Wu Yingdong, Yu Jiang, Huang Zhi, Jiang Yinying, Zeng Zixin, Han Lei, Deng Siwei, Yu Jie
Department of Environmental Science and Engineering, College of Architecture and Environment, Sichuan University No. 24 South Section 1, Yihuan Road Chengdu 610065 PR China
Institute of New Energy and Low Carbon Technology, Sichuan University Chengdu 610065 PR China.
RSC Adv. 2024 Oct 14;14(44):32304-32313. doi: 10.1039/d4ra06060a. eCollection 2024 Oct 9.
Convection and diffusion are key pathways for the migration of total petroleum hydrocarbons (TPH) and heavy metals (HMs) from soil to groundwater. However, the extent of their influence on pollutant migration, as well as the nonlinear relationships between these processes and pollutants, remains unclear. This study investigates the spatial distribution of TPH and HMs at a petrochemical site with complex hydrogeological conditions in southwestern China. In addition, machine learning (ML) was used to assess the effects of convection and diffusion on pollutant migration at the soil-groundwater interface. The analysis identifies and reveals TPH, Co, and Ni as the primary pollutants, with soil concentrations reaching 47.427, 7.024, and 4.766 times their respective screening values. Among various ML models, Random Forest (RF) was identified as the most effective, based on , and RMSE performance metrics. The RF model demonstrates that the concentrations of TPH and As are closely related to soil depth. Furthermore, importance indices calculated by RF indicate that the significance of convection and diffusion varies across different soil-groundwater systems. Specifically, at the soil-perched water interface, convection plays a more significant role than diffusion in influencing the migration of TPH and As. However, at the soil-pore water interface, diffusion more significantly influences the migration of all pollutants compared to convection. Additionally, a threshold or saturation effect was observed for the impact of the convection factor on pollutant concentrations in groundwater. These findings highlight the distinct roles of convection and diffusion across various water interfaces, providing new insights into the mechanisms governing contaminant migration and fate.
对流和扩散是总石油烃(TPH)和重金属(HMs)从土壤迁移至地下水的关键途径。然而,它们对污染物迁移的影响程度,以及这些过程与污染物之间的非线性关系仍不明确。本研究调查了中国西南部一个水文地质条件复杂的石化场地中TPH和HMs的空间分布。此外,利用机器学习(ML)评估对流和扩散对土壤-地下水界面处污染物迁移的影响。分析确定并揭示TPH、钴和镍为主要污染物,土壤浓度分别达到其各自筛选值的47.427倍、7.024倍和4.766倍。在各种ML模型中,基于 和均方根误差(RMSE)性能指标,随机森林(RF)被确定为最有效的模型。RF模型表明,TPH和砷的浓度与土壤深度密切相关。此外,RF计算的重要性指数表明,对流和扩散的重要性在不同的土壤-地下水系统中有所不同。具体而言,在土壤上层滞水界面处,对流在影响TPH和砷的迁移方面比扩散发挥更重要的作用。然而,在土壤孔隙水界面处,与对流相比,扩散对所有污染物迁移的影响更为显著。此外,观察到对流因子对地下水中污染物浓度的影响存在阈值或饱和效应。这些发现突出了对流和扩散在各种水界面中的不同作用,为控制污染物迁移和归宿的机制提供了新的见解。