{"pageNumber":"283","pageRowStart":"7050","pageSize":"25","recordCount":16446,"records":[{"id":70029164,"text":"70029164 - 2005 - Radiation pattern of a borehole radar antenna","interactions":[],"lastModifiedDate":"2018-10-31T10:20:34","indexId":"70029164","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1808,"text":"Geophysics","active":true,"publicationSubtype":{"id":10}},"title":"Radiation pattern of a borehole radar antenna","docAbstract":"<p>The finite-difference time-domain method was used to simulate radar waves that were generated by a transmitting antenna inside a borehole. The simulations were of four different models that included features such as a water-filled borehole and an antenna with resistive loading. For each model, radiation patterns for the far-field region were calculated. The radiation patterns show that the amplitude of the radar wave was strongly affected by its frequency, the water-filled borehole, the resistive loading of the antenna, and the external metal parts of the antenna (e.g., the cable head and the battery pack). For the models with a water-filled borehole, their normalized radiation patterns were practically identical to the normalized radiation pattern of a finite-length electric dipole when the wavelength in the formation was significantly greater than the total length of the radiating elements of the model antenna. The minimum wavelength at which this criterion was satisfied depended upon the features of the antenna, especially its external metal parts.</p>","language":"English","publisher":"GSW","doi":"10.1190/1.1852779","issn":"00168033","usgsCitation":"Ellefsen, K., and Wright, D., 2005, Radiation pattern of a borehole radar antenna: Geophysics, v. 70, no. 1, p. K1-K11, https://doi.org/10.1190/1.1852779.","productDescription":"11 p.","startPage":"K1","endPage":"K11","costCenters":[{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":210634,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1190/1.1852779"},{"id":237617,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"70","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a9395e4b0c8380cd80ef9","contributors":{"authors":[{"text":"Ellefsen, K.J. 0000-0003-3075-4703","orcid":"https://orcid.org/0000-0003-3075-4703","contributorId":12061,"corporation":false,"usgs":true,"family":"Ellefsen","given":"K.J.","affiliations":[],"preferred":false,"id":421595,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Wright, D.L.","contributorId":88758,"corporation":false,"usgs":true,"family":"Wright","given":"D.L.","email":"","affiliations":[],"preferred":false,"id":421596,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70029381,"text":"70029381 - 2005 - Wave spectral energy variability in the northeast Pacific","interactions":[],"lastModifiedDate":"2018-11-05T07:29:05","indexId":"70029381","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2315,"text":"Journal of Geophysical Research C: Oceans","active":true,"publicationSubtype":{"id":10}},"title":"Wave spectral energy variability in the northeast Pacific","docAbstract":"<p><span>The dominant characteristics of wave energy variability in the eastern North Pacific are described from NOAA National Data Buoy Center (NDBC) buoy data collected from 1981 to 2003. Ten buoys at distributed locations were selected for comparison based on record duration and data continuity. Long‐period (LP) [</span><i>T</i><span>&nbsp;&gt; 12] s, intermediate‐period [6 ≤&nbsp;</span><i>T</i><span>&nbsp;≤ 12] s, and short‐period [</span><i>T</i><span>&nbsp;&lt; 6] s wave spectral energy components are considered separately. Empirical orthogonal function (EOF) analyses of monthly wave energy anomalies reveal that all three wave energy components exhibit similar patterns of spatial variability. The dominant mode represents coherent heightened (or diminished) wave energy along the West Coast from Alaska to southern California, as indicated by composites of the 700 hPa height field. The second EOF mode reveals a distinct El Niño‐Southern Oscillation (ENSO)‐associated spatial distribution of wave energy, which occurs when the North Pacific storm track is extended unusually far south or has receded to the north. Monthly means and principal components (PCs) of wave energy levels indicate that the 1997–1998 El Niño winter had the highest basin‐wide wave energy within this record, substantially higher than the 1982–1983 El Niño. An increasing trend in the dominant PC of LP wave energy suggests that storminess has increased in the northeast Pacific since 1980. This trend is emphasized at central eastern North Pacific locations. Patterns of storminess variability are consistent with increasing activity in the central North Pacific as well as the tendency for more extreme waves in the south during El Niño episodes and in the north during La Niña.</span></p>","language":"English","publisher":"AGU","doi":"10.1029/2004JC002398","issn":"01480227","usgsCitation":"Bromirski, P., Cayan, D., and Flick, R., 2005, Wave spectral energy variability in the northeast Pacific: Journal of Geophysical Research C: Oceans, v. 110, no. 3, p. 1-15, https://doi.org/10.1029/2004JC002398.","productDescription":"15 p.","startPage":"1","endPage":"15","costCenters":[{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":477843,"rank":10000,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1029/2004jc002398","text":"Publisher Index Page"},{"id":237596,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":210620,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1029/2004JC002398"}],"volume":"110","issue":"3","noUsgsAuthors":false,"publicationDate":"2005-03-08","publicationStatus":"PW","scienceBaseUri":"505bcf97e4b08c986b32e9b4","contributors":{"authors":[{"text":"Bromirski, P.D.","contributorId":82521,"corporation":false,"usgs":true,"family":"Bromirski","given":"P.D.","email":"","affiliations":[],"preferred":false,"id":422495,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Cayan, D.R.","contributorId":25961,"corporation":false,"usgs":false,"family":"Cayan","given":"D.R.","email":"","affiliations":[{"id":16196,"text":"Scripps Institution of Oceanography, La Jolla, CA","active":true,"usgs":false}],"preferred":false,"id":422494,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Flick, R.E.","contributorId":17820,"corporation":false,"usgs":true,"family":"Flick","given":"R.E.","email":"","affiliations":[],"preferred":false,"id":422493,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70029377,"text":"70029377 - 2005 - Use of dissolved and vapor‐phase gases to investigate methanogenic degradation of petroleum hydrocarbon contamination in the subsurface","interactions":[],"lastModifiedDate":"2018-11-05T09:36:18","indexId":"70029377","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3722,"text":"Water Resources Research","onlineIssn":"1944-7973","printIssn":"0043-1397","active":true,"publicationSubtype":{"id":10}},"title":"Use of dissolved and vapor‐phase gases to investigate methanogenic degradation of petroleum hydrocarbon contamination in the subsurface","docAbstract":"<p><span>At many sites contaminated with petroleum hydrocarbons, methanogenesis is a significant degradation pathway. Techniques to estimate CH</span><sub>4</sub><span><span>&nbsp;</span>production, consumption, and transport processes are needed to understand the geochemical system, provide a complete carbon mass balance, and quantify the hydrocarbon degradation rate. Dissolved and vapor‐phase gas data collected at a petroleum hydrocarbon contaminated site near Bemidji, Minnesota, demonstrate that naturally occurring nonreactive or relatively inert gases such as Ar and N</span><sub>2</sub><span><span>&nbsp;</span>can be effectively used to better understand and quantify physical and chemical processes related to methanogenic activity in the subsurface. In the vadose zone, regions of Ar and N</span><sub>2</sub><span><span>&nbsp;</span>depletion and enrichment are indicative of methanogenic and methanotrophic zones, and concentration gradients between the regions suggest that reaction‐induced advection can be an important gas transport process. In the saturated zone, dissolved Ar and N</span><sub>2</sub><span><span>&nbsp;</span>concentrations are used to quantify degassing driven by methanogenesis and also suggest that attenuation of methane along the flow path, into the downgradient aquifer, is largely controlled by physical processes. Slight but discernable preferential depletion of N</span><sub>2</sub><span><span>&nbsp;</span>over Ar, in both the saturated and unsaturated zones near the free‐phase oil, suggests reactivity of N</span><sub>2</sub><span><span>&nbsp;</span>and is consistent with other evidence indicating that nitrogen fixation by microbial activity is taking place at this site.</span></p>","language":"English","publisher":"American Geophysical Union","doi":"10.1029/2004WR003433","usgsCitation":"Amos, R.T., Mayer, K.U., Bekins, B.A., Delin, G.N., and Williams, R.L., 2005, Use of dissolved and vapor‐phase gases to investigate methanogenic degradation of petroleum hydrocarbon contamination in the subsurface: Water Resources Research, v. 41, no. 2, W02001; 15 p., https://doi.org/10.1029/2004WR003433.","productDescription":"W02001; 15 p.","costCenters":[{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":477950,"rank":1,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1029/2004wr003433","text":"Publisher Index Page"},{"id":237520,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"41","issue":"2","noUsgsAuthors":false,"publicationDate":"2005-02-02","publicationStatus":"PW","scienceBaseUri":"505bbee6e4b08c986b329852","contributors":{"authors":[{"text":"Amos, Richard T.","contributorId":69081,"corporation":false,"usgs":true,"family":"Amos","given":"Richard","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":422472,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Mayer, K. Ulrich","contributorId":151069,"corporation":false,"usgs":false,"family":"Mayer","given":"K.","email":"","middleInitial":"Ulrich","affiliations":[{"id":18176,"text":"Department of Earth and Ocean Science, University of British Columbia, Vancouver, British Columbia, Canada","active":true,"usgs":false}],"preferred":false,"id":422474,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Bekins, Barbara A. 0000-0002-1411-6018 babekins@usgs.gov","orcid":"https://orcid.org/0000-0002-1411-6018","contributorId":1348,"corporation":false,"usgs":true,"family":"Bekins","given":"Barbara","email":"babekins@usgs.gov","middleInitial":"A.","affiliations":[{"id":438,"text":"National Research Program - Western Branch","active":true,"usgs":true},{"id":36183,"text":"Hydro-Ecological Interactions Branch","active":true,"usgs":true},{"id":436,"text":"National Research Program - Eastern Branch","active":true,"usgs":true},{"id":37277,"text":"WMA - Earth System Processes Division","active":true,"usgs":true}],"preferred":true,"id":422475,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Delin, Geoffrey N. 0000-0001-7991-6158 delin@usgs.gov","orcid":"https://orcid.org/0000-0001-7991-6158","contributorId":2610,"corporation":false,"usgs":true,"family":"Delin","given":"Geoffrey","email":"delin@usgs.gov","middleInitial":"N.","affiliations":[{"id":5063,"text":"Central Water Science Field Team","active":true,"usgs":true}],"preferred":true,"id":422471,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Williams, Randi L.","contributorId":150556,"corporation":false,"usgs":false,"family":"Williams","given":"Randi","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":422473,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":70028183,"text":"70028183 - 2005 - Geochemistry of speleothem records from southern Illinois: Development of (234U)/(238U) as a proxy for paleoprecipitation","interactions":[],"lastModifiedDate":"2012-03-12T17:20:43","indexId":"70028183","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1213,"text":"Chemical Geology","active":true,"publicationSubtype":{"id":10}},"title":"Geochemistry of speleothem records from southern Illinois: Development of (234U)/(238U) as a proxy for paleoprecipitation","docAbstract":"Natural waters universally show fractionation of uranium series (U-series) parent-daughter pairs, with the disequilibrium between 234U and 238U (234U)/(238U) commonly used as a tracer of groundwater flow. Because speleothems provide a temporal record of geochemical variations in groundwater precipitating calcite, (234U)/(238U) variations in speleothems provide a unique method of investigating water-rock interaction processes over millennium time scales. We present high precision Thermal Ionization Mass Spectrometric (TIMS) U-series analyses of speleothems and drip waters from Fogelpole Cave in southern Illinois. Data from all speleothems from the cave show an inverse correlation between (234U)/(238U) and U concentration, following the pattern observed in groundwaters globally. Within a 65-cm-long stalagmite, concordant 234U-238 U-230Th and 235U-231Pa ages for 5 samples indicate accurate chronology from 78.5 ka to 30 ka. Notably, (234U)/(238U)o which differs from most speleothems by having (234U)/(238U)o <1, positively correlates with speleothem growth rate. We generalize this to the observation that speleothems globally show (234U)/ (238U)o deviating farther from secular equilibrium at lower growth rates and approaching secular equilibrium at higher grow rates. Based on the Fogelpole observations, we suggest that groundwater (234U)/(238U) is controlled by the U oxidation state, the U concentration of the water and the fluid velocity. A transport model whereby U-series nuclides react and exchange with mineral surfaces can reproduce the observed trend between growth rate and (234U)/(238U)o. Based on this result, we suggest that (234U)/(238U)o in speleothems may record changes in hydrologic flux with time and thus could provide a useful proxy for long term records of paleoprecipitation. ?? 