A multiple well aquifer test to determine anisotropic transmissivity was conducted on a coal-bed in the Powder River Basin, southeastern Montana, as part of a multidisciplinary investigation to determine hydrologic conditions of coal-beds in the area. For the test, three wells were drilled equidistant from and at different angles to a production well tapping the Flowers–Goodale coal seam, a 7.6-m thick seam confined at a depth of about 110 m. The test was conducted by air-lift pumping for 9 h, and water levels were monitored in the three observation wells using pressure transducers. Drawdown data collected early in the test were affected by interporosity flow between the coal fracture network and the matrix, but later data were suitable to determine aquifer anisotropy, as the slopes of the late-time semilog time-drawdown curves are nearly identical, and the zero-drawdown intercepts are different. The maximum transmissivity, trending N87°E, is 14.9 m2/d, and the minimum transmissivity 6.8 m2/d, giving an anisotropy ratio of 2.2:1. Combined specific storage of the fractures and matrix is 2×10−5/m, and of the fracture network alone 5×10−6/m. The principal direction of the anisotropy tensor is not aligned with the face cleats, but instead is aligned with another fracture set and with dominant east–west tectonic compression. Results of the test indicate that the Flowers–Goodale coal-bed is more permeable than many coals in the Powder River Basin, but the anisotropy ratio and specific storage are similar to those found for other coal-beds in the basin.
","language":"English","publisher":"Elsevier","doi":"10.1016/j.jhydrol.2004.11.002","issn":"00221694","usgsCitation":"Weeks, E., 2005, Hydrologic properties of coal-beds in the Powder River Basin, Montana: II. Aquifer test analysis: Journal of Hydrology, v. 308, no. 1-4, p. 242-257, https://doi.org/10.1016/j.jhydrol.2004.11.002.","productDescription":"16 p.","startPage":"242","endPage":"257","costCenters":[{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":237516,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":210557,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1016/j.jhydrol.2004.11.002"}],"country":"United States","state":"Montana","otherGeospatial":"Powder River Basin","volume":"308","issue":"1-4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a3667e4b0c8380cd606ad","contributors":{"authors":[{"text":"Weeks, E.P.","contributorId":38514,"corporation":false,"usgs":true,"family":"Weeks","given":"E.P.","email":"","affiliations":[],"preferred":false,"id":422161,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70029303,"text":"70029303 - 2005 - Utility of Penman-Monteith, Priestley-Taylor, reference evapotranspiration, and pan evaporation methods to estimate pasture evapotranspiration","interactions":[],"lastModifiedDate":"2012-03-12T17:20:55","indexId":"70029303","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2342,"text":"Journal of Hydrology","active":true,"publicationSubtype":{"id":10}},"title":"Utility of Penman-Monteith, Priestley-Taylor, reference evapotranspiration, and pan evaporation methods to estimate pasture evapotranspiration","docAbstract":"Actual evapotranspiration (ETa) was measured at 30-min resolution over a 19-month period (September 28, 2000-April 23, 2002) from a nonirrigated pasture site in Florida, USA, using eddy correlation methods. The relative magnitude of measured ETa (about 66% of long-term annual precipitation at the study site) indicates the importance of accurate ET a estimates for water resources planning. The time and cost associated with direct measurements of ETa and the rarity of historical measurements of ETa make the use of methods relying on more easily obtainable data desirable. Several such methods (Penman-Monteith (PM), modified Priestley-Taylor (PT), reference evapotranspiration (ET 0), and pan evaporation (Ep)) were related to measured ETa using regression methods to estimate PM bulk surface conductance, PT ??, ET0 vegetation coefficient, and Ep pan coefficient. The PT method, where the PT ?? is a function of green-leaf area index (LAI) and solar radiation, provided the best relation with ET a (standard error (SE) for daily ETa of 0.11 mm). The PM method, in which the bulk surface conductance was a function of net radiation and vapor-pressure deficit, was slightly less effective (SE=0.15 mm) than the PT method. Vegetation coefficients for the ET0 method (SE=0.29 mm) were found to be a simple function of LAI. Pan coefficients for the Ep method (SE=0.40 mm) were found to be a function of LAI and Ep. Historical or future meteorological, LAI, and pan evaporation data from the study site could be used, along with the relations developed within this study, to provide estimates of ETa in the absence of direct measurements of ETa. Additionally, relations among PM, PT, and ET0 methods and ETa can provide estimates of ETa in other, environmentally similar, pasture settings for which meteorological and LAI data can be obtained or estimated. ?? 2004 Elsevier B.V. All rights reserved.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Journal of Hydrology","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1016/j.jhydrol.2004.10.023","issn":"00221694","usgsCitation":"Sumner, D.M., and Jacobs, J., 2005, Utility of Penman-Monteith, Priestley-Taylor, reference evapotranspiration, and pan evaporation methods to estimate pasture evapotranspiration: Journal of Hydrology, v. 308, no. 1-4, p. 81-104, https://doi.org/10.1016/j.jhydrol.2004.10.023.","startPage":"81","endPage":"104","numberOfPages":"24","costCenters":[],"links":[{"id":210556,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1016/j.jhydrol.2004.10.023"},{"id":237515,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"308","issue":"1-4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505bc0cce4b08c986b32a310","contributors":{"authors":[{"text":"Sumner, D. M.","contributorId":100827,"corporation":false,"usgs":true,"family":"Sumner","given":"D.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":422160,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Jacobs, J.M.","contributorId":10446,"corporation":false,"usgs":true,"family":"Jacobs","given":"J.M.","email":"","affiliations":[],"preferred":false,"id":422159,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70029301,"text":"70029301 - 2005 - Episodic incision of the Colorado River in Glen Canyon, Utah","interactions":[],"lastModifiedDate":"2012-03-12T17:20:55","indexId":"70029301","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1425,"text":"Earth Surface Processes and Landforms","active":true,"publicationSubtype":{"id":10}},"title":"Episodic incision of the Colorado River in Glen Canyon, Utah","docAbstract":"Incision rates of the Colorado River are integral to understanding the development of the Colorado Plateau. Here we calculate episodic incision rates of the Colorado River based on absolute ages of two levels of Quaternary deposits adjacent to Glen Canyon, Utah, along the north flank of Navajo Mountain. Minimum surface ages are determined by a combination of cosmogenic radionuclide surface exposure ages, uranium series and soil-development formation times. Bedrock incision rates of the Colorado River between c. 500 ka and c. 250 ka, and c. 250 ka to present are c. 0??4 m ka-1 and c. 0??7 m ka-1, respectively. These rates are more than double the rates reported in the Grand Canyon, suggesting that the Colorado River above Lees Ferry is out of equilibrium with the lower section of the river. We also determine incision rates of two tributaries to the Colorado River. Oak Creek and Bridge Creek flow off Navajo Mountain into Glen Canyon from the southeast. Oak Creek and Bridge Creek both have incision rates of c. 0??6 m ka-1 over the past c. 100 ka at points about 9 km away from the main stem of the Colorado River. Copyright ?? 2005 John Wiley & Sons, Ltd.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Earth Surface Processes and Landforms","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1002/esp.1257","issn":"01979337","usgsCitation":"Garvin, C.D., Hanks, T.C., Finkel, R., and Heimsath, A., 2005, Episodic incision of the Colorado River in Glen Canyon, Utah: Earth Surface Processes and Landforms, v. 30, no. 8, p. 973-984, https://doi.org/10.1002/esp.1257.","startPage":"973","endPage":"984","numberOfPages":"12","costCenters":[],"links":[{"id":210531,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1002/esp.1257"},{"id":237477,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"30","issue":"8","noUsgsAuthors":false,"publicationDate":"2005-08-30","publicationStatus":"PW","scienceBaseUri":"505a0a11e4b0c8380cd521b0","contributors":{"authors":[{"text":"Garvin, C. D.","contributorId":84390,"corporation":false,"usgs":true,"family":"Garvin","given":"C.","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":422154,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hanks, Thomas C.","contributorId":35763,"corporation":false,"usgs":true,"family":"Hanks","given":"Thomas","middleInitial":"C.","affiliations":[],"preferred":false,"id":422151,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Finkel, R.C.","contributorId":79677,"corporation":false,"usgs":true,"family":"Finkel","given":"R.C.","email":"","affiliations":[],"preferred":false,"id":422153,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Heimsath, A.M.","contributorId":52781,"corporation":false,"usgs":true,"family":"Heimsath","given":"A.M.","affiliations":[],"preferred":false,"id":422152,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":70029300,"text":"70029300 - 2005 - Evidence for subsurface water ice in Korolev crater, Mars","interactions":[],"lastModifiedDate":"2019-02-22T08:32:06","indexId":"70029300","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1963,"text":"Icarus","active":true,"publicationSubtype":{"id":10}},"title":"Evidence for subsurface water ice in Korolev crater, Mars","docAbstract":"Following the work of Kieffer and Titus (2001, Icarus 154, 162–180), we present results of thermal IR observations of Korolev crater, located at
The rate of chick growth in high-latitude breeding shorebirds is rapid, but little is known about the effect of chick mass, growth, and brood movements on subsequent brood survival. To address these topics, we monitored chick growth patterns, daily brood movements, and survival of Western Sandpipers (Calidris mauri) on the Yukon-Kuskokwim Delta, Alaska. We assessed the effect of chick age, mass, and hatch date on brood survival using Program MARK. We mapped brood locations daily, and compared brood movement patterns between successful and unsuccessful broods. Younger chicks survived at lower rates and moved shorter distances than older chicks. The overall probability of one or more chicks from a brood surviving to 15 days of age was 0.73 ± 0.05 SE. Brood survival declined seasonally, and broods with heavier chicks survived at higher rates than those with lighter chicks. On average, successful broods fledged 1.7 ± 0.1 SE chicks. Rate of chick growth was intermediate between those of high arctic and temperate-breeding shorebirds, and chick mass at hatching declined seasonally. Western Sandpiper brood survival was lowest when chicks were young, spatially clumped, and unable to maintain homeothermy, probably because young chicks were more vulnerable to both complete depredation events and extreme weather. Our data suggest that larger, older chicks are able to avoid predators by being spatially dispersed and highly mobile; thermal independence, achieved after approximately day five, enables chicks to better endure prolonged periods of cold and low food availability.
