概括
地震波可能会激发地球的地磁力发电机. 地震活动可能会产生足够强大的流体运动,以影响磁场,每17万年发生一次大冲击.
科学领域:
- 地质物理学 地质物理学
- 地球科学 地球科学 地球科学
- 动力机理论 动力机理论
背景情况:
- 地球的地磁场是由地磁场产生的.
- 驱动地力发动机的精确机制和能源尚未完全理解.
研究的目的:
- 提出一种用于激活地磁力发电机的新机制.
- 研究地震波在地震和动力发电机过程中的潜在作用.
主要方法:
- 由地震波产生的流体运动的理论建模.
- 在地震波运动和地磁场之间进行能量均分分析.
主要成果:
- 地震产生的流体运动拥有足够的能量,可以与高达100高斯的地磁场相匹配.
- 来自大型石撞击的地震波可能拥有足够的能量来逆转地磁场.
结论:
- 地震波能量代表了一个可能的,尽管间歇性的,地磁力发电机活动的来源.
- 大规模冲击可能会在地质时间尺度上引发地磁场逆转.
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