8 research outputs found

    New Invariants for the Graph Isomorphism Problem

    No full text

    Application of electroprospecting methods in the study of landslides

    No full text
    แƒ”แƒšแƒ”แƒฅแƒขแƒ แƒแƒซแƒ˜แƒ”แƒ‘แƒ˜แƒก แƒ›แƒ”แƒ—แƒแƒ“แƒ”แƒ‘แƒ˜แƒก แƒกแƒแƒจแƒฃแƒแƒšแƒ”แƒ‘แƒ˜แƒ— แƒจแƒ”แƒกแƒแƒซแƒšแƒ”แƒ‘แƒ”แƒšแƒ˜แƒ แƒ’แƒ”แƒแƒšแƒแƒ’แƒ˜แƒฃแƒ แƒ˜ แƒ’แƒแƒ แƒ”แƒ›แƒแƒก แƒ”แƒšแƒ”แƒฅแƒขแƒ แƒแƒ›แƒแƒ’แƒœแƒ˜แƒขแƒฃแƒ แƒ˜ แƒ›แƒแƒฎแƒแƒกแƒ˜แƒแƒ—แƒ”แƒ‘แƒšแƒ”แƒ‘แƒ˜แƒก (แƒฌแƒ˜แƒœแƒแƒแƒฆแƒ›แƒ“แƒ”แƒ’แƒแƒ‘แƒ, แƒ’แƒแƒ›แƒขแƒแƒ แƒแƒ‘แƒ แƒ“แƒ แƒ.แƒจ.) แƒ“แƒแƒ“แƒ’แƒ”แƒœแƒ, แƒกแƒแƒ˜แƒ“แƒแƒœแƒแƒช แƒจแƒ”แƒ˜แƒซแƒšแƒ”แƒ‘แƒ แƒ’แƒแƒ•แƒแƒ™แƒ”แƒ—แƒแƒ— แƒ“แƒแƒกแƒ™แƒ•แƒœแƒ”แƒ‘แƒ˜ แƒจแƒ”แƒกแƒฌแƒแƒ•แƒšแƒ˜แƒšแƒ˜ แƒขแƒ”แƒ แƒ˜แƒขแƒแƒ แƒ˜แƒ˜แƒก แƒแƒ’แƒ”แƒ‘แƒฃแƒšแƒ”แƒ‘แƒ˜แƒก แƒ“แƒ แƒ“แƒแƒขแƒ”แƒœแƒ˜แƒแƒœแƒ”แƒ‘แƒ˜แƒก แƒจแƒ”แƒกแƒแƒฎแƒ”แƒ‘. แƒ”แƒšแƒ”แƒฅแƒขแƒ แƒฃแƒšแƒ˜ แƒ’แƒแƒ›แƒแƒ™แƒ•แƒšแƒ”แƒ•แƒ, แƒ˜แƒกแƒ”แƒ•แƒ” แƒ แƒแƒ’แƒแƒ แƒช แƒ’แƒ”แƒแƒคแƒ˜แƒ–แƒ˜แƒ™แƒฃแƒ แƒ˜ แƒ™แƒ•แƒšแƒ”แƒ•แƒ”แƒ‘แƒ˜แƒก แƒซแƒ˜แƒ แƒ˜แƒ—แƒแƒ“แƒ˜ แƒœแƒแƒฌแƒ˜แƒšแƒ˜, แƒจแƒ”แƒ˜แƒซแƒšแƒ”แƒ‘แƒ แƒ“แƒแƒ˜แƒงแƒแƒก แƒแƒ  แƒฏแƒ’แƒฃแƒคแƒแƒ“: แƒžแƒแƒกแƒ˜แƒฃแƒ แƒ˜ แƒ“แƒ แƒแƒฅแƒขแƒ˜แƒฃแƒ แƒ˜ แƒ›แƒ”แƒ—แƒแƒ“แƒ”แƒ‘แƒ˜. แƒžแƒ˜แƒ แƒ•แƒ”แƒš แƒ›แƒแƒ—แƒ’แƒแƒœแƒก แƒ›แƒ˜แƒ”แƒ™แƒฃแƒ—แƒ•แƒœแƒ”แƒ‘แƒ แƒ‘แƒฃแƒœแƒ”แƒ‘แƒ แƒ˜แƒ•แƒ˜ แƒ”แƒšแƒ”แƒฅแƒขแƒ แƒฃแƒšแƒ˜ แƒ•แƒ”แƒšแƒ˜แƒก แƒ›แƒ”แƒ—แƒแƒ“แƒ”แƒ‘แƒ˜, แƒฎแƒแƒšแƒ แƒ›แƒ”แƒแƒ แƒ”แƒก - แƒฎแƒ”แƒšแƒแƒ•แƒœแƒฃแƒ แƒ˜ แƒ”แƒšแƒ”แƒฅแƒขแƒ แƒฃแƒšแƒ˜ แƒ•แƒ”แƒšแƒ˜แƒก