Roosevelt City, Utah, asserts a need for an additional supply of water to meet municipal demands and has identified a potential location for additional groundwater development at the Sprouse well field near the West Channel of the Uinta River. Groundwater is commonly hydraulically linked to surface water and, under some conditions, the pumpage of groundwater can deplete water in streams and other water bodies. In 2008, the U.S. Geological Survey, in cooperation with Roosevelt City, the Utah Department of Natural Resources, and the Ute Indian Tribe, began a study to improve understanding of the local interconnection between groundwater and surface water and to assess the potential for streamflow depletion from future groundwater withdrawals at a potential Roosevelt City development location—the Sprouse well field near the West Channel of the Uinta River.
In the study, streamflow gains and losses at the river/aquifer boundary near the well field and changes in those conditions over time were assessed through (1) synoptic measurement of discharge in the stream at multiple sites using tracer-dilution methods, (2) periodic measurement of the vertical hydraulic gradient across the streambed, and (3) continuous measurement of stream and streambed water temperature using heat as a tracer of flow across the streambed. Although some contradictions among the results of the three assessment methods were observed, results of the approaches generally indicated (1) losing streamflow conditions on the West Channel of the Uinta River north of and upstream from the Sprouse well field within the study area, (2) gaining streamflow conditions south of and downstream from the well field, and (3) some seasonal changes in those conditions that correspond with seasonal changes in stream stage and local water-table altitudes.
A numerical groundwater flow model was developed on the basis of previously reported observations and observations made during this study, and was used to estimate potential streamflow depletion that might result from future groundwater withdrawals at the Sprouse well field. The model incorporates concepts of transient groundwater flow conditions including fluctuations in groundwater levels and storage, and the distribution of and temporal variations in gains to and losses from streamflow in the West Channel of the Uinta River near the Sprouse well field. Two predictive model simulations incorporated additional future discharge from the Sprouse well field totaling 325 acre-feet annually and biennially during summer months. Results of the predictive model simulations indicate that the water withdrawn by the additional pumping was derived initially from aquifer storage and then, with time, predominantly from streamflow depletion. By the 10th year of the predictive simulation incorporating annual summer pumping from an additional public-supply well in the Sprouse well field, the simulation results indicate that 89 percent of a future annual 325 acre-feet of discharge is derived from depletion of streamflow in the West Channel of the Uinta River. A similar result was observed in a predictive model simulating the same discharge rate but with the new well being pumped every other year.
","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/sir20115044","collaboration":"Prepared in cooperation with Roosevelt City, the Utah Department of Natural Resources, and the Ute Indian Tribe","usgsCitation":"Lambert, P., Marston, T., Kimball, B.A., and Stolp, B., 2011, Assessment of groundwater/surface-water interaction and simulation of potential streamflow depletion induced by groundwater withdrawal, Uinta River near Roosevelt, Utah: U.S. Geological Survey Scientific Investigations Report 2011-5044, vi, 48 p., https://doi.org/10.3133/sir20115044.","productDescription":"vi, 48 p.","numberOfPages":"58","additionalOnlineFiles":"N","costCenters":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":116225,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/sir_2011_5044.jpg"},{"id":21886,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/sir/2011/5044/","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Utah","otherGeospatial":"Uinta River","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -110.643310546875,\n 39.7240885773337\n ],\n [\n -110.643310546875,\n 40.91351257612758\n ],\n [\n -109.193115234375,\n 40.91351257612758\n ],\n [\n -109.193115234375,\n 39.7240885773337\n ],\n [\n -110.643310546875,\n 39.7240885773337\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4abae4b07f02db671fca","contributors":{"authors":[{"text":"Lambert, P. M.","contributorId":74380,"corporation":false,"usgs":true,"family":"Lambert","given":"P. M.","affiliations":[],"preferred":false,"id":350986,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Marston, T.","contributorId":98446,"corporation":false,"usgs":true,"family":"Marston","given":"T.","email":"","affiliations":[],"preferred":false,"id":350988,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Kimball, B. A.","contributorId":87583,"corporation":false,"usgs":false,"family":"Kimball","given":"B.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":350987,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Stolp, Bernard J. 0000-0003-3803-1497","orcid":"https://orcid.org/0000-0003-3803-1497","contributorId":71942,"corporation":false,"usgs":true,"family":"Stolp","given":"Bernard J.","affiliations":[],"preferred":false,"id":350985,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":70043973,"text":"70043973 - 2011 - Pacific lamprey artificial propogation and rearing investigations: Rocky Reach Lamprey Management Plan","interactions":[],"lastModifiedDate":"2016-06-29T13:07:36","indexId":"70043973","displayToPublicDate":"2011-06-15T14:30:00","publicationYear":"2011","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":9,"text":"Other Report"},"seriesNumber":"36958","title":"Pacific lamprey artificial propogation and rearing investigations: Rocky Reach Lamprey Management Plan","docAbstract":"The impetus for developing this document is through implementing the Rocky Reach Pacific Lamprey Management Plan (PLMP), a component of the Rocky Reach Comprehensive Settlement Agreement, both of which are discussed more thoroughly in Section 1.2. The ultimate goal of the PLMP is to achieve No Net Impact (NNI) to Pacific lamprey of ongoing operations of the Rocky Reach Hydroelectric Project. Conducting artificial propagation of Pacific lamprey was considered by the state and federal fishery agencies and Tribes that are parties to the Settlement Agreement as a potential Protection, Mitigation, and Enhancement measure (PME) for achieving NNI during the term of the current Rocky Reach license. This document is intended to provide guidance as to the feas ibility of culturing Pacific lamprey, the associated facilities necessary for culture practices, and identifying uncertainties for monitoring culture efficacy and rationale for implementing Pacific lamprey artificial propagation
","language":"English","publisher":"Chelan County PUD, Rocky Reach Hydroelectric Project","usgsCitation":"Chelan County PUD, Rocky Reach Fish Forum, U.S. Fish and Wildlife Service, United States Geological Survey, and GeoEngineers, 2011, Pacific lamprey artificial propogation and rearing investigations: Rocky Reach Lamprey Management Plan, 148 p.","productDescription":"148 p.","startPage":"1","endPage":"148","onlineOnly":"N","additionalOnlineFiles":"N","ipdsId":"IP-030247","costCenters":[{"id":654,"text":"Western Fisheries Research Center","active":true,"usgs":true}],"links":[{"id":324623,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":324621,"rank":1,"type":{"id":11,"text":"Document"},"url":"https://clio.chelanpud.org/documents/36958.pdf"}],"country":"United States","state":"Washington","county":"Chelan County, Douglas County, Grant County, Kittitas County, Okanogan County","otherGeospatial":"Lake Chelan Watershed, Methow Watershed, Upper Columbia-Entiat Watershed, Wenatchee Watershed","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -121.55273437499999,\n 46.924007100770275\n ],\n [\n -121.55273437499999,\n 48.94415123418794\n ],\n [\n -119.11376953125,\n 48.94415123418794\n ],\n [\n -119.11376953125,\n 46.924007100770275\n ],\n [\n -121.55273437499999,\n 46.924007100770275\n ]\n ]\n ]\n }\n }\n ]\n}","publicComments":"Rocky Reach Hydroelectric Project FERC Project No. 2145","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5774f2a9e4b07dd077c6a7f6","contributors":{"authors":[{"text":"Chelan County PUD","contributorId":172566,"corporation":true,"usgs":false,"organization":"Chelan County PUD","id":641279,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Rocky Reach Fish Forum","contributorId":172567,"corporation":true,"usgs":false,"organization":"Rocky Reach Fish Forum","id":641280,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"U.S. Fish and Wildlife Service","contributorId":128143,"corporation":true,"usgs":false,"organization":"U.S. Fish and Wildlife Service","id":641281,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"United States Geological Survey","contributorId":128013,"corporation":true,"usgs":false,"organization":"United States Geological Survey","id":641282,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"GeoEngineers","contributorId":172568,"corporation":true,"usgs":false,"organization":"GeoEngineers","id":641283,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}} ,{"id":70004633,"text":"fs20113050 - 2011 - Assessment of undiscovered oil and gas resources of the West Siberian Basin Province, Russia, 2010","interactions":[{"subject":{"id":86120,"text":"fs20083064 - 2008 - Assessment of undiscovered oil and gas resources of the West Siberian Basin Province, Russia, 2008","indexId":"fs20083064","publicationYear":"2008","noYear":false,"title":"Assessment of undiscovered oil and gas resources of the West Siberian Basin Province, Russia, 2008"},"predicate":"SUPERSEDED_BY","object":{"id":70004633,"text":"fs20113050 - 2011 - Assessment of undiscovered oil and gas resources of the West Siberian Basin Province, Russia, 2010","indexId":"fs20113050","publicationYear":"2011","noYear":false,"title":"Assessment of undiscovered oil and gas resources of the West Siberian Basin Province, Russia, 2010"},"id":1}],"lastModifiedDate":"2012-02-10T00:11:58","indexId":"fs20113050","displayToPublicDate":"2011-06-15T13:50:03","publicationYear":"2011","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":"2011-3050","title":"Assessment of undiscovered oil and gas resources of the West Siberian Basin Province, Russia, 2010","docAbstract":"The U.S. Geological Survey, using a geology-based assessment methodology, estimated mean volumes of technically recoverable, conventional, undiscovered petroleum resources at 8 billion barrels of crude oil, 670 trillion cubic feet of natural gas, and 21 billion barrels of natural gas liquids for the West Siberian Basin Province in Russia as part of a program to estimate petroleum resources for priority basins throughout the world.