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initial soil中文是什么意思

  • 原始土壤

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  • 例句與用法
  • The influence of initial soil conditions on water penetration and soil moisture distribution
    荒漠地區(qū)土壤初始狀況對水平入滲的影響
  • 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
    當(dāng)初始含水量分布均勻時(shí),降雨入滲過程中濕潤鋒面幾乎平行坡面運(yùn)移,濕潤鋒深度與時(shí)間的關(guān)系可用冪函數(shù)描述。
  • By the experiments , some main factors influenced watering effect were analyzed . the results show that watering volume , initial soil water content , and width of water ditch influenced the watering effect differently
    對影響灌水效果的幾個(gè)主要因素進(jìn)行了分析,實(shí)驗(yàn)表明,灌水量、土壤初始含水率、灌水溝寬度對灌水效果都有不同程度的影響。
  • The results indicated that even if there was different at initial soil condition , such as initial moisture content and initial salt content , salt content in soil profile and sar at top soil increased greatly after the high salinity water infiltrated
    結(jié)果表明盡管土壤初始條件存在差異,但灌高礦化度水后,土壤含鹽量和溶液濃度總體增加,且土壤剖面特別是表層的sar明顯增大。
  • 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
    通過對土壤初始含水量下土壤水鹽運(yùn)移規(guī)律室內(nèi)模擬試驗(yàn)研究,發(fā)現(xiàn)隨著土壤初始含水量的增加,相同入滲歷時(shí)內(nèi)的累積入滲量和濕潤鋒都在增加。
  • When the saline water ( < 3g / l ) infiltrated to 45cm , the top soil of 0 - 37cm was desalinized , when the saline water of 3g / l infiltrated , the desalinized depth was 0 - 15cm . moreover , sar of top soil increased with the sar of the infiltration water . 3 . through lab experiment , the characteristics of soil water and salt movement under different initial soil moisture content were analyzed
    當(dāng)濕潤深度為45cm時(shí),小于3g l的微咸水入滲后, 0 - 37cm土層處于脫鹽狀態(tài),而3g l的微咸水入滲, 0 - 15cm土層處于脫鹽狀態(tài), 15cm - 35cm土層含鹽量基本等于初始含鹽量,但濕潤鋒處含鹽量很高。
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