在山地不连续的永久土中对流金属的季节性控制 ((loid) 签名
E K Skierszkan1, S K Carey2, S I Jackson3
1Department of Geological Sciences, University of Saskatchewan, 114 Geological Sciences Place, Saskatoon S7N 5E2, Canada.
The Science of the total environment
|November 1, 2023
概括
永久土解中的季节性流动模式会影响微量金属度. 地下水排放会释放出和,而融雪会动员与有机碳复合的金属.
科学领域:
- 环境科学 环境科学
- 地质化学 地质化学
- 水文学的水文学
背景情况:
- 不连续的永久土中的亚北极流体呈现季节性微量金属 (化物) 波动.
- 了解这些动态对于评估水资源质量至关重要.
研究的目的:
- 研究控制亚北极流中的季节性微量金属变化的物理和化学过程.
- 开发一种由永久土融化影响的金属化物释放的概念模型.
主要方法:
- 整合多年流量,地化学数据和地质样本分析 (基岩,永久土,活性层).
- 对季节性水文系统的分析:冬季的底流,春季的新鲜水和夏季的高流.
主要成果:
- 在基流过程中地下水的排放会释放出和.
- ,,铜,铁,,和的峰值度与高流量和新鲜水源有关.
- 的度表现出复杂的季节性变化,受活动层和基岩地下水流道的影响.
结论:
- 季节性水文制度显著控制了亚北极流中的微量金属度.
- 提出了一个概念模型来解释在不连续的永久土环境中的金属 (体) 释放机制.
- 这些发现为预测永久土融化对水资源的影响提供了一个框架.
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