Determining Stress State of Source Media with Identified Difference between Groundwater Level during Loading and Unloading Induced by Earth Tides

• Published in: Water (Basel) Vol. 13; no. 20; p. 2843
• Main Authors: Yu, Huaizhong, Yu, Chen, Ma, Yuchuan, Zhao, Binbin, Yue, Chong, Gao, Rong, Chang, Yulong
• Format: Journal Article
• Language: English
• Published: Basel MDPI AG 01.10.2021
• Subjects: coulomb failure stress change; Dilatancy; Earth crust; earth tide; Earth tides; Earthquakes; geodetic time series; Groundwater; groundwater level; Groundwater levels; loading and unloading phases; Observation wells; Seismic activity; Shear stress; Stress; Stress state; Tides; Time series; Water levels; China; Japan
• ISSN: 2073-4441; 2073-4441
• DOI: 10.3390/w13202843

The groundwater level might be adopted as a useful tool to explore pre-seismic stress change in the earth crust, because it circulates in the deep crust and should be altered by the processes associated with the preparation of earthquakes. This work makes a new attempt that applies the load/unload response ratio (LURR) technique to study the stress state of the source media before the large earthquakes by calculating the ratio between the water levels during the loading and unloading phases. The change of Coulomb failure stress induced by earth tides in the tectonically preferred slip direction on the fault surface of the mainshock is adopted for differentiating the loading and unloading periods. Using this approach, we tested the groundwater level in the wells near the epicenters of some large earthquakes that occurred in the Sichuan-Yunnan region of southwest China. Results show that the LURR time series fluctuated narrowly around 1.0 for many years and reached anomalously high peaks 2~8 months prior to the mainshocks. For the earthquakes with multiple observation wells, the magnitude of the maximum values decreases with the distance from the epicenter. The underlying physics of these changes should be caused by the pre-seismic dilatancy. The corresponding volume variations in the crust could be observed in the geodetic time series in the same neighborhoods and during the same period.