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,{"id":70206228,"text":"70206228 - 2006 - Solute transport processes","interactions":[],"lastModifiedDate":"2019-10-28T06:23:11","indexId":"70206228","displayToPublicDate":"2006-12-31T10:02:10","publicationYear":"2006","noYear":false,"publicationType":{"id":5,"text":"Book chapter"},"publicationSubtype":{"id":24,"text":"Book Chapter"},"title":"Solute transport processes","docAbstract":"<p><span>Soils and aquifers are major compartments of the subsurface environment, which together control the terrestrial hydrological cycle. This subsurface is important for water resources and also as repository for municipal, industrial, and government waste. Aquifers are typically recharged by natural rainfall entering the soil profile and leaching into deeper soil layers. Due to intensive agricultural or industrial activities the leachate leaving the soil profile and entering the aquifer may contain concentrations of toxic substances such as agrochemicals, heavy metals, and polycyclic aromatic hydrocarbons. At contaminated industrial sites light and dense non-aqueous phase liquids (LNAPLs, DNAPLs) may be transported as a separate phase to the underlying aquifer systems. Once any of these chemicals have entered the aquifer they can be transported over large horizontal distances thus contaminating large parts of the aquifer and threateningwater supplywells. Remediation of highly contaminated aquifer systems is commonly a long-term and expensive proposition. As safe and effective use of the subsurface environment is a major challenge facing our society, there is a great need to improve our understanding of the shallow subsurface and the groundwater systems. This particularly includes the understanding of transport processes, which are responsible for the fate of contaminants.</span></p>","language":"English","publisher":"Springer","doi":"10.1007/978-1-4020-4912-5_5","usgsCitation":"Kemna, A., Binley, A., Day-Lewis, F.D., Englert, A., Tezkan, B., Vanderborght, J., Vereecken, H., and Winship, P., 2006, Solute transport processes, p. 117-159, https://doi.org/10.1007/978-1-4020-4912-5_5.","productDescription":"43 p.","startPage":"117","endPage":"159","costCenters":[{"id":493,"text":"Office of Ground Water","active":true,"usgs":true}],"links":[{"id":368600,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Kemna, A.","contributorId":72223,"corporation":false,"usgs":true,"family":"Kemna","given":"A.","email":"","affiliations":[],"preferred":false,"id":773876,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Binley, Andrew 0000-0002-0938-9070","orcid":"https://orcid.org/0000-0002-0938-9070","contributorId":192556,"corporation":false,"usgs":false,"family":"Binley","given":"Andrew","email":"","affiliations":[],"preferred":false,"id":773877,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Day-Lewis, Frederick D. 0000-0003-3526-886X daylewis@usgs.gov","orcid":"https://orcid.org/0000-0003-3526-886X","contributorId":1672,"corporation":false,"usgs":true,"family":"Day-Lewis","given":"Frederick","email":"daylewis@usgs.gov","middleInitial":"D.","affiliations":[{"id":37277,"text":"WMA - Earth System Processes Division","active":true,"usgs":true},{"id":493,"text":"Office of Ground Water","active":true,"usgs":true},{"id":486,"text":"OGW Branch of Geophysics","active":true,"usgs":true}],"preferred":true,"id":773878,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Englert, Andreas","contributorId":220034,"corporation":false,"usgs":false,"family":"Englert","given":"Andreas","email":"","affiliations":[],"preferred":false,"id":773879,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Tezkan, Bulent","contributorId":220035,"corporation":false,"usgs":false,"family":"Tezkan","given":"Bulent","email":"","affiliations":[],"preferred":false,"id":773880,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Vanderborght, Jan","contributorId":220036,"corporation":false,"usgs":false,"family":"Vanderborght","given":"Jan","email":"","affiliations":[],"preferred":false,"id":773881,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Vereecken, Harry","contributorId":220037,"corporation":false,"usgs":false,"family":"Vereecken","given":"Harry","email":"","affiliations":[],"preferred":false,"id":773882,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Winship, Peter","contributorId":220038,"corporation":false,"usgs":false,"family":"Winship","given":"Peter","email":"","affiliations":[],"preferred":false,"id":773883,"contributorType":{"id":1,"text":"Authors"},"rank":8}]}}
,{"id":70195408,"text":"70195408 - 2006 - Physical properties of pressurized sediment from hydrate ridge","interactions":[],"lastModifiedDate":"2018-02-13T16:26:14","indexId":"70195408","displayToPublicDate":"2006-12-31T00:00:00","publicationYear":"2006","noYear":false,"publicationType":{"id":18,"text":"Report"},"title":"Physical properties of pressurized sediment from hydrate ridge","docAbstract":"<p>As part of an ongoing laboratory study, preliminary acoustic, triaxial strength, and electrical resistivity results are presented from a test performed on a clayey silt sediment sample recovered from Site 1249 at the summit of southern Hydrate Ridge during Ocean Drilling Program Leg 204. The test specimen was stored and transported in two different methane-charged pressure vessels until it was tested using the Gas Hydrate and Sediment Test Laboratory Instrument (GHASTLI). Although gas hydrate may have existed in the core section immediately after recovery, little (if any) hydrate was present in the specimen during testing. We therefore present background physical property results for sediment that may have hosted gas hydrate in situ. Because we consolidated the test specimen in increments beyond its in situ stress state, we are able to present properties representative of similar but deeper subbottom sediment. The increased consolidation stress also helped to mitigate some, but not all, types of disturbance caused by the recovery process. P-wave velocities from 1.54 to 1.74 km/s varied linearly with consolidation stress, σ′c, up to 970 kPa (equivalent to ~160 meters below seafloor). Electrical resistivity was periodically measured by a Wenner array and varied between 1.0 and 2.8 Ωm. These values reflect both the pore water salinity and soft, fine-grained texture of the sediment. Shear behavior is consistent with the induced normally consolidated behavior of clayey silt.</p>","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Proceedings of the Ocean Drilling Program, Scientific Results","language":"English","publisher":"The Ocean Drilling Program","usgsCitation":"Winters, W.J., Waite, W., Mason, D.H., and Gilbert, L., 2006, Physical properties of pressurized sediment from hydrate ridge, v. 204, 19 p.","productDescription":"19 p.","startPage":"1","endPage":"19","costCenters":[{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"links":[{"id":351564,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":351563,"rank":1,"type":{"id":15,"text":"Index Page"},"url":"https://www-odp.tamu.edu/publications/204_SR/VOLUME/CHAPTERS/119.PDF"}],"volume":"204","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5aff01c0e4b0da30c1bfcc14","contributors":{"authors":[{"text":"Winters, William J. bwinters@usgs.gov","contributorId":522,"corporation":false,"usgs":true,"family":"Winters","given":"William","email":"bwinters@usgs.gov","middleInitial":"J.","affiliations":[{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":true,"id":728473,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Waite, William F. 0000-0002-9436-4109 wwaite@usgs.gov","orcid":"https://orcid.org/0000-0002-9436-4109","contributorId":625,"corporation":false,"usgs":true,"family":"Waite","given":"William F.","email":"wwaite@usgs.gov","affiliations":[{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true},{"id":186,"text":"Coastal and Marine Geology Program","active":true,"usgs":true}],"preferred":true,"id":728474,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Mason, David H. dmason@usgs.gov","contributorId":624,"corporation":false,"usgs":true,"family":"Mason","given":"David","email":"dmason@usgs.gov","middleInitial":"H.","affiliations":[],"preferred":true,"id":728475,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Gilbert, Lauren","contributorId":99240,"corporation":false,"usgs":true,"family":"Gilbert","given":"Lauren","email":"","affiliations":[],"preferred":false,"id":728476,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70186360,"text":"70186360 - 2006 - Response of Everglades tree islands to environmental change","interactions":[],"lastModifiedDate":"2017-04-04T11:54:57","indexId":"70186360","displayToPublicDate":"2006-12-31T00:00:00","publicationYear":"2006","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1459,"text":"Ecological Monographs","active":true,"publicationSubtype":{"id":10}},"title":"Response of Everglades tree islands to environmental change","docAbstract":"<p><span>Tree islands are centers of biodiversity within the Florida Everglades, USA, but the factors controlling their distribution, formation, and development are poorly understood. We use pollen assemblages from tree islands throughout the greater Everglades ecosystem to reconstruct the timing of tree island formation, patterns of development, and response to specific climatic and environmental stressors. These data indicate that fixed (teardrop-shaped) and strand tree islands developed well before substantial human alteration of the system, with initial tree island vegetation in place between 3500 and 500 calibrated years before present (cal yr BP), depending on the location in the Everglades wetland. Tree island development appears to have been triggered by regional- to global-scale climatic events at 2800 cal yr BP, 1600–1500 cal yr BP, 1200–1000 cal yr BP (early Medieval Warm Period), and 500–200 cal yr BP (Little Ice Age). These periods correspond to drought intervals documented in Central and South America and periods of southward displacement of the Intertropical Convergence Zone. The records indicate a coherence of climate patterns in both subtropical North America and the Northern Hemisphere Neotropics. Water management practices of the 20th century altered plant communities and size of tree islands throughout the Everglades. Responses range from loss of tree islands due to artificially long hydroperiods and deep water to expansion of tree islands after flow reductions. These data provide evidence for the rapidity of tree island response to specific hydrologic change and facilitate prediction of the response to future changes associated with Everglades restoration plans.</span></p>","language":"English","publisher":"Wiley","doi":"10.1890/0012-9615(2006)076[0565:ROETIT]2.0.CO;2","usgsCitation":"Willard, D.A., Bernhardt, C.E., Holmes, C.W., Landacre, B., and Marot, M.E., 2006, Response of Everglades tree islands to environmental change: Ecological Monographs, v. 76, no. 4, p. 565-583, https://doi.org/10.1890/0012-9615(2006)076[0565:ROETIT]2.0.CO;2.","productDescription":"19 p.","startPage":"565","endPage":"583","costCenters":[{"id":574,"text":"St. Petersburg Coastal and Marine Science Center","active":true,"usgs":true}],"links":[{"id":339129,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Florida","otherGeospatial":"Florida Everglades","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -82.12280273437499,\n              24.52213723599524\n            ],\n            [\n              -79.79919433593749,\n              24.52213723599524\n            ],\n            [\n              -79.79919433593749,\n              26.63763888664592\n            ],\n            [\n              -82.12280273437499,\n              26.63763888664592\n            ],\n            [\n              -82.12280273437499,\n              24.52213723599524\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"76","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"58e4b0b3e4b09da67999779a","contributors":{"authors":[{"text":"Willard, Debra A. 0000-0003-4878-0942 dwillard@usgs.gov","orcid":"https://orcid.org/0000-0003-4878-0942","contributorId":2076,"corporation":false,"usgs":true,"family":"Willard","given":"Debra","email":"dwillard@usgs.gov","middleInitial":"A.","affiliations":[{"id":24693,"text":"Climate Research and Development","active":true,"usgs":true},{"id":411,"text":"National Climate Change and Wildlife Science Center","active":true,"usgs":true}],"preferred":true,"id":688371,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bernhardt, Christopher E. 0000-0003-0082-4731 cbernhardt@usgs.gov","orcid":"https://orcid.org/0000-0003-0082-4731","contributorId":2131,"corporation":false,"usgs":true,"family":"Bernhardt","given":"Christopher","email":"cbernhardt@usgs.gov","middleInitial":"E.","affiliations":[{"id":40020,"text":"Florence Bascom Geoscience Center","active":true,"usgs":true},{"id":243,"text":"Eastern Geology and Paleoclimate Science Center","active":true,"usgs":true}],"preferred":true,"id":688372,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Holmes, Charles W.","contributorId":31071,"corporation":false,"usgs":true,"family":"Holmes","given":"Charles","email":"","middleInitial":"W.","affiliations":[{"id":218,"text":"Denver Federal Center","active":false,"usgs":true}],"preferred":false,"id":688373,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Landacre, Bryan","contributorId":74468,"corporation":false,"usgs":true,"family":"Landacre","given":"Bryan","affiliations":[],"preferred":false,"id":688374,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Marot, Marci