石振明, 刘巍然, 彭铭, 李建中. 2018: 网纹红土土水特征曲线试验研究及其在边坡稳定性评价中的应用. 工程地质学报, 26(1): 164-171. DOI: 10.13544/j.cnki.jeg.2018.01.018
    引用本文: 石振明, 刘巍然, 彭铭, 李建中. 2018: 网纹红土土水特征曲线试验研究及其在边坡稳定性评价中的应用. 工程地质学报, 26(1): 164-171. DOI: 10.13544/j.cnki.jeg.2018.01.018
    SHI Zhenming, LIU Weiran, PENG Ming, LI Jianzhong. 2018: EXPERIMENTAL STUDY ON SOIL-WATER CHARACTERISTIC CURVE OF RETICULATE RED CLAY AND ITS APPLICATION IN SLOPE STABILITY EVALUATION. JOURNAL OF ENGINEERING GEOLOGY, 26(1): 164-171. DOI: 10.13544/j.cnki.jeg.2018.01.018
    Citation: SHI Zhenming, LIU Weiran, PENG Ming, LI Jianzhong. 2018: EXPERIMENTAL STUDY ON SOIL-WATER CHARACTERISTIC CURVE OF RETICULATE RED CLAY AND ITS APPLICATION IN SLOPE STABILITY EVALUATION. JOURNAL OF ENGINEERING GEOLOGY, 26(1): 164-171. DOI: 10.13544/j.cnki.jeg.2018.01.018

    网纹红土土水特征曲线试验研究及其在边坡稳定性评价中的应用

    EXPERIMENTAL STUDY ON SOIL-WATER CHARACTERISTIC CURVE OF RETICULATE RED CLAY AND ITS APPLICATION IN SLOPE STABILITY EVALUATION

    • 摘要: 网纹红土在中国南方地区有着广泛的分布,常见于各类岩土工程中。目前对网纹红土的研究主要集中在成因和粒度特性等方面,对于其非饱和特性方面的研究相对有限。本文采用滤纸法测量不同饱和度条件下网纹红土的基质吸力,利用Van Genuchten模型得到网纹红土的干燥-浸湿过程的土水特征曲线。研究发现,由于网纹红土孔隙较小且均匀,使得网纹红土存在进气值(约为100 kPa)相对于一般黏土较大、其土水特征曲线没有明显的残余段。利用干燥-浸湿过程的土水特征曲线对一维无限边坡的干燥和浸湿过程稳定性进行研究,发现在饱和度相同的情况下,边坡处于脱湿过程的稳定性要高于吸湿过程。随着深度的增加,脱湿与吸湿过程稳定性系数相差值减小;随着饱和度的提高,两者差值也出现减小的趋势。同时,网纹红土中基质吸力对抗滑力的贡献度较大,使得网纹红土质边坡较为稳定。

       

      Abstract: Reticulate red clay is widely distributed in southern China area and common in many kinds of geotechnical engineering. At present, the research of the reticulate red clay mainly focused on the causes and granularity characteristics. The study on its unsaturated characteristics is relatively limited. In this paper, the filter paper method is applied to measure the matrix suction of reticulate red clay in different saturation conditions. Van Genuchten model is used to get the soil-water characteristic curve in drying-wetting process. It is found that due to the small and relatively uniform void, the air entry value of reticulate red clay(about 100 kPa) is relatively larger than that of normal clays. There is no obvious residual stage in its soil-water characteristic curve. The soil water characteristic curve is applied to analyze the stability of one dimensional infinite slope in drying and wetting process. The results indicate that in the same saturation, the slope is more stable in the drying process than in the wetting process. With the increase of depth and saturation, the difference of stability factor in the two processes tends to decrease. Due to the larger contribution of matrix suction, reticulate red clay slope is relatively stable.

       

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