火星的流体核心大小从太阳潮的检测
C F Yoder1, A S Konopliv, D N Yuan
1Jet Propulsion Laboratory, California Institute of Technology, Pasadena, CA 91109, USA. Charles.F.Yoder@jpl.nasa.gov
概括
火星 火星 火星 火星 火星
科学领域:
- 行星科学 行星科学
- 地质物理学 地质物理学
- 天文学 天文学
背景情况:
- 了解火星的内部结构是其地质演变的关键.
- 以前的模型建议固体铁芯,但新的数据提供了更精细的见解.
- 星球的潮变形为其核心组成提供了关键的线索.
研究的目的:
- 用太阳潮变形来确定火星核心 (液体或固体) 的状态.
- 为了改进火星核心半径的估计.
- 分析季节性冰盖质量变化及其对重力波的影响.
主要方法:
- 分析火星全球测量仪 (MGS) 无线电跟踪数据.
- 测量k2潜在的爱数量化潮变形.
- 从气压的季节性变化和J3重力调中减去冰盖质量变化.
主要成果:
- 观察到的k2 Love数 (0.153 +/- 0.017) 表明有液态外核,排除了固体铁核.
- 推断火星核心半径范围从1520公里到1840公里.
- 南极冰盖的季节性质量变化比北极冰盖大30-40%.
结论:
- 火星拥有液态外核,显著影响其地力学.
- 推断的核心大小为行星形成模型提供了关键的约束.
- 不对称的冰盖动态在火星的季节性重力场变化中起着可衡量的作用.
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