{"pageNumber":"1852","pageRowStart":"46275","pageSize":"25","recordCount":184606,"records":[{"id":70045102,"text":"70045102 - 2010 - Inference of lithologic distributions in an alluvial aquifer using airborne transient electromagnetic surveys","interactions":[],"lastModifiedDate":"2018-04-02T15:21:41","indexId":"70045102","displayToPublicDate":"2013-01-01T00:00:00","publicationYear":"2010","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1808,"text":"Geophysics","active":true,"publicationSubtype":{"id":10}},"title":"Inference of lithologic distributions in an alluvial aquifer using airborne transient electromagnetic surveys","docAbstract":"An airborne transient electromagnetic (TEM) survey was completed in the Upper San Pedro Basin in southeastern Arizona to map resistivity distributions within the alluvial aquifer. This investigation evaluated the utility of 1D vertical resistivity models of the TEM data to infer lithologic distributions in an alluvial aquifer. Comparisons of the resistivity values and layers in the 1D resistivity models of airborne TEM data to 1D resistivity models of ground TEM data, borehole resistivity logs, and lithologic descriptions in drill logs indicated that the airborne TEM identified thick conductive fine-grained sediments that result in semiconfined groundwater conditions. One-dimensional models of ground-based TEM surveys and subsurface lithology at three sites were used to determine starting models and constraints to invert airborne TEM data using a constrained Marquardt-styleunderparameterized method. A maximum structural resolution of six layers underlain by a half-space was determined from the resistivity structure of the 1D models of the ground TEM data. The 1D resistivity models of the airborne TEM data compared well with the control data to depths of approximately 100 m in areas of thick conductive silt and clay and to depths of 200 m in areas of resistive sand and gravel. Comparison of a 3D interpolation of the 1D resistivity models to drill logs indicated resistive (mean of 65 ohm-m ) coarse-grained sediments along basin margins and conductive (mean of 8 ohm-m ) fine-grained sediments at the basin center. Extents of hydrologically significant thick silt and clay were well mapped by the 1D resistivity models of airborne TEM data. Areas of uncertain lithology remain below conductive fine-grained sediments where the 1D resistivity structure is not resolved: in areas where multiple lithologies have similar resistivity values and in areas of high salinity.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Geophysics","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"Society of Exploration Geophysicists","doi":"10.1190/1.3464325","usgsCitation":"Dickinson, J.E., Pool, D.R., Groom, R., and Davis, L., 2010, Inference of lithologic distributions in an alluvial aquifer using airborne transient electromagnetic surveys: Geophysics, v. 75, no. 4, p. WA149-WA161, https://doi.org/10.1190/1.3464325.","productDescription":"13 p.","startPage":"WA149","endPage":"WA161","ipdsId":"IP-014910","costCenters":[{"id":128,"text":"Arizona Water Science Center","active":true,"usgs":true}],"links":[{"id":273425,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":273424,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1190/1.3464325"}],"country":"United States","state":"Arizona","otherGeospatial":"San Pedro Basin","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -114.82,31.33 ], [ -114.82,37.0 ], [ -109.05,37.0 ], [ -109.05,31.33 ], [ -114.82,31.33 ] ] ] } } ] }","volume":"75","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"51b300e4e4b01368e589e3d5","contributors":{"authors":[{"text":"Dickinson, Jesse E. 0000-0002-0048-0839 jdickins@usgs.gov","orcid":"https://orcid.org/0000-0002-0048-0839","contributorId":152545,"corporation":false,"usgs":true,"family":"Dickinson","given":"Jesse","email":"jdickins@usgs.gov","middleInitial":"E.","affiliations":[{"id":128,"text":"Arizona Water Science Center","active":true,"usgs":true}],"preferred":true,"id":476798,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Pool, D. R.","contributorId":75581,"corporation":false,"usgs":true,"family":"Pool","given":"D.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":476800,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Groom, R.W.","contributorId":59634,"corporation":false,"usgs":true,"family":"Groom","given":"R.W.","email":"","affiliations":[],"preferred":false,"id":476799,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Davis, L.J.","contributorId":99454,"corporation":false,"usgs":true,"family":"Davis","given":"L.J.","email":"","affiliations":[],"preferred":false,"id":476801,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70003630,"text":"70003630 - 2010 - Use of geochemical, isotopic, and age tracer data to develop models of groundwater flow for the purpose of water management, northern High Plains aquifer, USA","interactions":[],"lastModifiedDate":"2021-04-26T17:11:30.015372","indexId":"70003630","displayToPublicDate":"2013-01-01T00:00:00","publicationYear":"2010","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2982,"text":"PNAS","active":true,"publicationSubtype":{"id":10}},"title":"Use of geochemical, isotopic, and age tracer data to develop models of groundwater flow for the purpose of water management, northern High Plains aquifer, USA","docAbstract":"<p><span>A prolonged drought in the High Plains of Nebraska prompted the use of groundwater for cooling at the largest coal-fired power plant in the State. Prior to the drought, groundwater was used primarily for irrigation and the power plant relied exclusively on surface water stored in a nearby reservoir for cooling. Seepage from the reservoir system during the past ∼75</span><span>&nbsp;</span><span>a has resulted in the buildup of a large mound of water in the underlying unconfined aquifer. A well field was installed during the drought for the purpose of tapping the groundwater mound as a supplemental source of water for cooling. Concentrations of dissolved Cl</span><sup>−</sup><span>&nbsp;and&nbsp;</span><span class=\"math\"><span id=\"MathJax-Element-1-Frame\" class=\"MathJax_SVG\" data-mathml=\"<math xmlns=&quot;http://www.w3.org/1998/Math/MathML&quot;><mrow is=&quot;true&quot;><msubsup is=&quot;true&quot;><mrow is=&quot;true&quot;><mtext is=&quot;true&quot;>SO</mtext></mrow><mrow is=&quot;true&quot;><mn is=&quot;true&quot;>4</mn></mrow><mrow is=&quot;true&quot;><mn is=&quot;true&quot;>2</mn><mo is=&quot;true&quot;>-</mo></mrow></msubsup></mrow></math>\"><span class=\"MJX_Assistive_MathML\">SO<sub>4</sub><sup>2-</sup></span></span></span><span>&nbsp;indicate 65–100% of shallow groundwater and 0–100% of deep groundwater (saturated thickness ∼115</span><span>&nbsp;</span><span>m) in the immediate vicinity of the reservoir was from seepage out of the reservoir system. Hydrogen and O isotopic data indicate most surface-water seepage occurred in the late spring and early summer when reservoir stage was at its highest level. Tritium/</span><sup>3</sup><span>He apparent groundwater ages imply horizontal flow velocities from the reservoir were on the order of 60–600</span><span>&nbsp;</span><span>m/a. These diverse data provided information regarding the spatial distribution, timing, and rate of seepage from the reservoir that could not have been obtained from the available geologic, hydraulic head, and conductivity data. In particular, mixing fractions of surface water and regional groundwater in the aquifer could not have been determined using hydraulic information. Mixing fractions were of special interest in this study because of the management objective to maximize the capture of surface-water seepage in the cooling water wells. Groundwater-flow models developed as well-field management tools were calibrated using inverse modeling techniques and observations of groundwater age, surface-water flow, reservoir stage, and groundwater levels. The age data only accounted for 6 of the 2574 field observations used to calibrate the groundwater-flow models, yet they were among the most influential for refining estimates of hydraulic conductivity, recharge, and seepage from the reservoir. Results from this study demonstrate the benefits of using geochemical, isotopic, and age tracer data to develop conceptual and numerical models of groundwater flow for the purpose of water management.</span></p>","language":"English","publisher":"Elsevier","doi":"10.1016/j.apgeochem.2010.04.001","usgsCitation":"McMahon, P.B., Carney, C.P., Poeter, E.P., and Peterson, S.M., 2010, Use of geochemical, isotopic, and age tracer data to develop models of groundwater flow for the purpose of water management, northern High Plains aquifer, USA: PNAS, v. 25, no. 6, p. 910-922, https://doi.org/10.1016/j.apgeochem.2010.04.001.","productDescription":"13 p.","startPage":"910","endPage":"922","ipdsId":"IP-016647","costCenters":[{"id":154,"text":"California Water Science Center","active":true,"usgs":true}],"links":[{"id":273443,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Nebraska","otherGeospatial":"Platte River","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -101.38870239257812,\n              40.93634011692373\n            ],\n            [\n              -100.98907470703124,\n              40.93634011692373\n            ],\n            [\n              -100.98907470703124,\n              41.26438836965208\n            ],\n            [\n              -101.38870239257812,\n              41.26438836965208\n            ],\n            [\n              -101.38870239257812,\n              40.93634011692373\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"25","issue":"6","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"51b300e3e4b01368e589e3cd","contributors":{"authors":[{"text":"McMahon, Peter B. 0000-0001-7452-2379 pmcmahon@usgs.gov","orcid":"https://orcid.org/0000-0001-7452-2379","contributorId":724,"corporation":false,"usgs":true,"family":"McMahon","given":"Peter","email":"pmcmahon@usgs.gov","middleInitial":"B.","affiliations":[{"id":191,"text":"Colorado Water Science Center","active":true,"usgs":true}],"preferred":true,"id":814706,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Carney, C. P.","contributorId":100084,"corporation":false,"usgs":false,"family":"Carney","given":"C.","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":814707,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Poeter, E. P.","contributorId":63851,"corporation":false,"usgs":false,"family":"Poeter","given":"E.","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":814708,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Peterson, Steven M. 0000-0002-9130-1284 speterson@usgs.gov","orcid":"https://orcid.org/0000-0002-9130-1284","contributorId":847,"corporation":false,"usgs":true,"family":"Peterson","given":"Steven","email":"speterson@usgs.gov","middleInitial":"M.","affiliations":[{"id":464,"text":"Nebraska Water Science Center","active":true,"usgs":true}],"preferred":true,"id":814709,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70044408,"text":"70044408 - 2010 - Chemical fractionation of Cu and Zn in stormwater, roadway dust and stormwater pond sediments","interactions":[],"lastModifiedDate":"2018-10-10T10:44:19","indexId":"70044408","displayToPublicDate":"2013-01-01T00:00:00","publicationYear":"2010","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1555,"text":"Environmental Pollution","active":true,"publicationSubtype":{"id":10}},"title":"Chemical fractionation of Cu and Zn in stormwater, roadway dust and stormwater pond sediments","docAbstract":"This study evaluated the chemical fractionation of Cu and Zn from source to deposition in a stormwater system. Cu and Zn concentrations and chemical fractionation were determined for roadway dust, roadway runoff and pond sediments. Stormwater Cu and Zn concentrations were used to generate cumulative frequency distributions to characterize potential exposure to pond-dwelling organisms. Dissolved stormwater Zn exceeded USEPA acute and chronic water quality criteria in approximately 20% of storm samples and 20% of the storm duration sampled. Dissolved Cu exceeded the previously published chronic criterion in 75% of storm samples and duration and exceeded the acute criterion in 45% of samples and duration. The majority of sediment Cu (92–98%) occurred in the most recalcitrant phase, suggesting low bioavailability; Zn was substantially more available (39–62% recalcitrant). Most sediment concentrations for Cu and Zn exceeded published threshold effect concentrations and Zn often exceeded probable effect concentrations in surface sediments.