Fate of injected CO sub(2) in the Wilcox Group, Louisiana, Gulf Coast Basin: Chemical and isotopic tracers of microbial-brine-rock-CO sub(2) interactions

• Published in: Applied geochemistry 2014-12, Vol.51, p.155-169
• Main Authors: Shelton, Jenna L, McIntosh, Jennifer C, Warwick, Peter D, Yi, Amelia Lee Zhi
• Format: Article
• Language: English
• Subjects: Carbon dioxide; Geochemistry; Indicators; Microorganisms; Reservoirs; Sand; Sandstone; Tracers
• ISSN: 0883-2927
• DOI: 10.1016/j.apgeochem.2014.09.015

The "2800' sandstone" of the Olla oil field is an oil and gas-producing reservoir in a coal-bearing interval of the Paleocene-Eocene Wilcox Group in north-central Louisiana, USA. In the 1980s, this producing unit was flooded with CO sub(2) in an enhanced oil recovery (EOR) project, leaving similar to 30% of the injected CO sub(2) in the 2800' sandstone post-injection. This study utilizes isotopic and geochemical tracers from co-produced natural gas, oil and brine to determine the fate of the injected CO sub(2), including the possibility of enhanced microbial conversion of CO sub(2) to CH sub(4) via methanogenesis. Stable carbon isotopes of CO sub(2), CH sub(4) and DIC, together with mol% CO sub(2) show that 4 out of 17 wells sampled in the 2800' sandstone are still producing injected CO sub(2). The dominant fate of the injected CO sub(2) appears to be dissolution in formation fluids and gas-phase trapping. There is some isotopic and geochemical evidence for enhanced microbial methanogenesis in 2 samples; however, the CO sub(2) spread unevenly throughout the reservoir, and thus cannot explain the elevated indicators for methanogenesis observed across the entire field. Vertical migration out of the target 2800' sandstone reservoir is also apparent in 3 samples located stratigraphically above the target sand. Reservoirs comparable to the 2800' sandstone, located along a 90-km transect, were also sampled to investigate regional trends in gas composition, brine chemistry and microbial activity. Microbial methane, likely sourced from biodegradation of organic substrates within the formation, was found in all oil fields sampled, while indicators of methanogenesis (e.g. high alkalinity, delta super(13)C-CO sub(2) and delta super(13)C-DIC values) and oxidation of propane were greatest in the Olla Field, likely due to its more ideal environmental conditions (i.e. suitable range of pH, temperature, salinity, sulfate and iron concentrations).