{"pageNumber":"915","pageRowStart":"22850","pageSize":"25","recordCount":46734,"records":[{"id":76691,"text":"ds178 - 2006 - Two-dimensional resistivity investigation along West Fork Trinity River, Naval Air Station-Joint Reserve Base Carswell Field, Fort Worth, Texas, October 2004","interactions":[],"lastModifiedDate":"2023-09-19T20:48:29.611729","indexId":"ds178","displayToPublicDate":"2006-05-04T00:00:00","publicationYear":"2006","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":310,"text":"Data Series","code":"DS","onlineIssn":"2327-638X","printIssn":"2327-0271","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"178","title":"Two-dimensional resistivity investigation along West Fork Trinity River, Naval Air Station-Joint Reserve Base Carswell Field, Fort Worth, Texas, October 2004","docAbstract":"Naval Air Station-Joint Reserve Base Carswell Field (NAS-JRB) at Fort Worth, Tex., constitutes a government-owned, contractor-operated facility that has been in operation since 1942. Contaminants, primarily volatile organic compounds and metals, have entered the ground-water-flow system through leakage from waste-disposal sites and manufacturing processes. Ground water flows from west to east toward the West Fork Trinity River. During October 2004, the U.S. Geological Survey conducted a two-dimensional (2D) resistivity investigation at a site along the West Fork Trinity River at the eastern boundary of NAS-JRB to characterize the distribution of subsurface resistivity. Five 2D resistivity profiles were collected, which ranged from 500 to 750 feet long and extended to a depth of 25 feet. The Goodland Limestone and the underlying Walnut Formation form a confining unit that underlies the alluvial aquifer. The top of this confining unit is the top of bedrock at NAS-JRB. The bedrock confining unit is the zone of interest because of the potential for contaminated ground water to enter the West Fork Trinity River through saturated bedrock. The study involved a capacitively-coupled resistivity survey and inverse modeling to obtain true or actual resistivity from apparent resistivity. The apparent resistivity was processed using an inverse modeling software program. The results of this program were used to generate distributions (images) of actual resistivity referred to as inverted sections or profiles. The images along the five profiles show a wide range of resistivity values. The two profiles nearest the West Fork Trinity River generally showed less resistivity than the three other profiles.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ds178","collaboration":"Prepared in cooperation with the U.S. Air Force, Aeronautical Systems Center, Environmental Management Directorate, Wright-Patterson Air Force Base, Ohio","usgsCitation":"Shah, S., and Stanton, G.P., 2006, Two-dimensional resistivity investigation along West Fork Trinity River, Naval Air Station-Joint Reserve Base Carswell Field, Fort Worth, Texas, October 2004: U.S. Geological Survey Data Series 178, iv, 24 p., https://doi.org/10.3133/ds178.","productDescription":"iv, 24 p.","numberOfPages":"31","costCenters":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"links":[{"id":420955,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_76486.htm","linkFileType":{"id":5,"text":"html"}},{"id":7739,"rank":2,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/ds/ds178/","linkFileType":{"id":5,"text":"html"}},{"id":192620,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.er.usgs.gov/thumbnails/usgs_thumb.jpg"}],"country":"United States","state":"Texas","city":"Fort Worth","otherGeospatial":"Carswell Field, West Fork Trinity River","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -97.42589950561523,\n              32.75638608388472\n            ],\n            [\n              -97.42589950561523,\n              32.80011749844536\n            ],\n            [\n              -97.40049362182617,\n              32.80011749844536\n            ],\n            [\n              -97.40049362182617,\n              32.75638608388472\n            ],\n            [\n              -97.42589950561523,\n              32.75638608388472\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b05e4b07f02db699833","contributors":{"authors":[{"text":"Shah, Sachin D.","contributorId":60174,"corporation":false,"usgs":true,"family":"Shah","given":"Sachin D.","affiliations":[],"preferred":false,"id":287627,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Stanton, Gregory P. 0000-0001-8622-0933 gstanton@usgs.gov","orcid":"https://orcid.org/0000-0001-8622-0933","contributorId":1583,"corporation":false,"usgs":true,"family":"Stanton","given":"Gregory","email":"gstanton@usgs.gov","middleInitial":"P.","affiliations":[],"preferred":true,"id":287626,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":76687,"text":"sir20065036 - 2006 - An evaluation and review of water-use estimates and flow data for the Lower Klamath and Tule Lake National Wildlife Refuges, Oregon and California","interactions":[],"lastModifiedDate":"2012-03-08T17:16:20","indexId":"sir20065036","displayToPublicDate":"2006-05-04T00:00:00","publicationYear":"2006","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":334,"text":"Scientific Investigations Report","code":"SIR","onlineIssn":"2328-0328","printIssn":"2328-031X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2006-5036","title":"An evaluation and review of water-use estimates and flow data for the Lower Klamath and Tule Lake National Wildlife Refuges, Oregon and California","docAbstract":"The Lower Klamath and Tule Lake National Wildlife Refuges, located in the upper Klamath Basin of Oregon and California, encompass approximately 46,700 and 39,100 acres, respectively. Demand for water in the semiarid upper Klamath Basin has increased in recent years, resulting in the need to better quantify water availability and use in the refuges. This report presents an evaluation of water-use estimates for both refuges derived on the basis of two approaches. One approach used evaporation and evapotranspiration estimates and the other used measured inflow and outflow data. The quality of the inflow and outflow data also was assessed.\r\n\r\nAnnual water use in the refuges, using evapotranspiration estimates, was computed with the use of different rates for each of four land-use categories. Annual water-use rates for grain fields, seasonal wetlands, permanently flooded wetlands with emergent vegetation, and open-water bodies were 2.5, 2.9, 2.63, and 4.07 feet per year, respectively. Total water use was estimated as the sum of the products of each rate and the number of acres in its associated land-use category. Mean annual (2003-2005) water use for the Lower Klamath and Tule Lake refuges was approximately 124,000 and 95,900 acre-feet, respectively. To estimate water deliveries needed for each refuge, first, annual precipitation for 2003-2005 was subtracted from the annual water use for those years. Then, an adjusted total was obtained by adding 20 percent to the difference to account for salinity flushing. Resulting estimated mean annual adjusted needed water deliveries in 2003-2005 for the Lower Klamath and Tule Lake refuges were 107,000 and 82,800 acre-feet, respectively.\r\n\r\nMean annual net inflow to the refuges for 2003-2005 was computed by subtracting estimated and measured surface-water outflows from inflows. Mean annual net inflow during the 3-year period for the Lower Klamath refuge, calculated for a subsection of the refuge, was approximately 73,700 acre-feet. The adjusted needed water delivery for this section of the refuge, calculated from evapotranspiration estimates, was approximately 77,600 acre-feet. For the Tule Lake refuge, mean annual net inflow during the 3-year period was approximately 76,100 acre-feet, which is comparable to the estimated annual needed water delivery for the refuge of 82,800 acre-feet.\r\n\r\nFor 1962-2005, mean annual net inflow to the Lower Klamath refuge was approximately 49,800 acre-feet, about 23,900 acre-feet less than for 2003-2005. Although mean April-September net inflows for 1962-2005 and 2003-2005 have remained fairly constant, annual net inflow has increased for October-March, which accounts for the difference. Consistently higher autumn and winter flow deliveries since the mid-1980s reflect a significant change in refuge management. More sections of the refuge are currently managed as seasonal wetlands than were in the 1960s and 1970s.\r\n\r\nFlow records for the Ady Canal at State Line Road, Klamath Straits Drain at State Line Road, and D Pumping Plant were evaluated for their data quality. On the basis of USGS flow-record criteria, all three flow records were rated as 'poor.' By definition, 95 percent of the daily flows in a record having this rating could be in error by more than 15 percent. ","language":"ENGLISH","doi":"10.3133/sir20065036","usgsCitation":"Risley, J.C., and Gannett, M.W., 2006, An evaluation and review of water-use estimates and flow data for the Lower Klamath and Tule Lake National Wildlife Refuges, Oregon and California: U.S. Geological Survey Scientific Investigations Report 2006-5036, 28 p., https://doi.org/10.3133/sir20065036.","productDescription":"28 p.","numberOfPages":"28","costCenters":[{"id":518,"text":"Oregon Water Science Center","active":true,"usgs":true}],"links":[{"id":192154,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":7734,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/sir/2006/5036/","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b25e4b07f02db6af10c","contributors":{"authors":[{"text":"Risley, John C. 0000-0002-8206-5443 jrisley@usgs.gov","orcid":"https://orcid.org/0000-0002-8206-5443","contributorId":2698,"corporation":false,"usgs":true,"family":"Risley","given":"John","email":"jrisley@usgs.gov","middleInitial":"C.","affiliations":[{"id":518,"text":"Oregon Water Science Center","active":true,"usgs":true}],"preferred":true,"id":287619,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Gannett, Marshall W. 0000-0003-2498-2427 mgannett@usgs.gov","orcid":"https://orcid.org/0000-0003-2498-2427","contributorId":2942,"corporation":false,"usgs":true,"family":"Gannett","given":"Marshall","email":"mgannett@usgs.gov","middleInitial":"W.","affiliations":[{"id":518,"text":"Oregon Water Science Center","active":true,"usgs":true}],"preferred":true,"id":287620,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":76678,"text":"sir20065007 - 2006 - Summary of Environmental Monitoring and Assessment Program (EMAP) activities in South Dakota, 2000–2004","interactions":[],"lastModifiedDate":"2021-12-30T19:43:10.396056","indexId":"sir20065007","displayToPublicDate":"2006-05-02T00:00:00","publicationYear":"2006","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":334,"text":"Scientific Investigations Report","code":"SIR","onlineIssn":"2328-0328","printIssn":"2328-031X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2006-5007","title":"Summary of Environmental Monitoring and Assessment Program (EMAP) activities in South Dakota, 2000–2004","docAbstract":"The U.S. Environmental Protection Agency (USEPA) initiated data-collection activities for the Environmental Monitoring and Assessment Program-West (EMAP-West) in South Dakota during 2000. The objectives of the study were to develop the monitoring tools necessary to produce unbiased estimates of the ecological condition of surface waters across a large geographic area of the western United States, and to demonstrate the effectiveness of those tools in a large-scale assessment.\r\n\r\nIn 2001, the U.S. Geological Survey (USGS) and the South Dakota Department of Game, Fish and Parks (GF&P) established a cooperative agreement and assumed responsibility for completing the remaining assessments for the perennial, wadable streams of the EMAP-West in the State. Stream assessment sites were divided into two broad categories-the first category of sites was randomly selected and assigned by the USEPA for South Dakota. The second category consisted of sites that were specifically selected because they appeared to have reasonable potential for representing the best available physical, chemical, and biological conditions in the State. These sites comprise the second category of assessment sites and were called 'reference' sites and were selected following a detailed evaluation process. Candidate reference site data will serve as a standard or benchmark for assessing the overall ecological condition of the randomly selected sites.\r\n\r\nDuring 2000, the USEPA completed 22 statewide stream assessments in South Dakota. During 2001-2003, the USGS and GF&P completed another 42 stream assessments bringing the total of randomly selected stream assessments within South Dakota to 64. In addition, 18 repeat assessments designed to meet established quality-assurance/quality-control requirements were completed at 12 of these 64 sites. During 2002-2004, the USGS in cooperation with GF&P completed stream assessments at 45 candidate reference sites. Thus, 109 sites had stream assessments completed in South Dakota for EMAP-West (2000-2004).\r\n\r\nRelatively early in the EMAP-West stream-assessment process, it became apparent that for some streams in south-central South Dakota, in-stream conditions varied considerably over relatively short distances of only a few miles. These changes appeared to be a result of geomorphic changes associated with changes in the underlying geology. For these streams, moving stream assessment sites short distances upstream or downstream had the potential to provide substantially different bioassessment data. In order to obtain a better understanding of how geology influences stream conditions, two streams located in south-central South Dakota were chosen for multiple stream sampling at sites located along their longitudinal profile at points where notable changes in geomorphology were observed. Subsequently, three sites on Bear-in-the-Lodge Creek and three sites on Black Pipe Creek were selected for multiple stream sampling using EMAP-West protocols so that more could be learned about geologic influences on stream conditions.\r\n\r\nValues for dissolved oxygen and specific conductance generally increased from upstream to downstream locations on Bear-in-the-Lodge Creek. Values for pH and water temperature generally decreased from upstream to downstream locations. Decreasing water temperature could be indicative of ground-water inflows.