{"pageNumber":"666","pageRowStart":"16625","pageSize":"25","recordCount":68919,"records":[{"id":70039301,"text":"70039301 - 2012 - Volatile organic compounds in the unsaturated zone from radioactive wastes","interactions":[],"lastModifiedDate":"2018-01-24T14:21:20","indexId":"70039301","displayToPublicDate":"2012-08-08T00:00:00","publicationYear":"2012","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2262,"text":"Journal of Environmental Quality","active":true,"publicationSubtype":{"id":10}},"title":"Volatile organic compounds in the unsaturated zone from radioactive wastes","docAbstract":"Volatile organic compounds (VOCs) are often comingled with low-level radioactive wastes (LLRW), but little is known about subsurface VOC emanations from LLRW landfills. The current study systematically quantified VOCs associated with LLRW over an 11-yr period at the USGS Amargosa Desert Research Site (ADRS) in southwestern Nevada. Unsaturated-zone gas samples of VOCs were collected by adsorption on resin cartridges and analyzed by thermal desorption and GC/MS. Sixty of 87 VOC method analytes were detected in the 110-m-thick unsaturated zone surrounding a LLRW disposal facility. Chlorofluorocarbons (CFCs) were detected in 100% of samples collected. Chlorofluorocarbons are powerful greenhouse gases, deplete stratospheric ozone, and are likely released from LLRW facilities worldwide. Soil-gas samples collected from a depth of 24 m and a horizontal distance 100 m south of the nearest waste-disposal trench contained >60,000 ppbv total VOCs, including >37,000 ppbv CFCs. Extensive sampling in the shallow unsaturated zone (0&ndash;2 m deep) identified areas where total VOC concentrations exceeded 5000 ppbv at the 1.5-m depth. Volatile organic compound concentrations exceeded background levels up to 300 m from the facility. Maximum vertical diffusive fluxes of total VOCs were estimated to be 1 g m<sup>-2</sup> yr<sup>-1</sup>. Volatile organic compound distributions were similar but not identical to those previously determined for tritium and elemental mercury. To our knowledge, this study is the first to characterize the unsaturated zone distribution of VOCs emanating from a LLRW landfill. Our results may help explain anomalous transport of radionuclides at the ADRS and elsewhere.","language":"English","publisher":"American Society of Agronomy","publisherLocation":"Madison, WI","doi":"10.2134/jeq2011.0480","usgsCitation":"Baker, R.J., Andraski, B.J., Stonestrom, D.A., and Luo, W., 2012, Volatile organic compounds in the unsaturated zone from radioactive wastes: Journal of Environmental Quality, v. 41, no. 4, p. 1324-1336, https://doi.org/10.2134/jeq2011.0480.","productDescription":"13 p.","startPage":"1324","endPage":"1336","costCenters":[{"id":470,"text":"New Jersey Water Science Center","active":true,"usgs":true}],"links":[{"id":259515,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.2134/jeq2011.0480","linkFileType":{"id":5,"text":"html"}},{"id":259516,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Nevada","otherGeospatial":"Amargosa Desert Research Site","volume":"41","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505bc2c8e4b08c986b32ad6c","contributors":{"authors":[{"text":"Baker, Ronald J. rbaker@usgs.gov","contributorId":1436,"corporation":false,"usgs":true,"family":"Baker","given":"Ronald","email":"rbaker@usgs.gov","middleInitial":"J.","affiliations":[{"id":470,"text":"New Jersey Water Science Center","active":true,"usgs":true}],"preferred":true,"id":466004,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Andraski, Brian J. 0000-0002-2086-0417 andraski@usgs.gov","orcid":"https://orcid.org/0000-0002-2086-0417","contributorId":168800,"corporation":false,"usgs":true,"family":"Andraski","given":"Brian","email":"andraski@usgs.gov","middleInitial":"J.","affiliations":[{"id":465,"text":"Nevada Water Science Center","active":true,"usgs":true},{"id":38175,"text":"Toxics Substances Hydrology Program","active":true,"usgs":true},{"id":438,"text":"National Research Program - Western Branch","active":true,"usgs":true}],"preferred":false,"id":466003,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Stonestrom, David A. 0000-0001-7883-3385 dastones@usgs.gov","orcid":"https://orcid.org/0000-0001-7883-3385","contributorId":2280,"corporation":false,"usgs":true,"family":"Stonestrom","given":"David","email":"dastones@usgs.gov","middleInitial":"A.","affiliations":[{"id":438,"text":"National Research Program - Western Branch","active":true,"usgs":true}],"preferred":true,"id":466005,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Luo, Wentai","contributorId":7551,"corporation":false,"usgs":true,"family":"Luo","given":"Wentai","affiliations":[],"preferred":false,"id":466006,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70039482,"text":"sim3220 - 2012 - Flood-inundation maps for Sweetwater Creek from above the confluence of Powder Springs Creek to the Interstate 20 bridge, Cobb and Douglas Counties, Georgia","interactions":[],"lastModifiedDate":"2017-01-31T08:37:59","indexId":"sim3220","displayToPublicDate":"2012-08-07T00:00:00","publicationYear":"2012","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":333,"text":"Scientific Investigations Map","code":"SIM","onlineIssn":"2329-132X","printIssn":"2329-1311","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"3220","title":"Flood-inundation maps for Sweetwater Creek from above the confluence of Powder Springs Creek to the Interstate 20 bridge, Cobb and Douglas Counties, Georgia","docAbstract":"Digital flood-inundation maps for a 10.5-mile reach of Sweetwater Creek, from about 1,800 feet above the confluence of Powder Springs Creek to about 160 feet below the Interstate 20 bridge, were developed by the U.S. Geological Survey (USGS) in cooperation with Cobb County, Georgia. The inundation maps, which can be accessed through the USGS Flood Inundation Mapping Science Web site at http://water.usgs.gov/osw/flood_inundation/, depict estimates of the areal extent and depth of flooding corresponding to selected water levels (stages) at the USGS streamgage at Sweetwater Creek near Austell, Georgia (02337000). Current stage at this USGS streamgage may be obtained at http://waterdata.usgs.gov/ and can be used in conjunction with these maps to estimate near real-time areas of inundation. The National Weather Service (NWS) is incorporating results from this study into the Advanced Hydrologic Prediction Service (AHPS) flood-warning system (http://water.weather.gov/ahps/). The NWS forecasts flood hydrographs at many places that commonly are collocated at USGS streamgages. The forecasted peak-stage information for the USGS streamgage at Sweetwater Creek near Austell (02337000), which is available through the AHPS Web site, may be used in conjunction with the maps developed in this study to show predicted areas of flood inundation. A one-dimensional step-backwater model was developed using the U.S. Army Corps of Engineers Hydrologic Engineering Centers River Analysis System (HEC&ndash;RAS) software for Sweetwater Creek and was used to compute flood profiles for a 10.5-mile reach of the creek. The model was calibrated using the most current stage-discharge relations at the Sweetwater Creek near Austell streamgage (02337000), as well as high-water marks collected during annual peak-flow events in 1982 and 2009. The hydraulic model was then used to determine 21 water-surface profiles for flood stages at the Sweetwater Creek streamgage at 1-foot intervals referenced to the streamgage datum and ranging from just above bankfull stage (12.0 feet) to approximately 1.2 feet above the highest recorded water level at the streamgage (32.0 feet). The simulated water-surface profiles were then combined with a geographic information system digital elevation model&mdash;derived from contour data (8-foot horizontal resolution), in Cobb County, and USGS National Elevation Dataset (31-foot horizontal resolution), in Douglas County&mdash;to delineate the area flooded for each 1-foot increment of stream stage. The availability of these maps, when combined with real-time information regarding current stage from USGS streamgages and forecasted stream stages from the NWS, provides emergency management personnel and residents with critical information during flood-response activities, such as evacuations and road closures, as well as for post-flood recovery efforts.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/sim3220","collaboration":"Prepared in cooperation with Cobb County, Georgia","usgsCitation":"Musser, J.W., 2012, Flood-inundation maps for Sweetwater Creek from above the confluence of Powder Springs Creek to the Interstate 20 bridge, Cobb and Douglas Counties, Georgia: U.S. Geological Survey Scientific Investigations Map 3220, v, 10 p.; maps (col.); PDF and JPG Downloads of Sheets 1-21: 27 x 36 inches; Downloads Directory, https://doi.org/10.3133/sim3220.","productDescription":"v, 10 p.; maps (col.); PDF and JPG Downloads of 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,{"id":70039463,"text":"ofr20121161 - 2012 - Modeling of depth to base of Last Glacial Maximum and seafloor sediment thickness for the California State Waters Map Series, eastern Santa Barbara Channel, California","interactions":[],"lastModifiedDate":"2012-08-09T01:02:14","indexId":"ofr20121161","displayToPublicDate":"2012-08-07T00:00:00","publicationYear":"2012","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2012-1161","title":"Modeling of depth to base of Last Glacial Maximum and seafloor sediment thickness for the California State Waters Map Series, eastern Santa Barbara Channel, California","docAbstract":"Models of the depth to the base of Last Glacial Maximum and sediment thickness over the base of Last Glacial Maximum for the eastern Santa Barbara Channel are a key part of the maps of shallow subsurface geology and structure for offshore Refugio to Hueneme Canyon, California, in the California State Waters Map Series. A satisfactory interpolation of the two datasets that accounted for regional geologic structure was developed using geographic information systems modeling and graphics software tools. Regional sediment volumes were determined from the model. Source data files suitable for geographic information systems mapping applications are provided.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr20121161","usgsCitation":"Wong, F.L., Phillips, E., Johnson, S.Y., and Sliter, R.W., 2012, Modeling of depth to base of Last Glacial Maximum and seafloor sediment thickness for the California State Waters Map Series, eastern Santa Barbara Channel, California: U.S. Geological Survey Open-File Report 2012-1161, v, 16 p.; col. ill.; maps col.; GIS Data, https://doi.org/10.3133/ofr20121161.","productDescription":"v, 16 p.; col. ill.; maps col.; GIS Data","startPage":"i","endPage":"16","numberOfPages":"21","onlineOnly":"Y","additionalOnlineFiles":"Y","costCenters":[{"id":520,"text":"Pacific Coastal and Marine Science Center","active":true,"usgs":true}],"links":[{"id":259488,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ofr_2012_1161.gif"},{"id":259476,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2012/1161/","linkFileType":{"id":5,"text":"html"}},{"id":259477,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/2012/1161/of2012-1161.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"California","otherGeospatial":"Santa Barbara Channel","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -120.206232,34.027787 ], [ -120.206232,34.492447 ], [ -119.123028,34.492447 ], [ -119.123028,34.027787 ], [ -120.206232,34.027787 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a5c12e4b0c8380cd6f9eb","contributors":{"authors":[{"text":"Wong, Florence L. 0000-0002-3918-5896 fwong@usgs.gov","orcid":"https://orcid.org/0000-0002-3918-5896","contributorId":1990,"corporation":false,"usgs":true,"family":"Wong","given":"Florence","email":"fwong@usgs.gov","middleInitial":"L.","affiliations":[{"id":520,"text":"Pacific Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":true,"id":466291,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Phillips, Eleyne L.","contributorId":104289,"corporation":false,"usgs":true,"family":"Phillips","given":"Eleyne L.","affiliations":[],"preferred":false,"id":466294,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Johnson, Samuel Y. 0000-0001-7972-9977 sjohnson@usgs.gov","orcid":"https://orcid.org/0000-0001-7972-9977","contributorId":2607,"corporation":false,"usgs":true,"family":"Johnson","given":"Samuel","email":"sjohnson@usgs.gov","middleInitial":"Y.","affiliations":[{"id":520,"text":"Pacific Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":true,"id":466293,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Sliter, Ray W. 0000-0003-0337-3454 rsliter@usgs.gov","orcid":"https://orcid.org/0000-0003-0337-3454","contributorId":1992,"corporation":false,"usgs":true,"family":"Sliter","given":"Ray","email":"rsliter@usgs.gov","middleInitial":"W.","affiliations":[{"id":520,"text":"Pacific Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":true,"id":466292,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70039462,"text":"ofr20121091 - 2012 - Global prediction of continuous hydrocarbon accumulations in self-sourced reservoirs","interactions":[],"lastModifiedDate":"2012-08-08T01:02:14","indexId":"ofr20121091","displayToPublicDate":"2012-08-07T00:00:00","publicationYear":"2012","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2012-1091","title":"Global prediction of continuous hydrocarbon accumulations in self-sourced reservoirs","docAbstract":"This report was first presented as an abstract in poster format at the American Association of Petroleum Geologists (AAPG) 2012 Annual Convention and Exhibition, April 22-25, Long Beach, Calif., as Search and Discovery Article no. 90142. Shale resource plays occur in predictable tectonic settings within similar orders of magnitude of eustatic events. A conceptual model for predicting the presence of resource-quality shales is essential for evaluating components of continuous petroleum systems. Basin geometry often distinguishes self-sourced resource plays from conventional plays. Intracratonic or intrashelf foreland basins at active margins are the predominant depositional settings among those explored for the development of self-sourced continuous accumulations, whereas source rocks associated with conventional accumulations typically were deposited in rifted passive margin settings (or other cratonic environments). Generally, the former are associated with the assembly of supercontinents, and the latter often resulted during or subsequent to the breakup of landmasses. Spreading rates, climate, and eustasy are influenced by these global tectonic events, such that deposition of self-sourced reservoirs occurred during periods characterized by rapid plate reconfiguration, predominantly greenhouse climate conditions, and in areas adjacent to extensive carbonate sedimentation. Combined tectonic histories, eustatic curves, and paleogeographic reconstructions may be useful in global predictions of organic-rich shale accumulations suitable for continuous resource development. Accumulation of marine organic material is attributed to upwellings that enhance productivity and oxygen-minimum bottom waters that prevent destruction of organic matter. The accumulation of potential self-sourced resources can be attributed to slow sedimentation rates in rapidly subsiding (incipient, flexural) foreland basins, while flooding of adjacent carbonate platforms and other cratonic highs occurred. In contrast, deposition of this resource type on rifted passive margins was likely the result of reactivation of long-lived cratonic features or salt tectonic regimes that created semi-confined basins. Commonly, loading by thick sections of clastic material, following thermal relaxation after plate collision or rift phases, advances kerogen maturation. With few exceptions, North American self-sourced reservoirs appear to be associated with calcitic seas and predominantly greenhouse or transitional (\"warm\" to \"cool\") global climatic conditions. Significant changes to the global carbon budget may also be a contributing factor in the stratigraphic distribution of continuous resource plays, requiring additional evaluation.