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Titlebook: Geophysical Interpretation using Integral Equations; L. Eskola Book 1992 L. Eskola 1992 DEX.Integral equation.Mathematica.Volume.boundary

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书目名称Geophysical Interpretation using Integral Equations
编辑L. Eskola
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图书封面Titlebook: Geophysical Interpretation using Integral Equations;  L. Eskola Book 1992 L. Eskola 1992 DEX.Integral equation.Mathematica.Volume.boundary
描述Along with the general development of numerical methods in pure and applied to apply integral equations to geophysical modelling has sciences, the ability improved considerably within the last thirty years or so. This is due to the successful derivation of integral equations that are applicable to the modelling of complex structures, and efficient numerical algorithms for their solution. A significant stimulus for this development has been the advent of fast digital computers. The purpose of this book is to give an idea of the principles by which boundary-value problems describing geophysical models can be converted into integral equations. The end results are the integral formulas and integral equations that form the theoretical framework for practical applications. The details of mathematical analysis have been kept to a minimum. Numerical algorithms are discussed only in connection with some illustrative examples involving well-documented numerical modelling results. The reader is assu­ med to have a background in the fundamental field theories that form the basis for various geophysical methods, such as potential theory, electromagnetic theory, and elastic strain theory. A fair
出版日期Book 1992
关键词DEX; Integral equation; Mathematica; Volume; boundary element method; distribution; equation; form; integral
版次1
doihttps://doi.org/10.1007/978-94-011-2370-9
isbn_softcover978-94-010-5045-6
isbn_ebook978-94-011-2370-9
copyrightL. Eskola 1992
The information of publication is updating

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Elements of magnetostatics,roblem, in the absence of currents, is formally analogous to the electrical field problem. Owing to this analogy, the sources of anomalous magnetic fields can be represented by magnetic pole distributions. Since physically real magnetic monopoles have not been found, they should be regarded merely a
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Wilhelm Anton Fischer,Gerhard Pateiskyroblem, in the absence of currents, is formally analogous to the electrical field problem. Owing to this analogy, the sources of anomalous magnetic fields can be represented by magnetic pole distributions. Since physically real magnetic monopoles have not been found, they should be regarded merely a
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Anwendung der Elektrochirurgie am Auge,is conducted by gene rating a seismic disturbance in the earth and then recording the transmitted scattered waves with aseries of geophones. The disturbance propagates from the source point into the surrounding medium as two isolated wave modes, namely . (P) and . (S) waves that expand with characte
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