Piezomagnetic field associated with the Mogi model revisited: analytic solution for finite spherical source

DOI 被引用文献5件 オープンアクセス

書誌事項

タイトル別名
  • Piezomagneti field associated with the Mogi model revisited: Analytic solution for finite spherical source.
  • Analytic Solution for Finite Spherical Source
公開日
1991
DOI
  • 10.5636/jgg.43.21
公開者
地球電磁気・地球惑星圏学会

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説明

The piezomagnetic field associated with the Mogi model was reexamined for the point source and the finite spherical source problems. In the point source case the question was how to deal with divergent stresses near the pressure source. In SASAI's (1979) method, the magnetized crust was divided into two layers, i.e. the upper half shallower than the source (0<z<D) and the lower half deeper than the source (D<z<H). The solution (type I) was simply the sum of the two contributions as calculated by the Fourier transform method. An alternative calculation (type II) integrates the whole magnetized area except for an infinitesimally small sphere involving the pressure source. This was achieved with the aid of a theorem for spherical harmonics. These two procedures gave different results. In order to identify the cause of the discrepancy, the finite source problem was further investigated. The piezomagnetic field was represented in the form of a one-dimensional integral containing complete elliptic integrals. It can be evaluated numerically with the aid of the double exponential formula (DEF). We called it the type III solution. The present analytic approach verifies the results of numerical 3-D integrations by DAVIS (1976), and SUZUKI and OSHIMAN (1990). The solution as the spherical radius diminishes to zero coincides with the type II solution. The type II solution had a gap across H=D. The potential value at H=D was just the average of the two limiting values for H=D-ε and H=D+ε. In the type I solution, the magnetization along a thin layer at H=D was ignored, which produced the pressure source term in the type II solution. Accordingly the type II solution was appropriate for the point source problem: the previous result by SASAI (1979) should be rejected.

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被引用文献 (5)*注記

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詳細情報 詳細情報について

  • CRID
    1390282681487828480
  • NII論文ID
    130003558853
  • DOI
    10.5636/jgg.43.21
  • ISSN
    21855765
    00221392
    http://id.crossref.org/issn/00221392
  • 本文言語コード
    en
  • データソース種別
    • JaLC
    • Crossref
    • CiNii Articles
    • OpenAIRE
  • 抄録ライセンスフラグ
    使用不可

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