This is part of a response I've just posted in the Soil Testing Section under "Machintosh, DCP, CPT." It sort of relates to this thread too:
I’ve done some work with our DCP in our area to provide us with a correlation of the DCP blow counts with the soil density, and as a comparison to the SPT values. Our soils in Northern Michigan are generally water deposited, fine to medium quartz sands at many locations. Other organic deposits (Lake Marl, Muck, Peat) and clay deposits exist, but much of the area is the sand described above.
I’m not sure what the difference between our DCP and the Mackintosh probe are, but our DCP uses a 15lb weight falling 20 inches, advanced 1.75” at a time. The cone angle is 45 degrees, slightly rounded at the end. A paper was completed by G.F. Sowers and C.S. Hedges “Dynamic cone for Shallow In-Situ Penetration Testing” ASTM STP 399, Am. Soc. Testing Mats., 1966, p 29. This paper also has some correlations of the DCP blows to SPT blows for various soils including piedmont soils in the south.
The testing I’ve done has included DCP’s performed adjacent to SPT’s, and DCP’s performed at various levels below the surface on a given site with excavation afterwards to those levels, and actual density testing with a nuclear gauge at the various levels. I’ve also obtained some bulk samples to determine limit densities and use the nuke gauge to determine the estimated relative density of the soil in-situ in some cases. In this way, I’ve been able to establish a few good correlations. The sites I chose were uniform in soil type and relatively uniform in soil density. Here are some of my main conclusions to date:
Overburden: approximately 1’ to 6’ below subgrade level:
Average DCP blows per 1.75” after seating increment Relative density
1-3 Very loose to loose
4-7 Loose to Medium dense
8-12 Medium dense to dense
>13 Dense to very dense
If blows are less than say 2, it is usually a good indication that there may be loosely placed imported fill, since most of the soils usually have a in-place RD of 40% or greater (meaning it is sometimes difficult to find natural soils with an RD less than 30-40% (in my experience) unless some major particle bulking is still occurring since deposition. As the relative density approaches 90-100%, the DCP blows tend to be very high (>30/increment or more). Additionally, the DCP is affected the same as the SPT when it comes to silty and very fine sands in that unrealistic values may result from dilative tendencies. Gravel influences the DCP blow counts by raising the values, similar to the SPT. The values are also influenced by the amount of overburden as with the SPT. I’ve found that if you’re 1’ to 6’ below subgrade, the effects are not very pronounced. If deeper DCP’s are made, you should think about an overburden correction similar to the SPT to arrive at a better indication of the in-place relative density. DCP’s below the groundwater table are usually not possible since an auger hole will not stay open as they would with drilling mud or hollow stem augers-this is one of the main limitations of the DCP in my opinion.
Please share your own findings too. I’d like to hear them. I hope some of this is useful to someone.