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JAEA Reports

Study on modeling and analysis of groundwater flow with inverse analysis, 2 (Joint research)

Onoe, Hironori; Yamamoto, Shinya*; Kohashi, Akio; Ozaki, Yusuke; Sakurai, Hideyuki*; Masumoto, Kiyoshi*

JAEA-Research 2018-003, 84 Pages, 2018/06

JAEA-Research-2018-003.pdf:17.44MB

In this study, numerical experiments considered hydrogeological structures, which has high heterogeneity around the Mizunami Underground Research Laboratory and inverse analysis using in-situ data were carried out. The results showed that concentration of hydrogeological structure to be estimated and location of monitoring point is important for application of inverse analysis. Furthermore, it is concluded that inverse analysis using hydraulic response due to pumping test is effective for hydrogeological characterization.

JAEA Reports

Study on modeling and analysis of groundwater flow with inverse analysis (Joint research)

Kohashi, Akio; Onoe, Hironori; Yamamoto, Shinya*; Honda, Makoto*; Sakurai, Hideyuki*; Masumoto, Kiyoshi*

JAEA-Research 2015-022, 89 Pages, 2016/03

JAEA-Research-2015-022.pdf:27.85MB

In Japan, high-level radioactive waste (HLW) will be emplaced in a stable host rock formation deeper than 300 meters underground for geological disposal. It is important to understand heterogeneous distribution of hydraulic conductivity from the viewpoints of the safety assessment of geological disposal of HLW and construction of underground facilities. Inverse analysis based on the transient data is an efficient technique for estimating the heterogeneous distribution. In this study, numerical experiments with the adjoint state method and the ensemble Kalman filter were carried out in order to understand effective method for application of these inverse analysis. As a result of this study, the capability of each analysis techniques was shown.

Journal Articles

Groundwater flow modeling focused on the Fukushima Daiichi Nuclear Power Plant site

Saegusa, Hiromitsu; Onoe, Hironori; Kohashi, Akio; Watanabe, Masahisa

Proceedings of 23rd International Conference on Nuclear Engineering (ICONE-23) (DVD-ROM), 7 Pages, 2015/05

Fukushima Daiichi Nuclear Power Plant of Tokyo Electric Power Company is facing contaminated water issues. The amount of contaminated water is continuously increasing due to groundwater leakage into the underground part of reactor and turbine buildings. Therefore, it is important to understand the groundwater flow conditions at the site and to predict the impact of countermeasures taken for isolating groundwater from the source of the contamination, i.e. the reactor buildings. Installations, such as of land-side and sea-side impermeable walls have been planned as countermeasures. In this study, groundwater flow modeling has been performed to estimate the response of groundwater flow conditions to the countermeasures. From the modeling, groundwater conditions and changes in response to implementation of the countermeasures could be reasonably estimated. The results indicate that the countermeasures will decrease the volume of inflow into underground part of the buildings. This means that the countermeasures will be effective in reducing the discharge volume of contaminated groundwater to ocean.

Oral presentation

Mizunami Underground Research Laboratory Project; Hydrogeological study during the construction phase

Onoe, Hironori; Beppu, Shinji; Onuki, Kenji; Kohashi, Akio; Takeuchi, Ryuji; Saegusa, Hiromitsu

no journal, , 

no abstracts in English

Oral presentation

Inverse analysis methods for characterization of hydrogeological heterogeneity, 1; Numerical experiments with adjoint state method

Masumoto, Kiyoshi*; Onoe, Hironori; Kohashi, Akio; Yamamoto, Shinya*

no journal, , 

no abstracts in English

Oral presentation

Inverse analysis methods for characterization of hydrogeological heterogeneity, 3; The Influence of analysis methodology on the estimated result