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/fs20113050","collaboration":"World Petroleum Resources Project","usgsCitation":"Klett, T., 2011, Assessment of undiscovered oil and gas resources of the West Siberian Basin Province, Russia, 2010: U.S. Geological Survey Fact Sheet 2011-3050, 2 p., https://doi.org/10.3133/fs20113050.","productDescription":"2 p.","startPage":"1","endPage":"2","numberOfPages":"2","costCenters":[{"id":164,"text":"Central Energy Resources Science Center","active":true,"usgs":true}],"links":[{"id":116135,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/fs_2011_3050.gif"},{"id":21885,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/fs/2011/3050/","linkFileType":{"id":5,"text":"html"}}],"country":"Russia","otherGeospatial":"West Siberian Basin Province","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ 45,50 ], [ 45,70 ], [ 90,70 ], [ 90,50 ], [ 45,50 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4acfe4b07f02db680357","contributors":{"authors":[{"text":"Klett, T. R. 0000-0001-9779-1168","orcid":"https://orcid.org/0000-0001-9779-1168","contributorId":83067,"corporation":false,"usgs":true,"family":"Klett","given":"T. R.","affiliations":[],"preferred":false,"id":350907,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70004634,"text":"fs20113051 - 2011 - Assessment of undiscovered oil and gas resources of the Dnieper-Donets Basin Province and Pripyat Basin Province, Russia, Ukraine, and Belarus, 2010","interactions":[],"lastModifiedDate":"2012-02-10T00:11:58","indexId":"fs20113051","displayToPublicDate":"2011-06-15T13:50:03","publicationYear":"2011","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":"2011-3051","title":"Assessment of undiscovered oil and gas resources of the Dnieper-Donets Basin Province and Pripyat Basin Province, Russia, Ukraine, and Belarus, 2010","docAbstract":"The U.S. Geological Survey, using a geology-based assessment methodology, estimated mean volumes of technically recoverable, conventional, undiscovered petroleum resources at 84 million barrels of crude oil, 4.7 trillion cubic feet of natural gas, and 130 million barrels of natural gas liquids for the Dnieper-Donets Basin Province and 39 million barrels of crude oil, 48 billion cubic feet of natural gas, and 1 million barrels of natural gas liquids for the Pripyat Basin Province. The assessments are part of a program to estimate these resources for priority basins throughout the world.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/fs20113051","collaboration":"World Petroleum Resources Project","usgsCitation":"Klett, T., 2011, Assessment of undiscovered oil and gas resources of the Dnieper-Donets Basin Province and Pripyat Basin Province, Russia, Ukraine, and Belarus, 2010: U.S. Geological Survey Fact Sheet 2011-3051, 2 p., https://doi.org/10.3133/fs20113051.","productDescription":"2 p.","startPage":"1","endPage":"2","numberOfPages":"2","temporalStart":"2010-01-01","temporalEnd":"2010-12-31","costCenters":[{"id":164,"text":"Central Energy Resources Science Center","active":true,"usgs":true}],"links":[{"id":116136,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/fs_2011_3051.gif"},{"id":21878,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/fs/2011/3051/","linkFileType":{"id":5,"text":"html"}}],"country":"Russia;Ukraine;Belarus","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ 25,45 ], [ 25,55 ], [ 45,55 ], [ 45,45 ], [ 25,45 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aafe4b07f02db66cc2e","contributors":{"authors":[{"text":"Klett, T. 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R.","affiliations":[],"preferred":false,"id":350908,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70003976,"text":"70003976 - 2011 - A noninvasive, direct real-time PCR method for sex determination in multiple avian species","interactions":[],"lastModifiedDate":"2020-01-14T08:11:28","indexId":"70003976","displayToPublicDate":"2011-06-15T13:50:03","publicationYear":"2011","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2776,"text":"Molecular Ecology Resources","active":true,"publicationSubtype":{"id":10}},"title":"A noninvasive, direct real-time PCR method for sex determination in multiple avian species","docAbstract":"Polymerase chain reaction (PCR)-based methods to determine the sex of birds are well established and have seen few modifications since they were first introduced in the 1990s. Although these methods allowed for sex determination in species that were previously difficult to analyse, they were not conducive to high-throughput analysis because of the laboriousness of DNA extraction and gel electrophoresis. We developed a high-throughput real-time PCR-based method for analysis of sex in birds, which uses noninvasive sample collection and avoids DNA extraction and gel electrophoresis.","language":"English","publisher":"Wiley","doi":"10.1111/j.1755-0998.2010.02951.x","usgsCitation":"Brubaker, J.L., Karouna-Renier, N., Chen, Y., Jenko, K., Sprague, D.T., and Henry, P.F., 2011, A noninvasive, direct real-time PCR method for sex determination in multiple avian species: Molecular Ecology Resources, v. 11, no. 2, p. 415-417, https://doi.org/10.1111/j.1755-0998.2010.02951.x.","productDescription":"3 p.","startPage":"415","endPage":"417","numberOfPages":"3","costCenters":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true},{"id":34983,"text":"Contaminant Biology Program","active":true,"usgs":true}],"links":[{"id":203826,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"11","issue":"2","noUsgsAuthors":false,"publicationDate":"2010-12-12","publicationStatus":"PW","scienceBaseUri":"4f4e4b20e4b07f02db6ab99f","contributors":{"authors":[{"text":"Brubaker, Jessica L.","contributorId":49241,"corporation":false,"usgs":true,"family":"Brubaker","given":"Jessica","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":350004,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Karouna-Renier, Natalie K. 0000-0001-7127-033X","orcid":"https://orcid.org/0000-0001-7127-033X","contributorId":17357,"corporation":false,"usgs":true,"family":"Karouna-Renier","given":"Natalie K.","affiliations":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"preferred":false,"id":350002,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Chen, Yu","contributorId":77785,"corporation":false,"usgs":true,"family":"Chen","given":"Yu","email":"","affiliations":[],"preferred":false,"id":350005,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Jenko, Kathryn","contributorId":6720,"corporation":false,"usgs":true,"family":"Jenko","given":"Kathryn","email":"","affiliations":[],"preferred":false,"id":350000,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Sprague, Daniel T.","contributorId":43219,"corporation":false,"usgs":true,"family":"Sprague","given":"Daniel","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":350003,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Henry, Paula F.P.","contributorId":12311,"corporation":false,"usgs":true,"family":"Henry","given":"Paula","email":"","middleInitial":"F.P.","affiliations":[],"preferred":false,"id":350001,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}} ,{"id":70004636,"text":"ds598 - 2011 - Groundwater quality of the Gulf Coast aquifer system, Houston, Texas, 2010","interactions":[],"lastModifiedDate":"2016-08-11T15:30:40","indexId":"ds598","displayToPublicDate":"2011-06-15T13:50:03","publicationYear":"2011","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":"598","title":"Groundwater quality of the Gulf Coast aquifer system, Houston, Texas, 2010","docAbstract":"During March–December 2010, the U.S. Geological Survey, in cooperation with the city of Houston, collected source-water samples from 60 municipal supply wells in the Houston area. These data were collected as part of an ongoing study to determine concentrations, spatial extent, and associated geochemical conditions that might be conducive for mobility and transport of selected naturally occurring contaminants (selected trace elements and radionuclides) in the Gulf Coast aquifer system in the Houston area. In the summers of 2007 and 2008, a reconnaissance-level survey of these constituents in untreated water from 28 municipal supply wells was completed in the Houston area. Included in this report are the complete analytical results for 47 of the 60 samples collected in 2010—those results which were received from the laboratories and reviewed by the authors as of December 31, 2010. All of the wells sampled were screened in the Gulf Coast aquifer system; 22 were screened entirely in the Evangeline aquifer, and the remaining 25 wells contained screened intervals that intersected both Evangeline and Chicot aquifers. The data documented in this report were collected as part of an ongoing study to characterize source-water-quality conditions in untreated groundwater prior to drinking-water treatment. An evaluation of contaminant occurrence in source water provides background information regarding the presence of a contaminant in the environment. Because source-water samples were collected prior to any treatment or blending that potentially could alter contaminant concentrations, the water-quality results documented by this report represent the quality of the source water, not the quality of finished drinking water provided to the public.
\nSamples were analyzed for major ions (calcium, magnesium, potassium, sodium, bromide, chloride, fluoride, silica, and sulfate), residue on evaporation (dissolved solids), trace elements (arsenic, barium, boron, chromium, iron, lithium, manganese, molybdenum, selenium, strontium, and vanadium), and selected radionuclides (gross alpha- and beta-particle activity [at 72 hours and 30 days], carbon-14, radium-226, radon-222, and uranium). Field measurements were made of selected physicochemical (relating to both physical and chemical) properties (oxidation-reduction potential, turbidity, dissolved-oxygen concentration, pH, specific conductance, water temperature, and alkalinity) and unfiltered sulfides.
\nSimilar to the results from the reconnaissance survey, physicochemical properties, major ions, and trace elements varied considerably. The ranges of selected physicochemical properties were as follows: oxidation-reduction potential ranged from -173 to 466 millivolts, dissolved oxygen ranged from less than 0.1 to 4.4 milligrams per liter, pH ranged from 7.2 to 7.8, specific conductance ranged from 439 to 724 microsiemens per centimeter at 25 degrees Celsius, and alkalinity ranged from 159 to 276 milligrams per liter as calcium carbonate. The largest ranges in concentration for filtered major ion constituents were obtained for cations sodium and calcium and for anions chloride and sulfate. Arsenic concentrations measured in samples from the 47 wells ranged from 1.6 to 23.5 micrograms per liter. The maximum concentration of arsenic (23.5 micrograms per liter) was measured in the source-water sample from well LJ-65-12-328.
\nQuantifiable concentrations of barium, boron, lithium, molybdenum, and strontium were measured in all 47 filtered, source-water samples. Quantifiable concentrations of manganese were measured in 46 source-water samples, and an estimated concentration of manganese was measured in 1 sample. Chromium, iron, selenium, and vanadium were detected in 24 or more of the 47 source-water samples.
