State Key Laboratory of Simulation and Regulation of Water Cycle in River Basin, China Institute of Water Resources and Hydropower Research, Beijing 100038, China; State Key Laboratory of Water Environment Simulation, School of Environment, Beijing Normal University, Beijing 100875, China.
State Key Laboratory of Water Environment Simulation, School of Environment, Beijing Normal University, Beijing 100875, China.
Ecotoxicol Environ Saf. 2018 Sep 30;160:184-190. doi: 10.1016/j.ecoenv.2018.05.039. Epub 2018 May 26.
The middle route of the South-to-North Water Diversion project alleviates drought in northern China, especially reducing water shortage pressure in Beijing. However, after submersion, the potential release risk of metals in newly submerged soils into the water in the receiving reservoir remains unclear. Here, we assess the labile Zn in the riparian soils of Miyun Reservoir (MYR) using the diffusive gradients in thin films (DGT), DGT-induced fluxes in soils (DIFS) model, and Community Bureau of Reference (BCR) sequential extraction. The results showed that the average Zn concentrations at three sampling sites (S2, S3, and S5) exceeded soil background value (74.8 mg/kg), indicative of Zn accumulation in the MYR. The concentrations of DGT-labile Zn varied within 39.7-62.4 μg/L (average: 56.7 μg/L), with the greatest value observed at 145 m at sampling site S3, attributed to anthropogenic activities in recreational areas. The DGT-labile Zn showed no correlation with classes of land, elevations, or soil properties. Sequential extraction results demonstrated that Zn predominantly existed in the residual fraction, but still showed a strong capability for resupply from the solid phase (R >1). The DIFS model simulation results showed that Zn underwent irreversible diffusion of intra-particle metals from the solid phase to the soil solution. Therefore, the potential release risk of labile Zn in riparian soils in MYR cannot be ignored, especially for areas experiencing human disturbance.
南水北调中线工程缓解了中国北方的干旱,特别是减轻了北京的缺水压力。然而,在淹没后,新淹没土壤中金属向受纳水库释放的潜在风险尚不清楚。在这里,我们使用薄膜扩散梯度(DGT)、土壤中 DGT 诱导通量(DIFS)模型和社区参考局(BCR)顺序提取法评估了密云水库(MYR)滨岸土壤中的可利用锌。结果表明,在三个采样点(S2、S3 和 S5)的平均 Zn 浓度超过了土壤背景值(74.8mg/kg),表明 MYR 中的 Zn 积累。DGT-可利用 Zn 的浓度变化范围为 39.7-62.4μg/L(平均值:56.7μg/L),在采样点 S3 的 145m 处最大,这归因于娱乐区的人为活动。DGT-可利用 Zn 与土地类别、海拔或土壤性质均无相关性。顺序提取结果表明,Zn 主要存在于残余物中,但仍具有从固相强烈供应的能力(R>1)。DIFS 模型模拟结果表明,Zn 经历了不可逆的金属从固相到土壤溶液的颗粒内扩散。因此,不能忽视 MYR 滨岸土壤中可利用 Zn 的潜在释放风险,特别是在受到人为干扰的地区。