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wetting front中文是什么意思

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用"wetting front"造句"wetting front"怎么读"wetting front" in a sentence

中文翻译手机手机版

  • 浸湿锋面
  • 湿润锋
  • 湿润线

例句与用法

  • The influence of soil bulk density on wetting front is related to discharge rate
    土壤容重对滴灌湿润体特征值有较明显的影响。
  • Based on the approximate estimation of wetted front edge of one dimension soil column , the design parameters of sdi were determined primarily
    粘壤土湿润锋运移速度明显慢于沙土,特别是容重较大时更为明显。
  • 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。
  • The wetting front moved nearly parallel to the soil surface , and its length could be described by a power function of time , when the distribution of initial soil water was uniform
    当初始含水量分布均匀时,降雨入渗过程中湿润锋面几乎平行坡面运移,湿润锋深度与时间的关系可用幂函数描述。
  • And compared to the vertical wetting front , the rate of horizontal wetting front was 1 . 22 times higher . different models were used to fit the movement of wetting front , it is found that the polynomial function was a good model
    粘质(土娄)土,由于质地细小,在滴灌速率为2 . 67l h时,湿润锋径向移动速率远大于垂向移动速率,前者是后者的1 . 22倍。
  • 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 results showed that the lower initial soil moisture content was , the less infiltration occurred and wetting front moved slowly , and soil salt were leached more efficiently . at the same time , salt reduced in the top soil and salt accumulated at the wetting front
    通过对土壤初始含水量下土壤水盐运移规律室内模拟试验研究,发现随着土壤初始含水量的增加,相同入渗历时内的累积入渗量和湿润锋都在增加。
  • The infiltration rate in wetting front interface is speeder than that under single trickle source . the wetted soil volume shape becomes a strip which parallel lateral . the soil water content distribution under trickle source wetting front overlapping is more than that of single source
    在滴头流量为5 . 3l h条件下,在相同的入渗时间内大容重土壤的水平入渗距离较低容重的土壤大27 ,而其竖直入渗距离则较小容重土壤小14 。
  • In case of big discharge rate , the influence in horizontal is notable . however , in case of small discharge rate , the influence in vertical wetting front is notable , ( 3 ) in case of trickle source wetting front overlapping , the infiltration pattern is different from that of single trickle source infiltration
    在滴头流量为2l h条件下,在相同的入渗时间内,大容重土壤的地表水平入渗距离较小容重土壤大7 ,而其垂向入渗距离则较小容重土壤小20 。
  • Under subsurface drip irrigation , soil wetted front movement when higher soil initial moisture content was quicker than that of when it is lower , so did the supplied water pressure and soil bulk density . the wetted front movement of clay loam was clearly slow than that of sandy soil , especially in the larger soil bulk density
    地下滴灌条件下,初始含水量较高的土柱,湿润锋运移速度快于含水量较低的;在较高的供水压力条件下,各个方向的湿润锋运移都比低水头情况下的快;容重越大的土柱湿润锋运移速度越缓慢。
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