2005 Elsevier B.V. All rights reserved.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Chemical Geology","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1016/j.chemgeo.2005.02.005","issn":"00092541","usgsCitation":"Zhou, J., Lundstrom, C., Fouke, B., Panno, S., Hackley, K., and Curry, B., 2005, Geochemistry of speleothem records from southern Illinois: Development of (234U)/(238U) as a proxy for paleoprecipitation: Chemical Geology, v. 221, no. 1-2, p. 1-20, https://doi.org/10.1016/j.chemgeo.2005.02.005.","startPage":"1","endPage":"20","numberOfPages":"20","costCenters":[],"links":[{"id":210096,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1016/j.chemgeo.2005.02.005"},{"id":236914,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"221","issue":"1-2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a1714e4b0c8380cd5538e","contributors":{"authors":[{"text":"Zhou, Juanzuo","contributorId":59217,"corporation":false,"usgs":true,"family":"Zhou","given":"Juanzuo","email":"","affiliations":[],"preferred":false,"id":416946,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Lundstrom, C.C.","contributorId":72997,"corporation":false,"usgs":true,"family":"Lundstrom","given":"C.C.","email":"","affiliations":[],"preferred":false,"id":416947,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Fouke, B.","contributorId":31187,"corporation":false,"usgs":true,"family":"Fouke","given":"B.","affiliations":[],"preferred":false,"id":416943,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Panno, S.","contributorId":42016,"corporation":false,"usgs":true,"family":"Panno","given":"S.","email":"","affiliations":[],"preferred":false,"id":416944,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Hackley, K.","contributorId":44343,"corporation":false,"usgs":true,"family":"Hackley","given":"K.","email":"","affiliations":[],"preferred":false,"id":416945,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Curry, B.","contributorId":89320,"corporation":false,"usgs":true,"family":"Curry","given":"B.","email":"","affiliations":[],"preferred":false,"id":416948,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}}
,{"id":70028192,"text":"70028192 - 2005 - Aminobacter ciceronei sp. nov. and Aminobacter lissarensis sp. nov., isolated from various terrestrial environments","interactions":[],"lastModifiedDate":"2018-10-31T09:30:23","indexId":"70028192","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2076,"text":"International Journal of Systematic and Evolutionary Microbiology","active":true,"publicationSubtype":{"id":10}},"title":"Aminobacter ciceronei sp. nov. and Aminobacter lissarensis sp. nov., isolated from various terrestrial environments","docAbstract":"<p>The&nbsp;<span>bacterial strains IMB-1</span><span class=\"jp-sup\">T</span><span>&nbsp;and CC495</span><span class=\"jp-sup\">T</span><span>, which are capable of growth on methyl chloride (CH</span><span class=\"jp-sub\">3</span><span>Cl, chloromethane) and methyl bromide (CH</span><span class=\"jp-sub\">3</span><span>Br, bromomethane), were isolated from agricultural soil in California fumigated with CH</span><span class=\"jp-sub\">3</span><span>Br, and woodland soil in Northern Ireland, respectively. Two pesticide-/herbicide-degrading bacteria, strains ER2 and C147, were isolated from agricultural soil in Canada. Strain ER2 degrades&nbsp;</span><span class=\"jp-italic\">N</span><span>-methyl carbamate insecticides, and strain C147 degrades triazine herbicides widely used in agriculture. On the basis of their morphological, physiological and genotypic characteristics, these four strains are considered to represent two novel species of the genus&nbsp;</span><span class=\"jp-italic\">Aminobacter</span><span>, for which the names&nbsp;</span><span class=\"jp-italic\">Aminobacter ciceronei</span><span>&nbsp;sp. nov. (type strain IMB-1</span><span class=\"jp-sup\">T</span><span>=ATCC 202197</span><span class=\"jp-sup\">T</span><span>=CIP 108660</span><span class=\"jp-sup\">T</span><span>=CCUG 50580</span><span class=\"jp-sup\">T</span><span>; strains ER2 and C147) and&nbsp;</span><span class=\"jp-italic\">Aminobacter lissarensis</span><span>&nbsp;sp. nov. (type strain CC495</span><span class=\"jp-sup\">T</span><span>=NCIMB 13798</span><span class=\"jp-sup\">T</span><span>=CIP 108661</span><span class=\"jp-sup\">T</span><span>=CCUG 50579</span><span class=\"jp-sup\">T</span><span>) are proposed.</span></p>","language":"English","publisher":"Microbiology Society ","doi":"10.1099/ijs.0.63716-0","issn":"14665026","usgsCitation":"McDonald, I., Kampfer, P., Topp, E., Warner, K., Cox, M., Connell, H.T., Miller, L., Larkin, M., Ducrocq, V., Coulter, C., Harper, D., Murrell, J., and Oremland, R., 2005, Aminobacter ciceronei sp. nov. and Aminobacter lissarensis sp. nov., isolated from various terrestrial environments: International Journal of Systematic and Evolutionary Microbiology, v. 55, no. 5, p. 1827-1832, https://doi.org/10.1099/ijs.0.63716-0.","productDescription":"6 p.","startPage":"1827","endPage":"1832","costCenters":[{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":477815,"rank":10000,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"http://resolver.tudelft.nl/uuid:baf9e3e5-d554-4215-903e-a299daaddb57","text":"Publisher Index Page"},{"id":237093,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":210233,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1099/ijs.0.63716-0"}],"volume":"55","issue":"5","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059e9bce4b0c8380cd48400","contributors":{"authors":[{"text":"McDonald, I.R.","contributorId":23313,"corporation":false,"usgs":true,"family":"McDonald","given":"I.R.","email":"","affiliations":[],"preferred":false,"id":416978,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Kampfer, P.","contributorId":51525,"corporation":false,"usgs":true,"family":"Kampfer","given":"P.","email":"","affiliations":[],"preferred":false,"id":416982,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Topp, E.","contributorId":51526,"corporation":false,"usgs":true,"family":"Topp","given":"E.","email":"","affiliations":[],"preferred":false,"id":416983,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Warner, K.L.","contributorId":73781,"corporation":false,"usgs":true,"family":"Warner","given":"K.L.","email":"","affiliations":[],"preferred":false,"id":416985,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Cox, M.J.","contributorId":22562,"corporation":false,"usgs":true,"family":"Cox","given":"M.J.","email":"","affiliations":[],"preferred":false,"id":416977,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Connell, Hancock T.L.","contributorId":9418,"corporation":false,"usgs":true,"family":"Connell","given":"Hancock","email":"","middleInitial":"T.L.","affiliations":[],"preferred":false,"id":416976,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Miller, L.G.","contributorId":32522,"corporation":false,"usgs":true,"family":"Miller","given":"L.G.","email":"","affiliations":[],"preferred":false,"id":416980,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Larkin, M.J.","contributorId":103856,"corporation":false,"usgs":true,"family":"Larkin","given":"M.J.","email":"","affiliations":[],"preferred":false,"id":416988,"contributorType":{"id":1,"text":"Authors"},"rank":8},{"text":"Ducrocq, V.","contributorId":33913,"corporation":false,"usgs":true,"family":"Ducrocq","given":"V.","email":"","affiliations":[],"preferred":false,"id":416981,"contributorType":{"id":1,"text":"Authors"},"rank":9},{"text":"Coulter, C.","contributorId":64875,"corporation":false,"usgs":true,"family":"Coulter","given":"C.","email":"","affiliations":[],"preferred":false,"id":416984,"contributorType":{"id":1,"text":"Authors"},"rank":10},{"text":"Harper, D.B.","contributorId":76506,"corporation":false,"usgs":true,"family":"Harper","given":"D.B.","email":"","affiliations":[],"preferred":false,"id":416986,"contributorType":{"id":1,"text":"Authors"},"rank":11},{"text":"Murrell, J.C.","contributorId":25731,"corporation":false,"usgs":true,"family":"Murrell","given":"J.C.","email":"","affiliations":[],"preferred":false,"id":416979,"contributorType":{"id":1,"text":"Authors"},"rank":12},{"text":"Oremland, R.S.","contributorId":97512,"corporation":false,"usgs":true,"family":"Oremland","given":"R.S.","email":"","affiliations":[],"preferred":false,"id":416987,"contributorType":{"id":1,"text":"Authors"},"rank":13}]}}
,{"id":70029110,"text":"70029110 - 2005 - Enhanced zinc consumption causes memory deficits and increased brain levels of zinc","interactions":[],"lastModifiedDate":"2018-10-31T10:03:02","indexId":"70029110","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3077,"text":"Physiology & Behavior","printIssn":"0031-9384","active":true,"publicationSubtype":{"id":10}},"title":"Enhanced zinc consumption causes memory deficits and increased brain levels of zinc","docAbstract":"<div id=\"abstracts\" class=\"Abstracts\"><div id=\"aep-abstract-id12\" class=\"abstract author\"><div id=\"aep-abstract-sec-id13\"><p>Zinc deficiency has been shown to impair cognitive functioning, but little work has been done on the effects of elevated zinc. This research examined the effect on memory of raising Sprague–Dawley rats on enhanced levels of zinc (10 ppm ZnCO<sub>3</sub>; 0.153 mM) in the drinking water for periods of 3 or 9 months, both pre- and postnatally. Controls were raised on lab water. Memory was tested in a series of Morris Water Maze (MWM) experiments, and zinc-treated rats were found to have impairments in both reference and working memory. They were significantly slower to find a stationary platform and showed greater thigmotaxicity, a measure of anxiety. On a working memory task, where the platform was moved each day, zinc-treated animals had longer latencies over both trials and days, swam further from the platform, and showed greater thigmotaxicity. On trials using an Atlantis platform, which remained in one place but was lowered on probe trials, the zinc-treated animals had significantly fewer platform crossings, spent less time in the target quadrant, and did not swim as close to the platform position. They had significantly greater latency on nonprobe trials. Microprobe synchrotron X-ray fluorescence (μSXRF) confirmed that brain zinc levels were increased by adding ZnCO<sub>3</sub><span>&nbsp;</span>to the drinking water. These data show that long-term dietary administration of zinc can lead to impairments in cognitive function.</p></div></div></div>","language":"English","publisher":"Elsevier","doi":"10.1016/j.physbeh.2004.10.009","issn":"00319384","usgsCitation":"Flinn, J., Hunter, D., Linkous, D., Lanzirotti, A., Smith, L., Brightwell, J., and Jones, B., 2005, Enhanced zinc consumption causes memory deficits and increased brain levels of zinc: Physiology & Behavior, v. 83, no. 5, p. 793-803, https://doi.org/10.1016/j.physbeh.2004.10.009.","productDescription":"11 p.","startPage":"793","endPage":"803","costCenters":[{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":237359,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":210442,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1016/j.physbeh.2004.10.009"}],"volume":"83","issue":"5","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a0970e4b0c8380cd51ef6","contributors":{"authors":[{"text":"Flinn, J.M.","contributorId":45892,"corporation":false,"usgs":true,"family":"Flinn","given":"J.M.","email":"","affiliations":[],"preferred":false,"id":421361,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hunter, D.","contributorId":70130,"corporation":false,"usgs":true,"family":"Hunter","given":"D.","affiliations":[],"preferred":false,"id":421364,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Linkous, D.H.","contributorId":81303,"corporation":false,"usgs":true,"family":"Linkous","given":"D.H.","email":"","affiliations":[],"preferred":false,"id":421365,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Lanzirotti, A.","contributorId":52772,"corporation":false,"usgs":true,"family":"Lanzirotti","given":"A.","affiliations":[],"preferred":false,"id":421363,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Smith, L.N.","contributorId":20533,"corporation":false,"usgs":true,"family":"Smith","given":"L.N.","email":"","affiliations":[],"preferred":false,"id":421360,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Brightwell, J.","contributorId":20142,"corporation":false,"usgs":true,"family":"Brightwell","given":"J.","email":"","affiliations":[],"preferred":false,"id":421359,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Jones, B.F.","contributorId":52156,"corporation":false,"usgs":true,"family":"Jones","given":"B.F.","email":"","affiliations":[],"preferred":false,"id":421362,"contributorType":{"id":1,"text":"Authors"},"rank":7}]}}
