{"pageNumber":"2544","pageRowStart":"63575","pageSize":"25","recordCount":184652,"records":[{"id":70201356,"text":"70201356 - 2005 - Utility of Viking Orbiter images and products for Mars mapping","interactions":[],"lastModifiedDate":"2018-12-11T10:10:41","indexId":"70201356","displayToPublicDate":"2005-10-01T10:10:16","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3052,"text":"Photogrammetric Engineering and Remote Sensing","active":true,"publicationSubtype":{"id":10}},"title":"Utility of Viking Orbiter images and products for Mars mapping","docAbstract":"<p><span>This paper reports on mapping procedures developed by the U.S. Geological Survey that use Viking Orbiter imagery and Mars Orbiter Laser Altimeter (MOLA) derived radii to produce topographic data. The use of Mosaiced Digital Image Models (MDIMs), created from Viking Orbiter images, and MOLA data to provide horizontal and vertical control is reviewed. We describe procedures to adapt a commercial digital photogrammetric workstation to work with planetary data.</span></p>","language":"English","publisher":"American Society for Photogrammetry and Remote Sensing","doi":"10.14358/PERS.71.10.1187","usgsCitation":"Rosiek, M.R., Kirk, R.L., Archinal, B.A., Howington-Kraus, E., Hare, T.M., Galuszka, D.M., and Redding, B.L., 2005, Utility of Viking Orbiter images and products for Mars mapping: Photogrammetric Engineering and Remote Sensing, v. 10, p. 1187-1195, https://doi.org/10.14358/PERS.71.10.1187.","productDescription":"9 p.","startPage":"1187","endPage":"1195","costCenters":[{"id":131,"text":"Astrogeology Science Center","active":true,"usgs":true}],"links":[{"id":477646,"rank":0,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.14358/pers.71.10.1187","text":"Publisher Index Page"},{"id":360141,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"otherGeospatial":"Mars","volume":"10","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5c10dadee4b034bf6a7fcc53","contributors":{"authors":[{"text":"Rosiek, Mark R. mrosiek@usgs.gov","contributorId":824,"corporation":false,"usgs":true,"family":"Rosiek","given":"Mark","email":"mrosiek@usgs.gov","middleInitial":"R.","affiliations":[],"preferred":true,"id":753755,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Kirk, Randolph L. 0000-0003-0842-9226 rkirk@usgs.gov","orcid":"https://orcid.org/0000-0003-0842-9226","contributorId":2765,"corporation":false,"usgs":true,"family":"Kirk","given":"Randolph","email":"rkirk@usgs.gov","middleInitial":"L.","affiliations":[{"id":131,"text":"Astrogeology Science Center","active":true,"usgs":true}],"preferred":true,"id":753756,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Archinal, Brent A. 0000-0002-6654-0742 barchinal@usgs.gov","orcid":"https://orcid.org/0000-0002-6654-0742","contributorId":2816,"corporation":false,"usgs":true,"family":"Archinal","given":"Brent","email":"barchinal@usgs.gov","middleInitial":"A.","affiliations":[{"id":131,"text":"Astrogeology Science Center","active":true,"usgs":true}],"preferred":true,"id":753757,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Howington-Kraus, Elpitha 0000-0001-5787-6554 ahowington@usgs.gov","orcid":"https://orcid.org/0000-0001-5787-6554","contributorId":2815,"corporation":false,"usgs":true,"family":"Howington-Kraus","given":"Elpitha","email":"ahowington@usgs.gov","affiliations":[{"id":131,"text":"Astrogeology Science Center","active":true,"usgs":true}],"preferred":true,"id":753758,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Hare, Trent M. 0000-0001-8842-389X thare@usgs.gov","orcid":"https://orcid.org/0000-0001-8842-389X","contributorId":3188,"corporation":false,"usgs":true,"family":"Hare","given":"Trent","email":"thare@usgs.gov","middleInitial":"M.","affiliations":[{"id":131,"text":"Astrogeology Science Center","active":true,"usgs":true}],"preferred":true,"id":753759,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Galuszka, Donna M. 0000-0003-1870-1182 dgaluszka@usgs.gov","orcid":"https://orcid.org/0000-0003-1870-1182","contributorId":3186,"corporation":false,"usgs":true,"family":"Galuszka","given":"Donna","email":"dgaluszka@usgs.gov","middleInitial":"M.","affiliations":[{"id":131,"text":"Astrogeology Science Center","active":true,"usgs":true}],"preferred":true,"id":753760,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Redding, Bonnie L. 0000-0001-8178-1467 bredding@usgs.gov","orcid":"https://orcid.org/0000-0001-8178-1467","contributorId":4798,"corporation":false,"usgs":true,"family":"Redding","given":"Bonnie","email":"bredding@usgs.gov","middleInitial":"L.","affiliations":[{"id":131,"text":"Astrogeology Science Center","active":true,"usgs":true}],"preferred":true,"id":753761,"contributorType":{"id":1,"text":"Authors"},"rank":7}]}}
,{"id":70201528,"text":"70201528 - 2005 - Three in one: Multiscale Hardcopy Depiction of the Mars Surface in True3D","interactions":[],"lastModifiedDate":"2018-12-18T11:43:53","indexId":"70201528","displayToPublicDate":"2005-10-01T09:54:52","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3052,"text":"Photogrammetric Engineering and Remote Sensing","active":true,"publicationSubtype":{"id":10}},"title":"Three in one: Multiscale Hardcopy Depiction of the Mars Surface in True3D","docAbstract":"<p><span>The visualisation of both geospatial Earth data and extra-terrestrial objects is gain- ing increasing importance. Until recently, hardcopy displays were confined to mostly static, two-dimensional or pseudo-three-dimensional depictions. The various effects offered by lenticular foil technology allow the generation of flip-image effects, short animations, and true-3D displays in hardcopy form. One advantage of this method is that these effects can be spontaneously viewed with the unaided eye. This article gives a concise overview of the lenticular foil technology (hereafter lenticular technology) and describes the production of the lenticular display presented on the cover of this month's issue of PE&amp;RS.</span></p>","language":"English","publisher":"ASPRS","issn":"0099-1112","usgsCitation":"Buchroithner, M., Grundemann, T., Kirk, R.L., and Habermann, K., 2005, Three in one: Multiscale Hardcopy Depiction of the Mars Surface in True3D: Photogrammetric Engineering and Remote Sensing, v. 71, no. 10, p. 1105-1108.","productDescription":"4 p.","startPage":"1105","endPage":"1108","costCenters":[{"id":131,"text":"Astrogeology Science Center","active":true,"usgs":true}],"links":[{"id":360357,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"otherGeospatial":"Mars","volume":"71","issue":"10","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5c18c426e4b006c4f856ace6","contributors":{"authors":[{"text":"Buchroithner, Manfred","contributorId":211565,"corporation":false,"usgs":false,"family":"Buchroithner","given":"Manfred","email":"","affiliations":[],"preferred":false,"id":754398,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Grundemann, Thomas","contributorId":211566,"corporation":false,"usgs":false,"family":"Grundemann","given":"Thomas","email":"","affiliations":[],"preferred":false,"id":754399,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Kirk, Randolph L. 0000-0003-0842-9226 rkirk@usgs.gov","orcid":"https://orcid.org/0000-0003-0842-9226","contributorId":2765,"corporation":false,"usgs":true,"family":"Kirk","given":"Randolph","email":"rkirk@usgs.gov","middleInitial":"L.","affiliations":[{"id":131,"text":"Astrogeology Science Center","active":true,"usgs":true}],"preferred":true,"id":754400,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Habermann, Klaus","contributorId":211567,"corporation":false,"usgs":false,"family":"Habermann","given":"Klaus","email":"","affiliations":[],"preferred":false,"id":754401,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70201355,"text":"70201355 - 2005 - Initial results of rover localization and topographic mapping for the 2003 mars exploration rover mission","interactions":[],"lastModifiedDate":"2019-02-25T09:44:03","indexId":"70201355","displayToPublicDate":"2005-10-01T09:53:37","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3052,"text":"Photogrammetric Engineering and Remote Sensing","active":true,"publicationSubtype":{"id":10}},"title":"Initial results of rover localization and topographic mapping for the 2003 mars exploration rover mission","docAbstract":"<p><span>This paper presents the initial results of lander and rover localization and topographic mapping of the MER 2003 mission (by Sol 225 for Spirit and Sol 206 for Opportunity). The Spirit rover has traversed a distance of 3.2 km (actual distance traveled instead of odometry) and Opportunity at 1.2 km. We localized the landers in the Gusev Crater and on the Meridiani Planum using two-way Doppler radio positioning technology and cartographic triangulations through landmarks visible in both orbital and ground images. Additional high-resolution orbital images were taken to verify the determined lander positions. Visual odometry and bundle-adjustment technologies were applied to overcome wheel slippages, azimuthal angle drift and other navigation errors (as large as 21 percent). We generated timely topographic products including 68 orthophoto maps and 3D Digital Terrain Models, eight horizontal rover traverse maps, vertical traverse profiles up to Sol 214 for Spirit and Sol 62 for Opportunity, and five 3D crater models. A web-based landing-site Geographic Information System (GIS) has been set up at The Ohio State University to update and disseminate the daily localization and topographic information to support tactical and strategic operations of the mission. Also described in this paper are applications of the data for science operations planning, geological traverse survey, survey of wind-related features, and other science applications. The majority of the instruments onboard both rovers are healthy at this moment, and they will continue to explore the two landing sites on the Martian surface. We expect to report further localization and topographic mapping results to be achieved in the rest of the mission period and in post-mission data processing.</span></p>","language":"English","publisher":"American Society for Photogrammetry and Remote Sensing","doi":"10.14358/PERS.71.10.1129","usgsCitation":"Li, R., Squyres, S.W., Arvidson, R.E., Archinal, B.A., Bell, J., Cheng, Y., Crumpler, L.S., Des Marais, D.J., Di, K., Ely, T.A., Golombek, M.P., Graat, E., Grant, J., Guinn, J., Johnson, A.C., Greeley, R., Kirk, R.L., Maimone, M., Soderblom, L.A., Thompson, S.D., Wang, J., Whelley, P.L., and Xu, F., 2005, Initial results of rover localization and topographic mapping for the 2003 mars exploration rover mission: Photogrammetric Engineering and Remote Sensing, v. 10, p. 1129-1142, https://doi.org/10.14358/PERS.71.10.1129.","productDescription":"14 p.","startPage":"1129","endPage":"1142","costCenters":[{"id":131,"text":"Astrogeology Science Center","active":true,"usgs":true}],"links":[{"id":477647,"rank":0,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.14358/pers.71.10.1129","text":"Publisher Index Page"},{"id":360136,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"otherGeospatial":"Mars","volume":"10","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5c10dadee4b034bf6a7fcc55","contributors":{"authors":[{"text":"Li, Rongxing","contributorId":211216,"corporation":false,"usgs":false,"family":"Li","given":"Rongxing","email":"","affiliations":[],"preferred":false,"id":753732,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Squyres, Steven W.","contributorId":10537,"corporation":false,"usgs":true,"family":"Squyres","given":"Steven","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":753733,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Arvidson, Raymond E.","contributorId":106626,"corporation":false,"usgs":false,"family":"Arvidson","given":"Raymond","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":753734,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Archinal, Brent A. 0000-0002-6654-0742 barchinal@usgs.gov","orcid":"https://orcid.org/0000-0002-6654-0742","contributorId":2816,"corporation":false,"usgs":true,"family":"Archinal","given":"Brent","email":"barchinal@usgs.gov","middleInitial":"A.","affiliations":[{"id":131,"text":"Astrogeology Science Center","active":true,"usgs":true}],"preferred":true,"id":753735,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Bell, James F.  