Data for kinetic isotopic fractionation of water during bare soil evaporation
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The kinetic fractionation factor (αK) controls to a large extent the isotopic enrichment of surface waters during evaporation (E). In contrast to the well-known vapor-to-liquid...
动力学分馏系数(kinetic fractionation factor,α_K)在很大程度上控制着蒸发过程(E)中地表水的同位素富集。与广为人知的汽-液相变过程形成鲜明对比,




