左玉涛, 孔文亮, 代义彬, SEIDOU C. D., 王铁军. 某工业场地土壤砷的空间分布及As(Ⅲ)迁移规律研究[J]. 土壤通报, 2024, 55(2): 502 − 512. DOI: 10.19336/j.cnki.trtb.2023021702
引用本文: 左玉涛, 孔文亮, 代义彬, SEIDOU C. D., 王铁军. 某工业场地土壤砷的空间分布及As(Ⅲ)迁移规律研究[J]. 土壤通报, 2024, 55(2): 502 − 512. DOI: 10.19336/j.cnki.trtb.2023021702
ZUO Yu-tao, KONG Wen-liang, DAI Yi-bin, SEIDOU C. D., WANG Tie-jun. Investigation of Spatial Distribution and Migration Pattern of Arsenic in Soils of Industrial Sites[J]. Chinese Journal of Soil Science, 2024, 55(2): 502 − 512. DOI: 10.19336/j.cnki.trtb.2023021702
Citation: ZUO Yu-tao, KONG Wen-liang, DAI Yi-bin, SEIDOU C. D., WANG Tie-jun. Investigation of Spatial Distribution and Migration Pattern of Arsenic in Soils of Industrial Sites[J]. Chinese Journal of Soil Science, 2024, 55(2): 502 − 512. DOI: 10.19336/j.cnki.trtb.2023021702

某工业场地土壤砷的空间分布及As(Ⅲ)迁移规律研究

Investigation of Spatial Distribution and Migration Pattern of Arsenic in Soils of Industrial Sites

  • 摘要:
    目的 旨在掌握某工业场地土壤中砷(As)的空间分布特征并揭示其迁移规律,为该工业场地土壤As污染防治提供数据与理论基础。
    方法 本文选取葫芦岛市某工业场地为研究区,首先统计分析了场地内土壤As含量的空间分布特征,并比较了等温与动态吸附两种获取土壤中As (Ⅲ)吸附参数的实验方法的特点与适用性,最终利用HYDRUS-1D模型反演计算了As (Ⅲ)在供试土壤中的DLKαβ等迁移参数。
    结果 场地土壤As浓度水平分布具有显著差异,在垂向上主要富集于40 cm深度内,且随深度增加而降低。等温吸附实验的结果表明:土样中As (Ⅲ)的平衡固相浓度随液相浓度增加呈非线性增长趋势,Langmuir模型(R2 = 0.988)对实测数据的拟合效果优于Henry和Freundlich模型。动态吸附实验结果展示了As (Ⅲ)相对浓度完全穿透土柱所需的污染液体积随As (Ⅲ)初始浓度的增加而减少的规律;HYDRUS-1D反演结果表明三类吸附模型中,Langmuir模型(R2 = 0.990)更适用于模拟土样中As(Ⅲ)的动态吸附过程。相较于等温吸附实验,使用动态吸附实验模拟As (Ⅲ)迁移行为更接近其在土壤中的真实迁移过程。
    结论 该场地中的As污染来源于工业活动,主要集中在浅层土壤;土壤中As (Ⅲ)的迁移行为表现为非线性过程,较高的初始浓度将加速As (Ⅲ)的垂向迁移。动态吸附实验方法应优先应用于土壤As迁移过程及其参数获取的研究中。

     

    Abstract:
    Objective The present study aims to investigate the spatial distribution characteristics of As in the soil of industrial sites, and to reveal its migration rules via relevant in-situ and indoor experiments based on field sampling. The research seeks to provide data and a theoretical basis for the prevention and control of As pollution in industrial site soil.
    Method An industrial site in Huludao was selected as the research area. Firstly, the spatial distribution characteristics of soil As content in the site were described. Two experimental methods (including isothermal and dynamic adsorption experiments) were compared for the determination of As(Ⅲ) adsorption parameters in soil. Finally, the HYDRUS-1D model was employed to calculate the migration parameters of As (Ⅲ).
    Result The results of in-situ soil experiments revealed significant differences in the horizontal distribution of As in the site, with the element being primarily enriched at a depth of 40 cm in the vertical direction, and decreasing with increasing depth. Based on the results of isothermal adsorption experiments, the equilibrium solid phase concentration of As (Ⅲ) in soil samples displayed a nonlinear growth trend with increasing liquid phase concentration. The Langmuir model (R2 = 0.988) exhibited better fitting performance than the Henry and Freundlich models. The dynamic adsorption experiments demonstrated that the relative concentration of As (Ⅲ) completely penetrated the soil column, and the volume of liquid required to achieve full penetration decreased with increasing initial concentration. Among the three types of adsorption models, the Langmuir model (R2 = 0.990) was deemed more suitable for simulating the dynamic adsorption process of As (Ⅲ) in soil samples. When simulating the migration behavior of As(Ⅲ), the dynamic adsorption experiment more closely approximated the actual migration process.
    Conclusion The research results indicate that the As pollution in this site stemmed from industrial activities, and was primarily concentrated in shallow soil. The migration behavior of As (Ⅲ) exhibited a nonlinear process, with higher initial concentrations accelerating vertical migration. The dynamic adsorption experimental method should be preferentially employed in the study of soil As migration and parameter acquisition.

     

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