III","contributorId":195298,"corporation":false,"usgs":false,"family":"Bell","given":"James F. ","suffix":"III","affiliations":[{"id":34032,"text":"School of Earth and Space Exploration, Arizona State University, Tempe, AZ 85287","active":true,"usgs":false}],"preferred":false,"id":753736,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Cheng, Yang","contributorId":211352,"corporation":false,"usgs":false,"family":"Cheng","given":"Yang","email":"","affiliations":[],"preferred":false,"id":753737,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Crumpler, Larry S.","contributorId":196268,"corporation":false,"usgs":false,"family":"Crumpler","given":"Larry","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":753738,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Des Marais, David J.","contributorId":211218,"corporation":false,"usgs":false,"family":"Des Marais","given":"David","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":753739,"contributorType":{"id":1,"text":"Authors"},"rank":8},{"text":"Di, 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Eric","contributorId":211354,"corporation":false,"usgs":false,"family":"Graat","given":"Eric","email":"","affiliations":[],"preferred":false,"id":753743,"contributorType":{"id":1,"text":"Authors"},"rank":12},{"text":"Grant, John","contributorId":210872,"corporation":false,"usgs":false,"family":"Grant","given":"John","affiliations":[],"preferred":false,"id":753744,"contributorType":{"id":1,"text":"Authors"},"rank":13},{"text":"Guinn, Joe","contributorId":211220,"corporation":false,"usgs":false,"family":"Guinn","given":"Joe","email":"","affiliations":[],"preferred":false,"id":753745,"contributorType":{"id":1,"text":"Authors"},"rank":14},{"text":"Johnson, Andrew C.","contributorId":169346,"corporation":false,"usgs":false,"family":"Johnson","given":"Andrew","email":"","middleInitial":"C.","affiliations":[{"id":7217,"text":"Bureau of Land Management","active":true,"usgs":false}],"preferred":true,"id":753746,"contributorType":{"id":1,"text":"Authors"},"rank":15},{"text":"Greeley, 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lsoderblom@usgs.gov","orcid":"https://orcid.org/0000-0002-0917-853X","contributorId":2721,"corporation":false,"usgs":true,"family":"Soderblom","given":"Laurence","email":"lsoderblom@usgs.gov","middleInitial":"A.","affiliations":[{"id":131,"text":"Astrogeology Science Center","active":true,"usgs":true}],"preferred":true,"id":753750,"contributorType":{"id":1,"text":"Authors"},"rank":19},{"text":"Thompson, Shane D.","contributorId":22079,"corporation":false,"usgs":true,"family":"Thompson","given":"Shane","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":753751,"contributorType":{"id":1,"text":"Authors"},"rank":20},{"text":"Wang, Jue","contributorId":211355,"corporation":false,"usgs":false,"family":"Wang","given":"Jue","email":"","affiliations":[],"preferred":false,"id":753752,"contributorType":{"id":1,"text":"Authors"},"rank":21},{"text":"Whelley, Patrick L.","contributorId":77288,"corporation":false,"usgs":true,"family":"Whelley","given":"Patrick","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":753753,"contributorType":{"id":1,"text":"Authors"},"rank":22},{"text":"Xu, Fengliang","contributorId":211356,"corporation":false,"usgs":false,"family":"Xu","given":"Fengliang","email":"","affiliations":[],"preferred":false,"id":753754,"contributorType":{"id":1,"text":"Authors"},"rank":23}]}}
,{"id":70201354,"text":"70201354 - 2005 - Joint analysis of visible and infrared images","interactions":[],"lastModifiedDate":"2018-12-11T09:24:52","indexId":"70201354","displayToPublicDate":"2005-10-01T09:24:28","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3052,"text":"Photogrammetric Engineering and Remote Sensing","active":true,"publicationSubtype":{"id":10}},"title":"Joint analysis of visible and infrared images","docAbstract":"<p>Analysis of data combining daytime visible reflected, daytime IR emitted, and nighttime<span>&nbsp;IR&nbsp;</span>emitted images allows us to isolate the physical effects of topography, albedo, and thermal inertia. To a good approximation, these physical influences interact linearly so that maps showing topographic shading, albedo, and relative thermal inertia can be produced by simple algebraic manipulation of the co-registered images. The shading map resembles an airbrush, shaded relief portrayal of the surface, and can be used as the input for quantitative reconstruction of topography by photoclinometry (shape-fromshading). We demonstrate the method with imagery from the<span>&nbsp;NASA 2001&nbsp;</span>Mars Odyssey Thermal Emission Imaging System (THEMIS), a dataset that could support mapping most of Mars in this way at 100 m resolution<span>.</span></p>","language":"English","publisher":"American Society for Photogrammetry and Remote Sensing","doi":"10.14358/PERS.71.10.1167","usgsCitation":"Kirk, R.L., Soderblom, L.A., Cushing, G.E., and Tituus, T.A., 2005, Joint analysis of visible and infrared images: Photogrammetric Engineering and Remote Sensing, v. 10, p. 1167-1178, https://doi.org/10.14358/PERS.71.10.1167.","productDescription":"12 p.","startPage":"1167","endPage":"1178","costCenters":[{"id":131,"text":"Astrogeology Science Center","active":true,"usgs":true}],"links":[{"id":477648,"rank":0,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.14358/pers.71.10.1167","text":"Publisher Index Page"},{"id":360135,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"10","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5c10dadee4b034bf6a7fcc57","contributors":{"authors":[{"text":"Kirk, Randolph L. 0000-0003-0842-9226 rkirk@usgs.gov","orcid":"https://orcid.org/0000-0003-0842-9226","contributorId":2765,"corporation":false,"usgs":true,"family":"Kirk","given":"Randolph","email":"rkirk@usgs.gov","middleInitial":"L.","affiliations":[{"id":131,"text":"Astrogeology Science Center","active":true,"usgs":true}],"preferred":true,"id":753728,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Soderblom, Laurence A. 0000-0002-0917-853X lsoderblom@usgs.gov","orcid":"https://orcid.org/0000-0002-0917-853X","contributorId":2721,"corporation":false,"usgs":true,"family":"Soderblom","given":"Laurence","email":"lsoderblom@usgs.gov","middleInitial":"A.","affiliations":[{"id":131,"text":"Astrogeology Science Center","active":true,"usgs":true}],"preferred":true,"id":753729,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Cushing, Glen E. 0000-0002-9673-8207 gcushing@usgs.gov","orcid":"https://orcid.org/0000-0002-9673-8207","contributorId":175449,"corporation":false,"usgs":true,"family":"Cushing","given":"Glen","email":"gcushing@usgs.gov","middleInitial":"E.","affiliations":[{"id":131,"text":"Astrogeology Science Center","active":true,"usgs":true}],"preferred":true,"id":753730,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Tituus, Timothy A.","contributorId":211351,"corporation":false,"usgs":false,"family":"Tituus","given":"Timothy","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":753731,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70201352,"text":"70201352 - 2005 - HRSC on Mars Express: Photogrammetric and cartographic research","interactions":[],"lastModifiedDate":"2018-12-11T09:10:09","indexId":"70201352","displayToPublicDate":"2005-10-01T09:09:45","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3052,"text":"Photogrammetric Engineering and Remote Sensing","active":true,"publicationSubtype":{"id":10}},"title":"HRSC on Mars Express: Photogrammetric and cartographic research","docAbstract":"<p>The High Resolution Stereo Camera (HRSC) on the European spacecraft Mars Express is the first camera on a planetary mission especially designed for photogrammetric and cartographic purposes. Since January 2004 the camera has been taking image data from the Martian surface, characterized by high-resolution, stereo capability and color. These data provide an enormous potential for the generation of 3D surface models, color orthoimages, topographic and thematic maps, and additional products. The image data acquired undergo calibration and systematic processing to orthoimages and 3D data products. Within the international HRSC Science Team the members of the Photogrammetric/Cartographic Working Group are concerned with further refinements in order to achieve highest quality data products. These activities comprise improvements of the exterior orientation of the camera, various approaches to enhance DTM quality, and the generation of maps in the standard scale of 1:200 000 and larger scales as well. The paper reports on these activities and the results achieved so far<span>.</span></p>","language":"English","publisher":"American Society for Photogrammetry and Remote Sensing","doi":"10.14358/PERS.71.10.1153","usgsCitation":"Albertz, J., Attwenger, M., Barrett, J.M., Casley, S., Dorninger, P., Dorrer, E., Ebner, H., Gehrke, S., Giese, B., Gwinner, K., Heipke, C., Howington-Kraus, E., Kirk, R.L., Lehmann, H., Mayer, H., Muller, J., Oberst, J., Ostrovskiy, A., Renter, J., Reznik, S., Schmidt, R.G., Scholten, F., Spiegel, M., Stilla, U., Wahlisch, M., and Neukum, G., 2005, HRSC on Mars Express: Photogrammetric and cartographic research: Photogrammetric Engineering and Remote Sensing, v. 10, p. 1153-1166, https://doi.org/10.14358/PERS.71.10.1153.","productDescription":"14 p.","startPage":"1153","endPage":"1166","costCenters":[{"id":131,"text":"Astrogeology Science Center","active":true,"usgs":true}],"links":[{"id":477649,"rank":0,"type":{"id":40,"text":"Open Access Publisher Index 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rkirk@usgs.gov","orcid":"https://orcid.org/0000-0003-0842-9226","contributorId":2765,"corporation":false,"usgs":true,"family":"Kirk","given":"Randolph","email":"rkirk@usgs.gov","middleInitial":"L.","affiliations":[{"id":131,"text":"Astrogeology Science Center","active":true,"usgs":true}],"preferred":true,"id":753702,"contributorType":{"id":1,"text":"Authors"},"rank":13},{"text":"Lehmann, Hartmut","contributorId":211339,"corporation":false,"usgs":false,"family":"Lehmann","given":"Hartmut","email":"","affiliations":[],"preferred":false,"id":753703,"contributorType":{"id":1,"text":"Authors"},"rank":14},{"text":"Mayer, Helmut","contributorId":211340,"corporation":false,"usgs":false,"family":"Mayer","given":"Helmut","email":"","affiliations":[],"preferred":false,"id":753704,"contributorType":{"id":1,"text":"Authors"},"rank":15},{"text":"Muller, 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Uwe","contributorId":211348,"corporation":false,"usgs":false,"family":"Stilla","given":"Uwe","email":"","affiliations":[],"preferred":false,"id":753713,"contributorType":{"id":1,"text":"Authors"},"rank":24},{"text":"Wahlisch, Marita","contributorId":211349,"corporation":false,"usgs":false,"family":"Wahlisch","given":"Marita","email":"","affiliations":[],"preferred":false,"id":753714,"contributorType":{"id":1,"text":"Authors"},"rank":25},{"text":"Neukum, Gerhard","contributorId":211350,"corporation":false,"usgs":false,"family":"Neukum","given":"Gerhard","email":"","affiliations":[],"preferred":false,"id":753715,"contributorType":{"id":1,"text":"Authors"},"rank":26}]}}
,{"id":70184386,"text":"70184386 - 2005 - The U-tube: A novel system for acquiring borehole fluid samples from a deep geologic CO2 sequestration experiment","interactions":[],"lastModifiedDate":"2024-06-06T16:42:09.667272","indexId":"70184386","displayToPublicDate":"2005-10-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":6453,"text":"Journal of Geophysical Research Solid Earth","active":true,"publicationSubtype":{"id":10}},"title":"The U-tube: A novel system for acquiring borehole fluid samples from a deep geologic CO2 sequestration experiment","docAbstract":"<p><span>A novel system has been deployed to obtain geochemical samples of water and gas, at in situ pressure, during a geologic CO</span><sub>2</sub><span> sequestration experiment conducted in the Frio brine aquifer in Liberty County, Texas. Project goals required high-frequency recovery of representative and uncontaminated aliquots of a rapidly changing two-phase fluid (supercritical CO</span><sub>2</sub><span> and brine) fluid from 1.5 km depth. The data sets collected, using both the liquid and gas portions of the downhole samples, provide insights into the coupled hydrogeochemical issues affecting CO</span><sub>2</sub><span>sequestration in brine-filled formations. While the basic premise underlying the U-tube sampler is not new, the system is unique because careful consideration was given to the processing of the recovered two-phase fluids. In particular, strain gauges mounted beneath the high-pressure surface sample cylinders measured the ratio of recovered brine to supercritical CO</span><sub>2</sub><span>. A quadrupole mass spectrometer provided real-time gas analysis for perfluorocarbon and noble gas tracers that were injected along with the CO</span><sub>2</sub><span>. The U-tube successfully acquired frequent samples, facilitating accurate delineation of the arrival of the CO</span><sub>2</sub><span> plume, and on-site analysis revealed rapid changes in geochemical conditions.