State Key Laboratory of Simulation and Regulation of Water Cycle in River Basin, China Institute of Water Resources and Hydropower Research, Beijing 100038, China; Department of Water Ecology and Environment, China Institute of Water Resources and Hydropower Research, Beijing 100038, China.
Department of Water Ecology and Environment, China Institute of Water Resources and Hydropower Research, Beijing 100038, China.
Sci Total Environ. 2023 Jul 10;881:163495. doi: 10.1016/j.scitotenv.2023.163495. Epub 2023 Apr 15.
The Three Gorges Reservoir (TGR) has formed the water-level-fluctuation zone (WLFZ) due to reservoir regulation. However, as a sensitive zone in reservoir, little is known about the geochemical process and ecotoxicological risk of arsenic (As) in WLFZ soils under the anti-seasonal flow regulation. Hence, the anthropogenic contamination, mobility and ecotoxicological risks of As in WLFZ soils of the TGR were comprehensively assessed using the geochemical baseline concentration (GBC), chemical fractions, diffusive gradients in thin films (DGT) and toxicity data. The As concentrations in WLFZ soils showed a trend of increasing at the early stage of water impoundment and then stabilizing in recent years, which presented a low ecological risk of As according to the assessment by pollution indices. Based on GBC calculations, the average anthropogenic contribution of As was 13.95 %, indicating a slight influence of human activities. The distribution of labile As measured by DGT in WLFZ soils was mainly controlled by the Fe/Mn oxides, pH and organic matter. The DGT-induced fluxes in soils (DIFS) model further implied that resupply of As to soil solution was partially sustained by the soil solid phase, in which the resupply capacity was low and limited by the adsorption and desorption kinetics. In addition, the DGT was combined with toxicity data to obtain the risk quotient (RQ) and probabilistic risk assessment. The RQ value was lower than 1, indicating a low toxicity risk in WLFZ soils. Furthermore, the As in WLFZ soils had a low probability (5.97E-3 % and 7.77E-2 % in the mainstream and tributary, respectively) of toxic effects toward the aquatic biota. This study provides a comprehensive evaluation for the mobility and toxicity risk of As in WLFZ soils, which is beneficial to the prevention and control of heavy metals pollution in the riparian soils of lakes and reservoirs.
三峡水库因水库调节而形成了水位变动带(WLFZ)。然而,作为水库的一个敏感区域,在反季节水流调节下,WLFZ 土壤中砷的地球化学过程和生态毒理学风险知之甚少。因此,本研究采用地球化学基线浓度(GBC)、化学形态、薄膜扩散梯度(DGT)和毒性数据,综合评估了三峡水库 WLFZ 土壤中砷的人为污染、迁移和生态毒理风险。WLFZ 土壤中的砷浓度在蓄水初期呈上升趋势,近年来趋于稳定,根据污染指数评估,呈现出低生态风险的砷。基于 GBC 计算,砷的平均人为贡献为 13.95%,表明人类活动的影响较小。DGT 测量的 WLFZ 土壤中可利用砷的分布主要受铁/锰氧化物、pH 值和有机质的控制。DGT 诱导的土壤通量(DIFS)模型进一步表明,土壤固相部分维持了砷向土壤溶液的再供应,其再供应能力较低,受到吸附和解吸动力学的限制。此外,将 DGT 与毒性数据相结合,得到风险商(RQ)和概率风险评估。RQ 值低于 1,表明 WLFZ 土壤的毒性风险较低。此外,WLFZ 土壤中的砷对水生生物的毒性较低(主流和支流中的 RQ 值分别为 5.97E-3%和 7.77E-2%)。本研究对 WLFZ 土壤中砷的迁移性和毒性风险进行了综合评价,有利于湖泊和水库滨岸土壤重金属污染的防治。