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Analysis of Groundwater Level Changes Due to Earthquake in Jeju Island (For the Indonesian Earthquake with Magnitude 7.7 in 2010)

지진에 의한 제주도 지하수위 변동 분석 (2010년 인도네시아 규모 7.7 지진)

  • Lee, Soo-Hyoung (Korea Institute of Geoscience and Mineral Resources) ;
  • Hamm, Se-Yeong (Division of Earth Environmental System, Pusan National University) ;
  • Ha, Kyoo-Chul (Korea Institute of Geoscience and Mineral Resources) ;
  • Kim, Yong-Cheol (Korea Institute of Geoscience and Mineral Resources) ;
  • Cheong, Beom-Keun (Korea Institute of Geoscience and Mineral Resources) ;
  • Ko, Kyung-Seok (Korea Institute of Geoscience and Mineral Resources) ;
  • Koh, Gi-Won (Water Resource Headquarter, Jeju Special Self-Governing Province) ;
  • Kim, Gee-Pyo (Water Resource Headquarter, Jeju Special Self-Governing Province)
  • Received : 2010.11.29
  • Accepted : 2011.04.01
  • Published : 2011.04.30

Abstract

This study was conducted to investigate the relationship between groundwater level change and a large earthquake using the data of groundwater and seawater intrusion monitoring wells in Jeju Island. Groundwater level data from 13 observation wells were analyzed with a large earthquake. The Earthquake occurred at Sumatra, Indonesia (Mw = 7.7) on 13 June 2010, and groundwater level anomalies which seems to be related to the Earthquake were found in 6 monitoring wells. They lasted for approximately 16~27 minutes and the range of groundwater level fluctuations were about 1.4~2.4 cm. Coefficient of determination values for relationship between groundwater level change and transmissivity, and response time were calculated to be $R^2$ = 0.76 and $R^2$ = 0.96, respectively. The study also indicates that the high transmissivity of aquifer showed the high goundwater level changes and longer response time.

Keywords

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