在南极冰流下绘制的动态盐水系统
Chloe D Gustafson1,2, Kerry Key1, Matthew R Siegfried3
1Lamont-Doherty Earth Observatory, Columbia University, Palisades, NY, USA.
概括
科学家在南极洲的威兰斯冰流下发现了巨大的地下水系统. 这一发现显示出一个比以前更大的冰下水库, 影响了冰流动力和冰下过程.
科学领域:
- 地质学
- 冰川学
- 水文地质学
背景情况:
- 南极洲的冰流对于冰盖排水至关重要,
- 目前对冰下水系统的了解仅限于冰床接口附近的浅层地区.
- 深层地下水在调节冰流速度方面的潜在作用仍在很大程度上未被探索.
研究的目的:
- 在南极的威兰斯冰流下调查深层地下水的存在和特征.
- 确定深层地下水库是否会影响冰下水系统和冰流动力.
主要方法:
- 使用磁和被动地震地质物理技术.
- 收集了来自西南极洲威兰斯冰流的数据.
- 分析数据以绘制深层地下结构并确定地下水的存在.
主要成果:
- 提供了南极冰流下深层地下水的第一次直接观测.
- 在厚度大于1公里的沉积盆地内确定了大量的地下水,超过已知的冰下水系统的数量.
- 检测到垂直盐度梯度, 这表明古代海水与现代基础水之间的相互作用.
结论:
- 深层地下水系统是南极冰川下水文学的重要,以前未知的组成部分.
- 这些深层系统可能在调节冰流速度和相关的生物地化学过程中发挥关键作用.
- 这些发现需要修改冰下水流和冰盖动态的模型.
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