagioclase ??sanidine ?? quartz + augite + pigeonite ?? hypersthene ?? fayalitic olivine + Fe-Ti oxides + apatite + zircon which provides an opportunity to compare feldspar, pyroxene, and Fe-Ti oxide equilibration temperatures for the same rocks. Estimated pyroxene equilibration temperatures (based on the geothermometers of Lindsley and coworkers) range from 850 to 1000??C, and these are well correlated with whole-rock compositions. With the exception of one sample, agreement between the two-pyroxene thermometers tested is well within 50??C. Fe-Ti oxide geothermometers applied to fresh magnetite and ilmenite generally yield temperatures about 50 to 100??C lower than the pyroxene temperatures, and erratic results are obtained if these minerals exhibit effects of subsolidus oxidation and exsolution. Results of feldspar thermometry are more complicated, and reflect uncertainties in the thermometer calibrations as well as in the degree of attainment of equilibrium between plagioclase and sanidine. In general, temperatures obtained using the Ghiorso (1984) and Green and Usdansky (1986) feldspar thermometers agree with the pyroxene temperatures within the respective uncertainties. However, uncertainties in the feldspar temperatures are the larger of the two (and exceed ??60??C for many samples). The feldspar thermometer of Fuhrman and Lindsley (1988) produces systematically lower temperatures for many of the samples studied. The estimated pyroxene temperatures are considered most representative of actual magmatic temperatures for these rhyolites. This range of temperatures is significantly higher than those for rhyolites from many other suites, and is consistent with the hypothesis that the Snake River Plain rhyolitic magmas formed by partial fusion of relatively dry (e.g. granulitic) crustal lithologies. ?? 1992 Springer-Verlag.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Bulletin of Volcanology","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisherLocation":"Springer-Verlag","doi":"10.1007/BF00278390","issn":"02588900","usgsCitation":"Honjo, N., Bonnichsen, B., Leeman, W., and Stormer, J., 1992, Mineralogy and geothermometry of high-temperature rhyolites from the central and western Snake River Plain: Bulletin of Volcanology, v. 54, no. 3, p. 220-237, https://doi.org/10.1007/BF00278390.","startPage":"220","endPage":"237","numberOfPages":"18","costCenters":[],"links":[{"id":205491,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1007/BF00278390"},{"id":224491,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"54","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a5abee4b0c8380cd6f0cd","contributors":{"authors":[{"text":"Honjo, N.","contributorId":30764,"corporation":false,"usgs":true,"family":"Honjo","given":"N.","email":"","affiliations":[],"preferred":false,"id":375945,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bonnichsen, B.","contributorId":19300,"corporation":false,"usgs":true,"family":"Bonnichsen","given":"B.","affiliations":[],"preferred":false,"id":375943,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Leeman, W.P.","contributorId":7841,"corporation":false,"usgs":true,"family":"Leeman","given":"W.P.","affiliations":[],"preferred":false,"id":375942,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Stormer, J.C. Jr.","contributorId":25709,"corporation":false,"usgs":true,"family":"Stormer","given":"J.C.","suffix":"Jr.","email":"","affiliations":[],"preferred":false,"id":375944,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
]}