\nGross alpha-particle activities and beta-particle activities for all 47 samples were analyzed at 72 hours after sample collection and again at 30 days after sample collection, allowing for the measurement of the activity of short-lived isotopes. Gross alpha-particle activities reported in this report were not adjusted for activity contributions by radon or uranium and, therefore, are conservatively high estimates if compared to the U.S. Environmental Protection Agency National Primary Drinking Water Regulation for adjusted gross alpha-particle activity. The gross alpha-particle activities at 30 days in the samples ranged from R0.60 to 25.5 picocuries per liter and at 72 hours ranged from 2.58 to 39.7 picocuries per liter, and the \"R\" preceding the value of 0.60 picocuries per liter refers to a nondetected result less than the sample-specific critical level. Gross beta-particle activities measured at 30 days ranged from 1.17 to 14.4 picocuries per liter and at 72 hours ranged from 1.97 to 4.4 picocuries per liter. Filtered uranium was detected in quantifiable amounts in all of the 47 wells sampled. The uranium concentrations ranged from 0.03 to 42.7 micrograms per liter. One sample was analyzed for carbon-14, and the amount of modern atmospheric carbon was reported as 0.2 percent. Six source-water samples collected from municipal supply wells were analyzed for radium-226, and all of the concentrations were considered detectable concentrations (greater than their associated sample-specific critical level). Three source-water samples collected were analyzed for radon-222, and all of the concentrations were substantially greater than the associated sample-specific critical level.
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2011 - The Global Seismographic Network","interactions":[],"lastModifiedDate":"2012-02-10T00:11:58","indexId":"fs20113021","displayToPublicDate":"2011-06-15T13:50:02","publicationYear":"2011","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":"2011-3021","title":"The Global Seismographic Network","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/fs20113021","usgsCitation":"Gee, L., and Leith, W.S., 2011, The Global Seismographic Network: U.S. Geological Survey Fact Sheet 2011-3021, 2 p., https://doi.org/10.3133/fs20113021.","productDescription":"2 p.","startPage":"1","endPage":"2","numberOfPages":"2","costCenters":[{"id":301,"text":"Geologic Hazards Team","active":false,"usgs":true}],"links":[{"id":116132,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/fs_2011_3021.png"},{"id":21877,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/fs/2011/3021/","linkFileType":{"id":5,"text":"html"}}],"geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ 180,-90 ], [ 180,90 ], [ -180,90 ], [ -180,-90 ], [ 180,-90 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac9e4b07f02db67c49f","contributors":{"authors":[{"text":"Gee, Lind S. lgee@usgs.gov","contributorId":2247,"corporation":false,"usgs":true,"family":"Gee","given":"Lind S.","email":"lgee@usgs.gov","affiliations":[{"id":300,"text":"Geologic Hazards Science Center","active":true,"usgs":true}],"preferred":false,"id":350905,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Leith, William S. 0000-0002-3463-3119 wleith@usgs.gov","orcid":"https://orcid.org/0000-0002-3463-3119","contributorId":2248,"corporation":false,"usgs":true,"family":"Leith","given":"William","email":"wleith@usgs.gov","middleInitial":"S.","affiliations":[{"id":234,"text":"Earthquake Hazards Program","active":true,"usgs":true},{"id":300,"text":"Geologic Hazards Science Center","active":true,"usgs":true}],"preferred":true,"id":350906,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70004635,"text":"fs20113052 - 2011 - Assessment of undiscovered oil and gas resources of the Azov-Kuban Basin Province, Ukraine and Russia, 2010","interactions":[],"lastModifiedDate":"2012-02-10T00:11:58","indexId":"fs20113052","displayToPublicDate":"2011-06-15T13:50:02","publicationYear":"2011","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":"2011-3052","title":"Assessment of undiscovered oil and gas resources of the Azov-Kuban Basin Province, Ukraine and Russia, 2010","docAbstract":"The U.S. Geological Survey, using a geology-based assessment methodology, estimated mean volumes of technically recoverable, conventional, undiscovered petroleum resources at 218 million barrels of crude oil, 4.1 trillion cubic feet of natural gas, and 94 million barrels of natural gas liquids for the Azov-Kuban Basin Province as part of a program to estimate petroleum resources for priority basins throughout the world.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/fs20113052","collaboration":"World Petroleum Resources Project","usgsCitation":"Klett, T., 2011, Assessment of undiscovered oil and gas resources of the Azov-Kuban Basin Province, Ukraine and Russia, 2010: U.S. Geological Survey Fact Sheet 2011-3052, 2 p., https://doi.org/10.3133/fs20113052.","productDescription":"2 p.","startPage":"1","endPage":"2","numberOfPages":"2","temporalStart":"2010-01-01","temporalEnd":"2010-12-31","costCenters":[{"id":164,"text":"Central Energy Resources Science Center","active":true,"usgs":true}],"links":[{"id":116133,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/fs_2011_3052.gif"},{"id":21879,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/fs/2011/3052/","linkFileType":{"id":5,"text":"html"}}],"country":"Ukraine;Russia","otherGeospatial":"Azov-kuban Basin Province","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ 35,40 ], [ 35,50 ], [ 45,50 ], [ 45,40 ], [ 35,40 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aa9e4b07f02db667f56","contributors":{"authors":[{"text":"Klett, T. 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The study area hosts the world-class Pebble porphyry Cu-Au-Mo deposit, and through collaboration with the Pebble Limited Partnership, a range of geophysical and geochemical investigations was carried out in proximity to the deposit. The deposit is almost entirely concealed by tundra, glacial deposits, and post-mineralization volcanic rocks. The discovery of mineral resources beneath cover is becoming more important because most of the mineral resources at the surface have already been discovered. Research is needed to identify ways in which to assess for concealed mineral resources. This report presents the uninterpreted geophysical measurements and geochemical and mineralogical analytical data from samples collected during the summer field seasons from 2007 to 2010, and makes the data available in a single Geographic Information System (GIS) database.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ds608","usgsCitation":"Anderson, E., Smith, S.M., Giles, S.A., Granitto, M., Eppinger, R., Bedrosian, P.A., Shah, A., Kelley, K., Fey, D., Minsley, B., and Brown, P., 2011, Geophysical, geochemical, and mineralogical data from the Pebble Cu-Au-Mo porphyry deposit area, southwest Alaska: Contributions to assessment techniques for concealed mineral resources: U.S. Geological Survey Data Series 608, viii, 43 p., https://doi.org/10.3133/ds608.","productDescription":"viii, 43 p.","numberOfPages":"54","costCenters":[{"id":211,"text":"Crustal Geophysics and Geochemistry Science Center","active":true,"usgs":true}],"links":[{"id":116199,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ds_608.jpg"},{"id":388809,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_95238.htm"},{"id":21875,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/ds/608/","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Alaska","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -156.5,\n 60.5444\n ],\n [\n -154.5833,\n 60.5444\n ],\n [\n -154.5833,\n 59.6167\n ],\n [\n -156.5,\n 59.6167\n ],\n [\n -156.5,\n 60.5444\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac8e4b07f02db67c28d","contributors":{"authors":[{"text":"Anderson, E. 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Collectively, surface water temperature ranged from a mean of ~22 C in May to 28 C in July, and individual summer maxima typically were 28–32 C. Most (~95%) reservoirs stably stratify by mid-May, but few are deep enough to have hypolimnia with near-uniform temperatures. Among stratified reservoirs, maximum effective length and maximum depth accounted for 75% of the variation in mixed depth and thermocline depth. Ephemeral, near-surface thermoclines occurred in 39% of summer profiles and were most frequent in small, turbid reservoirs. Isotherms below the mixed layer deepen during stratification, and the water column is >20 C by August in all but the deepest reservoirs. Most reservoirs showed incipient dissolved oxygen (DO) depletion by mid-May, and by August, 80% of profiles had DO minima of <1 mg/L. Surface area and chlorophyll (Chl) explained 37% of variation in the earliest date of anoxia, and Chl explained >50% of variation in DO below the mixed layer during summer. Warm summer temperatures and widespread low DO often limit available fish habitat in Missouri reservoirs and compress warm-water fish communities into subsurface layers that exceed their thermal preferences. This study provides a regional baseline of reservoir temperature and oxygen conditions useful for future evaluations of eutrophication and the effects of a warming climate.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Lake and Reservoir Management","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"Taylor & Francis","publisherLocation":"London, UK","doi":"10.1080/07438141.2011.583713","usgsCitation":"Jones, J., Knowlton, M.F., Obrecht, D.V., and Graham, J.L., 2011, Temperature and oxygen in Missouri reservoirs: Lake and Reservoir Management, v. 27, no. 2, p. 173-182, https://doi.org/10.1080/07438141.2011.583713.","productDescription":"10 p.","startPage":"173","endPage":"182","numberOfPages":"10","ipdsId":"IP-014524","costCenters":[{"id":353,"text":"Kansas Water Science Center","active":false,"usgs":true}],"links":[{"id":268644,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":268640,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1080/07438141.2011.583713"}],"country":"United States","state":"Missouri","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -95.7747,35.9957 ], [ -95.7747,40.6136 ], [ -89.0995,40.6136 ], [ -89.0995,35.9957 ], [ -95.7747,35.9957 ] ] ] } } ] }","volume":"27","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5131dc12e4b0140546f53c3e","contributors":{"authors":[{"text":"Jones, John R.","contributorId":48459,"corporation":false,"usgs":false,"family":"Jones","given":"John R.","affiliations":[{"id":6754,"text":"University of Missouri","active":true,"usgs":false}],"preferred":false,"id":473557,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Knowlton, Matthew F.","contributorId":83810,"corporation":false,"usgs":true,"family":"Knowlton","given":"Matthew","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":473559,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Obrecht, Daniel V.","contributorId":65352,"corporation":false,"usgs":true,"family":"Obrecht","given":"Daniel","email":"","middleInitial":"V.","affiliations":[],"preferred":false,"id":473558,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Graham, Jennifer L. 0000-0002-6420-9335 jlgraham@usgs.gov","orcid":"https://orcid.org/0000-0002-6420-9335","contributorId":1769,"corporation":false,"usgs":true,"family":"Graham","given":"Jennifer","email":"jlgraham@usgs.gov","middleInitial":"L.","affiliations":[{"id":474,"text":"New York Water Science Center","active":true,"usgs":true}],"preferred":true,"id":473556,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":70189056,"text":"70189056 - 2011 - Aqueous mineralogy and stratigraphy at and around the proposed Mawrth Vallis MSL Landing Site: New insights into the aqueous history of the region","interactions":[],"lastModifiedDate":"2017-06-30T09:31:08","indexId":"70189056","displayToPublicDate":"2011-06-15T00:00:00","publicationYear":"2011","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2686,"text":"Mars, The International Journal of Mars Science and Exploration","active":true,"publicationSubtype":{"id":10}},"title":"Aqueous mineralogy and stratigraphy at and around the proposed Mawrth Vallis MSL Landing Site: New insights into the aqueous history of the region","docAbstract":"In this work, we have confirmed the mineralogical stratigraphy previously inferred by other authors, but also demonstrate the presence of additional minerals, including a possible acid-leaching product near the top of the sequence, an Mh-OH bearing phyllosilicate at the to of the sequence, and potentially a Ca-sulfate at the bottom of the phyllosilicate sequence. The latter has important implications regarding the relative timing of sulfate vs clay formation on Mars.
