New Spectrophotometric Method for Quantitative Characterization of Density-Driven Convective Instability

CO<sub>2</sub> convective dissolution has been regarded as one of the fundamental mechanisms to accelerate the mass transfer of CO<sub>2</sub> into brine. We present a new spectrophotometric method to characterize the convective instability and measure the dissolved CO<sub...

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Main Authors: Ying Teng, Pengfei Wang, Lanlan Jiang, Yu Liu, Yang Wei
Format: Article
Language:English
Published: MDPI AG 2021-02-01
Series:Polymers
Subjects:
Online Access:https://www.mdpi.com/2073-4360/13/4/661
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spelling doaj-2057c04848694038a61e7b56ce567ea12021-02-24T00:02:17ZengMDPI AGPolymers2073-43602021-02-011366166110.3390/polym13040661New Spectrophotometric Method for Quantitative Characterization of Density-Driven Convective InstabilityYing Teng0Pengfei Wang1Lanlan Jiang2Yu Liu3Yang Wei4Institute for Advanced Study, Shenzhen University, Shenzhen 518060, ChinaSchool of Earth and Space Sciences, University of Science and Technology of China, Hefei 230026, ChinaKey Laboratory of Ocean Energy Utilization and Energy Conservation of Ministry of Education, Dalian University of Technology, Dalian 116024, ChinaKey Laboratory of Ocean Energy Utilization and Energy Conservation of Ministry of Education, Dalian University of Technology, Dalian 116024, ChinaInstitute for Advanced Study, Shenzhen University, Shenzhen 518060, ChinaCO<sub>2</sub> convective dissolution has been regarded as one of the fundamental mechanisms to accelerate the mass transfer of CO<sub>2</sub> into brine. We present a new spectrophotometric method to characterize the convective instability and measure the dissolved CO<sub>2</sub> mass, which enables the real-time quantitative visualization of CO<sub>2</sub>/brine transport mechanisms. Successive images were captured to identify the finger development regimes, and the convection morphologies were analyzed by the fingers length and affected area. CO<sub>2</sub> solubility was experimentally studied, and the results are in agreement with the theoretical calculations. CO<sub>2 </sub>mass transfer flux was investigated as the Sherwood number changed. The increase in salinity and temperature has a negative effect on CO<sub>2 </sub>dissolution; here, numerical simulation and experimental phenomena are qualitatively consistent. In general, these findings confirm the feasibility of the method and improve the understanding of the physical process of CO<sub>2</sub> convective dissolution, which can help assess the CO<sub>2</sub> solubility trapping mass.https://www.mdpi.com/2073-4360/13/4/661convective dissolutiondissolved CO<sub>2</sub> mass measurementsspectrophotometric methodCO<sub>2</sub> storage in saline formations
collection DOAJ
language English
format Article
sources DOAJ
author Ying Teng
Pengfei Wang
Lanlan Jiang
Yu Liu
Yang Wei
spellingShingle Ying Teng
Pengfei Wang
Lanlan Jiang
Yu Liu
Yang Wei
New Spectrophotometric Method for Quantitative Characterization of Density-Driven Convective Instability
Polymers
convective dissolution
dissolved CO<sub>2</sub> mass measurements
spectrophotometric method
CO<sub>2</sub> storage in saline formations
author_facet Ying Teng
Pengfei Wang
Lanlan Jiang
Yu Liu
Yang Wei
author_sort Ying Teng
title New Spectrophotometric Method for Quantitative Characterization of Density-Driven Convective Instability
title_short New Spectrophotometric Method for Quantitative Characterization of Density-Driven Convective Instability
title_full New Spectrophotometric Method for Quantitative Characterization of Density-Driven Convective Instability
title_fullStr New Spectrophotometric Method for Quantitative Characterization of Density-Driven Convective Instability
title_full_unstemmed New Spectrophotometric Method for Quantitative Characterization of Density-Driven Convective Instability
title_sort new spectrophotometric method for quantitative characterization of density-driven convective instability
publisher MDPI AG
series Polymers
issn 2073-4360
publishDate 2021-02-01
description CO<sub>2</sub> convective dissolution has been regarded as one of the fundamental mechanisms to accelerate the mass transfer of CO<sub>2</sub> into brine. We present a new spectrophotometric method to characterize the convective instability and measure the dissolved CO<sub>2</sub> mass, which enables the real-time quantitative visualization of CO<sub>2</sub>/brine transport mechanisms. Successive images were captured to identify the finger development regimes, and the convection morphologies were analyzed by the fingers length and affected area. CO<sub>2</sub> solubility was experimentally studied, and the results are in agreement with the theoretical calculations. CO<sub>2 </sub>mass transfer flux was investigated as the Sherwood number changed. The increase in salinity and temperature has a negative effect on CO<sub>2 </sub>dissolution; here, numerical simulation and experimental phenomena are qualitatively consistent. In general, these findings confirm the feasibility of the method and improve the understanding of the physical process of CO<sub>2</sub> convective dissolution, which can help assess the CO<sub>2</sub> solubility trapping mass.
topic convective dissolution
dissolved CO<sub>2</sub> mass measurements
spectrophotometric method
CO<sub>2</sub> storage in saline formations
url https://www.mdpi.com/2073-4360/13/4/661
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AT pengfeiwang newspectrophotometricmethodforquantitativecharacterizationofdensitydrivenconvectiveinstability
AT lanlanjiang newspectrophotometricmethodforquantitativecharacterizationofdensitydrivenconvectiveinstability
AT yuliu newspectrophotometricmethodforquantitativecharacterizationofdensitydrivenconvectiveinstability
AT yangwei newspectrophotometricmethodforquantitativecharacterizationofdensitydrivenconvectiveinstability
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