Des Moines grew up along the confluence of the Des Moines and Raccoon Rivers, and much of its early expansion spread across the broad floodplain that now underlies the downtown core. That legacy of alluvial deposition means the ground beneath our city’s buildings is far from uniform—layers of soft clay, loose silts, and buried sand lenses are common within the first 30 meters. Base isolation seismic design in Des Moines starts with a clear picture of that subsurface variability, because an isolator is only as reliable as the soil it sits on. Our laboratory team runs the full suite of index and dynamic tests on samples pulled from borings across Polk County, so that the stiffness and damping parameters fed into isolation models reflect the actual stratigraphy. When the project sits near the river or on glacial till in the western neighborhoods, we often recommend pairing the lab campaign with a MASW survey to capture Vs profiles and confirm the site class before finalizing the isolator properties.
The dynamic shear modulus of the Des Moines lobe till can vary by a factor of two across the metro—generic profiles don't work here.
