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

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The ground shifts fast when you move from the riverfront alluvium near the St. Clair toward the dense till east of Oil Heritage Drive. In one Sarnia neighborhood, a shallow trench hits sandy silt at half a meter; three kilometers south, the same depth bottoms out in stiff, overconsolidated clay that hasn't seen daylight in ten thousand years. That contrast is exactly why generalized site classes fall apart here. The seismic microzonation research done across southwestern Ontario shows that a single postal code can straddle Site Class C and Site Class E, which changes the seismic demand on a structure by a factor of two or more. Our MASW survey maps shear wave velocity directly across the footprint of the project, giving the structural engineer a VS30 value that holds up under NBCC 2020 review instead of the default assumption that often overestimates soil stiffness in Sarnia's lacustrine deposits.

A VS30 value derived from MASW replaces the code-default travel-time assumptions with measured stiffness data, often moving a Sarnia site up one NBCC class and saving foundation concrete.

Process and scope

We recently ran a profile behind a chemical storage facility off Vidal Street where the client had assumed competent hardpan below three meters. The linear array of 24 geophones picked up a low-velocity trough at twelve meters depth—buried channel fill from a post-glacial drainage course that didn't show up in any borehole log. That kind of blind spot is common in Sarnia because the shallow stratigraphy mixes stiff clay crusts with softer, normally consolidated layers left by glacial Lake Warren. The active-source MASW setup we deploy uses a 10-kg sledgehammer on a reinforced strike plate, generating Rayleigh waves that are recorded across the spread and processed through dispersion analysis using the multichannel approach outlined by Park et al. The resulting one-dimensional VS profile resolves velocity inversions that refraction alone would miss. When the geophone spacing is tightened to 1.5 meters, we achieve resolution down to 20 meters depth, which covers most foundation bearing strata in the region. The data feeds directly into the site-specific response spectrum that the liquefaction assessment requires if silty sand layers are present near the groundwater table, which sits high in the floodplain zones.
MASW / VS30 Testing in Sarnia: Shear Wave Velocity for Site Classification
Technical reference image — Sarnia

Local ground factors

The Ontario Geological Survey maps show the Sarnia area underlain by glaciolacustrine clays and silts that can vary from soft to very stiff over distances of fifty meters. When a structural design relies on the default Site Class D without measured shear wave velocity, the resulting base shear calculation may be off by 30%, either overspending on lateral systems or underestimating seismic demand. A VS30 value below 180 m/s puts the site into Class E territory, triggering a higher design spectrum that affects everything from footing dimensions to drift limits in steel moment frames. We have seen this exact situation on expansion projects near the chemical valley, where the combination of high water table and compressible clay layers created a velocity profile that conventional SPT blow counts alone did not flag. The NBCC 2020 commentary is explicit: where more than 3 meters of soft clay overlie bedrock, site-specific shear wave velocity measurement is the preferred method for classification over N-value proxies.

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Technical parameters

ParameterTypical value
Source typeActive (10 kg sledgehammer) with 24-channel seismograph
Array length46 m to 69 m, adjustable per target depth
Depth range investigated20 m to 30 m below grade in typical Sarnia soil conditions
Frequency bandwidth recorded5 Hz to 80 Hz, 4.5 Hz geophones
Output parameterVS30, VS profile, fundamental site period (T0)
NBCC site class resolvedClasses C, D, and E differentiated by measured VS30
Acquisition time for one spreadApproximately 45 minutes, including setup and calibration

Associated technical services

01

MASW Line Survey (Single Spread)

One 46-meter linear array yielding a 1D VS profile and VS30 value for a single building footprint. Suitable for NBCC site classification on lots under 2,000 m².

02

Multi-Line MASW for 2D Cross-Sections

Three to five parallel spreads processed into a 2D shear wave velocity cross-section, revealing lateral variation across larger industrial parcels in Sarnia's heavy manufacturing zones.

03

Combined MASW and Seismic Refraction

Joint acquisition using the same geophone spread to capture both P-wave refraction and Rayleigh wave dispersion, providing a layered stiffness model with Poisson's ratio estimates.

04

VS30 Report for Permit Submission

Stamped report with processed dispersion curves, inversion parameters, VS profile plots, and the computed VS30 value formatted for municipal building permit review under the Ontario Building Code.

Applicable standards

NBCC 2020 (National Building Code of Canada, seismic provisions), CSA A23.3 (Design of concrete structures, seismic clauses), ASTM D7400 / D4428 (crosshole and surface wave methods referenced in geophysical procedure)

Quick answers

How much does a MASW survey cost for a standard lot in Sarnia?

For a single-spread MASW survey on a residential or small commercial lot in Sarnia, the fee ranges from CA$2,540 to CA$4,790. The final quote depends on array length, number of spreads, and whether we combine the acquisition with other geophysical methods during the same mobilization.

Does the NBCC require VS30 measurement for all building permits?

The NBCC 2020 permits default site classification based on soil type and standard penetration resistance, but the commentary encourages site-specific shear wave velocity measurement when more than 3 meters of soft clay or loose sand is present. Given Sarnia's glaciolacustrine stratigraphy, many structural reviewers now request measured VS30 to justify the seismic design parameters.

How long does it take to get the final VS30 report?

Field acquisition for one or two spreads is completed in a single day. The dispersion analysis and inversion modeling require two to three business days afterward, and the stamped report is delivered by the end of the week under normal scheduling.

Can MASW be done on a paved parking lot or inside an existing building?

Active-source MASW needs direct geophone coupling to the ground, so pavement must be cored or a soil patch prepared for each sensor. Inside operating facilities, vibrations from machinery can degrade the dispersion image; we schedule acquisitions during shutdowns or use nighttime windows to minimize ambient noise.

Location and service area

We serve projects in Sarnia and surrounding areas.

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