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HomeGeophysicsMASW / VS30 (velocidad de ondas de corte)

MASW / VS30 Testing in Baltimore – Seismic Site Classification

Under ASCE 7-22 and IBC 2021, every structure in Baltimore must be assigned a seismic site class based on VS30 measurements of the upper 100 feet. The city's coastal geology — a mix of Pleistocene terrace deposits, alluvial silts, and deep Cretaceous clays — produces shear wave velocities that vary sharply within a single block. MASW (Multichannel Analysis of Surface Waves) captures that variability by recording Rayleigh wave dispersion along a 2D array, yielding a continuous 1D or 2D velocity profile without boreholes. This non-invasive method is especially relevant in Baltimore, where buried stream channels and filled tidal marshes create velocity inversions that a single SPT blow count would miss. A reliable VS30 value supports seismic design of foundations, retaining walls, and pile-supported structures in the Inner Harbor and Fells Point districts.

Illustrative image of MASW / VS30 (shear wave velocity) in Baltimore
A single MASW profile can resolve velocity inversions hidden by SPT alone, critical for sites on Baltimore's filled tidal marshes.

Method and coverage

Baltimore's urban development since the 18th century has heavily modified its original topography. Landfills, wharf extensions, and railway embankments have buried the natural soil profile under variable fill layers that can exceed 6 meters in depth. A MASW survey in such areas must deploy a 24-channel geophone spread with 3-meter spacing to resolve the velocity contrast between loose anthropogenic fill (VS around 180-250 m/s) and the underlying Pleistocene sand (VS 350-500 m/s). The method's depth of investigation often reaches 35 meters, enough to characterize the stiff clay layer that controls bearing capacity for deep foundations. When combined with a borehole SPT for calibration and a sand cone density test on the fill cap, the team can validate the inversion model against measured unit weight and blow counts. This hybrid approach reduces uncertainty in the VS20-VS30 interval that governs the site class boundary between D and C.

Regional considerations

Compare two blocks in Canton — one over natural Pleistocene sand (VS30 ~400 m/s, site class C) and another only 200 meters away over a filled former ship slip (VS30 ~240 m/s, site class D). A building designed with the same seismic base shear on both would be under-designed on the fill. The difference stems not from soil strength but from shear wave velocity: softer sites amplify long-period motions more severely. For downtown Baltimore, where many structures are 10+ stories on spread footings, misclassifying the site can lead to dangerous underestimation of drift demands. A focused MASW line across the property boundary catches the transition, allowing the structural engineer to adjust the response spectrum coefficient (Fa, Fv) per ASCE 7 Table 11.4-1.

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Standards that apply


ASCE 7-22 – Seismic site classification per Chapter 20, ASTM D4428 – Standard Test Methods for Crosshole Seismic Testing, NEHRP Recommended Seismic Provisions (FEMA P-1050), IBC 2021 – Site class requirements in Section 1613

Related services

01

2D MASW Profile

Single-line roll-along survey for linear infrastructure, foundation footprints, or site-wide seismic classification. Includes dispersion curve picking and inversion to 35 m depth.

02

1D VS30 Measurement

Targeted 1D profile at a single geophone array for quick site class determination. Ideal for small projects or as a complement to existing boreholes.

03

MASW + SPT Integration

Combined field campaign where MASW lines are calibrated against SPT N-values and lab-measured unit weights. Provides both velocity and strength data for foundation design.

04

Liquefaction Screening (VS-based)

Using the MASW velocity profile to evaluate cyclic resistance ratio (CRR) per Youd et al. (2001). Outputs a factor-of-safety map for loose to medium sands in Baltimore's coastal areas.

Typical parameters


ParameterTypical value
Array length72 m (24 channels x 3 m spacing)
Frequency range4.5 Hz – 40 Hz (Rayleigh wave)
Depth of investigation25–35 m typical; up to 50 m with larger spread
VS30 uncertainty±15% after inversion (Monte Carlo)
Standard complianceASTM D4428 / NEHRP site class criteria
Field crew size2 technicians + 1 geophysicist

Common questions

How is MASW different from the seismic CPT or downhole method?

MASW uses surface waves (Rayleigh waves) recorded by a linear geophone array, providing a 2D velocity profile over a depth of 25–50 m without a borehole. Seismic CPT and downhole methods require a pre-drilled hole and measure P and S waves only at discrete depths. MASW is faster and cheaper for large areas, while CPT gives continuous tip resistance alongside velocity.

What VS30 values are typical for Baltimore's different neighborhoods?

In areas with deep Pleistocene sand and gravel (e.g., Roland Park, Mount Washington), VS30 often exceeds 400 m/s, placing them in site class C. Downtown and the Inner Harbor, where fill over soft clay is common, typically yield VS30 between 200 and 300 m/s (site class D). The transition can be abrupt, so a single MASW line is recommended per 0.5 acre parcel.

How long does a MASW survey take on a typical Baltimore site?

For a standard 72 m array with 24 geophones, field deployment and data collection take about 2 hours. Inversion processing and report generation require another 2–3 working days. Total turnaround for a single profile is 5–7 business days from mobilization.

Do I need a MASW survey if I already have SPT boreholes?

SPT blow counts do not directly measure shear wave velocity. ASCE 7 allows site class assignment based on SPT N-values only for site class A through D, but the correlation is weak. MASW provides the VS30 value required for accurate Fa and Fv factors, and it can detect velocity inversions (e.g., loose fill over stiff clay) that SPT alone may miss. For Baltimore's filled waterfront sites, MASW is strongly recommended.

Location and service area

We serve projects across Baltimore.

Location and service area