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入渗水的英文

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"入渗水"怎么读用"入渗水"造句

英文翻译手机手机版

  • infiltrating water

例句与用法

  • Grey water enters a soakaway via a grease trap
    废水通过油脂分离器后汇入渗水坑。
  • The results indicated that the higher the salinity of infiltration water was , the faster cumulative infiltration and wetting front increased , and more salt accumulated at the wetting front
    入渗水的矿化度越高,土壤剖面含盐量越高,且湿润锋附近积聚的盐分越多。
  • Though the desalinized depth was different under different cumulative infiltration , the ratio of desalinized depth and wetting front distance was about 0 . 342 and the ratio of desalinized depth and cumulative infiltration was 0 . 862
    尽管不同湿润深度对应脱盐深度不同,但脱盐深度与湿润深度的比值却近似为0 . 342 。且脱盐深度与入渗水量的比值也近似为0 . 862 。
  • The function of desert microbiotic crusts in erdos was analyzed , the results ahowed that : microbiotic crusts consist of fine sand and thick powder sand , but differs with the wind - drift sand , wind - drift sand are coarse sand and fine sand ; microbiotic crusts influence the rainfall distribution again and effect on the evaporation of infiltration moisture ; microbiotic crusts has the power of water conservation and the function of enrichment of nutrients
    摘要本文对鄂尔多斯沙漠生物结皮作用进行了初步研究,结果表明结皮层的机械组成以细沙和粗粉沙为主,而流沙以粗沙和细沙为主;生物结皮层影响降水的再分配作用,并影响入渗水的蒸发规律;生物结皮层县有较好的保水特性和养分富集作用。
  • The middle and lower parts of woodland and grassland had higher soil water contents during rainy season , which resulted from smaller evapotranspiration and more infiltrated water with a lower gradient . however , upslope runoff infiltration was another reason for hillslope with a lower cover ratio , such as bare land
    雨季林草地坡中下部土壤水分含量较高的原因,可能主要与其蒸散较小且坡度较缓导致入渗水量较多有关;但是对于植被覆盖度较低的坡地(如裸地) ,坡中下部土壤水分含量较高还与上方来水有较大的关系。
  • The results were as follows : 1 . on the basis of saline water infiltration , the characteristics of movement of soil water and salt under different cumulative infiltration were studied . the results indicated that when the salinity of the infiltration water was 3g / l , the top soil was desalinized and salt accumulated at the wetting front
    通过对不同入渗水量下土壤水盐运移规律的室内模拟试验研究,结果表明利用矿化度为3g l水入渗后,土壤从上至下逐渐脱盐,上层土壤含盐量略低于土壤初始含盐量,中间土层基本保持土壤初始含盐量值,但湿润锋附近发生突变,含盐量达最大值。
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