","language":"English","publisher":"Cooper Ornithological Society","doi":"10.1650/0010-5422(2005)107[0597:SOWSBO]2.0.CO;2","usgsCitation":"Ruthrauff, D.R., and McCaffery, B.J., 2005, Survival of Western Sandpiper broods on the Yukon-Kuskokwim Delta, Alaska: Condor, v. 107, no. 3, p. 597-604, https://doi.org/10.1650/0010-5422(2005)107[0597:SOWSBO]2.0.CO;2.","productDescription":"8 p.","startPage":"597","endPage":"604","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":114,"text":"Alaska Science Center","active":true,"usgs":true}],"links":[{"id":477841,"rank":1,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1650/0010-5422(2005)107[0597:sowsbo]2.0.co;2","text":"Publisher Index Page"},{"id":237407,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"107","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505ba2c3e4b08c986b31f942","contributors":{"authors":[{"text":"Ruthrauff, Daniel R. 0000-0003-1355-9156 druthrauff@usgs.gov","orcid":"https://orcid.org/0000-0003-1355-9156","contributorId":4181,"corporation":false,"usgs":true,"family":"Ruthrauff","given":"Daniel","email":"druthrauff@usgs.gov","middleInitial":"R.","affiliations":[{"id":114,"text":"Alaska Science Center","active":true,"usgs":true},{"id":117,"text":"Alaska Science Center Biology WTEB","active":true,"usgs":true}],"preferred":true,"id":422129,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"McCaffery, Brian J.","contributorId":37617,"corporation":false,"usgs":true,"family":"McCaffery","given":"Brian","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":422130,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70029291,"text":"70029291 - 2005 - p,p'-DDE depresses the immune competence of chinook salmon (Oncorhynchus tshawytscha) leukocytes","interactions":[],"lastModifiedDate":"2019-10-04T09:01:01","indexId":"70029291","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1653,"text":"Fish and Shellfish Immunology","active":true,"publicationSubtype":{"id":10}},"displayTitle":"p,p'-DDE depresses the immune competence of chinook salmon (Oncorhynchus tshawytscha) leukocytes","title":"p,p'-DDE depresses the immune competence of chinook salmon (Oncorhynchus tshawytscha) leukocytes","docAbstract":"p,p′-DDE, the main metabolite of DDT, is still detected in aquatic environments throughout the world. Here, the effects and mechanisms by which p,p′-DDE exposure might affect the immune system of chinook salmon (Oncorhynchus tshawytscha) was studied. Isolated salmon splenic and pronephric leukocytes were incubated with different concentrations of p,p′-DDE, and cell viability, induction of apoptosis, and mitogenic responses were measured by flow cytometry and Alamar Blue assay. p,p′-DDE significantly reduced cell viability and proliferation and increased apoptosis. The effect of p,p′-DDE on pronephric leukocytes was more severe than on splenic leukocytes, likely because pronephric leukocytes had a higher proportion of granulocytes, cells that appear more sensitive to p,p′-DDE. The effect of p,p′-DDE on leukocytes appeared to vary between developmental stages or seasonal differences. The mitogenic response of leukocytes of chinook salmon exposed to p,p′-DDE in vivo exhibited a biphasic dose–response relationship. Only leukocytes isolated from salmon treated with 59 ppm p,p′-DDE had a significantly lower percentage of Ig+ blasting cells than controls, although the response was biphasic. These results support the theory that exposure to chemical contaminants could lead to an increase in disease susceptibility and mortality of fish due to immune suppression.
","language":"English","publisher":"Elsevier","doi":"10.1016/j.fsi.2004.11.005","issn":"10504648","usgsCitation":"Misumi, I., Vella, A.T., Leong, J.C., Nakanishi, T., and Schreck, C.B., 2005, p,p'-DDE depresses the immune competence of chinook salmon (Oncorhynchus tshawytscha) leukocytes: Fish and Shellfish Immunology, v. 19, no. 2, p. 97-114, https://doi.org/10.1016/j.fsi.2004.11.005.","productDescription":"18 p.","startPage":"97","endPage":"114","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":200,"text":"Coop Res Unit Seattle","active":true,"usgs":true},{"id":289,"text":"Forest and Rangeland Ecosys Science Center","active":true,"usgs":true}],"links":[{"id":210863,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1016/j.fsi.2004.11.005"},{"id":237912,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"19","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505bd34ce4b08c986b32fcc6","contributors":{"authors":[{"text":"Misumi, Ichiro","contributorId":103073,"corporation":false,"usgs":true,"family":"Misumi","given":"Ichiro","email":"","affiliations":[],"preferred":false,"id":422101,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Vella, Anthony T.","contributorId":40413,"corporation":false,"usgs":true,"family":"Vella","given":"Anthony","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":422099,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Leong, Jo-Ann C.","contributorId":96135,"corporation":false,"usgs":true,"family":"Leong","given":"Jo-Ann","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":422100,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Nakanishi, Teruyuki","contributorId":18964,"corporation":false,"usgs":true,"family":"Nakanishi","given":"Teruyuki","email":"","affiliations":[],"preferred":false,"id":422098,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Schreck, Carl B. 0000-0001-8347-1139 carl.schreck@usgs.gov","orcid":"https://orcid.org/0000-0001-8347-1139","contributorId":878,"corporation":false,"usgs":true,"family":"Schreck","given":"Carl","email":"carl.schreck@usgs.gov","middleInitial":"B.","affiliations":[{"id":289,"text":"Forest and Rangeland Ecosys Science Center","active":true,"usgs":true},{"id":200,"text":"Coop Res Unit Seattle","active":true,"usgs":true}],"preferred":true,"id":422097,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}} ,{"id":70029288,"text":"70029288 - 2005 - The composition of coexisting jarosite-group minerals and water from the Richmond mine, Iron Mountain, California","interactions":[],"lastModifiedDate":"2018-10-31T09:22:55","indexId":"70029288","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1177,"text":"Canadian Mineralogist","active":true,"publicationSubtype":{"id":10}},"title":"The composition of coexisting jarosite-group minerals and water from the Richmond mine, Iron Mountain, California","docAbstract":"Jarosite-group minerals accumulate in the form of stalactites and fine-grained mud on massive pyrite in the D drift of the Richmond mine, Iron Mountain, California. Water samples were collected by placing beakers under the dripping stalactites and by extracting pore water from the mud using a centrifuge. The water is rich in Fe3+ and SO4 2−, with a pH of approximately 2.1, which is significantly higher than the extremely acidic waters found elsewhere in the mine. Electron-microprobe analysis and X-ray mapping indicate that the small crystals (<10 μm in diameter) are compositionally zoned with respect to Na and K, and include hydronium jarosite corresponding to the formula (H3O)0.6K0.3Na0.1Fe3 3+(SO4)2(OH)6. The proton-microprobe analyses indicate that the jarosite-group minerals contain significant amounts of As, Pb and Zn, and minor levels of Bi, Rb, Sb, Se, Sn and Sr. Speciation modeling indicates that the drip waters are supersaturated with respect to jarosite-group minerals. The expected range in composition of jarosite-group solid-solution in equilibrium with the pore water extracted from the mud was found to be consistent with the observed range in composition.
