1)  unsaturation
非饱和性
2)  unsaturated characteristics
非饱和性状
1.
By changing the boundary conditions,the unsaturated characteristics of sand and loam soils with finite and infinite depth of water-bearing bed under different unstable rainfall intensities are numerically modeled respectively,and the corresponding variations of unsaturated characteristics are obtained.
采用Gardner提出的对于土壤土-水特征曲线的指数分布假设建立数学模型,通过改变边界条件,对含水层厚度为有限和无穷深的砂土和壤土,在不同非恒定降雨强度条件下土壤非饱和性状分别进行数值模拟,得出了相应的非饱和性状变化情况。
3)  unsaturated
非饱和
1.
Rocky Slope Stability Analysis Taking into Account Saturated-unsaturated Seepage Flow;
饱和—非饱和非稳定渗流作用下岩质边坡稳定性分析
2.
Research on capillary pressure-saturation curve for a single fracture in an unsaturated fractured mass;
岩体单裂隙非饱和渗流毛管压力-饱和度关系研究
3.
Analysis on saturated-unsaturated steady seepage;
饱和-非饱和稳定渗流分析
4)  unsaturated zone
非饱和带
1.
It mainly includes the transportation and transformation on contaminant in soil, unsaturated zone, underground water and clay impermeable layer, and numerical models stimulated the contaminant transportation.
系统地评述了近年来国内外对污染物在土壤、非饱和带、地下水和粘土防渗层中迁移转化规律研究的最新进展,以及模拟污染物迁移的数值模型,并提出了需要进一步解决的关键性问题,为环境污染的治理、控制污染和水资源管理与评价的研究提供了可靠依据。
2.
The utilization of soil water in the unsaturated zone is of significance for agriculture,forestry,stock raising and the local eco-system.
如何保持和利用非饱和带中的土壤水对农、林、牧生态系统具有重要意义。
5)  unsaturated soil
非饱和土
1.
Migration behavior of heavy metal and LNAPLs in unsaturated soils;
重金属离子和LNAPLs在非饱和土中的运移规律研究
2.
Centrifuge modeling of copper ionic migration in unsaturated soils;
铜离子在非饱和土中迁移的离心模型试验研究
3.
Experimental study of BTEX transport in an unsaturated soil and groundwater system;
BTEX在非饱和土和地下水系统中迁移的试验研究
6)  Unsaturated Water
非饱和水
参考词条
补充资料:连续性与非连续性(见间断性与不间断性)


连续性与非连续性(见间断性与不间断性)
continuity and discontinuity

11an父ux泊g四f“山。麻以角g、.连续性与非连续性(c。nt,n琳t:nuity一)_见间断性与不间断性。and diseo红ti-
说明:补充资料仅用于学习参考,请勿用于其它任何用途。