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr20121091","usgsCitation":"Eoff, J.D., 2012, Global prediction of continuous hydrocarbon accumulations in self-sourced reservoirs: U.S. Geological Survey Open-File Report 2012-1091, 4 Sheets: 61 x 37 inches; maps (col.), https://doi.org/10.3133/ofr20121091.","productDescription":"4 Sheets: 61 x 37 inches; maps (col.)","numberOfPages":"4","onlineOnly":"Y","additionalOnlineFiles":"Y","costCenters":[{"id":164,"text":"Central Energy Resources Science Center","active":true,"usgs":true}],"links":[{"id":259466,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ofr_2012_1091.png"},{"id":259454,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2012/1091/","linkFileType":{"id":5,"text":"html"}}],"otherGeospatial":"Earth","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a295ae4b0c8380cd5a8b3","contributors":{"authors":[{"text":"Eoff, Jennifer D. jeoff@usgs.gov","contributorId":3418,"corporation":false,"usgs":true,"family":"Eoff","given":"Jennifer","email":"jeoff@usgs.gov","middleInitial":"D.","affiliations":[{"id":164,"text":"Central Energy Resources Science Center","active":true,"usgs":true}],"preferred":true,"id":466290,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70039477,"text":"ofr20121004 - 2012 - Sea-floor geology in central Rhode Island Sound south of Sakonnet Point, Rhode Island","interactions":[],"lastModifiedDate":"2012-08-08T01:02:14","indexId":"ofr20121004","displayToPublicDate":"2012-08-07T00:00:00","publicationYear":"2012","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2012-1004","title":"Sea-floor geology in central Rhode Island Sound south of Sakonnet Point, Rhode Island","docAbstract":"The U.S. Geological Survey (USGS) and the National Oceanic and Atmospheric Administration (NOAA) are working together to study the sea floor along the northeastern coast of the United States. NOAA collected multibeam-echosounder data during hydrographic survey H11995 in a 63-square-kilometer area in central Rhode Island Sound, south of Sakonnet Point, Rhode Island. The USGS collected sediment samples, bottom video, and still photographs from 27 stations in this study area to verify an interpretation of the bathymetric data. Collected data are used to map areas of scour depressions and erosional outliers, megaripples, boulders, and relatively undisturbed modern marine sediments. In general, much of the eastern part of the study area, a submerged segment of the Harbor Hill-Roanoke Point-Charlestown-Buzzards Bay moraine, is bouldery. Bottom photography shows boulders are generally encrusted with hydrozoans, algae, and anemone. Scour depressions, presumably formed by long-period storm waves, and erosional outliers of Holocene sediments dominate the western part of the study area and several large areas in the east. The scour depressions tend to have coarser grained sediment than intervening erosional outliers. The coarseness likely creates turbulence in the water over these areas, which prevents fine-grained sediment deposition. Several small areas of megaripples are visible in the bathymetry data in the west. Other sandy areas are typically rippled, with burrows, worm tubes, and starfish present.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr20121004","usgsCitation":"McMullen, K., Poppe, L., Ackerman, S., Worley, C., Nadeau, M., and Van Hoy, M.V., 2012, Sea-floor geology in central Rhode Island Sound south of Sakonnet Point, Rhode Island: U.S. Geological Survey Open-File Report 2012-1004, HTML Document, https://doi.org/10.3133/ofr20121004.","productDescription":"HTML Document","onlineOnly":"N","additionalOnlineFiles":"Y","costCenters":[{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"links":[{"id":259471,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ofr_2012_1004.png"},{"id":259459,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2012/1004/","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Rhode Island","otherGeospatial":"Rhode Island Sound","geographicExtents":"{\"crs\": {\"type\": \"name\", \"properties\": {\"name\": \"urn:ogc:def:crs:OGC:1.3:CRS84\"}}, \"geometry\": {\"type\": \"Polygon\", \"coordinates\": [[[-71.26580619466932, 41.297435949285784], [-71.19556111567424, 41.31782968189743], [-71.11867998082937, 41.335957444218685], [-71.11867998082937, 41.332558488783526], [-71.12709644190716, 41.31572556662802], [-71.12062224107808, 41.31410701642072], [-71.09553471286557, 41.29792151434809], [-71.24152794156043, 41.25389694871062], [-71.26580619466932, 41.297435949285784]]]}, \"properties\": {\"extentType\": \"Custom\", \"code\": \"\", \"name\": \"\", \"notes\": \"\", \"promotedForReuse\": false, \"abbreviation\": \"\", \"shortName\": \"\", \"description\": \"\"}, \"bbox\": [-71.26580619466932, 41.25389694871062, -71.09553471286557, 41.335957444218685], \"type\": \"Feature\", \"id\": \"3091970\"}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505b8808e4b08c986b31679d","contributors":{"authors":[{"text":"McMullen, K.Y.","contributorId":51857,"corporation":false,"usgs":true,"family":"McMullen","given":"K.Y.","email":"","affiliations":[],"preferred":false,"id":466322,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Poppe, L.J.","contributorId":72782,"corporation":false,"usgs":true,"family":"Poppe","given":"L.J.","affiliations":[],"preferred":false,"id":466324,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Ackerman, S.D.","contributorId":88843,"corporation":false,"usgs":true,"family":"Ackerman","given":"S.D.","email":"","affiliations":[],"preferred":false,"id":466325,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Worley, C.R.","contributorId":43479,"corporation":false,"usgs":true,"family":"Worley","given":"C.R.","email":"","affiliations":[],"preferred":false,"id":466320,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Nadeau, M.A.","contributorId":47901,"corporation":false,"usgs":true,"family":"Nadeau","given":"M.A.","email":"","affiliations":[],"preferred":false,"id":466321,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Van Hoy, M. V.","contributorId":69406,"corporation":false,"usgs":true,"family":"Van Hoy","given":"M.","email":"","middleInitial":"V.","affiliations":[],"preferred":false,"id":466323,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}}
,{"id":70039465,"text":"tm10C19 - 2012 - Determination of the &delta;<sup>2</sup>H and &delta;<sup>18</sup>O of soil water and water in plant matter; RSIL lab code 1700","interactions":[],"lastModifiedDate":"2012-08-08T01:02:14","indexId":"tm10C19","displayToPublicDate":"2012-08-06T10:15:30","publicationYear":"2012","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":335,"text":"Techniques and Methods","code":"TM","onlineIssn":"2328-7055","printIssn":"2328-7047","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"10-C19","title":"Determination of the &delta;<sup>2</sup>H and &delta;<sup>18</sup>O of soil water and water in plant matter; RSIL lab code 1700","docAbstract":"The purpose of the Reston Stable Isotope Laboratory lab code 1700 is to determine the &delta;<sup>2</sup>H/<sup>1</sup>H), abbreviated as &delta;<sup>2</sup>H, and the &delta;<sup>18</sup>O/<sup>16</sup>O), abbreviated as &delta;<sup>18</sup>O, of soil water and water in plant matter. This method is based on the observation that water and toluene form an azeotropic mixture at 84.1 &deg;C. This temperature is substantially lower than the boiling points of water (100 &deg;C) and toluene (110 &deg;C), but water and toluene are immiscible at ambient temperature. The water content of a soil or plant is determined by weighing, drying, and reweighing a small amount of sample. Sufficient sample to collect 3 to 5 milliliters of water after distillation is loaded into a distillation flask. Sufficient toluene is added so that the sample is immersed throughout the entire distillation to minimize evaporation of water, which would affect the &delta;<sup>2</sup>H and &delta;<sup>18</sup>O values. The mixture of sample and toluene is heated in a flask to its boiling point (84.1 &deg;C) so that water from the sample and toluene can distill together into a specially designed collection funnel. The temperature of 84.1 &deg;C is maintained until the water has been quantitatively transferred to the collection funnel, at which time the temperature is raised to the boiling point of the remaining component (toluene, 110 &deg;C). The collection funnel is maintained at ambient temperature so that the sample water and toluene can be separated physically. After separation, the sample water is purified by addition of paraffin wax to the container with the sample water, capping the container, and heating to approximately 60 &deg;C to melt the wax. Trace amounts of toluene will dissolve in the wax, purifying the sample water for isotopic analysis. The isotopic composition of the purified water is then determined by equilibration with gaseous hydrogen or carbon dioxide, followed by dual-inlet isotope-ratio mass spectrometry. Because laser-absorption spectrometry is sensitive to organic compounds, such as trace toluene remaining in water samples, water samples should be analyzed for isotopic composition only by mass spectrometry and not by laser-absorption spectrometry.","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Stable Isotope Ratio Methods","largerWorkSubtype":{"id":9,"text":"Other Report"},"language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/tm10C19","usgsCitation":"Revesz, K.M., Buck, B., and Coplen, T.B., 2012, Determination of the &delta;<sup>2</sup>H and &delta;<sup>18</sup>O of soil water and water in plant matter; RSIL lab code 1700: U.S. Geological Survey Techniques and Methods 10-C19, vii, 21 p.; ill.; Appendices, https://doi.org/10.3133/tm10C19.","productDescription":"vii, 21 p.; ill.; Appendices","numberOfPages":"30","onlineOnly":"Y","additionalOnlineFiles":"N","costCenters":[{"id":543,"text":"Reston Stable Isotope Laboratory","active":false,"usgs":true}],"links":[{"id":259467,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/tm_10_C19.gif"},{"id":259452,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/tm/10c19/TM10-C19.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":259453,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/tm/10c19/","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059ffd0e4b0c8380cd4f3ee","contributors":{"authors":[{"text":"Revesz, Kinga M. krevesz@usgs.gov","contributorId":506,"corporation":false,"usgs":true,"family":"Revesz","given":"Kinga","email":"krevesz@usgs.gov","middleInitial":"M.","affiliations":[],"preferred":true,"id":466298,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Buck, Bryan bbuck@usgs.gov","contributorId":2326,"corporation":false,"usgs":true,"family":"Buck","given":"Bryan","email":"bbuck@usgs.gov","affiliations":[{"id":436,"text":"National Research Program - Eastern Branch","active":true,"usgs":true}],"preferred":true,"id":466300,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Coplen, Tyler B. 0000-0003-4884-6008 tbcoplen@usgs.gov","orcid":"https://orcid.org/0000-0003-4884-6008","contributorId":508,"corporation":false,"usgs":true,"family":"Coplen","given":"Tyler","email":"tbcoplen@usgs.gov","middleInitial":"B.","affiliations":[{"id":27111,"text":"National Water Quality Program","active":true,"usgs":true},{"id":436,"text":"National Research Program - Eastern Branch","active":true,"usgs":true},{"id":37277,"text":"WMA - Earth System Processes Division","active":true,"usgs":true},{"id":37464,"text":"WMA - Laboratory & Analytical Services Division","active":true,"usgs":true}],"preferred":true,"id":466299,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70039424,"text":"sir20125141 - 2012 - Estimates of tracer-based piston-flow ages of groundwater from selected sites: National Water-Quality Assessment Program, 2006-2010","interactions":[],"lastModifiedDate":"2018-03-21T15:12:18","indexId":"sir20125141","displayToPublicDate":"2012-08-04T00:00:00","publicationYear":"2012","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":334,"text":"Scientific Investigations Report","code":"SIR","onlineIssn":"2328-0328","printIssn":"2328-031X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2012-5141","title":"Estimates of tracer-based piston-flow ages of groundwater from selected sites: National Water-Quality Assessment Program, 2006-2010","docAbstract":"Piston-flow age dates were interpreted from measured concentrations of environmental tracers from 812 National Water-Quality Assessment (NAWQA) Program groundwater sites from 27 Study Units across the United States. The tracers of interest include chlorofluorocarbons (CFCs), sulfur hexafluoride (SF<sub>6</sub>), and tritium/helium-3 (<sup>3</sup>H/<sup>3</sup>He). Tracer data compiled for this analysis were collected from 2006 to 2010 from groundwater wells in NAWQA studies, including: * Land-Use Studies (LUS, shallow wells, usually monitoring wells, located in recharge areas under dominant land-use settings), * Major-Aquifer Studies (MAS, wells, usually domestic supply wells, located in principal aquifers and representing the shallow drinking water supply), * Flow System Studies (FSS, networks of clustered wells located along a flowpath extending from a recharge zone to a discharge zone, preferably a shallow stream) associated with Land-Use Studies, and * Reference wells (wells representing groundwater minimally impacted by anthropogenic activities) also associated with Land-Use Studies. Tracer data were evaluated using documented methods and are presented as aqueous concentrations, equivalent atmospheric concentrations (for CFCs and SF<sub>6</sub>), and tracer-based piston-flow ages. Selected ancillary data, such as redox data, well-construction data, and major dissolved-gas (N<sub>2</sub>, O<sub>2</sub>, Ar, CH<sub>4</sub>, and CO<sub>2</sub>) data, also are presented. Recharge temperature was inferred using climate data (approximated by mean annual air temperature plus 1&deg;C [MAAT +1&deg;C]) as well as major dissolved-gas data (N<sub>2</sub>-Ar-based) where available. The N<sub>2</sub>-Ar-based temperatures showed significantly more variation than the climate-based data, as well as the effects of denitrification and degassing resulting from reducing conditions. The N<sub>2</sub>-Ar-based temperatures were colder than the climate-based temperatures in networks where recharge was limited to the winter months when evapotranspiration was reduced.  The tracer-based piston-flow ages compiled in this report are provided as a consistent means of reporting the tracer data. The tracer-based piston-flow ages may provide an initial interpretation of age in cases in which mixing is minimal and may aid in developing a basic conceptualization of groundwater age in an aquifer. These interpretations are based on the assumption that tracer transport is by advection only and that no mixing occurs. In addition, it is assumed that other uncertainties are minimized, including tracer degradation, sorption, contamination, or fractionation, and that terrigenic (natural) sources of tracers, and spatially variable atmospheric tracer concentrations are constrained.