Abstract

Abstract An empirical model is presented for the flow properties of rocks which is consistent with Archie’s equation1. The parameters for the important pore types for both elastics and carbonates are obtained from fits of measured formation factors to thin section point count data. These same parameters are used to model the saturation dependence and permeability.

Full Text
Published version (Free)

Talk to us

Join us for a 30 min session where you can share your feedback and ask us any queries you have

Schedule a call