The velocity of Rayleigh waves along a prestressed semi-infinite medium assuming a two-dimensional anisotropy
The velocity equation for the surface ivavesof the Rayleigh type is derived in the caseof an idealized medium of uniform twodimensionalanisotropy: the elastic constantsare assumed to be everywhere the same buidifferent as far as vertical and horizontaldirections are concerned, and moreover thepossib...
| الحاوية / القاعدة: | Annals of Geophysics |
|---|---|
| المؤلف الرئيسي: | |
| التنسيق: | مقال |
| اللغة: | الإنجليزية |
| منشور في: |
Istituto Nazionale di Geofisica e Vulcanologia (INGV)
1958-06-01
|
| الوصول للمادة أونلاين: | http://www.annalsofgeophysics.eu/index.php/annals/article/view/5743 |
| _version_ | 1857029291970134016 |
|---|---|
| author | f. buckens |
| author_facet | f. buckens |
| author_sort | f. buckens |
| collection | DOAJ |
| container_title | Annals of Geophysics |
| description | The velocity equation for the surface ivavesof the Rayleigh type is derived in the caseof an idealized medium of uniform twodimensionalanisotropy: the elastic constantsare assumed to be everywhere the same buidifferent as far as vertical and horizontaldirections are concerned, and moreover thepossible inference of uniform initial stresses,(horizontal tensions or compressions) is included.There are then five independantelastic constants instead of four to be takenin account, in order to study the propagationof a tivo-dimensional surface-wave, the effectof a transverse initial stress being todestroy the symmetry of the cross elasticconstants. |
| format | Article |
| id | doaj-art-9f7b8a316088409aa1dab9f976ea611d |
| institution | Directory of Open Access Journals |
| issn | 1593-5213 2037-416X |
| language | English |
| publishDate | 1958-06-01 |
| publisher | Istituto Nazionale di Geofisica e Vulcanologia (INGV) |
| record_format | Article |
| spelling | doaj-art-9f7b8a316088409aa1dab9f976ea611d2025-08-19T19:40:49ZengIstituto Nazionale di Geofisica e Vulcanologia (INGV)Annals of Geophysics1593-52132037-416X1958-06-011129911210.4401/ag-5743The velocity of Rayleigh waves along a prestressed semi-infinite medium assuming a two-dimensional anisotropyf. buckensThe velocity equation for the surface ivavesof the Rayleigh type is derived in the caseof an idealized medium of uniform twodimensionalanisotropy: the elastic constantsare assumed to be everywhere the same buidifferent as far as vertical and horizontaldirections are concerned, and moreover thepossible inference of uniform initial stresses,(horizontal tensions or compressions) is included.There are then five independantelastic constants instead of four to be takenin account, in order to study the propagationof a tivo-dimensional surface-wave, the effectof a transverse initial stress being todestroy the symmetry of the cross elasticconstants.http://www.annalsofgeophysics.eu/index.php/annals/article/view/5743 |
| spellingShingle | f. buckens The velocity of Rayleigh waves along a prestressed semi-infinite medium assuming a two-dimensional anisotropy |
| title | The velocity of Rayleigh waves along a prestressed semi-infinite medium assuming a two-dimensional anisotropy |
| title_full | The velocity of Rayleigh waves along a prestressed semi-infinite medium assuming a two-dimensional anisotropy |
| title_fullStr | The velocity of Rayleigh waves along a prestressed semi-infinite medium assuming a two-dimensional anisotropy |
| title_full_unstemmed | The velocity of Rayleigh waves along a prestressed semi-infinite medium assuming a two-dimensional anisotropy |
| title_short | The velocity of Rayleigh waves along a prestressed semi-infinite medium assuming a two-dimensional anisotropy |
| title_sort | velocity of rayleigh waves along a prestressed semi infinite medium assuming a two dimensional anisotropy |
| url | http://www.annalsofgeophysics.eu/index.php/annals/article/view/5743 |
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