{"pageNumber":"1004","pageRowStart":"25075","pageSize":"25","recordCount":40818,"records":[{"id":1001072,"text":"1001072 - 2006 - Modeling wetland plant community response to assess water-level regulation scenarios in the Lake Ontario-St. Lawrence River basin","interactions":[],"lastModifiedDate":"2016-05-09T10:45:38","indexId":"1001072","displayToPublicDate":"2006-01-01T00:00:00","publicationYear":"2006","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1552,"text":"Environmental Monitoring and Assessment","onlineIssn":"1573-2959","printIssn":"0167-6369","active":true,"publicationSubtype":{"id":10}},"title":"Modeling wetland plant community response to assess water-level regulation scenarios in the Lake Ontario-St. Lawrence River basin","docAbstract":"<p>The International Joint Commission has recently completed a five-year study (2000-2005) to review the operation of structures controlling the flows and levels of the Lake Ontario - St. Lawrence River system. In addition to addressing the multitude of stakeholder interests, the regulation plan review also considers environmental sustainability and integrity of wetlands and various ecosystem components. The present paper outlines the general approach, scientific methodology and applied management considerations of studies quantifying the relationships between hydrology and wetland plant assemblages (% occurrence, surface area) in Lake Ontario and the Upper and Lower St. Lawrence River. Although similar study designs were used across the study region, different methodologies were required that were specifically adapted to suit the important regional differences between the lake and river systems, range in water-level variations, and confounding factors (geomorphic types, exposure, sediment characteristics, downstream gradient of water quality, origin of water masses in the Lower River). Performance indicators (metrics), such as total area of wetland in meadow marsh vegetation type, that link wetland response to water levels will be used to assess the effects of different regulation plans under current and future (climate change) water-supply scenarios.</p>","language":"English","publisher":"Springer","doi":"10.1007/s10661-005-9086-4","usgsCitation":"Hudon, C., Wilcox, D., and Ingram, J., 2006, Modeling wetland plant community response to assess water-level regulation scenarios in the Lake Ontario-St. Lawrence River basin: Environmental Monitoring and Assessment, v. 113, no. 1-3, p. 303-328, https://doi.org/10.1007/s10661-005-9086-4.","productDescription":"26 p.","startPage":"303","endPage":"328","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":324,"text":"Great Lakes Science Center","active":true,"usgs":true}],"links":[{"id":477564,"rank":1,"type":{"id":41,"text":"Open Access External Repository Page"},"url":"http://hdl.handle.net/20.500.12648/2305","text":"External Repository"},{"id":133564,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"113","issue":"1-3","noUsgsAuthors":false,"publicationDate":"2006-02-24","publicationStatus":"PW","scienceBaseUri":"4f4e4b05e4b07f02db69976f","contributors":{"authors":[{"text":"Hudon, Christiane","contributorId":80632,"corporation":false,"usgs":true,"family":"Hudon","given":"Christiane","email":"","affiliations":[],"preferred":false,"id":310395,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Wilcox, Douglas","contributorId":72764,"corporation":false,"usgs":true,"family":"Wilcox","given":"Douglas","affiliations":[],"preferred":false,"id":310394,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Ingram, Joel","contributorId":65046,"corporation":false,"usgs":true,"family":"Ingram","given":"Joel","affiliations":[],"preferred":false,"id":310393,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70030653,"text":"70030653 - 2006 - Estimating hydraulic properties using a moving-model approach and multiple aquifer tests","interactions":[],"lastModifiedDate":"2012-03-12T17:21:05","indexId":"70030653","displayToPublicDate":"2006-01-01T00:00:00","publicationYear":"2006","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1861,"text":"Ground Water","active":true,"publicationSubtype":{"id":10}},"title":"Estimating hydraulic properties using a moving-model approach and multiple aquifer tests","docAbstract":"A new method was developed for characterizing geohydrologic columns that extended >600 m deep at sites with as many as six discrete aquifers. This method was applied at 12 sites within the Southwest Florida Water Management District. Sites typically were equipped with multiple production wells, one for each aquifer and one or more observation wells per aquifer. The average hydraulic properties of the aquifers and confining units within radii of 30 to >300 m were characterized at each site. Aquifers were pumped individually and water levels were monitored in stressed and adjacent aquifers during each pumping event. Drawdowns at a site were interpreted using a radial numerical model that extended from land surface to the base of the geohydrologic column and simulated all pumping events. Conceptually, the radial model moves between stress periods and recenters on the production well during each test. Hydraulic conductivity was assumed homogeneous and isotropic within each aquifer and confining unit. Hydraulic property estimates for all of the aquifers and confining units were consistent and reasonable because results from multiple aquifers and pumping events were analyzed simultaneously. Copyright ?? 2005 National Ground Water Association.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Ground Water","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1111/j.1745-6584.2005.00109.x","issn":"0017467X","usgsCitation":"Halford, K.J., and Yobbi, D., 2006, Estimating hydraulic properties using a moving-model approach and multiple aquifer tests: Ground Water, v. 44, no. 2, p. 284-291, https://doi.org/10.1111/j.1745-6584.2005.00109.x.","startPage":"284","endPage":"291","numberOfPages":"8","costCenters":[],"links":[{"id":211731,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1111/j.1745-6584.2005.00109.x"},{"id":239078,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"44","issue":"2","noUsgsAuthors":false,"publicationDate":"2005-08-24","publicationStatus":"PW","scienceBaseUri":"505a0b22e4b0c8380cd525b4","contributors":{"authors":[{"text":"Halford, K. J. 0000-0002-7322-1846","orcid":"https://orcid.org/0000-0002-7322-1846","contributorId":61077,"corporation":false,"usgs":true,"family":"Halford","given":"K.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":428044,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Yobbi, D.","contributorId":77735,"corporation":false,"usgs":true,"family":"Yobbi","given":"D.","affiliations":[],"preferred":false,"id":428045,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70030634,"text":"70030634 - 2006 - Simulation of reactive transport of uranium(VI) in groundwater with variable chemical conditions","interactions":[],"lastModifiedDate":"2018-04-03T13:58:42","indexId":"70030634","displayToPublicDate":"2006-01-01T00:00:00","publicationYear":"2006","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3722,"text":"Water Resources Research","onlineIssn":"1944-7973","printIssn":"0043-1397","active":true,"publicationSubtype":{"id":10}},"title":"Simulation of reactive transport of uranium(VI) in groundwater with variable chemical conditions","docAbstract":"<p><span>The reactive transport of U(VI) in a shallow alluvial aquifer beneath a former U(VI) mill located near Naturita, CO, was simulated using a surface complexation model (SCM) to describe U(VI) adsorption. The groundwater had variable U(VI) concentrations (0.01–20 μM), variable alkalinity (2.5–18 meq/L), and a nearly constant pH equal to 7.1. U(VI) K</span><sub>D</sub><span>values decreased with increasing U(VI) and alkalinity, and these parameters were more important than sediment variability in controlling K</span><sub>D</sub><span><span>&nbsp;</span>values. Reactive transport simulations were fit to the observed U(VI) and alkalinity by varying the concentration of U(VI) and alkalinity in recharge at the source area. Simulated K</span><sub>D</sub><span><span>&nbsp;</span>values varied temporally and spatially because of the differential transport of U(VI) and alkalinity and the nonlinearity of U(VI) adsorption. The model also simulated the observed U(VI) tailing, which would not be expected from a constant K</span><sub>D</sub><span><span>&nbsp;</span>model. The simulated U(VI) concentrations were sensitive to the recharge flux because of the increased flux of U(VI) to the aquifer. The geochemical behavior of U(VI) was most sensitive to the alkalinity and was relatively insensitive to pH.</span></p>","language":"English","publisher":"American Geophysical Union","doi":"10.1029/2005WR003979","usgsCitation":"Curtis, G.P., Davis, J., and Naftz, D.L., 2006, Simulation of reactive transport of uranium(VI) in groundwater with variable chemical conditions: Water Resources Research, v. 42, no. 4, Article W04404; 15 p., https://doi.org/10.1029/2005WR003979.","productDescription":"Article W04404; 15 p.","costCenters":[],"links":[{"id":477434,"rank":1,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1029/2005wr003979","text":"Publisher Index Page"},{"id":239353,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"42","issue":"4","noUsgsAuthors":false,"publicationDate":"2006-04-07","publicationStatus":"PW","scienceBaseUri":"505b9078e4b08c986b31950d","contributors":{"authors":[{"text":"Curtis, Gary P. 0000-0003-3975-8882 gpcurtis@usgs.gov","orcid":"https://orcid.org/0000-0003-3975-8882","contributorId":2346,"corporation":false,"usgs":true,"family":"Curtis","given":"Gary","email":"gpcurtis@usgs.gov","middleInitial":"P.","affiliations":[{"id":438,"text":"National Research Program - Western Branch","active":true,"usgs":true}],"preferred":true,"id":427964,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Davis, James A.","contributorId":69289,"corporation":false,"usgs":true,"family":"Davis","given":"James A.","affiliations":[],"preferred":false,"id":427965,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"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":427963,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70030621,"text":"70030621 - 2006 - Importance of recent shifts in soil thermal dynamics on growing season length, productivity, and carbon sequestration in terrestrial high-latitude ecosystems","interactions":[],"lastModifiedDate":"2012-03-12T17:21:05","indexId":"70030621","displayToPublicDate":"2006-01-01T00:00:00","publicationYear":"2006","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1837,"text":"Global Change Biology","active":true,"publicationSubtype":{"id":10}},"title":"Importance of recent shifts in soil thermal dynamics on growing season length, productivity, and carbon sequestration in terrestrial high-latitude ecosystems","docAbstract":"In terrestrial high-latitude regions, observations indicate recent changes in snow cover, permafrost, and soil freeze-thaw transitions due to climate change. These modifications may result in temporal shifts in the growing season and the associated rates of terrestrial productivity. Changes in productivity will influence the ability of these ecosystems to sequester atmospheric CO2. We use the terrestrial ecosystem model (TEM), which simulates the soil thermal regime, in addition to terrestrial carbon (C), nitrogen and water dynamics, to explore these issues over the years 1960-2100 in extratropical regions (30-90??N). Our model simulations show decreases in snow cover and permafrost stability from 1960 to 2100. Decreases in snow cover agree well with National Oceanic and Atmospheric Administration satellite observations collected between the years 1972 and 2000, with Pearson rank correlation coefficients between 0.58 and 0.65. Model analyses also indicate a trend towards an earlier thaw date of frozen soils and the onset of the growing season in the spring by approximately 2-4 days from 1988 to 2000. Between 1988 and 2000, satellite records yield a slightly stronger trend in thaw and the onset of the growing season, averaging between 5 and 8 days earlier. In both, the TEM simulations and satellite records, trends in day of freeze in the autumn are weaker, such that overall increases in growing season length are due primarily to earlier thaw. Although regions with the longest snow cover duration displayed the greatest increase in growing season length, these regions maintained smaller increases in productivity and heterotrophic respiration than those regions with shorter duration of snow cover and less of an increase in growing season length. Concurrent with increases in growing season length, we found a reduction in soil C and increases in vegetation C, with greatest losses of soil C occurring in those areas with more vegetation, but simulations also suggest that this trend could reverse in the future. Our results reveal noteworthy changes in snow, permafrost, growing season length, productivity, and net C uptake, indicating that prediction of terrestrial C dynamics from one decade to the next will require that large-scale models adequately take into account the corresponding changes in soil thermal regimes. ?? 2006 Blackwell Publishing Ltd.