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Environmental Pollution","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"Elsevier","publisherLocation":"Amsterdam, Netherlands","doi":"10.1016/j.envpol.2010.02.024","usgsCitation":"Camponelli, K.M., Lev, S.M., Snodgrass, J.W., Landa, E.R., and Casey, R.E., 2010, Chemical fractionation of Cu and Zn in stormwater, roadway dust and stormwater pond sediments: Environmental Pollution, v. 158, no. 6, p. 2143-2149, https://doi.org/10.1016/j.envpol.2010.02.024.","productDescription":"7 p.","startPage":"2143","endPage":"2149","ipdsId":"IP-016905","costCenters":[{"id":436,"text":"National Research Program - Eastern Branch","active":true,"usgs":true},{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":271303,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"158","issue":"6","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5173b8e4e4b0e619a5806ed2","contributors":{"authors":[{"text":"Camponelli, Kimberly M.","contributorId":18649,"corporation":false,"usgs":true,"family":"Camponelli","given":"Kimberly","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":475533,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Lev, Steven M.","contributorId":28880,"corporation":false,"usgs":true,"family":"Lev","given":"Steven","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":475534,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Snodgrass, Joel W.","contributorId":61318,"corporation":false,"usgs":true,"family":"Snodgrass","given":"Joel","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":475535,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Landa, Edward R. erlanda@usgs.gov","contributorId":2112,"corporation":false,"usgs":true,"family":"Landa","given":"Edward","email":"erlanda@usgs.gov","middleInitial":"R.","affiliations":[],"preferred":true,"id":475532,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Casey, Ryan E.","contributorId":85485,"corporation":false,"usgs":true,"family":"Casey","given":"Ryan","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":475536,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":70045716,"text":"70045716 - 2010 - Understanding the potential dispersal of HPAI H5N1 virus by migratory wildfowl","interactions":[],"lastModifiedDate":"2017-08-23T09:19:47","indexId":"70045716","displayToPublicDate":"2013-01-01T00:00:00","publicationYear":"2010","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":901,"text":"Argos Forum","active":true,"publicationSubtype":{"id":10}},"title":"Understanding the potential dispersal of HPAI H5N1 virus by migratory wildfowl","docAbstract":"We analysed wildfowl movements between 2006-2009, including 228 birds from 19 species, part of a larger international programme (see Figure 1) coordinated by the Food and Agricultural Organisation (FAO) of the United Nations aimed at understanding if there are temporal or spatial relationships between HPAI H5N1 outbreaks and movements of migratory wildfowl, the first large scale data set available for such an analysis.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Argos Forum","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"CLS Group","usgsCitation":"Gaidet, N., Cappelle, J., Takekawa, J.Y., Prosser, D.J., Iverson, S.A., Douglas, D.C., Perry, W.M., Mundkur, T., and Newman, S.H., 2010, Understanding the potential dispersal of HPAI H5N1 virus by migratory wildfowl: Argos Forum, v. 71, p. 4-5.","productDescription":"2 p.","startPage":"4","endPage":"5","costCenters":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":271674,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":271673,"type":{"id":11,"text":"Document"},"url":"https://www.argos-system.org/files/Publication/public/r234_f34_anl_71-2.pdf"}],"volume":"71","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5180e7efe4b0df838b924dd0","contributors":{"authors":[{"text":"Gaidet, Nicolas","contributorId":37601,"corporation":false,"usgs":true,"family":"Gaidet","given":"Nicolas","email":"","affiliations":[],"preferred":false,"id":478176,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Cappelle, Julien","contributorId":71440,"corporation":false,"usgs":true,"family":"Cappelle","given":"Julien","email":"","affiliations":[],"preferred":false,"id":478178,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Takekawa, John Y. 0000-0003-0217-5907 john_takekawa@usgs.gov","orcid":"https://orcid.org/0000-0003-0217-5907","contributorId":176168,"corporation":false,"usgs":true,"family":"Takekawa","given":"John","email":"john_takekawa@usgs.gov","middleInitial":"Y.","affiliations":[{"id":651,"text":"Western Ecological Research Center","active":true,"usgs":true}],"preferred":false,"id":478172,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Prosser, Diann J. 0000-0002-5251-1799 dprosser@usgs.gov","orcid":"https://orcid.org/0000-0002-5251-1799","contributorId":2389,"corporation":false,"usgs":true,"family":"Prosser","given":"Diann","email":"dprosser@usgs.gov","middleInitial":"J.","affiliations":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"preferred":true,"id":478174,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Iverson, Samuel A.","contributorId":52308,"corporation":false,"usgs":false,"family":"Iverson","given":"Samuel","email":"","middleInitial":"A.","affiliations":[{"id":12437,"text":"Simon Fraser University, Centre for Wildlife Ecology","active":true,"usgs":false}],"preferred":false,"id":478177,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Douglas, David C. 0000-0003-0186-1104 ddouglas@usgs.gov","orcid":"https://orcid.org/0000-0003-0186-1104","contributorId":2388,"corporation":false,"usgs":true,"family":"Douglas","given":"David","email":"ddouglas@usgs.gov","middleInitial":"C.","affiliations":[{"id":116,"text":"Alaska Science Center Biology MFEB","active":true,"usgs":true}],"preferred":true,"id":478173,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Perry, William M. 0000-0002-6180-8180 wmperry@usgs.gov","orcid":"https://orcid.org/0000-0002-6180-8180","contributorId":5124,"corporation":false,"usgs":true,"family":"Perry","given":"William","email":"wmperry@usgs.gov","middleInitial":"M.","affiliations":[{"id":651,"text":"Western Ecological Research Center","active":true,"usgs":true}],"preferred":true,"id":478175,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Mundkur, Taej","contributorId":107843,"corporation":false,"usgs":true,"family":"Mundkur","given":"Taej","affiliations":[],"preferred":false,"id":478180,"contributorType":{"id":1,"text":"Authors"},"rank":8},{"text":"Newman, Scott H.","contributorId":101372,"corporation":false,"usgs":true,"family":"Newman","given":"Scott","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":478179,"contributorType":{"id":1,"text":"Authors"},"rank":9}]}}
,{"id":70044768,"text":"70044768 - 2010 - Nitrogen","interactions":[],"lastModifiedDate":"2013-04-28T22:21:51","indexId":"70044768","displayToPublicDate":"2013-01-01T00:00:00","publicationYear":"2010","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2755,"text":"Mining Engineering","active":true,"publicationSubtype":{"id":10}},"title":"Nitrogen","docAbstract":"Ammonia was produced by 13 companies at 23 plants in 16 states during 2009. Sixty percent of all U.S. ammonia production capacity was centered in Louisiana. Oklahoma and Texas because of those states' large reserves of natural gas, the dominant domestic feedstock. In 2009, U.S. producers operated at about 83 percent of their rated capacity (excluding plants that were idle for the entire year). Five companies — Koch Nitrogen Co.; Terra Industries Inc.; CF Industries Inc.; PCS Nitrogen Inc. and Agrium Inc., in descending order — accounted for 80 percent of the total U.S. ammonia production capacity. U.S. production was estimated to be 7.7 Mt (8.5 million st) of nitrogen (N) content in 2009 compared with 7.85 Mt (8.65 million st) of N content in 2008. Apparent consumption was estimated to have decreased to 12.1 Mt (13.3 million st) of N, a 10-percent decrease from 2008. The United States was the world's fourth-ranked ammonia producer and consumer following China, India and Russia. Urea, ammonium nitrate, ammonium phosphates, nitric acid and ammonium sulfate were the major derivatives of ammonia in the United States, in descending order of importance.