Author: Belikov V.
Publisher: MAIK Nauka/Interperiodica
ISSN: 1061-8309
Source: Russian Journal of Nondestructive Testing, Vol.47, Iss.5, 2011-05, pp. : 343-351
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Abstract
Experimental data on radon concentration variations were quantitatively interpreted on the basis of a proposed quantitative model that describes the process of the formation of high-amplitude radon anomalies. As a result, relative time variations in the structural (porosity and specific inner surface) and dynamic (pressure) characteristics of a disintegrating massif of rocks were reconstructed.
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