{"pageNumber":"1850","pageRowStart":"46225","pageSize":"25","recordCount":184617,"records":[{"id":70042496,"text":"70042496 - 2010 - Viscoelastic-cycle model of interseismic deformation in the northwestern United States","interactions":[],"lastModifiedDate":"2013-01-10T14:48:14","indexId":"70042496","displayToPublicDate":"2013-01-07T00:00:00","publicationYear":"2010","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1803,"text":"Geophysical Journal International","active":true,"publicationSubtype":{"id":10}},"title":"Viscoelastic-cycle model of interseismic deformation in the northwestern United States","docAbstract":"We apply a viscoelastic cycle model to a compilation of GPS velocity fields in order to address the kinematics of deformation in the northwestern United States. A viscoelastic cycle model accounts for time-dependent deformation following large crustal earthquakes and is an alternative to block models for explaining the interseismic crustal velocity field. Building on the approach taken in Pollitz et al., we construct a deformation model for the entire western United States-based on combined fault slip and distributed deformation-and focus on the implications for the Mendocino triple junction (MTJ), Cascadia megathrust, and western Washington. We find significant partitioning between strike-slip and dip-slip motion near the MTJ as the tectonic environment shifts from northwest-directed shear along the San Andreas fault system to east-west convergence along the Juan de Fuca Plate. By better accounting for the budget of aseismic and seismic slip along the Cascadia subduction interface in conjunction with an assumed rheology, we revise a previous model of slip for the M~ 9 1700 Cascadia earthquake. In western Washington, we infer slip rates on a number of strike-slip and dip-slip faults that accommodate northward convergence of the Oregon Coast block and northwestward convergence of the Juan de Fuca Plate. Lateral variations in first order mechanical properties (e.g. mantle viscosity, vertically averaged rigidity) explain, to a large extent, crustal strain that cannot be rationalized with cyclic deformation on a laterally homogeneous viscoelastic structure. Our analysis also shows that present crustal deformation measurements, particularly with the addition of the Plate Boundary Observatory, can constrain such lateral variations.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Geophysical Journal International","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"Wiley","publisherLocation":"Hoboken, NJ","doi":"10.1111/j.1365-246X.2010.04546.x","usgsCitation":"Pollitz, F., McCrory, P., Wilson, D., Svarc, J., Puskas, C., and Smith, R.B., 2010, Viscoelastic-cycle model of interseismic deformation in the northwestern United States: Geophysical Journal International, v. 181, no. 2, p. 665-696, https://doi.org/10.1111/j.1365-246X.2010.04546.x.","productDescription":"32 p.","startPage":"665","endPage":"696","numberOfPages":"32","ipdsId":"IP-013321","costCenters":[{"id":237,"text":"Earthquake Science Center","active":true,"usgs":true}],"links":[{"id":475460,"rank":0,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1111/j.1365-246x.2010.04546.x","text":"Publisher Index Page"},{"id":265514,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":265513,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1111/j.1365-246X.2010.04546.x"}],"country":"United States","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -124.41,32.53 ], [ -124.41,49.99 ], [ -107.36,49.99 ], [ -107.36,32.53 ], [ -124.41,32.53 ] ] ] } } ] }","volume":"181","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53cd7b1ee4b0b2908510dece","contributors":{"authors":[{"text":"Pollitz, F. F.","contributorId":108280,"corporation":false,"usgs":true,"family":"Pollitz","given":"F. F.","affiliations":[],"preferred":false,"id":471650,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"McCrory, Patricia","contributorId":96560,"corporation":false,"usgs":true,"family":"McCrory","given":"Patricia","affiliations":[],"preferred":false,"id":471649,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Wilson, Doug","contributorId":7581,"corporation":false,"usgs":true,"family":"Wilson","given":"Doug","email":"","affiliations":[],"preferred":false,"id":471645,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Svarc, Jerry","contributorId":82012,"corporation":false,"usgs":true,"family":"Svarc","given":"Jerry","affiliations":[],"preferred":false,"id":471647,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Puskas, Christine","contributorId":17109,"corporation":false,"usgs":true,"family":"Puskas","given":"Christine","email":"","affiliations":[],"preferred":false,"id":471646,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Smith, Robert B.","contributorId":90824,"corporation":false,"usgs":true,"family":"Smith","given":"Robert","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":471648,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}}
,{"id":70042341,"text":"70042341 - 2010 - Understanding behavioral responses of fish to pheromones in natural freshwater environments","interactions":[],"lastModifiedDate":"2013-01-10T15:59:54","indexId":"70042341","displayToPublicDate":"2013-01-07T00:00:00","publicationYear":"2010","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2225,"text":"Journal of Comparative Physiology A","active":true,"publicationSubtype":{"id":10}},"title":"Understanding behavioral responses of fish to pheromones in natural freshwater environments","docAbstract":"There is an abundance of experimental studies and reviews that describe odorant-mediated behaviors of fish in laboratory microcosms, but research in natural field conditions has received considerably less attention. Fish pheromone studies in laboratory settings can be highly productive and allow for controlled experimental designs; however, laboratory tanks and flumes often cannot replicate all the physical, physiological and social contexts associated with natural environments. Field experiments can be a critical step in affirming and enhancing understanding of laboratory discoveries and often implicate the ecological significance of pheromones employed by fishes. When findings from laboratory experiments have been further tested in field environments, often different and sometimes contradictory conclusions are found. Examples include studies of sea lamprey (Petromyzon marinus) mating pheromones and fish alarm substances. Here, we review field research conducted on fish pheromones and alarm substances, highlighting the following topics: (1) contradictory results obtained in laboratory and field experiments, (2) how environmental context and physiological status influences behavior, (3) challenges and constraints of aquatic field research and (4) innovative techniques and experimental designs that advance understanding of fish chemical ecology through field research.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Journal of Comparative Physiology A","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"Springer","publisherLocation":"Amsterdam, Netherlands","doi":"10.1007/s00359-010-0523-7","usgsCitation":"Johnson, N.S., and Li, W., 2010, Understanding behavioral responses of fish to pheromones in natural freshwater environments: Journal of Comparative Physiology A, v. 196, no. 10, p. 701-711, https://doi.org/10.1007/s00359-010-0523-7.","productDescription":"11 p.","startPage":"701","endPage":"711","numberOfPages":"11","ipdsId":"IP-017172","costCenters":[{"id":324,"text":"Great Lakes Science Center","active":true,"usgs":true}],"links":[{"id":265529,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":265527,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1007/s00359-010-0523-7"}],"country":"United States","volume":"196","issue":"10","noUsgsAuthors":false,"publicationDate":"2010-03-30","publicationStatus":"PW","scienceBaseUri":"53cd7a2ee4b0b2908510d51d","contributors":{"authors":[{"text":"Johnson, Nicholas S. 0000-0002-7419-6013 njohnson@usgs.gov","orcid":"https://orcid.org/0000-0002-7419-6013","contributorId":597,"corporation":false,"usgs":true,"family":"Johnson","given":"Nicholas","email":"njohnson@usgs.gov","middleInitial":"S.","affiliations":[{"id":324,"text":"Great Lakes Science Center","active":true,"usgs":true}],"preferred":true,"id":471342,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Li, Weiming","contributorId":65440,"corporation":false,"usgs":true,"family":"Li","given":"Weiming","affiliations":[],"preferred":false,"id":471343,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70047525,"text":"70047525 - 2010 - Correction to “Constraints on the stress state of the San Andreas Fault with analysis based on core and cuttings from San Andreas Fault Observatory at Depth (SAFOD) drilling phases 1 and 2”","interactions":[],"lastModifiedDate":"2019-07-17T16:29:56","indexId":"70047525","displayToPublicDate":"2013-01-01T17:12:39","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":"Correction to “Constraints on the stress state of the San Andreas Fault with analysis based on core and cuttings from San Andreas Fault Observatory at Depth (SAFOD) drilling phases 1 and 2”","docAbstract":"This article corrects: Constraints on the stress state of the San Andreas Fault with analysis based on core and cuttings from San Andreas Fault Observatory at Depth (SAFOD) drilling phases 1 and 2. Vol. 114, Issue B11, Article first published online: 5 NOV 2009.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Journal of Geophysical Research B: Solid Earth","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"American Geophysical Union","doi":"10.1029/2009JB000818","usgsCitation":"Tembe, S., Lockner, D., and Wong, T., 2010, Correction to “Constraints on the stress state of the San Andreas Fault with analysis based on core and cuttings from San Andreas Fault Observatory at Depth (SAFOD) drilling phases 1 and 2”: Journal of Geophysical Research B: Solid Earth, v. 115, no. B3, B03418, https://doi.org/10.1029/2009JB000818.","productDescription":"B03418","ipdsId":"IP-018805","costCenters":[{"id":234,"text":"Earthquake Hazards Program","active":true,"usgs":true},{"id":237,"text":"Earthquake Science Center","active":true,"usgs":true}],"links":[{"id":475461,"rank":0,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1029/2009jb000818","text":"Publisher Index Page"},{"id":276283,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":276282,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1029/2009JB000818"}],"volume":"115","issue":"B3","noUsgsAuthors":false,"publicationDate":"2010-03-27","publicationStatus":"PW","scienceBaseUri":"5208b262e4b0058b906bf5c2","contributors":{"authors":[{"text":"Tembe, Sheryl","contributorId":87436,"corporation":false,"usgs":true,"family":"Tembe","given":"Sheryl","email":"","affiliations":[],"preferred":false,"id":482263,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Lockner, David","contributorId":21058,"corporation":false,"usgs":true,"family":"Lockner","given":"David","affiliations":[],"preferred":false,"id":482261,"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":482262,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70047109,"text":"70047109 - 2010 - Analytical models for the groundwater tidal prism and associated benthic water flux","interactions":[],"lastModifiedDate":"2013-07-18T13:32:25","indexId":"70047109","displayToPublicDate":"2013-01-01T13:29:00","publicationYear":"2010","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1923,"text":"Hydrogeology Journal","active":true,"publicationSubtype":{"id":10}},"title":"Analytical models for the groundwater tidal prism and associated benthic water flux","docAbstract":"The groundwater tidal prism is defined as the volume of water that inundates a porous medium, forced by one tidal oscillation in surface water. The pressure gradient that generates the prism acts on the subterranean estuary. Analytical models for the groundwater tidal prism and associated benthic flux are presented. The prism and flux are shown to be directly proportional to porosity, tidal amplitude, and the length of the groundwater wave; flux is inversely proportional to tidal period. The duration of discharge flux exceeds the duration of recharge flux over one tidal period; and discharge flux continues for some time following low tide. Models compare favorably with laboratory observations and are applied to a South Atlantic Bight study area, where tide generates an 11-m<sup>3</sup> groundwater tidal prism per m of shoreline, and drives 81 m<sup>3</sup> s<sup> −1</sup> to the study area, which describes 23% of an observational estimate. In a marine water body, the discharge component of any oscillatory benthic water flux is submarine groundwater discharge. Benthic flux transports constituents between groundwater and surface water, and is a process by which pollutant loading and saltwater intrusion may occur in coastal areas.