\r\n\r\nValues for dissolved oxygen, pH, and water temperature generally increased from upstream to downstream locations on Black Pipe Creek. The increase in temperature at the lower sites is a result of less dense riparian cover, and the warmer water also could account for the lower concentrations of dissolved oxygen found in the lower reaches of Black Pipe Creek. Values for specific conductance were more than three times greater at the lower site (1,342 microsiemens per centimeter (?S/cm)) than at the upper site (434 ?S/cm). The increase probably occurs when the stream transitions from contacting the underlying Ar","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/sir20065007","usgsCitation":"Heakin, A.J., Neitzert, K.M., and Shearer, J.S., 2006, Summary of Environmental Monitoring and Assessment Program (EMAP) activities in South Dakota, 2000–2004: U.S. Geological Survey Scientific Investigations Report 2006-5007, vi, 45 p., https://doi.org/10.3133/sir20065007.","productDescription":"vi, 45 p.","numberOfPages":"51","temporalStart":"2000-01-01","temporalEnd":"2004-12-31","costCenters":[{"id":562,"text":"South Dakota Water Science Center","active":true,"usgs":true},{"id":34685,"text":"Dakota Water Science Center","active":true,"usgs":true}],"links":[{"id":122374,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/sir_2006_5007.jpg"},{"id":393694,"rank":3,"type":{"id":36,"text":"NGMDB Index 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S.","contributorId":85678,"corporation":false,"usgs":true,"family":"Shearer","given":"Jeffrey","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":287593,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":76677,"text":"fs20063001 - 2006 - The Environmental Monitoring and Assessment Program (EMAP)-West: Summary of activities and accomplishments in South Dakota, 2000-2004","interactions":[],"lastModifiedDate":"2017-10-15T11:32:44","indexId":"fs20063001","displayToPublicDate":"2006-05-02T00:00:00","publicationYear":"2006","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":313,"text":"Fact Sheet","code":"FS","onlineIssn":"2327-6932","printIssn":"2327-6916","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2006-3001","title":"The Environmental Monitoring and Assessment Program (EMAP)-West: Summary of activities and accomplishments in South Dakota, 2000-2004","docAbstract":"<p class=\"body\">The Environmental Monitoring and Assessment Program (EMAP)-West was initiated in South Dakota in 2000 by the U.S. Environmental Protection Agency (USEPA). The two primary objectives of the surface waters component of EMAP-West were to (1) develop the monitoring tools (biological indicators, stream survey design, estimates of reference condition) necessary to produce unbiased estimates of the ecological condition of surface waters across a large geographic area of the West; and (2) demonstrate the effectiveness of those tools in a large-scale assessment. Although not specifically defined as an objective, data collected during EMAP-West also will help to establish a baseline for comparisons with data obtained from future monitoring efforts and could document changing biological conditions resulting from changing land-use or land-management practices associated with regulatory or restorative efforts.</p><p class=\"body\">EMAP-West is a partnership between USEPA, States, Tribes, and other inter­ested parties in USEPA Regions 8, 9, and 10. In South Dakota, the principle EMAP-West cooperators include the USEPA, South Dakota Department of Game, Fish and Parks (GF&amp;P), and the U.S. Geological Survey (USGS). Other agencies such as the Natural Resource Conservation ­Service, the South Dakota Department of Environment and Natural Resources (SDDENR), State Conservation Dis­tricts, and various Tribal departments also have provided valuable expertise and assistance.</p><p class=\"body\">This fact sheet summarizes the activities and accomplishments associated with EMAP-West in South Dakota during 2000–2004. Efforts were focused on perennial streams that usually can be waded. Large rivers also were assessed during EMAP-West under the auspices of USEPA using boats and similar techniques, but are not included in the activities discussed here. Data-collection activities for wadeable streams were conducted under the auspices of USEPA in South Dakota during 2000 and by the USGS during 2001–2004. A more detailed description of EMAP-West activities and assessments in South Dakota is available in Heakin and others (<i>in press</i>).</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/fs20063001","usgsCitation":"Heakin, A.J., and Neitzert, K.M., 2006, The Environmental Monitoring and Assessment Program (EMAP)-West: Summary of activities and accomplishments in South Dakota, 2000-2004: U.S. Geological Survey Fact Sheet 2006-3001, 4 p., https://doi.org/10.3133/fs20063001.","productDescription":"4 p.","numberOfPages":"4","temporalStart":"2000-01-01","temporalEnd":"2004-12-31","costCenters":[{"id":562,"text":"South Dakota Water Science Center","active":true,"usgs":true},{"id":34685,"text":"Dakota Water Science Center","active":true,"usgs":true}],"links":[{"id":121161,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/fs_2006_3001.jpg"},{"id":7816,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/fs/2006/3001/","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"South Dakota","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac9e4b07f02db67c8f2","contributors":{"authors":[{"text":"Heakin, Allen J.","contributorId":20366,"corporation":false,"usgs":true,"family":"Heakin","given":"Allen","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":287590,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Neitzert, Kathleen M. kmneitze@usgs.gov","contributorId":1833,"corporation":false,"usgs":true,"family":"Neitzert","given":"Kathleen","email":"kmneitze@usgs.gov","middleInitial":"M.","affiliations":[{"id":562,"text":"South Dakota Water Science Center","active":true,"usgs":true}],"preferred":true,"id":287589,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70176754,"text":"70176754 - 2006 - Applications of geophysical methods to volcano monitoring","interactions":[],"lastModifiedDate":"2018-06-12T15:55:20","indexId":"70176754","displayToPublicDate":"2006-05-01T00:00:00","publicationYear":"2006","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"title":"Applications of geophysical methods to volcano monitoring","docAbstract":"<div data-canvas-width=\"352.12399999999997\">The array of geophysical technologies used in volcano hazards studies - some developed originally only for volcano monitoring - ranges from satellite remote sensing including InSAR to leveling and EDM surveys, campaign and telemetered GPS networks, electronic tiltmeters and strainmeters, airborne magnetic and electromagnetic surveys, short-period and broadband seismic monitoring, even microphones tuned for infrasound. They include virtually every method used in resource exploration except large-scale seismic reflection. By “geophysical ” we include both active and passive methods as well as geodetic technologies. Volcano monitoring incorporates telemetry to handle high-bandwith cameras and broadband seismometers. Critical geophysical targets include the flux of magma in shallow reservoir and lava-tube systems, changes in active hydrothermal systems, volcanic edifice stability, and lahars. Since the eruption of Mount St. Helens in Washington State in 1980, and the eruption at Pu’u O’o in Hawai’i beginning in 1983 and still continuing, dramatic advances have occurred in monitoring technology such as “crisis GIS” and lahar modeling, InSAR interferograms, as well as gas emission geochemistry sampling, and hazards mapping and eruption predictions. The on-going eruption of Mount St. Helens has led to new monitoring technologies, including advances in broadband Wi-Fi and satellite telemetry as well as new instrumentation. Assessment of the gap between adequate monitoring and threat at the 169 potentially dangerous Holocene volcanoes shows where populations are dangerously exposed to volcanic catastrophes in the United States and its territories . This paper focuses primarily on Hawai’ian volcanoes and the northern Pacific and Cascades volcanoes. The US Geological Survey, the US National Park System, and the University of Utah cooperate in a program to monitor the huge Yellowstone volcanic system, and a separate observatory monitors the restive Long Valley caldera in collaboration with the US Forest Service.&nbsp;</div>","largerWorkType":{"id":24,"text":"Conference Paper"},"largerWorkTitle":"19th Symposium on the Application of Geophysics to Engineering and Environmental Problems (SAGEEP 2006): Geophysical applications for environmental and engineering hazards - Advances and constraints","conferenceTitle":"19th Symposium on the Application of Geophysics to Engineering and Environmental Problems","conferenceDate":"April 2-6, 2006","conferenceLocation":"Seattle, WA","language":"English","publisher":"Curran Associates Inc.","isbn":"9781622760657","usgsCitation":"Wynn, J., Dzurisin, D., Finn, C., Kauahikaua, J.P., and Lahusen, R.G., 2006, Applications of geophysical methods to volcano monitoring, <i>in</i> 19th Symposium on the Application of Geophysics to Engineering and Environmental Problems (SAGEEP 2006): Geophysical applications for environmental and engineering hazards - Advances and constraints, v. 1, Seattle, WA, April 2-6, 2006, p. 174-183.","productDescription":"10 p.","startPage":"174","endPage":"183","costCenters":[{"id":615,"text":"Volcano Hazards Program","active":true,"usgs":true}],"links":[{"id":329317,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":329316,"rank":1,"type":{"id":15,"text":"Index Page"},"url":"https://www.proceedings.com/15059.html"}],"volume":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"57fe8d33e4b0824b2d14b0e7","contributors":{"authors":[{"text":"Wynn, Jeff 0000-0002-8102-3882 jwynn@usgs.gov","orcid":"https://orcid.org/0000-0002-8102-3882","contributorId":2803,"corporation":false,"usgs":true,"family":"Wynn","given":"Jeff","email":"jwynn@usgs.gov","affiliations":[{"id":617,"text":"Volcano Science Center","active":true,"usgs":true}],"preferred":true,"id":650181,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Dzurisin, Daniel 0000-0002-0138-5067 dzurisin@usgs.gov","orcid":"https://orcid.org/0000-0002-0138-5067","contributorId":538,"corporation":false,"usgs":true,"family":"Dzurisin","given":"Daniel","email":"dzurisin@usgs.gov","affiliations":[{"id":617,"text":"Volcano Science Center","active":true,"usgs":true}],"preferred":true,"id":650182,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Finn, Carol A. 0000-0002-6178-0405","orcid":"https://orcid.org/0000-0002-6178-0405","contributorId":205010,"corporation":false,"usgs":true,"family":"Finn","given":"Carol A.","affiliations":[{"id":211,"text":"Crustal Geophysics and Geochemistry Science Center","active":true,"usgs":true}],"preferred":false,"id":650183,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Kauahikaua, James P. 0000-0003-3777-503X jimk@usgs.gov","orcid":"https://orcid.org/0000-0003-3777-503X","contributorId":2146,"corporation":false,"usgs":true,"family":"Kauahikaua","given":"James","email":"jimk@usgs.gov","middleInitial":"P.","affiliations":[{"id":617,"text":"Volcano Science Center","active":true,"usgs":true}],"preferred":true,"id":650184,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Lahusen, Richard G. rlahusen@usgs.gov","contributorId":535,"corporation":false,"usgs":true,"family":"Lahusen","given":"Richard","email":"rlahusen@usgs.gov","middleInitial":"G.","affiliations":[{"id":617,"text":"Volcano Science Center","active":true,"usgs":true}],"preferred":true,"id":650185,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":70176769,"text":"70176769 - 2006 - Infrasonic array observations at I53US of the 2006 Augustine Volcano eruptions","interactions":[],"lastModifiedDate":"2016-10-05T14:55:03","indexId":"70176769","displayToPublicDate":"2006-05-01T00:00:00","publicationYear":"2006","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":5210,"text":"InfraMatics","onlineIssn":"2169-2696","printIssn":"2169-270X","active":true,"publicationSubtype":{"id":10}},"title":"Infrasonic array observations at I53US of the 2006 Augustine Volcano eruptions","docAbstract":"<div class=\"t m0 x1 h9 y14 ff3 fs6 fc0 sc0 ls0 wsb\">The recent January 2006 Augustine eruptions, from the 11th to the 28th, have produced a series of 12 infrasonic signals that were observed at the I53US array at UAF. the eruption times for the signals were provided by the Alaska Volcanic Observatory at UAF using seismic sensors and a Chaparral microphone that are installed on Augustine Island. The bearing and distance of Augustine from I53US are, respectively, 207.8 degrees and 675 km. The analysis of the signals is done with a least-squares detector/estimator that calculates, from the 28 different sensor-pairs in the array, the mean of the cross-correlation maxima (MCCM), the horizontal trace-velocity and the azimuth of arrival of the signal using a sliding-window of 2000 data points. The data were bandpass filtered from 0.03 to 0.10 Hz. The data are digitized at a rate of 20 Hz. The average values of the signal parameters for all 12 Augustine signals are as follows: MCCM=0.85 (std 0.14), Trace-velocity=0.346 (std 0.016) km/sec, Azimuth=209 (std 2) deg. The celerity for each signal was calculated using the range 675 km and the individual travel times to I53US. The average celerity for all ten eruption signals was 0.27 (std 0.02) km/sec. Ray tracing studies, using mean values of the wind speed and temperature profiles (along the path) from NRL, have shown that there was propagation to I53US by both stratospheric and thermospheric ray paths from the volcano.