{"pageNumber":"2404","pageRowStart":"60075","pageSize":"25","recordCount":184617,"records":[{"id":79143,"text":"ds205 - 2006 - Database for the geologic map of the Mount Baker 30-minute by 60-minute quadrangle, Washington (I-2660)","interactions":[],"lastModifiedDate":"2024-01-10T23:53:47.396801","indexId":"ds205","displayToPublicDate":"2006-09-19T00:00:00","publicationYear":"2006","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":310,"text":"Data Series","code":"DS","onlineIssn":"2327-638X","printIssn":"2327-0271","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"205","title":"Database for the geologic map of the Mount Baker 30-minute by 60-minute quadrangle, Washington (I-2660)","docAbstract":"<p>This digital map database has been prepared by R.W. Tabor from the published Geologic map of the Mount Baker 30- by 60-Minute Quadrangle, Washington. Together with the accompanying text files as PDF, it provides information on the geologic structure and stratigraphy of the area covered. The database delineates map units that are identified by general age and lithology following the stratigraphic nomenclature of the U.S. Geological Survey. The authors mapped most of the geology at 1:100,000. The Quaternary contacts and structural data have been much simplified for the 1:100,000-scale map and database. The spatial resolution (scale) of the database is 1:100,000 or smaller.</p><p>This database depicts the distribution of geologic materials and structures at a regional (1:100,000) scale. The report is intended to provide geologic information for the regional study of materials properties, earthquake shaking, landslide potential, mineral hazards, seismic velocity, and earthquake faults. In addition, the report contains information and interpretations about the regional geologic history and framework. However, the regional scale of this report does not provide sufficient detail for site development purposes.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ds205","usgsCitation":"Tabor, R.W., Haugerud, R., Hildreth, W., and Brown, E.H., 2006, Database for the geologic map of the Mount Baker 30-minute by 60-minute quadrangle, Washington (I-2660) (Version 1.0): U.S. Geological Survey Data Series 205, Report: 73 p.; Spatial Data; Metadata, https://doi.org/10.3133/ds205.","productDescription":"Report: 73 p.; Spatial Data; Metadata","additionalOnlineFiles":"Y","costCenters":[{"id":647,"text":"Western Earth Surface Processes","active":false,"usgs":true}],"links":[{"id":424297,"rank":7,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_77674.htm","linkFileType":{"id":5,"text":"html"}},{"id":8595,"rank":4,"type":{"id":16,"text":"Metadata"},"url":"https://pubs.usgs.gov/ds/2006/205/mbmetadata.txt","linkFileType":{"id":2,"text":"txt"}},{"id":8597,"rank":3,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/imap/i2660/pamphlet.pdf","text":"Pamphlet","linkFileType":{"id":1,"text":"pdf"},"description":"Pamphlet"},{"id":424296,"rank":6,"type":{"id":22,"text":"Related Work"},"url":"https://pubs.usgs.gov/publication/i2660","text":"IMAP 2660","linkFileType":{"id":5,"text":"html"}},{"id":8596,"rank":5,"type":{"id":23,"text":"Spatial Data"},"url":"https://pubs.usgs.gov/ds/2006/205/mbcovers2.tar.gz"},{"id":8594,"rank":2,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/ds/2006/205/","linkFileType":{"id":5,"text":"html"}},{"id":191243,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ds205.PNG"}],"scale":"100000","country":"United States","state":"Washington","otherGeospatial":"Mount Baker quadrangle","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -121,\n              48.5\n            ],\n            [\n              -121,\n              49\n            ],\n            [\n              -122,\n              49\n            ],\n            [\n              -122,\n              48.5\n            ],\n            [\n              -121,\n              48.5\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","edition":"Version 1.0","publicComments":"Map is cataloged on publication I2660, see related work link.","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4abce4b07f02db672cc7","contributors":{"authors":[{"text":"Tabor, R. W.","contributorId":16002,"corporation":false,"usgs":true,"family":"Tabor","given":"R.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":289217,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Haugerud, R. A. 0000-0001-7302-4351","orcid":"https://orcid.org/0000-0001-7302-4351","contributorId":42953,"corporation":false,"usgs":true,"family":"Haugerud","given":"R. A.","affiliations":[],"preferred":false,"id":289218,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Hildreth, Wes","contributorId":15996,"corporation":false,"usgs":true,"family":"Hildreth","given":"Wes","email":"","affiliations":[],"preferred":false,"id":289216,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Brown, E. H.","contributorId":78757,"corporation":false,"usgs":true,"family":"Brown","given":"E.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":289219,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":79144,"text":"ofr20061278 - 2006 - Photographs, correspondence, and presentations related to the La Conchita, California, landslide","interactions":[],"lastModifiedDate":"2012-02-02T00:14:15","indexId":"ofr20061278","displayToPublicDate":"2006-09-19T00:00:00","publicationYear":"2006","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":"2006-1278","title":"Photographs, correspondence, and presentations related to the La Conchita, California, landslide","docAbstract":"This report contains the following photographs and information related to the La Conchita, California, landslide: 1) Digital photographs taken by the author during a visit to the La Conchita landslide on January 14, 2005. 2) Correspondence related to the approval and release of USGS Open-File Report 2005-1067, Landslide Hazards at La Conchita, California. 3) A presentation on the La Conchita landslide that has been given to various organizations and groups since 2005.","language":"ENGLISH","doi":"10.3133/ofr20061278","collaboration":"see also OFR 2005-1067","usgsCitation":"Jibson, R.W., 2006, Photographs, correspondence, and presentations related to the La Conchita, California, landslide (Version 1.0): U.S. Geological Survey Open-File Report 2006-1278, 4 p. cover; 39 p. presentation; photographs, https://doi.org/10.3133/ofr20061278.","productDescription":"4 p. cover; 39 p. presentation; photographs","numberOfPages":"41","onlineOnly":"Y","additionalOnlineFiles":"Y","costCenters":[],"links":[{"id":190595,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":8598,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2006/1278/","linkFileType":{"id":5,"text":"html"}}],"edition":"Version 1.0","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adbe4b07f02db685dfb","contributors":{"authors":[{"text":"Jibson, Randall W. 0000-0003-3399-0875 jibson@usgs.gov","orcid":"https://orcid.org/0000-0003-3399-0875","contributorId":2985,"corporation":false,"usgs":true,"family":"Jibson","given":"Randall","email":"jibson@usgs.gov","middleInitial":"W.","affiliations":[{"id":300,"text":"Geologic Hazards Science Center","active":true,"usgs":true}],"preferred":true,"id":289220,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":79145,"text":"sir20065090 - 2006 - Evaluation of geophysical logs and aquifer-isolation tests, Phase III, August 2002 to March 2004, Crossley Farm superfund site, Hereford township, Berks County, Pennsylvania","interactions":[],"lastModifiedDate":"2017-07-06T16:12:35","indexId":"sir20065090","displayToPublicDate":"2006-09-19T00:00:00","publicationYear":"2006","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":"2006-5090","title":"Evaluation of geophysical logs and aquifer-isolation tests, Phase III, August 2002 to March 2004, Crossley Farm superfund site, Hereford township, Berks County, Pennsylvania","docAbstract":"<p>Between August 2002 and March 2004, geophysical logging was conducted in 23 boreholes at the Crossley Farm Superfund Site, Hereford Township, Berks County, Pa., to determine the water-producing zones, water-receiving zones, zones of vertical-borehole flow, and fracture orientation where applicable. The boreholes ranged in depth from 71 to 503 ft (feet) below land surface. The geophysical logging determined the placement of well screens and packers, which allow monitoring and sampling of water-bearing zones in the fractured bedrock so the horizontal and vertical distribution of contaminated ground water migrating from known sources could be determined. Geophysical logging included collection of caliper (22 boreholes), fluid-temperature (17 boreholes), single-pointresistance (17 boreholes), natural-gamma (17 boreholes), fluidflow (18 boreholes), and acoustic-televiewer (13 boreholes) logs. Caliper and acoustic-televiewer logs were used to locate fractures, joints, and weathered zones. Inflections on fluid-temperature and single-point-resistance logs indicated possible water-bearing zones, and flowmeter measurements verified these locations. Single-point-resistance, natural-gamma, and geologist logs provided information on stratigraphy; the geologist log also provided information on the location of possible water-producing zones.</p><p>Borehole geophysical logging and heatpulse flowmetering indicated active flow in 10 boreholes. Seven of the boreholes are in ground-water discharge areas and three boreholes are in ground-water recharge areas. Heatpulse flowmetering, in conjunction with the geologist logs, indicates lithologic contacts (changes in lithology from a gneiss dominated by quartz-plagioclase-feldspar mineralogy to a gneiss dominated by hornblende mineralogy) are typically fractured, permeable, and effective transmitters of water. </p><p>Single-well, aquifer-isolation (packer) tests were performed on two boreholes. Packers were set at depths ranging from 210 to 465 ft below land surface to isolate water-bearing zones at discrete intervals. Placement and inflation of the packers provided information on hydraulic heads, specific capacities, the hydraulic connection between intervals, and depth-specific water-quality samples. </p><p>Upon completion of borehole geophysical logging and interpretation of geophysical logs, geologist logs, drillers notes, and packer work, 13 boreholes were reconstructed such that water levels could be monitored and water samples could be collected from discrete shallow, intermediate, and deep waterbearing fractures in each borehole. Boreholes BE-1672, BE-1674, BE-1676, and BE-1677 remained open-hole for sampling purposes. Boreholes RI-2, RI-3, and RI-4 remained openhole for injection purposes. Boreholes P-1, P-2, and P-3 remained open and were converted to pumping wells. </p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/sir20065090","collaboration":"In cooperation with the U.S. Environmental Protection Agency","usgsCitation":"Conger, R.W., and Low, D.J., 2006, Evaluation of geophysical logs and aquifer-isolation tests, Phase III, August 2002 to March 2004, Crossley Farm superfund site, Hereford township, Berks County, Pennsylvania: U.S. Geological Survey Scientific Investigations Report 2006-5090, ix, 96 p., https://doi.org/10.3133/sir20065090.","productDescription":"ix, 96 p.","onlineOnly":"Y","temporalStart":"2002-08-01","temporalEnd":"2004-03-30","costCenters":[{"id":532,"text":"Pennsylvania Water Science Center","active":true,"usgs":true}],"links":[{"id":191987,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":8599,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/sir/2006/5090/","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Pennsylvania","county":"Hereford Township, Berks County","otherGeospatial":"Crossley Farm Superfund Site","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -76.08333333333333,40.666666666666664 ], [ -76.08333333333333,40.75 ], [ -75.91666666666667,40.75 ], [ -75.91666666666667,40.666666666666664 ], [ -76.08333333333333,40.666666666666664 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae0e4b07f02db688303","contributors":{"authors":[{"text":"Conger, Randall W. rwconger@usgs.gov","contributorId":2086,"corporation":false,"usgs":true,"family":"Conger","given":"Randall","email":"rwconger@usgs.gov","middleInitial":"W.","affiliations":[{"id":532,"text":"Pennsylvania Water Science Center","active":true,"usgs":true}],"preferred":true,"id":289221,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Low, Dennis J. djlow@usgs.gov","contributorId":3450,"corporation":false,"usgs":true,"family":"Low","given":"Dennis","email":"djlow@usgs.gov","middleInitial":"J.","affiliations":[{"id":532,"text":"Pennsylvania Water Science Center","active":true,"usgs":true}],"preferred":true,"id":289222,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":79142,"text":"ofr20051193 - 2006 - Report of the USGS Coastal and Marine Geology Modeling Workshop, Pacific Marine Science Center, Santa Cruz, CA, March 22-23, 2005","interactions":[],"lastModifiedDate":"2012-02-02T00:14:11","indexId":"ofr20051193","displayToPublicDate":"2006-09-19T00:00:00","publicationYear":"2006","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":"2005-1193","title":"Report of the USGS Coastal and Marine Geology Modeling Workshop, Pacific Marine Science Center, Santa Cruz, CA, March 22-23, 2005","docAbstract":"A U.S. Geological Survey (USGS) Coastal and Marine Geology (CMG) Modeling Workshop was held to discuss the general topic of coastal modeling, defined broadly to include circulation, waves, sediment transport, water quality, ecology, sediment diagenesis, morphology change, and coastal evolution, on scales ranging from seconds and a few centimeters (individual