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Hydrogeology Journal","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"Springer","doi":"10.1007/s10040-009-0519-y","usgsCitation":"King, J.N., Mehta, A.J., and Dean, R., 2010, Analytical models for the groundwater tidal prism and associated benthic water flux: Hydrogeology Journal, v. 18, no. 1, p. 203-215, https://doi.org/10.1007/s10040-009-0519-y.","productDescription":"13","startPage":"203","endPage":"215","ipdsId":"IP-010801","costCenters":[{"id":275,"text":"Florida Integrated Science Center","active":false,"usgs":true}],"links":[{"id":275147,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":275145,"type":{"id":15,"text":"Index Page"},"url":"https://link.springer.com/article/10.1007%2Fs10040-009-0519-y"},{"id":275144,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1007/s10040-009-0519-y"}],"volume":"18","issue":"1","noUsgsAuthors":false,"publicationDate":"2009-10-02","publicationStatus":"PW","scienceBaseUri":"51e90e5fe4b0e157e9e86ef4","contributors":{"authors":[{"text":"King, Jeffrey N. jking@usgs.gov","contributorId":10783,"corporation":false,"usgs":true,"family":"King","given":"Jeffrey","email":"jking@usgs.gov","middleInitial":"N.","affiliations":[],"preferred":false,"id":481076,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Mehta, Ashish J.","contributorId":21051,"corporation":false,"usgs":true,"family":"Mehta","given":"Ashish","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":481078,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Dean, Robert G.","contributorId":11916,"corporation":false,"usgs":true,"family":"Dean","given":"Robert G.","affiliations":[],"preferred":false,"id":481077,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70046817,"text":"70046817 - 2010 - Creation of next generation U.S. Geological Survey topographic maps","interactions":[],"lastModifiedDate":"2013-08-26T13:31:54","indexId":"70046817","displayToPublicDate":"2013-01-01T13:15:00","publicationYear":"2010","noYear":false,"publicationType":{"id":4,"text":"Book"},"publicationSubtype":{"id":12,"text":"Conference publication"},"title":"Creation of next generation U.S. Geological Survey topographic maps","docAbstract":"The U.S. Geological Survey (USGS) is 2 years into a 3-year cycle to create new digital topographic map products for the conterminous United States from data acquired and maintained as part of The National Map databases. These products are in the traditional, USGS topographic quadrangle, 7.5-minute (latitude and longitude) cell format. The 3-year cycle was conceived to follow the acquisition of National Aerial Imagery Program (NAIP) orthorectified imagery, a key layer in the new product. In fiscal year (FY) 2009 (ending September 30, 2009), the first year of the 3-year cycle, the USGS produced 13,200 products. These initial products of the “Digital MapBeta” series had limited feature content, including only the NAIP image, some roads, geographic names, and grid and collar information. The products were created in layered georegistered Portable Document Format (PDF) files, allowing users with freely available Adobe® Reader® software to view, print, and perform simple Geographic Information System-like functions. In FY 2010 (ending September 30, 2010), the USGS produced 20,380 products. These products of the “US Topo” series added hydrography (surface water features), contours, and some boundaries. In FY 2011 (ending September 30, 2011), the USGS will complete the initial coverage with US Topo products and will add additional feature content to the maps. The design, development, and production associated with the US Topo products provide management and technical challenges for the USGS and its public and private sector partners. One challenge is the acquisition and maintenance of nationally consistent base map data from multiple sources. Another is the use of these data to create a  consistent, current series of cartographic products that can be used by the broad spectrum of traditional topographic map users. Although the USGS and its partners have overcome many of these challenges, many, such as establishing and funding a sustainable base data-maintenance program, remain to be resolved for the long term.","conferenceTitle":"ASPRS/CaGIS 2010 Fall Specialty Conference","conferenceDate":"2010-11-01T00:00:00","conferenceLocation":"Orlando, FL","language":"English","publisher":"ISPRS Technical Commission","usgsCitation":"Craun, K.J., 2010, Creation of next generation U.S. Geological Survey topographic maps, 4 p.","productDescription":"4 p.","numberOfPages":"4","ipdsId":"IP-024012","costCenters":[],"links":[{"id":277004,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":277002,"type":{"id":11,"text":"Document"},"url":"https://www.isprs.org/proceedings/XXXVIII/part4/files/Craun.pdf"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"521c78e4e4b01458f7842920","contributors":{"authors":[{"text":"Craun, Kari J. 0000-0001-7875-2809 kcraun@usgs.gov","orcid":"https://orcid.org/0000-0001-7875-2809","contributorId":3526,"corporation":false,"usgs":true,"family":"Craun","given":"Kari","email":"kcraun@usgs.gov","middleInitial":"J.","affiliations":[{"id":404,"text":"NGTOC Rolla","active":true,"usgs":true},{"id":423,"text":"National Geospatial Program","active":true,"usgs":true}],"preferred":true,"id":480359,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70047163,"text":"70047163 - 2010 - Making lidar more photogenic: creating band combinations from lidar information","interactions":[],"lastModifiedDate":"2013-07-23T12:46:44","indexId":"70047163","displayToPublicDate":"2013-01-01T12:32:00","publicationYear":"2010","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3052,"text":"Photogrammetric Engineering and Remote Sensing","active":true,"publicationSubtype":{"id":10}},"title":"Making lidar more photogenic: creating band combinations from lidar information","docAbstract":"Over the past five to ten years the use and applicability of light detection and ranging (lidar) technology has increased dramatically. As a result, an almost exponential amount of lidar data is being collected across the country for a wide range of applications, and it is currently the technology of choice for high resolution terrain model creation, 3-dimensional city and infrastructure modeling, forestry and a wide range of scientific applications (Lin and Mills, 2010). The amount of data that is being delivered across the country is impressive. For example, the U.S. Geological Survey’s (USGS) Center for Lidar Information Coordination and Knowledge (CLICK), which is a National repository of USGS and partner lidar point cloud datasets (Stoker et al., 2006), currently has 3.5 percent of the United States covered by lidar, and has approximately another 5 percent in the processing queue. The majority of data being collected by the commercial sector are from discrete-return systems, which collect billions of lidar points in an average project. There are also a lot of discussions involving a potential National-scale Lidar effort (Stoker et al., 2008).","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Photogrammetric Engineering and Remote Sensing","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"Photogrammetric Engineering and Remote Sensing","usgsCitation":"Stoker, J.M., 2010, Making lidar more photogenic: creating band combinations from lidar information: Photogrammetric Engineering and Remote Sensing, v. 76, no. 3, p. 216-220.","productDescription":"5 p.","startPage":"216","endPage":"220","ipdsId":"IP-018975","costCenters":[{"id":222,"text":"Earth Resources Observation and Science (EROS) Center","active":true,"usgs":true}],"links":[{"id":275295,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":275294,"type":{"id":11,"text":"Document"},"url":"https://digital.ipcprintservices.com/publication/?i=32898&&l=&m=&ver=&pp=&p=15"}],"volume":"76","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"51efa5f2e4b0b09fbe58f199","contributors":{"authors":[{"text":"Stoker, Jason M. 0000-0003-2455-0931 jstoker@usgs.gov","orcid":"https://orcid.org/0000-0003-2455-0931","contributorId":3021,"corporation":false,"usgs":true,"family":"Stoker","given":"Jason","email":"jstoker@usgs.gov","middleInitial":"M.","affiliations":[{"id":423,"text":"National Geospatial Program","active":true,"usgs":true},{"id":223,"text":"Earth Resources Observation and Science (EROS) Center (Geography)","active":false,"usgs":true}],"preferred":true,"id":481196,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70044471,"text":"70044471 - 2010 - Petrography, mineralogy, and geochemistry of deep gravelly sands in the Eyreville B core, Chesapeake Bay impact structure","interactions":[],"lastModifiedDate":"2013-07-22T12:46:27","indexId":"70044471","displayToPublicDate":"2013-01-01T11:52:30","publicationYear":"2010","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2715,"text":"Meteoritics and Planetary Science","active":true,"publicationSubtype":{"id":10}},"title":"Petrography, mineralogy, and geochemistry of deep gravelly sands in the Eyreville B core, Chesapeake Bay impact structure","docAbstract":"The ICDP–USGS Eyreville drill cores in the Chesapeake Bay impact structure reached a total depth of 1766 m and comprise (from the bottom upwards) basement-derived schists and granites/pegmatites, impact breccias, mostly poorly lithified gravelly sand and crystalline blocks, a granitic slab, sedimentary breccias, and postimpact sediments. The gravelly sand and crystalline block section forms an approximately 26 m thick interval that includes an amphibolite block and boulders of cataclastic gneiss and suevite. Three gravelly sands (basal, middle, and upper) are distinguished within this interval. The gravelly sands are poorly sorted, clast