Estimation of groundwater residence time based on $^{4}$ He, $^{36}$ Cl at Horonobe area, Hokkaido

Nakata, Kotaro*; Hasegawa, Takuma*; Iwatsuki, Teruki

Groundwater residence time were inferred by $^{4}$ He, $^{36}$ Cl at Horonobe area, Hokkaido, Japan. Both estimated value based on $^{4}$ He and $^{36}$ Cl range from 2Ma to 10Ma for the groundwater deeper than -250m S.L. Those values correspond to sedimentation age of rock formations. This indicates the possibility that the groundwaters are in stagnant condition since sedimentation.

Language	:	Japanese
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Meeting title	:	日本地下水学会2009年秋季講演会
Held date	:	2009/10
Location (city)	:	札幌
Location (country)	:	日本
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Keywords	:	no keyword
Research Facility	:	深地層研究所
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Article of JAEA R&D Review	:
Cooperating Institute	:	電力中央研究所

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Registration No. : BB20091991
JAEA Abstracts No. :
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Estimation of groundwater residence time based on He, Cl at Horonobe area, Hokkaido

Estimation of groundwater residence time based on $^{4}$ He, $^{36}$ Cl at Horonobe area, Hokkaido