基于多种同位素证据,确定矿山 - 农村 - 城市聚合区的地表水中酸盐积累机制
Xing Chen1, Mengxi Ren2, Guolian Li3
1School of Environment and Energy Engineering, Anhui Jianzhu University, Hefei 230601, China; Anhui Province Engineering Laboratory for Mine Ecological Remediation, Anhui University, Hefei 230601, China.
The Science of the total environment
|December 9, 2023
概括
采矿区的酸盐污染主要是由化引起的,而不是脱化. 这项研究揭示了管理水质和防止进一步破坏环境的关键机制.
科学领域:
- 环境科学 环境科学
- 地质化学 地质化学
- 水质管理水质管理
背景情况:
- 矿业和城市化造成的酸盐在地表水中的积累是一个重大的环境问题.
- 有效的循环阐明和水质管理需要了解酸盐转化过程.
研究的目的:
- 调查酸盐 (NO3-) 含量的时间和空间变化,在华北矿区.
- 通过稳定同位素和水化学分析,确定推动酸盐积累的关键机制.
主要方法:
- 监测NO3度和多个同位素 (δD, δ18O-H2O, δ15N-NO3-, δ18O-NO3-, δ15N-NH4+) 的情况.
- 分析水化学指标以确定循环过程.
- 评估氧化还原条件和同位素特征,以区分化和脱化.
主要成果:
- 地表水NO3度在0.28至7.50毫克/升之间,NO3是主要的污染物.
- 与雨季相比,在干旱季节观察到较高的平均NO3水平.
- 亚化被确定为NO3积累的主要驱动因素;发现亚化被削弱.
结论:
- 化是导致酸盐在北矿区地表水中积累的主要过程.
- 植物浮游生物减弱的脱和优先吸收氨有助于酸盐的持久性.
- 调查结果为开发矿区有针对性的水环境管理战略提供了关键的见解.
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