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Soil-water characteristics of unsaturated undisturbed loess under isotropic compression condition

机译:各向同性压缩条件下非饱和原状黄土的水土特征

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Using triaxial apparatus for unsaturated soils, the isotropic compression tests at constant water content are conducted on unsaturated undisturbed loess in Xi'an under different water contents. The maximum of net confining pressure is 400 kPa. Matric suction is measured by an elevated all round air pressure and with measured pore-water pressure under zero-applied stress and applied stress. Influences of net confining pressure on matric suction characteristics of unsaturated undisturbed loess are determined and illustrated during isotropic compression at constant water content. The formula of soil-water characteristics of unsaturated undisturbed loess is obtained to determine the matric suction under zero-applied stress. Experimental results show that the influence of net confining pressure on matrix suction is related to water content. When water content is smaller than shrinkage limit, the relationship between matrix suction and net confining pressures is different from that larger than Shrinkage limit. The influence of net confining pressure is large when water content is between shrinkage limit and plastic limit, and it is slight when water content is smaller than shrinkage limit or larger than plastic limit. The relation between matric suction and degree of saturated related to net confining pressure with water content smaller than shrinkage limit is different from that related to water content. The influence of degree of saturated related to net confining pressure on matric suction is much smaller than that related to water content. Net confining pressure has relatively large influence on the relation between degree of saturated and matric suction. When net confining pressure is smaller than 400kPa, its influence on he relation between water content and matric suction is negligible, and the soil-water characteristics of undisturbed loess is illustrated by the logarithm function relation between water content and matric suction under zero-applied stress.
机译:采用三轴仪对不饱和土壤进行了水含量恒定的各向同性压缩试验。净围压的最大值为400 kPa。基质吸力是通过升高的全方位气压以及在零施加应力和施加应力下测得的孔隙水压力来测量的。在恒定含水量的各向同性压缩过程中,确定并说明了净围压对不饱和原状黄土基质吸力特性的影响。推导了非饱和黄土的土-水特征公式,确定了零施加应力下的基质吸力。实验结果表明,净围压对基质吸力的影响与含水量有关。当水含量小于收缩极限时,基体吸力与净围压之间的关系与大于收缩极限的关系不同。当含水量在收缩极限和塑性极限之间时,净围压的影响很大,而当含水量小于收缩极限或大于塑性极限时,净围压的影响很小。含水量小于收缩极限的基质吸力与饱和度之间的关系与净围压有关,与含水量有关。与净围压有关的饱和度对基质吸力的影响远小于与含水量有关的影响。净围压对饱和吸力与基质吸力之间的关系影响较大。当净围压小于400kPa时,其对含水量与基质吸力的关系的影响可忽略不计,而零扰动条件下含水量与基质吸力的对数函数关系说明了原状黄土的土壤水特征。 。

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