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Global Change Biology","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1111/j.1365-2486.2006.01113.x","issn":"13541013","usgsCitation":"Euskirchen, E., McGuire, A., Kicklighter, D., Zhuang, Q., Clein, J.S., Dargaville, R., Dye, D., Kimball, J., McDonald, K., Melillo, J.M., Romanovsky, V., and Smith, N., 2006, Importance of recent shifts in soil thermal dynamics on growing season length, productivity, and carbon sequestration in terrestrial high-latitude ecosystems: Global Change Biology, v. 12, no. 4, p. 731-750, https://doi.org/10.1111/j.1365-2486.2006.01113.x.","startPage":"731","endPage":"750","numberOfPages":"20","costCenters":[],"links":[{"id":477437,"rank":10000,"type":{"id":41,"text":"Open Access External Repository Page"},"url":"https://hdl.handle.net/1912/909","text":"External Repository"},{"id":211760,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1111/j.1365-2486.2006.01113.x"},{"id":239111,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"12","issue":"4","noUsgsAuthors":false,"publicationDate":"2006-03-14","publicationStatus":"PW","scienceBaseUri":"505a3941e4b0c8380cd6186d","contributors":{"authors":[{"text":"Euskirchen, E.S.","contributorId":44737,"corporation":false,"usgs":true,"family":"Euskirchen","given":"E.S.","affiliations":[],"preferred":false,"id":427901,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"McGuire, A. D.","contributorId":16552,"corporation":false,"usgs":true,"family":"McGuire","given":"A. D.","affiliations":[],"preferred":false,"id":427896,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Kicklighter, D. W.","contributorId":31537,"corporation":false,"usgs":false,"family":"Kicklighter","given":"D. W.","affiliations":[{"id":13627,"text":"Woods Hole Oceanographic Institution, Woods Hole, MA","active":true,"usgs":false}],"preferred":false,"id":427898,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Zhuang, Q.","contributorId":40772,"corporation":false,"usgs":true,"family":"Zhuang","given":"Q.","email":"","affiliations":[],"preferred":false,"id":427899,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Clein, Joy S.","contributorId":83697,"corporation":false,"usgs":true,"family":"Clein","given":"Joy","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":427905,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Dargaville, R.J.","contributorId":41992,"corporation":false,"usgs":true,"family":"Dargaville","given":"R.J.","email":"","affiliations":[],"preferred":false,"id":427900,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Dye, D.G.","contributorId":14193,"corporation":false,"usgs":true,"family":"Dye","given":"D.G.","email":"","affiliations":[],"preferred":false,"id":427895,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Kimball, J.S.","contributorId":79141,"corporation":false,"usgs":true,"family":"Kimball","given":"J.S.","email":"","affiliations":[],"preferred":false,"id":427904,"contributorType":{"id":1,"text":"Authors"},"rank":8},{"text":"McDonald, K.C.","contributorId":89718,"corporation":false,"usgs":true,"family":"McDonald","given":"K.C.","email":"","affiliations":[],"preferred":false,"id":427906,"contributorType":{"id":1,"text":"Authors"},"rank":9},{"text":"Melillo, J. M.","contributorId":73139,"corporation":false,"usgs":false,"family":"Melillo","given":"J.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":427903,"contributorType":{"id":1,"text":"Authors"},"rank":10},{"text":"Romanovsky, V.E.","contributorId":54721,"corporation":false,"usgs":true,"family":"Romanovsky","given":"V.E.","email":"","affiliations":[],"preferred":false,"id":427902,"contributorType":{"id":1,"text":"Authors"},"rank":11},{"text":"Smith, N.V.","contributorId":27672,"corporation":false,"usgs":true,"family":"Smith","given":"N.V.","email":"","affiliations":[],"preferred":false,"id":427897,"contributorType":{"id":1,"text":"Authors"},"rank":12}]}}
,{"id":70171135,"text":"70171135 - 2006 - Comprehensive gene expression profiling following DNA vaccination of rainbow trout against infectious hematopoietic necrosis virus","interactions":[],"lastModifiedDate":"2016-05-23T15:42:38","indexId":"70171135","displayToPublicDate":"2006-01-01T00:00:00","publicationYear":"2006","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2777,"text":"Molecular Immunology","active":true,"publicationSubtype":{"id":10}},"title":"Comprehensive gene expression profiling following DNA vaccination of rainbow trout against infectious hematopoietic necrosis virus","docAbstract":"<p><span>The DNA vaccine based on the glycoprotein gene of&nbsp;</span><i>Infectious hematopoietic necrosis virus</i><span>&nbsp;induces a non-specific anti-viral immune response and long-term specific immunity against IHNV. This study characterized gene expression responses associated with the early anti-viral response. Homozygous rainbow trout were injected intra-muscularly (I.M.) with vector DNA or the IHNV DNA vaccine. Gene expression in muscle tissue (I.M. site) was evaluated using a 16,008 feature salmon cDNA microarray. Eighty different genes were significantly modulated in the vector DNA group while 910 genes were modulated in the IHNV DNA vaccinate group relative to control group. Quantitative reverse-transcriptase PCR was used to examine expression of selected immune genes at the I.M. site and in other secondary tissues. In the localized response (I.M. site), the magnitudes of gene expression changes were much greater in the vaccinate group relative to the vector DNA group for the majority of genes analyzed. At secondary systemic sites (e.g. gill, kidney and spleen), type I IFN-related genes were up-regulated in only the IHNV DNA vaccinated group. The results presented here suggest that the IHNV DNA vaccine induces up-regulation of the type I IFN system across multiple tissues, which is the functional basis of early anti-viral immunity.</span></p>","language":"English","publisher":"Elsevier","doi":"10.1016/j.molimm.2005.12.005","usgsCitation":"Purcell, M., Nichols, K.M., Winton, J.R., Kurath, G., Thorgaard, G.H., Wheeler, P., Hansen, J.D., Herwig, R.P., and Park, L.K., 2006, Comprehensive gene expression profiling following DNA vaccination of rainbow trout against infectious hematopoietic necrosis virus: Molecular Immunology, v. 43, no. 13, p. 2089-2106, https://doi.org/10.1016/j.molimm.2005.12.005.","productDescription":"18 p.","startPage":"2089","endPage":"2106","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":654,"text":"Western Fisheries Research Center","active":true,"usgs":true}],"links":[{"id":321523,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"43","issue":"13","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"574d6461e4b07e28b66836ce","contributors":{"authors":[{"text":"Purcell, Maureen K. mpurcell@usgs.gov","contributorId":138685,"corporation":false,"usgs":true,"family":"Purcell","given":"Maureen K.","email":"mpurcell@usgs.gov","affiliations":[{"id":654,"text":"Western Fisheries Research Center","active":true,"usgs":true}],"preferred":false,"id":630060,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Nichols, Krista M.","contributorId":169573,"corporation":false,"usgs":false,"family":"Nichols","given":"Krista","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":630061,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Winton, James R. 0000-0002-3505-5509 jwinton@usgs.gov","orcid":"https://orcid.org/0000-0002-3505-5509","contributorId":1944,"corporation":false,"usgs":true,"family":"Winton","given":"James","email":"jwinton@usgs.gov","middleInitial":"R.","affiliations":[{"id":654,"text":"Western Fisheries Research Center","active":true,"usgs":true}],"preferred":false,"id":630062,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Kurath, Gael 0000-0003-3294-560X gkurath@usgs.gov","orcid":"https://orcid.org/0000-0003-3294-560X","contributorId":2629,"corporation":false,"usgs":true,"family":"Kurath","given":"Gael","email":"gkurath@usgs.gov","affiliations":[{"id":654,"text":"Western Fisheries Research Center","active":true,"usgs":true}],"preferred":true,"id":630063,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Thorgaard, Gary H.","contributorId":60512,"corporation":false,"usgs":true,"family":"Thorgaard","given":"Gary","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":630064,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Wheeler, Paul","contributorId":169574,"corporation":false,"usgs":false,"family":"Wheeler","given":"Paul","email":"","affiliations":[{"id":24743,"text":"School of Biological Sciences, Washington State University, Pullman, WA 99164, USA","active":true,"usgs":false}],"preferred":false,"id":630065,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Hansen, John D. 0000-0002-3006-2734 jhansen@usgs.gov","orcid":"https://orcid.org/0000-0002-3006-2734","contributorId":3440,"corporation":false,"usgs":true,"family":"Hansen","given":"John","email":"jhansen@usgs.gov","middleInitial":"D.","affiliations":[{"id":654,"text":"Western Fisheries Research Center","active":true,"usgs":true}],"preferred":true,"id":630066,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Herwig, Russell P.","contributorId":169137,"corporation":false,"usgs":false,"family":"Herwig","given":"Russell","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":630067,"contributorType":{"id":1,"text":"Authors"},"rank":8},{"text":"Park, Linda K.","contributorId":28525,"corporation":false,"usgs":true,"family":"Park","given":"Linda","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":630068,"contributorType":{"id":1,"text":"Authors"},"rank":9}]}}
,{"id":70031055,"text":"70031055 - 2006 - Constraints on the mechanism of long-term, steady subsidence at Medicine Lake volcano, northern California, from GPS, leveling, and InSAR","interactions":[],"lastModifiedDate":"2019-04-15T10:07:35","indexId":"70031055","displayToPublicDate":"2006-01-01T00:00:00","publicationYear":"2006","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":"Constraints on the mechanism of long-term, steady subsidence at Medicine Lake volcano, northern California, from GPS, leveling, and InSAR","docAbstract":"<div class=\"abstract svAbstract \" data-etype=\"ab\"><p id=\"\">Leveling surveys across Medicine Lake volcano (MLV) have documented subsidence that is centered on the summit caldera and decays symmetrically on the flanks of the edifice. Possible mechanisms for this deformation include fluid withdrawal from a subsurface reservoir, cooling/crystallization of subsurface magma, loading by the volcano and dense intrusions, and crustal thinning due to tectonic extension (Dzurisin et al., 1991 [Dzurisin, D., Donnelly-Nolan, J.M., Evans, J.R., Walter, S.R., 1991. Crustal subsidence, seismicity, and structure near Medicine Lake Volcano, California. Journal of Geophysical Research 96, 16, 319-16, 333.]; Dzurisin et al., 2002 [Dzurisin, D., Poland, M.P., Bürgmann, R., 2002. Steady subsidence of Medicine Lake Volcano, Northern California, revealed by repeated leveling surveys. Journal of Geophysical Research 107, 2372, doi:10.1029/2001JB000893.]). InSAR data that approximate vertical displacements are similar to the leveling results; however, vertical deformation data alone are not sufficient to distinguish between source mechanisms. Horizontal displacements from GPS were collected in the Mt. Shasta/MLV region in 1996, 1999, 2000, 2003, and 2004. These results suggest that the region is part of the western Oregon block that is rotating about an Euler pole in eastern Oregon. With this rotation removed, most sites in the network have negligible velocities except for those near MLV caldera. There, measured horizontal velocities are less than predicted from ∼10 km deep point and dislocation sources of volume loss based on the leveling data; therefore volumetric losses simulated by these sources are probably not causing the observed subsidence at MLV. This result demonstrates that elastic models of subsurface volume change can provide misleading results where additional geophysical and geological constraints are unavailable, or if only vertical deformation is known. The deformation source must be capable of causing broad vertical deformation with comparatively smaller horizontal displacements. Thermoelastic contraction of a column of hot rock beneath the volcano cannot reproduce the observed ratio of vertical to horizontal surface displacements. Models that determine deformation due to loading by the volcano and dense intrusions can be made to fit the pattern of vertical displacements by assuming a weak upper crust beneath MLV, though the subsidence rates due to surface loading must be lower than the observed displacements. Tectonic extension is almost certainly occurring based on fault orientations and focal mechanisms, but does not appear to be a major contributor to the observed deformation. We favor a model that includes a combination of sources, including extension and loading of a hot weak crust with thermal contraction of a cooling mass of rock beneath MLV, which are processes that are probably occurring at MLV. Future microgravity surveys and the planned deployment of an array of continuous GPS stations as part of a Plate Boundary Observatory volcano cluster will help to refine this model.</p></div>","language":"English","publisher":"Elsevier","doi":"10.1016/j.jvolgeores.2005.07.007","issn":"03770273","usgsCitation":"Poland, M.P., Burgmann, R., Dzurisin, D., Lisowski, M., Masterlark, T., Owen, S., and Fink, J., 2006, Constraints on the mechanism of long-term, steady subsidence at Medicine Lake volcano, northern California, from GPS, leveling, and InSAR: Journal of Volcanology and Geothermal Research, v. 150, no. 1-3, p. 55-78, https://doi.org/10.1016/j.jvolgeores.2005.07.007.","productDescription":"24 p.","startPage":"55","endPage":"78","numberOfPages":"24","costCenters":[{"id":222,"text":"Earth Resources Observation and Science (EROS) Center","active":true,"usgs":true},{"id":336,"text":"Hawaiian Volcano Observatory","active":false,"usgs":true},{"id":615,"text":"Volcano Hazards Program","active":true,"usgs":true}],"links":[{"id":238540,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"California","otherGeospatial":"Medicine Lake volcano","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -121.9921875,\n              41.265420628926684\n            ],\n            [\n              -121.9921875,\n              41.96357478222518\n            ],\n            [\n              -121.12152099609375,\n              41.96357478222518\n            ],\n            [\n              -121.12152099609375,\n              41.265420628926684\n            ],\n            [\n              -121.9921875,\n              41.265420628926684\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"150","issue":"1-3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059fa0fe4b0c8380cd4d8f1","contributors":{"authors":[{"text":"Poland, Michael P. 0000-0001-5240-6123 mpoland@usgs.gov","orcid":"https://orcid.org/0000-0001-5240-6123","contributorId":127857,"corporation":false,"usgs":true,"family":"Poland","given":"Michael","email":"mpoland@usgs.gov","middleInitial":"P.","affiliations":[{"id":617,"text":"Volcano Science Center","active":true,"usgs":true}],"preferred":false,"id":429846,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Burgmann, Roland","contributorId":95128,"corporation":false,"usgs":true,"family":"Burgmann","given":"Roland","affiliations":[],"preferred":false,"id":429845,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Dzurisin, Daniel 0000-0002-0138-5067 dzurisin@usgs.gov","orcid":"https://orcid.org/0000-0002-0138-5067","contributorId":538,"corporation":false,"usgs":true,"family":"Dzurisin","given":"Daniel","email":"dzurisin@usgs.gov","affiliations":[{"id":617,"text":"Volcano Science Center","active":true,"usgs":true}],"preferred":true,"id":429850,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Lisowski, Michael 0000-0003-4818-2504 mlisowski@usgs.gov","orcid":"https://orcid.org/0000-0003-4818-2504","contributorId":637,"corporation":false,"usgs":true,"family":"Lisowski","given":"Michael","email":"mlisowski@usgs.gov","affiliations":[{"id":615,"text":"Volcano Hazards Program","active":true,"usgs":true},{"id":617,"text":"Volcano Science Center","active":true,"usgs":true}],"preferred":true,"id":429849,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Masterlark, Timothy","contributorId":92829,"corporation":false,"usgs":false,"family":"Masterlark","given":"Timothy","email":"","affiliations":[{"id":35607,"text":"South Dakota School of Mines","active":true,"usgs":false}],"preferred":false,"id":429851,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Owen, Susan","contributorId":29004,"corporation":false,"usgs":true,"family":"Owen","given":"Susan","affiliations":[],"preferred":false,"id":429847,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Fink, Jonathan","contributorId":58456,"corporation":false,"usgs":false,"family":"Fink","given":"Jonathan","affiliations":[{"id":6607,"text":"Arizona State University","active":true,"usgs":false}],"preferred":false,"id":429848,"contributorType":{"id":1,"text":"Authors"},"rank":7}]}}