E. 0000-0003-0504-315X mmarot@usgs.gov","orcid":"https://orcid.org/0000-0003-0504-315X","contributorId":2078,"corporation":false,"usgs":true,"family":"Marot","given":"Marci","email":"mmarot@usgs.gov","middleInitial":"E.","affiliations":[{"id":186,"text":"Coastal and Marine Geology Program","active":true,"usgs":true},{"id":574,"text":"St. Petersburg Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":true,"id":688375,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":70193421,"text":"70193421 - 2006 - Fate and effects of nitrogen and phosphorus in shallow vegetated aquatic ecosystems","interactions":[],"lastModifiedDate":"2017-11-01T12:35:33","indexId":"70193421","displayToPublicDate":"2006-12-31T00:00:00","publicationYear":"2006","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":4,"text":"Other Government Series"},"seriesNumber":"EPA 660/R-06/058","title":"Fate and effects of nitrogen and phosphorus in shallow vegetated aquatic ecosystems","docAbstract":"<p><span>Nitrate concentrations have greatly increased in streams and rivers draining agricultural regions of the Midwestern United States, increasing nitrate transport to the Gulf of Mexico has been implicated in the hypoxic conditions that threaten the productivity of marine fisheries. Increases in nitrate concentrations have been attributed to a combination of factors including agricultural expansion, increased nitrogen application rates, increased tile drainage, and loss of riparian Wetlands, These landscape-level changes have resulted in a decreased natural capacity for nitrogen uptake, removal, and cycling back to the atmosphere. Land managers are increasingly interested in using wetland construction and rehabilitation as a management practice to reduce loss of nitrate from the terrestrial systems. Yet, relatively little is known about the limnological factors involved in nitrate removal by Wetland systems.</span></p><p><span>We conducted a series of studies from 1999-2000 to investigate the functional capacity of shallow, macrophyte-dominated pond wetland systems for uptake, assimilation, and retention of nitrogen (N) and phosphorus (P). We evaluated four factors that were hypothesized to influence nutrient uptake and assimilation: 1) nitrate loading rates; 2) nitrogen to phosphorus (N.P) ratios; 3) frequency of dosing/application; and 4) timing of dose initiation.</span></p><p><span>Nutrient assimilation was rapid; store than 90% of added nutrients were removed from the water column in all treatments. Neither variation in N:P ratios (evaluated range, &lt;13:1 to -114.1), frequency of application (weekly or bi-weekly), nor liming of dose initiation relative to macrophyte development (0%, 15-25%, or 75-90% maximum biomass) had significant effects on nutrient assimilation of wetland community dynamics. Maximum loading of nitrate (60 g N/m<sup>2</sup> 2.4 g P/m<sup>2</sup>) applied as six weekly doses stimulated algal communities, but inhibited macrophyte communities.</span></p><p><span>Predicted shifts from a stable state of macrophyte- to phytoplankton-dominance did not occur due to nutrient additions. Macrophytes, phytoplankton, and the sediment surface were all significant factors in the removal of nitrate from the Water column. Overall, these shallow macrophyte-dominated systems provided an efficient means of removing nutrients from the water column. Construction or rehabilitation of shallow, vegetated wetlands may offer promise as land management practices for nutrient removal in agricultural watersheds.</span></p>","language":"English","publisher":"Environmental Protection Agency","usgsCitation":"Fairchild, J.F., and Vradenburg, L.A., 2006, Fate and effects of nitrogen and phosphorus in shallow vegetated aquatic ecosystems, 169 p.","productDescription":"169 p.","costCenters":[{"id":192,"text":"Columbia Environmental Research Center","active":true,"usgs":true}],"links":[{"id":347993,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":347992,"rank":1,"type":{"id":15,"text":"Index Page"},"url":"https://nepis.epa.gov/Exe/ZyPURL.cgi?Dockey=2000ZXIN.txt"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"59fadd26e4b0531197b13cde","contributors":{"authors":[{"text":"Fairchild, James F. jfairchild@usgs.gov","contributorId":492,"corporation":false,"usgs":true,"family":"Fairchild","given":"James","email":"jfairchild@usgs.gov","middleInitial":"F.","affiliations":[{"id":192,"text":"Columbia Environmental Research Center","active":true,"usgs":true}],"preferred":false,"id":718986,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Vradenburg, Leigh Ann","contributorId":35813,"corporation":false,"usgs":true,"family":"Vradenburg","given":"Leigh","email":"","middleInitial":"Ann","affiliations":[],"preferred":false,"id":718987,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70189257,"text":"70189257 - 2006 - Relations among pH, sulfate, and metals concentrations in anthracite and bituminous coal-mine discharges, Pennsylvania","interactions":[],"lastModifiedDate":"2017-07-06T15:21:03","indexId":"70189257","displayToPublicDate":"2006-12-31T00:00:00","publicationYear":"2006","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"Relations among pH, sulfate, and metals concentrations in anthracite and bituminous coal-mine discharges, Pennsylvania","docAbstract":"<p>Water-quality data for discharges from 140 abandoned mines in the Bituminous and Anthracite Coalfields of Pennsylvania illustrate relations among pH, sulfate, and dissolved metal concentrations. The pH for the 140 samples ranged from 2.7 to 7.3, with two modes at pH 2.5 to 4 (acidic) and 6 to 7 (near neutral). Generally, flow rates were smaller and solute concentrations were greater for low-pH samples; flow rates increased with pH. Although the pH distribution was similar for the bituminous and anthracite subsets, the bituminous discharges had smaller median flow rates, greater concentrations of sulfate, iron, and aluminum, and smaller concentrations of barium and lead than anthracite discharges with the same pH values. The observed relations between the pH and constituent concentrations can be attributed to (1) dilution of acidic water by alkaline ground water; (2) solubility control of aluminum, iron, manganese, barium, and lead by hydroxide, sulfate, and/or carbonate minerals; and (3) aqueous sulfate-complex formation. The formation of AlSO<sub>4</sub><sup>+</sup> and AlHSO<sub>4</sub><sup>+2</sup> complexes adds to the total dissolved aluminum concentration at pH of equilibrium with aluminum hydroxide or hydroxysulfate minerals and can account for 10 to 20 times greater concentrations of dissolved aluminum in bituminous discharges compared to anthracite discharges at similar pH. Sulfate complexation also can account for 10 to 30 times greater concentrations of dissolved ferric iron concentrations at equilibrium with ferrihydrite (Fe(OH)<sub>3</sub>) and/or schwertmannite (Fe<sub>8</sub>O<sub>8</sub>(OH)<sub>4.5</sub>(SO<sub>4</sub>)<sub>1.75</sub>) at pH of 3 to 5. In contrast, lower barium and lead concentrations in bituminous than anthracite discharges indicates elevated sulfate concentration could decrease mobility of these metals by the formation of insoluble minerals such as barite (BaSO<sub>4</sub>) or anglesite (PbSO<sub>4</sub>). Most samples were saturated with barite, but none were saturated with anglesite. Hence, lead concentrations could be controlled by coprecipitation with barite and/or by adsorption to schwertmannite or another sulfate-bearing oxide.</p>","largerWorkType":{"id":24,"text":"Conference Paper"},"largerWorkTitle":"Proceedings: 23rd Annual Meeting of the ASMR, March 26-30, 2006, St. Louis, Missouri","conferenceTitle":"23rd Annual Meeting of the ASMR, March 26-30, 2006, St. Louis, Missouri","conferenceDate":"March 26-30, 2006","conferenceLocation":"St. Louis, MO","language":"English","publisher":"American Society of Mining and Reclamation","publisherLocation":"Champaign, IL","usgsCitation":"Cravotta, I., 2006, Relations among pH, sulfate, and metals concentrations in anthracite and bituminous coal-mine discharges, Pennsylvania, <i>in</i> Proceedings: 23rd Annual Meeting of the ASMR, March 26-30, 2006, St. Louis, Missouri, St. Louis, MO, March 26-30, 2006, p. 378-404.","productDescription":"27 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,{"id":81070,"text":"gap14 - 2006 - GAP Analysis Bulletin Number 14","interactions":[],"lastModifiedDate":"2018-12-21T13:08:57","indexId":"gap14","displayToPublicDate":"2006-12-31T00:00:00","publicationYear":"2006","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":1,"text":"Federal Government Series"},"seriesTitle":{"id":30,"text":"GAP Bulletin","active":false,"publicationSubtype":{"id":1}},"seriesNumber":"14","title":"GAP Analysis Bulletin Number 14","language":"ENGLISH","publisher":"U.S. Fish and Wildlife Service","usgsCitation":"Water Resources Division, U.S. Geological Survey, 2006, GAP Analysis Bulletin Number 14: GAP Bulletin 14, 80 p.","productDescription":"80 p.","costCenters":[{"id":37226,"text":"Core Science Analytics, Synthesis, and Libraries","active":true,"usgs":true},{"id":38315,"text":"GAP Analysis Project","active":true,"usgs":true}],"links":[{"id":195583,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/gap/14/report-thumb.jpg"},{"id":91244,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/gap/14/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b31e4b07f02db6b4143","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":534953,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":79523,"text":"ofr20051082 - 2006 - Ground-Water Levels in Huron County, Michigan, 2004-05","interactions":[{"subject":{"id":79523,"text":"ofr20051082 - 2006 - Ground-Water Levels in Huron County, Michigan, 2004-05","indexId":"ofr20051082","publicationYear":"2006","noYear":false,"title":"Ground-Water Levels in Huron County, Michigan, 2004-05"},"predicate":"SUPERSEDED_BY","object":{"id":81295,"text":"ofr20051082B - 2006 - Ground-water levels in Huron County, Michigan, 2004-05","indexId":"ofr20051082B","publicationYear":"2006","noYear":false,"chapter":"B","title":"Ground-water levels in Huron County, Michigan, 2004-05"},"id":1}],"supersededBy":{"id":81295,"text":"ofr20051082B - 2006 - Ground-water levels in Huron County, Michigan, 2004-05","indexId":"ofr20051082B","publicationYear":"2006","noYear":false,"title":"Ground-water levels in Huron County, Michigan, 2004-05"},"lastModifiedDate":"2017-02-06T13:28:27","indexId":"ofr20051082","displayToPublicDate":"2006-12-30T00:00:00","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":"2005-1082","title":"Ground-Water Levels in Huron County, Michigan, 2004-05","docAbstract":"<p class=\"body\">In 1990, the U.S. Geological Survey (USGS) completed a study of the hydrogeology of Huron County, Michigan (Sweat, 1991). In 1993, Huron County and the USGS entered into a continuing agreement to measure water levels at selected wells throughout Huron County. As part of the agreement, USGS has operated four continuous water-level recorders, installed from 1988 to 1991 on wells in Bingham, Fairhaven, Grant, and Lake Townships (fig. 1) and summarized the data collected in an annual or bi-annual report. The agreement was altered in 2003, and beginning January 1, 2004, only the wells in Fairhaven and Lake Townships retained continuous waterlevel recorders, while the wells in Grant and Bingham Townships reverted primarily to periodic or quarterly measurement status. USGS also has provided training for County or Huron Conservation District personnel to measure the water level, on a quarterly basis, in 25 wells. USGS personnel regularly accompany County or Huron Conservation District personnel to provide a quality assurance/quality control check of all measurements being made. Water-level data collected from the 25 periodically or quarterly-measured wells is summarized in an annual or bi-annual report. In 1998, the USGS also completed a temporal and spatial analysis of the monitoring well network in Huron County (Holtschlag and Sweat, 1998).</p><p class=\"body\">The altitude of Lake Huron and precipitation are good indicators of general climatic conditions and, therefore, provide an environmental context for ground-water levels in Huron County. Figure 2 shows the mean-monthly water-level altitude of Lake Huron, averaged from measurements made by the U.S. Army Corps of Engineers at sites near Essexville or Harbor Beach, or both (National Oceanic and Atmospheric Administration, 2003-05), and monthly precipitation measured in Bad Axe (National Oceanic and Atmospheric Administration, 2003-05). In March 2003, a new low-water level for the period from 1991 through 2005 was measured in Lake Huron. There was almost no net change in the water level of Lake Huron from January 2004 through December 2005. In 2004, annual precipitation measured in Port Hope was about 3.7 inches above normal, but precipitation measured in Bad Axe was about 1.4 inches below normal. About 14.5 inches of precipitation was measured in Bad Axe during the 2004 summer growing season (May through August), which is about the same as was measured in Port Hope during the same period. Provisional precipitation totals for 2005 were 30.7 inches for January through November in Port Hope, and about 31.7 inches for the year in Bad Axe. About 10.6 inches of precipitation was measured in Bad Axe during the 2005 summer growing season, which is about 0.2 inches more than was recorded at Port Hope during the same period.