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基于PSInSAR技术的山东半岛蓝黄交迭区地面沉降发育特征与影响因素识别

刘宏伟, 杜东, 许静波, 马震, 赵青松, 裴艳东, 胡云壮, 苗晋杰, 白耀楠, 张竞. 2018. 基于PSInSAR技术的山东半岛蓝黄交迭区地面沉降发育特征与影响因素识别[J]. 中国地质, 45(6): 1116-1127. doi: 10.12029/gc20180603
引用本文: 刘宏伟, 杜东, 许静波, 马震, 赵青松, 裴艳东, 胡云壮, 苗晋杰, 白耀楠, 张竞. 2018. 基于PSInSAR技术的山东半岛蓝黄交迭区地面沉降发育特征与影响因素识别[J]. 中国地质, 45(6): 1116-1127. doi: 10.12029/gc20180603
LIU Hongwei, DU Dong, XU Jingbo, MA Zhen, ZHAO Qingsong, PEI Yandong, HU Yunzhuang, MIAO Jinjie, BAI Yaonan, ZHANG Jing. 2018. Characteristics and affecting factors of land subsidence identification based on PSInSAR measures in Shandong Peninsula Blue-Yellow Overlapping Economic Zone[J]. Geology in China, 45(6): 1116-1127. doi: 10.12029/gc20180603
Citation: LIU Hongwei, DU Dong, XU Jingbo, MA Zhen, ZHAO Qingsong, PEI Yandong, HU Yunzhuang, MIAO Jinjie, BAI Yaonan, ZHANG Jing. 2018. Characteristics and affecting factors of land subsidence identification based on PSInSAR measures in Shandong Peninsula Blue-Yellow Overlapping Economic Zone[J]. Geology in China, 45(6): 1116-1127. doi: 10.12029/gc20180603

基于PSInSAR技术的山东半岛蓝黄交迭区地面沉降发育特征与影响因素识别

  • 基金项目:
    中国地质调查局项目(DD20160229,12120113003800)、国家自然科学基金项目(41602205)和中丹地质调查局国际合作项目(SUBSOL)联合资助
详细信息
    作者简介: 刘宏伟, 男, 1982年生, 高级工程师, 主要从事环境地质、海水入侵等研究工作; E-mail:liuhenry022@163.com
    通讯作者: 杜东, 男, 1981年生, 高级工程师, 主要从事水文地质、环境地质等研究工作; E-mail:yndd24@163.com
  • 中图分类号: P542.3

Characteristics and affecting factors of land subsidence identification based on PSInSAR measures in Shandong Peninsula Blue-Yellow Overlapping Economic Zone

  • Fund Project: Supported by China Geological Survey Program(No. DD20160229, No.12120113003800), National Natural Science Foundation of China(No.41602205)and International cooperation projects between CGS and GEUS(No.SUBSOL)
More Information
    Author Bio: LIU Hongwei, male, born in 1982, senior engineer, majors in research on environmental geology and seawater intrusion; E-mail:liuhenry022@163.com .
    Corresponding author: DU Dong, male, born in 1981, senior engineer, majors in research on environmental geology; Email:yndd24@163.com
  • 研究区位于山东半岛蓝色经济区和黄河三角洲高效生态经济区的交迭地带,区位优势明显。地面沉降灾害的发生对该区规划建设和港口防潮堤高程构成了威胁,因此,全面了解该区地面沉降的发育特征,尤其是掌握地面沉降的主要影响因素极其重要。前人在不同时段内应用GPS和水准测量方法对该区局部地段地面沉降开展了相应研究,但未对全区地面沉降状况进行分析评价,尚不能有效支撑区域规划建设及地面沉降防控管理。文章在前人研究基础上,基于PSInSAR遥感技术分析了该区地面沉降速率及其变化状况,并与水准测量成果进行了对比。认为多年来该区地面沉降现象明显,超过75%的区域发生了不同程度的地面沉降,在寿光-广饶交界处、寿光-滨海开发区北部、寿光城区西北部和昌邑-滨海开发区北部等存在多个显著片区,且多年变化总体呈现加重趋势;区内存在16个沉降中心,最大沉降速率达到29~168 mm/a,沉降速率超过40 mm/a的占比达到62%以上,主要分布于研究区西部和西北部;该区地面沉降受区域构造、地层结构、地下水开采和地面荷载等因素影响,其中地下水开采是区域地面沉降发生的主致因素,地面荷载加强了局部地段的不均匀沉降程度,区域构造和地层结构为地面沉降发育和加剧提供了地质背景条件。

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  • 图 1  研究区位置及地面沉降速率(2014)

    Figure 1. 

    图 2  南柴西北片区2012-2014年地面沉降速率

    Figure 2. 

    图 3  大家洼—杨庄—南河—广陵—岔河片区2012—2014年地面沉降速率

    Figure 3. 

    图 4  古城—北洛—寿光片区2012—2014年地面沉降速率

    Figure 4. 

    图 5  央子—泊子—固堤—龙池—青乡片区2012—2014年地面沉降速率

    Figure 5. 

    图 6  多年平均地面沉降评价分区

    Figure 6. 

    图 7  地层沉积相与地下水位

    Figure 7. 

    图 8  A-A’水文地质剖面

    Figure 8. 

    图 9  剖面一沿程地面沉降量变化

    Figure 9. 

    图 10  剖面二沿程地面沉降量变化

    Figure 10. 

    图 11  剖面三沿程地面沉降量变化

    Figure 11. 

    表 1  区域地面沉降速率分级标准

    Table 1.  Classification of regional land subsidence rate

    下载: 导出CSV

    表 2  沉降中心地面沉降速率分级标准

    Table 2.  Rate classification of land subsidence center

    下载: 导出CSV

    表 3  2012-2014年地面沉降面积统计

    Table 3.  Area statistics of multi-year land subsidence

    下载: 导出CSV

    表 4  2012—2014年地面沉降评价分区

    Table 4.  Land subsidence evaluation divisions in different years

    下载: 导出CSV

    表 5  沉降中心地面沉降评价

    Table 5.  Evaluation of land subsidence center

    下载: 导出CSV
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出版历程
收稿日期:  2018-05-27
修回日期:  2018-07-20
刊出日期:  2018-12-25

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