INVESTIGATION OF THE STRESS-DEFORMED STATE OF LANDSLIDE SLOPES BY MEANS OF ELECTROMETRICAL AND RADIOMETRICAL METHODS.

Some peculiarities of radiometrical and electrometrical methods for landslide slope study are considered. Taking as a basis the theory of slope abyssal creepage, the mechanism of formation of emanation anomalies within the limits of an active landslide is suggested. It is noted that all the three preparation phases of the abyssal creepage process are characterized by the extreme values of radioactive emanation field. The revealed statistic intercomunication between ground geoelectrical and physical-mechanical properties makes it possible to carry out effective calculation of landslide slope stability reserve