1)基质势/间质势、基模势(matric potential): 土壤固体颗粒作为吸水基质,水分被土壤基质吸 附,自由活动能降低,即基质吸力使水势降低; 随含水量增加而增大,土壤水饱和时...
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The method is an implicit iterative scheme with a hyperbolic sine transform for the matric potential.
这个方法使用了水土势双曲正弦变换的隐式差分格式。
The influence caused irrigation (rainfall) is to each layer soil matric potential reduces with depth of increment.
灌水(降雨)对各层土壤基质势的影响随深度的增加而减小。
Soil matric potential, leaf water potential and atmosphere water potential is diversity in temporal and spatial variation.
通过相关性分析得出土壤基质势,叶水势,大气水势三者在时间和空间上都有很大的差别。
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