对惠更斯原理的多重思考

IF 1.8 3区 地球科学 Q3 GEOCHEMISTRY & GEOPHYSICS
Kees Wapenaar
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引用次数: 0

摘要

根据惠更斯原理,波前的所有点都是发射球形波的次级源,这些球形波的包络层形成一个新的波前。在惠更斯原理的数学公式中,二次源发射的波用格林函数表示。在惠更斯原理的许多现代应用中,这些格林函数被它们的时间反转版本所取代,从而形成了反向传播、成像、反演、地震干涉测量等的基础。然而,当输入波场仅在单一开放边界上可用时,这种方法有其局限性。特别是,它不能很好地解释多次反射波。这被惠更斯原理的一种修正形式所弥补,其中格林函数被聚焦函数所取代。修正后的惠更斯原理为成像、逆散射、感应源监测等奠定了基础,从而适当地考虑了多重反射波。
本文章由计算机程序翻译,如有差异,请以英文原文为准。

Multiple Reflections on Huygens' Principle

Multiple Reflections on Huygens' Principle

According to Huygens' principle, all points on a wave front act as secondary sources emitting spherical waves and the envelope of these spherical waves forms a new wave front. In the mathematical formulation of Huygens' principle, the waves emitted by the secondary sources are represented by Green's functions. In many present-day applications of Huygens' principle, these Green's functions are replaced by their time-reversed versions, thus forming a basis for backpropagation, imaging, inversion, seismic interferometry, etc. However, when the input wave field is available only on a single open boundary, this approach has its limitations. In particular, it does not properly account for multiply reflected waves. This is remedied by a modified form of Huygens' principle, in which the Green's functions are replaced by focusing functions. The modified Huygens' principle forms a basis for imaging, inverse scattering, monitoring of induced sources, etc., thereby properly taking multiply reflected waves into account.

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来源期刊
Geophysical Prospecting
Geophysical Prospecting 地学-地球化学与地球物理
CiteScore
4.90
自引率
11.50%
发文量
118
审稿时长
4.5 months
期刊介绍: Geophysical Prospecting publishes the best in primary research on the science of geophysics as it applies to the exploration, evaluation and extraction of earth resources. Drawing heavily on contributions from researchers in the oil and mineral exploration industries, the journal has a very practical slant. Although the journal provides a valuable forum for communication among workers in these fields, it is also ideally suited to researchers in academic geophysics.
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