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非饱和土

"非饱和土"的翻译和解释

例句与用法

  • Three boundary condition expressions of unsaturated soil slope under rainfall infiltration and evaporation conditions are presented
    摘要讨论了非饱和土边坡在入渗、蒸发条件下的三类边界条件表达形式。
  • Arranging the settlement - time test data of saturated soil and unsaturated soil , the paper acquire two kinds of fitting method
    对饱和和非饱和土样试验资料整理了变形与时间的关系曲线,得到了两种简单的拟合形式。
  • The variation of water distribution in unsaturated slope and the slope stability due to rain infiltration is studied in this paper
    本论文研究降雨入渗条件下非饱和土边坡内水分分布规律以及由此而引起的边坡稳定性的变化。
  • The ratio of water vapor transfer contrasting with admixture transfer reveals that usually water vapor transfer can not be neglected
    气态水迁移量占混合迁移量的比例数值表明,通常非饱和土水分迁移中气态水迁移是不可忽视的。
  • Based on the wave equation in unsaturated soil , the dynamic response of a pile under transient torsional loading was theoretically investigated
    摘要基于己建立的非饱和土中的波动方程,研究了瞬间扭转荷载作用下桩的动力响应问题。
  • The mechanical characteristics of unsaturated soils are usually expressed by using two kinds of variable ( single stress variable and double stress variable )
    摘要对非饱和土力学性质,通常采用两种变量表示形式,一种是单应力变量,另一种是双应力变量。
  • The thesis studies the theories of water vapor transfer in unsaturated soil , and gets the water contents equations of water vapor transfer in unsaturated soils
    本论文进行了非饱和土气态水迁移的理论研究,得到非饱和土中气态水迁移引起的含水量变化方程。
  • Since loess is a typical unsaturated soil , some of scholars have studyed some questiones of loess by the theorey and ways of modern unsaturated soil mechanics
    由于黄土是一种典型的非饱和土,所以近年来不少学者用现代非饱和土的理论和方法研究黄土的有关问题。
  • Problem on water infiltration in unsaturated soil are in the research field of water science research on problem is very important in many field
    非饱和土中水流入渗问题属于水科学研究领域。该问题的研究在农田水利、水土工程、水文地质、生态环境等领域都占有重要地位。
  • Variation of the soil suction of unsaturated soil slope under alternative action of infiltration and evaporation is studied taking a filled road slope and an excavated one as examples
    将公路填方和挖方路基边坡作为典型算例,研究了入渗、蒸发交替作用下非饱和土边坡内吸力的变化。
  • 更多例句:  1  2  3  4  5
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