A laboratory pyrolysis study to investigate the effect of water pressure on hydrocarbon generation and maturation of coals in geological basins

Uguna, Clement N.; Carr, Andrew D.; Snape, Colin E.; Meredith, Will; Castro-Díaz, Miguel. 2012 A laboratory pyrolysis study to investigate the effect of water pressure on hydrocarbon generation and maturation of coals in geological basins. Organic Geochemistry, 52. 103-113. https://doi.org/10.1016/j.orggeochem.2012.09.003

Before downloading, please read NORA policies.

Preview

Text (Abstract only)
WaterPress.pdf
Download (21kB) | Preview

Official URL: http://dx.doi.org/10.1016/j.orggeochem.2012.09.003

Abstract/Summary

This study investigates the effect of water pressure on hydrocarbon generation and maturation of coals. Using a 25 ml Hastalloy pressure vessel, two high-volatile coals (Longannet, UK 0.75% Ro, and perhydrous Svalbard (Spitsbergen), Norway 0.68% Ro) were pyrolysed under non-hydrous, hydrous at 175 bar pressure, and high water pressure hydrous (500 bar and 900 bar) conditions at 350 °C for 24 h. The bitumen yield obtained during pyrolysis, together with the Rock–Eval S2, hydrogen index (HI) and vitrinite reflectance (VR) results from the pyrolysed coal residues indicated that water under relatively low pressure (175 bar) hydrous conditions promoted hydrocarbon generation and coal maturation in relation to non-hydrous conditions, consistent with previous work. However, under high water pressure (500 and 900 bar) conditions, a combination of the hydrocarbon gas (C1–C4) and bitumen yields, Rock–Eval S2, HI, VR and solid state 13C NMR results demonstrated that the changes in reaction pathways occurring with increasing pressure resulted in both hydrocarbon generation and maturation being retarded. The observed effect of pressure implies that for Type III source rocks, hydrocarbon generation will be retarded in high pressure geological basins, with gas yields being proportionally reduced more than bitumen yields. Source rock maturation (or coalification) is also retarded, with the decreases in vitrinite reflectance and carbon aromaticity being relatively small but significant in terms of explaining retardation in geological basins.

Item Type:	Publication - Article
Digital Object Identifier (DOI):	https://doi.org/10.1016/j.orggeochem.2012.09.003
Programmes:	BGS Programmes 2010 > BGS Corporate
ISSN:	01466380
Date made live:	19 Mar 2013 11:57 +0 (UTC)
URI:	https://nora.nerc.ac.uk/id/eprint/500538

Item Type:

Publication - Article

Digital Object Identifier (DOI):

https://doi.org/10.1016/j.orggeochem.2012.09.003

Programmes:

BGS Programmes 2010 > BGS Corporate

ISSN:

01466380

Date made live:

19 Mar 2013 11:57 +0 (UTC)

URI:

https://nora.nerc.ac.uk/id/eprint/500538