测绘学报 ›› 2017, Vol. 46 ›› Issue (10): 1290-1299.doi: 10.11947/j.AGCS.2017.20170298

• 大地测量学与导航 • 上一篇    下一篇

重力场的地球动力学与内部结构应用研究进展

孙和平1,2, 徐建桥1, 崔小明1   

  1. 1. 中国科学院测量与地球物理研究所大地测量与地球动力学国家重点实验室, 湖北 武汉 430077;
    2. 中国科学院大学, 北京 100049
  • 收稿日期:2017-06-07 修回日期:2017-08-29 出版日期:2017-10-20 发布日期:2017-10-26
  • 作者简介:孙和平(1955-),男,博士,研究员,研究方向为地球重力场理论、资料处理和地球动力学应用解释等。E-mail:heping@asch.whigg.ac.cn
  • 基金资助:
    国家自然科学基金(41621091;41674083);中国科学院基金(Y504191019)

Research Progress of the Gravity Field Application in Earth's Geodynamics and Interior Structure

SUN Heping1,2, XU Jianqiao1, CUI Xiaoming1   

  1. 1. State Key Laboratory of Geodesy and Earth's Dynamics, Institute of Geodesy and Geophysics, CAS, Wuhan 430077, China;
    2. University of Chinese Academy of Sciences, Beijing 100049, China
  • Received:2017-06-07 Revised:2017-08-29 Online:2017-10-20 Published:2017-10-26
  • Supported by:
    The National Natural Science Foundation of China (Nos. 41621091;41674083);Science Foundation of the Chinese Academy of Sciences (No. Y504191019)

摘要: 深入认识地球深内部结构和内部动力学问题一直是基础地球科学研究领域的前沿热点,传统方法主要依赖于地震技术。近几十年来,随着新兴的现代重力观测技术革新(尤其是高精度超导重力技术的成功应用),使得检测地球内部动力学现象和物性信息成为可能。本文简述了我国在本领域近年来利用现代高精度重力技术在检测地球自由振荡、自由核章动、内核平动振荡、潮汐模型与极潮和内部结构方面的研究成果进展。

关键词: 重力潮汐变化, 地球自由振荡, 自由核章动, 内核平动振荡

Abstract: The exploration of deep internal structure and internal dynamics of the earth has always been a hot topic in the field of basic geoscience research.Traditional approach relies mainly on seismic technology. However, in recent decades, the innovation of modern gravity observation technology (especially the successful application of high-precision superconducting gravity technology) makes it possible to detect the earth's internal dynamics and physical information. In this paper, we summarize the research progress of Chinese group in detecting the earth's free oscillation, free core nutation, inner core translational oscillation, tidal model and polar tide and the internal structure by using modern high-precision gravity technology in recent years.

Key words: gravity tide variation, free oscillation, free core nutation, inner core translational oscillation

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