ripples) to centuries (coastal evolution) and thousands of kilometers (tsunami propagation). The workshop was convened at the suggestion of CMG Program Management to improve communication among modelers and model users, assess modeling-related activities being conducted at the three centers (Florida Integrated Science Center, FISC; Pacific Marine Science Center; PMSC; and Woods Hole Science Center; WHSC), and develop goals, strategies, and plans for future modeling activities. The workshop represents a step toward developing a five-year strategic plan, and was timed to provide input for the FY06 prospectus. The workshop was held at the USGS Pacific Marine Science Center in Santa Cruz on March 22-23, 2005.","language":"ENGLISH","doi":"10.3133/ofr20051193","usgsCitation":"Sherwood, C.R., 2006, Report of the USGS Coastal and Marine Geology Modeling Workshop, Pacific Marine Science Center, Santa Cruz, CA, March 22-23, 2005: U.S. Geological Survey Open-File Report 2005-1193, iii, 15 p., https://doi.org/10.3133/ofr20051193.","productDescription":"iii, 15 p.","numberOfPages":"18","onlineOnly":"Y","temporalStart":"2005-03-22","temporalEnd":"2005-03-23","costCenters":[],"links":[{"id":191986,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":8593,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2005/1193/","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a5ae4b07f02db630906","contributors":{"authors":[{"text":"Sherwood, Christopher R. 0000-0001-6135-3553 csherwood@usgs.gov","orcid":"https://orcid.org/0000-0001-6135-3553","contributorId":2866,"corporation":false,"usgs":true,"family":"Sherwood","given":"Christopher","email":"csherwood@usgs.gov","middleInitial":"R.","affiliations":[{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":true,"id":289215,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":79137,"text":"ofr20061231 - 2006 - Hawaiian Volcano Observatory seismic data, January to December 2005","interactions":[],"lastModifiedDate":"2012-02-02T00:13:57","indexId":"ofr20061231","displayToPublicDate":"2006-09-16T00:00:00","publicationYear":"2006","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":"2006-1231","title":"Hawaiian Volcano Observatory seismic data, January to December 2005","docAbstract":"The Hawaiian Volcano Observatory (HVO) summary presents seismic data gathered during the year. The seismic summary is offered without interpretation as a source of preliminary data. It is complete in the sense that most data for events of M-1.5 routinely gathered by the Observatory are included.\r\n\r\nThe HVO summaries have been published in various forms since 1956. Summaries prior to 1974 were issued quarterly, but cost, convenience of preparation and distribution, and the large quantities of data dictated an annual publication beginning with Summary 74 for the year 1974. Summary 86 (the introduction of CUSP at HVO) includes a description of the seismic instrumentation, calibration, and processing used in recent years. Beginning with 2004, summaries will simply be identified by the year, rather than Summary number. The present summary includes background information on the seismic network and processing to allow use of the data and to provide an understanding of how they were gathered.\r\n\r\nA report by Klein and Koyanagi (1980) tabulates instrumentation, calibration, and recording history of each seismic station in the network. It is designed as a reference for users of seismograms and phase data and includes and augments the information in the station table in this summary. ","language":"ENGLISH","doi":"10.3133/ofr20061231","usgsCitation":"Nakata, J.S., 2006, Hawaiian Volcano Observatory seismic data, January to December 2005: U.S. Geological Survey Open-File Report 2006-1231, 84 p., https://doi.org/10.3133/ofr20061231.","productDescription":"84 p.","numberOfPages":"84","temporalStart":"2005-01-01","temporalEnd":"2005-12-31","costCenters":[{"id":615,"text":"Volcano Hazards Program","active":true,"usgs":true}],"links":[{"id":191151,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":8585,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2006/1231/","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a6be4b07f02db63d86d","contributors":{"authors":[{"text":"Nakata, Jennifer S.","contributorId":18364,"corporation":false,"usgs":true,"family":"Nakata","given":"Jennifer","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":289202,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":79132,"text":"ofr20061253 - 2006 - Assessment of undiscovered technically recoverable conventional petroleum resources of northern Afghanistan","interactions":[],"lastModifiedDate":"2021-09-29T11:46:52.700687","indexId":"ofr20061253","displayToPublicDate":"2006-09-16T00:00:00","publicationYear":"2006","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":"2006-1253","title":"Assessment of undiscovered technically recoverable conventional petroleum resources of northern Afghanistan","docAbstract":"<p>Using a geology-based assessment methodology, the U.S. Geological Survey - Afghanistan Ministry of Mines and Industry Joint Oil and Gas Resource Assessment Team estimated mean volumes of undiscovered petroleum in northern Afghanistan; the resulting estimates are 1.6 billion barrels (0.2 billion metric tons) of crude oil, 16 trillion cubic feet (0.4 trillion cubic meters) of natural gas, and 0.5 billion barrels (0.8 billion metric tons) of natural gas liquids. Most of the undiscovered crude oil is in the Afghan-Tajik Basin and most of the undiscovered natural gas is in the Amu Darya Basin. Four total petroleum systems were identified, and these were subdivided into eight assessment units for the purpose of this resource assessment. The area with the greatest potential for undiscovered natural gas accumulations is in Upper Jurassic carbonate and reef reservoirs beneath an impermeable salt layer in relatively unexplored parts of northern Afghanistan. The Afghan-Tajik Basin has the greatest potential for undiscovered crude oil accumulations, and these are potentially in Cretaceous to Paleogene carbonate reservoir rocks associated with thrust faulting and folding.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr20061253","collaboration":"see also FS 2006-3031","usgsCitation":"Klett, T., Ulmishek, G., Wandrey, C., Agena, W.F., and Steinshouer, D., 2006, Assessment of undiscovered technically recoverable conventional petroleum resources of northern Afghanistan (Version 1.0): U.S. Geological Survey Open-File Report 2006-1253, Report: vii, 237 p.; Figure 11; Table 1; CD-ROM, https://doi.org/10.3133/ofr20061253.","productDescription":"Report: vii, 237 p.; Figure 11; Table 1; CD-ROM","numberOfPages":"244","onlineOnly":"N","additionalOnlineFiles":"Y","costCenters":[],"links":[{"id":300170,"rank":5,"type":{"id":7,"text":"Companion Files"},"url":"https://pubs.usgs.gov/of/2006/1253/ofr2006-1253_pdf_documents.zip","text":"Assessment Figures and Appendices","size":"17.6 MB","linkFileType":{"id":6,"text":"zip"},"description":"Assessment Figures and Appendices"},{"id":300040,"rank":4,"type":{"id":7,"text":"Companion Files"},"url":"https://pubs.usgs.gov/of/2006/1253/pdf_documents/Table1.pdf","text":"Table 1","linkFileType":{"id":1,"text":"pdf"},"description":"Table 1","linkHelpText":"Assessment Result"},{"id":300038,"rank":3,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/2006/1253/of2006-1253.pdf","text":"Report","linkFileType":{"id":1,"text":"pdf"},"description":"Report"},{"id":195617,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ofr20061253.PNG"},{"id":8578,"rank":2,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2006/1253/","linkFileType":{"id":5,"text":"html"}}],"country":"Afghanistan","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"Polygon\",\"coordinates\":[[[61.21082,35.65007],[62.23065,35.27066],[62.98466,35.40404],[63.19354,35.85717],[63.9829,36.00796],[64.54648,36.31207],[64.74611,37.11182],[65.58895,37.30522],[65.74563,37.66116],[66.21738,37.39379],[66.51861,37.36278],[67.07578,37.35614],[67.83,37.14499],[68.13556,37.02312],[68.85945,37.34434],[69.19627,37.15114],[69.51879,37.609],[70.11658,37.58822],[70.27057,37.73516],[70.3763,38.1384],[70.80682,38.48628],[71.34813,38.25891],[71.2394,37.95327],[71.54192,37.90577],[71.44869,37.06564],[71.84464,36.73817],[72.19304,36.94829],[72.63689,37.04756],[73.26006,37.49526],[73.9487,37.42157],[74.98,37.41999],[75.15803,37.13303],[74.57589,37.02084],[74.06755,36.83618],[72.92002,36.72001],[71.84629,36.50994],[71.26235,36.07439],[71.49877,35.65056],[71.61308,35.1532],[71.11502,34.73313],[71.15677,34.34891],[70.8818,33.98886],[69.93054,34.02012],[70.32359,33.35853],[69.68715,33.1055],[69.26252,32.50194],[69.31776,31.90141],[68.92668,31.62019],[68.55693,31.71331],[67.79269,31.58293],[67.68339,31.30315],[66.93889,31.30491],[66.38146,30.7389],[66.34647,29.88794],[65.04686,29.47218],[64.35042,29.56003],[64.148,29.34082],[63.55026,29.46833],[62.54986,29.31857],[60.87425,29.82924],[61.78122,30.73585],[61.69931,31.37951],[60.94194,31.54807],[60.86365,32.18292],[60.53608,32.98127],[60.9637,33.52883],[60.52843,33.67645],[60.80319,34.4041],[61.21082,35.65007]]]},\"properties\":{\"name\":\"Afghanistan\"}}]}","edition":"Version 1.0","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4acfe4b07f02db680219","contributors":{"authors":[{"text":"Klett, T. R. 0000-0001-9779-1168","orcid":"https://orcid.org/0000-0001-9779-1168","contributorId":83067,"corporation":false,"usgs":true,"family":"Klett","given":"T. R.","affiliations":[],"preferred":false,"id":289191,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Ulmishek, G. F.","contributorId":89144,"corporation":false,"usgs":true,"family":"Ulmishek","given":"G. F.","affiliations":[],"preferred":false,"id":289192,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Wandrey, C. J.","contributorId":99578,"corporation":false,"usgs":true,"family":"Wandrey","given":"C. J.","affiliations":[],"preferred":false,"id":289193,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Agena, Warren F. wagena@usgs.gov","contributorId":3181,"corporation":false,"usgs":true,"family":"Agena","given":"Warren","email":"wagena@usgs.gov","middleInitial":"F.","affiliations":[{"id":164,"text":"Central Energy Resources Science Center","active":true,"usgs":true}],"preferred":true,"id":289189,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Steinshouer, Douglas","contributorId":10502,"corporation":false,"usgs":true,"family":"Steinshouer","given":"Douglas","affiliations":[],"preferred":false,"id":289190,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":79133,"text":"ofr20061237 - 2006 - Assessment of Appalachian basin oil and gas resources: Devonian shale— Middle and Upper Paleozoic Total Petroleum System","interactions":[],"lastModifiedDate":"2021-09-14T18:31:02.404869","indexId":"ofr20061237","displayToPublicDate":"2006-09-16T00:00:00","publicationYear":"2006","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":"2006-1237","title":"Assessment of Appalachian basin oil and gas resources: Devonian shale— Middle and Upper Paleozoic Total Petroleum System","docAbstract":"The U.S. Geological Survey (USGS) recently completed an assessment of the technically recoverable undiscovered hydrocarbon resources of the Appalachian Basin Province. The assessment province includes parts of New York, Pennsylvania, Ohio, Maryland, West Virginia, Virginia, Kentucky, Tennessee, Georgia and Alabama. The assessment was based on six major petroleum systems, which include strata that range in age from Cambrian to Pennsylvanian. The Devonian Shale-Middle and Upper Paleozoic Total Petroleum System (TPS) extends generally from New York to Tennessee. This petroleum system has produced a large proportion of the oil and natural gas that has been discovered in the Appalachian basin since the drilling of the Drake well in Pennsylvania in 1859.\r\n\r\nFor assessment purposes, the TPS was divided into 10 assessment units (plays), 4 of which were classified as conventional and 6 as continuous. The results were reported as fully risked fractiles (F95, F50, F5 and the Mean), with the fractiles indicating the probability of recovery of the assessment amount. Products reported were oil (millions of barrels of oil, MMBO), gas (billions of cubic feet of gas, BCFG), and natural gas liquids (millions of barrels of natural gas liquids, MMBNGL). The mean estimates for technically recoverable undiscovered hydrocarbons in the TPS are: 7.53 MMBO, 31,418.88 BCFG (31.42 trillion cubic feet) of gas, and 562.07 MMBNGL.