Comparison of the impact of moisture on methane adsorption and nanoporosity for over mature shales and their kerogens

Li, Wei; Stevens, Lee A.; Uguna, Clement N.; Vane, Christopher H. ORCID: https://orcid.org/0000-0002-8150-3640; Meredith, Will; Tang, Ling; Li, Qianwen; Snape, Colin E.. 2021 Comparison of the impact of moisture on methane adsorption and nanoporosity for over mature shales and their kerogens. International Journal of Coal Geology, 237, 103705. 10.1016/j.coal.2021.103705

Before downloading, please read NORA policies.

Preview

Text
COGEL-S-20-00273.pdf - Accepted Version
Available under License Creative Commons Attribution Non-commercial No Derivatives 4.0.
Download (1MB) | Preview

Official URL: http://dx.doi.org/10.1016/j.coal.2021.103705

Abstract/Summary

Moisture in shales under reservoir conditions adversely affects gas adsorption and nanoporosity and is also likely to impact on the contribution that kerogen makes to the methane adsorption capacity. To investigate these phenomena, two over mature shales from the Wufeng-Longmaxi Formation, south of the Sichuan basin, and their kerogens isolated by demineralisation were investigated dry and at 95% relative humidity (R.H.) by high-pressure methane adsorption, and low-pressure nitrogen (N2) and carbon dioxide (CO2) sorption. The kerogen concentrates account for 68–97% and 50–64% of the methane adsorption capacities for the shales dry and at 95% R.H. respectively. However, the isolated kerogens could adsorb more methane than the organic matter in the shales because their shallower adsorption isotherms indicate large micropores and small mesopores not evident for the shales. Methane adsorption capacities of the kerogens and shales reduced by 46–72% at 95% R.H. This compares with the reductions in surface area (SA) and pore volume of 81% and 48–59%, respectively, for the kerogens and 98–99% for both SA and pore volume of the shales at 95% R.H. Water can block most micropores less than 1.3 nm reducing the micropores volume and blocking the micropore necks connecting the larger pores, and vastly reducing accessible pores for gas transport. The greater proportional losses in SA and pore volume compared to the methane adsorption capacities is probably due to ice forming at −196 °C in the low-pressure N2 analysis. Failure to take moisture into account for free and adsorbed methane overestimates the total gas in place (GIP) by 36–45% for the shales investigated.

Item Type:	Publication - Article
Digital Object Identifier (DOI):	10.1016/j.coal.2021.103705
ISSN:	01665162
Date made live:	15 Feb 2021 16:13 +0 (UTC)
URI:	https://nora.nerc.ac.uk/id/eprint/529667

Item Type:

Publication - Article

Digital Object Identifier (DOI):

10.1016/j.coal.2021.103705

ISSN:

01665162

Date made live:

15 Feb 2021 16:13 +0 (UTC)

URI:

https://nora.nerc.ac.uk/id/eprint/529667