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Nakamura, Takahiro; Sanada, Hiroyuki; Sugita, Yutaka; Teshima, Minoru*; Kasagi, Toshio*; Kishimoto, Munemaru*; Deguchi, Tomonori*; Makuuchi, Ayumu*
JAEA-Research 2010-006, 68 Pages, 2010/06
JAEA-Research-2010-006.pdf:33.19MB
The present document is to report the result of geophysical survey by electric survey around a site proposed for the Horonobe Underground Research Laboratory Project at Horonobe-cho, Hokkaido by the Japan Atomic Energy Agency. This Electric survey using pole-pole array in Horonobe Underground Research Laboratory Area was the third survey. Resistivity distribution near surface was about 20 
m and it become to about 2 m as the depth increasing. Resistivity distribution was good agreement with existing survey results and existing electrical resistivity log data. By comparing resistivity model with hydrology model, it was confirmed that resistivity reflected the density of salinity. The range and distribution trends of apparent resistivity in this year were similar to the results of last year. It is thought that the data in which reproducibility is high is acquired in this survey. The influence on the underground water flow by construction is not admitted now.
Nakamura, Takahiro; Sanada, Hiroyuki; Sugita, Yutaka; Teshima, Minoru*; Kishimoto, Munemaru*; Matsuo, Koichi*
JAEA-Research 2008-102, 58 Pages, 2009/03
JAEA-Research-2008-102.pdf:48.97MB
The present document is to report the result of geophysical survey by electric survey around a site proposed for the Horonobe Underground Research Laboratory Project at Horonobe-cho, Hokkaido by the Japan Atomic Energy Agency. This Electric survey using pole-pole array in Horonobe Underground Research Laboratory Area was the second survey. Resistivity distribution near surface was about 20 ohm-m and it become to about 2 ohm-m as the depth increasing. Resistivity distribution was good agreement with existing survey results and existing electrical resistivity log data. By comparing resistivity model with hydrology model, it was confirmed that resistivity reflected the density of salinity. The range and distribution trends of apparent resistivity in this year were similar to the results of last year. It is thought that the data in which reproducibility is high is acquired in this survey. The influence on the underground water flow by construction is not admitted now.
Matsuo, Koichi*; Kishimoto, Munemaru*; Makuuchi, Ayumu*; Teshima, Minoru*; Sanada, Hiroyuki; Niunoya, Sumio*; Matsui, Hiroya
JAEA-Research 2008-071, 44 Pages, 2008/09
JAEA-Research-2008-071.pdf:29.04MB
Correlation between resistivity in rock mass and groundwater quality is shown from the results of investigation such as borings and geophysical exploration. Electrical resistivity survey had been done to understand impact on behavior of groundwater by construction of underground research laboratory. This paper shows distribution of resistivity around underground research laboratory obtained from electrical resistivity survey.
Matsuo, Koichi*; Kishimoto, Munemaru*; Negi, Tateyuki*; Teshima, Minoru*
JNC TJ5440 2005-001, 51 Pages, 2005/08
JNC-TJ5440-2005-001.pdf:15.08MB
The present document is to report the results of geophysical survey by electric syrvey around a site proposed for the Horonobe Underground Research Project at Horonobe-cho, Hokkaidou by JNC. Electrical survey using dipole-diple array was carried out at the area of Hokushin in Horonobe-cho near presumued Omagari-fault. Two dimensional resistivity inversion analysis was carried out and the resistivity structure from the surface to 250m below the sea level became clear.