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Mining Engineering","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"SME","usgsCitation":"Apodaca, L., 2010, Nitrogen: Mining Engineering, v. 62, no. 6, p. 65-66.","productDescription":"2 p.","startPage":"65","endPage":"66","ipdsId":"IP-020574","costCenters":[{"id":432,"text":"National Minerals Information Center","active":true,"usgs":true}],"links":[{"id":271583,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"62","issue":"6","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"517e44f1e4b0eff6bc003201","contributors":{"authors":[{"text":"Apodaca, L.E.","contributorId":73635,"corporation":false,"usgs":true,"family":"Apodaca","given":"L.E.","email":"","affiliations":[],"preferred":false,"id":476296,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70043486,"text":"70043486 - 2010 - Longitudinal structure in temperate stream fish communities: evaluating conceptual models with temporal data","interactions":[],"lastModifiedDate":"2013-03-26T14:31:33","indexId":"70043486","displayToPublicDate":"2013-01-01T00:00:00","publicationYear":"2010","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"Longitudinal structure in temperate stream fish communities: evaluating conceptual models with temporal data","docAbstract":"Five conceptual models of longitudinal fish community organization in streams were examined: (1) niche diversity model (NDM), (2) stream continuum model (SCM), (3) immigrant accessibility model (IAM), (4) environmental stability model (ESM), and (5) adventitious stream model (ASM). We used differences among models in their predictions about temporal species turnover, along with five spatiotemporal fish community data sets, to evaluate model applicability. Models were similar in predicting a positive species richness–stream size relationship and longitudinal species nestedness, but differed in predicting either similar temporal species turnover throughout the stream continuum (NDM, SCM), higher turnover upstream (IAM, ESM), or higher turnover downstream (ASM). We calculated measures of spatial and temporal variation from spatiotemporal fish data in five wadeable streams in central and eastern North America spanning 34–68 years (French Creek [New York], Piasa Creek [Illinois], Spruce Run [Virginia], Little Stony Creek [Virginia], and Sinking Creek [Virginia]). All streams exhibited substantial species turnover (i.e., at least 27% turnover in stream-scale species pools), in contrast to the predictions of the SCM. Furthermore, community change was greater in downstream than upstream reaches in four of five streams. This result is most consistent with the ASM and suggests that downstream communities are strongly influenced by migrants to and from species pools outside the focal stream. In Sinking Creek, which is isolated from external species pools, temporal species turnover (via increased richness) was higher upstream than downstream, which is a pattern most consistent with the IAM or ESM. These results corroborate the hypothesis that temperate stream habitats and fish communities are temporally dynamic and that fish migration and environmental disturbances play fundamental roles in stream fish community organization.","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Community ecology of stream fishes : concepts, approaches, and techniques; American Fisheries Symposium 73","largerWorkSubtype":{"id":12,"text":"Conference publication"},"language":"English","publisher":"American Fisheries Society","publisherLocation":"Bethesda, MD","usgsCitation":"Roberts, J.H., and Hitt, N.P., 2010, Longitudinal structure in temperate stream fish communities: evaluating conceptual models with temporal data, <i>in</i> Community ecology of stream fishes : concepts, approaches, and techniques; American Fisheries Symposium 73, 19 p.","productDescription":"19 p.","ipdsId":"IP-024159","costCenters":[{"id":365,"text":"Leetown Science Center","active":true,"usgs":true}],"links":[{"id":270191,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5152c398e4b01197b08e9cb5","contributors":{"authors":[{"text":"Roberts, James H.","contributorId":83811,"corporation":false,"usgs":true,"family":"Roberts","given":"James","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":473692,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hitt, Nathaniel P. 0000-0002-1046-4568 nhitt@usgs.gov","orcid":"https://orcid.org/0000-0002-1046-4568","contributorId":4435,"corporation":false,"usgs":true,"family":"Hitt","given":"Nathaniel","email":"nhitt@usgs.gov","middleInitial":"P.","affiliations":[{"id":365,"text":"Leetown Science Center","active":true,"usgs":true}],"preferred":true,"id":473691,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70045913,"text":"70045913 - 2010 - Mineral resource of the month: sulfur","interactions":[],"lastModifiedDate":"2013-05-08T17:58:13","indexId":"70045913","displayToPublicDate":"2013-01-01T00:00:00","publicationYear":"2010","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1419,"text":"Earth","active":true,"publicationSubtype":{"id":10}},"title":"Mineral resource of the month: sulfur","docAbstract":"The article presents information on sulfur. Sulfur is said to be among the few solid elements found in elemental form in nature and has industrial uses. Changes in the sulfur production process over the years are discussed as well as the mining process developed by German engineer Herman Frasch that involves melting the sulfur underground and pumping it to the surface.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Earth","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"AGI","usgsCitation":"Water Resources Division, U.S. Geological Survey, 2010, Mineral resource of the month: sulfur: Earth, v. 55, no. 6, p. 26-27.","productDescription":"2 p.","startPage":"26","endPage":"27","costCenters":[{"id":432,"text":"National Minerals Information Center","active":true,"usgs":true}],"links":[{"id":272095,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"55","issue":"6","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"518b73f3e4b0037667dbc8a6","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":535506,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70045912,"text":"70045912 - 2010 - Mineral resource of the month: platinum group metals","interactions":[],"lastModifiedDate":"2013-05-08T17:55:36","indexId":"70045912","displayToPublicDate":"2013-01-01T00:00:00","publicationYear":"2010","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1419,"text":"Earth","active":true,"publicationSubtype":{"id":10}},"title":"Mineral resource of the month: platinum group metals","docAbstract":"The article focuses on platinum group metals (PGMs) and their properties. According to the author, PGMs, which include iridium, osmium, palladium, platinum, rhodium, and ruthenium, are among the rarest mineral commodities in the Earth's crust. PGMs are primarily used as catalytic converters that clean harmful exhaust from vehicle engines. They are also used in the chemical industry as catalysts in the production of nitric acid and in the petroleum refining industry.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Earth","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"AGI","usgsCitation":"Loferski, P.J., 2010, Mineral resource of the month: platinum group metals: Earth, v. 55, no. 7, p. 28-29.","productDescription":"2 p.","startPage":"28","endPage":"29","costCenters":[{"id":432,"text":"National Minerals Information Center","active":true,"usgs":true}],"links":[{"id":272094,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"55","issue":"7","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"518b73f0e4b0037667dbc88b","contributors":{"authors":[{"text":"Loferski, Patricia J. ploferski@usgs.gov","contributorId":4096,"corporation":false,"usgs":true,"family":"Loferski","given":"Patricia","email":"ploferski@usgs.gov","middleInitial":"J.","affiliations":[],"preferred":true,"id":478526,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70043823,"text":"70043823 - 2010 - Diel behavior of rearing fall Chinook salmon","interactions":[],"lastModifiedDate":"2013-04-25T09:39:29","indexId":"70043823","displayToPublicDate":"2013-01-01T00:00:00","publicationYear":"2010","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2901,"text":"Northwestern Naturalist","active":true,"publicationSubtype":{"id":10}},"title":"Diel behavior of rearing fall Chinook salmon","docAbstract":"In fisheries science, habitat use is often inferred when fish are sampled or observed in a particular location. Physical habitat is typically measured where fish are found, and thus deemed important to habitat use. Although less common, a more informative approach is to measure or observe fish behavior within given habitats to more thoroughly assess their use of those locations. While this approach better reflects how fish use habitat, fish behavior can be difficult to quantify, particularly at night. For example, Tiffan and others (2002, 2006) were able to quantify habitat availability and characteristics that were important for rearing juvenile fall Chinook Salmon (Oncorhynchus tshawytscha) in the Hanford Reach of the Columbia River. The authors, however, could only speculate as to how juvenile salmon use habitat and respond to changes in water level fluctuations. Conversely, in this study we provide data on the diel activities of rearing juvenile wild fall Chinook Salmon which provides a better understanding of how fish “use” these rearing habitats. Diel behavior patterns are important because fish in the Hanford Reach are often stranded on shorelines when the water level rapidly recedes because of hydroelectric power generation at upriver dams (Nugent and others 2002; Anglin and others 2006). We hypothesize that juvenile salmon are at greater risk of stranding at night because they are less active and occupy habitat differently than during the day. We used underwater videography to collect behavioral information during the day and night to determine if juvenile fall Chinook Salmon are more susceptible to stranding when water level fluctuations occur at night.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Northwestern Naturalist","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"Society for Northwestern Vertebrate Biology","doi":"10.1898/NWN10-11.1","usgsCitation":"Tiffan, K.F., Kock, T.J., and Skalicky, J., 2010, Diel behavior of rearing fall Chinook salmon: Northwestern Naturalist, v. 91, no. 3, p. 342-345, https://doi.org/10.1898/NWN10-11.1.","productDescription":"4 p.","startPage":"342","endPage":"345","ipdsId":"IP-019739","costCenters":[{"id":654,"text":"Western Fisheries Research Center","active":true,"usgs":true}],"links":[{"id":271451,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":271450,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1898/NWN10-11.1"}],"volume":"91","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"517a5066e4b072c16ef14b04","contributors":{"authors":[{"text":"Tiffan, Kenneth F. 0000-0002-5831-2846 ktiffan@usgs.gov","orcid":"https://orcid.org/0000-0002-5831-2846","contributorId":3200,"corporation":false,"usgs":true,"family":"Tiffan","given":"Kenneth","email":"ktiffan@usgs.gov","middleInitial":"F.","affiliations":[{"id":654,"text":"Western Fisheries Research Center","active":true,"usgs":true}],"preferred":true,"id":474275,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Kock, Tobias J. 0000-0001-8976-0230 tkock@usgs.gov","orcid":"https://orcid.org/0000-0001-8976-0230","contributorId":3038,"corporation":false,"usgs":true,"family":"Kock","given":"Tobias","email":"tkock@usgs.gov","middleInitial":"J.","affiliations":[{"id":654,"text":"Western Fisheries Research Center","active":true,"usgs":true}],"preferred":true,"id":474274,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Skalicky, Joseph J.","contributorId":91386,"corporation":false,"usgs":true,"family":"Skalicky","given":"Joseph J.","affiliations":[],"preferred":false,"id":474276,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70045899,"text":"70045899 - 2010 - Mineral resource of the month: lead","interactions":[],"lastModifiedDate":"2013-05-08T16:54:57","indexId":"70045899","displayToPublicDate":"2013-01-01T00:00:00","publicationYear":"2010","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1419,"text":"Earth","active":true,"publicationSubtype":{"id":10}},"title":"Mineral resource of the month: lead","docAbstract":"The article discusses the properties and uses lead as a mineral resource. According to the author, lead is a corrosion-resistant, dense, ductile, and malleable blue-gray metal that has been used by humans for 5,000 years. Lead was first used in decorative, fixtures, roofs, pipes, and windows. The author says that lead is the fifth-most consumed metal based on tonnage after iron, aluminum, copper and zinc.