Columbus sits on a complex glacial till plain. The soils shift dramatically across the city—from lean clays near the Scioto River to silty deposits up toward Worthington. These subtle transitions wreck foundations when nobody checks the plasticity. We run Atterberg limits on every sample that shows fines. It’s not optional here. The high seasonal moisture variation in Franklin County means your subgrade needs a quantified PI before any pavement design. A grain size analysis pairs with the limits to classify the material per USCS and confirm the AASHTO group. That’s the only way to know if the clay will pump water into your base course come March.
A PI above 25 in Columbus glacial till signals high shrink-swell potential—ignore it and the slab will telegraph every weather event.