","language":"English","publisher":"U.S. Jet Propulsion Laboratory","usgsCitation":"Dobrea, E.Z., Michalski, J., and Swayze, G., 2011, Aqueous mineralogy and stratigraphy at and around the proposed Mawrth Vallis MSL Landing Site: New insights into the aqueous history of the region: Mars, The International Journal of Mars Science and Exploration, v. 6, p. 32-46.","productDescription":"15 p.","startPage":"32","endPage":"46","ipdsId":"IP-027291","costCenters":[{"id":211,"text":"Crustal Geophysics and Geochemistry Science Center","active":true,"usgs":true}],"links":[{"id":343210,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":343209,"rank":1,"type":{"id":15,"text":"Index Page"},"url":"https://www.marsjournal.org/contents/2011/0003/"}],"otherGeospatial":"Mars, Mawrth Vallis","volume":"6","publishingServiceCenter":{"id":2,"text":"Denver PSC"},"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5957633ae4b0d1f9f051b565","contributors":{"authors":[{"text":"Dobrea, Eldar Z. Noe","contributorId":194044,"corporation":false,"usgs":false,"family":"Dobrea","given":"Eldar","email":"","middleInitial":"Z. Noe","affiliations":[],"preferred":false,"id":702997,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Michalski, Joseph","contributorId":194045,"corporation":false,"usgs":false,"family":"Michalski","given":"Joseph","email":"","affiliations":[],"preferred":false,"id":702998,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Swayze, Gregg 0000-0002-1814-7823","orcid":"https://orcid.org/0000-0002-1814-7823","contributorId":12092,"corporation":false,"usgs":true,"family":"Swayze","given":"Gregg","affiliations":[],"preferred":false,"id":702999,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":70173651,"text":"70173651 - 2011 - Shrimp trawlers as a local attractor of seabirds in nearshore waters of South Carolina, USA","interactions":[],"lastModifiedDate":"2016-06-07T15:16:16","indexId":"70173651","displayToPublicDate":"2011-06-15T00:00:00","publicationYear":"2011","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2660,"text":"Marine Biology","active":true,"publicationSubtype":{"id":10}},"title":"Shrimp trawlers as a local attractor of seabirds in nearshore waters of South Carolina, USA","docAbstract":"Shrimp trawling is common throughout the southeastern and Gulf of Mexico coasts of the USA and is the primary contributor to fisheries discards in these regions. Tens of thousands of nearshore seabirds nest near shrimp trawling grounds in the USA, but to date, there has been no assessment of the relationship between seabirds and shrimp trawlers. We examined the taxonomic composition of bycatch, rate at which seabirds scavenged bycatch, and energy density of discarded bycatch in a nearshore commercial shrimp fishery. Bycatch was primarily comprised of demersal fish that are not typically accessible to the plunge-diving and surface-feeding seabirds that occur in the area. Hence, seabird diets in the region appear to be broadened taxonomically by the availability of discards. Results from discard experiments indicated that 70% of the nearly 5,500 items discarded by hand were scavenged by seabirds and that the fate of a discarded item was most strongly predicted by its taxonomic order. Laughing gulls scavenged the greatest proportion of discards, although brown pelicans were the only species to scavenge more discards than predicted based upon their abundance. Because this is the first such study in the region, it is difficult to ascertain the extent or intensity of the impact that discards have on nearshore seabirds. Nonetheless, our results suggest that it will be difficult for managers to clearly understand fluctuations in local seabird population dynamics without first understanding the extent to which these species rely upon discards. This may be especially problematic in situations where seabird populations are recovering following natural or anthropogenic stressors.
","language":"English","publisher":"Springer-Verlag","doi":"10.1007/s00227-011-1733-4","usgsCitation":"Jodice, P.G., Wickliffe, L.C., and Sachs, E.B., 2011, Shrimp trawlers as a local attractor of seabirds in nearshore waters of South Carolina, USA: Marine Biology, v. 158, p. 2289-2298, https://doi.org/10.1007/s00227-011-1733-4.","productDescription":"10 p.","startPage":"2289","endPage":"2298","onlineOnly":"N","additionalOnlineFiles":"N","ipdsId":"IP-013184","costCenters":[{"id":198,"text":"Coop Res Unit Atlanta","active":true,"usgs":true}],"links":[{"id":323197,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"South Carolina","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -79.19769287109375,\n 33.169743600216165\n ],\n [\n -79.1180419921875,\n 33.09614359735857\n ],\n [\n -79.5849609375,\n 32.900344287496445\n ],\n [\n -79.73052978515625,\n 32.844981178306114\n ],\n [\n -79.62615966796875,\n 32.983324091837474\n ],\n [\n -79.310302734375,\n 33.16284622181141\n ],\n [\n -79.2169189453125,\n 33.18123802491263\n ],\n [\n -79.19769287109375,\n 33.169743600216165\n ]\n ]\n ]\n }\n },\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -79.7552490234375,\n 32.8334428466495\n ],\n [\n -79.69757080078124,\n 32.81959486923976\n ],\n [\n -79.68109130859375,\n 32.7572522610541\n ],\n [\n -79.81292724609375,\n 32.535236240827224\n ],\n [\n -80.10543823242188,\n 32.6093028087336\n ],\n [\n -79.95437622070312,\n 32.7872745269555\n ],\n [\n -79.78271484375,\n 32.84382741262935\n ],\n [\n -79.7552490234375,\n 32.8334428466495\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"158","publishingServiceCenter":{"id":8,"text":"Raleigh PSC"},"noUsgsAuthors":false,"publicationDate":"2011-06-15","publicationStatus":"PW","scienceBaseUri":"5757f064e4b04f417c24dd19","contributors":{"authors":[{"text":"Jodice, Patrick G.R. 0000-0001-8716-120X pjodice@usgs.gov","orcid":"https://orcid.org/0000-0001-8716-120X","contributorId":1119,"corporation":false,"usgs":true,"family":"Jodice","given":"Patrick","email":"pjodice@usgs.gov","middleInitial":"G.R.","affiliations":[{"id":198,"text":"Coop Res Unit Atlanta","active":true,"usgs":true}],"preferred":false,"id":637592,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Wickliffe, Lisa C.","contributorId":171480,"corporation":false,"usgs":false,"family":"Wickliffe","given":"Lisa","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":637593,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Sachs, Elena B.","contributorId":171481,"corporation":false,"usgs":false,"family":"Sachs","given":"Elena","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":637594,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":70189064,"text":"70189064 - 2011 - Mine wastes and human health","interactions":[],"lastModifiedDate":"2017-06-30T09:16:14","indexId":"70189064","displayToPublicDate":"2011-06-15T00:00:00","publicationYear":"2011","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1490,"text":"Elements","active":true,"publicationSubtype":{"id":10}},"title":"Mine wastes and human health","docAbstract":"Historical mining and mineral processing have been linked definitively to health problems resulting from occupational and environmental exposures to mine wastes. Modern mining and processing methods, when properly designed and implemented, prevent or greatly reduce potential environmental health impacts. However, particularly in developing countries, there are examples of health problems linked to recent mining. In other cases, recent mining has been blamed for health problems but no clear links have been found. The types and abundances of potential toxicants in mine wastes are predictably influenced by the geologic characteristics of the deposit being mined. Hence, Earth scientists can help understand, anticipate, and mitigate potential health issues associated with mining and mineral processing.