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Earth","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"AGI","usgsCitation":"Guberman, D.E., 2010, Mineral resource of the month: lead: Earth, v. 55, no. 11, p. 29-29.","productDescription":"1 p.","startPage":"29","endPage":"29","costCenters":[{"id":432,"text":"National Minerals Information Center","active":true,"usgs":true}],"links":[{"id":272081,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"55","issue":"11","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"518b73eee4b0037667dbc871","contributors":{"authors":[{"text":"Guberman, David E. dguberman@usgs.gov","contributorId":2660,"corporation":false,"usgs":true,"family":"Guberman","given":"David","email":"dguberman@usgs.gov","middleInitial":"E.","affiliations":[{"id":432,"text":"National Minerals Information Center","active":true,"usgs":true}],"preferred":true,"id":478504,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70045703,"text":"70045703 - 2010 - Prevalence of antibodies to type A influenza virus in wild avian species using two serologic assays","interactions":[],"lastModifiedDate":"2018-01-03T14:46:56","indexId":"70045703","displayToPublicDate":"2013-01-01T00:00:00","publicationYear":"2010","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2507,"text":"Journal of Wildlife Diseases","active":true,"publicationSubtype":{"id":10}},"title":"Prevalence of antibodies to type A influenza virus in wild avian species using two serologic assays","docAbstract":"<p><span>Serologic testing to detect antibodies to avian influenza (AI) virus has been an underused tool for the study of these viruses in wild bird populations, which traditionally has relied on virus isolation and reverse transcriptase-polymerase chain reaction (RT-PCR). In a preliminary study, a recently developed commercial blocking enzyme-linked immunosorbent assay (bELISA) had sensitivity and specificity estimates of 82% and 100%, respectively, for detection of antibodies to AI virus in multiple wild bird species after experimental infection. To further evaluate the efficacy of this commercial bELISA and the agar gel immunodiffusion (AGID) test for AI virus antibody detection in wild birds, we tested 2,249 serum samples collected from 62 wild bird species, representing 10 taxonomic orders. Overall, the bELISA detected 25.4% positive samples, whereas the AGID test detected 14.8%. At the species level, the bELISA detected as many or more positive serum samples than the AGID in all 62 avian species. The majority of positive samples, detected by both assays, were from species that use aquatic habitats, with the highest prevalence from species in the orders Anseriformes and Charadriiformes. Conversely, antibodies to AI virus were rarely detected in the terrestrial species. The serologic data yielded by both assays are consistent with the known epidemiology of AI virus in wild birds and published reports of host range based on virus isolation and RT-PCR. The results of this research are also consistent with the aforementioned study, which evaluated the performance of the bELISA and AGID test on experimental samples. Collectively, the data from these two studies indicate that the bELISA is a more sensitive serologic assay than the AGID test for detecting prior exposure to AI virus in wild birds. Based on these results, the bELISA is a reliable species-independent assay with potentially valuable applications for wild bird AI surveillance.</span></p>","language":"English","publisher":"Wildlife Disease Association","doi":"10.7589/0090-3558-46.3.896","usgsCitation":"Brown, J.D., Luttrell, M.P., Berghaus, R., Kistler, W., Keeler, S.P., Howey, A., Wilcox, B., Hall, J.S., Niles, L., Dey, A., Knutsen, G., Fritz, K., and Stallknecht, D.E., 2010, Prevalence of antibodies to type A influenza virus in wild avian species using two serologic assays: Journal of Wildlife Diseases, v. 46, no. 3, p. 896-911, https://doi.org/10.7589/0090-3558-46.3.896.","productDescription":"16 p.","startPage":"896","endPage":"911","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":456,"text":"National Wildlife Health Center","active":true,"usgs":true}],"links":[{"id":475474,"rank":2,"type":{"id":40,"text":"Open Access Publisher Index 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,{"id":70043673,"text":"70043673 - 2010 - Dioszegia antarctica sp. nov. and Dioszegia cryoxerica sp. nov., psychrophilic basidiomycetous yeasts from polar desert soils in Antarctica","interactions":[],"lastModifiedDate":"2013-04-25T11:52:43","indexId":"70043673","displayToPublicDate":"2013-01-01T00:00:00","publicationYear":"2010","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":"Dioszegia antarctica sp. nov. and Dioszegia cryoxerica sp. nov., psychrophilic basidiomycetous yeasts from polar desert soils in Antarctica","docAbstract":"During a survey of the culturable soil fungal population in samples collected in Taylor Valley, South Victoria Land, Antarctica, 13 basidiomycetous yeast strains with orange-coloured colonies were isolated. Phylogenetic analyses of internal transcribed spacer (ITS) and partial LSU rRNA gene sequences showed that the strains belong to the Dioszegia clade of the Tremellales (Tremellomycetes, Agaricomycotina), but did not correspond to any of the hitherto recognized species. Two novel species, Dioszegia antarctica sp. nov. (type strain ANT-03-116<sup>T</sup> =CBS 10920<sup>T</sup> =PYCC 5970<sup>T</sup>) and Dioszegia cryoxerica sp. nov. (type strain ANT-03-071<sup>T</sup> =CBS 10919<sup>T</sup> =PYCC 5967<sup>T</sup>), are described to accommodate ten and three of these strains, respectively. Analysis of ITS sequences demonstrated intrastrain sequence heterogeneity in D. cryoxerica. The latter species is also notable for producing true hyphae with clamp connections and haustoria. However, no sexual structures were observed. The two novel species can be considered obligate psychrophiles, since they failed to grow above 20 °C and grew best between 10 and 15 °C.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"International Journal of Systematic and Evolutionary Microbiology","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"International Union of Microbiological Scientists","doi":"10.1099/ijs.0.015412-0","usgsCitation":"Rodriguez, R.J., Connell, L., Redman, R., Barrett, A., Iszard, M., and Fonseca, A., 2010, Dioszegia antarctica sp. nov. and Dioszegia cryoxerica sp. nov., psychrophilic basidiomycetous yeasts from polar desert soils in Antarctica: International Journal of Systematic and Evolutionary Microbiology, v. 60, no. 6, p. 1466-1472, https://doi.org/10.1099/ijs.0.015412-0.","productDescription":"7 p.","startPage":"1466","endPage":"1472","ipdsId":"IP-014820","costCenters":[{"id":654,"text":"Western Fisheries Research Center","active":true,"usgs":true}],"links":[{"id":475465,"rank":0,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1099/ijs.0.015412-0","text":"Publisher Index Page"},{"id":271464,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":271463,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1099/ijs.0.015412-0"}],"country":"United States","volume":"60","issue":"6","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"517a5068e4b072c16ef14b16","contributors":{"authors":[{"text":"Rodriguez, Russell J.","contributorId":75035,"corporation":false,"usgs":true,"family":"Rodriguez","given":"Russell","email":"","middleInitial":"J.","affiliations":[{"id":654,"text":"Western Fisheries Research Center","active":true,"usgs":true}],"preferred":false,"id":474021,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Connell, L.","contributorId":81612,"corporation":false,"usgs":true,"family":"Connell","given":"L.","email":"","affiliations":[],"preferred":false,"id":474022,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Redman, R.","contributorId":12602,"corporation":false,"usgs":true,"family":"Redman","given":"R.","affiliations":[],"preferred":false,"id":474019,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Barrett, A.","contributorId":89038,"corporation":false,"usgs":true,"family":"Barrett","given":"A.","email":"","affiliations":[],"preferred":false,"id":474023,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Iszard, M.","contributorId":74855,"corporation":false,"usgs":true,"family":"Iszard","given":"M.","email":"","affiliations":[],"preferred":false,"id":474020,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Fonseca, A.","contributorId":92145,"corporation":false,"usgs":true,"family":"Fonseca","given":"A.","email":"","affiliations":[],"preferred":false,"id":474024,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}}
,{"id":70044937,"text":"70044937 - 2010 - Changes in the North American ferroalloys industry structure and trends in the industry during the past 20 years","interactions":[],"lastModifiedDate":"2013-04-02T10:14:20","indexId":"70044937","displayToPublicDate":"2013-01-01T00:00:00","publicationYear":"2010","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"Changes in the North American ferroalloys industry structure and trends in the industry during the past 20 years","docAbstract":"This analysis of changes in the North American (Canada, Mexico, and the United States) ferroalloys industry between 1987 and 2007 includes the locations and types of ferroalloy plants in North America and the changes in production, imports, exports, pricing, and the structure of ownership since 1987, which was just prior to the implementation of the North American Free Trade Agreement. Significant events affect the supply of and demand for North American ferroalloys -- changes in end uses, global industry structure, political stability, and technology. Mergers and acquisitions in the ferroalloys industries of North America and their impact on trade are other significant issues in international trade as are antidumping and countervailing duty orders, and trade agreements and policies related to ferroalloys occurring during this period and affecting the North American region. Raw materials and energy supply to the ferroalloy industry, the logistics involved in the trade of North American ferroalloys, and the use of ferroalloys within major downstream industries are also important factors. Emphasis is placed on the bulk ferroalloys—ferrochromium, ferromanganese, ferrosilicon, and silicomanganese. Other