1) saturated soil paste
饱和土浆
2) saturated soil
饱和土壤
1.
For saturated soil,a membrane cell was designed to measure the effective diffusion coefficient.
在低渗透性的饱和土壤微生物修复过程中,扩散是物质运移的重要因素。
3) 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
4) unsaturated soils
非饱和土
1.
FEM strength reduction method based on consolidation theories of unsaturated soils;
基于非饱和土固结理论的有限元强度折减法
2.
Influence of matric suction on shear strength behavior of unsaturated soils;
基质吸力对非饱和土抗剪强度的影响
3.
Expressions of coefficients of lateral earth pressure for unsaturated soils considering change of volume mass;
考虑体积质量变化时非饱和土的土压力系数
5) saturated silt soil
饱和粉土
1.
The influence of dewatering on the slope stability of saturated silt soil slope;
降水对饱和粉土边坡稳定性影响研究
2.
In order to eliminate the unfavorable effect of excess water pore pressure induced during dynamic consolidation, a consolidating method with heavily rammed stone columns on saturated silt soil and silt clay is put forward.
为了解决强夯时产生的超孔隙水压力问题 ,提出了加固饱和粉土、粉质粘土地基的强夯碎石桩法。
6) air-saturated soil
气饱和土
1.
The characteristics of propagation and attenuation of compressible waves in water-saturated,pseudo water-saturated and air-saturated soils were discussed by using numerical methods.
气饱和土中,P1波速度比水饱和时显著降低且基本无弥散和衰减;P2波速度比水饱和时有很大提高,同时弥散和衰减加强,且特征频率向高频漂移。
2.
The velocity and attenuation of elastic waves in air-saturated soil were given and compared with the solutions in water-saturated soil by using numerical methods.
通过数值算例,分析了气饱和土中弹性波速度与衰减特性,并与水饱和土中的计算结果进行了比较。
补充资料：土壤盐基饱和度
分子式：
CAS号：
性质：交换性盐基离子与阳离子交换量(或交换性阳离子总量)的百分比。盐基饱和度=(交换性盐基离子总量/阳离子交换量)×100％。土壤胶体表面所吸附的阳离子大都属于盐基离子，如钙、镁、钠、铵等离子。若不含交换性酸，土壤全被盐基所饱和时称盐基饱和土壤。若土壤胶体表面除吸附盐基离子外，还吸附有氢离子和铝离子时，称盐基不饱和土壤。盐基饱和度对土壤的pH值、酸化、碱化均有直接影响，对养分离子的有效性影响尤甚。对某些离子危害也有直接关系。
CAS号：
性质：交换性盐基离子与阳离子交换量(或交换性阳离子总量)的百分比。盐基饱和度=(交换性盐基离子总量/阳离子交换量)×100％。土壤胶体表面所吸附的阳离子大都属于盐基离子，如钙、镁、钠、铵等离子。若不含交换性酸，土壤全被盐基所饱和时称盐基饱和土壤。若土壤胶体表面除吸附盐基离子外，还吸附有氢离子和铝离子时，称盐基不饱和土壤。盐基饱和度对土壤的pH值、酸化、碱化均有直接影响，对养分离子的有效性影响尤甚。对某些离子危害也有直接关系。
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