Abstract:In order to determine the recharge source of a radon geothermal well in Pingyin county of Jinan city, environmental isotope method has been used. First, by using 14C dating, it is determined that the radon spring is mainly composed of ancient water. Then, by using isotope analysis result, the elevation has been calculated, it is determined that the elevation of recharge source of radon geothermal well is +140m. The recharge area is the same as determined by hydrogeological conditions (the elevation of Taishan stretching Mountain is 100~180m). It is indicated that the recharge area of the radon geothermal wells is Taishan stretching Mountains southeast 40 ~ 50km away from there.