,{"id":70030600,"text":"70030600 - 2006 - An evaluation of factors influencing pore pressure in accretionary complexes: Implications for taper angle and wedge mechanics","interactions":[],"lastModifiedDate":"2012-03-12T17:21:05","indexId":"70030600","displayToPublicDate":"2006-01-01T00:00:00","publicationYear":"2006","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2314,"text":"Journal of Geophysical Research B: Solid Earth","active":true,"publicationSubtype":{"id":10}},"title":"An evaluation of factors influencing pore pressure in accretionary complexes: Implications for taper angle and wedge mechanics","docAbstract":"At many subduction zones, accretionary complexes form as sediment is off-scraped from the subducting plate. Mechanical models that treat accretionary complexes as critically tapered wedges of sediment demonstrate that pore pressure controls their taper angle by modifying basal and internal shear strength. Here, we combine a numerical model of groundwater flow with critical taper theory to quantify the effects of sediment and de??collement permeability, sediment thickness, sediment partitioning between accretion and underthrusting, and plate convergence rate on steady state pore pressure. Our results show that pore pressure in accretionary wedges can be viewed as a dynamically maintained response to factors which drive pore pressure (source terms) and those that limit flow (permeability and drainage path length). We find that sediment permeability and incoming sediment thickness are the most important factors, whereas fault permeability and the partitioning of sediment have a small effect. For our base case model scenario, as sediment permeability is increased, pore pressure decreases from near-lithostatic to hydrostatic values and allows stable taper angles to increase from ??? 2.5?? to 8??-12.5??. With increased sediment thickness in our models (from 100 to 8000 m), increased pore pressure drives a decrease in stable taper angle from 8.4??-12.5?? to <2.5-5??. In general, low-permeability and thick incoming sediment sustain high pore pressures consistent with shallowly tapered geometry, whereas high-permeability and thin incoming sediment should result in steep geometry. Our model results compare favorably with available data from active accretionary complexes. Active margins characterized by a significant proportion of fine-grained sediment within the incoming section, such as northern Antilles and eastern Nankai, exhibit thin taper angles, whereas those characterized by a higher proportion of sandy turbidites, such as Cascadia, Chile, and Mexico, have steep taper angles. Observations from active margins also indicate a strong trend of decreasing taper angle (from >15?? to <4??) with increased sediment thickness (from <1 to 7 km). One key implication is that hydrologic properties may strongly influence the strength of the crust in a wide range of geologic settings. Copyright 2006 by the American Geophysical Union.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Journal of Geophysical Research B: Solid Earth","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1029/2005JB003990","issn":"01480227","usgsCitation":"Saffer, D., and Bekins, B., 2006, An evaluation of factors influencing pore pressure in accretionary complexes: Implications for taper angle and wedge mechanics: Journal of Geophysical Research B: Solid Earth, v. 111, no. 4, https://doi.org/10.1029/2005JB003990.","costCenters":[],"links":[{"id":477417,"rank":10000,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1029/2005jb003990","text":"Publisher Index Page"},{"id":211961,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1029/2005JB003990"},{"id":239351,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"111","issue":"4","noUsgsAuthors":false,"publicationDate":"2006-04-04","publicationStatus":"PW","scienceBaseUri":"5059ea4be4b0c8380cd4876d","contributors":{"authors":[{"text":"Saffer, D.M.","contributorId":72945,"corporation":false,"usgs":true,"family":"Saffer","given":"D.M.","email":"","affiliations":[],"preferred":false,"id":427802,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bekins, B.A.","contributorId":98309,"corporation":false,"usgs":true,"family":"Bekins","given":"B.A.","email":"","affiliations":[],"preferred":false,"id":427803,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":1016477,"text":"1016477 - 2006 - GIS-based niche modeling for mapping species' habitats","interactions":[],"lastModifiedDate":"2012-02-02T00:04:42","indexId":"1016477","displayToPublicDate":"2006-01-01T00:00:00","publicationYear":"2006","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1465,"text":"Ecology","active":true,"publicationSubtype":{"id":10}},"title":"GIS-based niche modeling for mapping species' habitats","docAbstract":"Ecological a??niche modelinga?? using presence-only locality data and large-scale environmental variables provides a powerful tool for identifying and mapping suitable habitat for species over large spatial extents. We describe a niche modeling approach that identifies a minimum (rather than an optimum) set of basic habitat requirements for a species, based on the assumption that constant environmental relationships in a species' distribution (i.e., variables that maintain a consistent value where the species occurs) are most likely to be associated with limiting factors. Environmental variables that take on a wide range of values where a species occurs are less informative because they do not limit a species' distribution, at least over the range of variation sampled. This approach is operationalized by partitioning Mahalanobis D2 (standardized difference between values of a set of environmental variables for any point and mean values for those same variables calculated from all points at which a species was detected) into independent components. The smallest of these components represents the linear combination of variables with minimum variance; increasingly larger components represent larger variances and are increasingly less limiting. We illustrate this approach using the California Gnatcatcher (Polioptila californica Brewster) and provide SAS code to implement it.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Ecology","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","usgsCitation":"Rotenberry, J., Preston, K., and Knick, S., 2006, GIS-based niche modeling for mapping species' habitats: Ecology, v. 87, no. 6, p. 1458-1464.","productDescription":"p. 1458-1464","startPage":"1458","endPage":"1464","numberOfPages":"7","costCenters":[{"id":290,"text":"Forest and Rangeland Ecosystem Science Center","active":false,"usgs":true}],"links":[{"id":133175,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"87","issue":"6","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b30e4b07f02db6b40af","contributors":{"authors":[{"text":"Rotenberry, J.T.","contributorId":57015,"corporation":false,"usgs":true,"family":"Rotenberry","given":"J.T.","affiliations":[],"preferred":false,"id":324284,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Preston, K.L.","contributorId":68689,"corporation":false,"usgs":true,"family":"Preston","given":"K.L.","email":"","affiliations":[],"preferred":false,"id":324285,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Knick, S.","contributorId":33676,"corporation":false,"usgs":true,"family":"Knick","given":"S.","email":"","affiliations":[],"preferred":false,"id":324283,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70031166,"text":"70031166 - 2006 - Iron isotope fractionation during microbially stimulated Fe(II) oxidation and Fe(III) precipitation","interactions":[],"lastModifiedDate":"2012-03-12T17:21:17","indexId":"70031166","displayToPublicDate":"2006-01-01T00:00:00","publicationYear":"2006","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":"Iron isotope fractionation during microbially stimulated Fe(II) oxidation and Fe(III) precipitation","docAbstract":"Interpretation of the origins of iron-bearing minerals preserved in modern and ancient rocks based on measured iron isotope ratios depends on our ability to distinguish between biological and non-biological iron isotope fractionation processes. In this study, we compared 56Fe/54Fe ratios of coexisting aqueous iron (Fe(II)aq, Fe(III)aq) and iron oxyhydroxide precipitates (Fe(III)ppt) resulting from the oxidation of ferrous iron under experimental conditions at low pH (<3). Experiments were carried out using both pure cultures of Acidothiobacillus ferrooxidans and sterile controls to assess possible biological overprinting of non-biological fractionation, and both SO42- and Cl- salts as Fe(II) sources to determine possible ionic/speciation effects that may be associated with oxidation/precipitation reactions. In addition, a series of ferric iron precipitation experiments were performed at pH ranging from 1.9 to 3.5 to determine if different precipitation rates cause differences in the isotopic composition of the iron oxyhydroxides. During microbially stimulated Fe(II) oxidation in both the sulfate and chloride systems, 56Fe/54Fe ratios of residual Fe(II)aq sampled in a time series evolved along an apparent Rayleigh trend characterized by a fractionation factor ??Fe(III)aq-Fe(II)aq???1.0022. This fractionation factor was significantly less than that measured in our sterile control experiments (???1.0034) and that predicted for isotopic equilibrium between Fe(II)aq and Fe(III)aq (???1.0029), and thus might be interpreted to reflect a biological isotope effect. However, in our biological experiments the measured difference in 56Fe/54Fe ratios between Fe(III)aq, isolated as a solid by the addition of NaOH to the final solution at each time point under N2-atmosphere, and Fe(II)aq was in most cases and on average close to 2.9??? (??Fe(III)aq-Fe(II)aq ???1.0029), consistent with isotopic equilibrium between Fe(II)aq and Fe(III)aq. The ferric iron precipitation experiments revealed that 56Fe/54Fe ratios of Fe(III)aq were generally equal to or greater than those of Fe(III)ppt, and isotopic fractionation between these phases decreased with increasing precipitation rate and decreasing grain size. Considered together, the data confirm that the iron isotope variations observed in our microbial experiments are primarily controlled by non-biological equilibrium and kinetic factors, a result that aids our ability to interpret present-day iron cycling processes but further complicates our ability to use iron isotopes alone to identify biological processing in the rock record. ?? 2005 Elsevier Inc. All rights reserved.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Geochimica et Cosmochimica Acta","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1016/j.gca.2005.09.025","issn":"00167037","usgsCitation":"Balci, N., Bullen, T., Witte-Lien, K., Shanks, W., Motelica, M., and Mandernack, K., 2006, Iron isotope fractionation during microbially stimulated Fe(II) oxidation and Fe(III) precipitation: Geochimica et Cosmochimica Acta, v. 70, no. 3, p. 622-639, https://doi.org/10.1016/j.gca.2005.09.025.","startPage":"622","endPage":"639","numberOfPages":"18","costCenters":[],"links":[{"id":238751,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":211459,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1016/j.gca.2005.09.025"}],"volume":"70","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a3eece4b0c8380cd6414b","contributors":{"authors":[{"text":"Balci, N.","contributorId":15005,"corporation":false,"usgs":true,"family":"Balci","given":"N.","email":"","affiliations":[],"preferred":false,"id":430330,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bullen, T.D.","contributorId":79911,"corporation":false,"usgs":true,"family":"Bullen","given":"T.D.","email":"","affiliations":[],"preferred":false,"id":430333,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Witte-Lien, K.","contributorId":84973,"corporation":false,"usgs":true,"family":"Witte-Lien","given":"K.","email":"","affiliations":[],"preferred":false,"id":430334,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Shanks, Wayne C.","contributorId":39419,"corporation":false,"usgs":true,"family":"Shanks","given":"Wayne C.","affiliations":[],"preferred":false,"id":430331,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Motelica, M.","contributorId":92488,"corporation":false,"usgs":true,"family":"Motelica","given":"M.","email":"","affiliations":[],"preferred":false,"id":430335,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Mandernack, K.W.","contributorId":68913,"corporation":false,"usgs":true,"family":"Mandernack","given":"K.W.","email":"","affiliations":[],"preferred":false,"id":430332,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}}