supported, and generally massive, but crude size-sorting and subtle, discontinuous layers occur locally. Quartz and K-feldspar are the main sand-size minerals and smectite and kaolinite are the principal clay minerals. Other mineral grains occur only in accessory amounts and lithic clasts are sparse (only a few vol%). The gravelly sands are silica rich (~80 wt% SiO<sub>2</sub>). Trends with depth include a slight decrease in SiO<sub>2</sub> and slight increase in Fe<sub>2</sub>O<sub>3</sub>. The basal gravelly sand (below the cataclasite boulder) has a lower SiO<sub>2</sub> content, less K-feldspar, and more mica than the higher sands, and it contains more lithic clasts and melt particles that are probably reworked from the underlying suevite. The middle gravelly sand (below the amphibolite block) is finer-grained, contains more abundant clay minerals, and displays more variable chemical compositions than upper gravelly sand (above the block). Our mineralogical and geochemical results suggest that the gravelly sands are avalanche deposits derived probably from the nonmarine Potomac Formation in the lower part of the target sediment layer, in contrast to polymict diamictons higher in the core that have been interpreted as ocean-resurge debris flows, which is in agreement with previous interpretations. The mineralogy and geochemistry of the gravelly sands are typical for a passive continental margin source. There is no discernible mixing with marine sediments (no glauconite or Paleogene marine microfossils noted) during the impact remobilization and redeposition. The unshocked amphibolite block and cataclasite boulder might have originated from the outer parts of the transient crater.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Meteoritics and Planetary Science","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"Wiley","doi":"10.1111/j.1945-5100.2010.01077.x","usgsCitation":"Bartosova, K., Gier, S., Horton, J., Koeberl, C., Mader, D., and Dypvik, H., 2010, Petrography, mineralogy, and geochemistry of deep gravelly sands in the Eyreville B core, Chesapeake Bay impact structure: Meteoritics and Planetary Science, v. 45, no. 6, p. 1021-1052, https://doi.org/10.1111/j.1945-5100.2010.01077.x.","productDescription":"32 p.","startPage":"1021","endPage":"1052","ipdsId":"IP-019802","costCenters":[{"id":243,"text":"Eastern Geology and Paleoclimate Science Center","active":true,"usgs":true}],"links":[{"id":475462,"rank":0,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1111/j.1945-5100.2010.01077.x","text":"Publisher Index Page"},{"id":275220,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":275217,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1111/j.1945-5100.2010.01077.x"}],"country":"United States","state":"Virginia","otherGeospatial":"Chesapeake Bay","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -76.4633,36.9078 ], [ -76.4633,37.9656 ], [ -75.6353,37.9656 ], [ -75.6353,36.9078 ], [ -76.4633,36.9078 ] ] ] } } ] }","volume":"45","issue":"6","noUsgsAuthors":false,"publicationDate":"2010-10-15","publicationStatus":"PW","scienceBaseUri":"51ee5467e4b00ffbed48f8be","contributors":{"authors":[{"text":"Bartosova, Katerina","contributorId":33045,"corporation":false,"usgs":true,"family":"Bartosova","given":"Katerina","email":"","affiliations":[],"preferred":false,"id":475678,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Gier, Susanne","contributorId":72284,"corporation":false,"usgs":true,"family":"Gier","given":"Susanne","email":"","affiliations":[],"preferred":false,"id":475681,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Horton, J. Wright Jr. 0000-0001-6756-6365 whorton@usgs.gov","orcid":"https://orcid.org/0000-0001-6756-6365","contributorId":423,"corporation":false,"usgs":true,"family":"Horton","given":"J. Wright","suffix":"Jr.","email":"whorton@usgs.gov","affiliations":[{"id":243,"text":"Eastern Geology and Paleoclimate Science Center","active":true,"usgs":true}],"preferred":false,"id":475677,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Koeberl, Christian","contributorId":89432,"corporation":false,"usgs":true,"family":"Koeberl","given":"Christian","affiliations":[],"preferred":false,"id":475682,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Mader, Dieter","contributorId":34024,"corporation":false,"usgs":true,"family":"Mader","given":"Dieter","email":"","affiliations":[],"preferred":false,"id":475679,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Dypvik, Henning","contributorId":41318,"corporation":false,"usgs":true,"family":"Dypvik","given":"Henning","affiliations":[],"preferred":false,"id":475680,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}}
,{"id":70047018,"text":"70047018 - 2010 - Emerging themes in the ecology and management of North American forests","interactions":[],"lastModifiedDate":"2013-07-15T10:48:34","indexId":"70047018","displayToPublicDate":"2013-01-01T10:41:44","publicationYear":"2010","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2043,"text":"International Journal of Forestry Research","active":true,"publicationSubtype":{"id":10}},"title":"Emerging themes in the ecology and management of North American forests","docAbstract":"The 7th North American Forest Ecology Workshop, consisting of 149 presentations in 16 oral sessions and a poster session, reflected a broad range of topical areas currently under investigation in forest ecology and management. There was an overarching emphasis on the role of disturbance, both natural and anthropogenic, in the dynamics of forest ecosystems, and the recognition that legacies from past disturbances strongly influence future trajectories. Climate was invoked as a major driver of ecosystem change. An emphasis was placed on application of research findings for predicting system responses to changing forest management initiatives. Several “needs” emerged from the discussions regarding approaches to the study of forest ecosystems, including (1) consideration of variable spatial and temporal scales, (2) long-term monitoring, (3) development of universal databases more encompassing of time and space to facilitate meta-analyses, (4) combining field studies and modeling approaches, (5) standardizing methods of measurement and assessment, (6) guarding against oversimplification or overgeneralization from limited site-specific results, (7) greater emphasis on plant-animal interactions, and (8) better alignment of needs and communication of results between researchers and managers.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"International Journal of Forestry Research","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"Hindawi Publishing Corporation","doi":"10.1155/2010/964260","usgsCitation":"Sharik, T.L., Adair, W., Baker, F.A., Battaglia, M., Comfort, E.J., D’Amato, A.W., Delong, C., DeRose, R., Ducey, M.J., Harmon, M., Levy, L., Logan, J.A., O'Brien, J., Palik, B.J., Roberts, S.D., Rogers, P., Shinneman, D., Spies, T., Taylor, S.L., Woodall, C., and Youngblood, A., 2010, Emerging themes in the ecology and management of North American forests: International Journal of Forestry Research, v. 2010, Article ID 964260; 11 p., https://doi.org/10.1155/2010/964260.","productDescription":"Article ID 964260; 11 p.","ipdsId":"IP-015599","costCenters":[{"id":290,"text":"Forest and Rangeland Ecosystem Science Center","active":false,"usgs":true}],"links":[{"id":475463,"rank":0,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1155/2010/964260","text":"Publisher Index Page"},{"id":274970,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":274960,"type":{"id":15,"text":"Index Page"},"url":"https://www.sciencedirect.com/science/article/pii/S0378112712007086"},{"id":274969,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1155/2010/964260"}],"otherGeospatial":"North America","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ 177.1,5.6 ], [ 177.1,85.4 ], [ -4.0,85.4 ], [ -4.0,5.6 ], [ 177.1,5.6 ] ] ] } } ] }","volume":"2010","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"51e519e9e4b069f8d27ccad3","contributors":{"authors":[{"text":"Sharik, Terry L.","contributorId":98201,"corporation":false,"usgs":true,"family":"Sharik","given":"Terry","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":480882,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Adair, William","contributorId":88636,"corporation":false,"usgs":true,"family":"Adair","given":"William","email":"","affiliations":[],"preferred":false,"id":480879,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Baker, Fred A.","contributorId":73096,"corporation":false,"usgs":true,"family":"Baker","given":"Fred","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":480876,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Battaglia, Michael","contributorId":30529,"corporation":false,"usgs":true,"family":"Battaglia","given":"Michael","affiliations":[],"preferred":false,"id":480870,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Comfort, Emily J.","contributorId":103551,"corporation":false,"usgs":true,"family":"Comfort","given":"Emily","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":480883,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"D’Amato, Anthony W.","contributorId":28140,"corporation":false,"usgs":false,"family":"D’Amato","given":"Anthony","email":"","middleInitial":"W.","affiliations":[{"id":13478,"text":"Department of Forest Resources, University of Minnesota, St. Paul, Minnesota (Correspondence to: russellm@umn.edu)","active":true,"usgs":false},{"id":6735,"text":"University of Vermont, Rubenstein School of Environment and Natural Resources","active":true,"usgs":false}],"preferred":false,"id":480868,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Delong, Craig","contributorId":27341,"corporation":false,"usgs":true,"family":"Delong","given":"Craig","email":"","affiliations":[],"preferred":false,"id":480867,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"DeRose, R. Justin","contributorId":11494,"corporation":false,"usgs":true,"family":"DeRose","given":"R. Justin","affiliations":[],"preferred":false,"id":480864,"contributorType":{"id":1,"text":"Authors"},"rank":8},{"text":"Ducey, Mark J.","contributorId":31659,"corporation":false,"usgs":true,"family":"Ducey","given":"Mark","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":480871,"contributorType":{"id":1,"text":"Authors"},"rank":9},{"text":"Harmon, Mark","contributorId":14278,"corporation":false,"usgs":true,"family":"Harmon","given":"Mark","affiliations":[],"preferred":false,"id":480865,"contributorType":{"id":1,"text":"Authors"},"rank":10},{"text":"Levy, Louise","contributorId":25061,"corporation":false,"usgs":true,"family":"Levy","given":"Louise","email":"","affiliations":[],"preferred":false,"id":480866,"contributorType":{"id":1,"text":"Authors"},"rank":11},{"text":"Logan, Jesse A.","contributorId":85488,"corporation":false,"usgs":true,"family":"Logan","given":"Jesse","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":480878,"contributorType":{"id":1,"text":"Authors"},"rank":12},{"text":"O'Brien, Joseph","contributorId":105993,"corporation":false,"usgs":true,"family":"O'Brien","given":"Joseph","affiliations":[],"preferred":false,"id":480884,"contributorType":{"id":1,"text":"Authors"},"rank":13},{"text":"Palik, Brian J.","contributorId":78619,"corporation":false,"usgs":true,"family":"Palik","given":"Brian","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":480877,"contributorType":{"id":1,"text":"Authors"},"rank":14},{"text":"Roberts, Scott D.","contributorId":28147,"corporation":false,"usgs":true,"family":"Roberts","given":"Scott","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":480869,"contributorType":{"id":1,"text":"Authors"},"rank":15},{"text":"Rogers, Paul C.","contributorId":38452,"corporation":false,"usgs":true,"family":"Rogers","given":"Paul C.","affiliations":[],"preferred":false,"id":480873,"contributorType":{"id":1,"text":"Authors"},"rank":16},{"text":"Shinneman, Douglas J.","contributorId":70195,"corporation":false,"usgs":true,"family":"Shinneman","given":"Douglas J.","affiliations":[],"preferred":false,"id":480875,"contributorType":{"id":1,"text":"Authors"},"rank":17},{"text":"Spies, Thomas","contributorId":91772,"corporation":false,"usgs":true,"family":"Spies","given":"Thomas","affiliations":[],"preferred":false,"id":480880,"contributorType":{"id":1,"text":"Authors"},"rank":18},{"text":"Taylor, Sarah L.","contributorId":45209,"corporation":false,"usgs":true,"family":"Taylor","given":"Sarah","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":480874,"contributorType":{"id":1,"text":"Authors"},"rank":19},{"text":"Woodall, Christopher","contributorId":34409,"corporation":false,"usgs":true,"family":"Woodall","given":"Christopher","affiliations":[],"preferred":false,"id":480872,"contributorType":{"id":1,"text":"Authors"},"rank":20},{"text":"Youngblood, Andrew","contributorId":94193,"corporation":false,"usgs":true,"family":"Youngblood","given":"Andrew","affiliations":[],"preferred":false,"id":480881,"contributorType":{"id":1,"text":"Authors"},"rank":21}]}}
