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本文用增湿变形的概念对黄土的湿陷起始压力和起始含水量进行了论述,并根据实际试验资料得出了相应的关系曲线。湿陷起始压力和起始含水量都与黄土的初始(天然)含水量有关,湿陷起始含水量还与作用的压力有关。
In this paper, the concept of humidification deformation is used to describe the initial collapse and initial water content of loess, and the corresponding relationship curve is obtained based on the actual experimental data. Both the initial collapse pressure and the initial water content are related to the initial (natural) water content of the loess, and the initial water content of the collapse is also related to the applied pressure.