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr20061237","usgsCitation":"Milici, R.C., and Swezey, C., 2006, Assessment of Appalachian basin oil and gas resources: Devonian shale— Middle and Upper Paleozoic Total Petroleum System: U.S. Geological Survey Open-File Report 2006-1237, 70 p., https://doi.org/10.3133/ofr20061237.","productDescription":"70 p.","numberOfPages":"70","onlineOnly":"Y","additionalOnlineFiles":"Y","costCenters":[],"links":[{"id":194634,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":8579,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2006/1237/","linkFileType":{"id":5,"text":"html"}},{"id":389221,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_77661.htm"}],"country":"United States","otherGeospatial":"Appalachian Basin oil and gas resources","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -85,36 ], [ -85,43 ], [ -75,43 ], [ -75,36 ], [ -85,36 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4abbe4b07f02db67299f","contributors":{"authors":[{"text":"Milici, Robert C. rmilici@usgs.gov","contributorId":563,"corporation":false,"usgs":true,"family":"Milici","given":"Robert","email":"rmilici@usgs.gov","middleInitial":"C.","affiliations":[{"id":241,"text":"Eastern Energy Resources Science Center","active":true,"usgs":true}],"preferred":true,"id":289194,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Swezey, Christopher S.","contributorId":52640,"corporation":false,"usgs":true,"family":"Swezey","given":"Christopher S.","affiliations":[],"preferred":false,"id":289195,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":79136,"text":"ofr20061263 - 2006 - Abstracts of the Annual Meeting of Planetary Geologic Mappers, Nampa, Idaho 2006","interactions":[],"lastModifiedDate":"2018-09-19T19:00:41","indexId":"ofr20061263","displayToPublicDate":"2006-09-16T00:00:00","publicationYear":"2006","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":"2006-1263","title":"Abstracts of the Annual Meeting of Planetary Geologic Mappers, Nampa, Idaho 2006","docAbstract":"Approximately 18 people attended this year's mappers meeting, and many more submitted abstracts and maps in absentia. The meeting was held on the campus of Northwest Nazarene University (NNU), and was graciously hosted by NNU's School of Health and Science. Planetary mapper Dr. Jim Zimbelman is an alumnus of NNU, and he was pivotal in organizing the meeting at this location. Oral and poster presentations were given on Friday, June 30. Drs. Bill Bonnichsen and Marty Godchaux led field excursions on July 1 and 2. \r\n\r\nUSGS Astrogeology Team Chief Scientist Lisa Gaddis led the meeting with a brief discussion of the status of the planetary mapping program at USGS, and a more detailed description of the Lunar Mapping Program. She indicated that there is now a functioning website (http://astrogeology.usgs.gov/Projects/PlanetaryMapping/Lunar/) which shows which lunar quadrangles are available to be mapped. Like other USGS-published maps, proposals to complete a lunar geologic map must be submitted to the regular Planetary Geology & Geophysics (PGG) program for peer review. Jim Skinner (USGS) later presented the progress of the 1:2.5M-scale map of the lunar Copernicus quadrangle, and demonstrated the wide range of data that are available to support these maps. Gaddis and Skinner encouraged the community to submit proposals for generating lunar geologic maps, and reminded us that, as for all planetary maps, the project must be science-driven. \r\n\r\nVenus mapper Jim Zimbelman of the Smithsonian Institution (SI) presented the progress for his V-15 and V-16 quadrangles; Vicki Hansen (University of Minnesota Duluth) showed her preliminary work on V-45. Zimbelman addressed an issue that has been plaguing the community: 'delinquent Venus mappers'. In short, there were a number of Venus maps funded in the early 1990s under the Venus Data Analysis Program (VDAP). Unfortunately, funding for this program was cut before many Venus maps could be completed, resulting in about 10 Venus maps that were initially assigned but have shown little or no progress in many years. Zimbelman announced that he was not going to be able to complete quadrangle V-27 that he was assigned under VDAP, and was therefore returning that quadrangle to the community; he invited people to propose to PGG to map this quadrangle. \r\n\r\nDave Williams of Arizona State University (ASU) reported on the progress of his global Io map. His mapping team recently received the completed, controlled global mosaic (using Voyager and Galileo images) from the USGS; this will be the basemap for their geologic mapping. Furthermore, the three team members (Laszlo Keszthelyi, David Crown and Dave Williams) have calibrated their individual mapping techniques by each mapping the same region for comparison. Thomas Doggett (ASU) showed progress on the global Europa map that was awarded to Ron Greeley. There was some consternation expressed on the methodology for determining relative ages of the lineaments; it was suggested that Vicki Hansen contact Patricio Figueredo (Exxon) directly, because Figueredo is the one who has been developing the lineament mapping techniques. \r\n\r\nMars remains the most popular planet to map. Kevin Williams (SI) and Corey Fortezzo (SI) presented progress on their 1:500K maps in the Margaritifer Terra region of Mars. Jim Zimbelman described his 1:1M Medusae Fossae map, which is nearing completion. Peter Mouginis-Mark (University of Hawai'i) reported progress on his 1:200K maps of Tooting crater and of the Olympus Mons summit caldera. Jim Skinner discussed the progress of his and Ken Herkenhoff?s (USGS) map (1:500K) on the Olympia Cavi region of Mars? north pole, and Eric Kolb (USGS) presented work that he and Ken Tanaka (USGS) are completing on the Martian south pole. David Crown of the Planetary Science Institute (PSI) reported on numerous 1:500K and 1:1M maps in the Hellas and Hesperia regions of Mars. Frank Chuang (PSI) discussed progress on mapping the Deuteronilus Mensae reg","language":"ENGLISH","publisher":"Geological Survey (U.S.)","doi":"10.3133/ofr20061263","usgsCitation":"Tanaka, K.L., and Saunders, R.S., 2006, Abstracts of the Annual Meeting of Planetary Geologic Mappers, Nampa, Idaho 2006 (Version 1.0): U.S. Geological Survey Open-File Report 2006-1263, 54 p., https://doi.org/10.3133/ofr20061263.","productDescription":"54 p.","numberOfPages":"54","onlineOnly":"Y","temporalStart":"2006-06-30","temporalEnd":"2006-07-02","costCenters":[{"id":130,"text":"Astrogeology Research Center","active":false,"usgs":true}],"links":[{"id":191150,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":8582,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2006/1263/","linkFileType":{"id":5,"text":"html"}},{"id":8583,"rank":9999,"type":{"id":25,"text":"Version History"},"url":"https://pubs.usgs.gov/of/2006/1263/version_history.txt","linkFileType":{"id":2,"text":"txt"}}],"edition":"Version 1.0","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b13e4b07f02db6a3a23","contributors":{"editors":[{"text":"Gregg, Tracy K. P.","contributorId":57937,"corporation":false,"usgs":true,"family":"Gregg","given":"Tracy K. P.","affiliations":[],"preferred":false,"id":745706,"contributorType":{"id":2,"text":"Editors"},"rank":1}],"authors":[{"text":"Tanaka, Kenneth L. ktanaka@usgs.gov","contributorId":610,"corporation":false,"usgs":true,"family":"Tanaka","given":"Kenneth","email":"ktanaka@usgs.gov","middleInitial":"L.","affiliations":[{"id":131,"text":"Astrogeology Science Center","active":true,"usgs":true}],"preferred":true,"id":289199,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Saunders, R. Stephen","contributorId":70842,"corporation":false,"usgs":true,"family":"Saunders","given":"R.","email":"","middleInitial":"Stephen","affiliations":[],"preferred":false,"id":289201,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":79140,"text":"fs20063094N - 2006 - Navajo coal and air quality in Shiprock, New Mexico","interactions":[],"lastModifiedDate":"2026-01-29T20:55:42.703812","indexId":"fs20063094N","displayToPublicDate":"2006-09-16T00:00:00","publicationYear":"2006","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":"2006-3094","title":"Navajo coal and air quality in Shiprock, New Mexico","docAbstract":"Among the Navajo people, high levels of respiratory disease, such as asthma, exist in a population with low rates of cigarette smoking. Air quality outdoors and indoors affects respiratory health. Many Navajo Nation residents burn locally mined coal in their homes for heat, as coal is the most economical energy source. The U.S. Geological Survey and Dine College, in cooperation with the Navajo Division of Health, are conducting a study in the Shiprock, New Mexico, area to determine if indoor use of this coal might be contributing to some of the respiratory health problems experienced by the residents. Researchers in this study will (1) examine respiratory health data, (2) identify stove type and use, (3) analyze samples of coal that are used locally, and (4) measure and characterize air quality inside selected homes. This Fact Sheet summarizes the interim results of the study in both English and Navajo.\r\n\r\nThis Fact Sheet is available in three versions:\r\n\r\n    * English [800-KB PDF file ]\r\n    * Navajo [computer must have Navajo language fonts installed - 304-KB PDF file]\r\n    * Image of the Navajo language version [19.8-MB PDF file]","language":"English, Navajo","publisher":"U.S. Geological Survey","doi":"10.3133/fs20063094N","usgsCitation":"Bunnell, J.E., and Garcia, L.V., 2006, Navajo coal and air quality in Shiprock, New Mexico (Navajo Version 1.0): U.S. Geological Survey Fact Sheet 2006-3094, 1 p., https://doi.org/10.3133/fs20063094N.","productDescription":"1 p.","numberOfPages":"1","costCenters":[],"links":[{"id":8588,"rank":2,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/fs/2006/3094/","linkFileType":{"id":5,"text":"html"}},{"id":125032,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/fs_2006_3094.jpg"}],"edition":"Navajo Version 1.0","publicComments":"Computer must have Navajo language fonts installed; see also English version","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b00e4b07f02db697f6b","contributors":{"authors":[{"text":"Bunnell, Joseph E. jbunnell@usgs.gov","contributorId":556,"corporation":false,"usgs":true,"family":"Bunnell","given":"Joseph","email":"jbunnell@usgs.gov","middleInitial":"E.","affiliations":[],"preferred":true,"id":289206,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Garcia, Linda V.","contributorId":107787,"corporation":false,"usgs":true,"family":"Garcia","given":"Linda","email":"","middleInitial":"V.","affiliations":[],"preferred":false,"id":289207,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":79135,"text":"ofr20061230 - 2006 - Physical properties of two core samples from Well 34-9RD2 at the Coso geothermal field, California","interactions":[],"lastModifiedDate":"2019-07-17T17:02:48","indexId":"ofr20061230","displayToPublicDate":"2006-09-16T00:00:00","publicationYear":"2006","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":"2006-1230","title":"Physical properties of two core samples from Well 34-9RD2 at the Coso geothermal field, California","docAbstract":"The Coso geothermal field, located along the Eastern California Shear Zone, is composed of fractured granitic rocks above a shallow heat source. Temperatures exceed 640 ?F (~338 ?C) at a depth of less than 10000 feet (3 km). Permeability varies throughout the geothermal field due to the competing processes of alteration and mineral precipitation, acting to reduce the interconnectivity of faults and fractures, and the generation of new fractures through faulting and brecciation. Currently, several hot regions display very low permeability, not conducive to the efficient extraction of heat. Because high rates of seismicity in the field indicate that the area is highly stressed, enhanced permeability can be stimulated by increasing the fluid pressure at depth to induce faulting along the existing network of fractures. Such an Enhanced Geothermal System (EGS), planned for well 46A-19RD, would greatly facilitate the extraction of geothermal fluids from depth by increasing the extent and depth of the fracture network.\r\n\r\nIn order to prepare for and interpret data from such a stimulation experiment, the physical properties and failure behavior of the target rocks must be fully understood. Various diorites and granodiorites are the predominant rock types in the target area of the well, which will be pressurized from 10000 feet measured depth (MD) (3048m MD) to the bottom of the well at 13,000 feet MD (3962 m MD). Because there are no core rocks currently available from well 46A-19RD, we report here on the results of compressive strength, frictional sliding behavior, and elastic measurements of a granodiorite and diorite from another well, 34-9RD2, at the Coso site. Rocks cored from well 34-9RD2 are the deepest samples to date available for testing, and are representative of rocks from the field in general.