Next Article in Journal
The Multi-Pattern Approach for Systematic Analysis of Transition Pathways
Previous Article in Journal
New Drawings of the Alhambra: Deformations of Muqarnas in the Pendentives of the Sala de la Barca
Article Menu

Export Article

Open AccessArticle
Sustainability 2019, 11(2), 317; https://doi.org/10.3390/su11020317

Experimental Investigation and Numerical Simulation of CO2–Brine–Rock Interactions during CO2 Sequestration in a Deep Saline Aquifer

1
School of Resources and Geosciences, China University of Mining and Technology, Xuzhou 221116, China
2
BMILP Science and Technology Development Co., Ltd., Beijing 100054, China
*
Author to whom correspondence should be addressed.
Received: 19 November 2018 / Revised: 10 December 2018 / Accepted: 31 December 2018 / Published: 9 January 2019
(This article belongs to the Section Sustainable Use of the Environment and Resources)
Full-Text   |   PDF [7772 KB, uploaded 14 January 2019]   |  

Abstract

CO2 mineralization is a long-term and secure solution for geological CO2 storage that primarily depends on the CO2–brine–rock interaction during CO2 sequestration in subsurface formations. In this study, lab experiments were conducted to investigate the CO2–brine–rock interaction over short timescales, and numerical simulations were performed to reveal dynamic interactions and equilibrium interactions by applying TOUGHREACT and PHREEQC, respectively. In the experiments, the main ions of HCO3 and Ca2+ were detected in the solution, and calcite dissolution and dawsonite precipitation were observed from SEM images. The simulation results showed that the CO2 dissolution and the solution pH were affected by the temperatures, pressures, types of solutions, and solution concentrations and were further influenced by mineral dissolution and precipitation. The results of the equilibrium simulation showed that the dissolved minerals were albite, anhydrite, calcite, Ca-montmorillonite, illite, K-feldspar, and chlorite, and the precipitated minerals were dolomite, kaolinite, and quartz, which led to HCO3, K+, and Na+ being the main ions in solutions. The results of the dynamic simulation showed that calcite and dolomite dissolved in the early period, while other minerals began to dissolve or precipitate after 100 years. The dissolved minerals were mainly albite, kaolinite, K-feldspar, and chlorite, and precipitated minerals were Ca-montmorillonite, illite, and quartz. Anhydrite and pyrite did not change during the simulation period, and the main ions were HCO3, Na+, Ca2+, and Mg2+ in the simulation period. This study provides an effective approach for analyzing the CO2–brine–rock interaction at different stages during CO2 storage, and the results are helpful for understanding the CO2 mineralization processes in deep saline aquifers. View Full-Text
Keywords: experiment; simulation; CO2–brine–rock interaction; CO2 sequestration; saline aquifer experiment; simulation; CO2–brine–rock interaction; CO2 sequestration; saline aquifer
Figures

Figure 1

This is an open access article distributed under the Creative Commons Attribution License which permits unrestricted use, distribution, and reproduction in any medium, provided the original work is properly cited (CC BY 4.0).
SciFeed

Share & Cite This Article

MDPI and ACS Style

Liu, B.; Zhao, F.; Xu, J.; Qi, Y. Experimental Investigation and Numerical Simulation of CO2–Brine–Rock Interactions during CO2 Sequestration in a Deep Saline Aquifer. Sustainability 2019, 11, 317.

Show more citation formats Show less citations formats

Note that from the first issue of 2016, MDPI journals use article numbers instead of page numbers. See further details here.

Related Articles

Article Metrics

Article Access Statistics

1

Comments

[Return to top]
Sustainability EISSN 2071-1050 Published by MDPI AG, Basel, Switzerland RSS E-Mail Table of Contents Alert
Back to Top