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/sir20125141","collaboration":"National Water Quality Assessment Program","usgsCitation":"Shapiro, S., Plummer, N., Busenberg, E., Widman, P.K., Casile, G.C., Wayland, J.E., and Runkle, D.L., 2012, Estimates of tracer-based piston-flow ages of groundwater from selected sites: National Water-Quality Assessment Program, 2006-2010: U.S. Geological Survey Scientific Investigations Report 2012-5141, Title Page; Table of Contents; List of Figures; List of Tables; PDF: viii, 100 p.; Table 1 XLS; Table A1 XLS; Appendix B PDF; Appendix B Tables XLS ZIP, https://doi.org/10.3133/sir20125141.","productDescription":"Title Page; Table of Contents; List of Figures; List of Tables; PDF: viii, 100 p.; Table 1 XLS; Table A1 XLS; Appendix B PDF; Appendix B Tables XLS ZIP","numberOfPages":"112","onlineOnly":"Y","costCenters":[{"id":451,"text":"National Water Quality Assessment Program","active":true,"usgs":true}],"links":[{"id":259437,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/sir_2012_5141.jpg"},{"id":259434,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/sir/2012/5141/","linkFileType":{"id":5,"text":"html"}},{"id":259435,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/sir/2012/5141/pdf/sir20125141.pdf","linkFileType":{"id":1,"text":"pdf"}}],"projection":"Albers Equal-Area Conic","datum":"North American Datum 1983","country":"United States","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -124.8,24.5 ], [ -124.8,49.38333333333333 ], [ -66.95,49.38333333333333 ], [ -66.95,24.5 ], [ -124.8,24.5 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a0af5e4b0c8380cd524db","contributors":{"authors":[{"text":"Shapiro, Stephanie D.","contributorId":29350,"corporation":false,"usgs":true,"family":"Shapiro","given":"Stephanie D.","affiliations":[],"preferred":false,"id":466222,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Plummer, Niel 0000-0002-4020-1013 nplummer@usgs.gov","orcid":"https://orcid.org/0000-0002-4020-1013","contributorId":190100,"corporation":false,"usgs":true,"family":"Plummer","given":"Niel","email":"nplummer@usgs.gov","affiliations":[{"id":436,"text":"National Research Program - Eastern Branch","active":true,"usgs":true}],"preferred":true,"id":466221,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Busenberg, Eurybiades ebusenbe@usgs.gov","contributorId":2271,"corporation":false,"usgs":true,"family":"Busenberg","given":"Eurybiades","email":"ebusenbe@usgs.gov","affiliations":[{"id":436,"text":"National Research Program - Eastern Branch","active":true,"usgs":true}],"preferred":true,"id":466216,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Widman, Peggy K. pkwidman@usgs.gov","contributorId":4009,"corporation":false,"usgs":true,"family":"Widman","given":"Peggy","email":"pkwidman@usgs.gov","middleInitial":"K.","affiliations":[{"id":436,"text":"National Research Program - Eastern Branch","active":true,"usgs":true}],"preferred":true,"id":466220,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Casile, Gerolamo C. jcasile@usgs.gov","contributorId":4007,"corporation":false,"usgs":true,"family":"Casile","given":"Gerolamo","email":"jcasile@usgs.gov","middleInitial":"C.","affiliations":[{"id":436,"text":"National Research Program - Eastern Branch","active":true,"usgs":true}],"preferred":true,"id":466218,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Wayland, Julian E. jwayland@usgs.gov","contributorId":4008,"corporation":false,"usgs":true,"family":"Wayland","given":"Julian","email":"jwayland@usgs.gov","middleInitial":"E.","affiliations":[{"id":436,"text":"National Research Program - Eastern Branch","active":true,"usgs":true}],"preferred":true,"id":466219,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Runkle, Donna L. dlrunkle@usgs.gov","contributorId":2556,"corporation":false,"usgs":true,"family":"Runkle","given":"Donna","email":"dlrunkle@usgs.gov","middleInitial":"L.","affiliations":[],"preferred":true,"id":466217,"contributorType":{"id":1,"text":"Authors"},"rank":7}]}}
,{"id":70133843,"text":"70133843 - 2012 - Regression modeling of particle size distributions in urban stormwater: Advancements through improved sample collection methods","interactions":[],"lastModifiedDate":"2021-02-04T18:42:02.643375","indexId":"70133843","displayToPublicDate":"2012-08-03T12:41:39","publicationYear":"2012","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2255,"text":"Journal of Environmental Engineering","active":true,"publicationSubtype":{"id":10}},"title":"Regression modeling of particle size distributions in urban stormwater: Advancements through improved sample collection methods","docAbstract":"<div class=\"NLM_sec NLM_sec_level_1 hlFld-Abstract\"><p>A new sample collection system was developed to improve the representation of sediment entrained in urban storm water by integrating water quality samples from the entire water column. The depth-integrated sampler arm (DISA) was able to mitigate sediment stratification bias in storm water, thereby improving the characterization of suspended-sediment concentration and particle size distribution at three independent study locations. Use of the DISA decreased variability, which improved statistical regression to predict particle size distribution using surrogate environmental parameters, such as precipitation depth and intensity. The performance of this statistical modeling technique was compared to results using traditional fixed-point sampling methods and was found to perform better. When environmental parameters can be used to predict particle size distributions, environmental managers have more options when characterizing concentrations, loads, and particle size distributions in urban runoff.</p></div>","language":"English","publisher":"ASCE","doi":"10.1061/(ASCE)EE.1943-7870.0000612","usgsCitation":"Selbig, W.R., and Fienen, M., 2012, Regression modeling of particle size distributions in urban stormwater: Advancements through improved sample collection methods: Journal of Environmental Engineering, v. 138, no. 12, p. 1186-1193, https://doi.org/10.1061/(ASCE)EE.1943-7870.0000612.","productDescription":"8 p.","startPage":"1186","endPage":"1193","ipdsId":"IP-027539","costCenters":[{"id":677,"text":"Wisconsin Water Science Center","active":true,"usgs":true}],"links":[{"id":383023,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Wisconsin","city":"Madison","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -89.63470458984375,\n              42.96044267380142\n            ],\n            [\n              -89.20623779296875,\n              42.96044267380142\n            ],\n            [\n              -89.20623779296875,\n              43.18114705939968\n            ],\n            [\n              -89.63470458984375,\n              43.18114705939968\n            ],\n            [\n              -89.63470458984375,\n              42.96044267380142\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"138","issue":"12","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"546dbf2be4b0fc7976bf1e5e","contributors":{"authors":[{"text":"Selbig, William R. 0000-0003-1403-8280 wrselbig@usgs.gov","orcid":"https://orcid.org/0000-0003-1403-8280","contributorId":877,"corporation":false,"usgs":true,"family":"Selbig","given":"William","email":"wrselbig@usgs.gov","middleInitial":"R.","affiliations":[{"id":37947,"text":"Upper Midwest Water Science Center","active":true,"usgs":true}],"preferred":true,"id":525481,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Fienen, Michael N. 0000-0002-7756-4651 mnfienen@usgs.gov","orcid":"https://orcid.org/0000-0002-7756-4651","contributorId":893,"corporation":false,"usgs":true,"family":"Fienen","given":"Michael N.","email":"mnfienen@usgs.gov","affiliations":[{"id":677,"text":"Wisconsin Water Science Center","active":true,"usgs":true}],"preferred":false,"id":525480,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70039425,"text":"sir20125132 - 2012 - Simulation of climate change in San Francisco Bay Basins, California: Case studies in the Russian River Valley and Santa Cruz Mountains","interactions":[],"lastModifiedDate":"2012-08-28T15:40:09","indexId":"sir20125132","displayToPublicDate":"2012-08-03T00:00:00","publicationYear":"2012","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":334,"text":"Scientific Investigations Report","code":"SIR","onlineIssn":"2328-0328","printIssn":"2328-031X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2012-5132","title":"Simulation of climate change in San Francisco Bay Basins, California: Case studies in the Russian River Valley and Santa Cruz Mountains","docAbstract":"As a result of ongoing changes in climate, hydrologic and ecologic effects are being seen across the western United States. A regional study of how climate change affects water resources and habitats in the San Francisco Bay area relied on historical climate data and future projections of climate, which were downscaled to fine spatial scales for application to a regional water-balance model. Changes in climate, potential evapotranspiration, recharge, runoff, and climatic water deficit were modeled for the Bay Area. In addition, detailed studies in the Russian River Valley and Santa Cruz Mountains, which are on the northern and southern extremes of the Bay Area, respectively, were carried out in collaboration with local water agencies. Resource managers depend on science-based projections to inform planning exercises that result in competent adaptation to ongoing and future changes in water supply and environmental conditions. Results indicated large spatial variability in climate change and the hydrologic response across the region; although there is warming under all projections, potential change in precipitation by the end of the 21st century differed according to model. Hydrologic models predicted reduced early and late wet season runoff for the end of the century for both wetter and drier future climate projections, which could result in an extended dry season. In fact, summers are projected to be longer and drier in the future than in the past regardless of precipitation trends. While water supply could be subject to increased variability (that is, reduced reliability) due to greater variability in precipitation, water demand is likely to steadily increase because of increased evapotranspiration rates and climatic water deficit during the extended summers. Extended dry season conditions and the potential for drought, combined with unprecedented increases in precipitation, could serve as additional stressors on water quality and habitat.  By focusing on the relationship between soil moisture storage and evapotranspiration pressures, climatic water deficit integrates the effects of increasing temperature and varying precipitation on basin conditions. At the fine-scale used for these analyses, this variable is an effective indicator of the areas in the landscape that are the most resilient or vulnerable to projected changes. These analyses have shown that regardless of the direction of precipitation change, climatic water deficit is projected to increase, which implies greater water demand to maintain current agricultural resources or land cover. Fine-scale modeling provides a spatially distributed view of locations in the landscape that could prove to be resilient to climatic changes in contrast to locations where vegetation is currently living on the edge of its present-day bioclimatic distribution and, therefore, is more likely to perish or shift to other dominant species under future warming. This type of modeling and the associated analyses provide a useful means for greater understanding of water and land resources, which can lead to better resource management and planning.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/sir20125132","collaboration":"Prepared in cooperation with Sonoma County Water Agency and Santa Cruz County Department of Environmental Health Services","usgsCitation":"Flint, L.E., and Flint, A.L., 2012, Simulation of climate change in San Francisco Bay Basins, California: Case studies in the Russian River Valley and Santa Cruz Mountains: U.S. Geological Survey Scientific Investigations Report 2012-5132, xi, 55 p., https://doi.org/10.3133/sir20125132.","productDescription":"xi, 55 p.","numberOfPages":"61","onlineOnly":"Y","costCenters":[{"id":154,"text":"California Water Science Center","active":true,"usgs":true}],"links":[{"id":259440,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/sir_2012_5132.jpg"},{"id":259438,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/sir/2012/5132/","linkFileType":{"id":5,"text":"html"}},{"id":259439,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/sir/2012/5132/pdf/sir20125132.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"California","otherGeospatial":"Russian River Valley;Santa Cruz Mountains","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -124,35.666666666666664 ], [ -124,39.5 ], [ -122,39.5 ], [ -122,35.666666666666664 ], [ -124,35.666666666666664 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505b9018e4b08c986b319306","contributors":{"authors":[{"text":"Flint, Lorraine E. 0000-0002-7868-441X lflint@usgs.gov","orcid":"https://orcid.org/0000-0002-7868-441X","contributorId":1184,"corporation":false,"usgs":true,"family":"Flint","given":"Lorraine","email":"lflint@usgs.gov","middleInitial":"E.","affiliations":[{"id":154,"text":"California Water Science Center","active":true,"usgs":true}],"preferred":true,"id":466223,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Flint, Alan L. 0000-0002-5118-751X aflint@usgs.gov","orcid":"https://orcid.org/0000-0002-5118-751X","contributorId":1492,"corporation":false,"usgs":true,"family":"Flint","given":"Alan","email":"aflint@usgs.gov","middleInitial":"L.","affiliations":[{"id":154,"text":"California Water Science Center","active":true,"usgs":true},{"id":657,"text":"Western Geographic Science Center","active":true,"usgs":true}],"preferred":true,"id":466224,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70039421,"text":"ofr20121135 - 2012 - Groundwater quality in the Genesee River Basin, New York, 2010","interactions":[],"lastModifiedDate":"2012-08-06T17:16:49","indexId":"ofr20121135","displayToPublicDate":"2012-08-03T00:00:00","publicationYear":"2012","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2012-1135","title":"Groundwater quality in the Genesee River Basin, New York, 2010","docAbstract":"Water samples collected from eight production wells and eight private residential wells in the Genesee River Basin from September through December 2010 were analyzed to characterize the groundwater quality in the basin. Eight of the wells were completed in sand and gravel aquifers, and eight were finished in bedrock aquifers. Three of the 16 wells were sampled in the first Genesee River Basin study during 2005-2006. Water samples from the 2010 study were analyzed for 147 physiochemical properties and constituents that included major ions, nutrients, trace elements, radionuclides, pesticides, volatile organic compounds (VOCs), and indicator bacteria. Results of the water-quality analyses are presented in tabular form for individual wells, and summary statistics for specific constituents are presented by aquifer type. The results are compared with Federal and New York State drinking-water standards, which typically are identical. The results indicate that groundwater generally is of acceptable quality, although concentrations of the following constituents exceeded current or proposed Federal or New York State drinking-water standards at each of the 16 wells sampled: color (one sample), sodium (three samples), sulfate (three samples), total dissolved solids (four samples), aluminum (one sample), arsenic (two samples), copper (one sample), iron (nine samples), manganese (eight samples), radon-222 (nine samples), and total coliform bacteria (six samples). Existing drinking-water standards for pH, chloride, fluoride, nitrate, nitrite, antimony, barium, beryllium, cadmium, chromium, lead, mercury, selenium, silver, thallium, zinc, gross alpha radioactivity, uranium, fecal coliform, Escherichia coli, and heterotrophic bacteria were not exceeded in any of the samples collected. None of the pesticides and VOCs analyzed exceeded existing drinking-water standards.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr20121135","collaboration":"Prepared in cooperation with the New York State Department of Environmental Conservation","usgsCitation":"Reddy, J.E., 2012, Groundwater quality in the Genesee River Basin, New York, 2010: U.S. Geological Survey Open-File Report 2012-1135, vi, 29 p., https://doi.org/10.3133/ofr20121135.","productDescription":"vi, 29 p.","numberOfPages":"40","onlineOnly":"Y","costCenters":[{"id":474,"text":"New York Water Science Center","active":true,"usgs":true}],"links":[{"id":259436,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ofr_2012_1135.gif"},{"id":259427,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2012/1135/","linkFileType":{"id":5,"text":"html"}},{"id":259428,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/2012/1135/pdf/ofr2012-1135_reddy_508.