Field-based simulation of a demonstration site for carbon dioxide sequestration in low-permeability saline aquifers in the Ordos Basin, China

Saline formations are considered to be candidates for carbon sequestration due to their great depths, large storage volumes, and widespread occurrence. However, injecting carbon dioxide into low-permeability reservoirs is challenging. An active demonstration project for carbon dioxide sequestration...

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Autores principales: Xie, J., Zhang, K., Hu, L., Pavelic, Paul, Wang, Y., Chen, M.
Formato: Journal Article
Lenguaje:Inglés
Publicado: Springer 2015
Materias:
Acceso en línea:https://hdl.handle.net/10568/77534
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author Xie, J.
Zhang, K.
Hu, L.
Pavelic, Paul
Wang, Y.
Chen, M.
author_browse Chen, M.
Hu, L.
Pavelic, Paul
Wang, Y.
Xie, J.
Zhang, K.
author_facet Xie, J.
Zhang, K.
Hu, L.
Pavelic, Paul
Wang, Y.
Chen, M.
author_sort Xie, J.
collection Repository of Agricultural Research Outputs (CGSpace)
description Saline formations are considered to be candidates for carbon sequestration due to their great depths, large storage volumes, and widespread occurrence. However, injecting carbon dioxide into low-permeability reservoirs is challenging. An active demonstration project for carbon dioxide sequestration in the Ordos Basin, China, began in 2010. The site is characterized by a deep, multi-layered saline reservoir with permeability mostly below 1.0×10-14 m2. Field observations so far suggest that only small-to-moderate pressure buildup has taken place due to injection. The Triassic Liujiagou sandstone at the top of the reservoir has surprisingly high injectivity and accepts approximately 80 % of the injected mass at the site. Based on these key observations, a three-dimensional numerical model was developed and applied, to predict the plume dynamics and pressure propagation, and in the assessment of storage safety. The model is assembled with the most recent data and the simulations are calibrated to the latest available observations. The model explains most of the observed phenomena at the site. With the current operation scheme, the CO2 plume at the uppermost reservoir would reach a lateral distance of 658 m by the end of the project in 2015, and approximately 1,000 m after 100 years since injection. The resulting pressure buildup in the reservoir was below 5 MPa, far below the threshold to cause fracturing of the sealing cap (around 33 MPa).
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spelling CGSpace775342025-06-17T08:23:21Z Field-based simulation of a demonstration site for carbon dioxide sequestration in low-permeability saline aquifers in the Ordos Basin, China Xie, J. Zhang, K. Hu, L. Pavelic, Paul Wang, Y. Chen, M. carbon dioxide carbon sequestration saline water aquifers river basins geological process reservoir storage wells temperature porosity permeability Saline formations are considered to be candidates for carbon sequestration due to their great depths, large storage volumes, and widespread occurrence. However, injecting carbon dioxide into low-permeability reservoirs is challenging. An active demonstration project for carbon dioxide sequestration in the Ordos Basin, China, began in 2010. The site is characterized by a deep, multi-layered saline reservoir with permeability mostly below 1.0×10-14 m2. Field observations so far suggest that only small-to-moderate pressure buildup has taken place due to injection. The Triassic Liujiagou sandstone at the top of the reservoir has surprisingly high injectivity and accepts approximately 80 % of the injected mass at the site. Based on these key observations, a three-dimensional numerical model was developed and applied, to predict the plume dynamics and pressure propagation, and in the assessment of storage safety. The model is assembled with the most recent data and the simulations are calibrated to the latest available observations. The model explains most of the observed phenomena at the site. With the current operation scheme, the CO2 plume at the uppermost reservoir would reach a lateral distance of 658 m by the end of the project in 2015, and approximately 1,000 m after 100 years since injection. The resulting pressure buildup in the reservoir was below 5 MPa, far below the threshold to cause fracturing of the sealing cap (around 33 MPa). 2015-11 2016-11-01T13:39:55Z 2016-11-01T13:39:55Z Journal Article https://hdl.handle.net/10568/77534 en Limited Access Springer Xie, J.; Zhang, K.; Hu, L.; Pavelic, Paul; Wang, Y.; Chen, M. 2015. Field-based simulation of a demonstration site for carbon dioxide sequestration in low-permeability saline aquifers in the Ordos Basin, China. Hydrogeology Journal, 18p. (Online first) doi: https://doi.org/10.1007/s10040-015-1267-9
spellingShingle carbon dioxide
carbon sequestration
saline water
aquifers
river basins
geological process
reservoir storage
wells
temperature
porosity
permeability
Xie, J.
Zhang, K.
Hu, L.
Pavelic, Paul
Wang, Y.
Chen, M.
Field-based simulation of a demonstration site for carbon dioxide sequestration in low-permeability saline aquifers in the Ordos Basin, China
title Field-based simulation of a demonstration site for carbon dioxide sequestration in low-permeability saline aquifers in the Ordos Basin, China
title_full Field-based simulation of a demonstration site for carbon dioxide sequestration in low-permeability saline aquifers in the Ordos Basin, China
title_fullStr Field-based simulation of a demonstration site for carbon dioxide sequestration in low-permeability saline aquifers in the Ordos Basin, China
title_full_unstemmed Field-based simulation of a demonstration site for carbon dioxide sequestration in low-permeability saline aquifers in the Ordos Basin, China
title_short Field-based simulation of a demonstration site for carbon dioxide sequestration in low-permeability saline aquifers in the Ordos Basin, China
title_sort field based simulation of a demonstration site for carbon dioxide sequestration in low permeability saline aquifers in the ordos basin china
topic carbon dioxide
carbon sequestration
saline water
aquifers
river basins
geological process
reservoir storage
wells
temperature
porosity
permeability
url https://hdl.handle.net/10568/77534
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