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滨海新区建筑场地的地震效应研究

王鹏 刘晓磊 张博夫 周世冲 王磊

王鹏, 刘晓磊, 张博夫, 周世冲, 王磊. 滨海新区建筑场地的地震效应研究[J]. 岩土工程技术, 2026, 40(4): 526-533. doi: 10.20265/j.cnki.issn.1007-2993.2025-0077
引用本文: 王鹏, 刘晓磊, 张博夫, 周世冲, 王磊. 滨海新区建筑场地的地震效应研究[J]. 岩土工程技术, 2026, 40(4): 526-533. doi: 10.20265/j.cnki.issn.1007-2993.2025-0077
WANG Peng, LIU Xiaolei, ZHANG Bofu, ZHOU Shichong, WANG Lei. Seismic effects of construction sites in Binhai New Area[J]. GEOTECHNICAL ENGINEERING TECHNIQUE, 2026, 40(4): 526-533. doi: 10.20265/j.cnki.issn.1007-2993.2025-0077
Citation: WANG Peng, LIU Xiaolei, ZHANG Bofu, ZHOU Shichong, WANG Lei. Seismic effects of construction sites in Binhai New Area[J]. GEOTECHNICAL ENGINEERING TECHNIQUE, 2026, 40(4): 526-533. doi: 10.20265/j.cnki.issn.1007-2993.2025-0077

滨海新区建筑场地的地震效应研究

doi: 10.20265/j.cnki.issn.1007-2993.2025-0077
基金项目: 天津市科技支撑计划项目(14ZCDZGX00828)
详细信息
    作者简介:

    王 鹏,男,1988年生,硕士,高级工程师,主要从事岩土设计方面工作。E-mail:878845244@qq.com

    通讯作者:

    刘晓磊,男,1986年生,硕士,高级工程师,从事岩土勘察设计工作。E-mail:xiaogoudagou@163.com

  • 中图分类号: P641

Seismic effects of construction sites in Binhai New Area

  • 摘要: 在对滨海新区区域地质背景进行分析的基础上,统计了滨海新区百余项工程的地基土等效剪切波速、场地覆盖层厚度,并对滨海新区的场地类别进行了划分,给出了滨海新区不同建筑场地的分布范围及地震动参数;对滨海新区3932个岩土工程勘察钻孔进行了液化判定,综合滨海新区地震调查实际喷水冒砂调查点位及非液化勘察钻孔分布情况,给出了滨海新区液化土层的分布范围及液化等级分区。研究结果表明:(1)滨海新区埋深20 m以内的地基土等效剪切波速一般介于140.0~170.0 m/s,均属软弱—中软土,场地覆盖层厚度多在90~100 m;(2)滨海新区大部分地区场地类别为Ⅳ类场地,仅北部滨海旅游区、西部空港经济区以及北大港水库以西地区为Ⅲ类场地;(3)滨海新区液化区域主要分布在汉沽、塘沽及大港部分地区,其中,中等液化区主要分布在大港、汉沽南部、军粮城及塘沽海河附近,严重液化区仅在中新生态城附近分布。

     

  • 图  1  滨海新区工程地质分区图

    Figure  1.  Engineering geological zonation map of Binhai New Area

    图  2  滨海新区等效剪切波速试验实际材料图

    Figure  2.  Actual material map of equivalent shear wave velocity test in Binhai New Area

    图  3  地基土等效剪切波速等值线及分区图

    Figure  3.  Contour and zonation map of equivalent shear wave velocity of foundation soil

    图  4  滨海新区场地覆盖层厚度试验实际材料图

    Figure  4.  Actual material map of site overburden thickness test in Binhai New Area

    图  5  滨海新区场地覆盖层厚度等值线图

    Figure  5.  Contour map of site overburden thickness in Binhai New Area

    图  6  滨海新区场地类别分区图

    Figure  6.  Site classification zonation map of Binhai New Area

    图  7  滨海新区地震动参数区划图

    Figure  7.  Seismic ground motion parameter zonation map of Binhai New Area

    图  8  滨海新区地震喷水冒砂点位图

    Figure  8.  Distribution map of sand-blowing points induced by earthquake in Binhai New Area

