期刊文献+

蒸发蒸腾作用下非饱和土的吸力和变形影响因素分析 被引量:20

On influence factors of suction and deformation of unsaturated soil under evaporation and transpiration effect
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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
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参考文献16

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二级参考文献13

  • 1弗雷德隆德,等.非饱和土土力学[M].北京:中国建筑工业出版社,1997.
  • 2柯尊敬,黄绍铿.膨胀土工程性质的研究总报告[R].南宁:广西大学土木系,1995.
  • 3Thomas H R,Rees S W.The numerical simulation of seasonal soil drying in an unsaturated clay soil[J].International Journal for Numerical & Analytical Methods Geomechanics,1993,17(1):119-132.
  • 4Thomas H R,Rees S W.Seasonal ground movement in unsaturated clay:an examination of field behaviour[J].Geotechnique,1994,44:353-358.
  • 5Thomas H R,Zhou Z.A comparison of field measured and numerically simulated seasonal ground movement in unsaturated clay[J].International Journal for Numerical and Analytical Methods in Geomechanics,1995,19(4):249-265.
  • 6Gray D M.Handbook on the principles of hydrology[M].Ottawa:Canadian National Committee for the Intemational Hydrological Decade,National Research Council of Canada,1970.
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