Arid
DOI10.2172/207591
报告编号DOE/ID/13223--T3
来源IDOSTI_ID: 207591
Low-temperature geothermal resources of Washington
Schuster, J.E. [Washington State Dept. of Natural Resources, Olympia, WA (United States). Div. of Geology and Earth Resources]; Bloomquist, R.G. [Washington State Energy Office, Olympia, WA (United States)]
英文摘要This report presents information on the location, physical characteristics, and water chemistry of low-temperature geothermal resources in Washington. The database includes 941 thermal (>20C or 68F) wells, 34 thermal springs, lakes, and fumaroles, and 238 chemical analyses. Most thermal springs occur in the Cascade Range, and many are associated with stratovolcanoes. In contrast, 97 percent of thermal wells are located in the Columbia Basin of southeastern Washington. Some 83.5 percent are located in Adams, Benton, Franklin, Grant, Walla Walla, and Yakima Counties. Yakima County, with 259 thermal wells, has the most. Thermal wells do not seem to owe their origin to local sources of heat, such as cooling magma in the Earth`s upper crust, but to moderate to deep circulation of ground water in extensive aquifers of the Columbia River Basalt Group and interflow sedimentary deposits, under the influence of a moderately elevated (41C/km) average geothermal gradient.
出版年1994
报告类型Technical Report
语种英语
国家美国
来源学科分类15 GEOTHERMAL ENERGY ; GEOTHERMAL ENERGY ; RESOURCE ASSESSMENT ; GEOTHERMAL RESOURCES ; WASHINGTON Geothermal Legacy
URLhttp://www.osti.gov/scitech/servlets/purl/207591
资源类型科技报告
条目标识符http://119.78.100.177/qdio/handle/2XILL650/265687
推荐引用方式
GB/T 7714
Schuster, J.E. [Washington State Dept. of Natural Resources, Olympia, WA ,Bloomquist, R.G. [Washington State Energy Office, Olympia, WA . Low-temperature geothermal resources of Washington,1994.
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