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作 者:XuYang Liu WenXiao Ning ZhenTing Wang
机构地区:[1]Key Laboratory of Desert and Desertification,Northwest Institute of Eco-Environment and Resources,Chinese Academy of Sciences,Lanzhou,Gansu 730000,China [2]University of Chinese Academy of Sciences,Beijing 100049,China
出 处:《Research in Cold and Arid Regions》2020年第4期234-241,共8页寒旱区科学(英文版)
基 金:supported by Natural Science Foundation of China projects(Nos.41971011 and 41630747).
摘 要:Saltation bombardment is a dominate dust emission mechanism in wind erosion.For loose surfaces,splash entrainment has been well understood theoretically.However,the mass loss predictions of cohesive soils are generally empirical in most wind erosion models.In this study,the soil particle detachment of a bare,smooth,dry,and uncrusted soil surface caused by saltation bombardment is modeled by means of classical mechanics.It is shown that detachment rate can be analytically expressed in terms of the kinetic energy or mass flux of saltating grains and several common mechanical parameters of soils,including Poisson's ratio,Young's modulus,cohesion and friction angle.The novel expressions can describe dust emission rate from cohesive surfaces and are helpful to quantify the anti-erodibility of soil.It is proposed that the mechanical properties of soils should be appropriately included in physically-based wind erosion models.
关 键 词:wind erosion saltation bombardment cohesive soil anti-erodibility
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