,{"id":70047440,"text":"70047440 - 2010 - The Nation's top 25 construction aggregates producers","interactions":[],"lastModifiedDate":"2013-08-06T10:38:02","indexId":"70047440","displayToPublicDate":"2013-01-01T10:37:00","publicationYear":"2010","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":674,"text":"Aggregates Manager","active":true,"publicationSubtype":{"id":10}},"title":"The Nation's top 25 construction aggregates producers","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Aggregates Manager","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"Randall Reilly Publishing","usgsCitation":"Willett, J., 2010, The Nation's top 25 construction aggregates producers: Aggregates Manager, v. 15, no. 3, p. 16-19.","productDescription":"4 p.","startPage":"16","endPage":"19","costCenters":[{"id":432,"text":"National Minerals Information Center","active":true,"usgs":true}],"links":[{"id":276104,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"15","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"52021aeae4b0e21cafa49cae","contributors":{"authors":[{"text":"Willett, Jason Christopher","contributorId":85480,"corporation":false,"usgs":true,"family":"Willett","given":"Jason Christopher","affiliations":[],"preferred":false,"id":482045,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70041896,"text":"70041896 - 2010 - Habitat selection and spawning success of walleye in a tributary to Owasco Lake, New York","interactions":[],"lastModifiedDate":"2013-02-28T11:59:13","indexId":"70041896","displayToPublicDate":"2013-01-01T00:00:00","publicationYear":"2010","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2886,"text":"North American Journal of Fisheries Management","active":true,"publicationSubtype":{"id":10}},"title":"Habitat selection and spawning success of walleye in a tributary to Owasco Lake, New York","docAbstract":"Walleyes <i>Sander vitreus</i> are stocked into Owasco Lake, New York, to provide a sport fishery, but the population must be sustained by annual hatchery supplementation despite the presence of appropriate habitat. Therefore, we evaluated walleye spawning success in Dutch Hollow Brook, a tributary of Owasco Lake, to determine whether early survival limited recruitment. Spawning success during spring 2006 and 2007 was evaluated by estimating egg densities from samples collected in the lower 725 m of the stream. Environmental variables were also recorded to characterize the selected spawning habitat. Drift nets were set downstream of the spawning section to assess egg survival and larval drift. We estimated that 162,596 larvae hatched in 2006. For 2007, we estimated that 360,026 eggs were deposited, with a hatch of 127,500 larvae and hatching success of 35.4%. Egg density was significantly correlated to percent cover, substrate type, and depth : velocity ratio. Two sections had significantly higher egg deposition than other areas. Adult spawning walleyes selected shallow, slow habitats with some cover and gravel substrate in the accessible reaches of Dutch Hollow Brook. Our results show that walleyes found suitable spawning habitat in Dutch Hollow Brook and that egg and larval development does not appear to limit natural reproduction.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"North American Journal of Fisheries Management","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"Taylor & Francis","publisherLocation":"Philadelphia, PA","doi":"10.1577/M09-033.1","usgsCitation":"Chalupnicki, M., Johnson, J.H., McKenna, J., and Dittman, D.E., 2010, Habitat selection and spawning success of walleye in a tributary to Owasco Lake, New York: North American Journal of Fisheries Management, v. 30, no. 1, p. 170-178, https://doi.org/10.1577/M09-033.1.","productDescription":"9 p.","startPage":"170","endPage":"178","ipdsId":"IP-012547","costCenters":[{"id":324,"text":"Great Lakes Science Center","active":true,"usgs":true}],"links":[{"id":268550,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":268549,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1577/M09-033.1"}],"country":"United States","state":"New York","otherGeospatial":"Owasco Lake","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -79.76,40.5 ], [ -79.76,45.0 ], [ -71.86,45.0 ], [ -71.86,40.5 ], [ -79.76,40.5 ] ] ] } } ] }","volume":"30","issue":"1","noUsgsAuthors":false,"publicationDate":"2010-02-01","publicationStatus":"PW","scienceBaseUri":"51308a8ce4b04c194073adf3","contributors":{"authors":[{"text":"Chalupnicki, Marc A. 0000-0002-3792-9345","orcid":"https://orcid.org/0000-0002-3792-9345","contributorId":11033,"corporation":false,"usgs":true,"family":"Chalupnicki","given":"Marc A.","affiliations":[{"id":324,"text":"Great Lakes Science Center","active":true,"usgs":true}],"preferred":false,"id":470328,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Johnson, James H. 0000-0002-5619-3871 jhjohnson@usgs.gov","orcid":"https://orcid.org/0000-0002-5619-3871","contributorId":389,"corporation":false,"usgs":true,"family":"Johnson","given":"James","email":"jhjohnson@usgs.gov","middleInitial":"H.","affiliations":[{"id":324,"text":"Great Lakes Science Center","active":true,"usgs":true}],"preferred":true,"id":470326,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"McKenna, James E. Jr.","contributorId":56992,"corporation":false,"usgs":true,"family":"McKenna","given":"James E.","suffix":"Jr.","affiliations":[],"preferred":false,"id":470329,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Dittman, Dawn E. 0000-0002-0711-3732 ddittman@usgs.gov","orcid":"https://orcid.org/0000-0002-0711-3732","contributorId":2762,"corporation":false,"usgs":true,"family":"Dittman","given":"Dawn","email":"ddittman@usgs.gov","middleInitial":"E.","affiliations":[{"id":324,"text":"Great Lakes Science Center","active":true,"usgs":true}],"preferred":true,"id":470327,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"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":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":70045902,"text":"70045902 - 2010 - Mineral resource of the month: fluorspar","interactions":[],"lastModifiedDate":"2013-05-08T17:04:40","indexId":"70045902","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: fluorspar","docAbstract":"The article features the industrial mineral fluorspar, used in the manufacture of fluorochemicals, aluminum and steel. It defines fluorspar as crude or beneficiated material, mined or milled for the non-metallic mineral fluorite or calcium fluoride. Applications of acid-grade fluorspar in the U.S. are presented, including production of hydrofluoric acid for chemical production of refrigerants such as chlorofluorocarbons or CFCs. World demand for fluorspar decreased with the CFC ban in the 1990s, but recovered with the use of hydrofluorocarbons or HFCs.","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: fluorspar: Earth, v. 55, no. 9, p. 28-29.","productDescription":"2 p.","startPage":"28","endPage":"29","costCenters":[{"id":432,"text":"National Minerals Information Center","active":true,"usgs":true}],"links":[{"id":272084,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"55","issue":"9","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"518b73ebe4b0037667dbc846","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":535500,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70046093,"text":"70046093 - 2010 - Current challenges using models to forecast seawater intrusion: lessons from the Eastern Shore of Virginia, USA","interactions":[],"lastModifiedDate":"2018-10-11T17:47:42","indexId":"70046093","displayToPublicDate":"2013-01-01T00:00:00","publicationYear":"2010","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1923,"text":"Hydrogeology Journal","active":true,"publicationSubtype":{"id":10}},"title":"Current challenges using models to forecast seawater intrusion: lessons from the Eastern Shore of Virginia, USA","docAbstract":"A three-dimensional model of the aquifer system of the Eastern Shore of Virginia, USA was calibrated to reproduce historical water levels and forecast the potential for saltwater intrusion. Future scenarios were simulated with two pumping schemes to predict potential areas of saltwater intrusion. Simulations suggest that only a few wells would be threatened with detectable salinity increases before 2050. The objective was to examine whether salinity increases can be accurately forecast for individual wells with such a model, and to address what the challenges are in making such model forecasts given current (2009) simulation capabilities. The analysis suggests that even with current computer capabilities, accurate simulations of concentrations within a regional-scale (many km) transition zone are computationally prohibitive. The relative paucity of data that is typical for such regions relative to what is needed for accurate transport simulations suggests that even with an infinitely powerful computer, accurate forecasting for a single well would still be elusive. Useful approaches may include local-grid refinement near wells and geophysical surveys, but it is important to keep expectations for simulated forecasts at wells in line with chloride concentration and other data that can be obtained at that local scale.