摘要
采用热湿耦合非等温流方程,结合实际蒸发和植物蒸腾的边界条件,考虑了水分迁移所引发的非饱和土应力变形行为,从而建立了大气-非饱和土相互作用模型。采用该模型对控制非饱和土吸力和变形的大气蒸发和植物蒸腾等多参数进行了影响程度分析。结果表明,控制地面吸力和变形的主导因素是外部气象条件,尤其太阳净辐射量和风速,土体水力和热力特性参数影响程度有限;在植被覆盖条件下,吸力变化主要取决于植物叶面积指数LAI,而总腾发量的大小决定了地表变形量。
Based on the equations of coupled heat-moisture anisothermal flow and the behaviors of stress-strain of unsaturated soil,an interaction model of atmosphere-unsaturated soil is established with the boundaries of actual evaporation and vegetation transpiration.The influence of climatic evaporation and vegetation transpiration on the suction and deformation of soil surface are analyzed by the interaction model.It is shown that the major governing factor for the suction and deformation of soil surface is outer climatic condition where solar net radiation and wind velocity are the most contribution,while the internal hydraulic and thermal parameters of soil property play a less role in the estimation of evaporation.With the cover of vegetation,the behavior of suction depends on the leaf area index(LAI),while the magnitude of total evaporation and transpiration determines the deformation of soil surface.
出处
《岩土力学》
EI
CAS
CSCD
北大核心
2007年第9期1767-1772,1778,共7页
Rock and Soil Mechanics
基金
国家重大基础研究前期研究专项(No.2003CCA02200)
交通部西部交通建设科技项目(200631878530)
中国科学院武汉岩土力学研究所领域前沿基金项目(No.Q110301)
关键词
非饱和土
大气蒸发
植物蒸腾
吸力
变形
影响因素
unsaturated soil
climatic evaporation
vegetation transpiration
suction
deformation
influence factor