Issue |
E3S Web Conf.
Volume 89, 2019
The 2018 International Symposium of the Society of Core Analysts (SCA 2018)
|
|
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Article Number | 04005 | |
Number of page(s) | 8 | |
Section | Displacement Mechanisms / EOR | |
DOI | https://doi.org/10.1051/e3sconf/20198904005 | |
Published online | 29 March 2019 |
CO2-brine injectivity tests in high co2 content carbonate field, sarawak basin, offshore east Malaysia
1
CSIRO, Australia
2
PETRONAS Research Sdn Bhd, Malaysia
3
Curtin University
* corresponding author: Ausama.Giwelli@csiro.au
We conducted relatively long duration core-flooding tests on three representative core samples under reservoir conditions to quantify the potential impact of flow rates on fines production/permeability change. Supercritical CO2 was injected cyclically with incremental increases in flow rate (2─14 ml/min) with live brine until a total of 7 cycles were completed. To avoid unwanted fluid-rock reaction when live brine was injected into the sample, and to mimic the in-situ geochemical conditions of the reservoir, a packed column was installed on the inflow accumulator line to pre-equilibrate the fluid before entering the core sample. The change in the gas porosity and permeability of the tested plug samples due to different mechanisms (dissolution and/or precipitation) that may occur during scCO2/live brine injection was investigated. Nuclear magnetic resonance (NMR) T2 determination, X-ray CT scans and chemical analyses of the produced brine were also conducted. Results of pre- and post-test analyses (poroperm, NMR, X-ray CT) showed no clear evidence of formation damage even after long testing cycles and only minor or no dissolution (after large injected pore volumes (PVs) ~ 200). The critical flow rates (if there is one) were higher than the maximum rates applied. Chemical analyses of the core effluent showed that the rock samples for which a pre-column was installed do not experience carbonate dissolution.
© The Authors, published by EDP Sciences, 2019
This is an open access article distributed under the terms of the Creative Commons Attribution License 4.0 (http://creativecommons.org/licenses/by/4.0), which permits unrestricted use, distribution, and reproduction in any medium, provided the original work is properly cited.
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