摘要
After flowing out of Yingluoxia Gorge, Heihe River experiences several conversions of leakage to underground and recharge back to the river. With the aim to study this conversion relation between surface and ground water, 222Rn is employed as the tracer to determine location where ground water discharge and recharge rate, analysis of electrical conductivity (EC) and section flow measurement are used. The measured data show that the surface water leak into the underground at the part from Yinluoxia Gorge to Heihe Bridge in Zhangye, where the leakage rate is 0.248~0.433m3/s·km; but the ground water seeps out to the river at the part from Heihe Bridge to Zhengyi Gorge, where the seepage rate is 0.042~1.057 m3/s·km. On the basis of calculation of inter-recharge rate, further the inter-recharge volume could be calculated accordingly in the various reaches and period.