Earth Planets Space, Vol. 56 (No. 3), pp. 395-400, 2004LETTER
Tsutomu Sato1, Norio Matsumoto1, Yuichi Kitagawa1, Naoji Koizumi1, Makoto Takahashi1, Yasuto Kuwahara1, Hisao Ito1, Akio Cho1, Takashi Satoh1, Kunio Ozawa2, and Shigeki Tasaka3
1Geological Survey of Japan, AIST, 1-1-1 Higashi, Tsukuba, Ibaraki 305-8567, Japan
2Shizuoka Prefectural Government, 9-6 Ote-machi, Shizuoka, Shizuoka 420-8601, Japan
3Gifu University, 1-1 Yanagido, Gifu, Gifu 501-1193, Japan
(Received December 8, 2003; Revised February 5, 2004; Accepted February 18, 2004)
Groundwater level and flow rate at 44 wells are continuously observed by the Geological Survey of Japan and the Shizuoka and Gifu Prefectural Governments for monitoring seismic and volcanic activities. The 2003 Tokachi-oki earthquake (M8.0) occurred off the south coast of Hokkaido Island, Japan on September 26, 2003. The epicentral distance to the nearest observation well is about 250 km and that to the farthest is about 1200 km. At the 22 wells, we detected changes in groundwater level or flow rate in relation to the earthquake. Most of the changes are coseismic step-like changes and/or short-period oscillations. In the nearest two observation wells, long-period oscillations with the periods of 39 and 53 minutes were also observed for several days after the earthquake, which is likely due to tsunami. In comparison between distributions of changes in groundwater level and theoretical coseismic strain by the fault model, it is clear that step-like increases were found in the contraction area of the coseismic strain. The relationship between amounts of the observed step-like groundwater-level changes and theoretical ones, calculated by the fault model using strain sensitivities of groundwater level indicates that the groundwater levels in the several wells responded to the coseismic strain.
Key words: Groundwater level, flow rate, 2003 Tokachi-oki earthquake, coseismic strain, oscillation, tsunami.