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Three-dimensional analysis of groundwater flow in neogene rocks at the Rokkasho low-level radioactive waste disposal center, Japan
Authors:Tai Sasaki  Naro Hashimoto  Takayuki Nakato  Tomonari Shiraishi  Kazuaki Yajima  Tomoyuki Hishiya
Institution:

aJapan Nuclear Fuel, Ltd, Civil and Architectural Engineering Department, Uchisaiwai, Chiyoda, Fukoku seimei Bld. 2-2-2, Tokyo 100,Japan

bMitsubishi Materials Corporation, 1-3-25, Koishikawa Bunkyo, Tokyo 112,Japan

cShimizu Corporation, 1-2-3, Shibaura, Minato, Tokyo 105-07,Japan

dDia Consultants Co., Ltd., 2-272-3, Yoshino, Oomiya, Saitama 330,Japan

Abstract:As a preliminary step for predicting groundwater flow in a plateau 30–50 m above sea level, a model for three-dimensional analysis of groundwater flow was formulated and its validity was verified. The plateau consists of Neogene sedimentary rocks and a Quaternary deposit. Most of the groundwater originates in precipitation, with the groundwater table lying in the Quaternary deposit. Steady-state analysis was conducted by using the finite element method. The results of pore-water pressure measurement and water examination were useful in verifying the validity of the model. In constructing the model, reducing the hydraulic conductivity according to the depth on the basis of the results of the actual measurement was important.
Keywords:Groundwater flow analysis  Hydraulic conductivity  Water quality
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