下蜀土
- 网络xiashu loess
下蜀土-
下蜀土较强的化学风化过程可能受长江下游地区较强的季风性气候控制。
Strong chemical weathering underwent by the Xiashu loess might be related to strong monsoon climate in the lower reaches of the Changjiang River .
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应用该方法对初始含水率分别为20%，40%与60%的下蜀土试样在一个冻融循环内的瞬态温度场进行了实时监测；
Three Xiashu soil specimens with their respective water content of20 % , 40 % and60 % were monitored under a cycle of freezing and thawing , when the method was employed in real time .
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根据实际工程资料及试验成果，研究了仪征市下蜀组粘性土的物理-水理、物理力学性质及变化规律。
Ananalysis on The Shear Strength of Xiashu Loess between the Three-axial Test and The Direct Shear Test in Zhenjiang ;