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr20061230","usgsCitation":"Morrow, C., and Lockner, D., 2006, Physical properties of two core samples from Well 34-9RD2 at the Coso geothermal field, California (Version 1.0): U.S. Geological Survey Open-File Report 2006-1230, 32 p., https://doi.org/10.3133/ofr20061230.","productDescription":"32 p.","numberOfPages":"32","costCenters":[{"id":234,"text":"Earthquake Hazards Program","active":true,"usgs":true},{"id":237,"text":"Earthquake Science Center","active":true,"usgs":true}],"links":[{"id":194508,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":8581,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2006/1230/","linkFileType":{"id":5,"text":"html"}}],"edition":"Version 1.0","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adbe4b07f02db685b47","contributors":{"authors":[{"text":"Morrow, C.A.","contributorId":99977,"corporation":false,"usgs":true,"family":"Morrow","given":"C.A.","email":"","affiliations":[],"preferred":false,"id":289198,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Lockner, D.A. 0000-0001-8630-6833","orcid":"https://orcid.org/0000-0001-8630-6833","contributorId":85603,"corporation":false,"usgs":true,"family":"Lockner","given":"D.A.","affiliations":[],"preferred":false,"id":289197,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":79139,"text":"fs20063094 - 2006 - Navajo coal and air quality in Shiprock, New Mexico","interactions":[],"lastModifiedDate":"2012-02-02T00:14:11","indexId":"fs20063094","displayToPublicDate":"2006-09-16T00:00:00","publicationYear":"2006","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":"2006-3094","title":"Navajo coal and air quality in Shiprock, New Mexico","docAbstract":"Among the Navajo people, high levels of respiratory disease, such as asthma, exist in a population with low rates of cigarette smoking. Air quality outdoors and indoors affects respiratory health. Many Navajo Nation residents burn locally mined coal in their homes for heat, as coal is the most economical energy source. The U.S. Geological Survey and Dine College, in cooperation with the Navajo Division of Health, are conducting a study in the Shiprock, New Mexico, area to determine if indoor use of this coal might be contributing to some of the respiratory health problems experienced by the residents. Researchers in this study will (1) examine respiratory health data, (2) identify stove type and use, (3) analyze samples of coal that are used locally, and (4) measure and characterize air quality inside selected homes. This Fact Sheet summarizes the interim results of the study in both English and Navajo.","language":"ENGLISH","doi":"10.3133/fs20063094","collaboration":"see also Navajo version","usgsCitation":"Bunnell, J.E., and Garcia, L.V., 2006, Navajo coal and air quality in Shiprock, New Mexico (English Version 1.0): U.S. Geological Survey Fact Sheet 2006-3094, 1 p., https://doi.org/10.3133/fs20063094.","productDescription":"1 p.","numberOfPages":"1","onlineOnly":"N","additionalOnlineFiles":"Y","costCenters":[],"links":[{"id":122416,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/fs_2006_3094.jpg"},{"id":8587,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/fs/2006/3094/","linkFileType":{"id":5,"text":"html"}},{"id":8589,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/fs/2006/3094/fs2006-3094_nav.pdf","linkFileType":{"id":1,"text":"pdf"}}],"edition":"English Version 1.0","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b00e4b07f02db697f2b","contributors":{"authors":[{"text":"Bunnell, Joseph E. jbunnell@usgs.gov","contributorId":556,"corporation":false,"usgs":true,"family":"Bunnell","given":"Joseph","email":"jbunnell@usgs.gov","middleInitial":"E.","affiliations":[],"preferred":true,"id":289204,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Garcia, Linda V.","contributorId":107787,"corporation":false,"usgs":true,"family":"Garcia","given":"Linda","email":"","middleInitial":"V.","affiliations":[],"preferred":false,"id":289205,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":79138,"text":"ofr20061279 - 2006 - A Spatial Overlay Ranking Method for a Geospatial Search of Text Objects","interactions":[],"lastModifiedDate":"2012-02-02T00:14:21","indexId":"ofr20061279","displayToPublicDate":"2006-09-16T00:00:00","publicationYear":"2006","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":"2006-1279","title":"A Spatial Overlay Ranking Method for a Geospatial Search of Text Objects","docAbstract":"Earth-science researchers need the capability to find relevant information by location and topic. Conventional geographic techniques that simply check whether polygons intersect can efficiently achieve a high recall on location, but can not achieve precision for ranking results in likely order of importance to the reader. A spatial overlay ranking based upon how well an object's footprint matches the search area provides a more effective way to spatially search a collection of reports, and avoids many of the problems associated with an 'in/out' (True/False) boolean search. Moreover, spatial overlay ranking appears to work well even when spatial extent is defined only by a simple bounding box.","language":"ENGLISH","publisher":"Geological Survey (U.S.)","doi":"10.3133/ofr20061279","usgsCitation":"Lanfear, K.J., 2006, A Spatial Overlay Ranking Method for a Geospatial Search of Text Objects: U.S. Geological Survey Open-File Report 2006-1279, 9 p., https://doi.org/10.3133/ofr20061279.","productDescription":"9 p.","numberOfPages":"9","onlineOnly":"Y","costCenters":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"links":[{"id":194524,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":8586,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2006/1279/","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53cd4969e4b0b290850ef248","contributors":{"authors":[{"text":"Lanfear, Kenneth J.","contributorId":20738,"corporation":false,"usgs":true,"family":"Lanfear","given":"Kenneth","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":289203,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":79134,"text":"sir20065188 - 2006 - Annual trace-metal load estimates and flow-weighted concentrations of cadmium, lead, and zinc, in the Spokane River basin, Idaho and Washington, 1999-2004","interactions":[],"lastModifiedDate":"2022-01-27T20:41:45.606501","indexId":"sir20065188","displayToPublicDate":"2006-09-16T00:00:00","publicationYear":"2006","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":"2006-5188","title":"Annual trace-metal load estimates and flow-weighted concentrations of cadmium, lead, and zinc, in the Spokane River basin, Idaho and Washington, 1999-2004","docAbstract":"<p class=\"indent\">Streamflow and trace-metal concentration data collected at 10 locations in the Spokane River basin of northern Idaho and eastern Washington during 1999-2004 were used as input for the U.S. Geological Survey software, LOADEST, to estimate annual loads and mean flow-weighted concentrations of total and dissolved cadmium, lead, and zinc.</p><p class=\"indent\">Cadmium composed less than 1 percent of the total metal load at all stations; lead constituted from 6 to 42 percent of the total load at stations upstream from Coeur d’Alene Lake and from 2 to 4 percent at stations downstream of the lake. Zinc composed more than 90 percent of the total metal load at 6 of the 10 stations examined in this study.</p><p class=\"indent\">Trace-metal loads were lowest at the station on Pine Creek below Amy Gulch, where the mean annual total cadmium load for 1999–2004 was 39 kilograms per year (kg/yr), the mean estimated total lead load was about 1,700 kg/yr, and the mean annual total zinc load was 14,000 kg/yr. The trace-metal loads at stations on North Fork Coeur d’Alene River at Enaville, Ninemile Creek, and Canyon Creek also were relatively low.</p><p class=\"indent\">Trace-metal loads were highest at the station at Coeur d’Alene River near Harrison. The mean annual total cadmium load was 3,400 kg/yr, the mean total lead load was 240,000 kg/yr, and the mean total zinc load was 510,000 kg/yr for 1999–2004. Trace-metal loads at the station at South Fork Coeur d’Alene River near Pinehurst and the three stations on the Spokane River downstream of Coeur d’Alene Lake also were relatively high. Differences in metal loads, particularly lead, between stations upstream and downstream of Coeur d’Alene Lake likely are due to trapping and retention of metals in lakebed sediments.</p><p class=\"indent\">LOADEST software was used to estimate loads for water years 1999–2001 for many of the same sites discussed in this report. Overall, results from this study and those from a previous study are in good agreement. Observed differences between the two studies are attributable to streamflow differences in the two regression models, 1999–2001 and 1999-2004.</p><p class=\"indent\">Flow-weighted concentrations (FWCs) calculated from the estimated loads for 1999–2004 were examined to aid interpretation of metal load estimates, which were influenced by large spatial and temporal variations in streamflow. FWCs of total cadmium ranged from 0.04 micrograms per liter (µg/L) at Enaville to 14 µg/L at Ninemile Creek. Total lead FWCs were lowest at Long Lake (1.3 µg/L) and highest at Ninemile Creek (120 µg/L). Elevated total lead FWCs at Harrison confirmed that the high total lead loads at this station were not simply due to higher streamflow. Conversely, relatively low total lead loads combined with high total lead FWCs at Ninemile and Canyon Creeks reflected low streamflow but high concentrations of total lead. Very low total lead FWCs (1.3 to 2.7 µg/L) at the stations downstream of Coeur d’Alene Lake are a result both of deposition of lead-laden sediments in the lake and dilution by additional streamflow. Total zinc FWCs also demonstrated the effect of streamflow on load calculations, and highlighted source areas for zinc in the basin. Total zinc FWCs at Canyon and Ninemile Creeks, 1,600 µg/L and 2,200 µg/L, respectively, were by far the highest in the basin but contributed among the lowest total zinc loads due to their relatively low streamflow. Total zinc FWCs ranged from 38 to 67 µg/L at stations downstream of Coeur d’Alene Lake, but total zinc load estimates at these stations were relatively high because of high mean streamflow compared to other stations in the basin.</p><p class=\"indent\">Long-term regression models for 1991 to 2003 or 2004 were developed and annual trace-metal loads and FWCs were estimated for Pinehurst, Enaville, Harrison, and Post Falls to better understand the variability of metal loading with time. Long-term load estimates are similar to the results for 1999‑2004 in terms of spatial distribution of metal loads throughout the basin.</p><p class=\"indent\">LOADEST results for 1991-2004 indicated that statistically significant downward temporal trends for dissolved and total cadmium, dissolved zinc, and total lead were occurring at Pinehurst, Enaville, Harrison, and Post Falls. Additionally, data for Enaville and Post Falls showed significant downward trends for dissolved lead and total zinc loads; Harrison total zinc loads also decreased with time. The Mann-Kendall trend test results agreed with the LOADEST trend results in most cases, but gave contradictory results for total zinc at Pinehurst and at Post Falls.</p><p class=\"indent\">Long- and short-term load and flow-weighted concentration estimates yielded valuable information about metal storage and transport processes, and demonstrated that water quality data are a great aid in understanding these processes.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/sir20065188","usgsCitation":"Donato, M.M., 2006, Annual trace-metal load estimates and flow-weighted concentrations of cadmium, lead, and zinc, in the Spokane River basin, Idaho and Washington, 1999-2004: U.S. Geological Survey Scientific Investigations Report 2006-5188, vi, 38 p., https://doi.org/10.3133/sir20065188.","productDescription":"vi, 38 p.","numberOfPages":"44","additionalOnlineFiles":"Y","temporalStart":"1994-01-01","temporalEnd":"2004-12-31","costCenters":[{"id":343,"text":"Idaho Water Science Center","active":true,"usgs":true}],"links":[{"id":194376,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":395005,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_77639.htm"},{"id":8580,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/sir/2006/5188/","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Idaho, Washington","otherGeospatial":"Spokane River basin","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -118,\n              47.3333\n            ],\n            [\n              -115.6667,\n              47.3333\n            ],\n            [\n              -115.6667,\n              47.9167\n            ],\n            [\n              -118,\n              47.9167\n            ],\n            [\n              -118,\n              47.3333\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac8e4b07f02db67b809","contributors":{"authors":[{"text":"Donato, Mary M.","contributorId":30962,"corporation":false,"usgs":true,"family":"Donato","given":"Mary","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":289196,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70199181,"text":"70199181 - 2006 - Mass spectrometric in the analysis of inorganic substances","interactions":[],"lastModifiedDate":"2018-09-10T07:26:46","indexId":"70199181","displayToPublicDate":"2006-09-15T07:25:04","publicationYear":"2006","noYear":false,"publicationType":{"id":5,"text":"Book chapter"},"publicationSubtype":{"id":24,"text":"Book Chapter"},"title":"Mass spectrometric in the analysis of inorganic substances","docAbstract":"<p>Mass spectrometry is an analytical technique used to measure the composition of a substance by isolating specific analyte components according to their individual atomic or molecular mass‐to‐charge ratios. Inorganic mass spectrometry is specifically used to determine the elemental and isotopic composition of the material being analyzed. The techniques are capable of the measurement of a range of concentrations from major components to ultratrace constituents. Several instrumental approaches are used to separate and measure the abundance of component ions formed from the sample. These techniques include electron ionization mass spectrometry (EIMS), inductively coupled plasma mass spectrometry (ICPMS), thermal ionization mass spectrometry (TIMS) and spark source mass spectrometry (SSMS). These techniques utilize a variety of mass spectrometers including ion trap, quadrupole, magnetic sector and time‐of‐flight mass analyzers, depending on the type of sample being analyzed and the desired quality of the results. Often sample introduction techniques can be utilized to enhance the capabilities for solving specific analytical chemistry problems.