ISSN 1000-3665 CN 11-2202/P

    珊瑚砂的压缩特性及影响因素

    Compression characteristics and influencing factors of coral sands

    • 摘要: 珊瑚砂形状不规则、易破碎的性质使其压缩性质十分特殊,给珊瑚砂地区建(构)筑物的沉降控制带来了较大困难。通过开展不同粒径、级配特征、含水率、初始孔隙比等条件下的珊瑚砂侧限压缩试验,分析不同条件下珊瑚砂的压缩特征,厘清珊瑚砂压缩特征的影响因素。试验结果表明:(1)粒径(D)较大的珊瑚砂(D=2~5 mm)尖角断裂或颗粒破碎等现象使其级配得到优化;粒径较小的珊瑚砂(D<2 mm)的颗粒破碎现象主要以研磨,对级配的优化作用有限。(2)中值粒径D50较大的珊瑚砂,竖向压力P≤50 kPa时其压缩变形也较小, P>400 kPa时其压缩变形更大;不均匀系数大的珊瑚砂压缩性更高。(3)竖向压力P≤50 kPa时含水率对珊瑚砂的压缩特性的影响不明显;P>50 kPa时含水率为10%的珊瑚砂压缩变形最大。(4)加载梯度ΔP≤200 kPa时,含水率为10%的珊瑚砂压缩变形量最大;加载梯度ΔP>200 kPa时,ΔP越大,产生最大压缩变形量的珊瑚砂含水率越高。(5)初始孔隙比越大的珊瑚砂压缩性越高,各梯度下的压缩变形量随ΔP呈非线性增长。珊瑚砂侧限压缩过程可根据孔隙比变化率分为压密阶段(P≤100 kPa)和颗粒破碎(P>100 kPa)两个阶段。研究结果为珊瑚砂地区岛礁填筑工程的设计施工和建(构)筑物沉降控制与安全运营有重要指导意义。

       

      Abstract: The irregular morphology and fragile nature of coral sands result in distinctive compression behavior, posing significant challenges for settlement control of engineering structures in coral sands area. Confining compression tests of coral sands with different particle sizes, gradation characteristics, water content, and initial pore ratio were carried out to analyze its compression characteristics in different conditions and to clarify the influencing factors of its compression characteristics. The results show that the distribution of coral sands with large particle size (D=2−5 mm) can be optimized by the sharp-angle fracture or particle breakage. The particle breakage of small particle size coral sands (D<2 mm) is mainly caused by grinding, which has limited effect on the optimization of gradation. The coral sands with larger median particle size D50 have smaller compression deformation in lower vertical pressure P (P≤50 kPa), and larger compression deformation in higher P (P>400 kPa). The compressibility of coral sands with larger inhomogeneity coefficient is also greater. Water content has little influence on compressibility under low vertical pressure (P≤50 kPa); however, under higher pressure P (P>50 kPa), the compression deformation of coral sands with 10% water content w was the largest. When the loading gradient ΔP does not exceed 200 kPa, the coral sands with 10% water content have the largest compressive deformation; when ΔP exceeds 200 kPa, the larger ΔP, the largest compressive deformation, and the higher the water content of the coral sands. The larger the initial porosity ratio, the higher the compressibility of coral sands, and the compressive deformation under each gradient increased nonlinearly with ΔP. The lateral limit compression process of coral sands can be categorized into two stages with the rate of change of pore ratio: compaction stage (P≤100 kPa) and particle crushing (P>100 kPa). The results are important to guide significance for the design and construction of filling projects and the settlement control and safe operation of structures in the coral sands area.

       

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