แƒ›แƒ”แƒ—แƒแƒ“แƒ”แƒ‘แƒ˜. แƒœแƒแƒจแƒ แƒแƒ›แƒจแƒ˜ แƒฌแƒแƒ แƒ›แƒแƒ“แƒ’แƒ”แƒœแƒ˜แƒšแƒ˜ แƒ›แƒแƒกแƒแƒšแƒ”แƒ‘แƒ˜ แƒ›แƒ˜แƒฆแƒ”แƒ‘แƒฃแƒšแƒ˜แƒ, แƒ›แƒ”แƒฌแƒงแƒ แƒฃแƒš แƒกแƒฎแƒ”แƒฃแƒšแƒ–แƒ”, แƒ•แƒ”แƒ แƒขแƒ˜แƒ™แƒแƒšแƒฃแƒ แƒ˜ แƒ”แƒšแƒ”แƒฅแƒขแƒ แƒฃแƒšแƒ˜ แƒ–แƒแƒœแƒ“แƒ˜แƒ แƒ”แƒ‘แƒ˜แƒก แƒ“แƒ แƒ‘แƒฃแƒœแƒ”แƒ‘แƒ แƒ˜แƒ•แƒ˜ แƒ”แƒšแƒ”แƒฅแƒขแƒ แƒฃแƒšแƒ˜ แƒ•แƒ”แƒšแƒ˜แƒก แƒ›แƒ”แƒ—แƒแƒ“แƒ”แƒ‘แƒ˜แƒ—. แƒ›แƒ˜แƒฆแƒ”แƒ‘แƒฃแƒšแƒ˜ แƒจแƒ”แƒ“แƒ”แƒ’แƒ”แƒ‘แƒ˜แƒก แƒแƒœแƒแƒšแƒ˜แƒ–แƒ˜แƒก แƒกแƒแƒคแƒฃแƒซแƒ•แƒ”แƒšแƒ–แƒ” แƒ’แƒแƒ™แƒ”แƒ—แƒ”แƒ‘แƒฃแƒšแƒ˜แƒ แƒ“แƒแƒกแƒ™แƒ•แƒœแƒ”แƒ‘แƒ˜ แƒฅแƒแƒœแƒ”แƒ‘แƒ˜แƒก แƒ’แƒแƒฌแƒงแƒšแƒ˜แƒแƒœแƒ”แƒ‘แƒ˜แƒก แƒ“แƒ แƒ›แƒ˜แƒฌแƒ˜แƒกแƒฅแƒ•แƒ”แƒจแƒ แƒฌแƒงแƒšแƒ”แƒ‘แƒ˜แƒก แƒœแƒแƒ™แƒแƒ“แƒ”แƒ‘แƒ˜แƒก แƒจแƒ”แƒกแƒแƒซแƒšแƒ แƒแƒ แƒกแƒ”แƒ‘แƒแƒ‘แƒ˜แƒก แƒจแƒ”แƒกแƒแƒฎแƒ”แƒ‘.With the help of electrorprospecting methods, it is possible to determine the electromagnetic characteristics of the geological environment (resistance, conductivity, etc.), from which we can draw conclusions about the structure and moisture content of the studied area. Electrical survey, like the main part of geophysical surveys, can be divided into two groups: passive and active methods. The first of them includes natural electric field methods, and the second - artificial electric field methods. The materials presented in the work were obtained, on the landslide body, by vertical electric sounding and natural electric field methods. Based on the analysis of the obtained results, conclusions are made about the possible existence of rock humidity and underground water flows

