Seismically induced changes in groundwater levels and temperatures following the ML5.8 (ML5.1) Gyeongju earthquake in South Korea

Hydrogeological responses to earthquakes such as changes in groundwater level, temperature, and chemistry, have been observed for several decades. This study examines behavior associated with M L 5.8 and M L 5.1 earthquakes that occurred on 12 September 2016 near Gyeongju, a city located on the sout...

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Veröffentlicht in:Hydrogeology journal 2021-06, Vol.29 (4), p.1679-1689
Hauptverfasser: Lee, Soo-Hyoung, Lee, Jae Min, Moon, Sang-Ho, Ha, Kyoochul, Kim, Yongcheol, Jeong, Dan Bi, Kim, Yongje
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Kim, Yongje
description Hydrogeological responses to earthquakes such as changes in groundwater level, temperature, and chemistry, have been observed for several decades. This study examines behavior associated with M L 5.8 and M L 5.1 earthquakes that occurred on 12 September 2016 near Gyeongju, a city located on the southeast coast of the Korean peninsula. The M L 5.8 event stands as the largest recorded earthquake in South Korea since the advent of modern recording systems. There was considerable damage associated with the earthquakes and many aftershocks. Records from monitoring wells located about 135 km west of the epicenter displayed various patterns of change in both water level and temperature. There were transient-type, step-like-type (up and down), and persistent-type (rise and fall) changes in water levels. The water temperature changes were of transient, shift-change, and tendency-change types. Transient changes in the groundwater level and temperature were particularly well developed in monitoring wells installed along a major boundary fault that bisected the study area. These changes were interpreted as representing an aquifer system deformed by seismic waves. The various patterns in groundwater level and temperature, therefore, suggested that seismic waves impacted the fractured units through the reactivation of fractures, joints, and microcracks, which resulted from a pulse in fluid pressure. This study points to the value of long-term monitoring efforts, which in this case were able to provide detailed information needed to manage the groundwater resources in areas potentially affected by further earthquakes.
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source Springer Nature - Complete Springer Journals
subjects Aquatic Pollution
Aquifer systems
Aquifers
Earth and Environmental Science
Earth Sciences
Earthquake damage
Earthquakes
Fluid pressure
Fractures
Geology
Geophysics/Geodesy
Groundwater
Groundwater chemistry
Groundwater levels
Groundwater resources
Hydrogeology
Hydrology/Water Resources
Information management
Joints (timber)
Microcracks
Monitoring
P-waves
Seismic activity
Seismic response
Seismic waves
Temperature changes
Waste Water Technology
Water level fluctuations
Water levels
Water Management
Water Pollution Control
Water Quality/Water Pollution
Water resources
Water temperature
title Seismically induced changes in groundwater levels and temperatures following the ML5.8 (ML5.1) Gyeongju earthquake in South Korea
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