VAD - good question and one I've pondered about but not for purposes of skin friction. There is no question that in granular (sandy, silty sand with very low plasticity - or coarser) you would use effective stresses. The driving or installation would have expected pore water pressure increases dissapate quite quickly. I think this is well established - Nordland method or others.
For clayey soils, traditionally the total stress concept has been used and for adhesion, the use of the Tomlinson or Focht factors would be used. For the stiffer clays, they values are quite low (nearly 0.4) - [red]
but you know this[/red]. The use of effective stress analysis would be a step forward, but the problem as is well known, too, is that it is likely near impossible to determine the pore water pressure increases due to the driving or boring. The postive pore water pressure increases would have to be subtracted from the in situ stresses to get your effective stress at a point against which you would make your estimate of the skin friction. Since this is very difficult, as in slope stability, we would use total stress analysis.
I've always wondered, though, if we shouldn't use effective stress parameters for long term end bearing in heavily overconsolidated clays (given, of course, that the bulk of the load has been transferred, in fact, to end-bearing. If the loads are high enough, the negative pore water pressures could dissapate (negatively) to the failure line and, in fact, you would have reducing factors of safety with time. But, in almost all problems, though, only 20% or so of the load at most would ever get to the base in normal circumstances so that the base is, in fact, the factor of safety.
I would love to use lots of in situ testing - but the jobs would have to be able to spring for the added costs - and there will be more costs than in the normal run of things - at least for now. Hopefully, things will change.
Again - good question -
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