气态水的英文

• vaporous water
• vapour water

• "气态"英文翻译    gaseous state
• "水"英文翻译    water
• "土壤气态水" 英文翻译 :    soil water in vapor phase
• "气态" 英文翻译 :    [物理学] gas state; gaseity; gaseousness; gaseous state
• "变态水" 英文翻译 :    distorted water
• "液态水" 英文翻译 :    aqueous water; liquid water
• "将气态" 英文翻译 :    uf coo
• "气态氨" 英文翻译 :    gaseous ammonia
• "气态氮" 英文翻译 :    gaseous nitrogen
• "气态的" 英文翻译 :    gaseous; gassy; vaporous
• "气态铃" 英文翻译 :    gaseous fluid
• "气态氯" 英文翻译 :    gaseous chlorine
• "气态镁" 英文翻译 :    gaseous magnesium
• "气态膜" 英文翻译 :    gaseous film
• "气态氢" 英文翻译 :    gaseous hydrogen
• "气态碳" 英文翻译 :    gaseouscarbon
• "气态烃" 英文翻译 :    gaseous hydrocarbon
• "气态氧" 英文翻译 :    gas oxygen; gaseous oxygen; gaseous-oxygen
• "不可给态水" 英文翻译 :    unavailable water
• "低焓液态水" 英文翻译 :    low-enthalpy liquid water
• "动态水位" 英文翻译 :    dynamic water-table
• "非稳态水流" 英文翻译 :    nonsteady state water flow
• "非液态水" 英文翻译 :    non-liquid water
• "静态水源" 英文翻译 :    static water su ly; static water supply
• "生态水文学" 英文翻译 :    eco-hydrology

• 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。
• 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。
• 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。