“…The hydrogeochemical studies mainly include the monitoring in water level changes, Rn variability in either air, soil, or groundwater, an emanation of soil gases (CO 2 , CH 4 , and He), and other constituents such as Cl − , SO 2− 4 , and HCO − 3 are also used as a forerunner to access the earthquake-induced changes [7,10,11,[24][25][26][27]. However, the use of Rn is globally preferred in comparison with other precursors due to its relatively long half-life and ease of predictability [14].…”