← Home · Seismic

Seismic Microzonation in Regina: Soil Response and Ground Motion for Safer Design

Together, we solve the challenges of tomorrow.

LEARN MORE →

Regina sits on a deep sequence of glaciolacustrine clays and tills within the Bearpaw Formation—materials that amplify ground motion in ways generic NBCC values cannot capture. The city’s seismic hazard is modest but real, driven by intraplate events east of the Rockies. A site-specific seismic microzonation study maps the spatial variability of peak ground acceleration, spectral response, and soil fundamental period across a property. We integrate MASW surveys to measure Vs profiles down to 30 metres, then feed that data into 1D equivalent-linear site response models. The result is a set of design spectra that reflect actual stratigraphy—not just a conservative envelope. For engineers working under Part 4 of the National Building Code, this level of detail supports performance-based design and avoids overdesigning foundations or underrepresenting short-period amplification in soft clay.

A site class boundary can shift within a single lot on Regina's lake plain—microzonation catches that before the concrete does.

Methodology and scope

In Regina, we often see a misleading assumption: that uniform soil class C or D applies across an entire site. It rarely does. A glacial lake plain like this one conceals lateral transitions—from high-plasticity lacustrine clay to dense till—within tens of metres. Seismic microzonation work here must start with a dense grid of shear-wave velocity measurements, typically using MASW or downhole methods, then layer in borehole data to constrain material damping curves. We correlate Atterberg limits and SPT N-values with modulus reduction behaviour using published curves for Canadian clays. The output includes maps of PGA amplification factor, T0 (site period), and spectral acceleration at 0.2s and 1.0s. A CPT test can be added to refine the stratigraphic boundary between soft clay and underlying till, which directly controls impedance contrast and amplification potential. The final deliverable is a set of design spectra per zone, ready for structural input, and a report that satisfies the geotechnical review requirements of local building officials.
Seismic Microzonation in Regina: Soil Response and Ground Motion for Safer Design
Technical reference image — Regina

Local geotechnical context

Regina’s growth through the 20th century followed the rail lines and the flat prairie grid—not the subsurface. Many older commercial and institutional buildings were sited on what was convenient, not on what was geotechnically homogeneous. The risk today is that a uniform seismic design assumption applied to a variably thick clay deposit can produce two very different structural responses under the same ground motion. Short-period amplification in soft clay can increase spectral accelerations well above the NBCC’s default site class values, especially where the depth to till changes abruptly. We have seen this in post-construction reviews on the city’s east side, where clay thickness varies from 5 to 15 metres across a single block. A seismic microzonation study identifies these transitions before design locks in, allowing structural engineers to adjust base shear, drift limits, and detailing requirements per zone. Ignoring this step means the building code is being applied with incomplete site data—and the difference can show up as unexpected damage in a moderate event.

Need a geotechnical assessment?

Reply within 24h.

Email: info@geotechnicalengineering.vip

Explanatory video

Typical values

ParameterTypical value
Vs30 (shear-wave velocity)Measured via MASW or downhole, classified per NBCC Table 4.1.8.4.A
Site ClassA through E, mapped spatially across the property
PGA amplification factorRatio of surface PGA to reference rock PGA, per NBCC 2020
Spectral acceleration Sa(0.2s)Mapped for short-period structures
Spectral acceleration Sa(1.0s)Mapped for mid-rise and taller structures
Fundamental site period T04H/Vs, verified via HVSR where applicable
Design spectra per zone1D site response output (SHAKE or DEEPSOIL), CSA A23.3 compliant

Related services

01

Site-Specific Seismic Hazard & Response Analysis

Field measurement of Vs profiles using MASW and downhole methods, combined with 1D equivalent-linear or nonlinear site response modelling. Deliverables include mapped PGA amplification, spectral acceleration contours, and design spectra per NBCC 2020 for each microzone identified on site.

02

Soil Dynamic Properties & Laboratory Testing

Resonant column and cyclic triaxial testing on undisturbed Shelby tube samples from key stratigraphic units. We derive modulus reduction and damping curves specific to Regina's glaciolacustrine clays, replacing generic literature curves with project-specific data for higher-confidence response analysis.

Applicable standards

NBCC 2020 (National Building Code of Canada, Part 4 – Structural Design), CSA A23.3:19 (Design of Concrete Structures – seismic provisions), ASTM D7400 / D4428 (MASW and crosshole seismic testing), ASTM D5778 (CPT for stratigraphic correlation in site response)

Common questions

What is the difference between a seismic hazard map and a microzonation study?

A seismic hazard map like Canada's national model provides uniform hazard spectra for reference rock conditions over a grid. A microzonation study takes that rock motion and propagates it through the actual soil column at your site, accounting for stratigraphy, Vs profile, and dynamic soil properties. The result is a site-specific spectrum that can differ significantly from the default NBCC site class values—especially in a city like Regina where clay thickness varies over short distances.

How is seismic microzonation used in structural design?

The design spectra from a microzonation study feed directly into the structural analysis. Rather than using the generic acceleration values from NBCC Table 4.1.8.4, the structural engineer applies the site-specific Sa(0.2s) and Sa(1.0s) values for each building zone. This supports more accurate base shear calculations, drift checks, and detailing under CSA A23.3, and can reduce unnecessary conservatism where soil conditions are more favourable than the default site class suggests.

What field methods do you use to measure shear-wave velocity in Regina?

Our primary tool is MASW (Multichannel Analysis of Surface Waves), which produces a continuous Vs profile down to 30 metres without drilling. On larger or more complex sites we supplement with downhole seismic testing in boreholes to verify the MASW results at depth. For sites with very soft near-surface clay, we may also run HVSR measurements to corroborate the fundamental site period. All testing follows ASTM D7400 and D4428.

What does a seismic microzonation study cost for a site in Regina?

Cost depends on site area, number of measurement points, and whether laboratory dynamic testing is included. For a typical commercial or institutional site in Regina, a complete microzonation study with MASW, site response modelling, and a design spectra report generally ranges from CA$5,130 to CA$21,750. We provide a fixed-fee proposal after reviewing your site plan and project requirements.

Location and service area

We serve projects in Regina and surrounding areas.

View larger map