Onoe, Hironori; Yamamoto, Shinya*; Masumoto, Kiyoshi*; Kohashi, Akio; Saegusa, Hiromitsu

no journal, , 

no abstracts in English

Oral presentation

Inverse analysis methods for characterization of hydrogeological heterogeneity

Kohashi, Akio; Onoe, Hironori; Yamamoto, Shinya*; Honda, Makoto*; Sakurai, Hideyuki*; Masumoto, Kiyoshi*

no journal, , 

no abstracts in English

Oral presentation

Mizunami Underground Research Laboratory Project; Hydrogeological study during the operation phase; Understanding of hydrogeological study on groundwater recovery experiment in tunnel

Beppu, Shinji; Onoe, Hironori; Kohashi, Akio; Ueno, Tetsuro; Takayasu, Kentaro; Takeuchi, Ryuji; Ishibashi, Masayuki; Sawada, Atsushi

no journal, , 

no abstracts in English

Oral presentation

Estimation of hydraulic conductivity in fault zone by inversion of water head data

Ozaki, Yusuke; Kohashi, Akio; Onoe, Hironori; Yamamoto, Shinya*; Masumoto, Kiyoshi*

no journal, , 

The objective of this study is verification of feasibility to estimate hydraulic conductivity with inversion method of water head data in fault zone. Hydraulic conductivity in a fault zone is focused on as a target of inversion because the fault would significantly affect a water head field. A series of numerical test with synthetic model is performed under the condition that the number of fault to estimate hydraulic conductivity and the degree of freedom of hydraulic conductivity distribution in a fault zone is different. The information of hydraulic conductivity outside the faults and location of fault is given to the inversion a priori. Our inversion results shows that the accuracy of estimation is improved by constrain to the number of fault to estimate the hydraulic conductivity and freedom of hydraulic conductivity distribution in a fault. In addition, the number of fault to estimate the hydraulic conductivity should be limited for the certain estimation of hydraulic conductivity in all faults.

Oral presentation

Large scale transient hydraulic tomography with smoothness constraint

Ozaki, Yusuke; Kohashi, Akio; Onoe, Hironori

no journal, , 

no abstracts in English

Oral presentation

Mizunami Underground Research Laboratory Project; Study on groundwater recovery experiment; Water pressure change of groundwater during the water filling of the research gallery

Keya, Hiromichi; Takayasu, Kentaro; Kohashi, Akio; Onoe, Hironori; Takeuchi, Ryuji

no journal, , 

no abstracts in English

Oral presentation

Joint research of Shimizu corporation and Japan Atomic Energy Agency; Study on modeling and analysis of groundwater flow with inverse analysis

Ozaki, Yusuke; Kohashi, Akio; Onoe, Hironori; Yamamoto, Shinya*; Sakurai, Hideyuki*; Masumoto, Kiyoshi*

no journal, , 

no abstracts in English

Oral presentation

Mizunami Underground Research Laboratory Project, Study on groundwater recovery experiment; Hydrological investigation and analysis during temporal decompression test

Ozaki, Yusuke; Kohashi, Akio; Keya, Hiromichi; Onoe, Hironori; Takeuchi, Ryuji

no journal, , 

In Mizunami Underground Research Laboratory, groundwater recovery experiment test is performed at a part of research tunnel at 500m depth for research of recovery process of subsurface environment disturbed by construction of subsurface structure. During 2017, three times temporal decompression tests of hydraulic pressure in closure test drift keeping closed condition were conducted. We report the reproductivity of time variation of hydraulic pressure during the tests. We also report the estimation results of hydrogeological structure from the data during tests.

Oral presentation

Hydro-Mechanical (HM) response during compression and decompression of hydraulic pressure

Ozaki, Yusuke; Matsui, Hiroya; Kohashi, Akio; Onoe, Hironori

no journal, , 

In this study, we introduce the hydro-mechanical behavior observed in the fracture granite medium. The rock deformation due to the change in hydraulic pressure according to the borehole drilling was observed at the 500m stage in Mizunami underground research laboratory. The observed data of rock deformation shows the elastic behavior although the several fractures are observed in the monitoring borehole. We conduct a numerical simulation for the evaluation of this behavior by using finite element methods. The magnitude of simulated deformation is similar value with the observed data. From these results, we conclude that the movement of fracture joints is slight and the subsurface facility is stable to the change in hydraulic response.

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