Site Characterization by Ambient Noise Geophysical and by Geotechnical Investigations at Mirpur, Dhaka, Bangladesh
DOI:
https://doi.org/10.64862/Keywords:
Site characterization, Microtremor, H/V spectral ratio, Climate-change resilient urbanizationAbstract
Seismic site effects are crucial for seismic hazard assessment and earthquake-resilient urban planning as they play a key role in controlling the intensity of ground shaking experienced during earthquakes. Geophysical measurements based on ambient seismic vibrations, particularly the Horizontal to Vertical spectral ratio (H/V) and array-based methods, provide cost-effective and noninvasive techniques to estimate the fundamental resonance frequency and one-dimensional shear-wave velocity (Vs) profiles, which are directly related to sediment thickness and the site effect potential. Geomorphologically, Dhaka city, including the Mirpur area, occupies the southern part of the Madhupur Tract, surrounded by floodplains of the surrounding rivers. Mirpur, located in the north of Dhaka, falls within the Seismic Zone II of Bangladesh (Z = 0.20g) and is considered moderately earthquake-prone (BNBC, 2020). In this research, 17 H/V measurements were carried out using OYO McSEIS-MT NEO three-component sensors and processed using the Geopsy software. These microtremor results were compared with the borehole standard penetration test (SPT) values with lithological descriptions, multichannel analysis of surface wave (MASW) and downhole PS logging from the Dhaka Urban Geo-information Atlas (2023) to characterize the subsurface conditions. Previous studies reported fundamental frequencies between 0.5 and 4 Hz in Mirpur (Helaly and Ansary, 2021), indicating significant local variation. Nevertheless, the analysis of ambient noise measurements revealed fundamental frequencies between 0.5 and 1.2 Hz, suggesting lower fundamental frequencies than previously reported. The results suggest that the generalized zonation may overestimate local resonance conditions, emphasizing the necessity for site-specific microtremor investigations for reliable seismic site characterization.
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