Geophysical research of underground hydraulic structures, old Glubochinsky water tunnel case study

IF 0.2 Q4 FORESTRY
V. Davydov, V. Gorshkov, A. Vdovin
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Abstract

Research objective is to study the features of geophysical fields and parameters in the area of the artificial underground water tunnel and estimate the capabilities of geophysical methods of identifying hidden underground industrial facilities. Methods of research. Measurements of self-potential signals (SP) were carried out using nonpolarizing electrodes and an electrical exploration receiver. The magnetic exploration was carried out by a proton magnetometer. Electrotomography was carried out using multielectrode electrical survey equipment with a Schlumberger symmetrical scheme of surveys. The microseismic background was recorded using an autonomous seismic station. The georadar survey was carried out using the SIR-3000 ground penetrating radar and antennas with the frequencies of 100 MHz and 270 MHz. Results. Based on the survey results, graphs of magnetic and self-potential fields, electrotomographic and microseismic sections, and radarogram were built on the research profile. The research has shown different levels of the magnetic field and the SP in the area of volcanic rocks and dikes of gabbro-dolerites occurrence. A significant increase in microseismic noise was observed with an increase in the weathering crust thickness. A local decrease in the SP potential, abnormally high values of specific electrical resistivity and intensive reflections of radio waves from the tunnel top were recorded above the underground water tunnel. Conclusions. Qualitative and quantitative geophysical characteristics were obtained in the area of the old underground water tunnel. The research showed different levels of the magnetic field and spontaneous polarization potentials in the occurrence area of rocks of different composition. A significant increase in microseismic noise was recorded with an increase in the weathering crust thickness. Geophysical signs of the boundaries between geological structures and artificial underground objects are revealed. The exact position and depth of the old underground tunnel of Glubochinsky hydraulic structures was determined.
地下水工构筑物地球物理研究,老格洛博钦斯基水洞实例研究
研究目的是研究人工地下水隧洞区域的地球物理场特征和参数,评价地球物理方法识别地下隐伏工业设施的能力。研究方法。采用非极化电极和电探测接收机对自电位信号进行测量。磁探测是用质子磁强计进行的。采用斯伦贝谢对称测量方案的多电极电测量设备进行电层析成像。微地震背景是用自主地震台站记录的。地质雷达调查使用SIR-3000型探地雷达和频率分别为100兆赫和270兆赫的天线进行。结果。根据调查结果,建立了研究剖面的磁场图、自势场图、电断层图、微地震剖面和射线图。研究表明,在火山岩区和辉长榴辉岩脉区存在不同程度的磁场和SP。微震噪声随风化壳厚度的增加而显著增加。地下水隧道上方局部电位下降,比电阻率异常高,隧道顶部无线电波反射强烈。结论。获得了旧地下水隧洞区域的定性和定量地球物理特征。研究表明,不同成分岩石的赋存区具有不同的磁场强度和自发极化电位。微震噪声随风化壳厚度的增加而显著增加。揭示了地质构造与地下人工物体边界的地球物理标志。确定了格洛博钦斯基水工建筑物旧地下隧道的确切位置和深度。
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