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Hydrogeology Journal","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"Springer","doi":"10.1007/s10040-009-0513-4","usgsCitation":"Sanford, W.E., and Pope, J.P., 2010, Current challenges using models to forecast seawater intrusion: lessons from the Eastern Shore of Virginia, USA: Hydrogeology Journal, v. 18, no. 1, p. 73-93, https://doi.org/10.1007/s10040-009-0513-4.","productDescription":"21 p.","startPage":"73","endPage":"93","ipdsId":"IP-011118","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":272784,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":294165,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1007/s10040-009-0513-4"}],"country":"United States","state":"Virginia","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -83.6754,36.5408 ], [ -83.6754,39.466 ], [ -75.2422,39.466 ], [ -75.2422,36.5408 ], [ -83.6754,36.5408 ] ] ] } } ] }","volume":"18","issue":"1","noUsgsAuthors":false,"publicationDate":"2009-08-25","publicationStatus":"PW","scienceBaseUri":"51a08be0e4b0e42455806566","contributors":{"authors":[{"text":"Sanford, Ward E. 0000-0002-6624-0280 wsanford@usgs.gov","orcid":"https://orcid.org/0000-0002-6624-0280","contributorId":2268,"corporation":false,"usgs":true,"family":"Sanford","given":"Ward","email":"wsanford@usgs.gov","middleInitial":"E.","affiliations":[{"id":436,"text":"National Research Program - Eastern Branch","active":true,"usgs":true},{"id":37778,"text":"WMA - Integrated Modeling and Prediction Division","active":true,"usgs":true}],"preferred":true,"id":478893,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Pope, Jason P. 0000-0003-3199-993X jpope@usgs.gov","orcid":"https://orcid.org/0000-0003-3199-993X","contributorId":2044,"corporation":false,"usgs":true,"family":"Pope","given":"Jason","email":"jpope@usgs.gov","middleInitial":"P.","affiliations":[{"id":37759,"text":"VA/WV Water Science Center","active":true,"usgs":true},{"id":614,"text":"Virginia Water Science Center","active":true,"usgs":true}],"preferred":true,"id":478892,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70045705,"text":"70045705 - 2010 - Model-based evaluation of highly and low pathogenic avian influenza dynamics in wild birds","interactions":[],"lastModifiedDate":"2013-04-30T10:54:26","indexId":"70045705","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":"Model-based evaluation of highly and low pathogenic avian influenza dynamics in wild birds","docAbstract":"There is growing interest in avian influenza (AI) epidemiology to predict disease risk in wild and domestic birds, and prevent transmission to humans. However, understanding the epidemic dynamics of highly pathogenic (HPAI) viruses remains challenging because they have rarely been detected in wild birds. We used modeling to integrate available scientific information from laboratory and field studies, evaluate AI dynamics in individual hosts and waterfowl populations, and identify key areas for future research. We developed a Susceptible-Exposed-Infectious-Recovered (SEIR) model and used published laboratory challenge studies to estimate epidemiological parameters (rate of infection, latency period, recovery and mortality rates), considering the importance of age classes, and virus pathogenicity. Infectious contact leads to infection and virus shedding within 1–2 days, followed by relatively slower period for recovery or mortality. We found a shorter infectious period for HPAI than low pathogenic (LP) AI, which may explain that HPAI has been much harder to detect than LPAI during surveillance programs. Our model predicted a rapid LPAI epidemic curve, with a median duration of infection of 50–60 days and no fatalities. In contrast, HPAI dynamics had lower prevalence and higher mortality, especially in young birds. Based on field data from LPAI studies, our model suggests to increase surveillance for HPAI in post-breeding areas, because the presence of immunologically naïve young birds is predicted to cause higher HPAI prevalence and bird losses during this season. Our results indicate a better understanding of the transmission, infection, and immunity-related processes is required to refine predictions of AI risk and spread, improve surveillance for HPAI in wild birds, and develop disease control strategies to reduce potential transmission to domestic birds and/or humans.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"PLoS ONE","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"Public Library of Science","usgsCitation":"Hénaux, V., Samuel, M.D., and Bunck, C.M., 2010, Model-based evaluation of highly and low pathogenic avian influenza dynamics in wild birds: PLoS ONE, v. 5, no. 6, e10997.","productDescription":"e10997","costCenters":[{"id":675,"text":"Wisconsin Cooperative Wildlife Research Unit","active":false,"usgs":true}],"links":[{"id":271638,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"5","issue":"6","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5180e7e8e4b0df838b924d75","contributors":{"authors":[{"text":"Hénaux, Viviane","contributorId":47670,"corporation":false,"usgs":true,"family":"Hénaux","given":"Viviane","affiliations":[],"preferred":false,"id":478120,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Samuel, Michael D. msamuel@usgs.gov","contributorId":1419,"corporation":false,"usgs":true,"family":"Samuel","given":"Michael","email":"msamuel@usgs.gov","middleInitial":"D.","affiliations":[{"id":199,"text":"Coop Res Unit Leetown","active":true,"usgs":true}],"preferred":true,"id":478119,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Bunck, Christine M. cbunck@usgs.gov","contributorId":731,"corporation":false,"usgs":true,"family":"Bunck","given":"Christine","email":"cbunck@usgs.gov","middleInitial":"M.","affiliations":[],"preferred":true,"id":478118,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70043232,"text":"70043232 - 2010 - An overview of sensor calibration inter-comparison and applications","interactions":[],"lastModifiedDate":"2013-04-08T20:29:34","indexId":"70043232","displayToPublicDate":"2013-01-01T00:00:00","publicationYear":"2010","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1707,"text":"Frontiers of Earth Science in China","active":true,"publicationSubtype":{"id":10}},"title":"An overview of sensor calibration inter-comparison and applications","docAbstract":"Long-term climate data records (CDR) are often constructed using observations made by multiple Earth observing sensors over a broad range of spectra and a large scale in both time and space. These sensors can be of the same or different types operated on the same or different platforms. They can be developed and built with different technologies and are likely operated over different time spans. It has been known that the uncertainty of climate models and data records depends not only on the calibration quality (accuracy and stability) of individual sensors, but also on their calibration consistency across instruments and platforms. Therefore, sensor calibration inter-comparison and validation have become increasingly demanding and will continue to play an important role for a better understanding of the science product quality. This paper provides an overview of different methodologies, which have been successfully applied for sensor calibration inter-comparison. Specific examples using different sensors, including MODIS, AVHRR, and ETM+, are presented to illustrate the implementation of these methodologies.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Frontiers of Earth Science in China","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"Springer","publisherLocation":"Amsterdam, Netherlands","doi":"10.1007/s11707-010-0002-z","usgsCitation":"Xiong, X., Cao, C., and Chander, G., 2010, An overview of sensor calibration inter-comparison and applications: Frontiers of Earth Science in China, v. 4, no. 2, p. 237-252, https://doi.org/10.1007/s11707-010-0002-z.","productDescription":"16 p.","startPage":"237","endPage":"252","ipdsId":"IP-017283","costCenters":[{"id":222,"text":"Earth Resources Observation and Science (EROS) Center","active":true,"usgs":true}],"links":[{"id":270674,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":270673,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1007/s11707-010-0002-z"}],"volume":"4","issue":"2","noUsgsAuthors":false,"publicationDate":"2010-02-12","publicationStatus":"PW","scienceBaseUri":"5163e6e7e4b0b7010f820160","contributors":{"authors":[{"text":"Xiong, Xiaoxiong","contributorId":15088,"corporation":false,"usgs":true,"family":"Xiong","given":"Xiaoxiong","email":"","affiliations":[],"preferred":false,"id":473195,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Cao, Changyong","contributorId":24663,"corporation":false,"usgs":true,"family":"Cao","given":"Changyong","email":"","affiliations":[],"preferred":false,"id":473196,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Chander, Gyanesh gchander@usgs.gov","contributorId":3013,"corporation":false,"usgs":true,"family":"Chander","given":"Gyanesh","email":"gchander@usgs.gov","affiliations":[],"preferred":true,"id":473194,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"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":70003353,"text":"70003353 - 2010 - Groundwater sustainability strategies","interactions":[],"lastModifiedDate":"2013-06-11T14:18:24","indexId":"70003353","displayToPublicDate":"2013-01-01T00:00:00","publicationYear":"2010","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2845,"text":"Nature Geoscience","active":true,"publicationSubtype":{"id":10}},"title":"Groundwater sustainability strategies","docAbstract":"Groundwater extraction has facilitated significant social development and economic growth, enhanced food security and alleviated drought in many farming regions. But groundwater development has also depressed water tables, degraded ecosystems and led to the deterioration of groundwater quality, as well as to conflict among water users. The effects are not evenly spread. In some areas of India, for example, groundwater depletion has preferentially affected the poor. Importantly, groundwater in some aquifers is renewed slowly, over decades to millennia, and coupled climate–aquifer models predict that the flux and/or timing of recharge to many aquifers will change under future climate scenarios. Here we argue that communities need to set multigenerational goals if groundwater is to be managed sustainably.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Nature Geoscience","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"Nature Publishing Group","doi":"10.1038/ngeo881","usgsCitation":"Gleeson, T., VanderSteen, J., Sophocleous, M.A., Taniguchi, M., Alley, W., Allen, D.M., and Zhou, Y., 2010, Groundwater sustainability strategies: Nature Geoscience, v. 3, p. 378-379, https://doi.org/10.1038/ngeo881.","productDescription":"2 p.","startPage":"378","endPage":"379","ipdsId":"IP-019958","costCenters":[{"id":494,"text":"Office of Groundwater","active":false,"usgs":true}],"links":[{"id":273611,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":273609,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1038/ngeo881"}],"volume":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"51b846e7e4b03203c522b1da","contributors":{"authors":[{"text":"Gleeson, Tom","contributorId":42694,"corporation":false,"usgs":false,"family":"Gleeson","given":"Tom","affiliations":[{"id":6646,"text":"McGill University","active":true,"usgs":false}],"preferred":false,"id":346991,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"VanderSteen, Jonathan","contributorId":56539,"corporation":false,"usgs":true,"family":"VanderSteen","given":"Jonathan","email":"","affiliations":[],"preferred":false,"id":346992,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Sophocleous, Marios A.","contributorId":64976,"corporation":false,"usgs":true,"family":"Sophocleous","given":"Marios","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":346994,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Taniguchi, Makoto","contributorId":89789,"corporation":false,"usgs":true,"family":"Taniguchi","given":"Makoto","email":"","affiliations":[],"preferred":false,"id":346996,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Alley, William M.","contributorId":93030,"corporation":false,"usgs":true,"family":"Alley","given":"William M.","affiliations":[],"preferred":false,"id":346997,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Allen, Diana M.","contributorId":83010,"corporation":false,"usgs":true,"family":"Allen","given":"Diana","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":346995,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Zhou, Yangxiao","contributorId":57749,"corporation":false,"usgs":true,"family":"Zhou","given":"Yangxiao","email":"","affiliations":[],"preferred":false,"id":346993,"contributorType":{"id":1,"text":"Authors"},"rank":7}]}}
