CO                         2                          sequestration by mineral trapping in natural analogues in the Yinggehai Basin, South China Sea

Rui Liu; Niklas Heinemann; Jianzhang Liu; Weilin Zhu; Mark Wilkinson; Yuhong Xie; Zhenfeng Wang; Tao Wen; Fang Hao; R. Stuart Haszeldine

doi:10.1016/j.marpetgeo.2019.03.018

CO ₂ sequestration by mineral trapping in natural analogues in the Yinggehai Basin, South China Sea

Rui Liu, Niklas Heinemann, Jianzhang Liu, Weilin Zhu, Mark Wilkinson, Yuhong Xie, Zhenfeng Wang, Tao Wen, Fang Hao, R. Stuart Haszeldine

Research output: Contribution to journal › Article › peer-review

5 Scopus citations

Abstract

Mineral trapping of CO ₂ by precipitation of carbonate minerals is seen as the most permanent and secure mechanism of CO ₂ storage. We have investigated mineral trapping in CO ₂ -rich siliciclastic reservoirs of the Upper Miocene age in the Yinggehai Basin (South China Sea) and used nearby CO ₂ -poor reservoirs of similar age as benchmarks for the analysis. Within the reservoir, the CO ₂ has triggered the reaction from calcite plus chlorite to ankerite plus kaolinite, which traps 5 mol of CO ₂ per mole of chlorite. Geochemical modelling shows that the total amount of permanently trapped CO ₂ is approximately one half of the CO ₂ in the newly formed ankerite. Caprock mineralogy shows that CO ₂ leakage has occurred and CO ₂ has migrated into the shale-rich caprock, but without loss of caprock integrity.

Original language	English (US)
Pages (from-to)	190-199
Number of pages	10
Journal	Marine and Petroleum Geology
Volume	104
DOIs	https://doi.org/10.1016/j.marpetgeo.2019.03.018
State	Published - Jun 2019
Externally published	Yes

Keywords

CO geological storage
Mineral trapping
Reservoir overpressure
Yinggehai basin

ASJC Scopus subject areas

Oceanography
Geophysics
Geology
Economic Geology
Stratigraphy

Access to Document

10.1016/j.marpetgeo.2019.03.018

Cite this

Liu, R., Heinemann, N., Liu, J., Zhu, W., Wilkinson, M., Xie, Y., Wang, Z., Wen, T., Hao, F., & Haszeldine, R. S. (2019). CO ₂ sequestration by mineral trapping in natural analogues in the Yinggehai Basin, South China Sea Marine and Petroleum Geology, 104, 190-199. https://doi.org/10.1016/j.marpetgeo.2019.03.018

CO ₂ sequestration by mineral trapping in natural analogues in the Yinggehai Basin, South China Sea . / Liu, Rui; Heinemann, Niklas; Liu, Jianzhang et al.
In: Marine and Petroleum Geology, Vol. 104, 06.2019, p. 190-199.

Research output: Contribution to journal › Article › peer-review

Liu, R, Heinemann, N, Liu, J, Zhu, W, Wilkinson, M, Xie, Y, Wang, Z, Wen, T, Hao, F & Haszeldine, RS 2019, ' CO ₂ sequestration by mineral trapping in natural analogues in the Yinggehai Basin, South China Sea ', Marine and Petroleum Geology, vol. 104, pp. 190-199. https://doi.org/10.1016/j.marpetgeo.2019.03.018