</span></p>","language":"English","publisher":"American Geophysical Union","doi":"10.1029/2005JB003735","usgsCitation":"Freifeild, B.M., Trautz, R.C., Kharaka, Y.K., Phelps, T.J., Myer, L.R., Hovorka, S.D., and Collins, D.J., 2005, The U-tube: A novel system for acquiring borehole fluid samples from a deep geologic CO2 sequestration experiment: Journal of Geophysical Research Solid Earth, v. 110, no. B10, B10203, 10 p., https://doi.org/10.1029/2005JB003735.","productDescription":"B10203, 10 p.","costCenters":[{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":477651,"rank":2,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1029/2005jb003735","text":"Publisher Index Page"},{"id":337061,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"110","issue":"B10","noUsgsAuthors":false,"publicationDate":"2005-10-11","publicationStatus":"PW","scienceBaseUri":"58c1263ee4b014cc3a3d34b6","contributors":{"authors":[{"text":"Freifeild, Barry M.","contributorId":42444,"corporation":false,"usgs":false,"family":"Freifeild","given":"Barry","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":681264,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Trautz, Robert C.","contributorId":171754,"corporation":false,"usgs":false,"family":"Trautz","given":"Robert","email":"","middleInitial":"C.","affiliations":[{"id":26941,"text":"Electric Power Research Institute, Palo Alto, CA","active":true,"usgs":false}],"preferred":false,"id":681265,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Kharaka, Yousif K. 0000-0001-9861-8260 ykharaka@usgs.gov","orcid":"https://orcid.org/0000-0001-9861-8260","contributorId":1928,"corporation":false,"usgs":true,"family":"Kharaka","given":"Yousif","email":"ykharaka@usgs.gov","middleInitial":"K.","affiliations":[{"id":438,"text":"National Research Program - Western Branch","active":true,"usgs":true}],"preferred":true,"id":681266,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Phelps, Tommy J.","contributorId":175588,"corporation":false,"usgs":false,"family":"Phelps","given":"Tommy","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":681267,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Myer, Larry R.","contributorId":177239,"corporation":false,"usgs":false,"family":"Myer","given":"Larry","email":"","middleInitial":"R.","affiliations":[{"id":6670,"text":"Lawrence Berkeley National Laboratory, Berkeley, CA","active":true,"usgs":false}],"preferred":false,"id":681268,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Hovorka, Susan D.","contributorId":175572,"corporation":false,"usgs":false,"family":"Hovorka","given":"Susan","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":681269,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Collins, Daniel J.","contributorId":177241,"corporation":false,"usgs":false,"family":"Collins","given":"Daniel","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":681270,"contributorType":{"id":1,"text":"Authors"},"rank":7}]}}
,{"id":70159119,"text":"70159119 - 2005 - Satellite imagery maps Hurricane Katrina-induced flooding and oil slicks","interactions":[],"lastModifiedDate":"2015-10-15T13:30:16","indexId":"70159119","displayToPublicDate":"2005-10-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3879,"text":"Eos, Earth and Space Science News","active":true,"publicationSubtype":{"id":10}},"title":"Satellite imagery maps Hurricane Katrina-induced flooding and oil slicks","docAbstract":"<p>In the early morning of 29 August 2005, Hurricane Katrina made landfall near Buras, Louisiana, as a Category 4 hurricane. With wind speeds of about 233 kilometers per hour, a storm surge of 8.5 meters, and heavy rains, Katrina pounded the U.S. Gulf Coast states of Alabama, Louisiana, and Mississippi with lifethreatening flooding and destruction. Katrina's high winds and storm surge breached the levees protecting New Orleans, a city located below sea level, and flooded approximately 80% of the city.</p>\n<p>Katrina also caused major damage to the region's oil and natural gas production and refining capabilities. On 2 September 2005, the Associated Press reported that Katrina had damaged 58 oil platforms, 30 of which were reported lost; one damaged platform had been blown nearly 100 km from its original location.</p>","language":"English","publisher":"American Geophysical Union","doi":"10.1029/2005EO410003","usgsCitation":"Rykhus, R.P., 2005, Satellite imagery maps Hurricane Katrina-induced flooding and oil slicks: Eos, Earth and Space Science News, v. 86, no. 41, p. 381-382, https://doi.org/10.1029/2005EO410003.","productDescription":"2 p.","startPage":"381","endPage":"382","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":222,"text":"Earth Resources Observation and Science (EROS) Center","active":true,"usgs":true}],"links":[{"id":477650,"rank":0,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1029/2005eo410003","text":"Publisher Index Page"},{"id":309942,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"86","issue":"41","noUsgsAuthors":false,"publicationDate":"2011-06-03","publicationStatus":"PW","scienceBaseUri":"5620ce9fe4b06217fc478b18","contributors":{"authors":[{"text":"Rykhus, Russell P.","contributorId":27337,"corporation":false,"usgs":true,"family":"Rykhus","given":"Russell","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":577647,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70192241,"text":"70192241 - 2005 - Genetic typing of infectious hematopoietic necrosis virus","interactions":[],"lastModifiedDate":"2018-07-17T15:08:31","indexId":"70192241","displayToPublicDate":"2005-10-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"Genetic typing of infectious hematopoietic necrosis virus","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Health and diseases of aquatic organisms: Bilateral perspectives","largerWorkSubtype":{"id":12,"text":"Conference publication"},"conferenceTitle":"Proceedings of the second bilateral conference between Russia and the United States","conferenceDate":"September 21-28, 2003","conferenceLocation":"Shepherdstown, WV.  ","language":"English","publisher":"Michigan State University","publisherLocation":"East Lansing, MI","usgsCitation":"Kurath, G., Garver, A.K., Batts, W.N., and Emmenegger, E.J., 2005, Genetic typing of infectious hematopoietic necrosis virus, <i>in</i> Health and diseases of aquatic organisms: Bilateral perspectives, Shepherdstown, WV.  , September 21-28, 2003, p. 195-206.","productDescription":"12 p.","startPage":"195","endPage":"206","costCenters":[{"id":654,"text":"Western Fisheries Research Center","active":true,"usgs":true}],"links":[{"id":347161,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"59eeffade4b0220bbd988fd8","contributors":{"editors":[{"text":"Cipriano, Rocco C. rcipriano@usgs.gov","contributorId":2487,"corporation":false,"usgs":true,"family":"Cipriano","given":"Rocco","email":"rcipriano@usgs.gov","middleInitial":"C.","affiliations":[],"preferred":true,"id":714968,"contributorType":{"id":2,"text":"Editors"},"rank":1},{"text":"Shchelkunov, I.S.","contributorId":21326,"corporation":false,"usgs":true,"family":"Shchelkunov","given":"I.S.","email":"","affiliations":[],"preferred":false,"id":714969,"contributorType":{"id":2,"text":"Editors"},"rank":2},{"text":"Faisal, M.","contributorId":19116,"corporation":false,"usgs":true,"family":"Faisal","given":"M.","affiliations":[],"preferred":false,"id":714970,"contributorType":{"id":2,"text":"Editors"},"rank":3}],"authors":[{"text":"Kurath, Gael 0000-0003-3294-560X gkurath@usgs.gov","orcid":"https://orcid.org/0000-0003-3294-560X","contributorId":2629,"corporation":false,"usgs":true,"family":"Kurath","given":"Gael","email":"gkurath@usgs.gov","affiliations":[{"id":654,"text":"Western Fisheries Research Center","active":true,"usgs":true}],"preferred":true,"id":714964,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Garver, A. K. K.","contributorId":118318,"corporation":false,"usgs":true,"family":"Garver","given":"A.","suffix":"K.","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":714965,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Batts, William N. 0000-0002-6469-9004 bbatts@usgs.gov","orcid":"https://orcid.org/0000-0002-6469-9004","contributorId":3815,"corporation":false,"usgs":true,"family":"Batts","given":"William","email":"bbatts@usgs.gov","middleInitial":"N.","affiliations":[{"id":654,"text":"Western Fisheries Research Center","active":true,"usgs":true}],"preferred":true,"id":714966,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Emmenegger, Eveline J. 0000-0001-5217-6030 eemmenegger@usgs.gov","orcid":"https://orcid.org/0000-0001-5217-6030","contributorId":2434,"corporation":false,"usgs":true,"family":"Emmenegger","given":"Eveline","email":"eemmenegger@usgs.gov","middleInitial":"J.","affiliations":[{"id":654,"text":"Western Fisheries Research Center","active":true,"usgs":true}],"preferred":true,"id":714967,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":72368,"text":"sir20055174 - 2005 - Historical perspective of statewide streamflows during the 2002 and 1977 droughts in Colorado","interactions":[],"lastModifiedDate":"2012-02-02T00:14:01","indexId":"sir20055174","displayToPublicDate":"2005-09-29T00:00:00","publicationYear":"2005","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":"2005-5174","title":"Historical perspective of statewide streamflows during the 2002 and 1977 droughts in Colorado","docAbstract":"Since 1890, Colorado has experienced a number of widespread drought periods; the most recent statewide drought began during 1999 and includes 2002, a year characterized by precipitation, snowpack accumulation, and streamflows that were much lower than normal. Because the drought of 2002 had a substantial effect on streamflows in Colorado, the U.S. Geological Survey, in cooperation with the Colorado Water Conservation Board, began a study in 2004 to analyze statewide streamflows during 2002 and develop a historical perspective of those streamflows. The purpose of this report is to describe an analysis of streamflows recorded throughout Colorado during the drought of 2002, as well as other drought years such as 1977, and to provide some historical perspective of drought-diminished streamflows in Colorado. \r\n\r\nBecause most streamflows in Colorado are derived from melting of mountain snowpacks during April through July, streamflows primarily were analyzed for the snowmelt (high-flow) period, but streamflows also were analyzed for the winter (low-flow) period. The snowmelt period is defined as April 1 through September 30 and the winter period is defined as October 1 through March 31. Historical daily average streamflows were analyzed on the basis of 7, 30, 90, and 180 consecutive-day periods (N-day) for 154 selected stations in Colorado. Methods used for analysis of the N-day snowmelt and winter streamflows include evaluation of trends in the historical streamflow records, computation of the rank of each annual N-day streamflow value for each station, analysis for years other than 2002 and 1977 with drought-diminished streamflows, and frequency analysis (on the basis of nonexceedance probability) of the 180-day streamflows. \r\n\r\nRanking analyses for the N-day snowmelt streamflows indicated that streamflows during 2002 were ranked as the lowest or second lowest historical values at 114-123 stations, or about 74-80 percent of the stations; by comparison, the N-day snowmelt streamflows during 1977 were ranked as the lowest or second lowest historical values at 69-87 stations, or about 47-59 percent of the stations. Many of the stations in the mountainous headwaters where snowmelt streamflows were ranked lowest during 2002 were ranked second lowest during 1977. These results indicate that snowmelt streamflows during 2002 were considerably more diminished than those during 1977. \r\n\r\nThe 180-day snowmelt streamflows were ranked among the five lowest historical values at about 90 percent of the stations during 2002 and were ranked among the five lowest historical values at about 77 percent of the stations during 1977. Other years during which the 180-day snowmelt streamflows were ranked among the five lowest values at a substantial percentage of stations include 1934, 1954, 1963, and 1981, but the percentages of stations with 180-day snowmelt streamflows ranked among the five lowest values were smaller during those years than during 2002 and 1977.