,{"id":70031046,"text":"70031046 - 2006 - Trace element geochemistry and surface water chemistry of the Bon Air coal, Franklin County, Cumberland Plateau, southeast Tennessee","interactions":[],"lastModifiedDate":"2012-03-12T17:21:15","indexId":"70031046","displayToPublicDate":"2006-01-01T00:00:00","publicationYear":"2006","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2033,"text":"International Journal of Coal Geology","active":true,"publicationSubtype":{"id":10}},"title":"Trace element geochemistry and surface water chemistry of the Bon Air coal, Franklin County, Cumberland Plateau, southeast Tennessee","docAbstract":"Mean contents of trace elements and ash in channel, bench-column, and dump samples of the abandoned Bon Air coal (Lower Pennsylvanian) in Franklin County, Tennessee are similar to Appalachian COALQUAL mean values, but are slightly lower for As, Fe, Hg, Mn, Na, Th, and U, and slightly higher for ash, Be, Cd, Co, Cr, REEs, Sr, and V, at the 95% confidence level. Compared to channel samples, dump sample means are slightly lower in chalcophile elements (As, Cu, Fe, Ni, Pb, S, Sb, and V) and slightly higher in clay or heavy-mineral elements (Al, K, Mn, REEs, Th, Ti, U, and Y), but at the 95% confidence level, only As and Fe are different. Consistent abundances of clay or heavy-mineral elements in low-Br, high-S, high-ash benches that are relatively enriched in quartz and mire-to-levee species like Paralycopodites suggest trace elements are largely fluvial in origin. Factor analysis loadings and correlation coefficients between elements suggest that clays host most Al, Cr, K, Ti, and Th, significant Mn and V, and some Sc, U, Ba, and Ni. Heavy accessory minerals likely house most REEs and Y, lesser Sc, U, and Th, and minor Cr, Ni, and Ti. Pyrite appears to host As, some V and Ni, and perhaps some Cu, but Cu probably exists largely as chalcopyrite. Data suggest that organic debris houses most Be and some Ni and U, and that Pb and Sb occur as Pb-Sb sulfosalt(s) within organic matrix. Most Hg, and some Mn and Y, appear to be hosted by calcite, suggesting potential Hg remobilization from original pyrite, and Hg sorption by calcite, which may be important processes in abandoned coals. Most Co, Zn, Mo, and Cd, significant V and Ni, and some Mn probably occur in non-pyritic sulfides; Ba, Sr, and P are largely in crandallite-group phosphates. Selenium does not show organic or \"clausthalite\" affinities, but Se occurrence is otherwise unclear. Barium, Mn, Ni, Sc, U, and V, with strongly divided statistical affinities, likely occur subequally in multiple modes. For study area surface waters, highest levels of most trace elements occur in mine-adit or mine-dump drainage. Effluent flow rates strongly affect both acidity and trace element levels. Adit drainages where flow is only a trickle have the most acidic waters (pH 3.78-4.80) and highest trace element levels (up to two orders of magnitude higher than in non-mine site waters). Nonetheless, nearly all surface waters have low absolute concentrations of trace elements of environmental concern, and all waters sampled meet U.S. EPA primary drinking water standards and aquatic life criteria for all elements analyzed. Secondary drinking water standards are also met for all parameters except Al, pH, Fe, and Mn, but even in extreme cases (mine waters with pH as low as 3.78 and up to 1243 ppb Al, 6280 ppb Fe, and 721 ppb Mn, and non-mine dam-outflow waters with up to 18,400 ppb Fe and 1540 ppb Mn) downslope attenuation is apparently rapid, as down-drainage plateau-base streams show background levels for all these parameters. ?? 2005 Elsevier B.V. All rights reserved.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"International Journal of Coal Geology","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1016/j.coal.2005.08.005","issn":"01665162","usgsCitation":"Shaver, S., Hower, J., Eble, C., McLamb, E., and Kuers, K., 2006, Trace element geochemistry and surface water chemistry of the Bon Air coal, Franklin County, Cumberland Plateau, southeast Tennessee: International Journal of Coal Geology, v. 67, no. 1-2, p. 47-78, https://doi.org/10.1016/j.coal.2005.08.005.","startPage":"47","endPage":"78","numberOfPages":"32","costCenters":[],"links":[{"id":238907,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":211593,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1016/j.coal.2005.08.005"}],"volume":"67","issue":"1-2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505bb63be4b08c986b326b4c","contributors":{"authors":[{"text":"Shaver, S.A.","contributorId":34719,"corporation":false,"usgs":true,"family":"Shaver","given":"S.A.","email":"","affiliations":[],"preferred":false,"id":429761,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hower, J.C.","contributorId":100541,"corporation":false,"usgs":true,"family":"Hower","given":"J.C.","email":"","affiliations":[],"preferred":false,"id":429765,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Eble, C.F.","contributorId":35346,"corporation":false,"usgs":true,"family":"Eble","given":"C.F.","email":"","affiliations":[],"preferred":false,"id":429762,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"McLamb, E.D.","contributorId":94093,"corporation":false,"usgs":true,"family":"McLamb","given":"E.D.","email":"","affiliations":[],"preferred":false,"id":429764,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Kuers, K.","contributorId":70183,"corporation":false,"usgs":true,"family":"Kuers","given":"K.","email":"","affiliations":[],"preferred":false,"id":429763,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":70031094,"text":"70031094 - 2006 - Timing of Cenozoic volcanism and Basin and Range extension in northwestern Nevada: New constraints from the northern Pine Forest Range","interactions":[],"lastModifiedDate":"2012-03-12T17:21:17","indexId":"70031094","displayToPublicDate":"2006-01-01T00:00:00","publicationYear":"2006","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1786,"text":"Geological Society of America Bulletin","active":true,"publicationSubtype":{"id":10}},"title":"Timing of Cenozoic volcanism and Basin and Range extension in northwestern Nevada: New constraints from the northern Pine Forest Range","docAbstract":"Eocene-middle Miocene volcanic rocks in the northern Pine Forest Range, Nevada, are ideally situated for reconstructing the timing and style of volcanism and extensional faulting in the northwesternmost part of the Basin and Range province. A conformable sequence of Cenozoic volcanic and sedimentary strata in the northern Pine Forest Range dips ???30??W, and 11 new 40Ar/39Ar ages from this sequence define 3 major episodes of volcanic activity. Pre-Tertiary basement and older (ca. 38 Ma) Tertiary intrusive rocks are overlain unconformably by Oligocene (ca. 30-23 Ma) basalt flows and dacitic to rhyolitic ash-flow tuffs interbedded with fine-grained tuffaceous sedimentary rocks. Oligocene rocks are overlain by ???550 m of ca. 17-16 Ma basalt flows equivalent to the Steens Basalt in southern Oregon, and basalt flows are capped by a thin 16.3 Ma ignimbrite that likely is correlative with either the Idaho Canyon Tuff or the Tuff of Oregon Canyon. The northern Pine Forest Range is bounded to the east by a major down-to-the-east normal fault that dips ???40??E with well-developed fault striations indicative of dip-slip motion. This fault initiated at an angle of ???70?? and was rotated ???30?? during uplift of the range. A suite of 17 apatite fission-track ages from the Pine Forest footwall block demonstrates that exhumation, uplift, and slip on the range-bounding fault began ca. 12-11 Ma and continued until at least 7 Ma, with moderate slip since then. The Pine Forest Range did not undergo significant extension before or during peak Oligocene and Miocene volcanism, and similar geologic relationships in nearby ranges suggest that a larger region of northwestern Nevada was also little extended during this interval. Basin and Range faulting in northwestern Nevada appears to have begun no earlier than 12 Ma, making it distinctly younger than deformation in much of central and southern Nevada, where peak extension occurred in the middle Miocene or earlier. ?? 2006 Geological Society of America.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Geological Society of America Bulletin","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1130/B25681.1","issn":"00167606","usgsCitation":"Colgan, J., Dumitru, T., McWilliams, M., and Miller, E.L., 2006, Timing of Cenozoic volcanism and Basin and Range extension in northwestern Nevada: New constraints from the northern Pine Forest Range: Geological Society of America Bulletin, v. 118, no. 1-2, p. 126-139, https://doi.org/10.1130/B25681.1.","startPage":"126","endPage":"139","numberOfPages":"14","costCenters":[],"links":[{"id":211367,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1130/B25681.1"},{"id":238646,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"118","issue":"1-2","noUsgsAuthors":false,"publicationDate":"2006-01-06","publicationStatus":"PW","scienceBaseUri":"505bb3ebe4b08c986b326071","contributors":{"authors":[{"text":"Colgan, J.P.","contributorId":71678,"corporation":false,"usgs":true,"family":"Colgan","given":"J.P.","affiliations":[],"preferred":false,"id":429991,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Dumitru, T.A.","contributorId":24973,"corporation":false,"usgs":true,"family":"Dumitru","given":"T.A.","affiliations":[],"preferred":false,"id":429989,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"McWilliams, M.","contributorId":39121,"corporation":false,"usgs":true,"family":"McWilliams","given":"M.","email":"","affiliations":[],"preferred":false,"id":429990,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Miller, E. L.","contributorId":75583,"corporation":false,"usgs":true,"family":"Miller","given":"E.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":429992,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70030794,"text":"70030794 - 2006 - Cosmogenic 10Be and 26Al exposure ages of tors and erratics, Cairngorm Mountains, Scotland: Timescales for the development of a classic landscape of selective linear glacial erosion","interactions":[],"lastModifiedDate":"2012-03-12T17:21:20","indexId":"70030794","displayToPublicDate":"2006-01-01T00:00:00","publicationYear":"2006","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1801,"text":"Geomorphology","active":true,"publicationSubtype":{"id":10}},"title":"Cosmogenic 10Be and 26Al exposure ages of tors and erratics, Cairngorm Mountains, Scotland: Timescales for the development of a classic landscape of selective linear glacial erosion","docAbstract":"The occurrence of tors within glaciated regions has been widely cited as evidence for the preservation of relic pre-Quaternary landscapes beneath protective covers of non-erosive dry-based ice. Here, we test for the preservation of pre-Quaternary landscapes with cosmogenic surface exposure dating of tors. Numerous granite tors are present on summit plateaus in the Cairngorm Mountains of Scotland where they were covered by local ice caps many times during the Pleistocene. Cosmogenic 10Be and 26Al data together with geomorphic relationships reveal that these landforms are more dynamic and younger than previously suspected. Many Cairngorm tors have been bulldozed and toppled along horizontal joints by ice motion, leaving event surfaces on tor remnants and erratics that can be dated with cosmogenic nuclides. As the surfaces have been subject to episodic burial by ice, an exposure model based upon ice and marine sediment core proxies for local glacial cover is necessary to interpret the cosmogenic nuclide data. Exposure ages and weathering characteristics of tors are closely correlated. Glacially modified tors and boulder erratics with slightly weathered surfaces have 10Be exposure ages of about 15 to 43 ka. Nuclide inheritance is present in many of these surfaces. Correction for inheritance indicates that the eastern Cairngorms were deglaciated at 15.6 ?? 0.9 ka. Glacially modified tors with moderate to advanced weathering features have 10Be exposure ages of 19 to 92 ka. These surfaces were only slightly modified during the last glacial cycle and gained much of their exposure during the interstadial of marine Oxygen Isotope Stage 5 or earlier. Tors lacking evidence of glacial modification and exhibiting advanced weathering have 10Be exposure ages between 52 and 297 ka. Nuclide concentrations in these surfaces are probably controlled by bedrock erosion rates instead of discrete glacial events. Maximum erosion rates estimated from 10Be range from 2.8 to 12.0 mm/ka, with an error weighted mean of 4.1 ?? 0.2 mm/ka. Three of these surfaces yield model exposure-plus-burial ages of 295-71+84, 520-141+178, and 626-85+102 ka. A vertical cosmogenic nuclide profile across the oldest sampled tor indicates a long-term emergence rate of 31 ?? 2 mm/ka. These findings show that dry-based ice caps are capable of substantially eroding tors by entraining blocks previously detached by weathering processes. Bedrock surfaces and erratic boulders in such settings are likely to have nuclide inheritance and may yield erroneous (too old) exposure ages. While many Cairngorm tors have survived multiple glacial cycles, rates of regolith stripping and bedrock erosion are too high to permit the widespread preservation of pre-Quaternary rock surfaces. ?? 