    Institute of Geophysics - 90 years

    No full text
    1933 แƒฌแƒšแƒ˜แƒก 1 แƒœแƒแƒ”แƒ›แƒ‘แƒ”แƒ แƒก แƒกแƒแƒฅแƒแƒ แƒ—แƒ•แƒ”แƒšแƒแƒก แƒ›แƒ—แƒแƒ•แƒ แƒแƒ‘แƒ˜แƒก แƒ“แƒแƒ“แƒ’แƒ”แƒœแƒ˜แƒšแƒ”แƒ‘แƒ˜แƒ— แƒ“แƒแƒแƒ แƒกแƒ“แƒ แƒกแƒกแƒ แƒ™ แƒ›แƒ”แƒชแƒœแƒ˜แƒ”แƒ แƒ”แƒ‘แƒแƒ—แƒ แƒแƒ™แƒแƒ“แƒ”แƒ›แƒ˜แƒ˜แƒก แƒแƒ›แƒ˜แƒ”แƒ แƒ™แƒแƒ•แƒ™แƒแƒกแƒ˜แƒ˜แƒก แƒคแƒ˜แƒšแƒ˜แƒแƒšแƒ˜แƒก แƒกแƒแƒฅแƒแƒ แƒ—แƒ•แƒ”แƒšแƒแƒก แƒ’แƒแƒœแƒงแƒแƒคแƒ˜แƒšแƒ”แƒ‘แƒ˜แƒก แƒ’แƒ”แƒแƒคแƒ˜แƒ–แƒ˜แƒ™แƒฃแƒ แƒ˜ แƒ˜แƒœแƒกแƒขแƒ˜แƒขแƒฃแƒขแƒ˜. แƒแƒ›แƒŸแƒแƒ›แƒแƒ“ แƒ”แƒก แƒแƒ แƒ˜แƒก แƒ˜แƒ•. แƒฏแƒแƒ•แƒแƒฎแƒ˜แƒจแƒ•แƒ˜แƒšแƒ˜แƒก แƒกแƒแƒฎ. แƒ—แƒ‘แƒ˜แƒšแƒ˜แƒกแƒ˜แƒก แƒกแƒแƒฎแƒ”แƒšแƒ›แƒฌแƒ˜แƒคแƒ แƒฃแƒœแƒ˜แƒ•แƒ”แƒ แƒกแƒ˜แƒขแƒ”แƒขแƒ˜แƒก แƒžแƒ แƒแƒคแƒ”แƒกแƒแƒ  แƒ›แƒ˜แƒฎแƒ”แƒ˜แƒš แƒœแƒแƒ“แƒ˜แƒแƒก แƒกแƒแƒฎ. แƒ’แƒ”แƒแƒคแƒ˜แƒ–แƒ˜แƒ™แƒ˜แƒก แƒ˜แƒœแƒกแƒขแƒ˜แƒขแƒฃแƒขแƒ˜. แƒกแƒขแƒแƒขแƒ˜แƒแƒจแƒ˜ แƒฌแƒแƒ แƒ›แƒแƒ“แƒ’แƒ”แƒœแƒ˜แƒšแƒ˜แƒ แƒ˜แƒœแƒกแƒขแƒ˜แƒขแƒฃแƒขแƒ˜แƒก แƒ›แƒแƒ™แƒšแƒ” แƒ˜แƒกแƒขแƒแƒ แƒ˜แƒ.On November 1, 1933, by a decree of the Government of Georgia, based on the decision of the Presidium of the Academy of Sciences of the former USSR, the Geophysical Institute was established as part of the Georgian Branch of the Transcaucasian Branch of the USSR Academy of Sciences, now the M. Nodia Institute of Geophysics of Iv. Javakhishvili Tbilisi State University. The article gives a brief history of the Institute