","language":"English","publisher":"Mineralogical Associaion of Canada","doi":"10.2113/gscanmin.43.4.1225","usgsCitation":"Jamieson, H.E., Robinson, C., Alpers, C.N., Nordstrom, D.K., Poustovetov, A., and Lowers, H., 2005, The composition of coexisting jarosite-group minerals and water from the Richmond mine, Iron Mountain, California: Canadian Mineralogist, v. 43, no. 4, p. 1225-1242, https://doi.org/10.2113/gscanmin.43.4.1225.","productDescription":"18 p.","startPage":"1225","endPage":"1242","costCenters":[{"id":154,"text":"California Water Science Center","active":true,"usgs":true},{"id":171,"text":"Central Mineral and Environmental Resources Science Center","active":true,"usgs":true},{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true},{"id":5044,"text":"National Research Program - Central Branch","active":true,"usgs":true}],"links":[{"id":237874,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"California","otherGeospatial":"Iron Mountain","volume":"43","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505baa4be4b08c986b3227b6","contributors":{"authors":[{"text":"Jamieson, Heather E.","contributorId":150176,"corporation":false,"usgs":false,"family":"Jamieson","given":"Heather","email":"","middleInitial":"E.","affiliations":[{"id":7029,"text":"Queen's University, Kingston, Ontario, Canada","active":true,"usgs":false}],"preferred":false,"id":422084,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Robinson, Clare","contributorId":195273,"corporation":false,"usgs":false,"family":"Robinson","given":"Clare","email":"","affiliations":[],"preferred":false,"id":422086,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Alpers, Charles N. 0000-0001-6945-7365 cnalpers@usgs.gov","orcid":"https://orcid.org/0000-0001-6945-7365","contributorId":411,"corporation":false,"usgs":true,"family":"Alpers","given":"Charles","email":"cnalpers@usgs.gov","middleInitial":"N.","affiliations":[{"id":154,"text":"California Water Science Center","active":true,"usgs":true}],"preferred":true,"id":422088,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Nordstrom, D. Kirk 0000-0003-3283-5136 dkn@usgs.gov","orcid":"https://orcid.org/0000-0003-3283-5136","contributorId":749,"corporation":false,"usgs":true,"family":"Nordstrom","given":"D.","email":"dkn@usgs.gov","middleInitial":"Kirk","affiliations":[{"id":5044,"text":"National Research Program - Central Branch","active":true,"usgs":true},{"id":37277,"text":"WMA - Earth System Processes Division","active":true,"usgs":true}],"preferred":false,"id":422087,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Poustovetov, Alexei","contributorId":68516,"corporation":false,"usgs":false,"family":"Poustovetov","given":"Alexei","email":"","affiliations":[],"preferred":false,"id":422085,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Lowers, Heather A. hlowers@usgs.gov","contributorId":149265,"corporation":false,"usgs":true,"family":"Lowers","given":"Heather A.","email":"hlowers@usgs.gov","affiliations":[{"id":171,"text":"Central Mineral and Environmental Resources Science Center","active":true,"usgs":true}],"preferred":false,"id":422083,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}} ,{"id":70029284,"text":"70029284 - 2005 - El Niño and displays of spring-flowering annuals in the Mojave and Sonoran deserts","interactions":[],"lastModifiedDate":"2015-05-04T13:18:54","indexId":"70029284","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2571,"text":"Journal of the Torrey Botanical Society","active":true,"publicationSubtype":{"id":10}},"title":"El Niño and displays of spring-flowering annuals in the Mojave and Sonoran deserts","docAbstract":"Although popular and scientific literature frequently assumes a strong connection between El Niño-Southern Oscillation (ENSO) and good displays of spring-flowering annuals in the southwestern United States, such assumptions are based on anecdotal, short-term evidence. The goals of this study were to identify good wildflower years as objectively as possible, to assess the correlation between El Niño and good displays of spring-flowering annuals, and to examine the influence of rainfall amounts on good wildflower years. The terms “good displays” and “good wildflower years” refer to times or places when populations of showy spring-flowering annuals (often called winter annuals) are abundant, robust, and diverse. In the deserts of southeastern California and southern Arizona, good wildflower years occurred about once every 5 to 7 years in the 20th century. The connection between good wildflower years and traditionally defined El Niño episodes was weak, but when El Niño was redefined in a phenologically meaningful way as any calendar year in which the average Southern Oscillation Index (SOI) between July and December was negative, 21 of 27 good wildflower years in the combined deserts were associated with El Niño. Good wildflower years were 3.6 times more likely after redefined El Niño years than after other years. Rain in the months before good wildflower years was at least 30% greater than the long-term average in the Mojave Desert and at least 50% greater in the Sonoran Desert. A diverse flora of spring-flowering annuals occurred in the region during the late Wisconsin and early Holocene, which was a period of wetter, milder winters and cooler summers. Perhaps some species of spring-flowering annuals persist today in the arid southwestern United States only because frequent El Niño conditions recreate the cool, moist conditions of the late Pleistocene.
","language":"English","publisher":"Torrey Botanical Society","doi":"10.3159/1095-5674(2005)132[38:ENADOS]2.0.CO;2","issn":"10955674","usgsCitation":"Bowers, J.E., 2005, El Niño and displays of spring-flowering annuals in the Mojave and Sonoran deserts: Journal of the Torrey Botanical Society, v. 132, no. 1, p. 38-49, https://doi.org/10.3159/1095-5674(2005)132[38:ENADOS]2.0.CO;2.","productDescription":"12 p.","startPage":"38","endPage":"49","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":237802,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"132","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a087de4b0c8380cd51b38","contributors":{"authors":[{"text":"Bowers, Janice E.","contributorId":18119,"corporation":false,"usgs":true,"family":"Bowers","given":"Janice","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":422071,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70029320,"text":"70029320 - 2005 - Clustered streamlined forms in Athabasca Valles, Mars: Evidence for sediment deposition during floodwater ponding","interactions":[],"lastModifiedDate":"2012-03-12T17:20:50","indexId":"70029320","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1801,"text":"Geomorphology","active":true,"publicationSubtype":{"id":10}},"title":"Clustered streamlined forms in Athabasca Valles, Mars: Evidence for sediment deposition during floodwater ponding","docAbstract":"A unique clustering of layered streamlined forms in Athabasca Valles is hypothesized to reflect a significant hydraulic event. The forms, interpreted as sedimentary, are attributed to extensive sediment deposition during ponding and then streamlining of this sediment behind flow obstacles during ponded water outflow. These streamlined forms are analogous to those found in depositional basins and other loci of ponding in terrestrial catastrophic flood landscapes. These terrestrial streamlined forms can provide the best opportunity for reconstructing the history of the terrestrial flooding. Likewise, the streamlined forms in Athabasca Valles may provide the best opportunity to reconstruct the recent geologic history of this young Martian outflow channel. ?? 2005 Elsevier B.V. All rights reserved.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Geomorphology","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1016/j.geomorph.2005.01.009","issn":"0169555X","usgsCitation":"Burr, D., 2005, Clustered streamlined forms in Athabasca Valles, Mars: Evidence for sediment deposition during floodwater ponding: Geomorphology, v. 69, no. 1-4, p. 242-252, https://doi.org/10.1016/j.geomorph.2005.01.009.","startPage":"242","endPage":"252","numberOfPages":"11","costCenters":[],"links":[{"id":210780,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1016/j.geomorph.2005.01.009"},{"id":237805,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"69","issue":"1-4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059f678e4b0c8380cd4c7a9","contributors":{"authors":[{"text":"Burr, D.","contributorId":19367,"corporation":false,"usgs":true,"family":"Burr","given":"D.","email":"","affiliations":[],"preferred":false,"id":422246,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70029322,"text":"70029322 - 2005 - Fundamental challenges to methane recovery from gas hydrates","interactions":[],"lastModifiedDate":"2017-08-31T10:47:17","indexId":"70029322","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3601,"text":"Topics in Catalysis","active":true,"publicationSubtype":{"id":10}},"title":"Fundamental challenges to methane recovery from gas hydrates","docAbstract":"The fundamental challenges, the location, magnitude, and feasibility of recovery, which must be addressed to recover methane from dispersed hydrate sources, are presented. To induce dissociation of gas hydrate prior to methane recovery, two potential methods are typically considered. Because thermal stimulation requires a large energy input, it is less economically feasible than depressurization. The new data will allow the study of the effect of pressure, temperature, diffusion, porosity, tortuosity, composition of gas and water, and porous media on gas-hydrate production. These data also will allow one to improve existing models related to the stability and dissociation of sea floor hydrates. The reproducible kinetic data from the planned runs together with sediment properties will aid in developing a process to economically recover methane from a potential untapped hydrate source. The availability of plentiful methane will allow economical and large-scale production of methane-derived clean fuels to help avert future energy crises.","language":"English","doi":"10.1007/s11244-005-2881-x","issn":"10225528","usgsCitation":"Servio, P., Eaton, M., Mahajan, D., and