</p>","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Encyclopedia of analytical chemistry: Applications, theory and instrumentation ","language":"English","publisher":"Wiley","doi":"10.1002/9780470027318.a6010","usgsCitation":"Taylor, H.E., 2006, Mass spectrometric in the analysis of inorganic substances, chap. <i>of</i> Encyclopedia of analytical chemistry: Applications, theory and instrumentation , p. 11761-11773, https://doi.org/10.1002/9780470027318.a6010.","productDescription":"13 p.","startPage":"11761","endPage":"11773","costCenters":[{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true},{"id":5044,"text":"National Research Program - Central Branch","active":true,"usgs":true}],"links":[{"id":357151,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationDate":"2006-09-15","publicationStatus":"PW","scienceBaseUri":"5b98c33de4b0702d0e845e9b","contributors":{"editors":[{"text":"Meyers, Robert A.","contributorId":206476,"corporation":false,"usgs":false,"family":"Meyers","given":"Robert","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":744591,"contributorType":{"id":2,"text":"Editors"},"rank":1}],"authors":[{"text":"Taylor, Howard E. hetaylor@usgs.gov","contributorId":1551,"corporation":false,"usgs":true,"family":"Taylor","given":"Howard","email":"hetaylor@usgs.gov","middleInitial":"E.","affiliations":[{"id":5044,"text":"National Research Program - Central Branch","active":true,"usgs":true}],"preferred":true,"id":744590,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70028711,"text":"70028711 - 2006 - The reawakening of Alaska's Augustine volcano","interactions":[],"lastModifiedDate":"2019-04-15T10:22:45","indexId":"70028711","displayToPublicDate":"2006-09-12T09:15:00","publicationYear":"2006","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1578,"text":"Eos, Transactions, American Geophysical Union","onlineIssn":"2324-9250","printIssn":"0096-394","active":true,"publicationSubtype":{"id":10}},"title":"The reawakening of Alaska's Augustine volcano","docAbstract":"<p class=\"p1\"><span class=\"s1\">Augustine volcano, in south central Alaska, ended a 20-year period of repose on 11 January 2006 with 13 explosive eruptions in 20 days. Explosive activity shifted to a quieter effusion of lava in early February, forming a new summit lava dome and two short, blocky lava flows by late March (Figure 1).</span></p>\n<p class=\"p2\"><span class=\"s2\">The eruption was heralded by eight months of increasing seismicity, deformation, gas emission, and small phreatic eruptions, the latter consisting of explosions of steam and debris caused by heating and expansion of groundwater due to an underlying heat source.</span></p>","language":"English","publisher":"American Geophysical Union","doi":"10.1029/2006EO370002","issn":"00963941","usgsCitation":"Power, J.A., Nye, C.J., Coombs, M.L., Wessels, R.L., Cervelli, P.F., Dehn, J., Wallace, K., Freymueller, J.T., and Doukas, M.P., 2006, The reawakening of Alaska's Augustine volcano: Eos, Transactions, American Geophysical Union, v. 87, no. 37, p. 374-376, https://doi.org/10.1029/2006EO370002.","productDescription":"3 p.","startPage":"374","endPage":"376","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":615,"text":"Volcano Hazards Program","active":true,"usgs":true}],"links":[{"id":477313,"rank":1,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1029/2006eo370002","text":"Publisher Index Page"},{"id":236576,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Alaska","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -153.51470947265625,\n              59.412945785071\n            ],\n            [\n              -153.47625732421875,\n              59.41993301322722\n            ],\n            [\n              -153.446044921875,\n              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jpower@usgs.gov","orcid":"https://orcid.org/0000-0002-7233-4398","contributorId":2768,"corporation":false,"usgs":true,"family":"Power","given":"John","email":"jpower@usgs.gov","middleInitial":"A.","affiliations":[],"preferred":true,"id":419377,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Nye, Christopher J.","contributorId":55418,"corporation":false,"usgs":true,"family":"Nye","given":"Christopher","email":"","middleInitial":"J.","affiliations":[{"id":121,"text":"Alaska Volcano Observatory","active":false,"usgs":true}],"preferred":false,"id":419380,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Coombs, Michelle L. 0000-0002-6002-6806 mcoombs@usgs.gov","orcid":"https://orcid.org/0000-0002-6002-6806","contributorId":2809,"corporation":false,"usgs":true,"family":"Coombs","given":"Michelle","email":"mcoombs@usgs.gov","middleInitial":"L.","affiliations":[{"id":617,"text":"Volcano Science Center","active":true,"usgs":true}],"preferred":true,"id":419382,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Wessels, Rick L. rwessels@usgs.gov","contributorId":566,"corporation":false,"usgs":true,"family":"Wessels","given":"Rick","email":"rwessels@usgs.gov","middleInitial":"L.","affiliations":[{"id":245,"text":"Eastern Mineral and Environmental Resources Science Center","active":true,"usgs":true}],"preferred":false,"id":419385,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Cervelli, Peter F. 0000-0001-6765-1009 pcervelli@usgs.gov","orcid":"https://orcid.org/0000-0001-6765-1009","contributorId":1936,"corporation":false,"usgs":true,"family":"Cervelli","given":"Peter","email":"pcervelli@usgs.gov","middleInitial":"F.","affiliations":[{"id":617,"text":"Volcano Science Center","active":true,"usgs":true}],"preferred":true,"id":419383,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Dehn, Jon","contributorId":174120,"corporation":false,"usgs":true,"family":"Dehn","given":"Jon","email":"","affiliations":[{"id":121,"text":"Alaska Volcano Observatory","active":false,"usgs":true}],"preferred":false,"id":419379,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Wallace, Kristi L.","contributorId":20054,"corporation":false,"usgs":true,"family":"Wallace","given":"Kristi L.","affiliations":[],"preferred":false,"id":419384,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Freymueller, Jeffrey T.","contributorId":97458,"corporation":false,"usgs":true,"family":"Freymueller","given":"Jeffrey","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":419381,"contributorType":{"id":1,"text":"Authors"},"rank":8},{"text":"Doukas, Michael P. mdoukas@usgs.gov","contributorId":2686,"corporation":false,"usgs":true,"family":"Doukas","given":"Michael","email":"mdoukas@usgs.gov","middleInitial":"P.","affiliations":[{"id":617,"text":"Volcano Science Center","active":true,"usgs":true}],"preferred":true,"id":419378,"contributorType":{"id":1,"text":"Authors"},"rank":9}]}}
,{"id":70239127,"text":"70239127 - 2006 - Data Report: Acetate and Hydrogen Concentrations in Pore Fluids Associated with a Large Gas Hydrate Reservoir, Southern Hydrate Ridge, offshore Oregon, USA","interactions":[],"lastModifiedDate":"2022-12-28T15:05:45.418526","indexId":"70239127","displayToPublicDate":"2006-09-11T08:46:09","publicationYear":"2006","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":3,"text":"Organization Series"},"seriesTitle":{"id":5640,"text":"Proceedings of the Ocean Drilling Program: Scientific Results","onlineIssn":"1096-7451","printIssn":"0884-5891","active":true,"publicationSubtype":{"id":3}},"seriesNumber":"204","chapter":"17","title":"Data Report: Acetate and Hydrogen Concentrations in Pore Fluids Associated with a Large Gas Hydrate Reservoir, Southern Hydrate Ridge, offshore Oregon, USA","docAbstract":"<p><span>Acetate and hydrogen concentrations in pore fluids were measured in samples taken at seven sites from southern Hydrate Ridge (SHR) offshore Oregon, USA. Acetate concentrations ranged from 3.17 to 2515 µM. The maximum acetate concentrations occurred at Site 1251, which was drilled on a slope basin to the east of SHR at depths just above the bottom-simulating reflector (BSR) that marks the boundary of gas hydrate stability. Acetate maxima and localized high acetate concentrations occurred at the BSR at all sites and frequently corresponded with areas of gas hydrate accumulation, suggesting an empirical relationship. Acetate concentrations were typically at a minimum near the seafloor and above the sulfate/methane interface, where sulfate-reducing bacteria may consume acetate. Hydrogen concentrations in pressure core samples ranged from 16.45 to 1036 parts per million by volume (ppmv). In some cases, hydrogen and acetate concentrations were elevated concurrently, suggesting a positive correlation. However, sampling of hydrogen was limited in comparison to acetate, so any relationships between the two analytes, if present, were difficult to discern.</span></p>","language":"English","publisher":"Ocean Drilling Program, Texas A&M University","doi":"10.2973/odp.proc.sr.204.126.2006","usgsCitation":"Lorenson, T., Colwell, F.S., Delwiche, M., and Dougherty, J.A., 2006, Data Report: Acetate and Hydrogen Concentrations in Pore Fluids Associated with a Large Gas Hydrate Reservoir, Southern Hydrate Ridge, offshore Oregon, USA: Proceedings of the Ocean Drilling Program: Scientific Results 204, v. 204, 20 p., https://doi.org/10.2973/odp.proc.sr.204.126.2006.","productDescription":"20 p.","costCenters":[],"links":[{"id":411119,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Oregon","otherGeospatial":"Pacific Ocean, Southern Hydrate Ridge","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -128.6109789353847,\n              44.301310138828995\n            ],\n            [\n              -128.6109789353847,\n              43.18221251863619\n            ],\n            [\n              -125.03492913069705,\n              43.18221251863619\n            ],\n            [\n              -125.03492913069705,\n              44.301310138828995\n            ],\n            [\n              -128.6109789353847,\n              44.301310138828995\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","volume":"204","noUsgsAuthors":false,"publicationDate":"2006-09-11","publicationStatus":"PW","contributors":{"editors":[{"text":"Trehu, Anne M.","contributorId":49884,"corporation":false,"usgs":false,"family":"Trehu","given":"Anne","email":"","middleInitial":"M.","affiliations":[{"id":6680,"text":"Oregon State University","active":true,"usgs":false}],"preferred":false,"id":860271,"contributorType":{"id":2,"text":"Editors"},"rank":1},{"text":"Bohrmann, G.","contributorId":50700,"corporation":false,"usgs":true,"family":"Bohrmann","given":"G.","email":"","affiliations":[],"preferred":false,"id":860272,"contributorType":{"id":2,"text":"Editors"},"rank":2},{"text":"Torres, Marta E.","contributorId":196035,"corporation":false,"usgs":false,"family":"Torres","given":"Marta","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":860273,"contributorType":{"id":2,"text":"Editors"},"rank":3}],"authors":[{"text":"Lorenson, Thomas 0000-0001-7669-2873 tlorenson@usgs.gov","orcid":"https://orcid.org/0000-0001-7669-2873","contributorId":174599,"corporation":false,"usgs":true,"family":"Lorenson","given":"Thomas","email":"tlorenson@usgs.gov","affiliations":[{"id":520,"text":"Pacific Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":true,"id":860267,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Colwell, Frederick S.","contributorId":140946,"corporation":false,"usgs":false,"family":"Colwell","given":"Frederick","email":"","middleInitial":"S.","affiliations":[{"id":6680,"text":"Oregon State University","active":true,"usgs":false}],"preferred":false,"id":860268,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Delwiche, M.E.","contributorId":42003,"corporation":false,"usgs":true,"family":"Delwiche","given":"M.E.","email":"","affiliations":[],"preferred":false,"id":860269,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Dougherty, Jennifer A.","contributorId":6114,"corporation":false,"usgs":true,"family":"Dougherty","given":"Jennifer","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":860270,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":79123,"text":"fs20063103 - 2006 - Water quality in the Blue River Basin, Kansas City metropolitan area, Missouri and Kansas, July 1998 to October 2004","interactions":[],"lastModifiedDate":"2020-01-26T11:17:56","indexId":"fs20063103","displayToPublicDate":"2006-09-11T00:00:00","publicationYear":"2006","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":"2006-3103","title":"Water quality in the Blue River Basin, Kansas City metropolitan area, Missouri and Kansas, July 1998 to October 2004","docAbstract":"Water-quality data were collected from sites in the Blue River Basin from July 1998 to October. Sites upstream from wastewater-treatment plants or the combined sewer system area had lower concentrations of total nitrogen, phosphorus, organic wastewater compounds, and pharmaceuticals, and more diverse aquatic communities. Sites downstream from wastewater-treatment plants had the largest concentrations and loads of nutrients, organic wastewater compounds, and pharmaceuticals. Approximately 60 percent of the total nitrogen and phosphorus in Blue River originated from the Indian Creek, smaller amounts from the upper Blue River (from 28 to 16 percent), and less than 5 percent from Brush Creek. Nutrient yields from the Indian Creek and the middle Blue River were significantly greater than yields from the upper Blue River, lower Brush Creek, the outside control site, and other U.S. urban sites. Large concentrations of nutrients led to eutrophication of impounded Brush Creek reaches. Bottom sediment samples collected from impoundments generally had concentrations of organic wastewater and pharmaceutical compounds equivalent to or greater than, concentrations observed in streambed sediments downstream from wastewater-treatment plants. Bacteria in streams largely was the result of nonpoint-source contributions during storms. Based on genetic source-tracking, average contributions of in-stream Esherichia coli bacteria in the basin from dogs ranged from 26-32 percent of the total concentration, and human sources ranged from 28-42 percent. Macro invertebrate diversity was highest at sites with the largest percentage of upstream land use devoted to forests and grasslands. Declines in macro invertebrate community metrics were correlated strongly with increases in several, inter-related urbanization factors.