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MASW & VS30 Testing in Belleville Ontario | Shear Wave Velocity Site Classification

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A 24-channel seismograph with a sledgehammer source and a spread of 4.5 Hz geophones gets deployed on a Belleville lot. The setup is straightforward: a linear array captures Rayleigh wave dispersion, then inversion software extracts the shear wave velocity profile. In Belleville, the target is clear: a reliable VS30 value for the National Building Code of Canada site classification. The local geology alternates between shallow Ordovician limestone bedrock, glacial till, and pockets of the Champlain Sea clay plain. Each profile reacts differently to surface waves. A stiff till near Highway 401 gives a VS30 above 760 m/s, while a clay deposit south of Dundas Street drops below 180 m/s. The MASW method cuts through this variability in under an hour per line. The data feeds directly into foundation design, seismic hazard assessment, and liquefaction screening. An SPT drilling program often runs parallel to the MASW survey for a complete stratigraphic picture.

A VS30 of 195 m/s versus 820 m/s changes the site class from D to B, directly multiplying the seismic base shear in the Belleville structural design.

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Methodology and scope

Two sites in Belleville, one on the limestone plateau near the Bayshore and another in the Moira River floodplain, illustrate the range. The Bayshore site shows a rock-refraction kick at 12 m depth with a VS30 of 820 m/s, placing it squarely in NBCC Site Class B. The floodplain site reveals 22 m of soft silty clay over bedrock, with a VS30 of 195 m/s, landing in Site Class D. The difference drives everything: base shear, spectral acceleration, and foundation typology. MASW captures the transition from normally dispersive to inversely dispersive profiles when a stiff layer overlies soft material, a scenario common in Belleville's buried valley aquifers. The raw dispersion image gets processed through a solid inversion routine, and the 1D VS profile is validated against seismic refraction picks and available borehole logs.
MASW & VS30 Testing in Belleville Ontario | Shear Wave Velocity Site Classification
Technical reference — Belleville Ontario

Site-specific factors

Belleville sits within the Western Quebec Seismic Zone, a region with a documented history of moderate intraplate earthquakes. The 5.0 magnitude event near Buckingham in 2010 and the 5.8 Mineral, Virginia quake in 2011 serve as reminders that stable continental regions transmit energy efficiently over long distances. A site classified by NBCC as Class E or D carries a site amplification factor that can double the spectral acceleration relative to a Class C reference. Skipping the VS30 measurement and defaulting to a conservative class can add unnecessary cost to the structural design. Worse, assuming a Class C profile on a soft clay site underestimates the seismic demand. The Moira River alluvial corridor and the low-lying areas near the Bay of Quinte are particularly susceptible. Combining the shear wave profile with a liquefaction assessment clarifies the true risk for granular deposits below the water table.

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Relevant standards

ASTM D4428/D4428M-14, NBCC 2020 Division B, 4.1.8.4, ASCE/SEI 7-22 Chapter 20, Eurocode 8 (EN 1998-1:2004) for comparative analysis

Technical data

ParameterTypical value
StandardASTM D4428/D4428M-14
Array length46 m to 92 m
Geophone frequency4.5 Hz vertical component
Recording system24-bit, 24-channel seismograph
Source8 kg sledgehammer with strike plate
Inversion methodGenetic algorithm / Occam's inversion
Max investigation depth~30 m (function of array length)
OutputVS30, VS profile, NBCC site class

Common questions

What does a MASW test cost in Belleville?
How deep can MASW investigate in Belleville's glacial till?

The maximum reliable depth is roughly one-half to one-third of the receiver spread length. With a 92 m array on competent till, the investigation reaches 30 to 35 m. On softer Champlain Sea clay, the same array can push beyond 40 m because the longer wavelengths penetrate deeper before attenuating.

Can MASW work on a paved parking lot in Belleville?

Yes. The geophones are mounted on metal base plates and coupled to the asphalt with a thin layer of sand or plumber's putty. The sledgehammer source is struck on a steel plate. The high-frequency pavement noise is filtered during processing, and the dispersion curve remains usable for VS30 calculation.

What is the difference between MASW and seismic refraction for site classification?

Seismic refraction measures P-wave velocity and requires a velocity increase with depth. It misses low-velocity layers. MASW measures shear wave velocity directly, handles velocity inversions (stiff over soft), and produces the VS30 parameter required by NBCC 2020. The two methods complement each other: refraction maps bedrock topography; MASW delivers the shear wave profile.

Location and service area

We serve projects across Belleville Ontario and surrounding areas.

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