,{"id":70029288,"text":"70029288 - 2005 - The composition of coexisting jarosite-group minerals and water from the Richmond mine, Iron Mountain, California","interactions":[],"lastModifiedDate":"2018-10-31T09:22:55","indexId":"70029288","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1177,"text":"Canadian Mineralogist","active":true,"publicationSubtype":{"id":10}},"title":"The composition of coexisting jarosite-group minerals and water from the Richmond mine, Iron Mountain, California","docAbstract":"<p><span>Jarosite-group minerals accumulate in the form of stalactites and fine-grained mud on massive pyrite in the D drift of the Richmond mine, Iron Mountain, California. Water samples were collected by placing beakers under the dripping stalactites and by extracting pore water from the mud using a centrifuge. The water is rich in Fe</span><sup>3+</sup><span><span>&nbsp;</span>and SO</span><sub>4</sub><span>&nbsp;</span><sup>2−</sup><span>, with a pH of approximately 2.1, which is significantly higher than the extremely acidic waters found elsewhere in the mine. Electron-microprobe analysis and X-ray mapping indicate that the small crystals (&lt;10 μm in diameter) are compositionally zoned with respect to Na and K, and include hydronium jarosite corresponding to the formula (H</span><sub>3</sub><span>O)</span><sub>0.6</sub><span>K</span><sub>0.3</sub><span>Na</span><sub>0.1</sub><span>Fe</span><sub>3</sub><span>&nbsp;</span><sup>3+</sup><span>(SO</span><sub>4</sub><span>)</span><sub>2</sub><span>(OH)</span><sub>6</sub><span>. The proton-microprobe analyses indicate that the jarosite-group minerals contain significant amounts of As, Pb and Zn, and minor levels of Bi, Rb, Sb, Se, Sn and Sr. Speciation modeling indicates that the drip waters are supersaturated with respect to jarosite-group minerals. The expected range in composition of jarosite-group solid-solution in equilibrium with the pore water extracted from the mud was found to be consistent with the observed range in composition.</span></p>","language":"English","publisher":"Mineralogical Associaion of Canada","doi":"10.2113/gscanmin.43.4.1225","usgsCitation":"Jamieson, H.E., Robinson, C., Alpers, C.N., Nordstrom, D.K., Poustovetov, A., and Lowers, H., 2005, The composition of coexisting jarosite-group minerals and water from the Richmond mine, Iron Mountain, California: Canadian Mineralogist, v. 43, no. 4, p. 1225-1242, https://doi.org/10.2113/gscanmin.43.4.1225.","productDescription":"18 p.","startPage":"1225","endPage":"1242","costCenters":[{"id":154,"text":"California Water Science Center","active":true,"usgs":true},{"id":171,"text":"Central Mineral and Environmental Resources Science Center","active":true,"usgs":true},{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true},{"id":5044,"text":"National Research Program - Central Branch","active":true,"usgs":true}],"links":[{"id":237874,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"California","otherGeospatial":"Iron Mountain","volume":"43","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505baa4be4b08c986b3227b6","contributors":{"authors":[{"text":"Jamieson, Heather E.","contributorId":150176,"corporation":false,"usgs":false,"family":"Jamieson","given":"Heather","email":"","middleInitial":"E.","affiliations":[{"id":7029,"text":"Queen's University, Kingston, Ontario, Canada","active":true,"usgs":false}],"preferred":false,"id":422084,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Robinson, Clare","contributorId":195273,"corporation":false,"usgs":false,"family":"Robinson","given":"Clare","email":"","affiliations":[],"preferred":false,"id":422086,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Alpers, Charles N. 0000-0001-6945-7365 cnalpers@usgs.gov","orcid":"https://orcid.org/0000-0001-6945-7365","contributorId":411,"corporation":false,"usgs":true,"family":"Alpers","given":"Charles","email":"cnalpers@usgs.gov","middleInitial":"N.","affiliations":[{"id":154,"text":"California Water Science Center","active":true,"usgs":true}],"preferred":true,"id":422088,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Nordstrom, D. Kirk 0000-0003-3283-5136 dkn@usgs.gov","orcid":"https://orcid.org/0000-0003-3283-5136","contributorId":749,"corporation":false,"usgs":true,"family":"Nordstrom","given":"D.","email":"dkn@usgs.gov","middleInitial":"Kirk","affiliations":[{"id":37277,"text":"WMA - Earth System Processes Division","active":true,"usgs":true},{"id":5044,"text":"National Research Program - Central Branch","active":true,"usgs":true}],"preferred":false,"id":422087,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Poustovetov, Alexei","contributorId":68516,"corporation":false,"usgs":false,"family":"Poustovetov","given":"Alexei","email":"","affiliations":[],"preferred":false,"id":422085,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Lowers, Heather A. hlowers@usgs.gov","contributorId":149265,"corporation":false,"usgs":true,"family":"Lowers","given":"Heather A.","email":"hlowers@usgs.gov","affiliations":[{"id":171,"text":"Central Mineral and Environmental Resources Science Center","active":true,"usgs":true}],"preferred":false,"id":422083,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}}
,{"id":70027602,"text":"70027602 - 2005 - Variations in climate and ephemeral channel recharge in southeastern Arizona, United States","interactions":[],"lastModifiedDate":"2018-03-30T11:03:32","indexId":"70027602","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3722,"text":"Water Resources Research","onlineIssn":"1944-7973","printIssn":"0043-1397","active":true,"publicationSubtype":{"id":10}},"title":"Variations in climate and ephemeral channel recharge in southeastern Arizona, United States","docAbstract":"<p><span>Significant variations in interannual and decadal recharge rates are likely in alluvial basins of the semiarid southwestern United States on the basis of decadal variations in climate and precipitation and correlation of El Niño with high rates of winter precipitation and streamflow. A better understanding of the magnitude of recharge variations in semiarid and arid regions would reduce water budget uncertainty. Variability of ephemeral channel recharge with climate in southeastern Arizona was investigated through analysis of hydrologic monitoring near three ephemeral streams in southeastern Arizona during the middle to late 1990s and by relating the results to long‐term hydrologic and climatic trends. The analysis used precipitation, streamflow, water levels in wells, estimates of groundwater storage change from repeat gravity surveys, and two climatic indicators of El Niño–Southern Oscillation (ENSO), Southern Oscillation index, and Pacific Decadal Oscillation (PDO). Results indicate that variations in winter recharge are related to ENSO. El Niño conditions correspond with a greater probability of high rates of winter precipitation, streamflow, and recharge. La Niña conditions are almost exclusively associated with below‐average recharge. Rates of recharge along Rillito Creek near Tucson during 1977–1998, a period of frequent El Niño conditions and positive PDO values, were 3 times recharge rates during 1941–1957, a period dominated by La Niña conditions and low PDO values. Quantification of recharge variability with decadal climate cycles should improve estimates of rates of aquifer drainage and replenishment in the region. Similar methods are applicable to other regions where thick unsaturated zones can accept significant periodic recharge.</span></p>","language":"English","publisher":"American Geophysical Union","doi":"10.1029/2004WR003255","usgsCitation":"Pool, D.R., 2005, Variations in climate and ephemeral channel recharge in southeastern Arizona, United States: Water Resources Research, v. 41, no. 11, Article W11403; 25 p., https://doi.org/10.1029/2004WR003255.","productDescription":"Article W11403; 25 p.","costCenters":[],"links":[{"id":489773,"rank":1,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1029/2004wr003255","text":"Publisher Index Page"},{"id":238456,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Arizona","volume":"41","issue":"11","noUsgsAuthors":false,"publicationDate":"2005-11-02","publicationStatus":"PW","scienceBaseUri":"505bc179e4b08c986b32a5b7","contributors":{"authors":[{"text":"Pool, D. R.","contributorId":75581,"corporation":false,"usgs":true,"family":"Pool","given":"D.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":414317,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70027638,"text":"70027638 - 2005 - Quasi‐steady centrifuge method for unsaturated hydraulic properties","interactions":[],"lastModifiedDate":"2018-10-31T10:44:31","indexId":"70027638","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3722,"text":"Water Resources Research","onlineIssn":"1944-7973","printIssn":"0043-1397","active":true,"publicationSubtype":{"id":10}},"title":"Quasi‐steady centrifuge method for unsaturated hydraulic properties","docAbstract":"<p><span>We have developed the quasi‐steady centrifuge (QSC) method as a variation of the steady state centrifuge method that can be implemented simply and inexpensively with greater versatility in terms of sample size and other features. It achieves these advantages by somewhat relaxing the criterion for steadiness of flow through the sample. This compromise entails an increase in measurement uncertainty but to a degree that is tolerable in most applications. We have tested this new approach with an easily constructed apparatus to establish a quasi‐steady flow of water in unsaturated porous rock samples spinning in a centrifuge, obtaining measurements of unsaturated hydraulic conductivity and water retention that agree with results of other methods. The QSC method is adaptable to essentially any centrifuge suitable for hydrogeologic applications, over a wide range of sizes and operating speeds. The simplified apparatus and greater adaptability of this method expands the potential for exploring situations that are common in nature but have been the subject of few laboratory investigations.</span></p>","language":"English","publisher":"American Geophysical Union","doi":"10.1029/2005WR003957","usgsCitation":"Caputo, M., and Nimmo, J.R., 2005, Quasi‐steady centrifuge method for unsaturated hydraulic properties: Water Resources Research, v. 41, no. 11, W11504; 5 p., https://doi.org/10.1029/2005WR003957.","productDescription":"W11504; 5 p.","costCenters":[{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":238498,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"41","issue":"11","noUsgsAuthors":false,"publicationDate":"2005-11-16","publicationStatus":"PW","scienceBaseUri":"505a927ce4b0c8380cd808a9","contributors":{"authors":[{"text":"Caputo, Maria C.","contributorId":48756,"corporation":false,"usgs":false,"family":"Caputo","given":"Maria C.","affiliations":[],"preferred":false,"id":414514,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Nimmo, John R. 0000-0001-8191-1727 jrnimmo@usgs.gov","orcid":"https://orcid.org/0000-0001-8191-1727","contributorId":757,"corporation":false,"usgs":true,"family":"Nimmo","given":"John","email":"jrnimmo@usgs.gov","middleInitial":"R.","affiliations":[{"id":37277,"text":"WMA - Earth System Processes Division","active":true,"usgs":true},{"id":438,"text":"National Research Program - Western Branch","active":true,"usgs":true}],"preferred":true,"id":414515,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70027714,"text":"70027714 - 2005 - Steam injection pilot study in a contaminated fractured limestone (Maine, USA): Modeling and analysis of borehole radar reflection data","interactions":[],"lastModifiedDate":"2020-03-10T15:59:19","indexId":"70027714","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"Steam injection pilot study in a contaminated fractured limestone (Maine, USA): Modeling and analysis of borehole radar reflection data","docAbstract":"Steam-enhanced remediation (SER) has been successfully used to remove DNAPL and LNAPL contaminants in porous media. Between August and November 2002, SER was tested in fractured limestone at the former Loring Air Force Base, in Maine, USA. During the SER investigation, the U.S. Geological Survey conducted a series of borehole radar surveys to evaluate the effectiveness of radar methods for monitoring the movement of steam and heat through the fractured limestone. The data were collected before steam injection, 10 days after the beginning of injection, and at the end of injection. In this paper, reflection-mode borehole radar data from wells JBW-7816 and JBW-7817A are presented and discussed. Theoretical modeling was performed to predict the variation of fracture reflectivity owed to heating, to show displacement of water and to assess the effect of SER at the site. Analysis of the radar profile data indicates some variations resulting from heating (increase of continuity of reflectors, attenuation of deeper reflections) but no substantial variation of traveltimes. Spectral content analysis of several individual reflections surrounding the boreholes was used to investigate the replacement of water by steam in the fractures. Observed decrease in radar reflectivity was too small to be explained by a replacement of water by steam, except for two high-amplitude reflectors, which disappeared near the end of the injection; moreover, no change of polarity, consistent with steam replacing water, was observed. The decrease of amplitude was greater for reflectors near well JBW-7817A and is explained by a greater heating around this well.","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Proceedings of the 3rd International Workshop on Advanced Ground Penetrating Radar, IWAGPR 2005","largerWorkSubtype":{"id":12,"text":"Conference publication"},"conferenceTitle":"3rd International Workshop on Advanced Ground Penetrating Radar, IWAGPR 2005","conferenceDate":"May 3-5, 2005","conferenceLocation":"Delft, Netherlands","language":"English","publisher":"IEEE","doi":"10.1109/AGPR.2005.1487846","isbn":"9080970115; 9789080970113","usgsCitation":"Gregoire, C., Lane, J., and Joesten, P., 2005, Steam injection pilot study in a contaminated fractured limestone (Maine, USA): Modeling and analysis of borehole radar reflection data, <i>in</i> Proceedings of the 3rd International Workshop on Advanced Ground Penetrating Radar, IWAGPR 2005, v. 2005, Delft, Netherlands, May 3-5, 2005, p. 55-59, https://doi.org/10.1109/AGPR.2005.1487846.","productDescription":"5 p.","startPage":"55","endPage":"59","numberOfPages":"5","costCenters":[{"id":493,"text":"Office of Ground Water","active":true,"usgs":true},{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":237992,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United 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 \"}}]}","volume":"2005","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505b9821e4b08c986b31be4d","contributors":{"authors":[{"text":"Gregoire, C.","contributorId":37142,"corporation":false,"usgs":true,"family":"Gregoire","given":"C.","email":"","affiliations":[],"preferred":false,"id":414879,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Lane, J.W. Jr.","contributorId":66723,"corporation":false,"usgs":true,"family":"Lane","given":"J.W.","suffix":"Jr.","email":"","affiliations":[],"preferred":false,"id":414881,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Joesten, P. K.","contributorId":62818,"corporation":false,"usgs":true,"family":"Joesten","given":"P. K.","affiliations":[],"preferred":false,"id":414880,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70027746,"text":"70027746 - 2005 - Delineating copper accumulation pathways for the freshwater bivalve Corbicula using stable copper isotopes","interactions":[],"lastModifiedDate":"2018-10-31T10:56:15","indexId":"70027746","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1571,"text":"Environmental Toxicology and Chemistry","active":true,"publicationSubtype":{"id":10}},"title":"Delineating copper accumulation pathways for the freshwater bivalve Corbicula using stable copper isotopes","docAbstract":"<div class=\"abstract-group\"><div class=\"article-section__content en main\"><p>Delineation of metal uptake routes in aquatic invertebrates is critical for characterizing bioaccumulation dynamics and assessing risks associated with metal exposure. Here we demonstrate that Cu stable isotopic ratios can be manipulated in both exposure media and algae to determine the efflux rate constant (<i>k</i><sub>e</sub>) and to estimate Cu assimilation efficiency (AE) from ingested food in a freshwater bivalve (<i>Corbicula fluminea</i>). The Cu AE in<span>&nbsp;</span><i>Corbicula</i><span>&nbsp;</span>fed<span>&nbsp;</span><sup>65</sup>Cu‐spiked<span>&nbsp;</span><i>Cryptomonas ozolini</i><span>&nbsp;</span>was 38%. Copper uptake routes had no significant influence on efflux;<span>&nbsp;</span><i>k</i><sub>e</sub><span>&nbsp;</span>of 0.004 per day characterized the slowest component of efflux following short‐term exposures to<span>&nbsp;</span><sup>65</sup>Cu in water or in both food and water. Incorporation of the physiological parameters for dietary and dissolved uptake as well as rate constants of loss into a bioaccumulation model allowed for assessing the relative contribution of water and food as Cu sources. At [<sup>65</sup>Cu<sup>2+</sup>] of 6.7 μg/L,<span>&nbsp;</span><i>Corbicula</i>accumulated twice as much Cu from diet as from water. In most freshwater systems, the dietary pathway is likely to act as the major Cu uptake route for<span>&nbsp;</span><i>Corbicula</i>. Extrapolation of our laboratory results to the San Francisco Bay—Delta (California, USA) indicated that our biodynamic model and the laboratory‐derived parameters for dietary<span>&nbsp;</span><sup>65</sup>Cu uptake provided a realistic representation of the processes involved in Cu accumulation by the bivalve<span>&nbsp;</span><i>Corbicula</i>.</p></div></div>","language":"English","publisher":"SETAC","doi":"10.1897/04-608R.1","issn":"07307268","usgsCitation":"Croteau, M., and Luoma, S., 2005, Delineating copper accumulation pathways for the freshwater bivalve Corbicula using stable copper isotopes: Environmental Toxicology and Chemistry, v. 24, no. 11, p. 2871-2878, https://doi.org/10.1897/04-608R.1.","productDescription":"8 p.","startPage":"2871","endPage":"2878","onlineOnly":"N","costCenters":[{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":238429,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":211201,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1897/04-608R.1"}],"volume":"24","issue":"11","noUsgsAuthors":false,"publicationDate":"2005-11-01","publicationStatus":"PW","scienceBaseUri":"5059fe61e4b0c8380cd4ece8","contributors":{"authors":[{"text":"Croteau, M.-N.","contributorId":37511,"corporation":false,"usgs":true,"family":"Croteau","given":"M.-N.","email":"","affiliations":[],"preferred":false,"id":415045,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Luoma, S. N.","contributorId":86353,"corporation":false,"usgs":true,"family":"Luoma","given":"S. N.","affiliations":[],"preferred":false,"id":415046,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70027769,"text":"70027769 - 2005 - Assessing water source and channel type as factors affecting benthic macroinvertebrate and periphyton assemblages in the highly urbanized Santa Ana River Basin, California","interactions":[],"lastModifiedDate":"2018-06-08T12:59:53","indexId":"70027769","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":718,"text":"American Fisheries Society Symposium","active":true,"publicationSubtype":{"id":10}},"title":"Assessing water source and channel type as factors affecting benthic macroinvertebrate and periphyton assemblages in the highly urbanized Santa Ana River Basin, California","docAbstract":"The Santa Ana River basin is the largest stream system in Southern California and includes a densely populated coastal area. Extensive urbanization has altered the geomorphology and hydrology of the streams, adversely affecting aquatic communities. We studied macroinvertebrate and periphyton assemblages in relation to two categorical features of the highly engineered hydrologic system-water source and channel type. Four water sources were identified-natural, urban-impacted groundwater, urban runoff, and treated wastewater. Three channel types were identified-natural, channelized with natural bottom, and concrete-lined. Nineteen sites, covering the range of these two categorical features, were sampled in summer 2000. To minimize the effects of different substrate types among sites, artificial substrates were used for assessing macroinvertebrate and periphyton assemblages. Physical and chemical variables and metrics calculated from macroinvertebrate and periphyton assemblage data were compared among water sources and channel types using analysis of variance and multiple comparison tests. Macroinvertebrate metrics exhibiting significant (P < 0.05) differences between water sources included taxa and Ephemeroptera-Plecoptera-Trichoptera richness, relative richness and abundance of nonchironomid dipterans, orthoclads, oligochaetes, and some functional-feeding groups such as parasites and shredders. Periphyton metrics showing significant differences between water sources included blue-green algae biovolume and relative abundance of nitrogen heterotrophic, eutrophic, motile, and pollution-sensitive diatoms. The relative abundance of trichopterans, tanytarsini chironomids, noninsects, and filter feeders, as well as the relative richness and abundance of diatoms, were significantly different between channel types. Most physical variables were related to channel type, whereas chemical variables and some physical variables (e.g., discharge, velocity, and channel width) were related to water source. These associations were reflected in correlations between metrics, chemical variables, and physical variables. Significant improvements in the aquatic ecosystem of the Santa Ana River basin are possible with management actions such as conversion of concrete-lined channels to channelized streams with natural bottoms that can still maintain flood control to protect life and property.","language":"English","publisher":"American Fisheries Society","issn":"08922284","usgsCitation":"Burton, C.A., Brown, L.R., and Belitz, K., 2005, Assessing water source and channel type as factors affecting benthic macroinvertebrate and periphyton assemblages in the highly urbanized Santa Ana River Basin, California: American Fisheries Society Symposium, v. 2005, no. 47, p. 239-262.","productDescription":"24 p.","startPage":"239","endPage":"262","costCenters":[{"id":154,"text":"California Water Science Center","active":true,"usgs":true}],"links":[{"id":238245,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"2005","issue":"47","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059edf5e4b0c8380cd49b36","contributors":{"authors":[{"text":"Burton, Carmen A. 0000-0002-6381-8833 caburton@usgs.gov","orcid":"https://orcid.org/0000-0002-6381-8833","contributorId":444,"corporation":false,"usgs":true,"family":"Burton","given":"Carmen","email":"caburton@usgs.gov","middleInitial":"A.","affiliations":[{"id":154,"text":"California Water Science Center","active":true,"usgs":true}],"preferred":true,"id":415138,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Brown, Larry R. 0000-0001-6702-4531 lrbrown@usgs.gov","orcid":"https://orcid.org/0000-0001-6702-4531","contributorId":1717,"corporation":false,"usgs":true,"family":"Brown","given":"Larry","email":"lrbrown@usgs.gov","middleInitial":"R.","affiliations":[{"id":154,"text":"California Water Science Center","active":true,"usgs":true}],"preferred":true,"id":415137,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Belitz, Kenneth 0000-0003-4481-2345 kbelitz@usgs.gov","orcid":"https://orcid.org/0000-0003-4481-2345","contributorId":442,"corporation":false,"usgs":true,"family":"Belitz","given":"Kenneth","email":"kbelitz@usgs.gov","affiliations":[{"id":376,"text":"Massachusetts Water Science Center","active":true,"usgs":true},{"id":503,"text":"Office of Water Quality","active":true,"usgs":true},{"id":27111,"text":"National Water Quality Program","active":true,"usgs":true},{"id":451,"text":"National Water Quality Assessment Program","active":true,"usgs":true},{"id":466,"text":"New England Water Science Center","active":true,"usgs":true}],"preferred":true,"id":415136,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70027771,"text":"70027771 - 2005 - Reconstructing a mid-Cretaceous landscape from paleosols in western Canada","interactions":[],"lastModifiedDate":"2012-03-12T17:20:49","indexId":"70027771","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2451,"text":"Journal of Sedimentary Research","onlineIssn":"1938-3681","printIssn":"1527-1404","active":true,"publicationSubtype":{"id":10}},"title":"Reconstructing a mid-Cretaceous landscape from paleosols in western Canada","docAbstract":"The Albian Stage of the mid-Cretaceous was a time of equable climate conditions with high sea levels and broad shallow epeiric seas that may have had a moderating affect on continental climates. A Late Albian landscape surface that developed during a regression and subsequent sea-level rise in the Western Canada Foreland Basin is reconstructed on the basis of correlation of paleosols penetrated by cores through the Paddy Member of the Peace River Formation. Reconstruction of this landscape refines chronostratigraphic relationships and will benefit future paleoclimatological studies milizing continental sphaerosiderite proxy records. The paleosols developed in estuarine sandstones and mudstones, and they exhibit evidence of a polygenetic history. Upon initial exposure and pedogenesis, the Paddy Member developed deeply weathered, well-drained cumulative soil profiles. Later stages of pedogenesis were characterized by hydromorphic soil conditions. The stages of soil development interpreted for the Paddy Member correlate with inferred stages of pedogenic development in time-equivalent formations located both basinward and downslope (upper Viking Formation), and landward and upslope (Boulder Creek Formation). On the basis of the genetic similarity among paleosols in these three correlative formations, the paleosols are interpreted as having formed along a single, continuous landscape surface. Results of this study indicate that the catena concept of pedogenesis along sloping landscapes is applicable to ancient successions. Sphaerosiderites in the Paddy Mem ber paleosols are used to provide proxy values for meteoric ??18O values at 52?? N paleolatitude in the Cretaceous Western Interior Basin. The meteoric ??18O values are used to refine existing interpretations about the mid-Cretaceous paleolatitudinal gradient in meteoric ?? 18O values, and the mid-Cretaceous hydrologic cycle. Copyright ?? 2005, SEPM (Society for Sedimentary Geology).","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Journal of Sedimentary Research","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.2110/jsr.2005.074","issn":"15271404","usgsCitation":"Ufnar, D.F., Gonzalez, L.A., Ludvigson, G.A., Brenner, R.L., Witzke, B., and Leckie, D., 2005, Reconstructing a mid-Cretaceous landscape from paleosols in western Canada: Journal of Sedimentary Research, v. 75, no. 6, p. 984-996, https://doi.org/10.2110/jsr.2005.074.","startPage":"984","endPage":"996","numberOfPages":"13","costCenters":[],"links":[{"id":477829,"rank":10000,"type":{"id":41,"text":"Open Access External Repository Page"},"url":"http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.722.2603","text":"External Repository"},{"id":211099,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.2110/jsr.2005.074"},{"id":238282,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"75","issue":"6","noUsgsAuthors":false,"publicationDate":"2005-11-28","publicationStatus":"PW","scienceBaseUri":"50e4a24de4b0e8fec6cdb560","contributors":{"authors":[{"text":"Ufnar, David F.","contributorId":64371,"corporation":false,"usgs":true,"family":"Ufnar","given":"David","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":415143,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Gonzalez, Luis A.","contributorId":20922,"corporation":false,"usgs":true,"family":"Gonzalez","given":"Luis","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":415142,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Ludvigson, Greg A.","contributorId":80803,"corporation":false,"usgs":true,"family":"Ludvigson","given":"Greg","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":415144,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Brenner, Richard L.","contributorId":94457,"corporation":false,"usgs":false,"family":"Brenner","given":"Richard","email":"","middleInitial":"L.","affiliations":[{"id":13387,"text":"Alaska Department of Fish and Game - Commercial Fisheries, P.O. Box 669, Cordova, AK  99574","active":true,"usgs":false}],"preferred":false,"id":415145,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Witzke, B.J.","contributorId":12976,"corporation":false,"usgs":true,"family":"Witzke","given":"B.J.","affiliations":[],"preferred":false,"id":415141,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Leckie, D.","contributorId":98103,"corporation":false,"usgs":true,"family":"Leckie","given":"D.","email":"","affiliations":[],"preferred":false,"id":415146,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}}
