摘要

Hailuogou (HLG) River and Huangbengliu (HBL) Gulley are typical alpine glacial and nonglacial rivers in Mount Gongga China, respectively. To differentiate distinct hydrologic regimes of the two rivers, delta O-18 and delta H-2 were measured on 196 water samples collected almost monthly from May 2008 to December 2009. The results indicate that: (i) the measured isotopic data show that stream water is overall isotopically more enriched in H-2 and O-18 than ice-snow meltwater but more depleted than precipitation and ground water; (ii) these data also suggest that stream flow is generally more dominated by ice-snow meltwater in HLG River than in HBL Gulley; (iii) delta H-2/delta O-18 relationship suggests that isotopic composition of precipitation is well preserved in stream flow, and evaporation is only minor in both HBL Gulley and HLG River; (iv) this study highlights that ice-snow meltwater is a substantially important water source in alpine regions on south-eastern edge of Tibetan Plateau.

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