Japan Geoscience Union Meeting 2019

Presentation information

[J] Oral

H (Human Geosciences ) » H-CG Complex & General

[H-CG31] Nuclear Energy and Geoscience

Thu. May 30, 2019 9:00 AM - 10:30 AM 101 (1F)

convener:Eiji Sasao(Tono Geoscience Center, Japan Atomic Energy Agency), Ryuta Hataya(Central Research Institute of Electric Power Industry), Shinji Takeuchi(Department of Earth and Environmental Sciences, College of Humanities & Sciences, Nihon University), Chairperson:Tadafumi Niizato

9:15 AM - 9:30 AM

[HCG31-02] Deep groundwater mobility at costal area estimated by groundwater dating

*Takuma HASEGAWA1, Kotaro NAKATA1, Yuichi Tomioka1, Tomoko Ota1, Atsunao Marui2, Isao Machida2, Reo Ikawa2, Masahiko Ono2, Shinji Matsumoto2 (1.Central Research Institute of Electric Power Industry, 2.The National Institute of Advanced Industrial Science and Technology)

Keywords:groundwater dating, costal area, radioactive isotopes

On high-level radioactive waste disposal, “Nationwide map of Scientific Features for Geological Disposal” was published and costal area is the favorable from transportation point of view. To evaluate deep groundwater mobility at coastal area, groundwater was sampled from deep borehole at the order of 1000 m in depth. Major ions, tritium, carbon-14, chorine-36 were measured. Based on these results, the groundwaters were categorized into four groups, which are modern meteoric water, modern seawater, glacial meteoric water, fossil sea water. Meteoric water and seawater was divided by 1900 mg/l of Cl concentration. Modern and old groundwater was divided by 10 pMC of 14C concentration. The type of seawaters was well categorized into modern seawater and fossil seawater by 14C concentration because residence times of modern seawater and fossil seawater are quite different. 36Cl/Cl of Modern sea water is equivalent to that of present seawater (≒0.7×10-15), and that of fossil sea water is higher than that of present seawater. It indicates that 36C/Cl of fossil seawater influenced by in-situ production, which takes at least a few ten thousand years. Thus, the category of modern seawater and fossil seawater was validated by not only 14C but also 36Cl. Due to the lack of information, which are shallow groundwater and surface investigation, it could not be confirmed that modern meteoric water and glacial meteoric water was categorized by water isotopes and noble gas temperature. However, it is deduced the origin of Cl of meteoric water is from modern seawater and that of glacial meteoric water is from fossil sea water. It is though that the age of mixing water reflects the groundwater age.

As a result, the deep groundwaters at costal area were categorized into modern meteoric water and modern seawater about 40%, glacial and fossil seawater about 60%.

This study was performed under contracts “Development and Improvement on waste disposal system at coastal area” awarded by the Japanese Ministry of Economy, Trade and Industry.