地球液核动力学效应的研究和检测(英文)

Study and Detection on the Geodynamic Effects of the Earth's Fluid Outer Core

综合分析处理了包括武汉台在内的全球地球动力学(GGP)台站超导重力仪长期、连续重力观测资料,研究和检测了地球液核的动力学效应。系统讨论了在日月引潮力、表面负荷和液核动力学行为引起的核幔边界及内核边界上,压力和重力扰动等不同驱动力作用下,地球的弹性引力形变响应.基于周日重力潮汐观测中的共振放大特征,通过国际超导重力仪观测资料的迭积,研究了地球的自由和章动(FCN),精密确定了FCN参数.采用位移场的变分方法研究了液核的自由振荡,严密推导获得了用于有限元数值计算的本征值 本征向量问题.同时采用GGP台站超导重力仪长期、连续、高质量重力观测数据。

The long-term, continuous gravity data, recorded with superconducting gravimeters (SCG) at the Global Geodynamics Project (GGP) observatories including one at Wuhan, and the corresponding station atmospheric pressure records have been comprehensively processed and analyzed in order to study and detect the geodynamical effects of the Earth's fluid outer core (FOC). The elasto-gravitational deformation responses of the Earth to thesolar-luni tidal forces, surface tractions and 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 FOC, are systematically discussed. Based on the resonance enhancement in diurnal tidal gravity observations, the Earth's free core nutation (FCN) is studied by stacking the tidal gravity data obtained with the international SCG. As a result, the FCN parameters are determined accurately. The free oscillations of the FOC are theoretically investigated by using a variational approach of the displacement field. And the corresponding eigenvalue-eigenvector problem for the finite element computation is deduced. By simultaneouslyusing the long-term, continuous and high-quality gravity data observed with the SCG at the GGP observatories, the translational oscillations of the solid inner core is studied.