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Refraction Microtremor (ReMi) is one of the methods that used in geotechnical engineering to determine the S wave velocity profile. The S wave velocity profile was obtained from the Rayleigh wave which has the largest amplitude waves than the other. Ambient Noise was used to generate the Rayleigh wa...
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| 主要作者: | |
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| 格式: | Final Project |
| 語言: | Indonesia |
| 在線閱讀: | https://digilib.itb.ac.id/gdl/view/14784 |
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| 機構: | Institut Teknologi Bandung |
| 語言: | Indonesia |
| 總結: | Refraction Microtremor (ReMi) is one of the methods that used in geotechnical engineering to determine the S wave velocity profile. The S wave velocity profile was obtained from the Rayleigh wave which has the largest amplitude waves than the other. Ambient Noise was used to generate the Rayleigh wave that in former methods treated as a nuisance that should be eliminated. The acquisition of ReMi data using ordinary refraction configuration that commonly used to find the P wave profile. |
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