As I recall, George Sowers developed the dynamic cone penetrometer (DCP) test while working as an engineer for Law Engineering and serving as a professor at Georgia Tech. The SPT correlations that are provided with the DCP equipment are likely related to his work in Piedmont residual soils encountered through much of Georgia and the Carolinas and further up the east coast. It is reasonable to expect that similar correlations could be developed in other geologic settings. According to Sowers, the DCP is suited for construction control and field exploration for lightweight structures. In general, the penetrometer produces the best correlations between 4 and 30 blows. Below 4 blows, for the required 1-3/4 inch penetration increment, the soils are too soft or loose to produce significant results. Above 30 blows per penetration increment the correlations are quite variable.
The DCP does not work well below the water table unless the borehole is stabilized to prevent inflow and soil softening. The DCP is of limited use in evaluating alluvial soils of Piedmont or Blue Ridge origin (which includes the Upstate of South Carolina and western North Carolina) in that the calibration ratios vary without specific pattern.