Sulfur hexafluoride (SF
6), chlorofluorocarbons (CFCs), stable isotopic composition of oxygen and deuterium (δ
18O, δD), radioisotope tritium and dissolved major ions in groundwater were measured for groundwater age dating to provide indication of the groundwater flow mechanism in the Shimekake landslide area, Yamagata, Japan. It can be found from this study that SF
6 is effective in dating the shallower groundwater, and tritium is effective in dating the deeper groundwater in the landslide. The comparison of the results of groundwater age dating and the observed groundwater chemistry suggests that older groundwater indicates the lower (Ca
2++Mg
2+)/HCO
3- ratio, especially, and this ratio can be thus applicable to the validation of age dating. Investigating δ
18O in groundwater with depth, in addition to topographical and geological data, can reveal the multi-layered groundwater flow in the landslide block, and can be effective in implying that groundwater flows into the landslide block from different recharge areas with different residence times. It is thus deduced that when used together, these environmental tracers applied in this study can help to classify groundwater drained from countermeasure works in a landslide area based on groundwater age.
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