I've just come accross this thread and I have a quick note to add to the relationship mentioned by jdmm. Quite often I will schedule a whole series of relationships on soils where I will do MC vs CBR and MC vs Shear strength on the same samples. After reading the relationship noted by jdmm, I did a qucik check on some of the values I had got recently, and found that typically the range for Glacial Lake Deposits in the north of the UK were in the range of CBR = Su/15 to CBR = Su/17 for a range of samples tested prior to the earthworks (SI stage) and during the actual earthworks.
So in light of this, I would suggest that it is always worth checking out the relationship, and not relying soley on historical values, the difference between CBR = Su/23 and Su/15 would be fairly dramatic to the final CBR.