,{"id":70027836,"text":"70027836 - 2005 - Impact of land use and land cover change on groundwater recharge and quality in the southwestern US","interactions":[],"lastModifiedDate":"2018-10-31T08:08:50","indexId":"70027836","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","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":"Impact of land use and land cover change on groundwater recharge and quality in the southwestern US","docAbstract":"<p><span>Humans have exerted large‐scale changes on the terrestrial biosphere, primarily through agriculture; however, the impacts of such changes on the hydrologic cycle are poorly understood. The purpose of this study was to test the hypothesis that the conversion of natural rangeland ecosystems to agricultural ecosystems impacts the subsurface portion of the hydrologic cycle by changing groundwater recharge and flushing salts to underlying aquifers. The hypothesis was examined through point and areal studies investigating the effects of land use/land cover (LU/LC) changes on groundwater recharge and solute transport in the Amargosa Desert (AD) in Nevada and in the High Plains (HP) in Texas, US. Studies use the fact that matric (pore‐water‐pressure) potential and environmental‐tracer profiles in thick unsaturated zones archive past changes in recharging fluxes. Results show that recharge is related to LU/LC as follows: discharge through evapotranspiration (i.e., no recharge; upward fluxes &lt;0.1 mm yr</span><sup>−1</sup><span>) in natural rangeland ecosystems (low matric potentials; high chloride and nitrate concentrations); moderate‐to‐high recharge in irrigated agricultural ecosystems (high matric potentials; low‐to‐moderate chloride and nitrate concentrations) (AD recharge: ∼130–640 mm yr</span><sup>−1</sup><span>); and moderate recharge in nonirrigated (dryland) agricultural ecosystems (high matric potentials; low chloride and nitrate concentrations, and increasing groundwater levels) (HP recharge: ∼9–32 mm yr</span><sup>−1</sup><span>). Replacement of rangeland with agriculture changed flow directions from upward (discharge) to downward (recharge). Recent replacement of rangeland with irrigated ecosystems was documented through downward displacement of chloride and nitrate fronts. Thick unsaturated zones contain a reservoir of salts that are readily mobilized under increased recharge related to LU/LC changes, potentially degrading groundwater quality. Sustainable land use requires quantitative knowledge of the linkages between ecosystem change, recharge, and groundwater quality.</span></p>","language":"English","publisher":"Wiley","doi":"10.1111/j.1365-2486.2005.01026.x","usgsCitation":"Scanlon, B., Reedy, R.C., Stonestrom, D.A., Prudic, D.E., and Dennehy, K.F., 2005, Impact of land use and land cover change on groundwater recharge and quality in the southwestern US: Global Change Biology, v. 11, no. 10, p. 1577-1593, https://doi.org/10.1111/j.1365-2486.2005.01026.x.","productDescription":"17 p.","startPage":"1577","endPage":"1593","costCenters":[{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":238146,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"11","issue":"10","noUsgsAuthors":false,"publicationDate":"2005-09-19","publicationStatus":"PW","scienceBaseUri":"505a38bfe4b0c8380cd61696","contributors":{"authors":[{"text":"Scanlon, Bridget R.","contributorId":74093,"corporation":false,"usgs":true,"family":"Scanlon","given":"Bridget R.","affiliations":[],"preferred":false,"id":415444,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Reedy, Robert C.","contributorId":187509,"corporation":false,"usgs":false,"family":"Reedy","given":"Robert","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":415443,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Stonestrom, David A. 0000-0001-7883-3385 dastones@usgs.gov","orcid":"https://orcid.org/0000-0001-7883-3385","contributorId":2280,"corporation":false,"usgs":true,"family":"Stonestrom","given":"David","email":"dastones@usgs.gov","middleInitial":"A.","affiliations":[{"id":438,"text":"National Research Program - Western Branch","active":true,"usgs":true}],"preferred":true,"id":415445,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Prudic, David E. deprudic@usgs.gov","contributorId":3430,"corporation":false,"usgs":true,"family":"Prudic","given":"David","email":"deprudic@usgs.gov","middleInitial":"E.","affiliations":[{"id":465,"text":"Nevada Water Science Center","active":true,"usgs":true}],"preferred":true,"id":415441,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Dennehy, Kevin F. kdennehy@usgs.gov","contributorId":1128,"corporation":false,"usgs":true,"family":"Dennehy","given":"Kevin","email":"kdennehy@usgs.gov","middleInitial":"F.","affiliations":[{"id":509,"text":"Office of the Associate Director for Water","active":true,"usgs":true}],"preferred":true,"id":415442,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":70027837,"text":"70027837 - 2005 - Evidence and implications of recent climate change in Northern Alaska and other Arctic regions","interactions":[],"lastModifiedDate":"2018-06-12T21:03:17","indexId":"70027837","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1252,"text":"Climatic Change","active":true,"publicationSubtype":{"id":10}},"title":"Evidence and implications of recent climate change in Northern Alaska and other Arctic regions","docAbstract":"The Arctic climate is changing. Permafrost is warming, hydrological processes are changing and biological and social systems are also evolving in response to these changing conditions. Knowing how the structure and function of arctic terrestrial ecosystems are responding to recent and persistent climate change is paramount to understanding the future state of the Earth system and how humans will need to adapt. Our holistic review presents a broad array of evidence that illustrates convincingly; the Arctic is undergoing a system-wide response to an altered climatic state. New extreme and seasonal surface climatic conditions are being experienced, a range of biophysical states and processes influenced by the threshold and phase change of freezing point are being altered, hydrological and biogeochemical cycles are shifting, and more regularly human sub-systems are being affected. Importantly, the patterns, magnitude and mechanisms of change have sometimes been unpredictable or difficult to isolate due to compounding factors. In almost every discipline represented, we show how the biocomplexity of the Arctic system has highlighted and challenged a paucity of integrated scientific knowledge, the lack of sustained observational and experimental time series, and the technical and logistic constraints of researching the Arctic environment. This study supports ongoing efforts to strengthen the interdisciplinarity of arctic system science and improve the coupling of large scale experimental manipulation with sustained time series observations by incorporating and integrating novel technologies, remote sensing and modeling. ?? Springer 2005.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Climatic Change","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1007/s10584-005-5352-2","issn":"01650009","usgsCitation":"Hinzman, L., Bettez, N., Bolton, W., Chapin, F., Dyurgerov, M., Fastie, C., Griffith, B., Hollister, R., Hope, A., Huntington, H., Jensen, A., Jia, G., Jorgenson, T., Kane, D., Klein, D., Kofinas, G., Lynch, A., Lloyd, A., McGuire, A., Nelson, F.E., Oechel, W., Osterkamp, T., Racine, C., Romanovsky, V., Stone, R.S., Stow, D., Sturm, M., Tweedie, C., Vourlitis, G., Walker, M., Walker, D., Webber, P., Welker, J., Winker, K., and Yoshikawa, K., 2005, Evidence and implications of recent climate change in Northern Alaska and other Arctic regions: Climatic Change, v. 72, no. 3, p. 251-298, https://doi.org/10.1007/s10584-005-5352-2.","startPage":"251","endPage":"298","numberOfPages":"48","costCenters":[],"links":[{"id":238179,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":211033,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1007/s10584-005-5352-2"}],"volume":"72","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a0d28e4b0c8380cd52e46","contributors":{"authors":[{"text":"Hinzman, L. D.","contributorId":90083,"corporation":false,"usgs":false,"family":"Hinzman","given":"L. D.","affiliations":[],"preferred":false,"id":415473,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bettez, N.D.","contributorId":94090,"corporation":false,"usgs":true,"family":"Bettez","given":"N.D.","affiliations":[],"preferred":false,"id":415477,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Bolton, W.R.","contributorId":90531,"corporation":false,"usgs":true,"family":"Bolton","given":"W.R.","email":"","affiliations":[],"preferred":false,"id":415474,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Chapin, F.S.","contributorId":48384,"corporation":false,"usgs":true,"family":"Chapin","given":"F.S.","affiliations":[],"preferred":false,"id":415462,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Dyurgerov, M.B.","contributorId":43953,"corporation":false,"usgs":true,"family":"Dyurgerov","given":"M.B.","email":"","affiliations":[],"preferred":false,"id":415459,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Fastie, C.L.","contributorId":66034,"corporation":false,"usgs":true,"family":"Fastie","given":"C.L.","email":"","affiliations":[],"preferred":false,"id":415466,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Griffith, B.","contributorId":25905,"corporation":false,"usgs":true,"family":"Griffith","given":"B.","email":"","affiliations":[],"preferred":false,"id":415455,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Hollister, R.D.","contributorId":90532,"corporation":false,"usgs":true,"family":"Hollister","given":"R.D.","email":"","affiliations":[],"preferred":false,"id":415475,"contributorType":{"id":1,"text":"Authors"},"rank":8},{"text":"Hope, Allen","contributorId":21379,"corporation":false,"usgs":false,"family":"Hope","given":"Allen","email":"","affiliations":[],"preferred":false,"id":415478,"contributorType":{"id":1,"text":"Authors"},"rank":9},{"text":"Huntington, H.P.","contributorId":59621,"corporation":false,"usgs":true,"family":"Huntington","given":"H.P.","email":"","affiliations":[],"preferred":false,"id":415465,"contributorType":{"id":1,"text":"Authors"},"rank":10},{"text":"Jensen, A.M.","contributorId":13806,"corporation":false,"usgs":true,"family":"Jensen","given":"A.M.","email":"","affiliations":[],"preferred":false,"id":415449,"contributorType":{"id":1,"text":"Authors"},"rank":11},{"text":"Jia, G.J.","contributorId":6631,"corporation":false,"usgs":true,"family":"Jia","given":"G.J.","email":"","affiliations":[],"preferred":false,"id":415446,"contributorType":{"id":1,"text":"Authors"},"rank":12},{"text":"Jorgenson, T.","contributorId":19769,"corporation":false,"usgs":true,"family":"Jorgenson","given":"T.","email":"","affiliations":[],"preferred":false,"id":415451,"contributorType":{"id":1,"text":"Authors"},"rank":13},{"text":"Kane, D.L.","contributorId":6633,"corporation":false,"usgs":true,"family":"Kane","given":"D.L.","email":"","affiliations":[],"preferred":false,"id":415447,"contributorType":{"id":1,"text":"Authors"},"rank":14},{"text":"Klein, D.R.","contributorId":7748,"corporation":false,"usgs":true,"family":"Klein","given":"D.R.","email":"","affiliations":[],"preferred":false,"id":415448,"contributorType":{"id":1,"text":"Authors"},"rank":15},{"text":"Kofinas, G.","contributorId":23752,"corporation":false,"usgs":true,"family":"Kofinas","given":"G.","affiliations":[],"preferred":false,"id":415453,"contributorType":{"id":1,"text":"Authors"},"rank":16},{"text":"Lynch, A.H.","contributorId":29629,"corporation":false,"usgs":true,"family":"Lynch","given":"A.H.","email":"","affiliations":[],"preferred":false,"id":415457,"contributorType":{"id":1,"text":"Authors"},"rank":17},{"text":"Lloyd, A.H.","contributorId":91683,"corporation":false,"usgs":true,"family":"Lloyd","given":"A.H.","email":"","affiliations":[],"preferred":false,"id":415476,"contributorType":{"id":1,"text":"Authors"},"rank":18},{"text":"McGuire, A. 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S.","contributorId":47021,"corporation":false,"usgs":true,"family":"Stone","given":"R.","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":415461,"contributorType":{"id":1,"text":"Authors"},"rank":25},{"text":"Stow, D.A.","contributorId":44336,"corporation":false,"usgs":true,"family":"Stow","given":"D.A.","email":"","affiliations":[],"preferred":false,"id":415460,"contributorType":{"id":1,"text":"Authors"},"rank":26},{"text":"Sturm, M.","contributorId":81834,"corporation":false,"usgs":true,"family":"Sturm","given":"M.","email":"","affiliations":[],"preferred":false,"id":415470,"contributorType":{"id":1,"text":"Authors"},"rank":27},{"text":"Tweedie, C.E.","contributorId":49588,"corporation":false,"usgs":true,"family":"Tweedie","given":"C.E.","affiliations":[],"preferred":false,"id":415463,"contributorType":{"id":1,"text":"Authors"},"rank":28},{"text":"Vourlitis, G.L.","contributorId":21758,"corporation":false,"usgs":true,"family":"Vourlitis","given":"G.L.","affiliations":[],"preferred":false,"id":415452,"contributorType":{"id":1,"text":"Authors"},"rank":29},{"text":"Walker, M.D.","contributorId":31937,"corporation":false,"usgs":true,"family":"Walker","given":"M.D.","email":"","affiliations":[],"preferred":false,"id":415458,"contributorType":{"id":1,"text":"Authors"},"rank":30},{"text":"Walker, D.A.","contributorId":82484,"corporation":false,"usgs":false,"family":"Walker","given":"D.A.","email":"","affiliations":[],"preferred":false,"id":415471,"contributorType":{"id":1,"text":"Authors"},"rank":31},{"text":"Webber, P.J.","contributorId":25351,"corporation":false,"usgs":false,"family":"Webber","given":"P.J.","email":"","affiliations":[],"preferred":false,"id":415454,"contributorType":{"id":1,"text":"Authors"},"rank":32},{"text":"Welker, J.M.","contributorId":82868,"corporation":false,"usgs":true,"family":"Welker","given":"J.M.","affiliations":[],"preferred":false,"id":415472,"contributorType":{"id":1,"text":"Authors"},"rank":33},{"text":"Winker, K.S.","contributorId":28426,"corporation":false,"usgs":true,"family":"Winker","given":"K.S.","email":"","affiliations":[],"preferred":false,"id":415456,"contributorType":{"id":1,"text":"Authors"},"rank":34},{"text":"Yoshikawa, K.","contributorId":72736,"corporation":false,"usgs":true,"family":"Yoshikawa","given":"K.","email":"","affiliations":[],"preferred":false,"id":415468,"contributorType":{"id":1,"text":"Authors"},"rank":35}]}}