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.2005.06.009","issn":"0169555X","usgsCitation":"Phillips, W., Hall, A., Mottram, R., Fifield, L., and Sugden, D., 2006, Cosmogenic 10Be and 26Al exposure ages of tors and erratics, Cairngorm Mountains, Scotland: Timescales for the development of a classic landscape of selective linear glacial erosion: Geomorphology, v. 73, no. 3-4, p. 222-245, https://doi.org/10.1016/j.geomorph.2005.06.009.","startPage":"222","endPage":"245","numberOfPages":"24","costCenters":[],"links":[{"id":211383,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1016/j.geomorph.2005.06.009"},{"id":238663,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"73","issue":"3-4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059fc5ee4b0c8380cd4e259","contributors":{"authors":[{"text":"Phillips, W.M.","contributorId":49332,"corporation":false,"usgs":true,"family":"Phillips","given":"W.M.","email":"","affiliations":[],"preferred":false,"id":428717,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hall, A.M.","contributorId":40400,"corporation":false,"usgs":true,"family":"Hall","given":"A.M.","email":"","affiliations":[],"preferred":false,"id":428715,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Mottram, R.","contributorId":63609,"corporation":false,"usgs":true,"family":"Mottram","given":"R.","affiliations":[],"preferred":false,"id":428718,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Fifield, L.K.","contributorId":47575,"corporation":false,"usgs":true,"family":"Fifield","given":"L.K.","email":"","affiliations":[],"preferred":false,"id":428716,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Sugden, D.E.","contributorId":80072,"corporation":false,"usgs":true,"family":"Sugden","given":"D.E.","email":"","affiliations":[],"preferred":false,"id":428719,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":70031060,"text":"70031060 - 2006 - The quest for the perfect gravity anomaly: Part 1 - New calculation standards","interactions":[],"lastModifiedDate":"2012-03-12T17:21:17","indexId":"70031060","displayToPublicDate":"2006-01-01T00:00:00","publicationYear":"2006","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3317,"text":"SEG Technical Program Expanded Abstracts","active":true,"publicationSubtype":{"id":10}},"title":"The quest for the perfect gravity anomaly: Part 1 - New calculation standards","docAbstract":"The North American gravity database together with databases from Canada, Mexico, and the United States are being revised to improve their coverage, versatility, and accuracy. An important part of this effort is revision of procedures and standards for calculating gravity anomalies taking into account our enhanced computational power, modern satellite-based positioning technology, improved terrain databases, and increased interest in more accurately defining different anomaly components. The most striking revision is the use of one single internationally accepted reference ellipsoid for the horizontal and vertical datums of gravity stations as well as for the computation of the theoretical gravity. The new standards hardly impact the interpretation of local anomalies, but do improve regional anomalies. Most importantly, such new standards can be consistently applied to gravity database compilations of nations, continents, and even the entire world. ?? 2005 Society of Exploration Geophysicists.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"SEG Technical Program Expanded Abstracts","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1190/1.2370391","issn":"10523812","usgsCitation":"Li, X., Hildenbrand, T., Hinze, W.J., Keller, G.R., Ravat, D., and Webring, M., 2006, The quest for the perfect gravity anomaly: Part 1 - New calculation standards: SEG Technical Program Expanded Abstracts, v. 25, no. 1, p. 859-863, https://doi.org/10.1190/1.2370391.","startPage":"859","endPage":"863","numberOfPages":"5","costCenters":[],"links":[{"id":211365,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1190/1.2370391"},{"id":238644,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"25","issue":"1","noUsgsAuthors":false,"publicationDate":"2006-10-06","publicationStatus":"PW","scienceBaseUri":"505baeeae4b08c986b324414","contributors":{"authors":[{"text":"Li, X.","contributorId":67635,"corporation":false,"usgs":true,"family":"Li","given":"X.","email":"","affiliations":[],"preferred":false,"id":429869,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hildenbrand, T.G.","contributorId":83892,"corporation":false,"usgs":true,"family":"Hildenbrand","given":"T.G.","email":"","affiliations":[],"preferred":false,"id":429871,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Hinze, W. J.","contributorId":52607,"corporation":false,"usgs":false,"family":"Hinze","given":"W.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":429868,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Keller, Gordon R.","contributorId":90280,"corporation":false,"usgs":true,"family":"Keller","given":"Gordon","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":429872,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Ravat, D.","contributorId":102971,"corporation":false,"usgs":true,"family":"Ravat","given":"D.","email":"","affiliations":[],"preferred":false,"id":429873,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Webring, M.","contributorId":67662,"corporation":false,"usgs":true,"family":"Webring","given":"M.","affiliations":[],"preferred":false,"id":429870,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}}
,{"id":70030798,"text":"70030798 - 2006 - Relationships between avian richness and landscape structure at multiple scales using multiple landscapes","interactions":[],"lastModifiedDate":"2012-03-12T17:21:19","indexId":"70030798","displayToPublicDate":"2006-01-01T00:00:00","publicationYear":"2006","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":"Relationships between avian richness and landscape structure at multiple scales using multiple landscapes","docAbstract":"Little is known about factors that structure biodiversity on landscape scales, yet current land management protocols, such as forest certification programs, place an increasing emphasis on managing for sustainable biodiversity at landscape scales. We used a replicated landscape study to evaluate relationships between forest structure and avian diversity at both stand and landscape-levels. We used data on bird communities collected under comparable sampling protocols on four managed forests located across the Southeastern US to develop logistic regression models describing relationships between habitat factors and the distribution of overall richness and richness of selected guilds. Landscape models generated for eight of nine guilds showed a strong relationship between richness and both availability and configuration of landscape features. Diversity of topographic features and heterogeneity of forest structure were primary determinants of avian species richness. Forest heterogeneity, in both age and forest type, were strongly and positively associated with overall avian richness and richness for most guilds. Road density was associated positively but weakly with avian richness. Landscape variables dominated all models generated, but no consistent patterns in metrics or scale were evident. Model fit was strong for neotropical migrants and relatively weak for short-distance migrants and resident species. Our models provide a tool that will allow managers to evaluate and demonstrate quantitatively how management practices affect avian diversity on landscapes.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Forest Ecology and Management","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1016/j.foreco.2005.09.023","issn":"03781127","usgsCitation":"Mitchell, M., Rutzmoser, S., Wigley, T., Loehle, C., Gerwin, J., Keyser, P., Lancia, R., Perry, R., Reynolds, C., Thill, R., Weih, R., White, D., and Wood, P., 2006, Relationships between avian richness and landscape structure at multiple scales using multiple landscapes: Forest Ecology and Management, v. 221, no. 1-3, p. 155-169, https://doi.org/10.1016/j.foreco.2005.09.023.","startPage":"155","endPage":"169","numberOfPages":"15","costCenters":[],"links":[{"id":211437,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1016/j.foreco.2005.09.023"},{"id":238727,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"221","issue":"1-3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"50e4a793e4b0e8fec6cdc4f0","contributors":{"authors":[{"text":"Mitchell, M.S.","contributorId":26724,"corporation":false,"usgs":true,"family":"Mitchell","given":"M.S.","email":"","affiliations":[],"preferred":false,"id":428732,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Rutzmoser, S.H.","contributorId":68951,"corporation":false,"usgs":true,"family":"Rutzmoser","given":"S.H.","email":"","affiliations":[],"preferred":false,"id":428739,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Wigley, T.B.","contributorId":67254,"corporation":false,"usgs":true,"family":"Wigley","given":"T.B.","email":"","affiliations":[],"preferred":false,"id":428738,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Loehle, C.","contributorId":92823,"corporation":false,"usgs":true,"family":"Loehle","given":"C.","email":"","affiliations":[],"preferred":false,"id":428742,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Gerwin, J.A.","contributorId":88149,"corporation":false,"usgs":true,"family":"Gerwin","given":"J.A.","email":"","affiliations":[],"preferred":false,"id":428741,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Keyser, P.D.","contributorId":20857,"corporation":false,"usgs":true,"family":"Keyser","given":"P.D.","email":"","affiliations":[],"preferred":false,"id":428731,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Lancia, R.A.","contributorId":42327,"corporation":false,"usgs":true,"family":"Lancia","given":"R.A.","email":"","affiliations":[],"preferred":false,"id":428734,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Perry, R.W.","contributorId":43947,"corporation":false,"usgs":true,"family":"Perry","given":"R.W.","email":"","affiliations":[],"preferred":false,"id":428735,"contributorType":{"id":1,"text":"Authors"},"rank":8},{"text":"Reynolds, C.J.","contributorId":69779,"corporation":false,"usgs":true,"family":"Reynolds","given":"C.J.","email":"","affiliations":[],"preferred":false,"id":428740,"contributorType":{"id":1,"text":"Authors"},"rank":9},{"text":"Thill, R.E.","contributorId":46727,"corporation":false,"usgs":true,"family":"Thill","given":"R.E.","email":"","affiliations":[],"preferred":false,"id":428736,"contributorType":{"id":1,"text":"Authors"},"rank":10},{"text":"Weih, R.","contributorId":56028,"corporation":false,"usgs":true,"family":"Weih","given":"R.","email":"","affiliations":[],"preferred":false,"id":428737,"contributorType":{"id":1,"text":"Authors"},"rank":11},{"text":"White, D.","contributorId":39103,"corporation":false,"usgs":true,"family":"White","given":"D.","affiliations":[],"preferred":false,"id":428733,"contributorType":{"id":1,"text":"Authors"},"rank":12},{"text":"Wood, P.B. 0000-0002-8575-1705","orcid":"https://orcid.org/0000-0002-8575-1705","contributorId":103992,"corporation":false,"usgs":true,"family":"Wood","given":"P.B.","affiliations":[],"preferred":false,"id":428743,"contributorType":{"id":1,"text":"Authors"},"rank":13}]}}
,{"id":70031031,"text":"70031031 - 2006 - Estimating recharge rates with analytic element models and parameter estimation","interactions":[],"lastModifiedDate":"2012-03-12T17:21:16","indexId":"70031031","displayToPublicDate":"2006-01-01T00:00:00","publicationYear":"2006","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1861,"text":"Ground Water","active":true,"publicationSubtype":{"id":10}},"title":"Estimating recharge rates with analytic element models and parameter estimation","docAbstract":"Quantifying the spatial and temporal distribution of recharge is usually a prerequisite for effective ground water flow modeling. In this study, an analytic element (AE) code (GFLOW) was used with a nonlinear parameter estimation code (UCODE) to quantify the spatial and temporal distribution of recharge using measured base flows as calibration targets. The ease and flexibility of AE model construction and evaluation make this approach well suited for recharge estimation. An AE flow model of an undeveloped watershed in northern Wisconsin was optimized to match median annual base flows at four stream gages for 1996 to 2000 to demonstrate the approach. Initial optimizations that assumed a constant distributed recharge rate provided good matches (within 5%) to most of the annual base flow estimates, but discrepancies of >12% at certain gages suggested that a single value of recharge for the entire watershed is inappropriate. Subsequent optimizations that allowed for spatially distributed recharge zones based on the distribution of vegetation types improved the fit and confirmed that vegetation can influence spatial recharge variability in this watershed. Temporally, the annual recharge values varied >2.5-fold between 1996 and 2000 during which there was an observed 1.7-fold difference in annual precipitation, underscoring the influence of nonclimatic factors on interannual recharge variability for regional flow modeling. The final recharge values compared favorably with more labor-intensive field measurements of recharge and results from studies, supporting the utility of using linked AE-parameter estimation codes for recharge estimation. Copyright ?? 2005 The Author(s).","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Ground Water","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1111/j.1745-6584.2005.00115.x","issn":"0017467X","usgsCitation":"Dripps, W.R., Hunt, R.J., and Anderson, M.P., 2006, Estimating recharge rates with analytic element models and parameter estimation: Ground Water, v. 44, no. 1, p. 47-55, https://doi.org/10.1111/j.1745-6584.2005.00115.x.","startPage":"47","endPage":"55","numberOfPages":"9","costCenters":[],"links":[{"id":211394,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1111/j.1745-6584.2005.00115.x"},{"id":238677,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"44","issue":"1","noUsgsAuthors":false,"publicationDate":"2005-08-24","publicationStatus":"PW","scienceBaseUri":"505a0b3de4b0c8380cd5262f","contributors":{"authors":[{"text":"Dripps, W. R.","contributorId":27978,"corporation":false,"usgs":true,"family":"Dripps","given":"W.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":429696,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hunt, R. J.","contributorId":40164,"corporation":false,"usgs":true,"family":"Hunt","given":"R.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":429697,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Anderson, Marilyn P.","contributorId":102970,"corporation":false,"usgs":true,"family":"Anderson","given":"Marilyn","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":429698,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70030808,"text":"70030808 - 2006 - Case study: Mapping tsunami hazards associated with debris flow into a reservoir","interactions":[],"lastModifiedDate":"2012-03-12T17:21:18","indexId":"70030808","displayToPublicDate":"2006-01-01T00:00:00","publicationYear":"2006","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2338,"text":"Journal of Hydraulic Engineering","active":true,"publicationSubtype":{"id":10}},"title":"Case study: Mapping tsunami hazards associated with debris flow into a reservoir","docAbstract":"Debris-flow generated impulse waves (tsunamis) pose hazards in lakes, especially those used for hydropower or recreation. We describe a method for assessing tsunami-related hazards for the case in which inundation by coherent water waves, rather than chaotic splashing, is of primary concern. The method involves an experimentally based initial condition (tsunami source) and a Boussinesq model for tsunami propagation and inundation. Model results are used to create hazard maps that offer guidance for emergency planners and responders. An example application explores tsunami hazards associated with potential debris flows entering Baker Lake, a reservoir on the flanks of the Mount Baker volcano in the northwestern United States. ?? 