Modified refracted ray path method for determination of shear wave velocity profiles using seismic cone
The commonly used data reduction methods to determine shear wave velocity (Vs) require the depth interval of the Vs profile to be the same as the in-situ testing interval. The Vs values derived in this way are the mean values within the depth intervals. However, the in-situ multilayer interfaces do...
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sg-ntu-dr.10356-1594652022-06-24T02:46:38Z Modified refracted ray path method for determination of shear wave velocity profiles using seismic cone Wang, Hao Wu, Shifan Qi, Xiaohui Chu, Jian School of Civil and Environmental Engineering Engineering::Civil engineering Seismic Cone Penetration Test Shear Wave Velocity The commonly used data reduction methods to determine shear wave velocity (Vs) require the depth interval of the Vs profile to be the same as the in-situ testing interval. The Vs values derived in this way are the mean values within the depth intervals. However, the in-situ multilayer interfaces do not always coincide with the predetermined testing depths, and the materials may change dramatically across layers and thus the above interpretation methods may not always produce representative soil properties. In this study, a modified refracted ray path method for more flexible Vs calculation is proposed. The method takes advantage of the routine cone penetration testing data obtained in SCPT tests and applies a combined approach for the soil layer identification using both the corrected cone tip resistance (qt) and the Soil Behavior Type Index (Ic) as indicators. Vs is then calculated using the Snell's law based on the original shear wave travel times and the newly identified layer profiles. The proposed method can avoid the error caused by crossing the multilayer boundaries and provide a more accurate prediction of soil type and the corresponding stiffness properties. The data show that by using the proposed method, the accuracy of the estimated Vs can be improved by up to 77% for a soil layer with interface not located at testing depths, as compared to Vs obtained from the conventional methods. Nanyang Technological University This study forms part of a strategic initiative program. The support from Nanyang Technological University and the Centre for Urban Solutions are gratefully acknowledged. 2022-06-24T02:46:37Z 2022-06-24T02:46:37Z 2021 Journal Article Wang, H., Wu, S., Qi, X. & Chu, J. (2021). Modified refracted ray path method for determination of shear wave velocity profiles using seismic cone. Engineering Geology, 293, 106330-. https://dx.doi.org/10.1016/j.enggeo.2021.106330 0013-7952 https://hdl.handle.net/10356/159465 10.1016/j.enggeo.2021.106330 2-s2.0-85112768005 293 106330 en Engineering Geology © 2021 Elsevier B.V. All rights reserved. |
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Engineering::Civil engineering Seismic Cone Penetration Test Shear Wave Velocity Wang, Hao Wu, Shifan Qi, Xiaohui Chu, Jian Modified refracted ray path method for determination of shear wave velocity profiles using seismic cone |
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The commonly used data reduction methods to determine shear wave velocity (Vs) require the depth interval of the Vs profile to be the same as the in-situ testing interval. The Vs values derived in this way are the mean values within the depth intervals. However, the in-situ multilayer interfaces do not always coincide with the predetermined testing depths, and the materials may change dramatically across layers and thus the above interpretation methods may not always produce representative soil properties. In this study, a modified refracted ray path method for more flexible Vs calculation is proposed. The method takes advantage of the routine cone penetration testing data obtained in SCPT tests and applies a combined approach for the soil layer identification using both the corrected cone tip resistance (qt) and the Soil Behavior Type Index (Ic) as indicators. Vs is then calculated using the Snell's law based on the original shear wave travel times and the newly identified layer profiles. The proposed method can avoid the error caused by crossing the multilayer boundaries and provide a more accurate prediction of soil type and the corresponding stiffness properties. The data show that by using the proposed method, the accuracy of the estimated Vs can be improved by up to 77% for a soil layer with interface not located at testing depths, as compared to Vs obtained from the conventional methods. |
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School of Civil and Environmental Engineering |
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School of Civil and Environmental Engineering Wang, Hao Wu, Shifan Qi, Xiaohui Chu, Jian |
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Article |
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Wang, Hao Wu, Shifan Qi, Xiaohui Chu, Jian |
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Wang, Hao |
title |
Modified refracted ray path method for determination of shear wave velocity profiles using seismic cone |
title_short |
Modified refracted ray path method for determination of shear wave velocity profiles using seismic cone |
title_full |
Modified refracted ray path method for determination of shear wave velocity profiles using seismic cone |
title_fullStr |
Modified refracted ray path method for determination of shear wave velocity profiles using seismic cone |
title_full_unstemmed |
Modified refracted ray path method for determination of shear wave velocity profiles using seismic cone |
title_sort |
modified refracted ray path method for determination of shear wave velocity profiles using seismic cone |
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2022 |
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https://hdl.handle.net/10356/159465 |
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1736856414542888960 |