长江科学院院报 ›› 2016, Vol. 33 ›› Issue (4): 91-94.DOI: 10.11988/ckyyb.20140888

• 岩土工程 • 上一篇    下一篇

武汉后湖地区土层剪切波速与深度的关系

林亚洲1,2,王秋良1,李井冈1,廖武林1,张丽芬1   

  1. 1.中国地震局地震研究所 地震大地测量重点实验室,武汉 430071;
    2.武汉地震工程研究院有限公司,武汉 430071
  • 收稿日期:2014-10-20 出版日期:2016-04-01 发布日期:2016-04-08
  • 作者简介:林亚洲(1990 - ),男,湖北武汉人,硕士研究生,主要研究方向为防灾减灾工程及防护工程,(电话)18674005913(电子信箱)lyzx112@163.com。
       通讯作者:王秋良(1972 - ),男,湖北黄冈人,副研究员,博士,主要从事地震地质和水库诱发地震等方面的研究,(电话)18507183023(电子信箱)wql0703@sohu.com。
  • 基金资助:
    中国地震局地震研究所所长基金项目(IS201216023)

Relation Between Shear Wave Velocity and Depth of Soilsin Houhu Area of Wuhan

LIN Ya-zhou1,2, WANG Qiu-liang1, LI Jing-gang1, LIAO Wu-lin1, ZHANG Li-fen1   

  1. 1.Key Laboratory of Earthquake Geodesy, Institute of Seismology of China Earthquake Administration,Wuhan 430071,China;
    2. Wuhan Institute of Earthquake Engineering Co., Ltd., Wuhan 430071,China
  • Received:2014-10-20 Online:2016-04-01 Published:2016-04-08

摘要: 基于对武汉后湖地区78个地震安全性评价钻孔地层资料及实测剪切波速数据的分析,根据岩土类型和物理状态将岩土体分为11个组别,并运用线性关系、二次多项式关系、幂函数关系等3种经验公式,分别对各土层的剪切波速(Vs)与深度(H)的关系进行回归分析。得到了武汉后湖地区各土层的回归关系式和相关系数,并分析了导致土层拟合优度差异的原因。结果表明,黏土层(可塑-硬塑)、粉砂质黏土层(稍密、中密-密实)、粉细砂层(稍密、中密-密实)等土层拟合优度较高,相关系数范围为0.71~0.95,可供该地区无波速测试的场地参考使用。

关键词: 剪切波速, 土层深度, 回归分析, 最小二乘法, 武汉后湖地区

Abstract: According to the analysis of soil layer and shear wave velocity data of 78 boreholes from seismic safety evaluation reports of Houhu area in Wuhan, we classify rock and soil into 11 groups in terms of rock and soil types and mechanical properties. Furthermore, we carry out regression analysis on the relationship between shear wave velocity and soil depth using 3 empirical formulas inclusive of linear fitting, polynomial fitting and exponential fitting. Finally, we obtain regression formulas and coefficients of different soil layers in Houhu area of Wuhan, and analyze the causes of the difference in fitting accuracy. The result shows that there is high correlation between shear wave velocity and depth of soils in clay layer (plastic and hard plastic), silty clay layer(slightly dense, medium dense, and dense), and fine silty sand layer(slightly dense, medium dense, and dense), with coefficients from 0.71 to 0.95. The empirical relationship of these soils in this paper can be used as a reference for sites in the absence of shear wave velocity test.

Key words: shear wave velocity, soil depth, regression analysis, least squares method, Houhu area of Wuhan

中图分类号: