Excavatability Assessment of Weathered Sedimentary Rock Mass Using Seismic Velocity Method
Abstract
Seismic refraction method is one of the most popular methods in assessing surface excavation. The main objective of the seismic data acquisition is to delineate the subsurface into velocity profiles as different velocity can be correlated to identify different materials. The physical principal used for the determination of excavatability is that seismic waves travel faster through denser material as compared to less consolidated material. In general, a lower velocity indicates material that is soft and a higher velocity indicates more difficult to be excavated. However, a few researchers have noted that seismic velocity method alone does not correlate well with the excavatability of the material. In this study, a seismic velocity method was used in Nusajaya, Johor to assess the accuracy of this seismic velocity method with excavatability of the weathered sedimentary rock mass. A direct ripping run by monitoring the actual production of ripping has been employed at later stage and compared to the ripper manufacturer's recommendation. This paper presents the findings of the seismic velocity tests in weathered sedimentary area. The reliability of using this method with the actual rippability trials is also presented.
- Authors:
-
- Department of Geotechnics and Transportation, Faculty of Civil Engineering, Universiti Teknologi Malaysia, 81310 UTM Skudai. Johor (Malaysia)
- Universiti Sains Malaysia, Penang (Malaysia)
- Publication Date:
- OSTI Identifier:
- 21513131
- Resource Type:
- Journal Article
- Journal Name:
- AIP Conference Proceedings
- Additional Journal Information:
- Journal Volume: 1325; Journal Issue: 1; Conference: 4. Asian physics international symposium, Bandung, West Java (Indonesia), 12-13 Oct 2010; Other Information: DOI: 10.1063/1.3537880; (c) 2010 American Institute of Physics; Journal ID: ISSN 0094-243X
- Country of Publication:
- United States
- Language:
- English
- Subject:
- 58 GEOSCIENCES; ACCURACY; DATA ACQUISITION; EXCAVATION; MANUFACTURERS; MASS; REFRACTION; RELIABILITY; SEDIMENTARY ROCKS; SEISMIC WAVES; SEISMOGRAPHS; SURFACES; VELOCITY; MEASURING INSTRUMENTS; ROCKS
Citation Formats
Bin Mohamad, Edy Tonnizam, Noor, Muhazian Md, Isa, Mohamed Fauzi Bin Md., Mazlan, Ain Naadia, and Saad, Rosli. Excavatability Assessment of Weathered Sedimentary Rock Mass Using Seismic Velocity Method. United States: N. p., 2010.
Web. doi:10.1063/1.3537880.
Bin Mohamad, Edy Tonnizam, Noor, Muhazian Md, Isa, Mohamed Fauzi Bin Md., Mazlan, Ain Naadia, & Saad, Rosli. Excavatability Assessment of Weathered Sedimentary Rock Mass Using Seismic Velocity Method. United States. https://doi.org/10.1063/1.3537880
Bin Mohamad, Edy Tonnizam, Noor, Muhazian Md, Isa, Mohamed Fauzi Bin Md., Mazlan, Ain Naadia, and Saad, Rosli. 2010.
"Excavatability Assessment of Weathered Sedimentary Rock Mass Using Seismic Velocity Method". United States. https://doi.org/10.1063/1.3537880.
@article{osti_21513131,
title = {Excavatability Assessment of Weathered Sedimentary Rock Mass Using Seismic Velocity Method},
author = {Bin Mohamad, Edy Tonnizam and Noor, Muhazian Md and Isa, Mohamed Fauzi Bin Md. and Mazlan, Ain Naadia and Saad, Rosli},
abstractNote = {Seismic refraction method is one of the most popular methods in assessing surface excavation. The main objective of the seismic data acquisition is to delineate the subsurface into velocity profiles as different velocity can be correlated to identify different materials. The physical principal used for the determination of excavatability is that seismic waves travel faster through denser material as compared to less consolidated material. In general, a lower velocity indicates material that is soft and a higher velocity indicates more difficult to be excavated. However, a few researchers have noted that seismic velocity method alone does not correlate well with the excavatability of the material. In this study, a seismic velocity method was used in Nusajaya, Johor to assess the accuracy of this seismic velocity method with excavatability of the weathered sedimentary rock mass. A direct ripping run by monitoring the actual production of ripping has been employed at later stage and compared to the ripper manufacturer's recommendation. This paper presents the findings of the seismic velocity tests in weathered sedimentary area. The reliability of using this method with the actual rippability trials is also presented.},
doi = {10.1063/1.3537880},
url = {https://www.osti.gov/biblio/21513131},
journal = {AIP Conference Proceedings},
issn = {0094-243X},
number = 1,
volume = 1325,
place = {United States},
year = {Thu Dec 23 00:00:00 EST 2010},
month = {Thu Dec 23 00:00:00 EST 2010}
}