MODERN GEOPHYSICAL METHODS IN STUDYING THE GEOMECHANICAL STATE OF A ROCK MASS

Abstract

This paper discusses modern geophysical methods used to analyze the geomechanical state of rock massifs. The main attention is paid to the methods of spectral seismic profiling and ground penetrating radar sounding, which allows obtaining detailed information about the internal structure of rocks at significant depths and over vast territories without destroying the integrity of the massif.

Experimental studies have shown the high efficiency of these methods both when used together and separately. They provide a detailed study of the structure of rocks, identification of fracturing zones, tectonic faults and karst voids, which significantly increases the safety and productivity of mining operations, and the construction of buildings and structures.

Despite the specifics of each of these methods and their inherent limitations, their combined use can level out individual shortcomings and provide more accurate information about the state of the rock mass. Thus, the spectral seismic profiling method is a highly effective technology for deep surveys, while the ground penetrating radar sounding method is preferably used to study shallow depths.

The practical significance of these approaches is expressed in the prompt detection of potentially hazardous areas, development of preventive measures against emergency situations and increasing the stability of mine workings. The use of these technologies allows optimizing the processes of mineral extraction and construction of subsoil use facilities, minimizing the risks of natural and man-made disasters.

The obtained results indicate that modern geophysical technologies are key tools for studying the geomechanical state of rock massifs. Further evolution and integration of these methods will open new horizons for in-depth knowledge and safe exploitation of natural resources.