Dipartimento di Scienze Agrarie, Forestali e Alimentari, Università Degli Studi Di Torino, Largo Paolo Braccini 2, 10095, Torino, Grugliasco, Italy.
Soil and Water Management and Conservation Program, University Federal of Pelotas, Pelotas, Brazil.
Arch Environ Contam Toxicol. 2020 Nov;79(4):421-434. doi: 10.1007/s00244-020-00777-0. Epub 2020 Nov 11.
Metal-contaminated mining soils pose serious environmental and health risks if not properly managed, especially in mountainous areas, which are more susceptible to perturbation. Currently, climate change is leading to more frequent and intense rain events, which cause flooding episodes, thereby altering soil redox equilibria and contaminants stability. We evaluated the potential release of Zn and Cd (two of the most common inorganic contaminants) and the factors regulating their solubility and speciation in two heavily contaminated soils representative of a Zn-mining area. The soils were flooded under aerobic (for 24 h) and anaerobic (for 62 days) conditions using mesocosm experiments, sequential extractions, and geochemical modelling. Leaching trials under aerobic conditions showed a high release of Zn and Cd (10 times the legislative limits), with metals possibly migrating via water infiltration or runoff. Under anaerobic conditions Zn and Cd were initially released. Then, solution concentrations decreased gradually (Zn) or sharply (Cd) until the end of the experiment. Sequential extractions and multisurface modelling indicated that both metals precipitated mainly as carbonates. This was confirmed by a geochemical multisurface modelling, which also predicted the formation of sulphides after 60 days in one soil. The model calculated metals to be preferentially complexed by organic matter and well predicted the observed soil solution concentrations. The results showed that during flooding episodes contaminants could be promptly transferred to other environmental compartments. The use of multisurface modelling coupled with laboratory experiments provided useful indications on the potential release and speciation in case of anoxic conditions.
如果矿山土壤中的金属污染物得不到妥善管理,尤其是在容易受到干扰的多山地区,将会对环境和健康造成严重威胁。目前,气候变化导致暴雨和洪水等极端天气事件更加频繁和剧烈,这些事件会改变土壤的氧化还原平衡和污染物的稳定性。本研究采用中观实验、连续提取和地球化学模拟等方法,评估了两种具有代表性的 Zn 矿区重度污染土壤中 Zn 和 Cd(两种最常见的无机污染物)的潜在释放风险,以及影响其溶解和形态的因素。在好氧(24 h)和厌氧(62 天)条件下对土壤进行淹没实验,随后进行淋溶实验、连续提取和地球化学模拟。好氧条件下的淋溶实验表明,Zn 和 Cd 的释放量很高(是法定限量的 10 倍),金属可能通过水的渗透或径流迁移。厌氧条件下,Zn 和 Cd 最初被释放出来,然后溶液浓度逐渐(Zn)或急剧(Cd)下降,直到实验结束。连续提取和多表面模型表明,两种金属主要以碳酸盐的形式沉淀。这一结论得到了地球化学多表面模型的证实,该模型还预测了一种土壤中硫化物在 60 天后的形成。该模型计算出金属优先与有机物络合,并很好地预测了观察到的土壤溶液浓度。研究结果表明,在洪水事件期间,污染物可能会迅速转移到其他环境介质中。多表面模型与实验室实验的结合使用,为缺氧条件下污染物的潜在释放和形态提供了有用的指示。