Petrophysical characterisation of tight sandstone gas reservoirs using nuclear magnetic resonance: a case study of the upper Paleozoic strata in the Kangning area, eastern margin of the Ordos Basin, China

• Published in: Australian journal of earth sciences 2018-08, Vol.65 (6), p.863-875
• Main Authors: Huyan, Y. Y., Pang, X. Q., Liu, T. S., Jiang, F. J., Chen, X. Z., Ma, X. Q., Li, L. L., Shao, X. H., Zheng, D. Y.
• Format: Article
• Language: English
• Subjects: Area; Case studies; Clay; Electron microscopy; Evaluation; Fractures; gas; Grain; Lithology; Magnetic permeability; Magnetic resonance; Membrane permeability; NMR; Nuclear magnetic resonance; Paleozoic; Permeability; Petrography; Petrology; petrophysics; Pore size; Pore size distribution; Pores; Porosity; Relaxation time; Reservoirs; Resonance; Sandstone; Scanning electron microscopy; Sedimentary rocks; Size distribution; Spectra; Strata; tight sandstone
• ISSN: 0812-0099; 1440-0952
• DOI: 10.1080/08120099.2018.1472664

Residual and movable porosity are significant parameters for characterising petrophysical properties, especially in tight reservoirs. Eight tight sandstone samples from the upper Paleozoic gas-bearing strata in the Kangning area, from the eastern margin of the Ordos Basin, were analysed using nuclear magnetic resonance (NMR), scanning electron microscopy (SEM), petrography, and porosity and permeability tests. The lithology and pore types were identified and classified using petrography and SEM. The residual and movable porosity were obtained with NMR. In addition, NMR was used to visualise pore structure and pore size distribution. The results suggest that the upper Paleozoic sandstones in the study area mainly comprise feldspathic litharenite and litharenite. The sandstone porosity and permeability are low, with means of 5.9% and 0.549 mD, respectively. Four pore types exist in the tight sandstones: residual primary pores, grain dissolution pores, micropores (clay-dominated) and microfractures. The T 2 spectra under water-saturated conditions correlate with pore size and can be used to distinguish small and large pores based on the transverse relaxation time cutoff value of 10 ms, which corresponds to a pore diameter of 0.232 μm. Small pores account for 72% of the pores in the tight sandstones. The continuous bimodal T 2 spectra suggest good connectivity between small and large pores, despite the low porosity and permeability. In this study, the movable porosity of the major tight sandstone gas reservoirs is higher than the residual porosity, which confirms the effective evaluation of movable porosity to tight sandstone reservoirs, based on NMR experiments.