概括
超声波测量显示,月球岩石的速度随着压力显著增加,与地震数据相匹配. 月球样本在低压下显示出高衰减,表明复杂的地震波行为.
科学领域:
- 地质物理学 地质物理学
- 行星科学 行星科学
- 地震学 地震学
背景情况:
- 了解月球地震波传播对于描述月球内部结构至关重要.
- 以前的阿波罗任务的地震数据提供了有限的关于不同压力下的材料特性信息.
研究的目的:
- 在受控压力条件下测量阿波罗11号月球样本中的P和S波速度和衰减.
- 为了比较实验室衍生的速度-深度概况与阿波罗任务的现场地震观测.
主要方法:
- 超声波脉冲传输用于确定P (压缩) 和S (剪切) 波速.
- 对月球样本 (10020,10057,10065) 在室温高达5千巴的温度进行测量.
- 质量因子 (Q),表示衰减,在压力低于200bar时进行评估.
主要成果:
- 月球样本速度与压力显著增加 (高达两倍),特别是在前2千巴里内.
- 从样本10057的速度-深度曲线预测的旅行时间与阿波罗12号地震实验结果保持一致.
- 在低于200bar的压力下,样品显示出高衰减,P波和S波的Q值约为10.
结论:
- 月球的地震波速度对压力非常敏感,特别是在浅水深处.
- 实验室超声波测量为解释月球地震实验和了解月球浅层地下提供了有价值的数据.
- 在低压下高衰减表明月球 regolith 内的多孔或断裂区域.
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