Abstract
The Cooper Marl is a massive geological group, consisting of stiff, cohesive calcareous soils, which serves as the bearing stratum for the large majority of deep foundations in the Charleston, South Carolina, area. It has long been recognized that piles driven into the material experience tremendous setup, or capacity gain with time. Numerous driven piles that bear within the Cooper Marl have been statically or dynamically tested at various times after installation. This pile-testing database has been used to backcalculate the coefficients of a logarithmic expression (
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