Application of the MASW Method to Know the Road Stiffness Structure By Using Accelerometer Sensors

A surface wave method is often used to map shear wave velocity variation of soil with depth. However, measured seismic wave field usually contains such unfavorable waves as higher modes of surface waves, body waves, and ambient noise. These waves can significantly influence results of the analysis i...

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Main Author: BUDI LESTARI (NIM 10205046), NOVITA
Format: Final Project
Language:Indonesia
Online Access:https://digilib.itb.ac.id/gdl/view/11072
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Institution: Institut Teknologi Bandung
Language: Indonesia
id id-itb.:11072
spelling id-itb.:110722017-09-27T11:45:14ZApplication of the MASW Method to Know the Road Stiffness Structure By Using Accelerometer Sensors BUDI LESTARI (NIM 10205046), NOVITA Indonesia Final Project INSTITUT TEKNOLOGI BANDUNG https://digilib.itb.ac.id/gdl/view/11072 A surface wave method is often used to map shear wave velocity variation of soil with depth. However, measured seismic wave field usually contains such unfavorable waves as higher modes of surface waves, body waves, and ambient noise. These waves can significantly influence results of the analysis if not properly handled. In an attempt to increase confidence in the interpreted Vs profile as a result of the ambiguity in the analyzed dispersion characteristics, multichannel method is used in this research to characterize the structure of road stiffness on the PU Cikampek. The MASW method originated from the traditional seismic exploration approach that employs multiple (twelve or more) receivers placed along a linear survey line. Main advantage is its capability of recognizing different types of seismic waves based on wave propagation characteristics such as velocity and attenuation. The MASW method utilizes this capability to discriminate the fundamentalmode Rayleigh wave against all other types of surface and body waves generated not only from the seismic source but also from the ambient site conditions. Rayleigh wave is one of surface wave that commonly used to identify near surface layering structure. In what called heterogen medium, Rayleigh is dispersive with frequency function velocity, it can be used to structurized earth layering model based on shear wave velocity (Vs) versus depth (h). The inversion of MASW method which is used to land profiling resulting model and dispersion curve matching in shear waves velocity as depth function. At this final project, data is taken in the project of PU Cikampek by active method that used near offset 2 meters. Inversion processing has done by SWAN. At this line, the asphalt is indicated hard enough which has shear wave velocity at 273 m/s. text
institution Institut Teknologi Bandung
building Institut Teknologi Bandung Library
continent Asia
country Indonesia
Indonesia
content_provider Institut Teknologi Bandung
collection Digital ITB
language Indonesia
description A surface wave method is often used to map shear wave velocity variation of soil with depth. However, measured seismic wave field usually contains such unfavorable waves as higher modes of surface waves, body waves, and ambient noise. These waves can significantly influence results of the analysis if not properly handled. In an attempt to increase confidence in the interpreted Vs profile as a result of the ambiguity in the analyzed dispersion characteristics, multichannel method is used in this research to characterize the structure of road stiffness on the PU Cikampek. The MASW method originated from the traditional seismic exploration approach that employs multiple (twelve or more) receivers placed along a linear survey line. Main advantage is its capability of recognizing different types of seismic waves based on wave propagation characteristics such as velocity and attenuation. The MASW method utilizes this capability to discriminate the fundamentalmode Rayleigh wave against all other types of surface and body waves generated not only from the seismic source but also from the ambient site conditions. Rayleigh wave is one of surface wave that commonly used to identify near surface layering structure. In what called heterogen medium, Rayleigh is dispersive with frequency function velocity, it can be used to structurized earth layering model based on shear wave velocity (Vs) versus depth (h). The inversion of MASW method which is used to land profiling resulting model and dispersion curve matching in shear waves velocity as depth function. At this final project, data is taken in the project of PU Cikampek by active method that used near offset 2 meters. Inversion processing has done by SWAN. At this line, the asphalt is indicated hard enough which has shear wave velocity at 273 m/s.
format Final Project
author BUDI LESTARI (NIM 10205046), NOVITA
spellingShingle BUDI LESTARI (NIM 10205046), NOVITA
Application of the MASW Method to Know the Road Stiffness Structure By Using Accelerometer Sensors
author_facet BUDI LESTARI (NIM 10205046), NOVITA
author_sort BUDI LESTARI (NIM 10205046), NOVITA
title Application of the MASW Method to Know the Road Stiffness Structure By Using Accelerometer Sensors
title_short Application of the MASW Method to Know the Road Stiffness Structure By Using Accelerometer Sensors
title_full Application of the MASW Method to Know the Road Stiffness Structure By Using Accelerometer Sensors
title_fullStr Application of the MASW Method to Know the Road Stiffness Structure By Using Accelerometer Sensors
title_full_unstemmed Application of the MASW Method to Know the Road Stiffness Structure By Using Accelerometer Sensors
title_sort application of the masw method to know the road stiffness structure by using accelerometer sensors
url https://digilib.itb.ac.id/gdl/view/11072
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