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"100000","projection":"Universal Transverse Mercator projection, Zone 18","datum":"North American Datum 1983","country":"United States","state":"New York","county":"Allegany;Cattaraugus;Genesee;Livingston;Monroe;Ontario;Orleans;Steuben;Wyoming","otherGeospatial":"Genesee River Basin","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -78.25,42 ], [ -78.25,43.25 ], [ -77,43.25 ], [ -77,42 ], [ -78.25,42 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a2db2e4b0c8380cd5bfbd","contributors":{"authors":[{"text":"Reddy, James E. 0000-0002-6998-7267 jreddy@usgs.gov","orcid":"https://orcid.org/0000-0002-6998-7267","contributorId":1080,"corporation":false,"usgs":true,"family":"Reddy","given":"James","email":"jreddy@usgs.gov","middleInitial":"E.","affiliations":[{"id":474,"text":"New York Water Science Center","active":true,"usgs":true}],"preferred":true,"id":466215,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70039439,"text":"sir20125131 - 2012 - Control-structure ratings on the Chicago Sanitary and Ship Canal near Lockport, Illinois","interactions":[],"lastModifiedDate":"2012-08-04T01:01:57","indexId":"sir20125131","displayToPublicDate":"2012-08-03T00:00:00","publicationYear":"2012","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":334,"text":"Scientific Investigations Report","code":"SIR","onlineIssn":"2328-0328","printIssn":"2328-031X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2012-5131","title":"Control-structure ratings on the Chicago Sanitary and Ship Canal near Lockport, Illinois","docAbstract":"The U.S. Army Corps of Engineers and the Metropolitan Water Reclamation District of Greater Chicago regulate flows through control structures along the Lake Michigan lakefront and the Chicago Sanitary and Ship Canal (CSSC) for Lake Michigan diversion accounting, flood control, sanitary, and navigation purposes. This report documents the measurement and computation of flow through the Lockport Controlling Works (LCW) and the Lockport Powerhouse. This analysis aided in evaluation of the ratings at both structures, and the development of new ratings at the controlling works. The LCW structure consists of seven 30-feet (ft) wide sluice gates and is used to divert water from the CSSC and into the Des Plaines River. The flow regimes for the sluice gate included both free and submerged weir. Forty and 491 flow values from U.S. Geological Survey streamflow-gaging stations were used to develop equations describing free- and submerged-weir flow, respectively, through the sluice gates. The equations were developed for canal headwater elevations ranging from -7.0 to -10.5 ft Chicago City Datum (CCD), and tailwater (Des Plaines River at Lockport) to headwater (CSSC-LCW-Base) ratios ranging from 0.31 to 0.66. The Lockport Powerhouse structure consists of nine 9-ft wide by 14-ft high sluice gates and two 10-ft diameter turbines. Both tailwater and no-tailwater effect flow regimes occurred during nine measurements. Also, the canal headwater elevations ranged from -2.74 to -8.45 ft CCD, and the gates were configured six different ways during the measurements.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/sir20125131","collaboration":"Prepared in cooperation with the U.S. Army Corps of Engineers","usgsCitation":"Straub, T., Johnson, K.K., Hortness, J., and Duncker, J.J., 2012, Control-structure ratings on the Chicago Sanitary and Ship Canal near Lockport, Illinois: U.S. Geological Survey Scientific Investigations Report 2012-5131, vi, 25 p., https://doi.org/10.3133/sir20125131.","productDescription":"vi, 25 p.","onlineOnly":"Y","costCenters":[{"id":344,"text":"Illinois Water Science Center","active":true,"usgs":true}],"links":[{"id":259449,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/sir_2012_5131.gif"},{"id":259444,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/sir/2012/5131/pdf/sir2012-5131_080112.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":259445,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/sir/2012/5131/","linkFileType":{"id":5,"text":"html"}}],"scale":"10000","projection":"Albers Equal-Area Conic Projection","country":"United States","state":"Illinois","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -88.25,41.5 ], [ -88.25,42.25 ], [ -87.5,42.25 ], [ -87.5,41.5 ], [ -88.25,41.5 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059fb46e4b0c8380cd4ddc1","contributors":{"authors":[{"text":"Straub, Timothy D. 0000-0002-5896-0851 tdstraub@usgs.gov","orcid":"https://orcid.org/0000-0002-5896-0851","contributorId":2273,"corporation":false,"usgs":true,"family":"Straub","given":"Timothy D.","email":"tdstraub@usgs.gov","affiliations":[{"id":344,"text":"Illinois Water Science Center","active":true,"usgs":true}],"preferred":false,"id":466237,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Johnson, Kevin K. 0000-0003-2703-5994 johnsonk@usgs.gov","orcid":"https://orcid.org/0000-0003-2703-5994","contributorId":4220,"corporation":false,"usgs":true,"family":"Johnson","given":"Kevin","email":"johnsonk@usgs.gov","middleInitial":"K.","affiliations":[{"id":36532,"text":"Central Midwest Water Science Center","active":true,"usgs":true}],"preferred":true,"id":466239,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Hortness, Jon 0000-0002-9809-2876 hortness@usgs.gov","orcid":"https://orcid.org/0000-0002-9809-2876","contributorId":3601,"corporation":false,"usgs":true,"family":"Hortness","given":"Jon","email":"hortness@usgs.gov","affiliations":[],"preferred":true,"id":466238,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Duncker, James J. 0000-0001-5464-7991 jduncker@usgs.gov","orcid":"https://orcid.org/0000-0001-5464-7991","contributorId":4316,"corporation":false,"usgs":true,"family":"Duncker","given":"James","email":"jduncker@usgs.gov","middleInitial":"J.","affiliations":[{"id":344,"text":"Illinois Water Science Center","active":true,"usgs":true},{"id":36532,"text":"Central Midwest Water Science Center","active":true,"usgs":true},{"id":35680,"text":"Illinois-Iowa-Missouri Water Science Center","active":true,"usgs":true}],"preferred":true,"id":466240,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70039412,"text":"ofr20121145 - 2012 - Waterbird nest monitoring program in San Francisco Bay (2005-10)","interactions":[],"lastModifiedDate":"2018-02-14T14:47:24","indexId":"ofr20121145","displayToPublicDate":"2012-08-02T00:00:00","publicationYear":"2012","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2012-1145","title":"Waterbird nest monitoring program in San Francisco Bay (2005-10)","docAbstract":"<p>Historically, Forster’s Terns (<i>Sterna forsteri</i>), American Avocets (<i>Recurvirostra americana</i>), and Black-necked Stilts (<i>Himantopus mexicanus</i>) were uncommon residents of San Francisco Bay, California (Grinnell and others, 1918; Grinnell and Wythe, 1927; Sibley, 1952). Presently, however, avocets and stilts are the two most abundant breeding shorebirds in San Francisco Bay (Stenzel and others, 2002; Rintoul and others, 2003). More than 4,000 avocets and 1,000 stilts, roughly 20 percent of their San Francisco Bay wintering populations, breed within the estuary, making San Francisco Bay the largest breeding area for these species on the Pacific Coast (Stenzel and others, 2002; Rintoul and others, 2003). Forster’s Terns were first observed breeding in the San Francisco Bay in 1948 (110 nests); they had increased to over 4000 individuals by the 1980s (Sibley, 1952; Gill, 1977; Harvey and others, 1992; Carter and others, 1990) and were estimated at 2000–3000 for 1998–2002; (Strong and others, 2004).</p><p>It is hypothesized that the relatively large size of the current waterbird breeding populations is a result of the creation of artificial salt evaporation ponds from the 1930s through the 1950s (Gill, 1977; Goals Project, 1999). Until recently, these salt ponds and associated islands used by waterbirds for nesting have been managed relatively similarly and have supported large breeding waterbird populations. Recently, the South Bay Salt Pond Restoration Project has implemented plans to convert 50–90 percent of the 15,000 acres of salt ponds in the South San Francisco Bay back to tidal marsh habitat. Therefore, there is concern that the Restoration Project, while benefiting other native species, could negatively influence local breeding populations of waterbirds that are reliant on salt pond habitats for both breeding and foraging. A primary goal of the South Bay Salt Pond Restoration Project is to maintain current breeding waterbird populations (South Bay Salt Pond Long-Term Restoration Project, 2004); thus, specific efforts are planned to ensure that the Restoration Project enhances the habitats of the remaining salt ponds for breeding waterbirds.</p><p>Here, we provide a summary of nesting ecology data for Forster’s Terns, American Avocets, and Black-necked Stilts, collected from 2005 to 2010 in the areas of the South Bay Salt Pond Restoration Project, including lands managed by the Don Edwards San Francisco Bay National Wildlife Refuge and Eden Landing Ecological Reserve. These results provide baseline conditions for breeding waterbirds prior to implementation of most restoration actions and can be used to both guide future restoration actions as well as to determine the effect of the South Bay Salt Pond Restoration Project on breeding waterbirds. It is imperative to continue to collect nesting waterbird data annually to assess the response of birds to the South Bay Salt Pond Restoration Project.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr20121145","usgsCitation":"Ackerman, J., and Herzog, M., 2012, Waterbird nest monitoring program in San Francisco Bay (2005-10): U.S. Geological Survey Open-File Report 2012-1145, iv, 16 p., https://doi.org/10.3133/ofr20121145.","productDescription":"iv, 16 p.","onlineOnly":"Y","costCenters":[{"id":154,"text":"California Water Science Center","active":true,"usgs":true},{"id":651,"text":"Western Ecological Research Center","active":true,"usgs":true}],"links":[{"id":259429,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ofr_2012_1145.jpg"},{"id":259424,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/2012/1145/pdf/ofr20121145.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":259423,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2012/1145/","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"California","city":"San Francisco","otherGeospatial":"Don Edwards San Francisco Bay National Wildlife Refuge, Eden Landing Ecological Reserve;South Bay Salt Pond","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -122.25,37.416666666666664 ], [ -122.25,37.666666666666664 ], [ -121.91666666666667,37.666666666666664 ], [ -121.91666666666667,37.416666666666664 ], [ -122.25,37.416666666666664 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505bcf35e4b08c986b32e7a7","contributors":{"authors":[{"text":"Ackerman, Joshua T. 0000-0002-3074-8322 jackerman@usgs.gov","orcid":"https://orcid.org/0000-0002-3074-8322","contributorId":147078,"corporation":false,"usgs":true,"family":"Ackerman","given":"Joshua T.","email":"jackerman@usgs.gov","affiliations":[{"id":651,"text":"Western Ecological Research Center","active":true,"usgs":true}],"preferred":false,"id":466201,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Herzog, Mark P. mherzog@usgs.gov","contributorId":3965,"corporation":false,"usgs":true,"family":"Herzog","given":"Mark P.","email":"mherzog@usgs.gov","affiliations":[{"id":651,"text":"Western Ecological Research Center","active":true,"usgs":true}],"preferred":false,"id":466202,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70039420,"text":"ds689 - 2012 - Selected historic agricultural data important to environmental quality in the United States","interactions":[],"lastModifiedDate":"2012-08-04T17:16:28","indexId":"ds689","displayToPublicDate":"2012-08-02T00:00:00","publicationYear":"2012","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":310,"text":"Data Series","code":"DS","onlineIssn":"2327-638X","printIssn":"2327-0271","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"689","title":"Selected historic agricultural data important to environmental quality in the United States","docAbstract":"This report and the accompanying tables summarize some of the important changes in American agriculture in the form of a timeline and a compilation of selected annual time-series data that can be broadly related to environmental quality. Although these changes have been beneficial for increasing agricultural production, some of them have resulted in environmental concerns. The agriculture timeline is divided into four categories (1) crop and animal changes, (2) mechanical changes, (3) biological and chemical changes, and (4) regulatory and societal changes. The timeline attempts to compile events that have had a lasting impact on agriculture in the United States. The events and data presented in this report may help to improve the connections between agricultural activist and environmental concerns.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ds689","collaboration":"National Water Quality Assessment Program","usgsCitation":"Grey, K., Capel, P.D., Baker, N.T., and Thelin, G.P., 2012, Selected historic agricultural data important to environmental quality in the United States: U.S. Geological Survey Data Series 689, iii, 2 p.; XLS: Tables 1 to 4; PDF: Tables 1 to 4, https://doi.org/10.3133/ds689.","productDescription":"iii, 2 p.; XLS: Tables 1 to 4; PDF: Tables 1 to 4","numberOfPages":"10","onlineOnly":"Y","costCenters":[{"id":346,"text":"Indiana Water Science Center","active":true,"usgs":true}],"links":[{"id":259425,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/ds/689/","linkFileType":{"id":5,"text":"html"}},{"id":259426,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/ds/689/pdf/DS689.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":259431,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ds_689.jpg"}],"country":"United States","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ 173,16.916666666666668 ], [ 173,71.83333333333333 ], [ -66.95,71.83333333333333 ], [ -66.95,16.916666666666668 ], [ 173,16.916666666666668 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505b8c46e4b08c986b317dcf","contributors":{"authors":[{"text":"Grey, Katia M.","contributorId":36393,"corporation":false,"usgs":true,"family":"Grey","given":"Katia M.","affiliations":[],"preferred":false,"id":466213,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Capel, Paul D. 0000-0003-1620-5185 capel@usgs.gov","orcid":"https://orcid.org/0000-0003-1620-5185","contributorId":1002,"corporation":false,"usgs":true,"family":"Capel","given":"Paul","email":"capel@usgs.gov","middleInitial":"D.","affiliations":[{"id":392,"text":"Minnesota Water Science Center","active":true,"usgs":true},{"id":451,"text":"National Water Quality Assessment Program","active":true,"usgs":true},{"id":37778,"text":"WMA - Integrated Modeling and Prediction Division","active":true,"usgs":true}],"preferred":true,"id":466211,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Baker, Nancy T. 0000-0002-7979-5744 ntbaker@usgs.gov","orcid":"https://orcid.org/0000-0002-7979-5744","contributorId":1955,"corporation":false,"usgs":true,"family":"Baker","given":"Nancy","email":"ntbaker@usgs.gov","middleInitial":"T.","affiliations":[{"id":451,"text":"National Water Quality Assessment Program","active":true,"usgs":true},{"id":27111,"text":"National Water Quality Program","active":true,"usgs":true},{"id":346,"text":"Indiana Water Science Center","active":true,"usgs":true},{"id":27231,"text":"Indiana-Kentucky Water Science Center","active":true,"usgs":true}],"preferred":true,"id":466212,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Thelin, Gail P.","contributorId":75178,"corporation":false,"usgs":true,"family":"Thelin","given":"Gail","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":466214,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70039339,"text":"70039339 - 2012 - Emergence of fatal avian influenza in New England harbor seals","interactions":[],"lastModifiedDate":"2015-04-29T15:22:39","indexId":"70039339","displayToPublicDate":"2012-08-02T00:00:00","publicationYear":"2012","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3819,"text":"mBio","active":true,"publicationSubtype":{"id":10}},"title":"Emergence of fatal avian influenza in New England harbor seals","docAbstract":"<p>From September to December 2011, 162 New England harbor seals died in an outbreak of pneumonia. Sequence analysis of postmortem samples revealed the presence of an avian H3N8 influenza A virus, similar to a virus circulating in North American waterfowl since at least 2002 but with mutations that indicate recent adaption to mammalian hosts. These include a D701N mutation in the viral PB2 protein, previously reported in highly pathogenic H5N1 avian influenza viruses infecting people. Lectin staining and agglutination assays indicated the presence of the avian-preferred SA&alpha;-2,3 and mammalian SA&alpha;-2,6 receptors in seal respiratory tract, and the ability of the virus to agglutinate erythrocytes bearing either the SA&alpha;-2,3 or the SA&alpha;-2,6 receptor. The emergence of this A/harbor seal/Massachusetts/1/2011 virus may herald the appearance of an H3N8 influenza clade with potential for persistence and cross-species transmission.