</div>","language":"English","publisher":"Scientific Research Publ.","usgsCitation":"Wilson, C., Olson, J., Szuberla, C.A., McNutt, S., Tytgat, G., and Drob, D.P., 2006, Infrasonic array observations at I53US of the 2006 Augustine Volcano eruptions: InfraMatics, v. 13, p. 11-25.","productDescription":"14 p.","startPage":"11","endPage":"25","costCenters":[{"id":615,"text":"Volcano Hazards Program","active":true,"usgs":true}],"links":[{"id":329335,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":329334,"rank":1,"type":{"id":15,"text":"Index Page"},"url":"https://scholarcommons.usf.edu/geo_facpub/310/"}],"country":"United States","state":"Alaska","otherGeospatial":"Augustine Island","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -153.51470947265625, 59.412945785071 ], [ -153.47625732421875, 59.41993301322722 ], [ -153.446044921875, 59.428315784042574 ], [ -153.39385986328125, 59.428315784042574 ], [ -153.36090087890622, 59.41574084934491 ], [ -153.34442138671875, 59.39477224351409 ], [ -153.31695556640625, 59.37658895163648 ], [ -153.32794189453125, 59.33599107056162 ], [ -153.37188720703125, 59.32338185310805 ], [ -153.446044921875, 59.31777625443006 ], [ -153.5394287109375, 59.31076795603884 ], [ -153.577880859375, 59.32618430580267 ], [ -153.577880859375, 59.35139598294652 ], [ -153.60260009765625, 59.379387015928536 ], [ -153.59161376953125, 59.404559208021745 ], [ -153.55865478515625, 59.410150490100754 ], [ -153.51470947265625, 59.412945785071 ] ] ] } } ] }","volume":"13","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"57fe8d33e4b0824b2d14b0e5","contributors":{"authors":[{"text":"Wilson, C.R.","contributorId":78353,"corporation":false,"usgs":true,"family":"Wilson","given":"C.R.","email":"","affiliations":[],"preferred":false,"id":650247,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Olson, J.V.","contributorId":71836,"corporation":false,"usgs":true,"family":"Olson","given":"J.V.","email":"","affiliations":[],"preferred":false,"id":650248,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Szuberla, Curt A.L.","contributorId":175150,"corporation":false,"usgs":false,"family":"Szuberla","given":"Curt","email":"","middleInitial":"A.L.","affiliations":[],"preferred":false,"id":650249,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"McNutt, Steve","contributorId":101536,"corporation":false,"usgs":true,"family":"McNutt","given":"Steve","affiliations":[],"preferred":false,"id":650250,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Tytgat, Guy","contributorId":71152,"corporation":false,"usgs":true,"family":"Tytgat","given":"Guy","email":"","affiliations":[],"preferred":false,"id":650251,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Drob, Douglas P.","contributorId":175152,"corporation":false,"usgs":false,"family":"Drob","given":"Douglas","email":"","middleInitial":"P.","affiliations":[{"id":16692,"text":"Naval Research Laboratory","active":true,"usgs":false}],"preferred":false,"id":650252,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}}
,{"id":70184344,"text":"70184344 - 2006 - Effects of spatially variable resolution on field-scale estimates of tracer concentration from electrical inversions using Archie's law","interactions":[],"lastModifiedDate":"2019-10-16T17:48:02","indexId":"70184344","displayToPublicDate":"2006-05-01T00:00:00","publicationYear":"2006","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1808,"text":"Geophysics","active":true,"publicationSubtype":{"id":10}},"title":"Effects of spatially variable resolution on field-scale estimates of tracer concentration from electrical inversions using Archie's law","docAbstract":"<p><span>Two important mechanisms affect our ability to estimate solute concentrations quantitatively from the inversion of field-scale electrical resistivity tomography (ERT) data: (1) the spatially variable physical processes that govern the flow of current as well as the variation of physical properties in space and (2) the overparameterization of inverse models, which requires the imposition of a smoothing constraint (regularization) to facilitate convergence of the inverse solution. Based on analyses of field and synthetic data, we find that the ability of ERT to recover the 3D shape and magnitudes of a migrating conductive target is spatially variable. Additionally, the application of Archie's law to tomograms from field ERT data produced solute concentrations that are consistently less than 10% of point measurements collected in the field and estimated from transport modeling. Estimates of concentration from ERT using Archie's law only fit measured solute concentrations if the apparent formation factor is varied with space and time and allowed to take on unreasonably high values. Our analysis suggests that the inability to find a single petrophysical relation in space and time between concentration and electrical resistivity is largely an effect of two properties of ERT surveys: (1) decreased sensitivity of ERT to detect the target plume with increasing distance from the electrodes and (2) the smoothing imprint of regularization used in inversion.</span></p>","language":"English","publisher":"Society of Exploration Geophysicists","doi":"10.1190/1.2194900","usgsCitation":"Singha, K., and Gorelick, S.M., 2006, Effects of spatially variable resolution on field-scale estimates of tracer concentration from electrical inversions using Archie's law: Geophysics, v. 71, no. 3, p. G83-G91, https://doi.org/10.1190/1.2194900.","productDescription":"9 p. ","startPage":"G83","endPage":"G91","costCenters":[{"id":493,"text":"Office of Ground Water","active":true,"usgs":true},{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":336972,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"71","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"58bfd4fde4b014cc3a3ba527","contributors":{"authors":[{"text":"Singha, Kamini","contributorId":76733,"corporation":false,"usgs":true,"family":"Singha","given":"Kamini","affiliations":[],"preferred":false,"id":681078,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Gorelick, Steven M.","contributorId":8784,"corporation":false,"usgs":true,"family":"Gorelick","given":"Steven","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":681079,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70156276,"text":"70156276 - 2006 - New products from the shuttle radar topography mission","interactions":[],"lastModifiedDate":"2018-02-21T14:03:28","indexId":"70156276","displayToPublicDate":"2006-05-01T00:00:00","publicationYear":"2006","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1578,"text":"Eos, Transactions, American Geophysical Union","onlineIssn":"2324-9250","printIssn":"0096-394","active":true,"publicationSubtype":{"id":10}},"title":"New products from the shuttle radar topography mission","docAbstract":"<p>New data products with broad applicability to the Earth sciences are now available from the Shuttle Radar Topography Mission (SRTM). SRTM, a joint project of the National Geospatial-Intelligence Agency (NGA) and NASA, flew aboard the Space Shuttle Endeavour on an 11-day mission in February 2000 with the goal of collecting a near-global data set of high-resolution elevation data [<i>Fan and Kobrick</i>, 2000]. Data from the mission have been available to researchers for several years, but newly available products offer enhanced usability and applicability.</p>\n<p>Final products include elevation data resulting from a substantial editing effort by the NGA in which water bodies and coastlines were well defined and data artifacts known as spikes and wells (single pixel errors) were removed. This second version of the SRTM data set, also referred to as &lsquo;finished&rsquo; data, represents a significant improvement over earlier versions that had nonflat water bodies, poorly defined coastlines, and numerous noise artifacts. The edited data are available at a one-arc-second resolution (approximately 30 meters) for the United States and its territories, and at a three-arc-second resolution (approximately 90 meters) for non-U.S. areas.</p>","language":"English","publisher":"American Geophysical Union","doi":"10.1029/2006EO180003","usgsCitation":"Gesch, D.B., Farr, T., Slater, J., Muller, J., and Cook, S., 2006, New products from the shuttle radar topography mission: Eos, Transactions, American Geophysical Union, v. 87, no. 18, https://doi.org/10.1029/2006EO180003.","productDescription":"1 p.","startPage":"174","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":222,"text":"Earth Resources Observation and Science (EROS) Center","active":true,"usgs":true}],"links":[{"id":477332,"rank":0,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1029/2006eo180003","text":"Publisher Index Page"},{"id":306888,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"87","issue":"18","noUsgsAuthors":false,"publicationDate":"2011-06-03","publicationStatus":"PW","scienceBaseUri":"55d45732e4b0518e354694da","contributors":{"authors":[{"text":"Gesch, Dean B. 0000-0002-8992-4933 gesch@usgs.gov","orcid":"https://orcid.org/0000-0002-8992-4933","contributorId":2956,"corporation":false,"usgs":true,"family":"Gesch","given":"Dean","email":"gesch@usgs.gov","middleInitial":"B.","affiliations":[{"id":223,"text":"Earth Resources Observation and Science (EROS) Center (Geography)","active":false,"usgs":true},{"id":574,"text":"St. Petersburg Coastal and Marine Science Center","active":true,"usgs":true},{"id":222,"text":"Earth Resources Observation and Science (EROS) Center","active":true,"usgs":true}],"preferred":true,"id":568478,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Farr, Tom","contributorId":24903,"corporation":false,"usgs":true,"family":"Farr","given":"Tom","affiliations":[],"preferred":false,"id":568479,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Slater, James","contributorId":86630,"corporation":false,"usgs":true,"family":"Slater","given":"James","email":"","affiliations":[],"preferred":false,"id":568480,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Muller, Jan-Peter","contributorId":26882,"corporation":false,"usgs":true,"family":"Muller","given":"Jan-Peter","email":"","affiliations":[],"preferred":false,"id":568481,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Cook, Sally","contributorId":76387,"corporation":false,"usgs":true,"family":"Cook","given":"Sally","email":"","affiliations":[],"preferred":false,"id":568482,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":76671,"text":"wdrOH052 - 2006 - Water resources data, Ohio, water year 2005 : Volume 2. St. Lawrence River basin and statewide project data","interactions":[],"lastModifiedDate":"2012-03-08T17:16:23","indexId":"wdrOH052","displayToPublicDate":"2006-04-30T00:00:00","publicationYear":"2006","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":340,"text":"Water Data Report","code":"WDR","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"OH-05-2","title":"Water resources data, Ohio, water year 2005 : Volume 2. St. Lawrence River basin and statewide project data","language":"ENGLISH","doi":"10.3133/wdrOH052","usgsCitation":"Mangus, J., and Frum, S., 2006, Water resources data, Ohio, water year 2005 : Volume 2. St. Lawrence River basin and statewide project data: U.S. Geological Survey Water Data Report OH-05-2, 303 p., https://doi.org/10.3133/wdrOH052.","productDescription":"303 p.","numberOfPages":"303","temporalStart":"2004-10-01","temporalEnd":"2005-09-30","costCenters":[{"id":513,"text":"Ohio Water Science Center","active":true,"usgs":true}],"links":[{"id":194403,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":7722,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/wdr/2005/wdr-oh-05/","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f5e4b07f02db5f0d2c","contributors":{"authors":[{"text":"Mangus, J.P.","contributorId":28301,"corporation":false,"usgs":true,"family":"Mangus","given":"J.P.","email":"","affiliations":[],"preferred":false,"id":287572,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Frum, S.R.","contributorId":84843,"corporation":false,"usgs":true,"family":"Frum","given":"S.R.","email":"","affiliations":[],"preferred":false,"id":287573,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":76674,"text":"sir20065016 - 2006 - Suspended-sediment yields and stream-channel processes on Judy's Branch watershed in the St. Louis Metro East region in Illinois","interactions":[],"lastModifiedDate":"2012-03-08T17:16:23","indexId":"sir20065016","displayToPublicDate":"2006-04-30T00:00:00","publicationYear":"2006","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":334,"text":"Scientific Investigations Report","code":"SIR","onlineIssn":"2328-0328","printIssn":"2328-031X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2006-5016","title":"Suspended-sediment yields and stream-channel processes on Judy's Branch watershed in the St. Louis Metro East region in Illinois","docAbstract":"Judy's Branch watershed, a small basin (8.64 square miles) in the St. Louis Metro East region in Illinois, was selected as a pilot site to determine suspended-sediment yields and stream-channel processes in the bluffs and American Bottoms (expansive low-lying valley floor in the region). Suspended-sediment and stream-chan-nel data collected and analyzed for Judy's Branch watershed are presented in this report to establish a baseline of data for water-resource managers to evaluate future stream rehabilitation and manage-ment alternatives. The sediment yield analysis determines the amount of sediment being delivered from the watershed and two subwatersheds: an urban tributary and an undeveloped headwater (pri-marily agricultural). The analysis of the subwater-sheds is used to compare the effects of urbanization on sediment yield to the river. The stream-channel contribution to sediment yield was determined by evaluation of the stream-channel processes operat-ing on the streambed and banks of Judy's Branch watershed. Bank stability was related to hydrologic events, bank stratigraphy, and channel geometry through model development and simulation.\r\n\r\nThe average suspended-sediment yield from two upland subwatersheds (drainage areas of 0.23 and 0.40 sq.mi. was 1,163 tons per square mile per year (tons/sq.mi.-year) between July 2000 and June 2004. The suspended-sediment yield at the Route 157 station was 2,523 tons/sq.mi.-year, near the outlet of Judy's Branch watershed (drainage area = 8.33 sq.mi.). This is approximately 1,360 tons/sq.mi.-year greater than the average at the upland stations for the same time period. This result is unexpected in that, generally, the suspended-sediment yield decreases as the watershed area increases because of sediment stored in the channel and flood plain. The difference indicates a possible increase in yield from a source, such as bank retreat, and supports the concept that land-use changes increase stream-flows that may in turn result in higher rates of bank retreat. Utilizing both bank-rod data and resurveyed cross-section data, it was determined that approxi-mately half of the suspended- sediment yield at Route 157 during July 2000-June 2004 came from bank retreat.