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首页> 外文期刊>Journal of geophysical research. Solid earth: JGR >On the Mantle-Inner Core Gravitational Oscillation Under the Action of the Electromagnetic Coupling Effects
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On the Mantle-Inner Core Gravitational Oscillation Under the Action of the Electromagnetic Coupling Effects

机译:电磁耦合效应作用下的披风内核心重力振荡

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Previous works indicated that the eigenperiod of the mantle-inner core gravitational coupling mode can match the observed 6-year period in length-of-day. However, this mode is only an ideal model, since it does not involve the electromagnetic (EM) coupling effects. Here, we further study the mantle-inner core gravitational mode and its mathematical equation under the action of the EM coupling effects, while the relevant damping oscillation analytical solution is also given. According to this theoretical model, we can constrain the core-mantle gravitational coupling strength Gamma (>6.5 x 10(19) Nm) and infer the EM coupling information at the core-mantle boundary (CMB) and the inner core boundary. This work indicates that a partial liquid core is necessarily required to be coupled to the inner core (IC) and axially rotates with the IC as a single body, which supports the recent assumption that only a part fluid core within the so-called tangent cylinder is locked to the IC. This explanation can greatly weaken the perturbation magnetic field due to the shear oscillation at the inner core boundary and eliminate the relevant EM damping dissipation, otherwise, the predicted 6-year oscillation will be rapidly decayed with a relaxation time similar to 9.8 days. In addition, we give the physical expression of the theoretical quality factor Q value of the 6-year oscillation, which is mainly related to the EM coupling at the CMB. According to the typical EM coupling parameters at the CMB, the theoretical Q value is predicted in the range of 40-75, which coincides with the current observed result (similar to 51.6).
机译:以前的作品表明,地幔内核心重力耦合模式的特征化可以将观察到的6年期间与日期的长期相匹配。然而,这种模式只是理想的模型,因为它不涉及电磁(EM)耦合效应。在这里,我们进一步研究了Mantle内核心重力模式及其在EM耦合效应的作用下的数学方程,而还给出了相关阻尼振荡分析解决方案。根据该理论模型,我们可以限制核心地幔重力耦合强度伽马(> 6.5×10(19)Nm),并在核心地幔边界(CMB)和内核边界处推断EM耦合信息。该工作表明,部分液体芯必须耦合到内芯(IC)并用IC作为单个主体轴向旋转,这是最近仅仅是所谓的切线内的部件流体芯的假设被锁定到IC。由于内芯边界处的剪切振荡,这种解释可以大大削弱扰动磁场,并消除了相关的EM阻尼耗散,否则,预测的6年振荡将在类似于9.8天的放松时间迅速腐烂。此外,我们给出了6年振荡的理论质量因子Q值的物理表达,主要与CMB处的EM耦合有关。根据CMB处的典型EM耦合参数,理论Q值预测在40-75的范围内,这与当前观察结果相一致(类似于51.6)。

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