Title: Characterization of Nanoscale Pores in Tight Gas Sandstones Using Complex Techniques: A Case Study of a Linxing Tight Gas Sandstone Reservoir

Abstract

Pore structures with rich nanopores and permeability in tight gas reservoirs are poorly understood up to date. Advanced techniques are needed to be employed to accurately characterize pore structures, especially tiny pores which include micron and nanopores. In this study, various experimental techniques such as scanning electron microscopy (SEM), nuclear magnetic resonance (NMR) $T_2$ , nitrogen adsorption method, and NMR cryoporometry (NMRC) are combined to interrogate the complex pore systems of the tight gas reservoir in the Linxing formation, Ordos Basin, China. Results show that tight gas sandstones are primarily comprised of residual interparticle and clay-dominated pores. Clay and quartz are two dominate minerals while pyrite occupies a nontrivial amount as well. The permeability of tight gas sandstones is very low, exhibiting an extremely poor positive correlation with porosity. While pore types and relative pore contents are more influential factors on the permeability, accurate characterization of pore size distribution is critical for the permeability of tight gas sandstones. Therefore, complementary characterization methods are carried out, indicating that neither small pores with $\text{radii}<100\text{nm}$ (around peak 1 in NMR $T_2$ distribution) nor large pores with $\text{radii}>5\mu \text{m}$ (around peak 3 in NMR $T_2$ distribution) control the permeability by analyzing the connectivity of the pores in various size ranges, but rather pores averaging approximately $350\pm X\text{nm}$ (around peak 2 in NMR $T_2$ distribution) have sufficient connectivity to host and transmit hydrocarbons. The pore size of tight gas sandstones is dominated by the clay-rich mineral assemblage. The study shows that the NMRC technique can be a very promising method, especially when referred to as a promising “roadmap” on how to interrogate tight formations such as the tight gas sands or even shale especially for the nanopore characterization.

Authors:

Lyu, Chaohui  ^[1];

• Search DOE PAGES for author "Lyu, Chaohui"
• Search DOE PAGES for ORCID "0000-0001-9190-1071"

Zhong, Liguo ^[2]; Ning, Zhengfu ^[2]; Wang, Qing  ^[2];

• Search DOE PAGES for author "Wang, Qing"
• Search DOE PAGES for ORCID "0000-0002-5211-1322"

Cole, David R. ^[3]; Fattah, ed., Mohammed

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+ Show Author Affiliations

1. China University of Petroleum, Beijing, China, School of Earth Sciences, The Ohio State University, Columbus, Ohio, USA
2. China University of Petroleum, Beijing, China
3. School of Earth Sciences, The Ohio State University, Columbus, Ohio, USA

Publication Date:

Mon Dec 27 00:00:00 EST 2021

Research Org.:

The Ohio State University, Columbus, OH (United States)

Sponsoring Org.:

USDOE; USDOE Office of Science (SC), Basic Energy Sciences (BES). Chemical Sciences, Geosciences & Biosciences Division (CSGB); Science Foundation of China University of Petroleum

OSTI Identifier:

1837480

Alternate Identifier(s):

OSTI ID: 1980901

Grant/Contract Number:  

SC0006878; 2462021XKBH007

Resource Type:

Published Article

Journal Name:

Geofluids

Additional Journal Information:

Journal Name: Geofluids Journal Volume: 2021; Journal ID: ISSN 1468-8115

Publisher:

Hindawi Publishing Corporation

Country of Publication:

Canada

Language:

English

Subject:

15 GEOTHERMAL ENERGY