Hi jakeh76,
I see why you’re looking for minimum density now. I've never seen the equation form you show, but I think it's similar to one that provides an additional term onto the Ko=(1-sin(phi) term, which involves the OCR. The Ko of a compacted sand, at shallow depths, will usually be greater than simply (1-sin(phi)) due to the overconsolidation effect. This is assuming we are talking at rest. It appears that your equation provides a different way to estimate Ko of a soil that has been compacted, or one that has an OCR greater than unity. I still stand by my original recommendation and that is to run a minimum density test using ASTM D4254 (check on that # to be certain). The results of that test can be expressed in terms of dry density or moist density if required if you know the moisture content you're dealing with.
Since Focht3 has conditionally disagreed with what I said, I'll take a stab at explaining myself and clarifying what I said. I’m up for a challenge, I guess! Besides, it’s been a while since I was involved in a discussion! I think something just came out wrong when I said what I said, or the lines got cross somehow.
I think the problem with my original post was that instead of saying, "earth pressure coefficients are more dependent on friction angle than unit weights," I should have said, "earth pressure coefficients are more DIRECTLY dependant on friction angle than unit weights." And by “directly dependant” what I really mean is that “the unit weight is one of many variables required to arrive at a friction angle estimate for use in theoretical earth pressure relationships.” It is true that unit weights influence friction angle and earth pressures, but here’s why I think it’s confusing when you start talking about unit weight as a basis for earth pressures, or any other soil parameter. Here are three things to consider and probably none of them are new to us…
Soil density (unit weight, take your pick) alone explains nothing about the soil strength or compressibility characteristics of a soil. Two different soils can be at the same in place density, yet have different soil characteristics. This is because the soil characteristics depend on many other variables than simply "density." Example, “that soil has an in place density of 15kN/m^3.” Is that good? What are the friction angle, compressibility, and permeability? (Please note: I’ll catch myself now and state that friction angle itself is also dependant of type of failure, strain rate, plane strain vs. triax conditions, etc. before anyone else does!)
Relative density is a step forward toward providing a basis for soil characteristics and earth pressure estimated. If we know relative density, then at least we know where the soil's density falls between the min and max theoretical densities, right? However, talking about earth pressure with respect to relative density, solely, is also erroneous since, again, friction angle is dependent on many things-relative density being only one of them. What other things? Gradation, particle shape, mineral composition, etc. We know that.
When we break it down, simplify it, and just talk about friction angle (say drained friction angle for argument sake) we have taken a giant step forward in expressing a soil characteristic that can be used to solve theoretical problems, like estimating the earth pressure coefficients. A friction angle of 35 degrees, is a friction angle of 35 degrees regardless of the in-place density. It no longer matters. We’ve temporarily removed the “middleman” (intermediate variables required to develop the friction angle) in order to use a more direct parameter to solve the problem. The friction angle now represents the consideration of numerous variables involved in developing the friction angle parameter for use. That’s all I meant.