Jordan2
Geotechnical
- Jun 21, 2006
- 12
Dear Friends,
I have some doubt about the definition of the effective stress proposed by Terzaghi and reported in the book Underground Excavation in Rock (Hoek & Brown, 1980):
s'=s-(1-nb)u
where s'=effective stress; s=total stress; u=pore pressure and nb=boundary porosity.
Evidently the formula should adequate the concept of effective stress to low porosity material, but (maybe I am wrong) it seems to me that there is some problem. In fact, if I consider a very porous material, nb should be high and then the equation tends to s'=s, that is the opposite I expected. Do you have perhaps the original reference? Am I wrong to interpret the "boundary" porosity as the effective porosity (i.e. referred to interconnetted pores)?
Thank you in advance for your help/suggestion?
I have some doubt about the definition of the effective stress proposed by Terzaghi and reported in the book Underground Excavation in Rock (Hoek & Brown, 1980):
s'=s-(1-nb)u
where s'=effective stress; s=total stress; u=pore pressure and nb=boundary porosity.
Evidently the formula should adequate the concept of effective stress to low porosity material, but (maybe I am wrong) it seems to me that there is some problem. In fact, if I consider a very porous material, nb should be high and then the equation tends to s'=s, that is the opposite I expected. Do you have perhaps the original reference? Am I wrong to interpret the "boundary" porosity as the effective porosity (i.e. referred to interconnetted pores)?
Thank you in advance for your help/suggestion?