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液核动力学扰动引起的地球形变
引用本文:徐建桥,孙和平.液核动力学扰动引起的地球形变[J].地震学报,2002,24(4):397-406.
作者姓名:徐建桥  孙和平
作者单位:(中国武汉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)
基金项目:国家自然科学基金项目(40174022,49925411),中国科学院项目(KZ9S2-J1-411,KZ952-J1-411)联合资助.
摘    要:讨论了地球固体部分对液核动力学效应引发的核幔边界和内核边界上压力和引力扰动的形变响应.采用弹性-引力形变理论描述地幔和内核的形变,给出了内部负荷Love数的一般表达式.以初始参考地球模型为例,分别计算了在地球表面、核幔边界和内核边界上的内部负荷Love数.探讨了液核边界上压力和引力扰动导致的地球形变场的空间和频率分布特征.本文的结果可以为中短周期液核动力学理论模拟提供必要的边界条件. 

关 键 词:&    液核动力学效应&    液核边界&    内部负荷Love数&    地球的形变场&    边界条件
文章编号:0253-3782(2002)04-0397-10
修稿时间:2001年10月24

EARTH(S DEFORMATION DUE TO THE DYNAMICAL PERTURBATIONS OF THE FLUID OUTER CORE
Xu Jianqiao,Sun Heping.EARTH(S DEFORMATION DUE TO THE DYNAMICAL PERTURBATIONS OF THE FLUID OUTER CORE[J].Acta Seismologica Sinica,2002,24(4):397-406.
Authors:Xu Jianqiao  Sun Heping
Abstract:The elasto-gravitational deformation response of the Earths solid parts to the perturbations of the pressure and gravity on the core-mantle boundary (CMB) and the solid inner core boundary (ICB), due to the dynamical behaviors of the fluid outer core (FOC), is discussed. The internal load Love numbers, which are formulized in a general form in this study, are employed to describe the Earths deformation. The Preliminary reference Earth model (PREM) (Dziewonski, Anderson, 1981) is used as an example to calculate the internal load Love numbers on the Earths surface, CMB and ICB, respectively. The characteristics of the Earths deformation variation with the depth and the perturbation periods on the boundaries of the FOC are investigated also. The numerical results indicate that the internal load Love numbers decrease quickly with the increasing degree of the spherical harmonics of the displacement and depend strongly on the perturbation frequencies, especially on the high frequencies. The results, obtained in this work, can be used to construct the boundary conditions for the core dynamics of the long-period oscillations of the Earths fluid outer core.
Keywords:the dynamical effects of the fluid outer core  boundaries of the fluid outer core  the internal load Love numbers  the Earths deformation field  boundary conditions  
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