Winters, W., 2005, Fundamental challenges to methane recovery from gas hydrates: Topics in Catalysis, v. 32, no. 3-4, p. 101-107, https://doi.org/10.1007/s11244-005-2881-x.","productDescription":"7 p.","startPage":"101","endPage":"107","costCenters":[{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"links":[{"id":237841,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"32","issue":"3-4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a1418e4b0c8380cd548e1","contributors":{"authors":[{"text":"Servio, P.","contributorId":28059,"corporation":false,"usgs":true,"family":"Servio","given":"P.","affiliations":[],"preferred":false,"id":422258,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Eaton, M.W.","contributorId":26132,"corporation":false,"usgs":true,"family":"Eaton","given":"M.W.","email":"","affiliations":[],"preferred":false,"id":422257,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Mahajan, D.","contributorId":42019,"corporation":false,"usgs":true,"family":"Mahajan","given":"D.","affiliations":[],"preferred":false,"id":422259,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Winters, W.J.","contributorId":49796,"corporation":false,"usgs":true,"family":"Winters","given":"W.J.","email":"","affiliations":[],"preferred":false,"id":422260,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":70029283,"text":"70029283 - 2005 - Exposing extinction risk analysis to pathogens: Is disease just another form of density dependence?","interactions":[],"lastModifiedDate":"2021-07-06T23:38:43.759691","indexId":"70029283","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1450,"text":"Ecological Applications","active":true,"publicationSubtype":{"id":10}},"title":"Exposing extinction risk analysis to pathogens: Is disease just another form of density dependence?","docAbstract":"In the United States and several other countries, the development of population viability analyses (PVA) is a legal requirement of any species survival plan developed for threatened and endangered species. Despite the importance of pathogens in natural populations, little attention has been given to host-pathogen dynamics in PVA. To study the effect of infectious pathogens on extinction risk estimates generated from PVA, we review and synthesize the relevance of host-pathogen dynamics in analyses of extinction risk. We then develop a stochastic, density-dependent host-parasite model to investigate the effects of disease on the persistence of endangered populations. We show that this model converges on a Ricker model of density dependence under a suite of limiting assumptions, including a high probability that epidemics will arrive and occur. Using this modeling framework, we then quantify: (1) dynamic differences between time series generated by disease and Ricker processes with the same parameters; (2) observed probabilities of quasi-extinction for populations exposed to disease or self-limitation; and (3) bias in probabilities of quasi-extinction estimated by density-independent PVAs when populations experience either form of density dependence. Our results suggest two generalities about the relationships among disease, PVA, and the management of endangered species. First, disease more strongly increases variability in host abundance and, thus, the probability of quasi-extinction, than does self-limitation. This result stems from the fact that the effects and the probability of occurrence of disease are both density dependent. Second, estimates of quasi-extinction are more often overly optimistic for populations experiencing disease than for those subject to self-limitation. Thus, although the results of density-independent PVAs may be relatively robust to some particular assumptions about density dependence, they are less robust when endangered populations are known to be susceptible to disease. If potential management actions involve manipulating pathogens, then it may be useful to model disease explicitly. ?? 2005 by the Ecological Society of America.","language":"English","publisher":"Wiley","doi":"10.1890/04-0880","usgsCitation":"Gerber, L.R., McCallum, H., Lafferty, K.D., Sabo, J.L., and Dobson, A., 2005, Exposing extinction risk analysis to pathogens: Is disease just another form of density dependence?: Ecological Applications, v. 15, no. 4, p. 1402-1414, https://doi.org/10.1890/04-0880.","productDescription":"13 p.","startPage":"1402","endPage":"1414","numberOfPages":"13","costCenters":[{"id":651,"text":"Western Ecological Research Center","active":true,"usgs":true}],"links":[{"id":502634,"rank":1,"type":{"id":41,"text":"Open Access External Repository Page"},"url":"https://figshare.com/articles/journal_contribution/Exposing_extinction_risk_analysis_to_pathogens_Is_disease_just_another_form_of_density_dependence_/22860347","text":"External Repository"},{"id":237767,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"15","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a0e2de4b0c8380cd5332a","contributors":{"authors":[{"text":"Gerber, Leah R.","contributorId":147236,"corporation":false,"usgs":false,"family":"Gerber","given":"Leah","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":422066,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"McCallum, Hamish","contributorId":174852,"corporation":false,"usgs":false,"family":"McCallum","given":"Hamish","affiliations":[],"preferred":false,"id":422068,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Lafferty, Kevin D. 0000-0001-7583-4593 klafferty@usgs.gov","orcid":"https://orcid.org/0000-0001-7583-4593","contributorId":1415,"corporation":false,"usgs":true,"family":"Lafferty","given":"Kevin","email":"klafferty@usgs.gov","middleInitial":"D.","affiliations":[{"id":651,"text":"Western Ecological Research Center","active":true,"usgs":true}],"preferred":true,"id":422067,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Sabo, John L.","contributorId":39929,"corporation":false,"usgs":true,"family":"Sabo","given":"John","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":422069,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Dobson, Andy","contributorId":88076,"corporation":false,"usgs":true,"family":"Dobson","given":"Andy","affiliations":[],"preferred":false,"id":422070,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}} ,{"id":70029282,"text":"70029282 - 2005 - Earthquake and ambient vibration monitoring of the steel-frame UCLA factor building","interactions":[],"lastModifiedDate":"2012-03-12T17:20:49","indexId":"70029282","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1436,"text":"Earthquake Spectra","active":true,"publicationSubtype":{"id":10}},"title":"Earthquake and ambient vibration monitoring of the steel-frame UCLA factor building","docAbstract":"Dynamic property measurements of the moment-resisting steel-frame University of California, Los Angeles, Factor building are being made to assess how forces are distributed over the building. Fourier amplitude spectra have been calculated from several intervals of ambient vibrations, a 24-hour period of strong winds, and from the 28 March 2003 Encino, California (ML = 2.9), the 3 September 2002 Yorba Linda, California (ML = 4.7), and the 3 November 2002 Central Alaska (Mw = 7.9) earthquakes. Measurements made from the ambient vibration records show that the first-mode frequency of horizontal vibration is between 0.55 and 0.6 Hz. The second horizontal mode has a frequency between 1.6 and 1.9 Hz. In contrast, the first-mode frequencies measured from earthquake data are about 0.05 to 0.1 Hz lower than those corresponding to ambient vibration recordings indicating softening of the soil-structure system as amplitudes become larger. The frequencies revert to pre-earthquake levels within five minutes of the Yorba Linda earthquake. Shaking due to strong winds that occurred during the Encino earthquake dominates the frequency decrease, which correlates in time with the duration of the strong winds. The first shear wave recorded from the Encino and Yorba Linda earthquakes takes about 0.4 sec to travel up the 17-story building. ?? 2005, Earthquake Engineering Research Institute.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Earthquake Spectra","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1193/1.1946707","issn":"87552930","usgsCitation":"Kohler, M., Davis, P., and Safak, E., 2005, Earthquake and ambient vibration monitoring of the steel-frame UCLA factor building: Earthquake Spectra, v. 21, no. 3, p. 715-736, https://doi.org/10.1193/1.1946707.","startPage":"715","endPage":"736","numberOfPages":"22","costCenters":[],"links":[{"id":477802,"rank":10000,"type":{"id":41,"text":"Open Access External Repository Page"},"url":"https://resolver.caltech.edu/CaltechAUTHORS:20160122-140617171","text":"External Repository"},{"id":210749,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1193/1.1946707"},{"id":237766,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"21","issue":"3","noUsgsAuthors":false,"publicationDate":"2005-08-01","publicationStatus":"PW","scienceBaseUri":"505a04bae4b0c8380cd50ae2","contributors":{"authors":[{"text":"Kohler, M.D.","contributorId":47399,"corporation":false,"usgs":true,"family":"Kohler","given":"M.D.","email":"","affiliations":[],"preferred":false,"id":422064,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Davis, P.M.","contributorId":15229,"corporation":false,"usgs":true,"family":"Davis","given":"P.M.","email":"","affiliations":[],"preferred":false,"id":422063,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Safak, E.","contributorId":104070,"corporation":false,"usgs":true,"family":"Safak","given":"E.","email":"","affiliations":[],"preferred":false,"id":422065,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":70029281,"text":"70029281 - 2005 - The Shoemaker legacy to the Australian impact record","interactions":[],"lastModifiedDate":"2022-01-19T19:32:40.53435","indexId":"70029281","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":941,"text":"Australian Journal of Earth Sciences","active":true,"publicationSubtype":{"id":10}},"title":"The Shoemaker legacy to the Australian impact record","docAbstract":"No abstract available.
