关于北极高层永久土的水文和连续性的Ra同位素观点
Dotan Rotem1, Yishai Weinstein2, Hanne H Christiansen3
1Department of Environment, Planning and Sustainability, Bar-Ilan University, Ramat-Gan, Israel; Arctic Geology Department, the University Centre in Svalbard, UNIS, Longyearbyen, Norway.
The Science of the total environment
|August 10, 2024
概括
养斯瓦尔巴德岛的地下水.
科学领域:
- 地质科学 地质科学
- 水文学的水文学
- 同位素地球化学 同位素地球化学
背景情况:
- 斯瓦尔巴德的企是由地下水结而形成的.
- 该地区的永久土已有4000多年的历史.
研究的目的:
- 调查斯瓦尔巴德pingos地下水排放的地下居住时间.
- 使用同位素分析确定地下水的年龄.
主要方法:
- 对三同位素 (3H) 的分析.
- (Ra) 同位素测量,特别是226Ra/223Ra活动比.
主要成果:
- 三含量表明地下水年龄超过60年.
- 放射的同位素表明,它在地表下停留了几百年的时间.
- 观察到的Ra同位素比 (活性比<21.7) 支持更长的停留时间.
结论:
- 年轻的地下水在永久土形成后补充了含水层.
- 充电可能会通过断层或亚冰川通道发生.
- 活跃的水文学表明,在晚期全新纪期间,永久土是不连续的.
- 对工业化前的温室气体释放的潜在影响.
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