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强烈的对流解释了冥王星的多边形地形
A J Trowbridge1, H J Melosh1,2, J K Steckloff2
1Department of Earth, Atmospheric, and Planetary Sciences, Purdue University, West Lafayette, Indiana 47907, USA.
Nature
|June 3, 2016
概括
冥王星的Sputnik Planum有 (N2) 冰的多边形. 在N2冰层内的对流流是最有可能的原因,
科学领域:
- 星球科学
- 地质学
- 化学
背景情况:
- 冥王星的Sputnik Planum呈现出独特的多边形地形,主要由 (N2) 冰组成.
- 之前关于多边形形成的假设,如热收缩,与观察到的N2冰变形不一致.
研究的目的:
- 在冥王星的斯普特尼克平面上形成多边形地形的地质过程.
- 确定解释观察到的表面特征和N2冰的最合理的机制.
主要方法:
- 一个参数化的对流模型的开发和应用.
- 对 (N2) 冰层的雷利数的计算.
- 分析多边形尺寸和"浮山"以推断冰厚.
主要成果:
- 计算的雷利数表明N2冰中的强烈对流.
- 雷利-贝纳德对流被认为是多边形形成的最可能的机制.
- 据估计N2冰层厚度约为10公里.
结论:
- 冥王星的Sputnik Planum在地质上非常活跃,
- 估计的对流速度表明表面年龄非常年轻,大约100万年.
- 这一发现挑战了以前关于冰冷天体的地质不活动的假设.
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