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MASW & VS30 Testing: Shear Wave Velocity for Seismic Site Class

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IBC Section 1613 and ASCE 7 Chapter 20 demand a shear wave velocity profile whenever you want to avoid the default Site Class D assumption in Oklahoma City. The financial penalty of that assumption can inflate foundation costs by 15 to 20 percent on mid-rise structures. Our active-source MASW survey uses a 24-channel land streamer with 4.5 Hz geophones and a 10-kg sledge source, delivering VS30 values in hours rather than the days required for downhole methods. The technique works well on the Quaternary alluvium along the North Canadian River corridor and equally on the Permian-age Garber Sandstone that outcrops across the northwest quadrant of the metro. We sample 30 to 40 meters of the velocity column, enough to satisfy the 100-ft requirement of the code and flag a soft layer that might require a liquefaction assessment before structural design proceeds.

A 10 percent drop in VS30 can shift site class from C to D, adding 20 percent to the design base shear on an Oklahoma City mid-rise.

Our service areas

Process and scope

The subsurface contrast between downtown Oklahoma City and the expanding suburbs around Lake Hefner illustrates the value of direct VS measurement. Downtown sits on Hennessey Shale, a stiff overconsolidated formation that can push VS30 above 500 m/s, often yielding Site Class C and lowering the seismic base shear demand. Move five miles northwest toward the lake, and the near-surface transitions to deeper residual clay with interbedded sandstone stringers, where VS30 values routinely fall between 300 and 450 m/s. In those zones, we couple the MASW line with CPT soundings because the cone resistance logs help separate stratigraphic boundaries that the phase-velocity dispersion curve suggests but cannot uniquely resolve. When the site straddles the transition between Site Class C and D boundaries, we also recommend a seismic refraction line to map the top of competent bedrock with P-wave arrivals, complementing the S-wave velocity model.
MASW & VS30 Testing: Shear Wave Velocity for Seismic Site Class
Technical reference — Oklahoma City

Local geotechnical context

Oklahoma City's building stock expanded rapidly after the 1940s, when the geology of the North Canadian floodplain was understood mainly through agricultural boreholes rather than geotechnical investigation. Many three- and four-story commercial buildings constructed before the adoption of the modern IBC sit on stiff clay that masks a deeper, weathered shale zone with reduced shear stiffness. MASW profiles we have acquired in the Midtown and Bricktown districts reveal a velocity inversion between 8 and 15 meters depth — a softer layer sandwiched between stiffer material — that a standard refraction survey cannot detect because refracted P-waves skip over low-velocity zones entirely. The inversion matters for site response: a 2D site response model using SHAKE or DEEPSOIL will show amplification at periods that coincide with the structural period of a six- to ten-story building. Ignoring that layer means underestimating spectral acceleration at the design period by 30 to 40 percent, a gap that the seismic microzonation framework in ASCE 7 is specifically designed to close through measured VS profiles.

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Applicable standards

ASCE/SEI 7-22 Chapter 20: Site Classification Procedure for Seismic Design, IBC 2021 Section 1613: Earthquake Loads – Site Class Definitions, ASTM D7400-19: Standard Test Methods for Downhole Seismic Testing (cross-reference for VS validation)

Technical parameters

ParameterTypical value
Source typeActive (10 kg sledge) with stacked impacts
Receiver array24-channel land streamer, 4.5 Hz vertical geophones
Spacing1.0 m or 2.0 m, adapted to target depth
Maximum investigation depth30–40 m below grade
VS30 outputTime-averaged shear wave velocity, upper 30 m
Dispersion processingMASWaves or Geometrics SurfSeis, fundamental mode
Site class per IBC/ASCE 7A through F based on measured VS30

Common questions

What does a MASW survey cost for a typical commercial lot in Oklahoma City?

For a single-family or small commercial parcel within the Oklahoma City metro, a complete active-source MASW survey with 1D VS profile, VS30 calculation, and signed engineering report typically falls between US$1,830 and US$3,190. The range depends on line length, number of spreads, and whether we need to trim vegetation or work around buried utilities. Sites in the alluvial corridor near the North Canadian River sometimes require longer spreads to reach the 30-meter target depth, which nudges the cost toward the upper end.

How does MASW compare to a downhole seismic test for site classification?

Downhole testing places a triaxial geophone in a borehole and measures direct arrival times, giving a high-resolution VS log at the cost of drilling a cased hole. MASW uses surface waves and inverts a dispersion curve to obtain a layered VS model without drilling. The trade-off is vertical resolution: downhole detects thin soft layers better, while MASW averages over a thickness of roughly one-half to one-third the wavelength. For most IBC site classification purposes, the VS30 from both methods agrees within 5 to 10 percent when the subsurface is laterally uniform, which is typical across the Hennessey Shale and Garber Sandstone formations that underlie most of Oklahoma County.

How long does the field work take, and will it disrupt site operations?

A single MASW spread with 24 geophones and a sledge source takes 45 to 90 minutes of active acquisition, plus setup and line layout. The crew works at ground level with no drilling mud, no casing, and no heavy equipment beyond a handheld hammer and a seismograph. We can work around light site traffic as long as the geophone line stays undisturbed during the stacking sequence. The raw data goes through dispersion analysis and inversion in the office, with the engineering report typically delivered within three to five business days after field completion.

Location and service area

We serve projects in Oklahoma City and surrounding areas.

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