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title = " CO 2 sequestration by mineral trapping in natural analogues in the Yinggehai Basin, South China Sea ",

abstract = " Mineral trapping of CO 2 by precipitation of carbonate minerals is seen as the most permanent and secure mechanism of CO 2 storage. We have investigated mineral trapping in CO 2 -rich siliciclastic reservoirs of the Upper Miocene age in the Yinggehai Basin (South China Sea) and used nearby CO 2 -poor reservoirs of similar age as benchmarks for the analysis. Within the reservoir, the CO 2 has triggered the reaction from calcite plus chlorite to ankerite plus kaolinite, which traps 5 mol of CO 2 per mole of chlorite. Geochemical modelling shows that the total amount of permanently trapped CO 2 is approximately one half of the CO 2 in the newly formed ankerite. Caprock mineralogy shows that CO 2 leakage has occurred and CO 2 has migrated into the shale-rich caprock, but without loss of caprock integrity. ",

keywords = "CO geological storage, Mineral trapping, Reservoir overpressure, Yinggehai basin",

author = "Rui Liu and Niklas Heinemann and Jianzhang Liu and Weilin Zhu and Mark Wilkinson and Yuhong Xie and Zhenfeng Wang and Tao Wen and Fang Hao and Haszeldine, {R. Stuart}",

note = "Funding Information: This research was supported by the 111 project (No. B14031), the National Natural Science Foundation of China (No. 41672141 and No. 41702157) and the Young scholars development fund of SWPU (No. 201699010085). NH has received funding from the European Union's H2020 Accelerating CCS technologies and UKCCSRC (EP/P026214/1). SH is funded by EPSRC and NERC. We appreciate the collaboration and enthusiastic support of Hongjun Yang, Jianxiang Pei, Antao Xiao, Lifeng Wang, Huolan Zhang, and Nengping Ai at the Zhanjiang Branch of CNOOC Ltd. Publisher Copyright: {\textcopyright} 2019 Elsevier Ltd",

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AU - Xie, Yuhong

AU - Wang, Zhenfeng

AU - Wen, Tao

AU - Hao, Fang

AU - Haszeldine, R. Stuart

N1 - Funding Information: This research was supported by the 111 project (No. B14031), the National Natural Science Foundation of China (No. 41672141 and No. 41702157) and the Young scholars development fund of SWPU (No. 201699010085). NH has received funding from the European Union's H2020 Accelerating CCS technologies and UKCCSRC (EP/P026214/1). SH is funded by EPSRC and NERC. We appreciate the collaboration and enthusiastic support of Hongjun Yang, Jianxiang Pei, Antao Xiao, Lifeng Wang, Huolan Zhang, and Nengping Ai at the Zhanjiang Branch of CNOOC Ltd. Publisher Copyright: © 2019 Elsevier Ltd

PY - 2019/6

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N2 - Mineral trapping of CO 2 by precipitation of carbonate minerals is seen as the most permanent and secure mechanism of CO 2 storage. We have investigated mineral trapping in CO 2 -rich siliciclastic reservoirs of the Upper Miocene age in the Yinggehai Basin (South China Sea) and used nearby CO 2 -poor reservoirs of similar age as benchmarks for the analysis. Within the reservoir, the CO 2 has triggered the reaction from calcite plus chlorite to ankerite plus kaolinite, which traps 5 mol of CO 2 per mole of chlorite. Geochemical modelling shows that the total amount of permanently trapped CO 2 is approximately one half of the CO 2 in the newly formed ankerite. Caprock mineralogy shows that CO 2 leakage has occurred and CO 2 has migrated into the shale-rich caprock, but without loss of caprock integrity.

AB - Mineral trapping of CO 2 by precipitation of carbonate minerals is seen as the most permanent and secure mechanism of CO 2 storage. We have investigated mineral trapping in CO 2 -rich siliciclastic reservoirs of the Upper Miocene age in the Yinggehai Basin (South China Sea) and used nearby CO 2 -poor reservoirs of similar age as benchmarks for the analysis. Within the reservoir, the CO 2 has triggered the reaction from calcite plus chlorite to ankerite plus kaolinite, which traps 5 mol of CO 2 per mole of chlorite. Geochemical modelling shows that the total amount of permanently trapped CO 2 is approximately one half of the CO 2 in the newly formed ankerite. Caprock mineralogy shows that CO 2 leakage has occurred and CO 2 has migrated into the shale-rich caprock, but without loss of caprock integrity.

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