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Analysis of the exchange of groundwater and river water by using Radon-222 in the middle Heihe Basin of northwestern China

Analysis of the exchange of groundwater and river water by using Radon-222 in the middle Heihe Basin of northwestern China

Environmental Geology 45(5): 647-653

DOI: 10.1007/s00254-003-0914-y

In arid regions of western China, water resources come from mountain watersheds and disappear in the desert plain. The exchange of surface water and groundwater takes place two or three times in a basin. It is essential to analyze the interaction of groundwater with surface water to use water resources effectively and predict the change in the water environment. The conventional method of analysis, however, measures only the flow of a stream and cannot determine groundwater seepage accurately.

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