","language":"English","publisher":"Taylor & Francis","doi":"10.1080/08120090500170492","issn":"08120099","usgsCitation":"Shoemaker, C., and Macdonald, F., 2005, The Shoemaker legacy to the Australian impact record: Australian Journal of Earth Sciences, v. 52, no. 4-5, p. 477-479, https://doi.org/10.1080/08120090500170492.","productDescription":"3 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C.S.","contributorId":32318,"corporation":false,"usgs":true,"family":"Shoemaker","given":"C.S.","email":"","affiliations":[],"preferred":false,"id":422061,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Macdonald, F.A.","contributorId":103071,"corporation":false,"usgs":true,"family":"Macdonald","given":"F.A.","email":"","affiliations":[],"preferred":false,"id":422062,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70029324,"text":"70029324 - 2005 - Comment on \"How can seismic hazard around the New Madrid seismic zone be similar to that in California?\" by Arthur Frankel","interactions":[],"lastModifiedDate":"2022-06-02T16:45:50.567312","indexId":"70029324","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3372,"text":"Seismological Research Letters","onlineIssn":"1938-2057","printIssn":"0895-0695","active":true,"publicationSubtype":{"id":10}},"title":"Comment on \"How can seismic hazard around the New Madrid seismic zone be similar to that in California?\" by Arthur Frankel","docAbstract":"A recent paper in the September/October 2004 issue of Seismological Research Letters, “How Can Seismic Hazard around the New Madrid Seismic Zone Be Similar to That in California?”, by Arthur Frankel, concludes “I have demonstrated how probabilistic seismic hazard for New Madrid can be greater than that at San Francisco at low probabilities for PGA and similar at low probabilities for 5 Hz S.A. By low probabilities, I mean annual probabilities less than the reciprocal of the return time of the New Madrid characteristic source, that is, 1/500. This is a consequence of the higher ground motions, for PGA and 5 Hz S.A. (and other high-frequency measures), expected for large New Madrid characteristic earthquakes compared to San Andreas earthquakes with similar magnitudes.” His conclusion is confusing and not necessarily true. The fundamental differences in assessing seismic hazard between San Francisco and the New Madrid seismic zone are the uncertainties, especially the uncertainties associated with the ground-motion attenuation relationship. The larger ground-motion uncertainties in both the median and its standard deviation derive a higher hazard in the New Madrid area. The larger standard deviation, in particular, derives a higher hazard at low annual probabilities of exceedance. Moreover, Frankel also equated the hazard (annual probability of exceedance) defined in probabilistic seismic hazard analysis (PSHA) with the average recurrence rate defined in engineering risk analysis. There is a fundamental difference in defining risk between PSHA and the engineering risk analysis. The risks—10%, 5%, and 2% probability of exceedance (PE) in 50 years—defined in PSHA are not interchangeable with those defined in engineering risk analysis. Hence, though Frankel's stated intention was to improve understanding of PSHA among nonpractitioners, the paper may cause more confusion and problems for users of the U.S. Geological Survey national seismic hazard maps.
","language":"English","publisher":"Seismological Society of America","doi":"10.1785/gssrl.76.4.466","usgsCitation":"Wang, Z., Shi, B., and Kiefer, J.D., 2005, Comment on \"How can seismic hazard around the New Madrid seismic zone be similar to that in California?\" by Arthur Frankel: Seismological Research Letters, v. 76, no. 4, p. 466-471, https://doi.org/10.1785/gssrl.76.4.466.","productDescription":"6 p.","startPage":"466","endPage":"471","numberOfPages":"6","costCenters":[],"links":[{"id":237877,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"76","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059f7e6e4b0c8380cd4cd7b","contributors":{"authors":[{"text":"Wang, Z.","contributorId":67976,"corporation":false,"usgs":true,"family":"Wang","given":"Z.","affiliations":[],"preferred":false,"id":422265,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Shi, B.","contributorId":85374,"corporation":false,"usgs":true,"family":"Shi","given":"B.","email":"","affiliations":[],"preferred":false,"id":422266,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Kiefer, J. D.","contributorId":12684,"corporation":false,"usgs":true,"family":"Kiefer","given":"J.","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":422264,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":70029326,"text":"70029326 - 2005 - Subsidence hazards due to evaporite dissolution in the United States","interactions":[],"lastModifiedDate":"2015-12-03T15:38:03","indexId":"70029326","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1539,"text":"Environmental Geology","active":true,"publicationSubtype":{"id":10}},"title":"Subsidence hazards due to evaporite dissolution in the United States","docAbstract":"Evaporites, including gypsum (or anhydrite) and salt, are the most soluble of common rocks; they are dissolved readily to form the same type of karst features that typically are found in limestones and dolomites, and their dissolution can locally result in major subsidence structures. The four basic requirements for evaporite dissolution to occur are: (1) a deposit of gypsum or salt; (2) water, unsaturated with CaSO4 or NaCl; (3) an outlet for escape of dissolving water; and (4) energy to cause water to flow through the system. Evaporites are present in 32 of the 48 contiguous states of the United States, and they underlie about 35–40% of the land area. Karst is known at least locally (and sometimes quite extensively) in almost all areas underlain by evaporites, and some of these karst features involve significant subsidence. The most widespread and pronounced examples of both gypsum and salt karst and subsidence are in the Permian basin of the southwestern United States, but many other areas also are significant. Human activities have caused some evaporite–subsidence development, primarily in salt deposits. Boreholes may enable (either intentionally or inadvertently) unsaturated water to flow through or against salt deposits, thus allowing development of small to large dissolution cavities. If the dissolution cavity is large enough and shallow enough, successive roof failures above the cavity can cause land subsidence or catastrophic collapse.
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slabs","interactions":[],"lastModifiedDate":"2012-03-12T17:20:54","indexId":"70029279","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"Seismic joint analysis for non-destructive testing of asphalt and concrete slabs","docAbstract":"A seismic approach is used to estimate the thickness and elastic stiffness constants of asphalt or concrete slabs. The overall concept of the approach utilizes the robustness of the multichannel seismic method. A multichannel-equivalent data set is compiled from multiple time series recorded from multiple hammer impacts at progressively different offsets from a fixed receiver. This multichannel simulation with one receiver (MSOR) replaces the true multichannel recording in a cost-effective and convenient manner. A recorded data set is first processed to evaluate the shear wave velocity through a wave field transformation, normally used in the multichannel analysis of surface waves (MASW) method, followed by a Lambwave inversion. Then, the same data set is used to evaluate compression wave velocity from a combined processing of the first-arrival picking and a linear regression. Finally, the amplitude spectra of the time series are used to evaluate the thickness by following the concepts utilized in the Impact Echo (IE) method. Due to the powerful signal extraction capabilities ensured by the multichannel processing schemes used, the entire procedure for all three evaluations can be fully automated and results can be obtained directly in the field. A field data set is used to demonstrate the proposed approach.","largerWorkTitle":"Geotechnical Special Publication","conferenceTitle":"Geo-Frontiers 2005","conferenceDate":"24 January 2005 through 26 January 2005","conferenceLocation":"Austin, TX","language":"English","issn":"08950563","usgsCitation":"Ryden, N., and Park, C., 2005, Seismic joint analysis for non-destructive testing of asphalt and concrete slabs, in Geotechnical Special Publication, no. 130-142, Austin, TX, 24 January 2005 through 26 January 2005, p. 991-1000.","startPage":"991","endPage":"1000","numberOfPages":"10","costCenters":[],"links":[{"id":237733,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"issue":"130-142","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505b8b29e4b08c986b31763a","contributors":{"authors":[{"text":"Ryden, N.","contributorId":23318,"corporation":false,"usgs":true,"family":"Ryden","given":"N.","email":"","affiliations":[],"preferred":false,"id":422056,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Park, C.B.","contributorId":21714,"corporation":false,"usgs":true,"family":"Park","given":"C.B.","email":"","affiliations":[],"preferred":false,"id":422055,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70029278,"text":"70029278 - 2005 - Leaf fluctuating asymmetry, soil disturbance and plant stress: A multiple year comparison using two herbs, Ipomoea pandurata and Cnidoscolus stimulosus","interactions":[],"lastModifiedDate":"2016-05-03T16:48:39","indexId":"70029278","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1456,"text":"Ecological Indicators","active":true,"publicationSubtype":{"id":10}},"title":"Leaf fluctuating asymmetry, soil disturbance and plant stress: A multiple year comparison using two herbs, Ipomoea pandurata and Cnidoscolus stimulosus","docAbstract":"We studied Cnidoscolus stimulosus and Ipomoea pandurata, two common herbs of the Fall Line Sandhills to assess their potential as ecosystem level stress indicators. We focused on plants because they are among the most persistent organisms in terrestrial ecosystems. We used developmental instability as an indicator of plant population stress. Developmental instability is usually measured as deviations from symmetry, in traits that normally develop symmetrically. Thus, symmetry represents an idealized a priori phenotype. Stress presumably causes perturbations during development that may exceed the capacity of the organism to buffer or correct, resulting in developmental instability, and hence deviations from this ideal. Soil disturbance imposed by different land use patterns at Fort Benning, Georgia provided a gradient of soil disturbance. In 2000-2002 we collected plants from nine different sites representing three levels of disturbance. In addition, in 2002 we collected microhabitat data in 1 m quadrats surrounding each plant whose developmental stability we also assessed. The developmental instability of both species was influenced by land use patterns, whether or not the sites had been previously burned, and microhabitat variables. Developmental instability increased with soil disturbance, burning in the prior year, and as the percentage of bare ground increased around the target individual. To some extent, favorable microhabitat conditions reduced developmental instability in sites with medium and high soil disturbance, whereas unfavorable conditions at low soil disturbance sites increased developmental instability. As an indicator of community level stress, developmental instability is best used in conjunction with other indices of environmental quality. ?? Published by Elsevier Ltd.
