Working in Lexington, you quickly learn that the ground beneath your feet changes dramatically from one drainage basin to the next. The deep alluvial deposits along the Kentucky River corridor bear little resemblance to the stiff, often cherty residual clays draped across the Inner Bluegrass plateau. At our lab, we have seen preliminary SPT refusal at 4 feet in the Hamburg area while, less than six miles southwest near the river, sandy silts extend past 30 feet with groundwater at 8 feet. That contrast matters enormously when a seismic event triggers excess pore pressure. Our liquefaction analysis quantifies factor of safety against triggering using site-specific cyclic stress ratios, corrected blow counts from ASTM D1586, and fines content from wash-sieve procedures, giving the design team a clear picture of post-earthquake settlement potential before a single footing is poured.
In Lexington's alluvial corridors, a factor of safety below 1.1 can mean the difference between serviceable settlement and a total loss of bearing capacity within seconds of shaking.