,{"id":70043294,"text":"70043294 - 2010 - A self-trained classification technique for producing 30 m percent-water maps from Landsat data","interactions":[],"lastModifiedDate":"2013-02-26T20:04:00","indexId":"70043294","displayToPublicDate":"2013-01-01T00:00:00","publicationYear":"2010","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2068,"text":"International Journal of Remote Sensing","active":true,"publicationSubtype":{"id":10}},"title":"A self-trained classification technique for producing 30 m percent-water maps from Landsat data","docAbstract":"Small bodies of water can be mapped with moderate-resolution satellite data using methods where water is mapped as subpixel fractions using field measurements or high-resolution images as training datasets. A new method, developed from a regression-tree technique, uses a 30 m Landsat image for training the regression tree that, in turn, is applied to the same image to map subpixel water. The self-trained method was evaluated by comparing the percent-water map with three other maps generated from established percent-water mapping methods: (1) a regression-tree model trained with a 5 m SPOT 5 image, (2) a regression-tree model based on endmembers and (3) a linear unmixing classification technique. The results suggest that subpixel water fractions can be accurately estimated when high-resolution satellite data or intensively interpreted training datasets are not available, which increases our ability to map small water bodies or small changes in lake size at a regional scale.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"International Journal of Remote Sensing","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"Taylor and Francis","publisherLocation":"Philadelphia, PA","doi":"10.1080/01431161003667455","usgsCitation":"Rover, J.R., Wylie, B.K., and Ji, L., 2010, A self-trained classification technique for producing 30 m percent-water maps from Landsat data: International Journal of Remote Sensing, v. 31, no. 8, p. 2197-2203, https://doi.org/10.1080/01431161003667455.","productDescription":"7 p.","startPage":"2197","endPage":"2203","ipdsId":"IP-017132","costCenters":[{"id":222,"text":"Earth Resources Observation and Science (EROS) Center","active":true,"usgs":true}],"links":[{"id":268426,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":268425,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1080/01431161003667455"}],"volume":"31","issue":"8","noUsgsAuthors":false,"publicationDate":"2010-04-28","publicationStatus":"PW","scienceBaseUri":"53cd4a8be4b0b290850efd77","contributors":{"authors":[{"text":"Rover, Jennifer R. 0000-0002-3437-4030 jrover@usgs.gov","orcid":"https://orcid.org/0000-0002-3437-4030","contributorId":2941,"corporation":false,"usgs":true,"family":"Rover","given":"Jennifer","email":"jrover@usgs.gov","middleInitial":"R.","affiliations":[],"preferred":false,"id":473315,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Wylie, Bruce K. 0000-0002-7374-1083 wylie@usgs.gov","orcid":"https://orcid.org/0000-0002-7374-1083","contributorId":750,"corporation":false,"usgs":true,"family":"Wylie","given":"Bruce","email":"wylie@usgs.gov","middleInitial":"K.","affiliations":[{"id":223,"text":"Earth Resources Observation and Science (EROS) Center (Geography)","active":false,"usgs":true},{"id":222,"text":"Earth Resources Observation and Science (EROS) Center","active":true,"usgs":true}],"preferred":true,"id":473313,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Ji, Lei 0000-0002-6133-1036 lji@usgs.gov","orcid":"https://orcid.org/0000-0002-6133-1036","contributorId":2832,"corporation":false,"usgs":true,"family":"Ji","given":"Lei","email":"lji@usgs.gov","affiliations":[{"id":223,"text":"Earth Resources Observation and Science (EROS) Center (Geography)","active":false,"usgs":true}],"preferred":false,"id":473314,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70042697,"text":"70042697 - 2010 - Do three massive coral species from the same reef record the same SST signal? A test from the Dry Tortugas, Florida Keys","interactions":[],"lastModifiedDate":"2022-11-14T16:42:25.452446","indexId":"70042697","displayToPublicDate":"2013-01-01T00:00:00","publicationYear":"2010","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"Do three massive coral species from the same reef record the same SST signal? A test from the Dry Tortugas, Florida Keys","docAbstract":"<p><span>Paleoclimatologists have reconstructed century-long records of sea surface temperature (SST) in the Pacific using the Sr/Ca of massive corals, whereas similar reconstructions in the Atlantic have not proceeded at the same pace. Past research in the Florida Keys has focused on&nbsp;</span><i>Montastrea spp.</i><span>, an abundant and fast-growing massive coral, thus a good candidate for climate reconstructions. However, coral records from the Florida Keys are complicated by freshwater flux, which varies the Sr/Ca in seawater, thus confounding the Sr/Ca to SST signal. In this research, we compared the monthly Sr/Ca variations in three massive corals species (</span><i>Montastraea faveolata, Diploria strigosa, and Siderastrea siderea</i><span>) from the same reef in the nearly pristine Dry Tortugas National Park (24.70N, 82.80W) at the southwestern extent of the Florida Keys. This location is ideal for a calibration study as hourly water temperature records are available and the remote reef is far from mainland freshwater influence. These corals experienced the same environmental conditions (water depth, clarity, Sr/Ca of seawater, etc.) but differ in the mean annual growth rates (0.86 &plusmn;0.10 (1&sigma;) cm/year&nbsp;</span><i>M. faveolata</i><span>; 0.67 &plusmn;0.04 (1&sigma;) cm/year&nbsp;</span><i>D. strigosa</i><span>; 0.44 &plusmn;0.04 (1&sigma;) cm/year&nbsp;</span><i>S. siderea</i><span>). The mean Sr/Ca values are not the same but decrease with mean annual growth rates (9.201 &plusmn;0.091 (1&sigma;) mmol/mol&nbsp;</span><i>M. faveolata</i><span>; 9.177 &plusmn;0.081 (1&sigma;) mmol/mol&nbsp;</span><i>D. strigosa</i><span>; 8.964 &plusmn;0.12 (1&sigma;) mmol/mol&nbsp;</span><i>S. siderea</i><span>), thus supporting the &ldquo;vital effect&rdquo; or biological differences during calcification between coral species. The amplitude of the seasonal cycle in Sr/Ca varies with the slower growing&nbsp;</span><i>S. siderea</i><span>having the largest mean amplitude and&nbsp;</span><i>D. strigosa</i><span>&nbsp;the smallest (0.340 mmol/mol&nbsp;</span><i>S. siderea</i><span>; 0.284 mmol/mol&nbsp;</span><i>M. faveolata</i><span>; 0.238 mmol/mol&nbsp;</span><i>D. strigosa</i><span>). We confirmed our sampling methods by conducting several intracolony and intercolony coral Sr/Ca replication tests and found a high correlation in all tests (&gt;0.95&nbsp;</span><i>S. siderea</i><span>; &gt;0.90&nbsp;</span><i>D. strigosa</i><span>; &gt;0.83&nbsp;</span><i>M. faveolata; p</i><span>&nbsp;&lt; 0.05). The weighted linear regression of monthly coral Sr/Ca to mean monthly SST revealed that&nbsp;</span><i>S. siderea</i><span>captured the seasonal and interannual variability in SST (</span><i>r</i><span>&nbsp;= -0.97, -0.61 monthly and monthly anomalies, respectively,&nbsp;</span><i>p</i><span>&nbsp;&lt; 0.05). The other corals have reduced correlation with monthly anomalies and do not capture the seasonal variability with the same fidelity as&nbsp;</span><i>S. siderea</i><span>. All three corals were sampled along the thecal wall following the same procedures; however, each coral species has a different skeletal structure, density, and micro-scale growth patterns. We hypothesize the thecal wall of&nbsp;</span><i>S. siderea</i><span>&nbsp;calcifies at a continuous rate along the time-growth axis whereas the wall of&nbsp;</span><i>D. strigosa</i><span>&nbsp;and&nbsp;</span><i>M. faveolata</i><span>&nbsp;reflects a more complex signal. Of the three species, the slow growing&nbsp;</span><i>S. siderea</i><span>&nbsp;provides a robust reconstruction of mean monthly SST for the Dry Tortugas thus suitable for longer centennial-scale reconstructions.</span></p>","conferenceTitle":"American Geophysical Union 2010 Joint Assembly","conferenceDate":"August 8-12, 2010","conferenceLocation":"Foz do Iguassu, Brazil","language":"English","publisher":"American Geophysical Union","usgsCitation":"DeLong, K.L., Poore, R., Reich, C., Flannery, J.A., Maupin, C.R., and Quinn, T.M., 2010, Do three massive coral species from the same reef record the same SST signal? A test from the Dry Tortugas, Florida Keys, American Geophysical Union 2010 Joint Assembly, Foz do Iguassu, Brazil, August 8-12, 2010.","onlineOnly":"N","additionalOnlineFiles":"N","ipdsId":"IP-022355","costCenters":[{"id":574,"text":"St. Petersburg Coastal and Marine Science Center","active":true,"usgs":true}],"links":[{"id":270214,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Florida","otherGeospatial":"Dry Tortugas National Park","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -82.76673820002982,\n              24.702032234521695\n            ],\n            [\n              -82.80111355697035,\n              24.72611070301882\n            ],\n            [\n              -82.86737930528973,\n              24.725734512768284\n            ],\n            [\n              -82.90051217944944,\n              24.717834254792294\n            ],\n            [\n              -82.96719208869578,\n              24.649344358619032\n            ],\n            [\n              -82.96553544498762,\n              24.5665042001456\n            ],\n            [\n              -82.89678473110656,\n              24.566880870376693\n            ],\n            [\n              -82.80028523511646,\n              24.617720954532814\n            ],\n            [\n              -82.76632403910288,\n              24.66891673942027\n            ],\n            [\n              -82.76632403910288,\n              24.702032234521695\n            ],\n            [\n              -82.76673820002982,\n              24.702032234521695\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5152c387e4b01197b08e9c7f","contributors":{"authors":[{"text":"DeLong, K. L.","contributorId":88980,"corporation":false,"usgs":true,"family":"DeLong","given":"K.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":472079,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Poore, R.Z.","contributorId":35314,"corporation":false,"usgs":true,"family":"Poore","given":"R.Z.","email":"","affiliations":[],"preferred":false,"id":472074,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Reich, C. D. 0000-0002-2534-1456","orcid":"https://orcid.org/0000-0002-2534-1456","contributorId":36978,"corporation":false,"usgs":true,"family":"Reich","given":"C. D.","affiliations":[],"preferred":false,"id":472075,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Flannery, J. A.","contributorId":43606,"corporation":false,"usgs":true,"family":"Flannery","given":"J.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":472076,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Maupin, Christopher R.","contributorId":85812,"corporation":false,"usgs":false,"family":"Maupin","given":"Christopher","email":"","middleInitial":"R.","affiliations":[{"id":12811,"text":"Institute for Geophysics, Jackson School of Geosciences, University of Texas, Austin","active":true,"usgs":false}],"preferred":false,"id":472078,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Quinn, T. M.","contributorId":71320,"corporation":false,"usgs":true,"family":"Quinn","given":"T.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":472077,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}}
