Specific electrical resistivity
R_t or specific electrical conductivity
\sigma_t = \frac{1}{R_t} of formations is defined by mineralization of the rock matrix and saturating fluids which depend on water-saturated shaliness
V_{sh} , formation porosity
\phi_e and water saturation volumetric share
s_w.
Archie Model |
Indonesia Model (Poupon-Leveaux) |
Simandeux Model |
Dual-Water Model (DW) |
Waxman-Smits-Thomas Model (WST) |