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陈晓平. 海陆交互相沉积软土固结效应[J]. 岩土工程学报, 2011, 33(4): 520.
引用本文: 陈晓平. 海陆交互相沉积软土固结效应[J]. 岩土工程学报, 2011, 33(4): 520.
CHEN Xiao-ping. Consolidation effect of soft soil in interactive marine and terrestrial deposit[J]. Chinese Journal of Geotechnical Engineering, 2011, 33(4): 520.
Citation: CHEN Xiao-ping. Consolidation effect of soft soil in interactive marine and terrestrial deposit[J]. Chinese Journal of Geotechnical Engineering, 2011, 33(4): 520.

海陆交互相沉积软土固结效应

Consolidation effect of soft soil in interactive marine and terrestrial deposit

  • 摘要: 海陆交互相沉积软土是珠江三角洲内广泛分布的不良地基土,土类主要为含粉细砂的淤泥和淤泥质黏土,基本力学特性较一般海相软土有所不同。基于广州南沙万顷沙组(Q4W)灰黑色淤泥质土的一系列室内试验成果,系统分析和研究了土体固结作用对基本力学特性的影响,包括渗透特性、剪切强度特性、次固结特性、直接剪切蠕变特性、三轴压缩蠕变特性、回弹特性等,提出了考虑固结效应的量化分析方法。为适应工程需要,这些分析方法所涉及的参数大多可通过简单/常规的试验方法确定。

     

    Abstract: The soft soil of interactive marine and terrestrial deposit, which is a kind of poor subsoil widely spreading over the Pearl River Delta, mainly consists of silt and mucky clay with silty/fine sand and has basic mechanical properties different from those of the marine soft soil. Based on a series of laboratory test results of the grayer silt-like soft soil from Q4W of Nansha, Guangzhou, the effect of consolidation on the mechanical properties, including permeability, shear strength, second consolidation, direct shear creep, triaxial compression creep, and rebound deformation, is systemically analyzed and studied, based on which the quantitative models are proposed. To facilitate engineering applications, the parameters of such models can be determined by simple and conventional experimental approaches.

     

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