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/fs20063103","collaboration":"Prepared in cooperation with the City of Kansas City, Missouri, Water Services Department","usgsCitation":"Wilkison, D.H., Armstrong, D., Norman, R.D., Polton, B.C., Furlong, E.T., and Zaugg, S.D., 2006, Water quality in the Blue River Basin, Kansas City metropolitan area, Missouri and Kansas, July 1998 to October 2004 (Version 1.0): U.S. Geological Survey Fact Sheet 2006-3103, 6 p., https://doi.org/10.3133/fs20063103.","productDescription":"6 p.","numberOfPages":"6","temporalStart":"1998-07-01","temporalEnd":"2004-10-31","costCenters":[{"id":396,"text":"Missouri Water Science Center","active":true,"usgs":true},{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":124797,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/fs_2006_3103.jpg"},{"id":8567,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/fs/2006/3103/","linkFileType":{"id":5,"text":"html"}}],"geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -94.86749999999999,38.8675 ], [ -94.86749999999999,39.1175 ], [ -94.5,39.1175 ], [ -94.5,38.8675 ], [ -94.86749999999999,38.8675 ] ] ] } } ] }","edition":"Version 1.0","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a4ce4b07f02db626a8a","contributors":{"authors":[{"text":"Wilkison, Donald H. wilkison@usgs.gov","contributorId":3824,"corporation":false,"usgs":true,"family":"Wilkison","given":"Donald","email":"wilkison@usgs.gov","middleInitial":"H.","affiliations":[{"id":396,"text":"Missouri Water Science Center","active":true,"usgs":true}],"preferred":true,"id":289151,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Armstrong, Daniel J. armstron@usgs.gov","contributorId":3823,"corporation":false,"usgs":true,"family":"Armstrong","given":"Daniel J.","email":"armstron@usgs.gov","affiliations":[{"id":396,"text":"Missouri Water Science Center","active":true,"usgs":true}],"preferred":true,"id":289150,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Norman, Richard D. rnorman@usgs.gov","contributorId":4086,"corporation":false,"usgs":true,"family":"Norman","given":"Richard","email":"rnorman@usgs.gov","middleInitial":"D.","affiliations":[],"preferred":true,"id":289152,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Polton, Barry C.","contributorId":74471,"corporation":false,"usgs":true,"family":"Polton","given":"Barry","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":289153,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Furlong, Edward T. 0000-0002-7305-4603 efurlong@usgs.gov","orcid":"https://orcid.org/0000-0002-7305-4603","contributorId":740,"corporation":false,"usgs":true,"family":"Furlong","given":"Edward","email":"efurlong@usgs.gov","middleInitial":"T.","affiliations":[{"id":27111,"text":"National Water Quality Program","active":true,"usgs":true},{"id":503,"text":"Office of Water Quality","active":true,"usgs":true},{"id":5046,"text":"Branch of Analytical Serv (NWQL)","active":true,"usgs":true},{"id":191,"text":"Colorado Water Science Center","active":true,"usgs":true}],"preferred":true,"id":289148,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Zaugg, Steven D. sdzaugg@usgs.gov","contributorId":768,"corporation":false,"usgs":true,"family":"Zaugg","given":"Steven","email":"sdzaugg@usgs.gov","middleInitial":"D.","affiliations":[],"preferred":true,"id":289149,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}}
,{"id":79130,"text":"ofr20061150 - 2006 - Geographic information systems (GIS) spatial data compilation of geodynamic, tectonic, metallogenic, mineral deposit, and geophysical maps and associated descriptive data for northeast Asia","interactions":[],"lastModifiedDate":"2012-02-10T00:11:45","indexId":"ofr20061150","displayToPublicDate":"2006-09-11T00:00:00","publicationYear":"2006","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":"2006-1150","title":"Geographic information systems (GIS) spatial data compilation of geodynamic, tectonic, metallogenic, mineral deposit, and geophysical maps and associated descriptive data for northeast Asia","docAbstract":"This is the online version of a CD-ROM publication. It contains all of the data that are on the disc but extra files have been removed: index files, software installers, and Windows autolaunch files.\r\n\r\nThe purpose of this publication is to provide a high-quality spatial data compilation (Geographical Information System or GIS) of geodynamic, mineral deposit, and metallogenic belt maps, and descriptive data for Northeast Asia for customers and users. This area consists of Eastern Siberia, Russian Far East, Mongolia, northern China, South Korea, and Japan. The GIS compilation contains integrated spatial data for: (1) a geodynamics map at a scale of 1:5,000,000; (2) a mineral deposit location map; (3) metallogenic belt maps; (4) detailed descriptions of geologic units, including tectonostratigraphic terranes, cratons, major melange zones, and overlap assemblages, with references; (5) detailed descriptions of metallogenic belts with references; (6) detailed mineral deposit descriptions with references; and (7) page-size stratigraphic columns for major terranes. ","language":"ENGLISH","doi":"10.3133/ofr20061150","isbn":"1411310640","usgsCitation":"Naumova, V.V., Patuk, M.I., Kapitanchuk, M.Y., Nokleberg, W.J., Khanchuk, A.I., Parfenov, L.M., Rodionov, S.M., Miller, R.J., and Diggles, M.F., 2006, Geographic information systems (GIS) spatial data compilation of geodynamic, tectonic, metallogenic, mineral deposit, and geophysical maps and associated descriptive data for northeast Asia (Version 1.0): U.S. Geological Survey Open-File Report 2006-1150, 11 p.; CD-ROM, https://doi.org/10.3133/ofr20061150.","productDescription":"11 p.; CD-ROM","numberOfPages":"11","additionalOnlineFiles":"Y","costCenters":[{"id":658,"text":"Western Mineral Resources","active":false,"usgs":true}],"links":[{"id":8573,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2006/1150/","linkFileType":{"id":5,"text":"html"}},{"id":195615,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":8575,"rank":9999,"type":{"id":20,"text":"Read Me"},"url":"https://pubs.usgs.gov/of/2006/1150/1_readme.txt","linkFileType":{"id":2,"text":"txt"}},{"id":8574,"rank":9999,"type":{"id":16,"text":"Metadata"},"url":"https://pubs.usgs.gov/of/2006/1150/metadata/","linkFileType":{"id":5,"text":"html"}},{"id":8576,"rank":9999,"type":{"id":23,"text":"Spatial Data"},"url":"https://pubs.usgs.gov/of/2006/1150/of2006_1150_data.zip"}],"geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ 75,30 ], [ 75,82 ], [ 144,82 ], [ 144,30 ], [ 75,30 ] ] ] } } ] }","edition":"Version 1.0","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae5e4b07f02db68a608","contributors":{"authors":[{"text":"Naumova, Vera V. (compiler)","contributorId":50789,"corporation":false,"usgs":true,"family":"Naumova","given":"Vera","suffix":"(compiler)","email":"","middleInitial":"V.","affiliations":[],"preferred":false,"id":289182,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Patuk, Mikhail I.","contributorId":73468,"corporation":false,"usgs":true,"family":"Patuk","given":"Mikhail","email":"","middleInitial":"I.","affiliations":[],"preferred":false,"id":289185,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Kapitanchuk, Marina Yu.","contributorId":45966,"corporation":false,"usgs":true,"family":"Kapitanchuk","given":"Marina","email":"","middleInitial":"Yu.","affiliations":[],"preferred":false,"id":289181,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Nokleberg, Warren J. 0000-0002-1574-8869 wnokleberg@usgs.gov","orcid":"https://orcid.org/0000-0002-1574-8869","contributorId":2077,"corporation":false,"usgs":true,"family":"Nokleberg","given":"Warren","email":"wnokleberg@usgs.gov","middleInitial":"J.","affiliations":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"preferred":true,"id":289178,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Khanchuk, Alexander I.","contributorId":19585,"corporation":false,"usgs":true,"family":"Khanchuk","given":"Alexander","email":"","middleInitial":"I.","affiliations":[],"preferred":false,"id":289180,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Parfenov, Leonid M.","contributorId":59112,"corporation":false,"usgs":true,"family":"Parfenov","given":"Leonid","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":289183,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Rodionov, Sergey M.","contributorId":64726,"corporation":false,"usgs":true,"family":"Rodionov","given":"Sergey","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":289184,"contributorType":{"id":1,"text":"Authors"},"rank":8},{"text":"Miller, Robert J. rjmiller@usgs.gov","contributorId":2516,"corporation":false,"usgs":true,"family":"Miller","given":"Robert","email":"rjmiller@usgs.gov","middleInitial":"J.","affiliations":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"preferred":true,"id":289179,"contributorType":{"id":1,"text":"Authors"},"rank":10},{"text":"Diggles, Michael F. 0000-0002-9946-0247 mdiggles@usgs.gov","orcid":"https://orcid.org/0000-0002-9946-0247","contributorId":810,"corporation":false,"usgs":true,"family":"Diggles","given":"Michael","email":"mdiggles@usgs.gov","middleInitial":"F.","affiliations":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true},{"id":5066,"text":"Office of the Director USGS","active":true,"usgs":true},{"id":5053,"text":"IPDS Training","active":true,"usgs":true},{"id":501,"text":"Office of Science Quality and Integrity","active":true,"usgs":true}],"preferred":true,"id":289177,"contributorType":{"id":1,"text":"Authors"},"rank":11}]}}
,{"id":79122,"text":"sir20065161 - 2006 - Assessment of possible sources of microbiological contamination in the water column and streambed sediment of the Jacks Fork, Ozark National Scenic Riverways, Missouri — Phase III","interactions":[],"lastModifiedDate":"2022-01-14T19:23:27.248252","indexId":"sir20065161","displayToPublicDate":"2006-09-11T00:00:00","publicationYear":"2006","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":"2006-5161","title":"Assessment of possible sources of microbiological contamination in the water column and streambed sediment of the Jacks Fork, Ozark National Scenic Riverways, Missouri — Phase III","docAbstract":"In 1998, a 5 river-mile reach of the Jacks Fork was included on Missouri's list of impaired waters as required by Section 303(d) of the Federal Clean Water Act. The identified pollutant on the Jacks Fork was fecal coliform bacteria. The length of the impaired reach was changed to 7 miles on the Missouri 2002 303(d) list because of data indicating the fecal coliform bacteria problem existed over a broader area. The U.S. Geological Survey, in cooperation with the National Park Service, conducted a study to better understand the extent and sources of microbiological contamination within the Jacks Fork from Alley Spring to the mouth, which includes the 7-mile 303(d) reach. Ten sites were sampled from June 2003 through October 2003 and from June 2004 through October 2004. Water-column and streambed sediment samples were collected from main-stem and tributary sites mostly during base-flow conditions during a variety of recreational season river uses and analyzed for fecal coliform and Escherichia coli bacteria. Isolates of Escherichia coli obtained from water samples collected at five sites were submitted for rep-PCR analysis to identify presumptive sources of fecal indicator bacteria in the Jacks Fork. Results indicate that recreational users (including boaters and swimmers) are not the primary source of fecal coliform bacteria in the Jacks Fork; rather, the presence of fecal coliform bacteria is associated with other animals, of which horses are the primary source. Increases in fecal coliform bacteria densities in the Jacks Fork are associated with cross-country horseback trail-riding events.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/sir20065161","usgsCitation":"Davis, J., and Barr, M.N., 2006, Assessment of possible sources of microbiological contamination in the water column and streambed sediment of the Jacks Fork, Ozark National Scenic Riverways, Missouri — Phase III (Version 1.0): U.S. Geological Survey Scientific Investigations Report 2006-5161, iv, 32 p., https://doi.org/10.3133/sir20065161.","productDescription":"iv, 32 p.","numberOfPages":"36","costCenters":[],"links":[{"id":192243,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":8566,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/sir/2006/5161/","linkFileType":{"id":5,"text":"html"}},{"id":394412,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_86822.htm"}],"country":"United States","state":"Missouri","otherGeospatial":"Jacks Fork, Ozark National Scenic Riverways","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -91.45,\n              37.1436\n            ],\n            [\n              -91.2667,\n              37.1436\n            ],\n            [\n              -91.2667,\n              37.1917\n            ],\n            [\n              -91.45,\n              37.1917\n            ],\n            [\n              -91.45,\n              37.1436\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","edition":"Version 1.0","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4abae4b07f02db671eca","contributors":{"authors":[{"text":"Davis, Jerri V. jdavis@usgs.gov","contributorId":2667,"corporation":false,"usgs":true,"family":"Davis","given":"Jerri V.","email":"jdavis@usgs.gov","affiliations":[{"id":396,"text":"Missouri Water Science Center","active":true,"usgs":true}],"preferred":false,"id":289146,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Barr, Miya N. 0000-0002-9961-9190 mnbarr@usgs.gov","orcid":"https://orcid.org/0000-0002-9961-9190","contributorId":3686,"corporation":false,"usgs":true,"family":"Barr","given":"Miya","email":"mnbarr@usgs.gov","middleInitial":"N.","affiliations":[{"id":36532,"text":"Central Midwest Water Science Center","active":true,"usgs":true},{"id":396,"text":"Missouri Water Science Center","active":true,"usgs":true}],"preferred":true,"id":289147,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":79129,"text":"fs20063099 - 2006 - Estimated water use in Wyoming during 2000","interactions":[],"lastModifiedDate":"2017-01-09T10:17:37","indexId":"fs20063099","displayToPublicDate":"2006-09-11T00:00:00","publicationYear":"2006","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":"2006-3099","title":"Estimated water use in Wyoming during 2000","docAbstract":"<p>The U.S. Geological Survey (USGS) has compiled and published estimates of water withdrawals every 5 years since 1950. This series of water-use reports serves as one of the few sources of information about regional or national trends in water withdrawals (Hutson and others, 2004).