</p><p class=\"body\">Two wells equipped with continuous-data recorders are completed in the Saginaw and Marshall aquifers in Fairhaven and Lake Townships, respectively. From January 2004 through December 2005, the net rise in the water level in the Fairhaven Township well was 0.71 ft, and the net rise in the Lake Township well was 0.98 ft. The Fairhaven Township well is drilled adjacent to Saginaw Bay (Lake Huron), and, as previously noted, there was almost no net change in the water level in Saginaw Bay over the same period. Hydrographs showing water levels are presented for the two wells equipped with continuous-data recorders. Continuous-data recorders were discontinued in the Grant and Bingham Township wells at the end of 2003 due to budget constraints. The decision of which two wells to discontinue was based on an analysis of the intrinsic value to Huron County of data from each well. The Grant Township well was selected for periodic or quarterly measurement at that time because it is completed in the glacial aquifer, which is little used for drinking water purposes or absent in much of Huron County. The Bingham Township well, which is completed in the Marshall aquifer, was selected for periodic or quarterly measurement because water levels in the well are often perturbed as a result of pumpage from nearby production wells and do not reflect baseline conditions within the aquifer.</p><p class=\"body\">Twenty five wells were measured on a periodic or quarterly basis in 2004-05. These wells are completed in the glacial, Saginaw, and Marshall aquifers, and the Coldwater confining unit. Although each quarterly measurement only provides a “snapshot” water level (measured in feet below land surface), the data adequately define the generalized water-level trend in the aquifer near the well. Water levels in 15 quarterlymeasured wells had a net rise ranging from 0.20 to 1.31 ft for the period from January 2004 to December 2005, while water levels in 10 of the wells had a net decline ranging from 0.07 to 0.99 ft over the same period (fig. 3; table 1). Period-of-record (the time period when water levels have been measured by U.S. Geological Survey or their cooperators) minimum depths to water (high-water levels) were measured in March 2004 in two quarterly-measured wells completed in the Marshall aquifer in Lake and Hume Townships. Period-of-record maximum depths to water were measured in September 2005 in three wells completed in the Marshall aquifer near Bad Axe. Water levels in those three wells recovered about 3 to 5 ft between September and December 2005. No period-of-record minimum or maximum depths to water were measured for the period from January 2004 through December 2005 in wells completed in either the glacial and Saginaw aquifers, or the Coldwater confining unit. Hydrographs showing water levels measured in each well are presented for the 25 wells measured on a quarterly basis.</p><p class=\"body\">Water-level trends measured for the period from January 2004 through December 2005 in other wells in Lower Michigan have similarities to those measured in Huron County wells. Several external factors influence water-level trends including proximity to nearby production wells, amount and timing of precipitation events, evapotranspiration and type of prevalent ground cover, proximity of aquifer to the surface, and hydraulic characteristics of overlying geologic materials.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr20051082","collaboration":"Prepared in cooperation with Huron County, Michigan","usgsCitation":"Weaver, T.L., Crowley, S.L., and Blumer, S.P., 2006, Ground-Water Levels in Huron County, Michigan, 2004-05: U.S. Geological Survey Open-File Report 2005-1082, iv, 16 p., https://doi.org/10.3133/ofr20051082.","productDescription":"iv, 16 p.","temporalStart":"2004-01-01","temporalEnd":"2005-12-31","costCenters":[{"id":382,"text":"Michigan Water Science 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,{"id":79521,"text":"ds230 - 2006 - Compilation of historical water-quality data for selected springs in Texas, by ecoregion","interactions":[],"lastModifiedDate":"2016-08-24T15:09:28","indexId":"ds230","displayToPublicDate":"2006-12-29T00:00:00","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":"230","title":"Compilation of historical water-quality data for selected springs in Texas, by ecoregion","docAbstract":"Springs are important hydrologic features in Texas. A database of about 2,000 historically documented springs and available spring-flow measurements previously has been compiled and published, but water-quality data remain scattered in published sources. This report by the U.S. Geological Survey, in cooperation with the Texas Parks and Wildlife Department, documents the compilation of data for 232 springs in Texas on the basis of a set of criteria and the development of a water-quality database for the selected springs. The selection of springs for compilation of historical water-quality data in Texas was made using existing digital and hard-copy data, responses to mailed surveys, selection criteria established by various stakeholders, geographic information systems, and digital database queries. Most springs were selected by computing the highest mean spring flows for each Texas level III ecoregion. A brief assessment of the water-quality data for springs in Texas shows that few data are available in the Arizona/New Mexico Mountains, High Plains, East Central Texas Plains, Western Gulf Coastal Plain, and South Central Plains ecoregions. Water-quality data are more abundant for the Chihuahuan Deserts, Edwards Plateau, and Texas Blackland Prairies ecoregions. Selected constituent concentrations in Texas springs, including silica, calcium, magnesium, sodium, potassium, strontium, sulfate, chloride, fluoride, nitrate (nitrogen), dissolved solids, and hardness (as calcium carbonate) are comparatively high in the Chihuahuan Deserts, Southwestern Tablelands, Central Great Plains, and Cross Timbers ecoregions, mostly as a result of subsurface geology. Comparatively low concentrations of selected constituents in Texas springs are associated with the Arizona/New Mexico Mountains, Southern Texas Plains, East Central Texas Plains, and South Central Plains ecoregions.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ds230","collaboration":"Prepared in cooperation with the Texas Parks and Wildlife Department","usgsCitation":"Heitmuller, F.T., and Williams, I.P., 2006, Compilation of historical water-quality data for selected springs in Texas, by ecoregion: U.S. Geological Survey Data Series 230, vi, 32 p.; database files (available online only), https://doi.org/10.3133/ds230.","productDescription":"vi, 32 p.; database files (available online only)","numberOfPages":"37","additionalOnlineFiles":"Y","costCenters":[{"id":583,"text":"Texas Water Science 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,{"id":79522,"text":"sir20065301 - 2006 - Sources of polychlorinated biphenyls to Devils Swamp Lake near Baton Rouge, Louisiana","interactions":[],"lastModifiedDate":"2016-08-23T14:47:33","indexId":"sir20065301","displayToPublicDate":"2006-12-29T00:00:00","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":"2006-5301","title":"Sources of polychlorinated biphenyls to Devils Swamp Lake near Baton Rouge, Louisiana","docAbstract":"<p>Devils Swamp Lake near Baton Rouge, Louisiana, created in 1973 by dredging in Devils Swamp along the Mississippi River, is contaminated with polychlorinated biphenyls (PCBs) from historical industrial discharges. This study involved the investigation of the occurrence, distribution, and sources of PCBs in the lake, including the possible historical contribution of PCBs from a hazardous-chemical disposal facility by way of a wastewater drainage ditch that was used from 1971 to 1993. Six bed sediment cores from the lake and three bed sediment grab samples from the drainage ditch were collected; 61 subsamples from selected intervals in five of the six cores and the three grab samples from the ditch were analyzed for PCBs using an immunoassay screening method. Sixteen of the core subsamples and one ditch sample were analyzed for organochlorine pesticides, PCBs, polycyclic aromatic hydrocarbons (PAHs) (15 samples), and major and trace elements. PCB congener profiles and a factor analysis of congener composition indicate that PCBs in sediment from the drainage ditch and in lake sediment deposited near the canal since the mid-1980s are similar, which indicates the disposal facility, by way of the wastewater drainage ditch, is the source of the PCBs. Sediment from several hundred meters down the lake to the west, near where Bayou Baton Rouge enters the lake, had a different PCB composition and in a sample deposited in the early 1980s, a much higher concentration, indicating a second source of PCBs in the watershed of Bayou Baton Rouge. Large differences in PAHs and metals between sediment near the ditch and sediment near Bayou Baton Rouge support this conclusion. The identity of the Bayou Baton Rouge source(s) cannot be established using available data. The short duration and relatively high concentrations of PCBs from the bayou source indicate either a spill or a flood-related release-there was a large flood on the Mississippi River in 1983. Older (deeper) samples from cores near the drainage ditch (dated as deposited before the mid-1980s) had PCB compositions that indicate a mixture of sources (Bayou Baton Rouge and the drainage ditch). Elevated PCB concentrations in sediment from the drainage ditch and cores from near the mouth of the ditch in recent (post-2000) samples indicate that some PCB inputs from the ditch might still be occurring.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/sir20065301","usgsCitation":"Van Metre, P., Wilson, J.T., and Kimball, B.A., 2006, Sources of polychlorinated biphenyls to Devils Swamp Lake near Baton Rouge, Louisiana: U.S. Geological Survey Scientific Investigations Report 2006-5301, iii, 50 p., https://doi.org/10.3133/sir20065301.","productDescription":"iii, 50 p.","numberOfPages":"53","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"links":[{"id":192043,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/sir20065301.PNG"},{"id":9077,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/sir/2006/5301/","linkFileType":{"id":5,"text":"html"}},{"id":327739,"rank":101,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/sir/2006/5301/pdf/sir2006-5301.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e6e4b07f02db5e769b","contributors":{"authors":[{"text":"Van Metre, Peter C.","contributorId":34104,"corporation":false,"usgs":true,"family":"Van Metre","given":"Peter C.","affiliations":[],"preferred":false,"id":290138,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Wilson, Jennifer T. 0000-0003-4481-6354 jenwilso@usgs.gov","orcid":"https://orcid.org/0000-0003-4481-6354","contributorId":1782,"corporation":false,"usgs":true,"family":"Wilson","given":"Jennifer","email":"jenwilso@usgs.gov","middleInitial":"T.","affiliations":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"preferred":true,"id":290137,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Kimball, Briant A. bkimball@usgs.gov","contributorId":533,"corporation":false,"usgs":true,"family":"Kimball","given":"Briant","email":"bkimball@usgs.gov","middleInitial":"A.","affiliations":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"preferred":true,"id":290136,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":79520,"text":"sir20065178 - 2006 - Changes in streamflow and water quality in selected nontidal basins in the Chesapeake Bay Watershed, 1985-2004","interactions":[],"lastModifiedDate":"2023-03-09T20:43:50.758155","indexId":"sir20065178","displayToPublicDate":"2006-12-29T00:00:00","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":"2006-5178","title":"Changes in streamflow and water quality in selected nontidal basins in the Chesapeake Bay Watershed, 1985-2004","docAbstract":"<p>As part of an annual evaluation of water-quality conditions by the Chesapeake Bay Program, water-quality and streamflow data from 32 sites in nontidal parts of the Chesapeake Bay watershed were analyzed to document annual nutrient and sediment trends for 1985 through 2004. This study also formalized different trend tests and methodologies used in assessing the effectiveness of man-agement actions in reducing nutrients and sediments to the Chesapeake Bay. Trends in streamflow were tested at multiple time scales (daily, seasonal, and annual), resulting in only one significant trend (annual-mean streamflow for the Choptank River near Greensboro, Md.). Total freshwater flow entering the bay for the July-August-September 'summer' season 2004 was the highest ever estimated for that 3-month period (1937-2004). Observed (unbiased) concentration summaries indi-cate higher ranges in total-nitrogen concentrations in the northern major river basins, those in Pennsylvania, Maryland, and northern Virginia, compared to the more southern basins in Virginia. Almost half of the monitoring sites in the northern basins exhibited significant downward trends in total nitrogen with time. Comparisons with total phosphorus and sediment showed similar results to total nitrogen. </p><p>Monthly and annual loads were available for the River Input Monitoring Program sites from the U.S. Geological Survey. Although loads were significantly reduced from 2003, in 2004, the combined estimated total nitrogen loads were the third highest since 1990, whereas total phosphorus and sediment loads were the fifth highest. A flow-weighted concentration (FWC) is useful in evaluating changes through time. Combined annual mean total nitrogen FWC from the 9 River Input Monitoring Program sites indicated a downward tendency from 1985 through 1998 and an upward tendency since 2001. From 1990 to 2004, the mean concentrations of total nitrogen, total phosphorus, and sediment were 1.58, 0.085, and 51 milligrams per liter, respectively. Flow-weighted concentrations for phosphorus and sediment were lower in the Susquehanna River at Conowingo, Md., most likely due to the trapping efficiency of three large reservoirs upstream from the sampling point. </p><p>Trends in concentrations, not adjusted for flow, identified 10 statistically significant upward trends, and 50 statistically significant downward trends in concentration for the period 1985 through 2004. Trends in concentrations, when adjusted for flow, can be used as an indicator of human activity and management actions. The flow-adjusted trends indicated significant downward trends at approx-imately 72, 81, and 43 percent of the sites for total nitrogen, total phosphorus, and sediment, respectively. This indicates that management actions are having some effect in reducing nutrients and sediments.