\r\n\r\nFrequency analysis of snowmelt streamflows indicated that recurrence intervals for the 180-day snowmelt streamflows during 2002 were greater than 50 years for about 57 percent of the stations and were more than 100 years for about 14 percent of the stations. By comparison, recurrence intervals for the 180-day snowmelt streamflows during 1977 were greater than 50 years only for about 15 percent of the stations and were more than 100 years only for about 1 percent of the stations. Generally, snowmelt streamflows during 2002 were more diminished and have higher recurrence intervals than snowmelt streamflows during 1977. \r\n\r\nThe N-day winter streamflows during 2002 and 1977 were not ranked among the five lowest historical values at about 86-103 stations, or about 58-70 percent of the stations, compared to about 10-27 percent of the stations for the N-day snowmelt streamflows. These results indicate that winter streamflows during the 2002 and 1977 droughts were diminished to a lesser extent than t","language":"ENGLISH","doi":"10.3133/sir20055174","usgsCitation":"Kuhn, G., 2005, Historical perspective of statewide streamflows during the 2002 and 1977 droughts in Colorado: U.S. Geological Survey Scientific Investigations Report 2005-5174, 90 p., https://doi.org/10.3133/sir20055174.","productDescription":"90 p.","costCenters":[],"links":[{"id":193101,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":7330,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/sir/2005/5174/","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae0e4b07f02db6884df","contributors":{"authors":[{"text":"Kuhn, Gerhard","contributorId":102080,"corporation":false,"usgs":true,"family":"Kuhn","given":"Gerhard","email":"","affiliations":[],"preferred":false,"id":285497,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":72373,"text":"fs20053107 - 2005 - Southern California landslides-an overview","interactions":[],"lastModifiedDate":"2015-11-17T11:14:12","indexId":"fs20053107","displayToPublicDate":"2005-09-29T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":313,"text":"Fact Sheet","code":"FS","onlineIssn":"2327-6932","printIssn":"2327-6916","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2005-3107","title":"Southern California landslides-an overview","docAbstract":"<p>Southern California lies astride a major tectonic plate boundary defined by the San Andreas Fault and numerous related faults that are spread across a broad region. This dynamic tectonic environment has created a spectacular landscape of rugged mountains and steep-walled valleys that compose much of the region&rsquo;s scenic beauty. Unfortunately, this extraordinary landscape also presents serious geologic hazards. Just as tectonic forces are steadily pushing the landscape upward, gravity is relentlessly tugging it downward. When gravity prevails, landslides can occur.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/fs20053107","collaboration":"Prepared in Cooperation with the California Geological Survey","usgsCitation":"Water Resources Division, U.S. Geological Survey, 2005, Southern California landslides-an overview (Version 1.0): U.S. Geological Survey Fact Sheet 2005-3107, 4 p., https://doi.org/10.3133/fs20053107.","productDescription":"4 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":120893,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/fs_2005_3107.jpg"},{"id":7335,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/fs/2005/3107/","linkFileType":{"id":5,"text":"html"}},{"id":311420,"rank":101,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/fs/2005/3107/pdf/FS-3107.pdf"}],"country":"United States","state":"California","edition":"Version 1.0","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e6e4b07f02db5e723b","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":534743,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":72369,"text":"sir20055167 - 2005 - Effects of emission reductions at the Hayden powerplant on precipitation, snowpack, and surface-water chemistry in the Mount Zirkel Wilderness Area, Colorado, 1995-2003","interactions":[],"lastModifiedDate":"2023-01-04T20:17:31.795702","indexId":"sir20055167","displayToPublicDate":"2005-09-29T00:00:00","publicationYear":"2005","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":"2005-5167","title":"Effects of emission reductions at the Hayden powerplant on precipitation, snowpack, and surface-water chemistry in the Mount Zirkel Wilderness Area, Colorado, 1995-2003","docAbstract":"<p class=\"text\">Precipitation, snowpack, and surface-water samples collected during 1995-2003 were analyzed to evaluate the effects of emission reductions at the Hayden powerplant on water chemistry in the Mount Zirkel Wilderness Area. The Hayden powerplant, one of two large coal-fired powerplants in the Yampa Valley, was retrofitted with control systems during late 1998 and 1999 to reduce emissions of sulfur dioxide and nitrogen oxide--the primary precursors of haze and acidic precipitation. The U.S. Geological Survey, in cooperation with the Colorado Department of Public Health and Environment, evaluated three water-chemistry data sets: wet-only precipitation chemistry from the National Atmospheric Deposition Program, snowpack chemistry from the Rocky Mountain snowpack network, and surface-water chemistry from a U.S. Geological Survey long-term lakes monitoring program. Concentrations and deposition rates of selected constituents were compared for the periods before and after emission reductions at the Hayden powerplant. Data collected during 1995-98 were used to represent the pre-control period, and data collected during 2000-2003 were used to represent the post-control period.</p><p class=\"text\">Ten stations in the National Atmospheric Deposition Program were evaluated including two that were directly downwind from the Hayden powerplant (Dry Lake and Buffalo Pass) and eight that were upwind or more distant (more than 100 kilometers) from the powerplant. Precipitation amount at all 10 precipitation stations was lower in the post-control period than the pre-control period as a result of a regional drought that persisted during the post-control period. In contrast to precipitation amount, there was no consistent pattern of change in sulfate concentrations between periods, indicating that the drought did not have a concentrating effect on sulfate or that trends in regional sulfur dioxide emissions masked its influence. Sulfate concentrations increased at three stations between periods, remained the same at three stations, and decreased at four stations. The largest change in average annual sulfate concentrations occurred at the two precipitation stations downwind from the Hayden powerplant, decreasing by 3.3 microequivalents per liter at Dry Lake and by 2.2 microequivalents per liter at Buffalo Pass. Declines in annual sulfate deposition also were greater at Dry Lake (3.4 kilograms per hectare) and Buffalo Pass (3.3 kilograms per hectare) than at the other stations, which ranged from 0.2 to 1.7 kilograms per hectare. These results indicate that emission reductions at the Hayden powerplant have been a factor in declines in atmospheric deposition of sulfate downwind from the powerplant. Nitrate, ammonium, and base-cation concentrations, in contrast to sulfate, were higher in the post-control period than the pre-control period at all 10 stations, most likely due to a concentrating effect of the drought.</p><p class=\"text\">Twenty-two snowpack sites in the Rocky Mountain snowpack network were evaluated including 4 sites that were located directly downwind from the Hayden powerplant and 18 sites that were upwind or more distant (as much as 200 kilometers) from the powerplant. The water content of the snowpack at maximum accumulation was lower in the post-control period than the pre-control period, reflecting the regional drought. Although there were small declines in snowpack sulfate concentrations at the downwind stations between the pre- and post-control periods, the difference was not statistically significant, indicating emission reductions had a weaker effect on snowpack chemistry than precipitation chemistry. Sulfate deposition decreased at all four downwind sites in the post-control period, primarily reflecting both lower water content and concentrations in the snowpack. As observed at the precipitation stations, nitrate, ammonium, and base-cation concentrations at all 22 sites were significantly higher in the post-control period than the pre-control period, reflecting drier conditions caused by drought.</p><p class=\"text\">The chemistry at six surface-water sites in and near the Mount Zirkel Wilderness Area and five control sites in the Flat Tops Wilderness Area was examined. No response to emission reductions was detectable in chemistry of the surface water in the Mount Zirkel Wilderness Area. Detection of a response to changes in emissions and deposition in the lake-chemistry data may have been confounded by drought conditions during the period after emission reductions occurred. The magnitude of reduced sulfate in atmospheric deposition indicates that at some time in the future, a reduction in lake sulfate attributable to Yampa Valley emission reduction should be detectable. The trend of decreasing sulfur dioxide emissions throughout western North America over the past 20 years is reflected in reduced concentrations of sulfate in lakes that were part of this study, as well as other lakes in the Rocky Mountains. However, detection of the surface-water response to changes in deposition requires a sufficiently long record to minimize effects of climate variability and to allow for lag time as sulfate moves through storage in soil, ground water, and lake reservoirs.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/sir20055167","usgsCitation":"Mast, M.A., Campbell, D.H., and Ingersoll, G.P., 2005, Effects of emission reductions at the Hayden powerplant on precipitation, snowpack, and surface-water chemistry in the Mount Zirkel Wilderness Area, Colorado, 1995-2003: U.S. Geological Survey Scientific Investigations Report 2005-5167, v, 32 p., https://doi.org/10.3133/sir20055167.","productDescription":"v, 32 p.","costCenters":[{"id":191,"text":"Colorado Water Science Center","active":true,"usgs":true}],"links":[{"id":193102,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":411373,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_73819.htm","linkFileType":{"id":5,"text":"html"}},{"id":7331,"rank":2,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/sir/2005/5167/","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Colorado","otherGeospatial":"Mount Zirkel Wilderness Area","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -106.8389,\n              40.9711\n            ],\n            [\n              -106.8389,\n              40.5583\n            ],\n            [\n              -106.5678,\n              40.5583\n            ],\n            [\n              -106.5678,\n              40.9711\n            ],\n            [\n              -106.8389,\n              40.9711\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a2ee4b07f02db6159e7","contributors":{"authors":[{"text":"Mast, M. Alisa 0000-0001-6253-8162 mamast@usgs.gov","orcid":"https://orcid.org/0000-0001-6253-8162","contributorId":827,"corporation":false,"usgs":true,"family":"Mast","given":"M.","email":"mamast@usgs.gov","middleInitial":"Alisa","affiliations":[{"id":191,"text":"Colorado Water Science Center","active":true,"usgs":true}],"preferred":true,"id":285498,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Campbell, Donald H. dhcampbe@usgs.gov","contributorId":1670,"corporation":false,"usgs":true,"family":"Campbell","given":"Donald","email":"dhcampbe@usgs.gov","middleInitial":"H.","affiliations":[],"preferred":true,"id":285500,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Ingersoll, George P. gpingers@usgs.gov","contributorId":1469,"corporation":false,"usgs":true,"family":"Ingersoll","given":"George","email":"gpingers@usgs.gov","middleInitial":"P.","affiliations":[{"id":191,"text":"Colorado Water Science Center","active":true,"usgs":true}],"preferred":true,"id":285499,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":72372,"text":"fs20053100 - 2005 - A simple field leach test to assess potential leaching of soluble constituents from mine wastes, soils, and other geologic materials","interactions":[],"lastModifiedDate":"2012-02-02T00:14:02","indexId":"fs20053100","displayToPublicDate":"2005-09-29T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":313,"text":"Fact Sheet","code":"FS","onlineIssn":"2327-6932","printIssn":"2327-6916","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2005-3100","title":"A simple field leach test to assess potential leaching of soluble constituents from mine wastes, soils, and other geologic materials","language":"ENGLISH","doi":"10.3133/fs20053100","usgsCitation":"Water Resources Division, U.S. Geological Survey, 2005, A simple field leach test to assess potential leaching of soluble constituents from mine wastes, soils, and other geologic materials (Version 1.0): U.S. Geological Survey Fact Sheet 2005-3100, 4 p., https://doi.org/10.3133/fs20053100.","productDescription":"4 p.","costCenters":[],"links":[{"id":122331,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/fs_2005_3100.jpg"},{"id":7334,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/fs/2005/3100/","linkFileType":{"id":5,"text":"html"}}],"edition":"Version 1.0","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b17e4b07f02db6a6504","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":534742,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":72374,"text":"b2136 - 2005 - Kinematics of the Short Hill fault — Late Paleozoic contractional reactivation of an Early Paleozoic extensional fault, Blue Ridge-South Mountain anticlinorium, northern Virginia and Southern