会议专题

A preliminary interpretation of groundwater chemistry in the Horonobe area, Japan

A present study shows a preliminary interpretation of groundwater chemistry based on data obtained from the surface-based investigation phase in the Horonobe URL. The evolution of groundwater in the argillaceous rock could be interpreted as the dilution of fossil seawater, accompanied by diagenetic waterrock interactions. The groundwaters were categorized into three types on the basis of multivariate geostatistical techniques. Results of thermodynamic calculations suggested that the effect on groundwater chemistry by perturbation during sampling. Thus a simple correction method assuming a partial equilibrium with mineral-water interactions was provisionally applied to estimate the in-situ geochemical conditions of groundwater.

H.Sasamoto M.Yui K.Hama

Japan Atomic Energy Agency (JAEA)*, Tokai Research and Development Center, Nuclear Fuel Cycle Engine Japan Atomic Energy Agency*, Mizunami Underground Research Laboratory, Yamanouchi, Akeyo-cho,Mizunam

国际会议

第十二届水-岩相互作用国际研讨会(P0roceedings of the 12th International Symposium on Water-Rock Interaction)

昆明

英文

385-389

2007-07-31(万方平台首次上网日期,不代表论文的发表时间)