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莱州湾滨海平原沉积环境对古卤水盐分迁移能力的影响

韩汝杰 李静 李晓波

韩汝杰, 李静, 李晓波. 莱州湾滨海平原沉积环境对古卤水盐分迁移能力的影响[J]. 地质科技通报, 2024, 43(5): 259-271. doi: 10.19509/j.cnki.dzkq.tb20230307
引用本文: 韩汝杰, 李静, 李晓波. 莱州湾滨海平原沉积环境对古卤水盐分迁移能力的影响[J]. 地质科技通报, 2024, 43(5): 259-271. doi: 10.19509/j.cnki.dzkq.tb20230307
HAN Rujie, LI Jing, LI Xiaobo. Influence of the sedimentary environment on the salt migration ability of ancient brine in the coastal plain of Laizhou Bay[J]. Bulletin of Geological Science and Technology, 2024, 43(5): 259-271. doi: 10.19509/j.cnki.dzkq.tb20230307
Citation: HAN Rujie, LI Jing, LI Xiaobo. Influence of the sedimentary environment on the salt migration ability of ancient brine in the coastal plain of Laizhou Bay[J]. Bulletin of Geological Science and Technology, 2024, 43(5): 259-271. doi: 10.19509/j.cnki.dzkq.tb20230307

莱州湾滨海平原沉积环境对古卤水盐分迁移能力的影响

doi: 10.19509/j.cnki.dzkq.tb20230307
基金项目: 

国家自然科学基金项目 41977167

国家自然科学基金项目 423377071

广西重点研发计划项目 桂科AB21196026

详细信息
    作者简介:

    韩汝杰, E-mail: hanrujiecug@163.com

    通讯作者:

    李静, E-mail: lijing915@cug.edu.cn

  • 中图分类号: P641

Influence of the sedimentary environment on the salt migration ability of ancient brine in the coastal plain of Laizhou Bay

More Information
  • 摘要:

    海岸带沉积环境是研究地下水演化与运移的基础。为探讨莱州湾南岸沉积环境对咸-淡地下水空间分布及迁移能力的影响,钻探采集了2个第四纪典型钻孔(LZ01和LZ02)样品,利用压榨法提取了孔隙水,测定了沉积物的粒度组成和孔隙水Cl-浓度。结果表明,2个钻孔均以细粒沉积物为主,平均粒径为5.5ϕ。根据沉积物岩性和粒度参数特征,得出LZ01与LZ02钻孔分别包含10、9个沉积相态交替,揭露了晚更新世以来的3套海相地层单元。孔隙水以卤(咸)水为主,Cl-浓度剖面形态呈现3个峰值,3个卤水层分别与3套海相地层对应,表明沉积物中残留海相古卤水,并向相邻沉积物中扩散。沉积物的水动力指数与Cl-浓度垂向变化率呈现明显的分区性;中等水动力条件下,孔隙水Cl-扩散迁移能力强。敏感粒径分析表明孔隙水迁移的优势粒径范围为45.61~111.47 μm。研究区古海侵事件控制了卤水的分布,而低渗透性及岩性组合对封存古卤水起着重要作用。研究结果可为莱州湾滨海平原卤水成因、地下水咸化及运移研究提供理论依据。

     

  • 图 1  莱州湾南岸研究钻孔位置及地层柱状简图(据文献[17-18]修改)

    Figure 1.  Boreholes locations and stratigraphic column diagram for southern Laizhou Bay

    图 2  莱州湾南A-A′(昌邑-青乡)地层剖面(据文献[10]修改)

    Figure 2.  A-A′(Changyi-Qingxiang) stratigraphic section in southern Laizhou Bay

    图 3  LZ01钻孔典型沉积物粒度频率分布曲线

    a.不对称双峰或三峰型;b.极不对称双峰型;c.三峰或多峰型。图中数值均为埋深

    Figure 3.  Grain size frequency curves for typical sediments of borehole LZ01

    图 4  LZ01(a)和LZ02(b)钻孔沉积物粒度参数特征及沉积相(岩性图例同图 1)

    Figure 4.  Grain size distribution parameters and sedimentary facies of boreholes LZ01(a) and LZ02(b)

    图 5  莱州湾南岸钻孔地层划分对比(WFZK07钻孔引自文献[40];LZ908钻孔引自文献[41];岩性图例同图 1)

    Figure 5.  Division and comparison of the studied boreholes in southern Laizhou Bay

    图 6  钻孔沉积物孔隙水Cl-质量浓度及变化率(岩性图例同图 1)

    Figure 6.  Cl- concentration and variation rate of porewater borehole sediments

    图 7  ρ(Cl-)变化率-区域水动力指数图

    Figure 7.  Diagram of Cl- concentration change rate-interval hydrodynamic index

    图 8  钻孔LZ01(a)与LZ02(b)沉积物粒径-标准偏差曲线

    Figure 8.  Grain size versus standard deviation curves of LZ01(a) and LZ02(b) sediments

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出版历程
  • 收稿日期:  2023-05-29
  • 录用日期:  2023-09-28
  • 修回日期:  2023-09-17

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