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1)  soil moisture potential
水土势
1.
Three soil profiles were selected from the Ejin Oasis in the lower reaches of the Heihe River in northwest China to collect soil samples at different depths and groundwater samples for determination of chemical compositions of the samples, and to measure the changes in soil moisture potentials at different depths of the profiles.
在西北地区黑河流域下游的额济纳绿洲选择 3个土壤剖面采集不同深度土壤样品和潜水样品进行测试 ,并在野外观测非饱和带不同深度的水土势变化。
2)  soil-water potential
土水势
1.
The method introduced soil-water potential (SWP) equation and moving mesh FEM into the governing equations of traditional Biot s consolidation theory.
该方法在传统Blot固结控制方程组中引入土水势方程(SWP)和移动网格算法,根据虚功原理和加权残值法推导了相应的增量有限元方程。
2.
This paper analyzes two conditions required by vacuum preloading improving the soft soils,and explains the seepage mechanism during the course of improvement with the soil-water potential principle,the conversion from pore-water pressure to effective stress is illustrated,which demonstrates the incremental effective stress is consisted of difference of atmospheric and hydraulic pressure.
通过对真空预压法加固软基所具备的两个条件进行分析,以土水势的原理解释了加固过程中的渗流机制,并阐述了孔隙水压力向有效应力的转化过程,说明有效应力的增量是由气压差和静水压力差构成的,最后对卸除真空荷载后地基回弹作了分析。
3)  total soil-water potential
总土水势
4)  soil water potential
土水势
1.
The conception of soil water potential was used for the analysis and explanation of driving force and form of water migr.
运用土水势分析了冻融过程中水分迁移的动力和传输形式,研究表明:无压力四周给水冻融条件会导致土水势中出现压力势分势,由于压力势的存在,水分率先在试件的外围部分集中饱和,从而形成表层剥蚀;无压力单向给水冻融则消除了压力势的影响,水分得以高度分散而不能局部集中,当整个试件的含水率达到临界值时,试件发生整体的粉碎性破坏。
2.
To serve for engineering, ground water level in vacuum preloading is defined on the basis of conception of soil water potential.
在土水势概念的基础上,以工程应用为目的,定义了地下水位。
3.
The results showed that the saline-alkaline soil water potential Absolute value will be increased with the content of soil liquid decrease;the same kind soil of water potential Absolute value will be increased with the mcrease of concentration of soil liquid.
用压力排水法对氯化钠、氯化钙和碳酸氢钠盐渍土的持水特性进行了测定,结果表明,无论是氯盐土还是碳酸盐土其土水势绝对值都随含液量的减少而增大,同类盐渍土在含液量相同的情况下,土水势绝对值是随土壤溶液摩尔浓度增大而增大,并有很好的线性关系。
5)  soil water potential
土壤水势
1.
Effect of different nitrogen nutrition and soil water potential on physiological parameters and yield of hybrid rice;
不同土壤水势与氮素营养对杂交水稻生理特性和产量的影响
2.
Effects of soil water potential on radish growth under drip irrigation in North China Plain;
华北平原滴灌条件下土壤水势对萝卜生长的影响
3.
Measurement of soil water potential with thermocouple psychrometers;
用热电偶湿度计测定土壤水势的方法研究
6)  Low soil water potential
低土水势
补充资料:村村势势
1.犹言土头土脑。
说明:补充资料仅用于学习参考,请勿用于其它任何用途。
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