Estimation of VS30 using shallow depth time-averaged shear wave velocity of Rawalpindi–Islamabad, Pakistan
AbstractThe time-averaged shear wave velocity of top 30 m (VS30) is the most commonly used parameter to classify a site and evaluate its amplification characteristics for the seismic design. The in-situ seismic tests must be performed up to a depth of 30 m for obtaining the shear wave velocity (VS)...
| Main Authors: | , , , , , , |
|---|---|
| Format: | Article |
| Language: | English |
| Published: |
Taylor & Francis Group
2023-12-01
|
| Series: | Geomatics, Natural Hazards & Risk |
| Subjects: | |
| Online Access: | https://www.tandfonline.com/doi/10.1080/19475705.2022.2161953 |
| _version_ | 1797389232553066496 |
|---|---|
| author | Muhammad Bilal Adeel Zubair Ahmed Nizamani Muhammad Aaqib Sarfraz Khan Jawad Ur Rehman Bikram Bhusal Duhee Park |
| author_facet | Muhammad Bilal Adeel Zubair Ahmed Nizamani Muhammad Aaqib Sarfraz Khan Jawad Ur Rehman Bikram Bhusal Duhee Park |
| author_sort | Muhammad Bilal Adeel |
| collection | DOAJ |
| description | AbstractThe time-averaged shear wave velocity of top 30 m (VS30) is the most commonly used parameter to classify a site and evaluate its amplification characteristics for the seismic design. The in-situ seismic tests must be performed up to a depth of 30 m for obtaining the shear wave velocity (VS) profiles to estimate VS30. It is intimated that, in most of the cases, the measured VS profile does not extend up to 30 m due to numerous reasons including limitation of testing techniques and unfavorable field conditions. Since, the measurements of VS30 are unavailable for the majority of Pakistan and the world, the local geology and topographic slope or its combination are used to estimate VS30. However, there is no field-based validation of the estimated VS30 is performed in Islamabad–Rawalpindi region, the proxy-based estimation may lead to unrealistic results. To accommodate this, region specific extrapolation methods are developed. This study develops an empirical data-driven function of VS30 from shallow VS profiles by correlating VS30 with the time-averaged VS to depths less than 30 m. In this regard, 85 VS profiles are used from Rawalpindi-Islamabad region. A comparative analysis of the proposed procedure is carried out with the published methods. It is revealed that VS30 predicted by the proposed function results in close matches with the data measured in the western United States. In addition, the results indicate that the local geology and topographic slope proxies may not be acceptable for usage in the region due to their greater uncertainty. Finally, a procedure for extrapolating the VS profile from available shallow depth measurements up to 30 m is proposed. |
| first_indexed | 2024-03-08T22:52:52Z |
| format | Article |
| id | doaj.art-c98b12127ab54fdfa1a99bfacb6fa41c |
| institution | Directory Open Access Journal |
| issn | 1947-5705 1947-5713 |
| language | English |
| last_indexed | 2024-03-08T22:52:52Z |
| publishDate | 2023-12-01 |
| publisher | Taylor & Francis Group |
| record_format | Article |
| series | Geomatics, Natural Hazards & Risk |
| spelling | doaj.art-c98b12127ab54fdfa1a99bfacb6fa41c2023-12-16T08:49:46ZengTaylor & Francis GroupGeomatics, Natural Hazards & Risk1947-57051947-57132023-12-0114112110.1080/19475705.2022.2161953Estimation of VS30 using shallow depth time-averaged shear wave velocity of Rawalpindi–Islamabad, PakistanMuhammad Bilal Adeel0Zubair Ahmed Nizamani1Muhammad Aaqib2Sarfraz Khan3Jawad Ur Rehman4Bikram Bhusal5Duhee Park6Department of Transportation & Geotechnical Engineering, National University of Sciences and Technology, Risalpur, Pakistan; ;Department of Civil Engineering, National University of Sciences and Technology, Quetta, PakistanDepartment of Civil Engineering, National University of Technology, Islamabad, PakistanNational Centre of Excellence in Geology, University of Peshawar, Peshawar, PakistanDepartment of Civil and Environmental Engineering, Hanyang University, Seoul, Republic of KoreaDepartment of Civil