采矿影响的土壤中的Cd调动与不同的基岩石质:从稳定的Cd同位素的洞察力
Yuhui Liu1, Yafei Xia2, Jian-Ming Zhu3
1State Key Laboratory of Environmental Geochemistry, Institute of Geochemistry, Chinese Academy of Sciences, Guiyang 550081, PR China.
采矿活动将 (Cd) 释放到土壤中. 它的重新分配因土壤类型而异,影响环境风险,并需要对的土壤质量标准.
科学领域:
- 环境科学 环境科学
- 地质化学 地质化学
- 土壤科学 土壤科学
背景情况:
- 土壤 (Cd) 风险与其调动有关,但其从外部输入到各种地质环境中的再分配不明.
- 了解土壤中的外源性Cd命运对于评估环境风险和告知修复策略至关重要.
研究的目的:
- 调查外源 (Cd) 在矿区土壤中的再分配,其中有对比的岩和石灰岩石质.
- 用稳定的Cd同位素阐明石质学对Cd调动和植物吸收的影响.
主要方法:
- 稳定 (Cd) 同位素追踪被用来追踪的来源和再分配.
- 来自矿和石灰矿区的土壤样本分析了Cd度,同位素组成 (δ114/110Cd),矿物质含量和有机碳.
主要成果:
- 稳定同位素追踪证实采矿是两个研究区域的主要Cd来源.
- 在状土壤中,矿物溶解中的Cd释放和高可交换/结合Fe的Cd分数促进了重Cd同位素的上升植物运输.
- 在石灰质土壤中,Cd与有机碳相关,这表明受土壤有机物碳酸盐稳定影响的复合.
结论:
- 石质学显著影响了土壤中的外源的再分配途径.
- 在制定土壤质量指南时,必须考虑区域地质特征,特别是石质.
- 这些发现为管理各种采矿受影响的景观中的Cd污染提供了关键的见解.
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