</p>","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"mBio","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"American Society for Microbiology","publisherLocation":"Washington, D.C.","doi":"10.1128/mBio.00166-12","usgsCitation":"Anthony, S., St. Leger, J.A., Pugliares, K., Ip, H., Chan, J., Carpenter, Z., Navarrete-Macias, I., Sanchez-Leon, M., Saliki, J., Pedersen, J., Karesh, W., Daszak, P., Rabadan, R., Rowles, T., and Lipkin, W., 2012, Emergence of fatal avian influenza in New England harbor seals: mBio, v. 3, no. 4, published online, 10 p., https://doi.org/10.1128/mBio.00166-12.","productDescription":"published online, 10 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":456,"text":"National Wildlife Health 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A.","contributorId":6316,"corporation":false,"usgs":true,"family":"St. Leger","given":"J.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":466096,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Pugliares, K.","contributorId":46355,"corporation":false,"usgs":true,"family":"Pugliares","given":"K.","email":"","affiliations":[],"preferred":false,"id":466101,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Ip, Hon S. 0000-0003-4844-7533","orcid":"https://orcid.org/0000-0003-4844-7533","contributorId":15829,"corporation":false,"usgs":true,"family":"Ip","given":"Hon S.","affiliations":[],"preferred":false,"id":466099,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Chan, J.M.","contributorId":69408,"corporation":false,"usgs":true,"family":"Chan","given":"J.M.","email":"","affiliations":[],"preferred":false,"id":466106,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Carpenter, Z.W.","contributorId":80951,"corporation":false,"usgs":true,"family":"Carpenter","given":"Z.W.","email":"","affiliations":[],"preferred":false,"id":466107,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Navarrete-Macias, I.","contributorId":80952,"corporation":false,"usgs":true,"family":"Navarrete-Macias","given":"I.","email":"","affiliations":[],"preferred":false,"id":466108,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Sanchez-Leon, M.","contributorId":87019,"corporation":false,"usgs":true,"family":"Sanchez-Leon","given":"M.","affiliations":[],"preferred":false,"id":466110,"contributorType":{"id":1,"text":"Authors"},"rank":8},{"text":"Saliki, J.T.","contributorId":7131,"corporation":false,"usgs":true,"family":"Saliki","given":"J.T.","affiliations":[],"preferred":false,"id":466097,"contributorType":{"id":1,"text":"Authors"},"rank":9},{"text":"Pedersen, J.","contributorId":61269,"corporation":false,"usgs":true,"family":"Pedersen","given":"J.","affiliations":[],"preferred":false,"id":466105,"contributorType":{"id":1,"text":"Authors"},"rank":10},{"text":"Karesh, W.","contributorId":48434,"corporation":false,"usgs":true,"family":"Karesh","given":"W.","email":"","affiliations":[],"preferred":false,"id":466102,"contributorType":{"id":1,"text":"Authors"},"rank":11},{"text":"Daszak, P.","contributorId":58983,"corporation":false,"usgs":true,"family":"Daszak","given":"P.","affiliations":[],"preferred":false,"id":466104,"contributorType":{"id":1,"text":"Authors"},"rank":12},{"text":"Rabadan, R.","contributorId":53226,"corporation":false,"usgs":true,"family":"Rabadan","given":"R.","email":"","affiliations":[],"preferred":false,"id":466103,"contributorType":{"id":1,"text":"Authors"},"rank":13},{"text":"Rowles, T.","contributorId":16135,"corporation":false,"usgs":true,"family":"Rowles","given":"T.","affiliations":[],"preferred":false,"id":466100,"contributorType":{"id":1,"text":"Authors"},"rank":14},{"text":"Lipkin, W.I.","contributorId":9877,"corporation":false,"usgs":true,"family":"Lipkin","given":"W.I.","email":"","affiliations":[],"preferred":false,"id":466098,"contributorType":{"id":1,"text":"Authors"},"rank":15}]}}
,{"id":70039389,"text":"sir20125106 - 2012 - Occurrence of pharmaceuticals, hormones, and organic wastewater compounds in Pennsylvania waters, 2006-09","interactions":[],"lastModifiedDate":"2012-08-28T15:39:23","indexId":"sir20125106","displayToPublicDate":"2012-08-02T00:00:00","publicationYear":"2012","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":334,"text":"Scientific Investigations Report","code":"SIR","onlineIssn":"2328-0328","printIssn":"2328-031X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2012-5106","title":"Occurrence of pharmaceuticals, hormones, and organic wastewater compounds in Pennsylvania waters, 2006-09","docAbstract":"Concern over the presence of contaminants of emerging concern, such as pharmaceutical compounds, hormones, and organic wastewater compounds (OWCs), in waters of the United States and elsewhere is growing. Laboratory techniques developed within the last decade or new techniques currently under development within the U.S. Geological Survey now allow these compounds to be measured at concentrations in nanograms per liter. These new laboratory techniques were used in a reconnaissance study conducted by the U.S. Geological Survey, in cooperation with the Pennsylvania Department of Environmental Protection, to determine the occurrence of contaminants of emerging concern in streams, streambed sediment, and groundwater of Pennsylvania. Compounds analyzed for in the study are pharmaceuticals (human and veterinary drugs), hormones (natural and synthetic), and OWCs (detergents, fragrances, pesticides, industrial compounds, disinfectants, polycyclic aromatic hydrocarbons, fire retardants and plasticizers). Reconnaissance sampling was conducted from 2006 to 2009 to identify contaminants of emerging concern in (1) groundwater from wells used to supply livestock, (2) streamwater upstream and downstream from animal feeding operations, (3) streamwater upstream from and streamwater and streambed sediment downstream from municipal wastewater effluent discharges, (4) streamwater from sites within 5 miles of drinking-water intakes, and (5) streamwater and streambed sediment where fish health assessments were conducted. Of the 44 pharmaceutical compounds analyzed in groundwater samples collected in 2006 from six wells used to supply livestock, only cotinine (a nicotine metabolite) and the antibiotics tylosin and sulfamethoxazole were detected. The maximum concentration of any contaminant of emerging concern was 24 nanograms per liter (ng/L) for cotinine, and was detected in a groundwater sample from a Lebanon County, Pa., well. Seven pharmaceutical compounds including acetaminophen, caffeine, carbamazepine, and the four antibiotics tylosin, sulfadimethoxine, sulfamethoxazole, and oxytetracycline were detected in streamwater samples collected in 2006 from six paired stream sampling sites located upstream and downstream from animal-feeding operations. The highest reported concentration of these seven compounds was for the antibiotic sulfamethoxazole (157 ng/L), in a sample from the downstream site on Snitz Creek in Lancaster County, Pa. Twenty-one pharmaceutical compounds were detected in streamwater samples collected in 2006 from five paired stream sampling sites located upstream or downstream from a municipal wastewater-effluent-discharge site. The most commonly detected compounds and maximum concentrations were the anticonvulsant carbamazepine, 276 ng/L; the antihistamine diphenhydramine, 135 ng/L; and the antibiotics ofloxacin, 329 ng/L; sulfamethoxazole, 1,340 ng/L; and trimethoprim, 256 ng/L. A total of 51 different contaminants of emerging concern were detected in streamwater samples collected from 2007 through 2009 at 13 stream sampling sites located downstream from a wastewater-effluent-discharge site. The concentrations and numbers of compounds detected were higher in stream sites downstream from a wastewater-effluent-discharge site than in stream sites upstream from a wastewater-effluent-discharge site. This finding indicates that wastewater-effluent discharges are a source of contaminants of emerging concern; these contaminants were present more frequently in the streambed-sediment samples than in streamwater samples. Antibiotic compounds were often present in both the streamwater and streambed-sediment samples, but many OWCs were present exclusively in the streambed-sediment samples. Compounds with endocrine disrupting potential including detergent metabolites, pesticides, and flame retardants, were present in the streamwater and streambed-sediment samples. Killinger Creek, a stream where wastewater-effluent discharges contribute a large percentage of the total flow, stands out as a stream with particularly high numbers of compounds detected and detected at the highest concentrations measured in the reconnaissance sampling. Nineteen contaminants of emerging concern were detected in streamwater samples collected quarterly from 2007 through 2009 at 27 stream sites within 5 miles of a drinking-water intake. The number of contaminants and the concentrations detected at the stream sites within 5 miles of drinking-water intakes were generally very low (concentrations less than 50 ng/L), much lower than those at sites downstream from a wastewater-effluent discharge. The most commonly detected compounds and maximum concentrations were caffeine, 517 ng/L; carbamazepine, 95 ng/L; sulfamethoxazole, 146 ng/L; and estrone, 3.15 ng/L. The concentrations and frequencies of detection of some of the contaminants of emerging concern appear to vary by season, which could be explained by compound use, flow regime, or differences in degradation rates. Concentrations of some contaminants were associated with lower flows as a result of decreased in-stream dilution of wastewater effluents or other contamination sources. Twenty-two contaminants of emerging concern were detected once each in streamwater samples collected in 2007 and 2008 from 16 fish-health stream sites located statewide. The highest concentrations were for the OWCs, including flame retardants tri(2-butoxyethyl)phosphate (604 ng/L) and tri(2-chloroethyl)phosphate (272 ng/L) and the fragrance isoquinoline (330 ng/L). Far fewer numbers of contaminants of emerging concern were detected at the fish-health sites than at the wastewater-effluent-discharge sites. Most of the fish-health sites were not located directly downstream from a wastewater-effluent discharge, but there were multiple wastewater-effluent discharges in the drainage basins upstream from the sampling sites. No distinct pattern of contaminant occurrence could be discerned for the fish-health stream sites","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/sir20125106","collaboration":"Prepared in cooperation with the Pennsylvania Department of Environmental Protection","usgsCitation":"Reif, A.G., Crawford, J.K., Loper, C.A., Proctor, A., Manning, R., and Titler, R., 2012, Occurrence of pharmaceuticals, hormones, and organic wastewater compounds in Pennsylvania waters, 2006-09: U.S. Geological Survey Scientific Investigations Report 2012-5106, x, 99 p., https://doi.org/10.3133/sir20125106.","productDescription":"x, 99 p.","numberOfPages":"109","onlineOnly":"Y","costCenters":[{"id":532,"text":"Pennsylvania Water Science Center","active":true,"usgs":true}],"links":[{"id":259414,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/sir_2012_5106.png"},{"id":259411,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/sir/2012/5106/pdf/sir2012-5106.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":259412,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/sir/2012/5106/","linkFileType":{"id":5,"text":"html"}}],"scale":"100000","projection":"Albers Equal-Area Conic","datum":"North American Datum 1983","country":"United States","state":"Pennsylvania","otherGeospatial":"Allegheny River;Delaware River;East Branch Susquehanna River;Junniata River;Monongahela River;Ohio River;Schuylkill River;West Branch Susquehanna River;Youghiogeny River","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -78.33333333333333,39.71666666666667 ], [ -78.33333333333333,41.333333333333336 ], [ -75.83333333333333,41.333333333333336 ], [ -75.83333333333333,39.71666666666667 ], [ -78.33333333333333,39.71666666666667 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a6c27e4b0c8380cd74a9a","contributors":{"authors":[{"text":"Reif, Andrew G. 0000-0002-5054-5207 agreif@usgs.gov","orcid":"https://orcid.org/0000-0002-5054-5207","contributorId":2632,"corporation":false,"usgs":true,"family":"Reif","given":"Andrew","email":"agreif@usgs.gov","middleInitial":"G.","affiliations":[{"id":532,"text":"Pennsylvania Water Science Center","active":true,"usgs":true}],"preferred":true,"id":466174,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Crawford, J. Kent","contributorId":54176,"corporation":false,"usgs":true,"family":"Crawford","given":"J.","email":"","middleInitial":"Kent","affiliations":[],"preferred":false,"id":466178,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Loper, Connie A.","contributorId":62243,"corporation":false,"usgs":true,"family":"Loper","given":"Connie","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":466179,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Proctor, Arianne","contributorId":14225,"corporation":false,"usgs":true,"family":"Proctor","given":"Arianne","email":"","affiliations":[],"preferred":false,"id":466175,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Manning, Rhonda","contributorId":54044,"corporation":false,"usgs":true,"family":"Manning","given":"Rhonda","affiliations":[],"preferred":false,"id":466177,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Titler, Robert","contributorId":26548,"corporation":false,"usgs":true,"family":"Titler","given":"Robert","email":"","affiliations":[],"preferred":false,"id":466176,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}}
