Abstract
Radon and stable nuclides were used as a tracer of groundwater/surface water interaction study in a artificial groundwater recharge system near Nakdong river in Korea. The 222Rn concentration at the observation well groundwater was decreased. The activity variation of each monitoring wells during short and long term experiment were 6.5–12.4 Bq/L at OBS-1, 3.8–6.8 Bq/L at OBS-2, 30.9–55.9 Bq/L at OBS-3, 5.9–25.5 Bq/L at OBS-4, 22.1–34.6 Bq/L at OBS-5 and 7.1–28.3 Bq/L at OBS-6. The 222Rn concentration of OBS-1 and 5 were decrease about 35 % but OBS-6 was increased.
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