Maryland","interactions":[],"lastModifiedDate":"2022-05-06T19:12:43.720392","indexId":"b2136","displayToPublicDate":"2005-09-29T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":306,"text":"Bulletin","code":"B","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"2136","title":"Kinematics of the Short Hill fault — Late Paleozoic contractional reactivation of an Early Paleozoic extensional fault, Blue Ridge-South Mountain anticlinorium, northern Virginia and Southern Maryland","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/b2136","usgsCitation":"Southworth, S., 2005, Kinematics of the Short Hill fault — Late Paleozoic contractional reactivation of an Early Paleozoic extensional fault, Blue Ridge-South Mountain anticlinorium, northern Virginia and Southern Maryland (Online only, Version 1.0): U.S. Geological Survey Bulletin 2136, HTML Document, https://doi.org/10.3133/b2136.","productDescription":"HTML Document","onlineOnly":"Y","costCenters":[],"links":[{"id":192923,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":400313,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_73906.htm"},{"id":7336,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/bul/b2136/","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Maryland, Virginia","otherGeospatial":"Blue Ridge-South Mountain anticlinorium","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -79.376220703125,\n              38.487994609214795\n            ],\n            [\n              -77.607421875,\n              38.487994609214795\n            ],\n            [\n              -77.607421875,\n              39.715638134796336\n            ],\n            [\n              -79.376220703125,\n              39.715638134796336\n            ],\n            [\n              -79.376220703125,\n              38.487994609214795\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","edition":"Online only, Version 1.0","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b32e4b07f02db6b47a7","contributors":{"authors":[{"text":"Southworth, Scott","contributorId":93933,"corporation":false,"usgs":true,"family":"Southworth","given":"Scott","affiliations":[],"preferred":false,"id":285517,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":72375,"text":"sir20055102 - 2005 - Characterization of surface-water quality in the S-Line Canal and potential geochemical reactions from storage of surface water in the Basalt aquifer near Fallon, Nevada","interactions":[],"lastModifiedDate":"2022-10-18T11:14:33.586602","indexId":"sir20055102","displayToPublicDate":"2005-09-29T00:00:00","publicationYear":"2005","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":"2005-5102","title":"Characterization of surface-water quality in the S-Line Canal and potential geochemical reactions from storage of surface water in the Basalt aquifer near Fallon, Nevada","docAbstract":"The Fallon basalt aquifer serves as the sole source of municipal water supply for the Lahontan Valley in west-central Nevada. Principal users include the City of Fallon, Naval Air Station Fallon, and the Fallon Paiute-Shoshone Tribe. Pumpage from the aquifer increased from about 1,700 acre-feet per year in the early 1970's to more than 3,000 acre-feet per year in the late 1990's, and has been accompanied by declines in water levels and changes in water quality. Storage of surface water in the basalt may mitigate the effects of pumpage, but may cause undesirable changes in water chemistry. In May 2001, the U.S. Geological Survey began a study, in cooperation with the Fallon Paiute-Shoshone Tribe, to characterize the surface-water quality of the S-Line Canal, a likely source of water for augmenting recharge. Because arsenic concentrations in ground water of the basalt aquifer exceed drinking water standards, the potential for arsenic release to artificial recharge was explored by using geochemical modeling. Model results suggest that arsenic release may increase concentrations to levels that could limit the use of artificial recharge. Field-based experiments are needed to evaluate the underlying model assumptions.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/sir20055102","usgsCitation":"Welch, A., Maurer, D.K., Lico, M.S., and McCormack, J.K., 2005, Characterization of surface-water quality in the S-Line Canal and potential geochemical reactions from storage of surface water in the Basalt aquifer near Fallon, Nevada: U.S. Geological Survey Scientific Investigations Report 2005-5102, 52 p., https://doi.org/10.3133/sir20055102.","productDescription":"52 p.","costCenters":[],"links":[{"id":192924,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":7337,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/sir/2005/5102/","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e2e4b07f02db5e4d26","contributors":{"authors":[{"text":"Welch, Alan H.","contributorId":45286,"corporation":false,"usgs":true,"family":"Welch","given":"Alan H.","affiliations":[],"preferred":false,"id":285520,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Maurer, Douglas K. dkmaurer@usgs.gov","contributorId":2308,"corporation":false,"usgs":true,"family":"Maurer","given":"Douglas","email":"dkmaurer@usgs.gov","middleInitial":"K.","affiliations":[],"preferred":true,"id":285518,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Lico, Michael S.","contributorId":75897,"corporation":false,"usgs":true,"family":"Lico","given":"Michael","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":285521,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"McCormack, John K.","contributorId":39078,"corporation":false,"usgs":true,"family":"McCormack","given":"John","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":285519,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":72371,"text":"sim2873 - 2005 - Geologic map of the Edwards Aquifer recharge zone, south-central Texas","interactions":[],"lastModifiedDate":"2012-02-02T00:14:01","indexId":"sim2873","displayToPublicDate":"2005-09-29T00:00:00","publicationYear":"2005","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":"2873","title":"Geologic map of the Edwards Aquifer recharge zone, south-central Texas","language":"ENGLISH","doi":"10.3133/sim2873","usgsCitation":"Blome, C.D., Faith, J.R., Pedraza, D.E., Ozuna, G.B., Cole, J., Clark, A.K., Small, T.A., and Morris, R., 2005, Geologic map of the Edwards Aquifer recharge zone, south-central Texas (Version 1.0): U.S. Geological Survey Scientific Investigations Map 2873, 1 sheet, 55.75 x 39.5 in., https://doi.org/10.3133/sim2873.","productDescription":"1 sheet, 55.75 x 39.5 in.","costCenters":[],"links":[{"id":110580,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_73904.htm","linkFileType":{"id":5,"text":"html"},"description":"73904"},{"id":193104,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":7333,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/sim/2005/2873/","linkFileType":{"id":5,"text":"html"}}],"edition":"Version 1.0","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b04e4b07f02db699007","contributors":{"authors":[{"text":"Blome, Charles D. 0000-0002-3449-9378 cblome@usgs.gov","orcid":"https://orcid.org/0000-0002-3449-9378","contributorId":1246,"corporation":false,"usgs":true,"family":"Blome","given":"Charles","email":"cblome@usgs.gov","middleInitial":"D.","affiliations":[{"id":164,"text":"Central Energy Resources Science Center","active":true,"usgs":true}],"preferred":true,"id":285507,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Faith, Jason R.","contributorId":92758,"corporation":false,"usgs":true,"family":"Faith","given":"Jason","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":285513,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Pedraza, Diana E. 0000-0003-4483-8094 dpedraza@usgs.gov","orcid":"https://orcid.org/0000-0003-4483-8094","contributorId":1281,"corporation":false,"usgs":false,"family":"Pedraza","given":"Diana","email":"dpedraza@usgs.gov","middleInitial":"E.","affiliations":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"preferred":true,"id":285510,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Ozuna, George B. gbozuna@usgs.gov","contributorId":1247,"corporation":false,"usgs":true,"family":"Ozuna","given":"George","email":"gbozuna@usgs.gov","middleInitial":"B.","affiliations":[],"preferred":true,"id":285508,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Cole, J. C.","contributorId":21539,"corporation":false,"usgs":true,"family":"Cole","given":"J. C.","affiliations":[],"preferred":false,"id":285511,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Clark, Allan K. 0000-0003-0099-1521 akclark@usgs.gov","orcid":"https://orcid.org/0000-0003-0099-1521","contributorId":1279,"corporation":false,"usgs":true,"family":"Clark","given":"Allan","email":"akclark@usgs.gov","middleInitial":"K.","affiliations":[{"id":318,"text":"Geosciences and Environmental Change Science Center","active":true,"usgs":true},{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"preferred":true,"id":285509,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Small, Ted A.","contributorId":77533,"corporation":false,"usgs":true,"family":"Small","given":"Ted","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":285512,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Morris, Robert R. 0000-0001-7504-3732","orcid":"https://orcid.org/0000-0001-7504-3732","contributorId":106213,"corporation":false,"usgs":true,"family":"Morris","given":"Robert R.","affiliations":[{"id":48595,"text":"Oklahoma-Texas Water Science Center","active":true,"usgs":true}],"preferred":true,"id":285514,"contributorType":{"id":1,"text":"Authors"},"rank":8}]}}
,{"id":72370,"text":"sim2893 - 2005 - Data related to late Quaternary surface faulting on the Eastgate fault, Churchill County, Nevada","interactions":[],"lastModifiedDate":"2012-02-02T00:14:01","indexId":"sim2893","displayToPublicDate":"2005-09-29T00:00:00","publicationYear":"2005","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":"2893","title":"Data related to late Quaternary surface faulting on the Eastgate fault, Churchill County, Nevada","language":"ENGLISH","doi":"10.3133/sim2893","usgsCitation":"Crone, A.J., Kyung, J., Machette, M., Lidke, D.J., Okumura, K., and Mahan, S., 2005, Data related to late Quaternary surface faulting on the Eastgate fault, Churchill County, Nevada (Version 1.0): U.S. Geological Survey Scientific Investigations Map 2893, Pamphlet, 12 p.; Map, 1 sheet : 52 x 36 in., https://doi.org/10.3133/sim2893.","productDescription":"Pamphlet, 12 p.; Map, 1 sheet : 52 x 36 in.","costCenters":[],"links":[{"id":110581,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_73905.htm","linkFileType":{"id":5,"text":"html"},"description":"73905"},{"id":193103,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":7332,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/sim/2005/2893/","linkFileType":{"id":5,"text":"html"}}],"edition":"Version 1.0","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac7e4b07f02db67b569","contributors":{"authors":[{"text":"Crone, Anthony J. 0000-0002-3006-406X crone@usgs.gov","orcid":"https://orcid.org/0000-0002-3006-406X","contributorId":790,"corporation":false,"usgs":true,"family":"Crone","given":"Anthony","email":"crone@usgs.gov","middleInitial":"J.","affiliations":[{"id":300,"text":"Geologic Hazards Science Center","active":true,"usgs":true}],"preferred":true,"id":285501,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Kyung, Jai-Bok","contributorId":88224,"corporation":false,"usgs":true,"family":"Kyung","given":"Jai-Bok","email":"","affiliations":[],"preferred":false,"id":285506,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Machette, Michael N.","contributorId":28963,"corporation":false,"usgs":true,"family":"Machette","given":"Michael N.","affiliations":[],"preferred":false,"id":285504,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Lidke, David J. 0000-0003-4668-1617 dlidke@usgs.gov","orcid":"https://orcid.org/0000-0003-4668-1617","contributorId":1211,"corporation":false,"usgs":true,"family":"Lidke","given":"David","email":"dlidke@usgs.gov","middleInitial":"J.","affiliations":[{"id":318,"text":"Geosciences and Environmental Change Science Center","active":true,"usgs":true}],"preferred":true,"id":285502,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Okumura, Koji","contributorId":39457,"corporation":false,"usgs":true,"family":"Okumura","given":"Koji","email":"","affiliations":[],"preferred":false,"id":285505,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Mahan, Shannon 0000-0001-5214-7774 smahan@usgs.gov","orcid":"https://orcid.org/0000-0001-5214-7774","contributorId":1215,"corporation":false,"usgs":true,"family":"Mahan","given":"Shannon","email":"smahan@usgs.gov","affiliations":[{"id":211,"text":"Crustal Geophysics and Geochemistry Science Center","active":true,"usgs":true}],"preferred":false,"id":285503,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}}