\r\n\r\nGiven that bank retreat can be a substantial portion of the sediment yield, understanding bank stability processes is important. Bank stability can be assessed mathematically by computing the factor of safety, which is defined by the ratio of the shear strength (resisting force) along the failure surface and the shear stress (driving gravitational force). Once the factor of safety falls below one, the bank theoretically becomes unstable. Bank-stability conditions were related to hydrologic events, bank type, and channel geometry through model develop-ment and simulation. The most common type of bank in the watershed consists of cohesive alluvial soil deposits overlying a stiff glacial till. A stabil-ity chart for different bank types was developed using a bank-stability analysis. Banks steeper than 70 degrees and higher than from 10 to 11.5 feet (depending on bank type) become at risk for mass failure in the watershed under conditions that pro-mote saturation of the bank and a sudden drop in the river level. ","language":"ENGLISH","doi":"10.3133/sir20065016","usgsCitation":"Straub, T., Johnson, G.P., Roseboom, D., and Sierra, C.R., 2006, Suspended-sediment yields and stream-channel processes on Judy's Branch watershed in the St. Louis Metro East region in Illinois: U.S. Geological Survey Scientific Investigations Report 2006-5016, 51 p., https://doi.org/10.3133/sir20065016.","productDescription":"51 p.","numberOfPages":"51","costCenters":[{"id":344,"text":"Illinois Water Science Center","active":true,"usgs":true}],"links":[{"id":194437,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":7727,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/sir/2006/5016/","linkFileType":{"id":5,"text":"html"}}],"geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -90,39 ], [ -90,39.333333333333336 ], [ -90.5,39.333333333333336 ], [ -90.5,39 ], [ -90,39 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae0e4b07f02db68803c","contributors":{"authors":[{"text":"Straub, Timothy D. 0000-0002-5896-0851 tdstraub@usgs.gov","orcid":"https://orcid.org/0000-0002-5896-0851","contributorId":2273,"corporation":false,"usgs":true,"family":"Straub","given":"Timothy D.","email":"tdstraub@usgs.gov","affiliations":[{"id":344,"text":"Illinois Water Science Center","active":true,"usgs":true}],"preferred":false,"id":287580,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Johnson, Gary P. 0000-0003-0363-9873 gjohnson@usgs.gov","orcid":"https://orcid.org/0000-0003-0363-9873","contributorId":2959,"corporation":false,"usgs":true,"family":"Johnson","given":"Gary","email":"gjohnson@usgs.gov","middleInitial":"P.","affiliations":[],"preferred":true,"id":287581,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Roseboom, Donald P.","contributorId":94747,"corporation":false,"usgs":true,"family":"Roseboom","given":"Donald P.","affiliations":[],"preferred":false,"id":287583,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Sierra, Carlos R.","contributorId":9365,"corporation":false,"usgs":true,"family":"Sierra","given":"Carlos","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":287582,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":76673,"text":"sir20055270 - 2006 - Continuous hydrologic simulation and flood-frequency, hydraulic, and flood-hazard analysis of the Blackberry Creek watershed, Kane County, Illinois","interactions":[],"lastModifiedDate":"2012-03-08T17:16:23","indexId":"sir20055270","displayToPublicDate":"2006-04-30T00:00:00","publicationYear":"2006","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":334,"text":"Scientific Investigations Report","code":"SIR","onlineIssn":"2328-0328","printIssn":"2328-031X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2005-5270","title":"Continuous hydrologic simulation and flood-frequency, hydraulic, and flood-hazard analysis of the Blackberry Creek watershed, Kane County, Illinois","docAbstract":"Results of hydrologic model, flood-frequency, hydraulic model, and flood-hazard analysis of the Blackberry Creek watershed in Kane County, Illinois, indicate that the 100-year and 500-year flood plains range from approximately 25 acres in the tributary F watershed (a headwater subbasin at the northeastern corner of the watershed) to almost 1,800 acres in Blackberry Creek main stem. Based on 1996 land-cover data, most of the land in the 100-year and 500-year flood plains was cropland, forested and wooded land, and grassland. A relatively small percentage of urban land was in the flood plains.\r\n\r\nThe Blackberry Creek watershed has undergone rapid urbanization in recent decades. The population and urbanized lands in the watershed are projected to double from the 1990 condition by 2020. Recently, flood-induced damage has occurred more frequently in urbanized areas of the watershed. There are concerns about the effect of urbanization on flood peaks and volumes, future flood-mitigation plans, and potential effects on the water quality and stream habitats. This report describes the procedures used in developing the hydrologic models, estimating the flood-peak discharge magnitudes and recurrence intervals for flood-hazard analysis, developing the hydraulic model, and the results of the analysis in graphical and tabular form.\r\n\r\nThe hydrologic model, Hydrological Simulation Program-FORTRAN (HSPF), was used to perform the simulation of continuous water movements through various patterns of land uses in the watershed. Flood-frequency analysis was applied to an annual maximum series to determine flood quantiles in subbasins for flood-hazard analysis. The Hydrologic Engineering Center-River Analysis System (HEC-RAS) hydraulic model was used to determine the 100-year and 500-year flood elevations, and to determine the 100-year floodway. The hydraulic model was calibrated and verified using high water marks and observed inundation maps for the July 17-18, 1996, flood event. Digital maps of the 100-year and 500-year flood plains and the 100-year floodway for each tributary and the main stem of Blackberry Creek were compiled.","language":"ENGLISH","doi":"10.3133/sir20055270","usgsCitation":"Soong, D., Straub, T., and Murphy, E., 2006, Continuous hydrologic simulation and flood-frequency, hydraulic, and flood-hazard analysis of the Blackberry Creek watershed, Kane County, Illinois: U.S. Geological Survey Scientific Investigations Report 2005-5270, 78 p.; 1 map plate, 38 x 42 in.; 1 CD-ROM, https://doi.org/10.3133/sir20055270.","productDescription":"78 p.; 1 map plate, 38 x 42 in.; 1 CD-ROM","numberOfPages":"78","additionalOnlineFiles":"Y","costCenters":[{"id":344,"text":"Illinois Water Science Center","active":true,"usgs":true}],"links":[{"id":194436,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":7725,"rank":9999,"type":{"id":21,"text":"Referenced Work"},"url":"https://pubs.usgs.gov/sir/2005/5270/pdf/hydraulictable.pdf","size":"1280","linkFileType":{"id":1,"text":"pdf"}},{"id":7726,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/sir/2005/5270/pdf/plate.pdf","size":"160000","linkFileType":{"id":1,"text":"pdf"}},{"id":7724,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/sir/2005/5270/","linkFileType":{"id":5,"text":"html"}}],"geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -89,41 ], [ -89,42 ], [ -88,42 ], [ -88,41 ], [ -89,41 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae4e4b07f02db689cba","contributors":{"authors":[{"text":"Soong, David T.","contributorId":87487,"corporation":false,"usgs":true,"family":"Soong","given":"David T.","affiliations":[],"preferred":false,"id":287579,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Straub, Timothy D. 0000-0002-5896-0851 tdstraub@usgs.gov","orcid":"https://orcid.org/0000-0002-5896-0851","contributorId":2273,"corporation":false,"usgs":true,"family":"Straub","given":"Timothy D.","email":"tdstraub@usgs.gov","affiliations":[{"id":344,"text":"Illinois Water Science Center","active":true,"usgs":true}],"preferred":false,"id":287577,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Murphy, Elizabeth A.","contributorId":69660,"corporation":false,"usgs":true,"family":"Murphy","given":"Elizabeth A.","affiliations":[],"preferred":false,"id":287578,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":76670,"text":"wdrOH051 - 2006 - Water resources data, Ohio, water year 2005 : Volume 1. Ohio River basin excluding project data","interactions":[],"lastModifiedDate":"2012-03-08T17:16:23","indexId":"wdrOH051","displayToPublicDate":"2006-04-30T00:00:00","publicationYear":"2006","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":340,"text":"Water Data Report","code":"WDR","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"OH-05-1","title":"Water resources data, Ohio, water year 2005 : Volume 1. Ohio River basin excluding project data","language":"ENGLISH","doi":"10.3133/wdrOH051","usgsCitation":"Mangus, J., and Frum, S., 2006, Water resources data, Ohio, water year 2005 : Volume 1. Ohio River basin excluding project data: U.S. Geological Survey Water Data Report OH-05-1, 325 p., https://doi.org/10.3133/wdrOH051.","productDescription":"325 p.","numberOfPages":"325","temporalStart":"2004-10-01","temporalEnd":"2005-09-30","costCenters":[{"id":513,"text":"Ohio Water Science Center","active":true,"usgs":true}],"links":[{"id":194940,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":7721,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/wdr/2005/wdr-oh-05/","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f5e4b07f02db5f0d27","contributors":{"authors":[{"text":"Mangus, J.P.","contributorId":28301,"corporation":false,"usgs":true,"family":"Mangus","given":"J.P.","email":"","affiliations":[],"preferred":false,"id":287570,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Frum, S.R.","contributorId":84843,"corporation":false,"usgs":true,"family":"Frum","given":"S.R.","email":"","affiliations":[],"preferred":false,"id":287571,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":76669,"text":"sir20065027 - 2006 - Water resources of Carbon County, Wyoming","interactions":[],"lastModifiedDate":"2017-09-20T15:59:12","indexId":"sir20065027","displayToPublicDate":"2006-04-30T00:00:00","publicationYear":"2006","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":334,"text":"Scientific Investigations Report","code":"SIR","onlineIssn":"2328-0328","printIssn":"2328-031X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2006-5027","title":"Water resources of Carbon County, Wyoming","docAbstract":"Carbon County is located in the south-central part of Wyoming and is the third largest county in the State. A study to describe the physical and chemical characteristics of surface-water and ground-water resources in Carbon County was conducted by the U.S. Geological Survey in cooperation with the Wyoming State Engineer's Office. Evaluations of streamflow and stream-water quality were limited to analyses of historical data and descriptions of previous investigations. Surface-water data were not collected as part of the study. Forty-five ground-water-quality samples were collected as part of the study and the results from an additional 618 historical ground-water-quality samples were reviewed. Available hydrogeologic characteristics for various aquifers in hydrogeologic units throughout the county also are described.\r\n\r\nFlow characteristics of streams in Carbon County vary substantially depending on regional and local basin char-acteristics and anthropogenic factors. Precipitation in the county is variable with high mountainous areas receiving several times the annual precipitation of basin lowland areas. For this reason, streams with headwaters in mountainous areas generally are perennial, whereas most streams in the county with headwaters in basin lowland areas are ephemeral, flowing only as a result of regional or local rainfall or snowmelt runoff. Flow characteristics of most perennial streams are altered substantially by diversions and regulation.\r\n\r\nWater-quality characteristics of selected streams in and near Carbon County during water years 1966 through 1986 varied. Concentrations of dissolved constituents and suspended sediment were smallest at sites on streams with headwaters in mountainous areas because of resistant geologic units, large diluting streamflows, and increased vegetative cover compared to sites on streams with headwaters in basin lowlands.\r\n\r\nBoth water-table and artesian conditions occur in aquifers within the county. Shallow ground water is available throughout the county, although much of it is only marginally suitable or is unsuitable for domestic and irrigation uses mainly because of high total dissolved solids (TDS) concentrations. Suitable ground water for livestock use is available in most areas of the county. Ground-water quality tends to deteriorate with increasing distance from recharge areas and with increasing depth below land surface. Ground water from depths greater than a few thousand feet tends to have TDS concentrations that make it moderately saline to briny. In some areas, even shallow ground water is moderately saline. Specific constituents in parts of some aquifers in the county occur in relatively high concentrations when compared to U.S. Environmental Protection Agency drinking-water standards; for example, relatively high concentrations of sulfate, chloride, fluoride, boron, iron, manganese, and radon were found in several aquifers.