Classification of soil stiffness using p-wave.
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Date
2016-08
Authors
Samah, Rose Nadia Abu
Journal Title
Journal ISSN
Volume Title
Publisher
Universiti Sains Malaysia
Abstract
Tomografi seismik biasan (SRT) adalah satu kaedah geofizik yang mengukur perambatan gelombang bunyi di bawah permukaan bumi. Kaedah ini memerlukan tenaga tiruan sebagai sumber.
Seismic refraction tomography (SRT) is a geophysical method that measures the propagation of sound wave in Earth’s subsurface. This method required an artificial energy as a seismic source.
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Keywords
Stiffness , P wave