,{"id":70027843,"text":"70027843 - 2005 - Effects of suburban development on runoff generation in the Croton River basin, New York, USA","interactions":[],"lastModifiedDate":"2020-01-05T14:26:53","indexId":"70027843","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2342,"text":"Journal of Hydrology","active":true,"publicationSubtype":{"id":10}},"title":"Effects of suburban development on runoff generation in the Croton River basin, New York, USA","docAbstract":"<div id=\"abstracts\" class=\"Abstracts u-font-serif\"><div id=\"aep-abstract-id17\" class=\"abstract author\" lang=\"en\"><div id=\"aep-abstract-sec-id18\"><p><span>The effects of impervious area, septic leach-field&nbsp;effluent, and a riparian&nbsp;wetland&nbsp;on&nbsp;runoff&nbsp;generation were studied in three small (0.38–0.56</span>&nbsp;km<sup>2</sup><span>)&nbsp;headwater&nbsp;catchments that represent a range of suburban development (high density residential, medium density residential, and undeveloped) within the&nbsp;Croton&nbsp;River basin, 70</span>&nbsp;<span>km north of New York City. Precipitation, stream discharge, and&nbsp;groundwater&nbsp;levels were monitored at 10–30</span>&nbsp;min intervals for 1 year, and stream water and groundwater samples were collected biweekly for δ<sup>18</sup>O, NO<sub>3</sub><sup>−</sup>, and SO<sub>4</sub><sup>2−</sup><span>&nbsp;analysis for more than 2 years during an overlapping period in 2000–2002. Data from 27 storms confirmed that peak magnitudes increased and recession time decreased with increasing development, but lags in peak arrival and peak discharge/mean discharge were greatest in the medium density residential catchment, which contains a wetland in which storm runoff is retained before entering the stream. Baseflow during a dry period from Aug. 2001–Feb. 2002 was greatest in the high-density residential catchment, presumably from the discharge of septic effluent through the shallow groundwater system and into the stream. In contrast, moderate flows during a wet period from Mar.–Aug. 2002 were greatest in the undeveloped catchment, possibly as a result of greater subsurface storage or greater&nbsp;hydraulic conductivity&nbsp;at this site. The mean residence time of baseflow was about 30 weeks at all three catchments, indicating that human influence was insufficient to greatly affect the&nbsp;groundwater recharge&nbsp;and discharge properties that determine catchment residence time. These results suggest that while suburban development and its associated impervious surfaces and storm drains accelerate the transport of storm runoff into streams, the combined effects of remnant natural landscape features such as wetlands and human alterations such as deep groundwater supply and&nbsp;septic systems&nbsp;can change the expected effects of human development on storm runoff and groundwater recharge.</span></p></div></div></div>","language":"English","publisher":"Elsevier","doi":"10.1016/j.jhydrol.2005.01.022","issn":"00221694","usgsCitation":"Burns, D.A., Vitvar, T., McDonnell, J., Hassett, J., Duncan, J., and Kendall, C., 2005, Effects of suburban development on runoff generation in the Croton River basin, New York, USA: Journal of Hydrology, v. 311, no. 1-4, p. 266-281, https://doi.org/10.1016/j.jhydrol.2005.01.022.","productDescription":" 16 p.","startPage":"266","endPage":"281","numberOfPages":"16","costCenters":[{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":238286,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"New York","otherGeospatial":"Croton River 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York\",\"nation\":\"USA  \"}}]}","volume":"311","issue":"1-4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a07e7e4b0c8380cd518ba","contributors":{"authors":[{"text":"Burns, Douglas A. 0000-0001-6516-2869 daburns@usgs.gov","orcid":"https://orcid.org/0000-0001-6516-2869","contributorId":1237,"corporation":false,"usgs":true,"family":"Burns","given":"Douglas","email":"daburns@usgs.gov","middleInitial":"A.","affiliations":[{"id":474,"text":"New York Water Science Center","active":true,"usgs":true}],"preferred":true,"id":778870,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Vitvar, T.","contributorId":91758,"corporation":false,"usgs":true,"family":"Vitvar","given":"T.","email":"","affiliations":[],"preferred":false,"id":415519,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"McDonnell, J.","contributorId":61587,"corporation":false,"usgs":true,"family":"McDonnell","given":"J.","email":"","affiliations":[],"preferred":false,"id":415517,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Hassett, J.","contributorId":94936,"corporation":false,"usgs":true,"family":"Hassett","given":"J.","email":"","affiliations":[],"preferred":false,"id":415520,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Duncan, J.","contributorId":15900,"corporation":false,"usgs":true,"family":"Duncan","given":"J.","affiliations":[],"preferred":false,"id":415515,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Kendall, Carol 0000-0002-0247-3405 ckendall@usgs.gov","orcid":"https://orcid.org/0000-0002-0247-3405","contributorId":1462,"corporation":false,"usgs":true,"family":"Kendall","given":"Carol","email":"ckendall@usgs.gov","affiliations":[{"id":438,"text":"National Research Program - Western Branch","active":true,"usgs":true}],"preferred":true,"id":778871,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}}
,{"id":70027912,"text":"70027912 - 2005 - Effects of urbanization on the geomorphology, habitat, hydrology, and fish index of biotic integrity of streams in the Chicago area, Illinois and Wisconsin","interactions":[],"lastModifiedDate":"2012-03-12T17:20:46","indexId":"70027912","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":718,"text":"American Fisheries Society Symposium","active":true,"publicationSubtype":{"id":10}},"title":"Effects of urbanization on the geomorphology, habitat, hydrology, and fish index of biotic integrity of streams in the Chicago area, Illinois and Wisconsin","docAbstract":"Effects of urbanization on geomorphic, habitat, and hydrologic characteristics and fish biotic integrity of 45 streams in the Chicago area were examined by the U.S. Geological Survey from 2000 to 2001. An agricultural to urban land-cover gradient approach was used. Landscape characteristics such as texture of surficial deposits, slope, riparian land cover, and stream network position also were examined to determine if these factors influenced the effects of urbanization. Among geomorphic characteristics, channel enlargement occurred in urban streams with a high percent of watershed clayey surficial deposits. Other geomorphic and habitat characteristics such as stream power, fine substrate, and amount of riffles did not correlate with percent watershed urban land but instead correlated with reach slope. Bank erosion, habitat variability, and two habitat indexes did not correlate with watershed urban land. Below 30% watershed urban land, the unit area discharge for a 2-year flood increased with increasing urban land; however, above 30% urban land, unit area discharges for a 2-year flood were variable, most likely due to variations in stormwater management practices, point-source contributions, and the transport index. Streams with greater than 33% watershed urban land had low base flow, but the effects of urbanization on base flow were offset by point-source contributions. Fish index of biotic integrity (IBI) scores were low in streams with greater than 25% watershed urban land. Fish IBI scores also were low in streams with high percentages of watershed clayey surficial deposits and enlarged channels. The amount of riparian forest/wetland buffer had no moderating effect on geomorphic/habitat/hydrologic characteristics and fish IBI scores. Variations in the texture and topography of glacial landforms affected reach slope and some habitat characteristics. Longitudinal profiles were useful for distinguishing differences in local geologic settings among sampled sites.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"American Fisheries Society Symposium","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","issn":"08922284","usgsCitation":"Fitzpatrick, F., Diebel, M., Harris, M., Arnold, T., Lutz, M., and Richards, K., 2005, Effects of urbanization on the geomorphology, habitat, hydrology, and fish index of biotic integrity of streams in the Chicago area, Illinois and Wisconsin: American Fisheries Society Symposium, v. 2005, no. 47, p. 87-115.","startPage":"87","endPage":"115","numberOfPages":"29","costCenters":[],"links":[{"id":238289,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"2005","issue":"47","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a082be4b0c8380cd519e2","contributors":{"authors":[{"text":"Fitzpatrick, F. A. 0000-0002-9748-7075","orcid":"https://orcid.org/0000-0002-9748-7075","contributorId":61446,"corporation":false,"usgs":true,"family":"Fitzpatrick","given":"F. A.","affiliations":[],"preferred":false,"id":415766,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Diebel, M.W.","contributorId":103465,"corporation":false,"usgs":true,"family":"Diebel","given":"M.W.","affiliations":[],"preferred":false,"id":415769,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Harris, M.A.","contributorId":101278,"corporation":false,"usgs":true,"family":"Harris","given":"M.A.","email":"","affiliations":[],"preferred":false,"id":415768,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Arnold, T.L.","contributorId":11810,"corporation":false,"usgs":true,"family":"Arnold","given":"T.L.","email":"","affiliations":[],"preferred":false,"id":415764,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Lutz, M.A.","contributorId":88945,"corporation":false,"usgs":true,"family":"Lutz","given":"M.A.","email":"","affiliations":[],"preferred":false,"id":415767,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Richards, K.D.","contributorId":28635,"corporation":false,"usgs":true,"family":"Richards","given":"K.D.","email":"","affiliations":[],"preferred":false,"id":415765,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}}
,{"id":70027972,"text":"70027972 - 2005 - Parameter and observation importance in modelling virus transport in saturated porous media - Investigations in a homogenous system","interactions":[],"lastModifiedDate":"2012-03-12T17:20:42","indexId":"70027972","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2233,"text":"Journal of Contaminant Hydrology","active":true,"publicationSubtype":{"id":10}},"title":"Parameter and observation importance in modelling virus transport in saturated porous media - Investigations in a homogenous system","docAbstract":"This paper evaluates the importance of seven types of parameters to virus transport: hydraulic conductivity, porosity, dispersivity, sorption rate and distribution coefficient (representing physical-chemical filtration), and in-solution and adsorbed inactivation (representing virus inactivation). The first three parameters relate to subsurface transport in general while the last four, the sorption rate, distribution coefficient, and in-solution and adsorbed inactivation rates, represent the interaction of viruses with the porous medium and their ability to persist. The importance of four types of observations to estimate the virus-transport parameters are evaluated: hydraulic heads, flow, temporal moments of conservative-transport concentrations, and virus concentrations. The evaluations are conducted using one- and two-dimensional homogeneous simulations, designed from published field experiments, and recently developed sensitivity-analysis methods. Sensitivity to the transport-simulation time-step size is used to evaluate the importance of numerical solution difficulties. Results suggest that hydraulic conductivity, porosity, and sorption are most important to virus-transport predictions. Most observation types provide substantial information about hydraulic conductivity and porosity; only virus-concentration observations provide information about sorption and inactivation. The observations are not sufficient to estimate these important parameters uniquely. Even with all observation types, there is extreme parameter correlation between porosity and hydraulic conductivity and between the sorption rate and in-solution inactivation. Parameter estimation was accomplished by fixing values of porosity and in-solution inactivation.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Journal of Contaminant Hydrology","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1016/j.jconhyd.2005.06.012","issn":"01697722","usgsCitation":"Barth, G.R., and Hill, M.C., 2005, Parameter and observation importance in modelling virus transport in saturated porous media - Investigations in a homogenous system: Journal of Contaminant Hydrology, v. 80, no. 3-4, p. 107-129, https://doi.org/10.1016/j.jconhyd.2005.06.012.","startPage":"107","endPage":"129","numberOfPages":"23","costCenters":[],"links":[{"id":210061,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1016/j.jconhyd.2005.06.012"},{"id":236866,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"80","issue":"3-4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a74cde4b0c8380cd77839","contributors":{"authors":[{"text":"Barth, Gilbert R.","contributorId":15374,"corporation":false,"usgs":false,"family":"Barth","given":"Gilbert","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":415977,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hill, M. C.","contributorId":48993,"corporation":false,"usgs":true,"family":"Hill","given":"M.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":415978,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70029009,"text":"70029009 - 2005 - Arsenate adsorption mechanisms at the allophane: Water interface","interactions":[],"lastModifiedDate":"2018-11-05T10:54:43","indexId":"70029009","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1565,"text":"Environmental Science & Technology","onlineIssn":"1520-5851","printIssn":"0013-936X","active":true,"publicationSubtype":{"id":10}},"title":"Arsenate adsorption mechanisms at the allophane: Water interface","docAbstract":"<div class=\"hlFld-Abstract\"><div id=\"abstractBox\"><p class=\"articleBody_abstractText\">We investigated arsenate (As(V)) reactivity and surface speciation on amorphous aluminosilicate mineral (synthetic allophane) surfaces using batch adsorption experiments, powder X-ray diffraction (XRD), and X-ray absorption spectroscopy (XAS). The adsorption isotherm experiments indicated that As(V) uptake increased with increasing [As(V)]<sub>o</sub><span>&nbsp;</span>from 50 to 1000 μM (i.e., Langmuir type adsorption isotherm) and that the total As adsorption slightly decreased with increasing NaCl concentrations from 0.01 to 0.1 M. Arsenate adsorption was initially (0−10 h) rapid followed by a slow continuum uptake, and the adsorption processes reached the steady state after 720 h. X-ray absorption spectroscopic analyses suggest that As(V) predominantly forms bidentate binuclear surface species on aluminum octahedral structures, and these species are stable up to 11 months. Solubility calculations and powder XRD analyses indicate no evidence of crystalline Al−As(V) precipitates in the experimental systems. Overall, macroscopic and spectroscopic evidence suggest that the As(V) adsorption mechanisms at the allophane−water interface are attributable to ligand exchange reactions between As(V) and surface-coordinated water molecules and hydroxyl and silicate ions. The research findings imply that dissolved tetrahedral oxyanions (e.g., H<sub>2</sub>PO<sub>4</sub><sup>2</sup><sup>-</sup>and H<sub>2</sub>AsO<sub>4</sub><sup>2</sup><sup>-</sup>) are readily retained on amorphous aluminosilicate minerals in aquifer and soils at near neutral pH. The inner-sphere adsorption mechanisms might be important in controlling dissolved arsenate and phosphate in amorphous aluminosilicate-rich low-temperature geochemical environments.</p></div></div>","language":"English","publisher":"ACS","doi":"10.1021/es0486770","issn":"0013936X","usgsCitation":"Arai, Y., Sparks, D., and Davis, J., 2005, Arsenate adsorption mechanisms at the allophane: Water interface: Environmental Science & Technology, v. 39, no. 8, p. 2537-2544, https://doi.org/10.1021/es0486770.","productDescription":"8 p.","startPage":"2537","endPage":"2544","costCenters":[{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":236768,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":209986,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1021/es0486770"}],"volume":"39","issue":"8","noUsgsAuthors":false,"publicationDate":"2005-03-02","publicationStatus":"PW","scienceBaseUri":"5059ed86e4b0c8380cd49864","contributors":{"authors":[{"text":"Arai, Y.","contributorId":59214,"corporation":false,"usgs":true,"family":"Arai","given":"Y.","email":"","affiliations":[],"preferred":false,"id":420940,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Sparks, D.L.","contributorId":94072,"corporation":false,"usgs":true,"family":"Sparks","given":"D.L.","email":"","affiliations":[],"preferred":false,"id":420942,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Davis, J.A.","contributorId":71694,"corporation":false,"usgs":true,"family":"Davis","given":"J.A.","email":"","affiliations":[],"preferred":false,"id":420941,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70184385,"text":"70184385 - 2005 - Pacific volcanoes, mercury contaminated fish, and polynesian taboos","interactions":[],"lastModifiedDate":"2018-10-31T09:48:57","indexId":"70184385","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1257,"text":"Clinical Toxicology","active":true,"publicationSubtype":{"id":10}},"title":"Pacific volcanoes, mercury contaminated fish, and polynesian taboos","docAbstract":"<p>No abstract available.&nbsp;</p>","language":"English","publisher":"Taylor & Francis","doi":"10.1081/CLT-200068868","usgsCitation":"Dellinger, J., Hudson, J., Krabbenhoft, D., and Hinano Murphy, M., 2005, Pacific volcanoes, mercury contaminated fish, and polynesian taboos: Clinical Toxicology, v. 43, no. 6, p. 595-595, https://doi.org/10.1081/CLT-200068868.","productDescription":"2 p. ","startPage":"595","endPage":"595","costCenters":[{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":477886,"rank":0,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1081/clt-200068868","text":"Publisher Index Page"},{"id":337059,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"43","issue":"6","noUsgsAuthors":false,"publicationDate":"2008-10-07","publicationStatus":"PW","scienceBaseUri":"58c12641e4b014cc3a3d34de","contributors":{"authors":[{"text":"Dellinger, John","contributorId":187671,"corporation":false,"usgs":false,"family":"Dellinger","given":"John","email":"","affiliations":[],"preferred":false,"id":681257,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hudson, Jean","contributorId":187672,"corporation":false,"usgs":false,"family":"Hudson","given":"Jean","email":"","affiliations":[],"preferred":false,"id":681258,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Krabbenhoft, David","contributorId":92538,"corporation":false,"usgs":true,"family":"Krabbenhoft","given":"David","affiliations":[],"preferred":false,"id":681259,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Hinano Murphy, M.E.","contributorId":187670,"corporation":false,"usgs":false,"family":"Hinano Murphy","given":"M.E.","email":"","affiliations":[],"preferred":false,"id":681260,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70029333,"text":"70029333 - 2005 - Hydrologic regime controls soil phosphorus fluxes in restoration and undisturbed wetlands","interactions":[],"lastModifiedDate":"2012-03-12T17:20:51","indexId":"70029333","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3271,"text":"Restoration Ecology","active":true,"publicationSubtype":{"id":10}},"title":"Hydrologic regime controls soil phosphorus fluxes in restoration and undisturbed wetlands","docAbstract":"Many wetland restoration projects occur on former agricultural soils that have a history of disturbance and fertilization, making them prone to phosphorus (P) release upon flooding. To study the relationship between P release and hydrologic regime, we collected soil cores from three restoration wetlands and three undisturbed wetlands around Upper Klamath Lake in southern Oregon, U.S.A. Soil cores were subjected to one of three hydrologic regimes - flooded, moist, and dry - for 7.5 weeks, and P fluxes were measured upon reflooding. Soils from restoration wetlands released P upon reflooding regardless of the hydrologic regime, with the greatest releases coming from soils that had been flooded or dried. Undisturbed wetland soils released P only after drying. Patterns in P release can be explained by a combination of physical and biological processes, including the release of iron-bound P due to anoxia in the flooded treatment and the mineralization of organic P under aerobic conditions in the dry treatment. Higher rates of soil P release from restoration wetland soils, particularly under flooded conditions, were associated with higher total P concentrations compared with undisturbed wetland soils. We conclude that maintaining moist soil is the means to minimize P release from recently flooded wetland soils. Alternatively, prolonged flooding provides a means of liberating excess labile P from former agricultural soils while minimizing continued organic P mineralization and soil subsidence. ?? 2005 Society for Ecological Restoration International.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Restoration Ecology","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1111/j.1526-100X.2005.00043.x","issn":"10612971","usgsCitation":"Aldous, A., McCormick, P., Ferguson, C., Graham, S., and Craft, C., 2005, Hydrologic regime controls soil phosphorus fluxes in restoration and undisturbed wetlands: Restoration Ecology, v. 13, no. 2, p. 341-347, https://doi.org/10.1111/j.1526-100X.2005.00043.x.","startPage":"341","endPage":"347","numberOfPages":"7","costCenters":[],"links":[{"id":477899,"rank":10000,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1111/j.1526-100x.2005.00043.x","text":"Publisher Index Page"},{"id":237443,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":210505,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1111/j.1526-100X.2005.00043.x"}],"volume":"13","issue":"2","noUsgsAuthors":false,"publicationDate":"2005-05-24","publicationStatus":"PW","scienceBaseUri":"505a367fe4b0c8380cd6076d","contributors":{"authors":[{"text":"Aldous, A.","contributorId":105517,"corporation":false,"usgs":true,"family":"Aldous","given":"A.","email":"","affiliations":[],"preferred":false,"id":422307,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"McCormick, P.","contributorId":30022,"corporation":false,"usgs":true,"family":"McCormick","given":"P.","email":"","affiliations":[],"preferred":false,"id":422304,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Ferguson, C.","contributorId":18960,"corporation":false,"usgs":true,"family":"Ferguson","given":"C.","email":"","affiliations":[],"preferred":false,"id":422303,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Graham, S.","contributorId":70988,"corporation":false,"usgs":true,"family":"Graham","given":"S.","affiliations":[],"preferred":false,"id":422306,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Craft, C.","contributorId":67712,"corporation":false,"usgs":true,"family":"Craft","given":"C.","email":"","affiliations":[],"preferred":false,"id":422305,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":70029330,"text":"70029330 - 2005 - Vertical cross contamination of trichloroethylene in a borehole in fractured sandstone","interactions":[],"lastModifiedDate":"2019-10-16T16:58:21","indexId":"70029330","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","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":"Vertical cross contamination of trichloroethylene in a borehole in fractured sandstone","docAbstract":"<div class=\"abstract-group\"><div class=\"article-section__content en main\"><p>Boreholes drilled through contaminated zones in fractured rock create the potential for vertical movement of contaminated ground water between fractures. The usual assumption is that purging eliminates cross contamination; however, the results of a field study conducted in a trichloroethylene (TCE) plume in fractured sandstone with a mean matrix porosity of 13% demonstrates that matrix‐diffusion effects can be strong and persistent. A deep borehole was drilled to 110 m below ground surface (mbgs) near a shallow bedrock well containing high TCE concentrations. The borehole was cored continuously to collect closely spaced samples of rock for analysis of TCE concentrations. Geophysical logging and flowmetering were conducted in the open borehole, and a removable multilevel monitoring system was installed to provide hydraulic‐head and ground water samples from discrete fracture zones. The borehole was later reamed to complete a well screened from 89 to 100 mbgs; persistent TCE concentrations at this depth ranged from 2100 to 33,000 μg/L. Rock‐core analyses, combined with the other types of borehole information, show that nearly all of this deep contamination was due to the lingering effects of the downward flow of dissolved TCE from shallower depths during the few days of open‐hole conditions that existed prior to installation of the multilevel system. This study demonstrates that transfer of contaminant mass to the matrix by diffusion can cause severe cross contamination effects in sedimentary rocks, but these effects generally are not identified from information normally obtained in fractured‐rock investigations, resulting in potential misinterpretation of site conditions.</p></div></div>","language":"English","publisher":"Wiley","doi":"10.1111/j.1745-6584.2005.0087.x","issn":"0017467X","usgsCitation":"Sterling, S., Parker, B., Cherry, J.A., Williams, J., Lane, J., and Haeni, F., 2005, Vertical cross contamination of trichloroethylene in a borehole in fractured sandstone: Ground Water, v. 43, no. 4, p. 557-573, https://doi.org/10.1111/j.1745-6584.2005.0087.x.","productDescription":"17 p.","startPage":"557","endPage":"573","costCenters":[{"id":493,"text":"Office of Ground Water","active":true,"usgs":true},{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":237373,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"43","issue":"4","noUsgsAuthors":false,"publicationDate":"2005-07-04","publicationStatus":"PW","scienceBaseUri":"505bc22ee4b08c986b32a998","contributors":{"authors":[{"text":"Sterling, S.N.","contributorId":63601,"corporation":false,"usgs":true,"family":"Sterling","given":"S.N.","email":"","affiliations":[],"preferred":false,"id":422287,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Parker, B.L.","contributorId":51971,"corporation":false,"usgs":true,"family":"Parker","given":"B.L.","email":"","affiliations":[],"preferred":false,"id":422286,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Cherry, J. A.","contributorId":24880,"corporation":false,"usgs":true,"family":"Cherry","given":"J.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":422284,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Williams, J.H.","contributorId":29482,"corporation":false,"usgs":true,"family":"Williams","given":"J.H.","email":"","affiliations":[],"preferred":false,"id":422285,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Lane, J.W. Jr.","contributorId":66723,"corporation":false,"usgs":true,"family":"Lane","given":"J.W.","suffix":"Jr.","email":"","affiliations":[],"preferred":false,"id":422288,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Haeni, F.P.","contributorId":87105,"corporation":false,"usgs":true,"family":"Haeni","given":"F.P.","affiliations":[],"preferred":false,"id":422289,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}}
