分運動英文

• componental movement

• "分" 英文翻譯 :    component
• "運動" 英文翻譯 :    arrange things or get things ...
• "部分運動" 英文翻譯 :    componental movement; componentalmovement
• "水分運動" 英文翻譯 :    water movement
• "微分運動學" 英文翻譯 :    differential kinematics
• "土壤水分運動" 英文翻譯 :    soil water movement; soilwatermovement
• "直接組分運動" 英文翻譯 :    direct componental movement
• "水分運動到土壤內" 英文翻譯 :    movement of water into soil
• "分運" 英文翻譯 :    feeder ship; partite transport
• "分運單" 英文翻譯 :    hawb; house air way bill; house air waybill
• "分運點" 英文翻譯 :    extended delivery points
• "分運費" 英文翻譯 :    knock-down shipment; knocked-down shipment
• "不允許分運" 英文翻譯 :    partial shipments are ot) permitted
• "部分運輸" 英文翻譯 :    partial transport
• "部分運算" 英文翻譯 :    partial arithmetic
• "部分運轉" 英文翻譯 :    part-time service
• "拆卸分運" 英文翻譯 :    knocked down shipment
• "分運業務" 英文翻譯 :    feederservice
• "分運與轉運" 英文翻譯 :    partial shipments and tra hipment; partial shipments and transhipment; partial shipments are permitted
• "航空分運單" 英文翻譯 :    hawb: house airway bill; hawb house air waybill; house air waybill (hawb); house air waybill （hawb）
• "積分運算" 英文翻譯 :    integral operation; integration
• "節分運輸機" 英文翻譯 :    separator conveyer
• "禁止分運" 英文翻譯 :    partial shipment prohibited
• "空運分運單" 英文翻譯 :    house air way bill m.a.w.b h.a.w.b
• "篩分運輸機" 英文翻譯 :    separator conveyer; separator conveyor

• Discussion on a new model of water flow in soils
  一種新形式土壤水分運動模型的討論
• Review of effect of temperature on soil water movement
  溫度對土壤水分運動影響的研究進展
• The percentage of preferential flow flux over the total infiltrated water can reach 2 . 40 % ~ 48 . 72 %
  優先流水分通量最大可達剖面滲流水分通量的17200倍，會在很大程度上增加土壤水分運動通量。
• 2 . by using the experimental device of soil moisture movement of single water storage pit and suction gauge , irrigation experiment of single water storage pit are conducted
  2 .利用蓄水單坑土壤水分運動試驗裝置結合負壓計進行蓄水單坑灌水試驗。
• They decrease soil bulk density , increase soil porosity and soil saturated water content . the result of straw mulch is best , plastic mulch is better . the movement of soil water in gneiss area of tai - hang mountain has following regulation
  其中以秸稈覆蓋的效果最好，其次為地膜覆蓋；太行山片麻巖區土壤水分運動有如下規律，土壤含水量隨土壤深度的增加而逐漸降低。
• 5 . to describe soil water movement with fractal model . the effect of soil pore radius and pore connectivity on soil water movement was studied . in addition of pore connectivity , the prediction of unsaturated hydraulic conductivity is more improved in low water content
  將新的土壤結構分形維數應用于對土壤水分運動參數的描述，使飽和導水率和非飽和導水率預測的準確性有了很大程度地提高。
• In this paper , numerical simulation and experimental research on the soil moisture movement of water storage pit irrigation are conducted . at the same time , the technical parameter of water storage pit irrigation are discussed preliminarily . the research method and content include : 1
  本論文對蓄水坑灌法的土壤水分運動進行了數值模擬和試驗研究，并對蓄水坑灌法的技術要素進行了初步的探討。研究的方法和內容主要有： 1
• A experiment on the water movement rule of the soil had been done before the field experiment , and then four irrigation regimes were placed in it , that is to say , three sub - irrigated areas hi contrast to a general irrigated area
  在大田試驗前，做了滲灌土壤水分運動規律試驗，然后，在大田試驗中設置了四個處理，即：三個水平滲灌區和一個漫灌區對照。結果表明： ( 1 )滲灌區的實際灌水量比漫灌區下降了58 . 15 81 . 63 。
• Based on rainfall and evaporation amount , the change of soil water could be divided into three main periods , such as decreasing of soil water storage in spring , alternatively decreasing and increasing in summer and autumn , and relatively stable in winter
  根陳洪松博士學位論文:黃土區坡地土壤水分運動與轉化試驗研究據年內降雨和水面蒸發量的相對大小，可將土壤水分的變化分為三個主要時期:春季失墑期、夏秋增失交替期和冬季相對穩定期。
• It showed that the simulated value are in accordance with the experimental value by contrast of them . it indicates that the numerical modeling can reflect the status of soil moisture movement under the condition of water storage pit irrigation , and its method of solution is feasible
  3 .將計算結果與實測結果進行對比，可以看出兩者有較好的一致性。說明所建立的數學模型能夠反映蓄水坑灌條件下的土壤水分運動狀況，其數值求解方法也是可行的。