Figure F44. Estimated in situ hydraulic conductivity as a function of depth for Sites C0001, C0004, and C0008, determined by projecting the permeability-porosity trend for each sample to the value at the in situ void ratio and accounting for in situ fluid viscosity as a function of estimated temperature downsection, as reported in Table T3. MU = specimen data obtained at the University of Missouri; PSU = specimen data obtained at The Pennsylvania State University.
Previous | Close | Next | Top of page