,{"id":70160894,"text":"70160894 - 2012 - An at-grade stabilization structure impact on runoff and suspended sediment","interactions":[],"lastModifiedDate":"2016-01-04T15:10:00","indexId":"70160894","displayToPublicDate":"2012-08-01T16:15:00","publicationYear":"2012","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2456,"text":"Journal of Soil and Water Conservation","active":true,"publicationSubtype":{"id":10}},"title":"An at-grade stabilization structure impact on runoff and suspended sediment","docAbstract":"<p>In recent years, agricultural runoff has received more attention as a major contributor to surface water pollution. This is especially true for the unglaciated area of Wisconsin, given this area's steep topography, which makes it highly susceptible to runoff and soil loss. We evaluated the ability of an at-grade stabilization structure (AGSS), designed as a conservation practice to reduce the amount of overland runoff and suspended sediment transported to the surface waters of an agricultural watershed. Eight years of storm and baseflow data collected by the US Geological Survey&ndash;Wisconsin Water Science Center on a farm in west central Wisconsin were analyzed for changes in precipitation, storm runoff volume, and suspended sediment concentration before and after installation of an AGSS. The agricultural research site was designed as a paired watershed study in which monitoring stations were installed on the perennial streams draining both control and treatment watersheds. Linear mixed effects model analyses were conducted to determine if any statistically significant changes occurred in the water quality parameters before and after the AGSS was installed. Results indicated no significant changes (<i>p</i> = 0.51) in average event precipitation and runoff volumes before and after installation of the AGSS in either the treatment (NW) or control (SW) watersheds. However, the AGSS did significantly reduce the average suspended sediment concentration in the event runoff water (<i>p</i> = 0.02) in the NW from 972 to 263 mg L<sup>&ndash;1</sup>. In addition, particle size analyses, using light diffraction techniques, were conducted on soil samples taken from within the AGSS and adjacent valley and ridge top to determine if suspended sediments were being retained within the structure. Statistical analysis revealed a significantly (<i>p</i> &lt; 0.001) larger proportion of clay inside the AGSS (37%) than outside (30%). These results indicate that the AGSS was successful in reducing the amount of suspended sediment transported to nearby surface waters. The cost of an AGSS can range from US$3,500 to US$8,000, depending on size. Thus, these structures provide a cheap and effective means of improving water quality in highly erosive landscapes.</p>","language":"English","publisher":"Soil Conservation Society of America","publisherLocation":"Ankeny, IA","doi":"10.2489/jswc.67.4.237","usgsCitation":"Minks, K.R., Lowery, B., Madison, F.W., Ruark, M., Frame, D.R., Stuntebeck, T.D., and Komiskey, M.J., 2012, An at-grade stabilization structure impact on runoff and suspended sediment: Journal of Soil and Water Conservation, v. 67, no. 4, p. 237-248, https://doi.org/10.2489/jswc.67.4.237.","productDescription":"12 p.","startPage":"237","endPage":"248","numberOfPages":"12","onlineOnly":"N","additionalOnlineFiles":"N","ipdsId":"IP-031188","costCenters":[{"id":677,"text":"Wisconsin Water Science Center","active":true,"usgs":true}],"links":[{"id":313247,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Wisconsin","otherGeospatial":"Traverse Valley Creek Watersheds","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -91.40899658203125,\n              43.982933852960805\n            ],\n            [\n              -91.3128662109375,\n              44.06588017158586\n            ],\n            [\n              -90.9228515625,\n              44.16447445668458\n            ],\n            [\n              -90.82672119140625,\n              44.327777761284445\n            ],\n            [\n              -90.89813232421875,\n              44.51805165000557\n            ],\n            [\n              -91.0546875,\n              44.666699513609174\n            ],\n            [\n              -91.27166748046875,\n              44.766236875162335\n            ],\n            [\n              -91.4886474609375,\n   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]\n}","volume":"67","issue":"4","publishingServiceCenter":{"id":6,"text":"Columbus PSC"},"noUsgsAuthors":false,"publicationDate":"2012-07-09","publicationStatus":"PW","scienceBaseUri":"568ba5c0e4b0e7594ee77648","contributors":{"authors":[{"text":"Minks, Kyle R.","contributorId":151053,"corporation":false,"usgs":false,"family":"Minks","given":"Kyle","email":"","middleInitial":"R.","affiliations":[{"id":18172,"text":"UW-Madison Dept. of Soil Science, Madison, WI","active":true,"usgs":false}],"preferred":false,"id":584189,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Lowery, Birl","contributorId":151050,"corporation":false,"usgs":false,"family":"Lowery","given":"Birl","email":"","affiliations":[{"id":18172,"text":"UW-Madison Dept. of Soil Science, Madison, WI","active":true,"usgs":false}],"preferred":false,"id":584186,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Madison, Fred 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tdstunte@usgs.gov","orcid":"https://orcid.org/0000-0002-8405-7295","contributorId":902,"corporation":false,"usgs":true,"family":"Stuntebeck","given":"Todd","email":"tdstunte@usgs.gov","middleInitial":"D.","affiliations":[{"id":37947,"text":"Upper Midwest Water Science Center","active":true,"usgs":true},{"id":677,"text":"Wisconsin Water Science Center","active":true,"usgs":true}],"preferred":true,"id":584185,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Komiskey, Matthew J. 0000-0003-2962-6974 mjkomisk@usgs.gov","orcid":"https://orcid.org/0000-0003-2962-6974","contributorId":1776,"corporation":false,"usgs":true,"family":"Komiskey","given":"Matthew","email":"mjkomisk@usgs.gov","middleInitial":"J.","affiliations":[{"id":37947,"text":"Upper Midwest Water Science Center","active":true,"usgs":true}],"preferred":true,"id":584184,"contributorType":{"id":1,"text":"Authors"},"rank":7}]}}
,{"id":70110899,"text":"70110899 - 2012 - Updating the debate on model complexity","interactions":[],"lastModifiedDate":"2014-06-02T11:16:48","indexId":"70110899","displayToPublicDate":"2012-08-01T11:14:42","publicationYear":"2012","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1728,"text":"GSA Today","active":true,"publicationSubtype":{"id":10}},"title":"Updating the debate on model complexity","docAbstract":"As scientists who are trying to understand a complex natural world that cannot be fully characterized in the field, how can we best inform the society in which we live? This founding context was addressed in a special session, “Complexity in Modeling: How Much is Too Much?” convened at the 2011 Geological Society of America Annual Meeting. The session had a variety of thought-provoking presentations—ranging from philosophy to cost-benefit analyses—and provided some areas of broad agreement that were not evident in discussions of the topic in 1998 (Hunt and Zheng, 1999). The session began with a short introduction during which model complexity was framed borrowing from an economic concept, the Law of Diminishing Returns, and an example of enjoyment derived by eating ice cream. Initially, there is increasing satisfaction gained from eating more ice cream, to a point where the gain in satisfaction starts to decrease, ending at a point when the eater sees no value in eating more ice cream. A traditional view of model complexity is similar—understanding gained from modeling can actually decrease if models become unnecessarily complex. However, oversimplified models—those that omit important aspects of the problem needed to make a good prediction—can also limit and confound our understanding. Thus, the goal of all modeling is to find the “sweet spot” of model sophistication—regardless of whether complexity was added sequentially to an overly simple model or collapsed from an initial highly parameterized framework that uses mathematics and statistics to attain an optimum (e.g., Hunt et al., 2007). Thus, holistic parsimony is attained, incorporating “as simple as possible,” as well as the equally important corollary “but no simpler.”","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"GSA Today","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"Geological Society of America","publisherLocation":"Boulder, CO","doi":"10.1130/GSATG150GW.1","usgsCitation":"Simmons, C.T., and Hunt, R.J., 2012, Updating the debate on model complexity: GSA Today, v. 22, no. 8, p. 28-29, https://doi.org/10.1130/GSATG150GW.1.","productDescription":"2 p.","startPage":"28","endPage":"29","numberOfPages":"2","ipdsId":"IP-035327","costCenters":[{"id":677,"text":"Wisconsin Water Science Center","active":true,"usgs":true}],"links":[{"id":287955,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":287954,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1130/GSATG150GW.1"}],"volume":"22","issue":"8","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53ae788ce4b0abf75cf2d830","contributors":{"authors":[{"text":"Simmons, Craig T.","contributorId":71889,"corporation":false,"usgs":false,"family":"Simmons","given":"Craig","email":"","middleInitial":"T.","affiliations":[{"id":13412,"text":"Flinders University, Australia","active":true,"usgs":false}],"preferred":false,"id":494184,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hunt, Randall J. 0000-0001-6465-9304 rjhunt@usgs.gov","orcid":"https://orcid.org/0000-0001-6465-9304","contributorId":1129,"corporation":false,"usgs":true,"family":"Hunt","given":"Randall","email":"rjhunt@usgs.gov","middleInitial":"J.","affiliations":[{"id":677,"text":"Wisconsin Water Science Center","active":true,"usgs":true}],"preferred":true,"id":494183,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70156329,"text":"70156329 - 2012 - Identifying the decision to be supported: a review of papers from environmental modelling and software","interactions":[],"lastModifiedDate":"2021-10-21T14:48:30.002291","indexId":"70156329","displayToPublicDate":"2012-08-01T01:00:00","publicationYear":"2012","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"chapter":"A","subchapterNumber":"Environmental Information-, Decision Support-, and Software Systems","title":"Identifying the decision to be supported: a review of papers from environmental modelling and software","docAbstract":"<p>Two of the basic tenets of decision support system efforts are to help identify and structure the decisions to be supported, and to then provide analysis in how those decisions might be best made. One example from wetland management would be that wildlife biologists must decide when to draw down water levels to optimise aquatic invertebrates as food for breeding ducks. Once such a decision is identified, a system or tool to help them make that decision in the face of current and projected climate conditions could be developed. We examined a random sample of 100 papers published from 2001-2011 in Environmental Modelling and Software that used the phrase &ldquo;decision support system&rdquo; or &ldquo;decision support tool&rdquo;, and which are characteristic of different sectors. In our review, 41% of the systems and tools related to the water resources sector, 34% were related to agriculture, and 22% to the conservation of fish, wildlife, and protected area management. Only 60% of the papers were deemed to be reporting on DSS. This was based on the papers reviewed not having directly identified a specific decision to be supported. We also report on the techniques that were used to identify the decisions, such as formal survey, focus group, expert opinion, or sole judgment of the author(s). The primary underlying modelling system, e.g., expert system, agent based model, Bayesian belief network, geographical information system (GIS), and the like was categorised next. Finally, since decision support typically should target some aspect of unstructured decisions, we subjectively determined to what degree this was the case. In only 23% of the papers reviewed, did the system appear to tackle unstructured decisions. This knowledge should be useful in helping workers in the field develop more effective systems and tools, especially by being exposed to the approaches in different, but related, disciplines. We propose that a standard blueprint for reporting on DSS be developed for consideration by journal editors to aid them in filtering papers that use the term, &ldquo;decision support&rdquo;.</p>","largerWorkType":{"id":24,"text":"Conference Paper"},"largerWorkTitle":"International Environmental Modelling and Software Society (iEMSs) 2012 International Congress on Environmental Modelling and Software. Managing resources of a limited planet: pathways and visions under uncertainty, sixth biennial meeting, Leipzig, Germany","largerWorkSubtype":{"id":19,"text":"Conference Paper"},"conferenceTitle":"2012 International Congress on Environmental Modelling and Software","conferenceDate":"July 1-5, 2012","conferenceLocation":"Leipzig, Germany","language":"English","publisher":"International Environmental Modelling and Software Society","isbn":"978-88-9035-742-8","usgsCitation":"Sojda, R.S., Chen, S.H., Elsawah, S., Guillaume, J.H., Jakeman, A., Lautenbach, S., McIntosh, B.S., Rizzoli, A., Seppelt, R., Struss, P., Voinov, A., and Volk, M., 2012, Identifying the decision to be supported: a review of papers from environmental modelling and software, <i>in</i> International Environmental Modelling and Software Society (iEMSs) 2012 International Congress on Environmental Modelling and Software. Managing resources of a limited planet: pathways and visions under uncertainty, sixth biennial meeting, Leipzig, Germany, Leipzig, Germany, July 1-5, 2012, p. 73-80.","productDescription":"8 p.","startPage":"73","endPage":"80","onlineOnly":"N","additionalOnlineFiles":"N","ipdsId":"IP-036368","costCenters":[],"links":[{"id":306973,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"Germany","city":"Leipzig","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              11.7498779296875,\n              51.13110763758015\n            ],\n            [\n              11.7498779296875,\n              51.549751017014195\n            ],\n            [\n              13.0078125,\n              51.549751017014195\n            ],\n            [\n              13.0078125,\n              51.13110763758015\n            ],\n            [\n              11.7498779296875,\n              51.13110763758015\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"55d5a8b1e4b0518e3546a4c9","contributors":{"authors":[{"text":"Sojda, Richard S. sojda@usgs.gov","contributorId":1663,"corporation":false,"usgs":true,"family":"Sojda","given":"Richard","email":"sojda@usgs.gov","middleInitial":"S.","affiliations":[{"id":481,"text":"Northern Rocky Mountain Science Center","active":true,"usgs":true}],"preferred":true,"id":568730,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Chen, Serena H.","contributorId":146682,"corporation":false,"usgs":false,"family":"Chen","given":"Serena","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":568731,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Elsawah, Sondoss","contributorId":146686,"corporation":false,"usgs":false,"family":"Elsawah","given":"Sondoss","affiliations":[],"preferred":false,"id":568732,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Guillaume, Joseph H.A.","contributorId":146687,"corporation":false,"usgs":false,"family":"Guillaume","given":"Joseph","email":"","middleInitial":"H.A.","affiliations":[],"preferred":false,"id":568733,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Jakeman, A.J.","contributorId":12639,"corporation":false,"usgs":true,"family":"Jakeman","given":"A.J.","email":"","affiliations":[],"preferred":false,"id":568734,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Lautenbach, Sven","contributorId":146688,"corporation":false,"usgs":false,"family":"Lautenbach","given":"Sven","email":"","affiliations":[],"preferred":false,"id":568735,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"McIntosh, Brian S.","contributorId":146689,"corporation":false,"usgs":false,"family":"McIntosh","given":"Brian","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":568736,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Rizzoli, A.E.","contributorId":113184,"corporation":false,"usgs":true,"family":"Rizzoli","given":"A.E.","email":"","affiliations":[],"preferred":false,"id":568737,"contributorType":{"id":1,"text":"Authors"},"rank":8},{"text":"Seppelt, Ralf","contributorId":146691,"corporation":false,"usgs":false,"family":"Seppelt","given":"Ralf","email":"","affiliations":[],"preferred":false,"id":568738,"contributorType":{"id":1,"text":"Authors"},"rank":9},{"text":"Struss, Peter","contributorId":75853,"corporation":false,"usgs":true,"family":"Struss","given":"Peter","email":"","affiliations":[],"preferred":false,"id":568739,"contributorType":{"id":1,"text":"Authors"},"rank":10},{"text":"Voinov, Alexey","contributorId":23046,"corporation":false,"usgs":true,"family":"Voinov","given":"Alexey","affiliations":[],"preferred":false,"id":568740,"contributorType":{"id":1,"text":"Authors"},"rank":11},{"text":"Volk, Martin","contributorId":146695,"corporation":false,"usgs":false,"family":"Volk","given":"Martin","affiliations":[],"preferred":false,"id":568741,"contributorType":{"id":1,"text":"Authors"},"rank":12}]}}
