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English translation for "气态水"

vaporous water
vapour water


Related Translations:
气态:  [物理学] gas state; gaseity; gaseousness; gaseous state
气态溶液:  gas mixture
气态流体:  gaseous fluid
气态氢:  gaseous hydrogen
气态元素:  elementary gas
气态汽油:  compression gasolinegas spirit
气态氮:  gaseous nitrogen
气态夹杂:  air inclusioninclusion of air
气态发散:  gaseous emission
气态平衡:  mass balances
Example Sentences:
1.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。
2.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。
3.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。
4.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。
5.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。
Similar Words:
"气态燃烧" English translation, "气态燃烧产物部分" English translation, "气态溶液" English translation, "气态散放物" English translation, "气态石蜡" English translation, "气态碳" English translation, "气态碳氢化合物" English translation, "气态碳氢化合物;气态烃类" English translation, "气态烃" English translation, "气态烃类" English translation