","language":"English","publisher":"Mineralogical Society of America","doi":"10.2113/gselements.7.6.399","usgsCitation":"Plumlee, G.S., and Morman, S.A., 2011, Mine wastes and human health: Elements, v. 7, no. 6, p. 399-404, https://doi.org/10.2113/gselements.7.6.399.","productDescription":"6 p.","startPage":"399","endPage":"404","ipdsId":"IP-030587","costCenters":[{"id":211,"text":"Crustal Geophysics and Geochemistry Science Center","active":true,"usgs":true}],"links":[{"id":343206,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"7","issue":"6","publishingServiceCenter":{"id":2,"text":"Denver PSC"},"noUsgsAuthors":false,"publicationDate":"2011-12-12","publicationStatus":"PW","scienceBaseUri":"5957633ae4b0d1f9f051b560","contributors":{"authors":[{"text":"Plumlee, Geoffrey S. 0000-0002-9607-5626 gplumlee@usgs.gov","orcid":"https://orcid.org/0000-0002-9607-5626","contributorId":960,"corporation":false,"usgs":true,"family":"Plumlee","given":"Geoffrey","email":"gplumlee@usgs.gov","middleInitial":"S.","affiliations":[{"id":211,"text":"Crustal Geophysics and Geochemistry Science Center","active":true,"usgs":true}],"preferred":true,"id":702710,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Morman, Suzette A. 0000-0002-2532-1033 smorman@usgs.gov","orcid":"https://orcid.org/0000-0002-2532-1033","contributorId":996,"corporation":false,"usgs":true,"family":"Morman","given":"Suzette","email":"smorman@usgs.gov","middleInitial":"A.","affiliations":[{"id":211,"text":"Crustal Geophysics and Geochemistry Science Center","active":true,"usgs":true},{"id":171,"text":"Central Mineral and Environmental Resources Science Center","active":true,"usgs":true}],"preferred":true,"id":702711,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70045766,"text":"tm1A1 - 2011 - Groundwater technical procedures of the U.S. Geological Survey","interactions":[],"lastModifiedDate":"2013-05-05T10:25:19","indexId":"tm1A1","displayToPublicDate":"2011-06-15T00:00:00","publicationYear":"2011","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":335,"text":"Techniques and Methods","code":"TM","onlineIssn":"2328-7055","printIssn":"2328-7047","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"1-A1","title":"Groundwater technical procedures of the U.S. Geological Survey","docAbstract":"A series of groundwater technical procedures documents (GWPDs) has been released by the U.S. Geological Survey, Water-Resources Discipline, for general use by the public. These technical procedures were written in response to the need for standardized technical procedures of many aspects of groundwater science, including site and measuring-point establishment, measurement of water levels, and measurement of well discharge. The techniques are described in the GWPDs in concise language and are accompanied by necessary figures and tables derived from cited manuals, reports, and other documents. Because a goal of this series of procedures is to remain current with the state of the science, and because procedures change over time, this report is released in an online format only. As new procedures are developed and released, they will be linked to this document.","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Section A: Groundwater Technical Procedures of the U.S. Geological Survey in Book 1 Collection of Water Data by Direct Measurement","largerWorkSubtype":{"id":5,"text":"USGS Numbered Series"},"language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/tm1A1","collaboration":"Office of Groundwater; This report is Chapter 1 of Section A: Groundwater Technical Procedures of the U.S. Geological Survey in Book 1 Collection of Water Data by Direct Measurement","usgsCitation":"Cunningham, W.L., and Schalk, C.W., 2011, Groundwater technical procedures of the U.S. Geological Survey: U.S. Geological Survey Techniques and Methods 1-A1, vi, 154 p., https://doi.org/10.3133/tm1A1.","productDescription":"vi, 154 p.","numberOfPages":"162","onlineOnly":"Y","additionalOnlineFiles":"N","costCenters":[{"id":494,"text":"Office of Groundwater","active":false,"usgs":true}],"links":[{"id":271793,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/tm1a1.jpg"},{"id":271791,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/tm/1a1/"},{"id":271792,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/tm/1a1/pdf/tm1-a1.pdf"}],"country":"United States","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5184dc62e4b04d6ec94d62ab","contributors":{"authors":[{"text":"Cunningham, William L. wcunning@usgs.gov","contributorId":1198,"corporation":false,"usgs":true,"family":"Cunningham","given":"William","email":"wcunning@usgs.gov","middleInitial":"L.","affiliations":[{"id":493,"text":"Office of Ground Water","active":true,"usgs":true}],"preferred":true,"id":478319,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Schalk, Charles W. cwschalk@usgs.gov","contributorId":1726,"corporation":false,"usgs":true,"family":"Schalk","given":"Charles","email":"cwschalk@usgs.gov","middleInitial":"W.","affiliations":[{"id":371,"text":"Maine Water Science Center","active":true,"usgs":true}],"preferred":true,"id":478320,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70004625,"text":"ofr20111147 - 2011 - Spawning migration movements of Lost River and shortnose suckers in the Williamson and Sprague Rivers, Oregon, following the removal of Chiloquin Dam-2009 Annual Report","interactions":[],"lastModifiedDate":"2012-02-02T00:15:52","indexId":"ofr20111147","displayToPublicDate":"2011-06-14T16:50:03","publicationYear":"2011","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":"2011-1147","title":"Spawning migration movements of Lost River and shortnose suckers in the Williamson and Sprague Rivers, Oregon, following the removal of Chiloquin Dam-2009 Annual Report","docAbstract":"The Chiloquin Dam was located at river kilometer (rkm) 1.3 on the Sprague River near the town of Chiloquin, Oregon. The dam was identified as a barrier that potentially inhibited or prevented the upstream spawning migrations and other movements of endangered Lost River suckers (Deltistes luxatus), shortnose suckers (Chasmistes brevirostris), and other fish in the Sprague River. Our research objectives in 2009 were to evaluate adult catostomid spawning migration patterns using radio telemetry to identify and describe shifts in spawning area distribution and migration behavior following the removal of Chiloquin Dam in 2008. We attached external radio transmitters to 58 Lost River suckers and 59 shortnose suckers captured at the Williamson River fish weir. A total of 17 radio-tagged Lost River suckers and one radio-tagged shortnose sucker were detected approaching the site of the former Chiloquin Dam but only two radio-tagged fish (one male Lost River sucker and one female Lost River sucker) were detected crossing upstream of the dam site. A lower proportion of radio-tagged shortnose suckers were detected migrating into the Sprague River when compared with previous years. Detections on remote passive integrated transponder (PIT) tag arrays located in the Sprague River show that although the proportion of fish coming into the Sprague River is small when compared to the number of fish crossing the Williamson River fish weir, the number of fish migrating upstream of the Chiloquin Dam site increased exponentially in the first year since its removal. These data will be used in conjunction with larval production and adult spawning distribution data to evaluate the effectiveness of dam removal in order to provide increased access to underutilized spawning habitat located further upstream in the Sprague River and to reduce the crowding of spawning fish below the dam site.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr20111147","usgsCitation":"Ellsworth, C.M., and VanderKooi, S., 2011, Spawning migration movements of Lost River and shortnose suckers in the Williamson and Sprague Rivers, Oregon, following the removal of Chiloquin Dam-2009 Annual Report: U.S. Geological Survey Open-File Report 2011-1147, iv, 13 p.; Figures; Tables, https://doi.org/10.3133/ofr20111147.","productDescription":"iv, 13 p.; Figures; Tables","startPage":"i","endPage":"20","numberOfPages":"24","temporalStart":"2009-01-01","temporalEnd":"2009-12-31","costCenters":[{"id":654,"text":"Western Fisheries Research Center","active":true,"usgs":true}],"links":[{"id":116619,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ofr_2011_1147.bmp"},{"id":21873,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2011/1147/","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Oregon","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a02e4b07f02db5f804c","contributors":{"authors":[{"text":"Ellsworth, Craig M.","contributorId":14913,"corporation":false,"usgs":true,"family":"Ellsworth","given":"Craig","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":350879,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"VanderKooi, Scott P.","contributorId":106584,"corporation":false,"usgs":true,"family":"VanderKooi","given":"Scott P.","affiliations":[],"preferred":false,"id":350880,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70043631,"text":"70043631 - 2011 - Project Planning for Cougar Dam during 2010","interactions":[],"lastModifiedDate":"2016-06-29T12:05:44","indexId":"70043631","displayToPublicDate":"2011-06-14T13:15:00","publicationYear":"2011","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":4,"text":"Other Government Series"},"title":"Project Planning for Cougar Dam during 2010","docAbstract":"Cougar Dam is a 158 m-tall, rock fill dam located about 63 km east of Springfield, Oregon. Completed in 1963, the dam is owned and operated by the U.S. Army Corps of Engineers (USACE). It impounds Cougar Reservoir, which is 9.7 km long, has a surface area of 518 ha, and is predominately used for flood control. The pool elevation typically ranges from a maximum conservation pool of 515 m (1,690 ft) National Geodetic Vertical Datum (NGVD) in summer to a minimum flood control elevation of 467 m (1,532 ft NGVD) in winter. The reservoir thermally stratifies in the summer, has an average depth of 37 m, and holds 153,500 acre-feet when full. Cougar Dam is located on the South Fork of the McKenzie River 7 km upstream from the mainstem McKenzie River, a tributary of the Willamette River. The McKenzie River Basin basin supports the largest remaining population of wild spawning spring Chinook salmon in the Willamette River Basin (National Oceanic and Atmospheric Administration; NOAA, 2008). Cougar Dam and others were collectively deemed to cause jeopardy to the sustainability of anadromous fish stocks in the Willamette River Basin (NOAA, 2008). Prior to dam construction, as many as 805 redds were observed in the South Fork of the McKenzie River (Willis and others, 1960) and it is estimated that 40 km of spawning habitat were lost when access was blocked after dam construction. The 2008 Willamette Biological Opinion (BIOP) requires improvements to operations and structures to reduce impacts on Upper Willamette River (UWR) Chinook salmon (Oncorhynchus tshawytscha) and UWR steelhead (O. mykiss; NOAA, 2008). In 2010, an adult fish collection facility was completed below Cougar Dam to collect returning adult salmon for transport to spawning habitats above the dam. Before that time, returning adult spring Chinook salmon were transported to upstream spawning areas as part of a trap-and-haul program with adults passed ranging annually from 0 to 1,038 (Taylor, 2000). The progeny of adult fish that are allowed to spawn above Cougar Dam move downstream into Cougar Reservoir in the spring. Under the BIOP, the USACE is required to provide downstream fish passage or operational alternatives at Cougar Dam by 2014. Currently, there is little information about the seasonal timing of reservoir entry of juvenile Chinook salmon and what habitats they and other fishes use in the reservoir. However, rotary screw traps placed in the outlet channel below the dam indicate peak juvenile passage coinciding with seasonally low pool elevation in mid December and late January. It is unknown whether juveniles upstream of Cougar Dam can be captured in large enough numbers for tagging and subsequent survival studies to proceed. These studies are needed to examine the feasibility of installing downstream fish passage structures at Cougar Dam to meet BIOP requirements. Therefore, the USACE contracted with the U.S. Geological Survey (USGS) to test the efficacy of using a mid-water trawl and lampara seine to capture fish in Cougar Reservoir on three consecutive days in the fall of 2010. These collection methods could potentially provide fish for feasibility and subsequent survival studies and as verification of fish targets in future active hydroacoustic surveys.
