Three-dimensional MHD dynamo simulation

三维 MHD 发电机模拟

基本信息

  • 批准号:
    10640404
  • 负责人:
  • 金额:
    $ 1.98万
  • 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:
    1998
  • 资助国家:
    日本
  • 起止时间:
    1998 至 2000
  • 项目状态:
    已结题

项目摘要

Aiming at solving a dynamo problem as a mechanism of the origin of Earth and planetary magnetism, we have performed three-dimensional MHD dynamo simulation. So far, we have found that boundary layers develop depending on the Ekman number and in the layer small-scale phenomena are dominant, when a non-slip boundary condition is given to the velocity field. Therefore, we must evaluate the effect of boundary layers if we want to obtain reliable results of MHD dynamo simulation. In 1998 and 1999, we developed a new computer code for dynamo simulation and compared its results with those derived from our previous code and showed that our new code is valid. Then we modified this code so as to cope with parallel computing. In 2000, we have participated the dynamo benchmark test as an international group attempt. As a result, our results were found to agree with the others and therefore our computer code is as effective as the other codes developed by oversea researchers. From our results, we could find that crude spatial resolution in the radial direction greatly affects the drift rate of the velocity filed pattern. In other words, it is the most important to assure enough resolution in the boundary layers when we examine the results of numerical computation. A hypothetical cylinder, which is tangent to the inner core at its equator and parallel to the rotation axis, is called a tangent cylinder, which is also a boundary layer. The effect of this layer becomes prominent for the non-slip boundary condition. Inside the tangent cylinder, the flow is not violent when the Rayleigh number is small, but for a high Rayleigh number, convective motion becomes active, Such a feature has a great influence on the mechanism of magnetic field creation and variation. As a future work, we should try to under stand the dependence of the Rayleigh number on dynamics inside the tangent cylinder
针对作为地球和行星磁性起源机制的发电机问题,我们进行了三维MHD发电机模拟。到目前为止,我们已经发现,边界层的发展取决于Ekman数和层中的小尺度现象是占主导地位的,当无滑移边界条件的速度场。因此,要获得可靠的磁流体发电机模拟结果,就必须考虑边界层的影响。在1998年和1999年,我们开发了一个新的计算机程序的发电机模拟和比较其结果来自我们以前的代码,表明我们的新代码是有效的。然后,我们修改了这个代码,以科普并行计算。2000年,我们作为国际团体尝试参加了发电机基准测试。结果表明,我们的计算结果与其他人的计算结果一致,因此我们的计算机程序与国外研究人员开发的其他程序一样有效。结果表明,径向粗空间分辨率对速度场的漂移率有很大的影响。换句话说,当我们检验数值计算的结果时,保证边界层有足够的分辨率是最重要的。一个假设的圆柱体,在赤道处与内核相切,并平行于旋转轴,称为切向圆柱体,它也是边界层。在无滑移边界条件下,这一层的影响变得突出。在切向圆柱内部,当Rayleigh数较小时,流动并不剧烈,但当Rayleigh数较高时,对流运动变得活跃,这一特征对磁场的产生和变化机制有很大影响。作为未来的工作,我们应该尝试理解瑞利数对切向圆柱内部动力学的依赖性

