火星表面的重力曲线表明盖尔火山口的岩层密度较低
Kevin W Lewis1, Stephen Peters2, Kurt Gonter2
1Earth and Planetary Sciences Department, Johns Hopkins University, Baltimore, MD 21218, USA. klewis@jhu.edu.
概括
好奇号探测器
科学领域:
- 星球科学
- 地质学
- 火星的探索
背景情况:
- 重力测量精确地测量引力场,帮助研究行星的内部结构.
- 火星上的好奇号探测器有加速计用于导航和定位.
研究的目的:
- 要重新校准好奇号的加速度计, 以测量引力加速的变化.
- 使用重力测量推断盖尔坑的地下岩石密度.
主要方法:
- 探测器加速器的重新校准以检测引力场的变化.
- 测量火星上升过程中的重力场强度与高度的下降.
主要成果:
- 盖尔火山口的沉积岩石的密度为1680±180kg/m3.
- 这种密度低于预期,
结论:
- 推断的低岩石密度表明盖尔坑的沉积岩石具有显著的多孔性.
- 这一发现限制了这些火星岩石的最大历史埋葬深度.
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