Abstract
Radon-222 concentration in soils at shallow depth was measured at the “Los Azufres” geothermal field, Michoacan State, Mexico, in order to observe possible temporal variations in relation with the peculiar conditions of the area. A four years' survey is reported using the SSNTD technique. The obtained data indicate the feasibility of the technique for this type of investigation and illustrate the role of Radon-222 as a tracer of pore fluids motion in the substratum.
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Schedule a callMore From: International Journal of Radiation Applications and Instrumentation. Part D. Nuclear Tracks and Radiation Measurements
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