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    河流潜流带地表水-地下水交互作用对磺胺甲恶唑迁移转化过程的影响

    潘维艳 刘洋 徐征和 桑国庆

    潘维艳, 刘洋, 徐征和, 桑国庆, 2026. 河流潜流带地表水-地下水交互作用对磺胺甲恶唑迁移转化过程的影响. 地球科学, 51(6): 2216-2227. doi: 10.3799/dqkx.2025.267
    引用本文: 潘维艳, 刘洋, 徐征和, 桑国庆, 2026. 河流潜流带地表水-地下水交互作用对磺胺甲恶唑迁移转化过程的影响. 地球科学, 51(6): 2216-2227. doi: 10.3799/dqkx.2025.267
    Pan Weiyan, Liu Yang, Xu Zhenghe, Sang Guoqing, 2026. Influence of Surface Water-Groundwater Interaction in Hyporheic Zone on Sulfamethoxazole Migration and Transformation Process. Earth Science, 51(6): 2216-2227. doi: 10.3799/dqkx.2025.267
    Citation: Pan Weiyan, Liu Yang, Xu Zhenghe, Sang Guoqing, 2026. Influence of Surface Water-Groundwater Interaction in Hyporheic Zone on Sulfamethoxazole Migration and Transformation Process. Earth Science, 51(6): 2216-2227. doi: 10.3799/dqkx.2025.267

    河流潜流带地表水-地下水交互作用对磺胺甲恶唑迁移转化过程的影响

    doi: 10.3799/dqkx.2025.267
    基金项目: 

    国家自然科学基金 42307083

    济南大学2024年学科交叉会聚建设项目 XKJC-202407

    详细信息
      作者简介:

      潘维艳(1987-),女,副教授,主要从事地表水-地下水交互作用下污染物迁移转化方面研究. ORCID:0009-0005-6063-9759

    • 中图分类号: X52

    Influence of Surface Water-Groundwater Interaction in Hyporheic Zone on Sulfamethoxazole Migration and Transformation Process

    • 摘要:

      磺胺甲恶唑(sulfamethoxazole,SMX)作为一种广泛使用的抗生素,其在环境中的残留与检出频率持续增加,研究SMX在河流潜流带中的迁移转化行为对保障河流生态健康与水安全至关重要.本研究基于室内模拟实验,探讨了不同水力梯度下,地表水-地下水交互作用对潜流带沉积物中SMX迁移转化规律的影响.结果表明:地表水-地下水交互作用驱动着潜流带环境因子的动态变化,进而引起微生物多样性及群落结构的演替,最终影响SMX的迁移与转化行为.SMX在潜流带中的转化主要经由水解、脱硫化和生物降解途径实现,其主导衰减机制随交互作用时间的延长而转变.其中,变形菌门与厚壁菌门是参与SMX生物降解的优势菌群.此外,水力梯度对SMX的去除效率具有明显影响,在低水力梯度下,较小的水流流速更有利于SMX在沉积物中的滞留与降解,因而表现出更显著的去除效果.

       

    • 图  1  潜流带地表水-地下水交互过程模拟实验装置

      Fig.  1.  Simulation experimental device for the process of water exchange in hyporheic zone

      图  2  不同水力梯度下沉积物孔隙水DO变化特征

      a. H1组DO; b. H2组DO

      Fig.  2.  Concentration changes of DO in sediment interstitial water at different depths under different hydraulic gradients

      图  3  不同水力梯度下沉积物孔隙水SMX变化特征

      a. H1组SMX; b. H2组SMX

      Fig.  3.  Concentration changes of SMX in sediment interstitial water at different depths under different hydraulic gradients

      图  4  不同水力梯度下沉积物孔隙水NH4+变化特征

      a. H1组NH4+; b. H2组NH4+

      Fig.  4.  Concentration changes of NH4+ in sediment interstitial water at different depths under different hydraulic gradients

      图  5  不同水力梯度下沉积物孔隙水SO42-变化特征

      a. H1组SO42-; b. H2组SO42-

      Fig.  5.  Concentration changes of SO42- in sediment interstitial water at different depths under different hydraulic gradients

      图  6  潜流带沉积物样品Shannon指数稀释曲线(a)和Chao1指数(b)

      Fig.  6.  Shannon indices (a) and Chao1 index (b) in river sediment samples

      图  7  潜流带沉积物样品在门水平与属水平的微生物种群结构

      Fig.  7.  Microbial community members at the phylum level and the genus level in river sediment samples

      表  1  实验水力梯度设计

      Table  1.   Design of experimental hydraulic gradients

      实验分组 地表水补给地下水 地下水补给地表水
      地表水水位(cm) 地下水水位(cm) 水力梯度 地表水水位(cm) 地下水水位(cm) 水力梯度
      H1 75 52.5 0.225 62.5 75 0.125
      H2 80 48.5 0.315 57.5 80 0.225
      下载: 导出CSV

      表  2  地表水模拟液的配置组分及浓度

      Table  2.   Composition and concentration of constituents in simulated surface water

      物质 C6H12O6 NH4Cl KNO3 KCl
      浓度(mg/L) 3.64 1.34 11.59 18.39
      物质 Ca(HCO3)2 NaCl CaCl2 SMX
      浓度(mg/L) 330 3.33 18.34 0.5
      下载: 导出CSV

      表  3  地下水模拟液的配置组分及浓度

      Table  3.   Composition and concentration of constituents in simulated groundwater

      物质 C6H12O6 NH4Cl KNO3 Ca(HCO3)2 NaCl SMX
      浓度(mg/L) 13.44 0.475 30.3 630.87 8.95 0.5
      下载: 导出CSV
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    • 收稿日期:  2025-09-30
    • 刊出日期:  2026-06-25

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