饱和导水率的英文

• saturated hydraulic conductivity

• "饱和"英文翻译    saturation; saturated
• "导"英文翻译    lead; guide
• "水"英文翻译    water
• "率"英文翻译    rate; ratio; proportion
• "非饱和导水率" 英文翻译 :    unsaturated hydraulic conductivity
• "导水率" 英文翻译 :    specific water conductivity
• "比导水率" 英文翻译 :    specific conductivity
• "土壤导水率" 英文翻译 :    soil hydraulic conductivity
• "饱和含水率" 英文翻译 :    percentage of saturated water content
• "导水" 英文翻译 :    water diversion
• "升水率, 贴水率" 英文翻译 :    contango rate
• "滞水率，保水率" 英文翻译 :    specific retention
• "导水板" 英文翻译 :    fair water piece; weatherboard
• "导水槽" 英文翻译 :    water chute
• "导水堤" 英文翻译 :    training bank; training levee; trainingdike
• "导水沟" 英文翻译 :    conducting channel; guiding gutter; headrace cha el; headrace channel; pilot trench; pilottrench
• "导水管" 英文翻译 :    aquaeductus; aqueduct
• "导水门" 英文翻译 :    wicket gate
• "导水器" 英文翻译 :    water deflector
• "导水墙" 英文翻译 :    diversion wall; diverting wall; guide wall
• "导水渠" 英文翻译 :    headrace
• "导水性" 英文翻译 :    water transmissibility
• "电导水" 英文翻译 :    conductance water; conductivity water; conductivity watrer; conductivtiy water
• "前导水" 英文翻译 :    lead water
• "饱和" 英文翻译 :    (在一定温度压力下, 溶液可含溶质的量达到最大限度, 不能再溶解, 泛指事物达到最高限度) saturation; saturated 气体饱和 gas saturation; 旧汽车市场已经饱和。 the market for the used car is saturated.; 饱和参量 saturation parameter; 饱和值 saturation value

• The increasing of water transmetting rate in cultivated loessial soil was larger than that in lou soil
  在相同的土壤含水量条件下，增加温度可提高土壤非饱和导水率，其导水率温度效应值?土> ,黄绵土。
• The relationship of soil particle - size distributions and soil water retention characteristics , saturated and unsaturated hydraulic conductivity were studied in the lab
  本研究对陕西四种不同质地土壤的粒径分布与水分特征曲线及饱和、非饱和导水率的关系进行了研究。
• Water transmitting rate of unsaturated soil also increased with the increasing of relative partial molal free energy variation , , and relative partial molal enthalpy variation , , in case that soil water content was constant
  结果表明，在同一温度条件下，提高土壤水势可增加土壤非饱和导水率，呈现黄绵土> ,土。
• 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
  将新的土壤结构分形维数应用于对土壤水分运动参数的描述，使饱和导水率和非饱和导水率预测的准确性有了很大程度地提高。
• ( 3 ) sensitivity analyses were conducted for parameters in unsaturated soil conductivity model which was derived from redistribution process . the results calculated from measured data indicate that the sensitivities of conductivity to parameter b and n are higher than the other parameters
  ( 3 )对由再分布过程推求的土壤非饱和导水率模型中的参数进行了敏感性分析，根据实测资料的计算表明，非饱和导水率对参数b和n的敏感性均大于其它参数。
• The data needed by the research are collected from relevant materials and field sampling , including the soil saturation hydraulic conductivity , soil bulk density , various kinds of chemical parameters of soil layer ( such as organic nitrogen , organic phosphorus and soluble phosphorus ) , the transformation of organic carbon content of soil layer and the land use in 1993 etc .
  笔者两次参加对研究区的实地考察，并进行相关数据的收集和实测，包括1993年土地利用、土壤饱和导水率、土壤容重和土壤各种化学参数(如有机氮、有机磷和可溶性磷等) ，以及后来所进行的土壤层有机碳含量的转化等。