THE STUDY OF DISSOLVED HELIUM AND RADON CONCENTRATIONS IN GROUNDWATERS OF SOUTHERN PRIBAIKALIE IN CONNECTION WITH SEISMIC PROCESSES

It is known that changes in geochemical fields may be due to the formation and development of earthquake foci. Hydrogeochemical fields at observation sites can be disturbed by underground shocks of sufficient energy, which occur at specific epicentral distances. Our study aimed to reveal these relationships by analysing the concentrations of helium and radon in groundwaters of Southern Pribaikalie, the area around Lake Baikal in Russia. Water samples were taken daily at 10 a.m. from artesian well No. 3 in Zeleny Mys, Irkutsk region. After water sparging, radon concentrations were measured by beta-detection Camera-01 and INGEM-1 (magnetic discharge indicator of helium) to determine helium concentrations. We analysed the concentration values in connection with 22 seismic events that occurred from 2010 to 2016 at the hydrogeochemical observation site (energy classes K of 10.4–14.5; epicentral distances of 40–750 km; conditional energy of K’>6). Based on the radon and helium concentration diagrams, specific regularities were established in the concentration variations before the earthquakes. Generally, concentration variations (increasing/decreasing) in excess of 1.5–2.0 standard deviations preceded earthquakes. This article presents the study results and discusses variations in the radon and helium concentrations, which are due to the seismic process and can be considered as a short-term precursor of earthquakes.

seismicity, radon, helium, earthquake energy class, epicentral distance, earthquake precursor

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