,{"id":70184381,"text":"70184381 - 2005 - Biodegradation of N-nitrosodimethylamine in soil from a water reclamation facility","interactions":[],"lastModifiedDate":"2017-03-08T11:46:10","indexId":"70184381","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1042,"text":"Bioremediation Journal","active":true,"publicationSubtype":{"id":10}},"title":"Biodegradation of N-nitrosodimethylamine in soil from a water reclamation facility","docAbstract":"<p><span>The potential introduction of </span><i>N</i><span>-nitrosodimethylamine (NDMA) into groundwater during water reclamation activities poses a significant risk to groundwater drinking supplies. Greater than 54% biodegradation of </span><i>N</i><span>-[methyl-</span><sup>14</sup><span>C]NDMA to </span><sup>14</sup><span>CO</span><sub>2</sub><span> or to </span><sup>14</sup><span>CO</span><sub>2</sub><span> and </span><sup>14</sup><span>CH</span><sub>4</sub><span> was observed in soil from a water reclamation facility under oxic or anoxic conditions, respectively. Likewise, biodegradation was significant in microcosms containing soil with no history of NDMA contamination. These results indicate that aerobic and anaerobic biodegradation of NDMA may be an effective component of NDMA attenuation in water reclamation facility soils.</span></p>","language":"English","publisher":"Taylor & Francis","doi":"10.1080/10889860500276607","usgsCitation":"Bradley, P.M., Carr, S.A., Baird, R.B., and Chapelle, F.H., 2005, Biodegradation of N-nitrosodimethylamine in soil from a water reclamation facility: Bioremediation Journal, v. 9, no. 2, p. 115-120, https://doi.org/10.1080/10889860500276607.","productDescription":"6 p. ","startPage":"115","endPage":"120","costCenters":[{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":337054,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"9","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"58c12641e4b014cc3a3d34e2","contributors":{"authors":[{"text":"Bradley, Paul M. 0000-0001-7522-8606 pbradley@usgs.gov","orcid":"https://orcid.org/0000-0001-7522-8606","contributorId":361,"corporation":false,"usgs":true,"family":"Bradley","given":"Paul","email":"pbradley@usgs.gov","middleInitial":"M.","affiliations":[{"id":13634,"text":"South Atlantic Water Science Center","active":true,"usgs":true}],"preferred":true,"id":681245,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Carr, Steve A.","contributorId":187667,"corporation":false,"usgs":false,"family":"Carr","given":"Steve","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":681246,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Baird, Rodger B.","contributorId":187668,"corporation":false,"usgs":false,"family":"Baird","given":"Rodger","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":681247,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Chapelle, Francis H. chapelle@usgs.gov","contributorId":1350,"corporation":false,"usgs":true,"family":"Chapelle","given":"Francis","email":"chapelle@usgs.gov","middleInitial":"H.","affiliations":[{"id":13634,"text":"South Atlantic Water Science Center","active":true,"usgs":true},{"id":559,"text":"South Carolina Water Science Center","active":true,"usgs":true}],"preferred":true,"id":681248,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70031612,"text":"70031612 - 2005 - Influence of water chemistry and travel distance on bacteriophage PRD-1 transport in a sandy aquifer","interactions":[],"lastModifiedDate":"2018-11-05T10:47:16","indexId":"70031612","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3716,"text":"Water Research","onlineIssn":"1879-2448","printIssn":"0043-1354","active":true,"publicationSubtype":{"id":10}},"title":"Influence of water chemistry and travel distance on bacteriophage PRD-1 transport in a sandy aquifer","docAbstract":"<div id=\"abstracts\" class=\"Abstracts\"><div id=\"aep-abstract-id16\" class=\"abstract author\"><div id=\"aep-abstract-sec-id17\"><p>Experiments were conducted to evaluate the impact of groundwater chemistry and travel distance on the transport and fate behavior of PRD-1, a bacteriophage employed as a surrogate tracer for pathogenic enteric viruses. The experiments were conducted in the unconfined aquifer at the United States Geological Survey Cape Cod Toxic-Substances Hydrology Research Site in Falmouth, Massachusetts. The transport behavior of bromide (Br<sup>−</sup>) and PRD-1 were evaluated in a sewage-effluent contaminated zone and a shallower uncontaminated zone at this site. Several multilevel sampling devices located along a 13-m transect were used to collect vertically discrete samples to examine longitudinal and vertical variability of PRD-1 retardation and attenuation. The concentration of viable bacteriophage in the aqueous phase decreased greatly during the first few meters of transport. This decrease is attributed to a combination of colloid filtration (attachment) and inactivation. The removal was greater (10<sup>−12</sup><span>&nbsp;</span>relative recovery) and occurred within the first meter for the uncontaminated zone, whereas it was lesser (10<sup>−9</sup><span>&nbsp;</span>relative recovery) and occurred over 4&nbsp;m in the contaminated zone. The lesser removal observed for the contaminated zone is attributed to the influence of sorbed and dissolved organic matter, phosphate, and other anions, which are present in higher concentrations in the contaminated zone, on PRD-1 attachment. After the initial decrease, the aqueous PRD-1 concentrations remained essentially constant in both zones for the remainder of the tests (total travel distances of 13&nbsp;m), irrespective of variations in geochemical properties within and between the two zones. The viable, mobile PRD-1 particles traveled at nearly the rate of bromide, which was used as a non-reactive tracer. The results of this study indicate that a small fraction of viable virus particles may persist in the aqueous phase and travel significant distances in the subsurface environment.</p></div></div></div>","language":"English","publisher":"Elsevier","doi":"10.1016/j.watres.2005.04.009","issn":"00431354","usgsCitation":"Blanford, W., Brusseau, M., Jim Yeh, T., Gerba, C., and Harvey, R., 2005, Influence of water chemistry and travel distance on bacteriophage PRD-1 transport in a sandy aquifer: Water Research, v. 39, no. 11, p. 2345-2357, https://doi.org/10.1016/j.watres.2005.04.009.","productDescription":"13 p.","startPage":"2345","endPage":"2357","costCenters":[{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":239768,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":212303,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1016/j.watres.2005.04.009"}],"volume":"39","issue":"11","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a3b96e4b0c8380cd62691","contributors":{"authors":[{"text":"Blanford, W.J.","contributorId":20975,"corporation":false,"usgs":true,"family":"Blanford","given":"W.J.","email":"","affiliations":[],"preferred":false,"id":432331,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Brusseau, M.L.","contributorId":29213,"corporation":false,"usgs":true,"family":"Brusseau","given":"M.L.","affiliations":[],"preferred":false,"id":432332,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Jim Yeh, T.-C.","contributorId":95196,"corporation":false,"usgs":true,"family":"Jim Yeh","given":"T.-C.","email":"","affiliations":[],"preferred":false,"id":432335,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Gerba, C.P.","contributorId":40423,"corporation":false,"usgs":true,"family":"Gerba","given":"C.P.","affiliations":[],"preferred":false,"id":432333,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Harvey, R.","contributorId":84124,"corporation":false,"usgs":true,"family":"Harvey","given":"R.","affiliations":[],"preferred":false,"id":432334,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":70027595,"text":"70027595 - 2005 - Management scenarios for the Jordan River salinity crisis","interactions":[],"lastModifiedDate":"2012-03-12T17:20:47","indexId":"70027595","displayToPublicDate":"2005-01-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":835,"text":"Applied Geochemistry","active":true,"publicationSubtype":{"id":10}},"title":"Management scenarios for the Jordan River salinity crisis","docAbstract":"Recent geochemical and hydrological findings show that the water quality of the base flow of the Lower Jordan River, between the Sea of Galilee and the Dead Sea, is dependent upon the ratio between surface water flow and groundwater discharge. Using water quality data, mass-balance calculations, and actual flow-rate measurements, possible management scenarios for the Lower Jordan River and their potential affects on its salinity are investigated. The predicted scenarios reveal that implementation of some elements of the Israel-Jordan peace treaty will have negative effects on the Jordan River water salinity. It is predicted that removal of sewage effluents dumped into the river (???13 MCM/a) will significantly reduce the river water's flow and increase the relative proportion of the saline groundwater flux into the river. Under this scenario, the Cl content of the river at its southern point (Abdalla Bridge) will rise to almost 7000 mg/L during the summer. In contrast, removal of all the saline water (16.5 MCM/a) that is artificially discharged into the Lower Jordan River will significantly reduce its Cl concentration, to levels of 650-2600 and 3000-3500 mg/L in the northern and southern areas of the Lower Jordan River, respectively. However, because the removal of either the sewage effluents or the saline water will decrease the river's discharge to a level that could potentially cause river desiccation during the summer months, other water sources must be allocated to preserve in-stream flow needs and hence the river's ecosystem. ?? 2005 Elsevier Ltd. All rights reserved.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Applied Geochemistry","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1016/j.apgeochem.2005.07.007","issn":"08832927","usgsCitation":"Farber, E., Vengosh, A., Gavrieli, I., Marie, A., Bullen, T., Mayer, B., Holtzman, R., Segal, M., and Shavit, U., 2005, Management scenarios for the Jordan River salinity crisis: Applied Geochemistry, v. 20, no. 11, p. 2138-2153, https://doi.org/10.1016/j.apgeochem.2005.07.007.","startPage":"2138","endPage":"2153","numberOfPages":"16","costCenters":[],"links":[{"id":477953,"rank":10000,"type":{"id":41,"text":"Open Access External Repository Page"},"url":"https://doi.org/10.1016/j.apgeochem.2005.07.007","text":"External Repository"},{"id":238305,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":211114,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1016/j.apgeochem.2005.07.007"}],"volume":"20","issue":"11","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a4c7fe4b0c8380cd69cdf","contributors":{"authors":[{"text":"Farber, E.","contributorId":31955,"corporation":false,"usgs":true,"family":"Farber","given":"E.","email":"","affiliations":[],"preferred":false,"id":414285,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Vengosh, A.","contributorId":88925,"corporation":false,"usgs":true,"family":"Vengosh","given":"A.","affiliations":[],"preferred":false,"id":414290,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Gavrieli, I.","contributorId":88134,"corporation":false,"usgs":true,"family":"Gavrieli","given":"I.","email":"","affiliations":[],"preferred":false,"id":414289,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Marie, Amarisa","contributorId":83090,"corporation":false,"usgs":true,"family":"Marie","given":"Amarisa","affiliations":[],"preferred":false,"id":414287,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Bullen, T.D.","contributorId":79911,"corporation":false,"usgs":true,"family":"Bullen","given":"T.D.","email":"","affiliations":[],"preferred":false,"id":414286,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Mayer, B.","contributorId":84538,"corporation":false,"usgs":true,"family":"Mayer","given":"B.","email":"","affiliations":[],"preferred":false,"id":414288,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Holtzman, R.","contributorId":9044,"corporation":false,"usgs":true,"family":"Holtzman","given":"R.","email":"","affiliations":[],"preferred":false,"id":414283,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Segal, M.","contributorId":104683,"corporation":false,"usgs":true,"family":"Segal","given":"M.","email":"","affiliations":[],"preferred":false,"id":414291,"contributorType":{"id":1,"text":"Authors"},"rank":8},{"text":"Shavit, U.","contributorId":15807,"corporation":false,"usgs":true,"family":"Shavit","given":"U.","email":"","affiliations":[],"preferred":false,"id":414284,"contributorType":{"id":1,"text":"Authors"},"rank":9}]}}
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