Modeling a mechanism of MHD turbulent diffusion in Earth and Planetary fluid cores

模拟地球和行星流体核心 MHD 湍流扩散机制

基本信息

  • 批准号:
    15540405
  • 负责人:
  • 金额:
    $ 2.37万
  • 依托单位:
  • 依托单位国家:
    日本
  • 项目类别:
    Grant-in-Aid for Scientific Research (C)
  • 财政年份:
    2003
  • 资助国家:
    日本
  • 起止时间:
    2003 至 2005
  • 项目状态:
    已结题

项目摘要

Aiming at modeling an eddy diffusivity tensor, we have performed direct numerical simulations of MHD turbulence in a rapidly rotating system. To carry out computation using molecular diffusivity in a realistic planetary core, required is high resolution even for a very small region in the core. In the present research, the computational region is divided into several segments, which are allocated to respective CPUs on a parallel computer with large size of memory. Using results of direct numerical simulations thus obtained, we have examined scale similarity in MHD turbulence to model subgrid-scale physical processes, and we have found that scale similarity holds. On the basis of scale similarity law as well as spatial-filter width dependence, we have estimated the effect of subgrid-scales on grid-scales. We have then carried out large eddy simulations of MHD turbulence with the model of subgrid-scales. We have compared their results with those of direct numerical simulations, and confirmed that the present subgrid-scale model holds valid. That is, heat flux, kinetic energy, and magnetic energy averaged over computational time and computational region for large eddy simulation with the subgrid-scale model are closer to those for direct numerical simulations than those for numerical simulations without the model. It should be noted, however, that there is no significant difference among power spectra for velocity field, magnetic field, and temperature.
针对涡扩散系数张量模型,我们对快速旋转系统中的MHD湍流进行了直接数值模拟。为了在一个现实的行星核中使用分子扩散率进行计算,即使对于核中非常小的区域,也需要高分辨率。在本研究中,计算区域被划分为几个部分,这是分配给各自的CPU上的并行计算机与大容量的内存。利用直接数值模拟的结果,从而获得,我们已经检查了MHD湍流模型亚网格尺度的物理过程的尺度相似性,我们已经发现,尺度相似性持有。基于尺度相似律和空间滤波器宽度依赖性,我们估计了子网格尺度对网格尺度的影响。然后,我们进行了大涡模拟的MHD湍流的亚网格尺度模型。我们将它们的结果与直接数值模拟的结果进行了比较,证实了本亚网格模型的有效性。也就是说,在计算时间和计算区域上平均的热通量,动能和磁能的大涡模拟与亚网格尺度模型更接近直接数值模拟比那些没有模型的数值模拟。然而,应该注意的是,速度场、磁场和温度的功率谱之间没有显著差异。

项目成果

期刊论文数量(36)
专著数量(0)
科研奖励数量(0)
会议论文数量(0)
专利数量(0)
Dynamo action in rotating spherical shell at high Rayleigh numbers
高瑞利数旋转球壳中的发电机作用
  • DOI:
  • 发表时间:
    2005
  • 期刊:
  • 影响因子:
    0
  • 作者:
    F.Takahashi;M.Matsushima
  • 通讯作者:
    M.Matsushima
A scale-similarity model of the subgrid-scale flux with application to MHD turbulence in the Earth's core
应用于地核 MHD 湍流的亚网格尺度通量的尺度相似模型
Simulations of a QuasiTaylor State Geomagnetic Field Including Polarity Reversals on the Earth Simulator
  • DOI:
    10.1126/science.1111831
  • 发表时间:
    2005-07
  • 期刊:
  • 影响因子:
    56.9
  • 作者:
    F. Takahashi;M. Matsushima;Y. Honkura
  • 通讯作者:
    F. Takahashi;M. Matsushima;Y. Honkura
地球磁場から推定されるコアの流体運動
根据地球磁场估计的核心流体运动
  • DOI:
  • 发表时间:
    2005
  • 期刊:
  • 影响因子:
    0
  • 作者:
    F.Takahashi;M.Matyushima;Y.Honkura;松島政貴
  • 通讯作者:
    松島政貴
Fluid motion in the core estimated from the Earth's magnetic field
根据地球磁场估计地核中的流体运动
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MATSUSHIMA Masaki其他文献

MATSUSHIMA Masaki的其他文献

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{{ truncateString('MATSUSHIMA Masaki', 18)}}的其他基金

Generation of electromagnetic field due to resonance between ground velocity and ions motion in the Earth's magnetic field
由于地面速度和地球磁场中离子运动之间的共振而产生电磁场
  • 批准号:
    21340126
  • 财政年份:
    2009
  • 资助金额:
    $ 2.37万
  • 项目类别:
    Grant-in-Aid for Scientific Research (B)
Effects of anisotropic turbulent transport on generation mechanism of the Earth's magnetic field
各向异性湍流输运对地球磁场产生机制的影响
  • 批准号:
    11640412
  • 财政年份:
    1999
  • 资助金额:
    $ 2.37万
  • 项目类别:
    Grant-in-Aid for Scientific Research (C)
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