月球南极内部缺乏露出冰的沙克尔顿火山口
Junichi Haruyama1, Makiko Ohtake, Tsuneo Matsunaga
1Institute of Space and Astronautical Science, Japan Aerospace Exploration Agency, Sagamihara, Kanagawa 229-85105, Japan.
概括
沙克尔顿火山口可能有水冰,但成像显示地板上没有纯冰沉积物. 需要进一步分析以确认冰是否与土壤混合或不存在.
科学领域:
- 月球科学 月球科学
- 行星地质学 行星地质学
- 天体生物学 天体生物学
背景情况:
- 在月球南极的沙克尔顿火山口是永久的阴影.
- 以前的研究推断了火山口内存在水冰沉积物的存在.
研究的目的:
- 为了拍摄沙克尔顿火山口的内部图像.
- 评估水冰沉积物的存在和形式.
主要方法:
- 在Selenological and Engineering Explorer (SELENE) 航天器上使用了地形摄像头 (TC).
- 从TC立体数据开发了一个石坑形状模型.
- 分析了石坑底的白色和估计的温度.
主要成果:
- 成功拍摄了昏暗的火山口内部的图像.
- 估计火山口的地板温度低于90克尔文,适合水冰.
- TC的空间分辨率的白度数据表明没有暴露的纯水冰沉积物.
结论:
- 虽然条件足够冷以形成冰,但在目前的分辨率下没有发现纯水冰的直接证据.
- 水冰可能分布在 regolith内或不在石坑底.
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