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人工回灌过程中富里酸和Cu(Ⅱ)对多孔介质悬浮物堵塞的影响

梁昊志 王欢 张俊杰 刘勇毅 方运海

梁昊志,王欢,张俊杰,等. 人工回灌过程中富里酸和Cu(Ⅱ)对多孔介质悬浮物堵塞的影响[J]. 水文地质工程地质,2023,50(5): 212-221 doi:  10.16030/j.cnki.issn.1000-3665.202301011
引用本文: 梁昊志,王欢,张俊杰,等. 人工回灌过程中富里酸和Cu(Ⅱ)对多孔介质悬浮物堵塞的影响[J]. 水文地质工程地质,2023,50(5): 212-221 doi:  10.16030/j.cnki.issn.1000-3665.202301011
LIANG Haozhi, WANG Huan, ZHANG Junjie, et al. Effect of fulvic acid and Cu(II) on the suspended particles clogging of porous media during artificial recharge[J]. Hydrogeology & Engineering Geology, 2023, 50(5): 212-221 doi:  10.16030/j.cnki.issn.1000-3665.202301011
Citation: LIANG Haozhi, WANG Huan, ZHANG Junjie, et al. Effect of fulvic acid and Cu(II) on the suspended particles clogging of porous media during artificial recharge[J]. Hydrogeology & Engineering Geology, 2023, 50(5): 212-221 doi:  10.16030/j.cnki.issn.1000-3665.202301011

人工回灌过程中富里酸和Cu(Ⅱ)对多孔介质悬浮物堵塞的影响

doi: 10.16030/j.cnki.issn.1000-3665.202301011
基金项目: 国家自然科学青年基金项目(42207064);广西科技基地和人才专项项目(桂科 AD21220079)
详细信息
    作者简介:

    梁昊志(1998-),男,硕士研究生,主要从事水资源利用与保护研究。E-mail:lianghaozhi1106@163.com

    通讯作者:

    王欢(1990-),男,讲师,主要从事水资源利用与保护研究。E-mail: wanghuan@glut.edu.cn

  • 中图分类号: P641

Effect of fulvic acid and Cu(II) on the suspended particles clogging of porous media during artificial recharge

  • 摘要: 地下水人工回灌是解决地下水超采问题的有效措施,悬浮颗粒物堵塞是影响回灌进行的技术瓶颈。目前多数研究聚焦在悬浮物堵塞方面,然而地表回灌水中重金属离子以及腐殖质对多孔介质物理堵塞的影响缺乏研究。本研究采用室内渗流砂柱试验研究富里酸、Cu(Ⅱ)以及两者共存对多孔介质悬浮物堵塞的影响,分别采用高岭土(SS组)、富里酸+高岭土(SS+FA组)、富里酸+Cu(Ⅱ)+高岭土(SS+FA+Cu组)配置模拟回灌用水。研究结果表明:(1)回灌结束时,SS组、SS+FA组、SS+FA+Cu组多孔介质整体相对渗透系数K’分别降至0.233,0.095,0.182。SS组和SS+FA+Cu组在中上层(0~7.50 cm)相对渗透系数K’均降至0.28以下,而在底层(7.50~10.50 cm)相对渗透系数K’仅降至0.45左右,说明2组多孔介质中上层重度堵塞(0<K’<0.30)、底层中度堵塞(0.30<K’<0.60);SS+FA组在各渗流段(0~10.50 cm)相对渗透系数K’均降至0.18以下,说明SS+FA组各渗流段多孔介质均为重度堵塞,相对其它2组,SS+FA组中悬浮物更易向深层迁移。(2)富里酸、Cu(Ⅱ)的存在会改变悬浮颗粒粒径、荷电性及内部氢键作用,从而影响多孔介质的堵塞发生。(3)相对SS组,SS+FA组富里酸的存在会加剧多孔介质堵塞;SS+FA+Cu组多孔介质整体堵塞程度比SS+FA组小,说明Cu(Ⅱ)会缓解富里酸对堵塞的加剧作用。探明富里酸和Cu(Ⅱ)对多孔介质堵塞的影响机制,能够为人工回灌过程中多孔介质堵塞的防治提供理论基础和科学依据。
  • 图  1  试验装置示意图

    Figure  1.  Schematic diagram of experimental setup

    图  2  傅里叶变换红外光谱图

    Figure  2.  Fourier transform infrared spectrum

    图  3  多孔介质整体相对渗透系数随时间变化

    Figure  3.  Changes of relative hydraulic conductivity for the entire sand column with time

    图  4  不同试验组砂柱各渗流段相对渗透系数随时间变化

    注:AB段表示0~1.50 cm;BC段表示1.50~4.50 cm;CD段表示4.50~7.50 cm;DE段表示7.50~10.50 cm。

    Figure  4.  Changes in relative hydraulic conductivity of each seepage section of the sand columns in different test groups with time

    图  5  不同渗流段石英砂介质中悬浮颗粒沉积量

    Figure  5.  Deposition of suspended particles in the sand column of different seepage layers

    图  6  悬浮颗粒粒径和静电斥力对迁移能力的影响

    Figure  6.  Influence of particle size and electrostatic repulsion of suspended particles on migration ability

    图  7  悬浮物堵塞类型及微观机制示意图

    Figure  7.  Schematic diagrams showing the mechanism of suspended solids clogging and main clogging types

    表  1  渗流试验主要组别及参数设计

    Table  1.   Parameters of different experimental groups

    试验组别 模拟回灌用水 高岭土浊度
    /NTU
    富里酸质量浓度
    /(mg·L−1
    Cu(Ⅱ)质量浓度
    /(mg·L−1
    CK组 纯水
    FA组 富里酸 5.00
    SS组 高岭土 100
    SS+FA组 高岭土+富里酸 100 5.00
    SS+FA+
    Cu组
    高岭土+富里酸+
    Cu(Ⅱ)
    100 5.00 1.00
    下载: 导出CSV

    表  2  不同组别悬浮物Zeta电位及粒径

    Table  2.   Zeta potential and particle size of suspended solids in different experimental groups

    试验组别 悬浮颗粒 悬浮颗粒共存物质 Zeta电位/mV 中位粒径/μm
    SS组 高岭土 −5.64 2.47
    SS+FA组 高岭土 富里酸 −8.56 2.05
    SS+FA+Cu组 高岭土 富里酸+Cu(Ⅱ) −7.22 2.37
    下载: 导出CSV
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  • 收稿日期:  2023-01-15
  • 修回日期:  2023-03-19
  • 网络出版日期:  2023-09-19
  • 刊出日期:  2023-09-19

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