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SELECTION AND JUSTIFICATION OF THE LOCATION OF THE NETWORK OF POINTS OF STATIONARY OBSERVATIONS IN THE LOCAL ZONES OF KARSTOLOGICAL MONITORING
Abstract
The article devoted to issues of organization of regime observations in the system of geodynamic karstological monitoring, which is carried out with the active development of karst or karst-suffusion processes with a high degree of danger for the construction. It is noted that for stationary observations it is necessary to provide quantitative characteristics of changes in individual components of the geological environment in time and space that must be sufficient to assess and predict the development of the karst (karst-suffusion) process, the choice of design solutions and the justification of protective measures for structures. The functional dependencies of the technical characteristics of the locations of the observing network points on the speed (intensity) of the karst or karst-suffusion process, the natural and man-made conditions, the size of the surveyed area are determined, which are ranked according to the level of responsibility and features of buildings and structures. An example of the deployment of a system of karstological monitoring, which included hydrogeological regime stationary observations of the regime of underground and surface waters is given, as well as geophysical observations of the state of karst rocks and its overlapping deposits, the degree of their watering, the development of karst cavities, the appearance of zones of decompaction and liquefaction in the integumentary thicker.
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