Engineering, National College Engineering, Lalitpur, NepalDepartment of Civil and Environmental Engineering, Hanyang University, Seoul, Republic of KoreaAbstractThe time-averaged shear wave velocity of top 30 m (VS30) is the most commonly used parameter to classify a site and evaluate its amplification characteristics for the seismic design. The in-situ seismic tests must be performed up to a depth of 30 m for obtaining the shear wave velocity (VS) profiles to estimate VS30. It is intimated that, in most of the cases, the measured VS profile does not extend up to 30 m due to numerous reasons including limitation of testing techniques and unfavorable field conditions. Since, the measurements of VS30 are unavailable for the majority of Pakistan and the world, the local geology and topographic slope or its combination are used to estimate VS30. However, there is no field-based validation of the estimated VS30 is performed in Islamabad–Rawalpindi region, the proxy-based estimation may lead to unrealistic results. To accommodate this, region specific extrapolation methods are developed. This study develops an empirical data-driven function of VS30 from shallow VS profiles by correlating VS30 with the time-averaged VS to depths less than 30 m. In this regard, 85 VS profiles are used from Rawalpindi-Islamabad region. A comparative analysis of the proposed procedure is carried out with the published methods. It is revealed that VS30 predicted by the proposed function results in close matches with the data measured in the western United States. In addition, the results indicate that the local geology and topographic slope proxies may not be acceptable for usage in the region due to their greater uncertainty. Finally, a procedure for extrapolating the VS profile from available shallow depth measurements up to 30 m is proposed.https://www.tandfonline.com/doi/10.1080/19475705.2022.2161953Time-averaged shear wave velocityshallow depthVS30empirical functionbuilding code of Pakistan |
| spellingShingle | Muhammad Bilal Adeel Zubair Ahmed Nizamani Muhammad Aaqib Sarfraz Khan Jawad Ur Rehman Bikram Bhusal Duhee Park Estimation of VS30 using shallow depth time-averaged shear wave velocity of Rawalpindi–Islamabad, Pakistan Geomatics, Natural Hazards & Risk Time-averaged shear wave velocity shallow depth VS30 empirical function building code of Pakistan |
| title | Estimation of VS30 using shallow depth time-averaged shear wave velocity of Rawalpindi–Islamabad, Pakistan |
| title_full | Estimation of VS30 using shallow depth time-averaged shear wave velocity of Rawalpindi–Islamabad, Pakistan |
| title_fullStr | Estimation of VS30 using shallow depth time-averaged shear wave velocity of Rawalpindi–Islamabad, Pakistan |
| title_full_unstemmed | Estimation of VS30 using shallow depth time-averaged shear wave velocity of Rawalpindi–Islamabad, Pakistan |
| title_short | Estimation of VS30 using shallow depth time-averaged shear wave velocity of Rawalpindi–Islamabad, Pakistan |
| title_sort | estimation of vs30 using shallow depth time averaged shear wave velocity of rawalpindi islamabad pakistan |
| topic | Time-averaged shear wave velocity shallow depth VS30 empirical function building code of Pakistan |
| url | https://www.tandfonline.com/doi/10.1080/19475705.2022.2161953 |
| work_keys_str_mv | AT muhammadbilaladeel estimationofvs30usingshallowdepthtimeaveragedshearwavevelocityofrawalpindiislamabadpakistan AT zubairahmednizamani estimationofvs30usingshallowdepthtimeaveragedshearwavevelocityofrawalpindiislamabadpakistan AT muhammadaaqib estimationofvs30usingshallowdepthtimeaveragedshearwavevelocityofrawalpindiislamabadpakistan AT sarfrazkhan estimationofvs30usingshallowdepthtimeaveragedshearwavevelocityofrawalpindiislamabadpakistan AT jawadurrehman estimationofvs30usingshallowdepthtimeaveragedshearwavevelocityofrawalpindiislamabadpakistan AT bikrambhusal estimationofvs30usingshallowdepthtimeaveragedshearwavevelocityofrawalpindiislamabadpakistan AT duheepark estimationofvs30usingshallowdepthtimeaveragedshearwavevelocityofrawalpindiislamabadpakistan |