\r\n\r\nThe estimated mean daily water use in Carbon County in 2000 was about 320 million gallons per day. Water used for irrigation accounted for about 98 percent of this total. About 98 percent of the total water used was supplied by surface water and about 2 percent by ground water. Excluding irrigation, ground water comprised about 78 percent of total water use in Carbon County. Although ground water is used to a much lesser extent than surface water, in many areas of the county it is the only available water source.","language":"ENGLISH","doi":"10.3133/sir20065027","usgsCitation":"Bartos, T.T., Hallberg, L.L., Mason, J., Norris, J.R., and Miller, K.A., 2006, Water resources of Carbon County, Wyoming: U.S. Geological Survey Scientific Investigations Report 2006-5027, ix, 191 p., https://doi.org/10.3133/sir20065027.","productDescription":"ix, 191 p.","numberOfPages":"200","costCenters":[{"id":684,"text":"Wyoming Water Science Center","active":false,"usgs":true},{"id":5050,"text":"WY-MT Water Science Center","active":true,"usgs":true}],"links":[{"id":7720,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/sir/2006/5027/","linkFileType":{"id":5,"text":"html"}},{"id":194897,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -108,41 ], [ -108,42.833333333333336 ], [ -106,42.833333333333336 ], [ -106,41 ], [ -108,41 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f8e4b07f02db5f2bd9","contributors":{"authors":[{"text":"Bartos, Timothy T. 0000-0003-1803-4375 ttbartos@usgs.gov","orcid":"https://orcid.org/0000-0003-1803-4375","contributorId":1826,"corporation":false,"usgs":true,"family":"Bartos","given":"Timothy","email":"ttbartos@usgs.gov","middleInitial":"T.","affiliations":[{"id":685,"text":"Wyoming-Montana Water Science Center","active":false,"usgs":true}],"preferred":true,"id":287566,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hallberg, Laura L. 0000-0001-9983-8003 lhallber@usgs.gov","orcid":"https://orcid.org/0000-0001-9983-8003","contributorId":1825,"corporation":false,"usgs":true,"family":"Hallberg","given":"Laura","email":"lhallber@usgs.gov","middleInitial":"L.","affiliations":[{"id":5050,"text":"WY-MT Water Science Center","active":true,"usgs":true}],"preferred":true,"id":287565,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Mason, Jon P.","contributorId":26758,"corporation":false,"usgs":true,"family":"Mason","given":"Jon P.","affiliations":[],"preferred":false,"id":287568,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Norris, Jodi R.","contributorId":43746,"corporation":false,"usgs":true,"family":"Norris","given":"Jodi","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":287569,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Miller, Kirk A. 0000-0002-8141-2001 kmiller@usgs.gov","orcid":"https://orcid.org/0000-0002-8141-2001","contributorId":3959,"corporation":false,"usgs":true,"family":"Miller","given":"Kirk","email":"kmiller@usgs.gov","middleInitial":"A.","affiliations":[{"id":5050,"text":"WY-MT Water Science Center","active":true,"usgs":true}],"preferred":true,"id":287567,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":76664,"text":"ofr20061043 - 2006 - Chlorophyll a and inorganic suspended solids in backwaters of the upper Mississippi River system: Backwater lake effects and their associations with selected environmental predictors","interactions":[],"lastModifiedDate":"2012-02-02T00:14:23","indexId":"ofr20061043","displayToPublicDate":"2006-04-28T00:00:00","publicationYear":"2006","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2006-1043","title":"Chlorophyll a and inorganic suspended solids in backwaters of the upper Mississippi River system: Backwater lake effects and their associations with selected environmental predictors","docAbstract":"The Long Term Resource Monitoring Program (LTRMP) uses a stratified random sampling design to obtain water quality statistics within selected study reaches of the Upper Mississippi River System (UMRS). LTRMP sampling strata are based on aquatic area types generally found in large rivers (e.g., main channel, side channel, backwater, and impounded areas). For hydrologically well-mixed strata (i.e., main channel), variance associated with spatial scales smaller than the strata scale is a relatively minor issue for many water quality parameters. However, analysis of LTRMP water quality data has shown that within-strata variability at the strata scale is high in off-channel areas (i.e., backwaters). A portion of that variability may be associated with differences among individual backwater lakes (i.e., small and large backwater regions separated by channels) that cumulatively make up the backwater stratum. The objective of the statistical modeling presented here is to determine if differences among backwater lakes account for a large portion of the variance observed in the backwater stratum for selected parameters. If variance associated with backwater lakes is high, then inclusion of backwater lake effects within statistical models is warranted. Further, lakes themselves may represent natural experimental units where associations of interest to management may be estimated.","language":"ENGLISH","doi":"10.3133/ofr20061043","collaboration":"Product of the Long Term Resource Monitoring Program","usgsCitation":"Rogala, J.T., and Gray, B.R., 2006, Chlorophyll a and inorganic suspended solids in backwaters of the upper Mississippi River system: Backwater lake effects and their associations with selected environmental predictors: U.S. Geological Survey Open-File Report 2006-1043, 2 p.: ill., https://doi.org/10.3133/ofr20061043.","productDescription":"2 p.: ill.","startPage":"0","endPage":"2","numberOfPages":"2","costCenters":[{"id":606,"text":"Upper Midwest Environmental Sciences Center","active":true,"usgs":true}],"links":[{"id":195696,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":7714,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2006/1043/","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49dde4b07f02db5e252c","contributors":{"authors":[{"text":"Rogala, James T. 0000-0002-1954-4097 jrogala@usgs.gov","orcid":"https://orcid.org/0000-0002-1954-4097","contributorId":2651,"corporation":false,"usgs":true,"family":"Rogala","given":"James","email":"jrogala@usgs.gov","middleInitial":"T.","affiliations":[{"id":606,"text":"Upper Midwest Environmental Sciences Center","active":true,"usgs":true}],"preferred":true,"id":287553,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Gray, Brian R. 0000-0001-7682-9550 brgray@usgs.gov","orcid":"https://orcid.org/0000-0001-7682-9550","contributorId":2615,"corporation":false,"usgs":true,"family":"Gray","given":"Brian","email":"brgray@usgs.gov","middleInitial":"R.","affiliations":[{"id":606,"text":"Upper Midwest Environmental Sciences Center","active":true,"usgs":true}],"preferred":true,"id":287552,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":76665,"text":"ofr20061086 - 2006 - EMMMA: A web-based system for environmental mercury mapping, modeling, and analysis","interactions":[],"lastModifiedDate":"2012-04-15T17:28:14","indexId":"ofr20061086","displayToPublicDate":"2006-04-28T00:00:00","publicationYear":"2006","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2006-1086","title":"EMMMA: A web-based system for environmental mercury mapping, modeling, and analysis","docAbstract":"Mercury in our environment - in our air, water, soil, and especially our food - poses significant hazards to human health, particularly for developing fetuses and young children. Because of the importance of this issue and the length of time it has been studied, large and complex data sets of mercury concentrations in various media and associated ancillary data have been generated by many Federal, State, Tribal, and local agencies. To facilitate efficient and effective use of these\ndata in managing and mitigating human and wildlife exposure to mercury, the U.S. Geological Survey (USGS) and the National Institute of Environmental Health Sciences have developed a website for visualizing and studying the distribution of mercury in our environment. The Environmental Mercury Mapping, Modeling, and Analysis (EMMMA) website (http://emmma.usgs.gov) provides health and environmental researchers, managers, and other decision-makers the ability to: 1) Interactively view and access a nationwide collection of environmental mercury data (fish\ntissue, atmospheric emissions and deposition, stream sediments, soils, and coal) and mercuryrelated data (mine locations); 2) Interactively view and access predictions of the National Descriptive Model of Mercury in Fish (NDMMF) at 4,976 sites and 6,829 sampling events (events are unique combinations of site and sampling date) across the United States; and 3) Use interactive mapping and graphing capabilities to visualize spatial and temporal trends and study relationships between mercury and other variables.","language":"ENGLISH","doi":"10.3133/ofr20061086","usgsCitation":"Hearn, Wente, S.P., Donato, D.I., and Aguinaldo, J.J., 2006, EMMMA: A web-based system for environmental mercury mapping, modeling, and analysis: U.S. Geological Survey Open-File Report 2006-1086, 17 p., https://doi.org/10.3133/ofr20061086.","productDescription":"17 p.","numberOfPages":"17","costCenters":[{"id":247,"text":"Eastern Region Geography","active":false,"usgs":true}],"links":[{"id":191252,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":7715,"rank":300,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2006/1086/","size":"150000","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a54e4b07f02db62c30c","contributors":{"authors":[{"text":"Hearn, Jr. phearn@usgs.gov","contributorId":1950,"corporation":false,"usgs":true,"family":"Hearn","suffix":"Jr.","email":"phearn@usgs.gov","affiliations":[{"id":242,"text":"Eastern Geographic Science Center","active":true,"usgs":true}],"preferred":false,"id":287554,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Wente, Stephen P.","contributorId":75226,"corporation":false,"usgs":true,"family":"Wente","given":"Stephen","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":287557,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Donato, David I. 0000-0002-5412-0249 didonato@usgs.gov","orcid":"https://orcid.org/0000-0002-5412-0249","contributorId":2234,"corporation":false,"usgs":true,"family":"Donato","given":"David","email":"didonato@usgs.gov","middleInitial":"I.","affiliations":[{"id":242,"text":"Eastern Geographic Science Center","active":true,"usgs":true}],"preferred":true,"id":287555,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Aguinaldo, John J.","contributorId":73287,"corporation":false,"usgs":true,"family":"Aguinaldo","given":"John","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":287556,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":76660,"text":"ofr20061095 - 2006 - U.S. Geological Survey and Afghanistan Ministry of Mines and Industry cooperative assessment of Afghanistan's undiscovered oil and gas","interactions":[],"lastModifiedDate":"2021-09-28T16:02:07.790091","indexId":"ofr20061095","displayToPublicDate":"2006-04-28T00:00:00","publicationYear":"2006","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2006-1095","title":"U.S. Geological Survey and Afghanistan Ministry of Mines and Industry cooperative assessment of Afghanistan's undiscovered oil and gas","docAbstract":"<p>Results of the U.S. Geological Survey and Afghanistan Ministry of Mines and Industry cooperative assessment of undiscovered petroleum resources of northern Afghanistan were first released through this presentation on March 14, 2006, at the Afghan Embassy in Washington, D.C. On March 15 the results were presented in Kabul, Afghanistan. The purpose of the assessment and release of the results is to provide energy data required to implement the rebuilding and development of Afghanistan's energy infrastructure. This presentation includes a summary of the goals, process, methodology, results, and accomplishments of the assessment. It provides context for Fact Sheet 2006-3031, a summary of assessment results provided in the presentations.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr20061095","usgsCitation":"Wandrey, C.J., Ulmishek, G., Agena, W., Klett, T., and Afghanistan Oil and Gas Research Assessment Team, 2006, U.S. Geological Survey and Afghanistan Ministry of Mines and Industry cooperative assessment of Afghanistan's undiscovered oil and gas (Version 1.0): U.S. Geological Survey Open-File Report 2006-1095, 21 p., https://doi.org/10.3133/ofr20061095.","productDescription":"21 p.","numberOfPages":"21","onlineOnly":"Y","additionalOnlineFiles":"N","costCenters":[{"id":164,"text":"Central Energy Resources Science Center","active":true,"usgs":true}],"links":[{"id":191201,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ofr20061095.gif"},{"id":7708,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2006/1095/","linkFileType":{"id":5,"text":"html"}},{"id":300260,"rank":101,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/2006/1095/pdf/of-2006-1095.pdf","text":"Report","size":"4.5 MB","linkFileType":{"id":1,"text":"pdf"},"description":"Report"}],"country":"Afghanistan","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"Polygon\",\"coordinates\":[[[61.21082,35.65007],[62.23065,35.27066],[62.98466,35.40404],[63.19354,35.85717],[63.9829,36.00796],[64.54648,36.31207],[64.74611,37.11182],[65.58895,37.30522],[65.74563,37.66116],[66.21738,37.39379],[66.51861,37.36278],[67.07578,37.35614],[67.83,37.14499],[68.13556,37.02312],[68.85945,37.34434],[69.19627,37.15114],[69.51879,37.609],[70.11658,37.58822],[70.27057,37.73516],[70.3763,38.1384],[70.80682,38.48628],[71.34813,38.25891],[71.2394,37.95327],[71.54192,37.90577],[71.44869,37.06564],[71.84464,36.73817],[72.19304,36.94829],[72.63689,37.04756],[73.26006,37.49526],[73.9487,37.42157],[74.98,37.41999],[75.15803,37.13303],[74.57589,37.02084],[74.06755,36.83618],[72.92002,36.72001],[71.84629,36.50994],[71.26235,36.07439],[71.49877,35.65056],[71.61308,35.1532],[71.11502,34.73313],[71.15677,34.34891],[70.8818,33.98886],[69.93054,34.02012],[70.32359,33.35853],[69.68715,33.1055],[69.26252,32.50194],[69.31776,31.90141],[68.92668,31.62019],[68.55693,31.71331],[67.79269,31.58293],[67.68339,31.30315],[66.93889,31.30491],[66.38146,30.7389],[66.34647,29.88794],[65.04686,29.47218],[64.35042,29.56003],[64.148,29.34082],[63.55026,29.46833],[62.54986,29.31857],[60.87425,29.82924],[61.78122,30.73585],[61.69931,31.37951],[60.94194,31.54807],[60.86365,32.18292],[60.53608,32.98127],[60.9637,33.52883],[60.52843,33.67645],[60.80319,34.4041],[61.21082,35.65007]]]},\"properties\":{\"name\":\"Afghanistan\"}}]}","edition":"Version 1.0","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a2be4b07f02db612f7b","contributors":{"authors":[{"text":"Wandrey, Craig J. cwandrey@usgs.gov","contributorId":1590,"corporation":false,"usgs":true,"family":"Wandrey","given":"Craig","email":"cwandrey@usgs.gov","middleInitial":"J.","affiliations":[{"id":164,"text":"Central Energy Resources Science