","language":"English","publisher":"Elsevier","doi":"10.1016/j.ecolind.2004.05.002","issn":"1470160X","usgsCitation":"Freeman, D., Brown, M.L., Duda, J., Graraham, J., Emlen, J., Krzysik, A., Balbach, H., Kovacic, D., and Zak, J., 2005, Leaf fluctuating asymmetry, soil disturbance and plant stress: A multiple year comparison using two herbs, Ipomoea pandurata and Cnidoscolus stimulosus: Ecological Indicators, v. 5, no. 2, p. 85-95, https://doi.org/10.1016/j.ecolind.2004.05.002.","productDescription":"11 p.","startPage":"85","endPage":"95","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":654,"text":"Western Fisheries Research Center","active":true,"usgs":true}],"links":[{"id":237696,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":210696,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1016/j.ecolind.2004.05.002"}],"volume":"5","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a45ebe4b0c8380cd67524","contributors":{"authors":[{"text":"Freeman, D.C.","contributorId":21309,"corporation":false,"usgs":true,"family":"Freeman","given":"D.C.","email":"","affiliations":[],"preferred":false,"id":422046,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Brown, M. L.","contributorId":96063,"corporation":false,"usgs":true,"family":"Brown","given":"M.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":422052,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Duda, J.J. 0000-0001-7431-8634","orcid":"https://orcid.org/0000-0001-7431-8634","contributorId":105073,"corporation":false,"usgs":true,"family":"Duda","given":"J.J.","affiliations":[],"preferred":false,"id":422054,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Graraham, J.H.","contributorId":70989,"corporation":false,"usgs":true,"family":"Graraham","given":"J.H.","email":"","affiliations":[],"preferred":false,"id":422050,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Emlen, J.M.","contributorId":63979,"corporation":false,"usgs":true,"family":"Emlen","given":"J.M.","email":"","affiliations":[],"preferred":false,"id":422049,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Krzysik, A.J.","contributorId":63188,"corporation":false,"usgs":true,"family":"Krzysik","given":"A.J.","affiliations":[],"preferred":false,"id":422048,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Balbach, H.","contributorId":42778,"corporation":false,"usgs":true,"family":"Balbach","given":"H.","email":"","affiliations":[],"preferred":false,"id":422047,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Kovacic, D.A.","contributorId":102207,"corporation":false,"usgs":true,"family":"Kovacic","given":"D.A.","email":"","affiliations":[],"preferred":false,"id":422053,"contributorType":{"id":1,"text":"Authors"},"rank":8},{"text":"Zak, J.C.","contributorId":82097,"corporation":false,"usgs":true,"family":"Zak","given":"J.C.","email":"","affiliations":[],"preferred":false,"id":422051,"contributorType":{"id":1,"text":"Authors"},"rank":9}]}} ,{"id":70029277,"text":"70029277 - 2005 - Field determination of optimal dates for the discrimination of invasive wetland plant species using derivative spectral analysis","interactions":[],"lastModifiedDate":"2023-02-15T14:27:28.750937","indexId":"70029277","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3052,"text":"Photogrammetric Engineering and Remote Sensing","active":true,"publicationSubtype":{"id":10}},"title":"Field determination of optimal dates for the discrimination of invasive wetland plant species using derivative spectral analysis","docAbstract":"Mapping invasive plant species in aquatic and terrestrial ecosystems helps to understand the causes of their progression, manage some of their negative consequences, and control them. In recent years, a variety of new remote-sensing techniques, like Derivative Spectral Analysis (DSA) of hyperspectral data, have been developed to facilitate this mapping. A number of questions related to these techniques remain to be addressed. This article attempts to answer one of these questions: Is the application of DSA optimal at certain times of the year? Field radiometric data gathered weekly during the summer of 1999 at selected field sites in upstate New York, populated with purple loosestrife (Lythrum salicaria L.), common reed (Phragmites australis (Cav.)) and cattail (Typha L.) are analyzed using DSA to differentiate among plant community types. First, second and higher-order derivatives of the reflectance spectra of nine field plots, varying in plant composition, are calculated and analyzed in detail to identify spectral ranges in which one or more community types have distinguishing features. On the basis of the occurrence and extent of these spectral ranges, experimental observations suggest that a satisfactory differentiation among community types was feasible on 30 August, when plants experienced characteristic phenological changes (transition from flowers to seed heads). Generally, dates in August appear optimal from the point of view of species differentiability and could be selected for image acquisitions. This observation, as well as the methodology adopted in this article, should provide a firm basis for the acquisition of hyperspectral imagery and for mapping the targeted species over a broad range of spatial scales.
","language":"English","publisher":"American Society for Photogrammetry and Remote Sensing","doi":"10.14358/PERS.71.5.603","usgsCitation":"Laba, M., Tsai, F., Ogurcak, D., Smith, S., and Richmond, M.E., 2005, Field determination of optimal dates for the discrimination of invasive wetland plant species using derivative spectral analysis: Photogrammetric Engineering and Remote Sensing, v. 71, no. 5, p. 603-611, https://doi.org/10.14358/PERS.71.5.603.","productDescription":"9 p.","startPage":"603","endPage":"611","numberOfPages":"9","costCenters":[],"links":[{"id":477970,"rank":2,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.14358/pers.71.5.603","text":"Publisher Index Page"},{"id":237695,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"71","issue":"5","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a0fafe4b0c8380cd539a1","contributors":{"authors":[{"text":"Laba, M.","contributorId":55633,"corporation":false,"usgs":true,"family":"Laba","given":"M.","email":"","affiliations":[],"preferred":false,"id":422043,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Tsai, F.","contributorId":107086,"corporation":false,"usgs":true,"family":"Tsai","given":"F.","email":"","affiliations":[],"preferred":false,"id":422045,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Ogurcak, Danielle","contributorId":21815,"corporation":false,"usgs":true,"family":"Ogurcak","given":"Danielle","affiliations":[],"preferred":false,"id":422044,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Smith, S.","contributorId":20698,"corporation":false,"usgs":true,"family":"Smith","given":"S.","email":"","affiliations":[],"preferred":false,"id":422041,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Richmond, M. E.","contributorId":22729,"corporation":false,"usgs":true,"family":"Richmond","given":"M.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":422042,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}} ,{"id":70029272,"text":"70029272 - 2005 - Simulation of reactive transport of injected CO2 on the Colorado Plateau, Utah, USA","interactions":[],"lastModifiedDate":"2012-03-12T17:20:55","indexId":"70029272","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1213,"text":"Chemical Geology","active":true,"publicationSubtype":{"id":10}},"title":"Simulation of reactive transport of injected CO2 on the Colorado Plateau, Utah, USA","docAbstract":"This paper investigates injection of CO2 into non-dome-shaped geological structures that do not provide the traps traditionally deemed necessary for the development of artificial CO2 reservoirs. We have developed a conceptual and two numerical models of the geology and groundwater along a cross-section lying approximately NW-SE and in the vicinity of the Hunter power station on the Colorado Plateau, Central Utah and identified a number of potential sequestration sites on this cross-section. Preliminary modeling identified the White Rim Sandstone as appearing to offer the properties required of a successful sequestration site. Detailed modeling of injection of CO2 into the White Rim Sandstone using the reactive chemical simulator ChemTOUGH found that 1000 years after the 30 year injection period began approximately 21% of the injected CO2 was permanently sequestered as a mineral, 52% was beneath the ground surface as a gas or dissolved in the groundwater and 17% had leaked to the surface and leakage to the surface was continuing. ?? 2005 Elsevier B.V. All rights reserved.