水分运动的英文

• water movement

• "水分"英文翻译    moisture content; dew; humid ...
• "运动"英文翻译    arrange things or get things ...
• "土壤水分运动" 英文翻译 :    soil water movement; soilwatermovement
• "水分运动到土壤内" 英文翻译 :    movement of water into soil
• "分运动" 英文翻译 :    componental movement
• "部分运动" 英文翻译 :    componental movement; componentalmovement
• "微分运动学" 英文翻译 :    differential kinematics
• "直接组分运动" 英文翻译 :    direct componental movement
• "分运" 英文翻译 :    feeder ship; partite transport
• "水分上升运动" 英文翻译 :    upward movement of water
• "分运单" 英文翻译 :    hawb; house air way bill; house air waybill
• "分运点" 英文翻译 :    extended delivery points
• "分运费" 英文翻译 :    knock-down shipment; knocked-down shipment
• "水分" 英文翻译 :    1.(物体内所含的水) moisture [water] content; dew; humidity 吸收水分 absorb moisture2.(夸大的成分) exaggeration 这个报导有些水分, 需要核实。 this report seems somewhat exaggerated, and should be verified.; 水分保持力 moisture holding capacity; 水分代谢 water metabolism; 水分含量 moisture; humidity; 水分亏缺 water deficit; 水分平衡 water balance; 水分失调 water stress; 水分损失 [机械工程] moisture loss; 水分通道 passage of water; 水分循环 hydrologic cycle; damp; 水分应力 moisture stress; 水分张力 water [moisture] tension; 水分直减率 hydrolapse; 水分滞留过多 hyperhydropexis
• "不允许分运" 英文翻译 :    partial shipments are ot) permitted
• "部分运输" 英文翻译 :    partial transport
• "部分运算" 英文翻译 :    partial arithmetic
• "部分运转" 英文翻译 :    part-time service
• "拆卸分运" 英文翻译 :    knocked down shipment
• "分运业务" 英文翻译 :    feederservice
• "分运与转运" 英文翻译 :    partial shipments and tra hipment; partial shipments and transhipment; partial shipments are permitted
• "航空分运单" 英文翻译 :    hawb: house airway bill; hawb house air waybill; house air waybill (hawb); house air waybill （hawb）
• "积分运算" 英文翻译 :    integral operation; integration
• "节分运输机" 英文翻译 :    separator conveyer
• "禁止分运" 英文翻译 :    partial shipment prohibited

• Experimental study on water movement of latosol under drip irrigation
  滴灌条件下砖红壤水分运动试验研究
• According to the basic equation for water flow in subgrade soil , based on the basic soil properties of compacted loess , the redistribution of soil moisture and the soil water - migrate parameters are studied
  摘要基于黄土路基压实后土体的基本性质，根据路基土中水分运动的基本方程，通过室内一维土柱入渗试验，得到不同压实度的黄土湿润锋湿度与平均湿度、水分入渗速率的关系曲线。
• The change of big pore section shape has more influence on soil water movement , but in small pore channels , the influence is small , in addition of pore section shape , it can get better prediction of unsaturated hydraulic conductivity
  粗大孔隙通道的截面形状及变化对水分运动影响较大，较细空隙通道截面的形状对水分运动影响较小。修正孔隙截面形状对水分运动的影响，进一步考虑孔隙截面形状因子对土壤水分运动的影响，可以得到对土壤水分运动参数更正确地预测。
• On the basis of the theory about water potential in soils , a partial differential equation of water movement in unsaturated soils is derived , which chose volumetric water content as the control variable . the numerical solution of the equation using finite difference method is discussed in this paper , and the modality to calculate water movement in slope considering rain infiltration
  基于非饱和土的土水势理论，本文推导了以体积含水率为因变量的二维非饱和土的水分运动方程，并给出了用有限差分法来求解此偏微分方程的方法，得到了考虑降雨入渗影响的土坡水分运动的计算程式。
• There is a period of soil contents range from ten to twenty five days over the humid discussed area in summer , and the period is not obvious at the discussed zone of close oasis desert area in summer and winter . ( 2 ) soil temperature exits several periodic variations of different depths ranging from six to twenty four days in heihe region , and nine to thirty days in gaize and shiquanhe region . it also shows that gradient of soil temperature affects on the soil content movement more greatly in summer . ( 3 ) the land surface temperature of yangtze river lower region is retrieved from noaa - ahvrr data
  ( 2 )根据土壤温湿资料，采用功率谱分析、 pca分析等方法，分析了两种典型下垫面土壤温度的时空分布特征及其对土壤水分运动的影响，发现研究区土壤温度除日和年变化周期外还存在6 30天的不同周期；下垫面的非均匀性及其季节变化及温度梯度变化对土壤水分运动有很大影响，冬季温度梯度变化对土壤含水量影响大于夏季温度梯度对上壤含水量变化的影响，且温度梯度与水分运动方向相反。
• The approach for dealing with the upper surface boundary conditions to adapt the complicated situation such as infiltration of precipitation or irrigation , surface ponding , runoff formation , evaporation and evaportanspiration as well as the alternative occurrence of these situations are proposed
  提出了适应降雨灌溉、蒸发等复杂的上边界条件的处理方法，可以用来统一计算土壤剖面降雨灌溉入渗、地表积水、地表产流、蒸发、蒸腾以及当这些现象交替出现时的水分运动过程。
• Subsurface runoff is obviously closely related with soil water movement in the unsaturated soil zone and dynamic change of the groundwater table . there - fore , it is necessary to develop the subsurface runoff model with a physical base associated with recharge on the aquifer and total storage in the reservoir . also a soil model with a dynamic representation of the groundwater table makes it possible and reasonable to represent a more logical subsurface runoff parame - terization
  地下径流显然与非饱和土壤层中的水分运动以及地下水位的动态变化密切相关,因而有必要发展考虑土壤含水量与潜水面science in china ser . d earth sciences 376中国科学d辑地球科学第36卷水分通量以及地下水位动态变化的土壤水模型相适应且具有物理意义的地下径流模型;同时地下水位动态表示的土壤水模型也为发展更为合理的地下径流模型创造了很好的条件