Specifying a friction pendulum system without verifying the near-surface shear wave velocity against the Ohio State Seismic Zone 1 design spectra is a recurring mistake in Columbus. ASCE 7-22 Section 17.3 requires a site-specific probabilistic seismic hazard analysis when Site Class D or E governs, which is common in the Scioto River valley. We see isolation periods tuned to generic 1.0-second spectral accelerations that miss the amplification peaks in the 0.2–0.5 s range produced by the local glacial till and lacustrine clay sequence. A geophysical campaign with MASW profiling to 30 meters resolves the Vs100 and Vs30 needed to classify the site correctly per IBC 2024 Table 1613.2.3, and the data feeds directly into the upper- and lower-bound isolator property definitions for the bounding analysis. Without this step, the design engineer is iterating on a target period that may not match the soil column response at the project coordinates — 39.3321°N, 84.3509°W.
A one-size isolation period tuned to ASCE 7 mapped values can miss the local amplification spike that the glacial till column produces between 0.3 and 0.6 seconds in Columbus.