Center","active":true,"usgs":true}],"preferred":true,"id":287536,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Ulmishek, Gregory","contributorId":88361,"corporation":false,"usgs":true,"family":"Ulmishek","given":"Gregory","email":"","affiliations":[],"preferred":false,"id":287539,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Agena, Warren","contributorId":35001,"corporation":false,"usgs":true,"family":"Agena","given":"Warren","email":"","affiliations":[],"preferred":false,"id":287538,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Klett, Timothy R. 0000-0001-9779-1168 tklett@usgs.gov","orcid":"https://orcid.org/0000-0001-9779-1168","contributorId":709,"corporation":false,"usgs":true,"family":"Klett","given":"Timothy R.","email":"tklett@usgs.gov","affiliations":[{"id":164,"text":"Central Energy Resources Science Center","active":true,"usgs":true}],"preferred":false,"id":287535,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Afghanistan Oil and Gas Research Assessment Team","contributorId":127980,"corporation":true,"usgs":false,"organization":"Afghanistan Oil and Gas Research Assessment Team","id":534783,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":76661,"text":"tm1D3 - 2006 - Guidelines and standard procedures for continuous water-quality monitors: Station operation, record computation, and data reporting","interactions":[{"subject":{"id":25562,"text":"wri004252 - 2000 - Guidelines and standard procedures for continuous water-quality monitors: Site selection, field operation, calibration, record computation, and reporting","indexId":"wri004252","publicationYear":"2000","noYear":false,"title":"Guidelines and standard procedures for continuous water-quality monitors: Site selection, field operation, calibration, record computation, and reporting"},"predicate":"SUPERSEDED_BY","object":{"id":76661,"text":"tm1D3 - 2006 - Guidelines and standard procedures for continuous water-quality monitors: Station operation, record computation, and data reporting","indexId":"tm1D3","publicationYear":"2006","noYear":false,"title":"Guidelines and standard procedures for continuous water-quality monitors: Station operation, record computation, and data reporting"},"id":1}],"lastModifiedDate":"2012-02-02T00:13:57","indexId":"tm1D3","displayToPublicDate":"2006-04-28T00:00:00","publicationYear":"2006","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":335,"text":"Techniques and Methods","code":"TM","onlineIssn":"2328-7055","printIssn":"2328-7047","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"1-D3","title":"Guidelines and standard procedures for continuous water-quality monitors: Station operation, record computation, and data reporting","docAbstract":"The U.S. Geological Survey uses continuous water-quality monitors to assess the quality of the Nation's surface water. A common monitoring-system configuration for water-quality data collection is the four-parameter monitoring system, which collects temperature, specific conductance, dissolved oxygen, and pH data. Such systems also can be configured to measure other properties, such as turbidity or fluorescence. Data from sensors can be used in conjunction with chemical analyses of samples to estimate chemical loads. The sensors that are used to measure water-quality field parameters require careful field observation, cleaning, and calibration procedures, as well as thorough procedures for the computation and publication of final records. This report provides guidelines for site- and monitor-selection considerations; sensor inspection and calibration methods; field procedures; data evaluation, correction, and computation; and record-review and data-reporting processes, which supersede the guidelines presented previously in\r\nU.S. Geological Survey Water-Resources Investigations Report WRIR 00-4252. These procedures have evolved over the past three decades, and the process continues to evolve with newer technologies.","language":"ENGLISH","doi":"10.3133/tm1D3","collaboration":"This document supersedes WRI 00-4252","usgsCitation":"Wagner, R.J., Boulger, R.W., Oblinger, C.J., and Smith, B.A., 2006, Guidelines and standard procedures for continuous water-quality monitors: Station operation, record computation, and data reporting (Version 1.0): U.S. Geological Survey Techniques and Methods 1-D3, Variously paginated in 7 sections [51 p. plus 8 attachments], https://doi.org/10.3133/tm1D3.","productDescription":"Variously paginated in 7 sections [51 p. plus 8 attachments]","costCenters":[],"links":[{"id":124882,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/tm_1_d3.jpg"},{"id":7709,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/tm/2006/tm1D3/","linkFileType":{"id":5,"text":"html"}}],"edition":"Version 1.0","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a81e4b07f02db64a370","contributors":{"authors":[{"text":"Wagner, Richard J. rjwagner@usgs.gov","contributorId":3122,"corporation":false,"usgs":true,"family":"Wagner","given":"Richard","email":"rjwagner@usgs.gov","middleInitial":"J.","affiliations":[{"id":622,"text":"Washington Water Science Center","active":true,"usgs":true}],"preferred":true,"id":287540,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Boulger, Robert W. Jr.","contributorId":43051,"corporation":false,"usgs":true,"family":"Boulger","given":"Robert","suffix":"Jr.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":287542,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Oblinger, Carolyn J. 0000-0003-2914-1643 oblinger@usgs.gov","orcid":"https://orcid.org/0000-0003-2914-1643","contributorId":13275,"corporation":false,"usgs":true,"family":"Oblinger","given":"Carolyn","email":"oblinger@usgs.gov","middleInitial":"J.","affiliations":[],"preferred":false,"id":287541,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Smith, Brett A.","contributorId":78022,"corporation":false,"usgs":true,"family":"Smith","given":"Brett","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":287543,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":76663,"text":"ofr20061055 - 2006 - Micropaleontology of selected wells and seismic shot holes, northern Alaska","interactions":[],"lastModifiedDate":"2012-02-10T00:11:36","indexId":"ofr20061055","displayToPublicDate":"2006-04-28T00:00:00","publicationYear":"2006","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2006-1055","title":"Micropaleontology of selected wells and seismic shot holes, northern Alaska","docAbstract":"This report provides micropaleontologic data (foraminifera, pollen, spores, and\r\nmicroplankton) and interpretations of the rocks penetrated by 49 wells and 3,134 seismic shot holes distributed among 73 seismic lines (figs. 1, 2; table 1). All shot holes and 30 wells are located within the National Petroleum Reserve in Alaska (NPRA); the remaining 19 wells are located adjacent to the NPRA. The biostratigraphic zonation scheme, stratigraphy, and geologic ages followed in this study are summarized in figure 3. This update brings paleontologic analyses performed at various times over several decades to a current, unified set of interpretations that benefit from the evolution of northern Alaska biostratigraphic understanding developed during the past 33-years by Mickey and Haga. For each well, paleontologic information includes microfossil distribution charts, data spreadsheets, diversity graphs, and interpretive reports describing age and environments of deposition. Three biostratigraphic well-correlation sections that relate Chukchi Sea wells to onshore northwestern NPRA wells are also included. For all analyzed seismic shot hole samples, foraminiferal age and environmental interpretations are provided; palynological interpretations are provided only for those shot hole samples collected and analyzed after 1976, a little less than half of the total number of samples.","language":"ENGLISH","doi":"10.3133/ofr20061055","usgsCitation":"Mickey, M.B., Haga, H., and Bird, K.J., 2006, Micropaleontology of selected wells and seismic shot holes, northern Alaska (Version 1.0): U.S. Geological Survey Open-File Report 2006-1055, 11 p.; 3 plates; data files, https://doi.org/10.3133/ofr20061055.","productDescription":"11 p.; 3 plates; data files","numberOfPages":"11","additionalOnlineFiles":"Y","costCenters":[{"id":255,"text":"Energy Resources Program","active":true,"usgs":true}],"links":[{"id":191251,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":7713,"rank":9999,"type":{"id":25,"text":"Version History"},"url":"https://pubs.usgs.gov/of/2006/1055/version_history.txt","linkFileType":{"id":2,"text":"txt"}},{"id":7712,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2006/1055/","linkFileType":{"id":5,"text":"html"}}],"geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -165,68 ], [ -165,72 ], [ -150,72 ], [ -150,68 ], [ -165,68 ] ] ] } } ] }","edition":"Version 1.0","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a57e4b07f02db62e4eb","contributors":{"authors":[{"text":"Mickey, Michael B.","contributorId":9656,"corporation":false,"usgs":true,"family":"Mickey","given":"Michael","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":287550,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Haga, Hideyo","contributorId":10805,"corporation":false,"usgs":true,"family":"Haga","given":"Hideyo","email":"","affiliations":[],"preferred":false,"id":287551,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Bird, Kenneth J. kbird@usgs.gov","contributorId":1015,"corporation":false,"usgs":true,"family":"Bird","given":"Kenneth","email":"kbird@usgs.gov","middleInitial":"J.","affiliations":[{"id":255,"text":"Energy Resources Program","active":true,"usgs":true}],"preferred":true,"id":287549,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":76650,"text":"ofr20061090 - 2006 - Preliminary surficial geologic map of a Calico Mountains piedmont and part of Coyote Lake, Mojave desert, San Bernardino County, California","interactions":[],"lastModifiedDate":"2012-02-10T00:11:44","indexId":"ofr20061090","displayToPublicDate":"2006-04-26T00:00:00","publicationYear":"2006","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2006-1090","title":"Preliminary surficial geologic map of a Calico Mountains piedmont and part of Coyote Lake, Mojave desert, San Bernardino County, California","docAbstract":"This 1:24,000 scale detailed surficial geologic map and digital database of a Calico Mountains piedmont and part of Coyote Lake in south-central California depicts surficial deposits and generalized bedrock units. The mapping is part of a USGS project to investigate the spatial distribution of deposits linked to changes in climate, to provide framework geology for land use management (http://deserts.wr.usgs.gov), to understand the Quaternary tectonic history of the Mojave Desert, and to provide additional information on the history of Lake Manix, of which Coyote Lake is a sub-basin. Mapping is displayed on parts of four USGS 7.5 minute series topographic maps. The map area lies in the central Mojave Desert of California, northeast of Barstow, Calif. and south of Fort Irwin, Calif. and covers 258 sq.km. (99.5 sq.mi.). Geologic deposits in the area consist of Paleozoic metamorphic rocks, Mesozoic plutonic rocks, Miocene volcanic rocks, Pliocene-Pleistocene basin fill, and Quaternary surficial deposits. McCulloh (1960, 1965) conducted bedrock mapping and a generalized version of his maps are compiled into this map. McCulloh's maps contain many bedrock structures within the Calico Mountains that are not shown on the present map.\r\n\r\nThis study resulted in several new findings, including the discovery of previously unrecognized faults, one of which is the Tin Can Alley fault. The north-striking Tin Can Alley fault is part of the Paradise fault zone (Miller and others, 2005), a potentially important feature for studying neo-tectonic strain in the Mojave Desert. Additionally, many Anodonta shells were collected in Coyote Lake lacustrine sediments for radiocarbon dating. Preliminary results support some of Meek's (1999) conclusions on the timing of Mojave River inflow into the Coyote Basin.\r\n\r\nThe database includes information on geologic deposits, samples, and geochronology. The database is distributed in three parts: spatial map-based data, documentation, and printable map graphics of the database. Spatial data are distributed as an ArcInfo personal geodatabase, or as tabular data in the form of Microsoft Access Database (MDB) or dBase Format (DBF) file formats. Documentation includes this file, which provides a discussion of the surficial geology and describes the format and content of the map data, and Federal Geographic Data Committee (FGDC) metadata for the spatial map information. Map graphics files are distributed as Postscript and Adobe Acrobat Portable Document Format (PDF) files, and are appropriate for representing a view of the spatial database at the mapped scale. ","language":"ENGLISH","doi":"10.3133/ofr20061090","collaboration":"Map available through USGS Map on Demand at: http://store.usgs.gov/mod/","usgsCitation":"Dudash, S.L., 2006, Preliminary surficial geologic map of a Calico Mountains piedmont and part of Coyote Lake, Mojave desert, San Bernardino County, California: U.S. Geological Survey Open-File Report 2006-1090, 48 p. pamphlet; 1 map sheet, 52 x 31 in.; GIS files, https://doi.org/10.3133/ofr20061090.","productDescription":"48 p. pamphlet; 1 map sheet, 52 x 31 in.; GIS files","numberOfPages":"48","additionalOnlineFiles":"Y","costCenters":[{"id":647,"text":"Western Earth Surface Processes","active":false,"usgs":true}],"links":[{"id":110641,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_76419.htm","linkFileType":{"id":5,"text":"html"},"description":"76419"},{"id":194402,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":7703,"rank":9999,"type":{"id":25,"text":"Version History"},"url":"https://pubs.usgs.gov/of/2006/1090/version_history.txt","linkFileType":{"id":2,"text":"txt"}},{"id":7704,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/2006/1090/Plot_file/of06-1090_3a.pdf","size":"1887436","linkFileType":{"id":1,"text":"pdf"}},{"id":7702,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2006/1090/","linkFileType":{"id":5,"text":"html"}}],"scale":"24000","projection":"Universal Transverse Mercator, NAD83","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -116.85,34.96666666666667 ], [ -116.85,35.083333333333336 ], [ -116.68333333333334,35.083333333333336 ], [ -116.68333333333334,34.96666666666667 ], [ -116.85,34.96666666666667 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aabe4b07f02db669aab","contributors":{"authors":[{"text":"Dudash, Stephanie L.","contributorId":90839,"corporation":false,"usgs":true,"family":"Dudash","given":"Stephanie","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":287504,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":76644,"text":"sir20065021 - 2006 - Status of water levels and selected water-quality conditions in the Sparta-Memphis aquifer in Arkansas, Spring-Summer 2003","interactions":[],"lastModifiedDate":"2012-02-10T00:11:41","indexId":"sir20065021","displayToPublicDate":"2006-04-26T00:00:00","publicationYear":"2006","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":334,"text":"Scientific Investigations Report","code":"SIR","onlineIssn":"2328-0328","printIssn":"2328-031X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2006-5021","title":"Status of water levels and selected water-quality conditions in the Sparta-Memphis aquifer in Arkansas, Spring-Summer 2003","docAbstract":"During the spring of 2003, water levels were measured in 341 wells in the Sparta-Memphis aquifer in Arkansas. Waterquality samples were collected for temperature and specificconductance measurements during the spring-summer of 2003 from 70 wells in Arkansas in the Sparta-Memphis aquifer. Maps of areal distribution of potentiometric surface, change in waterlevel measurements from 1999 to 2003, and specific-conductance data reveal spatial trends across the study area. The highest water-level altitude measured in Arkansas was 328 feet above National Geodetic Vertical Datum of 1929 (NGVD of 1929) in Craighead County; the lowest water-level altitude was 199 feet below NGVD of 1929 in Union County.