齐俊修, 赵晓菊, 刘艳, 张中炎, 张广禹. 2017: 连续级配砂粗细颗粒区分粒径比较研究. 工程地质学报, 25(s1): 140-146. DOI: 10.13544/j.cnki.jeg.2017.s1.023
    引用本文: 齐俊修, 赵晓菊, 刘艳, 张中炎, 张广禹. 2017: 连续级配砂粗细颗粒区分粒径比较研究. 工程地质学报, 25(s1): 140-146. DOI: 10.13544/j.cnki.jeg.2017.s1.023
    QI Junxiu, ZHAO Xiaoju, LIU Yan, ZHANG Zhongyan, ZHANG Guangyu. 2017: COMPARATIVE STUDY ON DISTINGUISHING GRAIN SIZE OF COARSE AND FINE PARTICLES FOR CONTINUOUSLY GRADED SAND. JOURNAL OF ENGINEERING GEOLOGY, 25(s1): 140-146. DOI: 10.13544/j.cnki.jeg.2017.s1.023
    Citation: QI Junxiu, ZHAO Xiaoju, LIU Yan, ZHANG Zhongyan, ZHANG Guangyu. 2017: COMPARATIVE STUDY ON DISTINGUISHING GRAIN SIZE OF COARSE AND FINE PARTICLES FOR CONTINUOUSLY GRADED SAND. JOURNAL OF ENGINEERING GEOLOGY, 25(s1): 140-146. DOI: 10.13544/j.cnki.jeg.2017.s1.023

    连续级配砂粗细颗粒区分粒径比较研究

    COMPARATIVE STUDY ON DISTINGUISHING GRAIN SIZE OF COARSE AND FINE PARTICLES FOR CONTINUOUSLY GRADED SAND

    • 摘要: 粗细颗粒区分粒径是无黏性粗粒土判别渗透变形类型的重要指标,但其确定方法和量值均不统一,为验证不同方法的适宜性,我们统计分析了7个工程62个砂土试样的渗透变形试验结果,结果表明,以2mm作为粗细颗粒区分粒径时,其渗透变形类型判断结果与试验结果符合率达93.55%,远高于以d70d10为区分粒径时的符合率51.61%。推荐以2mm作为不均匀连续级配砂土粗细颗粒区分粒径。

       

      Abstract: The distinguishing grain size of coarse and fine particles is an important discriminant indicator for the seepage deformation type of cohesionless coarse grain soil. As the determination methods and the values are not unified, statistical analysis on seepage deformation testing results were taken with 62 sand samples from 7 projects to verify the suitability of different methods. The results show that the coincidence rate of the discrimination result and the testing result of seepage deformation is 93.55%when 2mm is used as the distinguishing grain size instead of d70d10, which is much higher than 51.61%. Thus, 2mm is recommended as the distinguishing grain size of coarse and fine particles for the non-uniform continuously graded sand.

       

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