ferroalloys investigated include those of boron, molybdenum, nickel, niobium, titanium, tungsten, and vanadium.","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Proceedings of the twelfth international ferroalloys congress: sustainable future: June 6 - 9, 2010, Helsinki, Finland","largerWorkSubtype":{"id":12,"text":"Conference publication"},"language":"English","publisher":"Outotec Oyj","publisherLocation":"Helsinki, Finland","usgsCitation":"Didaleusky, J., Jorgenson, J., Corathers, L., Fenton, M., Kuck, P., Papp, J., Polyak, D., and Shedd, K., 2010, Changes in the North American ferroalloys industry structure and trends in the industry during the past 20 years, <i>in</i> Proceedings of the twelfth international ferroalloys congress: sustainable future: June 6 - 9, 2010, Helsinki, Finland, 11 p.","productDescription":"11 p.","ipdsId":"IP-017282","costCenters":[{"id":432,"text":"National Minerals Information Center","active":true,"usgs":true}],"links":[{"id":270456,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":270450,"type":{"id":11,"text":"Document"},"url":"https://minerals.usgs.gov/minerals/pubs/commodity/ferroalloys/ferroalloys-trends.pdf"}],"otherGeospatial":"North America","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ 177.0,5.6 ], [ 177.0,85.4 ], [ -4.0,85.4 ], [ -4.0,5.6 ], [ 177.0,5.6 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"515bfde1e4b075500ee5ca22","contributors":{"authors":[{"text":"Didaleusky, J.R.","contributorId":23823,"corporation":false,"usgs":true,"family":"Didaleusky","given":"J.R.","email":"","affiliations":[],"preferred":false,"id":476487,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Jorgenson, J.D.","contributorId":92345,"corporation":false,"usgs":true,"family":"Jorgenson","given":"J.D.","email":"","affiliations":[],"preferred":false,"id":476493,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Corathers, L.A.","contributorId":75033,"corporation":false,"usgs":true,"family":"Corathers","given":"L.A.","affiliations":[],"preferred":false,"id":476492,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Fenton, M.D.","contributorId":102353,"corporation":false,"usgs":true,"family":"Fenton","given":"M.D.","email":"","affiliations":[],"preferred":false,"id":476494,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Kuck, P.H.","contributorId":68191,"corporation":false,"usgs":true,"family":"Kuck","given":"P.H.","email":"","affiliations":[],"preferred":false,"id":476490,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Papp, J.F.","contributorId":48604,"corporation":false,"usgs":true,"family":"Papp","given":"J.F.","email":"","affiliations":[],"preferred":false,"id":476489,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Polyak, D.E.","contributorId":43647,"corporation":false,"usgs":true,"family":"Polyak","given":"D.E.","email":"","affiliations":[],"preferred":false,"id":476488,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Shedd, Kim B.","contributorId":68192,"corporation":false,"usgs":true,"family":"Shedd","given":"Kim B.","affiliations":[],"preferred":false,"id":476491,"contributorType":{"id":1,"text":"Authors"},"rank":8}]}}
,{"id":70044346,"text":"70044346 - 2010 - Tectonics of the Maryland Piedmont along the Potomac River; insight since 1960 and potential transfer to the Pennsylvania Piedmont","interactions":[],"lastModifiedDate":"2013-03-09T16:48:13","indexId":"70044346","displayToPublicDate":"2013-01-01T00:00:00","publicationYear":"2010","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"Tectonics of the Maryland Piedmont along the Potomac River; insight since 1960 and potential transfer to the Pennsylvania Piedmont","docAbstract":"This is a summary of a half century of research in the Mary land Piedmont and how it may or may not have implications for the Piedmont of Pennsylvania. Much of the field mapping and all of the isotopic analyses of rocks and minerals of the Maryland Piedmont have been conducted since the 1960 Field Conference of Pennsylvania Geologists “Some tectonic and structural problems of the Appalachian Piedmont along the Susquehanna River”. The Piedmont rocks of Maryland and Pennsylvania occur in a critical place within the central Appalachian Pennsylvania embayment (Thomas, 1977), which likely contributed to the distribution of lithologies and structures.","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Tectonics of the Susquehanna Piedmont in Lancaster, Dauphin, and York Counties, Pa.: proceedings of a symposium associated with the 75th Field Conference of Pennsylvania Geologists, Lancaster, Pa., September 23, 2010","largerWorkSubtype":{"id":12,"text":"Conference publication"},"language":"English","publisher":"Field Conference of Pennsylvania Geologists","publisherLocation":"fcopg.org","usgsCitation":"Southworth, C.S., 2010, Tectonics of the Maryland Piedmont along the Potomac River; insight since 1960 and potential transfer to the Pennsylvania Piedmont, <i>in</i> Tectonics of the Susquehanna Piedmont in Lancaster, Dauphin, and York Counties, Pa.: proceedings of a symposium associated with the 75th Field Conference of Pennsylvania Geologists, Lancaster, Pa., September 23, 2010, v. 75, p. 11-20.","productDescription":"10 p.","startPage":"11","endPage":"20","ipdsId":"IP-023323","costCenters":[{"id":243,"text":"Eastern Geology and Paleoclimate Science Center","active":true,"usgs":true}],"links":[{"id":268989,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":268988,"type":{"id":11,"text":"Document"},"url":"https://fcopg.org/Documents/2010/00SympVolume.pdf"}],"country":"United States","state":"Maryl;Pennsylvania","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -80.52,37.89 ], [ -80.52,42.27 ], [ -74.69,42.27 ], [ -74.69,37.89 ], [ -80.52,37.89 ] ] ] } } ] }","volume":"75","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53cd766ee4b0b2908510ae59","contributors":{"editors":[{"text":"Wise, Donald U.","contributorId":112628,"corporation":false,"usgs":true,"family":"Wise","given":"Donald","email":"","middleInitial":"U.","affiliations":[],"preferred":false,"id":509255,"contributorType":{"id":2,"text":"Editors"},"rank":1},{"text":"Fleeger, Gary M.","contributorId":63436,"corporation":false,"usgs":true,"family":"Fleeger","given":"Gary","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":509254,"contributorType":{"id":2,"text":"Editors"},"rank":2}],"authors":[{"text":"Southworth, C. Scott 0000-0002-7976-7807 ssouthwo@usgs.gov","orcid":"https://orcid.org/0000-0002-7976-7807","contributorId":1608,"corporation":false,"usgs":true,"family":"Southworth","given":"C.","email":"ssouthwo@usgs.gov","middleInitial":"Scott","affiliations":[{"id":243,"text":"Eastern Geology and Paleoclimate Science Center","active":true,"usgs":true},{"id":40020,"text":"Florence Bascom Geoscience Center","active":true,"usgs":true}],"preferred":true,"id":475330,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70043619,"text":"70043619 - 2010 - Effect of clay content and mineralogy on frictional sliding behavior of simulated gouges: binary and ternary mixtures of quartz, illite, and montmorillonite","interactions":[],"lastModifiedDate":"2013-05-09T10:31:44","indexId":"70043619","displayToPublicDate":"2013-01-01T00:00:00","publicationYear":"2010","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2314,"text":"Journal of Geophysical Research B: Solid Earth","active":true,"publicationSubtype":{"id":10}},"title":"Effect of clay content and mineralogy on frictional sliding behavior of simulated gouges: binary and ternary mixtures of quartz, illite, and montmorillonite","docAbstract":"We investigated the frictional sliding behavior of simulated quartz-clay gouges under stress conditions relevant to seismogenic depths. Conventional triaxial compression tests were conducted at 40 MPa effective normal stress on saturated saw cut samples containing binary and ternary mixtures of quartz, montmorillonite, and illite. In all cases, frictional strengths of mixtures fall between the end-members of pure quartz (strongest) and clay (weakest). The overall trend was a decrease in strength with increasing clay content. In the illite/quartz mixture the trend was nearly linear, while in the montmorillonite mixtures a sigmoidal trend with three strength regimes was noted. Microstructural observations were performed on the deformed samples to characterize the geometric attributes of shear localization within the gouge layers. Two micromechanical models were used to analyze the critical clay fractions for the two-regime transitions on the basis of clay porosity and packing of the quartz grains. The transition from regime 1 (high strength) to 2 (intermediate strength) is associated with the shift from a stress-supporting framework of quartz grains to a clay matrix embedded with disperse quartz grains, manifested by the development of P-foliation and reduction in Riedel shear angle. The transition from regime 2 (intermediate strength) to 3 (low strength) is attributed to the development of shear localization in the clay matrix, occurring only when the neighboring layers of quartz grains are separated by a critical clay thickness. Our mixture data relating strength degradation to clay content agree well with strengths of natural shear zone materials obtained from scientific deep drilling projects.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Journal of Geophysical Research B: Solid Earth","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"AGU","doi":"10.1029/2009JB006383","usgsCitation":"Tembe, S., Lockner, D.A., and Wong, T., 2010, Effect of clay content and mineralogy on frictional sliding behavior of simulated gouges: binary and ternary mixtures of quartz, illite, and montmorillonite: Journal of Geophysical Research B: Solid Earth, v. 115, no. B3, B03416, https://doi.org/10.1029/2009JB006383.","productDescription":"B03416","ipdsId":"IP-008421","costCenters":[{"id":237,"text":"Earthquake Science Center","active":true,"usgs":true}],"links":[{"id":475477,"rank":0,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1029/2009jb006383","text":"Publisher Index Page"},{"id":272127,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":272126,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1029/2009JB006383"}],"volume":"115","issue":"B3","noUsgsAuthors":false,"publicationDate":"2010-03-24","publicationStatus":"PW","scienceBaseUri":"518cc563e4b05ebc8f7cc111","contributors":{"authors":[{"text":"Tembe, Sheryl","contributorId":87436,"corporation":false,"usgs":true,"family":"Tembe","given":"Sheryl","email":"","affiliations":[],"preferred":false,"id":473991,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Lockner, David A. 0000-0001-8630-6833 dlockner@usgs.gov","orcid":"https://orcid.org/0000-0001-8630-6833","contributorId":567,"corporation":false,"usgs":true,"family":"Lockner","given":"David","email":"dlockner@usgs.gov","middleInitial":"A.","affiliations":[{"id":237,"text":"Earthquake Science Center","active":true,"usgs":true},{"id":234,"text":"Earthquake Hazards