,{"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":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":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":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":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 Page"},{"id":273429,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Arizona","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"Polygon\",\"coordinates\":[[[-112.538593,37.000674],[-111.405517,37.001497],[-111.278286,37.000465],[-111.254853,37.001077],[-111.133718,37.000779],[-111.066496,37.002389],[-110.599512,37.003448],[-110.50069,37.00426],[-110.490908,37.003566],[-110.47019,36.997997],[-110.021778,36.998602],[-110.000876,36.998502],[-110.000677,36.997968],[-109.875673,36.998504],[-109.625668,36.998308],[-109.495338,36.999105],[-109.246917,36.999346],[-109.045223,36.999084],[-109.046796,35.363606],[-109.046084,35.250025],[-109.046072,34.828566],[-109.045624,34.814226],[-109.046104,34.799981],[-109.045363,34.785406],[-109.046086,34.771016],[-109.047006,34.00005],[-109.046426,33.875052],[-109.047145,33.74001],[-109.046662,33.625055],[-109.047298,33.409783],[-109.046564,33.37506],[-109.047045,33.36928],[-109.04747,33.250063],[-109.046905,33.091931],[-109.04748,33.06842],[-109.047117,32.77757],[-109.049112,31.636598],[-109.050173,31.480004],[-109.050044,31.332502],[-109.278489,31.333959],[-109.829689,31.334067],[-110.000613,31.333145],[-110.140512,31.333965],[-110.460172,31.332827],[-110.795467,31.33363],[-111.000643,31.332177],[-111.074825,31.332239],[-111.125646,31.348978],[-111.560194,31.488138],[-111.979417,31.620683],[-112.246102,31.704195],[-112.867074,31.895488],[-113.125961,31.97278],[-113.217308,32.002107],[-113.493196,32.088943],[-113.78168,32.179034],[-114.250775,32.32391],[-114.50078,32.400057],[-114.813613,32.494277],[-114.813991,32.497231],[-114.812316,32.500054],[-114.813694,32.505065],[-114.81237,32.507712],[-114.807726,32.508726],[-114.806017,32.510094],[-114.804694,32.512476],[-114.804958,32.517506],[-114.809723,32.520153],[-114.811576,32.523594],[-114.810563,32.527666],[-114.8064,32.531192],[-114.802181,32.536414],[-114.802018,32.53946],[-114.804776,32.541659],[-114.80583,32.546354],[-114.803883,32.548002],[-114.795635,32.550956],[-114.793769,32.552329],[-114.792065,32.555009],[-114.791551,32.557023],[-114.791988,32.560652],[-114.794635,32.563564],[-114.795959,32.564093],[-114.79766,32.564444],[-114.804429,32.561976],[-114.808929,32.561976],[-114.810517,32.563828],[-114.810517,32.56727],[-114.808929,32.569652],[-114.804421,32.572942],[-114.801877,32.57601],[-114.801471,32.578255],[-114.803879,32.580889],[-114.803987,32.582652],[-114.800441,32.58808],[-114.799683,32.593621],[-114.801548,32.598591],[-114.805932,32.600721],[-114.807906,32.602783],[-114.809042,32.608806],[-114.809393,32.617119],[-114.80739,32.621332],[-114.799302,32.625115],[-114.794102,32.622475],[-114.791179,32.621833],[-114.781872,32.62505],[-114.78267,32.628634],[-114.782235,32.630215],[-114.779215,32.633579],[-114.774482,32.635869],[-114.764382,32.642666],[-114.76331,32.644617],[-114.763512,32.645996],[-114.765067,32.648047],[-114.76495,32.649391],[-114.75831,32.655178],[-114.753111,32.658304],[-114.748,32.664184],[-114.747848,32.667693],[-114.745345,32.672187],[-114.744491,32.678671],[-114.730453,32.698843],[-114.730086,32.704298],[-114.722746,32.713071],[-114.717665,32.721654],[-114.714522,32.73039],[-114.701918,32.745548],[-114.69879,32.744846],[-114.688779,32.737675],[-114.684278,32.737537],[-114.667493,32.734226],[-114.65826,32.733799],[-114.632686,32.730846],[-114.618373,32.728245],[-114.615585,32.728446],[-114.614772,32.734089],[-114.612697,32.734516],[-114.581784,32.734946],[-114.581736,32.742321],[-114.564508,32.742298],[-114.564447,32.749554],[-114.539224,32.749812],[-114.539093,32.756949],[-114.526856,32.757094],[-114.528443,32.767276],[-114.531831,32.774264],[-114.532432,32.776923],[-114.531669,32.791185],[-114.528849,32.796307],[-114.522031,32.801675],[-114.515389,32.811439],[-114.510217,32.816417],[-114.494116,32.823288],[-114.468971,32.845155],[-114.465546,32.874809],[-114.465715,32.87942],[-114.463127,32.901884],[-114.462929,32.907944],[-114.464448,32.913129],[-114.47664,32.923628],[-114.479005,32.928291],[-114.48092,32.935252],[-114.48074,32.937027],[-114.478456,32.940555],[-114.474042,32.94515],[-114.470833,32.949333],[-114.469113,32.952673],[-114.46773,32.956323],[-114.467272,32.960675],[-114.467664,32.966861],[-114.469039,32.972295],[-114.470988,32.97406],[-114.476156,32.975168],[-114.480417,32.973665],[-114.481315,32.972064],[-114.488625,32.969946],[-114.490129,32.969885],[-114.492938,32.971781],[-114.494212,32.974262],[-114.495712,32.980076],[-114.499797,33.003905],[-114.50613,33.01701],[-114.511343,33.023455],[-114.52013,33.029984],[-114.523578,33.030961],[-114.538459,33.033422],[-114.553189,33.033974],[-114.571653,33.036624],[-114.575161,33.036542],[-114.578287,33.035375],[-114.581404,33.032545],[-114.584765,33.028231],[-114.589778,33.026228],[-114.601014,33.02541],[-114.618788,33.027202],[-114.625787,33.029436],[-114.628293,33.031052],[-114.639553,33.045291],[-114.64598,33.048903],[-114.649001,33.046763],[-114.655038,33.037107],[-114.657827,33.033825],[-114.659832,33.032665],[-114.662317,33.032671],[-114.66506,33.033908],[-114.670803,33.037984],[-114.673659,33.041897],[-114.675104,33.047532],[-114.674296,33.057171],[-114.686991,33.070969],[-114.68912,33.076122],[-114.689307,33.079179],[-114.688597,33.082869],[-114.68902,33.084036],[-114.692548,33.085786],[-114.701165,33.086368],[-114.70473,33.087051],[-114.706488,33.08816],[-114.707819,33.091102],[-114.707896,33.097432],[-114.703682,33.113769],[-114.696829,33.131209],[-114.689995,33.137883],[-114.687074,33.142196],[-114.682253,33.155214],[-114.679359,33.159519],[-114.678729,33.162948],[-114.680248,33.169717],[-114.679034,33.174738],[-114.675831,33.18152],[-114.67536,33.185489],[-114.67519,33.188179],[-114.678749,33.203448],[-114.673715,33.219245],[-114.673626,33.223121],[-114.674479,33.225504],[-114.678097,33.2303],[-114.682731,33.234918],[-114.689421,33.24525],[-114.689541,33.246428],[-114.688205,33.247966],[-114.674491,33.255597],[-114.672088,33.258499],[-114.672401,33.26047],[-114.677032,33.27017],[-114.680507,33.273577],[-114.684363,33.276025],[-114.694449,33.279786],[-114.711197,33.283342],[-114.717875,33.285157],[-114.72167,33.286982],[-114.723259,33.288079],[-114.731223,33.302434],[-114.731222,33.304039],[-114.729904,33.305745],[-114.723623,33.31211],[-114.710792,33.320607],[-114.707962,33.323421],[-114.705241,33.327767],[-114.700938,33.337014],[-114.698035,33.352442],[-114.699053,33.361148],[-114.707348,33.376628],[-114.70731,33.382542],[-114.708408,33.384147],[-114.713602,33.388257],[-114.722872,33.398779],[-114.725292,33.402342],[-114.725282,33.405048],[-114.723829,33.406531],[-114.720065,33.407891],[-114.710878,33.407254],[-114.701732,33.408388],[-114.697707,33.410942],[-114.695655,33.415127],[-114.687953,33.417944],[-114.673901,33.418299],[-114.658382,33.413036],[-114.652828,33.412922],[-114.64954,33.413633],[-114.643302,33.416745],[-114.635183,33.422726],[-114.62964,33.428138],[-114.627125,33.433554],[-114.622283,33.447558],[-114.623395,33.45449],[-114.622918,33.456561],[-114.612472,33.470768],[-114.601696,33.481394],[-114.599713,33.484315],[-114.597283,33.490653],[-114.591554,33.499443],[-114.588239,33.502453],[-114.580468,33.506465],[-114.573757,33.507543],[-114.569533,33.509219],[-114.560963,33.516739],[-114.560835,33.524334],[-114.558898,33.531819],[-114.542011,33.542481],[-114.524599,33.552231],[-114.524391,33.553683],[-114.526834,33.557466],[-114.535965,33.569154],[-114.5403,33.580615],[-114.540617,33.591412],[-114.529186,33.60665],[-114.524813,33.611351],[-114.524619,33.61426],[-114.525783,33.616588],[-114.527938,33.618839],[-114.529662,33.622794],[-114.529856,33.627448],[-114.526947,33.633073],[-114.526947,33.637534],[-114.53005,33.647619],[-114.530244,33.65014],[-114.525201,33.658092],[-114.525201,33.661583],[-114.529706,33.668031],[-114.530999,33.671102],[-114.531523,33.675108],[-114.530348,33.679245],[-114.527782,33.682684],[-114.523959,33.685879],[-114.512409,33.691282],[-114.504993,33.693022],[-114.496489,33.696901],[-114.495719,33.698454],[-114.494197,33.707922],[-114.494901,33.71443],[-114.496565,33.719155],[-114.500788,33.722204],[-114.502661,33.724584],[-114.504176,33.728055],[-114.506799,33.730518],[-114.510265,33.732146],[-114.512348,33.734214],[-114.508206,33.741587],[-114.504483,33.750998],[-114.504863,33.760465],[-114.507089,33.76793],[-114.516734,33.788345],[-114.520094,33.799473],[-114.52805,33.814963],[-114.527161,33.816191],[-114.522714,33.818979],[-114.520733,33.822031],[-114.51997,33.825381],[-114.523409,33.835323],[-114.525539,33.838614],[-114.529597,33.848063],[-114.529385,33.851755],[-114.528451,33.854929],[-114.526771,33.857357],[-114.52453,33.858477],[-114.516811,33.85812],[-114.514673,33.858638],[-114.505638,33.864276],[-114.503887,33.865754],[-114.503017,33.867998],[-114.503395,33.875018],[-114.50434,33.876882],[-114.516501,33.885926],[-114.518928,33.891714],[-114.517808,33.894889],[-114.516314,33.896196],[-114.508708,33.90064],[-114.507988,33.901813],[-114.50792,33.903807],[-114.508558,33.906098],[-114.511511,33.911092],[-114.518434,33.917518],[-114.525361,33.922272],[-114.533679,33.926072],[-114.534987,33.928499],[-114.535478,33.934651],[-114.52868,33.947817],[-114.522002,33.955623],[-114.51586,33.958106],[-114.511231,33.95704],[-114.509568,33.957264],[-114.499883,33.961789],[-114.495047,33.966835],[-114.484784,33.975519],[-114.481455,33.981261],[-114.475907,33.984424],[-114.471138,33.98804],[-114.467932,33.992877],[-114.462377,33.993781],[-114.46117,33.994687],[-114.460264,33.996649],[-114.460415,33.999215],[-114.46283,34.004497],[-114.463132,34.00661],[-114.46283,34.008421],[-114.46117,34.010081],[-114.458906,34.010835],[-114.454807,34.010968],[-114.450206,34.012574],[-114.443821,34.016176],[-114.44054,34.019329],