Bao Junsong, Chang Yanhong, Cheng Nuo, Li Yingxia, Chang Xuan, Feng Jiashen, Nan Xue, Ren Hongmin
State Key Laboratory of Water Environment Simulation, School of Environment, Beijing Normal University, 19 Xinjiekouwai Street, Haidian District, Beijing 100875, China.
College of Water Sciences, Beijing Normal University, 19 Xinjiekouwai Street, Haidian District, Beijing, China.
Sci Total Environ. 2024 Dec 1;954:176511. doi: 10.1016/j.scitotenv.2024.176511. Epub 2024 Sep 27.
In order to achieve effective management of urban stormwater runoff, green stormwater infrastructure (GSI) has been widely used worldwide. However, the problem of heavy metal contamination in GSI soils has gradually become a limiting factor for their development. In this paper, concentrations of 6 heavy metals were detected in soils from 0 to 80 cm depth in the GSI receiving roof runoff. The total concentration of the 6 heavy metals in topsoil of the GSI was 395 mg·kg, which was significantly higher than that of the control site (p < 0.01). Vertically, heavy metal concentrations in GSI soils decreased with depth. The concentrations of As, Cr, Cu, Pb and Zn in the soils at different depths (0-80 cm) of GSI were higher than those in the soils at the corresponding depths at the control site. This suggests that heavy metals may have migrated below 80 cm. The decrease in Zn/Cu ratios with depth indicated that Zn has a higher initial concentration and more of Zn accumulated in upper layer soil than Cu. Finally, we simulated the vertical migration of dissolved heavy metals in GSI soils by the Hydrus-1D model. Heavy metal concentrations in runoff and soil particle size distributions were examined, while adsorption isotherm experiments were conducted to determine input parameters for the model. The simulation results showed that only dissolved Zn would accumulate in the top soil layer. A short time of infiltration (<60 min) may have little effect on the profile shape of dissolved heavy metal levels in the soil. Substantial increases in infiltration may result in the migration of dissolved heavy metals to deeper depths in the soil.
为实现城市雨水径流的有效管理,绿色雨水基础设施(GSI)在全球范围内得到了广泛应用。然而,GSI土壤中的重金属污染问题已逐渐成为其发展的限制因素。本文检测了GSI接收屋面径流的土壤中0至80厘米深度内6种重金属的浓度。GSI表层土壤中6种重金属的总浓度为395毫克·千克,显著高于对照点(p < 0.01)。垂直方向上,GSI土壤中的重金属浓度随深度降低。GSI不同深度(0 - 80厘米)土壤中As、Cr、Cu、Pb和Zn的浓度高于对照点相应深度土壤中的浓度。这表明重金属可能已迁移至80厘米以下。Zn/Cu比值随深度降低表明Zn的初始浓度较高,且在上层土壤中积累的Zn比Cu更多。最后,我们利用Hydrus - 1D模型模拟了GSI土壤中溶解态重金属的垂直迁移。研究了径流中的重金属浓度和土壤粒径分布,同时进行吸附等温线实验以确定模型的输入参数。模拟结果表明,只有溶解态Zn会在表层土壤层积累。短时间的入渗(<60分钟)对土壤中溶解态重金属水平的剖面形状可能影响较小。入渗量大幅增加可能导致溶解态重金属向土壤更深层迁移。