The alluvial fans descending from the Sierra Nevada define Fresno's subsurface: silty sands, sandy silts, and the occasional hardpan layer that surprises contractors every season. With a shallow groundwater table barely 15 to 30 feet below downtown and summer temperatures that routinely exceed 100°F, moisture swings in the subgrade are not a textbook scenario here — they are the daily reality. A standard soaked CBR test run in a Fresno laboratory captures exactly this behavior, revealing how much strength the formation loses when it saturates after a wet winter. We complement that soaked value with unsoaked runs to bracket the range, and when the project sits on older terrace deposits we often pair the CBR with a grain-size distribution curve to confirm fines content before locking in the pavement structural number.
A soaked CBR value under 3% on a silty subgrade means the pavement section must either be thickened or the subgrade replaced — there is no middle ground in Fresno's shrink-swell regime.
