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MASW / VS30 Testing in Saguenay: Shear Wave Velocity for Seismic Site Classification

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With a population approaching 145,000, Saguenay sits in one of Canada's most active seismic zones, making the 1988 magnitude 5.9 earthquake a permanent reference point for local construction. The city spans thick sequences of Laflamme Sea clays, glacial tills, and bedrock outcrops that vary sharply between Jonquière and Chicoutimi, so a uniform foundation assumption simply does not work here. We run active and passive MASW surveys to deliver VS30 profiles that anchor the NBCC seismic site classification—moving the conversation from generic code assumptions to measured ground response. Because the Saguenay graben imposes real amplification risks, the shear wave velocity data feeds directly into the structural engineer's dynamic analysis and often reduces the seismic design category when stiff soils are proven at depth. For deeper verification in variable overburden, the S-wave refraction survey provides a complementary tomographic image that helps map the bedrock interface across the site.

A measured VS30 profile in Saguenay can shift a site from Site Class D to Site Class C, reducing the design spectral acceleration by 20 to 30 percent and unlocking substantial savings in the structural frame.

Scope of work

A project we recently supported in the Jonquière borough encountered dense till at 4 metres on one half of the lot, while the other half sat on 12 metres of soft silty clay—a textbook case of lateral soil contrast that only a surface-wave method could resolve efficiently. The MASW array captured the velocity reversal beneath the clay lens, and when combined with a CPT sounding that confirmed the undrained shear strength profile, the design team had the confidence to adopt a site-specific response spectrum instead of the conservative default. We deploy 24-channel or 48-channel linear arrays with 4.5 Hz geophones, processing the dispersion curve through fundamental and higher-mode inversion to extract a reliable 1D shear wave velocity column down to 30 metres. The output integrates seamlessly with NEHRP site classes A through E and the NBCC site classification tables, giving the structural engineer the parameters needed for modal analysis. In Saguenay, where post-glacial silts can mask competent rock within a few metres, the method's non-invasive nature also avoids disturbing sensitive clay fabric that could trigger retrogressive slides during drilling.
MASW / VS30 Testing in Saguenay: Shear Wave Velocity for Seismic Site Classification
Technical reference image — Saguenay

Area-specific notes

At a six-storey residential development on Boulevard Talbot, the initial geotechnical boreholes suggested competent till, but the developer questioned why two adjacent buildings of similar age had shown completely different damage patterns during the 1988 event. Our MASW line revealed a buried channel filled with soft estuarine sediment that the borehole grid had missed entirely—a discovery that led to targeted Improvement before the foundation pour. Skipping the shear wave velocity measurement in Saguenay is a gamble on soil continuity that the post-glacial stratigraphy simply does not honour. When the seismic hazard combines a short epicentral distance with site amplification in soft soils, the structural ductility demands can exceed what the original reinforcement detailing provides, and the cost of retrofitting later dwarfs the investment in a proper dynamic site characterization today.

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Reference parameters


ParameterTypical value
Array length46 m to 92 m (24 or 48 geophones)
Geophone frequency4.5 Hz vertical component
Source type10 kg sledgehammer or accelerated weight drop
Maximum investigation depth30 m (standard VS30, extensible to 45 m)
Dispersion processingFrequency-wavenumber (f-k) and SPAC
Inversion algorithmFundamental + higher-mode joint inversion
Output parameterVS30, VS profile, NEHRP / NBCC site class
Applicable standardASTM D4428 / D7400, NBCC 2020

Linked services

01

VS30 Site Classification

Active and passive MASW acquisition processed to deliver the average shear wave velocity in the upper 30 metres, classified per NBCC Table 4.1.8.4.A. Includes a signed engineering report suitable for permit submission.

02

Combined MASW + Refraction Tomography

Joint acquisition of surface-wave and P-wave refraction data along the same spread, providing both VS30 and a bedrock topography map for sites with complex overburden geometry.

03

Site-Specific Response Spectra

Collaboration with the structural engineer to translate the measured VS profile into a uniform hazard spectrum or site-specific design spectrum using equivalent-linear or non-linear ground response analysis.

Standards used


NBCC 2020 (National Building Code of Canada, seismic provisions), ASTM D4428 / D7400 (crosshole and surface-wave seismic testing), CSA A23.3-19 (concrete structures, seismic ductility requirements)

Quick answers

What does a MASW / VS30 survey cost for a typical Saguenay building site?

For a standard VS30 determination on a single-family or small commercial lot in the Saguenay region, the fee typically ranges from CA$2.440 to CA$3.740 depending on array length, site access, and whether passive-source recording is needed to reach the full 30-metre depth. We provide a fixed-price proposal after reviewing the site location and any existing borehole data.

How does the Saguenay soil affect the seismic site class?

The Laflamme Sea clays and interbedded silts that dominate the low-lying areas of Chicoutimi and Jonquière often produce VS30 values in the 180 to 300 m/s range, placing them in Site Class D or E. However, where glacial till or bedrock lies within a few metres of the surface—common on the terraces and toward Laterrière—the measured VS30 can exceed 360 m/s and qualify for Site Class C, which significantly reduces the design base shear.

Can you perform the survey on a site with existing structures or limited space?

Yes. While the ideal setup uses a straight 46-metre or 92-metre line, we adapt the array geometry for constrained urban lots in Saguenay by using shorter spreads combined with passive microtremor recording and the SPAC method. This hybrid approach lets us extract a reliable dispersion curve even when the available clearance is under 20 metres, provided we have enough ambient noise to process the low-frequency band passively.

Location and service area

We serve projects across Saguenay and surrounding areas.

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