Radon-hazard Potential of the Lower Weber River Area, Tooele Valley, and Southeastern Cache Valley, Cache, Davis, Tooele, and Weber Counties, Utah PDF Download
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Author: Bill D. Black
Publisher: Utah Geological Survey
ISBN: 155791379X
Category : Geology, Structural
Languages : en
Pages : 62
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Book Description
Radon is a radioactive gas of geologic origin that is an environmental concern because of its link to lung cancer. Radon is derived from the decay of uranium, and can accumulate indoors in sufficient quantities to pose a health hazard to building occupants. Although the influence of non-geologic factors such as construction type, lifestyle, and weather is difficult to measure, geologic factors that influence indoor-radon levels can be quantified to assess the hazard potential. Geologic factors that influence indoor-radon levels have been studied for three areas in northern Utah to indicate where indoor radon may be a hazard and radon-resistant techniques should be considered in new construction. The three areas include the lower Weber River area in Davis and Weber Counties, Tooele Valley in Tooele County, and southeastern Cache Valley in Cache County. These areas all lie in the depositional basin of Pleistocene Lake Bonneville, and display common geologic characteristics which affect their potential for radon hazards. A numerical rating system was used to assess and map the relative radon-hazard potential in the three study areas. A high-hazard potential was typically found along range fronts where uranium concentrations are higher, ground water is deep, and soils are permeable. Although soil-gas and indoor-radon concentrations broadly correlate to mapped hazard potential, the correlation is imperfect because of atmospheric contamination of soil-gas samples, the presence of locally anomalous concentrations of radon which are beyond the resolution of the sampling grid or map scale, and the effects of non-geologic factors which are not considered in this geologic assessment. 56 pages + 1 plate
Author: Bill D. Black
Publisher: Utah Geological Survey
ISBN: 155791379X
Category : Geology, Structural
Languages : en
Pages : 62
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Book Description
Radon is a radioactive gas of geologic origin that is an environmental concern because of its link to lung cancer. Radon is derived from the decay of uranium, and can accumulate indoors in sufficient quantities to pose a health hazard to building occupants. Although the influence of non-geologic factors such as construction type, lifestyle, and weather is difficult to measure, geologic factors that influence indoor-radon levels can be quantified to assess the hazard potential. Geologic factors that influence indoor-radon levels have been studied for three areas in northern Utah to indicate where indoor radon may be a hazard and radon-resistant techniques should be considered in new construction. The three areas include the lower Weber River area in Davis and Weber Counties, Tooele Valley in Tooele County, and southeastern Cache Valley in Cache County. These areas all lie in the depositional basin of Pleistocene Lake Bonneville, and display common geologic characteristics which affect their potential for radon hazards. A numerical rating system was used to assess and map the relative radon-hazard potential in the three study areas. A high-hazard potential was typically found along range fronts where uranium concentrations are higher, ground water is deep, and soils are permeable. Although soil-gas and indoor-radon concentrations broadly correlate to mapped hazard potential, the correlation is imperfect because of atmospheric contamination of soil-gas samples, the presence of locally anomalous concentrations of radon which are beyond the resolution of the sampling grid or map scale, and the effects of non-geologic factors which are not considered in this geologic assessment. 56 pages + 1 plate
Author: Charles E. Bishop
Publisher: Utah Geological Survey
ISBN: 1557916160
Category : Geology, Structural
Languages : en
Pages : 43
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Book Description
Indoor-radon levels in the Beaver basin of southwestern Utah are the highest recorded to date in Utah. Measured indoor-radon concentrations range from 17.5 to 495pCi/L. These levels are well above those considered a health risk by the U.S. Environmental Protection Agency. Both geologic (uranium content of soil, depth to ground water, soil permeability) and non-geologic (weather, home construction, life-style) factors affect indoor-radon levels. In this study, geologic factors are quantified and used to produce a radon-hazard-potential map of the Beaver basin area. The map helps prioritize radon testing and evaluation and the need for radon-resistant construction.
Author:
Publisher:
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Category : Uranium industry
Languages : en
Pages : 190
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Book Description
Author: G.K. Gillmore
Publisher: Geological Society of London
ISBN: 1786203081
Category : Science
Languages : en
Pages : 246
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Book Description
This volume draws together the final outputs of the five-year UNESCO/IUGS/IGCP Project 571 and presents new data on radon in the built and natural environments, radon as a diagnostic tool of geophysical phenomena, reflections and recommendations on the future of radon research and a critique of radon's asserted use as a therapy. By considering all the aspects of radon as a health hazard and potential indicator of natural hazards, the project brought together the dispersed research (from universities, governmental and non-governmental bodies as well as commercial companies) on radon within an interdisciplinary context to facilitate scientific advancement and understanding. Through the establishment of working groups at regional and local levels and the development of research networks, a variety of international meetings were organized and a number of journal special issues published to disseminate the results. The scale of the project was global: scientists from over 20 European countries, plus countries in the Americas, Asia and the Middle East have been participants of the project. This volume results from UNESCO/IUGS/IGCP Project 571 `Radon, Health and Natural Hazards'. Radon has significant socio-economic relevance in the developed and developing worlds, primarily in terms of the indoor radon hazard but also certain geohazards. This volume presents a broad range of papers including methodological, technological and interpretative aspects, as well as case-study material. This volume results from UNESCO/IUGS/IGCP Project 571 `Radon, Health and Natural Hazards'. This volume presents a broad range of papers including methodological, technological and interpretative aspects, as well as case-study material.
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Category : Physics
Languages : en
Pages : 1314
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Book Description
Author:
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Category : Geology
Languages : en
Pages : 342
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Book Description
Author:
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Category : Uranium industry
Languages : en
Pages : 194
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Book Description
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Category : Nuclear energy
Languages : en
Pages : 748
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Book Description
Author: Paul J. Lienau
Publisher:
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Category : Geothermal engineering
Languages : en
Pages : 430
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Book Description
Author: Giuseppe Etiope
Publisher: Springer
ISBN: 3319146017
Category : Science
Languages : en
Pages : 203
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Book Description
The book offers a modern, comprehensive, and holistic view of natural gas seepage, defined as the visible or invisible flow of gaseous hydrocarbons from subsurface sources to Earth’s surface. Beginning with definitions, classifications for onshore and offshore seepage, and fundamentals on gas migration mechanisms, the book reports the latest findings for the global distribution of gas seepage and describes detection methods. Seepage implications are discussed in relation to petroleum exploration, environmental impacts (hazards, pollution, atmospheric emissions, and past climate change), emerging scientific issues (abiotic gas and methane on Mars), and the role of seeps in ancient cultures. With an updated bibliography and an integrated analysis of available data, the book offers a new fundamental awareness - gas seepage is more widespread than previously thought and influences all of Earth’s external “spheres”, including the hydrosphere, atmosphere, biosphere, and anthroposphere.