","publisher":"U.S. Army Corps of Engineers","publisherLocation":"Portland, OR","usgsCitation":"Haskell, C.A., and Tiffan, K.F., 2011, Project Planning for Cougar Dam during 2010, 11 p.","productDescription":"11 p.","numberOfPages":"11","onlineOnly":"N","additionalOnlineFiles":"N","ipdsId":"IP-027693","costCenters":[{"id":654,"text":"Western Fisheries Research Center","active":true,"usgs":true}],"links":[{"id":324612,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Oregon","otherGeospatial":"Cougar Dam","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -122.2464394569397,\n 44.129553925224954\n ],\n [\n -122.24654674530028,\n 44.126442717235136\n ],\n [\n -122.23665475845337,\n 44.12631949770353\n ],\n [\n -122.23663330078124,\n 44.13007757778364\n ],\n [\n -122.24107503890993,\n 44.130262395225316\n ],\n [\n -122.2463321685791,\n 44.130262395225316\n ],\n [\n -122.2464394569397,\n 44.129553925224954\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5774f2b6e4b07dd077c6a904","contributors":{"authors":[{"text":"Haskell, Craig A. 0000-0002-3604-1758 chaskell@usgs.gov","orcid":"https://orcid.org/0000-0002-3604-1758","contributorId":3458,"corporation":false,"usgs":true,"family":"Haskell","given":"Craig","email":"chaskell@usgs.gov","middleInitial":"A.","affiliations":[{"id":654,"text":"Western Fisheries Research Center","active":true,"usgs":true}],"preferred":true,"id":625585,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Tiffan, Kenneth F. 0000-0002-5831-2846 ktiffan@usgs.gov","orcid":"https://orcid.org/0000-0002-5831-2846","contributorId":3200,"corporation":false,"usgs":true,"family":"Tiffan","given":"Kenneth","email":"ktiffan@usgs.gov","middleInitial":"F.","affiliations":[{"id":654,"text":"Western Fisheries Research Center","active":true,"usgs":true}],"preferred":true,"id":625586,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70004620,"text":"sir20115017 - 2011 - Arsenic, metals, and nutrients in runoff from two detention basins to Raccoon Creek, New Jersey Coastal Plain, 2008","interactions":[],"lastModifiedDate":"2012-03-08T17:16:41","indexId":"sir20115017","displayToPublicDate":"2011-06-14T10:50:03","publicationYear":"2011","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":"2011-5017","title":"Arsenic, metals, and nutrients in runoff from two detention basins to Raccoon Creek, New Jersey Coastal Plain, 2008","docAbstract":"Arsenic (As) concentrations in the waters of Raccoon Creek in southern New Jersey commonly exceed the State\\'s Surface Water Quality Standard (SWQS) for freshwater of 0.017 microgram per liter (mu or ug/L). In order to assess contributions of As from residential runoff to the creek, samples of runoff water were collected from a detention basin in each of two residential developments underlain by different geologic formations and at the outlets of those basins. Samples of streamwater also were collected from Raccoon Creek adjacent to the developments. The samples were analyzed to determine concentrations of As, selected metals, organic carbon, and nutrients. Soil samples in and downgradient from the basins also were collected and analyzed.\n\nConcentrations of As in unfiltered water samples of runoff from the basin underlain by glauconitic clays generally were higher (up to 4.35 mu or ug/L) than in runoff from the basin underlain by predominantly quartz sands and silts (up to 2.68 mu or ug/L). Chromium (Cr) concentrations also were higher in runoff from the basin underlain by glauconitic clays than in runoff from the basin underlain by quartz sand and silt. In addition, Cr concentrations were higher in the glauconitic soils than in the quartz-rich soils.\n\nMetals such as aluminum (Al), iron (Fe), lead (Pb), and manganese (Mn) in the runoff and in the streamwater were mostly in particulate form. Arsenic, most metals, and phosphorus (P) however, were mostly in dissolved form in runoff but in particulate form in the streamwater. Total organic carbon concentrations in the runoff ranged from about 10 to nearly 16 milligrams per liter (mg/L). Given such levels of organic carbon and strong correlations between concentrations of some metals and organic carbon, it may be that many of the metals were complexed with dissolved organic carbon and transported in that form in the runoff.\n\nAlthough underlying geologic materials and soils appear to be major contributors of As to the streamwater, As also could have been contributed from lead arsenate pesticide residues. The residential development underlain by quartz-rich sediments formerly had been an orchard where such pesticides may have been used. The substantial inputs of As to runoff at this site may be attributable to this former land use, although Pb concentrations were about the same in runoff from both sites. The streamwater at both sites, however, contained Pb concentrations well above those in runoff, indicating that there are additional inputs of Pb, perhaps from roadside soils, upstream from the two sampling sites in this study.\n\nPositive relations between concentrations of As and some metals with dissolved organic carbon in runoff and streamwater indicate that complexation with organic carbon may provide a mechanism by which these constituents can be transported. Sorption of As, Pb, and P to Fe hydroxides may be indicated by the observed positive relation of particulate As, Pb, and P to particulate Fe, however, representing an additional mechanism for transport of these constituents.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/sir20115017","usgsCitation":"Barringer, J., Szabo, Z., Bonin, J., and McGee, C.K., 2011, Arsenic, metals, and nutrients in runoff from two detention basins to Raccoon Creek, New Jersey Coastal Plain, 2008: U.S. Geological Survey Scientific Investigations Report 2011-5017, vi, 21 p.; Appendices, https://doi.org/10.3133/sir20115017.","productDescription":"vi, 21 p.; Appendices","startPage":"i","endPage":"28","numberOfPages":"32","temporalStart":"2008-05-01","temporalEnd":"2008-09-30","costCenters":[{"id":470,"text":"New Jersey Water Science Center","active":true,"usgs":true}],"links":[{"id":116618,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/sir_2011_5017.jpg"},{"id":21872,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/sir/2011/5017/","linkFileType":{"id":5,"text":"html"}}],"scale":"24000","projection":"Universal Transverse Mercator projection","country":"United States","state":"New Jersey","county":"Gloucester","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -75.41666666666667,39.666666666666664 ], [ -75.41666666666667,39.833333333333336 ], [ -75.13333333333334,39.833333333333336 ], [ -75.13333333333334,39.666666666666664 ], [ -75.41666666666667,39.666666666666664 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4abbe4b07f02db672c3a","contributors":{"authors":[{"text":"Barringer, Julia L.","contributorId":59419,"corporation":false,"usgs":true,"family":"Barringer","given":"Julia L.","affiliations":[],"preferred":false,"id":350872,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Szabo, Zoltan 0000-0002-0760-9607 zszabo@usgs.gov","orcid":"https://orcid.org/0000-0002-0760-9607","contributorId":2240,"corporation":false,"usgs":true,"family":"Szabo","given":"Zoltan","email":"zszabo@usgs.gov","affiliations":[{"id":451,"text":"National Water Quality Assessment Program","active":true,"usgs":true}],"preferred":false,"id":350869,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Bonin, Jennifer L. 0000-0002-7631-9734","orcid":"https://orcid.org/0000-0002-7631-9734","contributorId":59404,"corporation":false,"usgs":true,"family":"Bonin","given":"Jennifer L.","affiliations":[],"preferred":false,"id":350871,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"McGee, Craig K.","contributorId":56772,"corporation":false,"usgs":true,"family":"McGee","given":"Craig","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":350870,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":70156398,"text":"70156398 - 2011 - A two-phase debris-flow model that includes coupled evolution of volume fractions, granular dilatancy, and pore-fluid pressure","interactions":[],"lastModifiedDate":"2015-08-20T15:16:59","indexId":"70156398","displayToPublicDate":"2011-06-14T00:00:00","publicationYear":"2011","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"A two-phase debris-flow model that includes coupled evolution of volume fractions, granular dilatancy, and pore-fluid pressure","docAbstract":"Pore-fluid pressure plays a crucial role in debris flows because it counteracts normal stresses at grain contacts and thereby reduces intergranular friction. Pore-pressure feedback accompanying debris deformation is particularly important during the onset of debrisflow motion, when it can dramatically influence the balance of forces governing downslope acceleration. We consider further effects of this feedback by formulating a new, depth-averaged mathematical model that simulates coupled evolution of granular dilatancy, solid and fluid volume fractions, pore-fluid pressure, and flow depth and velocity during all stages of debris-flow motion. To illustrate implications of the model, we use a finite-volume method to compute one-dimensional motion of a debris flow descending a rigid, uniformly inclined slope, and we compare model predictions with data obtained in large-scale experiments at the USGS debris-flow flume. Predictions for the first 1 s of motion show that increasing pore pressures (due to debris contraction) cause liquefaction that enhances flow acceleration. As acceleration continues, however, debris dilation causes dissipation of pore pressures, and this dissipation helps stabilize debris-flow motion. Our numerical predictions of this process match experimental data reasonably well, but predictions might be improved by accounting for the effects of grain-size segregation.
