概括
强烈的局部加热发生在地球的地幔下降的寒板和撞击羽毛. 这种粘性加热明显超过内部放射性衰变,影响地幔动态.
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
- 计算地力学计算地力学
背景情况:
- 地球地幔的对流是由传热和物质流动驱动的.
- 温度依赖的粘度和粘性加热是地幔动态中的关键因素.
- 需要逼真的雷利数来准确模拟地幔对流.
研究的目的:
- 为了研究三维地幔对流的局部加热.
- 在降落的冷板和撞击羽毛的区域量化粘性加热.
- 为了比较粘性加热与内部放射性加热.
主要方法:
- 三维对流的数值模拟.
- 包括温度依赖的粘度和粘性加热.
- 用现实的雷利数来计算地球地幔.
主要成果:
- 在下降的冷板的顶部观察到强烈的局部加热.
- 显著的局部加热发生在上升的羽毛头撞击表面的地方.
- 对于粘度对比度为100,局部热源>10x大于内部放射性加热.
结论:
- 粘性消散是地幔特定区域的主要热源.
- 局部加热显著影响地幔动力学,特别是在上层地幔.
- 在上层的粘性消散的度相当于放射性加热.
相关概念视频
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