,{"id":70203528,"text":"70203528 - 2005 - Historical subsidence and wetland loss in the Mississippi delta plain","interactions":[],"lastModifiedDate":"2019-05-28T10:53:49","indexId":"70203528","displayToPublicDate":"2005-09-27T10:43:33","publicationYear":"2005","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"Historical subsidence and wetland loss in the Mississippi delta plain","docAbstract":"<p>Five representative areas of the Mississippi River delta plain were investigated using remote images, marsh elevations, water depths, sediment cores, and radiocarbon dates to estimate the timing, magnitudes, and relative rates of marsh erosion and land subsidence at geological and historical time scales. In the Terrebonne-Lafourche region of rapid interior-wetland loss, former marshes are now submerged beneath water that averages 0.5 to 1.0 m deep. Most of the permanent historical flooding was caused by rapid subsidence and collapse of the delta plain that occurred during the late 1960s and 1970s. Subsequent erosion of the submerged delta-plain marsh was relatively minor at most of the coring sites.<br></p><p>Widespread nearly simultaneous collapse of marshes across the Mississippi delta plain appears to be unprecedented and not repeated in the geological record of the past 1,000 years. Surface and subsurface data strongly indicate that the rapid subsidence and associated wetland loss were largely induced by extraction of hydrocarbons and associated formation water. Average historical rates of subsidence between 1965 and 1993 were about 8 to 12 mm/yr, whereas average geological rates of subsidence for the past 5,000 years were about 1 to 5 mm/yr. Natural processes such as deep-seated salt migration and fault movement cannot be discounted entirely, but there is no compelling evidence that these processes were responsible for the observed historical changes. Results of this study provide a basis for determining the relative importance of subsidence and shoreline erosion as causes of past wetland loss and for predicting sites and probable mechanisms of future wetland loss. This information should improve the selection of project sites and designs for wetland-loss mitigation and coastal restoration in south Louisiana.</p>","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Gulf Coast Association of Geological Societies Transactions","largerWorkSubtype":{"id":12,"text":"Conference publication"},"conferenceTitle":"Gulf Coast Association of Geological Societies 55th Annual Convention","conferenceDate":"September 25-27, 2005","conferenceLocation":"New Orleans, Louisiana","language":"English","publisher":"Gulf Coast Association of Geological Societies","usgsCitation":"Morton, R., Bernier, J., Barras, J.A., and Ferina, N.F., 2005, Historical subsidence and wetland loss in the Mississippi delta plain, <i>in</i> Gulf Coast Association of Geological Societies Transactions, v. 55, New Orleans, Louisiana, September 25-27, 2005, p. 555-571.","productDescription":"17 p.; CD-ROM","startPage":"555","endPage":"571","costCenters":[{"id":17705,"text":"Wetland and Aquatic Research Center","active":true,"usgs":true}],"links":[{"id":364008,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":364007,"rank":1,"type":{"id":15,"text":"Index Page"},"url":"https://store.beg.utexas.edu/gcags/1722-gcags055.html"}],"country":"United States","state":"Louisiana","otherGeospatial":"Mississippi delta","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -90.87890625,\n              28.9600886880068\n            ],\n            [\n              -90.02197265625,\n              28.9600886880068\n            ],\n            [\n              -90.02197265625,\n              29.7453016622136\n            ],\n            [\n              -90.87890625,\n              29.7453016622136\n            ],\n            [\n              -90.87890625,\n              28.9600886880068\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"55","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Morton, Robert A.","contributorId":88333,"corporation":false,"usgs":true,"family":"Morton","given":"Robert A.","affiliations":[],"preferred":false,"id":763017,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bernier, Julie 0000-0002-9918-5353 jbernier@usgs.gov","orcid":"https://orcid.org/0000-0002-9918-5353","contributorId":3549,"corporation":false,"usgs":true,"family":"Bernier","given":"Julie","email":"jbernier@usgs.gov","affiliations":[{"id":574,"text":"St. Petersburg Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":true,"id":763018,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Barras, John A. jbarras@usgs.gov","contributorId":149332,"corporation":false,"usgs":true,"family":"Barras","given":"John","email":"jbarras@usgs.gov","middleInitial":"A.","affiliations":[{"id":574,"text":"St. Petersburg Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":false,"id":763019,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Ferina, Nicholas F.","contributorId":14047,"corporation":false,"usgs":true,"family":"Ferina","given":"Nicholas","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":763020,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":72366,"text":"ofr20051329 - 2005 - Ground-water reconnaissance of the Bijou Creek watershed, South Lake Tahoe, California, June-October 2003","interactions":[],"lastModifiedDate":"2012-02-02T00:14:01","indexId":"ofr20051329","displayToPublicDate":"2005-09-27T00:00:00","publicationYear":"2005","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":"2005-1329","title":"Ground-water reconnaissance of the Bijou Creek watershed, South Lake Tahoe, California, June-October 2003","language":"ENGLISH","doi":"10.3133/ofr20051329","usgsCitation":"Allander, K.K., 2005, Ground-water reconnaissance of the Bijou Creek watershed, South Lake Tahoe, California, June-October 2003: U.S. Geological Survey Open-File Report 2005-1329, 41 p., https://doi.org/10.3133/ofr20051329.","productDescription":"41 p.","costCenters":[],"links":[{"id":193100,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":7329,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2005/1329/","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aa7e4b07f02db667091","contributors":{"authors":[{"text":"Allander, Kip K. 0000-0002-3317-298X kalland@usgs.gov","orcid":"https://orcid.org/0000-0002-3317-298X","contributorId":2290,"corporation":false,"usgs":true,"family":"Allander","given":"Kip","email":"kalland@usgs.gov","middleInitial":"K.","affiliations":[{"id":465,"text":"Nevada Water Science Center","active":true,"usgs":true}],"preferred":true,"id":285496,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":72363,"text":"sir20055165 - 2005 - Estimation of constituent concentrations, densities, loads, and yields in lower Kansas River, northeast Kansas, using regression models and continuous water-quality monitoring, January 2000 through December 2003","interactions":[],"lastModifiedDate":"2012-02-02T00:14:01","indexId":"sir20055165","displayToPublicDate":"2005-09-27T00:00:00","publicationYear":"2005","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":"2005-5165","title":"Estimation of constituent concentrations, densities, loads, and yields in lower Kansas River, northeast Kansas, using regression models and continuous water-quality monitoring, January 2000 through December 2003","docAbstract":"The lower Kansas River is an important source of drinking water for hundreds of thousands of people in northeast Kansas. Constituents of concern identified by the Kansas Department of Health and Environment (KDHE) for streams in the lower Kansas River Basin include sulfate, chloride, nutrients, atrazine, bacteria, and sediment. Real-time continuous water-quality monitors were operated at three locations along the lower Kansas River from July 1999 through September 2004 to provide in-stream measurements of specific conductance, pH, water temperature, turbidity, and dissolved oxygen and to estimate concentrations for constituents of concern. Estimates of concentration and densities were combined with streamflow to calculate constituent loads and yields from January 2000 through December 2003. The Wamego monitoring site is located 44 river miles upstream from the Topeka monitoring site, which is 65 river miles upstream from the DeSoto monitoring site, which is 18 river miles upstream from where the Kansas River flows into the Missouri River. Land use in the Kansas River Basin is dominated by grassland and cropland, and streamflow is affected substantially by reservoirs.\r\n\r\nWater quality at the three monitoring sites varied with hydrologic conditions, season, and proximity to constituent sources. Nutrient and sediment concentrations and bacteria densities were substantially larger during periods of increased streamflow, indicating important contributions from nonpoint sources in the drainage basin. \r\n\r\nDuring the study period, pH remained well above the KDHE lower criterion of 6.5 standard units at all sites in all years, but exceeded the upper criterion of 8.5 standard units annually between 2 percent of the time (Wamego in 2001) and 65 percent of the time (DeSoto in 2003). The dissolved oxygen concentration was less than the minimum aquatic-life-support criterion of 5.0 milligrams per liter less than 1 percent of the time at all sites.\r\n\r\nDissolved solids, a measure of the dissolved material in water, exceeded 500 milligrams per liter about one-half of the time at the three Kansas River sites. Larger dissolved-solids concentrations upstream likely were a result of water inflow from the highly mineralized Smoky Hill River that is diluted by tributary flow as it moves downstream.\r\n\r\nConcentrations of total nitrogen and total phosphorus at the three monitoring sites exceeded the ecoregion water-quality criteria suggested by the U.S. Environmental Protection Agency during the entire study period. Median nitrogen and phosphorus concentrations were similar at all three sites, and nutrient load increased moving from the upstream to downstream sites. Total nitrogen and total phosphorus yields were nearly the same from site to site indicating that nutrient sources were evenly distributed throughout the lower Kansas River Basin. About 11 percent of the total nitrogen load and 12 percent of the total phosphorus load at DeSoto during 2000-03 originated from wastewater-treatment facilities. \r\n\r\nEscherichia coli bacteria densities were largest at the middle site, Topeka. On average, 83 percent of the annual bacteria load at DeSoto during 2000-03 occurred during 10 percent of the time, primarily in conjunction with runoff.\r\n\r\nThe average annual sediment loads at the middle and downstream monitoring sites (Topeka and DeSoto) were nearly double those at the upstream site (Wamego). The average annual sediment yield was largest at Topeka. On average, 64 percent of the annual suspended-sediment load at DeSoto during 2000-03 occurred during 10 percent of the time. Trapping of sediment by reservoirs located on contributing tributaries decreases transport of sediment and sediment-related constituents. \r\n\r\nThe average annual suspended-sediment load in the Kansas River at DeSoto during 2000-03 was estimated at 1.66 million tons. An estimated 13 percent of this load consisted of sand-size particles, so approximately 216,000 tons of sand were transported ","language":"ENGLISH","doi":"10.3133/sir20055165","usgsCitation":"Rasmussen, T.J., Ziegler, A., and Rasmussen, P.P., 2005, Estimation of constituent concentrations, densities, loads, and yields in lower Kansas River, northeast Kansas, using regression models and continuous water-quality monitoring, January 2000 through December 2003: U.S. Geological Survey Scientific Investigations Report 2005-5165, 126 p., https://doi.org/10.3133/sir20055165.","productDescription":"126 p.","costCenters":[],"links":[{"id":193037,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":7326,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/sir/2005/5165/","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0ae4b07f02db5fba50","contributors":{"authors":[{"text":"Rasmussen, Teresa J. 0000-0002-7023-3868 rasmuss@usgs.gov","orcid":"https://orcid.org/0000-0002-7023-3868","contributorId":3336,"corporation":false,"usgs":true,"family":"Rasmussen","given":"Teresa","email":"rasmuss@usgs.gov","middleInitial":"J.","affiliations":[{"id":353,"text":"Kansas Water Science Center","active":false,"usgs":true}],"preferred":true,"id":285490,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Ziegler, Andrew C. aziegler@usgs.gov","contributorId":433,"corporation":false,"usgs":true,"family":"Ziegler","given":"Andrew C.","email":"aziegler@usgs.gov","affiliations":[{"id":353,"text":"Kansas Water Science Center","active":false,"usgs":true}],"preferred":false,"id":285489,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Rasmussen, Patrick P. 0000-0002-3287-6010 pras@usgs.gov","orcid":"https://orcid.org/0000-0002-3287-6010","contributorId":3530,"corporation":false,"usgs":true,"family":"Rasmussen","given":"Patrick","email":"pras@usgs.gov","middleInitial":"P.","affiliations":[{"id":353,"text":"Kansas Water Science Center","active":false,"usgs":true}],"preferred":true,"id":285491,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":72362,"text":"sir20055170 - 2005 - Hydrology and simulation of ground-water flow in Cedar Valley, Iron County, Utah","interactions":[],"lastModifiedDate":"2019-12-30T13:58:41","indexId":"sir20055170","displayToPublicDate":"2005-09-27T00:00:00","publicationYear":"2005","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":"2005-5170","title":"Hydrology and simulation of ground-water flow in Cedar Valley, Iron County, Utah","docAbstract":"<p>Cedar Valley, located in the eastern part of Iron County in southwestern Utah, is experiencing rapid population growth. Cedar Valley traditionally has supported agriculture, but the growing population needs a larger share of the available water resources. Water withdrawn from the unconsolidated basin fill is the primary source for public supply and is a major source of water for irrigation. Water managers are concerned about increasing demands on the water supply and need hydrologic information to manage this limited water resource and minimize flow of water unsuitable for domestic use toward present and future public-supply sources.