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/sir20065178","collaboration":"Prepared in cooperation with the U.S. Environmental Protection Agency Chesapeake Bay Program Office; Maryland Department of Natural Resources; Virginia Department of Environmental Quality","usgsCitation":"Langland, M.J., Raffensperger, J.P., Moyer, D., Landwehr, J.M., and Schwarz, G., 2006, Changes in streamflow and water quality in selected nontidal basins in the Chesapeake Bay Watershed, 1985-2004: U.S. Geological Survey Scientific Investigations Report 2006-5178, viii, 75 p., https://doi.org/10.3133/sir20065178.","productDescription":"viii, 75 p.","additionalOnlineFiles":"Y","temporalStart":"1985-01-01","temporalEnd":"2004-12-31","costCenters":[{"id":532,"text":"Pennsylvania Water Science 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Center","active":true,"usgs":true}],"preferred":true,"id":290133,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Moyer, Douglas 0000-0001-6330-478X dlmoyer@usgs.gov","orcid":"https://orcid.org/0000-0001-6330-478X","contributorId":2670,"corporation":false,"usgs":true,"family":"Moyer","given":"Douglas","email":"dlmoyer@usgs.gov","affiliations":[{"id":614,"text":"Virginia Water Science Center","active":true,"usgs":true}],"preferred":false,"id":290132,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Landwehr, Jurate M. jmlandwe@usgs.gov","contributorId":2345,"corporation":false,"usgs":true,"family":"Landwehr","given":"Jurate","email":"jmlandwe@usgs.gov","middleInitial":"M.","affiliations":[],"preferred":true,"id":290130,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Schwarz, Gregory E. 0000-0002-9239-4566 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,{"id":79519,"text":"ofr20051306 - 2006 - Continuous resistivity profiling data from the upper Neuse River Estuary, North Carolina, 2004-2005","interactions":[],"lastModifiedDate":"2022-10-04T19:16:44.746441","indexId":"ofr20051306","displayToPublicDate":"2006-12-29T00:00:00","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":"2005-1306","title":"Continuous resistivity profiling data from the upper Neuse River Estuary, North Carolina, 2004-2005","docAbstract":"<p>The Neuse River Estuary in North Carolina has suffered impacts of eutrophication in recent years. As part of a larger project to better constrain nutrient budgets in the estuary, field investigations were performed to study occurrence and discharge of fresh and brackish ground water and nutrients beneath the estuary itself (fig. 1). A Continuous Resistivity Profiling (CRP) system (Manheim and others, 2004) was used to map the depth of the freshwater-saltwater interface (FSI) in sub-estuarine groundwater. This study area serves as a typological representation of a submarine groundwater environment characteristic of a shallow estuary in a wide coastal plain that has not experienced glaciation. Similar settings extend from New Jersey to Georgia, and along the Gulf of Mexico in the U.S. This report archives 29 lines of data collected during 2004 and 2005 surveys representing almost 210 km of survey lines. 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,{"id":79510,"text":"fs20063122 - 2006 - Pesticides in ground water - Carbon County, Wyoming, 2004-2005","interactions":[],"lastModifiedDate":"2022-08-30T18:24:11.000969","indexId":"fs20063122","displayToPublicDate":"2006-12-28T00:00:00","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":"2006-3122","title":"Pesticides in ground water - Carbon County, Wyoming, 2004-2005","docAbstract":"In 1991, members of local, State, and Federal governments, as well as industry and interest groups, formed the Ground-water and Pesticide Strategy Committee to prepare the State of Wyoming's generic Management Plan for Pesticides in Ground Water. Part of this management plan is to sample and analyze Wyoming's ground water for pesticides. In 1995, the U.S. Geological Survey, in cooperation with the Ground-water and Pesticide Strategy Committee, began statewide implementation of the sampling component of the State of Wyoming's generic Management Plan for Pesticides in Ground Water. During 2004-2005, baseline monitoring was conducted in Carbon County. This fact sheet describes and summarizes results of the baseline monitoring in Carbon County.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/fs20063122","collaboration":"In cooperation with the Wyoming Department of Agriculture (WDA) and the Wyoming Department of Environmental Quality (WDEQ)","usgsCitation":"Eddy-Miller, C., and Remley, K., 2006, Pesticides in ground water - Carbon County, Wyoming, 2004-2005: U.S. Geological Survey Fact Sheet 2006-3122, 4 p., https://doi.org/10.3133/fs20063122.","productDescription":"4 p.","numberOfPages":"4","temporalStart":"2004-01-01","temporalEnd":"2005-12-31","costCenters":[{"id":684,"text":"Wyoming Water Science Center","active":false,"usgs":true},{"id":5050,"text":"WY-MT Water Science Center","active":true,"usgs":true}],"links":[{"id":122432,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/fs_2006_3122.jpg"},{"id":405928,"rank":3,"type":{"id":36,"text":"NGMDB Index 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,{"id":79511,"text":"fs20063123 - 2006 - Pesticides in ground water - Campbell County, Wyoming, 2004-2005","interactions":[],"lastModifiedDate":"2022-08-30T18:22:11.772416","indexId":"fs20063123","displayToPublicDate":"2006-12-28T00:00:00","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":"2006-3123","title":"Pesticides in ground water - Campbell County, Wyoming, 2004-2005","docAbstract":"In 1991, members of local, State, and Federal governments, as well as industry and interest groups, formed the Ground-water and Pesticide Strategy Committee to prepare the State of Wyoming's generic Management Plan for Pesticides in Ground Water. Part of this management plan is to sample and analyze Wyoming's ground water for pesticides. In 1995, the U.S. Geological Survey, in cooperation with the Ground-water and Pesticide Strategy Committee, began statewide implementation of the sampling component of the State of Wyoming's generic Management Plan for Pesticides in Ground Water. During 2004-2005, baseline monitoring was conducted in Campbell County. This fact sheet describes and summarizes results of the baseline monitoring in Campbell County.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/fs20063123","collaboration":"In cooperation with the Wyoming Department of Agriculture (WDA) and the Wyoming Department of Environmental Quality (WDEQ)","usgsCitation":"Eddy-Miller, C., and Remley, K., 2006, Pesticides in ground water - Campbell County, Wyoming, 2004-2005: U.S. Geological Survey Fact Sheet 2006-3123, 4 p., https://doi.org/10.3133/fs20063123.","productDescription":"4 p.","numberOfPages":"4","temporalStart":"2004-01-01","temporalEnd":"2005-12-31","costCenters":[{"id":684,"text":"Wyoming Water Science Center","active":false,"usgs":true}],"links":[{"id":122417,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/fs_2006_3123.jpg"},{"id":9182,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/fs/2006/3123/","linkFileType":{"id":5,"text":"html"}},{"id":405927,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_80466.htm","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Wyoming","county":"Campbell County","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"Polygon\",\"coordinates\":[[[-105.0874,45.0001],[-105.0855,44.9688],[-105.0861,44.8811],[-105.0764,44.8818],[-105.0773,44.8014],[-105.0773,44.7868],[-105.0863,44.787],[-105.0869,44.7574],[-105.0869,44.7277],[-105.0869,44.699],[-105.0863,44.6533],[-105.0869,44.6387],[-105.0861,44.6118],[-105.0859,44.5283],[-105.0853,44.5118],[-105.0853,44.4977],[-105.086,44.4826],[-105.0817,44.1793],[-105.076,44.1791],[-105.0776,44.1409],[-105.0776,44.1263],[-105.0804,44.0033],[-105.0842,44.0029],[-105.0849,43.9414],[-105.0849,43.9268],[-105.0848,43.9154],[-105.0851,43.8936],[-105.0848,43.8411],[-105.0847,43.8275],[-105.0809,43.8269],[-105.0821,43.7395],[-105.0821,43.7103],[-105.0821,43.6807],[-105.0822,43.6652],[-105.0821,43.6511],[-105.0822,43.6356],[-105.0821,43.6211],[-105.082,43.5942],[-105.082,43.5646],[-105.082,43.55],[-105.082,43.5341],[-105.082,43.5195],[-105.0817,43.4981],[-105.242,43.4984],[-105.2616,43.4979],[-105.2818,43.4978],[-105.302,43.4978],[-105.3216,43.4977],[-105.3418,43.4981],[-105.362,43.4981],[-105.4018,43.498],[-105.5028,43.4977],[-105.5236,43.4976],[-105.6833,43.4973],[-106.0204,43.4946],[-106.0197,43.7619],[-106.0198,43.822],[-106.0084,43.8223],[-106.0082,43.8501],[-106.0084,43.8647],[-106.008,43.8792],[-106.0082,43.8938],[-106.0078,43.9958],[-106.0076,44.0227],[-106.0078,44.0373],[-106.008,44.0524],[-106.0082,44.0665],[-106.0078,44.082],[-106.0087,44.0961],[-106.0089,44.1107],[-106.0091,44.1253],[-106.0093,44.1403],[-106.0095,44.1545],[-106.0097,44.1695],[-106.0199,44.1697],[-106.0204,44.1966],[-106.0206,44.2112],[-106.0208,44.2257],[-106.0218,44.2996],[-106.0203,44.3748],[-106.0205,44.3894],[-106.0207,44.404],[-106.0203,44.4191],[-106.0194,44.4478],[-106.0196,44.4642],[-106.0198,44.4783],[-106.02,44.4934],[-106.0203,44.5066],[-106.0205,44.5208],[-106.0115,44.5211],[-106.0115,44.5653],[-106.0078,44.8423],[-106.0076,44.8715],[-106.0166,44.8716],[-106.0164,44.8999],[-106.0171,44.9437],[-106.0165,44.962],[-106.0168,44.9968],[-106.0007,44.9967],[-105.9331,44.9973],[-105.9226,45.0007],[-105.9196,45.0017],[-105.897,45.0017],[-105.7601,45.0016],[-105.6974,45.0017],[-105.694,45.0016],[-105.6768,45.0016],[-105.5876,45.0013],[-105.2874,45.0009],[-105.2834,45.0009],[-105.2674,45.0009],[-105.2468,45.0009],[-105.2381,45.0009],[-105.2268,45.0009],[-105.0874,45.0001]]]},\"properties\":{\"name\":\"Campbell\",\"state\":\"WY\"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad4e4b07f02db682f51","contributors":{"authors":[{"text":"Eddy-Miller, Cheryl A.","contributorId":86755,"corporation":false,"usgs":true,"family":"Eddy-Miller","given":"Cheryl A.","affiliations":[],"preferred":false,"id":290099,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Remley, Kendra J.","contributorId":26753,"corporation":false,"usgs":true,"family":"Remley","given":"Kendra J.","affiliations":[],"preferred":false,"id":290098,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":79506,"text":"ofr20061350 - 2006 - Concentrations of elements in sediments and selective fractions of sediments, and in natural waters in contact with sediments from Lake Roosevelt, Washington, September 2004","interactions":[],"lastModifiedDate":"2022-06-17T13:30:02.369889","indexId":"ofr20061350","displayToPublicDate":"2006-12-28T00:00:00","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":"2006-1350","title":"Concentrations of elements in sediments and selective fractions of sediments, and in natural waters in contact with sediments from Lake Roosevelt, Washington, September 2004","docAbstract":"<p class=\"indent\">Twenty-eight composite and replicate sediment samples from 8 Lake Roosevelt sites were collected and analyzed for 10 alkali and alkaline earth elements, 2 non-metals, 20 metals, and 4 lanthanide and actinide elements. All elements were detected in all sediment samples except for silver (95&nbsp;percent of the elements detected for 1,008 analyses), which was detected only in 4 samples. Sequential selective extraction procedures were performed on single composite samples from the eight sites. The percentage of detections for the 31 elements analyzed ranged from 76 percent for the first extraction fraction using a weak extractant to 93 percent for the four-acid dissolution of the sediments remaining after the third sequential selective extraction.