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• W2320804517 abstract "Brief Report| May 01, 2013 Successive Groundwater Level Changes on Jeju Island due to the Mw 9.0 Off the Pacific Coast of Tohoku Earthquake Soo‐Hyoung Lee; Soo‐Hyoung Lee Korea Institute of Geoscience and Mineral Resources (KIGAM), 124 Gajeong‐dong Yuseong‐gu, Daejeon 305‐350, South Korearbagio@hanmail.nethasife@kigam.re.krjinsoo@kigam.re.krkyungsok@kigam.re.kr Search for other works by this author on: GSW Google Scholar Kyoochul Ha; Kyoochul Ha Korea Institute of Geoscience and Mineral Resources (KIGAM), 124 Gajeong‐dong Yuseong‐gu, Daejeon 305‐350, South Korearbagio@hanmail.nethasife@kigam.re.krjinsoo@kigam.re.krkyungsok@kigam.re.kr Search for other works by this author on: GSW Google Scholar Jin Soo Shin; Jin Soo Shin Korea Institute of Geoscience and Mineral Resources (KIGAM), 124 Gajeong‐dong Yuseong‐gu, Daejeon 305‐350, South Korearbagio@hanmail.nethasife@kigam.re.krjinsoo@kigam.re.krkyungsok@kigam.re.kr Search for other works by this author on: GSW Google Scholar Kyung‐Seok Ko; Kyung‐Seok Ko Korea Institute of Geoscience and Mineral Resources (KIGAM), 124 Gajeong‐dong Yuseong‐gu, Daejeon 305‐350, South Korearbagio@hanmail.nethasife@kigam.re.krjinsoo@kigam.re.krkyungsok@kigam.re.kr Search for other works by this author on: GSW Google Scholar Se‐Yeong Hamm Se‐Yeong Hamm Division of Earth Environmental System, Pusan National University, 30 Jangjeon‐Dong Geumjeong‐Gu, Busan 609‐735, South Koreahsy@pusan.ac.kr Search for other works by this author on: GSW Google Scholar Author and Article Information Soo‐Hyoung Lee Korea Institute of Geoscience and Mineral Resources (KIGAM), 124 Gajeong‐dong Yuseong‐gu, Daejeon 305‐350, South Korearbagio@hanmail.nethasife@kigam.re.krjinsoo@kigam.re.krkyungsok@kigam.re.kr Kyoochul Ha Korea Institute of Geoscience and Mineral Resources (KIGAM), 124 Gajeong‐dong Yuseong‐gu, Daejeon 305‐350, South Korearbagio@hanmail.nethasife@kigam.re.krjinsoo@kigam.re.krkyungsok@kigam.re.kr Jin Soo Shin Korea Institute of Geoscience and Mineral Resources (KIGAM), 124 Gajeong‐dong Yuseong‐gu, Daejeon 305‐350, South Korearbagio@hanmail.nethasife@kigam.re.krjinsoo@kigam.re.krkyungsok@kigam.re.kr Kyung‐Seok Ko Korea Institute of Geoscience and Mineral Resources (KIGAM), 124 Gajeong‐dong Yuseong‐gu, Daejeon 305‐350, South Korearbagio@hanmail.nethasife@kigam.re.krjinsoo@kigam.re.krkyungsok@kigam.re.kr Se‐Yeong Hamm Division of Earth Environmental System, Pusan National University, 30 Jangjeon‐Dong Geumjeong‐Gu, Busan 609‐735, South Koreahsy@pusan.ac.kr Publisher: Seismological Society of America First Online: 14 Jul 2017 Online ISSN: 1943-3573 Print ISSN: 0037-1106 Bulletin of the Seismological Society of America (2013) 103 (2B): 1614–1621. https://doi.org/10.1785/0120120054 Article history First Online: 14 Jul 2017 Cite View This Citation Add to Citation Manager Share Icon Share Facebook Twitter LinkedIn MailTo Tools Icon Tools Get Permissions Search Site Citation Soo‐Hyoung Lee, Kyoochul Ha, Jin Soo Shin, Kyung‐Seok Ko, Se‐Yeong Hamm; Successive Groundwater Level Changes on Jeju Island due to the Mw 9.0 Off the Pacific Coast of Tohoku Earthquake. Bulletin of the Seismological Society of America 2013;; 103 (2B): 1614–1621. doi: https://doi.org/10.1785/0120120054 Download citation file: Ris (Zotero) Refmanager EasyBib Bookends Mendeley Papers EndNote RefWorks BibTex toolbar search Search Dropdown Menu toolbar search search input Search input auto suggest filter your search All ContentBy SocietyBulletin of the Seismological Society of America Search Advanced Search Abstract Changes in groundwater levels on Jeju Island, which is ∼1500 km from the epicenter of the 2011 Mw 9.0 Off the Pacific Coast of Tohoku earthquake in Japan, were analyzed. The results show a series of water level fluctuations related to the foreshock (Mw 7.3 and Mw 6.1) and aftershock (Mw 7.9) in addition to the mainshock (Mw 9.0). The groundwater‐level changes in response to the earthquake were oscillatory, and the groundwater levels at some wells had an irregular pattern after the Mw 9.0 earthquake, although they recovered in five to seven days. This phenomenon may reflect the unstable elastic aquifer properties that are present for a period of time after a large earthquake. In addition, the successive groundwater‐level change was different for each magnitude and well location. The magnitude increases the groundwater‐level change, but the response amplitude is also dependent on the hydrogeological characteristics at the well. On Jeju Island, the groundwater‐level changes due to the earthquake generally increased where there was more volcanic hard rock and more permeable layers, but these changes were inversely correlated with the presence of sedimentary deposits with less permeability and less restrictive characteristics. You do not have access to this content, please speak to your institutional administrator if you feel you should have access." @default.
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