","largerWorkType":{"id":24,"text":"Conference Paper"},"largerWorkTitle":"Debris-flow hazards : mitigation, mechanics, prediction, and assessment : proceedings of 5th international conference : Padua, Italy, 14-17 June 2011","conferenceTitle":"Debris-flow hazards : mitigation, mechanics, prediction, and assessment : proceedings of 5th international conference : Padua, Italy, 14-17 June 2011","conferenceDate":"June 14-17, 2011","conferenceLocation":"Padua, Italy","language":"English","publisher":"Università La Sapienza","publisherLocation":"Padua, Italy","usgsCitation":"George, D., and Iverson, R.M., 2011, A two-phase debris-flow model that includes coupled evolution of volume fractions, granular dilatancy, and pore-fluid pressure, in Debris-flow hazards : mitigation, mechanics, prediction, and assessment : proceedings of 5th international conference : Padua, Italy, 14-17 June 2011, Padua, Italy, June 14-17, 2011, 10 p.","productDescription":"10 p.","numberOfPages":"10","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":617,"text":"Volcano Science Center","active":true,"usgs":true}],"links":[{"id":307060,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":307059,"rank":1,"type":{"id":15,"text":"Index Page"},"url":"https://www.ijege.uniroma1.it/rivista/5th-international-conference-on-debris-flow-hazards-mitigation-mechanics-prediction-and-assessment"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"55d6fa2ee4b0518e3546bc0e","contributors":{"authors":[{"text":"George, David L. dlgeorge@usgs.gov","contributorId":3416,"corporation":false,"usgs":true,"family":"George","given":"David L.","email":"dlgeorge@usgs.gov","affiliations":[],"preferred":true,"id":569026,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Iverson, Richard M. 0000-0002-7369-3819 riverson@usgs.gov","orcid":"https://orcid.org/0000-0002-7369-3819","contributorId":536,"corporation":false,"usgs":true,"family":"Iverson","given":"Richard","email":"riverson@usgs.gov","middleInitial":"M.","affiliations":[{"id":615,"text":"Volcano Hazards Program","active":true,"usgs":true},{"id":617,"text":"Volcano Science Center","active":true,"usgs":true}],"preferred":true,"id":569027,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70189126,"text":"70189126 - 2011 - A geospatial approach to identify water quality issues for National Wildlife Refuges in Oregon and Washington","interactions":[],"lastModifiedDate":"2020-01-11T12:19:02","indexId":"70189126","displayToPublicDate":"2011-06-14T00:00:00","publicationYear":"2011","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2287,"text":"Journal of Fish and Wildlife Management","active":true,"publicationSubtype":{"id":10}},"title":"A geospatial approach to identify water quality issues for National Wildlife Refuges in Oregon and Washington","docAbstract":"Many National Wildlife Refuges (Refuges) have impaired water quality resulting from historic and current land uses, upstream sources, and aerial pollutant deposition. Competing duties limit the time available for Refuge staff to identify and evaluate potential water quality issues. As a result, water quality–related issues may not be resolved until a problem has already arisen. This study developed a geospatial approach for identifying and prioritizing water quality issues affecting natural resources (including migratory birds and federally listed species) within Refuge boundaries. We assessed the location and status of streams pursuant to the Clean Water Act in relation to individual Refuges in Oregon and Washington, United States. Although twelve Refuges in Oregon (60%) and eight Refuges in Washington (40%) were assessed under the Clean Water Act, only 12% and 3% of total Refuge stream lengths were assessed, respectively. Very few assessed Refuge streams were not designated as impaired (0% in Oregon, 1% in Washington). Despite the low proportions of stream lengths assessed, most Refuges in Oregon (70%) and Washington (65%) are located in watersheds with approved total maximum daily loads. We developed summaries of current water quality issues for individual Refuges and identified large gaps for Refuge-specific water quality data and habitat utilization by sensitive species. We conclude that monitoring is warranted on many Refuges to better characterize water quality under the Clean Water Act.
","language":"English","publisher":"U.S. Fish and Wildlife Service","doi":"10.3996/112010-JFWM-043","usgsCitation":"Hinck, J.E., Chojnacki, K., Finger, S.E., Linder, G., and Kilbride, K., 2011, A geospatial approach to identify water quality issues for National Wildlife Refuges in Oregon and Washington: Journal of Fish and Wildlife Management, v. 2, no. 1, p. 12-21, https://doi.org/10.3996/112010-JFWM-043.","productDescription":"10 p.","startPage":"12","endPage":"21","numberOfPages":"10","ipdsId":"IP-023088","costCenters":[{"id":192,"text":"Columbia Environmental Research Center","active":true,"usgs":true},{"id":34983,"text":"Contaminant Biology Program","active":true,"usgs":true}],"links":[{"id":474990,"rank":0,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.3996/112010-jfwm-043","text":"Publisher Index Page"},{"id":343229,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United 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","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Invasive Asian Carps in North America","largerWorkSubtype":{"id":12,"text":"Conference publication"},"language":"English","publisher":"American Fisheries Society","publisherLocation":"Bethesda, MD","usgsCitation":"Chapman, D., and Hoff, M.H., 2011, Introduction, chap. of Invasive Asian Carps in North America.","ipdsId":"IP-006962","costCenters":[{"id":192,"text":"Columbia Environmental Research Center","active":true,"usgs":true}],"links":[{"id":343230,"rank":1,"type":{"id":15,"text":"Index Page"},"url":"https://fisheries.org/bookstore/all-titles/afs-symposia/54074p/"},{"id":343231,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"otherGeospatial":"North America","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"59576359e4b0d1f9f051b6ab","contributors":{"authors":[{"text":"Chapman, Duane 0000-0002-1086-8853 dchapman@usgs.gov","orcid":"https://orcid.org/0000-0002-1086-8853","contributorId":1291,"corporation":false,"usgs":true,"family":"Chapman","given":"Duane","email":"dchapman@usgs.gov","affiliations":[{"id":324,"text":"Great Lakes Science Center","active":true,"usgs":true},{"id":192,"text":"Columbia Environmental Research Center","active":true,"usgs":true}],"preferred":true,"id":703090,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hoff, Michael H.","contributorId":111519,"corporation":false,"usgs":true,"family":"Hoff","given":"Michael","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":703091,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70155228,"text":"70155228 - 2011 - Observations of mass fractionation of noble gases in synthetic methane hydrate","interactions":[],"lastModifiedDate":"2017-05-30T11:17:56","indexId":"70155228","displayToPublicDate":"2011-06-14T00:00:00","publicationYear":"2011","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"title":"Observations of mass fractionation of noble gases in synthetic methane hydrate","docAbstract":"As a consequence of contemporary or longer term (since 15 ka) climate warming, gas hydrates in some settings are presently dissociating and releasing methane and other gases to the oceanatmosphere system. A key challenge in assessing the susceptibility of gas hydrates to warming climate is the lack of a technique able to distinguish between methane recently released from gas hydrates and methane emitted from leaky thermogenic reservoirs, shallow sublake and subseafloor sediments, coalbeds, and other sources. Carbon and deuterium stable isotopic data provide only a first-order characterization of methane sources, while gas hydrate can sequester any type of methane. Here, we investigate the possibility of exploiting the pattern of noble gas fractionation within the gas hydrate lattice to fingerprint methane released from gas hydrates. Starting with synthetic gas hydrate formed under careful laboratory conditions, we document complex noble gas fractionation patterns in the gases liberated during dissociation and explore the effects of aging and storage (e.g., in liquid nitrogen), as well as sampling and preservation procedures. The laboratory results confirm a unique noble gas fractionation pattern for gas hydrates, one that shows promise in evaluating modern natural gas seeps for a signature associated with gas hydrate dissociation.
