That's an interesting question. My initial reaction is to say no, the overlying water isn't relevant at all, but then I thought that if the velocity at the soil surface is high enough the viscosity of the water might have some effect, perhaps increasing CSR a little because some of the water gets dragged along by the soil? I sure don't know how I would quantify it without a research project, but I think the effect would be small, based on no actual data or analysis. (Data without theory are trivia; theory without data is bull$#!+.)
I would start out with the simplifying assumption that the water is "soft" - so the cyclic stress would come only from the total mass of the solid soil below the mudline. (I say "mass" because total overburden stress is used in the simplified equation as a proxy for mass in f=ma, so we don't need to figure out slugs and pound forces and all that. Maybe if HBS had been working in a metric country, it would have come out looking different. rd is sometimes called the mass participation factor - how much of the mass of overlying soil participates in f=ma?)
Strictly speaking, the total overburden stress includes the weight of the free water above the mud line (sigma=sigma'+u), but the simplified equation only makes sense if you consider the total overburden stress to represent the mass that gets accelerated by the cyclic stress on the base of a layer.
Any other ideas?
Cheers!
DRG
PS: Does Firestone ever make it down your way from Paso Robles? A friend passing through CO left me with a sampler case that included their summer ale (which I liked), and their Double Barrel Ale, which I really liked. Their IPA was a bit too hoppy for my liking, so I'll save it for you if you'll be here soon.