</p><p class=\"indent\">Water samples in various degrees of contact with the sediment were analyzed for 10 alkali and alkaline earth elements, 5 non-metals, 25 metals, and 16 lanthanide and actinide elements. The filtered water samples included 10 samples from the reservoir water column at 8 sites, 32 samples of porewater, 55 samples from reservoir water overlying sediments in 8 cores from the site incubated in a field laboratory, and 24 water samples that were filtered after being tumbled with sediments from 8 sites. Overall, the concentrations of only 37 percent of the 6,776 analyses of the 121 water samples were greater than the reporting limit. Selenium, bismuth, chromium, niobium, silver, and zirconium were not detected in any water samples. The percentage of concentrations for the water samples that were above the reporting limit ranged from 14 percent for the lanthanide and actinide elements to 77 percent for the alkali and alkaline earth elements. Concentrations were greater than reporting limits in only 23 percent of the analyses of reservoir water and 29 percent of the analyses of reservoir water overlying incubation cores. In contrast, 47 and 48 percent of the concentrations of porewater and water samples tumbled with sediments, respectively, were greater than the reporting limit.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr20061350","collaboration":"Prepared in cooperation with the National Park Service","usgsCitation":"Paulson, A.J., Wagner, R.J., Sanzolone, R.F., and Cox, S.E., 2006, Concentrations of elements in sediments and selective fractions of sediments, and in natural waters in contact with sediments from Lake Roosevelt, Washington, September 2004: U.S. Geological Survey Open-File Report 2006-1350, vi, 84 p., https://doi.org/10.3133/ofr20061350.","productDescription":"vi, 84 p.","numberOfPages":"90","temporalStart":"2004-09-01","temporalEnd":"2004-09-30","costCenters":[{"id":622,"text":"Washington Water Science Center","active":true,"usgs":true}],"links":[{"id":195519,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":9063,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2006/1350/","linkFileType":{"id":5,"text":"html"}},{"id":402307,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_78794.htm","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Washington","otherGeospatial":"Lake Roosevelt","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -118.4271240234375,\n              47.84634433782511\n            ],\n            [\n              -117.960205078125,\n              47.84634433782511\n            ],\n            [\n              -117.960205078125,\n              48.777912755501845\n            ],\n            [\n              -118.4271240234375,\n              48.777912755501845\n            ],\n            [\n              -118.4271240234375,\n              47.84634433782511\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1ae4b07f02db6a8563","contributors":{"authors":[{"text":"Paulson, Anthony J. 0000-0002-2358-8834 apaulson@usgs.gov","orcid":"https://orcid.org/0000-0002-2358-8834","contributorId":5236,"corporation":false,"usgs":true,"family":"Paulson","given":"Anthony","email":"apaulson@usgs.gov","middleInitial":"J.","affiliations":[],"preferred":true,"id":290086,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Wagner, Richard J. rjwagner@usgs.gov","contributorId":3122,"corporation":false,"usgs":true,"family":"Wagner","given":"Richard","email":"rjwagner@usgs.gov","middleInitial":"J.","affiliations":[{"id":622,"text":"Washington Water Science Center","active":true,"usgs":true}],"preferred":true,"id":290085,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Sanzolone, Richard F.","contributorId":88007,"corporation":false,"usgs":true,"family":"Sanzolone","given":"Richard","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":290088,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Cox, Steven E.","contributorId":24875,"corporation":false,"usgs":true,"family":"Cox","given":"Steven","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":290087,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":79504,"text":"ofr20061374 - 2006 - Selected Natural Attenuation Monitoring Data, Operable Unit 1, Naval Undersea Warfare Center, Division Keyport, Washington, June 2005","interactions":[],"lastModifiedDate":"2012-03-08T17:16:22","indexId":"ofr20061374","displayToPublicDate":"2006-12-28T00:00:00","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":"2006-1374","title":"Selected Natural Attenuation Monitoring Data, Operable Unit 1, Naval Undersea Warfare Center, Division Keyport, Washington, June 2005","docAbstract":"Previous investigations have shown that natural attenuation and biodegradation of chlorinated volatile organic compounds (VOCs) are substantial in shallow ground water beneath the 9-acre former landfill at Operable Unit 1 (OU-1), Naval Undersea Warfare Center, Division Keyport, Washington. The U.S. Geological Survey (USGS) has continued to monitor ground-water geochemistry to assure that conditions remain favorable for contaminant biodegradation. This report presents the ground-water geochemical and selected VOC data collected at OU-1 by the USGS during June 21-24, 2005, in support of long-term monitoring for natural attenuation.\r\n\r\nFor June 2005, the strongly reducing conditions (sulfate reduction and methanogenesis) most favorable for reductive dechlorination of chlorinated VOCs were detected in fewer upper-aquifer wells than were detected during 2004. Redox conditions in ground water from the intermediate aquifer just downgradient of the landfill remained somewhat favorable for reductive dechlorination. Overall, the changes in redox conditions observed at individual wells have not been consistent or substantial throughout either the upper or the intermediate aquifers.\r\n\r\nIn apparent contrast to changes in redox conditions, the chlorinated VOC concentrations were lower than previously measured in many of the piezometers in the northern phytoremediation plantation. The decrease in contaminant concentrations beneath the northern plantation and the end-product (ethane and ethene) evidence for reductive dechlorination are consistent with 2000-04 results.\r\n\r\nIn the southern phytoremediation plantation, changes in chlorinated VOC concentrations were variable. Most notable was a substantial decrease in the sum of trichloroethene, cis-1,2-dichloroethene, and vinyl chloride concentrations at piezometer P1-9 from 75,000 to 1,000 micrograms per liter between 2004 and 2005. The high concentrations of the reductive dechlorination end-products ethane and ethene measured at the most contaminated sites (P1-6 and P1-7), as well as measurable concentrations at sites P1-9 and P1-10, are reliable evidence that reductive dechlorination of chlorinated VOCs is ongoing in the southern plantation.\r\n\r\nIn the 10 passive-diffusion samplers deployed beneath the marsh stream, the highest chlorinated VOC concentrations measured were at a site (S-4) about midway along the sampled stream reach. In 2005, the sum of trichloroethene, cis-1,2-dichloroethene, and vinyl chloride concentrations increased nearly twofold in comparison to 2004. It is not certain that the apparent increase in concentrations is representative of site conditions. However, the chlorinated VOC concentrations have increased each time at the two most contaminated passive-diffusion sampler sites that have been sampled for multiple years. In the marsh stream, chlorinated VOC concentrations in surface water were low at the site (SW-S6) near the upgradient margin of the former landfill. Concentrations in the stream increased substantially after flowing past the southern phytoremediation plantation to the downstream site (MA-12).\r\n\r\nOverall, the 2005 data were consistent with previous findings of continued biodegradation of chlorinated VOCs in ground water, along with continued discharge of some chlorinated VOCs to surface water in the marsh stream.\r\n\r\n","language":"ENGLISH","doi":"10.3133/ofr20061374","collaboration":"Prepared in cooperation with Department of the Navy, Naval Facilities Engineering Command, Northwest","usgsCitation":"Dinicola, R., and Huffman, R., 2006, Selected Natural Attenuation Monitoring Data, Operable Unit 1, Naval Undersea Warfare Center, Division Keyport, Washington, June 2005: U.S. Geological Survey Open-File Report 2006-1374, iv, 28 p.; 2 figs.; 3 tables, https://doi.org/10.3133/ofr20061374.","productDescription":"iv, 28 p.; 2 figs.; 3 tables","numberOfPages":"32","temporalStart":"2005-06-21","temporalEnd":"2005-06-24","costCenters":[{"id":622,"text":"Washington Water Science Center","active":true,"usgs":true}],"links":[{"id":190718,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":9061,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2006/1374/","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a09e4b07f02db5fa7dd","contributors":{"authors":[{"text":"Dinicola, Richard S. 0000-0003-4222-294X dinicola@usgs.gov","orcid":"https://orcid.org/0000-0003-4222-294X","contributorId":352,"corporation":false,"usgs":true,"family":"Dinicola","given":"Richard S.","email":"dinicola@usgs.gov","affiliations":[{"id":622,"text":"Washington Water Science Center","active":true,"usgs":true}],"preferred":true,"id":290080,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Huffman, R.L.","contributorId":44956,"corporation":false,"usgs":true,"family":"Huffman","given":"R.L.","email":"","affiliations":[],"preferred":false,"id":290081,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":79512,"text":"ofr20061312 - 2006 - Micrometeorological and Soil Data for Calculating Evapotranspiration for Rainier Mesa, Nevada Test Site, Nevada, 2002-05","interactions":[],"lastModifiedDate":"2012-03-08T17:16:23","indexId":"ofr20061312","displayToPublicDate":"2006-12-28T00:00:00","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":"2006-1312","title":"Micrometeorological and Soil Data for Calculating Evapotranspiration for Rainier Mesa, Nevada Test Site, Nevada, 2002-05","docAbstract":"Micrometeorological and soil-moisture data were collected at two instrumented sites on Rainier Mesa at the Nevada Test Site, January 1, 2002 - August 23, 2005. Data collected at each site include net radiation, air temperature, and relative humidity at two heights; wind speed and direction; subsurface soil heat flux; subsurface soil temperature; volumetric soil water; and matric water potential. These data were used to estimate 20-minute average and daily average evapotranspiration values. The data presented in this report are collected and calculated evapotranspiration rates.","language":"ENGLISH","doi":"10.3133/ofr20061312","collaboration":"Prepared in cooperation with the Nevada Operation Office of the U.S. Department of Energy, under Interagency Agreement DE-AI52-01NV13944","usgsCitation":"DeMeo, G.A., Flint, A.L., Laczniak, R.J., and Nylund, W.E., 2006, Micrometeorological and Soil Data for Calculating Evapotranspiration for Rainier Mesa, Nevada Test Site, Nevada, 2002-05: U.S. Geological Survey Open-File Report 2006-1312, iv, 12 p., https://doi.org/10.3133/ofr20061312.","productDescription":"iv, 12 p.","numberOfPages":"16","temporalStart":"2002-01-01","temporalEnd":"2005-08-23","costCenters":[{"id":465,"text":"Nevada Water Science Center","active":true,"usgs":true}],"links":[{"id":194429,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":9066,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2006/1312/","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a51e4b07f02db62a034","contributors":{"authors":[{"text":"DeMeo, Guy A. gademeo@usgs.gov","contributorId":2124,"corporation":false,"usgs":true,"family":"DeMeo","given":"Guy","email":"gademeo@usgs.gov","middleInitial":"A.","affiliations":[],"preferred":true,"id":290101,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Flint, Alan L. 0000-0002-5118-751X aflint@usgs.gov","orcid":"https://orcid.org/0000-0002-5118-751X","contributorId":1492,"corporation":false,"usgs":true,"family":"Flint","given":"Alan","email":"aflint@usgs.gov","middleInitial":"L.","affiliations":[{"id":657,"text":"Western Geographic Science Center","active":true,"usgs":true},{"id":154,"text":"California Water Science Center","active":true,"usgs":true}],"preferred":true,"id":290100,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Laczniak, Randell J.","contributorId":90687,"corporation":false,"usgs":true,"family":"Laczniak","given":"Randell","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":290103,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Nylund, Walter E.","contributorId":12913,"corporation":false,"usgs":true,"family":"Nylund","given":"Walter","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":290102,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":79509,"text":"fs20063121 - 2006 - Pesticides in ground water - Sublette County, Wyoming, 2004-2005","interactions":[],"lastModifiedDate":"2022-08-30T18:30:22.832538","indexId":"fs20063121","displayToPublicDate":"2006-12-28T00:00:00","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":"2006-3121","title":"Pesticides in ground water - Sublette County, Wyoming, 2004-2005","docAbstract":"In 1991, members of local, State, and Federal governments, as well as industry and interest groups, formed the Ground-water and Pesticide Strategy Committee to prepare the State of Wyoming's generic Management Plan for Pesticides in Ground Water. Part of this management plan is to sample and analyze Wyoming's ground water for pesticides. In 1995, the U.S. Geological Survey, in cooperation with the Ground-water and Pesticide Strategy Committee, began statewide implementation of the sampling component of the State of Wyoming's generic Management Plan for Pesticides in Ground Water. During 2004-2005, baseline monitoring was conducted in Sublette County. This fact sheet describes and summarizes results of the baseline monitoring in Sublette County.