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土壤斥水性是指水分不能或很难湿润土壤颗粒表面的物理现象。土壤斥水性是一个全球性现象,可以出现在各种气候背景、土壤类型和植被覆盖条件下,并且影响到地表水文过程的诸多重要环节,因此受到广泛关注。有关土壤斥水性的研究是表面科学、生物学、土壤学以及物理学等学科交叉的前沿研究领域,已成为国际生态水文学研究的重要核心科学问题。复杂多变的时空分布特征,是目前量化其生态水文效应的困难所在。在综述国内外研究动态的基础上,简要回顾了该领域的发展历史;对土壤斥水性的发生机理、影响因子及其对水文过程的影响机理,进行了较为全面的总结和讨论,并指出了目前存在的问题和未来的研究重点,以期促进我国相关研究,为生产实践及科学决策提供借鉴依据。
Soil water repellency refers to the physical phenomenon that water can not or hardly moisten the surface of soil particles. Soil water repellency is a global phenomenon that can occur in a variety of climate background, soil types and vegetation cover conditions, and affect many important aspects of surface hydrological processes, it has received widespread attention. Research on soil water repellency is a frontier research field of interdisciplinary studies in surface science, biology, soil science and physics, and has become an important core scientific issue in international ecohydrology research. Complex and changeable spatio-temporal distribution characteristics are the difficulties in quantifying its eco-hydrological effects. On the basis of a review of the research progress both at home and abroad, the development history of this area is briefly reviewed. The mechanism of occurrence, influence factors and mechanism of water repellency are summarized and discussed in detail. Existing problems and future research priorities, with a view to promoting relevant research in China, providing reference for production practice and scientific decision-making.