</p><p>Surface water in the study area is derived primarily from snowmelt at higher altitudes east of the study area or from occasional large thunderstorms during the summer. Coal Creek, a perennial stream with an average annual discharge of 24,200 acre-feet per year, is the largest stream in Cedar Valley. Typically, all of the water in Coal Creek is diverted for irrigation during the summer months. All surface water is consumed within the basin by irrigated crops, evapotranspiration, or recharge to the ground-water system.</p><p>Ground water in Cedar Valley generally moves from primary recharge areas along the eastern margin of the basin where Coal Creek enters, to areas of discharge or subsurface outflow. Recharge to the unconsolidated basin-fill aquifer is by seepage of unconsumed irrigation water, streams, direct precipitation on the unconsolidated basin fill, and subsurface inflow from consolidated rock and Parowan Valley and is estimated to be about 42,000 acre-feet per year. Stable-isotope data indicate that recharge is primarily from winter precipitation. The chloride mass-balance method indicates that recharge may be less than 42,000 acre-feet per year, but is considered a rough approximation because of limited chloride concentration data for precipitation and Coal Creek. Continued declining water levels indicate that recharge is not sufficient to meet demand. Water levels in many areas are at or close to historic lows.</p><p>In 2000, withdrawal from wells was estimated to be 36,000 acre-feet per year. About 4,000 acre-feet per year are estimated to discharge to evapotranspiration or as subsurface outflow. Prior to large-scale ground-water development, ground-water discharge by evapotranspiration and discharge to springs was much larger.</p><p>Ground water along the eastern margin of the valley between Cedar City and Enoch is unsuitable for domestic use because of high dissolved-solids and nitrate concentrations. The predominant ions of Ca and SO4 in this area indicate dissolution of gypsum in the Markagunt Plateau to the east. Data collected during this study were compared to historic data; there is no evidence to indicate deterioration in ground-water quality. The spatial distribution of ground water with high nitrate concentration does not appear to be migrating beyond its previously known extent. <br>No single source can be identified as the cause for elevated nitrate concentrations in ground water. Low nitrogen-15 values north of Cedar City indicate a natural geologic source. Higher nitrogen-15 values toward the center of the basin and associated hydrologic data indicate probable recharge from waste-water effluent. Excess dissolved nitrogen gas and low nitrate concentrations in shallow ground water indicate that denitrification is occurring in some areas.</p><p>A computer ground-water flow model was developed to simulate flow in the unconsolidated basin fill. The method of determining recharge from irrigation was changed during the calibration process to incorporate more areal and temporal variability. In general, the model accurately simulates water levels and water-level fluctuations and can be considered an adequate tool to help determine the valley-wide effects on water levels of additional ground-water withdrawals and changes in water use. The model was used to simulated water-level changes caused by projecting current withdrawal rates, increased withdrawal rates, and a 10-year drought. Water levels declined 20 to 275 feet in the southern and central parts of the valley and less than 20 feet north of Enoch</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Salt Lake City, UT","doi":"10.3133/sir20055170","collaboration":"Prepared in cooperation with the Central Iron County Water Conservancy District; Utah Department of Natural Resources, Division of Water Resources; Utah Department of Environmental Quality, Division of Water Quality; Cedar City, and City of Enoch","usgsCitation":"Brooks, L.E., and Mason, J.L., 2005, Hydrology and simulation of ground-water flow in Cedar Valley, Iron County, Utah (Online only): U.S. Geological Survey Scientific Investigations Report 2005-5170, x, 114 p., https://doi.org/10.3133/sir20055170.","productDescription":"x, 114 p.","numberOfPages":"127","onlineOnly":"Y","costCenters":[{"id":610,"text":"Utah Water Science 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Valley","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"Polygon\",\"coordinates\":[[[-112.4806,38.1474],[-112.4806,38.1379],[-112.4805,38.1293],[-112.481,38.1148],[-112.481,38.1098],[-112.4808,38.0862],[-112.4813,38.0658],[-112.4818,38.0572],[-112.4817,38.0418],[-112.4822,38.0273],[-112.4825,37.9847],[-112.483,37.9788],[-112.4696,37.9789],[-112.4707,37.9635],[-112.4706,37.9462],[-112.4711,37.9349],[-112.4715,37.9059],[-112.489,37.9063],[-112.4895,37.8913],[-112.5075,37.8912],[-112.5245,37.8912],[-112.5256,37.8912],[-112.5623,37.8905],[-112.5909,37.8909],[-112.5909,37.8832],[-112.5815,37.8832],[-112.5812,37.8383],[-112.5815,37.8057],[-112.5949,37.8065],[-112.6275,37.8082],[-112.6491,37.8085],[-112.6567,37.8076],[-112.6928,37.8065],[-112.6931,37.7752],[-112.6934,37.7525],[-112.6931,37.7185],[-112.6902,37.7186],[-112.6877,37.574],[-112.6874,37.545],[-112.7641,37.5445],[-112.7948,37.5448],[-112.8331,37.5449],[-112.8534,37.5448],[-112.9051,37.5449],[-112.9047,37.5154],[-112.9046,37.5005],[-112.9452,37.5006],[-113.0415,37.5007],[-113.0411,37.4744],[-113.0817,37.4745],[-113.1496,37.4748],[-113.1497,37.4803],[-113.2024,37.4807],[-113.2123,37.4806],[-113.2175,37.4805],[-113.2605,37.481],[-113.2601,37.4946],[-113.2604,37.5114],[-113.2601,37.5313],[-113.2775,37.5311],[-113.2955,37.5314],[-113.3153,37.5307],[-113.4772,37.5302],[-113.4779,37.5946],[-113.4784,37.6182],[-113.5144,37.6186],[-113.5324,37.6189],[-113.5353,37.6188],[-113.5539,37.619],[-113.5917,37.619],[-113.592,37.6059],[-113.61,37.6061],[-113.7204,37.6068],[-113.7402,37.6065],[-113.7564,37.6068],[-113.7599,37.6067],[-113.7936,37.6067],[-113.8128,37.6073],[-113.8686,37.6074],[-113.8872,37.6071],[-113.904,37.6068],[-113.9232,37.607],[-114.0539,37.6075],[-114.0541,37.6431],[-114.0541,37.6447],[-114.0539,37.666],[-114.0536,37.7109],[-114.0535,37.7259],[-114.0531,37.7887],[-114.0531,37.7903],[-114.0524,37.9039],[-114.0524,37.9059],[-114.0494,38.0308],[-114.0494,38.0329],[-114.0493,38.1503],[-114.0445,38.1499],[-114.0246,38.1502],[-114.0077,38.1505],[-113.9889,38.1504],[-113.955,38.1505],[-113.9368,38.1503],[-113.9333,38.1508],[-113.9164,38.1506],[-113.8988,38.1509],[-113.8807,38.1507],[-113.8438,38.1508],[-113.8239,38.1507],[-113.8069,38.1505],[-113.787,38.1508],[-113.7688,38.1506],[-113.7343,38.1506],[-113.7144,38.1504],[-113.6957,38.1507],[-113.6781,38.1509],[-113.6594,38.1507],[-113.643,38.151],[-113.6225,38.1508],[-113.605,38.151],[-113.5862,38.1508],[-113.5657,38.1506],[-113.5546,38.1508],[-113.547,38.1504],[-113.5142,38.1508],[-113.4961,38.1506],[-113.4926,38.1506],[-113.4738,38.1504],[-113.4545,38.1506],[-113.4364,38.1504],[-113.4042,38.1498],[-113.3814,38.1501],[-113.3638,38.1498],[-113.3474,38.1496],[-113.3351,38.1497],[-113.3111,38.1495],[-113.2924,38.1488],[-113.2736,38.149],[-113.2034,38.1493],[-113.1999,38.1493],[-113.1812,38.149],[-113.163,38.1488],[-113.1449,38.1485],[-113.1267,38.1491],[-113.108,38.1488],[-113.0717,38.1482],[-113.0536,38.1484],[-113.0325,38.1481],[-113.012,38.1483],[-112.9939,38.1484],[-112.9605,38.1482],[-112.9418,38.1484],[-112.9383,38.1484],[-112.9202,38.1485],[-112.9014,38.1487],[-112.8833,38.1484],[-112.8499,38.1491],[-112.8318,38.1487],[-112.8277,38.1488],[-112.8101,38.1489],[-112.7902,38.149],[-112.7715,38.1487],[-112.7381,38.1489],[-112.7194,38.1481],[-112.7165,38.1485],[-112.6989,38.1482],[-112.6773,38.1483],[-112.6585,38.1484],[-112.6275,38.1486],[-112.6094,38.1491],[-112.6035,38.1492],[-112.5854,38.1488],[-112.5673,38.1489],[-112.5485,38.1485],[-112.5356,38.1486],[-112.5304,38.1481],[-112.5134,38.1478],[-112.4806,38.1474]]]},\"properties\":{\"name\":\"Iron\",\"state\":\"UT\"}}]}","edition":"Online only","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4acce4b07f02db67e865","contributors":{"authors":[{"text":"Brooks, Lynette E. 0000-0002-9074-0939 lebrooks@usgs.gov","orcid":"https://orcid.org/0000-0002-9074-0939","contributorId":2718,"corporation":false,"usgs":true,"family":"Brooks","given":"Lynette","email":"lebrooks@usgs.gov","middleInitial":"E.","affiliations":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"preferred":true,"id":285487,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Mason, James L.","contributorId":14397,"corporation":false,"usgs":true,"family":"Mason","given":"James","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":285488,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":72359,"text":"ofr20051213 - 2005 - USGS science in Florida: proceedings of Florida Integrated Science Center meeting, Orlando, Florida, May 3-5, 2005","interactions":[],"lastModifiedDate":"2012-02-02T00:14:01","indexId":"ofr20051213","displayToPublicDate":"2005-09-27T00:00:00","publicationYear":"2005","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":"2005-1213","title":"USGS science in Florida: proceedings of Florida Integrated Science Center meeting, Orlando, Florida, May 3-5, 2005","language":"ENGLISH","doi":"10.3133/ofr20051213","usgsCitation":"Water Resources Division, U.S. Geological Survey, 2005, USGS science in Florida: proceedings of Florida Integrated Science Center meeting, Orlando, Florida, May 3-5, 2005: U.S. Geological Survey Open-File Report 2005-1213, 88 p., https://doi.org/10.3133/ofr20051213.","productDescription":"88 p.","costCenters":[],"links":[{"id":192979,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":7323,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2005/1213/","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a26e4b07f02db60f8e4","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":534740,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":72360,"text":"sir20055136 - 2005 - Influence of geologic setting on ground-water availability in the Lawrenceville area, Gwinnett County, Georgia","interactions":[],"lastModifiedDate":"2017-01-12T09:22:06","indexId":"sir20055136","displayToPublicDate":"2005-09-27T00:00:00","publicationYear":"2005","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":"2005-5136","title":"Influence of geologic setting on ground-water availability in the Lawrenceville area, Gwinnett County, Georgia","docAbstract":"Obtaining large quantities of ground water needed for municipal and industrial supply in the Piedmont and Blue Ridge physiographic provinces can be challenging because of the complex geology and the typically low primary permeability of igneous and metamorphic rocks. Areas of enhanced secondary permeability in the bedrock do occur, however, and 'high-yield' wells are not uncommon, particularly where careful site-selection techniques are used prior to test drilling. The U.S. Geological Survey - in cooperation with the City of Lawrenceville, Georgia - conducted this study from 2000 to 2002 to learn more about how different geologic settings influence the availability of ground water in igneous and metamorphic bedrock with the expectation that this knowledge could be used to help identify additional water resources in the area. \r\n\r\nIn compositionally layered-rock settings, wells derive water almost exclusively from lithologically and structurally controlled water-bearing zones formed parallel to foliation and compositional layering. These high-permeability, water-bearing zones - termed foliation-parallel parting systems -combined with high-angle joint systems, are the primary control for the high-yield wells drilled in the Lawrenceville area; yields range from 100 to several hundred gallons per minute (gal/min). Near Lawrenceville, areas with high ground-water yield are present in sequences of amphibolite, biotite gneiss, and button schist where the structural attitude of the rocks is gently dipping, in areas characterized by abundant jointing, and in topographic settings with a continuous source of recharge along these structures.