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/fs20063121","collaboration":"In cooperation with the Wyoming Department of Agriculture (WDA) and the Wyoming Department of Environmental Quality (WDEQ)","usgsCitation":"Eddy-Miller, C., and Remley, K., 2006, Pesticides in ground water - Sublette County, Wyoming, 2004-2005: U.S. Geological Survey Fact Sheet 2006-3121, 4 p., https://doi.org/10.3133/fs20063121.","productDescription":"4 p.","numberOfPages":"4","temporalStart":"2004-01-01","temporalEnd":"2005-12-31","costCenters":[{"id":684,"text":"Wyoming Water Science Center","active":false,"usgs":true}],"links":[{"id":120783,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/fs_2006_3121.jpg"},{"id":405930,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_80468.htm","linkFileType":{"id":5,"text":"html"}},{"id":9184,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/fs/2006/3121/","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Wyoming","county":"Sublette County","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"Polygon\",\"coordinates\":[[[-110.0545,43.4666],[-109.8172,43.4646],[-109.7775,43.4643],[-109.751,43.4642],[-109.7535,43.3895],[-109.7529,43.3672],[-109.7365,43.3638],[-109.7228,43.3735],[-109.704,43.3751],[-109.693,43.3666],[-109.6935,43.3571],[-109.6914,43.3498],[-109.6943,43.3397],[-109.6934,43.3293],[-109.6895,43.3257],[-109.6837,43.3212],[-109.6811,43.3158],[-109.6746,43.305],[-109.6769,43.2967],[-109.6775,43.2954],[-109.6797,43.2853],[-109.6834,43.2816],[-109.6826,43.2744],[-109.6794,43.2703],[-109.6792,43.2639],[-109.6809,43.2557],[-109.6789,43.2517],[-109.6743,43.2449],[-109.6729,43.2376],[-109.6747,43.2317],[-109.6769,43.2226],[-109.6749,43.2149],[-109.6681,43.194],[-109.6589,43.1768],[-109.6512,43.171],[-109.6391,43.1643],[-109.6333,43.1608],[-109.6288,43.1545],[-109.6239,43.135],[-109.6162,43.1264],[-109.5996,43.1153],[-109.5856,43.1031],[-109.5755,43.1019],[-109.5697,43.0974],[-109.5625,43.0839],[-109.5566,43.0735],[-109.5463,43.0618],[-109.565,43.0556],[-109.5661,43.0493],[-109.5604,43.0461],[-109.5558,43.0385],[-109.5569,43.0275],[-109.558,43.0202],[-109.5528,43.0158],[-109.5365,43.0132],[-109.5214,43.0134],[-109.5126,43.0103],[-109.498,43.0032],[-109.4866,42.9942],[-109.4758,42.9898],[-109.4651,42.9854],[-109.4586,42.9773],[-109.4566,42.9718],[-109.4409,42.967],[-109.4238,42.9572],[-109.4059,42.9485],[-109.4055,42.9482],[-109.3972,42.942],[-109.3977,42.9388],[-109.3846,42.9371],[-109.3734,42.9445],[-109.3588,42.9329],[-109.3561,42.9247],[-109.3473,42.9184],[-109.3381,42.8994],[-109.3286,42.8909],[-109.3307,42.8736],[-109.3269,42.8682],[-109.3117,42.8565],[-109.2985,42.8544],[-109.2794,42.8336],[-109.2691,42.821],[-109.2533,42.8116],[-109.2402,42.8095],[-109.2188,42.8051],[-109.2106,42.7952],[-109.2329,42.7886],[-109.2397,42.7826],[-109.2421,42.7785],[-109.2426,42.769],[-109.2382,42.7663],[-109.2225,42.7632],[-109.2188,42.766],[-109.2126,42.7688],[-109.2045,42.7684],[-109.1944,42.7626],[-109.1811,42.7554],[-109.1598,42.7456],[-109.1528,42.7402],[-109.147,42.7307],[-109.1381,42.7213],[-109.1336,42.7122],[-109.1265,42.695],[-109.0722,42.6959],[-109.0717,42.6659],[-109.0707,42.6],[-109.0708,42.565],[-109.0704,42.5355],[-109.0708,42.5214],[-109.0696,42.4482],[-109.0694,42.4333],[-109.0433,42.4335],[-109.0442,42.3662],[-109.0446,42.3517],[-109.0447,42.2781],[-109.0451,42.2635],[-109.0649,42.2634],[-109.1598,42.2635],[-109.179,42.2633],[-109.2776,42.2637],[-109.2955,42.264],[-109.3737,42.2641],[-109.3935,42.2639],[-109.4115,42.2641],[-109.435,42.2643],[-109.4499,42.2646],[-109.4605,42.2645],[-109.4729,42.2648],[-109.5132,42.2657],[-109.5312,42.266],[-109.5814,42.2658],[-109.6304,42.2661],[-109.649,42.2659],[-109.7463,42.266],[-109.7655,42.2662],[-109.8623,42.2675],[-110,42.2696],[-110.0533,42.2705],[-110.0887,42.2709],[-110.17,42.2736],[-110.1886,42.2747],[-110.1973,42.275],[-110.2085,42.2753],[-110.2283,42.2754],[-110.3133,42.2766],[-110.3258,42.2769],[-110.3468,42.2769],[-110.3866,42.2776],[-110.4058,42.2777],[-110.4262,42.2777],[-110.4455,42.2774],[-110.4783,42.2772],[-110.5242,42.2777],[-110.5428,42.2778],[-110.5426,42.3055],[-110.5427,42.3237],[-110.5423,42.365],[-110.541,42.4482],[-110.5908,42.4486],[-110.5891,42.5373],[-110.5912,42.7105],[-110.6261,42.7102],[-110.6257,42.7817],[-110.5876,42.7815],[-110.5874,42.7885],[-110.5869,43.126],[-110.5774,43.126],[-110.5774,43.2353],[-110.5824,43.2939],[-110.3457,43.2938],[-110.3456,43.3252],[-110.3456,43.3807],[-110.1584,43.3798],[-110.1117,43.3797],[-110.0538,43.3797],[-110.0547,43.452],[-110.0545,43.4666]]]},\"properties\":{\"name\":\"Sublette\",\"state\":\"WY\"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae0e4b07f02db6882b3","contributors":{"authors":[{"text":"Eddy-Miller, Cheryl A.","contributorId":86755,"corporation":false,"usgs":true,"family":"Eddy-Miller","given":"Cheryl A.","affiliations":[],"preferred":false,"id":290095,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Remley, Kendra J.","contributorId":26753,"corporation":false,"usgs":true,"family":"Remley","given":"Kendra J.","affiliations":[],"preferred":false,"id":290094,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":79513,"text":"ofr20061377 - 2006 - Distribution, thickness, and volume of fine-grained sediment from precipitation of metals from acid-mine waters in Keswick Reservoir, Shasta County, California","interactions":[],"lastModifiedDate":"2014-10-09T14:15:40","indexId":"ofr20061377","displayToPublicDate":"2006-12-28T00:00:00","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":"2006-1377","title":"Distribution, thickness, and volume of fine-grained sediment from precipitation of metals from acid-mine waters in Keswick Reservoir, Shasta County, California","docAbstract":"<p>In February 1993, the U.S. Geological Survey (USGS) acquired high-resolution seismic-reflection data to map the distribution and thickness of fine-grained sediments associated with acid-mine drainage in Keswick Reservoir on the Sacramento River, near Redding, California. In the Spring Creek Arm of Keswick Reservoir, the sediments occurred in three distinct accumulations; thicknesses are greater than 2 meters (m) in the western accumulation, greater than 5 m in the central accumulation, and up to 8 m in the eastern accumulation. In Keswick Reservoir, fine-grained sediments related to acid-mine drainage were present from slightly north of the Spring Creek Arm downstream to the Keswick Dam. Sediment thickness varies from about 3 m opposite the mouth of the Spring Creek Arm to less than 1 m near Keswick Dam.</p>\n<br>\n<p>Our estimate for the total volume of fine-grained sediments in the Spring Creek Arm at the time of the geophysical survey in February 1993 is about 152,000 cubic meters in three sediment accumulations, with about 14,000, 32,000, and 105,000 cubic meters respectively in the western, central, and eastern accumulations. We interpreted that an additional 110, 000 cubic meters of material was present in the main part of Keswick Reservoir. At the time of data collection, we therefore estimate that the total volume of fine-grained sediment was 260,000 cubic meters. In the main part of Keswick Reservoir, 42% to 50% of the reservoir area contiguous to Spring Creek Arm had mappable fine-grained sediments. Decreasing sediment supply down-reservoir meant that mappable sediment covered only about 35% of the reservoir in the area to the south, decreasing to about 12% near Keswick Dam. Much of the reservoir bottom below the Spring Creek Arm could have had a thin (less than 20-30 cm) cover of fine-grained sediment that was not mappable using the seismic-reflection data.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr20061377","usgsCitation":"Bruns, T.R., Alpers, C.N., and Carlson, P., 2006, Distribution, thickness, and volume of fine-grained sediment from precipitation of metals from acid-mine waters in Keswick Reservoir, Shasta County, California: U.S. Geological Survey Open-File Report 2006-1377, HTML Document, https://doi.org/10.3133/ofr20061377.","productDescription":"HTML Document","additionalOnlineFiles":"Y","costCenters":[{"id":186,"text":"Coastal and Marine Geology Program","active":true,"usgs":true}],"links":[{"id":192524,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ofr20061377.PNG"},{"id":9067,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2006/1377/","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"California","county":"Shasta County","otherGeospatial":"Keswick Reservoir","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a5fe4b07f02db634a01","contributors":{"authors":[{"text":"Bruns, Terry R.","contributorId":29420,"corporation":false,"usgs":true,"family":"Bruns","given":"Terry","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":290105,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Alpers, Charles N. 0000-0001-6945-7365 cnalpers@usgs.gov","orcid":"https://orcid.org/0000-0001-6945-7365","contributorId":411,"corporation":false,"usgs":true,"family":"Alpers","given":"Charles","email":"cnalpers@usgs.gov","middleInitial":"N.","affiliations":[{"id":154,"text":"California Water Science Center","active":true,"usgs":true}],"preferred":true,"id":290104,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Carlson, Paul","contributorId":52234,"corporation":false,"usgs":true,"family":"Carlson","given":"Paul","affiliations":[],"preferred":false,"id":290106,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":79508,"text":"sir20065210 - 2006 - Occurrence of anthropogenic organic compounds in ground water and finished water of community water systems in Eagle and Spanish Springs Valleys, Nevada, 2002-2004","interactions":[],"lastModifiedDate":"2012-03-08T17:16:25","indexId":"sir20065210","displayToPublicDate":"2006-12-28T00:00:00","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":"2006-5210","title":"Occurrence of anthropogenic organic compounds in ground water and finished water of community water systems in Eagle and Spanish Springs Valleys, Nevada, 2002-2004","docAbstract":"As a part of the U.S. Geological Survey's National Water-Quality Assessment Program, an effort to characterize the quality of major rivers and aquifers used as a source of supply to some of the largest community water systems (CWSs) in the United States has been initiated. These studies, termed Source Water-Quality Assessments (SWQAs), consist of two sampling phases. Phase 1 was designed to determine the frequency of detection and concentrations of about 260  volatile organic compounds (VOCs), pesticides and pesticide degradates, and other anthropogenic organic compounds in source water of 15 CWS wells in each study. Phase 2 monitors concentrations in the source water and also the associated finished water of CWSs for compounds most frequently detected during phase 1. One SWQA was completed in the Nevada Basin and Range area in Nevada. Ten CWS wells in Eagle Valley and five CWS wells in Spanish Springs Valley were sampled. For phase 2, two wells were resampled in Eagle Valley. Samples were collected during 2002-2004 for both phases.\r\n\r\nWater use in Eagle Valley is primarily for domestic purposes and is supplied through CWSs. Ground-water sources provide about 55 percent of the public-water supply, and surface-water sources supply about 45 percent. Lesser amounts of water are provided by domestic wells. Very little water is used for agriculture or manufacturing. Spanish Springs Valley has water-use characteristics similar to those in Eagle Valley, although there is more agricultural water use in Spanish Springs Valley than in Eagle Valley.\r\n\r\n\r\nMaximum contaminant concentrations were compared to two human-health benchmarks, if available, to describe the water-quality data in a human-health context for these findings. Measured concentrations of regulated contaminants were compared to U.S. Environmental Protection Agency and Nevada Maximum Contaminant Level (MCL) values. Measured concentrations of unregulated contaminants were compared to Health-Based Screening Levels, which are not regulatory standards and are not legally enforceable values. All of the contaminants detected in this study were found at concentrations less than available human-health benchmarks.\r\n\r\n\r\nIn the source waters sampled in phase 1, 10 contaminants of the approximately 260 measured were detected in samples collected from Eagle Valley, and 4 contaminants were detected in samples from Spanish Springs Valley. The most frequently detected compounds in the Eagle Valley source water were chloroform (a disinfection by-product), which was detected in samples from four wells, and deethylatrazine (a degradation product of the herbicide atrazine), which was detected in samples from three wells. Each of the four contaminants detected in the Spanish Springs Valley source waters was detected in samples from one well.\r\n\r\n\r\nThe detection frequencies of VOCs and pesticides in samples from the SWQA wells were similar to those in samples from both shallow and deep monitoring wells in Carson City, Reno, and Spanish Springs. This indicates that the SWQA sampling is representative of the organic chemical compounds likely to be detected in the aquifers sampled. However, more organic compounds were detected at low frequencies and concentrations in samples from the monitoring wells than in samples from SWQA wells.