[-114.438266,34.022609],[-114.436171,34.028083],[-114.434949,34.037784],[-114.435504,34.042615],[-114.438602,34.050205],[-114.439406,34.05381],[-114.43934,34.057893],[-114.437683,34.071937],[-114.435429,34.079727],[-114.434181,34.087379],[-114.428026,34.092787],[-114.426168,34.097042],[-114.420499,34.103466],[-114.415908,34.107636],[-114.411681,34.110031],[-114.405941,34.11154],[-114.401352,34.111652],[-114.390565,34.110084],[-114.379234,34.115988],[-114.369297,34.117517],[-114.366521,34.118575],[-114.360402,34.123577],[-114.356373,34.130429],[-114.353031,34.133121],[-114.348052,34.134458],[-114.336112,34.134035],[-114.324576,34.136759],[-114.320777,34.138635],[-114.312206,34.144776],[-114.292806,34.166725],[-114.287294,34.170529],[-114.275267,34.17215],[-114.268267,34.17021],[-114.254141,34.173831],[-114.244191,34.179625],[-114.240712,34.183232],[-114.229715,34.186928],[-114.227034,34.188866],[-114.224941,34.193896],[-114.225861,34.201774],[-114.225194,34.203642],[-114.211761,34.211539],[-114.208253,34.215505],[-114.190876,34.230858],[-114.17805,34.239969],[-114.176403,34.241512],[-114.173119,34.247226],[-114.166536,34.249647],[-114.164476,34.251667],[-114.161826,34.257038],[-114.159697,34.258242],[-114.153346,34.258289],[-114.147159,34.259564],[-114.139055,34.259538],[-114.136185,34.261296],[-114.134612,34.263518],[-114.134427,34.266387],[-114.137045,34.277018],[-114.13605,34.280833],[-114.138365,34.288564],[-114.139534,34.295844],[-114.138167,34.300936],[-114.138282,34.30323],[-114.14093,34.305919],[-114.157206,34.317862],[-114.168807,34.339513],[-114.176909,34.349306],[-114.185556,34.354386],[-114.191094,34.356125],[-114.199482,34.361373],[-114.213774,34.36246],[-114.226107,34.365916],[-114.229686,34.368908],[-114.234275,34.376662],[-114.245261,34.385659],[-114.252739,34.3901],[-114.264317,34.401329],[-114.267521,34.402486],[-114.280108,34.403147],[-114.286802,34.40534],[-114.288663,34.406623],[-114.291751,34.411104],[-114.292226,34.417606],[-114.294836,34.421389],[-114.301016,34.426807],[-114.312251,34.432726],[-114.319054,34.435831],[-114.32613,34.437251],[-114.330669,34.445295],[-114.335372,34.450038],[-114.339627,34.451435],[-114.342615,34.451442],[-114.356025,34.449744],[-114.363404,34.447773],[-114.373719,34.446938],[-114.375789,34.447798],[-114.378852,34.450376],[-114.386699,34.457911],[-114.387407,34.460492],[-114.387187,34.462021],[-114.381701,34.47604],[-114.383038,34.488903],[-114.382358,34.495757],[-114.378124,34.507288],[-114.378223,34.516521],[-114.380838,34.529724],[-114.389603,34.542982],[-114.405228,34.569637],[-114.422382,34.580711],[-114.429747,34.591734],[-114.43009,34.596874],[-114.424326,34.602338],[-114.424202,34.610453],[-114.428648,34.614641],[-114.438739,34.621455],[-114.441398,34.630171],[-114.440294,34.63824],[-114.441465,34.64253],[-114.444276,34.646542],[-114.449549,34.651423],[-114.451753,34.654321],[-114.452628,34.659573],[-114.451785,34.663891],[-114.451971,34.666795],[-114.454305,34.671234],[-114.456567,34.677956],[-114.462178,34.6858],[-114.465246,34.691202],[-114.46809,34.701786],[-114.46862,34.707573],[-114.470477,34.711368],[-114.47162,34.712966],[-114.473682,34.713964],[-114.481954,34.716036],[-114.486768,34.7191],[-114.490971,34.724848],[-114.495858,34.727956],[-114.510292,34.733582],[-114.516619,34.736745],[-114.529615,34.750822],[-114.540306,34.757109],[-114.552682,34.766871],[-114.558653,34.773852],[-114.57101,34.794294],[-114.574569,34.805746],[-114.576452,34.8153],[-114.581126,34.826115],[-114.586842,34.835672],[-114.592339,34.841153],[-114.600653,34.847361],[-114.619878,34.856873],[-114.623939,34.859738],[-114.630682,34.866352],[-114.635176,34.875003],[-114.636768,34.885705],[-114.636725,34.889107],[-114.635425,34.895192],[-114.630877,34.907263],[-114.630552,34.911852],[-114.633237,34.92123],[-114.633253,34.924608],[-114.632196,34.930628],[-114.629753,34.938684],[-114.629811,34.94481],[-114.631681,34.95131],[-114.634953,34.958918],[-114.635237,34.965149],[-114.634607,34.96906],[-114.629907,34.980791],[-114.629015,34.986148],[-114.62919,34.991887],[-114.629928,34.99474],[-114.633013,35.002085],[-114.636674,35.008807],[-114.638023,35.020556],[-114.636893,35.028367],[-114.632429,35.037586],[-114.627124,35.044721],[-114.606694,35.058941],[-114.603619,35.064226],[-114.602908,35.068588],[-114.604736,35.07483],[-114.613132,35.083097],[-114.622517,35.088703],[-114.642831,35.096503],[-114.646759,35.101872],[-114.644352,35.105904],[-114.629934,35.118272],[-114.619905,35.121632],[-114.59912,35.12105],[-114.58774,35.123729],[-114.578524,35.12875],[-114.572747,35.138725],[-114.569569,35.163053],[-114.569238,35.18348],[-114.572119,35.200591],[-114.574835,35.205898],[-114.579963,35.20964],[-114.583559,35.22993],[-114.583111,35.23809],[-114.587129,35.262376],[-114.597503,35.296954],[-114.595931,35.325234],[-114.604314,35.353584],[-114.611435,35.369056],[-114.627137,35.409504],[-114.652005,35.429165],[-114.662125,35.444241],[-114.6645,35.449497],[-114.666377,35.466856],[-114.672901,35.481708],[-114.677643,35.489742],[-114.679205,35.499992],[-114.677205,35.513491],[-114.673805,35.517891],[-114.663105,35.524491],[-114.658005,35.530491],[-114.656905,35.534391],[-114.657405,35.536391],[-114.660205,35.539291],[-114.662005,35.545491],[-114.663005,35.56369],[-114.666184,35.577576],[-114.665649,35.580428],[-114.659606,35.58749],[-114.654306,35.59759],[-114.653406,35.610789],[-114.658206,35.619089],[-114.677107,35.641489],[-114.689407,35.651412],[-114.690008,35.664688],[-114.682207,35.678188],[-114.680607,35.685488],[-114.683208,35.689387],[-114.694108,35.695187],[-114.701208,35.701187],[-114.705409,35.708287],[-114.705309,35.711587],[-114.697309,35.733686],[-114.695709,35.755986],[-114.701409,35.769086],[-114.69891,35.790185],[-114.71211,35.806185],[-114.70991,35.810185],[-114.70371,35.814585],[-114.69571,35.830601],[-114.699848,35.843283],[-114.699848,35.84837],[-114.697767,35.854844],[-114.68201,35.863284],[-114.679501,35.868023],[-114.67742,35.874728],[-114.68112,35.885364],[-114.700271,35.901772],[-114.708516,35.912313],[-114.707526,35.92806],[-114.715692,35.934709],[-114.729356,35.941413],[-114.731159,35.943916],[-114.728318,35.95629],[-114.729941,35.962183],[-114.740595,35.975656],[-114.743756,35.985095],[-114.742779,36.009963],[-114.740522,36.013336],[-114.731162,36.021862],[-114.729707,36.028166],[-114.730435,36.031317],[-114.734314,36.035681],[-114.739405,36.037863],[-114.740617,36.041015],[-114.740375,36.049258],[-114.736738,36.054349],[-114.736253,36.05847],[-114.743342,36.070535],[-114.754099,36.07944],[-114.755491,36.081601],[-114.755618,36.087166],[-114.753638,36.090705],[-114.747079,36.097005],[-114.736165,36.104367],[-114.717293,36.107686],[-114.709771,36.107742],[-114.666538,36.117343],[-114.66289,36.119932],[-114.65995,36.124145],[-114.631716,36.142306],[-114.627855,36.141012],[-114.621883,36.13213],[-114.616694,36.130101],[-114.608264,36.133949],[-114.597212,36.142103],[-114.572031,36.15161],[-114.545789,36.152248],[-114.511721,36.150956],[-114.506711,36.148277],[-114.504631,36.145629],[-114.506144,36.134659],[-114.505766,36.131444],[-114.504442,36.129741],[-114.502172,36.128796],[-114.49612,36.12785],[-114.487034,36.129396],[-114.470152,36.138801],[-114.463637,36.139695],[-114.458369,36.138586],[-114.453325,36.130726],[-114.448654,36.12641],[-114.446605,36.12597],[-114.427169,36.136305],[-114.41695,36.145761],[-114.412373,36.147254],[-114.405475,36.147371],[-114.372106,36.143114],[-114.363109,36.130246],[-114.337273,36.10802],[-114.328777,36.105501],[-114.30843,36.082443],[-114.305738,36.074882],[-114.307879,36.071291],[-114.314206,36.066619],[-114.316109,36.063109],[-114.315557,36.059494],[-114.314028,36.058165],[-114.280202,36.046362],[-114.270645,36.03572],[-114.266721,36.029238],[-114.263146,36.025937],[-114.252651,36.020193],[-114.238799,36.014561],[-114.233289,36.014289],[-114.21369,36.015613],[-114.19238,36.020993],[-114.176824,36.027651],[-114.166465,36.027738],[-114.15413,36.023862],[-114.151725,36.024563],[-114.148191,36.028013],[-114.138202,36.041284],[-114.137188,36.046785],[-114.138203,36.053161],[-114.136896,36.059467],[-114.114531,36.095217],[-114.114165,36.096982],[-114.117459,36.100893],[-114.123221,36.104746],[-114.123975,36.106515],[-114.123144,36.111576],[-114.120862,36.114596],[-114.111011,36.119875],[-114.103222,36.120176],[-114.09987,36.121654],[-114.088954,36.144381],[-114.068027,36.180663],[-114.060302,36.189363],[-114.046838,36.194069],[-114.046743,36.245246],[-114.048226,36.268874],[-114.048515,36.289598],[-114.046935,36.315449],[-114.047584,36.325573],[-114.045806,36.391071],[-114.045829,36.442973],[-114.046488,36.473449],[-114.048476,36.49998],[-114.04966,36.621113],[-114.050167,36.624978],[-114.050562,36.656259],[-114.050619,36.843128],[-114.049995,36.957769],[-114.0506,37.000396],[-112.538593,37.000674]]]},\"properties\":{\"name\":\"Arizona\",\"nation\":\"USA  \"}}]}","volume":"46","issue":"11","noUsgsAuthors":false,"publicationDate":"2010-11-11","publicationStatus":"PW","scienceBaseUri":"51b300e4e4b01368e589e3dd","contributors":{"authors":[{"text":"Keefe, Steffanie H. 0000-0002-3805-6101 shkeefe@usgs.gov","orcid":"https://orcid.org/0000-0002-3805-6101","contributorId":2843,"corporation":false,"usgs":true,"family":"Keefe","given":"Steffanie","email":"shkeefe@usgs.gov","middleInitial":"H.","affiliations":[{"id":37277,"text":"WMA - Earth System Processes Division","active":true,"usgs":true},{"id":5044,"text":"National Research Program - Central Branch","active":true,"usgs":true}],"preferred":true,"id":475278,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Daniels, Joan S. 0000-0002-7545-2402 joan_daniels@usgs.gov","orcid":"https://orcid.org/0000-0002-7545-2402","contributorId":2857,"corporation":false,"usgs":true,"family":"Daniels","given":"Joan","email":"joan_daniels@usgs.gov","middleInitial":"S.","affiliations":[{"id":291,"text":"Fort Collins Science Center","active":true,"usgs":true}],"preferred":true,"id":475279,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Runkel, Robert L. 0000-0003-3220-481X runkel@usgs.gov","orcid":"https://orcid.org/0000-0003-3220-481X","contributorId":685,"corporation":false,"usgs":true,"family":"Runkel","given":"Robert","email":"runkel@usgs.gov","middleInitial":"L.","affiliations":[{"id":191,"text":"Colorado Water Science Center","active":true,"usgs":true}],"preferred":true,"id":475276,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Wass, Roland D.","contributorId":72858,"corporation":false,"usgs":true,"family":"Wass","given":"Roland","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":475281,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Stiles, Eric A.","contributorId":8449,"corporation":false,"usgs":true,"family":"Stiles","given":"Eric","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":475280,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Barber, Larry B. 0000-0002-0561-0831 lbbarber@usgs.gov","orcid":"https://orcid.org/0000-0002-0561-0831","contributorId":921,"corporation":false,"usgs":true,"family":"Barber","given":"Larry","email":"lbbarber@usgs.gov","middleInitial":"B.","affiliations":[{"id":438,"text":"National Research Program - Western Branch","active":true,"usgs":true},{"id":5044,"text":"National Research Program - Central Branch","active":true,"usgs":true}],"preferred":true,"id":475277,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}}
]}