泥炭沼泽孔水中溶解微量元素的时空空间变化受到阿塔巴斯卡金沙 (ABS) 地区露天采矿活动的尘埃输入的影响
Sundas Arooj Butt1, Fiorella Barraza1, Kevin Devito2
1Department of Renewable Resources, University of Alberta, Edmonton, AB, Canada.
Environmental pollution (Barking, Essex : 1987)
|February 2, 2024
概括
矿开采的灰尘会在泥炭沼泽孔水中微微增加一些元素,如,但不会显著影响有毒的微量元素. 采矿对这些元素的生态影响是温和的.
科学领域:
- 环境科学 环境科学
- 地质化学 地质化学
- 生态毒理学 生态毒理学
背景情况:
- 在阿尔伯塔省北部,露天矿开采会产生大量的灰尘.
- 尘埃中的反应性矿物质可以溶解在酸性沼泽水中,可能释放微量元素 (TE).
- 这种溶解可能会改变泥炭地生态系统.
研究的目的:
- 评估尘埃溶解对泥炭孔水中微量元素丰度的影响.
- 评估采矿灰尘是否会改变沼泽生态系统的化学组成.
主要方法:
- 从阿塔巴斯卡砂 (ABS) 地区的五个泥炭地收集了孔水样本 (<0.45微米分数).
- 四个沼泽地靠近矿山;一个作为参考地点 (距离264公里).
- 溶解元素度在两年内进行了分析.
主要成果:
- 随着采矿区的接近,保守元素 (Al,Th,Y),石化元素 (Fe,Li,Mn,Sr) 和缩元素 (V,Ni,Mo) 的溶解度增加.
- 潜在的有毒TEs (As,Cd,Pb,Sb,Tl) 的度受到尘埃溶解的微不足道影响.
- 与参考标准相比,在采矿场附近的缩量最大 (>10倍).
结论:
- 从矿开采中产生的人为尘埃对泥炭孔水中微量元素的总体丰度的影响很小.
- 丰富元素主要是生态无害的或必需的微量营养素,无毒.
- 该研究表明,尘埃溶解对有毒微量元素的生态风险有限.
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