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液核自由运动的变分方法
引用本文:徐建桥,孙和平,傅容珊. 液核自由运动的变分方法[J]. 地球物理学报, 2004, 47(1): 61-74
作者姓名:徐建桥  孙和平  傅容珊
作者单位:中国科学技术大学地球和空间科学学院,合肥,230026;中国科学院测量与地球物理研究所动力大地测量学重点开放实验室,武汉,430077;中国科学院测量与地球物理研究所动力大地测量学重点开放实验室,武汉,430077;中国科学技术大学地球和空间科学学院,合肥,230026
基金项目:中国科学院知识创新项目 (KZCX3 SW 13 1),国家自然科学基金(4 0 1740 2 2 )
摘    要:从流体静力平衡地球的弹性-引力运动动量方程出发,以角动 量方程控制弹性地幔、液态外核和弹性内核之间的相对转动,在球对称近似下考虑了地幔和 内核对液核边界扰动的形变响应,并以此作为液核边界运动的约束条件.根据地球简正模对 称性的一般特征,建立了自转、非黏性、椭球分层流体外核自由振荡运动的变分原理并给出 了相应的泛函.

关 键 词:流体静力平衡  液核自由振荡  变分原理  泛函
文章编号:0001-5733(2004)01-0061-14
收稿时间:2002-12-11
修稿时间:2003-09-18

Variational Approach to Free Motion in the Earth's Fluid Outer Core
XU Jian Qiao , SUN He Ping FU Rong Shan College of Earth and Space Sciences,University of Science and Technology of China,Hefei ,China Key Laboratory of Dynamic Geodesy. Variational Approach to Free Motion in the Earth's Fluid Outer Core[J]. Chinese Journal of Geophysics, 2004, 47(1): 61-74
Authors:XU Jian Qiao    SUN He Ping FU Rong Shan College of Earth  Space Sciences  University of Science  Technology of China  Hefei   China Key Laboratory of Dynamic Geodesy
Affiliation:1.College of Earth and Space Sciences, University of Science an d Technology of China, Hefei 230026, China 2 Key Laboratory of Dynamic Geodesy, Institute of Geodesy and Geophysics, Chines e Academy of Sciences, Wuhan 430077, China
Abstract:This study is based on the elasto gravita t ional motion equations for a hydrostatic equilibrium Earth. The relative rotatio n among the solid elastic mantle, the fluid outer core and the solid elastic inn er core is governed by the angular momentum equation. The deformation response o f the mantle and inner core to the core dynamics, generated by the perturbations on the boundaries of the fluid outer core, is considered on the assumption of t he spherical symmetry. This response is employed to constrain the movement on th e boundaries of the fluid outer core. Based on the general symmetrical character istics of the Earth’s eigenmodes, the variational principle of free oscillation s in a rotating, inviscid and elliptically stratified fluid outer core is develo ped and the corresponding functional is deduced.
Keywords:Hydrostatic equilibrium   Free oscillations in the fluid outer core   Variational principle  Functional
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