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Chemical Geology","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1016/j.chemgeo.2004.12.020","issn":"00092541","usgsCitation":"White, S., Allis, R., Moore, J., Chidsey, T., Morgan, C., Gwynn, W., and Adams, M., 2005, Simulation of reactive transport of injected CO2 on the Colorado Plateau, Utah, USA: Chemical Geology, v. 217, no. 3-4 SPEC. ISS., p. 387-405, https://doi.org/10.1016/j.chemgeo.2004.12.020.","startPage":"387","endPage":"405","numberOfPages":"19","costCenters":[],"links":[{"id":237591,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":210617,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1016/j.chemgeo.2004.12.020"}],"volume":"217","issue":"3-4 SPEC. ISS.","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505b9077e4b08c986b319507","contributors":{"authors":[{"text":"White, S.P.","contributorId":61236,"corporation":false,"usgs":true,"family":"White","given":"S.P.","email":"","affiliations":[],"preferred":false,"id":422012,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Allis, R.G.","contributorId":86150,"corporation":false,"usgs":true,"family":"Allis","given":"R.G.","email":"","affiliations":[],"preferred":false,"id":422015,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Moore, Jeff","contributorId":49059,"corporation":false,"usgs":true,"family":"Moore","given":"Jeff","email":"","affiliations":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"preferred":false,"id":422011,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Chidsey, T.","contributorId":105113,"corporation":false,"usgs":true,"family":"Chidsey","given":"T.","email":"","affiliations":[],"preferred":false,"id":422017,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Morgan, C.","contributorId":94489,"corporation":false,"usgs":true,"family":"Morgan","given":"C.","affiliations":[],"preferred":false,"id":422016,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Gwynn, W.","contributorId":69772,"corporation":false,"usgs":true,"family":"Gwynn","given":"W.","email":"","affiliations":[],"preferred":false,"id":422013,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Adams, M.","contributorId":81176,"corporation":false,"usgs":true,"family":"Adams","given":"M.","email":"","affiliations":[],"preferred":false,"id":422014,"contributorType":{"id":1,"text":"Authors"},"rank":7}]}} ,{"id":70029270,"text":"70029270 - 2005 - Acquisition and evaluation of thermodynamic data for bieberite-moorhouseite equilibria at 0.1 MPa","interactions":[],"lastModifiedDate":"2012-03-12T17:20:54","indexId":"70029270","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":738,"text":"American Mineralogist","active":true,"publicationSubtype":{"id":10}},"title":"Acquisition and evaluation of thermodynamic data for bieberite-moorhouseite equilibria at 0.1 MPa","docAbstract":"Published estimates for the equilibrium relative humidity (RH) at 25 deg;C for the reaction: bieberite (CoSO4??7H2O) = moorhouseite (CoSO4??6H2O) + H2O, range from 69.8 to 74.5%. To evaluate these data, the humidity-buffer technique was used to determine equilibrium constants for this reaction between 14 and 43 ??C at 0.1 MPa. Reversals along five humidity-buffer curves yield In K = 18.03-6509.43/T, where K is the equilibrium constant, and T is temperature in K. The derived standard Gibbs free energy of reaction is 9.43 kJ/mol, which agrees well with several previously reported values based on vapor-pressure measurements. It also agrees well with values calculated from the data derived mostly from calorimetric measurements. Previous studies indicated that the temperature of the invariant point for the assemblage bieberite-moorhouseite-aqueous solution-vapor is near 44.7 ??C, and our extrapolated data predict 91.1% RH at this temperature; the predicted position for the invariant point is in excellent agreement with those reported previously.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"American Mineralogist","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.2138/am.2005.1695","issn":"0003004X","usgsCitation":"Chou, I., and Seal, R., 2005, Acquisition and evaluation of thermodynamic data for bieberite-moorhouseite equilibria at 0.1 MPa: American Mineralogist, v. 90, no. 5-6, p. 912-917, https://doi.org/10.2138/am.2005.1695.","startPage":"912","endPage":"917","numberOfPages":"6","costCenters":[],"links":[{"id":210615,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.2138/am.2005.1695"},{"id":237589,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"90","issue":"5-6","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059e6a3e4b0c8380cd47554","contributors":{"authors":[{"text":"Chou, I.-M. 0000-0001-5233-6479","orcid":"https://orcid.org/0000-0001-5233-6479","contributorId":44283,"corporation":false,"usgs":true,"family":"Chou","given":"I.-M.","affiliations":[{"id":245,"text":"Eastern Mineral and Environmental Resources Science Center","active":true,"usgs":true}],"preferred":false,"id":422004,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Seal, R.R. II","contributorId":102097,"corporation":false,"usgs":true,"family":"Seal","given":"R.R.","suffix":"II","email":"","affiliations":[],"preferred":false,"id":422005,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70029269,"text":"70029269 - 2005 - Influence of sediment storage on downstream delivery of contaminated sediment","interactions":[],"lastModifiedDate":"2018-03-30T11:16:07","indexId":"70029269","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3722,"text":"Water Resources Research","onlineIssn":"1944-7973","printIssn":"0043-1397","active":true,"publicationSubtype":{"id":10}},"title":"Influence of sediment storage on downstream delivery of contaminated sediment","docAbstract":"Sediment storage in alluvial valleys can strongly modulate the downstream migration of sediment and associated contaminants through landscapes. Traditional methods for routing contaminated sediment through valleys focus on in‐channel sediment transport but ignore the influence of sediment exchanges with temporary sediment storage reservoirs outside the channel, such as floodplains. In theory, probabilistic analysis of particle trajectories through valleys offers a useful strategy for quantifying the influence of sediment storage on the downstream movement of contaminated sediment. This paper describes a field application and test of this theory, using 137Cs as a sediment tracer over 45 years (1952–1997), downstream of a historical effluent outfall at the Los Alamos National Laboratory (LANL), New Mexico. The theory is parameterized using a sediment budget based on field data and an estimate of the 137Cs release history at the upstream boundary. The uncalibrated model reasonably replicates the approximate magnitude and spatial distribution of channel‐ and floodplain‐stored 137Cs measured in an independent field study. Model runs quantify the role of sediment storage in the long‐term migration of a pulse of contaminated sediment, quantify the downstream impact of upstream mitigation, and mathematically decompose the future 137Cs flux near the LANL property boundary to evaluate the relative contributions of various upstream contaminant sources. The fate of many sediment‐bound contaminants is determined by the relative timescales of contaminant degradation and particle residence time in different types of sedimentary environments. The theory provides a viable approach for quantifying the long‐term movement of contaminated sediment through valleys.
","language":"English","publisher":"American Geophysical Union","doi":"10.1029/2004WR003288","usgsCitation":"Malmon, D.V., Reneau, S.L., Dunne, T., Katzman, D., and Drakos, P., 2005, Influence of sediment storage on downstream delivery of contaminated sediment: Water Resources Research, v. 41, no. 5, Article W05008; 17 p., https://doi.org/10.1029/2004WR003288.","productDescription":"Article W05008; 17 p.","costCenters":[],"links":[{"id":477951,"rank":1,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1029/2004wr003288","text":"Publisher Index Page"},{"id":237553,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"41","issue":"5","noUsgsAuthors":false,"publicationDate":"2005-05-06","publicationStatus":"PW","scienceBaseUri":"505a3b7ae4b0c8380cd6257a","contributors":{"authors":[{"text":"Malmon, Daniel V.","contributorId":89998,"corporation":false,"usgs":true,"family":"Malmon","given":"Daniel","email":"","middleInitial":"V.","affiliations":[],"preferred":false,"id":422000,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Reneau, Steven L.","contributorId":99639,"corporation":false,"usgs":false,"family":"Reneau","given":"Steven","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":422003,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Dunne, Thomas","contributorId":146518,"corporation":false,"usgs":false,"family":"Dunne","given":"Thomas","email":"","affiliations":[{"id":6710,"text":"University of California, Santa Barbara, CA","active":true,"usgs":false}],"preferred":false,"id":422001,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Katzman, Danny","contributorId":102268,"corporation":false,"usgs":false,"family":"Katzman","given":"Danny","email":"","affiliations":[],"preferred":false,"id":422002,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Drakos, Paul G.","contributorId":8667,"corporation":false,"usgs":false,"family":"Drakos","given":"Paul G.","affiliations":[],"preferred":false,"id":421999,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}} ,{"id":70029268,"text":"70029268 - 2005 - Responses of hybrid striped bass to waterborne and dietary copper in freshwater and saltwater","interactions":[],"lastModifiedDate":"2017-05-06T15:29:16","indexId":"70029268","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1296,"text":"Comparative Biochemistry and Physiology, Part C: Toxicology & Pharmacology","active":true,"publicationSubtype":{"id":10}},"title":"Responses of hybrid striped bass to waterborne and dietary copper in freshwater and saltwater","docAbstract":"Mechanisms of copper toxicity and consequences of exposure vary due to uptake route and ionoregulatory status. The goal of this research was to develop a model fish system to assess the influence of different Cu exposure routes (waterborne or dietary) on bioavailability, uptake, and effects in hybrid striped bass (Morone chrysops×Morone saxatilis) acclimated to fresh- or saltwater. Initially, hybrid striped bass were exposed to dietary Cu concentrations of 571, 785, and 1013 μg Cu/g, along with a control (∼ 5 μg Cu/g), for 14 days in saltwater. Intestinal and liver Cu accumulated in a dose-dependent manner in fish exposed to increasing levels of dietary Cu. Chronic (42 days) experiments were then conducted to determine sub-lethal effects of aqueous, dietary, and combined aqueous and dietary Cu exposures to both freshwater- and saltwater-acclimated hybrid striped bass. Growth and Cu accumulation in the gill, intestine, and liver were measured. Although no significant effects were observed in fish exposed to waterborne Cu, those exposed through the diet accumulated significant liver and intestinal Cu but showed no significant change in growth. Overall, these results suggest that at the levels tested, exposure to elevated waterborne Cu did not cause significant long-term tissue Cu accumulation, whereas dietary Cu exposure caused significant liver and intestinal Cu accumulation in hybrid striped bass which was comparable in both freshwater and saltwater (15 g/L).
