The ice and snow melt of different seasons in high mountains can obviously affect the variation in isotope composition and deuterium excess parameters of surface flow and shallow groundwater.
不同季节高原高山冰雪的溶融，可以明显地影响地表径流和浅层地下水的同位素组成及氘过量参数的变化。
The ice and snow melt of different seasons in high mountains can obviously affect the variation in isotope composition and deuterium excess parameters of surface flow and shallow groundwater.
不同季节高原高山冰雪的溶融，可以明显地影响地表径流和浅层地下水的同位素组成及氘过量参数的变化。
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