Diffusion experiment using block sample of the Toki granite

Hama, Katsuhiro; Iwasaki, Riyo*; Morikawa, Keita*

JAEA-Technology 2017-015, 45 Pages, 2017/07

JAEA-Technology-2017-015.pdf:16.57MB

Tono Geoscience Center of Japan Atomic Energy Agency has been carrying out the Mizunami Underground Research Laboratory Project. The goal of mass transport study is to obtain a better understanding of mass transport phenomena in the geological environment as well as to develop technologies for measurement of the mass transport parameters, model construction, numerical analysis and validation of those technologies. This experiment was planned to understand the influence of the microscopic structure in the rock mass on the mass transport property. The diffusion experiment using rock sample was carried out. The macroscopic and microscopic observations were carried out to understand the distribution of tracer (uranine) after the diffusion experiment. The uranine was observed in the plagioclase, in the grain boundary and in the microfracture in the mineral grains. These results suggested that distribution of mineral and of microfracture could affect the diffusion property of uranine.

Comprehensive study of the migration property in representative rock of Japan at underground research laboratories

Iwatsuki, Teruki; Ishii, Eiichi

no journal, , 

The paper reviews the applicable knowledge of the migration properties in deep underground gained by R&D in Mizunami and Horonobe URL. Summing up the major migration path, it is necessary to consider the fracture continuity / connectivity of hundreds of meters in granite of Mizunami area, while several hundred meters in the shallow part of sedimentary rock and of tens m scale in the deep part of Horonobe. On the other hand, it was also demonstrated that analogue elements are practically immobile in rock masses and closed galleries.