2006 ASCE.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Journal of Hydraulic Engineering","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1061/(ASCE)0733-9429(2006)132:1(1)","issn":"07339429","usgsCitation":"Walder, J.S., Watts, P., and Waythomas, C.F., 2006, Case study: Mapping tsunami hazards associated with debris flow into a reservoir: Journal of Hydraulic Engineering, v. 132, no. 1, p. 1-11, https://doi.org/10.1061/(ASCE)0733-9429(2006)132:1(1).","startPage":"1","endPage":"11","numberOfPages":"11","costCenters":[],"links":[{"id":238891,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":211581,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1061/(ASCE)0733-9429(2006)132:1(1)"}],"volume":"132","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059f38ce4b0c8380cd4b88e","contributors":{"authors":[{"text":"Walder, J. S.","contributorId":32561,"corporation":false,"usgs":true,"family":"Walder","given":"J.","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":428777,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Watts, P.","contributorId":81669,"corporation":false,"usgs":true,"family":"Watts","given":"P.","email":"","affiliations":[],"preferred":false,"id":428778,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Waythomas, C. F.","contributorId":10065,"corporation":false,"usgs":true,"family":"Waythomas","given":"C.","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":428776,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70180915,"text":"70180915 - 2006 - The quest for a safe and effective canine distemper virus vaccine for black-footed ferrets","interactions":[],"lastModifiedDate":"2017-02-07T14:58:54","indexId":"70180915","displayToPublicDate":"2006-01-01T00:00:00","publicationYear":"2006","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"The quest for a safe and effective canine distemper virus vaccine for black-footed ferrets","docAbstract":"<p>Canine distemper virus (CDV) causes a systemic disease that is highly virulent to mustelids and other carnivore (Order Carnivora) species and is found worldwide. Endemic canine distemper in wild and domestic carnivores in the United States has made reintroduction of endangered black-footed ferrets (Mustela nigripes) difficult in the absence of safe and effective CDV vaccines and vaccination practices. Toward this end, researchers have explored appropriate animal models and vaccine preparations in highly susceptible species. Published studies involving domestic ferrets (M. putorius furo) using Galaxy-D® and evaluating a recombinant canarypox-vectored vaccine for oral administration are reviewed. In addition, we present new findings in domestic and black-footed ferrets and Siberian polecats (M. eversmannii) that have extended our understanding of CDV in the black-footed ferret and other at-risk carnivore species. Original research presented here includes trials that determined an effective challenge dose (by route) of virulent CDV in domestic ferrets and Siberian polecats; the low likelihood of collateral vaccination with Galaxy-D; the adverse effect of modified-live virus boostering in black-footed ferrets receiving killed vaccine previously and the response of Siberian polecats receiving canarypoxvectored recombinant CDV vaccine (reCDV); the absence of an effect of reCDV vaccination on conception, pregnancy, and neonatal growth in Siberian polecats; and the apparent inefficacy of active reCDV vaccination during the period of passive immunity in young Siberian polecats. In the final section, we discuss emerging concerns and avenues for disease intervention that may present new opportunities to solve problems in&nbsp;vaccine safety, vaccine availability, field vaccine delivery, and other therapeutic modalities.</p>","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Recovery of the black-footed ferret: Progress and continuing challenges- Proceedings of the Symposium on the Status of the Black-footed Ferret and Its Habitat, Fort Collins, Colorado, January 28-29, 2004 (Scientific Investigations Report 2005-5293)","largerWorkSubtype":{"id":5,"text":"USGS Numbered Series"},"conferenceTitle":"Symposium on the Status of the Black-footed Ferret and Its Habitat","conferenceDate":"January 28-29, 2004","conferenceLocation":"Fort Collins, CO","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","usgsCitation":"Wimsatt, J., Biggins, D.E., Williams, E., and Becerra, V.M., 2006, The quest for a safe and effective canine distemper virus vaccine for black-footed ferrets, <i>in</i> Recovery of the black-footed ferret: Progress and continuing challenges- Proceedings of the Symposium on the Status of the Black-footed Ferret and Its Habitat, Fort Collins, Colorado, January 28-29, 2004 (Scientific Investigations Report 2005-5293), Fort Collins, CO, January 28-29, 2004, p. 248-266.","productDescription":"19 p.","startPage":"248","endPage":"266","costCenters":[{"id":291,"text":"Fort Collins Science Center","active":true,"usgs":true}],"links":[{"id":334909,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":334908,"rank":1,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/sir/2005/5293/report.pdf#page=259","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"589aeab3e4b0efcedb72d251","contributors":{"authors":[{"text":"Wimsatt, Jeffrey","contributorId":173421,"corporation":false,"usgs":false,"family":"Wimsatt","given":"Jeffrey","email":"","affiliations":[],"preferred":false,"id":662806,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Biggins, Dean E. 0000-0003-2078-671X bigginsd@usgs.gov","orcid":"https://orcid.org/0000-0003-2078-671X","contributorId":2522,"corporation":false,"usgs":true,"family":"Biggins","given":"Dean","email":"bigginsd@usgs.gov","middleInitial":"E.","affiliations":[{"id":291,"text":"Fort Collins Science Center","active":true,"usgs":true}],"preferred":true,"id":662807,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Williams, Elizabeth S.","contributorId":179120,"corporation":false,"usgs":false,"family":"Williams","given":"Elizabeth S.","affiliations":[],"preferred":false,"id":662808,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Becerra, Victor M.","contributorId":179121,"corporation":false,"usgs":false,"family":"Becerra","given":"Victor","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":662809,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70031059,"text":"70031059 - 2006 - Trends in the nutrient enrichment of U.S. rivers during the late 20th century and their relation to changes in probable stream trophic conditions","interactions":[],"lastModifiedDate":"2012-03-12T17:21:17","indexId":"70031059","displayToPublicDate":"2006-01-01T00:00:00","publicationYear":"2006","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"Trends in the nutrient enrichment of U.S. rivers during the late 20th century and their relation to changes in probable stream trophic conditions","docAbstract":"We estimated trends in concentrations of total phosphorus (TP) and total nitrogen (TN) and the related change in the probabilities of trophic conditions from 1975 to 1994 at 250 nationally representative riverine monitoring locations in the U.S. with drainage areas larger than about 1,000 km2. Statistically significant (p < 0.05) declines were detected in TP and TN concentrations at 44% and 37% of the monitoring sites, and significant increases were detected at 3% and 9% of the sites, respectively. We used a statistical model to assess changes in the probable trophic-state classification of the sites after adjusting for climate-related variability in nutrient concentrations. The probabilistic assessment accounts for current knowledge of the trophic response of streams to nutrient enrichment, based on a recently proposed definition of \"eutrophic,\" \"mesotrophic,\" and \"oligotrophic\" conditions in relation to total nutrient concentrations. Based on these trophic definitions, we found that the trophic state improved at 25% of the monitoring sites and worsened at fewer than 5% of the sites; about 70% of the sites were unchanged. Improvements in trophic-state related to declines in TP were more common in predominantly forested and shrub-grassland watersheds, whereas the trophic state of predominantly agricultural sites was unchanged. Despite the declines in TP concentrations at many sites, about 50% of all monitoring sites, and more than 60% of the sites in predominantly agricultural and urban watersheds, were classified as eutrophic in 1994 based on TP concentrations. Contemporaneous reductions in major nutrient sources to streams, related to wastewater treatment upgrades, phosphate detergent bans, and declines in some agricultural sources, may have contributed to the declines in riverine nutrient concentrations and associated improvements in trophic conditions. ?? 2006, by the American Society of Limnology and Oceanography, Inc.","largerWorkTitle":"Limnology and Oceanography","language":"English","issn":"00243590","usgsCitation":"Alexander, R.B., and Smith, R.A., 2006, Trends in the nutrient enrichment of U.S. rivers during the late 20th century and their relation to changes in probable stream trophic conditions, <i>in</i> Limnology and Oceanography, v. 51, no. 1 II, p. 639-654.","startPage":"639","endPage":"654","numberOfPages":"16","costCenters":[],"links":[{"id":238611,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"51","issue":"1 II","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505bb812e4b08c986b327669","contributors":{"authors":[{"text":"Alexander, R. B.","contributorId":108103,"corporation":false,"usgs":true,"family":"Alexander","given":"R.","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":429867,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Smith, R. A.","contributorId":60584,"corporation":false,"usgs":true,"family":"Smith","given":"R.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":429866,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70030564,"text":"70030564 - 2006 - MODFLOW/MT3DMS-based simulation of variable-density ground water flow and transport","interactions":[],"lastModifiedDate":"2012-03-12T17:21:05","indexId":"70030564","displayToPublicDate":"2006-01-01T00:00:00","publicationYear":"2006","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1861,"text":"Ground Water","active":true,"publicationSubtype":{"id":10}},"title":"MODFLOW/MT3DMS-based simulation of variable-density ground water flow and transport","docAbstract":"This paper presents an approach for coupling MODFLOW and MT3DMS for the simulation of variable-density ground water flow. MODFLOW routines were modified to solve a variable-density form of the ground water flow equation in which the density terms are calculated using an equation of state and the simulated MT3DMS solute concentrations. Changes to the MODFLOW and MT3DMS input files were kept to a minimum, and thus existing data files and data files created with most pre- and postprocessors can be used directly with the SEAWAT code. The approach was tested by simulating the Henry problem and two of the saltpool laboratory experiments (low- and high-density cases). For the Henry problem, the simulated results compared well with the steady-state semianalytic solution and also the transient isochlor movement as simulated by a finite-element model. For the saltpool problem, the simulated breakthrough curves compared better with the laboratory measurements for the low-density case than for the high-density case but showed good agreement with the measured salinity isosurfaces for both cases. Results from the test cases presented here indicate that the MODFLOW/MT3DMS approach provides accurate solutions for problems involving variable-density ground water flow and solute transport. ?? 2006 National Ground Water Association.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Ground Water","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1111/j.1745-6584.2005.00156.x","issn":"0017467X","usgsCitation":"Langevin, C., and Guo, W., 2006, MODFLOW/MT3DMS-based simulation of variable-density ground water flow and transport: Ground Water, v. 44, no. 3, p. 339-351, https://doi.org/10.1111/j.1745-6584.2005.00156.x.","startPage":"339","endPage":"351","numberOfPages":"13","costCenters":[],"links":[{"id":477602,"rank":10000,"type":{"id":41,"text":"Open Access External Repository Page"},"url":"http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.549.1049","text":"External Repository"},{"id":211960,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1111/j.1745-6584.2005.00156.x"},{"id":239350,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"44","issue":"3","noUsgsAuthors":false,"publicationDate":"2005-12-06","publicationStatus":"PW","scienceBaseUri":"505a4ae4e4b0c8380cd69117","contributors":{"authors":[{"text":"Langevin, C.D.","contributorId":25976,"corporation":false,"usgs":true,"family":"Langevin","given":"C.D.","email":"","affiliations":[],"preferred":false,"id":427663,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Guo, W.","contributorId":43230,"corporation":false,"usgs":true,"family":"Guo","given":"W.","email":"","affiliations":[],"preferred":false,"id":427664,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70035311,"text":"70035311 - 2006 - A community effort to construct a gravity database for the United States and an associated Web portal","interactions":[],"lastModifiedDate":"2012-03-12T17:21:54","indexId":"70035311","displayToPublicDate":"2006-01-01T00:00:00","publicationYear":"2006","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3459,"text":"Special Paper of the Geological Society of America","active":true,"publicationSubtype":{"id":10}},"title":"A community effort to construct a gravity database for the United States and an associated Web portal","docAbstract":"Potential field data (gravity and magnetic measurements) are both useful and costeffective tools for many geologic investigations. Significant amounts of these data are traditionally in the public domain. A new magnetic database for North America was released in 2002, and as a result, a cooperative effort between government agencies, industry, and universities to compile an upgraded digital gravity anomaly database, grid, and map for the conterminous United States was initiated and is the subject of this paper. This database is being crafted into a data system that is accessible through a Web portal. This data system features the database, software tools, and convenient access. The Web portal will enhance the quality and quantity of data contributed to the gravity database that will be a shared community resource. The system's totally digital nature ensures that it will be flexible so that it can grow and evolve as new data, processing procedures, and modeling and visualization tools become available. Another goal of this Web-based data system is facilitation of the efforts of researchers and students who wish to collect data from regions currently not represented adequately in the database. The primary goal of upgrading the United States gravity database and this data system is to provide more reliable data that support societal and scientific investigations of national importance. An additional motivation is the international intent to compile an enhanced North American gravity database, which is critical to understanding regional geologic features, the tectonic evolution of the continent, and other issues that cross national boundaries. ?? 