    Vertical Electric Sounding in Water Search Tasks and for Landslide Hazards Assessment

    No full text
    แƒซแƒ˜แƒ”แƒ‘แƒ˜แƒก แƒ”แƒšแƒ”แƒฅแƒขแƒ แƒฃแƒšแƒ˜ แƒ›แƒ”แƒ—แƒแƒ“แƒ˜ (แƒ”แƒšแƒ”แƒฅแƒขแƒ แƒแƒซแƒ˜แƒ”แƒ‘แƒ) แƒ’แƒแƒ›แƒแƒงแƒ”แƒœแƒ”แƒ‘แƒ˜แƒ—แƒ˜ แƒ’แƒ”แƒแƒคแƒ˜แƒ–แƒ˜แƒ™แƒ˜แƒก แƒ”แƒ แƒ—-แƒ”แƒ แƒ—แƒ˜ แƒซแƒ˜แƒ แƒ˜แƒ—แƒแƒ“แƒ˜ แƒ“แƒแƒ แƒ’แƒ˜แƒ, แƒ แƒแƒ›แƒ”แƒšแƒ˜แƒช แƒ”แƒ›แƒงแƒแƒ แƒ”แƒ‘แƒ แƒ”แƒšแƒ”แƒฅแƒขแƒ แƒฃแƒšแƒ˜ แƒ“แƒ แƒ”แƒšแƒ”แƒฅแƒขแƒ แƒแƒ›แƒแƒ’แƒœแƒ˜แƒขแƒฃแƒ แƒ˜ แƒ•แƒ”แƒšแƒ”แƒ‘แƒ˜แƒก แƒ’แƒแƒœแƒแƒฌแƒ˜แƒšแƒ”แƒ‘แƒ˜แƒก แƒจแƒ”แƒกแƒฌแƒแƒ•แƒšแƒแƒก. แƒ”แƒšแƒ”แƒฅแƒขแƒ แƒฃแƒšแƒ˜ แƒ›แƒ”แƒ—แƒแƒ“แƒ”แƒ‘แƒ˜ แƒจแƒ”แƒ˜แƒซแƒšแƒ”แƒ‘แƒ แƒแƒ  แƒขแƒ˜แƒžแƒแƒ“ แƒ“แƒแƒ•แƒงแƒแƒ— แƒ˜แƒ›แƒ˜แƒก แƒ›แƒ˜แƒฎแƒ”แƒ“แƒ•แƒ˜แƒ—, แƒ—แƒฃ แƒ แƒ แƒฌแƒงแƒแƒ แƒ แƒ’แƒแƒ›แƒแƒ˜แƒงแƒ”แƒœแƒ”แƒ‘แƒ, แƒ‘แƒฃแƒœแƒ”แƒ‘แƒ แƒ˜แƒ•แƒ˜ แƒ—แƒฃ แƒฎแƒ”แƒšแƒแƒ•แƒœแƒฃแƒ แƒ˜. แƒžแƒ˜แƒ แƒ•แƒ”แƒš แƒ›แƒแƒ—แƒ’แƒแƒœแƒก แƒ‘แƒฃแƒœแƒ”แƒ‘แƒ แƒ˜แƒ•แƒ˜ แƒ”แƒšแƒ”แƒฅแƒขแƒ แƒฃแƒšแƒ˜ แƒ•แƒ”แƒšแƒ˜แƒก (แƒ‘แƒ”แƒ•) แƒ›แƒ”แƒ—แƒแƒ“แƒ”แƒ‘แƒก แƒฃแƒฌแƒแƒ“แƒ”แƒ‘แƒ”แƒœ, แƒฎแƒแƒšแƒ แƒ›แƒ”แƒแƒ แƒ”แƒก -แƒฌแƒ˜แƒœแƒแƒแƒฆแƒ›แƒ“แƒ”แƒ’แƒแƒ‘แƒ˜แƒก แƒ›แƒ”แƒ—แƒแƒ“แƒ”แƒ‘แƒก. แƒฉแƒ•แƒ”แƒœแƒก แƒœแƒแƒจแƒ แƒแƒ›แƒจแƒ˜ แƒฌแƒแƒ แƒ›แƒแƒ“แƒ’แƒ”แƒœแƒ˜แƒšแƒ˜ แƒ›แƒแƒกแƒแƒšแƒ”แƒ‘แƒ˜ แƒ›แƒ˜แƒฆแƒ”แƒ‘แƒฃแƒšแƒ˜แƒ แƒฌแƒ˜แƒœแƒแƒแƒฆแƒ›แƒ“แƒ”แƒ’แƒแƒ‘แƒ˜แƒก (แƒ•แƒ”แƒ แƒขแƒ˜แƒ™แƒแƒšแƒฃแƒ แƒ˜ แƒ”แƒšแƒ”แƒฅแƒขแƒ แƒฃแƒšแƒ˜ แƒ–แƒแƒœแƒ“แƒ˜แƒ แƒ”แƒ‘แƒ˜แƒก) แƒ›แƒ”แƒ—แƒแƒ“แƒ˜แƒ—. แƒฌแƒแƒ แƒ›แƒแƒ“แƒ’แƒ”แƒœแƒ˜แƒšแƒ˜แƒ แƒแƒ แƒ˜ แƒกแƒแƒฎแƒ˜แƒก แƒกแƒแƒ›แƒฃแƒจแƒแƒแƒ”แƒ‘แƒ˜แƒก แƒ›แƒแƒกแƒแƒšแƒ”แƒ‘แƒ˜. แƒ•แƒ˜แƒ™แƒ•แƒšแƒ”แƒ•แƒ“แƒ˜แƒ— แƒฅแƒแƒœแƒ”แƒ‘แƒ˜แƒก แƒ’แƒแƒฌแƒงแƒšแƒ˜แƒแƒœแƒ”แƒ‘แƒแƒก แƒ“แƒ แƒ›แƒ˜แƒฌแƒ˜แƒกแƒฅแƒ•แƒ”แƒจแƒ แƒฌแƒงแƒšแƒ”แƒ‘แƒ˜แƒก แƒจแƒ”แƒกแƒแƒซแƒšแƒ แƒแƒ แƒกแƒ”แƒ‘แƒแƒ‘แƒแƒก แƒกแƒฎแƒ•แƒแƒ“แƒแƒกแƒฎแƒ•แƒ แƒกแƒ˜แƒฆแƒ แƒ›แƒ”แƒ”แƒ‘แƒ–แƒ”. แƒแƒกแƒ”แƒ•แƒ” แƒ›แƒ”แƒฌแƒงแƒ แƒฃแƒš แƒ–แƒแƒœแƒ”แƒ‘แƒจแƒ˜ แƒ•แƒ˜แƒ™แƒ•แƒšแƒ”แƒ•แƒ“แƒ˜แƒ— แƒฅแƒแƒœแƒ”แƒ‘แƒ˜แƒก แƒšแƒ˜แƒ—แƒแƒšแƒแƒ’แƒ˜แƒแƒก, แƒจแƒ”แƒกแƒแƒซแƒšแƒ แƒ’แƒแƒฌแƒงแƒšแƒ˜แƒแƒœแƒ”แƒ‘แƒแƒก แƒ“แƒ แƒ•แƒแƒฎแƒ“แƒ”แƒœแƒ“แƒ˜แƒ— แƒ›แƒ”แƒฌแƒงแƒ แƒ˜แƒก แƒฃแƒกแƒแƒคแƒ แƒ—แƒฎแƒแƒ”แƒ‘แƒ˜แƒก แƒ™แƒแƒ”แƒคแƒ˜แƒชแƒ˜แƒ”แƒœแƒขแƒ˜แƒก (FS) แƒจแƒ”แƒคแƒแƒกแƒ”แƒ‘แƒแƒก.The electrical method of searching (electrosearching) is one of the basic fields of applied geophysics based on the study of the distribution of electrical and electromagnetic fields. Electrical methods can be divided into two types, depending on what source is used, natural or artificial. The first ones are called natural electric fields methods, and the other - methods of resistance. The materials presented in our work have been obtained with resistance (vertical electric sensing) method. The materials of the two types of works are presented. We are exploring rocks humidity and the possible existence of groundwater on different depths. In the landslide zones, we investigated lithology, the possible existence of water and an estimate of the safety factor of landslides (FS). Key words: Vertical Electrical Sounding, Resistivity, Groundwater, Landslide