Program","active":true,"usgs":true}],"preferred":true,"id":473989,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Wong, Teng-Fong","contributorId":83005,"corporation":false,"usgs":true,"family":"Wong","given":"Teng-Fong","affiliations":[],"preferred":false,"id":473990,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70044309,"text":"70044309 - 2010 - Influence of hummocks and emergent vegetation on hydraulic performance in a surface flow wastewater treatment wetland","interactions":[],"lastModifiedDate":"2018-10-10T15:50:12","indexId":"70044309","displayToPublicDate":"2013-01-01T00:00:00","publicationYear":"2010","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3722,"text":"Water Resources Research","onlineIssn":"1944-7973","printIssn":"0043-1397","active":true,"publicationSubtype":{"id":10}},"title":"Influence of hummocks and emergent vegetation on hydraulic performance in a surface flow wastewater treatment wetland","docAbstract":"<p><span>A series of tracer experiments were conducted biannually at the start and end of the vegetation growing season in a surface flow wastewater treatment wetland located near Phoenix, AZ. Tracer experiments were conducted prior to and following reconfiguration and replanting of a 1.2 ha treatment wetland from its original design of alternating shallow and deep zones to incorporate hummocks (shallow planting beds situated perpendicular to flow). Tracer test data were analyzed using analysis of moments and the one‐dimensional transport with inflow and storage numerical model to evaluate the effects of the seasonal vegetation growth cycle and hummocks on solute transport. Following reconfiguration, vegetation coverage was relatively small, and minor changes in spatial distribution influenced wetland hydraulics. During start‐up conditions, the wetland underwent an acclimation period characterized by small vegetation coverage and large transport cross‐sectional areas. At the start of the growing season, new growth of emergent vegetation enhanced hydraulic performance. At the end of the growing season, senescing vegetation created short‐circuiting. Wetland hydrodynamics were associated with high volumetric efficiencies and velocity heterogeneities. The hummock design resulted in breakthrough curves characterized by multiple secondary tracer peaks indicative of varied flow paths created by bottom topography.</span></p>","language":"English","publisher":"American Geophysical Union","doi":"10.1029/2010WR009512","usgsCitation":"Keefe, S.H., Daniels, J.S., Runkel, R.L., Wass, R.D., Stiles, E.A., and Barber, L.B., 2010, Influence of hummocks and emergent vegetation on hydraulic performance in a surface flow wastewater treatment wetland: Water Resources Research, v. 46, no. 11, W11518; 13 p., https://doi.org/10.1029/2010WR009512.","productDescription":"W11518; 13 p.","ipdsId":"IP-007397","costCenters":[{"id":435,"text":"National Research Program - Central Region","active":false,"usgs":true},{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":475468,"rank":0,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1029/2010wr009512","text":"Publisher Index 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,{"id":70044344,"text":"70044344 - 2010 - Conodont biostratigraphy of a more complete Reef Trail Member section near the type section, latest Guadalupian Series type region","interactions":[],"lastModifiedDate":"2013-04-21T20:33:14","indexId":"70044344","displayToPublicDate":"2013-01-01T00:00:00","publicationYear":"2010","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2735,"text":"Micropaleontology","active":true,"publicationSubtype":{"id":10}},"title":"Conodont biostratigraphy of a more complete Reef Trail Member section near the type section, latest Guadalupian Series type region","docAbstract":"The original type section of the Reef Trail Member (uppermost part of the Bell Canyon Formation) is called the Park Boundary Section, and is less than satisfactory in several aspects. We propose a new reference section designated Reef Trail Reference section 1 (RTR1) on the same hill as the original type section. Section RTR1 compensates for some of the Park Boundary Section’s shortcomings, including better exposure of a single measured section with only minor offset. The conodont biostratigraphy of section RTR1 is presented that, when combined with a better set of described correlation intervals, allows for improved correlation to recently discovered, complete, basinal sections in the Patterson Hills. In comparison with the South Boundary basin section, both the Park Boundary and RTR1 sections are missing approximately the upper third of the Reef Trail Member. Transitional conodonts from the basin demonstrate that Jinogondolella crofti evolved directly from J. altudaensis. We formally elevate Clarkina postbitteri hongshuiensis to C. hongshuiensis.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Micropaleontology","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"Micropaleontology Press","publisherLocation":"Flushing, NY","usgsCitation":"Wardlaw, B.R., Lambert, L., Bell, G., Fronimos, J., and Yisa, M., 2010, Conodont biostratigraphy of a more complete Reef Trail Member section near the type section, latest Guadalupian Series type region: Micropaleontology, v. 56, no. 1-2, p. 233-253.","productDescription":"21 p.","startPage":"233","endPage":"253","ipdsId":"IP-019269","costCenters":[{"id":243,"text":"Eastern Geology and Paleoclimate Science Center","active":true,"usgs":true}],"links":[{"id":271329,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Texas","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -106.65,25.84 ], [ -106.65,36.5 ], [ -93.51,36.5 ], [ -93.51,25.84 ], [ -106.65,25.84 ] ] ] } } ] }","volume":"56","issue":"1-2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"51751749e4b074c2b05564bb","contributors":{"authors":[{"text":"Wardlaw, Bruce R. bwardlaw@usgs.gov","contributorId":266,"corporation":false,"usgs":true,"family":"Wardlaw","given":"Bruce","email":"bwardlaw@usgs.gov","middleInitial":"R.","affiliations":[{"id":243,"text":"Eastern Geology and Paleoclimate Science Center","active":true,"usgs":true}],"preferred":true,"id":475325,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Lambert, L.L.","contributorId":23722,"corporation":false,"usgs":true,"family":"Lambert","given":"L.L.","email":"","affiliations":[],"preferred":false,"id":475326,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Bell, G.L. Jr.","contributorId":89043,"corporation":false,"usgs":true,"family":"Bell","given":"G.L.","suffix":"Jr.","email":"","affiliations":[],"preferred":false,"id":475328,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Fronimos, J.A.","contributorId":103552,"corporation":false,"usgs":true,"family":"Fronimos","given":"J.A.","email":"","affiliations":[],"preferred":false,"id":475329,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Yisa, M.O.","contributorId":50433,"corporation":false,"usgs":true,"family":"Yisa","given":"M.O.","email":"","affiliations":[],"preferred":false,"id":475327,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":70043197,"text":"70043197 - 2010 - Carbonate control of H<sub>2</sub> and CH<sub>4</sub> production in serpentinization systems at elevated P-Ts","interactions":[],"lastModifiedDate":"2013-04-20T19:05:51","indexId":"70043197","displayToPublicDate":"2013-01-01T00:00:00","publicationYear":"2010","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1807,"text":"Geophysical Research Letters","active":true,"publicationSubtype":{"id":10}},"title":"Carbonate control of H<sub>2</sub> and CH<sub>4</sub> production in serpentinization systems at elevated P-Ts","docAbstract":"Serpentinization of forsteritic olivine results in the inorganic synthesis of molecular hydrogen (H<sub>2</sub>) in ultramafic hydrothermal systems (e.g., mid-ocean ridge and forearc environments). Inorganic carbon in those hydrothermal systems may react with H<sub>2</sub> to produce methane (CH<sub>4</sub>) and other hydrocarbons or react with dissolved metal ions to form carbonate minerals. Here, we report serpentinization experiments at 200°C and 300 bar demonstrating Fe<sup>2+</sup> being incorporated into carbonates more rapidly than Fe<sup>2+</sup> oxidation (and concomitant H<sub>2</sub> formation) leading to diminished yields of H<sub>2</sub> and H<sub>2</sub>-dependent CH<sub>4</sub>. In addition, carbonate formation is temporally fast in carbonate oversaturated fluids. Our results demonstrate that carbonate chemistry ultimately modulates the abiotic synthesis of both H<sub>2</sub> and CH<sub>4</sub> in hydrothermal ultramafic systems and that ultramafic systems present great potential for CO<sub>2</sub>-mineral sequestration.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Geophysical Research Letters","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"AGU","publisherLocation":"Washington, D.C.","doi":"10.1029/2010GL043769","usgsCitation":"Jones, L.C., Rosenbauer, R., Goldsmith, J.I., and Oze, C., 2010, Carbonate control of H<sub>2</sub> and CH<sub>4</sub> production in serpentinization systems at elevated P-Ts: Geophysical Research Letters, v. 37, no. 14, L14306, https://doi.org/10.1029/2010GL043769.","productDescription":"L14306","ipdsId":"IP-022048","costCenters":[{"id":520,"text":"Pacific Coastal and Marine Science Center","active":true,"usgs":true}],"links":[{"id":475475,"rank":0,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1029/2010gl043769","text":"Publisher Index Page"},{"id":271294,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":271293,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1029/2010GL043769"}],"volume":"37","issue":"14","noUsgsAuthors":false,"publicationDate":"2010-07-23","publicationStatus":"PW","scienceBaseUri":"5173b8e2e4b0e619a5806eb9","contributors":{"authors":[{"text":"Jones, L. Camille 0000-0002-7394-2053 lejones@usgs.gov","orcid":"https://orcid.org/0000-0002-7394-2053","contributorId":39673,"corporation":false,"usgs":true,"family":"Jones","given":"L.","email":"lejones@usgs.gov","middleInitial":"Camille","affiliations":[],"preferred":false,"id":473145,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Rosenbauer, Robert","contributorId":9551,"corporation":false,"usgs":true,"family":"Rosenbauer","given":"Robert","affiliations":[],"preferred":false,"id":473144,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Goldsmith, Jonas I.","contributorId":85863,"corporation":false,"usgs":true,"family":"Goldsmith","given":"Jonas","email":"","middleInitial":"I.","affiliations":[],"preferred":false,"id":473147,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Oze, Christopher","contributorId":47267,"corporation":false,"usgs":true,"family":"Oze","given":"Christopher","affiliations":[],"preferred":false,"id":473146,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70043675,"text":"70043675 - 2010 - Distribution of an invasive aquatic pathogen (viral hemorrhagic septicemia virus) in the Great Lakes and its relationship to