\r\n\r\n\r\nThree contaminants were detected in one finished-water sample collected from Eagle Valley. Comparison of SWQA results in the Nevada Basin and Range Study Unit to results of an SWQA in the larger urban area of Salt Lake City showed that fewer anthropogenic compounds were detected in Eagle and Spanish Springs Valleys and generally at lower concentrations than in the Salt Lake City study.\r\n","language":"ENGLISH","doi":"10.3133/sir20065210","usgsCitation":"Rosen, M.R., Shaefer, D.H., Toccalino, P.A., and Delzer, G.C., 2006, Occurrence of anthropogenic organic compounds in ground water and finished water of community water systems in Eagle and Spanish Springs Valleys, Nevada, 2002-2004: U.S. Geological Survey Scientific Investigations Report 2006-5210, viii, 31 p.; 7 figs.; 6 tables, https://doi.org/10.3133/sir20065210.","productDescription":"viii, 31 p.; 7 figs.; 6 tables","numberOfPages":"31","temporalStart":"2002-01-01","temporalEnd":"2004-12-31","costCenters":[{"id":465,"text":"Nevada Water Science Center","active":true,"usgs":true}],"links":[{"id":195520,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":9091,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/sir/2006/5210/","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e6e4b07f02db5e76ca","contributors":{"authors":[{"text":"Rosen, Michael R. 0000-0003-3991-0522 mrosen@usgs.gov","orcid":"https://orcid.org/0000-0003-3991-0522","contributorId":495,"corporation":false,"usgs":true,"family":"Rosen","given":"Michael","email":"mrosen@usgs.gov","middleInitial":"R.","affiliations":[{"id":154,"text":"California Water Science Center","active":true,"usgs":true}],"preferred":true,"id":290090,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Shaefer, Donald H.","contributorId":100961,"corporation":false,"usgs":true,"family":"Shaefer","given":"Donald","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":290093,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Toccalino, Patricia A.","contributorId":8195,"corporation":false,"usgs":true,"family":"Toccalino","given":"Patricia","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":290092,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Delzer, Gregory C. 0000-0002-7077-4963 gcdelzer@usgs.gov","orcid":"https://orcid.org/0000-0002-7077-4963","contributorId":986,"corporation":false,"usgs":true,"family":"Delzer","given":"Gregory","email":"gcdelzer@usgs.gov","middleInitial":"C.","affiliations":[{"id":562,"text":"South Dakota Water Science Center","active":true,"usgs":true}],"preferred":true,"id":290091,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":79507,"text":"sir20065284 - 2006 - Peak Discharge, Flood Profile, Flood Inundation, and Debris Movement Accompanying the Failure of the Upper Reservoir at the Taum Sauk Pump Storage Facility near Lesterville, Missouri","interactions":[],"lastModifiedDate":"2012-02-02T00:14:22","indexId":"sir20065284","displayToPublicDate":"2006-12-28T00:00:00","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":"2006-5284","title":"Peak Discharge, Flood Profile, Flood Inundation, and Debris Movement Accompanying the Failure of the Upper Reservoir at the Taum Sauk Pump Storage Facility near Lesterville, Missouri","docAbstract":"The Taum Sauk pump-storage hydroelectric power plant located in Reynolds County, Missouri, uses turbines that operate as pumps and hydraulic head generated by discharging water from an upper to a lower reservoir to produce electricity. A 55-acre upper reservoir with a 1.5- billion gallon capacity was built on top of Proffit Mountain, approximately 760 feet above the floodplain of the East Fork Black River. At approximately 5:16 am on December 14, 2005, a 680-foot wide section of the upper reservoir embankment failed suddenly, sending water rushing down the western side of Proffit Mountain and emptying into the floodplain of East Fork Black River. Flood waters from the upper reservoir flowed downstream through Johnson's Shut-Ins State Park and into the lower reservoir of the East Fork Black River. Floods such as this present unique challenges and opportunities to analyze and document peak-flow characteristics, flood profiles, inundation extents, and debris movement. \r\n\r\nOn December 16, 2005, Light Detection and Ranging (LiDAR) data were collected and used to support hydraulic analyses, forensic failure analyses, damage extent, and mitigation of future disasters. To evaluate the impact of sedimentation in the lower reservoir, a bathymetric survey conducted on December 22 and 23, 2005, was compared to a previous bathymetric survey conducted in April, 2005. Survey results indicated the maximum reservoir capacity difference of 147 acre-feet existed at a pool elevation of 730 feet. \r\n\r\nPeak discharge estimates of 289,000 cubic feet per second along Proffit Mountain and 95,000 cubic feet per second along the East Fork Black River were determined through indirect measurement techniques. The magnitude of the embankment failure flood along the East Fork Black River was approximately 4 times greater than the 100-year flood frequency estimate of 21,900 cubic feet per second, and approximately 3 times greater than the 500-year flood frequency estimate of 30,500 cubic feet per second. Dynamic wave unsteady flow models Dam Break (DAMBRK) and Unsteady NETwork (UNET) were used to route the flood wave from the embankment failure breach of the upper reservoir to the spillway of the lower reservoir. Simulated velocities ranged from 20 to 51 feet per second along Proffit Mountain and 12 to 32 feet per second along the East Fork Black River. Simulated arrival time of the flood wave took approximately 5.5 to 6.0 minutes to enter into the floodplain of the East Fork Black River, and roughly 29 minutes to begin filling the lower reservoir. Simulated shear stress values reached as high as 232 pounds per square foot along the slope of Proffit Mountain and 144 pounds per square foot within the Shut-Ins. Flood depths from the embankment failure may have reached greater than 50 feet along Proffit Mountain and as much as 30 to 40 feet along the East Fork Black River. \r\n\r\nA steady-state model was used to develop 2-, 5-, 10-, 25-, 50-, 100-, and 500-year flood frequency profiles along the East Fork Black River. A similar flood event, hypothetically resulting from a breach of the east embankment above Taum Sauk Creek, was simulated along with the 100- and 500-year flood profiles on Taum Sauk Creek. Estimated extents of flood inundation were developed for each profile. \r\n\r\nDebris movement was extensive as a result of the flood wave moving down Proffit Mountain and through Johnson's Shut-Ins State Park. A quantitative assessment of debris movement was conducted to benefit rehabilitation efforts within the park. Approximately 180 acres of timber were affected as a result of the embankment failure flood.","language":"ENGLISH","doi":"10.3133/sir20065284","usgsCitation":"Rydlund, P.H., 2006, Peak Discharge, Flood Profile, Flood Inundation, and Debris Movement Accompanying the Failure of the Upper Reservoir at the Taum Sauk Pump Storage Facility near Lesterville, Missouri: U.S. Geological Survey Scientific Investigations Report 2006-5284, vi, 46 p., https://doi.org/10.3133/sir20065284.","productDescription":"vi, 46 p.","numberOfPages":"52","costCenters":[],"links":[{"id":194903,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":9064,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/sir/2006/5284/","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae1e4b07f02db688a27","contributors":{"authors":[{"text":"Rydlund, Paul H. Jr. 0000-0001-9461-9944 prydlund@usgs.gov","orcid":"https://orcid.org/0000-0001-9461-9944","contributorId":3840,"corporation":false,"usgs":true,"family":"Rydlund","given":"Paul","suffix":"Jr.","email":"prydlund@usgs.gov","middleInitial":"H.","affiliations":[{"id":36532,"text":"Central Midwest Water Science Center","active":true,"usgs":true},{"id":396,"text":"Missouri Water Science Center","active":true,"usgs":true},{"id":502,"text":"Office of Surface Water","active":true,"usgs":true}],"preferred":true,"id":290089,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":79514,"text":"ofr20061373 - 2006 - High-resolution boomer seismic-reflection profiles of the shelf off southern California from cruise A-1-00-SC: Santa Monica Bay to San Diego","interactions":[],"lastModifiedDate":"2023-03-24T20:01:10.221922","indexId":"ofr20061373","displayToPublicDate":"2006-12-28T00:00:00","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":"2006-1373","title":"High-resolution boomer seismic-reflection profiles of the shelf off southern California from cruise A-1-00-SC: Santa Monica Bay to San Diego","docAbstract":"High-resolution boomer data were collected in the California Continental Borderland as part of the southern California Earthquake Hazards Task of the Southern California Coastal and Marine Geology Regional Investigations Project. During the period from 1997 to 2002, five data-acquisition cruises collected seismic-reflection data using several different systems from offshore Santa Barbara, California, south to the Exclusive Economic Zone boundary with Mexico. A key mission of this project was to map late Quaternary deformation in addition to improving our understanding of which offshore fault zones might have potential to damage highly populated areas of southern California. State regulations concerning the use of seismic-reflection equipment within three miles of the coastline precluded the routine gathering of high-resolution multichannel data in that swath adjacent to the coast. Boomer seismic-reflection data, however, can be obtained within the state 3-mile limit provided the operation receives authorization from the California State Lands Commission. \r\n\r\nThe Geopulse boomer data accessible through this report were collected on the cruise A-1-00-SC, which was the only survey where we requested permission to work inside the 3-mile limit of the State of California. These data are critical to discovering connections between onshore and offshore faults, the overall lengths of which are related to the potential size of an earthquake that might be generated along them. The 2000 survey was designed to fill the gap between onshore data and reflection data obtained in deeper water on previous cruises as well as data anticipated from future surveys. This report includes trackline maps showing the location of the data, as well as both digital data files (SEG-Y) and images of all of the profiles.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr20061373","usgsCitation":"Gutmacher, C.E., Ross, S.L., Triezenberg, P., Sliter, R.W., Normark, W.R., and Edwards, B.D., 2006, High-resolution boomer seismic-reflection profiles of the shelf off southern California from cruise A-1-00-SC: Santa Monica Bay to San Diego (Version 1.0): U.S. Geological Survey Open-File Report 2006-1373, HTML Document, https://doi.org/10.3133/ofr20061373.","productDescription":"HTML Document","additionalOnlineFiles":"Y","temporalStart":"2000-06-05","temporalEnd":"2000-06-29","costCenters":[{"id":520,"text":"Pacific Coastal and Marine Science Center","active":true,"usgs":true},{"id":645,"text":"Western Coastal and Marine Geology","active":false,"usgs":true}],"links":[{"id":192424,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":414730,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_78843.htm","linkFileType":{"id":5,"text":"html"}},{"id":9068,"rank":2,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2006/1373/","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"California","city":"San Diego","otherGeospatial":"Santa Monica Bay","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -117.1208,\n              32.5828\n            ],\n            [\n              -117.1208,\n              34.0328\n            ],\n            [\n              -118.8056,\n              34.0328\n            ],\n            [\n              -118.8056,\n              32.5828\n            ],\n            [\n              -117.1208,\n              32.5828\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","edition":"Version 1.0","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a59e4b07f02db62fa08","contributors":{"authors":[{"text":"Gutmacher, Christina E.","contributorId":28272,"corporation":false,"usgs":true,"family":"Gutmacher","given":"Christina","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":290110,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Ross, Stephanie L. 0000-0003-1389-4405 sross@usgs.gov","orcid":"https://orcid.org/0000-0003-1389-4405","contributorId":1024,"corporation":false,"usgs":true,"family":"Ross","given":"Stephanie","email":"sross@usgs.gov","middleInitial":"L.","affiliations":[{"id":520,"text":"Pacific Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":true,"id":290107,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Triezenberg, Peter J.","contributorId":32625,"corporation":false,"usgs":true,"family":"Triezenberg","given":"Peter J.","affiliations":[],"preferred":false,"id":290111,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Sliter, Ray W. 0000-0003-0337-3454 rsliter@usgs.gov","orcid":"https://orcid.org/0000-0003-0337-3454","contributorId":1992,"corporation":false,"usgs":true,"family":"Sliter","given":"Ray","email":"rsliter@usgs.gov","middleInitial":"W.","affiliations":[{"id":520,"text":"Pacific Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":true,"id":290108,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Normark, William R.","contributorId":69570,"corporation":false,"usgs":true,"family":"Normark","given":"William","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":290112,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Edwards, Brian D. bedwards@usgs.gov","contributorId":3161,"corporation":false,"usgs":true,"family":"Edwards","given":"Brian","email":"bedwards@usgs.gov","middleInitial":"D.","affiliations":[{"id":520,"text":"Pacific Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":true,"id":290109,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}}
