在氧化还原交替下,在性大米土壤中的可溶性,具有对比的Cd来源和生物地球化学性质
Yizhang Liu1, Ying Wang1, Yongxiang Zhang2
1State Key Laboratory of Environmental Geochemistry, Institute of Geochemistry, Chinese Academy of Sciences, Guiyang 550081, China.
Journal of environmental sciences (China)
|November 2, 2025
概括
(Cd) 在性土中的溶解度受其来源和土壤特性的影响. 氧化转换会影响Cd的调动和再封存,影响其生物可用性.
科学领域:
- 环境科学 环境科学
- 土壤科学 土壤科学
- 地质化学 地质化学
背景情况:
- 碳酸盐地区的土面临着来自各种来源的 (Cd) 污染.
- 了解性土壤在氧化还原交替下Cd溶解度至关重要,但人们对其了解甚少.
研究的目的:
- 调查Cd溶解度,生物可用性和在米土壤中的物种化,在氧化还原变化下具有不同的Cd来源和特性.
- 确定地质与矿井排水Cd来源的影响,并对比和硫的丰度.
主要方法:
- 在交替的氧化还原条件下用地质或矿山排水衍生的Cd化米土壤.
- 监测水性化学,Cd生物可用性和物种.
- 分析微生物群落,特别是与硫有关的细菌.
主要成果:
- 矿井排水增加了可溶硫酸盐和与硫有关的细菌.
- 铁/氧化物和阴离子交换的减少溶解最初动员了Cd,随后进行了重新隔离.
- 在降解过程中,溶性Cd在地质土壤中减少,但在初始再氧化过程中增加.
- Cd的生物可用性随着减少时间而降低,随着氧化而增加.
结论:
- 碳酸的溶解度和命运高度依赖于石地区的土壤生物地球化学性质.
- 氧化还原变换显著改变了Cd的特异化,生物可用性和流动性.
- 土壤的特性,如硫和含量,在Cd行为中起着关键作用.
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