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Report No.
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A study of ground water flow in Japan

Hibiya, Keisuke*; not registered; Shiogama, Yukihiro*; not registered; Masumoto, Kazuhiko*; Furuichi, Mitsuaki*; Saegusa, Hiromitsu

In order to understand groundwater flow in Japan, it is important to know the hydraulic gradient and the sea / fresh-water boundaly. In particular, the hydraulic gradient is required to estimate very slow groundwater flow at depth. Also, the location of the sea / fresh-water boundary is required to characterize groundwater flow near the coast. In this study, we obtained the above-mentioned data from a number of published papers, and tried to find the suitable method to help evaluating the groundwater flow model.

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