regarding "relative humidity," the correct term is degree of saturation; the definition of relative humidity is the ratio of the vapor pressure of moisture in the air at a given temperature to the vapor pressure of saturated air at that temperature; i.e., the vapor pressure of the air at some temperature, x, where x is >= the dew point of the ambient condition relative to the vapor pressure at the dew point. These concepts have no significance in normal soil mechanics; they would only be relevant in mechanics of unsaturated soils, but perhaps that is why you need them. If so, I have learned something new today, and that is a good thing!
D. Bruce Nothdurft, MSCE, PE, PG, M.ASCE, etc, etc,...
Principal Engineer/Geologist
Atlantic Geoscience & Engineering
Charlotte, NC