项目成果

期刊论文数量(12)
专著数量(0)
科研奖励数量(0)
会议论文数量(0)
专利数量(0)
J.S.Katayama,M.Matsushima, and Y.Honkura: "Some characteristics of magnetic field behavior in a model of MHD dynamo Thermally driven in a rotating spherical shell"Physics of the Earth and Planetary Interiors. 111. 141-159 (1999)
J.S.Katayama、M.Matsushima 和 Y.Honkura:“旋转球壳热驱动 MHD 发电机模型中磁场行为的一些特征”地球和行星内部物理学。
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    0
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J.S.Katayama,F,Takahashi,M.Matsushima,and Y.Honkura: "Effects of boundary conditions on magnetic field behavior in a model of MHD dynamo thermally driven in a rotating spherical shell"The 7^<th> Symposium : Study of the Earth's Deep Interior. 133 (2000)
J.S.Katayama、F、Takahashi、M.Matsushima 和 Y.Honkura:“边界条件对旋转球壳热驱动 MHD 发电机模型中磁场行为的影响”第 7 届研讨会:研究
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J.S.Katayama, F.Takahashi, M.Matsushima, and Y.Honkura: "Effects of boundary conditions on magnetic field behavior in a model of MHD dynamo thermally driven in a rotating spherical shell"The 7^<th> Symposium : Study of the Earth's Deep Interior. 133. (200
J.S.Katayama、F.Takahashi、M.Matsushima 和 Y.Honkura:“边界条件对旋转球壳热驱动 MHD 发电机模型中磁场行为的影响”第 7 届研讨会:研究
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J.S.Katayama,M.Matsushima,and Y.Honkura: "The effect of boundary layers on geodynamo processes"International Workshop on Solid Earth Simulater and ACES WG Meeting. (2000)
J.S.Katayama、M.Matsushima 和 Y.Honkura:“边界层对地球发电机过程的影响”固体地球模拟器国际研讨会和 ACES 工作组会议。
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J.S.Katayama,M.Matsushima and Y.Honkura: "Some characteristics of magnetic field behavior in a model of MHD dynamo thermally driven in a rotating spherical shell"Phys. Earth Planet. Interiors. 111. 141-159 (1999)
J.S.Katayama、M.Matsushima 和 Y.Honkura:“旋转球壳中热驱动 MHD 发电机模型中磁场行为的一些特征”Phys。
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HONKURA Yoshimori其他文献

HONKURA Yoshimori的其他文献

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{{ truncateString('HONKURA Yoshimori', 18)}}的其他基金

Understanding of a Mechanism of Geomagnetic Field Reversals by Highly Precise Numerical Simulations of the Geodynamo
通过地球发电机的高精度数值模拟了解地磁场反转的机制
  • 批准号:
    18340131
  • 财政年份:
    2006
  • 资助金额:
    $ 1.98万
  • 项目类别:
    Grant-in-Aid for Scientific Research (B)
STUDY OF THE EVALUATION OF EARTHQUAKE OCCURRENCE POTENTIAL IN THE WESTERN PART OF THE NORTH ANATOLIAN FAULT ZONE
北安纳托利亚断层带西部地区地震发生潜力评价研究
  • 批准号:
    13373002
  • 财政年份:
    2001
  • 资助金额:
    $ 1.98万
  • 项目类别:
    Grant-in-Aid for Scientific Research (A)
Research on the deep structure of active faults in the North Anatolian fault zone, Turkey
土耳其北安纳托利亚断裂带活动断裂深部结构研究
  • 批准号:
    11694063
  • 财政年份:
    1999
  • 资助金额:
    $ 1.98万
  • 项目类别:
    Grant-in-Aid for Scientific Research (B).
Research on Fault Activity in the North Anatolian Fault Zone
北安纳托利亚断裂带断裂活动研究
  • 批准号:
    04041046
  • 财政年份:
    1992
  • 资助金额:
    $ 1.98万
  • 项目类别:
    Grant-in-Aid for international Scientific Research
Multidisciplinary Research on Fault Activity in the Western Part of the North Anatolian Fault Zone (The Second Phase)
北安纳托利亚断裂带西部断裂活动性多学科研究(第二期)
  • 批准号:
    63041054
  • 财政年份:
    1988
  • 资助金额:
    $ 1.98万
  • 项目类别:
    Grant-in-Aid for Overseas Scientific Survey.
MULTIDISCIPLINARY RESEARCH ON FAULT ACTIVITY IN THE WESTERN PART OF THE NORTH ANATOLIAN FAULT ZONE
北安纳托利亚断层带西部断层活动的多学科研究
  • 批准号:
    62043026
  • 财政年份:
    1986
  • 资助金额:
    $ 1.98万
  • 项目类别:
    Grant-in-Aid for Overseas Scientific Research
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