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Survey linked below the surface layer of the structure to be one very important thing nowadays. Establishment of building construction, site survey, mitigation and sore search needs to be strong reasons for the need for sub surface survey. Multichannel Analysis of Surface Waves ReMi can be categoriz...
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| Format: | Final Project |
| Language: | Indonesia |
| Online Access: | https://digilib.itb.ac.id/gdl/view/16830 |
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| Institution: | Institut Teknologi Bandung |
| Language: | Indonesia |
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id-itb.:168302017-09-27T11:45:15Z#TITLE_ALTERNATIVE# CRITIANTHA (NIM 10206005) : pembimbing ; Gunawan Handayani, MSCE, Ph.D , PRAJA Indonesia Final Project INSTITUT TEKNOLOGI BANDUNG https://digilib.itb.ac.id/gdl/view/16830 Survey linked below the surface layer of the structure to be one very important thing nowadays. Establishment of building construction, site survey, mitigation and sore search needs to be strong reasons for the need for sub surface survey. Multichannel Analysis of Surface Waves ReMi can be categorized as passive MASW type and can be used to determine the profile of the S wave velocity (Vs) of land. This method uses low frequency waves, so that the wavelength that would be generated would be much longer than using the source wave with high frequency (active). Penetration depth that can be achieved with this method is 100 meters below ground surface. Determination of wave profiles performed with field data collection using 12 pieces geophones placed on the media who wish to observe. text |
| institution |
Institut Teknologi Bandung |
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Institut Teknologi Bandung Library |
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Asia |
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Indonesia Indonesia |
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Institut Teknologi Bandung |
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| language |
Indonesia |
| description |
Survey linked below the surface layer of the structure to be one very important thing nowadays. Establishment of building construction, site survey, mitigation and sore search needs to be strong reasons for the need for sub surface survey. Multichannel Analysis of Surface Waves ReMi can be categorized as passive MASW type and can be used to determine the profile of the S wave velocity (Vs) of land. This method uses low frequency waves, so that the wavelength that would be generated would be much longer than using the source wave with high frequency (active). Penetration depth that can be achieved with this method is 100 meters below ground surface. Determination of wave profiles performed with field data collection using 12 pieces geophones placed on the media who wish to observe. |
| format |
Final Project |
| author |
CRITIANTHA (NIM 10206005) : pembimbing ; Gunawan Handayani, MSCE, Ph.D , PRAJA |
| spellingShingle |
CRITIANTHA (NIM 10206005) : pembimbing ; Gunawan Handayani, MSCE, Ph.D , PRAJA #TITLE_ALTERNATIVE# |
| author_facet |
CRITIANTHA (NIM 10206005) : pembimbing ; Gunawan Handayani, MSCE, Ph.D , PRAJA |
| author_sort |
CRITIANTHA (NIM 10206005) : pembimbing ; Gunawan Handayani, MSCE, Ph.D , PRAJA |
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| url |
https://digilib.itb.ac.id/gdl/view/16830 |
| _version_ |
1820745467285209088 |