Thermonuclear chlorine-36 in arid soil
Thermonuclear bomb testing in the 1950's and 1960's produced a significant amount of chlorine-36 (C1-36). This anthropogenic C1-36 pulse has been proposed as a tool in dating ground water and as an environmental tracer. The feasibility of bomb C1-36 as a hydrologic tool in the unsaturated...
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Language: | en |
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The University of Arizona.
1983
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Online Access: | http://hdl.handle.net/10150/191791 |