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ISSN 2096-7780 CN 10-1665/P

蒋其峰, 许洪泰, 付海清. 山东地区粉质黏土剪切波速与埋深关系研究[J]. 国际地震动态 , 2018, (6): 15-21. DOI: 10.3969/j.issn.0253-4975.2018.06.003
引用本文: 蒋其峰, 许洪泰, 付海清. 山东地区粉质黏土剪切波速与埋深关系研究[J]. 国际地震动态 , 2018, (6): 15-21. DOI: 10.3969/j.issn.0253-4975.2018.06.003
Qifeng Jiang, Hongtai Xu, Haiqing Fu. Study on the relationship between shear wave velocity and depthof silty clay in Shandong Province[J]. Progress in Earthquake Sciences, 2018, (6): 15-21. DOI: 10.3969/j.issn.0253-4975.2018.06.003
Citation: Qifeng Jiang, Hongtai Xu, Haiqing Fu. Study on the relationship between shear wave velocity and depthof silty clay in Shandong Province[J]. Progress in Earthquake Sciences, 2018, (6): 15-21. DOI: 10.3969/j.issn.0253-4975.2018.06.003

山东地区粉质黏土剪切波速与埋深关系研究

Study on the relationship between shear wave velocity and depthof silty clay in Shandong Province

  • 摘要: 粉质黏土在山东地区分布广泛,对粉质黏土剪切波速—埋深关系的研究可用于指导实践。根据山东境内的工程地质特征,本文将山东划分为鲁西地区、鲁中南地区和鲁东地区3个统计单元,分别对粉质黏土的剪切波速—埋深数据进行统计,使用4种回归模型对粉质黏土剪切波速—埋深数据进行回归分析,对比各回归模型的拟合效果。研究表明,粉质黏土剪切波速与埋深之间有明显的相关性,基于幂函数的回归模型( v_\rm si = ah_i^b + c )具有最佳的拟合效果,在Ⅱ类场地和Ⅲ类场地条件下都能很好的拟合剪切波速随埋深的变化,并且具有良好的拟合优度。基于该模型,本文得到了鲁西地区、鲁中南地区和鲁东地区粉质黏土剪切波速—埋深关系经验公式并给出了相应的误差,供实际工作中缺乏剪切波速时参考。

     

    Abstract: Silty clay is widely distributed in Shandong Province, and the study of the relationship between shear wave velocity and depth of silty clay is helpful to guide practice. According to the characteristics of engineering geology in Shandong, this paper divides Shandong into three statistical units as Western Shandong, Central-Southern Shandong and Eastern Shandong. The shear wave velocity and depth data of silty clay of each unit are counted. Regression analysis is performed on silty clay’s shear wave velocity and depth data using 4 kinds of regression model, and the fitting effect of each model is compared. The research shows that shear wave velocity of silty clay is obviously related to the depth in Shandong Province and the regression model based on power function( v_\rm si = ah_i^b + c )has the best fitting effect. It can well fit the variation of shear wave velocity with depth of type Ⅱ site or type Ⅲ site, and has good goodness of fit. Based on this model, this paper obtains shear wave velocity-depth empirical formulas and root mean square errors of silty clay in Western Shandong, Central-Southern Shandong and Eastern Shandong. The empirical formulas can be used in practice when lack of shear wave velocity.

     

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