Estimation of the permeability of hydrocarbon reservoir samples using induced polarization and nuclear magnetic resonance methods
Estimation of the permeability of hydrocarbon reservoir samples using induced polarization and nuclear magnetic resonance methods
Geophysics (March 2019) 84 (2): MR73-MR84
- Arabian Sea
- Asia
- clastic rocks
- clastic sediments
- cores
- electrical methods
- experimental studies
- fluid phase
- geophysical methods
- granular materials
- Indian Ocean
- induced polarization
- Iran
- laboratory studies
- Middle East
- nuclear magnetic resonance
- oil and gas fields
- permeability
- Persian Gulf
- petroleum
- relaxation
- reservoir rocks
- sand
- sandstone
- sedimentary rocks
- sediments
- spectroscopy
We have evaluated several published models using induced polarization (IP) and nuclear magnetic resonance (NMR) measurements for the estimation of permeability of hydrocarbon reservoir samples. IP and NMR measurements were made on 30 samples (clean sands and sandstones) from a Persian Gulf hydrocarbon reservoir. We assessed the applicability of a mechanistic IP-permeability model and an empirical IP-permeability model recently proposed. The mechanistic model results in a broader range of permeability estimates than those measured for sand samples, whereas the empirical model tends to overestimate the permeability of the samples that we tested. We also evaluated an NMR permeability prediction model that is based on porosity phi and the mean of the log transverse relaxation time (T (sub 2ml) ). This model provides reasonable permeability estimations for the clean sandstones that we tested but relies on calibrated parameters. We also examined an IP-NMR permeability model, which is based on the peak of the transverse relaxation time distribution, T (sub 2p) and the formation factor. This model consistently underestimates the permeability of the samples tested. We also evaluated a new model. This model estimates the permeability using the arithmetic mean of log transverse NMR relaxation time (T (sub 2ml) ) and diffusion coefficient of the pore fluid. Using this model, we improved estimates of permeability for sandstones and sand samples. This permeability model may offer a practical solution for geophysically derived estimates of permeability in the field, although testing on a larger database of clean granular materials is needed.