</p><p>In Wyoming, six categories—irrigation, mining, thermoelectric power, public supply, self-supplied domestic, and industrial—were included in the most recent (2000) USGS compilation of estimated water use. For each category, withdrawal volumes were compiled by water source (surface water or ground water), and by county. Irrigation, public supply, and industrial ground-water withdrawals also were compiled by aquifer. With the exception of saline ground-water mining withdrawals totaling 222 million gallons per day (Mgal/d), all withdrawals in Wyoming were freshwater. Estimated withdrawals are listed from largest to smallest throughout this fact sheet.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/fs20063099","usgsCitation":"Boughton, G.K., Remley, K.R., and Bartos, T.T., 2006, Estimated water use in Wyoming during 2000: U.S. Geological Survey Fact Sheet 2006-3099, 4 p., https://doi.org/10.3133/fs20063099.","productDescription":"4 p.","numberOfPages":"4","temporalStart":"2000-01-01","temporalEnd":"2000-12-31","costCenters":[{"id":684,"text":"Wyoming Water Science Center","active":false,"usgs":true}],"links":[{"id":124940,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/fs_2006_3099.jpg"},{"id":8572,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/fs/2006/3099/","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Wyoming","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -111,41 ], [ -111,45 ], [ -104,45 ], [ -104,41 ], [ -111,41 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0de4b07f02db5fd42f","contributors":{"authors":[{"text":"Boughton, Gregory K. 0000-0001-7355-4977 gkbought@usgs.gov","orcid":"https://orcid.org/0000-0001-7355-4977","contributorId":4254,"corporation":false,"usgs":true,"family":"Boughton","given":"Gregory","email":"gkbought@usgs.gov","middleInitial":"K.","affiliations":[{"id":5050,"text":"WY-MT Water Science Center","active":true,"usgs":true}],"preferred":true,"id":289175,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Remley, Kendra R.","contributorId":82412,"corporation":false,"usgs":true,"family":"Remley","given":"Kendra","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":289176,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Bartos, Timothy T. 0000-0003-1803-4375 ttbartos@usgs.gov","orcid":"https://orcid.org/0000-0003-1803-4375","contributorId":1826,"corporation":false,"usgs":true,"family":"Bartos","given":"Timothy","email":"ttbartos@usgs.gov","middleInitial":"T.","affiliations":[{"id":685,"text":"Wyoming-Montana Water Science Center","active":false,"usgs":true}],"preferred":true,"id":289174,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":79127,"text":"tm10C10 - 2006 - Determination of the &delta;<sup>34</sup>S of sulfate in water; RSIL lab code 1951","interactions":[],"lastModifiedDate":"2012-09-18T17:16:41","indexId":"tm10C10","displayToPublicDate":"2006-09-11T00:00:00","publicationYear":"2006","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":335,"text":"Techniques and Methods","code":"TM","onlineIssn":"2328-7055","printIssn":"2328-7047","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"10-C10","title":"Determination of the &delta;<sup>34</sup>S of sulfate in water; RSIL lab code 1951","docAbstract":"The purpose of the Reston Stable Isotope Laboratory (RSIL) lab code 1951 is to determine the &delta;(<sup>34</sup>S/<sup>32</sup>S), abbreviated as &delta;<sup>34</sup>S, of dissolved sulfate. Dissolved sulfate is collected in the field and precipitated with BaCl<sub>2</sub> at pH 3 to 4 as BaSO<sub>4</sub> in the laboratory. However, the dissolved organic sulfur (DOS) is oxidized to SO<sub>2</sub>, and the carbonate is acidified to CO<sub>2</sub>. Both are degassed from the water sample before the sulfate is precipitated. The precipitated BaSO<sub>4</sub> is filtered and dried before introduction into an elemental analyzer (EA) Carlo Erba NC 2500. The EA is used to convert sulfur in a BaSO<sub>4</sub> solid sample into SO<sub>2</sub> gas, and the EA is connected to a continuous flow isotope-ratio mass spectrometer (CF-IRMS), which determines the differences in the isotope-amount ratios of stable sulfur isotopes (<sup>34</sup>S/<sup>32</sup>S) of the product SO<sub>2</sub> gas. The combustion is quantitative; no isotopic fractionation is involved. Samples are placed in a tin capsule and loaded into the Costech Zero Blank Autosampler of the EA. Under computer control, samples are dropped into a heated tube reaction tube that combines the oxidation and reduction reactions. The combustion takes place in a helium atmosphere containing an excess of oxygen gas at the oxidation zone at the top of the reaction tube. Combustion products are transported by a helium carrier through the reduction zone at the bottom of the reaction tube to remove excess oxygen and through a separate drying tube to remove any water. The gas-phase products, mainly CO<sub>2</sub>, N<sub>2</sub>, and SO<sub>2</sub>, are separated by a gas chromatograph. The gas is then introduced into the isotope-ratio mass spectrometer (IRMS) through a Finnigan MAT (now Thermo Scientific) ConFlo II interface, which also is used to inject SO<sub>2</sub> reference gas and helium for sample dilution. The IRMS is a Thermo Scientific Delta V Plus CF-IRMS. It has a universal triple collector with two wide cups and a narrow cup in the middle. It is capable of measuring mass/charge (<i>m/z</i>) 64 and 66 simultaneously. The ion beams from SO<sub>2</sub> are as follows: <i>m/z</i> 64 = SO<sub>2</sub> = <sup>32</sup>S<sup>16</sup>O<sup>16</sup>O; <i>m/z</i> 66 = SO<sub>2</sub> = <sup>34</sup>S<sup>16</sup>O<sup>16</sup>O primarily.","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Chapter 10 of Book 10, Methods of the Reston Stable Isotope Laboratory Section C, Stable Isotope-Ratio Methods","largerWorkSubtype":{"id":5,"text":"USGS Numbered Series"},"language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/tm10C10","usgsCitation":"Revesz, K., Qi, H., and Coplen, T.B., 2006, Determination of the &delta;<sup>34</sup>S of sulfate in water; RSIL lab code 1951 (Version 1.0 - July 2006, Version 1.1 - 2007, Version 1.2 - September 2012): U.S. Geological Survey Techniques and Methods 10-C10, viii, 33 p., https://doi.org/10.3133/tm10C10.","productDescription":"viii, 33 p.","numberOfPages":"43","onlineOnly":"Y","costCenters":[{"id":543,"text":"Reston Stable Isotope Laboratory","active":false,"usgs":true}],"links":[{"id":192091,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/tm_10_C10.bmp"},{"id":9891,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/tm/2006/tm10c10/","linkFileType":{"id":5,"text":"html"}},{"id":261910,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/tm/2006/tm10c10/tm10c10.pdf","linkFileType":{"id":1,"text":"pdf"}}],"edition":"Version 1.0 - July 2006, Version 1.1 - 2007, Version 1.2 - September 2012","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e3e4b07f02db5e5cf5","contributors":{"authors":[{"text":"Revesz, Kinga","contributorId":64285,"corporation":false,"usgs":true,"family":"Revesz","given":"Kinga","affiliations":[],"preferred":false,"id":289168,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Qi, Haiping 0000-0002-8339-744X haipingq@usgs.gov","orcid":"https://orcid.org/0000-0002-8339-744X","contributorId":507,"corporation":false,"usgs":true,"family":"Qi","given":"Haiping","email":"haipingq@usgs.gov","affiliations":[{"id":436,"text":"National Research Program - Eastern Branch","active":true,"usgs":true}],"preferred":true,"id":289166,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Coplen, Tyler B. 0000-0003-4884-6008 tbcoplen@usgs.gov","orcid":"https://orcid.org/0000-0003-4884-6008","contributorId":508,"corporation":false,"usgs":true,"family":"Coplen","given":"Tyler","email":"tbcoplen@usgs.gov","middleInitial":"B.","affiliations":[{"id":27111,"text":"National Water Quality Program","active":true,"usgs":true},{"id":37464,"text":"WMA - Laboratory & Analytical Services Division","active":true,"usgs":true},{"id":436,"text":"National Research Program - Eastern Branch","active":true,"usgs":true},{"id":37277,"text":"WMA - Earth System Processes Division","active":true,"usgs":true}],"preferred":true,"id":289167,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":79126,"text":"fs20063098 - 2006 - Taking the pulse of a river system: first 20 years","interactions":[],"lastModifiedDate":"2012-02-10T00:11:36","indexId":"fs20063098","displayToPublicDate":"2006-09-11T00:00:00","publicationYear":"2006","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":"2006-3098","title":"Taking the pulse of a river system: first 20 years","docAbstract":"Your doctor would not base decisions for your health care today on one physical examination when you were age three! You would reasonably expect decisions to be based on records from over your lifetime. Likewise, those responsible for monitoring the health of the Upper Mississippi River System want a more comprehensive way to diagnose problems and find treatment options. To begin developing a comprehensive view of the river, the five neighboring states of the Upper Mississippi River System and several Federal agencies formed a partnership in 1986 to monitor river conditions and long-term trends in the Upper Mississippi and Illinois Rivers.","language":"ENGLISH","doi":"10.3133/fs20063098","usgsCitation":"Leake, L., and Johnson, B., 2006, Taking the pulse of a river system: first 20 years: U.S. Geological Survey Fact Sheet 2006-3098, 4 p., https://doi.org/10.3133/fs20063098.","productDescription":"4 p.","startPage":"0","endPage":"4","numberOfPages":"4","costCenters":[{"id":606,"text":"Upper Midwest Environmental Sciences Center","active":true,"usgs":true}],"links":[{"id":120845,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/fs_2006_3098.jpg"},{"id":8570,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/fs/2006/3098/","linkFileType":{"id":5,"text":"html"}}],"geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -97.41666666666667,36.9 ], [ -97.41666666666667,47.8 ], [ -85.81666666666666,47.8 ], [ -85.81666666666666,36.9 ], [ -97.41666666666667,36.9 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a08e4b07f02db5fa403","contributors":{"authors":[{"text":"Leake, Linda","contributorId":18461,"corporation":false,"usgs":true,"family":"Leake","given":"Linda","email":"","affiliations":[],"preferred":false,"id":289164,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Johnson, Barry","contributorId":27952,"corporation":false,"usgs":true,"family":"Johnson","given":"Barry","email":"","affiliations":[],"preferred":false,"id":289165,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":79125,"text":"wdrVA051 - 2006 - Water resources data Virginia water year 2005 Volume 1. Surface-water discharge and surface-water quality records","interactions":[],"lastModifiedDate":"2012-03-08T17:16:24","indexId":"wdrVA051","displayToPublicDate":"2006-09-11T00:00:00","publicationYear":"2006","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":340,"text":"Water Data Report","code":"WDR","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"VA-05-1","title":"Water resources data Virginia water year 2005 Volume 1. Surface-water discharge and surface-water quality records","docAbstract":"Water-resources data for the 2005 water year for Virginia includes records of stage, discharge, and water quality of streams and stage, contents, and water quality of lakes and reservoirs. This volume contains records for water discharge at 172 gaging stations; stage only at 2 gaging stations; elevation at 2 reservoirs and 2 tide gages; contents at 1 reservoir, and water quality at 25 gaging stations. Also included are data for 50 crest-stage partial-record stations. Locations of these sites are shown on figures 4A-B and 5A-B. Miscellaneous hydrologic data were collected at 128 measuring sites and 19 water-quality sampling sites not involved in the systematic data-collection program. The data in this report represent that part of the National Water Data System collected by the U.S. Geological Survey and cooperating State and Federal agencies in Virginia.","language":"ENGLISH","doi":"10.3133/wdrVA051","usgsCitation":"Wicklein, S., Powell, E.D., Guyer, J.R., and Owens, J.A., 2006, Water resources data Virginia water year 2005 Volume 1. Surface-water discharge and surface-water quality records: U.S. Geological Survey Water Data Report VA-05-1, 637 p., https://doi.org/10.3133/wdrVA051.","productDescription":"637 p.","numberOfPages":"637","onlineOnly":"Y","temporalStart":"2004-10-01","temporalEnd":"2005-09-30","costCenters":[{"id":614,"text":"Virginia