Working in Pomona, where the alluvial fans from the San Jose Hills meet the younger sediments of the Pomona Valley, we consistently encounter a mix of sandy loams and gravelly deposits that make compaction verification non-negotiable. A driveway poured on loosely placed fill over these old creek beds can show distress within two seasons. Our team performs field density tests using the sand cone method to confirm that every lift of backfill meets the specified relative compaction before concrete or asphalt is placed, integrating the results with Atterberg limits to understand how the fine fraction of the soil will behave when moisture fluctuates during Southern California's dry summers and occasional intense winter rains.
In the decomposed granite soils common across Pomona, achieving 95% relative compaction often requires moisture conditioning within a narrow 2% window.