","conferenceTitle":"International Conference on Gas Hydrates","conferenceDate":"July 17-21, 2011","conferenceLocation":"Edinburgh, Scotland","language":"English","usgsCitation":"Hunt, A.G., Pohlman, J.W., Stern, L.A., Ruppel, C., Moscati, R.J., Landis, G.P., and Pinkston, J., 2011, Observations of mass fractionation of noble gases in synthetic methane hydrate, International Conference on Gas Hydrates, Edinburgh, Scotland, July 17-21, 2011, 6 p.","productDescription":"6 p.","ipdsId":"IP-029211","costCenters":[{"id":211,"text":"Crustal Geophysics and Geochemistry Science Center","active":true,"usgs":true}],"links":[{"id":341831,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"publishingServiceCenter":{"id":2,"text":"Denver PSC"},"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"592e84cae4b092b266f10dd9","contributors":{"authors":[{"text":"Hunt, Andrew G. 0000-0002-3810-8610 ahunt@usgs.gov","orcid":"https://orcid.org/0000-0002-3810-8610","contributorId":1582,"corporation":false,"usgs":true,"family":"Hunt","given":"Andrew","email":"ahunt@usgs.gov","middleInitial":"G.","affiliations":[{"id":211,"text":"Crustal Geophysics and Geochemistry Science Center","active":true,"usgs":true}],"preferred":true,"id":565203,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Pohlman, John W. 0000-0002-3563-4586 jpohlman@usgs.gov","orcid":"https://orcid.org/0000-0002-3563-4586","contributorId":145771,"corporation":false,"usgs":true,"family":"Pohlman","given":"John","email":"jpohlman@usgs.gov","middleInitial":"W.","affiliations":[{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":true,"id":565207,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Stern, Laura A. 0000-0003-3440-5674 lstern@usgs.gov","orcid":"https://orcid.org/0000-0003-3440-5674","contributorId":1197,"corporation":false,"usgs":true,"family":"Stern","given":"Laura","email":"lstern@usgs.gov","middleInitial":"A.","affiliations":[{"id":237,"text":"Earthquake Science Center","active":true,"usgs":true}],"preferred":true,"id":565208,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Ruppel, Carolyn D. 0000-0003-2284-6632 cruppel@usgs.gov","orcid":"https://orcid.org/0000-0003-2284-6632","contributorId":145770,"corporation":false,"usgs":true,"family":"Ruppel","given":"Carolyn D.","email":"cruppel@usgs.gov","affiliations":[{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":false,"id":565204,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Moscati, Richard J. 0000-0002-0818-4401 rmoscati@usgs.gov","orcid":"https://orcid.org/0000-0002-0818-4401","contributorId":2462,"corporation":false,"usgs":true,"family":"Moscati","given":"Richard","email":"rmoscati@usgs.gov","middleInitial":"J.","affiliations":[{"id":211,"text":"Crustal Geophysics and Geochemistry Science Center","active":true,"usgs":true}],"preferred":true,"id":565209,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Landis, Gary P.","contributorId":72405,"corporation":false,"usgs":true,"family":"Landis","given":"Gary","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":696247,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Pinkston, John C.","contributorId":81381,"corporation":false,"usgs":true,"family":"Pinkston","given":"John C.","affiliations":[],"preferred":false,"id":696248,"contributorType":{"id":1,"text":"Authors"},"rank":7}]}} ,{"id":70004616,"text":"gip129 - 2011 - Poster for Ride the Rockies 2011","interactions":[],"lastModifiedDate":"2012-02-10T00:11:58","indexId":"gip129","displayToPublicDate":"2011-06-13T13:50:03","publicationYear":"2011","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":315,"text":"General Information Product","code":"GIP","onlineIssn":"2332-354X","printIssn":"2332-3531","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"129","title":"Poster for Ride the Rockies 2011","docAbstract":"To download other USGS materials related to Ride The Rockies, go to http://www.cr.usgs.gov/rtr/index.html","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/gip129","usgsCitation":"Slate, J.L., 2011, Poster for Ride the Rockies 2011: U.S. Geological Survey General Information Product 129, Poster: 57.49 x 34.76 inches, https://doi.org/10.3133/gip129.","productDescription":"Poster: 57.49 x 34.76 inches","startPage":"1","endPage":"1","numberOfPages":"1","temporalStart":"2011-01-01","temporalEnd":"2011-12-31","costCenters":[],"links":[{"id":116771,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/gip_129.gif"},{"id":19155,"rank":9999,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/gip/129/","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Colorado","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -102,37 ], [ -102,41 ], [ -109,41 ], [ -109,37 ], [ -102,37 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad5e4b07f02db683a59","contributors":{"authors":[{"text":"Slate, Janet L. 0000-0002-2870-9068 jslate@usgs.gov","orcid":"https://orcid.org/0000-0002-2870-9068","contributorId":252,"corporation":false,"usgs":true,"family":"Slate","given":"Janet","email":"jslate@usgs.gov","middleInitial":"L.","affiliations":[{"id":501,"text":"Office of Science Quality and Integrity","active":true,"usgs":true}],"preferred":true,"id":350865,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70004051,"text":"70004051 - 2011 - Better than a \"bird's eye view\"","interactions":[],"lastModifiedDate":"2014-05-30T13:26:51","indexId":"70004051","displayToPublicDate":"2011-06-13T13:50:00","publicationYear":"2011","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":977,"text":"Bay Soundings","active":true,"publicationSubtype":{"id":10}},"title":"Better than a \"bird's eye view\"","docAbstract":"No abstract available.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Bay Soundings","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"Tampa Bay Regional Planning Council","publisherLocation":"Pinellas Park, FL","usgsCitation":"Tihansky, A.B., Dadisman, S.V., and Dwyer, B., 2011, Better than a \"bird's eye view\": Bay Soundings, v. 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Although it is widely acknowledged that significant water-level changes have occurred in the past, the reviewed model does not represent changing water levels. The steady state approach limits the effectiveness of the following:\n\n1. identification of sources of contamination,\n\n2. analysis of model accuracy,\n\n3. model calibration, and\n\n4. simulations of future scenarios.\n\nFuture plume movement was simulated in an incomplete manner through an unchanging groundwater-flow field. Available time-series information on temporal variation of factors affecting groundwater-flow dynamics includes:\n\n1. public-supply pumping,\n\n2. groundwater discharges from systems remediating volatile organic compound (VOC) plumes,\n\n3. recharge and precipitation rates, and\n\n4. water levels and streamflows.\n\nTransient phenomena that might be useful in future hypothetical simulations include pumping variations, redirection of containment-system waters for industrial use, and climate-change scenarios. Public-domain computer programs, U.S. Geological Survey guidance reports on transient-state calibration and uncertainty methods (Doherty and Hunt, 2010), and additional local and regional datasets are available to provide additional confidence in model evaluations and allow better evaluation of their limitations.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr20111128","usgsCitation":"Misut, P.E., 2011, Simulation of groundwater flow in a volatile organic compound-contaminated area near Bethpage, Nassau County, New York: A discussion of modeling considerations: U.S. Geological Survey Open-File Report 2011-1128, vi, 19 p., https://doi.org/10.3133/ofr20111128.","productDescription":"vi, 19 p.","numberOfPages":"23","costCenters":[{"id":474,"text":"New York Water Science Center","active":true,"usgs":true}],"links":[{"id":410083,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_95236.htm","linkFileType":{"id":5,"text":"html"}},{"id":21868,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2011/1128/","linkFileType":{"id":5,"text":"html"}},{"id":116203,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ofr_2011_1128.gif"}],"scale":"24000","projection":"Universal Transverse Mercator projection","country":"United States","state":"New York","county":"Nassau County","city":"Bethpage","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -73.5308,\n 40.6769\n ],\n [\n -73.5308,\n 40.7728\n ],\n [\n -73.42,\n 40.7728\n ],\n [\n -73.42,\n 40.6769\n ],\n [\n -73.5308,\n 40.6769\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4abce4b07f02db67380d","contributors":{"authors":[{"text":"Misut, Paul E. 0000-0002-6502-5255 pemisut@usgs.gov","orcid":"https://orcid.org/0000-0002-6502-5255","contributorId":1073,"corporation":false,"usgs":true,"family":"Misut","given":"Paul","email":"pemisut@usgs.gov","middleInitial":"E.","affiliations":[{"id":474,"text":"New York Water Science Center","active":true,"usgs":true}],"preferred":true,"id":350864,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70004606,"text":"sir20115057 - 2011 - Sedimentation survey of Lago Cerrillos, Ponce, Puerto Rico, April-May 2008","interactions":[],"lastModifiedDate":"2012-03-08T17:16:41","indexId":"sir20115057","displayToPublicDate":"2011-06-13T10:50:04","publicationYear":"2011","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":"2011-5057","title":"Sedimentation survey of Lago Cerrillos, Ponce, Puerto Rico, April-May 2008","docAbstract":"Lago Cerrillos dam, located in the municipality of Ponce in southern Puerto Rico, was constructed in 1991 as part of the multipurpose Rio Portugues and Bucana Project. This project provides flood protection, water supply, and recreation facilities for the municipio of Ponce. The reservoir had an original storage capacity of 38.03 million cubic meters at maximum conservation pool elevation of 174.65 meters above mean sea level and a drainage area of 45.32 square kilometers. Sedimentation in Lago Cerrillos reservoir has reduced the storage capacity from 38.03 million cubic meters in 1991 to 37.26 million cubic meters in 2008, which represents a total storage loss of about 2 percent. During July 29 to August 23, 2002, 8,492 cubic meters of sediment were removed from the Rio Cerrillos mouth of the reservoir. Taking into account this removed material, the total water-storage loss as of 2008 is 778,492 cubic meters, and the long-term annual water-storage capacity loss rate is about 45,794 cubic meters per year or about 0.12 percent per year. The Lago Cerrillos net sediment-contributing drainage area has an average sediment yield of about 1,069 cubic meters per square kilometer per year. Sediment accumulation in Lago Cerrillos is not uniformly distributed and averages about 3 meters in thickness. This represents a sediment deposition rate of about 18 centimeters per year. On the basis of the 2008 reservoir storage capacity of 37.26 million cubic meters per year and a long-term sedimentation rate of 45,794 cubic meters per year, Lago Cerrillos is estimated to have a useful life of about 814 years or until the year 2822.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/sir20115057","usgsCitation":"Soler-Lopez, L.R., 2011, Sedimentation survey of Lago Cerrillos, Ponce, Puerto Rico, April-May 2008: U.S. Geological Survey Scientific Investigations Report 2011-5057, vi, 20 p.; 1 Plate: 17.00 x 22.00 inches, https://doi.org/10.3133/sir20115057.","productDescription":"vi, 20 p.; 1 Plate: 17.00 x 22.00 inches","temporalStart":"2008-04-01","temporalEnd":"2008-05-31","costCenters":[{"id":156,"text":"Caribbean Water Science Center","active":true,"usgs":true}],"links":[{"id":116202,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/sir_2011_5057.jpg"},{"id":19154,"rank":9999,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/sir/2011/5057/","linkFileType":{"id":5,"text":"html"}}],"projection":"Lambert Conic Conformal projection","datum":"Puerto Rico Datum, 1940 adjustment","country":"Puerto Rico","otherGeospatial":"Lago Cerrillos","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -66.6,18.066944444444445 ], [ -66.6,18.116666666666667 ], [ -66.56666666666666,18.116666666666667 ], [ -66.56666666666666,18.066944444444445 ], [ -66.6,18.066944444444445 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b00e4b07f02db6982b1","contributors":{"authors":[{"text":"Soler-Lopez, Luis R.","contributorId":27501,"corporation":false,"usgs":true,"family":"Soler-Lopez","given":"Luis","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":350838,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ]}