Oklahoma City's expansion from the 1889 Land Run into a sprawling metropolitan area of over 620 square miles has placed immense pressure on its underlying geology, particularly the Quaternary alluvial deposits along the North Canadian River. Many commercial and industrial developments now occupy land underlain by loose, poorly graded sands (SP) and low-plasticity silty sands (SM) that are highly susceptible to settlement. When structural loads exceed the tolerable bearing capacity of these native soils, vibrocompaction design becomes an essential ground improvement strategy. Our technical team evaluates the gradation envelope per ASTM D2487 to confirm suitability for deep vibratory densification, a method that has proven effective in the sandy lenses found at depths between 15 and 40 feet throughout the Oklahoma River corridor. A thorough grain size analysis often reveals the fines content that dictates whether vibrocompaction will achieve the specified relative density without excessive pore pressure buildup.
Effective vibrocompaction design in Oklahoma City hinges on distinguishing between true alluvial sands and residuum derived from the Garber-Wellington Formation, a nuance that directly impacts probe penetration and grid spacing.
