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堵塞对大型水库水地化学特征和潜在环境风险的影响:来自不同垂直层采样的见解
Di Wang1, Guilin Han1, Mingming Hu2
1Institute of Earth Sciences, China University of Geosciences (Beijing), Beijing, 100083, China.
Environmental research
|October 14, 2023
概括
三峡水库的水化学表明,主要离子随着深度的增加而增加. 多洛米特和石风化占主导地位,对农业的影响有限. 更深的水域揭示了额外的气候变化过程和对儿童的潜在风险.
科学领域:
- 地质化学 地质化学
- 环境科学 环境科学
- 水文学的水文学
背景情况:
- 由于大水库的水环境脆弱,原因是水调节和人类活动.
- 河流溶液化学对于理解化学气候变化和环境风险至关重要.
- 在水库中的垂直地质化学在气候和水质评估方面未得到充分探索.
研究的目的:
- 为了研究三峡水库 (TGR) 中分层水的溶液地化学.
- 量化化学气候变化的来源,评估灌和健康风险的水质.
- 探索垂直地质化学在大型水库环境中的重要性.
主要方法:
- 来自TGR的分层水样本中的化学成分的确定.
- 应用一个改进的反转模型来量化溶解物源的贡献.
- 评估水质的灌适用性和非致癌风险.
主要成果:
- (Ca2+) 和碳酸 (HCO3-) 是最丰富的离子.
- 主要离子度随着水深和下游流量的增加而增加.
- 多洛米特和石的气候变化是主要的阴离子来源;更深的水域显示了蒸发石和石的贡献,影响了CO2流量估计.
- TGR水适合灌,但酸盐 (NO3-) 对儿童构成潜在的非致癌风险,特别是在地表水中.
结论:
- 垂直水地化学为大水库中的气候变化过程和CO2流提供了关键的见解.
- 总体而言,TGR的水质对于灌是很好的,但酸盐含量存在特殊问题.
- 这项研究增强了TGR的水化学数据,为水库管理提供了理论指导.
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