\r\n\r\nIn massive-rock settings, wells derive water mostly from joint systems, although foliation-parallel parting systems also may be important. Wells deriving water primarily from steeply-dipping joint systems typically have low yields ranging from 1 to 5 gal/min. Joint systems in massive-rock settings can be identified and characterized by using many of the methods described in this report. Geologic mapping was the primary method used to determine the distribution, variability, and relative concentrations (intensity) of joint systems. In the subsurface, joints were characterized by taking orientation measurements in the open boreholes of wells using acoustic and/or optical televiewers. \r\n\r\nIn this investigation, the only practical approach found for locating areas of high ground-water potential was first through detailed geologic mapping followed by test drilling, borehole geophysical logging, and aquifer testing. Geologic methods help characterize both large- and small-scale structures and other lithologic and stratigraphic features that influence development of increased secondary permeability in the bedrock. The rock types, discontinuities, depth of weathering, topographic position, and recharge potential - which were the principal factors assessed through detailed geologic mapping - must be evaluated carefully, in relation to one another, to assess the ground-water potential in a given area.","language":"ENGLISH","doi":"10.3133/sir20055136","usgsCitation":"Williams, L.J., Kath, R.L., Crawford, T.J., and Chapman, M.J., 2005, Influence of geologic setting on ground-water availability in the Lawrenceville area, Gwinnett County, Georgia (Online only): U.S. Geological Survey Scientific Investigations Report 2005-5136, 43 p., https://doi.org/10.3133/sir20055136.","productDescription":"43 p.","onlineOnly":"Y","costCenters":[{"id":13634,"text":"South Atlantic Water Science Center","active":true,"usgs":true}],"links":[{"id":193035,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":7324,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/sir/2005/5136/","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Georgia","county":"Gwinnett County, ","city":"Lawrenceville","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -84,34.583333333333336 ], [ -84,34 ], [ -84.55,34 ], [ -84.55,34.583333333333336 ], [ -84,34.583333333333336 ] ] ] } } ] }","edition":"Online only","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f0e4b07f02db5ee220","contributors":{"authors":[{"text":"Williams, Lester J. lesterw@usgs.gov","contributorId":2395,"corporation":false,"usgs":true,"family":"Williams","given":"Lester","email":"lesterw@usgs.gov","middleInitial":"J.","affiliations":[],"preferred":true,"id":285484,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Kath, Randy L.","contributorId":49879,"corporation":false,"usgs":true,"family":"Kath","given":"Randy","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":285485,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Crawford, Thomas J.","contributorId":73640,"corporation":false,"usgs":true,"family":"Crawford","given":"Thomas","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":285486,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Chapman, Melinda J. 0000-0003-4021-0320 mjchap@usgs.gov","orcid":"https://orcid.org/0000-0003-4021-0320","contributorId":1597,"corporation":false,"usgs":true,"family":"Chapman","given":"Melinda","email":"mjchap@usgs.gov","middleInitial":"J.","affiliations":[{"id":476,"text":"North Carolina Water Science Center","active":true,"usgs":true},{"id":493,"text":"Office of Ground Water","active":true,"usgs":true}],"preferred":true,"id":285483,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":72364,"text":"fs20053079 - 2005 - Water use for irrigation in Michigan, 2001","interactions":[],"lastModifiedDate":"2017-01-20T11:06:21","indexId":"fs20053079","displayToPublicDate":"2005-09-27T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":313,"text":"Fact Sheet","code":"FS","onlineIssn":"2327-6932","printIssn":"2327-6916","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2005-3079","title":"Water use for irrigation in Michigan, 2001","docAbstract":"<p>Each year, water-use data for Michigan are compiled or estimated by the Michigan Department of Environmental Quality (MDEQ), working in cooperation with the U. S. Geological Survey (USGS). The resulting information provides a category-by-category profile of over 4,200 facilities throughout the State. The data are reported in the Michigan Water Use Reporting Program, which provides needed information for water-resources planning and enhances public understanding of the value of sustaining water resources within the Great Lakes Basin. The primary goal of the program is to inventory, analyze, and report baseline data for major water uses. </p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/fs20053079","collaboration":"Prepared in cooperation with the Michigan Department of Environmental Quality","usgsCitation":"Morenz, M.L., Van Til, R.L., and Luukkonen, C.L., 2005, Water use for irrigation in Michigan, 2001: U.S. Geological Survey Fact Sheet 2005-3079, 4 p., https://doi.org/10.3133/fs20053079.","productDescription":"4 p.","costCenters":[{"id":382,"text":"Michigan Water Science Center","active":true,"usgs":true}],"links":[{"id":122460,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/fs_2005_3079.jpg"},{"id":7327,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/fs/2005/3079/","linkFileType":{"id":5,"text":"html"}}],"country":"United 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,{"id":72365,"text":"fs20053071 - 2005 - Nevada water resources data","interactions":[],"lastModifiedDate":"2012-02-02T00:14:01","indexId":"fs20053071","displayToPublicDate":"2005-09-27T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":313,"text":"Fact Sheet","code":"FS","onlineIssn":"2327-6932","printIssn":"2327-6916","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2005-3071","title":"Nevada water resources data","language":"ENGLISH","doi":"10.3133/fs20053071","usgsCitation":"Water Resources Division, U.S. Geological Survey, 2005, Nevada water resources data: U.S. Geological Survey Fact Sheet 2005-3071, 2 p., https://doi.org/10.3133/fs20053071.","productDescription":"2 p.","costCenters":[],"links":[{"id":7328,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/fs/2005/3071/","linkFileType":{"id":5,"text":"html"}},{"id":120836,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/fs_2005_3071.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afee4b07f02db6979d5","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":534741,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":72354,"text":"sir20055148 - 2005 - Assessment of shallow ground-water quality in recently urbanized areas of Sacramento, California, 1998","interactions":[],"lastModifiedDate":"2012-02-02T00:14:01","indexId":"sir20055148","displayToPublicDate":"2005-09-24T00:00:00","publicationYear":"2005","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":"2005-5148","title":"Assessment of shallow ground-water quality in recently urbanized areas of Sacramento, California, 1998","docAbstract":"Evidence for anthropogenic impact on shallow ground-water quality beneath recently developed urban areas of Sacramento, California, has been observed in the sampling results from 19 monitoring wells in 1998. Eight volatile organic compounds (VOCs), four pesticides, and one pesticide transformation product were detected in low concentrations, and nitrate, as nitrogen, was detected in elevated concentrations; all of these concentrations were below National and State primary and secondary maximum contaminant levels. VOC results from this study are more consistent with the results from urban areas nationwide than from agricultural areas in the Central Valley, indicating that shallow ground-water quality has been impacted by urbanization. VOCs detected may be attributed to either the chlorination of drinking water, such as trichloromethane (chloroform) detected in 16 samples, or to the use of gasoline additives, such as methyl tert-butyl ether (MTBE), detected in 2 samples. Pesticides detected may be attributed to use on household lawns and gardens and rights-of-way, such as atrazine detected in three samples, or to past agricultural practices, and potentially to ground-water/surface-water interactions, such as bentazon detected in one sample from a well adjacent to the Sacramento River and downstream from where bentazon historically was used on rice. Concentrations of nitrate may be attributed to natural sources, animal waste, old septic tanks, and fertilizers used on lawns and gardens or previously used on agricultural crops. Seven sample concentrations of nitrate, as nitrogen, exceeded 3.0 milligrams per liter, a level that may indicate impact from human activities.\r\n\r\nGround-water recharge from rainfall or surface-water runoff also may contribute to the concentrations of VOCs and pesticides observed in ground water. Most VOCs and pesticides detected in ground-water samples also were detected in air and surface-water samples collected at sites within or adjacent to the recently developed urban areas.\r\n\r\nFive arsenic sample concentrations exceeded the U.S. Environmental Protection Agency (USEPA) primary maximum contaminant level (MCL) of 10 milligrams per liter adopted in 2001. Measurements that exceeded USEPA or California Department of Health Services recommended secondary maximum contaminant levels include manganese, iron, chloride, total dissolved solids, and specific conductance. These exceedances are probably a result of natural processes.\r\n\r\nVariations in stable isotope ratios of hydrogen (2H/1H) and oxygen (18O/16O) may indicate different sources or a mixing of recharge waters to the urban ground water. These variations also may indicate recharge directly from surface water in one well adjacent to the Sacramento River. Tritium concentrations indicate that most shallow ground water has been recharged since the mid-1950s, and tritium/helium-3 age dates suggest that recharge has occurred in the last 2 to 30 years in some areas. In areas where water table depths exceed 20 meters and wells are deeper, ground-water recharge may have occurred prior to 1950, but low concentrations of pesticides and VOCs detected in these deeper wells indicate a mixing of younger and older waters.\r\n\r\nOverall, the recently urbanized areas can be divided into two groups. One group contains wells where few VOCs and pesticides were detected, nitrate mostly was not detected, and National and State maximum contaminant levels, including the USEPA MCL for arsenic, were exceeded; these wells are adjacent to rivers and generally are characterized by younger water, shallow (1 to 4 meters) water table, chemically reducing conditions, finer grained sediments, and higher organics in the soils. In contrast, the other group contains wells where more VOCs, pesticides, and elevated nitrate concentrations were detected; these wells are farther from rivers and are generally characterized by a mixture of young and old waters, intermediate to deep (7 to 35 meters) wate","language":"ENGLISH","doi":"10.3133/sir20055148","usgsCitation":"Shelton, J.L., 2005, Assessment of shallow ground-water quality in recently urbanized areas of Sacramento, California, 1998 (Online only): U.S. Geological Survey Scientific Investigations Report 2005-5148, ix, 51 p. : ill., https://doi.org/10.3133/sir20055148.","productDescription":"ix, 51 p. : ill.","onlineOnly":"Y","costCenters":[],"links":[{"id":192977,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":7321,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/sir/2005/5148/","linkFileType":{"id":5,"text":"html"}}],"edition":"Online only","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4abae4b07f02db671e80","contributors":{"authors":[{"text":"Shelton, Jennifer L. 0000-0001-8508-0270 jshelton@usgs.gov","orcid":"https://orcid.org/0000-0001-8508-0270","contributorId":1155,"corporation":false,"usgs":true,"family":"Shelton","given":"Jennifer","email":"jshelton@usgs.gov","middleInitial":"L.","affiliations":[{"id":154,"text":"California Water Science Center","active":true,"usgs":true}],"preferred":true,"id":285479,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
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