Evaluation of the State of Rocks in Load Steps by Low-frequency Ultrasonic Flaw Detection

The purpose of this study was to quantitatively evaluate the state of rocks in load steps by using the low-frequency ultrasonic flaw detection method. The initial Vp-velocities measured with a CND tester were in the order of Z-axis < X-axis < Y-axis, with 1687.5 m/s along the X-axis, 1...

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Main Authors: Kang, S, Kim, J, Noh, J, Na, T, Jang, Hyong Doo, Ko, C
Format: Journal Article
Published: The Korean Society of Engineering Geology 2017
Online Access:http://hdl.handle.net/20.500.11937/52813
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author Kang, S
Kim, J
Noh, J
Na, T
Jang, Hyong Doo
Ko, C
author_facet Kang, S
Kim, J
Noh, J
Na, T
Jang, Hyong Doo
Ko, C
author_sort Kang, S
building Curtin Institutional Repository
collection Online Access
description The purpose of this study was to quantitatively evaluate the state of rocks in load steps by using the low-frequency ultrasonic flaw detection method. The initial Vp-velocities measured with a CND tester were in the order of Z-axis < X-axis < Y-axis, with 1687.5 m/s along the X-axis, 1690.7 m/s along the Y-axis, 1548.3 m/s along the Z-axis, and an average of 1642.2 m/s. The overall average of the Q vlaues, measured with a Silver Schmidt hammer, was 62.6, which corresponds to a uniaxial compressive strength of ~105 MPa. The Vp-velocity, measured with a low-frequency ultrasonic flaw detector at load steps of 50%, 60%, 70%, and 80%, typically decreases in the order of X-axis < Y-axis < Z-axis with increasing load steps. This order contrasts with that of the initial Vp-velocities. As the load step increases the factors that reduce the Vp-velocity in the X-axis direction are more influential than those in the Y-axis or Z-axis directions. This indicates that the initial state of rocks can vary and is dependent on the stress state.
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institution Curtin University Malaysia
institution_category Local University
last_indexed 2025-11-14T09:53:12Z
publishDate 2017
publisher The Korean Society of Engineering Geology
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spelling curtin-20.500.11937-528132020-09-07T05:38:10Z Evaluation of the State of Rocks in Load Steps by Low-frequency Ultrasonic Flaw Detection Kang, S Kim, J Noh, J Na, T Jang, Hyong Doo Ko, C The purpose of this study was to quantitatively evaluate the state of rocks in load steps by using the low-frequency ultrasonic flaw detection method. The initial Vp-velocities measured with a CND tester were in the order of Z-axis < X-axis < Y-axis, with 1687.5 m/s along the X-axis, 1690.7 m/s along the Y-axis, 1548.3 m/s along the Z-axis, and an average of 1642.2 m/s. The overall average of the Q vlaues, measured with a Silver Schmidt hammer, was 62.6, which corresponds to a uniaxial compressive strength of ~105 MPa. The Vp-velocity, measured with a low-frequency ultrasonic flaw detector at load steps of 50%, 60%, 70%, and 80%, typically decreases in the order of X-axis < Y-axis < Z-axis with increasing load steps. This order contrasts with that of the initial Vp-velocities. As the load step increases the factors that reduce the Vp-velocity in the X-axis direction are more influential than those in the Y-axis or Z-axis directions. This indicates that the initial state of rocks can vary and is dependent on the stress state. 2017 Journal Article http://hdl.handle.net/20.500.11937/52813 10.9720/kseg.2017.1.51 The Korean Society of Engineering Geology unknown
spellingShingle Kang, S
Kim, J
Noh, J
Na, T
Jang, Hyong Doo
Ko, C
Evaluation of the State of Rocks in Load Steps by Low-frequency Ultrasonic Flaw Detection
title Evaluation of the State of Rocks in Load Steps by Low-frequency Ultrasonic Flaw Detection
title_full Evaluation of the State of Rocks in Load Steps by Low-frequency Ultrasonic Flaw Detection
title_fullStr Evaluation of the State of Rocks in Load Steps by Low-frequency Ultrasonic Flaw Detection
title_full_unstemmed Evaluation of the State of Rocks in Load Steps by Low-frequency Ultrasonic Flaw Detection
title_short Evaluation of the State of Rocks in Load Steps by Low-frequency Ultrasonic Flaw Detection
title_sort evaluation of the state of rocks in load steps by low-frequency ultrasonic flaw detection
url http://hdl.handle.net/20.500.11937/52813