Simón M, García I, Martín F, Díez M, del Moral F, Sánchez J A
Departamento de Edafología y Química Agrícola, EPS CITE IIB, Universidad de Almería, 04120 Almería, Spain.
Sci Total Environ. 2008 Dec 15;407(1):23-39. doi: 10.1016/j.scitotenv.2008.07.040. Epub 2008 Oct 21.
The soils affected by the spill of a pyrite mine were analysed in 100 sampling points at three depths (0-10, 10-30, and 30-50 cm) in 1998 (after the tailings were removed), 1999 (after the cleaning of the highly contaminated areas), and 2004 (after the tilling of the upper 20-25 cm). The comparative study reveals that the removal of the tailings left a heterogeneous distribution pattern of the contaminants, with highly polluted spots alternating with less contaminated areas. The cleanup did not substantially lower the concentration in the highly polluted soils, and the spread of the pollutants increased the concentration in As and Pb in the uppermost 10 cm of 60% of the soils, while the Zn and Cd concentrations increased in only 30% of the soils. Given the high concentration of pollutants in the topsoil (especially As), the tilling of the upper 20-25 cm, despite reducing the average concentration of pollutants in the uppermost 10 cm, did not substantially lower the percentage of soils that exceeded the concentration of 40 mg As kg(-1) dry soil and almost doubled the percentage of soils that surpassed this concentration between 10 and 30 cm. Meanwhile, the displacement of Zn and Cd within the soil supported the reduction in the percentage of soils that in the upper 10 cm exceeded the reference concentrations of these elements (900 mg Zn kg(-1) dry soil and 2 mg Cd kg(-1) dry soil), and the percentage of soils exceeding these concentrations between 10 and 50 cm in depth did not increase. Six years after the spill and at the end of all remediation measures, the intervention levels defined by the Environmental Agency of the Regional Government of Andalusia for natural parks were exceeded in the uppermost 10 cm in 35% of the soils.
1998年(尾矿清除后)、1999年(高污染区域清理后)和2004年(上层20 - 25厘米土壤翻耕后),在三个深度(0 - 10厘米、10 - 30厘米和30 - 50厘米)的100个采样点对受黄铁矿矿山泄漏影响的土壤进行了分析。对比研究表明,尾矿的清除留下了污染物的不均匀分布模式,高污染点与污染较轻的区域交替出现。清理工作并未大幅降低高污染土壤中的污染物浓度,污染物的扩散使60%的土壤最上层10厘米中的砷和铅浓度增加,而锌和镉浓度仅在30%的土壤中增加。鉴于表层土壤中污染物浓度较高(尤其是砷),上层20 - 25厘米的翻耕,尽管降低了最上层10厘米土壤中污染物的平均浓度,但并未大幅降低超过40毫克砷/千克干土浓度的土壤百分比,并且使10至30厘米深度之间超过该浓度的土壤百分比几乎增加了一倍。同时,土壤中锌和镉的迁移有助于降低最上层10厘米中超过这些元素参考浓度(900毫克锌/千克干土和2毫克镉/千克干土)的土壤百分比,并且深度在10至50厘米之间超过这些浓度的土壤百分比没有增加。泄漏事件发生六年且所有修复措施结束后,安达卢西亚自治区政府环境局为自然公园定义的干预水平在35%的土壤最上层10厘米中被超过。