Water Science Center","active":true,"usgs":true}],"links":[{"id":194899,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":8569,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/wdr/2005/wdr-va-05-1/","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a01e4b07f02db5f7e18","contributors":{"authors":[{"text":"Wicklein, Shaun 0000-0003-4551-1237 smwickle@usgs.gov","orcid":"https://orcid.org/0000-0003-4551-1237","contributorId":3389,"corporation":false,"usgs":true,"family":"Wicklein","given":"Shaun","email":"smwickle@usgs.gov","affiliations":[{"id":37280,"text":"Virginia and West Virginia Water Science Center ","active":true,"usgs":true}],"preferred":true,"id":289160,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Powell, Eugene D.","contributorId":80309,"corporation":false,"usgs":true,"family":"Powell","given":"Eugene","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":289163,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Guyer, Joel R.","contributorId":47446,"corporation":false,"usgs":true,"family":"Guyer","given":"Joel","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":289161,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Owens, Joseph A.","contributorId":73690,"corporation":false,"usgs":true,"family":"Owens","given":"Joseph","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":289162,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":79124,"text":"sir20065147 - 2006 - Water quality in the Blue River basin, Kansas City metropolitan area, Missouri and Kansas, July 1998 to October 2004","interactions":[],"lastModifiedDate":"2020-01-26T11:26:04","indexId":"sir20065147","displayToPublicDate":"2006-09-11T00:00:00","publicationYear":"2006","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":"2006-5147","title":"Water quality in the Blue River basin, Kansas City metropolitan area, Missouri and Kansas, July 1998 to October 2004","docAbstract":"Water-quality data were collected from sites in the Blue River Basin from July 1998 to October. Sites upstream from wastewater-treatment plants or the combined sewer system area had lower concentrations of total nitrogen, phosphorus, organic wastewater compounds, and pharmaceuticals, and more diverse aquatic communities. Sites downstream from wastewater-treatment plants had the largest concentrations and loads of nutrients, organic wastewater compounds, and pharmaceuticals. Approximately 60 percent of the total nitrogen and phosphorus in Blue River originated from the Indian Creek, smaller amounts from the upper Blue River (from 28 to 16 percent), and less than 5 percent from Brush Creek. Nutrient yields from the Indian Creek and the middle Blue River were significantly greater than yields from the upper Blue River, lower Brush Creek, the outside control site, and other U.S. urban sites. Large concentrations of nutrients led to eutrophication of impounded Brush Creek reaches. Bottom sediment samples collected from impoundments generally had concentrations of organic wastewater and pharmaceutical compounds equivalent to or greater than, concentrations observed in streambed sediments downstream from wastewater-treatment plants. Bacteria in streams largely was the result of nonpoint-source contributions during storms. Based on genetic source-tracking, average contributions of in-stream Esherichia coli bacteria in the basin from dogs ranged from 26-32 percent of the total concentration, and human sources ranged from 28-42 percent. Macro invertebrate diversity was highest at sites with the largest percentage of upstream land use devoted to forests and grasslands. Declines in macro invertebrate community metrics were correlated strongly with increases in several, inter-related urbanization factors.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/sir20065147","usgsCitation":"Wilkison, D.H., Armstrong, D., Norman, R.D., Poulton, B.C., Furlong, E.T., and Zaugg, S.D., 2006, Water quality in the Blue River basin, Kansas City metropolitan area, Missouri and Kansas, July 1998 to October 2004 (Version 1.0): U.S. Geological Survey Scientific Investigations Report 2006-5147, viii, 170 p., https://doi.org/10.3133/sir20065147.","productDescription":"viii, 170 p.","numberOfPages":"178","temporalStart":"1998-07-01","temporalEnd":"2004-10-31","costCenters":[{"id":192,"text":"Columbia Environmental Research Center","active":true,"usgs":true},{"id":396,"text":"Missouri Water Science Center","active":true,"usgs":true},{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":195594,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":8568,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/sir/2006/5147/","linkFileType":{"id":5,"text":"html"}}],"geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -94.86749999999999,38.75 ], [ -94.86749999999999,39.1175 ], [ -94.5,39.1175 ], [ -94.5,38.75 ], [ -94.86749999999999,38.75 ] ] ] } } ] }","edition":"Version 1.0","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e47fee4b07f02db4ca2c8","contributors":{"authors":[{"text":"Wilkison, Donald H. wilkison@usgs.gov","contributorId":3824,"corporation":false,"usgs":true,"family":"Wilkison","given":"Donald","email":"wilkison@usgs.gov","middleInitial":"H.","affiliations":[{"id":396,"text":"Missouri Water Science Center","active":true,"usgs":true}],"preferred":true,"id":289158,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Armstrong, Daniel J. armstron@usgs.gov","contributorId":3823,"corporation":false,"usgs":true,"family":"Armstrong","given":"Daniel J.","email":"armstron@usgs.gov","affiliations":[{"id":396,"text":"Missouri Water Science Center","active":true,"usgs":true}],"preferred":true,"id":289157,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Norman, Richard D. rnorman@usgs.gov","contributorId":4086,"corporation":false,"usgs":true,"family":"Norman","given":"Richard","email":"rnorman@usgs.gov","middleInitial":"D.","affiliations":[],"preferred":true,"id":289159,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Poulton, Barry C. 0000-0002-7219-4911 bpoulton@usgs.gov","orcid":"https://orcid.org/0000-0002-7219-4911","contributorId":2421,"corporation":false,"usgs":true,"family":"Poulton","given":"Barry","email":"bpoulton@usgs.gov","middleInitial":"C.","affiliations":[{"id":192,"text":"Columbia Environmental Research Center","active":true,"usgs":true}],"preferred":true,"id":289156,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Furlong, Edward T. 0000-0002-7305-4603 efurlong@usgs.gov","orcid":"https://orcid.org/0000-0002-7305-4603","contributorId":740,"corporation":false,"usgs":true,"family":"Furlong","given":"Edward","email":"efurlong@usgs.gov","middleInitial":"T.","affiliations":[{"id":5046,"text":"Branch of Analytical Serv (NWQL)","active":true,"usgs":true},{"id":503,"text":"Office of Water Quality","active":true,"usgs":true},{"id":27111,"text":"National Water Quality Program","active":true,"usgs":true},{"id":191,"text":"Colorado Water Science Center","active":true,"usgs":true}],"preferred":true,"id":289154,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Zaugg, Steven D. sdzaugg@usgs.gov","contributorId":768,"corporation":false,"usgs":true,"family":"Zaugg","given":"Steven","email":"sdzaugg@usgs.gov","middleInitial":"D.","affiliations":[],"preferred":true,"id":289155,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}}
,{"id":79128,"text":"sir20065186 - 2006 - Hydrology and water quality in the Green River and surrounding agricultural areas near Green River in Emery and Grand Counties, Utah, 2004-05","interactions":[],"lastModifiedDate":"2017-01-27T12:09:28","indexId":"sir20065186","displayToPublicDate":"2006-09-11T00:00:00","publicationYear":"2006","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":"2006-5186","title":"Hydrology and water quality in the Green River and surrounding agricultural areas near Green River in Emery and Grand Counties, Utah, 2004-05","docAbstract":"<p>Water from the Colorado River and its tributaries is used for municipal and industrial purposes by about 27 million people and irrigates nearly 4 million acres of land in the Western United States. Water users in the Upper Colorado River Basin consume water from the Colorado River and its tributaries, reducing the amount of water in the river. In addition, application of water to agricultural land within the basin in excess of crop needs can increase the transport of dissolved solids to the river. As a result, dissolved-solids concentrations in the Colorado River have increased, affecting downstream water users. During 2004-05, the U.S. Geological Survey, in cooperation with the Natural Resources Conservation Service, investigated the occurrence and distribution of dissolved solids in water from the agricultural areas near Green River, Utah, and in the adjacent reach of the Green River, a principle tributary of the Colorado River.</p><p>The flow-weighted concentration of dissolved solids diverted from the Green River for irrigation during 2004 and 2005 was 357 milligrams per liter and the mean concentration of water collected from seeps and drains where water was returning to the river during low-flow conditions was 4,170 milligrams per liter. The dissolved-solids concentration in water from the shallow part of the ground-water system ranged from 687 to 55,900 milligrams per liter.</p><p>Measurable amounts of dissolved solids discharging to the Green River are present almost exclusively along the river banks or near the mouths of dry washes that bisect the agricultural areas. The median dissolved-solids load in discharge from the 17 drains and seeps visited during the study was 0.35 ton per day. Seasonal estimates of the dissolved-solids load discharging from the study area ranged from 2,800 tons in the winter to 6,400 tons in the spring. The estimate of dissolved solids discharging from the study area annually is 15,700 tons.</p><p>Water samples collected from selected sites within the Green River agricultural areas were analyzed for naturally occurring isotopes of strontium and boron, which can be useful for differentiating dissolved-solids sources. Substantial variations in the delta strontium-87 and delta boron-11 values among the sites were measured. Canal and river samples had relatively low concentrations of strontium and the most positive (heavier) isotopic ratios, while drains and seeps had a wide range of strontium concentrations and isotopic ratios that generally were less positive (lighter). Further study of the variation in strontium and boron concentrations and isotope ratios may provide a means to distinguish end members and discern processes affecting dissolved solids within the Green River study area; however, the results from isotope data collected during this study are inconclusive.</p><p>Flow and seepage losses were estimated for the three main canals in the study area for May 2 to October 4 in any given year. This period coincides with the frost-free period in the Green River area. Estimated diversion from the Green River into the Thayn, East Side, and Green River Canals is 6,600, 6,070, and 19,900 acre-feet, respectively. The estimated seepage loss to ground water from the Thayn, East Side, and Green River Canals during the same period is 1,550, 1,460, and 4,710 acre-feet, respectively.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/sir20065186","collaboration":"Prepared in cooperation with the Natural Resources Conservation Service","usgsCitation":"Gerner, S., Spangler, L., Kimball, B.A., Wilberg, D., and Naftz, D.L., 2006, Hydrology and water quality in the Green River and surrounding agricultural areas near Green River in Emery and Grand Counties, Utah, 2004-05: U.S. Geological Survey Scientific Investigations Report 2006-5186, vi, 42 p., https://doi.org/10.3133/sir20065186.","productDescription":"vi, 42 p.","numberOfPages":"51","onlineOnly":"Y","temporalStart":"2004-01-01","temporalEnd":"2005-12-31","costCenters":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":192479,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":8571,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/sir/2006/5186/","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Utah","county":"Emery County, Grand County","otherGeospatial":"Green River","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -110.18333333333334,38.96666666666667 ], [ -110.18333333333334,39.1 ], [ -110.11666666666666,39.1 ], [ -110.11666666666666,38.96666666666667 ], [ -110.18333333333334,38.96666666666667 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae1e4b07f02db6887e5","contributors":{"authors":[{"text":"Gerner, S.J.","contributorId":16083,"corporation":false,"usgs":true,"family":"Gerner","given":"S.J.","email":"","affiliations":[],"preferred":false,"id":289169,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Spangler, L.E.","contributorId":54230,"corporation":false,"usgs":true,"family":"Spangler","given":"L.E.","email":"","affiliations":[],"preferred":false,"id":289171,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Kimball, B. A.","contributorId":87583,"corporation":false,"usgs":false,"family":"Kimball","given":"B.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":289173,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Wilberg, Dale E.","contributorId":60215,"corporation":false,"usgs":true,"family":"Wilberg","given":"Dale E.","affiliations":[],"preferred":false,"id":289172,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Naftz, D. L.","contributorId":40624,"corporation":false,"usgs":true,"family":"Naftz","given":"D.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":289170,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
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