1) critical soil water content
土壤临界含水量
1.
According to the fundamental concept of crop water stress coefficient and some related equations in FAO56,a new formula computing crop water stress coefficient was deduced considered the temporal change of critical soil water content.
从作物水分胁迫系数的基本概念和FAO 56的相关公式出发,考虑土壤临界含水量的时间变化,推导出了一个水分胁迫系数计算公式,该公式比较全面地表达了土壤供水能力、作物潜在腾发量与作物所受水分胁迫之间的关系。
2) the lowest critical value of soil water content
最低临界土壤含水量
3) soil salinity threshold
土壤临界含盐量
4) critical water content
临界含水量
1.
So,the formula for computing the critical water content of unsaturated loess strength isput forward in th.
依据库伦－摩尔强度准则，非饱和黄土的抗剪强度随外部压力和含水量的变化规律可用强度曲面描述，提出了非饱和黄土强度的临界含水量计算式。
5) critical moisture content
临界含水量
1.
Test and regression model on critical moisture content of carrot and drying rate during the stage of constant rate by vacuum microwave drying
真空微波干燥胡萝卜的恒速干燥速度及临界含水量的实验和回归模型
6) Soil moisture
土壤含水量
1.
Correlation between soil moisture and transport and transformation of nitrogen compounds;
土壤含水量与氮化合物迁移转化的相关性分析
2.
Dynamic growth model for root and shoot of winter wheat considering the influence of soil moisture;
改变土壤含水量影响的冬小麦根和冠生长动态模型
3.
Correlations between soil moisture and δ~(13)C value of plant leave under karst and non-karst backgrounds——A case study in Wangjiazhai basin,Qingzhen city,Guizhou province;
喀斯特与非喀斯特区土壤含水量与植物叶片δ~(13)C关系的对比研究——以贵州清镇市王家寨小流域为例
补充资料：土壤水分运动基本方程(见土壤水运动)
土壤水分运动基本方程(见土壤水运动)
turang shuifen yundong iiben土壤水分运动基本方程fangeheng见土壤水运动。
说明：补充资料仅用于学习参考，请勿用于其它任何用途。
参考词条