Terikan ricih kitaran di dalam tanah disebabkan gelombang jasad
Theoretical expressions and charts for obtaining the maximum cyclic shear strains due to the passage of P and S waves in an elastic isotropic halfspace are presented. Plane, cylindrical and spherical P waves, and plane and cylindrical S waves are considered. The results are presented in terms of...
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| Format: | Article |
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1990
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| Online Access: | http://journalarticle.ukm.my/1280/ http://journalarticle.ukm.my/1280/ |
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ukm-1280 |
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eprints |
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ukm-12802011-10-11T03:45:22Z http://journalarticle.ukm.my/1280/ Terikan ricih kitaran di dalam tanah disebabkan gelombang jasad Ramli Mohamad, Theoretical expressions and charts for obtaining the maximum cyclic shear strains due to the passage of P and S waves in an elastic isotropic halfspace are presented. Plane, cylindrical and spherical P waves, and plane and cylindrical S waves are considered. The results are presented in terms of two main parameters which can be measured, ie. peak particle velocity and P or S wave velocity in the medium. The expressions and charts are of practical value in methods of analysis that require direct use of the shear strains induced by ground vibrations, e.g. in the 'threshold strain' approach 1990 Article PeerReviewed Ramli Mohamad, (1990) Terikan ricih kitaran di dalam tanah disebabkan gelombang jasad. Jurnal Kejuruteraan, 2 . pp. 109-126. http://www.ukm.my/jkukm/index.php/jkukm |
| repository_type |
Digital Repository |
| institution_category |
Local University |
| institution |
Universiti Kebangasaan Malaysia |
| building |
UKM Institutional Repository |
| collection |
Online Access |
| description |
Theoretical expressions and charts for obtaining the maximum cyclic shear strains due
to the passage of P and S waves in an elastic isotropic halfspace are presented. Plane,
cylindrical and spherical P waves, and plane and cylindrical S waves are considered.
The results are presented in terms of two main parameters which can be measured, ie.
peak particle velocity and P or S wave velocity in the medium. The expressions and
charts are of practical value in methods of analysis that require direct use of the shear
strains induced by ground vibrations, e.g. in the 'threshold strain' approach |
| format |
Article |
| author |
Ramli Mohamad, |
| spellingShingle |
Ramli Mohamad, Terikan ricih kitaran di dalam tanah disebabkan gelombang jasad |
| author_facet |
Ramli Mohamad, |
| author_sort |
Ramli Mohamad, |
| title |
Terikan ricih kitaran di dalam tanah disebabkan gelombang jasad |
| title_short |
Terikan ricih kitaran di dalam tanah disebabkan gelombang jasad |
| title_full |
Terikan ricih kitaran di dalam tanah disebabkan gelombang jasad |
| title_fullStr |
Terikan ricih kitaran di dalam tanah disebabkan gelombang jasad |
| title_full_unstemmed |
Terikan ricih kitaran di dalam tanah disebabkan gelombang jasad |
| title_sort |
terikan ricih kitaran di dalam tanah disebabkan gelombang jasad |
| publishDate |
1990 |
| url |
http://journalarticle.ukm.my/1280/ http://journalarticle.ukm.my/1280/ |
| first_indexed |
2023-09-18T19:32:54Z |
| last_indexed |
2023-09-18T19:32:54Z |
| _version_ |
1777405079376101376 |