水迁移的英文

• water migration

• "水"英文翻译    water
• "迁移"英文翻译    move; remove; migrate; shift ...
• "毛管水迁移" 英文翻译 :    capillary migration
• "水迁移的强度" 英文翻译 :    inte ity of water migration; intensity of water migration
• "元素的水迁移系数" 英文翻译 :    water migration coefficient of element
• "迁移" 英文翻译 :    move; remove; migrate; shift; transport; migration; transference; removal
• "电迁移" 英文翻译 :    electromigration
• "反迁移" 英文翻译 :    back migration
• "负迁移" 英文翻译 :    negative transfer
• "极迁移" 英文翻译 :    pole migration
• "键迁移" 英文翻译 :    bond migration
• "净迁移" 英文翻译 :    net migration
• "鸟迁移" 英文翻译 :    bird migration
• "迁移,除去" 英文翻译 :    remove
• "迁移，迁飞" 英文翻译 :    emigration
• "迁移，移居" 英文翻译 :    migrate
• "迁移；调迁" 英文翻译 :    decantation
• "迁移；运输" 英文翻译 :    transport
• "迁移波" 英文翻译 :    migrating wave
• "迁移层" 英文翻译 :    migrating layer
• "迁移的" 英文翻译 :    immigrant; immigratory; migratory
• "迁移度" 英文翻译 :    migration mobility
• "迁移法" 英文翻译 :    transfer method; transportation method
• "迁移费" 英文翻译 :    costs of removal
• "迁移管" 英文翻译 :    migration tube

• Usually there is two forms of water transfer which is water vapor transfer and liquid water transfer in unsaturated soil
  非饱和土中水分迁移通常有液态水和气态水迁移两种形式。
• 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。
• The amount ratio of water vapor transfer contrasting with admixture transfer is related to the value of water content , the water content gradients and the soil category
  气态水迁移量占混合迁移量比例数值与土性、含水量水平和含水量梯度有关。
• 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。
• When the experiment time prolongs , the amount of water vapor transfer increases a little , but the amount of admixture transfer increases obv iously , so the increase amount of admixture transfer mostly come from liquid water transfer
  当实验时间增长时，气态水迁移量略有增长，而混合迁移量增长较为明显，这时迁移量的增加主要来源于液态水的迁移。
• Using masson pine ( pinus massoniaha ) as specimen , experiments based on the research of water diffusion coefficient and floating coefficient have been carried out to reveal the fundamental principle of absorbed water movement in wood drying under vacuum - floating pressure
  摘要该文以马尾松为试验材料，通过对水分扩散系数和浮压系数的试验研究，总结出木材在真空浮压干燥过程中吸着水迁移的基本规律。
• Then this paper devises experiments to research on the laws of water vapor transfer in unsaturated soil , studies the amount of water vapor transfer under different water contents , different water content gradients , different densities , different transfer time and the difference between loess and sands , studies the ratio of water vapor transfer contrasting with admixture transfer , and which can make us judge the importance of water vapor transfer in unsaturated soils by intuition
  进而论文设计试验研究了非饱和土中气态水迁移的规律，考查了不同含水量梯度、不同含水量水平、不同密实度、不同迁移时间以及非饱和砂土和黄土这两种不同土性条件下气态水迁移量的大小，以及在上述不同条件下气态水迁移量约占总混合迁移量的比例，使我们可以定性地判断出非饱和土中气态水迁移的重要性。
• With the equation for water vapor transfer in unsaturated soil the thesis deduces the equation for liquid water transfer , and then puts forward the coupled calculation method for water vapor and liquid water transfer together , and then build the difference calculation program to realize the coupled calculation under the one - dimension and constant - temperature condition , and put the program into practice with the experiment conditions , the calculation result tallies well with the experiment data , the facts proves the reliabilities of theory deduction and the feasibility of coupled calculation method
  最后论文结合非饱和土气态水迁移引起的含水量变化方程，推导了液态水迁移引起的含水量变化方程，提出了非饱和土考虑气态水和液态水混合迁移的计算方法，编制差分计算程序实现了一维恒温条件下液态水和气态水的祸合计算，并将程序结合试验条件进行了应用，计算结果与试验结果较为吻合，表明了理论推导的可靠性和祸合计算思路的可行性。
• The experiments reveals that : the amount of water vapor transfer is affected by both water content gradient and the value of water contents , when the water content of one end is approximate , the water content gradient increases , then the amount of water vapor transfer increases ; when the water content gradients are approximate , the amounts of water vapor transfer can get great differences if the water contents are different , under this condition when the water content of the dry soil is very little , the amount of water vapor transfer is much greater ; the differences of density hav n ' t great effects on water vapor transfer , but have some effects on the admixture transfer , when the density is smaller , the amount of admixture transfer is greater . the water vapor transfer finishes more quickly and need less time , and the liquid water finishes more slowly and need less time
  当一端含水量一定时，增加含水量梯度，则气态水迁移量增大；当含水量梯度相近时，气态水迁移量随含水量不同可能相差很大，这种情况下当较干段含水量特别小时，气态水迁移量相对较大；密实度的大小对于气态水迁移的影响并不明显，但对液态水和气态水的混合迁移有一定的影响，在相同的实验时间内，土体密实度较小，则混合迁移量相对较大；气态水迁移完成速度较快，所需时间较短；液态水迁移完成速度较慢，所需时间较长。