    Study of the Ground Collapse (Sinkhole) Using Electroprospecting Methods

    No full text
    แƒ”แƒšแƒ”แƒฅแƒขแƒ แƒแƒซแƒ˜แƒ”แƒ‘แƒ˜แƒก แƒ›แƒ”แƒ—แƒแƒ“แƒ”แƒ‘แƒ˜ แƒ˜แƒซแƒšแƒ”แƒ•แƒ แƒกแƒแƒจแƒฃแƒแƒšแƒ”แƒ‘แƒแƒก แƒ“แƒแƒ•แƒแƒ“แƒ’แƒ˜แƒœแƒแƒ— แƒ’แƒ”แƒแƒšแƒแƒ’แƒ˜แƒฃแƒ แƒ˜ แƒ’แƒแƒ แƒ”แƒ›แƒแƒก แƒ”แƒšแƒ”แƒฅแƒขแƒ แƒฃแƒšแƒ˜ แƒ›แƒแƒฎแƒแƒกแƒ˜แƒแƒ—แƒ”แƒ‘แƒšแƒ”แƒ‘แƒ˜ (แƒฌแƒ˜แƒœแƒแƒแƒฆแƒ›แƒ“แƒ”แƒ’แƒแƒ‘แƒ, แƒ’แƒแƒ›แƒขแƒแƒ แƒแƒ‘แƒ แƒ“แƒ แƒ.แƒจ.) แƒ“แƒ แƒ›แƒแƒ—แƒ–แƒ” แƒ“แƒแƒงแƒ แƒ“แƒœแƒแƒ‘แƒ˜แƒ— แƒ’แƒแƒ•แƒแƒ™แƒ”แƒ—แƒแƒ— แƒ“แƒแƒกแƒ™แƒ•แƒœแƒ”แƒ‘แƒ˜ แƒจแƒ”แƒกแƒฌแƒแƒ•แƒšแƒ˜แƒšแƒ˜ แƒขแƒ”แƒ แƒ˜แƒขแƒแƒ แƒ˜แƒ˜แƒก แƒแƒ’แƒ”แƒ‘แƒฃแƒšแƒ”แƒ‘แƒ˜แƒก แƒ“แƒ แƒ“แƒแƒขแƒ”แƒœแƒ˜แƒแƒœแƒ”แƒ‘แƒ˜แƒก แƒจแƒ”แƒกแƒแƒฎแƒ”แƒ‘. แƒœแƒแƒจแƒ แƒแƒ›แƒจแƒ˜ แƒฌแƒแƒ แƒ›แƒแƒ“แƒ’แƒ”แƒœแƒ˜แƒšแƒ˜ แƒ›แƒแƒกแƒแƒšแƒ”แƒ‘แƒ˜ แƒ›แƒ˜แƒฆแƒ”แƒ‘แƒฃแƒšแƒ˜แƒ, แƒ’แƒ แƒฃแƒœแƒขแƒ˜แƒก แƒซแƒแƒ‘แƒ แƒ˜แƒกแƒ”แƒ‘แƒฃแƒ แƒ˜ แƒฉแƒแƒฅแƒชแƒ”แƒ•แƒ˜แƒก แƒ›แƒ˜แƒ“แƒแƒ›แƒแƒ”แƒ‘แƒจแƒ˜, แƒ•แƒ”แƒ แƒขแƒ˜แƒ™แƒแƒšแƒฃแƒ แƒ˜ แƒ”แƒšแƒ”แƒฅแƒขแƒ แƒฃแƒšแƒ˜ แƒ–แƒแƒœแƒ“แƒ˜แƒ แƒ”แƒ‘แƒ˜แƒก แƒ›แƒ”แƒ—แƒแƒ“แƒ˜แƒ— แƒฉแƒแƒขแƒแƒ แƒ”แƒ‘แƒฃแƒšแƒ˜ แƒ™แƒ•แƒšแƒ”แƒ•แƒ”แƒ‘แƒ˜แƒก แƒกแƒแƒคแƒฃแƒซแƒ•แƒ”แƒšแƒ–แƒ”. แƒ›แƒ˜แƒฆแƒ”แƒ‘แƒฃแƒšแƒ˜ แƒจแƒ”แƒ“แƒ”แƒ’แƒ”แƒ‘แƒ˜แƒก แƒแƒœแƒแƒšแƒ˜แƒ–แƒ–แƒ” แƒ“แƒแƒงแƒ แƒ“แƒœแƒแƒ‘แƒ˜แƒ— แƒ’แƒแƒ™แƒ”แƒ—แƒ”แƒ‘แƒฃแƒšแƒ˜แƒ แƒ“แƒแƒกแƒ™แƒ•แƒœแƒ”แƒ‘แƒ˜ แƒฅแƒแƒœแƒ”แƒ‘แƒ˜แƒก แƒขแƒ˜แƒžแƒ”แƒ‘แƒ˜แƒก, แƒ›แƒแƒ—แƒ˜ แƒกแƒ˜แƒฆแƒ แƒ›แƒฃแƒšแƒ˜ แƒ’แƒแƒœแƒแƒฌแƒ˜แƒšแƒ”แƒ‘แƒ˜แƒก แƒ“แƒ แƒ“แƒแƒขแƒ”แƒœแƒ˜แƒแƒœแƒ”แƒ‘แƒ˜แƒก แƒจแƒ”แƒกแƒแƒฎแƒ”แƒ‘. แƒ”แƒก แƒ’แƒ•แƒแƒซแƒšแƒ”แƒ•แƒก แƒกแƒแƒจแƒฃแƒแƒšแƒ”แƒ‘แƒแƒก แƒ’แƒแƒ•แƒแƒ™แƒ”แƒ—แƒแƒ— แƒ“แƒแƒกแƒ™แƒ•แƒœแƒ”แƒ‘แƒ˜ แƒ’แƒ แƒฃแƒœแƒขแƒ˜แƒก แƒฉแƒแƒฅแƒชแƒ”แƒ•แƒ˜แƒก แƒ’แƒ”แƒœแƒ”แƒ–แƒ˜แƒกแƒ˜แƒก, แƒ›แƒ˜แƒกแƒ˜ แƒกแƒแƒ•แƒแƒ แƒแƒฃแƒ“แƒ แƒ™แƒ•แƒ”แƒ‘แƒ˜แƒก แƒฌแƒงแƒแƒ แƒแƒก แƒ“แƒ แƒ›แƒ˜แƒกแƒ˜ แƒ’แƒแƒ•แƒ แƒชแƒ”แƒšแƒ”แƒ‘แƒ˜แƒก แƒแƒ แƒ˜แƒก แƒจแƒ”แƒกแƒแƒฎแƒ”แƒ‘.Electroresearch methods allow to determine the electrical characteristics of the geological environment (resistance, conductivity, etc.) and based on them to make conclusions about the structure and humidity of the studied area. The materials presented in the paper were obtained based on the research conducted by the method of vertical electrical sensing in the areas of the funnel-shaped subsidence (sinkhole) of the ground. Based on the analysis of the obtained results, conclusions are made about the types of rocks, their depth distribution and hydration. This allows us to draw conclusions about the genesis of soil subsidence, its likely source of nourishment, and its distribution

    แƒกแƒแƒฆแƒ แƒฃแƒ‘แƒšแƒ แƒ’แƒแƒ แƒ”แƒ›แƒแƒก แƒ™แƒแƒœแƒขแƒแƒฅแƒขแƒฃแƒ แƒ˜ แƒ”แƒšแƒ”แƒฅแƒขแƒ แƒ˜แƒ–แƒแƒชแƒ˜แƒ˜แƒก แƒžแƒ แƒแƒชแƒ”แƒกแƒ”แƒ‘แƒ˜แƒก แƒ”แƒฅแƒกแƒžแƒ”แƒ แƒ˜แƒ›แƒ”แƒœแƒขแƒฃแƒšแƒ˜ แƒ›แƒแƒ“แƒ”แƒšแƒ˜แƒ แƒ”แƒ‘แƒ