shipping","interactions":[],"lastModifiedDate":"2013-05-02T13:59:46","indexId":"70043675","displayToPublicDate":"2013-01-01T00:00:00","publicationYear":"2010","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2980,"text":"PLoS ONE","active":true,"publicationSubtype":{"id":10}},"title":"Distribution of an invasive aquatic pathogen (viral hemorrhagic septicemia virus) in the Great Lakes and its relationship to shipping","docAbstract":"Viral hemorrhagic septicemia virus (VHSV) is a rhabdovirus found in fish from oceans of the northern hemisphere and freshwaters of Europe. It has caused extensive losses of cultured and wild fish and has become established in the North American Great Lakes. Large die-offs of wild fish in the Great Lakes due to VHSV have alarmed the public and provoked government attention on the introduction and spread of aquatic animal pathogens in freshwaters. We investigated the relations between VHSV dispersion and shipping and boating activity in the Great Lakes by sampling fish and water at sites that were commercial shipping harbors, recreational boating centers, and open shorelines. Fish and water samples were individually analyzed for VHSV using quantitative reverse transcription-polymerase chain reaction (qRT-PCR) and cell culture assays. Of 1,221 fish of 17 species, 55 were VHSV positive with highly varied qRT-PCR titers (1 to 5,950,000 N gene copies). The detections of VHSV in fish and water samples were closely associated and the virus was detected in 21 of 30 sites sampled. The occurrence of VHSV was not related to type of site or shipping related invasion hotspots. Our results indicate that VHSV is widely dispersed in the Great Lakes and is both an enzootic and epizootic pathogen. We demonstrate that pathogen distribution information could be developed quickly and is clearly needed for aquatic ecosystem conservation, management of affected populations, and informed regulation of the worldwide trade of aquatic organisms.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"PLoS ONE","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"Public Library of Science","doi":"10.1371/journal.pone.0010156","usgsCitation":"Bain, M.B., Cornwell, E., Hope, K.M., Eckerlin, G.E., Casey, R.N., Groocock, G.H., Getchell, R.G., Bowser, P., Winton, J.R., Batts, W.N., Cangelosi, A., and Casey, J.W., 2010, Distribution of an invasive aquatic pathogen (viral hemorrhagic septicemia virus) in the Great Lakes and its relationship to shipping: PLoS ONE, v. 5, no. 4, e10156, https://doi.org/10.1371/journal.pone.0010156.","productDescription":"e10156","ipdsId":"IP-019986","costCenters":[{"id":654,"text":"Western Fisheries Research Center","active":true,"usgs":true}],"links":[{"id":475473,"rank":0,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1371/journal.pone.0010156","text":"Publisher Index Page"},{"id":271762,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":271761,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1371/journal.pone.0010156"}],"otherGeospatial":"Great Lakes","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -92.11,41.18 ], [ -92.11,49.1 ], [ -75.8,49.1 ], [ -75.8,41.18 ], [ -92.11,41.18 ] ] ] } } ] }","volume":"5","issue":"4","noUsgsAuthors":false,"publicationDate":"2010-04-13","publicationStatus":"PW","scienceBaseUri":"51838ae4e4b0a21483941a83","contributors":{"authors":[{"text":"Bain, Mark B.","contributorId":10084,"corporation":false,"usgs":true,"family":"Bain","given":"Mark","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":474027,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Cornwell, Emily R.","contributorId":64526,"corporation":false,"usgs":true,"family":"Cornwell","given":"Emily R.","affiliations":[],"preferred":false,"id":474032,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Hope, Kristine M.","contributorId":66986,"corporation":false,"usgs":true,"family":"Hope","given":"Kristine","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":474033,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Eckerlin, Geofrey E.","contributorId":106771,"corporation":false,"usgs":true,"family":"Eckerlin","given":"Geofrey","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":474036,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Casey, Rufina N.","contributorId":104364,"corporation":false,"usgs":true,"family":"Casey","given":"Rufina","email":"","middleInitial":"N.","affiliations":[],"preferred":false,"id":474035,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Groocock, Geoffrey H.","contributorId":13878,"corporation":false,"usgs":true,"family":"Groocock","given":"Geoffrey","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":474029,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Getchell, Rodman G.","contributorId":32416,"corporation":false,"usgs":true,"family":"Getchell","given":"Rodman","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":474030,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Bowser, Paul R.","contributorId":10391,"corporation":false,"usgs":true,"family":"Bowser","given":"Paul R.","affiliations":[],"preferred":false,"id":474028,"contributorType":{"id":1,"text":"Authors"},"rank":8},{"text":"Winton, James R. 0000-0002-3505-5509 jwinton@usgs.gov","orcid":"https://orcid.org/0000-0002-3505-5509","contributorId":1944,"corporation":false,"usgs":true,"family":"Winton","given":"James","email":"jwinton@usgs.gov","middleInitial":"R.","affiliations":[{"id":654,"text":"Western Fisheries Research Center","active":true,"usgs":true}],"preferred":false,"id":474025,"contributorType":{"id":1,"text":"Authors"},"rank":9},{"text":"Batts, William N. 0000-0002-6469-9004 bbatts@usgs.gov","orcid":"https://orcid.org/0000-0002-6469-9004","contributorId":3815,"corporation":false,"usgs":true,"family":"Batts","given":"William","email":"bbatts@usgs.gov","middleInitial":"N.","affiliations":[{"id":654,"text":"Western Fisheries Research Center","active":true,"usgs":true}],"preferred":true,"id":474026,"contributorType":{"id":1,"text":"Authors"},"rank":10},{"text":"Cangelosi, Allegra","contributorId":42506,"corporation":false,"usgs":true,"family":"Cangelosi","given":"Allegra","affiliations":[],"preferred":false,"id":474031,"contributorType":{"id":1,"text":"Authors"},"rank":11},{"text":"Casey, James W.","contributorId":92941,"corporation":false,"usgs":true,"family":"Casey","given":"James","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":474034,"contributorType":{"id":1,"text":"Authors"},"rank":12}]}}
,{"id":70044819,"text":"70044819 - 2010 - Mineral resource of the month: salt","interactions":[],"lastModifiedDate":"2013-05-08T20:19:16","indexId":"70044819","displayToPublicDate":"2013-01-01T00:00:00","publicationYear":"2010","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1419,"text":"Earth","active":true,"publicationSubtype":{"id":10}},"title":"Mineral resource of the month: salt","docAbstract":"The article presents information on various types of salt. Rock salt is either found from underground halite deposits or near the surface. Other types of salt include solar salt, salt brine, and vacuum pan salt. The different uses of salt are also given including its use as a flavor enhancer, as a road deicing agent, and to manufacture sodium hydroxide.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Earth","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"AGI","usgsCitation":"Kostick, D.S., 2010, Mineral resource of the month: salt: Earth, v. 55, no. 4, p. 27-27.","productDescription":"1 p.","startPage":"27","endPage":"27","ipdsId":"IP-019136","costCenters":[{"id":432,"text":"National Minerals Information Center","active":true,"usgs":true}],"links":[{"id":272105,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"55","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"518b73f2e4b0037667dbc89e","contributors":{"authors":[{"text":"Kostick, Dennis S.","contributorId":49919,"corporation":false,"usgs":true,"family":"Kostick","given":"Dennis","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":476373,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70044801,"text":"70044801 - 2010 - Mineral resource of the month: iron ore","interactions":[],"lastModifiedDate":"2013-05-08T20:22:02","indexId":"70044801","displayToPublicDate":"2013-01-01T00:00:00","publicationYear":"2010","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1419,"text":"Earth","active":true,"publicationSubtype":{"id":10}},"title":"Mineral resource of the month: iron ore","docAbstract":"The article provides information on iron ore, including its use in steelmaking.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Earth","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"AGI","usgsCitation":"Jorgenson, J., 2010, Mineral resource of the month: iron ore: Earth, v. 55, no. 1, p. 29-29.","productDescription":"1 p.","startPage":"29","endPage":"29","ipdsId":"IP-017293","costCenters":[{"id":432,"text":"National Minerals Information Center","active":true,"usgs":true}],"links":[{"id":272106,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"55","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"518b73ede4b0037667dbc869","contributors":{"authors":[{"text":"Jorgenson, John","contributorId":89223,"corporation":false,"usgs":true,"family":"Jorgenson","given":"John","affiliations":[],"preferred":false,"id":476343,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70042194,"text":"70042194 - 2010 - Predicting future changes in Muskegon River Watershed game fish distributions under future land cover alteration and climate change scenarios","interactions":[],"lastModifiedDate":"2013-03-12T14:14:24","indexId":"70042194","displayToPublicDate":"2013-01-01T00:00:00","publicationYear":"2010","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3624,"text":"Transactions of the American Fisheries Society","active":true,"publicationSubtype":{"id":10}},"title":"Predicting future changes in Muskegon River Watershed game fish distributions under future land cover alteration and climate change scenarios","docAbstract":"Future alterations in land cover and climate are likely to cause substantial changes in the ranges of fish species. Predictive distribution models are an important tool for assessing the probability that these changes will cause increases or decreases in or the extirpation of species. Classification tree models that predict the probability of game fish presence were applied to the streams of the Muskegon River watershed, Michigan. The models were used to study three potential future scenarios: (1) land cover change only, (2) land cover change and a 3°C increase in air temperature by 2100, and (3) land cover change and a 5°C increase in air temperature by 2100. The analysis indicated that the expected change in air temperature and subsequent change in water temperatures would result in the decline of coldwater fish in the Muskegon watershed by the end of the 21st century while cool- and warmwater species would significantly increase their ranges. The greatest decline detected was a 90% reduction in the probability that brook trout Salvelinus fontinalis would occur in Bigelow Creek. The greatest increase was a 276% increase in the probability that northern pike Esox lucius would occur in the Middle Branch River. Changes in land cover are expected to cause large changes in a few fish species, such as walleye Sander vitreus and Chinook salmon Oncorhynchus tshawytscha, but not to drive major changes in species composition. Managers can alter stream environmental conditions to maximize the probability that species will reside in particular stream reaches through application of the classification tree models. Such models represent a good way to predict future changes, as they give quantitative estimates of the n-dimensional niches for particular species.