The contrast between the decomposed granite slopes of Phillips Ranch and the deep alluvial deposits near the 71 Freeway is significant. In Phillips Ranch, you might find weathered bedrock within five feet. Down by the Fairplex, you can drill twenty feet and still be in silty sand. This variation across Pomona means a standard pavement section rarely works. We see joints faulting in industrial parks because the base saturation wasn't modeled correctly, or curling cracks on bus pads where the concrete mix didn't account for the valley's 40-degree diurnal temperature swing. A rigid pavement design here has to start with the subgrade, not the slab. We rely on our test pits to visually log the stratification, then pull undisturbed samples for lab analysis. For heavily loaded corridors, we also correlate findings with CPT soundings to catch soft lenses that a boring might miss.
A rigid pavement's service life is determined before the first pour. Get the k-value wrong on Pomona's alluvial fans and you are designing a replacement, not a road.



