• ISSN 2097-1893
  • CN 10-1855/P

地核的热输运性质与地核对流的驱动机制

张友君

引用本文: 张友君. 2023. 地核的热输运性质与地核对流的驱动机制. 地球与行星物理论评(中英文),54(1):100-101
Zhang Y J. 2023. Thermal transport property of the Earth's core and its convection. Reviews of Geophysics and Planetary Physics, 54(1): 100-101 (in Chinese)

地核的热输运性质与地核对流的驱动机制

doi: 10.19975/j.dqyxx.2022-035
基金项目: 国家自然科学基金资助项目(42074098)
详细信息
    通讯作者:

    张友君(1986-),男,研究员,主要从事高压物理与高压矿物物理研究. E-mail: zhangyoujun@scu.edu.cn

  • 中图分类号: P315

Thermal transport property of the Earth's core and its convection

Funds: Supported by the National Natural Science Foundation of China (Grant No. 42074098)
  • 图  1  地核的热流量、热分层以及对流示意图. 地核顶部的亚绝热环境可造成地核的热分层,该热分层会抑制热对流的产生并影响地震波的波速

    Figure  1.  Schematic of the heat flux, thermal stratification, and convection in Earth's core. A subadabatic temperature gradient at the top of the outer core may inhibit its thermal convection and change the seismic wave velocity

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出版历程
  • 收稿日期:  2022-04-18
  • 录用日期:  2022-04-19
  • 网络出版日期:  2022-04-24
  • 刊出日期:  2023-01-01

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