基质势的英文

• matric potential

• "基质"英文翻译    base material; bulk material ...
• "势"英文翻译    power; force; influence
• "衬质势，基质势" 英文翻译 :    matric potential
• "衬质势" 英文翻译 :    matric potential
• "溶质势" 英文翻译 :    solute potential; solute pressure
• "基质" 英文翻译 :    [植物学] base material; bulk material; stroma; substrate; substratum; ground mass; host; matrix
• "z基质" 英文翻译 :    z-material
• "胞基质" 英文翻译 :    cystomyxo-adenoma ground substance
• "底物；基质" 英文翻译 :    substrate
• "靛基质" 英文翻译 :    indole; indol
• "多基质" 英文翻译 :    dopatic
• "骨基质" 英文翻译 :    bone matrix; bony matrix; ground substance of bone; matrix of bone
• "核基质" 英文翻译 :    karyobasis; nuclear matrix
• "基质,受质" 英文翻译 :    substrate
• "基质，底物" 英文翻译 :    su trate; substrate
• "基质层" 英文翻译 :    substantia propria layer
• "基质丛" 英文翻译 :    plexus fundamental; stroma plexus
• "基质的" 英文翻译 :    matrical; stromal; stromatic
• "基质膜" 英文翻译 :    basal plasma membrane
• "基质桥" 英文翻译 :    matrix bridge
• "肌基质" 英文翻译 :    muscle stroma; myostroma
• "假基质" 英文翻译 :    pseudomatrix
• "间质, 基质" 英文翻译 :    interstitial substance
• "矩阵；基质" 英文翻译 :    matrix
• "壳基质" 英文翻译 :    conchiolin

• Infiltration mostly depended on matric potential gradient and the effect of upslope runoff could be omitted , when initial water content was very low
  当初始含水量较低时，入渗主要受控于基质势梯度的作用，上方来水对入渗几乎没有影响。
• The results indicate that soil water moves from the warm end to the cool end in both gaseous and aqueous phases under temperature gradient , which causes changes of matric po
  研究表明，在温度势梯度影响下土壤水分以液态和汽态两种状态从暖端向冷端迁移，从而引起暖端基质势的相应改变，导致水分在两种势梯度交互作用下逐渐达到平衡。
• ( 3 ) when evaporation was stopped during the process of soil water redistribution , soil water would move downslope by gravity . when evaporation was in process , due to low initial water content , most infiltrated water from small intensity and amount of rainfall would be consumed by intensive evapotranspiration during rainy season , and lateral downslope unsaturated flow seldom took place . however , soil water would move downslope by gravitational and matric potential gradients after continuous rainfall
  ( 3 )在防止蒸发条件下，再分布过程中，土壤水分在重力的作用下有沿坡向下运移的趋势；在蒸发条件下，由于初始含水量一般较低，雨季量小且分散的降雨极易为强烈的蒸发蒸腾所消耗，侧向沿坡向下流难以发生，但在持续的降雨条件下，土壤水分在重力势和基质势梯度的作用下易沿坡向下运移。

• 基质势的泰文
• 基质势的法语：potentiel hydrique du sol pression de succion
• 基质势的阿拉伯语：كمون ماء التربة;