,{"id":70004459,"text":"70004459 - 2012 - The early bird gets the shrimp: Confronting assumptions of isotopic equilibrium and homogeneity in a wild bird population","interactions":[],"lastModifiedDate":"2012-11-02T16:14:13","indexId":"70004459","displayToPublicDate":"2012-08-01T00:00:00","publicationYear":"2012","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2158,"text":"Journal of Animal Ecology","active":true,"publicationSubtype":{"id":10}},"title":"The early bird gets the shrimp: Confronting assumptions of isotopic equilibrium and homogeneity in a wild bird population","docAbstract":"1. Because stable isotope distributions in organic material vary systematically across energy gradients that exist in ecosystems, community and population structures, and in individual physiological systems, isotope values in animal tissues have helped address a broad range of questions in animal ecology. It follows that every tissue sample provides an isotopic profile that can be used to study dietary or movement histories of individual animals. Interpretations of these profiles depend on the assumption that metabolic pools are isotopically well mixed and in equilibrium with dietary resources prior to tissue synthesis, and they extend to the population level by assuming isotope profiles are identically distributed for animals using the same proximal dietary resource. As these assumptions are never fully met, studying structure in the variance of tissue isotope values from wild populations is informative. 2. We studied variation in &delta;<sup>13</sup>C, &delta;<sup>15</sup>N, &delta;<sup>2</sup>H and &delta;<sup>18</sup>O data for feathers from a population of eared grebes (Podiceps nigricollis) that migrate to Great Salt Lake each fall to moult feathers. During this time, they cannot fly and feed almost exclusively on superabundant brine shrimp (Artemia franciscana). The ecological simplicity of this situation minimized the usual spatial and trophic complexities often present in natural studies of feather isotope values. 3. Ranges and variances of isotope values for the feathers were larger than those from previously published studies that report feather isotopic variance, but they were bimodally distributed in all isotope dimensions. Isotope values for proximal dietary resources and local surface water show that some of the feathers we assumed to have been grown locally must have been grown before birds reached isotopic equilibrium with local diet or immediately prior to arrival at Great Salt Lake. 4. Our study provides novel insights about resource use strategies in eared grebes during migration. More generally, it demonstrates the utility of studying variance structures and questioning assumptions implicit in the interpretation of stable isotope data from wild animals.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Journal of Animal Ecology","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"Wiley","publisherLocation":"Hoboken, NJ","usgsCitation":"Wunder, M.B., Jehl, J.R., and Stricker, C.A., 2012, The early bird gets the shrimp: Confronting assumptions of isotopic equilibrium and homogeneity in a wild bird population: Journal of Animal Ecology, v. 81, no. 6, p. 1223-1232.","productDescription":"10 p.","startPage":"1223","endPage":"1232","costCenters":[{"id":291,"text":"Fort Collins Science Center","active":true,"usgs":true}],"links":[{"id":259397,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Utah","otherGeospatial":"Great Salt Lake","volume":"81","issue":"6","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505baaefe4b08c986b322ae7","contributors":{"authors":[{"text":"Wunder, Michael B.","contributorId":88594,"corporation":false,"usgs":true,"family":"Wunder","given":"Michael","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":350464,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Jehl, Joseph R. Jr.","contributorId":6309,"corporation":false,"usgs":true,"family":"Jehl","given":"Joseph","suffix":"Jr.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":350463,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Stricker, Craig A. 0000-0002-5031-9437 cstricker@usgs.gov","orcid":"https://orcid.org/0000-0002-5031-9437","contributorId":1097,"corporation":false,"usgs":true,"family":"Stricker","given":"Craig","email":"cstricker@usgs.gov","middleInitial":"A.","affiliations":[{"id":291,"text":"Fort Collins Science Center","active":true,"usgs":true}],"preferred":true,"id":350462,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70039293,"text":"70039293 - 2012 - PAH volatilization following application of coal-tar-based pavement sealant","interactions":[],"lastModifiedDate":"2012-08-02T01:01:49","indexId":"70039293","displayToPublicDate":"2012-08-01T00:00:00","publicationYear":"2012","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":924,"text":"Atmospheric Environment","active":true,"publicationSubtype":{"id":10}},"title":"PAH volatilization following application of coal-tar-based pavement sealant","docAbstract":"Coal-tar-based pavement sealants, a major source of PAHs to urban water bodies, have recently been identified as a source of volatile PAHs to the atmosphere. We tracked the volatilization of PAHs for 1 year after application of a coal-tar-based pavement sealant by measuring gas-phase PAH concentrations above the pavement surface and solid-phase PAH concentrations in sealant scraped from the surface. Gas-phase concentrations at two heights (0.03 and 1.28 m) and wind speed were used to estimate volatilization flux. The sum of the concentrations of eight frequently detected PAHs (&Sigma;PAH<sub>8</sub>) in the 0.03-m sample 1.6 h after application (297,000 ng m<sup>-3</sup>) was about 5000 times greater than that previously reported for the same height above unsealed parking lots (66 ng m<sup>-3</sup>). Flux at 1.6 h after application was estimated at 45,000 &mu;g m<sup>-2</sup> h<sup>-1</sup> and decreased rapidly during the 45 days after application to 160 &mu;g m<sup>-2</sup> h<sup>-1</sup>. Loss of PAHs from the adhered sealant also was rapid, with about a 50% decrease in solid-phase &Sigma;PAH<sub>8</sub> concentration over the 45 days after application. There was general agreement, given the uncertainties, in the estimated mass of &Sigma;PAH<sub>8</sub> lost to the atmosphere on the basis of air sampling (2&ndash;3 g m<sup>-2</sup>) and adhered sealant sampling (6 g m<sup>-2</sup>) during the first 16 days after application, translating to a loss to the atmosphere of one-quarter to one-half of the PAHs in the sealcoat product. Combining the estimated mass of &Sigma;PAH<sub>8</sub> released to the atmosphere with a national-use estimate of coal-tar-based sealant suggests that PAH emissions from new coal-tar-based sealcoat applications each year (~1000 Mg) are larger than annual vehicle emissions of PAHs for the United States.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Atmospheric Environment","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"Elsevier","publisherLocation":"Amsterdam, Netherlands","doi":"10.1016/j.atmosenv.2012.01.036","usgsCitation":"Van Metre, P., Majewski, M.S., Mahler, B., Foreman, W., Braun, C.L., Wilson, J.T., and Burbank, T.L., 2012, PAH volatilization following application of coal-tar-based pavement sealant: Atmospheric Environment, v. 51, p. 108-115, https://doi.org/10.1016/j.atmosenv.2012.01.036.","productDescription":"8 p.","startPage":"108","endPage":"115","numberOfPages":"8","costCenters":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"links":[{"id":259369,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":259353,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1016/j.atmosenv.2012.01.036","linkFileType":{"id":5,"text":"html"}}],"country":"United States","volume":"51","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a7325e4b0c8380cd76eb8","contributors":{"authors":[{"text":"Van Metre, Peter C.","contributorId":34104,"corporation":false,"usgs":true,"family":"Van Metre","given":"Peter C.","affiliations":[],"preferred":false,"id":465992,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Majewski, Michael S. majewski@usgs.gov","contributorId":440,"corporation":false,"usgs":true,"family":"Majewski","given":"Michael","email":"majewski@usgs.gov","middleInitial":"S.","affiliations":[{"id":154,"text":"California Water Science Center","active":true,"usgs":true}],"preferred":true,"id":465986,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Mahler, Barbara 0000-0002-9150-9552 bjmahler@usgs.gov","orcid":"https://orcid.org/0000-0002-9150-9552","contributorId":1249,"corporation":false,"usgs":true,"family":"Mahler","given":"Barbara","email":"bjmahler@usgs.gov","affiliations":[{"id":37277,"text":"WMA - Earth System Processes Division","active":true,"usgs":true},{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"preferred":true,"id":465988,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Foreman, William T. wforeman@usgs.gov","contributorId":1473,"corporation":false,"usgs":true,"family":"Foreman","given":"William T.","email":"wforeman@usgs.gov","affiliations":[{"id":452,"text":"National Water Quality Laboratory","active":true,"usgs":true}],"preferred":false,"id":465989,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Braun, Christopher L. 0000-0002-5540-2854 clbraun@usgs.gov","orcid":"https://orcid.org/0000-0002-5540-2854","contributorId":925,"corporation":false,"usgs":true,"family":"Braun","given":"Christopher","email":"clbraun@usgs.gov","middleInitial":"L.","affiliations":[{"id":48595,"text":"Oklahoma-Texas Water Science Center","active":true,"usgs":true}],"preferred":true,"id":465987,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Wilson, Jennifer T. 0000-0003-4481-6354 jenwilso@usgs.gov","orcid":"https://orcid.org/0000-0003-4481-6354","contributorId":1782,"corporation":false,"usgs":true,"family":"Wilson","given":"Jennifer","email":"jenwilso@usgs.gov","middleInitial":"T.","affiliations":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"preferred":true,"id":465990,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Burbank, Teresa L. tburbank@usgs.gov","contributorId":2048,"corporation":false,"usgs":true,"family":"Burbank","given":"Teresa","email":"tburbank@usgs.gov","middleInitial":"L.","affiliations":[],"preferred":true,"id":465991,"contributorType":{"id":1,"text":"Authors"},"rank":7}]}}
,{"id":70039289,"text":"70039289 - 2012 - Coal-tar pavement sealants might substantially increase children's PAH exposures","interactions":[],"lastModifiedDate":"2013-06-14T09:28:33","indexId":"70039289","displayToPublicDate":"2012-08-01T00:00:00","publicationYear":"2012","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":"Coal-tar pavement sealants might substantially increase children's PAH exposures","docAbstract":"Dietary ingestion has been identified repeatedly as the primary route of human exposure to polycyclic aromatic hydrocarbons (PAHs), seven of which are classified as probable human carcinogens (B2 PAHs) by the U.S. EPA. Humans are exposed to PAHs through ingestion of cooked and uncooked foods, incidental ingestion of soil and dust, inhalation of ambient air, and absorption through skin. Although PAH sources are ubiquitous in the environment, one recently identified PAH source stands out: Coal-tar-based pavement sealant&mdash;a product applied to many parking lots, driveways, and even playgrounds primarily in the central, southern, and eastern U.S.&mdash;has PAH concentrations 100&ndash;1000 times greater than most other PAH sources. It was reported recently that PAH concentrations in house dust in residences adjacent to parking lots with coal-tar-based sealant were 25 times higher than in residences adjacent to unsealed asphalt parking lots.","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.2012.01.010","usgsCitation":"Williams, E.S., Mahler, B., and Van Metre, P., 2012, Coal-tar pavement sealants might substantially increase children's PAH exposures: Environmental Pollution, v. 164, p. 40-41, https://doi.org/10.1016/j.envpol.2012.01.010.","productDescription":"2 p.","startPage":"40","endPage":"41","costCenters":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"links":[{"id":259350,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":259339,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1016/j.envpol.2012.01.010","linkFileType":{"id":5,"text":"html"}}],"volume":"164","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059f76ae4b0c8380cd4cae2","contributors":{"authors":[{"text":"Williams, E. Spencer","contributorId":53640,"corporation":false,"usgs":true,"family":"Williams","given":"E.","email":"","middleInitial":"Spencer","affiliations":[],"preferred":false,"id":465971,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Mahler, Barbara 0000-0002-9150-9552 bjmahler@usgs.gov","orcid":"https://orcid.org/0000-0002-9150-9552","contributorId":1249,"corporation":false,"usgs":true,"family":"Mahler","given":"Barbara","email":"bjmahler@usgs.gov","affiliations":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true},{"id":37277,"text":"WMA - Earth System Processes Division","active":true,"usgs":true}],"preferred":true,"id":465969,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Van Metre, Peter C.","contributorId":34104,"corporation":false,"usgs":true,"family":"Van Metre","given":"Peter C.","affiliations":[],"preferred":false,"id":465970,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70039322,"text":"70039322 - 2012 - Shallow groundwater mercury supply in a coastal plain stream","interactions":[],"lastModifiedDate":"2017-01-18T13:01:56","indexId":"70039322","displayToPublicDate":"2012-08-01T00:00:00","publicationYear":"2012","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1565,"text":"Environmental Science & Technology","onlineIssn":"1520-5851","printIssn":"0013-936X","active":true,"publicationSubtype":{"id":10}},"title":"Shallow groundwater mercury supply in a coastal plain stream","docAbstract":"Fluvial methylmercury (MeHg) is attributed to methylation in up-gradient wetland areas. This hypothesis depends on efficient wetland-to-stream hydraulic transport under nonflood and flood conditions. Fluxes of water and dissolved (filtered) mercury (Hg) species (FMeHg and total Hg (FTHg)) were quantified in April and July of 2009 in a reach at McTier Creek, South Carolina to determine the relative importance of tributary surface water and shallow groundwater Hg transport from wetland/floodplain areas to the stream under nonflood conditions. The reach represented less than 6% of upstream main-channel distance and 2% of upstream basin area. Surface-water discharge increased within the reach by approximately 10%. Mean FMeHg and FTHg fluxes increased within the reach by 23&ndash;27% and 9&ndash;15%, respectively. Mass balances indicated that, under nonflood conditions, the primary supply of water, FMeHg, and FTHg within the reach (excluding upstream surface water influx) was groundwater discharge, rather than tributary transport from wetlands, in-stream MeHg production, or atmospheric Hg deposition. These results illustrate the importance of riparian wetland/floodplain areas as sources of fluvial MeHg and of groundwater Hg transport as a fundamental control on Hg supply to Coastal Plain streams.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Environmental Science and Technology","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"American Chemical Society","publisherLocation":"Washington, D.C.","doi":"10.1021/es301540g","usgsCitation":"Bradley, P.M., Journey, C.A., Lowery, M.A., Brigham, M.E., Burns, D.A., Button, D.T., Chapelle, F.H., Lutz, M., Marvin-DiPasquale, M.C., and Riva-Murray, K., 2012, Shallow groundwater mercury supply in a coastal plain stream: Environmental Science & Technology, v. 46, no. 14, p. 7503-7511, https://doi.org/10.1021/es301540g.","productDescription":"9 p.","startPage":"7503","endPage":"7511","numberOfPages":"9","costCenters":[{"id":13634,"text":"South Atlantic Water Science 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chapelle@usgs.gov","contributorId":1350,"corporation":false,"usgs":true,"family":"Chapelle","given":"Francis","email":"chapelle@usgs.gov","middleInitial":"H.","affiliations":[{"id":559,"text":"South Carolina Water Science Center","active":true,"usgs":true},{"id":13634,"text":"South Atlantic Water Science Center","active":true,"usgs":true}],"preferred":true,"id":466071,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Lutz, Michelle A.","contributorId":32862,"corporation":false,"usgs":true,"family":"Lutz","given":"Michelle A.","affiliations":[],"preferred":false,"id":466076,"contributorType":{"id":1,"text":"Authors"},"rank":8},{"text":"Marvin-DiPasquale, Mark C. 0000-0002-8186-9167 mmarvin@usgs.gov","orcid":"https://orcid.org/0000-0002-8186-9167","contributorId":1485,"corporation":false,"usgs":true,"family":"Marvin-DiPasquale","given":"Mark","email":"mmarvin@usgs.gov","middleInitial":"C.","affiliations":[{"id":438,"text":"National Research Program - Western Branch","active":true,"usgs":true},{"id":37277,"text":"WMA - Earth System Processes Division","active":true,"usgs":true}],"preferred":true,"id":466072,"contributorType":{"id":1,"text":"Authors"},"rank":9},{"text":"Riva-Murray, Karen","contributorId":85650,"corporation":false,"usgs":true,"family":"Riva-Murray","given":"Karen","affiliations":[],"preferred":false,"id":466078,"contributorType":{"id":1,"text":"Authors"},"rank":10}]}}