2006 Geological Society of America. All rights reserved.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Special Paper of the Geological Society of America","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1130/2006.2397(02)","issn":"00721077","usgsCitation":"Keller, G.R., Hildenbrand, T., Kucks, R., Webring, M., Briesacher, A., Rujawitz, K., Hittleman, A., Roman, D., Winester, D., Aldouri, R., Seeley, J., Rasillo, J., Torres, R., Hinze, W.J., Gates, A., Kreinovich, V., and Salayandia, L., 2006, A community effort to construct a gravity database for the United States and an associated Web portal: Special Paper of the Geological Society of America, no. 397, p. 21-34, https://doi.org/10.1130/2006.2397(02).","startPage":"21","endPage":"34","numberOfPages":"14","costCenters":[],"links":[{"id":215401,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1130/2006.2397(02)"},{"id":243203,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"issue":"397","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059e34ce4b0c8380cd45f56","contributors":{"authors":[{"text":"Keller, Gordon R.","contributorId":90280,"corporation":false,"usgs":true,"family":"Keller","given":"Gordon","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":450137,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hildenbrand, T.G.","contributorId":83892,"corporation":false,"usgs":true,"family":"Hildenbrand","given":"T.G.","email":"","affiliations":[],"preferred":false,"id":450136,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Kucks, R.","contributorId":23246,"corporation":false,"usgs":true,"family":"Kucks","given":"R.","affiliations":[],"preferred":false,"id":450124,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Webring, M.","contributorId":67662,"corporation":false,"usgs":true,"family":"Webring","given":"M.","affiliations":[],"preferred":false,"id":450132,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Briesacher, A.","contributorId":69803,"corporation":false,"usgs":true,"family":"Briesacher","given":"A.","affiliations":[],"preferred":false,"id":450133,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Rujawitz, K.","contributorId":57288,"corporation":false,"usgs":true,"family":"Rujawitz","given":"K.","email":"","affiliations":[],"preferred":false,"id":450130,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Hittleman, A.M.","contributorId":67314,"corporation":false,"usgs":true,"family":"Hittleman","given":"A.M.","email":"","affiliations":[],"preferred":false,"id":450131,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Roman, D.R.","contributorId":20179,"corporation":false,"usgs":true,"family":"Roman","given":"D.R.","email":"","affiliations":[],"preferred":false,"id":450123,"contributorType":{"id":1,"text":"Authors"},"rank":8},{"text":"Winester, D.","contributorId":29197,"corporation":false,"usgs":true,"family":"Winester","given":"D.","affiliations":[],"preferred":false,"id":450126,"contributorType":{"id":1,"text":"Authors"},"rank":9},{"text":"Aldouri, R.","contributorId":42802,"corporation":false,"usgs":true,"family":"Aldouri","given":"R.","affiliations":[],"preferred":false,"id":450127,"contributorType":{"id":1,"text":"Authors"},"rank":10},{"text":"Seeley, J.","contributorId":70612,"corporation":false,"usgs":true,"family":"Seeley","given":"J.","affiliations":[],"preferred":false,"id":450134,"contributorType":{"id":1,"text":"Authors"},"rank":11},{"text":"Rasillo, J.","contributorId":79722,"corporation":false,"usgs":true,"family":"Rasillo","given":"J.","email":"","affiliations":[],"preferred":false,"id":450135,"contributorType":{"id":1,"text":"Authors"},"rank":12},{"text":"Torres, R.","contributorId":25006,"corporation":false,"usgs":true,"family":"Torres","given":"R.","email":"","affiliations":[],"preferred":false,"id":450125,"contributorType":{"id":1,"text":"Authors"},"rank":13},{"text":"Hinze, W. J.","contributorId":52607,"corporation":false,"usgs":false,"family":"Hinze","given":"W.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":450129,"contributorType":{"id":1,"text":"Authors"},"rank":14},{"text":"Gates, A.","contributorId":100203,"corporation":false,"usgs":true,"family":"Gates","given":"A.","email":"","affiliations":[],"preferred":false,"id":450138,"contributorType":{"id":1,"text":"Authors"},"rank":15},{"text":"Kreinovich, V.","contributorId":103108,"corporation":false,"usgs":true,"family":"Kreinovich","given":"V.","email":"","affiliations":[],"preferred":false,"id":450139,"contributorType":{"id":1,"text":"Authors"},"rank":16},{"text":"Salayandia, L.","contributorId":51566,"corporation":false,"usgs":true,"family":"Salayandia","given":"L.","email":"","affiliations":[],"preferred":false,"id":450128,"contributorType":{"id":1,"text":"Authors"},"rank":17}]}}
,{"id":70030933,"text":"70030933 - 2006 - Aqueous processes at Gusev crater inferred from physical properties of rocks and soils along the Spirit traverse","interactions":[],"lastModifiedDate":"2018-11-28T10:16:17","indexId":"70030933","displayToPublicDate":"2006-01-01T00:00:00","publicationYear":"2006","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2317,"text":"Journal of Geophysical Research E: Planets","active":true,"publicationSubtype":{"id":10}},"title":"Aqueous processes at Gusev crater inferred from physical properties of rocks and soils along the Spirit traverse","docAbstract":"<p>Gusev crater was selected as the landing site for Spirit on the basis of morphological evidence of long-lasting water activity, including possibly fluvial and lacustrine episodes. From the Columbia Memorial Station to the Columbia Hills, Spirit's traverse provides a journey back in time, from relatively recent volcanic plains showing little evidence for aqueous processes up to the older hills, where rock and soil composition are drastically different. For the first 156 sols, the only evidence of water action was weathering rinds, vein fillings, and soil crust cementation by salts. The trenches of Sols 112-145 marked the first significant findings of increased concentrations of sulfur and magnesium varying in parallel, suggesting that they be paired as magnesium-sulfate. Spirit's arrival at West Spur coincided with a shift in rock and soil composition with observations hinting at substantial amounts of water in Gusev's past. We used the Microscopic Imager data up to Sol 431 to analyze rock and soil properties and infer plausible types and magnitude of aqueous processes through time. We show the role played early by topography and structure. The morphology, texture, and deep alteration shown by the rocks in West Spur and the Columbia Hills Formation (CHF) suggest conditions that are not met in present-day Mars and required a wetter environment, which could have included transport of sulfur, chlorine, and bromine in water, vapor in volcanic gases, hydrothermal circulation, or saturation in a briny fluid containing the same elements. Changing conditions that might have affected flow circulation are suggested by different textural and morphological characteristics between the rocks in the CHF and those of the plains, with higher porosity proxy, higher void ratio, and higher water storage potential in the CHF. Soils were used to assess aqueous processes and water pathways in the top layers of modern soils. We conclude that infiltration might have become more difficult with time.</p>","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Journal of Geophysical Research E: Planets","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"American Geophysical Union","publisherLocation":"Washington, D.C.","doi":"10.1029/2005JE002490","issn":"01480227","usgsCitation":"Cabrol, N., Farmer, J., Grin, E., Ritcher, L., Soderblom, L., Li, R., Herkenhoff, K.E., Landis, G.A., and Arvidson, R., 2006, Aqueous processes at Gusev crater inferred from physical properties of rocks and soils along the Spirit traverse: Journal of Geophysical Research E: Planets, v. 111, no. E2, 15 p., https://doi.org/10.1029/2005JE002490.","productDescription":"15 p.","costCenters":[{"id":131,"text":"Astrogeology Science Center","active":true,"usgs":true}],"links":[{"id":238704,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"otherGeospatial":"Gusev crater; Mars","volume":"111","issue":"E2","noUsgsAuthors":false,"publicationDate":"2006-02-22","publicationStatus":"PW","scienceBaseUri":"5059ed19e4b0c8380cd49614","contributors":{"authors":[{"text":"Cabrol, N.A.","contributorId":65208,"corporation":false,"usgs":true,"family":"Cabrol","given":"N.A.","email":"","affiliations":[],"preferred":false,"id":429282,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Farmer, J.D.","contributorId":79671,"corporation":false,"usgs":true,"family":"Farmer","given":"J.D.","email":"","affiliations":[],"preferred":false,"id":429285,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Grin, E.A.","contributorId":53926,"corporation":false,"usgs":true,"family":"Grin","given":"E.A.","affiliations":[],"preferred":false,"id":429281,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Ritcher, L.","contributorId":45112,"corporation":false,"usgs":true,"family":"Ritcher","given":"L.","email":"","affiliations":[],"preferred":false,"id":429279,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Soderblom, L.","contributorId":106244,"corporation":false,"usgs":true,"family":"Soderblom","given":"L.","affiliations":[],"preferred":false,"id":429286,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Li, R.","contributorId":68441,"corporation":false,"usgs":true,"family":"Li","given":"R.","affiliations":[],"preferred":false,"id":429283,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Herkenhoff, Kenneth E. 0000-0002-3153-6663 kherkenhoff@usgs.gov","orcid":"https://orcid.org/0000-0002-3153-6663","contributorId":2275,"corporation":false,"usgs":true,"family":"Herkenhoff","given":"Kenneth","email":"kherkenhoff@usgs.gov","middleInitial":"E.","affiliations":[{"id":131,"text":"Astrogeology Science Center","active":true,"usgs":true}],"preferred":true,"id":429278,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Landis, G. A.","contributorId":76536,"corporation":false,"usgs":true,"family":"Landis","given":"G.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":429284,"contributorType":{"id":1,"text":"Authors"},"rank":8},{"text":"Arvidson, R. E.","contributorId":46666,"corporation":false,"usgs":true,"family":"Arvidson","given":"R. E.","affiliations":[],"preferred":false,"id":429280,"contributorType":{"id":1,"text":"Authors"},"rank":9}]}}
,{"id":70030252,"text":"70030252 - 2006 - Monitoring bird populations in small geographic areas","interactions":[],"lastModifiedDate":"2012-03-12T17:21:02","indexId":"70030252","displayToPublicDate":"2006-01-01T00:00:00","publicationYear":"2006","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2919,"text":"Occasional Paper of the Canadian Wildlife Service","active":true,"publicationSubtype":{"id":10}},"title":"Monitoring bird populations in small geographic areas","docAbstract":"Numerous methods exist for monitoring bird populations, and there is a large literature describing them. There are few resources, however, that provide comprehensive advice on every step of organizing and carrying out a survey, from the early stages of planning to final use of the data. Even fewer resources are designed to meet the needs of a wide variety of potential users, from amateurs interested in change of bird life in a local study preserve to professionals testing hypotheses on the response of birds to habitat management, although much of the advice should be the same for every monitoring program. Whether survey objectives are very modest or rigorously scientific, samples must be sufficiently numerous and well distributed to provide meaningful results, and the survey should be well designed to ensure that the money and effort going into it are not wasted. This document is intended to be a complete resource for anyone planning to organize monitoring of noncolonial landbirds within a relatively small geographic area (e.g., from the size of a woodlot to a large park). The first of its two parts provides background explaining the importance of good study design and gives specific advice on all aspects of project planning and execution of high-quality data collection for the purpose of hypothesis testing. The second part is self-contained and nontechnical and describes complete plans for a site-specific checklist survey, suitable for addressing monitoring questions frequently asked by amateurs and for involvement of volunteers in data collection. Throughout are references to additional resources, from background literature to sources of existing survey protocols, analysis software, and tools for archiving data.