Broad band synthetic seismograms for a spherical inhomogeneity in a manylayered elastic halfspace
(1987) In Geophysical Journal International 89(2). p.527547 Abstract
 The propagation of elastic waves in a manylayered elastic halfspace is considered. One of the layers contains a bounded inhomogeneity which in the numerical applications is taken as a sphere. The halfspace is excited by an explosion, modelled as a sudden isotropic point source.
First the timeharmonic problem is solved using the null field approach (the Tmatrix method). Starting from surface integral representations containing the free space Green's dyadic and field expansions in plane and spherical vector wave functions, the null field approach leads to a set of algebraic equations whose solution can be given in a form that naturally has a multiple scattering interpretation. The null field approach thus has a... (More)  The propagation of elastic waves in a manylayered elastic halfspace is considered. One of the layers contains a bounded inhomogeneity which in the numerical applications is taken as a sphere. The halfspace is excited by an explosion, modelled as a sudden isotropic point source.
First the timeharmonic problem is solved using the null field approach (the Tmatrix method). Starting from surface integral representations containing the free space Green's dyadic and field expansions in plane and spherical vector wave functions, the null field approach leads to a set of algebraic equations whose solution can be given in a form that naturally has a multiple scattering interpretation. The null field approach thus has a buildingblock structure, i.e. the transition matrix of the inhomogeneity and the reflection and transmission coefficients of the interfaces are used as parts in the total solution. It is noted that in the absence of the inhomogeneity the null field approach yields a more decoupled set of equations than the classical methods. The main practical limitation of the null field approach, which is, in principle, an exact method, is that only low and intermediate frequencies can be treated. In the numerical applications the highest frequency corresponds to a sphere diameter of about 12 S wavelengths. The transformations from the frequency domain to the time domain is performed with an FFT algorithm and to limit the bandwidth appropriate filters are placed at the receivers.
The numerical examples show synthetic seismograms consisting of data from 10 observation points at increasing distances from the source. The layers have been chosen relatively thick so that the reflections from the different interfaces can be separated in time. As long as the reflections from the spherical inhomogeneity are also separated in time from other reflections they can mostly be well recognized. As the distance between the source and inhomogeneity increases, it becomes progressively more difficult to see any influence of the inhomogeneity in the seismograms. (Less)
Please use this url to cite or link to this publication:
http://lup.lub.lu.se/record/1038697
 author
 Karlsson, Anders ^{LU} and Boström, Anders
 publishing date
 1987
 type
 Contribution to journal
 publication status
 published
 subject
 in
 Geophysical Journal International
 volume
 89
 issue
 2
 pages
 527  547
 publisher
 WileyBlackwell
 external identifiers

 scopus:0023480480
 ISSN
 0956540X
 DOI
 10.1111/j.1365246X.1987.tb05182.x
 language
 English
 LU publication?
 no
 id
 663b1f70b8eb4925b81a4bc9cc205927 (old id 1038697)
 date added to LUP
 20080227 14:43:35
 date last changed
 20180107 09:56:54
@article{663b1f70b8eb4925b81a4bc9cc205927, abstract = {The propagation of elastic waves in a manylayered elastic halfspace is considered. One of the layers contains a bounded inhomogeneity which in the numerical applications is taken as a sphere. The halfspace is excited by an explosion, modelled as a sudden isotropic point source.<br/><br> <br/><br> First the timeharmonic problem is solved using the null field approach (the Tmatrix method). Starting from surface integral representations containing the free space Green's dyadic and field expansions in plane and spherical vector wave functions, the null field approach leads to a set of algebraic equations whose solution can be given in a form that naturally has a multiple scattering interpretation. The null field approach thus has a buildingblock structure, i.e. the transition matrix of the inhomogeneity and the reflection and transmission coefficients of the interfaces are used as parts in the total solution. It is noted that in the absence of the inhomogeneity the null field approach yields a more decoupled set of equations than the classical methods. The main practical limitation of the null field approach, which is, in principle, an exact method, is that only low and intermediate frequencies can be treated. In the numerical applications the highest frequency corresponds to a sphere diameter of about 12 S wavelengths. The transformations from the frequency domain to the time domain is performed with an FFT algorithm and to limit the bandwidth appropriate filters are placed at the receivers.<br/><br> <br/><br> The numerical examples show synthetic seismograms consisting of data from 10 observation points at increasing distances from the source. The layers have been chosen relatively thick so that the reflections from the different interfaces can be separated in time. As long as the reflections from the spherical inhomogeneity are also separated in time from other reflections they can mostly be well recognized. As the distance between the source and inhomogeneity increases, it becomes progressively more difficult to see any influence of the inhomogeneity in the seismograms.}, author = {Karlsson, Anders and Boström, Anders}, issn = {0956540X}, language = {eng}, number = {2}, pages = {527547}, publisher = {WileyBlackwell}, series = {Geophysical Journal International}, title = {Broad band synthetic seismograms for a spherical inhomogeneity in a manylayered elastic halfspace}, url = {http://dx.doi.org/10.1111/j.1365246X.1987.tb05182.x}, volume = {89}, year = {1987}, }