Author: Charles E. Bishop
Publisher: Utah Geological Survey
ISBN: 1557916160
Category : Geology, Structural
Languages : en
Pages : 43
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.
Radon-hazard Potential of Beaver Basin Area, Beaver County, Utah
Author: Charles E. Bishop
Publisher: Utah Geological Survey
ISBN: 1557916160
Category : Geology, Structural
Languages : en
Pages : 43
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.
Publisher: Utah Geological Survey
ISBN: 1557916160
Category : Geology, Structural
Languages : en
Pages : 43
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.
Radon-hazard Potential of the Southern St. George Basin, Washington County, and Ogden Valley, Weber County, Utah
Author: Barry J. Solomon
Publisher:
ISBN: 9781557913692
Category : Air
Languages : en
Pages : 49
Book Description
Publisher:
ISBN: 9781557913692
Category : Air
Languages : en
Pages : 49
Book Description
Radon-hazard Potential of the Southern St. George Basin, Washington County, and Ogden Valley, Weber County, Utah
Author: Barry J. Solomon
Publisher:
ISBN:
Category :
Languages : en
Pages : 42
Book Description
Publisher:
ISBN:
Category :
Languages : en
Pages : 42
Book Description
Special Study
Author:
Publisher:
ISBN:
Category : Geology
Languages : en
Pages : 342
Book Description
Publisher:
ISBN:
Category : Geology
Languages : en
Pages : 342
Book Description
Report of Investigation
Author:
Publisher:
ISBN:
Category : Geology
Languages : en
Pages : 388
Book Description
Publisher:
ISBN:
Category : Geology
Languages : en
Pages : 388
Book Description
Survey Notes
Author:
Publisher:
ISBN:
Category : Geology
Languages : en
Pages : 174
Book Description
Publisher:
ISBN:
Category : Geology
Languages : en
Pages : 174
Book Description
Utah State Bulletin
Author:
Publisher:
ISBN:
Category : Administrative procedure
Languages : en
Pages : 964
Book Description
... the official noticing publication of the executive branch of Utah State Government.
Publisher:
ISBN:
Category : Administrative procedure
Languages : en
Pages : 964
Book Description
... the official noticing publication of the executive branch of Utah State Government.
Publications
Author: Utah Geological Survey
Publisher:
ISBN:
Category :
Languages : en
Pages : 32
Book Description
Publisher:
ISBN:
Category :
Languages : en
Pages : 32
Book Description
Books In Print 2004-2005
Author: Ed Bowker Staff
Publisher: R. R. Bowker
ISBN: 9780835246422
Category : Reference
Languages : en
Pages : 3274
Book Description
Publisher: R. R. Bowker
ISBN: 9780835246422
Category : Reference
Languages : en
Pages : 3274
Book Description
Radon-hazard Potential of the Lower Weber River Area, Tooele Valley, and Southeastern Cache Valley, Cache, Davis, Tooele, and Weber Counties, Utah
Author: Bill D. Black
Publisher: Utah Geological Survey
ISBN: 155791379X
Category : Geology, Structural
Languages : en
Pages : 62
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
Publisher: Utah Geological Survey
ISBN: 155791379X
Category : Geology, Structural
Languages : en
Pages : 62
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