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Transactions of the American Fisheries Society","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"Taylor & Francis","publisherLocation":"Philadelphia, PA","doi":"10.1577/T09-007.1","usgsCitation":"Steen, P.J., Wiley, M., and Schaeffer, J.S., 2010, Predicting future changes in Muskegon River Watershed game fish distributions under future land cover alteration and climate change scenarios: Transactions of the American Fisheries Society, v. 139, no. 2, p. 396-412, https://doi.org/10.1577/T09-007.1.","productDescription":"17 p.","startPage":"396","endPage":"412","ipdsId":"IP-010660","costCenters":[{"id":324,"text":"Great Lakes Science Center","active":true,"usgs":true}],"links":[{"id":475466,"rank":0,"type":{"id":41,"text":"Open Access External Repository Page"},"url":"https://hdl.handle.net/2027.42/141570","text":"External Repository"},{"id":269166,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":269164,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1577/T09-007.1"}],"country":"United States","state":"Michigan","otherGeospatial":"Muskegon River","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -90.4,41.7 ], [ -90.4,48.3 ], [ -82.4,48.3 ], [ -82.4,41.7 ], [ -90.4,41.7 ] ] ] } } ] }","volume":"139","issue":"2","noUsgsAuthors":false,"publicationDate":"2011-01-09","publicationStatus":"PW","scienceBaseUri":"51404e8de4b089809dbf44c4","contributors":{"authors":[{"text":"Steen, Paul J.","contributorId":12342,"corporation":false,"usgs":true,"family":"Steen","given":"Paul","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":470928,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Wiley, Michael J.","contributorId":30112,"corporation":false,"usgs":true,"family":"Wiley","given":"Michael J.","affiliations":[],"preferred":false,"id":470929,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Schaeffer, Jeffrey S.","contributorId":89083,"corporation":false,"usgs":true,"family":"Schaeffer","given":"Jeffrey","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":470930,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70042790,"text":"70042790 - 2010 - Importance of benthic production to fish populations in Lake Mead prior to the establishment of quagga mussels","interactions":[],"lastModifiedDate":"2013-06-06T08:33:50","indexId":"70042790","displayToPublicDate":"2013-01-01T00:00:00","publicationYear":"2010","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2592,"text":"Lake and Reservoir Management","active":true,"publicationSubtype":{"id":10}},"title":"Importance of benthic production to fish populations in Lake Mead prior to the establishment of quagga mussels","docAbstract":"Limnologists recently have developed an interest in quantifying benthic resource contributions to higher-level consumers. Much of this research focuses on natural lakes with very little research in reservoirs. In this study, we provide a contemporary snapshot of the food web structure of Lake Mead to evaluate the contribution of benthic resources to fish consumers. In addition, we document the available food to fishes on soft sediments and changes to the invertebrate community over 2 time periods. Benthic invertebrate food availability for fishes is greater in Las Vegas Bay than Overton Arm. Las Vegas Bay is dominated by oligochaetes, whose biomass increased with depth, while Overton Arm is dominated by chironomids, whose biomass did not change with depth. Diet and isotopic measurements indicate the fish community largely relies on benthic resources regardless of basin (Las Vegas Bay >80%; Overton Arm >92%); however, the threadfin shad likely contribute more to largemouth and striped bass production in Overton Arm versus Las Vegas Bay. A 2-time period analysis, pre and post quagga mussel establishment and during lake level declines, suggests there is no change in the density of benthic invertebrates in Boulder Basin, but there were greater abundances of select taxa in this basin by season and depth than in other basins. Given the potential of alterations as a result of the expansion of quagga mussel and the reliance of the fishery on benthic resources, future investigation of basin specific, benthic processes is recommended.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Lake and Reservoir Management","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"Taylor & Francis","doi":"10.1080/07438141.2010.541328","usgsCitation":"Umek, J., Chandra, S., Rosen, M., Wittmann, M., Sullivan, J., and Orsak, E., 2010, Importance of benthic production to fish populations in Lake Mead prior to the establishment of quagga mussels: Lake and Reservoir Management, v. 26, no. 4, p. 293-305, https://doi.org/10.1080/07438141.2010.541328.","productDescription":"13 p.","startPage":"293","endPage":"305","ipdsId":"IP-015326","costCenters":[{"id":465,"text":"Nevada Water Science Center","active":true,"usgs":true}],"links":[{"id":475467,"rank":0,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1080/07438141.2010.541328","text":"Publisher Index Page"},{"id":273349,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":266325,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1080/07438141.2010.541328"}],"country":"United States","state":"Nevada","otherGeospatial":"Lake Mead","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -114.9,35.99 ], [ -114.9,36.52 ], [ -113.78,36.52 ], [ -113.78,35.99 ], [ -114.9,35.99 ] ] ] } } ] }","volume":"26","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"51b1bbd3e4b022a6a540f9dd","contributors":{"authors":[{"text":"Umek, John","contributorId":23423,"corporation":false,"usgs":true,"family":"Umek","given":"John","email":"","affiliations":[],"preferred":false,"id":472271,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Chandra, Sudeep","contributorId":33195,"corporation":false,"usgs":false,"family":"Chandra","given":"Sudeep","affiliations":[{"id":12742,"text":"University of Nevada Reno","active":true,"usgs":false}],"preferred":false,"id":472272,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Rosen, Michael","contributorId":87441,"corporation":false,"usgs":true,"family":"Rosen","given":"Michael","affiliations":[],"preferred":false,"id":472274,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Wittmann, Marion","contributorId":87443,"corporation":false,"usgs":true,"family":"Wittmann","given":"Marion","affiliations":[],"preferred":false,"id":472275,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Sullivan, Joe","contributorId":83427,"corporation":false,"usgs":true,"family":"Sullivan","given":"Joe","email":"","affiliations":[],"preferred":false,"id":472273,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Orsak, Erik","contributorId":92763,"corporation":false,"usgs":true,"family":"Orsak","given":"Erik","affiliations":[],"preferred":false,"id":472276,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}}
,{"id":70044935,"text":"70044935 - 2010 - Earth mineral resource of the month: asbestos","interactions":[],"lastModifiedDate":"2013-05-08T20:01:08","indexId":"70044935","displayToPublicDate":"2013-01-01T00:00:00","publicationYear":"2010","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1419,"text":"Earth","active":true,"publicationSubtype":{"id":10}},"title":"Earth mineral resource of the month: asbestos","docAbstract":"The article discusses the characteristics and feature of asbestos. According to the author, asbestos is a generic name for six needle-shaped minerals that possess high tensile strengths, flexibility, and resistance to chemical and thermal degradation. These minerals are actinolite, amosite, anthophyllite, chrysolite, crocilodite and tremolite. Asbestos is used for strengthening concrete pipe, plastic components, and gypsum plasters.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Earth","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"AGI","usgsCitation":"Virta, R.L., 2010, Earth mineral resource of the month: asbestos: Earth, v. 55, no. 2, p. 27-27.","productDescription":"1 p.","startPage":"27","endPage":"27","ipdsId":"IP-017589","costCenters":[{"id":432,"text":"National Minerals Information Center","active":true,"usgs":true}],"links":[{"id":272101,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"55","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"518b73e4e4b0037667dbc7f8","contributors":{"authors":[{"text":"Virta, Robert L. rvirta@usgs.gov","contributorId":395,"corporation":false,"usgs":true,"family":"Virta","given":"Robert","email":"rvirta@usgs.gov","middleInitial":"L.","affiliations":[{"id":432,"text":"National Minerals Information Center","active":true,"usgs":true}],"preferred":true,"id":476486,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70045910,"text":"70045910 - 2010 - Mineral resource of the month: perlite","interactions":[],"lastModifiedDate":"2013-05-08T17:43:37","indexId":"70045910","displayToPublicDate":"2013-01-01T00:00:00","publicationYear":"2010","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1419,"text":"Earth","active":true,"publicationSubtype":{"id":10}},"title":"Mineral resource of the month: perlite","docAbstract":"The article talks about perlite, which is a mineral used as an aggregate for lightweight construction products, filler for paints and horticultural soil blends. Perlite comes from viscous lava, mined and processed to produce lightweight material that competes with pumice, exfoliated vermiculite and expanded clay and shale. It is mined in about 35 countries that include Greece, Japan and the U.S. Other uses include insulation, concrete and plaster aggregate, and stonewashing.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Earth","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"AGI","usgsCitation":"Water Resources Division, U.S. Geological Survey, 2010, Mineral resource of the month: perlite: Earth, v. 55, no. 8, p. 27-27.","productDescription":"1 p.","startPage":"27","endPage":"27","costCenters":[{"id":432,"text":"National Minerals Information Center","active":true,"usgs":true}],"links":[{"id":272092,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"55","issue":"8","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"518b73f0e4b0037667dbc887","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":535505,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
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