","language":"English","publisher":"Elsevier","doi":"10.1016/j.cca.2005.01.014","issn":"15320456","usgsCitation":"Bielmyer, G., Gatlin, D., Isely, J.J., Tomasso, J., and Klaine, S., 2005, Responses of hybrid striped bass to waterborne and dietary copper in freshwater and saltwater: Comparative Biochemistry and Physiology, Part C: Toxicology & Pharmacology, v. 140, no. 1, p. 131-137, https://doi.org/10.1016/j.cca.2005.01.014.","productDescription":"7 p.","startPage":"131","endPage":"137","costCenters":[],"links":[{"id":237552,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"140","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505aaaa1e4b0c8380cd86434","contributors":{"authors":[{"text":"Bielmyer, G.K.","contributorId":50345,"corporation":false,"usgs":true,"family":"Bielmyer","given":"G.K.","email":"","affiliations":[],"preferred":false,"id":421996,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Gatlin, D.","contributorId":100183,"corporation":false,"usgs":true,"family":"Gatlin","given":"D.","email":"","affiliations":[],"preferred":false,"id":421998,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Isely, J. Jeffery","contributorId":97224,"corporation":false,"usgs":true,"family":"Isely","given":"J.","email":"","middleInitial":"Jeffery","affiliations":[],"preferred":false,"id":421997,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Tomasso, J.","contributorId":23748,"corporation":false,"usgs":true,"family":"Tomasso","given":"J.","email":"","affiliations":[],"preferred":false,"id":421994,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Klaine, S.J.","contributorId":38304,"corporation":false,"usgs":true,"family":"Klaine","given":"S.J.","affiliations":[],"preferred":false,"id":421995,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}} ,{"id":70029265,"text":"70029265 - 2005 - Geotechnical aspects of the January 2003 Tecoma'n, Mexico, earthquake","interactions":[],"lastModifiedDate":"2015-05-04T13:10:36","indexId":"70029265","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1436,"text":"Earthquake Spectra","active":true,"publicationSubtype":{"id":10}},"title":"Geotechnical aspects of the January 2003 Tecoma'n, Mexico, earthquake","docAbstract":"Ground failure was the most prominent geotechnical engineering feature of the 21 January 2003 Mw 7.6 Tecoma´n earthquake. Ground failure impacted structures, industrial facilities, roads, water supply canals, and other critical infrastructure in the state of Colima and in parts of the neighboring states of Jalisco and Michoaca´n. Landslides and soil liquefaction were the most common type of ground failure, followed by seismic compression of unsaturated materials. Reinforced earth structures generally performed well during the earthquake, though some structures experienced permanent lateral deformations up to 10 cm. Different ground improvement techniques had been used to enhance the liquefaction resistance of several sites in the region, all of which performed well and exhibited no signs of damage or significant ground deformation. Earth dams in the region experienced some degree of permanent deformation but remained fully functional after the earthquake.
","language":"English","publisher":"Earthqauke Engineering Research Institute","doi":"10.1193/1.1904064","issn":"87552930","usgsCitation":"Wartman, J., Rodriguez-Marek, A., Macari, E.J., Deaton, S., Ramirez-Reynaga, M., Ochoa, C.N., Callan, S., Keefer, D., Repetto, P., and Ovando-Shelley, E., 2005, Geotechnical aspects of the January 2003 Tecoma'n, Mexico, earthquake: Earthquake Spectra, v. 21, no. 2, p. 493-538, https://doi.org/10.1193/1.1904064.","productDescription":"46 p.","startPage":"493","endPage":"538","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":237475,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":210529,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1193/1.1904064"}],"volume":"21","issue":"2","noUsgsAuthors":false,"publicationDate":"2005-05-01","publicationStatus":"PW","scienceBaseUri":"505a28b5e4b0c8380cd5a336","contributors":{"authors":[{"text":"Wartman, Joseph","contributorId":9053,"corporation":false,"usgs":true,"family":"Wartman","given":"Joseph","affiliations":[],"preferred":false,"id":421973,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Rodriguez-Marek, Adrian","contributorId":67711,"corporation":false,"usgs":true,"family":"Rodriguez-Marek","given":"Adrian","email":"","affiliations":[],"preferred":false,"id":421980,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Macari, Emir J.","contributorId":22135,"corporation":false,"usgs":true,"family":"Macari","given":"Emir","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":421975,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Deaton, Scott","contributorId":100602,"corporation":false,"usgs":true,"family":"Deaton","given":"Scott","email":"","affiliations":[],"preferred":false,"id":421982,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Ramirez-Reynaga, Marti’n","contributorId":49177,"corporation":false,"usgs":true,"family":"Ramirez-Reynaga","given":"Marti’n","email":"","affiliations":[],"preferred":false,"id":421978,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Ochoa, Carlos N.","contributorId":40408,"corporation":false,"usgs":true,"family":"Ochoa","given":"Carlos","email":"","middleInitial":"N.","affiliations":[],"preferred":false,"id":421976,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Callan, Sean","contributorId":74946,"corporation":false,"usgs":true,"family":"Callan","given":"Sean","email":"","affiliations":[],"preferred":false,"id":421981,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Keefer, David","contributorId":94152,"corporation":false,"usgs":true,"family":"Keefer","given":"David","affiliations":[],"preferred":false,"id":421977,"contributorType":{"id":1,"text":"Authors"},"rank":8},{"text":"Repetto, Pedro","contributorId":51975,"corporation":false,"usgs":true,"family":"Repetto","given":"Pedro","email":"","affiliations":[],"preferred":false,"id":421979,"contributorType":{"id":1,"text":"Authors"},"rank":9},{"text":"Ovando-Shelley, Efrai’n","contributorId":18961,"corporation":false,"usgs":true,"family":"Ovando-Shelley","given":"Efrai’n","email":"","affiliations":[],"preferred":false,"id":421974,"contributorType":{"id":1,"text":"Authors"},"rank":10}]}} ,{"id":70029264,"text":"70029264 - 2005 - Predictability of littoral-zone fish communities through ontogeny in Lake Texoma, Oklahoma-Texas, USA","interactions":[],"lastModifiedDate":"2012-03-12T17:20:55","indexId":"70029264","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1528,"text":"Environmental Biology of Fishes","active":true,"publicationSubtype":{"id":10}},"title":"Predictability of littoral-zone fish communities through ontogeny in Lake Texoma, Oklahoma-Texas, USA","docAbstract":"We sampled larval, juvenile and adult fishes from littoral-zone areas of a large reservoir (Lake Texoma, Oklahoma-Texas) (1) to characterize environmental factors that influenced fish community structure, (2) to examine how consistent fish-environment relationships were through ontogeny (i.e., larval vs. juvenile and adult), and (3) to measure the concordance of larval communities sampled during spring to juvenile and adult communities sampled at the same sites later in the year. Larval, juvenile and adult fish communities were dominated by Atherinidae (mainly inland silverside, Menidia beryllina) and Moronidae (mainly juvenile striped bass, Morone saxatilis) and were consistently structured along a gradient of site exposure to prevailing winds and waves. Larval, juvenile and adult communities along this gradient varied from atherinids and moronids at highly exposed sites to mostly centrarchids (primarily Lepomis and Micropterus spp.) at protected sites. Secondarily, zooplankton densities, water clarity, and land-use characteristics were related to fish community structure. Rank correlation analyses and Mantel tests indicated that the spatial consistency and predictability of fish communities was high as larval fishes sampled during spring were concordant with juvenile and adult fishes sampled at the same sites during summer and fall in terms of abundance, richness, and community structure. We propose that the high predictability and spatial consistency of littoral-zone fishes in Lake Texoma was a function of relatively simple communities (dominated by 1-2 species) that were structured by factors, such as site exposure to winds and waves, that varied little through time. ?? Springer 2005.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Environmental Biology of Fishes","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1007/s10641-004-3797-1","issn":"03781909","usgsCitation":"Eggleton, M., Ramirez, R., Hargrave, C., Gido, K., Masoner, J., Schnell, G., and Matthews, W., 2005, Predictability of littoral-zone fish communities through ontogeny in Lake Texoma, Oklahoma-Texas, USA: Environmental Biology of Fishes, v. 73, no. 1, p. 21-36, https://doi.org/10.1007/s10641-004-3797-1.","startPage":"21","endPage":"36","numberOfPages":"16","costCenters":[],"links":[{"id":210528,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1007/s10641-004-3797-1"},{"id":237474,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"73","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a8189e4b0c8380cd7b5a0","contributors":{"authors":[{"text":"Eggleton, M.A.","contributorId":40370,"corporation":false,"usgs":true,"family":"Eggleton","given":"M.A.","affiliations":[],"preferred":false,"id":421970,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Ramirez, R.","contributorId":26873,"corporation":false,"usgs":true,"family":"Ramirez","given":"R.","email":"","affiliations":[],"preferred":false,"id":421967,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Hargrave, C.W.","contributorId":40003,"corporation":false,"usgs":true,"family":"Hargrave","given":"C.W.","email":"","affiliations":[],"preferred":false,"id":421969,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Gido, K.B.","contributorId":106298,"corporation":false,"usgs":true,"family":"Gido","given":"K.B.","email":"","affiliations":[],"preferred":false,"id":421972,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Masoner, J.R.","contributorId":15690,"corporation":false,"usgs":true,"family":"Masoner","given":"J.R.","affiliations":[],"preferred":false,"id":421966,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Schnell, G.D.","contributorId":38352,"corporation":false,"usgs":true,"family":"Schnell","given":"G.D.","email":"","affiliations":[],"preferred":false,"id":421968,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Matthews, W.J.","contributorId":70343,"corporation":false,"usgs":true,"family":"Matthews","given":"W.J.","email":"","affiliations":[],"preferred":false,"id":421971,"contributorType":{"id":1,"text":"Authors"},"rank":7}]}} ]}