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MASW and VS30 Testing in Lévis for Seismic Site Classification

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A six-storey residential project on the bluffs above the St. Lawrence taught a hard lesson about Lévis soil assumptions. The developer had standard boreholes but the city requested a site-specific shear wave profile before permit. We ran a 69-meter MASW line across the parking area, right where Champlain Sea silts transition into the underlying glacial till. The VS30 came back at 210 m/s — site class E, not the class D they had penciled in. That shift changed the seismic base shear by nearly 35 percent under NBCC 2020. For design teams working on the South Shore, skipping the seismic refraction survey or assuming a default class can lead to structural redesigns nobody budgeted for. Our approach combines active-source MASW with the NEHRP VS30 calculation protocol, giving you a defensible number that the municipality accepts without back-and-forth.

Lévis bluffs can mask a soft Champlain Sea clay layer that drops VS30 below 180 m/s — missing it means designing a building for the wrong earthquake forces.

Process and scope

Lévis sits in a moderate-to-high seismic zone with a 2% in 50-year spectral acceleration around 0.42g at the bedrock level. That number means nothing without the site amplification factor, which depends entirely on the top 30 meters of stratigraphy. The old city core, built on compact till and shale bedrock, often grades as site class C. But the suburbs spreading into old agricultural land near Saint-Romuald or Pintendre sit on 15 to 25 meters of soft silty clay — classic class E territory, sometimes pushing class F where the clay is thicker than 30 meters. We run a 24-channel system with 4.5 Hz geophones and a 10-kg sledgehammer source, processing with the multichannel analysis of surface waves algorithm. The dispersion curve gets inverted to a 1D shear wave velocity profile, and we cross-check with grain size data from nearby boreholes when available to confirm the stratigraphic boundaries in the inversion model.
MASW and VS30 Testing in Lévis for Seismic Site Classification
Technical reference image — Levis

Local ground factors

Lévis grew in two distinct chapters. The old shoreline settlement hugged the escarpment on dense glacial till, where seismic amplification is modest. Post-1960s expansion pushed south into the former Champlain Sea basin, where thick sensitive clays dominate. That shift created a split seismic personality for the city. A project on the plateau can hit site class C, while a junior high school two kilometers inland might sit on class E with a fundamental period near 1 second — exactly where four-to-eight-storey buildings resonate. The 1988 Saguenay earthquake, though distant, reminded Quebec engineers that eastern Canada's intraplate events propagate efficiently through the Canadian Shield. Site effects in Lévis can amplify those long-period motions significantly. The NBCC 2020 now requires site-specific shear wave velocity where the default class is uncertain, and municipalities on the South Shore have been enforcing that clause more rigorously since 2021.

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Technical data

ParameterTypical value
Array configuration24-channel, 2 m spacing
Source type10 kg sledgehammer + plate
Geophone frequency4.5 Hz vertical-component
Max investigation depth35-40 m (active source)
VS30 calculationNEHRP travel-time method
Site class outputNBCC 2020 classes C, D, E, F
Typical survey time2-3 hours per line

Related services

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Site-specific VS30 profiling

Active-source MASW with 24-channel acquisition, dispersion analysis, and inversion to 1D shear wave velocity. Delivers NBCC site class (C through F) and the VS30 value in m/s for the structural engineer's seismic design package.

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Combined geophysical and geotechnical campaign

MASW lines paired with SPT boreholes or CPT soundings to constrain the inversion model with measured stratigraphy. Especially useful where Champlain Sea clays are interbedded with silt lenses that create ambiguous dispersion curves.

Applicable standards

NBCC 2020 (National Building Code of Canada), CSA A23.3-19, ASTM D7400 (downhole seismic testing reference), NEHRP VS30 protocol

Frequently asked questions

What does a MASW survey cost in the Lévis area?

For a single MASW line with VS30 calculation and NBCC site class determination, budgets typically fall between CA$2,500 and CA$4,210. The range depends on the line length, access constraints (sloped lots, wooded areas), and whether we need to run multiple arrays to reach the full 30-meter depth. If the survey is combined with SPT drilling or CPT soundings, the per-line cost drops because mobilization is shared. We provide firm quotes after reviewing the site plan and surficial geology map — no surprises after mobilization.

Which NBCC site class applies to my Lévis property?

We cannot tell you without measuring. Lévis spans site classes C through E, with pockets of F where the soft clay exceeds 30 meters. The bluffs near the river are typically class C (glacial till over shale). The inland neighborhoods south of Autoroute 20 lean toward class D or E depending on the thickness of Champlain Sea deposits. The only way to know is to run a MASW line and compute VS30. Guessing or using the default site class E per NBCC often overestimates seismic loads and inflates structural costs unnecessarily.

How long does the MASW testing take on site?

Fieldwork for a single MASW line takes about two to three hours, including setup, calibration shots, and the actual acquisition. Processing and inversion back at the office adds a couple of business days. The final report with the VS30 profile, dispersion curve, and NBCC classification is typically delivered within five to seven business days of the survey date. Rush processing is available for tight permit deadlines.

Do you need boreholes to run MASW?

No, MASW is a standalone surface method. The geophones are planted at the ground surface and the energy source is a sledgehammer — no drilling required. That said, having a borehole log nearby makes the inversion more solid because we can anchor the velocity model to known layer boundaries. For critical structures in Lévis on suspected class E or F sites, we often recommend pairing MASW with at least one SPT borehole to satisfy the geotechnical reviewer.

Is MASW accepted by the Ville de Lévis for building permits?

Yes, as long as the report is stamped by a Quebec-licensed professional engineer and follows the NBCC 2020 site classification framework. The city's urban planning department does not prescribe a specific geophysical method; they require a defensible VS30 value and the corresponding site class. MASW is widely accepted because it directly measures shear wave velocity over the full 30-meter profile, unlike proxy methods that estimate it from blow counts.

Location and service area

We serve projects in Levis and surrounding areas.

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