Referencing the original post, you should expect heterogenous nature of subsurface conditions even if for a "stratum" that is "geologically" the same. We commonly complete designs for embankments and foundation elements in areas that may have N-value ranges from WOH to refusal. Many designers still approach situations like this using a "average" value approach, or try to account for minor variations by correcting the exploration approach utilized to characterize the subsurface. However, we have found that using fairly simple methods of relability analysis, we get a much better handle on the "important" parameters and what their variability really means. For example, we completed DMT testing in an area of residual silty sands and were tasked with slope design. The interpreted effective friction angles ranged from 28 degrees to nearly 40 degrees. Instead of running our slope stability analyses with a phi of 28 degrees, we varied all of the parameters that went into our analyses (stengths, unit weights, depth to water, etc). We concluded that the governing factor of slope stability was not the strength of the soils, but in fact the depth to water in the slope (imagine that). This influenced our solution to focus on controling the water in the slope and not what was the "correct" strength of the soil. Reliablity methods require about 5% more work and yield substantially more information than more traditional approaches. Zdinak