12:15 〜 12:30
[AHW24-11] ^{85}Krを用いた地下水の滞留時間推定と他の水文トレーサーによるその検証
キーワード：クリプトン85, 地下水滞留時間, 地下水流動, 六フッ化硫黄, 年代トレーサー, 都城盆地
Krypton 85 (85Kr) is a man-made trace gas from reprocessing plant origin whose atmospheric concentrations have been increasing over the past few decades. As it is soluble in water, it can be used as groundwater age indicators over timescales ranging from a few years to a few decades. In this study, 85Kr specific activities in groundwater were measured with an on-site dissolved Kr gas extraction system using an external flow through type hollow fiber membrane modified after Ohta et al. (2009).
85Kr specific activities in groundwater were confirmed at 3 sites in Miyakonojo basin, south-western Japan, considering regional groundwater flow system. Estimated groundwater age were 2 years, 11 years and 60 years in the recharge, intermediate and stagnant discharge areas along the groundwater flow line, respectively. In order to verify these 85Kr ages, we also measured other age tracer gases such as Sulfur hexafluoride (SF6) and Chlorofluorocarbons (CFCs) at the same sampling wells of 85Kr measurement. The result of the SF6 age dating in the three locations were well harmonized with the 85Kr dating results; the SF6 age were 1 year, 23 years and over 60 years. However, CFCs could not show reasonable groundwater age due to the local contamination by the urban and industrial origin CFCs.
The seasonal fluctuation of the stable isotopes (δ18O and δD) in groundwater were also measured to evaluate the comprehensive groundwater age tendency. Relatively high seasonal fluctuation of the stable isotopes were measured only in the shallow unconfined well site at the recharge area, which reflect the seasonal isotopic fluctuation in the precipitation. This is another evidence of the relatively young groundwater characteristics to support the 85Kr and SF6 age in the recharge area.
85Kr specific activities in groundwater were confirmed at 3 sites in Miyakonojo basin, south-western Japan, considering regional groundwater flow system. Estimated groundwater age were 2 years, 11 years and 60 years in the recharge, intermediate and stagnant discharge areas along the groundwater flow line, respectively. In order to verify these 85Kr ages, we also measured other age tracer gases such as Sulfur hexafluoride (SF6) and Chlorofluorocarbons (CFCs) at the same sampling wells of 85Kr measurement. The result of the SF6 age dating in the three locations were well harmonized with the 85Kr dating results; the SF6 age were 1 year, 23 years and over 60 years. However, CFCs could not show reasonable groundwater age due to the local contamination by the urban and industrial origin CFCs.
The seasonal fluctuation of the stable isotopes (δ18O and δD) in groundwater were also measured to evaluate the comprehensive groundwater age tendency. Relatively high seasonal fluctuation of the stable isotopes were measured only in the shallow unconfined well site at the recharge area, which reflect the seasonal isotopic fluctuation in the precipitation. This is another evidence of the relatively young groundwater characteristics to support the 85Kr and SF6 age in the recharge area.