叶面积指数和表层土壤含水量是控制蒸发的两个基本因素。
Leaf area index and surface soil moisture are two basic factors of controlling evaporation.
并分析了返青后土壤蒸发随叶面积指数变化的规律。
Besides, the variation of evaporation from soil as related to leaf area index has also been calculated and analyzed.
分析认为，当叶面积指数较大时，棵间蒸发的现有研究结果尚存在较大的差别，而且高频灌溉条件下的土面蒸发有待于进一步研究。
In conclusion, there were some differences in the results of soil surface evaporation, when the leaf area index was large. A further study was needed under high-frequency irrigation.
并分析了返青后土壤蒸发随叶面积指数变化的规律。
Besides, the variation of evaporation from soil as related to leaf area index...
并分析了返青后土壤蒸发随叶面积指数变化的规律。
Besides, the variation of evaporation from soil as related to leaf area index...
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