Madison’s winter freeze-thaw cycles can destroy an asphalt pavement in three seasons if the subgrade isn't accounted for. The city sits on glacial till and lacustrine deposits, with a frost depth reaching 48 inches per WisDOT regional tables. Designing a flexible pavement here means balancing the structural number against a subgrade that loses strength every March. Our approach integrates AASHTO 1993 mechanistic-empirical procedures with local climate data from the Dane County Regional Airport weather station. We model the resilient modulus drop during the spring thaw, when the base course saturates and the subgrade CBR can fall below 3%. For projects near the Yahara chain of lakes, we also account for a perched water table that shortens the drainage path. Before finalizing layer coefficients, it’s common practice to verify in-situ density with the sand cone method on test strips, ensuring compaction meets the 95% modified Proctor target.
A Madison pavement lives or dies by its drainage design—granular base daylighted to a free-draining outlet adds more years than an extra inch of asphalt.