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Occasional Paper of the Canadian Wildlife Service","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","issn":"05766370","usgsCitation":"Dunn, E.H., Bart, J., Collins, B., Craig, B., Dale, B., Downes, C., Francis, C., Woodley, S., and Zorn, P., 2006, Monitoring bird populations in small geographic areas: Occasional Paper of the Canadian Wildlife Service, no. SPEC. ISS., p. 1-59.","startPage":"1","endPage":"59","numberOfPages":"59","costCenters":[],"links":[{"id":239294,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"issue":"SPEC. ISS.","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a5d91e4b0c8380cd70473","contributors":{"authors":[{"text":"Dunn, Erica H.","contributorId":35841,"corporation":false,"usgs":false,"family":"Dunn","given":"Erica","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":426321,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bart, J.","contributorId":76272,"corporation":false,"usgs":true,"family":"Bart","given":"J.","affiliations":[],"preferred":false,"id":426326,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Collins, B.T.","contributorId":97315,"corporation":false,"usgs":true,"family":"Collins","given":"B.T.","email":"","affiliations":[],"preferred":false,"id":426327,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Craig, B.","contributorId":15827,"corporation":false,"usgs":true,"family":"Craig","given":"B.","email":"","affiliations":[],"preferred":false,"id":426319,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Dale, B.","contributorId":60570,"corporation":false,"usgs":true,"family":"Dale","given":"B.","email":"","affiliations":[],"preferred":false,"id":426324,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Downes, C.M.","contributorId":46762,"corporation":false,"usgs":true,"family":"Downes","given":"C.M.","email":"","affiliations":[],"preferred":false,"id":426323,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Francis, C.M.","contributorId":29092,"corporation":false,"usgs":true,"family":"Francis","given":"C.M.","email":"","affiliations":[],"preferred":false,"id":426320,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Woodley, S.","contributorId":36361,"corporation":false,"usgs":true,"family":"Woodley","given":"S.","email":"","affiliations":[],"preferred":false,"id":426322,"contributorType":{"id":1,"text":"Authors"},"rank":8},{"text":"Zorn, P.","contributorId":61645,"corporation":false,"usgs":true,"family":"Zorn","given":"P.","email":"","affiliations":[],"preferred":false,"id":426325,"contributorType":{"id":1,"text":"Authors"},"rank":9}]}}
,{"id":70030256,"text":"70030256 - 2006 - Fault parameter constraints using relocated earthquakes: A validation of first-motion focal-mechanism data","interactions":[],"lastModifiedDate":"2016-08-29T15:25:25","indexId":"70030256","displayToPublicDate":"2006-01-01T00:00:00","publicationYear":"2006","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1135,"text":"Bulletin of the Seismological Society of America","onlineIssn":"1943-3573","printIssn":"0037-1106","active":true,"publicationSubtype":{"id":10}},"title":"Fault parameter constraints using relocated earthquakes: A validation of first-motion focal-mechanism data","docAbstract":"<p class=\"p1\"><span class=\"s1\">We estimate the strike and dip of three California fault segments (Calaveras, Sargent, and a portion of the San Andreas near San Jaun Bautistia) based on principle component analysis of accurately located microearthquakes. We compare these fault orientations with two different first-motion focal mechanism catalogs: the Northern California Earthquake Data Center (</span><span class=\"s2\">NCEDC</span><span class=\"s1\">) catalog, calculated using the </span><span class=\"s2\">FPFIT</span><span class=\"s1\"> algorithm (Reasenberg and Oppenheimer, 1985), and a catalog created using the </span><span class=\"s2\">HASH</span><span class=\"s1\"> algorithm that tests mechanism stability relative to seismic velocity model variations and earthquake location (Hardebeck and Shearer, 2002). We assume any disagreement (misfit &gt;30&deg; in strike, dip, or rake) indicates inaccurate focal mechanisms in the catalogs. With this assumption, we can quantify the parameters that identify the most optimally constrained focal mechanisms. For the </span><span class=\"s2\">NCEDC/FPFIT</span><span class=\"s1\"> catalogs, we find that the best quantitative discriminator of quality focal mechanisms is the station distribution ratio (</span><span class=\"s2\">STDR</span><span class=\"s1\">) parameter, an indicator of how the stations are distributed about the focal sphere. Requiring </span><span class=\"s2\">STDR</span><span class=\"s1\"> &gt; 0.65 increases the acceptable mechanisms from 34%&ndash;37% to 63%&ndash;68%. This suggests stations should be uniformly distributed surrounding, rather than aligning, known fault traces. For the </span><span class=\"s2\">HASH</span><span class=\"s1\"> catalogs, the fault plane uncertainty (</span><span class=\"s2\">FPU</span><span class=\"s1\">) parameter is the best discriminator, increasing the percent of acceptable mechanisms from 63%&ndash;78% to 81%&ndash;83% when </span><span class=\"s2\">FPU</span><span class=\"s1\"> &le; 35&deg;. The overall higher percentage of acceptable mechanisms and the usefulness of the formal uncertainty in identifying quality mechanisms validate the </span><span class=\"s2\">HASH</span><span class=\"s1\"> approach of testing for mechanism stability.</span></p>","language":"English","publisher":"Seismological Society of America","doi":"10.1785/0120040239","issn":"00371106","usgsCitation":"Kilb, D., and Hardebeck, J., 2006, Fault parameter constraints using relocated earthquakes: A validation of first-motion focal-mechanism data: Bulletin of the Seismological Society of America, v. 96, no. 3, p. 1140-1158, https://doi.org/10.1785/0120040239.","productDescription":"19 p.","startPage":"1140","endPage":"1158","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":239366,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"96","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a0f1ae4b0c8380cd5377e","contributors":{"authors":[{"text":"Kilb, Debi","contributorId":90892,"corporation":false,"usgs":true,"family":"Kilb","given":"Debi","affiliations":[],"preferred":false,"id":426349,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hardebeck, J.L.","contributorId":98862,"corporation":false,"usgs":true,"family":"Hardebeck","given":"J.L.","email":"","affiliations":[],"preferred":false,"id":426350,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70035415,"text":"70035415 - 2006 - Chapter 13 Petrogenesis of the Campanian Ignimbrite: Implications for crystal-melt separation and open-system processes from major and trace elements and Th isotopic data","interactions":[],"lastModifiedDate":"2022-12-20T16:03:03.032036","indexId":"70035415","displayToPublicDate":"2006-01-01T00:00:00","publicationYear":"2006","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1387,"text":"Developments in Volcanology","active":true,"publicationSubtype":{"id":10}},"title":"Chapter 13 Petrogenesis of the Campanian Ignimbrite: Implications for crystal-melt separation and open-system processes from major and trace elements and Th isotopic data","docAbstract":"<p><span>The Campanian Ignimbrite is a large-volume trachytic to phonolitic ignimbrite that was deposited at ≈39.3 ka and represents one of a number of highly explosive volcanic events that have occurred in the region near Naples, Italy. Thermodynamic modeling using the MELTS algorithm reveals that major element variations are dominated by crystal-liquid separation at 0.15 GPa. Initial dissolved H</span><sub>2</sub><span>O content in the parental melt is ∼3 wt.% and the magmatic system fugacity of oxygen was buffered along QFM+1. Significantly, MELTS results also indicate that the liquid line of descent is marked by a large change in the proportion of melt (from 0.46 to 0.09) at ∼884°C, which leads to a discontinuity in melt composition (i.e., a compositional gap) and different thermodynamic and transport properties of melt and magma across the gap. Crystallization of alkali feldspar and plagioclase dominates the phase assemblage at this pseudo-invariant point temperature of ∼884°C. Evaluation of the variations in the trace elements Zr, Nb, Th, U, Rb, Sm, and Sr using a mass balance equation that accounts for changing bulk mineral-melt partition coefficients as crystallization occurs indicates that crystal-liquid separation and open-system processes were important. Th isotope data yield an apparent isochron that is ∼20 kyr younger than the age of the deposit, and age-corrected Th isotope data indicate that the magma body was an open system at the time of eruption. Because open-system behavior can profoundly change isotopic and elemental characteristics of a magma body, these Th results illustrate that it is critical to understand the contribution that open-system processes make to magmatic systems prior to assigning relevance to age or timescale information derived from such systems. Fluid-magma interaction has been proposed as a mechanism to change isotopic and elemental characteristics of magma bodies, but an evaluation of the mass and thermal constraints on such a process suggests large-scale interaction is unlikely. In the case of the magma body associated with the Campanian Ignimbrite, the most likely source of the open-system signatures is assimilation of partial melts of compositionally heterogeneous basement composed of cumulates and intrusive equivalents of volcanic activity that has characterized the Campanian region for over 300 kyr.</span></p>","language":"English","publisher":"Elsevier","doi":"10.1016/S1871-644X(06)80027-6","usgsCitation":"Bohrson, W., Spera, F., Fowler, S.J., Belkin, H., de Vivo, B., and Rolandi, G., 2006, Chapter 13 Petrogenesis of the Campanian Ignimbrite: Implications for crystal-melt separation and open-system processes from major and trace elements and Th isotopic data: Developments in Volcanology, v. 9, p. 249-288, https://doi.org/10.1016/S1871-644X(06)80027-6.","productDescription":"40 p.","startPage":"249","endPage":"288","numberOfPages":"40","costCenters":[],"links":[{"id":243114,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"9","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059f463e4b0c8380cd4bcda","contributors":{"authors":[{"text":"Bohrson, W.A.","contributorId":102092,"corporation":false,"usgs":false,"family":"Bohrson","given":"W.A.","affiliations":[],"preferred":false,"id":450560,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Spera, F. J.","contributorId":89315,"corporation":false,"usgs":false,"family":"Spera","given":"F. J.","affiliations":[],"preferred":false,"id":450559,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Fowler, S. J.","contributorId":18586,"corporation":false,"usgs":false,"family":"Fowler","given":"S.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":450555,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Belkin, H. E. 0000-0001-7879-6529","orcid":"https://orcid.org/0000-0001-7879-6529","contributorId":38160,"corporation":false,"usgs":true,"family":"Belkin","given":"H. E.","affiliations":[],"preferred":false,"id":450556,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"de Vivo, B.","contributorId":50549,"corporation":false,"usgs":false,"family":"de Vivo","given":"B.","affiliations":[],"preferred":false,"id":450557,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Rolandi, G.","contributorId":76472,"corporation":false,"usgs":false,"family":"Rolandi","given":"G.","email":"","affiliations":[],"preferred":false,"id":450558,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}}
,{"id":70030340,"text":"70030340 - 2006 - The contingent behavior of charter fishing participants on the Chesapeake Bay: Welfare estimates associated with water quality improvements","interactions":[],"lastModifiedDate":"2012-03-12T17:21:02","indexId":"70030340","displayToPublicDate":"2006-01-01T00:00:00","publicationYear":"2006","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2261,"text":"Journal of Environmental Planning and Management","active":true,"publicationSubtype":{"id":10}},"title":"The contingent behavior of charter fishing participants on the Chesapeake Bay: Welfare estimates associated with water quality improvements","docAbstract":"Water quality in the Chesapeake Bay has deteriorated over recent years. Historically, fishing has contributed to the region's local economy in terms of commercial and recreational harvests. A contingent behavior model is used to estimate welfare measures for charter fishing participants with regard to a hypothetical improvement in water quality. Using a truncated Poisson count model corrected for endogenous stratification, it was found that charter fishers not only contribute to the local market economy, but they also place positive non-market value on preserving the Bay's water quality. Using two estimates for travels costs it is estimated that the individual consumer surplus is $200 and $117 per trip, and the average individual consumer surplus values for an improvement in water quality is $75 and $44 for two models estimated. ?? 2006 University of Newcastle upon Tyne.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Journal of Environmental Planning and Management","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1080/09640560500508064","issn":"09640568","usgsCitation":"Poor, P., and Breece, M., 2006, The contingent behavior of charter fishing participants on the Chesapeake Bay: Welfare estimates associated with water quality improvements: Journal of Environmental Planning and Management, v. 49, no. 2, p. 265-278, https://doi.org/10.1080/09640560500508064.","startPage":"265","endPage":"278","numberOfPages":"14","costCenters":[],"links":[{"id":211745,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1080/09640560500508064"},{"id":239094,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"49","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505baa5be4b08c986b3227e9","contributors":{"authors":[{"text":"Poor, P.J.","contributorId":21348,"corporation":false,"usgs":true,"family":"Poor","given":"P.J.","email":"","affiliations":[],"preferred":false,"id":426752,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Breece, M.","contributorId":16652,"corporation":false,"usgs":true,"family":"Breece","given":"M.","email":"","affiliations":[],"preferred":false,"id":426751,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
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