,{"id":70038239,"text":"70038239 - 2012 - Transport of biologically important nutrients by wind in an eroding cold desert","interactions":[],"lastModifiedDate":"2012-11-14T15:03:20","indexId":"70038239","displayToPublicDate":"2012-08-01T00:00:00","publicationYear":"2012","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":666,"text":"Aeolian Research","active":true,"publicationSubtype":{"id":10}},"title":"Transport of biologically important nutrients by wind in an eroding cold desert","docAbstract":"Wind erosion following fire is an important landscape process that can result in the redistribution of ecologically important soil resources. In this study we evaluated the potential for a fire patch in a desert shrubland to serve as a source of biologically important nutrients to the adjacent, downwind, unburned ecosystem. We analyzed nutrient concentrations (P, K, Ca, Mg, Cu, Fe, Mn, Al) in wind-transported sediments, and soils from burned and adjacent unburned surfaces, collected during the first to second growing seasons after a wildfire that burned in 2007 in Idaho, USA in sagebrush steppe; a type of cold desert shrubland. We also evaluated the timing of potential wind erosion events and weather conditions that might have contributed to nutrient availability in downwind shrubland. Findings indicated that post-fire wind erosion resulted in an important, but transient, addition of nutrients on the downwind shrubland. Aeolian sediments from the burned area were enriched relative to both the up- and down-wind soil and indicated the potential for a fertilization effect through the deposition of the nutrient-enriched sediment during the first, but not second, summer after wildfire. Weather conditions that could have produced nutrient transport events might have provided increased soil moisture necessary to make nutrients accessible for plants in the desert environment. Wind transport of nutrients following fire is likely important in the sagebrush steppe as it could contribute to pulses of resource availability that might, for example, affect plant species differently depending on their phenology, and nutrient- and water-use requirements.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Aeolian Research","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"Elsevier","publisherLocation":"Amsterdam, Netherlands","doi":"10.1016/j.aeolia.2012.01.003","usgsCitation":"Sankey, J.B., Germino, M., Benner, S.G., Glenn, N.F., and Hoover, A.N., 2012, Transport of biologically important nutrients by wind in an eroding cold desert: Aeolian Research, v. 7, p. 17-27, https://doi.org/10.1016/j.aeolia.2012.01.003.","productDescription":"11 p.","startPage":"17","endPage":"27","costCenters":[{"id":290,"text":"Forest and Rangeland Ecosystem Science Center","active":false,"usgs":true}],"links":[{"id":259400,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":254625,"rank":200,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1016/j.aeolia.2012.01.003","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Idaho","volume":"7","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505bb74ae4b08c986b327195","contributors":{"authors":[{"text":"Sankey, Joel B. 0000-0003-3150-4992 jsankey@usgs.gov","orcid":"https://orcid.org/0000-0003-3150-4992","contributorId":3935,"corporation":false,"usgs":true,"family":"Sankey","given":"Joel","email":"jsankey@usgs.gov","middleInitial":"B.","affiliations":[{"id":568,"text":"Southwest Biological Science Center","active":true,"usgs":true}],"preferred":true,"id":463718,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Germino, Matthew J.","contributorId":50029,"corporation":false,"usgs":true,"family":"Germino","given":"Matthew J.","affiliations":[],"preferred":false,"id":463720,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Benner, Shawn G.","contributorId":26562,"corporation":false,"usgs":true,"family":"Benner","given":"Shawn","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":463719,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Glenn, Nancy F.","contributorId":95321,"corporation":false,"usgs":true,"family":"Glenn","given":"Nancy","email":"","middleInitial":"F.","affiliations":[{"id":16201,"text":"Boise State University","active":true,"usgs":false}],"preferred":false,"id":463722,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Hoover, Amber N.","contributorId":75801,"corporation":false,"usgs":true,"family":"Hoover","given":"Amber","email":"","middleInitial":"N.","affiliations":[],"preferred":false,"id":463721,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":70039299,"text":"70039299 - 2012 - Searching for evidence of hydrothermal activity at Apollinaris Mons, Mars","interactions":[],"lastModifiedDate":"2024-04-19T21:58:55.728249","indexId":"70039299","displayToPublicDate":"2012-08-01T00:00:00","publicationYear":"2012","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1963,"text":"Icarus","active":true,"publicationSubtype":{"id":10}},"title":"Searching for evidence of hydrothermal activity at Apollinaris Mons, Mars","docAbstract":"<p id=\"sp010\">A multidisciplinary approach involving various remote sensing instruments is used to investigate Apollinaris Mons, a prominent volcano on Mars, as well as the surrounding plains for signs of prolonged hydrologic and volcanic, and possibly hydrothermal activity. The main findings include (1) evidence from laser altimetry indicating the large thickness (1.5–2&nbsp;km at some locations) of the fan deposits draping the southern flank contrary to previous estimates, coupled with possible layering which point to a significant emplacement phase at Apollinaris Mons, (2) corroboration of Robinson et al. (Robinson, M.S., Mouginis-Mark, P.J., Zimbelman, J.R., Wu, S.S.C., Ablin, K.K., Howington-Kraus, A.E. [1993]. Icarus 104, 301–323) hypothesis regarding the formation of incised valleys on the western flanks by density current erosion which would indicate magma–water interaction or, alternatively, volatile-rich magmas early in the volcano’s history, (3) mounds of diverse geometric shapes, many of which display summit depressions and occur among faults and fractures, possibly marking venting, (4) strong indicators on the flanks of the volcano for lahar events, and possibly, a caldera lake, (5) ubiquitous presence of impact craters displaying fluidized ejecta in both shield-forming (flank and caldera) materials and materials that surround the volcano that are indicative of water-rich target materials at the time of impact, (6) long-term complex association in time among shield-forming materials and Medusae Fossae Formation.</p><p id=\"sp015\">The findings point to a site of extensive volcanic and hydrologic activity with possibly a period of magma–water interaction and hydrothermal activity. Finally, we propose that the mound structures around Apollinaris should be prime targets for further in situ exploration and search for possible exobiological signatures.</p>","language":"English","publisher":"Elsevier","publisherLocation":"Amsterdam, Netherlands","doi":"10.1016/j.icarus.2011.10.022","usgsCitation":"El Maarry, M.R., Dohm, J.M., Marzo, G.A., Fergason, R., Goetz, W., Heggy, E., Pack, A., and Markiewicz, W.J., 2012, Searching for evidence of hydrothermal activity at Apollinaris Mons, Mars: Icarus, v. 217, no. 1, p. 297-314, https://doi.org/10.1016/j.icarus.2011.10.022.","productDescription":"18 p.","startPage":"297","endPage":"314","numberOfPages":"18","costCenters":[{"id":131,"text":"Astrogeology Science Center","active":true,"usgs":true}],"links":[{"id":259368,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"otherGeospatial":"Apollinaris Mons, Mars","volume":"217","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505b8854e4b08c986b316900","contributors":{"authors":[{"text":"El Maarry, M. Ramy","contributorId":97367,"corporation":false,"usgs":true,"family":"El Maarry","given":"M.","email":"","middleInitial":"Ramy","affiliations":[],"preferred":false,"id":466001,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Dohm, James M.","contributorId":83610,"corporation":false,"usgs":true,"family":"Dohm","given":"James","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":465999,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Marzo, Giuseppe A.","contributorId":28851,"corporation":false,"usgs":true,"family":"Marzo","given":"Giuseppe","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":465996,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Fergason, Robin","contributorId":67767,"corporation":false,"usgs":true,"family":"Fergason","given":"Robin","affiliations":[],"preferred":false,"id":465997,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Goetz, Walter","contributorId":74128,"corporation":false,"usgs":true,"family":"Goetz","given":"Walter","email":"","affiliations":[],"preferred":false,"id":465998,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Heggy, Essam","contributorId":96947,"corporation":false,"usgs":true,"family":"Heggy","given":"Essam","email":"","affiliations":[],"preferred":false,"id":466000,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Pack, Andreas","contributorId":100676,"corporation":false,"usgs":true,"family":"Pack","given":"Andreas","email":"","affiliations":[],"preferred":false,"id":466002,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Markiewicz, Wojciech J.","contributorId":13852,"corporation":false,"usgs":true,"family":"Markiewicz","given":"Wojciech","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":465995,"contributorType":{"id":1,"text":"Authors"},"rank":8}]}}
,{"id":70039359,"text":"70039359 - 2012 - Relative value of managed wetlands and tidal marshlands for wintering northern pintails","interactions":[],"lastModifiedDate":"2017-10-30T12:26:36","indexId":"70039359","displayToPublicDate":"2012-08-01T00:00:00","publicationYear":"2012","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2287,"text":"Journal of Fish and Wildlife Management","active":true,"publicationSubtype":{"id":10}},"title":"Relative value of managed wetlands and tidal marshlands for wintering northern pintails","docAbstract":"Northern pintail Anas acuta (hereafter, pintail) populations have declined substantially throughout the western US since the 1970s, largely as a result of converting wetlands to cropland. Managed wetlands have been developed throughout the San Francisco Bay estuaries to provide wildlife habitat, particularly for waterfowl. Many of these areas were historically tidal baylands and plans are underway to remove dikes and restore tidal action. The relationship between tidal baylands and waterfowl populations is poorly understood. Our objective was to provide information on selection and avoidance of managed and tidal marshland by pintails. During 1991&ndash;1993 and 1998&ndash;2000, we radio-marked and relocated 330 female pintails (relocations, <i>n</i> =11,574) at Suisun Marsh, the largest brackish water estuary within San Francisco Bay, to estimate resource selection functions during the nonbreeding months (winter). Using a distance-based modeling approach, we calculated selection functions for different ecological communities (e.g., tidal baylands) and investigated variation explained by time of day (day or night hours) to account for differences in pintail behavior (i.e., foraging vs. roosting). We found strong evidence for selection of managed wetlands. Pintails also avoided tidal marshes and bays and channels. We did not detect differences in selection function between day and night hours for managed wetlands but the degree of avoidance of other habitats varied by time of day. We also found that areas subjected to tidal action did not influence the selection of immediately adjacent managed wetlands. If current management goals include providing habitat for wintering waterfowl populations, particularly pintail, then we recommend wildlife managers focus tidal restoration on areas that are not currently managed wetland and/or improve conditions in areas of managed wetlands to increase local carrying capacities","language":"English","publisher":"U.S. Fish and Wildlife Service","publisherLocation":"Arlington, VA","doi":"10.3996/102011-JFWM-062","usgsCitation":"Coates, P.S., Casazza, M.L., Halstead, B., and Fleskes, J.P., 2012, Relative value of managed wetlands and tidal marshlands for wintering northern pintails: Journal of Fish and Wildlife Management, v. 3, no. 1, p. 98-109, https://doi.org/10.3996/102011-JFWM-062.","productDescription":"12 p.","startPage":"98","endPage":"109","numberOfPages":"12","costCenters":[{"id":552,"text":"San Francisco Bay-Delta","active":false,"usgs":true},{"id":651,"text":"Western Ecological Research Center","active":true,"usgs":true}],"links":[{"id":474393,"rank":1,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.3996/102011-jfwm-062","text":"Publisher Index Page"},{"id":259376,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"California","otherGeospatial":"San Francisco Bay","volume":"3","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505aa69ee4b0c8380cd84f60","contributors":{"authors":[{"text":"Coates, Peter S. 0000-0003-2672-9994 pcoates@usgs.gov","orcid":"https://orcid.org/0000-0003-2672-9994","contributorId":3263,"corporation":false,"usgs":true,"family":"Coates","given":"Peter","email":"pcoates@usgs.gov","middleInitial":"S.","affiliations":[{"id":651,"text":"Western Ecological Research Center","active":true,"usgs":true}],"preferred":true,"id":466138,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Casazza, Michael L. 0000-0002-5636-735X mike_casazza@usgs.gov","orcid":"https://orcid.org/0000-0002-5636-735X","contributorId":2091,"corporation":false,"usgs":true,"family":"Casazza","given":"Michael","email":"mike_casazza@usgs.gov","middleInitial":"L.","affiliations":[{"id":651,"text":"Western Ecological Research Center","active":true,"usgs":true}],"preferred":true,"id":466136,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Halstead, Brian J. 0000-0002-5535-6528 bhalstead@usgs.gov","orcid":"https://orcid.org/0000-0002-5535-6528","contributorId":3051,"corporation":false,"usgs":true,"family":"Halstead","given":"Brian J.","email":"bhalstead@usgs.gov","affiliations":[{"id":200,"text":"Coop Res Unit Seattle","active":true,"usgs":true},{"id":651,"text":"Western Ecological Research Center","active":true,"usgs":true}],"preferred":true,"id":466137,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Fleskes, Joseph P. 0000-0001-5388-6675 joe_fleskes@usgs.gov","orcid":"https://orcid.org/0000-0001-5388-6675","contributorId":1889,"corporation":false,"usgs":true,"family":"Fleskes","given":"Joseph","email":"joe_fleskes@usgs.gov","middleInitial":"P.","affiliations":[{"id":651,"text":"Western Ecological Research Center","active":true,"usgs":true}],"preferred":false,"id":466135,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
]}