    No full text
    แƒฌแƒแƒ แƒ›แƒแƒ“แƒ’แƒ”แƒœแƒ˜แƒšแƒ˜แƒ แƒกแƒแƒฆแƒ แƒฃแƒ‘แƒšแƒ แƒ’แƒแƒ แƒ”แƒ›แƒแƒก แƒ™แƒแƒœแƒขแƒแƒฅแƒขแƒฃแƒ แƒ˜ แƒ”แƒšแƒ”แƒฅแƒขแƒ แƒ˜แƒ–แƒแƒชแƒ˜แƒ˜แƒก แƒžแƒ แƒแƒชแƒ”แƒกแƒ”แƒ‘แƒ˜แƒก แƒ”แƒฅแƒกแƒžแƒ”แƒ แƒ˜แƒ›แƒ”แƒœแƒขแƒฃแƒšแƒ˜ แƒ›แƒแƒ“แƒ”แƒšแƒ˜แƒ แƒ”แƒ‘แƒ˜แƒก แƒจแƒ”แƒ“แƒ”แƒ’แƒ”แƒ‘แƒ˜. แƒ”แƒฅแƒกแƒžแƒ”แƒ แƒ˜แƒ›แƒ”แƒœแƒขแƒ”แƒ‘แƒ˜ แƒขแƒแƒ แƒ“แƒ”แƒ‘แƒแƒ“แƒ แƒกแƒแƒฅแƒแƒ แƒ—แƒ•แƒ”แƒšแƒแƒก แƒ›แƒ”แƒชแƒœแƒ˜แƒ”แƒ แƒ”แƒ‘แƒแƒ—แƒ แƒแƒ™แƒแƒ“แƒ”แƒ›แƒ˜แƒ˜แƒก แƒ’แƒ”แƒแƒคแƒ˜แƒ–แƒ˜แƒ™แƒ˜แƒก แƒ˜แƒœแƒกแƒขแƒ˜แƒขแƒฃแƒขแƒ˜แƒก แƒ—แƒ”แƒ แƒ›แƒแƒ‘แƒแƒ แƒแƒ™แƒแƒ›แƒ”แƒ แƒแƒจแƒ˜ แƒฌแƒ˜แƒœแƒ แƒกแƒแƒฃแƒ™แƒฃแƒœแƒ”แƒจแƒ˜. แƒ™แƒ”แƒ แƒซแƒแƒ“, แƒ“แƒแƒ›แƒฃแƒจแƒแƒ•แƒ”แƒ‘แƒฃแƒšแƒ˜ แƒ˜แƒงแƒ แƒšแƒแƒ‘แƒแƒ แƒแƒขแƒแƒ แƒ˜แƒฃแƒš แƒžแƒ˜แƒ แƒแƒ‘แƒ”แƒ‘แƒจแƒ˜ แƒ”แƒšแƒ”แƒฅแƒขแƒ แƒ˜แƒ–แƒแƒชแƒ˜แƒ˜แƒก แƒžแƒ แƒแƒชแƒ”แƒกแƒ”แƒ‘แƒ˜แƒก แƒ™แƒ•แƒšแƒ”แƒ•แƒ˜แƒก แƒแƒฎแƒแƒšแƒ˜ แƒ›แƒ”แƒ—แƒแƒ“แƒ˜, แƒ แƒแƒ›แƒ”แƒšแƒ›แƒแƒช แƒ›แƒแƒ’แƒ•แƒชแƒ แƒ แƒ˜แƒ’แƒ˜ แƒ›แƒแƒกแƒแƒšแƒ แƒฆแƒ แƒฃแƒ‘แƒšแƒ”แƒ‘แƒจแƒ˜ แƒ”แƒšแƒ”แƒฅแƒขแƒ แƒ˜แƒ–แƒ”แƒ‘แƒ˜แƒก แƒซแƒ˜แƒ แƒ˜แƒ—แƒแƒ“แƒ˜ แƒžแƒ แƒแƒชแƒ”แƒกแƒ”แƒ‘แƒ˜แƒก แƒ’แƒแƒ’แƒ”แƒ‘แƒ˜แƒกแƒ—แƒ•แƒ˜แƒก แƒ“แƒ แƒกแƒแƒคแƒฃแƒซแƒ•แƒšแƒ”แƒ‘แƒ˜ แƒ˜แƒ› แƒ›แƒแƒกแƒแƒšแƒ”แƒ‘แƒ˜แƒก แƒจแƒ”แƒกแƒแƒ แƒฉแƒ”แƒ•แƒแƒ“, แƒ แƒแƒ›แƒšแƒ”แƒ‘แƒ›แƒแƒช แƒจแƒ”แƒ˜แƒซแƒšแƒ”แƒ‘แƒ แƒ›แƒ˜แƒ’แƒ•แƒ˜แƒงแƒ•แƒแƒœแƒแƒก แƒฆแƒ แƒฃแƒ‘แƒšแƒ”แƒ‘แƒ˜แƒก แƒฎแƒ”แƒšแƒแƒ•แƒœแƒฃแƒ  แƒ”แƒšแƒ”แƒฅแƒขแƒ แƒ˜แƒ–แƒ”แƒ‘แƒแƒ›แƒ“แƒ”
    corecore