    图  9  滨海新区液化土层分布及液化等级分区图

    Figure  9.  Distribution of liquefied soil layers and liquefaction grade zonation map of Binhai New Area

    图  10  近10年滨海新区典型地下潜水观测井水位动态变化图

    Figure  10.  Dynamic variation of groundwater level in typical phreatic observation wells in Binhai New Area in the past 10 years

    表  1  滨海新区工程地质分区特征

    Table  1.   Characteristics of engineering geological zonation in Binhai New Area

    特征 工程地质Ⅰ区 工程地质Ⅱ区 工程地质Ⅲ区 工程地质Ⅳ区
    分布 分布界限 第Ⅱ贝壳堤以西 第Ⅱ贝壳堤以东;第Ⅰ贝壳堤以西 第Ⅰ贝壳堤以东 深切古河道区
    主要区域 茶淀镇—汉南路,军粮城—东丽湖,大港—津岐公路沿线以西 茶淀镇—汉南路,军粮城—东丽湖,大港—津岐公路沿线以东;老海防公路沿线以西 老海防公路沿线以东 北部黄港水库—天津港沿线;中部葛沽镇—临港沿线;南部南港工业区内
    工程地质特性评价 工程地质特性较好区,表层地基土沉积时间较长,陆相沉积层相对较厚,重要地基土厚度、埋深均较小,地基条件和施工条件相对较好 工程地质特性相对较好区,表层地基土沉积时间中等,陆相沉积厚度中等,重要地基土厚度、埋深中等,地基条件和施工条件一般 工程地质特性相对较差区,表层地基土沉积时间较短,陆相沉积厚度较薄,重要地基土厚度、埋深均较大,地基条件和施工条件相对较差 表层土工程地质特性与周边分区基本一致,但第Ⅰ海相层粉(砂)土厚度较大,工程性质较第Ⅱ、Ⅲ陆相层粉质黏土好,较第Ⅱ、Ⅲ陆相层粉(砂)土差
    下载: 导出CSV

    表  2  埋深20 m以内地基土等效剪切波速计算结果表

    Table  2.   Calculation results of equivalent shear wave velocity of foundation soil in 20 m buried depth

    场地土类别区间值/(m·s−1钻孔数所占比例/%
    软弱土103.2~149.638380
    中软土150.4~196.29520
    下载: 导出CSV

    表  3  滨海新区场地覆盖层厚度统计表

    Table  3.   Statistical table of site overburden thickness in Binhai New Area

    序号区间值/m钻孔数所占比例/%
    1<902428
    290~1005261
    3>100911
    下载: 导出CSV

    表  4  滨海新区场地特征周期调整表

    Table  4.   Adjustment table of site characteristic period in Binhai New Area

    Ⅱ类场地基本地震动加速度
    反应谱特征周期分区值
    场地类别
    0.40 0.55 0.75
    0.45 0.65 0.90
    下载: 导出CSV

    表  5  滨海新区场地地震动峰值加速度调整系数表

    Table  5.   Adjustment coefficient of peak ground acceleration for sites in Binhai New Area

    Ⅱ类场地基本地震动
    峰值加速度值
    场地类别
    0.15g 1.15 1.10
    0.20g 1.00 1.00
    下载: 导出CSV

    表  6  埋深20 m以上饱和粉土地震液化判别表

    Table  6.   Seismic liquefaction identification of saturated silt in 20 m buried depth

    液化
    判别
    液化
    等级
    液化指数 钻孔数 占比(液化点内
    部占比)/%
    液化点 轻微 0.1~5.8 162 4(53)
    中等 6.0~17.2 105 3(34)
    严重 18.1~43.2 39 1(13)
    非液
    化点
    3626 92
    下载: 导出CSV
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  • 收稿日期:  2025-02-25
  • 修回日期:  2025-04-14
  • 录用日期:  2025-06-26
  • 网络出版日期:  2026-08-07
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