\r\n\r\nThree large cones of depression are shown in the 2003 potentiometric surface map, centered in Columbia, Jefferson, and Union Counties in Arkansas as a result of large withdrawals for industrial and public supplies. A broad depression exists in western Poinsett County in Arkansas. The potentiometric surface indicates that large withdrawals have altered or reversed the natural direction of flow in most areas. In the northern third of the study area the flow is from the east, west, and north towards the broad depression in Poinsett County. In the central third of the study area the flow is dominated by the cone of depression centered in Jefferson County. In the southern third of the study area the flow is dominated by the two cones of depression in Union and Columbia Counties.\r\n\r\nA map of water-level changes from 1999 to 2003 was constructed using water-level measurements from 281 wells. The largest rise in water level measured was about 57.8 feet in Columbia County. The largest decline in water level measured was about -71.6 feet in Columbia County. Areas with a general rise are shown in Arkansas, Bradley, Calhoun, Cleveland, Columbia, Ouachita, and Union Counties. Areas with a general decline are shown in Craighead, Crittenden, Cross, Desha, Drew, Jefferson, Lonoke, Phillips, Poinsett, Prairie, and Woodruff Counties.\r\n\r\nHydrographs were constructed for wells with a minimum of 25 years of water-level measurements. A trend line using a linear regression was calculated for the period of record from spring of 1978 to spring of 2003 to determine the annual decline or rise in feet per year for water levels in each well. The hydrographs were grouped by county. The mean values for county annual water-level decline or rise ranged from -1.42 to 0.27 foot per year.\r\n\r\nSpecific conductance ranged from 82 microsiemens per centimeter at 25 degrees Celsius in Jefferson County to about 1,210 microsiemens per centimeter at 25 degrees Celsius in Lee County. The mean specific conductance was 400 microsiemens per centimeter at 25 degrees Celsius.","language":"ENGLISH","doi":"10.3133/sir20065021","usgsCitation":"Schrader, T., 2006, Status of water levels and selected water-quality conditions in the Sparta-Memphis aquifer in Arkansas, Spring-Summer 2003: U.S. Geological Survey Scientific Investigations Report 2006-5021, 43 p.: ill.; 2 plates, 34 x 44 in., https://doi.org/10.3133/sir20065021.","productDescription":"43 p.: ill.; 2 plates, 34 x 44 in.","numberOfPages":"43","temporalStart":"2003-03-01","temporalEnd":"2003-08-31","costCenters":[{"id":129,"text":"Arkansas Water Science Center","active":true,"usgs":true}],"links":[{"id":190936,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":7690,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/sir/2006/5021/","linkFileType":{"id":5,"text":"html"}}],"geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -94.83333333333333,33 ], [ -94.83333333333333,36.833333333333336 ], [ -89.83333333333333,36.833333333333336 ], [ -89.83333333333333,33 ], [ -94.83333333333333,33 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b32e4b07f02db6b48fc","contributors":{"authors":[{"text":"Schrader, T.P.","contributorId":56300,"corporation":false,"usgs":true,"family":"Schrader","given":"T.P.","email":"","affiliations":[],"preferred":false,"id":287486,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":76641,"text":"fs20053126 - 2006 - The U.S. Geological Survey and City of Atlanta water-quality and water-quantity monitoring network","interactions":[],"lastModifiedDate":"2017-02-03T12:06:51","indexId":"fs20053126","displayToPublicDate":"2006-04-26T00:00:00","publicationYear":"2006","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":313,"text":"Fact Sheet","code":"FS","onlineIssn":"2327-6932","printIssn":"2327-6916","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2005-3126","title":"The U.S. Geological Survey and City of Atlanta water-quality and water-quantity monitoring network","docAbstract":"Population growth and urbanization affect the landscape, and the quality and quantity of water in nearby rivers and streams, as well as downstream receiving waters (Ellis, 1999). Typical impacts include: (1) disruption of the hydrologic cycle through increases in the extent of impervious surfaces (e.g., roads, roofs, sidewalks) that increase the velocity and volume of surface-water runoff; (2) increased chemical loads to local and downstream receiving waters from industrial sources, nonpoint-source runoff, leaking sewer systems, and sewer overflows; (3) direct or indirect soil contamination from industrial sources, power-generating facilities, and landfills; and (4) reduction in the quantity and quality of aquatic habitats.\r\n\r\nThe City of Atlanta's monitoring network consists of 21 long-term sites. Eleven of these are 'fully instrumented' to provide real-time data on water temperature, pH, specific conductance, dissolved oxygen, turbidity (intended as a surrogate for suspended sediment concentration), water level (gage height, intended as a surrogate for discharge), and precipitation. Data are transmitted hourly and are available on a public Web site (http://ga.water.usgs.gov/). Two sites only measure water level and rainfall as an aid to stormwater monitoring. The eight remaining sites are used to assess water quality.","language":"ENGLISH","doi":"10.3133/fs20053126","usgsCitation":"Horowitz, A.J., and Hughes, W.B., 2006, The U.S. Geological Survey and City of Atlanta water-quality and water-quantity monitoring network: U.S. Geological Survey Fact Sheet 2005-3126, 4 p., https://doi.org/10.3133/fs20053126.","productDescription":"4 p.","numberOfPages":"4","costCenters":[{"id":13634,"text":"South Atlantic Water Science Center","active":true,"usgs":true}],"links":[{"id":123091,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/fs_2005_3126.jpg"},{"id":7686,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/fs/2005/3126/","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Georgia","city":"Atlanta","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -87,30 ], [ -87,37 ], [ -83,37 ], [ -83,30 ], [ -87,30 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4abce4b07f02db6731ed","contributors":{"authors":[{"text":"Horowitz, Arthur J. 0000-0002-3296-730X horowitz@usgs.gov","orcid":"https://orcid.org/0000-0002-3296-730X","contributorId":1400,"corporation":false,"usgs":true,"family":"Horowitz","given":"Arthur","email":"horowitz@usgs.gov","middleInitial":"J.","affiliations":[{"id":316,"text":"Georgia Water Science Center","active":true,"usgs":true},{"id":13634,"text":"South Atlantic Water Science Center","active":true,"usgs":true}],"preferred":true,"id":287480,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hughes, W. Brian","contributorId":84353,"corporation":false,"usgs":true,"family":"Hughes","given":"W.","email":"","middleInitial":"Brian","affiliations":[],"preferred":false,"id":287481,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":76649,"text":"sir20065057 - 2006 - A computer program for estimating instream travel times and concentrations of a potential contaminant in the Yellowstone River, Montana","interactions":[],"lastModifiedDate":"2012-03-08T17:16:20","indexId":"sir20065057","displayToPublicDate":"2006-04-26T00:00:00","publicationYear":"2006","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":334,"text":"Scientific Investigations Report","code":"SIR","onlineIssn":"2328-0328","printIssn":"2328-031X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2006-5057","title":"A computer program for estimating instream travel times and concentrations of a potential contaminant in the Yellowstone River, Montana","docAbstract":"The Yellowstone River is very important in a variety of ways to the residents of southeastern Montana; however, it is especially vulnerable to spilled contaminants. In 2004, the U.S. Geological Survey, in cooperation with Montana Department of Environmental Quality, initiated a study to develop a computer program to rapidly estimate instream travel times and concentrations of a potential contaminant in the Yellowstone River using regression equations developed in 1999 by the U.S. Geological Survey. The purpose of this report is to describe these equations and their limitations, describe the development of a computer program to apply the equations to the Yellowstone River, and provide detailed instructions on how to use the program. This program is available online at [http://pubs.water.usgs.gov/sir2006-5057/includes/ytot.xls].\r\n\r\nThe regression equations provide estimates of instream travel times and concentrations in rivers where little or no contaminant-transport data are available. Equations were developed and presented for the most probable flow velocity and the maximum probable flow velocity. These velocity estimates can then be used to calculate instream travel times and concentrations of a potential contaminant.\r\n\r\nThe computer program was developed so estimation equations for instream travel times and concentrations can be solved quickly for sites along the Yellowstone River between Corwin Springs and Sidney, Montana. The basic types of data needed to run the program are spill data, streamflow data, and data for locations of interest along the Yellowstone River. Data output from the program includes spill location, river mileage at specified locations, instantaneous discharge, mean-annual discharge, drainage area, and channel slope. Travel times and concentrations are provided for estimates of the most probable velocity of the peak concentration and the maximum probable velocity of the peak concentration.\r\n\r\nVerification of estimates of instream travel times and concentrations for the Yellowstone River requires information about the flow velocity throughout the 520 mi of river in the study area. Dye-tracer studies would provide the best data about flow velocities and would provide the best verification of instream travel times and concentrations estimated from this computer program; however, data from such studies does not currently (2006) exist and new studies would be expensive and time-consuming. An alternative approach used in this study for verification of instream travel times is based on the use of flood-wave velocities determined from recorded streamflow hydrographs at selected mainstem streamflow-gaging stations along the Yellowstone River. The ratios of flood-wave velocity to the most probable velocity for the base flow estimated from the computer program are within the accepted range of 2.5 to 4.0 and indicate that flow velocities estimated from the computer program are reasonable for the Yellowstone River. The ratios of flood-wave velocity to the maximum probable velocity are within a range of 1.9 to 2.8 and indicate that the maximum probable flow velocities estimated from the computer program, which corresponds to the shortest travel times and maximum probable concentrations, are conservative and reasonable for the Yellowstone River.","language":"ENGLISH","doi":"10.3133/sir20065057","usgsCitation":"McCarthy, P., 2006, A computer program for estimating instream travel times and concentrations of a potential contaminant in the Yellowstone River, Montana: U.S. Geological Survey Scientific Investigations Report 2006-5057, iv, 16 p., https://doi.org/10.3133/sir20065057.","productDescription":"iv, 16 p.","numberOfPages":"20","costCenters":[{"id":400,"text":"Montana Water Science Center","active":false,"usgs":true}],"links":[{"id":126840,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/sir_2006_5057.jpg"},{"id":7701,"rank":9999,"type":{"id":4,"text":"Application Site"},"url":"https://pubs.usgs.gov/sir/2006/5057/includes/ytot.xls"},{"id":7700,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/sir/2006/5057/","linkFileType":{"id":5,"text":"html"}}],"geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -111,45 ], [ -111,48 ], [ -104,48 ], [ -104,45 ], [ -111,45 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b26e4b07f02db6b02b5","contributors":{"authors":[{"text":"McCarthy, Peter 0000-0002-2396-7463 pmccarth@usgs.gov","orcid":"https://orcid.org/0000-0002-2396-7463","contributorId":2504,"corporation":false,"usgs":true,"family":"McCarthy","given":"Peter","email":"pmccarth@usgs.gov","affiliations":[{"id":5050,"text":"WY-MT Water Science Center","active":true,"usgs":true}],"preferred":true,"id":287503,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":76639,"text":"sir20065042 - 2006 - Physical and vegetative characteristics of a relocated stream reach, constructed wetland, and riparian buffer, Upper Saucon Township, Lehigh County, Pennsylvania, 