The contaminated water issues at the Fukushima Daiichi Nuclear Power Station (NPS) of the Tokyo Electric Power Company, Incorporated (TEPCO) have not been solved yet even after 4 years since the severe nuclear accident triggered by the 2011 off the Pacific coast of Tohoku Earthquake. The issues are crucial for the safe decommissioning of the Fukushima Daiichi NPS, however, there have been many problems related to the contaminated water. The groundwater bypass, that has been employed as one of the countermeasures to reduce the ingress of groundwater into the reactor and turbine buildings is not effective as expected. These are due to the lack of investigations and understanding on the complex geology and hydrogeology at the site. The hydrogeological profiles and subsequent groundwater simulation models prepared by the TEPCO and the Government of Japan are very simple. Although the disclosed columnar sections in the NPS site are limited, it was revealed that the facies of the D4 unit of the Dainenji Formation, which is mainly composed of mudstone and sandstone, significantly changes even in a local scale. In this paper, the author reviewed the geological background of the NPS site, brief history of the contaminated water issues, subsurface ground conditions below the contaminated water tanks, and problems on geological and hydrogeological data with subsequent groundwater modeling analysis. The author also pointed out the geological challenges of the on-going measures to reduce groundwater ingress, such as groundwater bypass, frozen (ice) wall, and the activating of the subdrain system in the NPS.
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