AccScience Publishing / AJWEP / Online First / DOI: 10.36922/AJWEP026170114
ORIGINAL RESEARCH ARTICLE

Broadband shear wave velocity profiling to evaluate subsidence vulnerability: A combined multichannel analysis of surface waves approach in Quang Ninh, Vietnam

Nguyen Nhat Kim Ngan1,2* Nguyen Thanh Hai3,4 Nguyen Van Thuan1,2
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1 Department of Geophysics, Faculty of Physics and Engineering Physics, University of Science, Ho Chi Minh City, Vietnam
2 Vietnam National University, Ho Chi Minh City, Vietnam
3 Department of Seismology, Institute of Earth Sciences, Hanoi, Vietnam
4 Viet Nam Academy of Science and Technology, Hanoi, Vietnam
Received: 23 March 2026 | Accepted: 18 May 2026 | Published online: 10 June 2026
© 2026 by the Author(s). This article is an open access article distributed under the terms and conditions of the Creative Commons Attribution 4.0 International License ( https://creativecommons.org/licenses/by/4.0/ )
Abstract

As urban centers expand into geologically complex and hazardous terrains, accurately characterizing deep subsurface stiffness becomes critical for disaster mitigation. Traditional active multichannel analysis of surface waves (MASW) provides excellent near-surface resolution but struggles to penetrate beyond 30 m. Conversely, passive MASW captures deep geological interfaces but lacks high-frequency data for shallow soil profiling. We addressed this limitation by deploying a combined active and passive MASW framework to extract broadband dispersion curves (2–11 Hz) in Quang Hanh, Quang Ninh Province, Vietnam—a region currently facing severe subsidence risks. Seismic data were acquired using a fixed 24-channel array (3 m spacing, 69 m length) utilizing both a sledgehammer source and ambient urban noise. Data processing was conducted using ParkSEIS v2.0, applying a phase-shift algorithm for active data and the extended spatial autocorrelation method for passive data. Through constrained iterative least-squares inversion, we generated one-dimensional shear wave velocity profiles down to a depth of 50 m. The results revealed a highly distinct stratigraphic profile correlating with local borehole data: a semi-stiff clayey topsoil (m/s), a transition zone (m/s), and a basal layer of fractured limestone (m/s). The time-averaged shear wave velocity of 408–517 m/s classifies the area as National Earthquake Hazards Reduction Program site class C. Crucially, the results identified a sharp impedance contrast at the 15 m soil–rock interface. This structural discontinuity indicates a zone of high susceptibility to internal erosion (piping) within the fractured limestone, significantly elevating the risk of karst sinkholes during extreme weather events. This study demonstrates that integrating active and passive MASW provides a robust, non-destructive diagnostic tool for engineers to assess deep geohazards in complex transitional geologies.

Keywords
Geohazards
Karst
Multichannel analysis of surface waves
Shear wave velocity
Subsurface characterization
Funding
This research is funded by Vietnam National University Ho Chi Minh City (VNU-HCM) under a project (grant number CB2025-18-11) within the framework of the Program titled “Strengthening the capacity for education and basic scientific research integrated with strategic technologies at VNU-HCM, aiming to achieve advanced standards comparable to regional and global levels during the 2025–2030 period, with a vision toward 2045.”
Conflict of interest
The authors declare that they have no known competing financial interests or personal relationships that could have appeared to influence the work reported in this paper.
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