,{"id":79518,"text":"ofr20061266 - 2006 - Water-quality, bed-sediment, and biological data (October 2004 through September 2005) and statistical summaries of data for streams in the Upper Clark Fork Basin, Montana","interactions":[],"lastModifiedDate":"2020-01-27T06:39:38","indexId":"ofr20061266","displayToPublicDate":"2006-12-28T00:00:00","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":"2006-1266","title":"Water-quality, bed-sediment, and biological data (October 2004 through September 2005) and statistical summaries of data for streams in the Upper Clark Fork Basin, Montana","docAbstract":"Water, bed sediment, and biota were sampled in streams from Butte to below Missoula as part of a long-term monitoring program, conducted in cooperation with the U.S. Environmental Protection Agency, to characterize aquatic resources in the upper Clark Fork basin of western Montana. Sampling sites were located on the Clark Fork, six major tributaries, and three smaller tributaries. Water-quality samples were collected periodically at 18 sites during October 2004 through September 2005 (water year 2005). Bed-sediment and biological samples were collected once in August 2005. The primary constituents analyzed were trace elements associated with tailings from historical mining and smelting activities. This report summarizes the results of water-quality, bed-sediment, and biota samples col-lected in water year 2005 and provides statistical summaries of data collected since 1985.\r\n\r\nWater-quality data for samples collected periodically from streams include concentrations of selected major ions, trace ele-ments, and suspended sediment. Daily values of suspended-sed-iment concentration and suspended-sediment discharge were determined for three sites. Bed-sediment data include trace-ele-ment concentrations in the fine-grained fraction. Bio-logical data include trace-element concentrations in whole-body tissue of aquatic benthic insects. Quality-assurance data are reported for analytical results of water, \r\nbed sediment, and biota. Statistical summaries of water-quality, bed-sediment, and biological data are provided for the period of record since 1985 for each site.\r\n\r\n","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr20061266","usgsCitation":"Dodge, K.A., Hornberger, M.I., and Dyke, J., 2006, Water-quality, bed-sediment, and biological data (October 2004 through September 2005) and statistical summaries of data for streams in the Upper Clark Fork Basin, Montana: U.S. Geological Survey Open-File Report 2006-1266, v, 109 p., https://doi.org/10.3133/ofr20061266.","productDescription":"v, 109 p.","numberOfPages":"114","temporalStart":"2004-10-01","temporalEnd":"2005-09-30","costCenters":[{"id":400,"text":"Montana Water Science Center","active":false,"usgs":true},{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":195393,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":9073,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2006/1266/","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Montana","otherGeospatial":"Upper Clark Fork 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jldyke@usgs.gov","contributorId":1035,"corporation":false,"usgs":true,"family":"Dyke","given":"Jessica","email":"jldyke@usgs.gov","affiliations":[{"id":438,"text":"National Research Program - Western Branch","active":true,"usgs":true}],"preferred":false,"id":290120,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":79503,"text":"ofr20061285 - 2006 - Selected Ground-Water Data for Yucca Mountain Region, Southern Nevada and Eastern California, January-December 2004","interactions":[],"lastModifiedDate":"2012-03-08T17:16:24","indexId":"ofr20061285","displayToPublicDate":"2006-12-23T00:00:00","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":"2006-1285","title":"Selected Ground-Water Data for Yucca Mountain Region, Southern Nevada and Eastern California, January-December 2004","docAbstract":"The U.S. Geological Survey, in support of the U.S. Department of Energy, Office of Repository Development, collects, compiles, and summarizes hydrologic data in the Yucca Mountain region of southern Nevada and eastern California. These data are collected to allow assessments of ground-water resources during activities to determine the potential suitability or development of Yucca Mountain for storing high-level nuclear waste.\r\n\r\nData on ground-water levels at 35 boreholes and 1 fissure (Devils Hole), ground-water discharge at 5 springs, both ground-water levels and discharge at 1 flowing borehole, and total reported ground-water withdrawals within Crater Flat, Jackass Flats, Mercury Valley, and the Amargosa Desert are tabulated from January through December 2004. Also tabulated are ground-water levels, discharges, and withdrawals collected by other agencies (or collected as part of other programs) and data revised from those previously published at monitoring sites. Historical data on water levels, discharges, and withdrawals are presented graphically to indicate variations through time.\r\n\r\nA statistical summary of ground-water levels at seven boreholes in Jackass Flats is presented for the period 1992-2004 to indicate potential effects of ground-water withdrawals associated with U.S. Department of Energy activities near Yucca Mountain. The statistical summary includes the annual number of measurements, maximum, minimum, and median water-level altitudes, and average deviation of measured water-level altitudes compared to the 1992-93 baseline period. At six boreholes in Jackass Flats, median water levels for 2004 were slightly higher (0.3-2.7 feet) than their median water levels for 1992-93. At one borehole in Jackass Flats, median water level for 2004 equaled the median water level for 1992-93.\r\n\r\n","language":"ENGLISH","doi":"10.3133/ofr20061285","usgsCitation":"La Camera, R.J., Locke, G.L., Habte, A.M., and Darnell, J.G., 2006, Selected Ground-Water Data for Yucca Mountain Region, Southern Nevada and Eastern California, January-December 2004: U.S. Geological Survey Open-File Report 2006-1285, vi, 71 p., https://doi.org/10.3133/ofr20061285.","productDescription":"vi, 71 p.","numberOfPages":"77","temporalStart":"2004-01-01","temporalEnd":"2004-12-31","costCenters":[{"id":465,"text":"Nevada Water Science Center","active":true,"usgs":true}],"links":[{"id":194867,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":9060,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2006/1285/","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a09e4b07f02db5fa7e9","contributors":{"authors":[{"text":"La Camera, Richard J.","contributorId":52212,"corporation":false,"usgs":true,"family":"La Camera","given":"Richard","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":290078,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Locke, Glenn L. gllocke@usgs.gov","contributorId":2479,"corporation":false,"usgs":true,"family":"Locke","given":"Glenn","email":"gllocke@usgs.gov","middleInitial":"L.","affiliations":[],"preferred":true,"id":290076,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Habte, Aron M.","contributorId":108206,"corporation":false,"usgs":true,"family":"Habte","given":"Aron","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":290079,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Darnell, Jon G.","contributorId":47042,"corporation":false,"usgs":true,"family":"Darnell","given":"Jon","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":290077,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":79500,"text":"sir20065131 - 2006 - Statistical analyses of hydrologic system components and simulation of Edwards aquifer water-level response to rainfall using transfer-function models, San Antonio region, Texas","interactions":[],"lastModifiedDate":"2022-09-29T20:27:50.343036","indexId":"sir20065131","displayToPublicDate":"2006-12-22T00:00:00","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":"2006-5131","title":"Statistical analyses of hydrologic system components and simulation of Edwards aquifer water-level response to rainfall using transfer-function models, San Antonio region, Texas","docAbstract":"In 2003 the U.S. Geological Survey, in cooperation with the San Antonio Water System, did a study using historical data to statistically analyze hydrologic system components in the San Antonio region of Texas and to develop transfer-function models to simulate water levels at selected sites (wells) in the Edwards aquifer on the basis of rainfall. Water levels for two wells in the confined zone in Medina County and one well in the confined zone in Bexar County were highly correlated and showed little or no lag time between water-level responses. Water levels in these wells also were highly correlated with springflow at Comal Springs. Water-level hydrographs for 35 storms showed that an individual well can respond differently to similar amounts of rainfall. Fourteen water-level-recession hydrographs for a Medina County well showed that recession rates were variable. Transfer-function models were developed to simulate water levels at one confined-zone well and two recharge-zone wells in response to rainfall. For the confined-zone well, 50 percent of the simulated water levels are within 10 feet of the measured water levels, and 80 percent of the simulated water levels are within 15 feet of the measured water levels. For one recharge-zone well, 50 percent of the simulated water levels are within 5 feet of the measured water levels, and 90 percent of the simulated water levels are within 14 feet of the measured water levels. For the other recharge-zone well, 50 percent of the simulated water levels are within 14 feet of the measured water levels, and 90 percent of the simulated water levels are within 27 feet of the measured water levels. The transfer-function models showed that (1) the Edwards aquifer in the San Antonio region responds differently to recharge (effective rainfall) at different wells; and (2) multiple flow components are present in the aquifer. If simulated long-term system response results from a change in the hydrologic budget, then water levels would be difficult to simulate accurately.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/sir20065131","collaboration":"Prepared in cooperation with the San Antonio Water System","usgsCitation":"Miller, L.D., and Long, A.J., 2006, Statistical analyses of hydrologic system components and simulation of Edwards aquifer water-level response to rainfall using transfer-function models, San Antonio region, Texas: U.S. Geological Survey Scientific Investigations Report 2006-5131, iv, 20 p., https://doi.org/10.3133/sir20065131.","productDescription":"iv, 20 p.","numberOfPages":"24","costCenters":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"links":[{"id":9057,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/sir/2006/5131/","linkFileType":{"id":5,"text":"html"}},{"id":407651,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_78788.htm","linkFileType":{"id":5,"text":"html"}},{"id":191321,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"country":"United States","state":"Texas","city":"San Antonio","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -100.4,\n              29\n            ],\n            [\n              -97.7444,\n              29\n            ],\n            [\n              -97.7444,\n              30.625\n            ],\n            [\n              -100.4,\n              30.625\n            ],\n            [\n              -100.4,\n              29\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e48aae4b07f02db52c769","contributors":{"authors":[{"text":"Miller, Lisa D. 0000-0002-3523-0768 ldmiller@usgs.gov","orcid":"https://orcid.org/0000-0002-3523-0768","contributorId":1125,"corporation":false,"usgs":true,"family":"Miller","given":"Lisa","email":"ldmiller@usgs.gov","middleInitial":"D.","affiliations":[{"id":191,"text":"Colorado Water Science Center","active":true,"usgs":true}],"preferred":true,"id":290069,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Long, Andrew J. 0000-0001-7385-8081 ajlong@usgs.gov","orcid":"https://orcid.org/0000-0001-7385-8081","contributorId":989,"corporation":false,"usgs":true,"family":"Long","given":"Andrew","email":"ajlong@usgs.gov","middleInitial":"J.","affiliations":[{"id":622,"text":"Washington Water Science Center","active":true,"usgs":true},{"id":562,"text":"South Dakota Water Science Center","active":true,"usgs":true}],"preferred":true,"id":290068,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
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