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刘鑫, 李飒, 尹福顺, 姚婷. 基于动态图像技术的南海钙质土颗粒形态特征研究[J]. 岩土工程学报, 2023, 45(3): 590-598. DOI: 10.11779/CJGE20220010
引用本文: 刘鑫, 李飒, 尹福顺, 姚婷. 基于动态图像技术的南海钙质土颗粒形态特征研究[J]. 岩土工程学报, 2023, 45(3): 590-598. DOI: 10.11779/CJGE20220010
LIU Xin, LI Sa, YIN Fushun, YAO Ting. Morphological characteristics of carbonate soil in South China Sea based on dynamic image technology[J]. Chinese Journal of Geotechnical Engineering, 2023, 45(3): 590-598. DOI: 10.11779/CJGE20220010
Citation: LIU Xin, LI Sa, YIN Fushun, YAO Ting. Morphological characteristics of carbonate soil in South China Sea based on dynamic image technology[J]. Chinese Journal of Geotechnical Engineering, 2023, 45(3): 590-598. DOI: 10.11779/CJGE20220010

基于动态图像技术的南海钙质土颗粒形态特征研究

Morphological characteristics of carbonate soil in South China Sea based on dynamic image technology

  • 摘要: 颗粒形态是一项重要的细观指标,影响着粒状土的物理力学性质。钙质土因为其特殊的生物成因,有着复杂的颗粒形态。为了研究其颗粒形态特征,采用PartAn 3D颗粒动态图像分析仪对粒径0.5~20 mm的南海钙质土颗粒开展形状测试,采用延伸率、扁平度、球形度、圆度、棱角度和凸度指标定量描述颗粒形态特征。结果显示:南海钙质土颗粒的延伸率、扁平度、球形度和圆度符合正态分布,而棱角度和凸度符合幂律分布;颗粒形状以块状居多,随着粒径的减小,钙质土颗粒变得更扁平,形状更规则;通过研究样本数量对颗粒形状量化结果的影响,建议采用形状指标的算术平均值量化单一粒组钙质土颗粒形状特征时,颗粒数目不少于600。最后,运用统计学中的主成分分析方法,得到一个综合考虑钙质土颗粒形状信息的新指标,建立了该指标与钙质土最大、最小孔隙比的关系。

     

    Abstract: The particle morphology is an important microscopic characteristic that affects the physical and mechanical properties of granular soils. Carbonate soil particles have complex morphology due to special biogenesis. In order to study the morphological characteristics of the soil particles, the PartAn 3D particle dynamic image analyzer was used to test the particle shape of the carbonate soil with grain sizes of 0.5 ~ 20 mm from the South China Sea. The elongation, flatness, sphericity, roundness, angularity and convexity were used to quantitatively describe the morphological characteristics of the particles. The results show that the frequency distribution of the elongation, flatness, sphericity and roundness of carbonate soil particles in the South China Sea complies with the normal one, while the frequency distribution of the angularity and convexity complies with that of the power law. The particle shape of the carbonate soil is mostly blocky, and with the decrease of grain size, the soil particles become flatter and more regular in shape. Through investigating the effects of sample size on the results of particle shape quantification, it is suggested that the number of particles should be not less than 600 when using the arithmetic mean of shape descriptors to quantify the morphological characteristics of the uniformly graded carbonate soil. Finally, a comprehensive shape index which can fully describe the morphological characteristics of the carbonate soil particles is obtained with the aid of the principal component analysis method in statistics, and the relationship between this shape index and the maximum to minimum void ratio of the carbonate soil is established.

     

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