2000-04","interactions":[],"lastModifiedDate":"2017-07-06T15:31:25","indexId":"sir20065042","displayToPublicDate":"2006-04-25T00:00:00","publicationYear":"2006","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":334,"text":"Scientific Investigations Report","code":"SIR","onlineIssn":"2328-0328","printIssn":"2328-031X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2006-5042","title":"Physical and vegetative characteristics of a relocated stream reach, constructed wetland, and riparian buffer, Upper Saucon Township, Lehigh County, Pennsylvania, 2000-04","docAbstract":"<p>The U.S. Geological Survey, in cooperation with the Pennsylvania Department of Transportation, Engineering District 5-0, investigated physical and vegetative changes within a relocated stream reach, constructed wetland, and riparian buffer from September 2000 to October 2004. This report presents an evaluation of data collected using methods from multiple sources that have been adapted into a consistent approach. This approach is intended to satisfy a need for consistent collection of different types of data with the goal of transferring technology and findings to similar projects. </p><p>Survey data indicate that adjustment of the upstream part of the relocated stream reach slowed over the monitoring period, but the downstream channel remains unstable as evidenced by excessive deposition. Upstream migration of a nick point has slowed or stopped altogether as of the 2003 assessment when this feature came in contact with the upstream-most part of the channel that is lined with riprap. Documented streambed erosion in the upstream cross sections, along with deposition downstream, has resulted in an overall decrease in slope of the stream channel over the monitoring period. Most streambed erosion took place prior to the 2002 assessment when annual mean streamflows were less than those in the final 2 years of monitoring. An abundance of fine sediment dominates the substrate of the relocated channel. Annual fluctuations of large particles within each cross section demonstrates the capacity of the relocated channel to transport the entire range of sediment. </p><p>The substrate within the 0.28-acre constructed wetland (a mixture of soil from an off-site naturally occurring wetland and woodchips) supported a hydrophytic-vegetation community throughout the investigation. Eleocharis obtusa (spike rush), an obligate-wetland herb, was the most prevalent species, having a maximum areal cover of 90 percent in fall 2001 and a minimum of 23 percent in fall 2004. Drought-like conditions in water year 2002 (cumulative precipitation was 28.11 inches) allowed species like Panicum dichotomiflorum (witch grass), Salix sp. (willow), Leersia oryzoides (rice cutgrass), and Echinocloa crusgalli (barnyard grass) to become established by fall 2002. Above-average precipitation in water years 2003 and 2004 (58.55 and 53.17 inches, respectively) coincided with increased areal cover by E. obtusa in fall 2003 (56 percent) and decreased areal cover in fall 2004 (23 percent). Pond-like conditions that probably persisted throughout the 2004 growing season favored aquatic species like Alisma subcordatum (water plantain) to the detriment of many emergent species, including E. obtusa. Despite the pond-like conditions, L. oryzoides, an obligate-wetland grass, increased in areal cover (from 12 to 34 percent) between the 2003 and 2004 growing seasons because it was established in the higher elevations and the peripheral areas of the constructed wetland that were less prone to persistent inundation. </p><p>Canopy development by trees and shrubs in the riparian buffer was initially (fall 2000) poor (39.7 percent), resulting in more available sunlight for the herbaceous understory than in any other growing season. As a result, areal cover of herbaceous species and trees and shrubs less than 1-meter tall was 108 percent in fall 2000 with Lolium perenne (perennial rye), Polygonum persicaria (lady's thumb), and Setaria faberi (foxtail) collectively contributing nearly half the cover (59.2 percent). Because of increases in canopy cover by trees and shrubs (39.7 percent in fall 2000 to 127 percent in fall 2004), herbaceous cover decreased to 76 percent by the fall of 2001 and varied between 72 and 77 percent for the rest of the study period. </p><p><br><span>Tree density in the riparian buffer ranged from 3,078 and 4,130 plants per acre (fall 2000 and 2003, respectively) over the study period but essentially remained constant after fall 2001; computations reported each fall between fall 2001 and fall 2004 are within 10 percent of one another. When the study ended in fall 2004,<span>&nbsp;</span></span><i>Acer negundo</i><span><span>&nbsp;</span>(box elder) and<span>&nbsp;</span></span><i>Fraxinus pennsylvanica</i><span><span>&nbsp;</span>(green ash) were the most populous tree species (1,526 and 1,084 plants per acre, respectively) followed by<span>&nbsp;</span></span><i>Quercus bicolor</i><span><span>&nbsp;</span>(swamp white oak; 720 plants per acre).<span>&nbsp;</span></span><i>A. negundo</i><span>,<span>&nbsp;</span></span><i>F. pennsylvanica</i><span>, and<span>&nbsp;</span></span><i>Q. bicolor</i><span><span>&nbsp;</span>also contributed the greatest areal cover in fall 2004 (31.2, 24.0, and 18.5 percent,respectively).<span>&nbsp;</span></span></p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/sir20065042","usgsCitation":"Chaplin, J.J., White, K., and Loper, C.A., 2006, Physical and vegetative characteristics of a relocated stream reach, constructed wetland, and riparian buffer, Upper Saucon Township, Lehigh County, Pennsylvania, 2000-04: U.S. Geological Survey Scientific Investigations Report 2006-5042, viii, 65 p., https://doi.org/10.3133/sir20065042.","productDescription":"viii, 65 p.","onlineOnly":"Y","temporalStart":"2000-01-01","temporalEnd":"2004-12-31","costCenters":[{"id":532,"text":"Pennsylvania Water Science Center","active":true,"usgs":true}],"links":[{"id":192802,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":7684,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/sir/2006/5042/","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Pennsylvania","county":"Lehigh County","city":"Upper Saucon Township","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"Polygon\",\"coordinates\":[[[-75.6107,40.7861],[-75.6079,40.7765],[-75.6064,40.7665],[-75.6037,40.7538],[-75.5996,40.746],[-75.5961,40.741],[-75.5932,40.7378],[-75.589,40.7345],[-75.5866,40.734],[-75.583,40.7344],[-75.5799,40.7348],[-75.5763,40.7352],[-75.5726,40.7338],[-75.5703,40.7311],[-75.5692,40.7283],[-75.5657,40.7237],[-75.559,40.7218],[-75.5548,40.7213],[-75.5499,40.723],[-75.5462,40.7248],[-75.5431,40.7284],[-75.543,40.732],[-75.5404,40.737],[-75.5373,40.7383],[-75.5319,40.7373],[-75.5283,40.7354],[-75.5261,40.7263],[-75.5193,40.7099],[-75.5129,40.7002],[-75.5024,40.6856],[-75.4959,40.6791],[-75.4894,40.6763],[-75.4876,40.6731],[-75.4791,40.6534],[-75.4332,40.6699],[-75.4167,40.6533],[-75.3901,40.6297],[-75.3948,40.5944],[-75.3949,40.5922],[-75.4049,40.581],[-75.3692,40.5586],[-75.3354,40.5372],[-75.3551,40.5239],[-75.3879,40.5018],[-75.3909,40.5],[-75.4008,40.4938],[-75.4026,40.4925],[-75.4094,40.4881],[-75.4113,40.4872],[-75.4454,40.4547],[-75.4492,40.4511],[-75.451,40.4493],[-75.4548,40.4457],[-75.4672,40.4346],[-75.4734,40.4292],[-75.4759,40.4266],[-75.4833,40.4194],[-75.4994,40.4283],[-75.5065,40.4325],[-75.5249,40.4441],[-75.5278,40.4464],[-75.5582,40.4641],[-75.6206,40.5023],[-75.6849,40.544],[-75.6956,40.5505],[-75.7188,40.5654],[-75.7402,40.5802],[-75.7498,40.5862],[-75.7677,40.5974],[-75.7701,40.5992],[-75.7796,40.6052],[-75.8005,40.6182],[-75.89,40.6761],[-75.8509,40.691],[-75.8032,40.709],[-75.7767,40.7236],[-75.7595,40.7333],[-75.7546,40.7351],[-75.7467,40.7382],[-75.7411,40.7412],[-75.733,40.7489],[-75.7281,40.7524],[-75.6993,40.7643],[-75.6943,40.7674],[-75.6857,40.7727],[-75.6821,40.7735],[-75.6656,40.7769],[-75.6277,40.7841],[-75.6107,40.7861]]]},\"properties\":{\"name\":\"Lehigh\",\"state\":\"PA\"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adbe4b07f02db685bf9","contributors":{"authors":[{"text":"Chaplin, Jeffrey J. 0000-0002-0617-5050 jchaplin@usgs.gov","orcid":"https://orcid.org/0000-0002-0617-5050","contributorId":147,"corporation":false,"usgs":true,"family":"Chaplin","given":"Jeffrey","email":"jchaplin@usgs.gov","middleInitial":"J.","affiliations":[{"id":532,"text":"Pennsylvania Water Science Center","active":true,"usgs":true}],"preferred":true,"id":287474,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"White, Kirk E. kewhite@usgs.gov","contributorId":2107,"corporation":false,"usgs":true,"family":"White","given":"Kirk E.","email":"kewhite@usgs.gov","affiliations":[],"preferred":true,"id":287475,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Loper, Connie A.","contributorId":62243,"corporation":false,"usgs":true,"family":"Loper","given":"Connie","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":287476,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":76640,"text":"wdrWI051 - 2006 - Water resources data - Wisconsin, water year 2005","interactions":[],"lastModifiedDate":"2012-03-08T17:16:19","indexId":"wdrWI051","displayToPublicDate":"2006-04-25T00:00:00","publicationYear":"2006","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":340,"text":"Water Data Report","code":"WDR","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"WI-05-1","title":"Water resources data - Wisconsin, water year 2005","docAbstract":"Water-resources data for the 2005 water year for Wisconsin include records of streamflow at gaging stations, partial-record stations, and miscellaneous sites, records of precipitation, and records of chemical, biological, and physical characteristics of surface water. In addition, water levels in observation wells are reported. These data were collected by the U.S. Geological Survey in cooperation with State and local agencies and other Federal agencies in Wisconsin.","language":"ENGLISH","doi":"10.3133/wdrWI051","issn":"07408803","usgsCitation":"Waschbusch, R., Olson, D., and Marsh, S., 2006, Water resources data - Wisconsin, water year 2005: U.S. Geological Survey Water Data Report WI-05-1, 982 p., https://doi.org/10.3133/wdrWI051.","productDescription":"982 p.","numberOfPages":"982","onlineOnly":"N","temporalStart":"2004-10-01","temporalEnd":"2005-09-30","costCenters":[{"id":677,"text":"Wisconsin Water Science Center","active":true,"usgs":true}],"links":[{"id":192803,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":7685,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/wdr/2005/wdr-wi-05-1/","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49bde4b07f02db5d0c49","contributors":{"authors":[{"text":"Waschbusch, R.J.","contributorId":107307,"corporation":false,"usgs":true,"family":"Waschbusch","given":"R.J.","affiliations":[],"preferred":false,"id":287479,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Olson, D.L.","contributorId":34943,"corporation":false,"usgs":true,"family":"Olson","given":"D.L.","email":"","affiliations":[],"preferred":false,"id":287477,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Marsh, S.B.","contributorId":105329,"corporation":false,"usgs":true,"family":"Marsh","given":"S.B.","email":"","affiliations":[],"preferred":false,"id":287478,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":76635,"text":"wdrFL051B - 2006 - Water resources data, Florida, water year 2005. Volume 1B: Northeast Florida ground water","interactions":[],"lastModifiedDate":"2012-02-02T00:14:10","indexId":"wdrFL051B","displayToPublicDate":"2006-04-25T00:00:00","publicationYear":"2006","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":340,"text":"Water Data Report","code":"WDR","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"FL-05-1B","title":"Water resources data, Florida, water year 2005. Volume 1B: Northeast Florida ground water","docAbstract":"Water resources data for the 2005 water year in Florida consist of continuous or daily discharge for 429 streams, periodic discharge for 9 streams, continuous or daily stage for 218 streams, periodic stage for 5 streams, peak stage and discharge for 28 streams; continuous or daily elevations for 15 lakes, periodic elevations for 23 lakes; continuous ground-water levels for 401 wells, periodic ground-water levels for 1,098 wells; quality-of-water data for 211 surface-water sites and 208 wells.The data for northeast Florida include continuous or daily discharge for 140 streams, periodic discharge for 4 streams, continuous or daily stage for 58 streams, periodic stage for 3 streams; peak stage and discharge for 0 streams; continuous or daily elevations for 10 lakes, periodic elevations for 20 lakes; continuous ground water levels for 45 wells, periodic ground-water levels for 520 wells; quality-of-water data for 40 surface-water sites and 65 wells.These data represent the National Water Data System records collected by the U.S. Geological Survey and cooperating local, State and Federal agencies in Florida.","language":"ENGLISH","doi":"10.3133/wdrFL051B","issn":"02752689","usgsCitation":"Nazarian, A., Simonds, E., and Dickerson, S., 2006, Water resources data, Florida, water year 2005. Volume 1B: Northeast Florida ground water: U.S. Geological Survey Water Data Report FL-05-1B, 297 p., https://doi.org/10.3133/wdrFL051B.","productDescription":"297 p.","numberOfPages":"297","temporalStart":"2004-10-01","temporalEnd":"2005-09-30","costCenters":[{"id":285,"text":"Florida Water Science Center","active":false,"usgs":true}],"links":[{"id":192455,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":7679,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/wdr/2005/wdr-fl-05-1b/","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a17e4b07f02db603f06","contributors":{"authors":[{"text":"Nazarian, A.P.","contributorId":32595,"corporation":false,"usgs":true,"family":"Nazarian","given":"A.P.","email":"","affiliations":[],"preferred":false,"id":287469,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Simonds, E.P.","contributorId":31479,"corporation":false,"usgs":true,"family":"Simonds","given":"E.P.","email":"","affiliations":[],"preferred":false,"id":287468,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Dickerson, S.M.","contributorId":26748,"corporation":false,"usgs":true,"family":"Dickerson","given":"S.M.","email":"","affiliations":[],"preferred":false,"id":287467,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
]}