概括
一个新的模型表明,南极的蓝色冰区稳步地集中了石. 这项研究表明不断的石流入和冰流,揭示了可能是地球上最古老的冰序列.
科学领域:
- 流星学和行星科学
- 冰川学的冰川学
- 南极研究南极研究
背景情况:
- 南极洲的蓝冰地区作为石的自然陷.
- 了解石积累需要冰流和积累速度的模型.
- 之前的研究已经估计了石流入,但缺乏集中过程的综合模型.
研究的目的:
- 在南极蓝冰地区开发石度模型.
- 为了估计石流入的速度和暴露的冰的年龄.
- 为了测试恒定的石流入和冰川流动的假设.
主要方法:
- 基于来自艾伦山地区的数据,开发了一个数学模型.
- 应用了恒定的石流入和冰川流速的假设.
- 进行了计算,以确定石流入和冰暴露年龄.
主要成果:
- 该模型估计石流入量为60 x 10^-6 kg/km^2/年.
- 艾伦山附近露出冰的年龄在0到60万年之间.
- 结果与流入和石陆地年龄的独立估计一致.
结论:
- 这些发现支持了该地区恒定状态石流入和冰川流动的假设.
- 这项研究提供了可能是发现的最古老的连续分层冰序列的证据.
- 在这个地区的东南极冰盖可能在很长一段时间内保持稳定.
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