Reconstructing the Temporal Changes in the Structural-Petrophysical Characteristics of a Disintegrating Massif of Rocks

摘要

Using the proposed algorithm as a basis, we performed the quantitative interpretation of experimental data on several temporally successive high-amplitude radon anomalies. As a result, the relative changes in the open porosity, the specific internal surface, and the pressure of a deteriorating massif of rocks were restored.